• MESO: Nws Weather Prediction Center College Park Md

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 15 16:04:25 2024
    AWUS01 KWNH 151604
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-152200-

    Mesoscale Precipitation Discussion 1014
    NWS Weather Prediction Center College Park MD
    1203 PM EDT Sun Sep 15 2024

    Areas affected...north-central MS to southern MS/AL and western FL
    Panhandle

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 151602Z - 152200Z

    SUMMARY...Areas of training are expected to develop from the
    central Gulf Coast into southwestern AL and central/eastern MS
    through 22Z. Rainfall rates of 1 to 3 in/hr are likely, which may
    result in localized areas of flash flooding.

    DISCUSSION...At 1530Z, visible satellite imagery showed thick
    cloud cover over much of central to northern MS while skies over
    southern MS into the Mobile Bay region had only scattered clouds.
    A low located in the 925-850 mb layer was identified over
    south-central MS via area VAD wind plots with very slow movement
    over the past few hours. Low level ESE winds of 20-30 kt were
    present to the east of the low over eastern portions of MS into AL
    while wind speeds dropped off to the west along the AR/MS border
    down to Mobile Bay. A combination of speed and directional low
    level convergence was supporting a broken axis of mostly warm
    topped showers from northeastern MS down to the offshore waters of
    MS/AL with increasing development noted across the
    southern/clearer-sky regions. The environment was very moist with
    area 12Z soundings indicating precipitable water values of 1.6 to
    2.0 inches and wet bulb zero heights between 13-14 kft. SPC
    mesoanalysis data from 15Z showed that MLCAPE of 500 to 1500 J/kg
    was focused from the central MS/AL border, southward to the Gulf
    Coast from central LA to the FL Panhandle, with higher values
    toward the south.

    Daytime heating is expected to expand the coverage of 500 to 1500
    J/kg MLCAPE across the region but likely keeping the better
    instability focused over southern areas where greater solar
    insolation is expected. Scattered showers and thunderstorms will
    likely increase through the afternoon with cell movement following
    the general flow around the MS low. However, slow movement and
    training will be possible with cells that form along the low level
    convergence axis from north-central MS to the southern MS/AL
    border, where lower topped cells will have a motion roughly
    parallel to the axis of convergence.

    Stronger low level convergence is expected from central to
    northern MS where greater coverage of rain is expected but lower
    instability may cap rain rates below 2 in/hr. Farther south,
    rainfall rates may get as high as 3 in/hr due to the greater
    instability combined with potential for slow movement but coverage
    will likely be more isolated compared to up north. Portions of
    this region have been anomalously wet over the past several days,
    but other portions have missed out on the bulk of rainfall and are
    nearer to average. At least localized flash flooding will be
    possible through the afternoon.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Rr85u_WY5NEi7Z2xYqOaH6FWEeE5pJGhjw9likVR8uDabJgGvCST6jJxSXG-xK9lVtm= U_KFBTniTQj21c3j3tg7yVE$ for graphic product...

    ATTN...WFO...BMX...JAN...LIX...MEG...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34089005 34078912 33328834 31958748 30698644=20
    30098675 29918785 29998896 30388928 31508959=20
    33139025=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 15 18:01:56 2024
    AWUS01 KWNH 151801
    FFGMPD
    TXZ000-152300-

    Mesoscale Precipitation Discussion 1015
    NWS Weather Prediction Center College Park MD
    201 PM EDT Sun Sep 15 2024

    Areas affected...South Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 151800Z - 152300Z

    SUMMARY...Slow moving showers and thunderstorms will pose a
    localized threat of flash flooding for southern TX through the
    late evening. Rainfall rates of 1-2 in/hr, but with localized
    maxima near 3 in/hr, will be possible along with totals of 3 to 5+
    inches.

    DISCUSSION...Local radar imagery out of southern TX at 1730Z
    showed showers and thunderstorms extending from near Laredo to the
    US 281 corridor near Encino along with isolated development near
    the Laguna Madre. Cells appear to be forming on an elevated
    convergence axis tied to the 850-700 mb remnants of an old frontal
    boundary that extended westward through the Gulf of Mexico into
    southern TX, as seen on Layered PW Imagery from CIRA and in recent
    visible satellite imagery. 850-300 mb mean layer winds of only
    5-10 kt from the S or SW were supporting the slow cell movement.
    The environment contained PWATs of 2.0 to 2.5 inches (highest to
    south) along with 1000-2000 J/kg MLCAPE. Moisture contributions in
    the middle/upper levels were tied to former T.S. Ileana in the Sea
    of Cortez and low level southeasterly winds funneling moisture
    into the region from northeastern Mexico and the adjacent Gulf
    waters.

    An elongated 700 mb low on the border of Coahuila and Nuevo Leon
    is expected to remain roughly in the same place over the next 6
    hours per recent runs of the RAP which will keep low level
    convergence focused across southern TX. In addition, a forecast
    for increasing easterly 850 mb winds by 00Z, reaching 10-15 kt
    between CRP and BRO, may support some slow moving cells near the
    coast depending on cell evolution with time given slow steering
    flow. Some southward propagation into the instability is also
    expected in the short term with instability likely diminishing
    from west to east over time. Slow cells movement will be capable
    of rainfall rates between 1-3 in/hr and localized areas of flash
    flooding that may end up being more of an urban flood threat due
    to relatively dry antecedent ground conditions, outside of
    isolated portions of far south TX.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_aIpGJAgzhzbkK9h-QgRQm3jhyRkctTUUBMEKlFvzA4CAIBMxd48qyfi-RULPSeWrilu= _li9Yqp40z9jS86evccmdhk$ for graphic product...

    ATTN...WFO...BRO...CRP...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 27879923 27419751 26959713 25959684 25649723=20
    25809821 26199917 26999959 27479973 27819956=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 15 19:39:56 2024
    AWUS01 KWNH 151939
    FFGMPD
    NMZ000-AZZ000-160137-

    Mesoscale Precipitation Discussion 1016
    NWS Weather Prediction Center College Park MD
    339 PM EDT Sun Sep 15 2024

    Areas affected...southeastern Arizona through central New Mexico

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 151937Z - 160137Z

    Summary...Thunderstorms continue to produce 1-2 inch rainfall
    amounts across portions of the Upper Mississippi Valley. Isolated
    flash flood potential continues with this activity.

    Discussion...Recent radar mosaic imagery depicts a mature,
    forward-propagating convective complex extending from near Eau
    Claire to Mason City. A few cell mergers have been noted with the
    complex over the past couple hours, and local rain rates continue
    to approach 2 inches/hr in spots despite appreciable forward
    movement. The immediate downstream airmass remains sufficiently
    moist/unstable for strong convection (2000+ J/kg MLCAPE and 1.5
    inch PW values), and current trends suggest that spots of 1+
    inch/hr rain rates should continue to materialize for at least
    another 2-4 hours or so as the complex migrates eastward.

    The greatest concern for isolated flash flood potential exists as
    storms traverse central and eastern Wisconsin (generally from Eau
    Claire eastward to Green Bay). Although some uncertainty exists
    with respect to eastward extent of the complex, these areas
    currently have the lowest FFG thresholds (around 1-1.5 inch/hr)
    and the greatest chance for those thresholds being exceeded on an
    isolated basis. Destabilization is slow to occur across
    northeastern Wisconsin, and it appears that the northern portions
    of the complex may undergo weakening (and lessening flash flood
    potential) especially north of Wisconsin State Highway 29. Higher
    FFGs (~2-3 inch/hr) across southwestern Wisconsin suggests an even
    more isolated/spotty flash flood threat in these areas through 06Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6kQwItSY1pgkFwuhZxGDSWiXbPnen-E1y6j_rcEUgNkiCoXki9TOattczPOnYWLBinJJ= kM8c9UEvTU3UwfhF9AfqVL4$ for graphic product...

    ATTN...WFO...ABQ...EPZ...FGZ...PSR...TWC...

    ATTN...RFC...ABRFC...CBRFC...WGRFC...NWC...

    LAT...LON 36620685 36310517 35330474 34370485 33480572=20
    32930692 31950803 31360853 31441153 33371128=20
    36100945=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 15 21:40:30 2024
    AWUS01 KWNH 152140
    FFGMPD
    NMZ000-AZZ000-160137-

    Mesoscale Precipitation Discussion 1016
    NWS Weather Prediction Center College Park MD
    539 PM EDT Sun Sep 15 2024

    Areas affected...southeastern Arizona through central New Mexico

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 151937Z - 160137Z

    Summary...Isolated flash flood potential exists as scattered
    thunderstorm activity drifts northward across the discussion area
    this afternoon.

    Discussion...Abundant insolation has enabled a gradual deepening
    of scattered convection across much of eastern Arizona and central
    New Mexico. The storms are developing in areas of 500-1500 J/kg
    of SBCAPE and 0.8-1.4 inch PW values - highest across southern
    Arizona. While these PWs are a bit on the low side for widespread
    flash flood potential, weak flow aloft was enabling slow storm
    motions and potential for a quick 0.5-1 inch of rainfall on a
    localized basis. Furthermore, localized terrain enhancement was
    enabling an estimated 0.5 inch/hr rain rates near Ruidoso and
    additional areas of New Mexico where burn scars have potential to
    create excessive runoff conditions. On the whole, these rain
    rates were occurring on an isolated/spotty basis, suggestive of
    low coverage of flash flood potential in the near term.

    Models (particularly the HREF) suggest continued thunderstorm
    potential through the afternoon, with the greatest coverage and
    persistence over southeastern Arizona through 00-01Z this evening.
    Isolated flash flood potential is expected through that timeframe.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7h3976Sdvuu0fgDbvBoyCZOfhlJBmz0LRSlqUktrDTBHiIYsrFrniUkJQZ6qM6k1TsYf= PDrN7dWASJWPGw8nLKK0UTw$ for graphic product...

    ATTN...WFO...ABQ...EPZ...FGZ...PSR...TWC...

    ATTN...RFC...ABRFC...CBRFC...WGRFC...NWC...

    LAT...LON 36620685 36310517 35330474 34370485 33480572=20
    32930692 31950803 31360853 31441153 33371128=20
    36100945=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 15 23:14:58 2024
    AWUS01 KWNH 152314
    FFGMPD
    TXZ000-160213-

    Mesoscale Precipitation Discussion 1017
    NWS Weather Prediction Center College Park MD
    714 PM EDT Sun Sep 15 2024

    Areas affected...Deep South Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 152313Z - 160213Z

    Summary...Lingering, isolated flash flood potential should remain
    across Deep South Texas for at least another couple hours or so.

    Discussion...A mature convective complex near
    Brownsville/Harlingen was producing areas of 2-3 inch/hr rain
    rates (estimated per MRMS) over the past hour. Immediately
    upstream/northwest of this complex, a lull in convection has been
    noted likely due to widespread overturning and temporary low-level stabilization. Surface observations indicate very moist low-level
    conditions in the wake of convection across the discussion area
    (with upper 70s dewpoints), and 1000+ J/kg SBCAPE values remain in
    place across the area. Additional convection just south of the
    Rio Grande seems persistent and slow-moving. These cells could
    drift back northward into the discussion area. Meanwhile
    mid-level vorticity over the region could result in additional
    updrafts over the discussion area for the next few hours. Any
    additional rainfall would occur over locations of estimated 3-5
    inch rainfall totals since 19Z. Wet ground conditions/urbanized
    areas could be sensitive to additional rainfall, and renewed flash
    flooding in the wake of ongoing activity cannot be completely
    ruled out.

    This conditional flash flood risk could persist for another 2-3
    hours at least. Models continue to depict additional heavy
    rainfall potential through the overnight hours (beyond 02Z) that
    may 1) redevelop into populated areas of south Texas and 2)
    require a new MPD issuance.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4WmQSHMt_rVePhThNLcPPxk354Kw4btmBTEWpd9quLmeMvkZUJ32hcmH7HRRsEzcbnVK= JnZP-nNVc33feYVq7C_RF5Q$ for graphic product...

    ATTN...WFO...BRO...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 27019930 26949846 26589733 26089691 25839712=20
    25879786 26209898 26599938=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 16 03:53:31 2024
    AWUS01 KWNH 160353
    FFGMPD
    CAZ000-160952-

    Mesoscale Precipitation Discussion 1018
    NWS Weather Prediction Center College Park MD
    1152 PM EDT Sun Sep 15 2024

    Areas affected...Portions of the Northern Sacramento Valley and
    Foothills of the Northern Sierra Nevada

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 160352Z - 160952Z

    SUMMARY...Slow-moving showers and thunderstorms with heavy
    rainfall rates may cause some instances of flash flooding over the
    next several hours, and especially with respect to the Park Fire
    burn area.

    DISCUSSION...The latest GOES-W WV satellite imagery shows a
    deepening mid-level trough and associated closed low pivoting south-southeastward across coastal areas of northern and central
    CA. This energy has facilitated the development of an area of low
    pressure in the northern Sacramento Valley which is oriented along
    a frontal zone. A corridor of locally enhanced moisture
    convergence and modest instability has pooled up across the region
    and into the foothills of the northern Sierra Nevada.

    This has led to the development and localized expansion of showers
    and thunderstorms across Tehama County and this activity is
    gradually settling down to the southeast as the stronger corridor
    of height falls and deeper layer forcing pivots over the region.
    MUCAPE values are only on the order of 250 to 500 J/kg, but the
    latest MRMS data shows rainfall rates of 1.0 to 1.5 inches/hour
    with the stronger storms.

    Given the amplification of the mid-level closed low circulation
    over northern CA that is expected overnight, an increase in deeper
    layer ascent is expected, and this coupled with steepening
    mid-level lapse rates and localized orographics should tend to
    favor convection persisting in the near-term across portions of
    the northern Sacramento Valley while also edging into the
    foothills of the northern Sierra Nevada.

    The 00Z HREF guidance suggests some spotty 2 to 3+ inch rainfall
    totals may be possible over the next several hours, and this will
    be supported by the aforementioned rainfall rates and slow
    cell-motions. These rains may result in some localized urban
    runoff/flooding concerns along the I-5 corridor. However, if these
    rains can make it a bit farther east into at least the eastern
    portions of Tehama County and the northern portions of Butte
    County, there will be concerns for impacts involving the large
    Park Fire burn area. Satellite and radar trends will need to be
    very closely monitored overnight for the potential of heavy
    rainfall impacting this burn scar, and especially since rainfall
    rates are already quite heavy just to the west near I-5 involving
    areas near and adjacent to Red Bluff vicinity. Instances of flash
    flooding and debris flow activity cannot be ruled out.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6O4J5mJIb3ZTjAJVNDWwawsePP80IPFsLGfGXcZk-K2X1yTSEf_Nghy4dIoI70sOMgfY= oOBrNbbyMXe3-gEKcZBH_G4$ for graphic product...

    ATTN...WFO...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 40972168 40742138 40172131 39642162 39472220=20
    39862261 40672238=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 16 09:02:07 2024
    AWUS01 KWNH 160901
    FFGMPD
    NCZ000-SCZ000-161500-

    Mesoscale Precipitation Discussion 1019
    NWS Weather Prediction Center College Park MD
    500 AM EDT Mon Sep 16 2024

    Areas affected...Southeast NC...Northeast SC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 160900Z - 161500Z

    SUMMARY...Heavy rainfall associated with Potential Tropical
    Cyclone Eight will be advancing inland this morning across
    southeast NC and northeast SC. A gradual increase in the threat
    for flash flooding can be expected as rainfall rates increase.

    DISCUSSION...The latest GOES-E Proxy Visible satellite imagery
    along with radar and aircraft data shows the low center of
    Potential Tropical Cyclone Eight centered approximately 95 miles
    east-southeast of Charleston, SC at 09Z (5AM EDT). The storm
    continues to advance slowly off to the northwest, and this will be
    allowing for heavy rainfall focused around the northern quadrant
    of the storm to begin cyclonically wrapping inland across the
    coastal plain of southeast NC and northeast SC this morning.

    The system still has a fair amount of baroclinicity associated
    with it for the time being given the proximity of multiple frontal
    features, but radar imagery shows pockets of very strong
    convection north of the low center with extremely heavy rainfall
    rates. This is also where there is much greater instability and
    the latest RAP analysis confirms MLCAPE values of as much as 1500
    J/kg near and to the northeast of the center where some of the
    colder convective tops are noted.

    Much more stable air is still noted along the immediate coastal
    plain of the Carolinas, and this will tend to keep rainfall rates
    a bit limited in the short-term across these areas as rains
    offshore gradually push inland. However, in time as stronger
    onshore flow arrives and the low center approaches by later this
    morning, there should be an influx of greater instability and
    stronger moisture convergence that will be conducive increasing
    rainfall rates.

    The 00Z HREF guidance supports rainfall rates in the 12Z to 15Z
    time frame reaching 1 to 2 inches/hour across especially the
    coastal areas of southeast NC around the Wilmington, NC vicinity.
    Some of these heavier rainfall rates may also spread into
    northeast SC near and to the north of Myrtle Beach.

    Expect rainfall amounts by 15Z (11AM EDT) to reach as high as 2 to
    4 inches with isolated amounts potentially up to around 5 inches.
    These rains will gradually increase the threat for flash flooding
    by later this morning.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!40FZpfYkV7YPK3F_dlYet3_nSNIlmMJYCKZtZyvQCwopHGqy1Hg4OmM_0YQO7gYQML3n= txgXXoipYj_WAvV-I0Cmjek$ for graphic product...

    ATTN...WFO...ILM...MHX...RAH...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 34667791 34667738 34437729 34177765 33837785=20
    33777842 33407907 33557953 33917961 34177945=20
    34357913 34487867=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 16 09:12:36 2024
    AWUS01 KWNH 160911
    FFGMPD
    NDZ000-161510-

    Mesoscale Precipitation Discussion 1020
    NWS Weather Prediction Center College Park MD
    510 AM EDT Mon Sep 16 2024

    Areas affected...Central ND

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 160910Z - 161510Z

    SUMMARY...Locally training showers and thunderstorms going through
    early to mid-morning may result in some isolated areas of flash
    flooding.

    DISCUSSION...GOES-E IR satellite imagery shows an axis of very
    cold topped convection impacting portions of central ND as strong
    thunderstorms developing within a well-defined warm air advection
    pattern lift gradually off to the northeast. The convection is
    aligned in close proximity to a frontal zone and a rather strong
    instability gradient with MUCAPE values of as much as 2000 J/kg
    noted across areas of central and southern ND.

    MRMS data has been showing some rainfall rates with the activity
    reach as high as 1.5 to 2.5 inches/hour and this is being aided by
    rather strong moisture transport associated with the nose of a 30+
    kt southerly low-level jet.

    Going through the early to mid-morning hours, there may be some
    additional concentration and alignment of convection that will
    promote some cell-training in close proximity to the front.
    Additionally, there is some weak vort energy/MCV activity arriving
    from weakening convection over western SD, and this energy may
    interact with the front and the low-level jet to further promote
    convective sustenance across areas of central ND this morning.

    Additional rainfall totals of 2 to 4 inches will be possible with
    isolated heavier amounts of 5 inches where any cell-training
    occurs this morning. The antecedent conditions across the region
    are quite dry, so any flash flooding concerns should be isolated
    in nature and mainly focused within the more urbanized locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ExnbWMMSCx0NH9GksyPfSN-u18puv6VRSkxBJtm2vmY6NIoSR47K8CvdogMU2pZ11DH= W89bBpfck4hPN8GjpnHuhkY$ for graphic product...

    ATTN...WFO...BIS...FGF...

    ATTN...RFC...MBRFC...NCRFC...NWC...

    LAT...LON 48859932 48609848 48069883 47389991 46650180=20
    47010252 47770206 48490084=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 16 12:14:37 2024
    AWUS01 KWNH 161214
    FFGMPD
    KSZ000-NEZ000-SDZ000-161700-

    Mesoscale Precipitation Discussion 1021
    NWS Weather Prediction Center College Park MD
    814 AM EDT Mon Sep 16 2024

    Areas affected...Southeast SD...Central NEB...North-central KS...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 161215Z - 161700Z

    SUMMARY...Persistent, stationary elevated thunderstorms continue
    to produce solid rain-rates that localized totals are nearing
    higher localized FFG values; suggesting flash flooding may become
    possible over the next few hours.

    DISCUSSION...GOES-E WV depicts stronger northern stream shortwave
    and resultant MCS across the Northern Plains; a more subtle wave
    is lifting northeastward along its southern flank across the
    Nebraska Panhandle. This is enhancing low level flow across the
    central Plains with backed 850mb veering through 700mb at 45kts
    reducing to 20kts while also becoming confluent along and just
    east of 99W. CIRA LPW and RAP TPW, show greatest ascent pattern
    is just along the western gradient of the moisture axis with
    1.25-1.5" values noted along it from SE SD into the northern KS
    where deep layer (mainly directional) convergence is maximized.=20
    MUCAPE appears to be sufficient at 500-1000 J/kg with axis of
    greatest values along and west of the moisture axis, ideally
    supporting the stronger convective ascent. This appears to be
    exhausting as the updrafts/overshooting tops are becoming a bit
    less in coverage and noting a generally slow warming with the
    cirrus canopies associated with the two linear clusters from SE
    SDak into N NEB and again along the NEB/KS line to Lincoln county,
    KS.

    The concern has been/continues to be the relative zero or very
    slight westward propagation of the lines allowing for localized
    enhanced rainfall totals. With deep layer steering more north;
    the inflow from the 850-700mb isentropic ascent/instability axis
    has been nearly equal/opposite to allow for the 1.5-2"/hr rates to
    overcome the regionally above normal FFG values (given the
    prolonged dry period across the region) which are about 3+"/3hrs.
    As such, localized observed totals (per backyard wx stations) are
    reaching 2-3" in spots, and MRMS Flash response are reaching
    300-400 cfs/smi suggesting enhanced flows may be reaching near
    levels typical of localized flash flooding concerns. Given
    overall trends are slowly downward, an additional hour or two will
    become more likely to exceed even these higher FFGs resulting in
    localized possible flash flooding conditions.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5Ue8Zkh7q1Gd5w6hynnEO-ARZ6rtd0TqMUtsNvmtrlJtHdC7ohbaT-gN4IMkVgjdBRNv= mLHGyR0_q2u4hX87wFugLuI$ for graphic product...

    ATTN...WFO...FSD...GID...ICT...LBF...OAX...TOP...

    ATTN...RFC...ABRFC...MBRFC...NWC...

    LAT...LON 44269842 44089772 42799758 40029761 38909767=20
    38569827 38689867 39079892 39909900 41439917=20
    42669922 43359916 43749895=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 16 14:43:10 2024
    AWUS01 KWNH 161443
    FFGMPD
    NCZ000-SCZ000-162045-

    Mesoscale Precipitation Discussion 1022
    NWS Weather Prediction Center College Park MD
    1042 AM EDT Mon Sep 16 2024

    Areas affected...Southeastern NC...Eastern SC...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 161445Z - 162045Z

    SUMMARY...Potential T.C. Eight. Add'l 4-8" possible, likely
    resulting in expanding flash flooding area; localized considerable
    flash flooding is likely as well.

    DISCUSSION...Sizable rainfall totals over 6"+ have been reported
    since midnight across portions of far southeastern North Carolina
    this morning resulting in flash flooding conditions. 14z surface
    obs and remote sensing suite depict the surface center of PTC
    Eight is about 60-70 nmi southeast of Myrtle Beach, showing fairly
    solid frontal structure with a well defined cold front associated
    low-topped tropical shower line along the northeast and eastern
    quadrants before angling along the Gulf Stream back to Florida.=20
    Theta-E gradient also depict a sharpening warm front parallel to
    the SC/NC coast to around Cape Fear before extending more
    eastward, but has been showing a trend of north-northwestward
    translation over the last few hours. This is expanding the warm
    sector which is well defined with a axis of enhanced MLCAPE
    increasing to 1500-2000 J/kg with a fairly saturated narrow skinny
    profile, though there is a bit of mid-level dry air nosing in
    along the southwest side. Along/north of the boundary the
    effective cool conveyor belt is fully saturated through depth with
    total PWat values over 2" reaching 2.25"; so with a highly
    convergent low level profile an strong instability; deep
    convection is likely to further develop/maintain through the late
    morning into the afternoon hours with the capability of 2-3"/hr
    rates (perhaps locally higher in short-duration) as convergence
    waves move through the warm sector/TROWAL. Given proximity of the
    warm front to the coastline, slow northward expansion of these
    stronger highly efficient showers, but may be more inconsistent in
    timing with reduced low level moisture convergence relative to
    Brunswick/New Hanover counties. An additional 4-8" are possible
    through the next 6 hours and considerable flash flooding will
    likely become more common across these counties.=20

    Further ashore...a mesoscale low/wave could be seen within the
    coastal observations along the southern coast of Brunswick county
    as well as within KLTX RADAR and appears to be strongly convergent
    along the western edge of the low to mid-level TROWAL. Given
    orientation to the core vorticity center that has recently rotated
    under the eastern edge of the canopy (noted by reduced warm temps
    in the WV suite); the wave will likely slow and translate a bit
    south of due west. The remaining strong moisture flux convergence
    but stabilizing air, will maintain enhanced rain rates but will
    reduce into the 1-2"/hr range but likely have some training given
    the orientation of the TROWAL should be consistent to expand heavy
    rainfall footprint toward Dillon counties in SC and
    Robeson/Columbus counties in NC with very slow northward
    translation expected. Totals of 2-4" over the next 6hrs are
    possible and should expand flash flooding problems that way as
    well with time.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5xwHMtQfPKsteE_vVreoz_AYW8LE883pkfAxZIQHbZvl7wPaB5u1hnY-UwZ7VlPEcRQ7= 5E5scPF4EkUykcP872PCBTU$ for graphic product...

    ATTN...WFO...CAE...ILM...MHX...RAH...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 35147832 35057741 34967685 34787644 34577652=20
    34617684 34547718 34427746 34217769 33977780=20
    33817802 33827837 33787887 33977988 34388018=20
    34818004 35027932=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 16 19:25:11 2024
    AWUS01 KWNH 161925
    FFGMPD
    MNZ000-NDZ000-170123-

    Mesoscale Precipitation Discussion 1023
    NWS Weather Prediction Center College Park MD
    324 PM EDT Mon Sep 16 2024

    Areas affected...near the northern ND/MN border

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 161923Z - 170123Z

    Summary...Showers and thunderstorms are expected to expand in
    coverage and shift more towards a front as an upper-level cyclone
    moves by the area and CIN reduces. Hourly rain totals to 2.5"
    with local totals to 4" are possible.

    Discussion...A northeast-moving upper low in western ND along with
    surface heating to leading to reduced CIN across portions of ND
    near a stationary front, which was earlier reinforced with
    convective outflow. Precipitable water values of 1.5" lie near
    the boundary. Effective bulk shear of ~40 kts exists. ML CAPE of
    500-2000 J/kg exists, and is increasing. Temperatures at 700 hPa
    are 6-9C.=20

    The expectation is for some convective expansion with time, as ML
    CAPE increases beyond 2500 J/kg in the warm sector. When CIN
    reduces to zero, there is a question of whether the instability
    shifts northward to the convection or if new convection forms
    closer to the returning boundary. The MPD area takes both into
    account. Also, the degree of effective bulk shear argues for
    mesocyclones, which can be effective heavy rain producers. At
    some point, the activity will try to forward propagate, which
    veering 850 hPa winds strongly suggest, but the returning front
    should limit southward propagation, favoring a vector more to the
    east with time. While there is a signal for heavy rainfall in the
    recent mesoscale guidance, there is a bit of spread, so
    uncertainty is greater than normal. The ingredients suggest
    hourly totals to 2.5" and local totals up to 4". Since it's
    falling over areas that received similar rainfall over the past 24
    hours, depressing flash flood guidance values, flash flooding is
    considered possible, with the more significant impact in urban
    areas.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_uBfQpEdXGiRGST_uUDGypJbtbtzzKwms6f5tTCfeIJeaScGr-d8jj6V1XmcCu2oSYF_= 0EH4pq2L6K69kg1S6-Oq7bY$ for graphic product...

    ATTN...WFO...BIS...FGF...

    ATTN...RFC...MBRFC...NCRFC...NWC...

    LAT...LON 49929486 49489441 48689448 48109673 47879792=20
    47649882 47939969 48360027 49389767=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 16 19:55:08 2024
    AWUS01 KWNH 161955
    FFGMPD
    COZ000-NMZ000-UTZ000-170053-

    Mesoscale Precipitation Discussion 1024
    NWS Weather Prediction Center College Park MD
    354 PM EDT Mon Sep 16 2024

    Areas affected...in and near southwest CO

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 161953Z - 170053Z

    Summary...Thunderstorms with heavy rainfall are expected to move
    into the area over the next several hours. Hourly rain totals up
    to 1.5" are possible, which would be problematic in steep terrain,
    arroyos/dry washes, burn scars, and slot canyons.

    Discussion...A deep upper-level trough across the West has led to
    the formation of a boundary moving through eastern AZ and along
    the UT/CO border at its leading edge which is spurring some shower
    and thunderstorm development. Clouds are eroding and those that
    exist are becoming more convective in appearance in recent GOES
    Veggie Band imagery. Precipitable water values are ~0.75",
    sufficiently moist considering the elevation, with ML CAPE values
    of 500-1500 J/kg, highest near the Four Corners. Effective bulk
    shear across the region is impressive, in the 40-50 kt range. CIN
    appears negligible.

    Guidance has a signal for heavy rainfall in the topography of
    southwest CO through 00z before fading thereafter, which could be
    due to the movement of the aforementioned boundary and related
    erosion of the instability pool near the Four Corners. In the
    meantime, convection with possible mesocyclones could lead to
    hourly rain totals to 1.5" where rain is most persistent due to
    either training, backbuilding, or cell mergers. This would be
    problematic is any steep terrain, arroyos/dry washes, burn scars,
    and slot canyons.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_VlaLZI1a52E-9Lby_akXp19B5AdovLCYDDj6cKXW8JWI9FwUeHmvz-cY416reH8u9TQ= afMVtRXBsIzhFWoCcUXXVzo$ for graphic product...

    ATTN...WFO...ABQ...GJT...PUB...

    ATTN...RFC...CBRFC...WGRFC...NWC...

    LAT...LON 38480817 37940652 36860591 36560608 36480666=20
    36860872 37290937 37970923=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 16 20:49:53 2024
    AWUS01 KWNH 162049
    FFGMPD
    NCZ000-SCZ000-170247-

    Mesoscale Precipitation Discussion 1025
    NWS Weather Prediction Center College Park MD
    448 PM EDT Mon Sep 16 2024

    Areas affected...portions of northeast SC & eastern NC

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 162047Z - 170247Z

    Summary...A deep layer cyclone will continue moving inland near
    the SC/NC border. Heavy rainfall within its comma head
    circulation and banding to its east will lead to flash flooding.

    Discussion...A deep layer cyclone, designated as Potential
    Tropical Cyclone Eight by NHC earlier, continues to move inland
    across far northeast SC. ML CAPE of 500-2000 J/kg is being
    imported into southeast NC on its eastern flank, which has been
    driving a narrow line of convection pushing slowly up the coastal
    plain of NC. Precipitable water values are 1.75-2.25" in this
    region. Effective bulk shear remains 30-35 kts.

    There are a few foci for heavy rainfall from this system -- the
    stratiform heavy rain shield to its west-northwest, the heavy rain
    band moving up the NC coast, and the coastal front moving towards
    the Fall Line on its northeast side. Within the stratiform rain
    shield, 1-2" an hour totals and additional totals to 3" remain
    possible over the next several hours as the system moves
    west-northwest. Within the primary heavy rain band, hourly totals
    up to 4" and local totals to 8" remain possible as it drifts
    northeast. Near the coastal front in eastern NC, hourly rain
    totals to 2.5" and local totals to 5" remain possible as it moves
    farther inland. The biggest concern is if a new heavy rain band
    forms closer to Southport-Oak Island-Bolivia-Carolina Beach while
    the cyclone moves inland as radar estimates of rain so far in that
    area are close to 18".=20

    In many areas of central and eastern NC, along with far northeast
    SC, soils are saturating if not saturated, causing 3 hourly flash
    flood guidance to be increasingly low and easier to achieve.=20
    Flash flooding is considered likely.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9AOZ3yU3haTnyz2q_qOSYWgEhkCdpWsntrNdokXsuoCwbJVB0f7BzlX4laLPswc6EGZS= w41OClstxl62XoA4iNIxsrg$ for graphic product...

    ATTN...WFO...CAE...GSP...ILM...MHX...RAH...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 36078040 35957828 35597658 35227581 35107569=20
    34587650 34287709 33827775 33417879 34038004=20
    34648089 35618162=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 17 00:30:13 2024
    AWUS01 KWNH 170030
    FFGMPD
    MNZ000-NDZ000-170627-

    Mesoscale Precipitation Discussion 1026
    NWS Weather Prediction Center College Park MD
    829 PM EDT Mon Sep 16 2024

    Areas affected...portions of northeast ND & northwest MN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 170027Z - 170627Z

    Summary...Isolated to widely scattered instances of flash flooding
    are expected to continue overnight. Hourly rain totals to 2.5"
    and additional local amounts to 5" are expected.

    Discussion...The three recent areas of convection across northern
    ND into northwest MN are beginning to bridge together as new
    convection forms at the present time. The western end moving east
    of Minot is associated with an upper level low/MCV moving
    northeast across ND. Farther east in northeast ND and northwest
    MN, additional thunderstorms are forming within a warm air
    advection pattern ahead of a related surface wave and near its
    warm front, which appears to be in the process of becoming
    stationary or perhaps nudging southward due to convective outflow.
    Precipitable water values are around 1.5" per GPS data.=20
    Effective bulk shear in the region is 25-35 kts, which is helping
    to organize the thunderstorms. MU CAPE is 1500-3000 J/kg. CIN is
    rebuilding across the region, which should keep most convection
    elevated.

    The upper low/MCV and its convective cluster marks the western
    fringe of the heavy rain threat and is forward propagating to the
    east. Mesoscale guidance still isn't agreeable on which side of
    the US/Canadian border -- if not right along it -- the rainfall
    maximum is expected over the next six hours, but radar
    reflectivity trends continue to support heavy rain on the U.S.
    side, or the southern side of the mesoscale guidance spread.=20
    Eastward propagation should continue. The Canadian Regional Model
    made a substantial southward shift in its 18z run, supporting the
    more southward placement. Given what's happened so far, hourly
    rain totals to 2.5" and additional local amounts to 5" are
    expected. This would be most problematic in areas that received
    heavy rainfall over the past 24 hours. Due to the isolated to
    widely scattered nature of the flash flooding/very heavy rainfall
    thus far and uncertainty in the model guidance, continue to use
    possible wording over likely.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!46Oww9KZBv0Ueck8mouLXpwz_dWjK7-7c3BnyaoEs4pm2gfdgbc0egNU4vYiUR--Btse= kCWfOIFLHHNg-6rN3Texr64$ for graphic product...

    ATTN...WFO...BIS...DLH...FGF...

    ATTN...RFC...MBRFC...NCRFC...NWC...

    LAT...LON 49509618 49459488 48669337 48089390 47919566=20
    47899642 47869755 47760140 48160139 48370122=20
    48729983 49129838 49389725=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 17 03:02:44 2024
    AWUS01 KWNH 170302
    FFGMPD
    NCZ000-170900-

    Mesoscale Precipitation Discussion 1027
    NWS Weather Prediction Center College Park MD
    1101 PM EDT Mon Sep 16 2024

    Areas affected...Central and Eastern NC

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 170300Z - 170900Z

    SUMMARY...The non-tropical low center along the SC/NC border
    continues to facilitate an influx of deep Atlantic tropical
    moisture into the southern Mid-Atlantic region. Additional areas
    of flash flooding are likely overnight across central and eastern
    NC, and this may include locally considerable impacts.

    DISCUSSION...Low pressure continues to gradually advance
    northwestward across the southern Mid-Atlantic which will continue
    to drive a significant amount of deep Atlantic tropical moisture
    inland. Strong moisture transport aided by an easterly low-level
    jet of 30 to 40+ kts will continue to combine with a nose of
    moderate instability for bands of strong convection with locally
    extreme rainfall rates. The latest RAP analysis shows MLCAPE
    values of 1000 to 1500 J/kg still nosing inland across parts of
    southeast NC just to the northeast of a frontal occlusion, and
    this should pivot gradually northward into adjacent areas of
    eastern NC overnight.

    Given the persistent level of low-level forcing and instability,
    some of these bands of convection should maintain a fair degree of
    organization over the next several hours. Given this and the pool
    of deep tropical moisture concentrated over especially eastern NC,
    some of the rainfall rates may still be capable of reaching 2 to
    3+ inches/hour.

    In fact, given the locally extreme rainfall rates and concerns for
    more training convective bands, additional rainfall amounts may
    reach 3 to 6 inches with isolated 8+ inch amounts just for the
    overnight period. The HRRR in particular suggests notable
    concentrations of heavy to extreme totals for portions of Jones,
    Craven, Beaufort, Pamlico and Carteret Counties, and this region
    will need to be closely monitored for considerable flash flooding
    impacts.

    Farther back to the west across central NC, including the
    Raleigh-Durham metropolitan area, the instability drops off rather substantially and this will yield lower rainfall rates by
    comparison to areas farther east. However, there should still be
    sufficient levels of moisture convergence/forcing for heavy
    showers that may yield an additional 2 to 3+ inches of rain
    overnight. This will likely sustain the ongoing areas of flash
    flooding including persistent urban runoff concerns.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5Jf9v5O4N5z-_NP-_rdeKeR6AgA-JYbcEVPU_isUllSge-li31K5NgbaTyqfmN--JeN-= KyQ8SdlFN5ieu1YfROSlcfg$ for graphic product...

    ATTN...WFO...AKQ...GSP...ILM...MHX...RAH...RNK...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 36477854 36257720 35837636 35397576 34867583=20
    34557655 34507730 34767796 34977890 35087986=20
    35798037 36387992=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 17 09:02:17 2024
    AWUS01 KWNH 170902
    FFGMPD
    VAZ000-NCZ000-171500-

    Mesoscale Precipitation Discussion 1028
    NWS Weather Prediction Center College Park MD
    500 AM EDT Tue Sep 17 2024

    Areas affected...Eastern NC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 170900Z - 171500Z

    SUMMARY...An area of low center over northern SC will maintain a
    threat of locally training bands of heavy showers and
    thunderstorms this morning over eastern NC. Some additional areas
    of flash flooding will be possible.

    DISCUSSION...The early morning GOES-E Proxy Visible satellite
    imagery along with surface observations shows low pressure over
    northern SC. This couple with surface high pressure over the
    Northeast continues to favor a persistent and moist, convergent
    low-level easterly Atlantic fetch across the southern Mid-Atlantic
    region. High PWs of 1.8 to 2.2 inches coupled with a nose of
    modest instability with MLCAPE values of 500 to 1000 J/kg
    continues to focus across eastern NC out ahead of a frontal
    occlusion. This is continuing to allow for the development of some
    broken bands of heavy shower and thunderstorm activity.

    The latest radar imagery shows the heaviest rains impacting
    portions of Carteret and Craven Counties where rainfall rates,
    especially in close proximity to Morehead City, have been locally
    as high as 2 to 3 inches/hour over the last couple of hours.

    Additional bands of heavy showers and thunderstorms are expected
    this morning to slowly lift north and northwestward across areas
    of eastern NC as the overall frontal occlusion pivots a bit
    farther north across the southern Mid-Atlantic region. Persistent
    easterly flow off the Atlantic and an influx of modest instability
    should favor high rainfall rates continuing with some of the
    broken convective bands that maintain some stronger organization.

    The latest hires model guidance generally favors areas of far
    eastern NC with the heaviest additional rainfall totals, with more
    modest amounts farther inland as the nose of instability wanes.
    Some localized additional totals of 3 to 6+ inches of rain cannot
    be ruled out this morning within any of the heavier training
    convective bands. This will certainly maintain an additional
    threat for areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5DReUK-ApGm8XuGkXCVbzdZsd6EQpj2K5Ko23cgVThT6dqAyvjXs_THH2Or21uhOYCWP= h46Bh770BBDc5bkcz5fztG4$ for graphic product...

    ATTN...WFO...AKQ...MHX...RAH...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 36577753 36377606 35877552 35427538 35207552=20
    34977599 34727630 34827674 35327723 35767829=20
    36327834=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 17 15:13:20 2024
    AWUS01 KWNH 171513
    FFGMPD
    VAZ000-NCZ000-172030-

    Mesoscale Precipitation Discussion 1029
    NWS Weather Prediction Center College Park MD
    1112 AM EDT Tue Sep 17 2024

    Areas affected...Southeast VA...Northeast NC...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 171510Z - 172030Z

    SUMMARY...South to north training and efficient rainfall rates up
    to 2-3"/hr approaching urban centers of SE VA pose possible
    localized flash flooding/rapid inundation flooding through early
    afternoon.

    DISCUSSION...Active convection this morning over the Pamlico River
    supported a tightening of the surface triple point as well as an
    associated boundary layer to 850mb low. While these two features
    have separated with the occluded low still remaining south toward
    the mouth of the Pamlico River; the elevated circulation has
    lifted northward over toward the Chowan/Albermarle Rivers
    continuing to lift north. The trailing tail has become highly
    convergent with easterly surface to 850mb both north of the warm
    front (near Roanoke Island) lifting north and veered southeasterly
    flow out of the warm sector over the central sound and Atlantic
    east of the Outer Banks. Tds in the mid to upper 70s with temps
    increasing to the mid-80s in the warm sector is supporting
    increasingly unstable air with MLCAPEs over 1500 J/kg fueling
    stronger updrafts within the strengthening deep layer convergence
    axis. Total PWats of 2-2.25" are more than sufficient (loaded
    with 1-1.2" in the lowest sfc-850mb per CIRA LPW) with the
    strength of flux to support 2-2.5"/hr perhaps occasionally ticking
    up to 3"+/hr for short-durations and highly localized.=20

    Deep layer steering will support a south to north training that
    may result in a few hours of training. This may result in 3-5"
    localized totals across far SE VA and NE NC; however, there is
    some uncertainty that propagation to the east due to the strength
    of inflow may reduce the training duration but also shift the
    focus along or just offshore, limiting the flash flooding/rapid
    inundation risk. While much of the area is sandy soils (FFG
    3-4"/3hrs) and supports higher infiltration, rates over 3"/hr or
    even proximity to urban centers have a higher probability of
    inducing flash flooding. Hi-Res CAMs are more persistent in
    allowing for more westerly cell motions expanding the flooding
    threat westward; however, nearly all do not resolve this low level
    wave lifting north acting like a barrier as well as reducing
    insolation with increased cirrus canopy and therefore unstable
    downstream air. The 12z ARW2 seems to handle this wave best of
    the overall solutions but trends appear west compared to
    observations. Bottom line, these variations due reduce overall
    confidence in precise placement but the rates/potential totals
    should result in localized flash flooding.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4-tE9V3JbwyxnL18d2N9b0WMH2zAyspkoH9Hc6iHHVIVzN2X3W6TPppy6me98rvUP4zJ= zD-j9FmiCdUhD-_CWG8qtwQ$ for graphic product...

    ATTN...WFO...AKQ...MHX...

    ATTN...RFC...MARFC...SERFC...NWC...

    LAT...LON 37847641 37717571 37347562 36797581 36067559=20
    35427534 35247557 35717611 36137646 36437669=20
    36857687 37347693 37667677=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 17 20:31:56 2024
    AWUS01 KWNH 172031
    FFGMPD
    VAZ000-NCZ000-TNZ000-180130-

    Mesoscale Precipitation Discussion 1030
    NWS Weather Prediction Center College Park MD
    431 PM EDT Tue Sep 17 2024

    Areas affected...Piedmont to Southern Blue Ridge

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 172027Z - 180130Z

    SUMMARY...East to West training and efficient rainfall rates up to
    2-3"/hr in a band developing over an occluded front over the
    Piedmont of northern North Carolina will continue to develop and
    shift across portions of the southern Blue Ridge near the NC/VA
    border into this evening. Localized flash flooding/rapid
    inundation flooding in this narrow corridor is likely.

    DISCUSSION...Convection has reinvigorated in broad convergence
    along/north of an occluded front over the NC Piedmont this
    afternoon from around the Raleigh-Durham Triangle west through the
    southern Blue Ridge near the NC/VA border. Dewpoints in the low
    70s with sufficient instability (1000 J/kg MUCAPE) along the
    occluded front are fueling stronger updrafts and the influx of
    tropical moisture is allowing redevelopment. PW of 1.6 to 1.8" are
    1.5 sigma from normal support 2-2.5"/hr rain rates that may
    locally peak at 3"/hr as seen from KFCX over Stokes Co NC,
    particularly in areas of upslope with the steep eastern side of
    the Blue Ridge (near and south of Fancy Gap) in the area of
    concern.=20

    Slow motion to the occluded low/front will support west to east
    training over the next few hours. This may result in 3-5"
    localized totals over the NC Piedmont and especially along the
    Blue Ridge. Given that around an inch of rain fall in advance of
    this activity over the past day, FFG is generally around 1.5"/hr.
    Recent HRRR runs have picked up on this activity and features
    splotches around 2" through 02Z. However, given the sufficient
    instability, slow motion, and heavy rates observed, flash flooding
    is considered likely.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4iXPljgjvgcyR0FGICswSwmsRvLrVzERXNg7vvedUxHvCrMPZI7HFFuuxvlxEs1xhvrn= P_RSa6bp75Iq4qYJuvQbN00$ for graphic product...

    ATTN...WFO...MRX...RAH...RNK...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36938152 36838049 36647977 36337900 36057852=20
    35827844 35757878 36218049 36398181=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 17 23:06:57 2024
    AWUS01 KWNH 172306
    FFGMPD
    VAZ000-NCZ000-180500-

    Mesoscale Precipitation Discussion 1031
    NWS Weather Prediction Center College Park MD
    706 PM EDT Tue Sep 17 2024

    Areas affected...Southeast Virginia and Northeast North Carolina

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 172302Z - 180500Z

    SUMMARY...Heavy rain will continue to drift northwest from the
    northern Outer Banks into or through the Hampton Roads metro area
    this evening. Considerable flash flooding is possible given the
    high rainfall rates and particularly slow motion.

    DISCUSSION...Convection continues to redevelop north of a warm
    front extending east near the Albemarle Sound in northeast NC.
    This has resulted in considerable flash flooding in the northern
    outer banks with 5-8" estimated from KAKQ between Duck and Corolla
    today. Rainfall rates of 2-2.5" have been estimated from KAKQ
    around Corolla between 22Z and 23Z. This activity is drifting
    north and has a reasonable chance of continuing at a similar
    intensity farther north over Virginia Beach and the Hampton Roads
    metro area.

    A tropically-sourced plume of moisture, with PW of 2.1" per SPC
    RAP mesoanalysis is north of the warm front and shifting into the
    Virginia Capes on convergent low level flow. Sufficient
    instability (1000 J/kg MUCAPE) should continue to support hourly
    rainfall of 2-3"/hr. FFG is generally 1.5-2"/hr over Virginia
    Beach given the around 2" of rain that fell there earlier today.
    Recent HRRR runs have been too progressive with this activity
    shifting northeast, but the NW direction of motion ahead of the
    warm front that is slowly drifting north is reasonable. Given the
    potential for these heavy rates to cross the vulnerable Hampton
    Roads metro area, the flash flood threat is considered likely for
    this evening.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5i63edGWENQrh8G7M1L-zHMuXRAkByVNiqOcTe-WYD0R3XAsv5uni710zTUIotrPVfJz= AJa9tKEPHZl6-lZ9E6N3IVw$ for graphic product...

    ATTN...WFO...AKQ...MHX...

    ATTN...RFC...MARFC...SERFC...NWC...

    LAT...LON 37387681 37387625 37257574 36587560 35807538=20
    36257625 36597675 37037716=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 18 09:06:33 2024
    AWUS01 KWNH 180906
    FFGMPD
    MTZ000-181505-

    Mesoscale Precipitation Discussion 1032
    NWS Weather Prediction Center College Park MD
    505 AM EDT Wed Sep 18 2024

    Areas affected...Central MT

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 180905Z - 181505Z

    SUMMARY...Heavy rainfall is expected to become more concentrated
    going through dawn and the early morning hours across portions of
    central MT. Generally this setup will favor an areal flood threat,
    but around any burn scar locations, there will be a more enhanced
    runoff concern with potential for localized flash flooding.

    DISCUSSION...A deepening upper-level trough and associated area of
    low pressure lifting up across the northern High Plains will be
    driving a rather impressive heavy rainfall event beginning early
    this morning across central MT. Facilitating this will be the
    evolution of a well-defined TROWAL working in tandem with an
    increasingly focused area of deep layer frontogenesis along with a
    strong mid-level deformation zone. This should yield enhanced
    forcing to help concentrate the heavy rainfall threat in time
    which will also include an increase in rainfall rates.

    Gradually the heavy rainfall axis should tend to become oriented
    in a general south-southwest to north-northeast fashion around the
    northwest flank of the deepening 500/700 mb mid-level low center
    and where frontogenetical forcing will be the strongest. However,
    there is already a fair amount of instability attempting to wrap
    westward around the north side of the deepening low, and there
    will likely be a corridor of elevated convective elements that
    will help drive locally heavier rainfall rates early this morning.

    The 00Z HREF guidance and recent runs of the HRRR suggest as much
    as 2 to 4+ inches of rain may fall through the early morning hours
    (15Z/9AM MDT), with some occasional rainfall rates that may reach
    upwards of 0.75" to 1"/hour with some of the stronger convective
    elements that materialize.

    These rains are expected to gradually drive an areal flood threat,
    which may also include a threat for localized flash flooding
    around any burn scars that receive some of these heavier rainfall
    rates.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-947VJ_LSEJIjrePRyZbbUk6grEIFxwzYOkTkMNeR1rw6NGCDbxj65jGw8U4-F2HNjW3= ZmFrWMNY7Gj3h8CUBy40ytk$ for graphic product...

    ATTN...WFO...BYZ...GGW...TFX...

    ATTN...RFC...MBRFC...NWC...

    LAT...LON 49270843 48780760 47520767 46370826 45740926=20
    45751071 46221151 47041177 47821154 48601088=20
    49220976=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 19 18:34:54 2024
    AWUS01 KWNH 191834
    FFGMPD
    FLZ000-200000-

    Mesoscale Precipitation Discussion 1033
    NWS Weather Prediction Center College Park MD
    234 PM EDT Thu Sep 19 2024

    Areas affected...Southeast Florida

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 191833Z - 200000Z

    Summary...Slow moving showers and thunderstorms will expand across
    Southern Florida through the afternoon. Rainfall rates of 2-3"/hr
    are likely, which could result in 2-4" of rain with locally higher
    amounts. This may result in flash flooding, primarily within urban
    areas.

    Discussion...The regional radar mosaic this afternoon depicts a
    slow increase in coverage of reflectivity across the southern and
    central portions of the Florida Peninsula. This coverage is
    increasing thanks to rapid destabilization characterized by 3-hr
    MLCAPE change as high as +1000 J/kg according to the SPC RAP
    analysis, in the presence of PWs around 2.1 inches, or about the
    90th percentile for the date. Into these impressive
    thermodynamics, ascent is occurring in the vicinity of a weakening
    surface boundary draped from near Cape Canaveral to Port
    Charlotte, with additional lift provided through a weak shortwave
    lifting eastward near the Everglades and a sharpening sea breeze
    boundary along the Gold Coast. Storms which have developed so far
    have been pulse thanks to weak shear, but have contained at least
    brief rainfall rates estimated by KAMX to be as high as 2.5"/hr.

    There is good agreement among the various high-res members that
    the coverage of convection will continue to expand the next few
    hours as instability maximizes and the different forcing
    mechanisms continue to impinge on the area. Although bulk shear
    will remain weak to limit much organization, widespread cell
    development, especially as the shortwave lifts northeast, should
    result in numerous outflow boundaries, suggesting disorganized
    clusters through storm mergers and boundary interactions. With the
    anomalous PWs in place, this should result in rainfall rates that
    have a 20-40% chance of exceeding 2"/hr according to the HREF,
    with short-duration rainfall rates potentially reaching 4"/hr as
    suggested by HRRR 15-min rainfall reaching 1" in some areas.

    Mean 850-300mb wind speeds are expected to remain weak at just
    5-10 kts, and Corfidi vectors collapse to 5 kts or less into the
    evening. This indicates slow and chaotic cell motions, especially
    during collisions/mergers, to lengthen residence times of these
    heavy rain rates. The most likely location for any persistent
    rainfall rates will be along the westward advancing sea breeze
    however, as anti-parallel mean flow to this boundary should result
    in regeneration of cells from west to east. This could create
    rainfall amounts of 2-4", with locally higher amounts possible
    across the urban Gold Coast. This will create a 40-60% chance of
    exceeding FFG according to the HREF, and if these intense rates
    linger across any urban areas this afternoon, instances of flash
    flooding could result.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!76iX0VNVa06d1Trrxj3E7GPWu4TM7_qLJln1pobkKeulQykaSrLTMQMZjeaeS3JM2_dl= cSpBPKRFnSG6RyM8_r_5fFg$ for graphic product...

    ATTN...WFO...MFL...MLB...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 27478032 27178010 26928001 26498001 26128003=20
    25768013 25438027 25308036 25408051 25768074=20
    26178092 26638083 26888062 27308073 27418058=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 19 22:29:29 2024
    AWUS01 KWNH 192229
    FFGMPD
    WIZ000-MNZ000-IAZ000-200428-

    Mesoscale Precipitation Discussion 1034
    NWS Weather Prediction Center College Park MD
    628 PM EDT Thu Sep 19 2024

    Areas affected...portions of southern/central Minnesota and
    Wisconsin

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 192228Z - 200428Z

    Summary...Isolated/localized flash flood potential exists through
    the early afternoon as a complex of thunderstorms produce heavy
    rainfall across the discussion area.

    Discussion...Over the past 1-2 hours, progressive convection has
    increased in coverage and evolved into a more organized/focused
    area of cells and linear segments generally extending from near
    LaCrosse to Owatonna (along I-90/US 14). These storms were in a
    moist, unstable warm sector, with 1.5 inch PW values and ~2000
    J/kg MLCAPE values supporting robust updrafts and spots of 1
    inch/hr rain rates. The storms were embedded in fairly strong
    flow aloft (resulting in 40-kt storm motions), but were oriented
    favorably for training especially along the aforementioned I-90/US
    14 corridor. As cells continue to mature in this corridor (while
    migrating east-northeastward into Wisconsin), the expectation is
    that a few areas of rain rates approaching 2 inches/hr could
    materialize and cause isolated/localized flash flood issues
    through at least 03Z tonight.

    The complex will produce these rain rates atop areas of ground
    conditions that exhibit slightly more sensitivity with
    northeastward extent. Soils are more moist in central Wisconsin,
    and FFGs are slightly lower there (1.5 inch/hr thresholds)
    compared to the remainder of the discussion area (closer to 2
    inches/hr). The overall threat of flash flooding is a bit
    conditional on heavier rain rates materializing on sensitive
    soils. This threat should persist through the 03-04Z timeframe.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7Sf-oiCjID2ImB73v7MUfwc0W7H1Uh93se50o9CyUswnxtmCO7CEJrCyCYYk-PBYJCSg= AMwPJST6PC2e-qCmb0C-lwY$ for graphic product...

    ATTN...WFO...ARX...DLH...GRB...MKX...MPX...

    ATTN...RFC...NCRFC...NWC...

    LAT...LON 45619071 45328955 44448918 43868942 43489096=20
    43559310 43909375 45119316 45459238=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 19 23:03:29 2024
    AWUS01 KWNH 192303
    FFGMPD
    CAZ000-200502-

    Mesoscale Precipitation Discussion 1035
    NWS Weather Prediction Center College Park MD
    703 PM EDT Thu Sep 19 2024

    Areas affected...a small part of southwestern California

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 192302Z - 200502Z

    Summary...A few slow-moving thunderstorms have developed along
    coastal ranges north of Santa Barbara. Some of these downpours
    were falling on sensitive areas from burn scars, potentially
    promoting excessive runoff. At least a few hours of locally
    enhanced flash flood potential is expected.

    Discussion...Abundant sunshine/destabilization beneath a cold
    upper trough (centered near 34.8N, -121.3W) has fostered scattered
    thunderstorm development near San Luis Obispo/Santa Barbara county
    coastal ranges this afternoon. These storms are very slow moving
    due to weak mid/upper flow beneath the trough. -17C temperatures
    at 500 hPa was promoting areas of 500-1000 J/kg SBCAPE in vicinity
    of the storms. Additionally, despite modest PW values (around 0.8
    inch), easterly low-level flow was promoting focused
    upslope/orogarphic lift against the coastal ranges to promote
    persistent updrafts and slow-moving downpours. Areas of 0.25-0.5
    inch/hr rain rates have been estimated per MRMS so far, with areas
    of rainfall occurring close to sensitive burn scars across the
    discussion area.

    Heavy rainfall/flash flood potential will exist in portions of the
    discussion area through/beyond 05Z per recent model guidance/CAMs.
    The persistence of this heavy rainfall regime is tied to expected
    slow movement of the mid/upper low over the area. Isolated areas
    of 1-1.5 inches are possible in this regime.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!52COZxdYxd4h-Qpe2pTYhqnVewRUkqt1LjyxEu_8pWBzcH7clVZTtACr5sCtsIqLn06g= vsNXx0ITaPhT_8ArmESHqMY$ for graphic product...

    ATTN...WFO...HNX...LOX...MTR...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 36232039 36071969 35431895 34861847 34621837=20
    34441887 34681960 35212047 36122109=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 20 19:44:13 2024
    AWUS01 KWNH 201944
    FFGMPD
    AZZ000-NVZ000-CAZ000-210130-

    Mesoscale Precipitation Discussion 1036
    NWS Weather Prediction Center College Park MD
    343 PM EDT Fri Sep 20 2024

    Areas affected...Southern CA...Far Southern NV....Far Northwest
    AZ...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 201945Z - 210130Z

    SUMMARY...Slow moving, back-building cells with rates of 1"/hr may
    pose localized 1-1.5" totals and possible flash flooding
    conditions.

    DISCUSSION...GOES-W and Regional RADAR mosaic have started to
    depict increasing convective activity in both coverage and
    vertical depth with peak heating of the day. The highly
    anomalous, over 3.5 standard anomaly units from climatology, core
    of the closed low is bottoming out across SW California with
    vorticity center at the southern base; this is allowing for an elongation/stretching of the mid-level deformation zone to extend
    across SW to NE San Bernadino county with increased deep layer
    convergence. Given steepening lapse rates with cold air advection
    aloft, surface heating into the 80s is starting to support surface
    based CAPE values from 500-1000 J/kg to develop over the Southern
    California Deserts toward the Colorado River Valley near S Nevada.
    While deep layer moisture is a bit limited with only Tds in the
    upper 40s, low 50s and total PWat values in the .75 to 1" range.=20
    The convergence within the band and orographic ascent confluent
    across the San Bernadino/Little Bernadino/San Jacinto Ranges
    supports stronger vertical development and sufficient moisture
    flux to support .5-1"/hr rates.=20

    Limited cell motions given proximity to the closed low/deformation
    zone will allow for very slow/stationary motion with upstream redevelopment/backbuilding along the deformation band across NE
    CA. Propagation may also allow cells along the mountain ridges
    into the Cochella Valley with time. This may allow for spotty
    .75-1" totals with an isolated 1.5" total remains possible. Given
    naturally low FFG values less than these hourly rates and
    potential; an isolated flash flooding incident or two is
    considered possible across the area through the late
    afternoon/evening hours.=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-GqRMhYZHk0M1T6xycX3xsEm8BRojKKapxGLzUDkw1h2W0EWZUrSFVO62--GscVb0taT= IqEaGraJfLMEU3T1ND87DHw$ for graphic product...

    ATTN...WFO...PSR...SGX...VEF...

    ATTN...RFC...CBRFC...CNRFC...NWC...

    LAT...LON 36051537 35651447 35091429 34421518 33621507=20
    33231522 33321587 32881615 32921657 33461673=20
    33991720 34191765 35011753 35581699 36001605=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 21 16:28:25 2024
    AWUS01 KWNH 211628
    FFGMPD
    TXZ000-OKZ000-KSZ000-COZ000-NMZ000-212230-

    Mesoscale Precipitation Discussion 1037
    NWS Weather Prediction Center College Park MD
    1227 PM EDT Sat Sep 21 2024

    Areas affected...High Plains of New Mexico into the Panhandles of
    Texas and Oklahoma

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 211630Z - 212230Z

    Summary...Showers and thunderstorms will expand in coverage
    through the afternoon while intensifying to feature rainfall rates
    nearing 1"/hr. Although storms will generally be fast moving,
    repeating rounds could result in 1-3" of rainfall and instances of
    flash flooding.

    Discussion...The GOES-E WV imagery shows an anomalously deep upper
    low moving over northern AZ with impressive downstream lift and
    moisture advecting into the southern High Plains of NM. Within
    this moisture plume, an area of moderate stratiform rain has
    lifted towards the TX Panhandle, while in its wake secondary
    convective development is gradually occurring as reflected by
    increasing glaciation in deepening cells noted via the day-cloud
    phase RGB. Rainfall from the morning precipitation has been as
    much as 0.5 inches measured by local mesonets, wetting the soils
    ahead of what should be increasing convective activity as PWs
    surge to 1.25-1.5 inches, and SBCAPE rises to 1000-2000 J/kg.

    As thermodynamics intensify through the aftn, forcing for ascent
    is also likely to become more impressive. The potent closed low
    and associated trough to the west will gradually push east,
    driving intense downstream divergence coincident with increasing
    upper diffluence over the southern High Plains. At the same time, unidirectional low-level southerly flow will begin to
    isentropically ascend the southward advancing cold front, and the
    overlap of these forcing mechanisms into the elevated
    PW/instability will result in widespread convective development as
    suggested by high-res simulated reflectivity. The HREF
    neighborhood probabilities indicate that rainfall rates have a
    20-40% chance of exceeding 1"/hr in the deeper convection, with
    some storm organization through 40-50 kts of bulk shear helping to
    enhance and lengthen the duration of these rain rates in some
    areas. Although 0-6km mean winds will remain around 30 kts,
    suggesting progressive cell motions, aligned Corfidi vectors
    indicate a strong likelihood for repeating cells which could
    produce 1-3" of rainfall in some areas.

    7-day rainfall for portions of northeast NM into the Panhandles of
    TX and OK has been as much as 400% of normal, leading to locally
    saturated 0-40cm soil moisture above the 95th percentile. While
    the progressive nature of these heavy rain rates should somewhat
    limit the flash flood potential this afternoon, any training or
    repeated rounds could cause impacts, especially atop the most
    saturated soils or across urban areas, sensitive terrain features,
    and burn scars.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5HkMDdsS2VTEbUgjFSqJPkVJAUTuD8un0vtvI72lMBBT0bDHOEtUlvwXSqyzoKryFZNR= XxBMTu1dJgswVlcXXG1QI3M$ for graphic product...

    ATTN...WFO...ABQ...AMA...DDC...LUB...MAF...PUB...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 37220299 37090182 36810118 36080098 35610122=20
    34730197 33830305 33340409 33480503 34320544=20
    35280538 35370537 36400491 36940409=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 21 22:57:33 2024
    AWUS01 KWNH 212257
    FFGMPD
    COZ000-NMZ000-220400-

    Mesoscale Precipitation Discussion 1038
    NWS Weather Prediction Center College Park MD
    656 PM EDT Sat Sep 21 2024

    Areas affected...southern CO into northern NM

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 212253Z - 220400Z

    Summary...Localized flash flooding will be possible across
    portions of northern NM into southern CO through 04Z due to the
    potential for multiple rounds of thunderstorms with brief
    training. Rainfall rates of 0.5 to 1 inch in 30-60 minutes will be
    possible along with localized totals of 1-2 inches.

    Discussion...GOES East water vapor imagery showed a closed low
    over northeastern AZ at 2230Z, tracking toward the ENE. Several
    rounds of showers and thunderstorms have developed out ahead of
    the closed low within a diffluent and divergent flow pattern
    aloft. SPC mesoanalysis data from 22Z showed MLCAPE ranged between
    500-1000 J/kg across northern NM but was less than 500 J/kg over
    southern CO. At the surface, an easterly/upslope component to the
    flow was present to the north of a cold front and outflow boundary
    where anomalous precipitable water values remained but were
    beginning to be pushed east ahead of the closed low.

    While instability values are likely near their max given the time
    of day, multiple rounds of thunderstorms will remain possible from
    northeastern NM into southern CO as the closed low continues east,
    each round carrying the potential for short term training with
    possible rainfall rates as high as 0.5 to 1 inch in 30-60 minutes.
    The multiple rounds could contribute to an additional 1-2 inches
    of rain by 04Z, though these higher totals are likely to remain
    highly localized. These storms will pose a localized flash flood
    threat to the region, mainly in/near the Sangre De Cristo
    Mountains and westward into adjacent terrain of north-central NM
    and mainly across sensitive burn scar locations.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-gAXF5fLBb9W6u_wUBwsLCkN6rVzUtX12lETvp8OelxZ2uaMZJ4CNuCzgzjF4RATMt0e= OF4_keESzFsHO3WG5kzWMkE$ for graphic product...

    ATTN...WFO...ABQ...GJT...PUB...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 38590488 38460454 37300452 36820409 36310360=20
    35520376 35140487 35120532 35290573 35540591=20
    35790606 35900638 36050671 36320683 36600683=20
    36950663 37170628 37410576 37650552 37840541=20
    38120542 38500520=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 21 23:59:33 2024
    AWUS01 KWNH 212359
    FFGMPD
    TXZ000-OKZ000-NMZ000-220555-

    Mesoscale Precipitation Discussion 1039
    NWS Weather Prediction Center College Park MD
    758 PM EDT Sat Sep 21 2024

    Areas affected...TX Panhandle into adjacent eastern NM/western OK

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 212357Z - 220555Z

    SUMMARY... Repeating and training of cells are expected to pose a
    threat for flash flooding from the TX Panhandle into adjacent
    eastern NM/western OK through 06Z. Rainfall rates of 1-2 in/hr and
    totals of 2-4 inches are expected.

    DISCUSSION...2330Z radar imagery showed a small cluster of
    thunderstorms advancing through the western TX Panhandle, with
    more widely scattered coverage extending westward into eastern NM.
    These cells were forming out ahead of a potent mid-level trough
    over the Four Corners region, which was advancing toward the ENE,
    with favorable shear for organized cells in place over the High
    Plains. While most cells were moving toward the NE at 25-35 kt,
    some deviant rightward motion of organized cells has been observed
    and instances of training have supported MRMS-derived rainfall
    rates of about 1-2 in/hr. Surface observations showed an effective
    cold front (outflow boundary enhancement) extended southwestward
    through northwestern OK into the TX Panhandle, and then
    west-northwestward into NM. A pool of 1000 to 2000+ J/kg MLCAPE
    was estimated via the 23Z SPC mesoanalysis from just south of AMA
    into eastern NM along with anomalous precipitable water values
    that ranged from 1.3 to 1.7 inches.

    A strengthening low level jet is forecast with 25 to 35+ kt
    through 06Z at 850 mb, which will act to overrun the southward
    sinking effective cold front. Moisture pooling and elevated
    instability of up to 1500 J/kg is forecast by the RAP to focus
    over the TX Panhandle north of the boundary, with weaker values of
    up to 500 into western OK. After the initial round of
    thunderstorms advances east from the western TX Panhandle,
    subsequent rounds are anticipated as the low level jet ramps up
    overnight, leading to instances of repeating and training due to
    the similar boundary orientation and anticipated storm motions.
    Rainfall rates should generally fall in the 1-2 in/hr range and
    total rainfall of 2-4 inches through 06Z may lead to some areas of
    flash flooding, though dry antecedent conditions may limit flash
    flooding to urban areas or otherwise flashy locations across the
    region.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6NGCwGcGTbj2wvEqWSZJpXOoLKxLgDO4P_yTFrGAwbOdOowl_mW55bGtHCsHmZOqWnFv= k6aBut3MHp198D0QWxYZ5n8$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...OUN...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36240090 36210007 35829981 35149991 34370074=20
    33860247 33950309 34330322 34830311 35300282=20
    35870192=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 22 01:55:33 2024
    AWUS01 KWNH 220155
    FFGMPD
    ILZ000-MOZ000-IAZ000-KSZ000-NEZ000-220700-

    Mesoscale Precipitation Discussion 1040
    NWS Weather Prediction Center College Park MD
    954 PM EDT Sat Sep 21 2024

    Areas affected...Mid-MO Valley into southern IA/northern MO

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 220153Z - 220700Z

    SUMMARY...Brief training of 1 to 3 in/hr rainfall rates may
    support localized flash flooding across portions of the MO River
    Valley into southern IA/northern MO through 07Z.

    DISCUSSION...0145Z radar imagery showed an expanding line segment
    of strong to severe convection extending from southeastern NE into
    far northwestern MO and southwestern IA. Additional convection was
    noted to be racing eastward across eastern KS. These storms were
    located just ahead of a wavy cold front and ahead of a low to
    mid-level vorticity max in northeastern KS, observed on KTWX radar
    imagery, advancing toward the northeast. A small ribbon of
    instability was in place ahead of the cold front with 1000 to
    2000+ J/kg MLCAPE and PWATs between 1.8 and 2.0 inches via the 01Z
    SPC mesoanalysis.

    Through 08Z, the cold front and instability are forecast to
    continue advancing south and east while forcing ahead of the
    northeastern KS vorticity max aids in lift with additional
    thunderstorms likely to fill in across the MO/IA border. There
    will be an overall progressive movement to individual cells and
    instability should trend downward with time, but
    repeating/training will also occur at times allowing for 1 to 2,
    perhaps as high as 3 in/hr rainfall rates to occur. These high
    rates could lead to short term rainfall totals of 3-4 inches in an
    isolated location or two. While dry antecedent conditions will
    likely limit the coverage of flash flooding, one cannot rule out
    urban or otherwise sensitive terrain being impacted by rapid rises
    of water.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!93FWATqQzFdWT9c8YIwZ994SCFEOmZI1RvdayzzEiJ-JIq9vE1CK5hz72nA-1xMR_MHr= IzeMbvkk34SZTtBLTOV4aEQ$ for graphic product...

    ATTN...WFO...DMX...DVN...EAX...LSX...OAX...TOP...

    ATTN...RFC...MBRFC...NCRFC...NWC...

    LAT...LON 41909358 41729253 41389184 40989149 40369132=20
    40119156 40029204 39969270 39849386 39709523=20
    39889618 40659533 41539467=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 22 03:19:34 2024
    AWUS01 KWNH 220319
    FFGMPD
    PAZ000-DEZ000-MDZ000-220718-

    Mesoscale Precipitation Discussion 1041
    NWS Weather Prediction Center College Park MD
    1119 PM EDT Sat Sep 21 2024

    Areas affected...central/eastern Pennsylvania, north/northeastern
    Maryland, northern Delaware

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 220318Z - 220718Z

    Summary...A cluster of deep convection over central Pennsylvania
    was producing spots of rainfall rates approaching 2 inches/hr.=20
    Isolated flash flood potential will exist with this activity as
    storms migrate toward the southeastern Pennsylvania/northeastern
    Maryland border region through 06-07Z.

    Discussion...A vigorous shortwave trough over Pennsylvania has
    helped to force a relatively fast-moving convective complex that
    currently extends from near Williamsport to State College. Ahead
    of this complex, cells have developed within a warm/moist axis
    characterized by ~1000 J/kg MLCAPE and 1-1.5 inch PW values -
    highest near Chesapeake Bay. The cells ahead of the linear
    complex were moving considerably slower (around 5-10 mph),
    allowing for several cell mergers and prolonged rainfall, with
    rates approaching 1.5-2 inches/hr at times generally from
    Williamsport to Harrisburg.

    Both models/observations and objective analyses indicate potential
    for the southward-moving convective complex to continue for a few
    hours, potentially reaching the MD/PA border region through 0530Z
    and the I-95 corridor thereafter. The combination of cells and
    linear convective structures suggests potential for at least an
    isolated flash flood risk to persist with this activity during
    that timeframe - especially near cell mergers and slower-moving
    storms. FFG thresholds in much of the region are in the 2.5
    inch/hr range, suggesting that the best risk of excessive runoff
    should remain 1) isolated and 2) tied to low/sensitive spots and
    urbanized land surfaces.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Xo6ruPuoxEk81-UYHxO7tn3Yi-GDj-WGsNLgtLkQi0v8_f_7qEfprDMsBsINvLctM_A= IoYZsPUsH7yZaKHseLQu9Lg$ for graphic product...

    ATTN...WFO...CTP...LWX...PHI...

    ATTN...RFC...MARFC...NWC...

    LAT...LON 41157682 40537581 39897560 39197581 38917653=20
    39237727 40497798=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 22 17:02:14 2024
    AWUS01 KWNH 221702
    FFGMPD
    TXZ000-OKZ000-222200-

    Mesoscale Precipitation Discussion 1042
    NWS Weather Prediction Center College Park MD
    101 PM EDT Sun Sep 22 2024

    Areas affected...Southwest to Central East OK...Southeast TX
    Panhandle...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 221700Z - 222200Z

    SUMMARY...Slow moving, back-building cells with rates of 1"/hr may
    pose localized 1-1.5" totals and possible flash flooding
    conditions.

    DISCUSSION...GOES-W and Regional RADAR mosaic have started to
    depict increasing convective activity in both coverage and
    vertical depth with peak heating of the day. The highly
    anomalous, over 3.5 standard anomaly units from climatology, core
    of the closed low is bottoming out across SW California with
    vorticity center at the southern base; this is allowing for an elongation/stretching of the mid-level deformation zone to extend
    across SW to NE San Bernadino county with increased deep layer
    convergence. Given steepening lapse rates with cold air advection
    aloft, surface heating into the 80s is starting to support surface
    based CAPE values from 500-1000 J/kg to develop over the Southern
    California Deserts toward the Colorado River Valley near S Nevada.
    While deep layer moisture is a bit limited with only Tds in the
    upper 40s, low 50s and total PWat values in the .75 to 1" range.=20
    The convergence within the band and orographic ascent confluent
    across the San Bernadino/Little Bernadino/San Jacinto Ranges
    supports stronger vertical development and sufficient moisture
    flux to support .5-1"/hr rates.=20

    Limited cell motions given proximity to the closed low/deformation
    zone will allow for very slow/stationary motion with upstream redevelopment/backbuilding along the deformation band across NE
    CA. Propagation may also allow cells along the mountain ridges
    into the Cochella Valley with time. This may allow for spotty
    .75-1" totals with an isolated 1.5" total remains possible. Given
    naturally low FFG values less than these hourly rates and
    potential; an isolated flash flooding incident or two is
    considered possible across the area through the late
    afternoon/evening hours.=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7Raf4jFpWLwzZnXM89GEBYYsNLqlif8rCj3u1a-UXyChH7ZjaLJXKLZBzBqkBK8BeHzR= 62Ek7z1HNOtP0vFSlRmWc1g$ for graphic product...

    ATTN...WFO...AMA...LUB...OUN...TSA...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36109607 36069525 35799487 35339499 34969571=20
    34729672 34459805 34099985 33890132 34520180=20
    35150101 35629991 35919906 36089804 36069700=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 22 17:35:17 2024
    AWUS01 KWNH 221735
    FFGMPD
    TXZ000-OKZ000-222200-

    Mesoscale Precipitation Discussion 1042...Corrected
    NWS Weather Prediction Center College Park MD
    134 PM EDT Sun Sep 22 2024

    Corrected for Resend of Text

    Areas affected...Southwest to Central East OK...Southeast TX
    Panhandle...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 221700Z - 222200Z

    SUMMARY...Potential for elevated training cells with rates slowly
    increasing as cells approach surface front and deep moisture flux
    inflow. Isolated rates up to 2"/hr and totals of 2-3" may result
    in localized flash flooding particularly near urban or hard/baked
    ground conditions.

    DISCUSSION...16z surface analysis depicts a stationary front from
    TQH at the the southward sagging cold front across the MOKSAROK
    across to SRE to OUN to FSI and a low near FDR before becoming a
    bit less defined across NW Texas into deeper low level status.=20=20
    This stratus is banked in west of the surface low, but also within
    the best isentropic ascent from return Gulf moisture along the low
    level jet. Upper-level jet is sliding east and as such, the
    mid-levels quickly veering across 850-700mb resulting in
    convergent flow aloft of the Eastern Cap Rock into SW OK. Modest
    500-1000 J/kg of MUCAPE and the FGEN forcing has been breaking out
    convection for the last few hours with increasing coverage across
    TX. Total moisture values through this eastward angling moisture
    plume are fairly solid at at 1.5-2 standard anomaly units above
    average between 1.5-1.75", but slowly climbing with the addition
    of the return Gulf moisture and increasing confluence into the
    mid-levels. As such, rainfall rates are slowly increasing from
    1-1.5"/hr into an increasingly favorable steering flow allowing
    for training elements over the next few hours.=20=20

    Recent drought conditions resulting in very high FFG values are
    likely still too high for these rates (with exception of central
    Cap Rock where values are more approachable); however, as the
    cells move eastward, the proximity to the surface front reduces
    and bases are lowering and trying to root more toward the surface.
    This is allowing for increased moisture flux into the updrafts
    with Tds in the upper 60s. As a result, rainfall rates are
    starting to increase to around 2"/hr with some occasional as well
    a approaching increased urbanization. While 1hr FFG values are
    still above 2.5"; the prolonged drought may have further hardened
    the upper ground surface making infiltration even more difficult
    and so may be over-estimating FFG. While, not likely to be large
    scale or significant in magnitude, isolated flash flooding is
    considered possible over the early afternoon hours across the repeating/training corridor particularly near urban centers.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9KdGmtOuz_OUcNklFbAeRysQRnJruYvZldQnH5pIp_Va_0wwL938X9qDU9K_60ot16TT= KcomUwZnyz2iHxDU5lHJp8E$ for graphic product...

    ATTN...WFO...AMA...LUB...OUN...TSA...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36109607 36069525 35799487 35339499 34969571=20
    34729672 34459805 34099985 33890132 34520180=20
    35150101 35629991 35919906 36089804 36069700=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 22 21:09:51 2024
    AWUS01 KWNH 222109
    FFGMPD
    TXZ000-230215-

    Mesoscale Precipitation Discussion 1043
    NWS Weather Prediction Center College Park MD
    509 PM EDT Sun Sep 22 2024

    Areas affected...Big Bend into northwestern TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 222107Z - 230215Z

    Summary...Increasing flash flood potential will setup across
    portions of Big Bend into the Permian Basin and northwestern TX
    through 02Z. Rainfall rates of 1-2 in/hr, but locally in excess of
    2 in/hr, are expected to lead to a couple of 3-4" totals.

    Discussion...Surface observations from 21Z and visible satellite
    imagery helped place a cold front across western TX, with an
    attached surface low just south of a MAF to BPG line. Convective
    development was increasing along the portion of the front
    extending northeast of the surface low, while development near the
    weaker cold frontal segment to the southwest of the low was
    isolated. 20Z SPC mesoanalysis data showed plenty of instability
    in place south of the front with 1000 to near 3000 J/kg MLCAPE
    (highest near Rio Grande) along with 1.4 to 1.8 inches of
    precipitable water.

    Lift across the region was occurring ahead of an advancing
    positively tilted upper trough axis extending from the central
    High Plains into the Desert Southwest and the right entrance
    region of an associated 70-90 kt jet max near 250 mb. Short term
    model forecasts show the front continuing to advance gradually off
    toward the southeast over the next 3-6 hours into weak
    southeasterly low level winds. Surface convergence and forcing
    aloft, coupled with the available instability, should be enough to
    support increasing convective coverage throughout the remainder of
    the afternoon and through the evening, especially between I-10 and
    I-20 where mean steering flow will be roughly parallel to the
    front, allowing for repeating and merging of cells along with
    rainfall rates of 1-2 in/hr (locally in excess of 2 in/hr
    possible).

    Farther south, coverage of convection may remain more isolated,
    especially in the vicinity of Big Bend N.P. where forcing is
    weaker and some pockets of weak inhibition likely remain. However,
    speed shear profiles will support some organized, possibly slower
    moving, cells. The potential for merging cells will also exist
    farther south, but this is conditional on higher coverage
    occurring closer to Big Bend. Despite dry antecedent conditions
    over roughly the past 3 weeks, at least isolated flash flood
    potential will exist across northwestern TX into the Big Bend
    region where a couple of 3-4" totals may occur.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9K-bFj-sylLBsR7j0mHcwfwqYt-TxrY4hDEg3KDcOpAwlKjqaEpDV1S1gdB0L66Rw3qF= sj0PYfsq-x4Osm22-C8W9_Q$ for graphic product...

    ATTN...WFO...EWX...FWD...LUB...MAF...OUN...SJT...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 33729859 32849831 32029859 31079965 30550040=20
    29920157 29560234 29280254 29000277 28820309=20
    28780346 28930371 29060390 29380406 29620412=20
    29790420 30210429 30510423 30620403 30470357=20
    30580305 31150249 31880211 32710136 33320000=20
    33649925=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 23 21:04:40 2024
    AWUS01 KWNH 232104
    FFGMPD
    VAZ000-NCZ000-WVZ000-TNZ000-KYZ000-240215-

    Mesoscale Precipitation Discussion 1044
    NWS Weather Prediction Center College Park MD
    504 PM EDT Mon Sep 23 2024

    Areas affected...eastern KY/TN into the central/southern
    Appalachians

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 232103Z - 240215Z

    Summary...Isolated flash flooding will be possible across portions
    of eastern KY/TN into the central/southern Appalachians. Rainfall
    rates of 1-2 in/hr will be possible where brief training of cells
    occurs.

    Discussion...2045Z visible satellite and regional radar imagery
    showed scattered thunderstorms ongoing from portions of central
    KY/northern TN into the central/southern Appalachians. A recent
    increase in the coverage of storms appears to be driven by daytime
    heating and increased ascent ahead of an elongated vorticity
    maximum observed on water vapor imagery from western TN into
    northern MS. SPC mesoanalysis data from 20Z showed 1000-2000 J/kg
    MLCAPE and weakly anomalous precipitable water values of 1.5 to
    1.9 inches across the region. The ongoing cells were moving with
    the deeper layer mean wind of 15-25 kt in a general eastward
    fashion.

    There is some concern that as the vorticity max over TN/MS
    continues to advance toward the northeast, increased forcing ahead
    of this feature will act on instability already in place to
    support greater coverage of cells heading through the remainder of
    the evening, increasing the potential for areas of brief training
    that could support locally higher rainfall rates of 1-2 in/hr.
    While this threat is expected to remain low, areas of low FFG
    exist ever portions of eastern KY/TN into the Appalachians with 1
    to 2 inches in an hour.

    Outside of terrain, no significant boundaries were analyzed that
    are expected to have an impact on cell placement and the
    expectation moving forward is that cells will continue to remain
    somewhat disorganized and multicellular in nature, although
    increasing shear from the west may support some more organized
    cells. However, beyond ~02Z, the expectation is that diminishing
    instability with the loss of daytime heating will contribute to a
    reduction in storm coverage and a lowering of the flash flood
    threat.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7xwZHjpOHFc8VP5Yl0hUJw2muici3tJZiNP8J4-9UyVi6AgGbQ_cNsgG5-SHlxkyU7lX= vjSUgTQ-gi3TDz2CxvFgOxo$ for graphic product...

    ATTN...WFO...GSP...JKL...LMK...MRX...RLX...RNK...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 37758313 37678264 37428100 37278083 36548088=20
    36148161 35238255 35358389 35848446 36568457=20
    37018485 37318493 37658490 37738455 37748401=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 23 23:14:43 2024
    AWUS01 KWNH 232314
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-240510-

    Mesoscale Precipitation Discussion 1045
    NWS Weather Prediction Center College Park MD
    714 PM EDT Mon Sep 23 2024

    Areas affected...southeastern MO/northeastern AR into Mid-MS
    Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 232312Z - 240510Z

    SUMMARY... The potential for SW to NE training of heavy rain will
    increase overnight from the eastern AR/MO border region into the
    and across the MS River. Rainfall rates of 1-2 in/hr are expected
    with totals of 2 to 4 possible on a localized basis.

    DISCUSSION...Fading visible satellite imagery at 23Z and regional
    radar imagery showed a recent increase in the intensity of
    thunderstorms over northern AR into MO, especially with a small
    line segment located between STL and UNO. Additionally, a
    northeastward tracking mesolow was observed in northern AR,
    co-located with a small area of showers to its north. The regional
    uptick in convection was occurring ahead of an upper level
    vorticity max over western MO seen on water vapor imagery,
    tracking ENE. At the surface, a low was located about 75 miles
    southwest of STL with a stationary front extending eastward into
    southern KY and cold front extending southward from the low into
    west-central AR. Earlier clearing on visible imagery ahead of the
    cold front from northeastern AR into southeastern MO had allowed
    for greater coverage of 500-1500 J/kg MLCAPE located in the warm
    sector over southeastern MO via SPC mesoanalysis data. Moisture
    via area GPS observations and mesoanalysis data revealed values of
    1.5 to 1.8 inches throughout the Mid-MS Valley.

    As the upstream vorticity max/trough axis continue to move east
    overnight, thunderstorm coverage is expected to expand across
    southeastern MO/northeastern AR into southern IL, especially for
    locations near/north of the stationary front. Some modest increase
    in 850 mb flow is expected beyond 00Z ahead of the trough with
    greater coverage of 20-25 kt southwesterlies forecast through 04Z
    by the latest RAP which should lead to greater isentropic ascent
    from the MO/IL border into southern IL and western portions of KY.
    Due to unidirectional southwesterly flow ahead of the cold front,
    instances of southwest to northeast training will be favored as
    the general precipitation axis advances toward the east, ahead of
    the upstream upper vort/trough axis. Rainfall rates of 1-2 in/hr
    and localized maxima of 2 to 4 inches will be possible

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5_6Emwuq6zhHW2iJFCI5PUcMQIN5Ahy_RM0Yxe-KA6KEFeOwR83_2faIU-LwAaPQ8-kD= VCb6uhEFlOVr3vBHJbBDhFs$ for graphic product...

    ATTN...WFO...ILX...LSX...LZK...MEG...PAH...SGF...

    ATTN...RFC...LMRFC...MBRFC...NCRFC...OHRFC...NWC...

    LAT...LON 39338855 38468784 36748875 36378912 35798979=20
    35479042 35419117 35679184 36149221 37119221=20
    38239099 38998989=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 24 03:26:16 2024
    AWUS01 KWNH 240326
    FFGMPD
    KYZ000-INZ000-ILZ000-MOZ000-240924-

    Mesoscale Precipitation Discussion 1046
    NWS Weather Prediction Center College Park MD
    1125 PM EDT Mon Sep 23 2024

    Areas affected...southern Illinois, southern Indiana, northern
    Kentucky

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 240324Z - 240924Z

    Summary...A cluster of thunderstorms was intensifying over
    southwestern Illinois and will move eastward across the discussion
    area over the next 6 hours. Isolated instances of flash flooding
    are possible with this activity.

    Discussion...Recent radar/satellite imagery depicts expanding
    convective coverage along an axis extending from near Mount
    Vernon, IL southwestward through Cape Girardeau, MO. These storms
    were loosely organized, with a number of cell mergers across
    south-central Illinois and a limited amount of training closer to
    Cape Girardeau. The storms were being forced by 1) a strong
    mid-level wave just east of St. Louis and 2) sufficient
    moisture/instability (~1000 J/kg MLCAPE and 1.7 inch PW values)
    for strong updrafts and efficient rainfall. Recent MRMS imagery
    depicts a gradual increase in coverage of 1-1.5 inch/hr rainfall
    rates that were beginning to approach one-hour FFG thresholds
    across southern Illinois.

    Models/objective guidance suggests that these trends will continue
    with eastward extent toward southern Indiana and northern Kentucky
    over the next 3-6 hours. Storms should reach southwestern Indiana
    and vicinity around 0530Z. The loosely organized nature of the
    storms (with occasional development but downstream and southwest
    of the majority of ongoing convection) should continue to allow
    for occasional cell mergers/training and spots of 1-2 inch/hr rain
    rates at times. These rates should fall on ground conditions
    characterized by 1.5-2.5 inch/hr FFG thresholds, and the spotty
    nature of the heavier rain rates suggest isolated flash flood
    potential especially in low spots and urbanized areas.=20

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7d4CwpoNKF4sSwzivgNOsflGcyeNSMtGWdfkhlUDVtLadz85CxGbafKDiS0J-KTDzgwx= sfXLj6xAmeVVf8P1EkM96RE$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...LMK...LSX...PAH...

    ATTN...RFC...LMRFC...NCRFC...OHRFC...NWC...

    LAT...LON 39438581 39148495 38508490 37678540 37188737=20
    37198911 37748959 38648932 39208835=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 24 17:38:45 2024
    AWUS01 KWNH 241738
    FFGMPD
    VAZ000-NCZ000-WVZ000-SCZ000-GAZ000-TNZ000-KYZ000-242300-

    Mesoscale Precipitation Discussion 1047
    NWS Weather Prediction Center College Park MD
    138 PM EDT Tue Sep 24 2024

    Areas affected...Southern to South-central Appalachians...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 241735Z - 242300Z

    SUMMARY...Scattered cells ahead of main convective lines may
    pre-soak rugged areas with spot of 1-2.5" resulting in scattered
    possible flash flooding.

    DISCUSSION...GOES-E visible imagery shows a fairly clear skies
    over the Appalachians across S WV/SW VA into E TN/W NC and far
    upstate SC. Temperatures have risen to upper 70s/low 80s with
    well above average low level moisture having filtered through the
    range with Tds in the mid to upper 60s. As such, the area has
    become fairly unstable with 1250-1750 J/kg of MLCAPE. Solid
    25-40kts of southwesterly 850-700mb flow has been advecting
    increasing moisture through the lowest levels to further moisten
    the lower column with total moisture reaching 1.5" even into the
    higher slopes with some suggestion of 1.7" starting to reach
    eastern TN through the Cumberland Plateau.

    While main northern stream trough remains well west over the
    Midwest digging into the Tri-Rivers area of W KY, a subtle
    southern stream wave can be seen sliding through E TN moving
    generally parallel to the slopes. This forcing combined with
    low-level convergence from approaching pre-frontal convective line
    out of KY, is starting to spark increasing TCu and incipient CBs
    across the clearer skies downstream. More mature cells along the
    pre-frontal trough as well as very near the shortwave lifting
    north will likely continue to enhance with cells capable of
    1.25-1.75"/hr rates. While cell motions will likely limit overall
    totals to about 30-60 minutes, it is the pre-cursory cells that
    given solid instability and updraft strength may be capable of a
    similar 1-2"/hr total prior to the main forcing lines that may
    result in spots of 1.5-2.5" totals over a 3 hour period as they
    repeat or at time merge with the cells in the effective warm
    sector ahead of the line.=20

    Hydrologically, the rugged area has naturally lower FFG values at
    1-1.5"/hr and 1-2"/3hr which suggest either slower moving
    pre-cursory cells or the stronger forced lines will have a solid
    potential of being exceeded. The scattered and transitory nature
    is likely to result in localized scattered incidents of flash
    flooding given 1.5-2.5" totals through 00z.=20=20=20=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5mft5fm8mf2N5imOwIwoq5Gk1GRjjKCLt02m9aPzM6Dg8tRMdIhlW0tN497hvPe5bHVu= yFmsBq5Z_jd0_DRdQbAikl8$ for graphic product...

    ATTN...WFO...GSP...JKL...LWX...MRX...RLX...RNK...

    ATTN...RFC...LMRFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 38798028 38517956 37897963 37337997 36208103=20
    35368190 34978242 34898304 35248336 35868325=20
    36378346 36968305 37638230 38528109=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 24 19:05:48 2024
    AWUS01 KWNH 241905
    FFGMPD
    VAZ000-WVZ000-OHZ000-TNZ000-KYZ000-INZ000-ALZ000-MSZ000-250104-

    Mesoscale Precipitation Discussion 1048
    NWS Weather Prediction Center College Park MD
    305 PM EDT Tue Sep 24 2024

    Areas affected...Middle Tennessee, Central/Eastern Kentucky, into
    southern Ohio

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 241904Z - 250104Z

    SUMMARY...Scattered thunderstorm clusters ahead of cold front may
    bring 1.5-2.5" resulting in isolated flash flooding into this
    evening.

    DISCUSSION...Regional NEXRAD and GOES-E IR imagery shows a few
    thunderstorm clusters have developed over middle TN and central KY
    which is ahead of a cold front. Recent rainfall estimates of
    1.5"/hr are seen south of Cincinnati and north of Nashville.
    Sufficient moisture of 1.6 to 1.7" PW and instability with MLCAPE
    1500-2000 J/kg are allowing this heavy development. SWly low level
    flow, which is parallel to the advancing cold front, is 25-30kt
    which will keep a repeating thunderstorm threat into the evening
    and slow eastward progression despite relatively quick storm
    motions in 45kt mean layer steering flow.

    There are more flash-flood susceptible areas in the outlook
    including south central KY where 2-3" fell overnight, urban areas
    such as the ones mentioned above, and over northern KY where 3hr
    FFG is around 1". This scattered activity will continue to produce
    1-2" in a couple hours with localized amounts of 3" possible into
    the evening. Should these higher totals fall on the more
    susceptible areas, flash flooding is possible. Overall the flash
    flooding is more of an isolated threat.
    =20=20=20=20

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7-7T1clRwaLuLTAgutQiZls3BhimUncxZuRrWD4Eul7s6j04z3xwrqHGfZ9f_liFCHYr= 2kJezEn-YshYLYYoDedV2t8$ for graphic product...

    ATTN...WFO...HUN...ILN...JKL...LMK...MEG...MRX...OHX...PAH...
    RLX...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 39678323 39028216 37978207 36338398 34478767=20
    34628872 35478823 36498724 37468652 38028600=20
    39098487=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 24 22:30:22 2024
    AWUS01 KWNH 242230
    FFGMPD
    VAZ000-NCZ000-WVZ000-SCZ000-250415-

    Mesoscale Precipitation Discussion 1049
    NWS Weather Prediction Center College Park MD
    629 PM EDT Tue Sep 24 2024

    Areas affected...Southwestern Virginia and West-Central North
    Carolina into Upstate South Carolina

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 242227Z - 250415Z

    SUMMARY...Increasing coverage of thunderstorms focusing over a
    stationary front near the NC/VA border brings the risk for quick 2
    to 4" rainfall and scattered flash flooding into this overnight.

    DISCUSSION...Thunderstorms, some of which are supercells, will
    continue to develop in a warm sector in southwest VA and western
    NC and further develop as they cross a stationary front/cold air
    damming wedge and into south-central VA and central NC. Recent
    rainfall estimates of 2.5"/hr are near Martinsburg, VA which is
    just beyond the stationary front. High moisture (PW 1.8 to 2.0")
    and instability (MLCAPE 1500 to 2500 J/kg) are allowing this heavy
    development in the warm sector which convergence and a sharp
    downward gradient over the front slowing activity that crosses it.
    SWly low level flow is 15 to 20 kt which will keep
    moisture/instability advection over the front and allow further
    development.

    Confidence has increased in the flash flood potential along the
    front with recent HRRRs/18Z NAMnest all featuring QPF of 2 to 4"=20
    before midnight along the west-central NC/VA border and into
    south-central VA. Stability well into the cold sector behind the
    front should continue to limit the progression of activity to a
    couple counties into south-central VA with ongoing activity
    expected west of the Blue Ridge to the Alleghenies of VA. Further
    development is likely down the eastern side of the Appalachians
    tonight, so the outlook area include western NC into Upstate SC
    given earlier heavy activity there today. Previous flooding in the Raleigh-Durham Triangle makes them vulnerable and the presence of
    the front through there should allow for further flooding
    concerns. All to say flash flooding is likely through this evening
    near the frontal zone and better characterized as possible farther
    south over western NC into SC.
    =20=20=20=20

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!58JoNc9J0GamLjSQ9HPixWWiI7gwoL3lfkh7uxN0BFzsdi5frmirA49hLkdj4eEPzpkv= ru_mMk4mSxJFr8W4jAkNMNI$ for graphic product...

    ATTN...WFO...AKQ...GSP...RAH...RNK...

    ATTN...RFC...LMRFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 37777959 37167911 36807809 36187811 35817869=20
    35247959 35448056 35428136 34988224 35398278=20
    35998190 36638133 37048113 37418058 37728013=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 24 23:13:52 2024
    AWUS01 KWNH 242313
    FFGMPD
    VAZ000-NCZ000-WVZ000-TNZ000-KYZ000-250500-

    Mesoscale Precipitation Discussion 1050
    NWS Weather Prediction Center College Park MD
    713 PM EDT Tue Sep 24 2024

    Areas affected...South-Central Appalachians

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 242311Z - 250500Z

    SUMMARY...Threat for further thunderstorm development overnight
    ahead of cold front may bring additional 2 to 3" resulting in
    isolated flash flooding overnight.

    DISCUSSION...Scattered supercells have developed east of the
    pre-frontal convection over east-central KY and middle TN in the
    broad warm sector west of the crest of the south-central
    Appalachians. Recent rainfall estimates from KJKL are up to
    1.5"/hr over far eastern KY. Sufficient moisture of 1.5 to 1.6" PW
    and instability with MLCAPE 1000 to 1500 J/kg will continue to
    allow redevelopment of activity this heavy. There are further
    threats for flash flooding as the main pre-frontal convection
    comes through later this evening along with topographical lift
    from the western slopes of the south-central Apps. Deviant motion
    has been noted from left-moving super cells, so cell mergers and
    local upwind propagation will continue to be where the greatest
    flash flood threat is into the overnight.

    This area has rather low FFG, generally 1 to 1.5"/hr and around
    2"/3hr. So overlap from ongoing activity and the next round
    further raises the potential for flash flooding. Recent HRRR runs
    have indicated generally 1 to 2" from both rounds, which helps
    point to an isolated flash flood threat overnight.
    =20=20=20=20

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!75eMTg0spooPsLUE1keXbR57wZa4sbuEhmAqL5dpbjCc5h6NXe_vGZILIcYyjPGOlC0A= hulzEaW9c_W3MoErGIBVbQs$ for graphic product...

    ATTN...WFO...GSP...JKL...MRX...RLX...RNK...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 38268090 37298082 36138197 35498348 36318409=20
    37188367 38208261=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 25 04:31:24 2024
    AWUS01 KWNH 250431
    FFGMPD
    VAZ000-NCZ000-SCZ000-251029-

    Mesoscale Precipitation Discussion 1051
    NWS Weather Prediction Center College Park MD
    1230 AM EDT Wed Sep 25 2024

    Areas affected...much of North Carolina, upstate South Carolina,
    and a small part of southern/southeastern Virginia

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 250429Z - 251029Z

    Summary...Continued rounds of thunderstorms are expected to
    repeat/train across the discussion area through 08-09Z/4-5am
    Eastern. Rain rates exceeding 2 inches/hour at times are expected
    to result in at least localized flash flood concerns.

    Discussion...Over the last 2-3 hours, thunderstorms have focused
    along an axis extending from far northwestern South Carolina (near
    Spartanburg) east-northeastward through Raleigh/Durham and on to
    Roanoke Rapids. These storms were oriented parallel to
    west-southwesterly steering flow aloft, allowing for spots of
    localized training along the aforementioned axis. Additionally,
    enhanced low-level flow (around 25 knots across the Piedmont) were
    aiding in persistent low-level convergence along the axis while
    also maintaining 1000-1500 J/kg MLCAPE and 1.5-2 inch PW values
    within the pre-convective environment. These factors are
    continuing to support areas of 1-2 inch/hr rain rates at times
    that were threatening local FFG thresholds across the region
    (generally in the 1.5-2 inch/hr range - lowest in western and
    central North Carolina). This regime is expected to persist, with
    at least isolated flash flood potential materializing across the
    discussion area. A few spots of 4 inch rainfall totals are
    possible through 10Z. Some concern exists that the Raleigh/Durham
    area could experience heavier rain rates and urbanized flash flood
    potential overnight. Additional concerns exist across areas that
    have received 1-3 inch rainfall totals over the past 6 hours,
    where wet soils are likely to contribute to a greater risk for
    excessive runoff (especially in south-central/southeastern
    Virginia and central North Carolina).

    Moisture/instability profiles support redevelopment north of the
    primary convective axis (across northwestern North
    Carolina/southwestern Virginia) as well. Thunderstorms are
    expected to be a bit less focused in these areas (with lower
    potential for training/repeating). Isolated instances of flash
    flooding are still possible in this regime, however, especially
    where 1.5 inch/hr rain rates can materialize over sensitive/low
    spots.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6QnbCKMXB2agTymKG-p9ro26LkVSQzd30BsDpzjNOZm1Sti2TuAqiYdZpbsfAwni5hl6= 2BY95B542irfj5fwy1xyN_4$ for graphic product...

    ATTN...WFO...AKQ...CAE...GSP...MHX...RAH...RNK...

    ATTN...RFC...LMRFC...MARFC...SERFC...NWC...

    LAT...LON 37467723 36997655 36377659 35677725 35247924=20
    34898198 35158287 35648240 36178142 36877979=20
    37317834=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 25 06:57:55 2024
    AWUS01 KWNH 250657
    FFGMPD
    VAZ000-NCZ000-WVZ000-TNZ000-KYZ000-251256-

    Mesoscale Precipitation Discussion 1052
    NWS Weather Prediction Center College Park MD
    257 AM EDT Wed Sep 25 2024

    Areas affected...eastern Kentucky, western Virginia, and
    northeastern Tennessee

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 250656Z - 251256Z

    Summary...Scattered showers and isolated thunderstorms continue to
    migrate northeastward across the southern/central Appalachians,
    where wet soils have left ground conditions vulnerable to
    excessive runoff. Isolated instances of flash flooding are
    possible through early morning (12Z/8am Eastern).

    Discussion...Ascent/difluence aloft associated with longwave
    troughing across the central U.S. continues to support persistent,
    but scattered thunderstorm activity across the discussion area.=20
    The convection continues to persist in a marginally unstable
    environment (~500 J/kg MLCAPE) although with sufficient moisture
    (1.5 inch PW) for heavier rainfall to materialize in a few of the
    cells. Modest low-level forcing/focus was allowing for convective
    bands to migrate northeastward amid appreciable steering flow
    (around 35 knots), with localized backbuilding/training and
    favorable orientation of the bands (to flow aloft) allowing for
    prolonged rainfall and spots of 1 inch/hr rain rates at times.=20
    FFG thresholds in the region were generally around an inch or
    less, and convection was occasionally exceeding those thresholds,
    suggesting isolated/sporadic flash flood potential in the short
    term.

    Models/observations suggest that the overall scenario supporting
    isolated flash flood potential should remain in place through the
    early morning hours (12Z or so). Scattered convection should
    continue to initially deepen across eastern Tennessee and migrate
    northeastward atop areas of wet soils and hilly terrain, with
    occasional and sporadic instances of flash flood guidance
    exceedance. Convective coverage and limited instability are
    mitigating factors for a larger-scale flash flood threat, though a
    few instances of flash flooding cannot be ruled out.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-uF8xM0IG71y07af3nQfOkcj8xQs7O_2wSe3nTHk46YTvQc1HUwseHxC6rDOJV4blgu9= UJitnDYvRC28jG316xvgKbk$ for graphic product...

    ATTN...WFO...GSP...JKL...MRX...RLX...RNK...

    ATTN...RFC...LMRFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 37738248 37278166 37368085 37448034 37078013=20
    36528032 36108159 35858306 35648356 35728397=20
    36218439 36928407 37558355=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 25 15:02:05 2024
    AWUS01 KWNH 251501
    FFGMPD
    VAZ000-NCZ000-GAZ000-TNZ000-KYZ000-ALZ000-252100-

    Mesoscale Precipitation Discussion 1053
    NWS Weather Prediction Center College Park MD
    1101 AM EDT Wed Sep 25 2024

    Areas affected...Southern Appalachians

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 251500Z - 252100Z

    SUMMARY...Flash flooding will be possible this afternoon as the
    Predecessor Rain Event (PRE) begins from northeast Alabama through
    the Southern Appalachians

    DISCUSSION...The well-advertised PRE has begin to take shape
    across portions of the Southeast this morning. Storms have
    developed in a cluster across eastern Alabama with another one
    over eastern Tennessee. FFGs in the area are high...generally
    around 2.5 inches in 1 hour for Alabama and Georgia, but they are
    much lower in eastern Tennessee around Knoxville.

    An upper level low across far western Tennessee is drawing
    increasing moisture northwestward across Georgia into this zone
    where the storms are forming. Upper level jet stream winds are
    expected to approach 100 kts, which will increase the upper level
    divergence over the storms in the right entrance region, thus
    further enhancing the lift.

    Through mid-afternoon, CAMs guidance suggests additional line
    segments of storms will develop generally aligned SSW to NNE
    across the area. Embedded cells within the lines, as now, will
    track NNE, roughly parallel to the lines. The result will be some
    areas seeing multiple rounds of training thunderstorms, each
    capable of producing rainfall rates to 2.5 inches per hour...with
    those heaviest rates more likely once the storms move more into
    Georgia later this afternoon. Further, since the storms will be
    moving roughly parallel to the lines, the lines' forward speed to
    the east will be slow, allowing for multiple cells repeating over
    the same areas. Even now with pockets of 2 inch per hour rates
    associated with the strongest storms, the training nature of the
    storms will result in multiple rounds over potentially flood-prone
    and urban areas. Thus, even where FFG values are higher, the
    repeating nature of the storms will locally lower values as
    repeated storms move overhead.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8fuzp5UF4MyLM5i4ice_SruJT_LUmPhvtYGUW8MjuAu0_gBz4F9ucTfRSImAXt0lc3gk= Rw4cLLKMvpdj6fkAj_k4YFo$ for graphic product...

    ATTN...WFO...BMX...FFC...GSP...HUN...JKL...MRX...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36768370 36298236 34918356 33728479 32768559=20
    33518664 34718567 35388522=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 25 17:01:34 2024
    AWUS01 KWNH 251701
    FFGMPD
    NCZ000-SCZ000-GAZ000-ALZ000-252100-

    Mesoscale Precipitation Discussion 1054
    NWS Weather Prediction Center College Park MD
    101 PM EDT Wed Sep 25 2024

    Areas affected...North Georgia

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 251700Z - 252100Z

    SUMMARY...Slow-moving and training thunderstorms associated with
    the developing predecessor rain event (PRE) are likely to cause an
    urban flash flooding threat as they approach Atlanta.

    DISCUSSION...A line of slow-moving and training thunderstorms has
    developed west of Atlanta this afternoon. The storms are making
    their way into the metro area. The storms have a history of
    producing rainfall rates up to 2.5 inches per hour across far
    northwestern Georgia.

    As the storms move into Atlanta within the next hour, potential
    for training as well as locally heavy rain with any stronger storm
    cores will likely cause flash flooding in the streams and creeks
    around the city that are most prone to flooding due to heavy rain.

    Beyond the initial round of heavy rain, backbuilding storms as
    well as new development south of town will likely result in a
    long-duration rain event where steady light to moderate rain may
    continue across the city through the afternoon.

    East of town the flash flooding threat through the afternoon will
    be significantly lower, as higher FFGs in the rural areas should
    mean much more rainfall will be needed before significant flash
    flooding occurs. However, given the increasing moisture out ahead
    of Helene, slow moving storms, and most importantly, training of
    the storms...even outside of town flash flooding will be possible
    through the afternoon.

    The much greater threat for flooding area-wide is expected to be
    later tonight as stronger easterly flow associated with the
    approach of Helene slows any eastward-moving storms significantly.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9mpvhlMUu9Aq2Zs1wxis2Q0CchZDvwR4RY3t5Gr396QjSW1VhmnT7NPnPbLBc8QIusML= 7SPiSIbuQaJ_DPWHBfdYcM0$ for graphic product...

    ATTN...WFO...BMX...FFC...GSP...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 35198318 34768295 34408294 33868312 33198372=20
    33098440 33098481 33028522 33848462 34728366=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 25 18:00:38 2024
    AWUS01 KWNH 251800
    FFGMPD
    GAZ000-ALZ000-252359-

    Mesoscale Precipitation Discussion 1055
    NWS Weather Prediction Center College Park MD
    200 PM EDT Wed Sep 25 2024

    Areas affected...Southern Alabama into Western Georgia

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 251759Z - 252359Z

    SUMMARY...Slow-moving bands of heavy thunderstorms in a plume of
    tropical moisture ahead of Helene will continue to produce areas
    of 2.5" hourly rainfall and the potential for 4" rest of the
    afternoon.

    DISCUSSION...Clusters of slow-moving heavy thunderstorm bands
    oriented SSW to NNE over southern/eastern AL will continue to
    converge and shift north over the next hour or so, then likely
    drift east into western Georgia rest of the afternoon. Hourly
    rainfall of 2.5"/hr has been estimated from both KMXX and KEOX
    over Butler Co AL. While 1hr FFG exceeds 3" there, lower FFG near
    2"/hr is in the Montgomery metro area as points east where an inch
    of rain fell overnight.

    This activity is on leading edge of the core of Helene-sourced
    moisture with PW of 2" just now entering southeast AL. A tongue of
    2.25" PW will shift up the AL/GA border by 00Z on 15 to 20kt
    southerly flow, further increasing the risk for extreme rainfall
    trough tonight.

    Guidance has generally underdone the coverage of activity though
    recent HRRRs are decent. Through 00Z, areas of 2-4" are likely.
    However, this area has been in drought, so FFG will only be
    exceeded in the most extreme rates and potentially in more
    sensitive urban areas like Montgomery, so flash flooding through
    the afternoon is considered possible.

    This event alone is the drought breaker for much of southeast AL,
    but unfortunately this area will continue to receive extreme
    rainfall at times now through the passage of Helene Thursday
    night. Further updates on this situation can be expected this
    evening and Helene in general at hurricanes dot gov.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4_E-pL511Oj2rc_woMysisJ7HgYCBVuJG5hJFlHVjDgcdZxF6aBRhbZ9eawPpWCoesqE= 6PidKCjNULmwP9J4_jcF71Q$ for graphic product...

    ATTN...WFO...BMX...FFC...MOB...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 33218473 33008406 32188449 31058522 31028696=20
    32408663 33038619=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 25 18:42:06 2024
    AWUS01 KWNH 251842
    FFGMPD
    VAZ000-NCZ000-WVZ000-OHZ000-TNZ000-KYZ000-260041-

    Mesoscale Precipitation Discussion 1056
    NWS Weather Prediction Center College Park MD
    241 PM EDT Wed Sep 25 2024

    Areas affected...Western Slopes of South-Central Appalachians

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 251841Z - 260041Z

    SUMMARY...Localized flash flooding into this evening as the
    Predecessor Rain Event (PRE) expands north west of the
    south-central Appalachian crest.

    DISCUSSION...Two north-south corridors of locally heavy rain have
    developed west of the crest of the Appalachians over eastern
    KY/southern OH and over far southeast VA into central WV.
    Localized rates of 1.25"/hr have been estimated recently south and
    east of KJKL. This heavy rain is currently moving out of an area
    in far southwest VA that received 3"+ over the past day.

    An upper level low centered over the western tip of Kentucky is
    drawing Gulf moisture on southwesterly low level flow around 10kt
    which is why activity has been on the west side of the Appalachian
    Crest thus far. Instability is somewhat limited with MLCAPE around
    500 J/kg. However broad scale lift east of the developing low will
    continue to overcome the lower instability.=20

    Through the rest of the afternoon expect embedded cells of heavier
    rain to continue lifting north with localized areas exceeding
    1"/hr rainfall with potential for 2-3" in some pockets through
    00Z. FFG is low in places, around 1"/3hrs where the heaviest rain
    fell in far southwest VA and generally 1.5"/3hr elsewhere. Given
    the lack of prolonged higher rates, flash flooding is considered
    possible with an isolated coverage.

    An intense moisture plume from Helene will shift up the southern
    Appalachians overnight which will shift the heavy rainfall focus
    to the eastern side of the southern Appalachian crest, so please
    stay tuned for further heavy rainfall updates.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8dGFpl2olqaoar73bLvnYKwMMCeOBWHRFcefpBU8_lLPWZ6DJPd4_DWNlcNbm4tz5Yu1= TH_odiAFPPN8uu0VhTiNifA$ for graphic product...

    ATTN...WFO...GSP...ILN...JKL...MRX...RLX...RNK...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 39208194 38218211 37998167 38898050 38788002=20
    38148034 37398116 36268191 36458364 37808331=20
    39108265=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 25 20:15:10 2024
    AWUS01 KWNH 252015
    FFGMPD
    NCZ000-SCZ000-GAZ000-TNZ000-260200-

    Mesoscale Precipitation Discussion 1057
    NWS Weather Prediction Center College Park MD
    414 PM EDT Wed Sep 25 2024

    Areas affected...North Georgia and the Southern Appalachians

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 252013Z - 260200Z

    SUMMARY...Training thunderstorms will continue to lift over the
    Atlanta Metro area rest of this afternoon and over the eastern
    side of the southern Appalachians through tonight. Flash flooding
    is likely, particularly in Appalachian terrain, through this
    evening before becoming considerable to catastrophic overnight.

    DISCUSSION...Convergence of the tropical plume of moisture ahead
    of Helene and a cold front over southern Alabama has allowed a
    particularly heavy line of slow-moving and training thunderstorms
    to develop over southeast AL into western GA. This northward shift
    in moisture is driven by an upper low centered over far western
    KY. Recent rainfall estimates of 2 to 3" per hour are from KFFC
    and KMXX over eastern AL/western GA. The heaviest rain thus far
    has stayed south of the Atlanta metro and outflow is seen on KFFC
    which indicates the main threat for now to be avoiding that
    particular area.

    However, the tropical moisture plume with PW of 2 to 2.25" will
    shift up the AL/GA border rest of the afternoon, pushing moisture
    and instability back over the Atlanta metro and then up the
    eastern side of the southern Appalachians through this evening.
    Terrain enhanced rainfall there will quickly fill in a gap of
    rainfall over the past day that in western NC (surrounding
    Asheville). Rates of 2"/hr is likely by this evening which would
    exceed the FFG of 1.5-2"/hr. Flash flooding is likely through 02Z.
    The 18Z HRRR depiction of 2-4" in terrain over western NC and
    northeast GA is reasonable, but around 1" additional seems low for north-central GA and the Atlanta metro with a few additional
    inches possible.

    The much greater threat for flooding area-wide is expected to be
    later tonight as even stronger southeasterly flow associated with
    the approach of Helene pushes ever greater moisture into the same
    eastern slopes of the southern Appalachians with potentially
    catastrophic flash flooding overnight.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9G545def8ARs157X46OEZ-10V0iw4FQu_LPb0uvj5WgbYbegSDjzE2wychwhfZbHECPL= y9Z-3OHKQcLxwU6yRDCLhco$ for graphic product...

    ATTN...WFO...FFC...GSP...MRX...RNK...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36478281 36268158 34908229 33878304 33158365=20
    33158508 33548517 34468443 35388418=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 25 22:47:13 2024
    AWUS01 KWNH 252247
    FFGMPD
    FLZ000-GAZ000-ALZ000-260445-

    Mesoscale Precipitation Discussion 1058
    NWS Weather Prediction Center College Park MD
    646 PM EDT Wed Sep 25 2024

    Areas affected...Florida Panhandle into Central Georgia

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 252245Z - 260445Z

    SUMMARY...Particularly heavy rain is expected in southwest Georgia
    into the Florida Panhandle this evening due to convergence of
    pre-frontal activity from the west and the outermost banding of
    Helene from the south. Flash flooding is likely despite dry
    preconditions due to extreme rainfall rates of 3" per hour.

    DISCUSSION...Heavy and locally excessive pre-frontal activity over
    southeast AL and west-central GA is shifting east on outflow while
    the outermost bands of Helene have been tracking north over the FL
    Peninsula. Convergence of these two areas is progged this evening
    over southwest Georgia into the FL Big Bend/eastern Panhandle.
    This outer band is on the leading edge of particularly high
    moisture, lining up with the 2.2" PW contour from recent RAP
    analysis with PW climbing to 2.4" farther down the Peninsula which
    is 2.5 sigma over normal. Sufficient instability is present with
    MLCAPE of 1000 to 1500 J/kg.

    Recent HRRR runs have been under realizing rainfall rates which
    are estimated from KTLH and KVAX over Thomas County, GA. However,
    the timing in recent HRRRs has been decent with the main
    convergence over southwest GA occurring between 00Z and 02Z. There
    is a risk for 2 to 5" rainfall through the rest of the evening
    which is only a little above the high 3hr FFG of 4 to 5" due to a
    lack of rain in this part of GA yet. However, these extreme rates
    from slow moving and merging cells warrants likely wording for
    this discussion.

    A trough extending southwest from western GA extends over the FL
    Panhandle and should provide a focus for some additional heavy
    rain, so the discussion area is extended west about halfway
    through the Panhandle. As of now the area west of Apalachee Bay
    which received heavy rain earlier today appears to be south of the
    main heavy rain risk area, but given this coast is in the main
    Helene moisture plume there is at least a localized excessive
    rainfall risk there.

    Further banding from Helene approaches this area overnight, so
    expect further MPDs tonight and through the passage of Helene
    Thursday night.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7gQy-L5rRb2YDCuFlBs4dXTBE357slN-AZ2GzHbhs4ufqAFgFZIzioZAvrmI1xNjA8Vy= _3ooxOdSwPTpoIKVBXAXnTY$ for graphic product...

    ATTN...WFO...BMX...FFC...JAX...MOB...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 33338324 32558294 30998309 30018392 29348506=20
    30198636 30938639 31758554 32598502 33278448=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 26 00:11:39 2024
    AWUS01 KWNH 260011
    FFGMPD
    VAZ000-NCZ000-WVZ000-TNZ000-260600-

    Mesoscale Precipitation Discussion 1059
    NWS Weather Prediction Center College Park MD
    810 PM EDT Wed Sep 25 2024

    Areas affected...Southern Virginia into West Virginia

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 260009Z - 260600Z

    SUMMARY...Localized flash flooding into the overnight as moisture
    ahead of Helene streams over a stationary front and into the
    eastern slopes of the Appalachians.

    DISCUSSION...The northern end of the moisture plume in advance of
    Helene is lifting across NC and will cross a persistent front over southern/southwestern VA rest of the evening. Scattered
    thunderstorms have broken out along this frontal zone and to the
    west there remains terrain enhanced rainfall along the eastern
    slopes of the Appalachians. There were two main areas of heavy
    rain in this region over the past day, farther east over the NC/VA
    border last night, and earlier today west of the stationary front.
    The main focus for heavy rain into the overnight is generally
    progged to be between these two areas, but this is where the Blue
    Ridge is, so a bit of a broader swath as been drawn for possible
    flash flooding.

    Instability is sufficient with MLCAPE of 1000 to 2000 J/kg and
    moisture influx has been noted with low level southerly flow will
    increase from 15 to 30 kt through midnight which will reinforce PW
    around 1.7". Deep layer mean flow is around 30kt which should keep
    activity east of the Blue Ridge progressive, but localized
    rainfall over 1"/hr may cause some flooding issues. Terrain
    enhanced rates of 1"/hr will also cause concern...flash flooding
    is considered possible into the overnight.=20

    Further activity in the southern Mid-Atlantic is likely into
    Thursday, so please be on the look out for updated heavy rainfall
    info.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!56Cb5WgNNgRrZQDnZzC0kwz7gCJUpY4QCWynC2pdhntabD3FeXxXi4cnQGuGebI-IJKF= kBCxNkSZVKrwnVQ0tS7Xl8E$ for graphic product...

    ATTN...WFO...AKQ...LWX...MRX...RAH...RLX...RNK...

    ATTN...RFC...LMRFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 38287993 37917941 37677879 37207740 36577758=20
    36257848 36118091 36658225 37368181 37738106=20
    38278046=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 26 02:49:48 2024
    AWUS01 KWNH 260249
    FFGMPD
    VAZ000-NCZ000-SCZ000-GAZ000-TNZ000-260600-

    Mesoscale Precipitation Discussion 1060
    NWS Weather Prediction Center College Park MD
    1049 PM EDT Wed Sep 25 2024

    Areas affected...Piedmont of GA and SC into the southern
    Appalachains

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 260248Z - 260600Z

    SUMMARY...Areas of training are expected to continue over the next
    few hours from the Piedmont of GA and SC into the southern
    Appalachians. Peak rainfall rates in excess of 2 in/hr are
    expected with potential for considerable impacts.

    DISCUSSION...Regional radar imagery over the Southeast showed an
    advancing area of heavy rain moving north through south-central GA
    along with a persistent axis of training heavy rain across the
    southeast facing slopes of the southern Appalachians/Blue Ridge
    Mountains. An axis of south to north training has been observed
    from just south of I-40 near Lake Lure in western NC northward
    toward the VA/NC border near Damascus. Observed peak rainfall
    rates have occasionally reached between 2-3 in/hr with rainfall
    totals for the day of 4 to 6 inches in the vicinity of I-40
    between Asheville and Marion.

    Low level southeasterly winds of 20-30 kt in the 925-850 mb layer
    are expected to maintain a plume of robust moisture transport into
    the terrain over the next few hours, with 500-1000 J/kg MLCAPE
    located just upstream across the Piedmont and adjacent foothills
    of the mountains. An axis of low level convergence and areas of
    training are expected to continue across western NC, and though
    some lower rainfall rates are likely at times, the persistent
    nature of training will continue a likely threat of flash flooding
    with locally significant/considerable flash flood impacts
    possible. Farther south into GA, the northward advancement of
    heavier rain will be moving into portions of the state which
    picked up 2 to 3 inches of rain since Wednesday afternoon with an
    additional inch or two possible by 06Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9uRkReJ5am0F6lbjtuStoZddiEjBCfZhdS_JySntPthWdIf3NEWU_zgWgKKSDX_vt3n9= RL_sllcvfYezbrWt4Jh7v3s$ for graphic product...

    ATTN...WFO...FFC...GSP...MRX...RNK...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36658178 36408143 36068111 35308187 34808214=20
    34318256 33568286 33438358 33588397 33778433=20
    34318452 34918431 35448364 36028295 36358267=20
    36608234=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 26 05:52:45 2024
    AWUS01 KWNH 260552
    FFGMPD
    VAZ000-WVZ000-261030-

    Mesoscale Precipitation Discussion 1061
    NWS Weather Prediction Center College Park MD
    152 AM EDT Thu Sep 26 2024

    Areas affected...eastern WV into central VA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 260548Z - 261030Z

    SUMMARY...A few areas of training will maintain a flash flood over
    the next 3-4 hours, but decreasing instability is expected to
    diminish the threat by 10Z. Peak rainfall rates of 1 to 1.5 in/hr
    are expected.

    DISCUSSION...Scattered showers and thunderstorms remained as of
    0530Z across central/western VA into eastern WV. MRMS-derived
    rainfall rates over the past 2 hours have been peaking in the 1 to
    1.5 in/hr range, mainly near areas of mesoscale rotation. Cells
    were being driven along the leading edge of moisture
    transport/warm air advection along an anomalous moisture plume
    extending well northward of Hurricane Helene located in the
    southern Gulf of Mexico. Low level upslope flow was also a factor
    with 20-30 kt of 925-850 mb oriented from the SSE, focused into
    the Blue Ridge and Appalachians Mountains, located beneath
    diffluent flow aloft to the east of an upper low positioned over
    the Lower OH Valley.

    A few factors are expected to influence flash flood potential over
    the next few hours. While a few pockets of south to north training
    and repeating are ongoing from eastern WV into western and central
    VA, instability has been...and will continue to fall...through the
    remainder of the night. A low level anticyclone off of the central
    Mid-Atlantic coast is forecast to shift eastward which should
    allow for veering of the low level flow in VA, with winds becoming
    oriented more parallel to the axis of terrain. While precipitable
    water values will remain high (1.5 to 2.5 standard deviations
    above the mean) and highly localized instances of higher rain
    rates may remain by 10Z, the overall threat is expected to
    diminish later this morning.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_2MzV1xwHkH74tyNhg-PRtf5AHCekb-1piLPcB9LunPN8SIIowq52t5W8RXcl3h8N5FG= AGIUlQs6EECw3Ti_eoZE5Zc$ for graphic product...

    ATTN...WFO...LWX...PBZ...RLX...RNK...

    ATTN...RFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 39317873 38997788 38317828 37597878 37447924=20
    37437971 37478029 37738058 38018053 38398036=20
    38797995 39177930=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 26 08:07:19 2024
    AWUS01 KWNH 260807
    FFGMPD
    FLZ000-261405-

    Mesoscale Precipitation Discussion 1063
    NWS Weather Prediction Center College Park MD
    406 AM EDT Thu Sep 26 2024

    Areas affected...Apalachicola region of FL Panhandle

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 260805Z - 261405Z

    SUMMARY...As bands of heavy rain located north of Hurricane Helene
    approach the eastern FL Panhandle, renewed areas of flash flooding
    are expected toward 12Z. An additional 2-4 inches is expected
    through 14Z.

    DISCUSSION...Hurricane Helene was located about 375 miles SSW of
    Apalachicola, FL according to the 06Z position by NHC, moving
    north around 8 kt, though an increase in forward speed is expected
    late this morning. While this position is still well south of the
    FL Panhandle, 0745Z radar imagery showed axes and spiral bands of
    heavy rain located in the eastern Gulf of Mexico, grazing the
    western FL Peninsula and Gulf/Franklin counties of the Panhandle.
    GOES East water vapor and infrared satellite imagery showed
    healthy outflow in the northern semicircle of Helene's circulation
    and enhanced divergence aloft was present along the FL Panhandle
    due to the presence of a potent upper level jet max centered over
    the upper TN/OH Valleys.

    An increasing frequency of bands of heavy rain are expected to
    impact the FL Panhandle over the next 3-6 hours as Helene
    continues to advance north. While rain bands oriented generally
    west to east should push north without too much in the way of
    training concerns, rain bands that are aligned more with the mean
    steering flow from SSE to NNW will be favored for training. Even
    short term training could still allow for a quick 1-2 inches of
    rain in as little as 15-30 minutes due to the tropical environment
    in place. It is expected that steady rain will continue throughout
    the remainder of the morning, but with bursts of heavy rain
    occurring at times and with an increased frequency through 14Z
    along with an additional 2-4 inches.

    Given multi-sensor MRMS estimates of 5 to 10 inches of rain over
    the past 24 hours from near Apalachicola to Lake Talquin, soil
    saturation will more easily support runoff from additional heavy
    rain. Since instability of 500 to 1000+ J/kg is forecast to remain
    along and offshore of the coast, higher rainfall rates may be
    limited to coastal sections of the east-central Peninsula, but
    longer duration/lower intensity rainfall could still have flood
    impacts farther north.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-uwol5Mp4pDUbDRleBlBuMxXeJNIQI5JtTkfRh_K1Dxz8zgZPVJCvYHKNRwPdm0KYkO7= wfWPNkuiQ1hSdoFhn3ZNCz8$ for graphic product...

    ATTN...WFO...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 30508455 30298420 29738424 29508479 29468531=20
    29588552 29758563 30098552 30318536 30458492=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 26 06:52:48 2024
    AWUS01 KWNH 260652
    FFGMPD
    VAZ000-NCZ000-SCZ000-GAZ000-TNZ000-261045-

    Mesoscale Precipitation Discussion 1062
    NWS Weather Prediction Center College Park MD
    252 AM EDT Thu Sep 26 2024

    Areas affected...central/northern GA into the southern to central
    Appalachians

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 260651Z - 261045Z

    SUMMARY...Areas of heavy rain with south to north training to
    build northward through GA into the southern and central
    Appalachians through the morning. Rainfall rates of 1-2 in/hr will
    be likely, but isolated 2+ in/hr cannot be ruled out.

    DISCUSSION...Regional radar imagery across the Southeast at 0630Z
    showed a "Y" shaped appearance in reflectivity with a branch of
    heavier rainfall extending northeastward from the FL Panhandle
    into central GA, co-located with a remnant outflow/effective
    frontal boundary. A second axis of higher reflectivity extended
    northwestward across the GA coast into central GA and a broken
    axis of higher reflectivity values was located from central GA
    into western NC. These axes of higher reflectivity/heavier
    rainfall aligned fairly well with the leading edge of low level
    (0-3 km AGL) moisture flux where a plume of 2+ inch precipitable
    water values was building northward across GA via southeasterly
    low level winds of 20-30 kt. Mesoscale areas of rotation were
    embedded within the precipitation shield, associated with enhanced
    convergence and higher reflectivity along with with south to north
    training following the deeper layer steering flow.

    Short term RAP forecasts showed an axis of low level moisture flux
    convergence focusing from central GA into the southern
    Appalachians through 11Z along with gradually strengthening
    925-850 mb winds as Hurricane Helene continues to advance north
    from the southern Gulf of Mexico, increasing the low level height
    gradient across the Southeast. Flow is expected to be especially
    focused along the northern GA/SA border with RAP forecasts of 40
    kt by 12Z. The increased low level flow into and perpendicular to
    the axis of terrain, coupled with lift within the right entrance
    region of a 110-120 kt jet max aloft, should allow for
    steady/periods of heavy rain with rainfall rates of 1-2 in/hr. The
    flash flood threat will also exist farther north toward the
    upslope regions of the central Appalachians into western NC and
    southwestern VA where heavy rain has already fallen over the past
    1-2 days, although reduced instability/moisture with northern
    extent may temper rainfall rates compared to those farther south.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_mf8Di26G500TgTbBXssuA17EmMKPTbty_iVZuLEhVaiDzKYKRNhX8wlFaPb9Hk6zscb= hHKQLgLumB83leSZcQ8gS-g$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...MRX...RNK...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36958081 36798069 36308087 35898114 35198192=20
    34738225 34178229 32608194 32398331 32648457=20
    33238469 34088456 34588434 35168392 35948323=20
    36168293 36418229 36588189 36758143 36938111=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 26 10:17:25 2024
    AWUS01 KWNH 261017
    FFGMPD
    VAZ000-NCZ000-SCZ000-GAZ000-TNZ000-261445-

    Mesoscale Precipitation Discussion 1064
    NWS Weather Prediction Center College Park MD
    616 AM EDT Thu Sep 26 2024

    Areas affected...eastern GA, Upstate SC into the southern/central
    Appalachians

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 261015Z - 261445Z

    SUMMARY...Flash flooding, with locally significant impacts
    possible, should be expected for portions of the southern
    Appalachians this morning. Training of heavy rain is also likely
    to produce areas of flash flooding for other portions of the
    Southeast through 14Z.

    DISCUSSION...Regional radar imagery at 10Z showed an axis of heavy
    rainfall with embedded mesoscale circulations extending from
    east-central GA along I-16 (Laurens and Treutlen counties)
    northward into far Upstate SC and western NC, along the southeast
    facing slopes of the Blue Ridge Mountains. MRMS-estimates
    indicated rainfall rates of 1 to 1.5, locally up to 2 in/hr over
    the past 1-2 hours within this axis. In addition, 24 hour
    estimates from MRMS showed 4 to 8 inch rainfall totals from Oconee
    County in far Upstate SC into McDowell County in western NC. The
    axis of heavy rain has been co-located with an area of strong low
    level moisture flux convergence centered from eastern and northern
    GA into western NC where 09Z SPC mesoanalysis data showed ~500
    J/kg MUCAPE but with higher values of instability closer to the
    Southeast coast (1000+ J/kg). Precipitable water values ranged
    from 1.7 to 2.3 inches across the region (higher toward the
    southeast), with an area of strong upper level divergence located
    within the right entrance region of a nearly stationary upper
    level jet max located east of a closed low positioned over the
    Lower OH Valley.

    Short term forecasts from the RAP show very little movement to the
    axis of low level moisture flux convergence over GA/SC/NC over the
    next 2-4 hours. Given little change in the forcing mechanisms in
    place, heavy rain potential looks to continue over the next couple
    of hours across many of the same locations already seeing heavy
    rain. The biggest change is a forecast minor reduction in the
    available instability, already somewhat low, over inland
    locations. Rainfall rates of 1-2 in/hr may reduce in magnitude but
    areas of heavy rain are likely to continue, overlapping with areas
    that have already seen heavy rainfall and are experiencing ongoing
    flash flooding. Additional rainfall totals of 2-4 inches are
    expected through 14 to 15Z with locally significant flash flooding
    possible across portions of the Blue Ridge from Upstate SC into
    western NC.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!85b-l1nzVvzOaXO0nT4KP2poRkJtHunD9gwP6wv_R-Zu4PYQCikfO6a2V6j0tGHNYWO7= xpJ46Pxy9Vy68CmprEwQ8DA$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...JAX...MRX...RNK...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36628109 36318087 35428126 34578160 33488154=20
    32718152 31958196 31978300 33478369 34918367=20
    36068281 36588194=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 26 13:53:24 2024
    AWUS01 KWNH 261353
    FFGMPD
    FLZ000-GAZ000-ALZ000-261900-

    Mesoscale Precipitation Discussion 1065
    NWS Weather Prediction Center College Park MD
    952 AM EDT Thu Sep 26 2024

    Areas affected...Central Florida Panhandle into central Georgia

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 261351Z - 261900Z

    Summary...Repeating rounds of heavy rainfall featuring rates of
    1-3"/hr will expand across the FL Panhandle and into the Southeast
    today. Where the most pronounced training occurs, rainfall of 2-3"
    is likely, with locally more than 5" possible across the central
    FL Panhandle. Flash flooding is likely.

    Discussion...The GOES-E WV imagery this morning clearly indicates
    the impressive tropical moisture plume being channeled northward
    from Hurricane Helene which is positioned in the southern Gulf of
    Mexico. Downstream, deep moisture characterized by PWs measured by
    GPS and regional 12Z soundings of 2-2.5" is funneling northward as
    it gets squeezed east of a pronounced upper low positioned over
    IL/IN. This impressive moisture will continue to be acted upon by
    robust deep layer ascent through downstream mid-level divergence
    between Helene and the upper low which will overlap with a
    persistent jet streak centered over TN leaving favorable RRQ
    diffluence from FL through western NC. A stationary front is
    analyzed across the region resulting in locally enhanced
    convergence and isentropic ascent as well. Despite abundant cloud
    cover which will somewhat minimize the instability potential, the
    impressive synoptic ascent into the deep moisture will continue to
    support heavy rainfall through the afternoon.

    The high-res CAMs are in pretty good agreement the next several
    hours that heavy rain will focus along the stationary front and expand/intensify downstream of Helene into the FL Panhandle. This
    will likely result in dual maxima for rainfall through the aftn.

    Along the front, 850mb winds surging to 30-45 kts will feature
    increasing isentropic ascent and converge into the boundary
    itself. This is reflected by increasing moisture transport vector
    convergence, and Corfidi vectors that become increasingly parallel
    to the mean flow and the front. This suggests persistent training
    of rainfall rates which the HREF probabilities indicate have a
    30-50% chance of exceeding 1"/hr. This could result in 2-3" of
    rainfall and instances of flash flooding through the afternoon.

    More significant flash flooding potential will gradually develop
    across the central FL Panhandle, especially in the vicinity of the
    Forgotten Coast. Here, 850mnb winds increasing to above 50 kts
    will exceed the mean 0-6km wind, suggesting more broad enhancement
    to the ascent. This will occur coincidentally with Corfidi vectors
    becoming increasingly anti-parallel to the mean flow, suggesting
    an enhanced backbuilding threat and training of rainfall rates
    which the HRRR suggests could exceed 3"/hr (0.75-1"/15 mins). This
    could produce locally as much as 5" of rain as reflected by 6-hr
    HREF neighborhood probabilities, and this will occur atop soils
    saturated from 24-hr rainfall that has been 4-8" in this region.
    Any of the most intense rain rates will likely result in flash
    flooding, with locally significant flash flooding possible in
    urban areas or where training occurs atop the most primed soils.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_zS2hmBoXZHeDf15hSPZ9bNwtzm-EInFPQlDT-PwK0MRn3sC83xP7iCTDuwR1zOnv3RX= xO6aKB0FY2dn9f_RT6iz7wM$ for graphic product...

    ATTN...WFO...BMX...FFC...JAX...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 33508431 33398358 32008269 30938294 29978357=20
    29798392 29498454 29378498 29518558 30218618=20
    31338605 32308558 33028496 33258477=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 26 14:50:31 2024
    AWUS01 KWNH 261450
    FFGMPD
    VAZ000-NCZ000-WVZ000-SCZ000-GAZ000-TNZ000-KYZ000-262030-

    Mesoscale Precipitation Discussion 1066
    NWS Weather Prediction Center College Park MD
    1049 AM EDT Thu Sep 26 2024

    Areas affected...Southern Appalachians

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 261449Z - 262030Z

    Summary...Widespread heavy rain downstream of Hurricane Helene
    will continue today into the Southern Appalachians. Rainfall rates
    of 1-2"/hr are likely, which through repeating rounds could
    produce 2-3" of rain with local maxima of 5". This will enhance
    flash flooding, with significant impacts becoming likely across
    the Southern Blue Ridge.

    Discussion...The regional radar mosaic this morning shows an
    expansive area of heavy rain across much of the Southeast and into
    the Southern Appalachians. This is associated with a pronounced
    moisture plume noted in the GOES-E WV imagery extending downstream
    from Hurricane Helene in the Gulf of Mexico. PWs within this
    moisture plume have been measured as high as 1.75 to 2.0 inches on
    the 12Z U/A observed soundings from KRAX and KFFC. Instability is
    somewhat limited, only around 100-250 J/kg of MLCAPE, but deep
    layer ascent is impressive. Mid-level divergence between Helene
    and a pronounced upper low over IN is combining with a nearly
    stationary poleward arcing jet streak over TN to leave favorable
    RRQ over the region, while low-level SE flow continues to upslope
    into the terrain. In this environment, rainfall rates have already
    been measured via MRMS as high as 1.25", and these will likely
    continue through the aftn.

    During the next several hours, persistent moderate to heavy rain
    with rates 0.5-1"/hr will lift northward across the area, with
    embedded convective cells producing locally enhanced rain rates to
    2"/hr as reflected by HRRR 15-min rainfall exceeding 0.5". 850mb
    inflow will remain out of the S/SE through the aftn while
    gradually intensifying to above 30 kts, resulting in moisture flux
    that is progged by the SREF to exceed +3 sigma later today. This
    impressive moisture advection combining with nearly unchanging
    robust ascent will result in continuous rainfall into areas that
    have already received 4-8+" of rain the past 24-hours. The HREF
    neighborhood probabilities indicate a 50-70% (10-20%) chance of
    more than 3" (5") of rain the next 6 hours, with the highest
    probabilities across Upstate SC and into far western NC along the
    Blue Ridge. Elsewhere in northeast GA, eastern TN, and southwest
    VA, 1-3" of additional rainfall is likely through the aftn.

    This rainfall occurring atop saturated soils, sensitive terrain,
    and ongoing flash flooding, will almost certainly enhance impacts
    across the region. FFG has been extremely compromised to as low as
    0.25"/3hrs for which the HREF exceedance probabilities reach above
    70%. This lends high confidence to flash flooding and impacts as
    rain continues across the region. However, across the Blue Ridge,
    current streamflow anomalies are as much as 400-600% of normal, so
    any additional rainfall could quickly result in significant and life-threatening flash flood impacts.

    Additional rainfall this evening will almost certainly necessitate
    future MPD issuances across this region with widespread
    significant flash flooding, and possibly locally catastrophic
    impacts, developing as the rain persists and becomes even more
    intense into tonight.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7VIaHIFGs9tb7z-yxhkxhUzgWCRF-29HSujbYUuEdnx4WuiB8dZAQFJz21TUzaVNkwNO= UzZp62A0V08YOLw-JYixReA$ for graphic product...

    ATTN...WFO...CAE...FFC...GSP...JKL...MRX...RLX...RNK...

    ATTN...RFC...LMRFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 37668066 37518005 37058039 35718133 35008180=20
    33918230 33768241 33478258 33238297 33248347=20
    33558382 34008415 34418448 35568425 36848340=20
    37388243 37648158=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 26 15:06:55 2024
    AWUS01 KWNH 261506
    FFGMPD
    SCZ000-GAZ000-262105-

    Mesoscale Precipitation Discussion 1067
    NWS Weather Prediction Center College Park MD
    1106 AM EDT Thu Sep 26 2024

    Areas affected...South Carolina and Eastern Georgia

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 261505Z - 262105Z

    SUMMARY...Extremely heavy rainfall in heavy banding will persist
    into the afternoon over eastern Georgia and central South Carolina
    including Columbia. Widespread flash flooding with locally
    significant impacts is likely through the mid-afternoon.

    DISCUSSION...Regional radar imagery at 15Z showed an axis of heavy
    rainfall extending north-south over southern to central SC. This
    band is redeveloping on the south end and shifting north, nearly
    along its axis causing hourly rates of 2.5"/hr. This particular
    band is tracking into Columbia which is rather flood prone. The
    axis of heavy rain has been co-located with an area of strong low
    level moisture flux convergence in a plume of 2.2 to 2.5" PW which
    is the core of moisture streaming ahead of Helene on southerly
    35kt low level flow. Instability is rather limited decreasing from
    1500 J/kg near the SC coast to less than 500 J/kg near Columbia,
    but this is overcome from strong dynamics where the mean layer
    southerly flow is 40kt and oriented with the activity, causing
    training.

    Recent HRRR runs are under doing this band and feature more
    scattered convective modes through the mid-afternoon. However, the
    channeling of this flow between the upper low that remains over
    western TN and the ridge east of FL will maintain redeveloping
    advection and banding ahead of Helene. Given little change in the
    forcing mechanisms in place, heavy rain potential will continue
    into the mid-afternoon across many of the same locations already
    seeing heavy rain. While FFG was rather elevated over these areas,
    it is quickly dropping as heavy rain spreads in. The extreme rates
    warrants likely wording for the flash flood risk.

    There should be some break in heavy rain here later this afternoon
    before banding from Helene returns this evening as the system
    passes to the west.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9fBehw2pX7PEGQstADx09gJFOvfS4Qj-UaJx0xcfY3AQGxWXiv4sAJ7E03NeNYZnxxIo= fU3iR6DYtSSLRq3nBO_Z9dk$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...ILM...JAX...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 35078146 34428010 33737988 32777985 32068065=20
    31248119 31618254 32388283 32908317 33288314=20
    33428275 33828248 34488209 35048177=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 26 18:54:00 2024
    AWUS01 KWNH 261853
    FFGMPD
    FLZ000-GAZ000-ALZ000-270000-

    Mesoscale Precipitation Discussion 1068
    NWS Weather Prediction Center College Park MD
    253 PM EDT Thu Sep 26 2024

    Areas affected...Central FL Panhandle into central GA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 261852Z - 270000Z

    Summary...Nearly continuous rainfall with rates of 1-3"/hr will
    persist into this evening ahead of Hurricane Helene. Training of
    these rates will result in widespread additional rainfall of 2-3"
    by this evening, with local maxima around 5" possible. This will
    expand and enhance ongoing flash flooding, with significant
    impacts likely in the central FL Panhandle.

    Discussion...The GOES-E visible imagery this afternoon shows a
    well defined and intensifying Hurricane Helene across the Gulf of
    Mexico blifting north towards the Florida Panhandle. Downstream of
    Helene, impressive moisture advection is persisting on
    strengthening SE flow around the hurricane, driving PWs to as high
    as 2.5" as measured by GPS, which is above the daily record for
    the central FL Panhandle and into southern GA. This exceptionally
    moist air is pivoting northward into an area of intense deep layer
    ascent driven via strong mid-level divergence overlapping the
    diffluent RRQ of a northward arcing jet streak. Additionally, a
    cold front draped from northern GA into the Gulf of Mexico is
    helping to produce focused moisture convergence along which heavy
    rain rates will train. 24-hr MRMS rainfall across this region has
    been generally 4-8" with locally as much as 12", and ongoing
    rainfall rates of 1-2"/hr are producing MRMS FLASH unit streamflow
    responses as high as 300-500 cfs/smi. Flash flooding is currently
    ongoing.

    During the next several hours, moisture north of Helene will
    continue to surge northward and impinge into a region of focused
    ascent from the central FL Panhandle to as far north as Atlanta,
    GA. This will likely result in both an expansion and
    intensification of rainfall, with rates potentially peaking around
    3"/hr in stronger convection, although will more commonly be
    1-2"/hr. The strengthening 850mb inflow will not only enhance
    moisture transport, resulting in stronger moisture convergence
    onshore and into the front, but also cause Corfidi vectors to
    become anti-parallel to the flow near the Gulf Coast, merging
    towards parallel along the front. This suggests increased
    backbuilding and training of echoes within spiraling and
    convergent convective clusters, and the HREF neighborhood
    probabilities indicate a 30-60% chance for 3" from the Forgotten
    Coast of FL northward along the front into central GA, while the
    WoFS confines the highest probabilities to the FL Panhandle where
    locally 4-5" is possible.

    This rain will be occurring atop soils that are fully saturated
    from heavy 24-hr rainfall,. This is reflected by NASA SPoRT 0-10cm
    RSM that is above 85%, and resultant 3-hr FFG as low as 0.75-1.5".
    This will likely be exceeded in many areas, and where the heaviest
    rates train across the most vulnerable soils, especially in the
    vicinity of Apalachicola, resultant impacts will become
    significant even before Helene's landfall later this evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_7khhClvHcPtlBSpgtOfIakkpGRxqIeRTsrNUjQnq9y-bUW8tULnGe2DZ7IL5tEjAiGA= -rrTUb2Xp09nXL4SOToL8Us$ for graphic product...

    ATTN...WFO...BMX...FFC...MOB...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 34078422 33438374 32898324 32088278 31858354=20
    31248398 30698390 30068403 29838433 29528491=20
    29678553 30278618 31508624 33388549 34058495=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 26 20:36:31 2024
    AWUS01 KWNH 262036
    FFGMPD
    VAZ000-NCZ000-SCZ000-GAZ000-TNZ000-270230-

    Mesoscale Precipitation Discussion 1069
    NWS Weather Prediction Center College Park MD
    435 PM EDT Thu Sep 26 2024

    Areas affected...North Georgia, Western Carolinas into Virginia

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 262034Z - 270230Z

    Summary...Swaths of heavy rain rates ahead of Helene will continue
    through this evening over portions of north Georgia and the
    western Carolinas into Southwest Virginia, including mainly the
    eastern side of the Southern Appalachians. Rainfall rates of
    1-2"/hr will continue, which through repeating rounds could
    produce 2-3" of rain and local maxima of 5" through 02Z. This will
    enhance flash flooding, with significant impacts
    continuing/expanding.

    Discussion...The regional radar mosaic late this afternoon shows
    continued swaths of heavy rain over north Georgia and western SC
    with continued enhancements of rainfall over the eastern slopes of
    the Southern Appalachians. This is associated with a pronounced
    moisture plume streaming north from Hurricane Helene which is now
    west of Tampa Bay. PWs within this moisture plume have been are
    2.25 to 2.5" with southeasterly flow of 20 to 35kt over central
    GA/SC expected to shift over the southern Appalachians over the
    next couple hours. Instability remains limited, 200 to 500 J/kg of
    MUCAPE, but deep layer ascent is impressive. Mid-level divergence
    between Helene and a pronounced upper low remaining over far
    western TN is combining with a nearly stationary poleward arcing
    jet streak from AL to KY with favorable right entrance dynamics
    over the region. In this environment, recent rainfall rates are
    estimated from KGSP and KFFC as up to 1.5"/hr which can be
    expected to continue through the evening. There is a notable gap
    in reflectivity over southeast GA and north FL Peninsula between
    bands, which should provide relief over the next few hours for
    southern portions of this outlook area.

    The impressive moisture advection combining with nearly unchanging
    robust ascent will result in continuous rainfall into areas that
    have already received 4 to 10" in the past 24 hours. This rainfall
    occurring atop saturated soils, sensitive terrain, and ongoing
    flash flooding with further enhanced impacts across the region
    which is still prior to the actual intense rainfall from Helene
    herself. This additional rainfall should quickly result in further life-threatening flash flooding.

    Locally catastrophic rainfall impacts are expected overnight as
    the core of Helene approaches, so please pay attention to further
    discussions and see the latest info on Helene at hurricanes dot
    gov.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4xwbFyCSaIjD0lOy9jJCTMDNq9YO2viUOiTuIBxURGuk_Fhpm3Sj8GErapO0FTqetHEF= PrhSeHGWTzeYUwxBWij4zk0$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...MRX...RNK...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36978187 36798079 35098067 33848074 32548124=20
    33028323 33988422 34478481 35358494 35808371=20
    36188283 36578241=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 26 23:08:33 2024
    AWUS01 KWNH 262308
    FFGMPD
    FLZ000-GAZ000-ALZ000-270500-

    Mesoscale Precipitation Discussion 1070
    NWS Weather Prediction Center College Park MD
    707 PM EDT Thu Sep 26 2024

    Areas affected...Florida Big Bend well up into Georgia

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 262305Z - 270500Z

    Summary...Hurricane Helene will make landfall late this evening
    along the Florida Big Bend with inner bands progressing up Georgia
    and converging on a stationary front over eastern AL. The eyewall
    will impact the Big Bend area 02 to 05Z which will include heavy
    rainfall that will exacerbate the extreme impacts from wind and
    storm surge there.

    Discussion...
    GOES-E IR imagery and regional NEXRAD here at 23Z depict a well
    defined eye on Helene with a central dense overcast extending into
    Apalachee Bay. Outer bands extend north through the Atlanta metro
    with a sharp cutoff on the west side on the stationary front that
    is just into AL. Extreme moisture advection persists ahead of
    Helene on ever strengthening cyclonic flow with 2.5"+ PW in the
    inner core of the storm. This exceptionally moist air continues to
    pivot northward into an area of intense deep layer ascent driven
    via strong mid-level divergence overlapping the diffluent right
    entrance portion of a northward arcing jet streak over northern
    AL.

    Continuous rainfall with rates around 1"/hr will persist ahead of
    Helene with embedded areas of 2"/hr in the heaviest bands through
    midnight. Training of these rates will result in widespread
    additional rainfall of 2-3" by midnight. A corridor of 3 to 6"
    along and west of the eyewall, which includes Tallahassee, is
    forecast through 05Z by the 20Z HRRR which seems reasonable given
    the increasing forward speed of the hurricane. The area southwest
    of Tallahassee which has seen 6-10" over the past 24hrs is progged
    to be just west this eyewall maxima through 04Z.

    Expect flooding concerns to continue in the Atlanta metro this
    evening with the additional couple inches. However, the greater
    threat for Atlanta is early Friday morning as the remnant eye
    passes to the east. Further details on rainfall from that will
    come from overnight products.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Fc9ClftjhxX5P-7NSu5XVb-QG-6u58Ed4VSc4s42YzqbugDcCEmasYtyB5Pdq8iHhty= FNWtpcABnvYSl_JOUc5Za6w$ for graphic product...

    ATTN...WFO...BMX...FFC...JAX...TAE...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 34218470 33868416 32948314 31568276 30448259=20
    29618275 29158322 29818392 29518483 29658539=20
    30228586 30348596 31698596 32868571=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 27 02:34:33 2024
    AWUS01 KWNH 270234
    FFGMPD
    VAZ000-NCZ000-SCZ000-GAZ000-TNZ000-270830-

    Mesoscale Precipitation Discussion 1071
    NWS Weather Prediction Center College Park MD
    1034 PM EDT Thu Sep 26 2024

    Areas affected...northeastern GA into the western Carolinas and
    southwestern VA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 270230Z - 270830Z

    Summary...Additional 1-3 inch rainfall totals, with localized 3-5
    inches into the Blue Ridge Mountains, are expected through 08Z
    across GA/SC/NC. Flash flooding is ongoing and will only worsen
    and expand with time.

    Discussion...Regional radar imagery from 0215Z showed widespread
    rain across much of the southeastern U.S. but with gaps over
    portions of SC in advance of an outer rain band from Helene
    tracking across the southeastern SC/GA border. A combination of
    MRMS and gauge reports showed peak rainfall rates ranging between
    0.5 to 1.5 in/hr across the upslope favored terrain of the
    southern Appalachians, specifically the Blue Ridge Mountains.

    Instability remains low in the vicinity of the terrain, less than
    250 J/kg (via 02Z SPC mesoanalysis data), increasing to over 1000
    J/kg near the SC/GA coast. However, strong forcing, including
    30-40 kt of southeasterly 925-850 mb winds (via KGSP and TCLT VAD
    wind data) was favorably oriented into the mountains, beneath
    divergent and diffluent flow aloft to the east of a closed low
    over southeastern MO and in advance of Hurricane Helene.

    No major changes to the current setup are expected through 08Z
    with the core of Helene perhaps just getting into the southern
    portions of the MPD threat area around 08Z. However, some increase
    in instability across inland is anticipated as Helene tracks
    northward overnight and an increase in the 925-850 mb wind into
    the 50-70 kt range overspreads the region. Rainfall rates of 0.5
    to 1.5 in/hr at times will continue with an additional 1-3 inches
    for many areas from northeastern GA into central and western SC/NC
    with locally 3 to 5 inch additional totals for the terrain.

    These rains will continue to make for an extremely dangerous
    situation later tonight as the core of Helene's rainfall arrives
    later this morning, for which another MPD will be issued.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8507ghn4_OfQ0msZxABfsw7hon-pAhQj4dJCRsRRojdNrckPRvz-ZJgfoZjuT2HuVaWq= zTeXznXhxMAZ7LnLrC83l1s$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...MRX...RNK...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36968025 36658015 36228066 34778055 33538070=20
    32718117 32598203 32798287 33448393 34458474=20
    35228414 36048240 36758121=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 27 05:26:36 2024
    AWUS01 KWNH 270526
    FFGMPD
    FLZ000-GAZ000-TNZ000-ALZ000-270845-

    Mesoscale Precipitation Discussion 1072
    NWS Weather Prediction Center College Park MD
    125 AM EDT Fri Sep 27 2024

    Areas affected...northern FL into GA and far eastern AL

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 270522Z - 270845Z

    Summary...Heavy rain from Helene's inner core to track NNE across
    GA through 08Z with an additional 3-5 inches through 09Z. Farther
    west, an axis of heavy rain is likely to develop 06-08Z. Rainfall
    rates of 1-2 in/hr will be common but localized rates near 3 in/hr
    will be found with Helene's eyewall.

    Discussion...Hurricane Helene was located just north of the FL/GA
    border, about 10 miles west of VLD, moving toward the NNE with an
    average 3-hr speed of ~28 kt calculated via hourly NHC position
    updates through 05Z. Radar imagery showed the heaviest rain
    located in the northern eyewall, while rain was considerably
    lighter in the southern semicircle of Helene's inner core. A
    second band of heavy rain was located northwest of the eyewall,
    pivoting over ABY to just east of TLH with training from NNE to
    SSW supporting increasing rainfall rates over the past hour. While
    accurate ground truth is difficult to assess along the path of a
    landfalling hurricane, MRMS-derived hourly rainfall has been
    between 1-3 inches over the past 3 hours to the north of Helene
    while waves of higher rainfall intensity have overspread central
    to northwestern GA with rainfall rates occasionally peaking above
    1 in/hr.

    Helene is expected to maintain a similar forward speed and track
    through 08Z with the core of the heaviest rain, associated with
    Helene's eyewall, tracking NNE across east-central GA. Rainfall
    rates of 1-3 in/hr are likely but with 15-minute rates of 0.5 to 1
    inch, leading to the rapid accumulation of water on the surface.
    This will especially be true as this path will take some of
    Helene's highest rainfall rates across a stripe of 5-8 inches
    which is estimated to have fallen in a stripe from near Dublin, GA
    to just west of Augusta over the past 24 hours.

    Farther west, low level convergence along an axis near or just
    east of the AL/GA border is expected to enhance rainfall intensity
    in the 07-09Z time frame. It is here where easterly winds of 30-50
    kt in the 925-850 mb layer will meet and converge with northerly
    to NNW winds over eastern AL. Mean steering flow oriented similar
    to the expected axis of convergence will allow for rainfall rates
    of 1-2 in/hr to develop later this morning, along with areas of
    flash flooding where these higher rates overlap with heavy rain
    which has fallen over the past 24-48 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-dMr0O-UIluqAyzpaY-o-LBoOGwkGEzXvhFtHGLzx9FBfZHrYr_um9N-tU_9d-CsWFaZ= jHhucZ022GapPFymvOYJtJY$ for graphic product...

    ATTN...WFO...BMX...CAE...CHS...FFC...GSP...HUN...JAX...MRX...
    OHX...TAE...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 35428610 35328552 34728498 34258438 34158318=20
    33508200 32108176 31148206 30428267 30208366=20
    30498471 31228523 33048573 34658633=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 27 08:34:42 2024
    AWUS01 KWNH 270834
    FFGMPD
    VAZ000-NCZ000-SCZ000-GAZ000-TNZ000-271430-

    Mesoscale Precipitation Discussion 1073
    NWS Weather Prediction Center College Park MD
    434 AM EDT Fri Sep 27 2024

    Areas affected...northeastern GA into western SC/NC and
    southwestern VA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 270830Z - 271430Z

    SUMMARY...Severe to catastrophic flash flooding will be likely for
    portions of western SC/TN this morning. Additional rainfall totals
    of 4 to 7 inches, at least locally through 14Z, will pose a threat
    to life with potential for landslides due to saturated soils and
    swollen rivers/creeks.

    DISCUSSION...Hurricane Helene was located over eastern GA at 08Z,
    just north of Eastman, tracking rapidly toward the NNE between
    25-30 kt over the past 6 hours. Water vapor imagery showed Helene
    interacting with a closed upper level low over northeastern AR,
    which is expected to cause the hurricane to turn toward the
    northwest later this morning. Recent trends in infrared satellite
    imagery showed some cloud top warming with Helene, indicative of
    weakening, but Helene remained a large and powerful tropical
    system with a symmetric appearance in colder cloud tops.

    925-850 mb winds were strongest to the east of Helene, with VAD
    wind data at KCLX showing 80-90 kt, with area VAD winds showing
    50-70 kt from the western NC/SC border into northeastern GA.
    Gradual weakening of these winds is expected over the next 3-6
    hours and the quick northward motion will at least limit the
    duration of extreme moist ascent into the terrain but a
    significant duration of high rainfall rates is still anticipated
    into portions of the Blue Ridge. As Helene continues its northward
    track, expect rainfall rates of 1-2 in/hr to expand northward with
    potential for some terrain locations to see 2-4 hours of rainfall
    rates near/above 1 in/hr.

    Estimated rainfall totals (via multi-sensor MRMS output) showed 6
    to 12+ inches of rain have fallen over the past 48 hours from
    northeastern GA into western SC/NC along the southeast facing
    slopes of the Blue Ridge Mountains. Areas of flash flooding are
    already ongoing and widespread across the region and an additional
    4 to 7 inches (locally) through 14Z is expected to produce severe
    to catastrophic levels of flash flooding with potential for
    landslides and threats to life and property. Experimental WoFS
    data from 07Z showed the probability of exceeding 5 inches through
    13Z to be 70+ percent in eastern Yancey County and 40+ percent in
    southern Haywood County (both in western NC) where upslope
    enhancement is expected to be maximized due to terrain influences.
    This is a high confidence forecast and there is strong model
    support for the location of heaviest rainfall over the next 6
    hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6BXGboausFe1dFHEiggLoycQfFYguQddmc1l6ql4tPcwOUxq0f4KHkNLNTZrwJ9HZ-Kg= OZrLR79MqaNqyDooGeKqodo$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...MRX...RAH...RNK...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36918091 36708038 35898033 34948050 34238069=20
    32818146 32448197 32538252 32798296 33168308=20
    33918302 34638360 35238396 35928289 36668161=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 27 08:47:40 2024
    AWUS01 KWNH 270847
    FFGMPD
    VAZ000-NCZ000-SCZ000-GAZ000-TNZ000-271430-

    Mesoscale Precipitation Discussion 1073...Corrected
    NWS Weather Prediction Center College Park MD
    447 AM EDT Fri Sep 27 2024

    Corrected for typo in summary section

    Areas affected...northeastern GA into western SC/NC and
    southwestern VA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 270830Z - 271430Z

    SUMMARY...Severe to catastrophic flash flooding will be likely for
    portions of western SC/NC this morning. Additional rainfall totals
    of 4 to 7 inches, at least locally through 14Z, will pose a threat
    to life with potential for landslides due to saturated soils and
    swollen rivers/creeks.

    DISCUSSION...Hurricane Helene was located over eastern GA at 08Z,
    just north of Eastman, tracking rapidly toward the NNE between
    25-30 kt over the past 6 hours. Water vapor imagery showed Helene
    interacting with a closed upper level low over northeastern AR,
    which is expected to cause the hurricane to turn toward the
    northwest later this morning. Recent trends in infrared satellite
    imagery showed some cloud top warming with Helene, indicative of
    weakening, but Helene remained a large and powerful tropical
    system with a symmetric appearance in colder cloud tops.

    925-850 mb winds were strongest to the east of Helene, with VAD
    wind data at KCLX showing 80-90 kt, with area VAD winds showing
    50-70 kt from the western NC/SC border into northeastern GA.
    Gradual weakening of these winds is expected over the next 3-6
    hours and the quick northward motion will at least limit the
    duration of extreme moist ascent into the terrain but a
    significant duration of high rainfall rates is still anticipated
    into portions of the Blue Ridge. As Helene continues its northward
    track, expect rainfall rates of 1-2 in/hr to expand northward with
    potential for some terrain locations to see 2-4 hours of rainfall
    rates near/above 1 in/hr.

    Estimated rainfall totals (via multi-sensor MRMS output) showed 6
    to 12+ inches of rain have fallen over the past 48 hours from
    northeastern GA into western SC/NC along the southeast facing
    slopes of the Blue Ridge Mountains. Areas of flash flooding are
    already ongoing and widespread across the region and an additional
    4 to 7 inches (locally) through 14Z is expected to produce severe
    to catastrophic levels of flash flooding with potential for
    landslides and threats to life and property. Experimental WoFS
    data from 07Z showed the probability of exceeding 5 inches through
    13Z to be 70+ percent in eastern Yancey County and 40+ percent in
    southern Haywood County (both in western NC) where upslope
    enhancement is expected to be maximized due to terrain influences.
    This is a high confidence forecast and there is strong model
    support for the location of heaviest rainfall over the next 6
    hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-99ZlzKPoaY5oreX2caTIot_Hou5qjA2r3pym3ovkclWo7KpD6tZRnoLlqWy6L6D9NrN= xVrOfCbZGYn5ZXsTvqcKFB4$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...MRX...RAH...RNK...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36918091 36708038 35898033 34948050 34238069=20
    32818146 32448197 32538252 32798296 33168308=20
    33918302 34638360 35238396 35928289 36668161=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 27 09:32:42 2024
    AWUS01 KWNH 270932
    FFGMPD
    GAZ000-TNZ000-ALZ000-271530-

    Mesoscale Precipitation Discussion 1074
    NWS Weather Prediction Center College Park MD
    531 AM EDT Fri Sep 27 2024

    Areas affected...northwestern GA into northeastern AL and Middle
    TN

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 270930Z - 271530Z

    SUMMARY...A pivoting axis of heavy rain is expected to focus a
    threat for flash flooding from northwestern GA into northeastern
    AL and Middle TN this morning. Rainfall rates of 1-2 in/hr,
    highest to the south and east, are likely with additional rainfall
    of 2-4 inches through 15Z.

    DISCUSSION...Regional radar imagery at 09Z showed Tropical Storm
    Helene's inner core tracking northward toward the central SC/GA
    border. Bands of heavy rain also extended west of the center of
    circulation into portions of western GA, northeastern AL and
    Middle TN. MRMS and gauge data showed rainfall rates of 0.5 to 1.0
    in/hr for most areas west of Helene, but localized rain rates of
    1-2 in/hr were estimated via MRMS to the northeast of CSG where
    locally higher instability (up to 500 J/kg) was present via 09Z
    SPC mesoanalysis data. However, instability values into TN were
    quite low at or below 250 J/kg. The bands of heavy rain from
    western GA into the tri-state region of GA/AL/TN appeared to be
    associated with a low level axis of convergence, centered in the
    925-850 mb layer between strong easterly winds to the north of
    Helene and northwesterly winds in eastern AL.

    Despite the lack of greater instability, strong low level
    convergence was present within a very moist airmass characterized
    by precipitable water values of 2 inches in Middle TN, increasing
    to over 2.5 inches in west-central GA. In addition, water vapor
    imagery revealed a diffluent flow pattern aloft across the region.
    RAP forecasts show the low level convergence axis slowly pivoting
    cyclonically about a point near the tri-state region (GA/AL/TN)
    through 15Z with southeasterly steering flow aligned with the
    convergence axis at times, which will allow for repeating and
    training areas of heavy rain. Due to the limited instability in
    place, rainfall rates may struggle to climb above 1 in/hr across
    northwestern locations, but a semi-longer duration heavy rainfall
    event is expected to produce 2 to 4 inches of rain in a 6 hour
    period from portions of Middle TN into northeastern AL and
    northwestern GA. Flash flooding is considered likely, especially
    in northwestern GA where some areas of flash flooding are ongoing
    due to recent heavy rain from Helene.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7AYmDCoLBC9MuXMcaVEpzMGmk5cgMJautne6I2glSen1g0lOTdHbzVKLrFnQ4YhMkl7y= ZfoQhJA-U90jAr7Ic9iKQlI$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...MRX...OHX...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36528620 36188562 35438513 34358387 33988352=20
    33438330 32758353 32688457 33558577 34798679=20
    36038742 36488722=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 27 10:06:13 2024
    AWUS01 KWNH 271006
    FFGMPD
    NCZ000-SCZ000-271600-

    Mesoscale Precipitation Discussion 1075
    NWS Weather Prediction Center College Park MD
    605 AM EDT Fri Sep 27 2024

    Areas affected...coastal/eastern SC into central/southern NC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 271004Z - 271600Z

    SUMMARY...Possible training and repeating of heavy rain associated
    with Tropical Storm Helene could produce localized flash flooding
    from central to coastal SC into central/southern NC through 16Z.
    The potential for 1-3 in/hr rainfall rates will exist.

    DISCUSSION...Regional radar imagery at 0950Z showed an outer rain
    band to the east of T.S. Helene focusing from the offshore waters
    of SC across the Charleston metro into central SC. Numerous cells
    were observed to be repeating across the region with brief
    training supporting MRMS-derived rainfall rates occasionally over
    1 in/hr. These cells were located with a very moist environment
    (2.3 to 2.6 inch precipitable water values) and MLCAPE of 500-1500
    J/kg via the 09Z SPC mesoanalysis.

    As Helene continues a northward to an eventual northwestward
    motion this morning, bands of heavy rain on the east side of
    Helene are expected to advance northward up the coast into the Pee
    Dee region and eventually central to southern NC. A general
    progressive motion is expected to these cells, but periods of
    stalling will be possible with the rainfall axis which could
    support locally higher rainfall rates, with 2-3 in/hr not out of
    the question. Some overlap of these rain bands with an axis of 2-5
    inches which impacted locations between CHS and MYR toward FLO.
    Additional rainfall totals of 2-4 inches will be possible through
    16Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8x45YJlt0BreI5eIeMsUFdDZTZJZFP1Q8DnSl9-9XX9ACV5zepE0nuWTD07znH416Jdk= ft-ka-X-eARSPPMyxZlhbyE$ for graphic product...

    ATTN...WFO...CAE...CHS...GSP...ILM...MHX...RAH...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 35667896 35087808 34027782 33397861 32557929=20
    32387970 32918039 34138092 35428010=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 27 13:13:45 2024
    AWUS01 KWNH 271313
    FFGMPD
    VAZ000-NCZ000-WVZ000-SCZ000-GAZ000-TNZ000-271810-

    Mesoscale Precipitation Discussion 1076
    NWS Weather Prediction Center College Park MD
    913 AM EDT Fri Sep 27 2024

    Areas affected...Upstate SC, western NC, far northeastern TN,
    southwest VA, and southern WV

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 271310Z - 271810Z

    SUMMARY...Life-threatening flash flooding and the likelihood of
    catastrophic impacts to continue across much of the southern
    Appalachians through at least early this afternoon with an
    additional 2-4" of rain.

    DISCUSSION...The center of Tropical Storm Helene is racing
    northward and entering Upstate SC as of 1245Z. Along with it
    resides an area of 2-3" per hour rainfall rates (via MRMS) in what
    is the leftovers of a northern eyewall over western NC. Peak
    3-hourly rainfall observations from NWS/AWOS/ARL sites also
    confirm these amounts. This torrential rainfall is occurring over
    a region that has experienced widespread rainfall amounts of 5-12"
    over the last 24 hours, making for a particularly dangerous and life-threatening situation as ground conditions are already
    oversaturated and FFGs remain extremely low. Flash flooding is
    ongoing and will likely continue/worsen over at least the next few
    hours across western NC.

    A large area of 60-80 kt southeasterly 850mb winds per the 11z RAP
    on the eastern periphery of Helene are leading to an extremely
    favorable upslope enhancement across western NC orthogonal to the
    Blue Ridge/southern Appalachians, along with record-breaking PWs
    (per the NAEFS ESAT) in the 2-2.5" range surging northward. This
    along with nearby MUCAPE values of 500 J/kg advecting northeast
    and wet bulb zero heights above 14k feet (near the daily record
    for GSO per SPC's sounding climo) will allow for warm rain
    processes.

    The only positive news is that Helene continues to race north at
    30 mph (per NHC) and lead to a quick exit of this extreme
    rainfall, with intense rates ending across Upstate SC first by 14Z
    and western NC by around 16Z. However, this region will also take
    the brunt of the tropical moisture surge and the highest
    additional totals. Heavy rain will slide northward as it exits the
    western Carolinas and impact regions of southwest VA and southern
    WV with rainfall rates of 1-2" per the 06z HREF through 19-20Z.
    This region also remains mostly saturated after 1-3" of rain over
    the past 24 hours.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6ecx4mCqBJ8EKCSwJa6MWjyHZvbUGxePGOkFskfSW7xeiBJZ65S7AMiTPU4I3Bz9-hEq= Nh3RMBfd1a3mcT0f0UD9Fhw$ for graphic product...

    ATTN...WFO...GSP...MRX...RAH...RLX...RNK...

    ATTN...RFC...LMRFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 37928066 37767976 37107967 35968032 35158118=20
    34928231 35008318 35328353 36048310 36828245=20
    37678156=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 27 15:26:16 2024
    AWUS01 KWNH 271526
    FFGMPD
    VAZ000-NCZ000-WVZ000-272124-

    Mesoscale Precipitation Discussion 1077
    NWS Weather Prediction Center College Park MD
    1125 AM EDT Fri Sep 27 2024

    Areas affected...Eastern NC into central VA and parts of central
    WV

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 271524Z - 272124Z

    SUMMARY...Heavy showers expanding northward with the main plume of
    tropical moisture associated with Tropical Storm Helene will shift
    into the central Appalachians this afternoon and could contain
    rainfall rates of 1-2", likely producing areas of flash flooding.
    Line of showers and thunderstorms progressing east-northeast
    across central/eastern NC extending into central VA this afternoon
    may briefly train and create flash flooding concerns.

    DISCUSSION...The center of Tropical Storm Helene is crossing the
    southern Appalachians late this morning as broad, strong
    southeasterly flow continues to pump a moist tropical airmass into
    the Mid-Atlantic. The core of the 850mb jet (50-60+ kts) is
    lifting northward along with the warm conveyor of moisture
    stretching all the way back to the Gulf of Mexico. Favorable
    upslope flow into the central Appalachians and central/northern VA
    section of the Blue Ridge will support hourly rainfall rates of
    1-2", which will likely overwhelm widespread hourly FFGs less than
    1" in the sensitive terrain of VA. MUCAPE values around 500 J/kg
    just east of the Blue Ridge will also increase chances for locally
    intense rainfall where embedded storms wrap northwestward around
    the main circulation. HREF neighborhood probabilities for
    exceeding 3-hourly FFG are high (>80%) along the Blue Ridge of
    central/northern VA.

    Rainfall rates per MRMS in the N-S oriented line of storms across
    central NC are in the 1-3" range. Although mostly moving
    progressively northeastward, parallel upper flow supports the
    potential for brief training, which could lead to areas of flash
    flooding. The environment also contains PWs of 2-2.5" and MLCAPE
    of 1000-2000 J/kg advected northward from the coastal Carolinas.
    Storms should be able to maintain themselves and could turn
    supercellular as effective bulk shear remains elevated and above
    50 kts for much of the Carolinas. Rainfall amounts of 1-3" are
    possible per the latest CAMs. 06z HREF neighborhood probabilities
    for at least 3" in 3-hours (also near the regions FFG) are around
    20-40%.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9LAnIh76x0XonNy9VIfOOyeqma8uMwP59ReP_XMWoMHl_6ydaE5MSVX_Mdughrg9q9Ws= wXv5tqDRBY9msiH0PLRtHk0$ for graphic product...

    ATTN...WFO...AKQ...ILM...LWX...MHX...PBZ...RAH...RLX...RNK...

    ATTN...RFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 38987981 38947853 38277766 37087713 35327700=20
    33987753 33797853 35727890 37057961 37738073=20
    38448075=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 27 18:04:17 2024
    AWUS01 KWNH 271804
    FFGMPD
    VAZ000-NCZ000-WVZ000-OHZ000-KYZ000-INZ000-272300-

    Mesoscale Precipitation Discussion 1078
    NWS Weather Prediction Center College Park MD
    203 PM EDT Fri Sep 27 2024

    Areas affected...Lower Ohio Valley into the Appalachians of
    WV/VA/NC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 271802Z - 272300Z

    Summary...Showers and thunderstorms developing around Tropical
    Storm Helene will train to the NW through the afternoon. Rainfall
    rates as high as 1.5"/hr are likely, which through this training
    could produce 1-3" of rain. Additional flash flooding is possible.

    Discussion...The regional radar mosaic this afternoon shows an
    expansive area of rainfall from the MS VLY eastward into the
    coastal Mid-Atlantic states. This precipitation shield is
    associated with the interaction of Tropical Storm Helene and an
    upper low centered near western TN. Drier air noted in WV imagery
    being ingested into Helene is impinging into an axis of higher
    boundary layer theta-e air over NC, driving local ascent to help
    to reinvigorate convection within this moist plume. PWs measured
    by GPS are generally 1.9 to 2.4 inches, nearing daily records,
    with U/A soundings featuring deep moist-adiabatic lapse rates to
    support efficient warm-rain processes. Instability is severely
    limited west of the Appalachians as noted via the SPC RAP
    analysis, but a ribbon of MLCAPE approaching 1000 J/kg over NC is
    slowly advecting westward on impressive 850mb SE inflow of 40-50
    kts.

    The evolution the next few hours is somewhat uncertain across this
    region due to CAM disagreement, but the models appear to be
    under-analyzing the current convective regeneration along the
    theta-e gradient across NC. This suggests that the overlap of
    ascent and thermodynamics is still robust, and sufficient to drive
    new convection to the NW through the aftn. The pronounced 850mb
    inflow should help advect the higher instability NW as well, which
    will support an expansion of rain rates which the HREF
    neighborhood probabilities suggest have a 20-40% chance of
    exceeding 1"hr at times. Mean storm motions will remain
    progressive on 0-6km winds of around 40 kts, but the accompanying
    850mb wind evolution will also result in collapsing and veering
    Corfidi vectors to become more anti-parallel to the flow
    indicating an increased potential for backbuilding and training.
    While the CAMs disagree on the greatest risk area for heavy
    rainfall this aftn, there is a 90% chance for 1"+ and 10-30%
    chance for 3+" of rain in both the HREF and REFS ensembles where
    the most pronounced training occurs.

    Much of this area has seen heavy rainfall the past 24-hrs reaching
    1-2" in the lower OH VLY and as much as 4-6" in SW VA. This
    suggests that the most vulnerable soils will remain in the terrain
    of the Appalachians of WV/VA and far eastern KY, but even into the
    OH VLY 3-hr FFG has fallen to around 1.5", and HREF FFG
    probabilities indicate a 20-50% chance of exceeding these values.
    While the greatest risk for flash flood impacts will be in the
    Appalachians atop the most saturated soils, any training could
    cause flash flooding into the evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4omrvPxFtolww6G2BzTDPQAYMxMUGNsW76EE3xIbu6Wu_zyaBoWT_l1x4nLoC3RZAmDM= TUoM0yEMkXX8UP1QWgWlX4c$ for graphic product...

    ATTN...WFO...GSP...ILN...JKL...LMK...MRX...RAH...RLX...RNK...

    ATTN...RFC...LMRFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 39508400 39448269 39058161 38338063 37347964=20
    36577943 36027944 35767998 35838043 36218101=20
    36748170 37198252 37818367 38168437 38278454=20
    38588491 39098472=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 27 21:31:19 2024
    AWUS01 KWNH 272131
    FFGMPD
    DEZ000-MDZ000-VAZ000-NCZ000-280201-

    Mesoscale Precipitation Discussion 1079
    NWS Weather Prediction Center College Park MD
    530 PM EDT Fri Sep 27 2024

    Areas affected...Southeast VA, eastern MD, far southern DE

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 272130Z - 280201Z

    Summary...Clusters of showers and thunderstorms with 2-3"/hr rain
    rates continue to lift northward this evening. Through training,
    these rates could produce 2-3" of rain with locally higher
    amounts. Flash flooding is possible.

    Discussion...The regional radar mosaic early this evening shows a
    cluster of thunderstorms lifting northward out of far northeast
    North Carolina towards Richmond and as far north as the Middle
    Peninsula of VA. These thunderstorms are lifting northward on mean
    0-6km winds of around 40 kts, so remain progressive, but are
    containing MRMS measured hourly rainfall accumulations of 2-2.5
    inches. These impressive rain rates are being fueled by an axis of
    tropical moisture characterized by PWs of 2-2.4 inches, above the
    daily maximum for the region according to the SPC sounding
    climatology, funneling northward around the periphery of what is
    now Post-T.C. Helene over Kentucky. An axis of SBCAPE exceeding
    500 J/kg is collocated with this PW plume, providing rich
    thermodynamics to support continued convection as ascent persists
    through 850mb wind convergence, modest upper jet diffluence, and a
    weak shortwave impulse rotating within the flow. This heavy rain
    has already resulted CREST unit streamflow responses above 500
    cfs/smi, leading to multiple active FFWs.

    The high-res CAMs differ in their evolution the next few hours,
    but the latest NAMNest appears to be handling the current
    convective activity the best, followed by the recent run of the
    HRRR which has caught onto to the eastward shift. These runs
    suggest convection will persist as it heads north, but will begin
    to encounter weaker instability into MD/DE. Some of this will be
    offset by thermodynamic advection as low level 850mb inflow pushes
    higher PW and instability to the north, but in general this should
    result in a slow wane of the intensity of this convection. This is
    reflected as well both by HRRR 15-min rainfall accumulations and
    HREF neighborhood probabilities for 1-hr rainfall exceeding 1"
    peaking around 20%. However, as propagation vectors veer to become
    more aligned into the more rich thermodynamics, this could result
    in short-term backbuilding and training to lengthen the duration
    of these rain rates leading to corridors of rainfall that could
    reach 2-3" in some areas.

    As long as the intense rain rates persist, they will pose a risk
    for flash flooding. However, much of eastern MD and DE has been
    dry recently, leading to elevated FFG that only has a 5-10% chance
    of being exceeded. This suggests the greatest risk for any impacts
    will be across SE VA, or where any training can move across an
    urban area through the evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!58W3cin_F4YkP2J__5_J-CiJOa7wa4Omsm_-6tOtquI9E3w5FH3fx4cjnChviSZyme61= z-NO63IO2h5zNFfqtn0m3WA$ for graphic product...

    ATTN...WFO...AKQ...LWX...PHI...

    ATTN...RFC...MARFC...SERFC...NWC...

    LAT...LON 38937572 38847530 38727506 38427502 38047501=20
    37617524 37267557 36987568 36677580 36407595=20
    36147616 36107656 36277695 36557747 37127763=20
    37707746 38437693 38827659 38927623=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 28 15:21:38 2024
    AWUS01 KWNH 281521
    FFGMPD
    FLZ000-281930-

    Mesoscale Precipitation Discussion 1080
    NWS Weather Prediction Center College Park MD
    1120 AM EDT Sat Sep 28 2024

    Areas affected...Southwest Florida

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 281520Z - 281930Z

    SUMMARY...Training convection tracking northeast into the west
    coast of Florida is producing rates to 2.5 inches per hour. Flash
    flooding is possible, especially in urban areas.

    DISCUSSION... The remnant trailing front behind Helene is nearly
    stationary across central Florida this morning. Localized
    convergence zones have developed within the broader frontal
    boundary that have been forcing storms that have a history of
    producing rainfall rates to 2.5 inches per hour. While each
    individual cell is moving along at around 20 mph, the
    redevelopment of convection is resulting in multiple cells moving
    across urban and flood-prone areas. PWAT values to 2.5 inches are
    draped across the Ft. Myers area, with a distinct moisture
    boundary over the Tampa area. SBCAPE values are over 2,500 J/kg
    with MUCAPE over 3,000 J/kg already.

    These very high values of both moisture and instability will
    support additional thunderstorm development into the afternoon
    across the Florida Gulf Coast. HiRes guidance has been variable on
    how long the storms will last, but given the ample moisture and
    instability both in place and will continue to be advected in from
    the Gulf, it appears probable that the storms capable of heavy
    rainfall rates will continue in this region. Given some of the
    CAMs guidance that are struggling to depict the activity going on
    right now are the drier solutions, have opted to favor the wetter
    guidance such as the 12Z HRRR and ARW for the near-term forecast.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8NOzAGnQK_Ymn8rhoRarwBOyVyP5WpUO6cob4aHz_1UFaJzjVQ8Tq1Szu9-dyOnVR7_1= 6YVqY_81uO_PJibE70iu5_c$ for graphic product...

    ATTN...WFO...MFL...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 28258185 27958140 27528123 26688140 26358172=20
    26398198 26508229 27558281 27808287 28108287=20
    28198256=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 29 17:44:25 2024
    AWUS01 KWNH 291744
    FFGMPD
    MDZ000-VAZ000-NCZ000-WVZ000-OHZ000-TNZ000-KYZ000-292300-

    Mesoscale Precipitation Discussion 1081
    NWS Weather Prediction Center College Park MD
    143 PM EDT Sun Sep 29 2024

    Areas affected...Central Appalachians

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 291743Z - 292300Z

    Summary...Clusters of showers and thunderstorms will develop and
    lift northward through the afternoon. Rainfall rates of 1-2"/hr
    within these cells could repeat to produce 1-3" of rainfall. This
    occurring atop pre-saturated soils may result in instances of
    flash flooding.

    Discussion...The regional radar mosaic this afternoon shows
    widespread light showers across the Ohio Valley and Mid-Atlantic,
    with embedded convective elements beginning to blossom across
    VA/WV. This convective activity is deepening in response to a
    ribbon of 500-1000 J/kg of SBCAPE which has expanded across the
    area south of a wedge front and north of a stationary front. PWs
    of 1.5-1.7 inches, or above the 90th percentile according to the
    SPC sounding climatology, are contributing to intensifying
    thermodynamics to support this convective activity. Forcing for
    ascent is additionally intensifying downstream of an upper low
    over KY, with SE 850mb winds of 10-15 kts lifting isentropically
    and orographically to combine with upper divergence and
    diffluence.

    As the aftn progresses, the high-res CAMs are in good agreement
    that convective coverage will expand in response to the increasing
    ascent within the favorable thermodynamics. Although coverage will
    likely remain scattered, aligned Corfidi vectors and mean 0-6km
    winds suggests repeating rounds of convection are likely in many
    areas. These thunderstorms will likely intensify through the aftn
    as well to produce rainfall rates for which both the HREF and REFS
    neighborhood probabilities indicate have a 40-50% of exceeding
    1"/hr, and 15-min HRRR fields indicate an isolated potential for
    2"/hr rates. Despite the progressive and scattered nature of these
    cells, multiple rounds lifting N/NW into the area could produce
    rainfall amounts of 1-3" in some areas.

    This region has been saturated recently, noted by 7-day rainfall
    departures from AHPS that area in most areas 300-600% of normal.
    This has led to fully saturated soils and compromised FFG that is
    as low as 0.75-1.5" in 3 hours. The HREF FFG exceedance
    probabilities peak as high as 70% by this evening, highest in the
    vicinity of Shenandoah NP and into the Allegheny Mountains.
    However, flash flooding will be possible anywhere the most intense
    rates repeat atop the saturated soils or across vulnerable terrain.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5tyMelmmVF7n88FDockXczyN7XEko1ADrfkvKXVVWSxA1IUbf-vVuPhKDK20snOiGBUR= 9tFNj56tN_Y3DUjIjjnURn8$ for graphic product...

    ATTN...WFO...AKQ...ILN...JKL...LWX...MRX...PBZ...RLX...RNK...

    ATTN...RFC...LMRFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 39688000 39577916 39057841 38017819 36697888=20
    36398001 36428122 36648186 37068204 37588244=20
    37798310 38078343 38628344 39078263 39468140=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 29 22:51:32 2024
    AWUS01 KWNH 292251
    FFGMPD
    MDZ000-VAZ000-WVZ000-300400-

    Mesoscale Precipitation Discussion 1082
    NWS Weather Prediction Center College Park MD
    651 PM EDT Sun Sep 29 2024

    Areas affected...Central Appalachians

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 292250Z - 300400Z

    Summary...Showers and thunderstorms are expected to increase in
    coverage and intensity during the next few hours. Rainfall rates
    within thunderstorms could reach 1-2"/hr, resulting in axes of
    1-3" of rain with locally higher amounts. Flash flooding is
    possible.

    Discussion...The regional radar mosaic this evening indicates that
    convective coverage is finally beginning to expand and intensify
    across parts of Virginia. This is occurring in response to a slow
    rise in favorable thermodynamics noted by the SPC RAP analysis of
    SBCAPE reaching above 500 J/kg, coincident with PWs that are above
    the 90th climatological percentile at 1.6-1.8 inches. Into this
    overlapping moisture/instability, ascent is intensifying through
    height falls and divergence downstream of an upper low positioned
    over KY, topped by modest LFQ upper diffluence, and in the
    presence of 15 kts of 850mb inflow out of the SE. Not only is this
    inflow advecting the more robust thermodynamics northward into
    VA/WV, it is also increasing ascent through convergence along the
    nose of these higher wind speeds and through both isentropic and
    orographic response to this wind trajectory. Rainfall rates within
    the stronger convection have produced MRMS measured 1-hr rainfall
    over 1 inch in southern VA.

    Although the guidance has been a tad aggressive with convective
    intensity this aftn, likely due to a slower increase in favorable
    instability, the recent radar returns suggest this evolution is
    beginning. The convection over southern VA should continue to
    expand and then push N/NW on 0-6km winds that will gradually back
    from SW to S at 15-20 kts through the evening. This evolution is
    supported by most available high-res models, and despite the
    generally progressive motion of cells, repeating rounds are likely
    as storms regenerate into the stronger thermodynamics and pivot
    northward. The HREF neighborhood probabilities for 1"/hr (2"/hr)
    rain rates peak this evening above 60% (20%), greatest in the
    higher terrain where orographic lift will enhance the rainfall
    intensity. Where storms can regenerate and repeat, these rain
    rates could result in 1-3" of rain, with locally higher amounts
    possible as progged by 10-15% HREF/REFS neighborhood probabilities
    for 5"/6hrs.

    This area has been saturated with heavy rainfall that has been 3
    to as much as 8 inches according to AHPS 7-day rainfall. This has
    led to compromised FFG and 0-10cm RSM from NASA SPoRT that is
    generally above 70%. Any heavy rain rates moving atop these
    sensitive soils could quickly become runoff leading to instances
    of flash flooding, but this appears most likely in the vulnerable
    terrain from the Blue Ridge through the Allegheny Mountains.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Z26pDTsDC_CfmR6kII5vahQlRmluBqy0MaMUOFnwP0CYQBTTt4t8mZ2TGYj8lEUYn2B= BqWuIl_emAL9eJatlXBqRjU$ for graphic product...

    ATTN...WFO...AKQ...LWX...PBZ...RLX...RNK...

    ATTN...RFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 39497924 39307868 38947824 38087791 37337793=20
    36797818 36617867 36577921 36697990 37368065=20
    37578109 38098128 39198033=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 30 04:14:35 2024
    AWUS01 KWNH 300414
    FFGMPD
    VAZ000-NCZ000-WVZ000-301010-

    Mesoscale Precipitation Discussion 1083
    NWS Weather Prediction Center College Park MD
    1213 AM EDT Mon Sep 30 2024

    Areas affected...east-central VA/NC border into central VA and far
    eastern WV

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 300412Z - 301010Z

    Summary...Heavy rain showers are expected to maintain a flash
    flood threat for portions of VA into WV over at least the next 3-6
    hours. Rainfall rates of 1 to 2+ in/hr are expected, overlapping
    with wet antecedent grounds.

    Discussion...Regional radar imagery at 0345Z showed an axis of
    showers extending from the foothills of the Blue Ridge Mountains
    in central VA, southeastward to the east-central VA/NC border
    between I-85 and I-95. These showers were warm-topped, only -5 to
    -15C on "clean channel" infrared imagery with collision and
    coalescence processes dominating and have been rather efficient
    despite the fact that the bulk of the available instability is
    weak and limited to the 0-6 km AGL layer (via 00Z RNK/IAD and RAP
    analysis soundings). MLCAPE was only a few hundred J/kg but
    precipitable water values were estimated via 03Z SPC mesoanalysis
    data to be 1.6 to 1.9 inches. It appears low level convergence
    (925-850 mb) was playing a role in the location of these showers
    with some degree of isentropic/orographic ascent aiding in lift.

    Short term forecasts of instability from the RAP indicate only
    gradual weakening and low level convergence of southeasterly winds
    to slowly shift north over the next 3-6 hours. Rainfall rates have
    been observed locally over 2 in/hr and similar potential will
    exist overnight with slow moving and repeating showers likely to
    continue, though some weakening should be expected where
    instability is lower or decreases with time.

    Much of the area still contains lower flash flood guidance due to
    wet antecedent conditions due to rainfall over the past week.
    Therefore, while perhaps not widespread in coverage, at least a
    localized flash flood threat will be likely to continue into the
    night with rainfall rates of 1 to 2+ in/hr at times. Additional
    storm totals may exceed 3 inches on an isolated basis.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7HhKlGoGFEHs219g6UzHep1ggd8hE1jfE2QHhsckvMD8v7RBCZ8qXVJORjQlUqtAZbw8= AYb6HvN_FyW-RLQDqXT4DI4$ for graphic product...

    ATTN...WFO...AKQ...LWX...RAH...RLX...RNK...

    ATTN...RFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 38757826 38247779 37147703 36477710 36337764=20
    36437820 37157878 37297994 37728022 38337988=20
    38737935=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 5 09:07:48 2024
    AWUS01 KWNH 050907
    FFGMPD
    TXZ000-051500-

    Mesoscale Precipitation Discussion 1089
    NWS Weather Prediction Center College Park MD
    507 AM EDT Sat Oct 05 2024

    Areas affected...Deep South Texas...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 050910Z - 051500Z

    SUMMARY...Persistent highly saturated, unstable onshore flow may
    support periods of scattered efficient showers/thunderstorms
    capable of 2-2.5"/hr rates and localized 3"+ totals. Given
    recently wetted grounds, additional intense rainfall may result in
    possible flash flooding this morning.

    DISCUSSION...Large scale cyclonic gyre centered in southern Gulf
    of Mexico/Western Bay of Campeche has seen a persistent convective
    flare up throughout the evening. The broader easterly to
    northeasterly flow has been persistent through the overnight
    period and brought some transistory but intense tropical
    showers/thunderstorms across Deep South Texas. The solid 15-20kts
    of onshore surface to boundary layer flow has been transporting
    .95-1.1" precipitable water in that layer per CIRA LPW. RAP
    analysis shows small surface heating over 80F over high 70s Tds
    and fairly saturated deep moisture profile to support unstable air
    with SBCAPEs of 1500-2500 J/kg to support stronger updraft
    strength and further vertical moisture flux to support efficient
    rainfall production. Rates of 2-2.5"/hr will remain probable
    throughout the morning, much as as they have for the last 6 hours
    or so. Spots of up to 1.5-3" have been observed between Bayview
    and Harlingen matching RADAR estimates, so values higher to the
    northeast over Laguna Madre and S Kenedy county nearing 4-5" seem
    plausible.=20

    The area has been fairly dry and FFG values suggest that this
    rainfall was able to be infiltrated fairly well, but now upper
    soil profiles from this 1-3" total will have reduced FFG values
    which are in the 2-3"/hr, 2.5-4"/3hr should be lowered. Over the
    next six hours, the environment will remain very similar and
    GOES-E 3.9um SWIR shows upstream shallow convective roll-clouds
    moving through the northeasterly flow in the NE Gulf that start to
    grow vertically near the coast given enhanced frictional speed
    convergence. As such, similar transient thunderstorms with
    2-2.5"/hr rates capable of 3-5" localized totals may continue
    through the later morning hours, especially as low level flow may
    increase under influence of the stregthening convective
    cluster/surface reflection east of Tampico, MX. Winds may back a
    bit more out of the NE, enhancing convective potential across E
    Willacy and Cameron counties. HREF probability of exceeding 3" by
    15z are 40-60% with 5" values near 25%. So with each passing
    convective cell, the potential for localized flash flooding
    increases slightly as longer term totals reach/exceed 5",
    especially near urban locales.=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8hmTe7dJX7P45WsANlAz34Z0BUNVW0ohsrw7BXkxUm3ffxcgfVf9AbnldJupXx0P4hGD= ljLRRPxn6fZPq0eg9n7HfMk$ for graphic product...

    ATTN...WFO...BRO...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 26789776 26749731 26409718 25979710 25819736=20
    25989777 26059827 26259843 26619820=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 5 19:50:59 2024
    AWUS01 KWNH 051950
    FFGMPD
    FLZ000-060149-

    Mesoscale Precipitation Discussion 1090
    NWS Weather Prediction Center College Park MD
    350 PM EDT Sat Oct 05 2024

    Areas affected...portions of southern FL & the Keys

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 051949Z - 060149Z

    Summary...Showers and thunderstorms with heavy rainfall are
    showing minimal movement across southern FL. Hourly rain totals
    to 3" with local totals to 6" possible over the next several hours.

    Discussion...Showers and thunderstorms are forming near sea breeze
    boundaries and in the proximity to a warm front draped across
    southern FL. Precipitable water values are 2.25-2.5". Low level
    inflow as well as the mean 850-400 hPa flow is weak, which is
    leading to minimal movement to activity across the southern tip of
    the peninsula and southwest FL. Other activity lurks near the
    Middle and Upper Keys. ML CAPE is approaching 2000 J/kg which is
    being aided by afternoon insolation.

    The concern is that with minimal cell movement that amounts which
    were seen south of Florida City and west of Key Largo could
    materialize across southwest FL and the Keys through the remainder
    of the afternoon into the early evening, with radar estimates near
    6". Areas of the West Coast in particular have been especially
    wet this year with large, in places 20"+, annual surpluses.=20
    Rainfall over the past week has continued this theme between Cape
    Coral and Naples. Hourly rain totals to 3" with local totals to
    6" remain possible into this evening, which could lead to flash
    flooding of urban areas and important thoroughfares, such as US 1,
    US 41, and I-75.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6wdggIxSWYv3WcBR5q0w5nDqxxgfUIsmbL4f_hRw6b-Am8lGnS7fQmlk98a0wghrMSF0= uW4BKvJe9iD1atTC6dfHMr8$ for graphic product...

    ATTN...WFO...KEY...MFL...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 26888208 26508120 25408019 25008035 24708113=20
    26428217=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 6 14:40:50 2024
    AWUS01 KWNH 061440
    FFGMPD
    FLZ000-062030-

    Mesoscale Precipitation Discussion 1091
    NWS Weather Prediction Center College Park MD
    1039 AM EDT Sun Oct 06 2024

    Areas affected...Southern Florida Peninsula

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 061439Z - 062030Z

    Summary...Slow moving showers and thunderstorms with high rainfall
    rates of 2 to 3 inches per hour are showing minimal movement
    across portions of South Florida. Localized rainfall totals up to
    5 inches are possible through 430 pm, and this will likely result
    in some instances of flooding.

    Discussion...Numerous showers and thunderstorms are forming near
    sea breeze boundaries and in the general proximity of a stationary
    front situated across southern Florida late this morning, and also
    ahead of a mid-level vortmax that is slowly approaching the
    southwest coast of Florida. Anomalous precipitable water values
    on the order of 2.3 to 2.6 inches are in place, per recent SPC
    mesoanalysis. Another concern is the very slow cell movements
    that have been observed by regional Doppler radar imagery over the
    past several hours, and this will likely remain the case going
    into the afternoon hours, with weak low level inflow and mean
    850-300 hPa flow. In addition, mixed layer CAPE is on the order
    of 1500-2000 J/kg, which is being aided by midday solar insolation.

    The latest CAM guidance suite depicts an increase in slow moving
    convection across the southern half of the Florida Peninsula
    through the mid-late afternoon hours, with localized rainfall
    totals on the order of 4 to 6 inches possible. Areas of the West
    Coast have picked up a few inches of rain over the past 24 hours,
    and this also holds true for areas near and to the south of Miami,
    and this will be an aggravating factor for flooding potential
    today. Hourly rain totals to 3 inches are possible, which will
    likely lead to some instances of flash flooding for urban and poor
    drainage areas.

    Hamrick

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4DwTbjyxM4wmD9Fetm4TQTSU7ZNS27xGAeZ5caSE9IDroOxcn-Jbfodt26kOvWnlfg2l= eSHVU7Mf1JUsviG94L0gvk0$ for graphic product...

    ATTN...WFO...KEY...MFL...MLB...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 27728071 27568016 26987993 26117990 25518007=20
    25088030 24818064 25048121 25608163 26128211=20
    26528230 26938256 27188265 27228266 27428259=20
    27428213 27308167 27388128=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 7 03:14:01 2024
    AWUS01 KWNH 070313
    FFGMPD
    FLZ000-070900-

    Mesoscale Precipitation Discussion 1092
    NWS Weather Prediction Center College Park MD
    1113 PM EDT Sun Oct 06 2024

    Areas affected...Southern Peninsular Florida and the Upper Keys...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 070315Z - 070900Z

    SUMMARY...Approaching surface frontal wave with bands of warm
    advective tropical showers/thunderstorms capable of 2-2.5"/hr
    rates and spots of 3-5" totals along the coasts may pose localized
    urban rapid inundation flooding through overnight hours.

    DISCUSSION...GOES-E 3.9um SWIR depicts a few boundary layer swirls
    of Cu and TCu across the eastern Gulf of Mexico (main one near
    25.8N 85.5W) with the frontal/convergence boundary extending
    eastward to just offshore of S Sarasota county before paralleling
    the SW Coast through the central Keys. VWP and RADAR mosaic
    suggests a 925-850mb wave in proximity of Naples, pressing
    eastward. This is spurring an increase in low level southwesterly
    flow and warm advection from the Florida Channel and enhancing
    convergence with new deepening convection through the central Keys
    starting to arch northeastward. Relative maxima in low level
    instability and available moisture along/ahead of this band are
    running about 2000-2500 J/kg SBCAPE and 1.05-1.25" per CIRA LPW
    values. This will allow for solid low level moisture loading for
    intense tropical rain showers and be capable of an easy 2-3"/hr
    rain rate, but translation/duration will be critical to pose
    flooding problems.

    As the aforementioned wave crosses southern FL, WAA and
    southwesterly flow is expected to lift north and replace the band.
    Deeper layer (700-500mb) flow appears to suggest weak ridging to
    delay or allow the wave to pivot across the Everglades while the
    band lifts north. This will bring stronger cells along/through
    areas of Miami-Dade with those high rates through the next few
    hours. There is potential the band will slow and increase
    duration near the pivoting wave over the urban corridor and
    present increasing duration of heavier rainfall totals with 3-5".=20
    HREF probability of 40-80% of 3" and 30-50% of 5" remains across
    the southern tip and up the east coast to Palm Beach county.=20=20
    Given a secondary boundary/theta-e gradient is also connected to
    a prior wave/WAA exists resulting in localized frictional
    convergence across Broward county lifting north potentially adding
    to/expanding the risk area of potential 3-5" totals by 09z. Given
    proximity to urban/flat and some already saturated areas, rapid
    inundation flooding may occur locally with these cells through the
    overnight period and is considered possible.

    Along the SW FL coast...
    The potential for excessive rainfall/higher totals, is diminished
    slightly compared to the SE FL coast as cells are more likely to
    reside along/just offshore through the overnight period. However,
    there remains solid convergence along the southeast angled frontal
    zone to support similar cells from Manatee to Lee/Charlotte county
    and with limited cell motions, so though the cells are likely to
    remain just offshore, there remains some potential for 2-2.5"/hr
    rates but could result in slightly higher overall totals if they
    sneak ashore.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9_7cGQdvrEw7ej5aqDEy8Z5IxL-XzFWS6mFU4daM6-UoumjKkf6Lm_uXSparPF6aTtcP= 87H0kDMJREFSlW_QoFuAcN4$ for graphic product...

    ATTN...WFO...KEY...MFL...MLB...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 27228016 26577992 25867999 25218020 24738081=20
    24798129 25718143 25828178 26208193 26538231=20
    26988253 27178260 27198225 26408162 26028113=20
    26028075 26568050 27178040=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 7 17:38:14 2024
    AWUS01 KWNH 071738
    FFGMPD
    FLZ000-072300-

    Mesoscale Precipitation Discussion 1093
    NWS Weather Prediction Center College Park MD
    137 PM EDT Mon Oct 07 2024

    Areas affected...southern FL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 071735Z - 072300Z

    Summary...Slow moving and training thunderstorms will pose a flash
    flood risk for southern FL through 22Z. Due to the environment,
    rainfall rates will easily have the potential for 2-3 in/hr, and
    may even exceed 3 in/hr on a localized basis.

    Discussion...While the exact placement is a little uncertain, 17Z
    surface observations showed a quasi-stationary front extending
    southwestward into Palm Beach County, through the northern
    Everglades before curving westward into the eastern Gulf near
    Naples. Local 88D radar and visible satellite imagery showed
    multiple mesoscale lows near and south of the front, while
    infrared imagery showed two areas of colder cloud tops, one west
    of the Lee Island Coast and the other west of the Lower Keys, that
    have been progressing eastward over the past few hours. Out ahead
    of these two relatively larger scale areas of lift were a couple
    of slow moving cells that have recently developed over northern
    Broward and southern Palm Beach counties. The environment near and
    south of the front consisted of 500-2000 J/kg MLCAPE (highest to
    southwest) and precipitable water values of approximately 2.3 to
    2.5 inches via 12Z sounding and 17Z SPC mesoanalysis data.

    Using the 850-300 mb layer as a proxy for storm motions, mean cell
    movement will be from the SW to WSW at 10-20 kt. Similarly
    oriented 850 mb winds of about the same magnitude will promote
    slow moving and training of cells over the southwestern and
    southeastern coasts into the Keys. Near the coast of St. Lucie and
    Martin counties, low level winds were from the east just north of
    a low located just above the surface (925-850 mb) where 850-300 mb
    mean winds were weakest across the region at 5-10 kt. Therefore,
    the northern Treasure Coast will have the potential for slow
    moving to stationary cell movement near the coast given sufficient
    instability in place.

    Much of southern FL will see an increase in thunderstorm coverage
    over the next couple of hours with potential for 2 to 3+ in/hr as
    forcing increases from the west, beneath a diffluent flow pattern
    in the upper levels. Flash flooding will be possible through 23Z,
    but is expected to remain localized and focused across urban
    corridors.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6St79PkaIYKxNPJYGEZgQtXgyMVzLF8UKjelGPZQcmv-8MCktKYgp0fK5LPEITxZGZkv= Zjt_qZH2tQSIIIiTj-GFRZ0$ for graphic product...

    ATTN...WFO...KEY...MFL...MLB...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 27298033 27227985 26377972 25308004 24628070=20
    24468159 24568189 24818201 25328171 26018214=20
    26448225 26728193 26458152 26378109 26398077=20
    26608041 27028044=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 7 23:16:48 2024
    AWUS01 KWNH 072316
    FFGMPD
    FLZ000-080500-

    Mesoscale Precipitation Discussion 1094
    NWS Weather Prediction Center College Park MD
    716 PM EDT Mon Oct 07 2024

    Areas affected...southern FL into the Keys

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 072314Z - 080500Z

    Summary...There is potential for a training axis of heavy rain to
    begin to impact portions of the southern FL Peninsula into the FL
    Keys by 03-06Z. Rainfall rates of 2 to 3+ in/hr will be possible,
    which may lead to flash flooding over impervious surfaces.

    Discussion...23Z surface observations, radar imagery and fading
    visible satellite imagery showed a quasi-stationary front
    extending east to west across the southern FL Peninsula with an
    apparent low on the front or at least the front aloft, located
    north of Grand Bahama Island. A secondary smaller low was noted
    just east of the Martin/Palm Beach County border, possibly
    connected to the front at the surface or just aloft.

    Low level easterly flow just north of the smaller low near the
    east coast of FL was helping to support locally heavy rain near
    and just east/offshore of Port Saint Lucie where a small bubble of
    500 J/kg MLCAPE was estimated via the 22Z SPC mesoanalysis. The
    coastal circulation may translate southward in the short term as
    the larger low to the north of Grand Bahama is forecast by short
    term RAP guidance to strengthen and become better organized
    tonight. This strengthening should result in increased northerly
    flow over the southern FL Peninsula, pushing the front southward
    toward the Middle and Upper Keys by 06Z. Farther southward
    progress of the front will likely be limited by southwesterly flow
    to the east of yet another surface low analyzed in the eastern
    Gulf near 26.4N 84.4W.

    The front is expected to act as a focus for the development of
    heavy rain where MLCAPE is forecast to be 1000+ J/kg along and
    south of the boundary, dropping off to less than 100 J/kg to the
    north. Mean steering flow should be roughly parallel to the
    boundary allowing for the repeating and training of cells, with
    rainfall rates possibly reaching 2 to 3+ in/hr within the tropical
    environment. These rates could overlap with localized urban
    centers and related impervious surfaces of the Middle/Upper Keys
    leading to localized flash flooding.

    Regarding the HRRR, while it has been fairly consistent with the
    idea of an axis of heavy rain developing in the vicinity of
    Florida Bay, the HRRR has struggled with placement of heavy rain
    from earlier today and has had differences in its forecast
    placement of the surface front and associated low pressure centers
    leading to lower confidence in its output. While the idea of
    recent HRRR cycles seems reasonable, some of its runs with 6 hr
    QPF maxima of 7 to 10 inches appears overdone.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!81lBakZcqkxyAMrt_INC1yfVMaUzPP5fc9MXMIQFQ-iTJJAHBu6jBnIu54Iq8EFzB4-n= yJu8lK0_FM9l0Uikwv_NxUI$ for graphic product...

    ATTN...WFO...KEY...MFL...MLB...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 27508019 27488009 27367996 27277992 27017985=20
    26607975 25927983 25387993 24768044 24468117=20
    24508196 25668170 25798099 26208030 26878038=20
    27248040 27418036=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Oct 8 05:54:53 2024
    AWUS01 KWNH 080554
    FFGMPD
    FLZ000-081145-

    Mesoscale Precipitation Discussion 1095
    NWS Weather Prediction Center College Park MD
    154 AM EDT Tue Oct 08 2024

    Areas affected...Florida Keys & Far Southern Florida Peninsula...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 080555Z - 081145Z

    SUMMARY...Favorable environment for training thunderstorms in
    vicinity of Florida Keys. While hard to hit, solid potential for
    2-3"/hr rates and spots of 4-6" totals. If intersecting,
    accompanying rapid inundation flooding is considered possible
    through morning.

    DISCUSSION...Surface and remote sensing suite depicts a developing
    surface low to the NW of Grand Bahama westerly winds pressing the
    front off southern Florida, before the front orients flat east to
    west across the Florida Bay before angling northwest along the
    coast to a shearing out and retrograding low near 25.6N 83.6W.=20
    VWP from BYX and AMX depict this stretching axis across the
    southern peninsula with unidirectional deep layer flow supporting
    a WSW to ENE training axis across the area of concern.
    GOES-E SWIR and RAP winds suggest broader but confluent warm
    advective low level flow regime along the spine of the Keys into
    Florida Bay with ample deep layer moisture AoA 2.5" with ample low
    level profile to support narrow skinny profile with solid unstable
    air given values of 2000-2500 J/kg. As such the strong low level
    convergence is supporting bands of developing CBs from upstream of
    Dry Tortugas through the area before strongest convergence resides
    just southwest of the base of the frontal zone where some sfc
    southwesterly flow is at or about 15-20kts supports stronger
    moisture flux convergence.=20=20

    The placement of features: isallobaric response to the growing
    complex in the eastern Florida Straits, retrograding low will
    support continual convergence upstream redevelopment and training
    profile to allow for thunderstorms to track through the Keys into
    far southern Florida for the next few hours. Given ample moisture
    flux, rates of 2-3"/hr are possible per Hi-Res CAMs. Solid
    probability from 00z HREF suggest 3-5" suggest the training cells
    have sufficient proximity to land that any intersection may result
    in localized totals in short enough duration to allow for rapid inundation/urban style flooding.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9KEv30E6oKWRUEGlbTyMneIR31mCoNLL99BX_pk2BEo6xgwVKx7J-M4I1KiHtNR3L3tZ= HQo-fHdrInhoUVRv8wYDH7o$ for graphic product...

    ATTN...WFO...KEY...MFL...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 25648022 25508014 25288021 25128032 24688089=20
    24518151 24528188 24708171 24938110 25078109=20
    25318121 25508099 25538062=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Oct 9 07:00:21 2024
    AWUS01 KWNH 090700
    FFGMPD
    FLZ000-091230-

    Mesoscale Precipitation Discussion 1096
    NWS Weather Prediction Center College Park MD
    259 AM EDT Wed Oct 09 2024

    Areas affected...Southwest Florida....

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 090700Z - 091230Z

    SUMMARY...Potential for coastal training rotating thunderstorms
    capable of 2.5"/hr rates and spots of

    DISCUSSION...06z surface analysis along with BYX VWP and RADAR
    animation shows winds have veered to more southerly, increasing
    starting to increase WAA, lifting the stalled boundary across
    southeast Gulf/Florida Bay northward. Upper 70s to lower 80s
    temp/dewpoints along the Florida Straits and the strengthening
    speed convergence with this warm air advection is allowing for
    increased instability advection northward expanding 2500+ J/kg
    SBCAPE values northward along the coastal boundary.

    SPC MCD and bulk shear values suggest main mode of shallow
    rotating thunderstorms along this band. While mean steering flow
    and approaching isallobaric influence would press cell motions
    further west, rotation and right movement is generally
    counteracting this influence and supporting a generally north or north-northeast cell motion for these thunderstorms allowing for a
    solid potential for training development given upstream moisture
    convergence in proximity of the lifting boundary and coastal
    frictional convergence may allow for this.

    While updrafts are narrow, the rotational flow increases speed and
    directional moisture flux into the updrafts allowing for intense
    low level moisture loading and therefore intense rainfall
    production. Overall moisture of 2.25-2.5", though clearly loaded
    in the sfc to 700mb layer will support efficient production with
    hourly rates of 2-3"/hr though inner cores will likely drive the
    majority of that rain in sub-hourly time frames (15-30 minutes)
    further increasing the potential for rapid inundation flooding
    across the flat/urban ground conditions. This is further
    compounding potential issues given recent moderate to heavy
    rainfall. NASA SPoRT 0-40cm soil moisture is well above normal at
    70-80% capacity and generally above 95th percentile for the time
    period.=20

    Much of the Hi-Res guidance suite does not place this warm
    advective training band ashore, but most have assimilated this
    band much further west than current trends would suggestion, with
    recent HRRR solutions slowly adjusting to RADAR with the 05z run
    getting closest, so far. So, while the band still may align
    along/just offshore with the most intense cores/training axis, the
    risk for this training band crossing the urban coastal zones has
    increased enough to suggest spots of 2-5", resulting in possible
    localized inundation flooding through early morning.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6ZhrXxQKLYOmd2Z2CcDQiyjY58k2Hra9IlNEoDNtq_WFl7MXVFPgqDvBYjqez6LiMERH= qUtWo8XjlKpl9BGDj5QMMIc$ for graphic product...

    ATTN...WFO...MFL...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 27488254 27148203 26648165 26078099 25338037=20
    25178105 25848176 26328196 26478225 27108255=20
    27348270=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Oct 9 07:13:23 2024
    AWUS01 KWNH 090713
    FFGMPD
    FLZ000-091230-

    Mesoscale Precipitation Discussion 1096...Corrected
    NWS Weather Prediction Center College Park MD
    311 AM EDT Wed Oct 09 2024

    Corrected for Summary statement

    Areas affected...Southwest Florida....

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 090700Z - 091230Z

    SUMMARY...Potential for coastal training rotating thunderstorms
    capable of 2.5"/hr rates and spots of 2-5" possible through
    morning.

    DISCUSSION...06z surface analysis along with BYX VWP and RADAR
    animation shows winds have veered to more southerly and starting
    to increase WAA, lifting the stalled boundary across southeast
    Gulf/Florida Bay northward. Upper 70s to lower 80s temp/dewpoints
    along the Florida Straits and the strengthening speed convergence
    with this warm air advection is allowing for increased instability
    advection northward expanding 2500+ J/kg SBCAPE values northward
    along the coastal boundary.

    SPC MCD and bulk shear values suggest main mode of shallow
    rotating thunderstorms along this band. While mean steering flow
    and approaching isallobaric influence would press cell motions
    further west, rotation and right movement is generally
    counteracting this influence and supporting a generally north or north-northeast cell motion for these thunderstorms allowing for a
    solid potential for training development given upstream moisture
    convergence in proximity of the lifting boundary and coastal
    frictional convergence may allow for this.

    While updrafts are narrow, the rotational flow increases speed and
    directional moisture flux into the updrafts allowing for intense
    low level moisture loading and therefore intense rainfall
    production. Overall moisture of 2.25-2.5", though clearly loaded
    in the sfc to 700mb layer will support efficient production with
    hourly rates of 2-3"/hr though inner cores will likely drive the
    majority of that rain in sub-hourly time frames (15-30 minutes)
    further increasing the potential for rapid inundation flooding
    across the flat/urban ground conditions. This is further
    compounding potential issues given recent moderate to heavy
    rainfall. NASA SPoRT 0-40cm soil moisture is well above normal at
    70-80% capacity and generally above 95th percentile for the time
    period.=20

    Much of the Hi-Res guidance suite does not place this warm
    advective training band ashore, but most have assimilated this
    band much further west than current trends would suggestion, with
    recent HRRR solutions slowly adjusting to RADAR with the 05z run
    getting closest, so far. So, while the band still may align
    along/just offshore with the most intense cores/training axis, the
    risk for this training band crossing the urban coastal zones has
    increased enough to suggest spots of 2-5", resulting in possible
    localized inundation flooding through early morning.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!616dJne68gZ0FK_N9zgLgg56Pwl21KkvT_oB9F_yiRk3kKVe4nDWG2nubPu104knwJLI= a-9Y3lAxgViYxvDHe-_P0fk$ for graphic product...

    ATTN...WFO...MFL...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 27488254 27148203 26648165 26078099 25338037=20
    25178105 25848176 26328196 26478225 27108255=20
    27348270=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Oct 9 14:35:30 2024
    AWUS01 KWNH 091435
    FFGMPD
    FLZ000-092000-

    Mesoscale Precipitation Discussion 1097
    NWS Weather Prediction Center College Park MD
    1034 AM EDT Wed Oct 09 2024

    Areas affected...eastern FL Peninsula

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 091433Z - 092000Z

    Summary...Slow moving showers and thunderstorms with rainfall
    rates between 1-3 in/hr are expected to pose a flash flood threat
    to the eastern FL Peninsula from east of Lake Okeechobee to
    Jacksonville. Additional rainfall totals of 2-4 inches through 20Z
    will be possible, but likely remaining localized.

    Discussion...14Z regional radar imagery showed a slow moving axis
    of heavy rainfall located in northeastern FL between Saint
    Augustine and Palm Coast, extending inland about 25 miles. Peak
    observed rainfall rates have been between 1-2 in/hr but the
    persistent slow moving nature of the rainfall has led to 2 to 4+
    inch rainfall totals since midnight, but with much of that falling
    over the past 4 hours. Another axis of heavy rain was occurring
    near Cape Canaveral with a northward movement observed, but with
    redevelopment and repeating from the south. Easterly winds of
    20-30 kt at 925 mb were contributing to low level axes of
    confluence, helping to focus the ongoing axes of heavy rainfall
    with mean steering flow from the south. Aloft, a strong upper
    level jet axis was located along the southern Mid-Atlantic coast
    with right entrance region ascent contributing to lift across the
    FL Peninsula.

    SPC mesoanalysis and RAP data showed a relative minimum in
    instability between the two ongoing axes of heavy rainfall that is
    forecast to persist over the next 3-5 hours, but the environment
    remained highly favorable for heavy rain with precipitable water
    values of 1.8 to 2.3 inches. Short term forecasts from the RAP
    indicate the northern confluence axis slowly edging northward
    through 20Z, possibly affecting the Jacksonville metro into the
    early afternoon. Farther south, development of
    showers/thunderstorms is expected from near northern Palm Beach
    County toward the Cape Canaveral region with slow northward
    translation but with regeneration and repeating from the south
    within the confluent flow. Additional rainfall totals of 2-4
    inches are expected through 20Z over portions of the eastern
    Peninsula, though cannot rule out localized additional totals over
    4 inches. Localized flash flooding will be possible, especially
    with overlap of urban corridors.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6m7X87byyiaCT1Dr08_3nVnvIw0masfV791yzaHZzyjV37yAQCDg8hjjNow46ed4PunT= cxMDIdnO2ekeFdMgl4UCWV0$ for graphic product...

    ATTN...WFO...JAX...MFL...MLB...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 30628125 29988090 28528033 27297993 26858053=20
    26948101 27528132 28138176 29118216 29668215=20
    30088200 30548181=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Oct 9 15:18:30 2024
    AWUS01 KWNH 091518
    FFGMPD
    FLZ000-092100-

    Mesoscale Precipitation Discussion 1098
    NWS Weather Prediction Center College Park MD
    1117 AM EDT Wed Oct 09 2024

    Areas affected...western FL Peninsula

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 091516Z - 092100Z

    Summary...A powerful outer rain band is expected to reach the west
    coast of FL over the next 1-2 hours. Rainfall rates of 2 to 3+
    in/hr will be possible where training occurs and flash flooding
    will be likely. Additional banding and heavy rain is likely to
    continue into the mid-afternoon, increasing the coverage of flash
    flooding.

    Discussion...15Z radar imagery from KTBW showed an outer rain band
    ahead of Hurricane Milton just offshore from Englewood to Naples.
    This powerful outer rain band has been edging closer to the coast
    and is expected to reach the coastal population centers from south
    to north over the next 1-2 hours. Due to the slow eastward
    movement of this band, peak MRMS-derived rainfall rates have been
    estimated at 2 to 2.5 in/hr offshore. As Milton continues to track northeastward toward the west coast of FL through 21Z, this outer
    band is expected to rotate inland and northward, bringing rainfall
    rates of 2-3 in/hr at times along the coast from near Tampa Bay to
    Charlotte Harbor.

    The outer rain band will likely followed by a temporary lull in
    heavy rainfall as it moves through, given a minimum in colder
    cloud tops on infrared satellite imagery between the band and the
    center of Milton. However, additional heavy rain will develop as
    subsequent bands associated with Milton form and move ashore. The
    15Z NHC advisory from NHC indicates Milton is moving toward the
    northeast at 15 kt, with the center forecast to be located about
    30 miles off the coast of Sarasota County at 00Z. Areas along the
    coast will be must susceptible to flash flooding over the next few
    hours given the urban nature and wet antecedent conditions
    including 1-2 inches of rain since midnight. Peak additional
    rainfall through 21Z of 3-5 inches will be possible with areas of
    flash flooding becoming likely.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!48k5BXyZi85lbruWbGFxuULkO0pPJvFTZJbdF8QQ4jRHoBBDhuEfpYhpIBfV_nRVkGb3= hPOPuqIonChvQNJ0gqq_hn4$ for graphic product...

    ATTN...WFO...MFL...MLB...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 28858251 28568204 27708163 26598143 25908133=20
    25688148 25748190 26418248 27238292 27988310=20
    28638278=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Oct 9 20:23:04 2024
    AWUS01 KWNH 092022
    FFGMPD
    FLZ000-092345-

    Mesoscale Precipitation Discussion 1099
    NWS Weather Prediction Center College Park MD
    422 PM EDT Wed Oct 09 2024

    Areas affected...central FL Peninsula

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 092018Z - 092345Z

    SUMMARY...Numerous areas of flash flooding are expected through
    00Z across the central FL Peninsula, including the I-4 corridor
    between Tampa and Orlando, and eastward toward Cape Canaveral.
    Rainfall rates of 2 to 3+ in/hr along with 3-hr rainfall totals of
    3 to 6 inches are likely.

    DISCUSSION...Hurricane Milton continued to approach the west coast
    of FL at 20Z, located about 100 miles SW of Tampa per the 20Z
    update from NHC. Dry air wrapping around from the west into the
    southern side of the circulation has contributed to relatively
    warmer cloud tops on IR imagery in the southern semicircle.
    Reflectivity data from KTBW confirmed this with a lack of higher
    dBZ values south of the center. Meanwhile, several bands of heavy
    rain have been merging into a broader area of torrential rainfall
    between the eye and the southern portion of Tampa Bay. To the
    east, an impressive and long-lived outer rain band was located
    from eastern Lake Okeechobee into the I-4 corridor, near a remnant
    frontal boundary which extended west-east across the central
    Peninsula between roughly a SRQ to MLB line with the elevated
    portion of this convergence axis just north. The low level
    convergence axis delineated MLCAPE values of 500-1500 J/kg to its
    south from values less than 500 J/kg to its north. Aloft, water
    vapor imagery inferred strongly diffluent/divergent flow aloft
    over the Peninsula between a strong jet max over the Mid-Atlantic
    coast and Milton.

    As Milton continues to approach the coast, while gradual weakening
    is still anticipated, an axis of very heavy rain is likely to set
    up just north of the center from the Tampa Bay vicinity, eastward
    toward Orlando and Cape Canaveral, following the low level
    convergence axis. This is confirmed via experimental WoFS output
    showing 50-80 percent probabilities of exceeding 5 inches from the
    19Z cycle over Pinellas County, and 40-60 percent probabilities
    farther east into Polk County through 00Z. Rainfall rates within
    this axis are expected to peak in the 2 to 3 in/hr range within
    areas of training but with localized hourly totals in excess of 3
    inches possible along with 3-hour totals in the 3-6 inch range.
    Given the expected location of this heavy rainfall axis
    overlapping high density population centers including Tampa and
    Orlando, significant areas of flash flooding with life-threatening
    impacts will be possible.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4JcPGw1PvptyXwlwNwMt1eeRCRkIFW603v86RFK7yeO8PCrijh3wFDOHLUZi4KeebhC2= 2aRYj7cBZRreAYV9drQH6TQ$ for graphic product...

    ATTN...WFO...JAX...MFL...MLB...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 29198115 29148080 28008013 27118000 26968067=20
    27228147 26898244 27358297 27828305 28478277=20
    28758243 28978184=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Oct 9 23:31:11 2024
    AWUS01 KWNH 092331
    FFGMPD
    FLZ000-100445-

    Mesoscale Precipitation Discussion 1100
    NWS Weather Prediction Center College Park MD
    730 PM EDT Wed Oct 09 2024

    Areas affected...north-central FL Peninsula

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 092328Z - 100445Z

    SUMMARY...An axis of extreme rainfall, stretching from the Tampa
    metropolitan region northeastward into the north-central FL
    Peninsula, is expected to result in major to locally catastrophic
    flash flooding with considerable threats to life and property.
    6-hr rainfall totals of at least 5-8 inches with hourly rainfall
    in the 2-3 in/hr range are expected.

    DISCUSSION...The 23Z update from NHC placed the center of
    Hurricane Milton 35 miles WSW of Sarasota, FL. Local radar imagery
    at 23Z from KTBW showed the heaviest rain located within what is
    effectively the northern eyewall which has pushed ashore and arced
    from Manatee into southern Hillsborough and much of Pinellas
    counties with MRMS and gauge data showing 1-2 in/hr rainfall
    rates. Portions of St. Petersburg to Bradenton have already picked
    up 5-8 inches of rain since midnight and flash flooding is
    ongoing. Farther east, an outer rain band had largely moved
    offshore of the eastern Peninsula but was arcing northwestward
    ashore just north of Cape Canaveral with 4-8 inches already
    reported across Brevard County.

    An axis of strong low level convergence tied to the northern
    eyewall, extending northeast from the center of Milton to Volusia
    County (just north of the forecast track of Milton) will support a
    prolonged period of high rainfall rates, 1-2 in/hr but locally in
    the 2 to 3+ in/hr range, with the axis training from WSW to ENE
    and slowly lifting north with time. Some locations could
    experience rainfall rates in excess of 1 in/hr for 2-4 hours,
    causing rapid rises of water above the surface as water will not
    have sufficient time to drain, especially across the mostly
    impervious surfaces of the St. Petersburg into the Tampa metro and
    possibly nearing Orlando later tonight. Additional rainfall of at
    least 5-8 inches is expected from St. Petersburg, northeastward
    into the central Peninsula where the WoFS has consistently painted
    high probabilities of exceeding 5 inches of rainfall. The 22Z WoFS
    cycle indicated 50 to 90 percent probabilities of 5+ inches and
    90th percentile (reasonable worse case scenario) values of 7-10
    inches. Major to locally catastrophic flash flooding is expected
    as a result of these high rainfall rates.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6gKF48B965Xqj-Jzk3hFPNzyaeldajk6aK1Bj6zQ7DDIysUYY_DgBDtRhDbDLz8puFHb= LiIRC4UVxA39mwYPAM3Wb8k$ for graphic product...

    ATTN...WFO...JAX...MLB...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 29888111 29688103 28598054 28528063 28238143=20
    27798205 27438295 27898313 28898262 29318212=20
    29678163=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Oct 10 04:34:44 2024
    AWUS01 KWNH 100434
    FFGMPD
    FLZ000-101045-

    Mesoscale Precipitation Discussion 1101
    NWS Weather Prediction Center College Park MD
    1231 AM EDT Thu Oct 10 2024

    Areas affected...portions of North-Central FL

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 100445Z - 101045Z

    Summary...Locally catastrophic flash flooding likely to continue
    as Hurricane Milton moves across the Florida Peninsula with
    2-3"/hr rainfall rates and 3-8" additional totals.

    Discussion...Hurricane Milton is progressing across the central FL
    Peninsula at this hour, undergoing extratropical transition in the
    process with heavy rainfall confined to the northern half of the
    circulation. Convection associated with Milton remains intense,
    largely due to this extratropical transition process (and the
    associated strong upper-level divergence from the right entrance
    region of a 140+ kt jet streak off the Northeast coast). GOES-East
    infrared imagery indicates cloud top temperatures of -85deg C or
    colder, along with multiple lightning strikes via the GLM
    instrument. This corresponds to estimated cloud top heights of
    40-50k feet (via KTBW/MRMS echo top data), and this continues to
    support significant tropical rainfall rates of 2-3"/hr (with
    precipitable water values at record breaking levels of 2.4-2.7
    inches).

    Hi-res models are in good agreement in keeping the remnant of the
    northern eyewall of Milton convectively active until its emergence
    over the Atlantic in the next 4-6 hours. This will bring the 50
    mile wide swath of 2-3"/hr rainfall rates from the
    Lakeland/Orlando metro areas northeastward into more rural
    portions of the peninsula between Orlando and Jacksonville, as
    well as into coastal cities such as Daytona Beach, Palm Coast, and
    St. Augustine. This will result in an additional 1-3" of rainfall
    in the vicinity of Lakeland/Orlando (where 6-12" of rainfall has
    already fallen over the past 12 hours), and an additional 3-8"
    over adjacent portions of the northeastern peninsula and coastal
    cities (where 2-4" has already fallen over the past 12 hours).
    Flash flooding (some locally catastrophic) will continue in the
    hard-hit areas of Lakeland/Orlando, while flash flooding is likely
    to continue and expand to those areas towards the northeast (which
    may also experience locally significant to catastrophic flash
    flooding).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!62KuibCvgzzgD5po1BTLbB2g4j0IWIy2wowkA6k0YwjMv_2VqqCqDR6bYKIVNnn4tUjs= D56zLGZoxgxjmcl9lQ6EQ54$ for graphic product...

    ATTN...WFO...JAX...MLB...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 30088126 29498102 28748065 28448090 28128151=20
    27938209 28378240 29238219 29618188 29978159=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 12 19:17:16 2024
    AWUS01 KWNH 121917
    FFGMPD
    FLZ000-130115-

    Mesoscale Precipitation Discussion 1102
    NWS Weather Prediction Center College Park MD
    315 PM EDT Sat Oct 12 2024

    Areas affected...South FL and the Keys

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 121915Z - 130115Z

    SUMMARY...Slow-moving bands of very heavy showers and
    thunderstorms are expected to overspread portions of especially
    southeast FL and the middle and upper FL Keys going through the
    remainder of the afternoon and evening hours. Some urban flash
    flooding will be possible.

    DISCUSSION...The latest GOES-E IR satellite imagery in conjunction
    with dual-pol radar is showing a gradual increase in very heavy
    shower and thunderstorm activity across the FL Straits which has
    been gradually lifting north-northeastward over the last few
    hours. A subtle/weak mid-level shortwave impulse is seen
    approaching the region and this energy coupled with the
    interaction with an inverted surface trough near the southeast
    coast of the FL Peninsula has been facilitating the development of
    some semi-organized bands of deeper convection.

    There has been an uptick in instability across far southern FL and
    in the upper portions of the Keys where MLCAPE values have risen
    to 500 to 1000 J/kg. An increase in low-level moisture convergence
    has been noted as well close to the coast, and this coupled with
    the aforementioned shortwave energy/deeper layer ascent and
    proximity of 30 to 40 kts of effective bulk shear should tend to
    maintain a threat for relatively organized bands or clusters of
    heavy showers and thunderstorms going at least into the evening
    hours.

    PWs are close to 2 inches and have been tending to rise throughout
    the day, and this coupled with the shear and instability should
    help drive some very efficient convection with high rainfall rates
    that may reach 1.5 to 2.5 inches/hour.

    The heavier rainfall threat should tend to overall stay over the
    Keys and coastal areas of southeast FL where the better
    instability is, but some of these bands of heavy showers and
    thunderstorms may impact some of the urbanized I-95 corridor of
    southeast FL including Fort Lauderdale and Miami, and also Rt. 1
    down through Homestead.

    Rainfall amounts of 3 to 5 inches cannot be ruled out in the
    middle and upper FL Keys, with the urbanized areas of southeast FL
    farther north seeing 2 to 4 inches. If any training of these
    slow-moving bands of convection can occur, it will be possible for
    locally heavier totals. These rains are expected to drive a threat
    for some urban flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9InmYdy9fRYuxNC7ADUSjuvKbnwR1mBXXhHE2fiEXaZZ2xJGK32QCcNavtNyjsHXWvBY= HDzq_Jqxmv9vUHbl2Fzkij4$ for graphic product...

    ATTN...WFO...KEY...MFL...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 26667994 26028000 25388020 24728061 24668118=20
    24898128 25228098 25838059 26608025=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 19 05:12:13 2024
    AWUS01 KWNH 190512
    FFGMPD
    COZ000-NMZ000-191110-

    Mesoscale Precipitation Discussion 1103
    NWS Weather Prediction Center College Park MD
    110 AM EDT Sat Oct 19 2024

    Areas affected...Central to Northeast NM...South-Central CO

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 190510Z - 191110Z

    SUMMARY...A localized threat for flash flooding will develop going
    through the overnight hours as greater concentrations of heavy
    shower and thunderstorm activity occurs. The burn scar locations
    will be most susceptible to runoff concerns.

    DISCUSSION...A deep upper-level trough and associated closed low
    over the Southwest U.S. will be moving very slowly down to the
    southeast overnight. This will favor downstream areas of central
    and eastern NM seeing an uptick deep layer ascent as divergence
    aloft overspreads the region. Coinciding with this will be the
    persistence of an increasingly moist southeast low-level jet of 30
    to 40 kts which will be advancing up across eastern NM. The
    overall PW environment currently is rather modest with PWs near
    0.75 inches, but the latest CIRA-ALPW data shows a notable fetch
    of moisture in the SFC-850 mb layer advancing gradually north and
    west across the TX High Plains which eventually will become more
    entrenched over eastern NM later tonight and Saturday morning.

    MUCAPE values are on the order of 500 to 1000+ J/kg across
    portions of central and eastern NM currently, and this coupled
    with the deeper layer ascent and moisture transport from the TX
    High Plains and Rio Grande Valley should favor a gradual increase
    in the coverage of heavy showers and thunderstorms. This will be
    mainly focused in a southwest to northeast fashion from central to
    northeast NM and to some extent over parts of south-central CO.

    The latest hires CAM guidance suggests more increase in the
    coverage and intensity of convection over the next few hours, and
    radar imagery in conjunction with GOES-E IR satellite imagery
    shows several clusters of fairly well-organized cold-topped
    convection already evolving across the region.

    Rainfall rates with the stronger pockets of convection overnight
    may reach as high as 1 to 1.25 inches/hour, and given some
    potential for localized cell-training, some rainfall totals may
    reach as high as 2 to 3 inches. This will especially be the case
    over the orographically favored Sangre De Cristo Mountains.

    A localized threat for some flash flooding will exist with the
    burn scar locations generally the most susceptible to seeing
    runoff problems. In particular, the Hermits Peak/Calf Canyon burn
    scar area in the Sangre De Cristo Mountains will be at risk for
    impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9t6GemCbgfS6ZnVadRJDe0JuwfzOxNQVOKUxeZhIUAIeb7IGRiJo8QoHkiXDmKZj6TiI= nmO8CfIe_bhki7gm0xhwv-4$ for graphic product...

    ATTN...WFO...ABQ...PUB...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 37580437 37210381 36580373 35620403 34870454=20
    34670502 34780561 35050594 35720606 36220606=20
    36670589 37090559 37430507=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 19 18:09:26 2024
    AWUS01 KWNH 191809
    FFGMPD
    NMZ000-192330-

    Mesoscale Precipitation Discussion 1104
    NWS Weather Prediction Center College Park MD
    208 PM EDT Sat Oct 19 2024

    Areas affected...central to east-central NM

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 191806Z - 192330Z

    SUMMARY...Localized flash flooding will be possible across
    central/east-central NM through 23Z. Rainfall rates of 0.5 to 1.5
    in/hr and 15 minute rates locally over 0.5 inches are expected
    within repeating/training regions of thunderstorms.

    DISCUSSION...18Z water vapor imagery showed a well-defined closed
    low over AZ, with only slow movement observed over the past 6
    hours. Upper level flow to the east of the closed low was fairly
    diffluent over NM with possible added lift occurring within the
    left-exit region of a weakly defined jet streak located on the
    south to southeast side of the closed low. MRMS-reflectivity has
    shown the recent development of a SSE to NNW oriented axis of
    stronger echoes over Lincoln into Torrance County, located on the
    western edge of an axis of 500-1000+ J/kg MLCAPE as depicted on
    the 17Z SPC mesoanalysis.

    Throughout the afternoon, greater insolation with breaks in cloud
    cover and continued southeasterly low level moisture transport
    will help to support an expanding coverage of 500 to 1500 J/kg
    MLCAPE over central to eastern NM as depicted by recent runs of
    the RAP, with the greatest instability over southeastern portions
    of the state. The increased instability and low level convergence
    on the eastern side of the closed low will likely contribute to
    increasing thunderstorm coverage through 23Z. The greatest concern
    for flash flood potential will exist along and just east of the
    southern Sangre de Cristo and Sacramento Mountains. While forecast
    LFC-EL mean flow of 30-50 kt from the south will keep individual
    cells moving, deep-layered southerly flow will allow for repeating
    and short-term training of cells at times, supporting localized
    hourly rainfall of 0.5 to 1.5 inches and 15-minute rates over 0.5
    inches.

    The southeast facing slopes of the southern Sangre de Cristo
    Mountains have received 2 to 3+ inches of rain, much of that over
    the past 12 hours, increasing soil moisture. While other areas of
    NM have seen less than an inch over the past 24 hours, localized
    potential for flash flooding will exist where higher intensity
    rainfall repeats over the same location, especially with any
    overlap of sensitive burn scar locations or flashy creeks/streams.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9cCkAtwuCgz9kCxaZfuzdpFSkckHH3TQgvmNlepUS0VF0gtzIFd_wB4vXseyR8NcLsKS= QkQ2A0NVUAQkTjLiMAK2Rzw$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...ABRFC...CBRFC...WGRFC...NWC...

    LAT...LON 36610437 36170409 35520412 33920435 32820478=20
    32500555 32500611 33100636 34680642 35800697=20
    36290701 36530678 36560631 36470601 36350589=20
    36230577 36160549 36200542 36300520 36420509=20
    36500487=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 19 19:38:56 2024
    AWUS01 KWNH 191938
    FFGMPD
    WAZ000-200400-

    Mesoscale Precipitation Discussion 1105
    NWS Weather Prediction Center College Park MD
    338 PM EDT Sat Oct 19 2024

    Areas affected...Olympic Peninsula into the northern Cascades

    Concerning...Heavy rainfall

    Valid 191936Z - 200400Z

    Summary...An ongoing atmospheric river is expected to produce an
    additional 2-4 inches over the upslope regions of the Olympic
    Peninsula and northern Cascades through 04Z. Hourly rainfall rates
    in excess of 0.5 inches will be possible for several hours (mainly
    the Olympics) with 36 hour rainfall totals of 4-8 inches.

    Discussion...GOES West water vapor imagery showed an elongated
    fetch of mid-upper level moisture streaming northeastward, ahead
    of a shortwave trough, located near 44N 150W, into the West Coast
    from southern Vancouver Island into northwestern WA. Layered PW
    imagery showed this atmospheric river contained high moisture
    content throughout the vertical column and Blended TPW data
    indicated the moisture values within the plume were 150 to 200+
    percent of normal. Moisture flux anomalies have weakened since 00Z
    when the moisture axis was directed into southern Vancouver
    Island, which has received over 10 inches of rain (preliminarily)
    according to information from the NWS Weather and Hazards Data
    Viewer, but high rainfall rates remained within the axis of
    strongest moisture transport where peak precipitable water values
    were near 1.5 inches along the coast. Recent observations across
    the western Olympic Peninsula showed hourly rainfall between 0.3
    and 0.5 inches, but with localized hourly totals in excess of 0.5
    inches across western Clallam and Jefferson counties.

    19Z visible satellite imagery and surface observations depicted a
    cold front extending southwestward from north-central Vancouver
    Island into the eastern Pacific. The cold front is forecast to
    continue slowly moving toward the south and east over the next 6-9
    hours, with continued hourly rainfall over 0.5 inches across the
    western Olympic Peninsula through at least 00Z.

    2 to 4+ inches of rain has been reported across the upslope
    regions of the Olympics and northern Cascades over the past 24
    hours. Additional rainfall totals of 2 to 4 inches are expected
    though about 04Z, with rainfall intensity lowering between 00-03Z
    as the moisture axis sinks south with the cold front and weakens.
    This weakening will be in advance of the upstream shortwave near
    150W, which is expected to re-align the offshore moisture axis in
    a more south to north orientation, ahead of a forecast surface low
    which is expected to approach northwestern WA after 12Z Sunday.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!85k5u--1SAM-u15faPCmct_U3BsrStafCNJPaWJ8UepJ04RcD7a4qLUgxITtBYwN5A4j= zXsKUI6TPSjZHIW9TpBgvWg$ for graphic product...

    ATTN...WFO...OTX...SEW...

    ATTN...RFC...NWRFC...NWC...

    LAT...LON 49002159 48952134 48882120 48782109 48642104=20
    48452102 48252108 48062115 47922120 47782128=20
    47632142 47542158 47572178 47732192 47962197=20
    48122204 48212222 48272240 48322257 48312279=20
    48302297 48172322 47942328 47772331 47522329=20
    47442332 47272340 47142381 47142429 47852471=20
    48312470 48432438 48622323 48992208=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 19 23:29:30 2024
    AWUS01 KWNH 192329
    FFGMPD
    NMZ000-200515-

    Mesoscale Precipitation Discussion 1106
    NWS Weather Prediction Center College Park MD
    728 PM EDT Sat Oct 19 2024

    Areas affected...eastern NM

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 192327Z - 200515Z

    SUMMARY...A south to north axis of heavy rain is likely to
    generate widely scattered to scattered flash flooding across
    eastern NM into the early overnight hours. Training/repeating
    cells are expected to produce 1 to 1.5+ in/hr rainfall rates
    leading to additional 2-4 inch totals through 05Z.

    DISCUSSION...Regional radar and GOES East visible imagery at 23Z
    showed a broken axis of thunderstorms extending from southwestern
    Chaves County, north-northeastward into southeastern Colfax
    County, containing several areas of overshooting tops. These
    storms were located within an instability axis containing 500 to
    1500+ J/kg MLCAPE and anomalous precipitable water values of 0.7
    to 1.1 inches via 23Z SPC mesoanalysis data. Accounting for
    sufficient wind shear aloft, some cells were organized containing
    mesocyclones and large hail, with trends in MRMS-derived rainfall
    increasing over the past 1-2 hours, currently showing a few areas
    with hourly rainfall in excess of 1 inch. Water vapor imagery
    showed a potent closed upper level low over AZ which has begun to
    slowly fill and was slowly retrograding toward the west, but
    individual vorticity maxima have been revolving about the low
    center with areas of upper level divergence and diffluence east of
    the low center over much of NM. VAD wind data at KFDX and KMAF
    showed 850 mb winds have been increasing as well over the past
    couple of hours, currently near 30 kt from the southeast.

    An axis of low level convergence near a quasi-stationary front
    located at the leading edge of an increasing low level jet is
    expected to maintain a roughly south to north axis of
    thunderstorms across eastern NM through at least 05Z. RAP
    forecasts indicate the magnitude of the 850 mb winds increasing
    over southeastern NM into the 40-50 kt range, with the leading
    edge possibly serving as a focal point for the highest rainfall
    rates. While instability is forecast to wane into the overnight
    with the loss of surface heating, likely contributing to lowering
    rainfall rates later in the night, RAP forecasts indicate at least
    500-1000 J/kg MLCAPE will remain over the east-central to
    southeastern portion of the state through 06Z. Mean steering flow,
    roughly parallel to the axis of low level convergence is expected
    to support repeating rounds and short term training of
    thunderstorms, allowing for 1 to 1.5+ in/hr rainfall rates in
    addition to 2-4 inches of rain along a south to north axis over
    eastern NM.

    It is thought that the heaviest rain will remain east of the
    sensitive burn scars located over the southern Sangre de Cristo
    and Sacramento Mountains through 05Z, however, additional, more
    isolated cells to the west of the main axis of thunderstorms may
    support an isolated flash flood threat within weaker pockets of
    instability, forced by strong dynamic lift east of the AZ closed
    low.

    Areas of flash flooding are considered likely over eastern NM,
    though may remain widely scattered in nature. Storms may propagate
    more to the east of current HRRR guidance but the flash flood
    threat will decrease with eastern extent due to higher FFG values
    toward the TX border.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9qvvrTzyEGHdVp6hoAIxULY2qbMqxx00Djeh1r7RZ3DBWHKMFBy495k6-sQGTkvpkUjc= 56O9wrhA-QGVwRBVO-QlXhI$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36720430 36450338 35750305 33090349 32160431=20
    32120546 32470583 33510612 34530606 35660576=20
    36440507=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 20 04:12:03 2024
    AWUS01 KWNH 200411
    FFGMPD
    TXZ000-NMZ000-201010-

    Mesoscale Precipitation Discussion 1107
    NWS Weather Prediction Center College Park MD
    1210 AM EDT Sun Oct 20 2024

    Areas affected...Eastern NM

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 200410Z - 201010Z

    SUMMARY...Heavy showers and thunderstorms are expected to continue
    to impact portions of eastern NM overnight. Additional areas of
    flash flooding are likely.

    DISCUSSION...The latest GOES-E IR satellite imagery shows a very
    divergent flow regime aloft over eastern NM with an expansive
    canopy of persistent cold convective tops associated with an
    elongated band of heavy showers and thunderstorms. All of this is
    occurring downstream of a rather strong upper-level low that is
    nearly stationary over central AZ.

    MLCAPE values over eastern AZ remain on the order of 500 to 1000
    J/kg out ahead of a quasi-stationary front, but the front is
    helping to focus a strong north/south axis moisture convergence
    which is being facilitated by a southeast low-level jet of 40 to
    50 kts that is persisting across the southern High Plains.

    This enhanced moisture convergence/transport working in tandem
    with the available instability and deep layer ascent downwind of
    the upper low has resulted in some very well-organized convection
    including a few occasional supercell structures this evening that
    have been resulting in locally extreme rainfall rates.

    In fact, Roswell, NM (KROW) picked up 0.73" of rain in just a
    7-minute period between 0148Z and 0155Z. The persistence of this
    extreme rainfall rate led to Roswell seeing 2.70" of rain in one
    hour from 0151Z to 0251Z. This has led to locally catastrophic
    flash flooding impacts, with a Flash Flood Emergency for the city
    of Roswell.

    The instability trends over eastern NM are somewhat negative with
    3-hour differentials in the MLCAPE of -200 to -400 J/kg. This
    suggests that the rainfall rates will likely tend to come down a
    bit in the hours ahead, however, the persistence of deep layer ascent/upper-level jet forcing and the low-level jet yielding
    enhanced moisture flux convergence should tend to compensate and
    help keep rainfall rates still capable of reaching 1.5" to
    2.0"/hour with the stronger cells.

    Some gradual eastward advance of the overall convective rainfall
    axis is expected overnight, but some additional rainfall amounts
    of 3 to 4 inches will be possible locally where any of these cells
    continue to train or backbuild over the same area. As a result,
    additional areas of flash flooding will be likely.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6Erj1W2ZbGyiBF-FSnt-SrG-9xoMutAVM4HNJIbSKgsAMN7kdXXu-NmMmIk8dTvWHuXU= eb0UGL4mjNc6pCwboFNLaog$ for graphic product...

    ATTN...WFO...ABQ...AMA...EPZ...LUB...MAF...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36490328 36060290 35190289 34000322 33170377=20
    32780425 32640496 33090539 33520542 34670525=20
    35840496 36450415=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 21 00:59:20 2024
    AWUS01 KWNH 210059
    FFGMPD
    COZ000-NMZ000-210657-

    Mesoscale Precipitation Discussion 1108
    NWS Weather Prediction Center College Park MD
    858 PM EDT Sun Oct 20 2024

    Areas affected...Eastern NM

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 210057Z - 210657Z

    SUMMARY...Localized training of showers and thunderstorms will
    likely result in some additional areas of flash flooding heading
    into the overnight hours. This will especially be the case given
    the wet antecedent conditions across the region.

    DISCUSSION...The latest GOES-E IR satellite imagery shows a closed
    upper low near the Four Corners region gradually beginning to
    shift off to the northeast. Divergent flow aloft ahead of the
    upper low associated with DPVA will be combining with a moderately
    unstable airmass over areas of eastern NM for locally broken
    coverage of heavy showers and thunderstorms heading into the
    overnight hours.

    MLCAPE values of 1500 to 2000 J/kg are in place which combined
    with a belt of 30 to 40 kts of effective bulk shear should yield a
    threat for locally organized bands of multicell convection and
    potentially a few supercells that will be capable of producing
    heavy rainfall rates. The PWs over eastern NM are quite moist and
    running 2 to 2.5 standard deviations above normal.

    The more organized pockets of convection may produce rainfall
    rates of 1.5 to 2.0 inches/hour, and given the environment that is
    conducive for some cell-training, there may be some rainfall
    totals going through 06Z that reach as high as 2 to 4 inches. This
    is generally consistent with the 18Z HREF guidance and reflects
    the expectation that there may be some additional uptick in the
    coverage of convection over the next few hours.

    Given the wet antecedent conditions over the region from recent
    heavy rainfall, some additional areas of flash flooding are likely
    heading into the overnight hours. This will also include a concern
    for burn scar impacts over portions of the Sangre De Cristo
    Mountains.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5MJ2sADZY9EmaYcnp_5h7RATo0dNis5ipsVUN-_hPtKQoCM-ueCzRVzqpwrrd3U7P-dk= RO0El7kihgwyWI15CMVS_z8$ for graphic product...

    ATTN...WFO...ABQ...MAF...PUB...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 37130455 37070359 36570311 35120310 33850331=20
    33330382 33240440 33600493 34060511 34960540=20
    35330598 35790629 36280607 36890540=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Oct 31 18:18:51 2024
    AWUS01 KWNH 311818
    FFGMPD
    MSZ000-LAZ000-TXZ000-010015-

    Mesoscale Precipitation Discussion 1109
    NWS Weather Prediction Center College Park MD
    218 PM EDT Thu Oct 31 2024

    Areas affected...Central & Southern LA...Southeast TX...Ext
    Southwest MS...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 311820Z - 010015Z

    SUMMARY...Potential for a widely scattered incident or two of
    flash flooding is possible through late afternoon into early
    evening hours.

    DISCUSSION...A potent autumn cyclone and associated cold front are
    pressing across the central portion of the U.S, while a strong
    ridge remains entrenched over the Southeast. As such, a solid
    core of return moisture across the central Gulf with total
    Precipitable water over 2.25" is lifting north across Louisiana
    and starting to interact/consolidate within the warm sector ahead
    of the approaching cold front. However, stronger mid to upper
    level jet remains well enough north that front is starting stretch
    and flatten from east to west under these low to mid-level
    shearing forces. Moderately clear skies throughout the morning
    into peak heating across the warm sector has brought temps into
    the mid-80s over low to mid-70s Tds, resulting in a moderately
    unstable environment across SE TX into much of central and
    southern LA with MLCAPEs reaching 1500 J/kg, though nearing 2000
    J/kg further west. This disparity is mainly driven by steepening
    lapse rates and drying mid-levels above 700mb per CIRA LPW and RAP
    analysis; while profiles are more satuated through depth in the
    core of the q-axis from Vermillion to Rapides parish in central
    LA.

    Divergence is maximized at the entrance of the upper-level jet in
    proximity to a weak surface inflection along the pre-frontal
    convergence axis/effective cold front across NW LA, extending
    northward into AR; while weaker flow exists across the Gulf Coast
    proper, the overall confluence through depth (mainly directional)
    is resulting in solid deep layer convergence. GOES-E and regional
    RADAR mosaic has noted a solid increase in convective coverage and
    intensity along the q-axis as well as a few upstream clusters in
    SE TX from Houston to the Sabine River. Effective bulk shear is
    modest to weak but sufficient for some organized structures and
    with deep layer flow from the southwest to the northeast (and
    convergent) cell motions may support occasional repeating/training
    profiles of these clusters. This is likely to be required to
    overcome dry conditions and high FFG values across much of the
    area. Still, available moisture and solid flux should result in
    efficient rainfall production as updrafts broaden in time, adding
    to localized duration and potential for 2" sub-hourly totals.=20

    While FFG values are 3-5"/1-3hrs across the area of concern, 12z
    HREF neighborhood probability of 3"/6hrs (mainly bolstered
    3"/3hrs) is greater than 50% from Brazoria county, TX to West
    Feliciana parish, LA with greater than 25% from Sabine River to
    St. Landry with greatest potential in Evangeline parish. This
    still may only result in widely scattered, low-end instance or two
    of localized flash flooding; however there are a few prone urban
    centers along that axis where scattered spots of 3-4" may occur.=20
    As such, flash flooding is considered possible this afternoon but
    mainly after 21z into this evening.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6n-ejLEnHOG6PoqUDNYEN2ZRXHoBotOpuW1NlaIqP3yng_onEqAHjYo__yKqqnTlUZ12= 1by6IcIG56sR0lS4QZBKW7g$ for graphic product...

    ATTN...WFO...HGX...JAN...LCH...LIX...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 32279173 31729101 30779125 29389127 29649367=20
    29189471 28949525 28999595 29639600 29979574=20
    30639496 31499402 31919331 32189273=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Nov 1 22:12:16 2024
    AWUS01 KWNH 012212
    FFGMPD
    LAZ000-020130-

    Mesoscale Precipitation Discussion 1110
    NWS Weather Prediction Center College Park MD
    610 PM EDT Fri Nov 01 2024

    Areas affected...South-Central LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 012210Z - 020130Z

    SUMMARY...A localized threat of flash flooding will exist through
    the early evening hours from slow-moving areas of heavy showers
    and thunderstorms.

    DISCUSSION...Radar imagery in conjunction with late-day GOES-E IR
    satellite imagery shows a general north/south axis of slow-moving
    showers and thunderstorms impacting some of the parishes of
    south-central LA. The convection is generally aligned in close
    proximity to a surface trough and is embedded within a modestly
    unstable, but moist environment.

    MLCAPE values of 500 to 1000 J/kg are noted along with PWs of 1.75
    to 2 inches, and this has been facilitating some rainfall rates of
    1 to 2 inches/hour with the stronger convective cores.
    Cell-motions though have been rather slow over the last couple of
    hours, and this is favoring some locally heavy storm totals.

    The loss of daytime heating combined with the convective
    overturning process should yield a gradual waning of the diurnal
    instability that is pooled across the region, and this will
    support an eventual weakening of the axis of convection with
    decreasing rainfall rates in time.

    Locally as much as an additional 2 to 4 inches of rain will be
    possible over the next few hours going through the early evening
    hours before the activity weakens. Given some of the rains that
    occurred yesterday, these additional totals may support a
    localized flash flood threat, but any runoff concerns will mainly
    be of the urban variety.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9YEuvS8gngSTPxI8jU8QsFwJP7aQC6OeiLUeUY7GEibCB8aE-UQnYkUMLVM6bQ5XRk0n= U3wXQbzinpsqJ0cilpJ-O7M$ for graphic product...

    ATTN...WFO...LCH...LIX...

    ATTN...RFC...LMRFC...NWC...

    LAT...LON 30929087 30239052 29579057 29469109 30069141=20
    30809146=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 2 04:19:49 2024
    AWUS01 KWNH 020419
    FFGMPD
    TXZ000-NMZ000-020930-

    Mesoscale Precipitation Discussion 1111
    NWS Weather Prediction Center College Park MD
    1219 AM EDT Sat Nov 02 2024

    Areas affected...eastern NM into the western TX Panhandle

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 020417Z - 020930Z

    SUMMARY...A flash flood threat is expected to increase across
    portions of eastern NM into the western TX Panhandle through 09Z.
    Rainfall rates of 1-2 in/hr are expected along with 6-hour totals
    2-4 inches.

    DISCUSSION...Regional radar and GOES East infrared satellite
    imagery has shown an increasing coverage of scattered
    thunderstorms over southeastern NM, between CNM to just northwest
    of CVS since 03Z. Southeasterly low level moisture transport, as
    seen on CIRA Layered PW imagery below 700 mb, was contributing to
    increasing instability over southeastern NM into the southern TX
    Panhandle with 500-1500 J/kg MLCAPE on the 03Z SPC mesoanalysis
    co-located with the ongoing storms. 850 mb winds of 30-35 kt were
    observed via VAD wind data at KMAF with speed convergence and low
    level upslope helping to focus storms.

    Back to the west, an eastward moving upper level trough was
    observed over the southwestern U.S. with lift out ahead likely to
    increase thunderstorm potential across the southern High Plains
    through the remainder of the night. The past few runs of the RAP
    have supported 30-40 kt 850 mb winds broadening over the Permian
    Basin with 40+ kt forecast over the Pecos River Valley in western
    TX developing between 06-07Z. Continued moisture advection should
    allow MLCAPE to expand as well with 500-1500 J/kg becoming more
    widespread across southeastern NM into the western TX Panhandle
    through 08Z. While it is not yet clear precisely where, an axis of
    low level convergence oriented SW to NE or similar to the mean
    steering flow will become better defined tonight, likely allowing
    for repeating and occasional training of thunderstorms, capable of
    producing 1-2 in/hr rainfall rates. Expectations are for 3 to 6-hr
    totals of 2-4 inches which may result in localized flash flooding
    through 09Z from portions of southeastern/east-central NM into the
    western TX Panhandle.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!57sdomWTh_bBJfA-P_ovTBj3LV_z286AyPyu1zucbTYPqUwm8Vu9YAUUBBZBE_ssU_Tm= MNhlia1Tm2xvM23pReqb1LE$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...MAF...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36400148 35040196 33620285 32730365 32320472=20
    32910505 34380481 35300412 35980338 36360268=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 2 09:41:29 2024
    AWUS01 KWNH 020941
    FFGMPD
    TXZ000-OKZ000-NMZ000-021540-

    Mesoscale Precipitation Discussion 1112
    NWS Weather Prediction Center College Park MD
    540 AM EDT Sat Nov 02 2024

    Areas affected...eastern NM into TX Panhandle and western OK

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 020940Z - 021540Z

    SUMMARY...The flash flood threat will continue through 15Z for
    eastern NM into the TX Panhandle and western OK with additional
    rainfall totals of 2-4 inches. While additional areas of flash
    flooding will be likely, coverage is expected to remain isolated
    to scattered.

    DISCUSSION...0915Z radar imagery showed that an axis of
    thunderstorms stretched northeastward from south-central NM into
    the TX Panhandle with 2 to 4+ inches of rain estimated via MRMS
    since 03Z between ROW and AMA near US 70 in NM and US 60 in TX.
    Some recent southeastward bowing was observed to the southeast of
    AMA which has reduced training due to the reflectivity axis
    falling out of alignment with the mean southwesterly steering
    flow. However, greater lift is approaching ahead of an eastward
    advancing shortwave trough axis extending SSW from CO into western
    NM and southeastern AZ with left-exit and right-entrance ascent
    occurring with a pair of developing 100 kt upper level jet streaks
    located over northwestern Mexico and the central Plains.

    Recent RAP forecasts indicate the 40 kt 850 mb southeasterly LLJ
    is at its peak and subtle veering and weakening of the flow is
    expected through 15Z across southeastern NM into western TX.
    Realignment of the low level convergence axis is forecast to occur
    a bit south of its current position as the veering occurs and a
    weakness in magnitude occurs over the TX Panhandle near I-40 as
    seen in RAP output. As the aforementioned shortwave trough
    advances east early this morning some eastward translation to the
    low level convergence axis will be possible, allowing for the axis
    of training heavy rain (1-2 in/hr rainfall rates) to shift south
    and eventually east, out of NM, remaining along the northern edge
    of a plume of 500-1500 J/kg MLCAPE.

    Additional rainfall totals of 2 to 4 inches (locally higher
    possible) are expected in a few locations along the low level
    convergence axis but coverage should remain isolated to scattered
    across the broader region of eastern NM into the TX Panhandle and
    western OK. Therefore, while additional flash flooding will be
    likely, it is not expected to be contiguous across the area
    through 15Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8w5Z6C4V381UeKdmunju8WV7RMesLDcBAXBV8jgfN_M9UNpTxks9uKQpFHPmwd3v4Caa= rjIw10UnJszxdk9DdDRwkKg$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...MAF...OUN...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36620010 36559949 36119924 35569926 34969966=20
    34260065 33780198 33370342 33230420 33530458=20
    34350398 35300280 36020156=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 2 16:37:34 2024
    AWUS01 KWNH 021637
    FFGMPD
    TXZ000-OKZ000-KSZ000-NMZ000-022200-

    Mesoscale Precipitation Discussion 1113
    NWS Weather Prediction Center College Park MD
    1236 PM EDT Sat Nov 02 2024

    Areas affected...Far eastern New Mexico, Texas Panhandle, western
    Oklahoma

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 021635Z - 022200Z

    Summary...Convective cells are expected to regenerate along an
    outflow boundary and track E/NE through the afternoon. Rainfall
    rates in excess of 1"/hr are likely, resulting in axes of 2-3" of
    rain with locally higher amounts. This could result in instances
    of flash flooding.

    Discussion...A longwave trough centered over the Great Basin is
    amplifying this morning as evidenced by RAP height falls across
    that region. This is resulting in sharpening downstream SW flow
    tapping moisture from the Pacific, and PWs of 1.1 to 1.3 inches
    have surged into the TX Panhandle, near daily records for early
    November. Into this moisture, deep layer lift is increasing as
    height falls and divergence downstream of the primary trough axis
    increase, and overlap with an impressively coupled jet structure
    to produce diffluence aloft. This ascent is being enhanced by
    mesoscale lift as low-level southerly flow from south Texas surges
    northward on 850mb winds of 20-30 kts, lifting isentropically atop
    an outflow boundary evident on the regional radar mosaic. Although
    this outflow boundary is progged via hig-res guidance to continue
    to shift progressively E/SE, this isentropic ascent should result
    in regeneration and training of cells through the aftn.

    Rainfall rates in current convection are generally modest, but
    MRMS 1-hr rainfall accumulations suggest isolated instances of
    1-1.5" of rain in the past hour. These rain rates are somewhat
    minimized by a lack of pronounced instability, as the SPC RAP
    indicates a sharp MLCAPE gradient from 250-1000 J/kg across the
    southern TX Panhandle. As the 850mb LLJ continues from the south
    however, there is good agreement that these more robust
    thermodynamics will surge northward, reaching 1000-2000 J/kg this
    aftn. This should result in increased coverage of rainfall rates
    exceeding 1"/hr as progged by both HREF and REFS hourly rain rate probabilities. At the same time, mean 0-6km flow will remain
    around 30 kts from the S/SW, suggesting cells that regenerate
    along the SW portion of this outflow as it stalls will shift N/NE
    and train. This indicates potentially two axes of heavy rainfall:
    one along this SW flank where cells repeatedly develop, and a
    second maxima into western OK where mean flow is more parallel to
    the boundary to enhance training. In both these areas, HREF
    neighborhood probabilities for 3"/6hrs reach 40-50%.

    Somewhat limiting to the flash flood potential today is
    exceptionally dry antecedent conditions reflected by AHPS 30-day
    rainfall that is generally less than 25% of normal, leading to
    NASA SPoRT 0-40cm soil moisture that is around the 10th
    percentile. This suggests that flash flooding should primarily be
    isolated the next several hours, but where any of these 1-2"/hr
    rates train/regenerate, instances of flash flooding will be
    possible.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_sivuCLqYWpUQiub-d02x7hSO9eQHxahb4Oq6eMz4jPq8QnsL-Ao_dEApWdSLfLdFcmJ= C2zuhuEeXPDLEwAeJ1F0xP8$ for graphic product...

    ATTN...WFO...ABQ...AMA...DDC...ICT...LUB...MAF...OUN...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 37109866 36999825 36129816 35579814 34769848=20
    34139894 33380018 33070197 33050336 33220390=20
    33780416 34500396 35100278 35530133 35930028=20
    36599923=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 2 21:01:36 2024
    AWUS01 KWNH 022101
    FFGMPD
    TXZ000-NMZ000-030300-

    Mesoscale Precipitation Discussion 1114
    NWS Weather Prediction Center College Park MD
    500 PM EDT Sat Nov 02 2024

    Areas affected...Far southeast NM into the Permian Basin and
    Rolling Plains of Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 022100Z - 030300Z

    Summary...Discrete thunderstorms blossoming across the High Plains
    of New Mexico will likely expand in coverage and grow upscale into
    clusters through the afternoon. Rainfall rates of 2"/hr or more
    are likely, which through several rounds could cause 2-3" of rain
    with locally higher amounts. Flash flooding is possible.

    Discussion...The regional radar mosaic this afternoon indicates
    that discrete thunderstorms, including supercells, have rapidly
    developed across southeast NM in the past few hours, and have
    expanded into the Permian Basin of Texas. This convection is
    blossoming in response to impressive deep layer ascent driven
    through PVA downstream of a shortwave lifting across the area
    combined with strong upper diffluence within an increasingly
    coupled upper jet structure. In the lower levels, 850mb inflow
    from the S/SE is lifting isentropically atop a weakening outflow
    boundary (which is reflected by a sharp instability gradient),
    while concurrently transporting robust thermodynamics northward
    characterized by PWs of 0.9-1.2 inches, near the daily record, and
    MLCAPE of 1500-2000 J/kg. Rainfall rates within this convection
    has been measured by MRMS as high as 1.25-1.5" in the last hour,
    leading to modest CREST unit streamflow responses already.

    The high-res CAMs appear to generally be under-doing the
    convective coverage this aftn, a theme that has been common
    through the day. This limits somewhat the confidence in the exact
    evolution the next several hours. However, despite coverage and
    timing issues with the guidance, they all agree that eventually
    thunderstorms will expand and grow upscale into clusters. This
    will be supported by a continued increase in deep layer ascent
    impinging into persistently elevated thermodynamics as the
    low-level flow remains. This should result in thunderstorms that
    intensify, supporting rainfall rates which have a 10-20% chance
    (HREF) and 30% chance (REFS) of exceeding 2"/hr through the aftn
    and into the evening. Mean 850-300mb winds are expected to remain
    progressive at 30 kts from the SW, but despite this, as storms
    organize through 0-6km bulk shear of 40-50 kts, intense rain rates
    through short-term training could result in maximum rainfall of
    2-3" with locally higher amounts.

    Far southeast NM, the southern Permian Basin, and the southern Cap
    Rock have all been very dry the past 7 days, but AHPS rainfall
    departures are well above normal north of there. This has lowered
    3-hr FFG to just 1-1.5" across the more saturated soils. As
    convection expands and organizes, it could move across these more
    sensitive soils, leading to potential instances of flash flooding
    into the evening.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9fZYSOBsfKMWwBrnJl09Fu18l1wFuP18o99ZBaEdAOste4iYZ2sOyVBwb40f3S14J5VE= a50tob3cOhtjGvoTB6Ao27U$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...MAF...OUN...SJT...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 35150214 35090174 35030081 34479995 33529946=20
    32739960 32020063 32010225 32340369 32760419=20
    33450422 34390390 35010320=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Nov 3 04:24:43 2024
    AWUS01 KWNH 030424
    FFGMPD
    MOZ000-TXZ000-OKZ000-KSZ000-030930-

    Mesoscale Precipitation Discussion 1115
    NWS Weather Prediction Center College Park MD
    1224 AM EDT Sun Nov 03 2024

    Areas affected...northwestern TX into central/northeastern OK, far
    southeastern KS, far southwestern MO

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 030422Z - 030930Z

    Summary...Areas of flash flooding are expected to develop in a
    zone from northwestern TX into central OK and northeastern OK
    through 09Z. Some spillover into southeastern KS and southwestern
    MO may occur as well. Rainfall rates of 1-2 in/hr and areas of
    training may support localized totals over 4 to 5 inches through
    10Z.

    Discussion...Regional radar imagery at 04Z showed an eastward
    propagating line of thunderstorms tracking across the southern TX
    Panhandle, just east of the Caprock Escarpment. Additional showers
    and thunderstorms were noted across the Red River into much of OK.
    All of this activity was located near or northwest of a remnant
    outflow boundary which extended from near MAF to RPH in TX, then
    northeastward into OK between TUL and OKM. SPC mesoanalysis data
    indicated MLCAPE values were 500-1500 J/kg along and south of the
    outflow boundary, while CAPE dropped off significantly to the
    north of the outflow. 850 mb winds of 35-45 kt from the south were
    present over west-central TX into central/eastern OK, overrunning
    the outflow and forcing convection. Large scale lift was present
    over the region out ahead of a longwave trough axis moving through
    the southwestern U.S. and within the divergent and diffluent
    left-exit region of a prominent 110-130 kt upper level jet max
    streaking across northern Mexico into southwestern TX.

    Broad forcing ahead of the eastward moving upper level trough over
    the Southwest will allow southerly low level winds to maintain and
    locally strengthen over TX/OK tonight, continuing overrunning
    thunderstorms north of the outflow. The outflow boundary itself is
    expected to become more diffuse with time over OK but stay better
    defined over TX, to the south of the eastward advancing line.

    Despite the forward progression of the convective line east of the
    Caprock, mean southwesterly steering flow will align with the axis
    of low level forcing, whether it be the outflow boundary or
    convective lines near/north of the outflow to support training.
    Rainfall rates of 1-2 in/hr (locally higher) are likely to develop
    within areas of training with multiple hours of heavy rain
    possible over a given location.

    Despite mostly dry ground conditions from ongoing drought, high
    rainfall rates over a short period of time are expected to
    overwhelm soils and support areas of flash flooding, with
    localized totals over 4 to 5 inches possible. The flash flood risk
    will be enhanced if these higher rates overlap with urban
    corridors, including the Oklahoma City and/or Tulsa metro.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-ZkYQZkpltbcbSITwUyr7lRNxPu9ZszvZsBo8UfV0cs4d_wCRn8s1Xvo6_3ly43CIlMl= xcbEvFbqWUm700Ae-eRUdrY$ for graphic product...

    ATTN...WFO...FWD...ICT...LUB...MAF...OUN...SGF...SJT...TSA...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 37399543 37189435 36199484 35119577 33759736=20
    33349826 32540053 32530124 32890105 33820040=20
    34779997 36239789=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Nov 3 09:31:18 2024
    AWUS01 KWNH 030931
    FFGMPD
    TXZ000-OKZ000-031500-

    Mesoscale Precipitation Discussion 1116
    NWS Weather Prediction Center College Park MD
    430 AM EST Sun Nov 03 2024

    Areas affected...northern TX into southern OK

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 030929Z - 031500Z

    Summary...An axis of training heavy rain is expected to impact
    portions of northern TX into southern OK through 15Z with rainfall
    rates of 1 to 2+ in/hr. Rainfall totals of 2 to 4+ inches are
    expected through 15Z along with possible flash flooding.

    Discussion...Looping regional radar imagery through 09Z showed a
    QLCS progressing eastward across OK at roughly 40-50 kt but the
    southwestern flank of this convective line has largely stalled
    across northwestern TX, between US 180 and US 380 to the north of
    Abilene. Area VAD winds at 850 mb showed 40-45 kt from the south
    across central to western TX, overrunning the rain-cooled airmass
    where 1000 to 2000+ J/kg MLCAPE was present along and south of the
    outflow boundary (per 09Z SPC mesoanalysis). In addition to the
    low level forcing in place, flow aloft was diffluent and
    divergent, within the left exit region of a RAP-estimated 110-120
    kt upper level jet max crossing Big Bend NP.

    Despite the typical diurnal cycle favoring weakening of the low
    level jet through 15Z, RAP forecasts suggest only slight weakening
    of the 850 mb winds (into the 30-40 kt range) as a shortwave
    trough axis over the southern AZ/NM border translates eastward
    this morning. However, infrared cloud tops have been warming
    across northwestern TX over the past hour, perhaps due to a
    combination of the intrusion of dry air aloft as seen on Layered
    PW imagery and weakening moisture flux.

    Despite the recent weakening, a flash flood threat will remain
    across the Red River Valley over the next few hours as areas of
    training will likely persist into the mid-morning hours with storm
    motions parallel to the low level axis of forcing. The threat for
    training and 1 to 2+ in/hr rates is expected to shift ENE across
    the Red River into portions of southern OK through 15Z along with
    additional rainfall totals of 2 to 4 inches (locally higher).
    Flash flooding will continue to be possible over the next few
    hours with an expected weakening of rainfall intensity and
    training potential toward the end of the MPD valid time (13-15Z).

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8SWgZZWagO723T5X43F4I2cxNKzGTFEXBk3v5gSAT5k1JR2e6gQC8jPncN_CMnario-l= 9iI12I6J3j0vcbkRePX4w9A$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...SJT...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 35269523 35099451 34269451 33389623 32939780=20
    32710002 33489970 34339837 34829718 35079643=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Nov 3 10:18:21 2024
    AWUS01 KWNH 031018
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-031435-

    Mesoscale Precipitation Discussion 1117
    NWS Weather Prediction Center College Park MD
    517 AM EST Sun Nov 03 2024

    Areas affected...southwestern MO, southeastern KS, northwestern
    AR, northeastern OK

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 031016Z - 031435Z

    Summary...A localized occurrence or two of flash flooding will be
    possible across southeastern KS/northeastern OK into the Ozarks
    through 15Z. While an overall weakening trend in flash flood
    potential is expected over the next few hours, rainfall rates of
    1-2 in/hr through training may overlap hydrologically sensitive
    locations, resulting in runoff issues.

    Discussion...10Z radar/satellite imagery showed an MCS tracking
    across eastern OK with a convectively induced vorticity max (MCV)
    inferred across east-central OK. South of the MCV, a convective
    line was rapidly advancing eastward, limiting the threat for
    short-term flash flooding over eastern OK. Farther north, rainfall
    was more stratiform in nature with embedded convective elements.
    Strong lift was occurring across eastern KS/OK within a coupled
    upper level jet exit/entrance region supporting a divergent and
    diffluent regime aloft. Instability was limited however, with
    MUCAPE values of ~500 J/kg or less per 09Z SPC mesoanalysis data.

    Expectations are for the MCV and associated areas of heavy rain
    with embedded training to track toward the northeast over the next
    2-4 hours. While instability is forecast to remain limited across
    northeastern OK/southeastern KS into adjacent areas of MO/AR,
    strong dynamic lift ahead of the MCV and within the favorable divergent/diffluent pattern aloft may favor brief instances of SW
    to NE training within the unidirectional SW flow. Rainfall rates
    of 1 to 2 in/hr will be possible along with an additional 2 to 3
    inches of rain (locally higher possible) through 15Z. Overlap of
    these heavier rainfall rates may overlap with urban areas or an
    estimated 4-6 inches of rain which impacted the I-44 corridor in
    northeastern OK over the past 12 hours, to generate localized
    flash flooding. However, with time, weakening of rainfall
    intensities are expected with increased forward progression and a
    less favorable thermodynamic environment.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5Cub1FPd4NFK64jn8GQ1EqyYez2ipYeVqsMrLaYvdXwAwh8_sCiDYnA4hlw5Mdglsc-R= f6cTdO_OJbAdFRZ6fbLpod0$ for graphic product...

    ATTN...WFO...EAX...ICT...SGF...TOP...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NWC...

    LAT...LON 38639458 38499366 37579339 35519420 35369575=20
    36089627 37589583=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Nov 3 19:56:28 2024
    AWUS01 KWNH 031956
    FFGMPD
    TXZ000-OKZ000-040200-

    Mesoscale Precipitation Discussion 1118
    NWS Weather Prediction Center College Park MD
    255 PM EST Sun Nov 03 2024

    Areas affected...central and southern OK...North TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 032000Z - 040200Z

    Summary...Localized 2-4" short term totals likely to result in
    isolated to scattered instances of flash flooding through the
    afternoon.

    Discussion...Convective coverage is increasing this afternoon
    across North TX and southern OK, the most intense of which
    initiated in the vicinity of the dry line this morning (and is
    quickly organizing into a distinct bow echo). This region is
    encompassed within a large warm sector and associated low-level
    convergence, and instability is once again building after the
    passage of an organized MCS overnight. The mesoscale environment
    is characterized by ML CAPE of 1000-2000 J/kg (except over
    northeast OK, though continued warm air advection and isentropic
    lift will change that over the next several hours), PWATs of
    1.4-1.7 inches (near record levels, per OUN sounding climatology),
    and effective bulk shear of 45-55 kts.

    Continued building instability within this favorable environment
    will support increased coverage and intensity of convection into
    the evening. This is especially the case given the upper-level
    support, as upper-level diffluence is even more impressive than
    the low-level convergence (with a phased northern and southern
    stream allowing for idealized left-exit region of a sub-tropical
    jet streak and right-entrance region of a polar jet streak). Given
    the prior rainfall over the past 24 hours (locally up to 3-6"+
    over much of OK, per MRMS estimates), antecedent conditions will
    be more supportive of excessive rainfall with this next round of
    storms.

    Hi-res CAMs are in relatively good agreement with convective
    evolution, suggesting the potential for localized 2-4" totals over
    the next 3-6 hours (per HREF probability-matched mean QPF). While
    fast storm motions should generally limit hourly totals to 1.5" or
    so (at least through 02z), localized repeating/training of these
    rates should support those advertised 3-6 hour totals. The
    corresponding Flash Flood Guidance (FFG) are on the order of only
    1.5-3.0" (given the aforementioned antecedent conditions), so
    isolated to scattered instances of flash flooding are considered
    likely.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9GoAKxlm-gjyqehAGTrt7i73DGblpUjZlVoVP1BmPCr1TKxp0RuyDh2p2TxivO--G7yp= S_OTBIUEhW8e9zT53YjaygU$ for graphic product...

    ATTN...WFO...FWD...OUN...SJT...TSA...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36849700 36489552 34709566 33309664 32669743=20
    32449864 32149960 32259996 33489973 34559997=20
    35109963 35689850=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 4 00:02:06 2024
    AWUS01 KWNH 040001
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-KSZ000-040559-

    Mesoscale Precipitation Discussion 1119
    NWS Weather Prediction Center College Park MD
    701 PM EST Sun Nov 03 2024

    Areas affected...in and near portions of eastern OK, AR, and
    southern MO

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 032359Z - 040559Z

    Summary...Training showers and thunderstorms over saturating soils
    and area terrain are expected to lead to scattered instances of
    flash flooding through 06z. Hourly rain totals to 2.5" with local
    totals to 5" are expected over that time frame.

    Discussion...An upper trough crossing the southern Rockies is
    causing a broad area of divergence aloft across portions of the
    southern Plains and Mid-South. An effective front, part synoptic
    scale and part outflow boundary, extends from a low near the Red
    River of the South across southern and eastern AR into the
    Bootheel of MO. Along and north of the boundary a broad area of
    showers and thunderstorms with heavy rainfall exists, with a
    slight break in easternmost OK. Precipitable water values are
    near 2" per GPS data. MU CAPE of 500-2000 J/kg exists near the
    convection. Effective bulk shear is near 60 kts, more than
    sufficient for mesocyclone development. The mean flow is out of
    the south-southwest at ~60 kts, with some veering seen in the
    low-levels. This is helping to support training convective bands.

    The mesoscale guidance broadly supports heavy rainfall in the
    region, with high chances of 3"+ across southeast OK, northwest
    AR, and some of southern MO. The two areas of heavy rainfall are
    expected to merge with a potential increase in intensity as warm
    air advection increases MU CAPE into the region over the next
    several hours due to strengthening 850 hPa inflow from the Gulf of
    Mexico. Some veering to the low-level flow should continue
    eastward progression, but also increase the likelihood for cell
    training as the flow becomes more unidirectional with height.=20
    Given the ingredients available, hourly rain totals to 2.5" with
    local totals to 5" are expected over the next several hours, which
    would prove too much for saturating soils across portions of
    eastern OK and southwest AR. Such rainfall would be problematic
    in the terrain of the Ozarks as well. Given the above, chose the
    flash flooding likely category as scattered instances of such are
    expected through 06z.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5roeQX5FJkgHaqNiYugR-h_BHSGYwzeRuOBttKnx0vGVCyXi9xIkJ9nsI1XZrgAJKz2O= qlqQtvL4M1H9-6pU3n9apao$ for graphic product...

    ATTN...WFO...FWD...ICT...LSX...LZK...MEG...OUN...PAH...SGF...
    SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NCRFC...WGRFC...NWC...

    LAT...LON 37909406 37639210 37599025 37038960 34749105=20
    33719305 33079646 33279801 34459757 34859724=20
    36089668 37419605 37489496=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 4 06:12:10 2024
    AWUS01 KWNH 040612
    FFGMPD
    MOZ000-ARZ000-OKZ000-041030-

    Mesoscale Precipitation Discussion 1120
    NWS Weather Prediction Center College Park MD
    111 AM EST Mon Nov 04 2024

    Areas affected...eastern OK, northwestern AR, southern MO

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 040610Z - 041030Z

    Summary...Periods of training convection may result in a few areas
    of flash flooding from eastern OK into northwestern AR and
    southern MO through 11Z. 2 to 4 inches of rain is expected where
    training sets up.

    Discussion...A composite outflow boundary was analyzed at 06Z from
    the eastern MO/AR border into central AR, eastern OK and then
    southwestward across the Red River between Denison and Wichita
    Falls, TX. Elevated thunderstorms were occurring to the north of
    the outflow with an eastward advancing contiguous convective line
    from central MO into northwestern AR. Convective line progression
    was stalled or retrograding slightly to the north over
    northwestern AR and a fragmented/broken axis of thunderstorms
    extended westward from northwest AR into central OK with
    individual cell motions off toward the NNE but better organization
    was lacking over OK. Southerly low level winds were overrunning
    the boundary supporting the continued regeneration of
    thunderstorms, acting on 1000-2000 J/kg MLCAPE along and south of
    the outflow boundary in eastern OK. While the better 850 mb flow
    was located ahead of the advancing convective line in MO/AR, 30 to
    50 kt of S to SSW 850 winds were reported via VAD wind data to the
    south of the outflow from eastern OK into northern TX.

    The eastward advancing convective line in MO/northern AR is
    expected to continue pushing off toward the east but back to the
    west in OK, the outflow boundary is expected to continue a modest
    retreat northward within deep-layered S to SW flow ahead of a
    longwave trough over the Four Corners region. Isentropic ascent
    across the composite outflow boundary will likely maintain some
    degree of convective regeneration over central to eastern OK into
    far western AR through 11Z. While not forecast to be widespread,
    instances of training will occur where convective orientation
    aligns with the deeper layer SSW steering flow. Training will
    support rainfall rates of 1-2 in/hr, some of which will overlap
    with saturated top layer soils given recent heavy rainfall over
    the past 24-36 hours.

    Areas of training are expected to be transient and scattered
    across the region overnight. Recent hires guidance does not have a
    good handle on the progression and timing of convection compared
    to recent radar trends, so their forecast coverage of 3 to 6
    inches through 12Z may be overdone. Nonetheless, 2-4 inches in a
    few locations is still expected which may lead to a few areas of
    flash flooding.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_BVvGhDVAZ2B8FPWrhcuMZmLwdopOzAjWuA1YbeFKJeLubKtRiA7uDVJjmgLGPeBsVcU= yFkojwnwl-Z6p-Gw2gLn5lU$ for graphic product...

    ATTN...WFO...LZK...OUN...SGF...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NWC...

    LAT...LON 37399216 37059129 36369142 35739212 35039398=20
    34879485 34829630 34919710 35249739 35859701=20
    36109634 36449520 36969385=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 4 10:56:19 2024
    AWUS01 KWNH 041056
    FFGMPD
    ILZ000-MOZ000-ARZ000-041545-

    Mesoscale Precipitation Discussion 1121
    NWS Weather Prediction Center College Park MD
    555 AM EST Mon Nov 04 2024

    Areas affected...northern AR into south-central/southeastern MO,
    southwestern IL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041052Z - 041545Z

    Summary...Areas of training heavy rain will continue to pose a
    possible threat for flash flooding across parts of northern AR
    into south-central/southeastern MO through 15Z. Portions of
    southwestern IL may also see impacts. Rainfall rates of 1-2 in/hr
    (locally higher) should be expected.

    Discussion...10Z surface observations showed an elongated outflow
    boundary extended southwestward from the southern IL/MO border
    into northwestern AR and southeastern OK. Training and repeating
    rounds of thunderstorms were occurring along and just north of the
    outflow boundary from northwestern AR into southern MO, with
    MRMS-derived peak rainfall rates of 1.0-1.5 in/hr. Area VAD wind
    plots of 850 mb winds showed 40-50 kt in place from Fort Smith to
    Memphis, overrunning the boundary and allowing training of heavy
    rainfall echoes given similarly oriented steering flow from the
    SSW. There was a gradient in MLCAPE across AR, with 10Z SPC
    mesoanalysis data showing 1500 j/kg along the OK/AR border,
    weakening to the east with less than 500 J/kg along the AR/TN
    border, with elevated instability only marginally greater to the
    north.

    There is little change expected to the regional pattern in place
    over the next 3-6 hours, with 850 mb winds of 40-50 kt forecast by
    the RAP to continue through 15Z, along with similar instability
    and broad/weak diffluent flow aloft. While convective overturning
    may moderate current instability values a bit with time,
    orographic ascent will enhance low level lift across the southern
    Ozark Plateau. Expectations are for occasional areas of training
    to setup from northern AR into south-central and southeastern MO,
    producing 1-2 in/hr rainfall rates as these relatively strong low
    level winds overrun the well-defined outflow boundary in place.
    Flash flooding will remain possible for at least another few hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6esZksp20i22w9zNGb6Tbxuho3rHSU6729EsWhE658bozFtJlDZuFfNE3fjM5uMtoDny= _pJLFzSNVC-N8gRcVVXbKYM$ for graphic product...

    ATTN...WFO...LSX...LZK...MEG...PAH...SGF...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NCRFC...NWC...

    LAT...LON 38518998 38458936 38288912 37378937 36069137=20
    35239281 34989325 34979377 35129412 35189422=20
    35629435 36219404 36999323 38339078=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 4 15:35:18 2024
    AWUS01 KWNH 041535
    FFGMPD
    ILZ000-MOZ000-ARZ000-042133-

    Mesoscale Precipitation Discussion 1122
    NWS Weather Prediction Center College Park MD
    1034 AM EST Mon Nov 04 2024

    Areas affected...Northern AR...South-Central to Southeast
    MO...Southwest IL

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 041533Z - 042133Z

    SUMMARY...Additional rounds of heavy showers and thunderstorms
    which will occasionally repeat over the same area will continue to
    foster areas of flash flooding heading into the afternoon hours.

    DISCUSSION....GOES-E IR satellite imagery in conjunction with
    dual-pol radar shows a fairly large broken area of heavy showers
    and thunderstorms impacting portions of northern AR through
    southeast MO and a small part of southwest IL. The activity
    continues to be strongly influenced by enhanced warm air
    advection/isentropic ascent and moisture transport across the
    region with deep layer southerly flow in place out ahead of a deep
    layer trough/closed low gradually ejecting east out of the
    southern Rockies.

    A southerly low-level jet of 40 to 50 kts in the 850/925 mb layer
    is noted in the latest VWP data across central to northern AR and
    across southeast MO and southern IL which is acting as a conduit
    for the poleward transfer of Gulf of Mexico moisture. PWs across
    the region are locally as high as 1.75 inches which are on the
    order of 2 to 3+ standard deviations above normal for this time of
    the year. This anomalous moisture environment will continue to
    favor a well-defined excessive rainfall threat with enhanced
    rainfall rates given the warm air advection and proximity of at
    least modest instability.

    MUCAPE values are on the order of 500 to 1000 J/kg up across
    northern AR through southeast MO and this is supporting a largely
    elevated convective environment at this time. Some increase in
    instability is expected going through mid-afternoon and this
    should favor some increase in the rainfall rates which will be
    capable of reaching 1 to 2 inches/hour with the stronger storms.

    Going through the mid-afternoon hours, additional rainfall totals
    of 2 to 4 inches will be possible, with the heaviest totals most
    likely over south-central to southeast MO based on the latest 12Z
    HREF guidance. The very wet/saturated antecedent conditions that
    are in place coupled with the arrival of additional rounds of
    heavy rain over the same area will continue to promote additional
    areas of flash flooding with locally considerable runoff concerns.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6GXloCu9o8ZI23AqUpAPdrA1vlbzXXVEvhxpVyv55LOvfXK-763HvBckSdXnu4BCvxz1= AIF6aQnKNba119zkyBfpiPA$ for graphic product...

    ATTN...WFO...LSX...LZK...MEG...PAH...SGF...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NCRFC...NWC...

    LAT...LON 38619040 38578962 37988941 37109001 36469070=20
    35479239 35129354 35689421 36669363 37929201=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 4 17:22:20 2024
    AWUS01 KWNH 041722
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-KSZ000-042320-

    Mesoscale Precipitation Discussion 1123
    NWS Weather Prediction Center College Park MD
    1221 PM EST Mon Nov 04 2024

    Areas affected...Eastern OK...Northwest AR...Far Southeast
    KS...Southwest MO

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 041720Z - 042320Z

    SUMMARY...Heavy showers and thunderstorms will gradually become
    more concentrated and organized by mid to late afternoon across
    eastern OK which will also impact portions of northwest AR, far
    southeast KS and southwest MO by this evening. Locally wet
    antecedent conditions and the additional rainfall will likely
    result in areas of flash flooding.

    DISCUSSION...A strong deep layer trough and associated closed low
    ejecting out of the southern Rockies will be interacting with a
    very moist and increasingly unstable airmass pooling north across
    the Red River Valley of the South, and will be setting the stage
    for a more organized and concentrated convective outbreak by mid
    to late afternoon across areas of eastern OK and eventually
    advancing into far southeast KS, northwest AR and southwest MO by
    early this evening. Many of these areas have already seen heavy
    rainfall over the last couple of days, and the arrival of
    additional rounds of strong convection and heavy rainfall rates
    will promote a likelihood for seeing additional flash flooding
    concerns.

    The latest surface analysis shows a cold front gradually shifting
    east across the Red River Valley of the South with a wave of low
    pressure seen crossing through central OK. Meanwhile, a warm front
    is noted out ahead of this stretching across eastern OK and into
    northwest AR. MLCAPE values of 1500+ J/kg have already pooled up
    across southeast OK and far western AR with 40 to 50+ kts of
    effective bulk shear in place given the stronger wind fields
    arriving ahead of the upper trough. Already the latest GOES-E
    visible satellite imagery shows a substantial amount of cloud
    street activity over eastern OK and this is suggestive of
    increasing boundary layer instability with a strong low-level jet.

    CIRA-ALPW data shows notably concentrated moisture in the
    low-levels of the column with enhanced layered vapor transport
    (LVT) seen extending up through northeast TX, eastern OK and
    western AR. This is being facilitated by a southerly low-level jet
    of 40 to 50 kts. This moisture transport coupled with the
    instability and shear should favor an environment conducive for
    enhanced rainfall rates.

    As height falls associated with the upper trough arrive this
    afternoon, a combination of DPVA/divergent flow aloft and the
    favorable thermodynamic and kinematic environments will support
    the development of more focused/organized convection which will
    likely include embedded supercell activity. Rainfall rates will be
    capable of reaching 1.5 to 2.5 inches/hour with the more organized
    cells, and as convection grows upscale this afternoon and early
    this evening, some additional storm totals may reach 2 to 4 inches
    which is supported by the 12Z HREF guidance.

    The wet antecedent conditions coupled with these additional rains
    will likely result in more concerns for flash flooding by late
    afternoon or early this evening.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!95vqJy86OmPuqhXcuLKln84-u1AkcPL89a_zxTnBQgrSnqC1KOAuuJfHhfXvAydRDGQd= VD5W9jBLYO2dYZASnpyjkfU$ for graphic product...

    ATTN...WFO...FWD...ICT...LZK...OUN...SGF...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NWC...

    LAT...LON 37609449 37279352 36209347 34739408 33879507=20
    33969662 34659700 35739666 36809615 37439530=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 4 21:46:25 2024
    AWUS01 KWNH 042146
    FFGMPD
    TXZ000-OKZ000-050345-

    Mesoscale Precipitation Discussion 1124
    NWS Weather Prediction Center College Park MD
    445 PM EST Mon Nov 04 2024

    Areas affected...Central to Northeast TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 042145Z - 050345Z

    SUMMARY...Showers and thunderstorms with very heavy rainfall rates
    may produce some isolated to scattered instances of flash
    flooding, and especially within the more urbanized corridors
    heading through the evening hours.

    DISCUSSION...An upper-level trough and associated closed low
    continues to eject gradually across the southern Rockies which is
    driving a cold front well to the east across the southern Plains.
    This front has been crossing through central and northern TX this
    afternoon and is bumping up against a very moist and unstable
    environment that is characterized by MLCAPE values of 1500 to 2500
    J/kg and PWs of 1.5 to 1.75 inches.

    A major driver of the moisture and instability transport continues
    to be a well-defined low-level jet that is locally reaching 40 to
    50 kts, and the latest GOES-E GeoColor satellite imagery shows a
    substantial amount of cloud street activity ahead of the
    approaching cold front.

    Increasingly divergent flow aloft associated with the ejecting
    height falls/DPVA will favor convection along and just ahead of
    the cold front becoming more organized and widespread heading
    through the evening hours, and especially with the strongly
    favorable thermodynamic environment. A substantial level of
    effective bulk shear is in place that will be conducive for a
    combination of multicell and supercell activity that aside from
    severe weather hazards will be conducive for producing high
    rainfall rates.

    The convective mode along and ahead of the front will likely
    attain a QLCS mode in time, and with a southward extension that
    will eventually include areas of south-central TX including
    eastern portions of the Hill Country by later this evening.
    Rainfall rates may reach as high as 2 inches/hour with the
    stronger convective cores heading through the evening hours.

    Generally the antecedent conditions across central to northeast TX
    are on the dry side, but the convective evolution over the next
    several hours will be conducive for some 2 to 4 inch rainfall
    amounts which may end up being locally higher if any cell-training
    or cell-merger activity takes place. Some isolated to scattered
    instances of flash flooding will be possible and especially within
    the more urbanized corridors.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Gd0Zmw3lA-9sBhCOOjiKxYBkmKijk3RdpC194yF9odQUX4QTtkQgry53i9TbbTl3VT0= oH7y1s-uQMzHDGJeGR5JCYg$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...OUN...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 33969545 33599491 32899484 31539550 30419629=20
    29569746 29649834 30429842 31859741 33629645=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 4 21:56:24 2024
    AWUS01 KWNH 042156
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-KSZ000-050355-

    Mesoscale Precipitation Discussion 1125
    NWS Weather Prediction Center College Park MD
    455 PM EST Mon Nov 04 2024

    Areas affected...Eastern OK...West-Central to Northwest
    AR...Southwest MO

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 042155Z - 050355Z

    SUMMARY...Well organized bands of showers and thunderstorms will
    continue through the evening hours. Heavy rainfall rates and wet
    antecedent conditions are expected to result in scattered to
    numerous areas of flash flooding this evening. Some locally
    significant and life-threatening impacts will be possible.

    DISCUSSION...A strong deep layer trough and associated closed low
    continues to advance very slowly across the southern Rockies and
    toward the southern High Plains. A strong cold front associated
    with this continues to gradually advance eastward with a notably
    unstable and highly sheared environment focused out ahead of it.
    Strong and well organized bands of convection are seen in GOES-E
    IR satellite imagery and dual-pol radar focusing across eastern OK
    with separate clusters of convection noted across portions of
    western AR and southwest MO.

    MLCAPE values ahead of the cold front over eastern OK and western
    AR are as high as 1500 to 2500 J/kg, and this instability axis has
    been gradually nosing up into areas of southwest MO over the last
    couple of hours. A southerly low-level jet of 40 to 50 kts remains
    in place across the region, and this will drive strong moisture
    and instability transport through the evening hours as the cold
    front off to the west approaches the region.

    Strong and well organized bands of convection including some
    occasional supercell structures are expected to result in heavy
    rainfall totals this evening over areas of especially east-central
    OK, northwest AR and southwest MO. This is where there will be
    concerns for some cell-training and rainfall rates capable of
    reaching 1.5 to 2.5 inches/hour. PWs are already running locally
    near 1.75 inches and with the enhanced instability/shear profiles
    and moisture transport across the region, the rates should be
    efficiently high.

    Additional rainfall amounts by late this evening of 2 to 4 inches
    are expected, with isolated heavier amounts of 5+ inches possible
    where areas of cell-training are maximized. The experimental WoFS
    and latest HREF guidance generally supports these amounts on the
    mesoscale level. Given the additional rainfall, and the wet
    antecedent conditions, scattered to numerous areas of flash
    flooding are likely. Locally significant and life-threatening
    impacts will be possible this evening which will include some of
    the more urbanized locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5RRnrqCtmH0jJ4PgRf_q-XgyLodShvGl6aZ6DOvFjKTQ3fTMI8NB4UVokbbGdD88Zpzr= NR3o-GtEtqJFuY-TY8SZG7s$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SGF...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NWC...

    LAT...LON 37939289 37459231 36839228 35819269 34899326=20
    34019406 33649469 33709514 33979596 34249607=20
    35289564 36289523 37209471 37819406=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 4 22:21:57 2024
    AWUS01 KWNH 042221
    FFGMPD
    ILZ000-MOZ000-050420-

    Mesoscale Precipitation Discussion 1126
    NWS Weather Prediction Center College Park MD
    520 PM EST Mon Nov 04 2024

    Areas affected...Central and Eastern MO...West-Central and
    Southwest IL

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 042220Z - 050420Z

    SUMMARY...Additional rounds of heavy showers and thunderstorms
    going well into the evening hours will maintain strong concerns
    for instances of flash flooding.

    DISCUSSION....GOES-E IR satellite imagery in conjunction with
    dual-pol radar shows broken areas of heavy showers and
    thunderstorms arriving across west-central to southwest MO with
    separate areas of convection noted farther east across portions of
    central and eastern MO. The activity continues to be strongly
    influenced by strong warm air advection/isentropic ascent and
    moisture transport across the region. This continues to be
    facilitated by persistent and strong deep layer southerly flow out
    ahead of a deep layer trough/closed low edging out into the
    southern High Plains from the southern Rockies.

    A southerly low-level jet of 40 to 50 kts remains in place and is
    nosing up across much of western AR and southern MO, and this is
    overrunning a warm front seen lifting north currently through
    northwest AR and southern MO. PWs across the region are locally as
    high as 1.75 inches which again are on the order of 2 to 3+
    standard deviations above normal for this time of the year. This
    will continue to favor an environment conducive for enhanced
    rainfall rates going through the evening hours and especially with
    the low-level jet yielding a gradual and steady increase in
    instability.

    MLCAPE values have risen to 500 to 1000 J/kg across all of
    southern MO, with values locally approaching 1500 J/kg across
    southwest MO. This coupled with strong forcing and shear
    parameters going through the evening hours will strongly support
    additional bands or clusters of heavy showers and thunderstorms.
    Areas of central and eastern MO north of the warm front will have
    concerns heading through this evening for repeating rounds of
    convection and cell-training that will yielding enhanced rainfall
    totals. Some of this may also impact areas of west-central to
    southwest IL.

    These additional rains will be on top of the earlier rainfall and
    will be falling on already very sensitive soil conditions. The
    latest HRRR guidance and HREF footprint suggests additional
    rainfall amounts through late this evening of 2 to 4 inches with
    isolated heavier amounts not out of the question. Given the
    environment, these rains are expected to result in additional
    instances of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8XP-KcNTm18TTlniNf-nojK7YjFoVdX-mOMZdeZe4gtlEdupk7aUq7NtbsJxcMKEG219= bY51OK6YzlSrLwojO64KCMM$ for graphic product...

    ATTN...WFO...EAX...ILX...LSX...SGF...

    ATTN...RFC...LMRFC...MBRFC...NCRFC...NWC...

    LAT...LON 39809122 39759030 39488971 39088952 38648982=20
    38189049 37799129 37159206 37529232 37949298=20
    37939403 38569395 39029351 39409287 39599236=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Nov 5 03:57:02 2024
    AWUS01 KWNH 050356
    FFGMPD
    ILZ000-MOZ000-ARZ000-TXZ000-OKZ000-050915-

    Mesoscale Precipitation Discussion 1127
    NWS Weather Prediction Center College Park MD
    1056 PM EST Mon Nov 04 2024

    Areas affected...northeastern TX/southeastern OK into western AR
    and central/southern MO

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 050354Z - 050915Z

    SUMMARY...A slow moving axis of heavy rain will result in
    continued flash flooding from northeastern TX/southeastern OK into
    western AR and central/southern MO through 09Z. Rainfall rates of
    1-2 in/hr should result in an additional 2-4 inches of rain
    (locally higher), atop saturated soils.

    DISCUSSION....03Z radar imagery and surface observations placed a
    SW to NE axis of thunderstorms from northeastern TX into
    northwestern AR and southern/eastern MO, out ahead of a cold front
    located west of the convective line. The convective line was
    nearly coincident with the front over northeastern TX, but was
    located increasingly east of the cold front into AR/MO as one
    moves north, located along an outflow boundary. The orientation of
    the convective axis matching the mean southwesterly steering flow
    has allowed for training with MRMS-derived rainfall rates of 1 to
    locally over 2 in/hr since 00Z. 03Z SPC mesoanalysis data showed
    MLCAPE was only about 500 J/kg along and immediately ahead of the
    convective line/outflow boundary but anomalous precipitable water
    values of 1.7 to 1.9 inches and divergence aloft within the
    right-entrance region of a 110-130 kt jet max over the
    middle/upper MS River Valley was leading to enhanced lift and
    efficient rainfall production.

    Infrared satellite imagery showed a gradual warming of cloud tops
    over the region since 00Z, but occasional bursts of colder cloud
    tops continued to occur. Following trends in radar imagery over
    the past few hours and understanding that height falls downstream
    of a slow moving upper trough axis over the TX Panhandle will only
    gradually push off to the east through 09Z, the axis of heavy rain
    is only expected to slowly shift eastward. There could be
    relatively faster movement with the rainfall axis located in MO
    compared to locations farther south, but regeneration and training
    of thunderstorms to the southwest could allow for a prolonged
    duration of heavy rain for some locations as cells move back to
    the north. Some gradual weakening of CAPE is anticipated through
    the night but strong forcing for ascent should maintain periods of
    high rainfall rates with 1 to 2 in/hr (locally higher) gradually
    translating toward the east through 09Z. Given heavy rain which
    has impacted northwestern AR over the past 48 hours, and the
    sensitive terrain of the Ozarks, additional flash flooding will be
    likely, with locally significant impacts possible through 09Z.
    Additional totals of 2 to 4 inches (locally higher) can be
    expected, with northern AR into southern MO possibly seeing the
    greatest additional rainfall over the next few hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9JlLNBDATprWAX3QV5Kjx_voQ0HDTuZk7kisiL1bP31h81pfjBnBFO9rUhxzWVZ7DcIQ= vx-V4-OoXeJgJaigPaqrzQw$ for graphic product...

    ATTN...WFO...FWD...LSX...LZK...PAH...SGF...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NCRFC...WGRFC...NWC...

    LAT...LON 39069025 38559023 36609106 34879217 33149390=20
    32219511 32499587 33739551 35329445 36869299=20
    38639153=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Nov 5 04:02:29 2024
    AWUS01 KWNH 050402
    FFGMPD
    TXZ000-050800-

    Mesoscale Precipitation Discussion 1128
    NWS Weather Prediction Center College Park MD
    1101 PM EST Mon Nov 04 2024

    Areas affected...Central Texas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 050400Z - 050800Z

    SUMMARY...Flash flooding likely as storms producing up to 3 inch
    per hour rainfall rates train over/near San Antonio and Austin.
    Urban flash flooding an increasing concern.

    DISCUSSION...A mesolow that has developed along a very slow moving
    cold front draped over central Texas is tapping into 30-35 kt
    southeasterly flow of Gulf moisture at 850 mb. This low and fronts
    are providing ample forcing for thunderstorms that have a history
    of producing 3 inch per hour rainfall rates northwest of San
    Antonio. The storms are aligned parallel to the I-35 corridor. As
    the storms grow upscale, they're backbuilding southwestward
    towards the Rio Grande. For the very near-term there is little
    pushing the front as the southeasterly flow ahead of the front is
    being countered by 10-20 kt NNW flow of dry air behind the front.
    Since these air flows are almost exactly antiparallel to each
    other, they're supporting the mesolow that has formed west of San
    Antonio. Further, they will work to keep the synoptic setup from
    moving too much for the next few hours.

    An approaching upper level shortwave over northwest Texas is
    gradually moving east towards the storm complex. This will
    increasingly work to push the complex of storms towards the east
    faster, which will consequently reduce the flash flooding threat
    with time. CAMs guidance is in good agreement in this scenario,
    albeit with variable timing due to poor handling of the current
    storms.

    The storms are currently over Austin and are just about into the
    San Antonio metro at the time of this writing. Expect a
    multiple-hour period of heavy rain associated with the storms.
    Considering the reduced FFGs associated with the urban centers,
    urban flash flooding is an increasing concern over the next few
    hours until the aforementioned shortwave moves the storms east of
    the I-35 corridor.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!61EcCrLagqB-PnpGFdGXXXNvzO_9Ansvi4vY338kfBocDm8ZRg_LpXoE_OTgMGb_gFMz= nb69J93CZIYdRcgzIQtA42k$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 30859753 30659687 29829679 28959744 28619830=20
    28489942 28939983 29159952 29379924 29809881=20
    30539813 30819789 30829787=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Nov 5 09:32:38 2024
    AWUS01 KWNH 050932
    FFGMPD
    ILZ000-LAZ000-MOZ000-ARZ000-TXZ000-051530-

    Mesoscale Precipitation Discussion 1129
    NWS Weather Prediction Center College Park MD
    431 AM EST Tue Nov 05 2024

    Areas affected...mid-MS Valley into central AR and the Arklatex

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 050930Z - 051530Z

    SUMMARY...Flash flooding is expected to continue from near and
    south of the St. Louis metro/mid-MS Valley southwestward into the
    Arklatex through 15Z. While rainfall rates will be lowering
    overall, occasional pockets of higher rates will maintain areas of
    flash flooding, especially atop saturated soils.

    DISCUSSION...Regional radar imagery at 09Z showed an elongated
    axis of showers and thunderstorms which stretched from the St.
    Louis metro into south-central MO, west-central AR and the
    Arklatex. This axis was located along a combined cold/stationary
    front and outflow boundary which was coincident with the leading
    edge of heavy rain. Trends in rainfall intensity have shown a
    decrease in higher rainfall rates over the past few hours as
    instability has been lowering. 09Z SPC mesoanalysis data showed
    MLCAPE values were at or less than 500 J/kg just ahead of the
    combo front/outflow boundary from MO into AR, but increased to
    1000+ J/kg over TX. However, the southern portion of the
    front/outflow was progressing steadily toward the east, to the
    south of weak wave located ~40 miles southeast of FSM, limiting
    the flash flood threat for these southern locations. To the north,
    the front/outflow has been very slow to progress with locations
    just south of I-44 in eastern MO to the St. Louis metro containing
    repeating and training echoes for the past 2-3 hours.

    Water vapor imagery showed the former closed mid-level low over
    the southern High Plains has begun to open up and elongate from
    SSW to NNE. Just ahead of the elongating upper vorticity max was a
    GOES-East DMV sampled 130+ kt jet streak over eastern KS,
    providing increased lift via strengthening divergence aloft over
    northern AR into MO within the right-entrance region. As the mid
    to upper-level trough axis continues to translate east, it is
    forecast to acquire more of a neutral tilt with the downstream jet
    streak allowing for an extended period of enhanced lift over MO.

    Therefore, while instability will continue to gradually lower
    until sunrise (~12Z), dynamic forcing will support occasional
    pockets of higher rainfall rates within areas of training that
    will continue to support pockets of rainfall rates of 1-2 in/hr
    within an anomalous moisture axis containing PWATs up to 1.8
    inches. This potential will exist from near the Arklatex to the
    central and southern MO/IL border, overlapping portions of the
    region which have seen heavy rainfall over the past 24 hours.
    Overlap of additional rainfall with prior rainfall is expected to
    be greatest across MO into northern AR, but at least an isolated
    flash flood threat will continue for locations farther south into
    northwestern LA and northeastern TX. Additional rainfall totals of
    2-3 inches are expected through 15Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_opc69QMvdrTu-My0ZY0aWZubvA7qylLDKEG21zAWZLR3L4iI5l4BGmrDf_vkk22iL_7= DsEYgJvmZ6xBI6QMY-JS9x0$ for graphic product...

    ATTN...WFO...LSX...LZK...PAH...SGF...SHV...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NCRFC...WGRFC...NWC...

    LAT...LON 39058971 38568953 37339024 35379164 33599272=20
    32389359 31859456 31949496 32439503 33479441=20
    35299351 36799266 38379143 39049063=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Nov 6 05:35:00 2024
    AWUS01 KWNH 060534
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MSZ000-LAZ000-MOZ000-ARZ000-061115-

    Mesoscale Precipitation Discussion 1130
    NWS Weather Prediction Center College Park MD
    1234 AM EST Wed Nov 06 2024

    Areas affected...AR/MS border into western TN/KY and the lower OH
    Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 060532Z - 061115Z

    SUMMARY...Training/repeating rounds of showers and thunderstorms
    may produce a couple areas of localized flash flooding through 11Z
    from the AR/MS border into western TN/KY and the lower OH Valley.
    Rainfall rates up to 3 in/hr will be possible, although 1-2 in/hr
    should be more common. Coverage is expected to remain localized.

    DISCUSSION...Regional radar imagery showed a broken axis of
    showers and thunderstorms stretching from southwestern IN into the
    lower MS Valley at 05Z, along and ahead of a slow moving cold
    front. 05Z data from the SPC mesoanalysis showed that MLCAPE of
    500-1000 J/kg extended from the lower MS Valley into southwestern
    TN with weak (<500 J/kg) MLCAPE and MUCAPE to the north into the
    lower OH Valley. Slow eastward movement of the boundary and
    anomalous moisture (PWATs of 1.5" along the IN/KY border,
    increasing to near 2.0" along the AR/MS border) were supporting
    locally high rainfall rates within areas of training. Peak
    rainfall rates were observed in the 2.5 to 2.7 in/hr range in
    Lauderdale County in western TN just prior to 05Z but that axis of
    heavy rain has since shifted east.

    Forecast movement of the boundary is for slow but steady eastward
    progress northward of northern TN, but for nearly stationary
    movement south of Memphis. Water vapor imagery showed a subtle
    shortwave trough over western LA into the Gulf with slight
    buckling of the downstream flow over the lower MS Valley which may
    help to support a weak surface wave along the front in LA and
    stalling of the front to its immediate north. 25-35 kt of 925-850
    mb flow from the S to SSW (despite gradual weakening overnight)
    may allow for the repeated regeneration of showers/thunderstorms
    over the AR/MS border with areas of training toward the NNE just
    ahead of the slow moving front. Rainfall rates of 1-2 in/hr
    (locally higher) will be possible within axes of training
    resulting in 2 to 3 inches (locally higher) through 11Z.

    Farther north, the flash flood threat is expected to be more
    limited due to the eastward progression of the cold front, limited
    instability and the departing of right-exit region ascent tied to
    a 120-140 kt over IL/IN/MI. However, an isolated flash flood
    cannot be completely ruled out overnight.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5Bk5mj0ywGnmHWHTyuAFOz-KVfnWT0oULFfhLEklzQV8SadaiI_X3Phr2Nx0D5CLUonO= sXd0xVKAs8i8HSXc7fIwlI0$ for graphic product...

    ATTN...WFO...JAN...LMK...LZK...MEG...OHX...PAH...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 38478748 38208676 37808664 36888701 35518831=20
    34298969 33449075 32979134 33159167 34189099=20
    35698987 36638920 38108796=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Nov 6 14:02:07 2024
    AWUS01 KWNH 061402
    FFGMPD
    MSZ000-LAZ000-061800-

    Mesoscale Precipitation Discussion 1131
    NWS Weather Prediction Center College Park MD
    901 AM EST Wed Nov 06 2024

    Areas affected...Central and Northeast LA...Southwest MS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 061400Z - 061800Z

    SUMMARY...Slow-moving areas of heavy showers and thunderstorms are
    expected to continue through the morning hours. Some localized
    areas of flash flooding will be possible, and especially given
    very high rainfall rates and some cell-training concerns.

    DISCUSSION...The latest GOES-E IR satellite imagery in conjunction
    with dual-pol radar shows slow-moving areas of heavy showers and
    thunderstorms focusing along and just ahead of a quasi-stationary
    front situated from southwest LA northeastward through
    west-central MS. The convection has been showing persistence and
    localized expansion in coverage over the last couple of hours, and
    is being influenced by proximity of a weak area of surface low
    pressure along the front.

    This is yielding an axis of relatively strong low-level moisture
    convergence which is also embedded within a somewhat unstable
    boundary layer characterized by MLCAPE values of around 1000 J/kg.
    The upper-level flow over the northwest Gulf Coast region is also
    seen becoming increasingly divergent and this is also facilitating
    deeper layer ascent with a low-level convergent response ahead of
    the aforementioned wave of low pressure.

    Recent MRMS data has been showing some of the active areas of
    convection over central LA producing rainfall rates of as much as
    2 to 3 inches/hour and this is being aided by PWs of 1.75 to 2
    inches which are about 2 standard deviations above normal for this
    time of the year.

    Additional rainfall amounts of up to 3 to 5 inches will be
    possible by late this morning given the slow cell-motions and
    occasional cell-training concerns. This is supported by the 12Z
    HRRR guidance, and this may result in some localized areas of
    flash flooding. The main threat will tend to be over central to
    northeast LA, but some of this could potentially spread into
    portions of southwest MS by later this morning.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7urNP6j1PqnxfxCgA5LmFnnJ2ZgtdLDh7bxmZtw7cVdlJA4xD0Xz2Puk9yUH3YzwW5o6= ClXO94nn4iWBtE11iYuxT_w$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...SHV...

    ATTN...RFC...LMRFC...NWC...

    LAT...LON 32769106 32379083 30989151 30219222 30239287=20
    30889267 32119195=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Nov 6 19:31:18 2024
    AWUS01 KWNH 061931
    FFGMPD
    SCZ000-GAZ000-ALZ000-070130-

    Mesoscale Precipitation Discussion 1132
    NWS Weather Prediction Center College Park MD
    230 PM EST Wed Nov 06 2024

    Areas affected...Central and Eastern GA...SC Midlands and
    Lowcountry

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 061930Z - 070130Z

    SUMMARY...Increasing coverage of showers and thunderstorms is
    expected going through the evening hours. Very heavy rainfall
    rates and localized areas of cell-training will result in a
    gradually increasing flash flood threat, and especially for the
    more urbanized locations.

    DISCUSSION...Deep layer tropical moisture transport extending well
    north of Hurricane Rafael is seen in CIRA-ALPW imagery advancing
    northwestward into the Southeast U.S. Already the PWs across much
    of southern GA have increased to 2.25+ inches, and some additional
    increase in the PWs will be expected this evening as deep layer
    southeast flow persists over the region.

    Meanwhile, this will couple with increasing boundary layer
    instability in vicinity of a surface trough and developing
    right-entrance region upper-level jet dynamics for broken areas of
    very heavy shower and thunderstorm activity. MLCAPE values are
    already locally on the order of 1000 to 1500 J/kg, and satellite
    imagery is showing an increasingly divergent flow pattern aloft
    associated with favorable placement of the upper-level jet near
    the Southeast U.S.

    Radar and satellite imagery are showing rather rapidly expanding
    areas of convection with cooling cloud tops across central and
    eastern GA, and some additional increase in coverage is expected
    going through the evening hours as deep layer forcing/ascent
    increases further which will likely include portions of the SC
    Midlands and Lowcountry.

    Some of the convection is expected to become locally very
    concentrated heading into the evening hours, with some potential
    for alignment of the activity in a cell-training manner. The 12Z
    HREF guidance and recent runs of the HRRR have been supporting
    this and suggest some impressive rainfall totals this evening,
    with additional heavy rainfall totals extending well into the
    overnight period.

    Given the deeply tropical environment, the rainfall rates will be
    extremely efficient with 2 to 3+ inch/hour rates eventually
    becoming likely. The cell-training concerns associated with this
    will favor some storm totals by mid-evening to reach as high as 3
    to 6 inches.

    Initially with the very dry antecedent conditions, the flash flood
    threat will tend to be a bit conditional, and will tend to be more
    of a concern for the more sensitive urbanized areas. However, the
    flash flood threat is expected to increase further overnight as
    additional heavy rains develop and persist over the same area.
    Additional MPDs will be issued accordingly.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5rF2haKG-qNTL-6Kg23eop2qrA7ZRId4zdFWFIBe9K1ugPsaom58G_0KTODq7h_81ams= x5YvuK9vHDq8YnNvPgPAQ6w$ for graphic product...

    ATTN...WFO...BMX...CAE...CHS...FFC...JAX...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 33918253 33868101 33028086 31778180 31408339=20
    31838466 32328510 32948489 33588379=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Nov 6 23:17:17 2024
    AWUS01 KWNH 062317
    FFGMPD
    SCZ000-FLZ000-GAZ000-070515-

    Mesoscale Precipitation Discussion 1133
    NWS Weather Prediction Center College Park MD
    615 PM EST Wed Nov 06 2024

    Areas affected...Portions of the FL Panhandle...Southern and
    Eastern GA...SC Midlands and Lowcountry

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 062315Z - 070515Z

    SUMMARY...Heavy showers and thunderstorms will continue to
    generally increase in coverage and concentration heading into the
    overnight hours. There will be concerns for extreme rainfall rates
    and some cell-training which is expected to result in scattered to
    numerous areas of flash flooding. Some of this may become
    particularly significant and life-threatening.

    DISCUSSION...Deep layer tropical moisture transport continues into
    the Southeast U.S. well to the north of Hurricane Rafael which is
    currently crossing western Cuba. The latest CIRA-ALPW imagery
    shows strong concentrations of this tropical moisture in the low
    and mid-levels of the vertical column, and overall the PWs now up
    across the FL Panhandle into central and southern GA have risen
    into the 2.25 to 2.5 inch range based on some of the polar
    microwave and GPS data.

    This moisture transport continues to work in tandem with MLCAPE
    values of as much as 1000 to 1500 J/kg and proximity of a surface
    trough to promote numerous areas of heavy showers and
    thunderstorms. Radar generally shows the greatest concentrations
    of convection focused over areas of southern and eastern GA and
    into portions of the central SC. The flow aloft continues to be
    increasingly divergent which is showing up well in the GOES-E IR
    satellite imagery along with the expansion of cooling convective
    tops as favorable upper-level jet divergence sets up.

    The latest 18Z HREF guidance and HRRR solutions support locally
    some additional expansion of convection along with a likelihood
    for this activity to become increasingly concentrated and focused
    over areas of east-central GA and potentially edging into parts of
    the SC Midlands and Lowcountry heading into the overnight hours.

    The deeply tropical environment coupled with the level of
    instability and low to mid-level shear may favor some particularly
    high rainfall rates overnight. Some of these rates may reach 2 to
    4 inches/hour and will tend to be maximized with any mesocyclone
    activity that occurs near the aforementioned surface trough axis.
    The cell-training concerns associated with these rates will favor
    additional rainfall totals of 4 to 6 inches by midnight with
    locally heavier amounts possible.

    Dry antecedent conditions at least in the short-term will continue
    to locally mitigate the flash flood threat, but as these extreme
    rainfall rates materialize and persist into the overnight hours,
    there will eventually be scattered to numerous areas of flash
    flooding, and some of this may become significant and
    life-threatening.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6RoZcw210YMUGotFsTAKGFrD0NmdNnBMQ1igOKYCIYatvrAKjY92RtY2oILmuvkyqikM= JEjmKTml0zvg7GUJhF7jNGA$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...JAX...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 34288093 33748053 32918090 32158149 31268222=20
    30418339 30288427 30828487 31858463 32988367=20
    34238202=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Nov 7 04:54:54 2024
    AWUS01 KWNH 070454
    FFGMPD
    SCZ000-FLZ000-GAZ000-071100-

    Mesoscale Precipitation Discussion 1134
    NWS Weather Prediction Center College Park MD
    1154 PM EST Wed Nov 06 2024

    Areas affected...Southeast GA...Eastern SC...Eastern FL
    Panhandle...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 070500Z - 071100Z

    SUMMARY...Flash flooding likely to continue with slow
    moving/stationary PRE-like precipitation shield. Embedded
    convective cells with 2-2.5"/hr may result in 5-8" totals thru 12z
    resulting in significant flash flooding.

    DISCUSSION...Regional RADAR mosaic depicts a broad mesoscale
    complex across stretching from the central GA/FL state line
    through southeast GA into the coastal plain of SC. Frontal-like
    features are starting to be more well defined, with surface 04z
    surface analysis suggesting a weak low near VDI as well as a
    meso-low responding to very strong convective complex near VLD. A
    surface trof/effective developing front extends northeast through
    the pressure trof to about DYB/CHS providing a favorable boundary
    for further ascent.=20

    RAP analysis continues to denote a very strong divergence
    signature at the right entrance of a passing polar jet across the
    Carolinas along with modest diffluent pattern over SE GA/N FL as
    contribution from anticyclonically curved outflow jet from
    periphery of approaching Tropical Cyclone Rafael. This
    divergence signal is slowly lifting north east, but its
    contribution to the development of the sfc to low level wave and
    encouragement of strengthening southeasterly confluent return
    moisture flow off the Gulf stream, is providing deep moisture flux
    convergence and isentropic ascent across the aforementioned
    boundary. CIRA LPW shows a marked increase in moisture generally
    parallel to the FL coast with 1.15" Sfc to 850mb moisture advected
    northeast on 25-30kts orthogonal to the boundary and as far
    northwest into GA toward Macon, GA. CIRA LPW also notes that
    solid core of 700-300mb moisture resides across the northeast Gulf
    through South Carolina resulting in total values over 2-2.25".=20
    While the profile is solidly saturated, there is sufficient low
    level heating to support weak to modestly unstable air with
    750-1250 J/kg of MLCAPE remaining along and southeast of the
    boundary, so embedded convective elements will remain likely
    through the overnight period...likely with SE to NE 'finger-like'
    filaments as the overall onshore flow is strong to support about
    5kts of southeast propagation.

    This will allow for a broad complex of moderate showers to remain
    across SE GA into SC where heavy rainfall has already resulted in
    flash flooding conditions additional 2-4" totals on .5-1"/hr rates
    can be expected. However, it is those embedded convective
    elements with back-building that are of greatest concern. Overall
    trends would suggest band of confluence showers/TCus off the Gulf
    stream lifting north into SW SC will likely result in the greatest
    potential totals, nearly all 00z Hi-Res CAMs support a localized
    maxima in the vicinity from Bulloch to Colleton counties (HREF
    neighborhood probability of 5"/6hr over 50%), providing solid
    confidence there.

    However, a secondary area of concern along the southern-most
    flanking line of the effective boundary in south-central GA
    remains a bit less certain...but already been very prolific near
    Valdosta, GA. With an exiting shortwave/right entrance region,
    there remains some veering of low level flow to maximize sfc to
    boundary layer moisture flux convergence in proximity to the
    greatest remaining instability pocket across the eastern portion
    of the FL panhandle across southern GA. Isallobaric response will
    likely remain the driver of this flux convergence and risk for
    2-3"/hr rates. Deeper layer flow suggests this area of
    convergence will drift north and westward toward an area of
    lowered FFG values from prior heavy rainfall recently. As such,
    while confidence that this area will be able to maintain relative
    to areas northward, the risk for more isolated but heavier
    rainfall rates and excessive totals remains.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4QsiGC3P41EoUF092UQbYMadJ1b-Rn0SDXhUK7WFfXdGOHCXlWbPqjrOrkAdh1t8Uru8= qLQyBbT48o6r3EM9gbuI7rw$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...ILM...JAX...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 34418013 33867906 33207910 32527986 31658092=20
    31008134 31078194 31048223 30238340 30218414=20
    30898440 32148370 33078284 34108136=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Nov 7 10:08:59 2024
    AWUS01 KWNH 071008
    FFGMPD
    SCZ000-GAZ000-071530-

    Mesoscale Precipitation Discussion 1135
    NWS Weather Prediction Center College Park MD
    508 AM EST Thu Nov 07 2024

    Areas affected...Southeast GA...Southern SC...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 071010Z - 071530Z

    SUMMARY...Flooding likely to continue though potential for intense
    rain-rates capable of inducing flash flooding reducing with time
    and overall coverage.

    DISCUSSION...A large area of 4-10" rainfall extends across eastern
    GA into southwest to south-central SC with slow expansion toward
    the coastal Plain over the past few hours. Large scale ascent
    pattern remains fairly strong with upper-level divergence pattern
    along right entrance of broad polar jet across the Carolinas.=20
    However, the area is shifting east-northeast and reducing
    slightly. Still, this is maintaining a solid dual fetch of
    low-level flow from the northeast Gulf as well as off the Gulf
    stream parallel to the NE FL/GA coast. Cold pool from the heavy
    rainfall continues to allow for a moderately steep isentropic
    boundary across the area from SE GA into the Low Country, with a
    very slow east-southeast drift due to the responding low level
    inflow from the south-southeast. VWP denotes continued 20-25kts
    of SE flow nearly orthogonally intersecting the boundary and
    northeasterly flow across central SC. CIRA LPW and RAP analysis
    denote deep profile of highly anomalous moisture with values of
    2.25" through depth with sfc-850mb over from .9" to 1.15" across
    the area of concern; so dynamics and moisture continue to be in
    place to maintain rainfall efficiency.=20

    However, unstable air mass continues to diminish in areal coverage
    and intensity as the profile becomes more staturated and warms
    aloft; restricting itself to the Gulf Stream and coastal GA where
    low level flow has been generally divergent before starting to
    accelerate into SE SC where convergence is maximized. Values of
    500-1000 J/kg remain but only along the upstream edge of the
    complex along the Savannah River Valley. As such, limited
    overall convection capable of rates over 1.5-2"/hr are expected
    over the diurnal minimum in activity of early morning/daybreak,
    mainly near/southeast of mid-level exiting shortwave seen near
    Wilkenson county, GA or at the 700-850mb low feature seen in RADAR
    in Montgomery county. Smaller localized spots of 2-4" totals
    remain possible to induce new incidents of flash flooding though
    the 15z period.

    Moderate downstream blow-off shield precipitation within the more
    gentle isentropic ascent pattern will maintain moderate rainfall
    rates across the flooded areas from Emanuel to Orangeburg with
    counties with occasional hourly rates exceeding .5". This will
    likely help to maintain the expanding riverine flooding as pluvial
    flooding continues to channel into localized creeks/streams. An
    additional 2-3" remains possible through the morning hours given
    favorable upstream redevelopment and training as the upper-level
    forcing moves northeast.

    As such, flooding will remain likely across the area of concern,
    though incidents of flash flooding are considered possible given
    reducing coverage/intensity required to exceed FFG where heavier
    rain did not fall last evening/overnight across coastal E GA/S Low
    Country of SC.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7KrKv4WH9irWGj-XPJJQSsd03infN2eK6yLMWHxkshwpLkQNiGmy677k2jkIUv-D8ixG= 2-gtf15TA2-jcdygL8CFC7A$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...ILM...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 34118019 33907956 33397924 32977945 32757980=20
    32578007 32208058 31698098 31418123 31528156=20
    31888193 32048228 31938282 32008307 32298309=20
    32688271 33158214 33478172 33678137 34038071=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Nov 7 15:35:58 2024
    AWUS01 KWNH 071535
    FFGMPD
    SCZ000-GAZ000-071930-

    Mesoscale Precipitation Discussion 1136
    NWS Weather Prediction Center College Park MD
    1035 AM EST Thu Nov 07 2024

    Areas affected...Southeast GA into Far Southern South Carolina

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 071534Z - 071930Z

    SUMMARY...Additional flooding is possible into the afternoon over
    parts of southeast Georgia into far southern South Carolina
    although the potential for intense rain-rates capable of inducing
    flash flooding should diminish with time.

    DISCUSSION...On-going convection capable of producing isolated
    areas of an additional 2 to 4 inches of rain will perisit over
    portions of southeast Georgia into far southern South Carolina
    with isolated spots receiving rainfall rates approaching 1.5 inche
    per hour. Large scale ascent pattern remains fairly strong with
    upper-level divergence pattern along right entrance of broad polar
    jet across the Carolinas. However, the area of heaviest rainfall
    rates has shifted south and east of the area hardest hit overnight
    and should continue to shift closer to the coast into th
    afternoon. Still, this is maintaining a solid dual fetch of
    low-level flow from the northeast Gulf as well as off the Gulf
    stream parallel to the NE FL/GA coast. Cold pool from the heavy
    rainfall continues to allow for a moderately steep isentropic
    boundary across the area from SE GA into the Low Country, with a
    very slow east-southeast drift due to the responding low level
    inflow from the south-southeast. CIRA LPW...RAP analysis and 12Z
    soundings denote deep profile of highly anomalous moisture with
    values of 2.25" through depth with sfc-850mb over from .9" to
    1.15" across the area of concern; so dynamics and moisture
    continue to be in place to maintain rainfall efficiency.=20

    However, instability should linger in an increasingly small areal
    coverage which should help limit overall convection capable of
    rates over 1.5 inches per hour and localized 2-4" totals remain
    possible to induce new incidents of flash flooding although any
    additional rainfall ovee areas soaked overnight will likely result
    in continued (if not worsening) ongoing flooding.=20

    Bann

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4vPr74HAmWnkcsSQ-9qcLHtsd97mnbkX8MuR_mRwriti8-Q8JPBVnk2AcJnjSvWpsBY_= u6zsupGjeo0N-JNjpId4VRY$ for graphic product...

    ATTN...WFO...CHS...FFC...JAX...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 32658107 32618067 32468052 32228064 31618117=20
    31288148 31078197 30908246 30988303 31178311=20
    32088219=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Nov 7 21:05:35 2024
    AWUS01 KWNH 072105
    FFGMPD
    TXZ000-OKZ000-080300-

    Mesoscale Precipitation Discussion 1137
    NWS Weather Prediction Center College Park MD
    404 PM EST Thu Nov 07 2024

    Areas affected...Parts of North Texas to Southwest Oklahoma

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 072103Z - 080300Z

    SUMMARY...Showers and thunderstorms capable of producing heavy
    rainfall that results in areas of excessive rainfall will become
    more numerous during the afternoon and evening.

    DISCUSSION...An increase in the coverage of showers and
    thunderstorms is expected to continue this afternoon and evening
    in a region of low level convergent flow while the flow aloft
    becomes increasingly difluent/divergent. With the low level flow
    tapping an airmass with precipitable water values at or above 1.5
    inches gets drawn towards the region of low level
    convergence...any convection in the area should become
    increasingly efficient rainfall producers.

    Moisture transport will be working in tandem with MLCAPE
    values approaching 1000 J/kg and the approach of a low level
    surface warm front later in the afternoon as shown by the 12Z HREF
    and latest HRRR runs...helping to provide a focus for the
    organized convection.

    The expectation is that risk of excessive rainfall will initially
    be widely scattered and tied more to rainfall rates.=20
    However...the synoptic scale forcing of upper level divergence
    combined with the mid and low level mesoscale forcing suggests
    that the risk of excessive rainfall will continue to grow in
    coverage for the remainder of the afternoon and into the evening.

    Bann

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9LO1tGJzq498dPI3ufT-sKRcmiHD91MR6OKGTMXeqC4ZCEQtdmcqSX_fO20Vo4lhExeh= rOO_1_B7vPIC5YvXLJSgusM$ for graphic product...

    ATTN...WFO...AMA...FWD...LUB...OUN...SJT...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36330047 35389891 34019734 32729703 32139698=20
    31519752 31889892 32489972 33080014 33500051=20
    34260098 35340122=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Nov 8 02:55:11 2024
    AWUS01 KWNH 080255
    FFGMPD
    TXZ000-OKZ000-080830-

    Mesoscale Precipitation Discussion 1138
    NWS Weather Prediction Center College Park MD
    954 PM EST Thu Nov 07 2024

    Areas affected...Lower Pecos/Concho Valleys into Northwest Texas
    Big Country...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 080300Z - 080830Z

    SUMMARY...Slow moving/training thunderstorms with 1.75-2"/hr rates
    pose line of 2-4" totals with possible embedded 5+" resulting in
    likely incidents of flash flooding through the overnight period.=20

    DISCUSSION...GOES-E WV suite continues to show anomalously deep
    closed low over northern NM with broad southwesterly flow aloft
    crossing the Southern High Plains. While the upper-low is filling
    slowly, there are two main vorticity centers with the northern
    swinging around the NE side of the circulation int SE CO, while
    the base energy is starting to advance out of AZ. This continues
    to support a very strong and diffluent jet across much of western
    Texas providing a broad area of vertical ascent. Near the
    surface, the low level jet has been responding throughout the
    evening with solid 30 kt south-easterly flow. Initial surge of
    enhanced moisture has already intersected the deeper NNE to SSW
    convergence axis from NW TX toward the Lower Pecos River Valley
    and has brought total PWat values into the 1.5" range in proximity
    to the western edge of the instability gradient and has supported
    expanding clusters of thunderstorms with a few rotating updrafts
    within a cluster or two across E OK into the northern Concho
    Valley, with a few more individual cells further south. CIRA LPW,
    notes that a secondary surge especially in the surface to 850mb
    layer is starting to reach the Lower Pecos and into Concho Valley
    with .6 to .75" values at the nose of the 30kts, this will
    continue through the early overnight period and eventually expand
    along the length of the convergence axis (area of concern). This
    will increase convective coverage as well as moisture flux into
    the cells. Modest instability (1000+ J/kg) will be aided by the
    divergence aloft to maintain stronger updrafts and result in
    expanding downdrafts capable of 1.5-2"/hr.

    Greater concern is going to be residency of this
    ascent/convergence axis to allow for additional development
    (particularly upstream in SW TX where a weak 850mb low will be
    forming and lifting northward through the evening with the
    approaching height-falls/dPVA. As the base shortwave swings
    east, overall orientation of the flow will back more southerly and
    allow for deeper steering flow to align more with the generally
    stationary convergence axis. Cells further south near the
    surface low (between) SJT/BRD and frontal zone, cells may have
    increased depth of moisture flux...before becoming more elevated
    across Nw Texas. As such, training may result in a band of
    excessive rainfall totals of 3-4" with embedded spots over 5" not
    out of the realm of possibility. While areas of the Concho/Pecos
    Valley have higher FFG values, there remains solid likelihood of
    exceeding resulting in flash flooding conditions tonight. Lower
    FFG values from Nolan/Callahan and points north increase the
    potential for exceedance (<2"/hr & 2-2.5" in 3hrs). As such,
    flash flooding is considered likely and with above normal
    confidence given the overlapped weather elements and fairly solid
    agreement in the Hi-Res CAM suite.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_A2Fs_mgfufkPhueckyGmQJMM-xfyGJa9SDVNnaa2sv3cw8XYm9uKUIKn8iQ-IT8C-lh= Cb1D2MKfy89NKxFZuq-bWPQ$ for graphic product...

    ATTN...WFO...EWX...FWD...LUB...MAF...OUN...SJT...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 34389920 34239832 33599779 32579782 31509872=20
    30699954 30140012 29650110 29940199 30700183=20
    31550137 32950059 33940019=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Nov 8 03:21:12 2024
    AWUS01 KWNH 080321
    FFGMPD
    TXZ000-OKZ000-080900-

    Mesoscale Precipitation Discussion 1139
    NWS Weather Prediction Center College Park MD
    1020 PM EST Thu Nov 07 2024

    Areas affected...Western Oklahoma...Eastern Texas Panhandle...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 080320Z - 080900Z

    SUMMARY...Scattered clusters of elevated thunderstorms with
    1-1.5"/hr rates and possible training/repeating may result in a
    scattered incident or two of localized flash flooding given lower
    FFG values in the area.=20

    DISCUSSION...GOES-E WV suite depicts an anomalously strong (2-3
    standard anomaly) closed low across S CO/N NM with lead vorticity
    center starting to retrograde over the top of the parent center of
    the closed low. This is resulting in downstream backing of deeper
    layer flow, particularly in the 850-700mb layer providing
    sufficient moisture flux and weakly steeper lapse rates for some
    weak MUCAPE (about 500 J/kg or less) in proximity of the Red
    River. Solid/consistent convergence along the TROWAL axis that is
    generally along 100W along with this instability has sprouted and
    helped to maintain redevelopment of convective clusters across far
    NW Texas into SW OK. Solid moisture flux values on 30-35kts
    850-700mb veering flow and CIRA LPW values at .33-.5" through the
    layer (and totals of 1.25") has supported modest rainfall
    production with these elevated cells. Spots of 1-1.5"/hr rates
    have been seen and current trends along the TX/OK border suggest
    similar rates may be expected over the coming hours.=20

    As the vorticity center continues to retrograde, deeper southerly
    influence and stronger moisture flux from the south (see MPD 1138
    for additional upstream development) should help to maintain
    scattered potential for training/repeating elements through the
    early overnight period and as such, spots of 1.5-3" are possible.
    Ground conditions have been wetter than most areas across the
    Plains recently, with slightly above average deep soil moisture
    and so FFG values are slightly lower and within range of these
    hourly and 3hrly totals. As such, a spot or two of flash flooding
    is considered possible.=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_2bhqxm_lXbf9rpwq-COCY8Dmg6MW0FYTV7OcZbasXcrpQD2RypU7YhE6RieIjP7RpqB= _A6pc3kU70py0BFq0RqNNgk$ for graphic product...

    ATTN...WFO...AMA...LUB...OUN...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36979834 36889762 36069744 34949802 34369893=20
    33789999 33540105 34170178 35290116 36010043=20
    36719966 36959913=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Nov 8 08:07:17 2024
    AWUS01 KWNH 080807
    FFGMPD
    TXZ000-OKZ000-081330-

    Mesoscale Precipitation Discussion 1140
    NWS Weather Prediction Center College Park MD
    306 AM EST Fri Nov 08 2024

    Areas affected...Central to North TX...far South-central OK...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 080815Z - 081330Z

    SUMMARY...Flash flooding threat continues with slow moving
    thunderstorms but with reducing instability coverage and intensity
    should be reducing through 12z.

    DISCUSSION...GOES-E WV suite shows large scale upper-level closed
    low has moved to a more neutral orientation on its way toward a
    weak negative tilt over eastern NM. VWP and RAP analysis suggest
    surface to 850 cyclogenesis is starting to break off into a closed
    low across the Lower Pecos moving into the Concho Valley. GOES-E
    3.9um SWIR and RADAR mosaic note the backed/slowing low level flow
    near the splitting point out of the Rio Grande Valley has resulted
    in the southern most cell starting to lift with the forcing wave
    as it lifts north. Still, along and downstream of the low within
    the weak split jet flow aloft/along the best divergence axis
    aloft, a classic-wedge EIR pattern has formed though is starting
    to broaden and round with weakening overall flow and slow
    breakdown of the best ascent. Still, VWP 850-700mb flow remains
    solid for the next few hours with deep moisture flux convergence
    maximized with said axis from Runnels to Stephens to Jack counties
    in Northwest Texas. Total Pwats over 1.75" and modest but still
    supportive 500-1000 J/kg CAPE will maintain the potential for
    1.5-2"/hr rates for the next 3-4 hours, slowly waning with time.=20

    Deep layer steering will continue to allow for convective elements
    to align and train/repeat and will support 2-4" totals with higher
    values north and east of the surface wave. However, the overall coverage/breadth of the downdrafts may reduce the overall coverage
    of the 3-4" in favor of a broader area of 2-3" as the best upper
    level support reaches the Red River Valley into south-central OK.=20
    As such, while flash flooding is likely to continue where the
    swath of 3-6" from Runnels to Palo Pinto county as the last cells
    in the train move through; the probability of new incidents of
    flash flooding northward will become more isolated with time and
    so the risk reaches the possible flash flooding assignment
    category versus likely...though potential increases with any
    crossing of urban or traditionally prone localized areas across
    Northwest and Northern Texas through 14z.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_K2yMoRbyrD22CT08Q6RGYnR85OHUV3sDkBUD-o_ZSXcX8iezfT9veSwlOmPPvMxFR57= -YzNe003ipu4xGfR-ub83DQ$ for graphic product...

    ATTN...WFO...FWD...OUN...SJT...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 34959734 34579682 34459669 33909670 32879731=20
    31729856 31209951 31390018 32080010 33199956=20
    34729835=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Nov 8 22:27:01 2024
    AWUS01 KWNH 082226
    FFGMPD
    LAZ000-TXZ000-090425-

    Mesoscale Precipitation Discussion 1141
    NWS Weather Prediction Center College Park MD
    525 PM EST Fri Nov 08 2024

    Areas affected...much of northern and eastern TX...adjacenet
    portions of northwestern LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 082225Z - 090425Z

    Summary...1-2"/hr rainfall rates may result in 2-4" localized
    totals, isolated to widely scattered instances of flash flooding.

    Discussion...Convective coverage and intensity is increasing
    across a narrow (but clearly defined) warm sector late this
    afternoon, encompassing much of northern and eastern TX. The
    mesoscale environment is characterized by ML CAPE of 500-1500
    J/kg, PWATs of 1.6-1.8 inches (above the 90th percentile, per
    FWD/SHV sounding climatology), and effective bulk shear of 30-40
    kts. While forcing is rather limited (with DPVA and jet dynamics
    displaced to the northwest with the occluded low), there is
    sufficient moisture, instability, and shear to result in loosely
    organized convection. The stronger cells are capable of localized
    rainfall rates of 1-2"/hr, which may locally repeat to result in
    some 2-4" totals. With antecedent conditions being relatively dry
    (as 3-hr FFGs generally ranging from 2-4"), isolated to widely
    scattered instances of flash flooding are considered possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_qFjaY6-bGcjlRihJsvbuldex8RDL9fI5kXEfqniJxyGoDHDQdZZ_kEJ1WTR9IfM3yDb= Yv_a0oFQh492S_v5ufP3-Go$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...LCH...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 33479740 33369634 32969547 32679460 32449374=20
    31739351 30469417 30149512 30139626 30359702=20
    31259743 32129762 32899763=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 9 03:54:34 2024
    AWUS01 KWNH 090354
    FFGMPD
    LAZ000-ARZ000-TXZ000-090900-

    Mesoscale Precipitation Discussion 1142
    NWS Weather Prediction Center College Park MD
    1054 PM EST Fri Nov 08 2024

    Areas affected...Eastern TX...Adj. Northwest/Western LA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 090400Z - 090900Z

    SUMMARY...Potential for intense but scattered clusters of cells
    with efficient rainfall production possibily resulting in
    localized flash flooding.=20

    DISCUSSION...03z surface analysis depicts a triple-point low near
    FF4 and TYR at eastern-most bulge in the progressive cold front
    across N Texas through to the Central Texas Coastal Plain. An
    ill-defined stationary front extends generally due east and
    demarcates sfc Tds in the high upper 60s/low 70s from lower values
    northward in NE TX. The upper-low pressing eastward and
    associated height-falls are diminishing with its filling and so
    low level response in wind flow has seen a marked decrease to
    20-25kts across the warm sector becoming more parallel to the cold
    front. Generally reducing flux and overall moisture convergence to
    maintain a broader area of ascent. However, this is resulting
    into increased orthogonal intersection with the the stationary
    front providing isentropic ascent/convergence where moisture
    remains most pooled. Total PWat values remain AoA 2", and while
    there is a weak connection to low level moisture from outer
    periphery of Rafael's moisture pool, the winds are generally below
    15kts and so not really connecting to increase, but more weakly
    maintain the moisture across the warm sector.

    Unstable air in the warm sector still is more than sufficient to
    promote stronger updrafts, but given the weakening flow cells may
    become a bit more clustered/isolated. MLCAPEs of 500-1000 J/kg,
    2" PWs and 20-25kts should still support downdrafts capable of
    1.75-2"/hr. The limiting factor is likely to be residency,
    probability of totals over 2.5-3" are likely to be limited to the
    strongest cores. Though there is some potential that expanding
    eastward development along the isentropic boundary into LA may
    allow for some repeating convection with slow eastward cell
    motions along the slowing front. As such, a widely scattered
    incident or two of 3-4" is not out of the realm of possibility and
    have the potential to result in localized flash flooding concerns
    with best chances along/downstream of the triple point and
    stationary front.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7-jK2R8d8jFPIAVX4plhszCimB7X3SQBM7bAJKjsHGzftCGy6YPdq9AArZUqiUBjXN4A= XOBTOHsi6DD3THFAgchYqHY$ for graphic product...

    ATTN...WFO...FWD...HGX...LCH...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 33329498 33259398 32849342 32319323 31709335=20
    31069371 30549439 30479540 30959577 31799570=20
    33049567=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 9 07:25:37 2024
    AWUS01 KWNH 090725
    FFGMPD
    LAZ000-TXZ000-091200-

    Mesoscale Precipitation Discussion 1143
    NWS Weather Prediction Center College Park MD
    225 AM EST Sat Nov 09 2024

    Areas affected...Far Southeast TX...Southwest LA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 090725Z - 091200Z

    SUMMARY...Persistent redeveloping warm cloud tropical showers
    likely to proliferate over the next few hours with localized
    totals over 4" possible. Flash flooding is becoming increasingly
    possible through early morning.

    DISCUSSION...GOES-E 10.3um and LCH RADAR loop shows a few shallow
    topped cells across Hardin/Jefferson county that are starting to
    expand in coverage along a boundary layer convergence axis from
    Galveston Bay north-northeastward eastward of the approaching cold
    front. VWP and RAP analysis 850mb analysis shows 15-20kts of ESE
    flow slowing and stretch both northward toward the exiting
    northern stream shortwave associated with diffluent portion of the
    cyclonically curved 3H jet streak over E TX, and peripheral
    influence approaching tropical cyclone Rafael. This is resulting
    in solid speed convergence at the nose/pool of enhanced surface to
    850mb moisture (which further totals to near 2-2.2"). Proximity
    to the warmer theta-E off the Gulf, convective development has
    been fueled by sufficient 1500-2000 J/kg SBCAPE. While the overall
    depth of the updrafts are not very deep, the overall moisture flux
    convergence is sufficient for 2"/hr rates.=20

    Localized storm effects and approach of the cold front also have
    been aiding some flanking line development to counteract the slow north-northeast cell motions and allowing for increased rainfall
    totals over the last few hours in Hardin county. While much of
    the Hi-Res CAM suite has been deficient of development, the
    placement in those hi-res CAM fields seem to be displaced west and
    reduced in overall deeper layer convergence. One solution that
    appears to have this stronger convective axis is the FV3 CAM,
    which does suggest an narrower overall distance in the low level
    convergence coverage. Confidence is not very high given the lack
    of guidance support but observational trends. As such, flash
    flooding is considered possible, intense, but localized.=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Z4k6xfze70Dcd_-n1561acaO5OLboDz9elAXcLpq93-9bNwOaWMmyF8gbLAjhWPv0gQ= Dz6IHVAeM1_RtGSKySad9-4$ for graphic product...

    ATTN...WFO...HGX...LCH...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 31039431 31039338 30609305 29929324 29599390=20
    29449446 29179529 29929534 30729490=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 9 11:05:42 2024
    AWUS01 KWNH 091105
    FFGMPD
    LAZ000-TXZ000-091600-

    Mesoscale Precipitation Discussion 1144
    NWS Weather Prediction Center College Park MD
    605 AM EST Sat Nov 09 2024

    Areas affected...Southeast TX...Western LA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 091100Z - 091600Z

    SUMMARY...Slow moving, highly efficient cells along the front will
    continue to produce pockets of heavy rainfall and totals capable
    of inducing localized flash flooding. Scattered totals over 3-5"
    remain possible.

    DISCUSSION...Deep layer convergence through the warm sector over
    the northern Gulf and southern LA continues to drive convective
    development along the slowing/approaching cold fronta across SE
    TX. Strong upper-level divergence at the inflection of the
    cyclonically curved jet with maximized diffluence aloft as further enhanced/expanded convective development and isentropic ascent
    along and east of the triple point northeast of JAS, TX. CIRA LPW
    shows enanced surface to 700mb moisture through the warm sector
    though stronger 700-500 moisture along the northern coreo of
    Rafael remains distant enough for stronger WAA ascent later today.
    So with some weak steepening of lapse rates, modest instability
    remains in proximity of the Sabine River Valley to the triple
    point and should help to maintain updraft strength and focus
    moisture flux convergence to support 2-2.5"/hr rates. Duration of
    heavy rainfall may be more limited further north towad the
    entrance of the jet/divergence maxima as it slides away with the
    speed max with time. Spots of 2-4" across west-central to
    north-central LA may result in possible flash flooding over the
    next few hours.

    Furhter south, the east-southeast surface to 850mb flow
    decelerates into a col/weak surface wave near BPT. As such,
    similar deep layer moisture convergence and slightly enahnced
    surface based CAPE of ~1500 J/kg (due to proximity to the warmer
    Gulf) is providings stronger updraft strength. Due to proximity
    of slower low to midlevel flow, cells have been a bit more
    stationary/slow moving with time and some suggestion of upstream
    redevelopment toward the south may allow for some repeating;
    duration may continue to result in very localized but intense
    rainfall up to 2.5"/hr and localized totals of 3-5" over the next
    few hours. Given higher natural FFG values (only locally reduced
    due to 5-8" totals over Hardin, E Liberty and NW Jefferson
    counties), flash flooding from similar cells may continue risk for
    flash flooding.=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6y0ja-kMndB2N4alvpKCt4jkeWcz9qOm2DoHAuXzp-dONTaKfsOdPZF0XD7kXCwRTV7E= mvWcBA-dyczh4TMf8fSPNi8$ for graphic product...

    ATTN...WFO...HGX...LCH...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 32749283 32599214 32029213 31029271 29919333=20
    29709366 29439446 29149487 28989532 29809504=20
    30979455 32399364=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 9 16:14:15 2024
    AWUS01 KWNH 091614
    FFGMPD
    LAZ000-TXZ000-092200-

    Mesoscale Precipitation Discussion 1145
    NWS Weather Prediction Center College Park MD
    1112 AM EST Sat Nov 09 2024

    Areas affected...southwestern and central LA and surrounding
    portions of Upper TX Coast

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 091600Z - 092200Z

    Summary...Deep tropical moisture will support very high rainfall
    rates of 2-3"/hr with 6-hr totals of 3-6"+. Isolated to scattered
    instances of flash flooding are likely (and may locally be
    significant).

    Discussion...A stalling cold front is combining with deep layer
    tropical moisture transport from the southeast (in association
    with Tropical Storm Rafael) to result in significant moisture flux
    convergence into western LA and surrounding portions of the Upper
    TX coast. Precipitable water levels are indicated to be as high as
    2.2 inches (per CIRA advected layered precipitable water analysis
    and RAP mesoanalysis), which is well above the 90th percentile
    (per experimental ALPW sfc-850mb and 850-700mb percentiles and LCH
    sounding climatology) and more typical of late August to early
    September. Although instability is somewhat limited (500-1000 J/kg
    of ML CAPE), it remains sufficient for convection and is unlikely
    to be eroded with steady low to mid level moisture transport
    coinciding with peak diurnal heating. Likewise, deep layer shear
    of 20-30 kts will be supportive of organizing updrafts, while
    10-15 kts of deep layer flow will keep storm motions near a crawl
    (particularly so closer to the coast). All in all, a concerning
    mesoscale setup that will be supportive of locally significant
    flash flooding.

    Updated CAM guidance (12z HREF suite) is increasingly supportive
    of significant rainfall totals over the next 6 hours (HREF 40-km
    neighborhood probabilities for 5" exceedance, near the 10-yr ARI,
    threshold being near 15%), suggesting the potential for localized
    amounts of 3-6" (with rainfall rates of 2-3" due to the deep
    tropical moisture and slow storm motions). With much of this same
    area already having received 3-6" over the prior 6 hours (mainly
    areas west of Alexandria, as well as near Winnie, TX), the
    associated 4.0" 6-hr FFGs are likely underrepresentative of the
    flash flood threat. Given these antecedent conditons AND the
    possibility for rainfall amounts to overperform (given the ARW2
    solution of localized 6"+ totals), isolated to scattered instances
    of flash flooding are considered likely, and locally this flash
    flooding may be significant. The threat for significant flash
    flooding is also to likely extend beyond the next 6 hours, so a
    subsequent MPD is expected (with the threat likely becoming even
    more significant later this evening).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_9GOqR31doEVg5fnc5xBLOKROmNKwmylL07Vg5HTjGA4LzWucYoszOgIEinx0Dto94TB= hUNxkmu2h2KiO5ZQ46z5h_E$ for graphic product...

    ATTN...WFO...HGX...JAN...LCH...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 32279211 32069174 31219173 30399213 29919256=20
    29559297 29489403 29509452 30089430 30329421=20
    30769397 31419340 31809308 32219254=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 9 22:01:24 2024
    AWUS01 KWNH 092201
    FFGMPD
    MSZ000-LAZ000-TXZ000-100400-

    Mesoscale Precipitation Discussion 1146
    NWS Weather Prediction Center College Park MD
    459 PM EST Sat Nov 09 2024

    Areas affected...south-central LA and surrounding portions of
    Upper TX Coast and southwest MS

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 092200Z - 100400Z

    Summary...Deep tropical moisture will remain support of high
    rainfall rates (of 1-2"/hr) with additional 6-hr totals of 3-6"+
    likely. Locally significant flash flooding is expected to
    continue, and overall coverage of flooding is likely to become
    more numerous to widespread.

    Discussion...A wide band of rainfall with embedded heavier showers
    has persisted over the past several hours along a surface trough
    and ahead of a stalling cold front. Deep layer tropical moisture
    remains in place over southwestern LA and surroundings (in
    association with southwesterly low to mid level moisture transport
    from Tropical Storm Rafael), as indicated by precipitable water
    levels of 2.1-2.3 inches (per CIRA advected layered precipitable
    water imagery and RAP mesoanalysis). This tropical moisture is
    well above the 90th percentile (per experimental ALPW sfc-850mb
    and 850-700mb percentiles and LCH sounding climatology), and much
    more typical of late August to early September. While instability
    remains the primary limiting factor (limiting peak rainfall rates
    to 1-2"/hr), 250-500 J/kg of SB/ML CAPE has been sufficient for
    sustained heavy rainfall. Going forward, convection may continue
    to slowly shift to the southeast (depsite the front stalling near
    the LA/TX border), as SB CAPE has risen to 500-1000 J/kg over
    south-central LA and southwest MS. Deep layer shear has also
    increased a bit (to 25-35 kts), which should continue to be
    supportive of at least embedded organized updrafts (with
    diffluence aloft also improving with the right-entrance region of
    a broad 75 kt jet streak at 250 mb). And with deep layer flow as
    low as 15 kts, slow storm motions will continue to support a
    mesoscale setup capable of locally significant flash flooding
    (particularly over areas that have already received as much as
    3-6" of rain over the past 6-12 hours).

    Updated CAM guidance (18z HREF suite) remains supportive of
    additional significant to extreme rainfall totals over the next 6
    hours (HREF 40-km neighborhood probabilities for 5" exceedance
    threshold, also corresponding to the 10-yr ARI, as high as 50%),
    suggesting the potential for additional localized amounts of 3-6"+
    (through 04z). Much of this rainfall may occur near the already
    hard hit region in and around Alexandria, though propagation
    towards higher instability (south and east) appears to be a more
    favorable outcome (as suggested by several HRRR runs, as well as
    the ARW/ARW2/FV3 members of the HREF). Locally significant (to
    even extreme) flash flooding remains possible, conditional upon
    the rainfall axis remaining stalled over southwestern and central
    LA. Should the rainfall axis eventually shift towards the south
    and east, then additional numerous (to possibly widespread)
    instances of flash flooding will shift in tandem.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!58w_B5qH0gL7vkdnmlE6WNLKVuAaAyq5k-4rq9x2zYAyFF1sCaM890kvNXRJFgTDXw3J= f9XVGoaIOqodXgt3k1-IZlQ$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 32009189 31859111 31459090 30629139 30049208=20
    29699262 29599388 29619424 29939427 30429390=20
    30979347 31309313 31809265 31969237=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Nov 10 03:28:27 2024
    AWUS01 KWNH 100328
    FFGMPD
    MSZ000-LAZ000-TXZ000-100900-

    Mesoscale Precipitation Discussion 1147
    NWS Weather Prediction Center College Park MD
    1027 PM EST Sat Nov 09 2024

    Areas affected...Southwest to Central Louisiana...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 100330Z - 100900Z

    SUMMARY...Stationary axis of isentropic ascent/stationary tropical
    showers likely to maintain ongoing flash flooding across central
    Louisiana into the middle overnight period.

    DISCUSSION...Most meteorological parameters are continue to reduce
    with time; temperatures are coming down with loss of day-time
    heating and low level moisture has dropped into the low 70s, so
    instability is limited to this limited area of mid 70s over low
    70s Tds, with MLCAPE in the 500-1000 range. RADAR and GOES-E
    3.9um along with observations from VWP and surface obs suggest,
    easterly flow is starting to slack over the southern Bayous of
    central LA and adjacent Gulf slowly reducing deeper layer
    convergence along the rainfall reinforced cold front. Still, this
    is weak WAA over a modestly steep frontal slope to continue to tap
    weak convective development and moisture flux to support 1.5-2"/hr
    rates, given the total PWats remain near record values in the low
    2" range. Storm related outflow/isallabaric may result in a few
    embedded narrow cored cells that may occasionally tick above
    2"/hr.=20=20

    GOES-E WV shows cluster across SW to central LA remains at the
    nose of a split in upper-level flow/diffluence from anticyclonic
    outflow jet from Rafael over the northern Gulf and the
    cyclonically curved polar jet across E TX into AR. This helps to
    pull/stretch convective cores toward the northeast with weak
    inflow, balance southeast propagation from inflow and slow
    north-northeast cell motions to allow for very slow cell motion
    with very weak northeastward motion along the isentropical
    boundary and already flooded/lowered FFG values into far SW MS.=20
    Given the compromised soils the additional 2-3" with localized 4"
    maxima (in the embedded convective cores) will likely continue to
    result in rapid inundation/flash flooding that is occurring from N
    Calcasieu to Concordia parish.=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-67ABM8ikrGdxIgEEnhMvIWna6qG-GpnX7ZbjtCy0sV7uKxnepzGDVrbq26swO1r9aTH= F-EwAza0zYszhj4GLMUu1yo$ for graphic product...

    ATTN...WFO...JAN...LCH...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 32149228 32009174 31699148 31459150 31049181=20
    30609239 30319287 30159341 30399367 30859365=20
    31209353 31789309=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Nov 10 07:56:01 2024
    AWUS01 KWNH 100755
    FFGMPD
    LAZ000-101200-

    Mesoscale Precipitation Discussion 1148
    NWS Weather Prediction Center College Park MD
    255 AM EST Sun Nov 10 2024

    Areas affected...Central Louisiana...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 100800Z - 101200Z

    SUMMARY...Stationary isentropic boundary starting to dislodge from
    anchored position. Lingering scattered showers may intersect
    compromised soils/flooded areas to maintain localized flooding
    conditions over the next few hours.

    DISCUSSION...Regional RADAR loop shows stationary isentropic
    ascent boundary has recently encountered an increase in low level
    winds from 15-20kts to 20-25kts. This increase has allowed for
    the stable balance over the last 4-6hrs resulting in 6-12" of
    rainfall over N Allen/S Rapides Parishes to finally support an
    additional 3-5kts of propagation to the southeast. In addition,
    CIRA LPW and RAP TPW analysis suggest air within the increased ESE
    and SE flow is also starting to dry realitive to the peak core of
    moisture which is currently being ingested allowing for at least
    one more good surge of enhanced rainfall rates across Evangeline
    parish. Rates of 2-2.5" are likely to be short-lived maybe for
    1-1.5 more hours before further evaporating.=20=20

    Recent HRRR solution appears to be catching on the trend noted in
    RADAR/GOES-E SWIR with increased aggitated Cu along the stationary
    front across E TX into NW LA as well as tropical offshore cells
    along the outer edges/convergence bands of Rafael. ARW/ARW2
    solutions help with this devoltuion as well though timing remains
    a bit slow (typical of bias). Still, scattered showers in the
    vicinity of the saturated/flooded soils and with ample moisture,
    additional .5-1" totals may help maintain/prolong the flooding
    across central LA; as such, flash flooding remains possible for
    the next 3-4 hours, with reducing probability in time.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5n9DS4WF82ijCc_htERuSdOwShCYM6FBvP0XdWF8DBPlNH1hcbvZ8Yup3FsvOqK22lB-= VkmmwyX8_hcqfu1VNvKp_QI$ for graphic product...

    ATTN...WFO...JAN...LCH...SHV...

    ATTN...RFC...LMRFC...NWC...

    LAT...LON 31809201 31549169 31329167 30979182 30649193=20
    30309213 30309307 30539342 30819334 31239300=20
    31709237=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Nov 10 12:45:07 2024
    AWUS01 KWNH 101245
    FFGMPD
    MSZ000-LAZ000-101613-

    Mesoscale Precipitation Discussion 1149
    NWS Weather Prediction Center College Park MD
    744 AM EST Sun Nov 10 2024

    Areas affected...Central LA into Southwest MS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 101243Z - 101613Z

    Summary...A localized flash flood risk will continue across
    portions of central Louisiana and southwest Mississippi into mid
    morning.

    Discussion...Radar imagery indicates heavy rainfall cores are
    persisting a bit longer than anticipated over portions of central
    LA into southwest MS this morning. The 12z sounding from New
    Orleans is indicative of the upstream environment feeding into
    this axis of rainfall...and it shows a saturated profile up to
    500mb with PWs around 2.1". The sounding dries significantly above
    500mb, but a moist and skinny CAPE profile below that continues to
    support efficient warm rain processes. Thus despite a lack of cold
    cloud tops, this activity continues to be capable of hourly
    rainfall around 2".

    Generally still expecting a downward trend in rainfall coverage
    and intensity as the morning progresses. The overall environment
    should continue to trend less conducive for excessive rainfall
    with lower level convergence gradually weakening and subsidence
    and drying continuing to increase in the mid to upper levels. With
    that said, recent radar and satellite imagery suggests a localized
    flash flood risk will continue for a few more hours. Recent HRRR
    runs have started to catch on to a bit more persistence of this
    activity, although these 10z and 11z runs are too far northwest
    with the rainfall max. Overall expecting additional rainfall of
    2-5" over the next couple hours, with the heaviest amounts likely
    staying pretty localized in nature.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8etVTqWRZso_51Tg4JcXyMSXXv5seVfeDO1t7GsmYnCzbDxJ7GmpfzHf55OoepDXA0tw= 6EeDJ18SnA13Sqs-81gfnxs$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...

    ATTN...RFC...LMRFC...NWC...

    LAT...LON 31679099 31629054 31169035 30779045 30399092=20
    30299157 30369195 30689223 31189194 31539141=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Nov 10 14:04:38 2024
    AWUS01 KWNH 101404
    FFGMPD
    OHZ000-TNZ000-KYZ000-INZ000-ILZ000-102000-

    Mesoscale Precipitation Discussion 1150
    NWS Weather Prediction Center College Park MD
    903 AM EST Sun Nov 10 2024

    Areas affected...western and northern KY and surrounding portions
    of TN/IN/OH

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 101400Z - 102000Z

    Summary...Additional localized totals of 2-3" likely to lead to
    isolated to scattered instances of flash flooding.

    Discussion...Streaks of moderate to heavy showers have been
    ongoing early this morning across much of western KY into far
    southern IN, producing hourly totals of 0.5-1.0" (with 3-hr totals
    as high as 2.0-3.0"). This efficient rainfall is occuring within
    the warm sector of a mature low pressure system, centered over the
    Midwest. A strong low-level jet (40-50 kts at 850 mb) is providing
    ample moisture transport into the region, and low-level (925-850
    mb) convergence is significant. This convergence is better
    visualized via isentropic analysis with upglide most evident on
    the 294K and 296K surfaces (centered near 900 mb) at 30-40 kts.
    Aloft, the right-entrance region of a 100 kt jet streak is
    providing divergence to offset the low-level convergence, and
    convection is expected to continue within this zone of highly
    anomolous moisture (with PWs near 1.6", indicated to be near the
    max moving average per BNA sounding climatology).

    While the 00z/06z CAMs mostly indiciate forward-looking 6-hr
    totals maximized near 1", the HRRR and FV3 are indicating
    localized totals closer to 1-2" (with 06z HREF 40-km neighborhood
    probabilities for 2" exceedance as high as 25%). Given that
    2.0-3.5" amounts have been recorded over the past 3-6 hrs (already
    at or exceeding corresponding FFGs), additional isolated to
    scattered instances of flash flooding are considered likely (as
    the FLASH CREST unit streamflow response is already fairly robust
    from southwest KY to the greater Louisville metro area).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-V6kMD2POGD-MT7PUplmGTCdCtsrHEG5cB1Br-nKyn-O_zlNukeKKHD2Fd--tScs4jWD= 1r224KkxjUMG8bVTJd5in_M$ for graphic product...

    ATTN...WFO...ILN...IND...LMK...MEG...OHX...PAH...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 39328439 38718390 37448548 36198733 36148874=20
    36718898 37928762 38478667 38978573=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Nov 10 14:28:38 2024
    AWUS01 KWNH 101428
    FFGMPD
    OHZ000-TNZ000-KYZ000-INZ000-ILZ000-102000-

    Mesoscale Precipitation Discussion 1150...Corrected
    NWS Weather Prediction Center College Park MD
    927 AM EST Sun Nov 10 2024

    Corrected for discussion typo

    Areas affected...western and northern KY and surrounding portions
    of TN/IN/OH

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 101400Z - 102000Z

    Summary...Additional localized totals of 2-3" likely to lead to
    isolated to scattered instances of flash flooding.

    Discussion...Streaks of moderate to heavy showers have been
    ongoing early this morning across much of western KY into far
    southern IN, producing hourly totals of 0.5-1.0" (with 3-hr totals
    as high as 2.0-3.0"). This efficient rainfall is occurring within
    the warm sector of a mature low pressure system, centered over the
    Midwest. A strong low-level jet (40-50 kts at 850 mb) is providing
    ample moisture transport into the region, and low-level (925-850
    mb) convergence is significant. This convergence is better
    visualized via isentropic analysis with upglide most evident on
    the 294K and 296K surfaces (centered near 900 mb) at 30-40 kts.
    Aloft, the right-entrance region of a 100 kt jet streak is
    providing divergence to compliment the low-level convergence, and
    convection is expected to continue within this zone of highly
    anomalous moisture (with PWs near 1.6", indicated to be near the
    max moving average per BNA sounding climatology).

    While the 00z/06z CAMs mostly indicate forward-looking 6-hr totals
    maximized near 1", the HRRR and FV3 are indicating localized
    totals closer to 1-2" (with 06z HREF 40-km neighborhood
    probabilities for 2" exceedance as high as 25%). Given that
    2.0-3.5" amounts have been recorded over the past 3-6 hrs (already
    at or exceeding corresponding FFGs), additional isolated to
    scattered instances of flash flooding are considered likely (as
    the FLASH CREST unit streamflow response is already fairly robust
    from southwest KY to the greater Louisville metro area).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8kT9qV7btrgtkYBd1C7SbGtvmidrZdv1xjSrmZgpfU_NHz_bkoTDFKVb27nXPw88LUi2= 2Q6xpP_uJSAAjkkNOh15F2M$ for graphic product...

    ATTN...WFO...ILN...IND...LMK...MEG...OHX...PAH...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 39328439 38718390 37448548 36198733 36148874=20
    36718898 37928762 38478667 38978573=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Nov 12 21:28:18 2024
    AWUS01 KWNH 122128
    FFGMPD
    ORZ000-WAZ000-130900-

    Mesoscale Precipitation Discussion 1151
    NWS Weather Prediction Center College Park MD
    427 PM EST Tue Nov 12 2024

    Areas affected...western WA

    Concerning...Heavy rainfall

    Valid 122123Z - 130900Z

    Summary...Areas of heavy rain will move into western WA this
    evening and overnight with occasional rainfall rates in excess of
    0.5 in/hr, especially across the Olympics. Peak 12 hour rainfall
    totals of 2 to 4 inches are expected across the favored upslope
    regions of the Olympics and Willapa Hills.

    Discussion...GOES West water vapor imagery at 21Z showed an upper
    level trough centered about 900 miles west of the Pacific
    Northwest coast, containing embedded shortwaves. One of the more
    notable shortwaves/vorticity maxima was reflected in the visible
    imagery with a well-defined swirl near 45N 143W. Surface and
    visible satellite data identified an occluded cyclone extending
    outward from a surface low near 50N 140W and widespread cloud
    cover extending downstream from the associated IVT plume ahead of
    the cold front.

    As the upper trough and embedded vorticity maxima continue to
    advance eastward through early tonight, a triple point low is
    forecast to develop by a consensus of the latest numerical
    guidance by 00Z just southwest of 50N 130W with northward movement
    overnight. The attendant occluded/cold front will likely remain
    progressive toward the south and east, reaching the Olympic
    Peninsula in the 06-09Z time frame along with the maximum IVT,
    forecast by the 12Z model consensus to near 800 kg/m/s along the
    coast. 850 mb winds are expected to peak into the 70-80 kt range
    from the SSW within precipitable water values of 1.0 to 1.1 along
    the WA coast.

    Rainfall intensity will gradually increase in the 00-06Z window
    with peak rainfall rates possibly exceeding 0.5 in/hr in the
    Olympics prior to 06Z (40-50 percent via 12Z HREF, but adjusted
    for the 18Z HRRR and 18Z NAM_nest). Those probabilities of 0.5+
    in/hr rates increase to just over 80 percent by 09Z for the
    Olympics. The low level moisture transport will favor the highest
    rates over SSW facing terrain, including the Willipa Hills,
    although the probabilities for 0.5 in/hr in southwestern WA are
    generally less than 10 percent for the overnight period via HREF
    output. While rainfall intensity will be increasing overnight, the
    greatest coverage of higher intensity rainfall will likely come
    with the arrival of the frontal boundary though limited
    instability may temper maximum rates a bit. Nonetheless, strong
    forcing for ascent ahead of the approaching upper trough axis,
    including increasingly diffluent flow aloft, should allow for
    localized 12 hour rainfall maxima of 2-4 inches across the favored
    terrain of western WA through 09Z. These rains are expected to
    increase the potential for minor flooding across the region, but
    mainly focused into the Olympics.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6EjfNNttL9lCkLUPpgQVfgCmVfv0nDin0tNpJQr3VQormG-WGCa0OU3CDkYBdgjKZXZN= 7UYGW65BPymlwS6HHx2kg60$ for graphic product...

    ATTN...WFO...PQR...SEW...

    ATTN...RFC...NWRFC...NWC...

    LAT...LON 48132389 48022339 47862310 47662299 46932314=20
    46282296 46232337 46262403 46472435 46802458=20
    47242477 47682501 48112467=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Nov 13 07:50:55 2024
    AWUS01 KWNH 130750
    FFGMPD
    CAZ000-ORZ000-WAZ000-131800-

    Mesoscale Precipitation Discussion 1152
    NWS Weather Prediction Center College Park MD
    250 AM EST Wed Nov 13 2024

    Areas affected...Coastal and Cascades Ranges of E WA & E
    OR...Northwest CA...

    Concerning...Heavy rainfall

    Valid 130800Z - 131800Z

    SUMMARY...Progressive but potent slug of enhanced moisture flux
    along Coastal and Cascade Ranges producing 2-4" totals with
    occasional hourly rates to .5"/hr with greatest totals in SW
    facing orography increasingly so in SW OR/NW CA.

    DISCUSSION...GOES-W WV shows main core of the upper-low just south
    of 47N near 132.5W starting to slide northeast with upstream
    energy starting to dig the upper-trough, expecting to go more
    neutral tilt over the next 6-12hrs as it approaches the West
    coast. The 150kt jet core just rounding the base of the trough is
    broadening with large cirrus shield. GOES-AMV and RAP analysis
    note a split in the jet downstream northeast of the 40N130W
    benchmark; this is enhancing broader and more intense upper-level
    divergence along the Oregon coastline. Additionally, a weak
    inflection is developing in the low levels with upstream
    height-falls leading to sharper boundary layer moisture
    convergence along and downstream backing the progressive frontal
    zone a bit more flat to the mean steering flow and increasing
    deeper layer moisture convergence. CIRA LPW notes, 1-1.25" total
    PWat in this area where surface and slug of 850-700mb moisture
    overlap. Given 60-70kts of 850mb flow (~700-900 kg/m/s IVT),
    convergence is going to result in enhanced showers capable of
    .5-.6"/hr rates likely to intersect the northwest to central OR
    Coastal Range over the next few hours. So while the strength of
    orographic ascent will be consistent along the front, this
    slightly backed flow ahead of the inflection will have increased
    totals compared to the average 2-3" totals, some localized 3-4"
    values may occur before midday. Strength of AR and moisture flux
    may be supportive enough to bleed through the coastal range with
    some enhanced rainfall totals across the western slopes of the
    northern and central Oregon Cascades.

    To the north western WA...
    Post cold front showers will remain widely scattered, and with
    steeper lapse rates will support higher but much shorter duration
    rainfall across areas with modest 2-3" totals so far through the
    event, while NASA SPoRT soil saturation values are higher than
    normal, the burst nature is still not likely to result in any
    rapid inundation/flashy conditions but maintain above normal
    run-off.

    South of the inflection across SW OR into NW CA...
    The core of the AR moisture stream will remain along/ahead of the
    cold front, but will be narrowing as the mid-level moisture slug
    slides ashore and surface moisture band narrows/stretches in
    width. Height-falls will swing through later in the morning/early
    afternoon, but traditionally favorable southwesterly flow into
    generally steeper terrain and confluent 45-50kts of 850 flow
    around the Cape, prolonged moderate rainfall with streaks of
    enhanced showers up to .5"/hr are probable. This is still fairly gentle/typical for the boreal rain forests to handle much of the
    rainfall, and while run-off will be enhanced is not likely to
    result in any significant concerns that would not be for an
    ordinary AR. IVT values will be decreasing with reduced
    moisture/low level flow from 800 kg/m/s across the central OR
    coast toward 500-600 kg/m/s. Still, traditional orographic ascent
    will support spots of 2-3" by 18z.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7uODexacBzF7PVCxHek5wHR6MKxnMQhwIpYoJvfvjup-0Ov8g6M2EFYEquio7vwODp9r= kefoCOKvFOlq7e_FfljxRcM$ for graphic product...

    ATTN...WFO...EKA...MFR...PQR...SEW...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 49052223 49052156 48412141 46912178 45782182=20
    44322201 43042201 42212223 41802250 41082314=20
    39922370 39922426 40262453 40672460 41272434=20
    41832441 42292464 42812479 43492460 44162434=20
    45292434 46312415 47362445 47962475 48452475=20
    48192381 47962344 47252329 46952317 46832291=20
    47102235 47622223=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Nov 13 11:11:59 2024
    AWUS01 KWNH 131111
    FFGMPD
    MSZ000-LAZ000-131635-

    Mesoscale Precipitation Discussion 1153
    NWS Weather Prediction Center College Park MD
    611 AM EST Wed Nov 13 2024

    Areas affected...South-central Louisiana...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 131110Z - 131635Z

    SUMMARY...Slow moving, efficient cells capable of 2.5"/hr rain
    rates. Training profile and upstream redevelopment pose risk of
    localized flash flooding with 3-4" totals possible.

    DISCUSSION...The remnant low level circulation of Rafael has been
    shearing north to south through a deep axis, but has retained a
    few convergent low-level bands and fairly robust core of anomalous
    deep layer moisture. Aloft, large scale ridge over-top the
    circulation is also being stretched/amplified along/ahead of
    height-falls coming out of the central Plains. As a result, weak
    850-500 DPVA is providing ascent and low level wind response to
    increase surface to boundary layer moisture convergence with 25kts
    of 850mb flow from the southeast cyclonically converging at the
    apex/downshear of the wave just south of central LA coastline. A
    core of enhanced inability also exists through this moisture
    transport axis with 2000-2500 J/kg of SBCAPE to provide strength
    to vertical development over the next few hours. Within this axis,
    CIRA LPW shows core of enhanced moisture with 1-1.1" in the
    sfc-850, and over .5" in the 850-700mb layer. Both are near the
    99th to maximum percentile for climatology in November.

    Current GOES-E SWIR/10.3um EIR along with RADAR denotes initial
    convective development near Marsh Island lifting north through the
    best convergence/confluence axis. Cells are initially weaker with
    1-1.5"/hr rates, but with increasing DPVA/strengthening of the
    winds strengthening convergence, coverage of cells capable of
    2-2.5"/hr are likely to become more numerous as winds strengthen
    to 20-30kts by 13-14Z. Deep layer moisture is confluent into
    increasing FGEN/moisture axis, deformation zone that extends into
    central LA and up the Lower MS River Valley/Delta Region. As
    such, a favorable upstream convergence should support upstream
    development for potential training/repeating into a slowly (0-5kt)
    eastward drifting moisture gradient. Modest effective bulk shear
    in the 25-30kt range, suggest some weak rotation to the updrafts
    could further slow forward propagation resulting in localized axis
    of 2-4".=20

    While current trends suggest most cells will remain near the coast
    in the near-term, mid-morning could see further downstream motions
    toward areas of recent heavy rainfall and saturated upper soil
    depths...while FFG value have rebounded, 0-40cm saturation ratios
    remain over .65 which is the 90th-95th percentile, suggesting
    increased runoff in more likely north of I-10 into central LA.=20
    Still, coastal regions may be more receptive and scattered flash
    flooding/rapid inundation is considered possible through 16z.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7FmBQaNyYyaxEGU7iJdSVbg2p9LNhtvNU1_Cen-a4I8nvgWLcQ7NlSXTASh6rV2FLbSV= x2yeN2Tusbdc0jS-_jVQtK4$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...SHV...

    ATTN...RFC...LMRFC...NWC...

    LAT...LON 31769219 31579159 30609114 29649066 29069024=20
    28929090 29369197 29489241 29539295 29939321=20
    31079309 31539277=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Nov 13 16:33:32 2024
    AWUS01 KWNH 131633
    FFGMPD
    MSZ000-LAZ000-ARZ000-132130-

    Mesoscale Precipitation Discussion 1154
    NWS Weather Prediction Center College Park MD
    1132 AM EST Wed Nov 13 2024

    Areas affected...south-central/southeastern LA into southwestern
    MS

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 131630Z - 132130Z

    SUMMARY...Training and repeating of thunderstorms should maintain
    at least localized flash flooding from south-central and
    southeastern LA into southwestern MS. Localized rainfall rates of
    2 to 3+ in/hr will remain possible, falling atop locations which
    received heavy rain in recent days. Additional totals of 2 to 4
    inches will be possible (perhaps locally higher) through 22Z, but
    the coverage of these higher rainfall totals should remain
    low/spotty.

    DISCUSSION...Areas of training thunderstorms in and around the
    Lafayette metro have resulted in numerous reports of 4-6 inches of
    rain over the past 4-5 hours with hourly rainfall as high as 4
    in/hr. Heavy rainfall has been focusing along an inverted trough
    or weak frontal boundary extending northward from a weak/elongated
    low located just south of Marsh Island with the coldest cloud tops
    over southwestern MS into adjacent areas of LA at 16Z. 12Z
    soundings from LCH and LIX combined with Layered PW Imagery from
    CIRA showed the bulk of the nearly 2 inch precipitable water
    values are focused below 700 mb, with a fair amount of dry air in
    the middle and upper troposphere.

    Over the next 3-6 hours, the elongated area of low pressure/shear
    axis across LA is expected to slowly but steadily get pushed east
    ahead of a large-scale 700-500 mb trough moving east across the central/southern Plains. Surface to 850 mb convergence will shift
    into the southwestern quadrant of MS and southeastern LA through
    21Z where MLCAPE of 500-1500 J/kg is forecast to reside (highest
    to south) via the latest RAP guidance. Areas of training
    thunderstorms are expected to continue with 2 to 3+ in/hr rainfall
    rates at times, overlapping with areas that received heavy rain
    over the weekend and may remain hydrologically more sensitive to
    runoff.

    Farther east, a low level axis of convergence/leading edge of
    moisture return to the south of an East Coast surface ridge has
    been producing a few showers and thunderstorms. This area of
    convection is likely to shift east as well in a mostly progressive
    fashion, but an isolated threat for short term training could
    result in urban flooding for the New Orleans metro over the next
    few hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4tLj5AP-59ex4RZwax1shPABq6k0zjoqsPm_gIICJlTSMXmSSdewwAoW9g_QzwMRn-Li= Em8Cr5v2lBAGXPU1O0pzBEM$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MEG...

    ATTN...RFC...LMRFC...NWC...

    LAT...LON 33859027 33688989 33368956 32838930 31428951=20
    30298983 29499014 29689133 30039181 30799201=20
    32179173 33329125 33839080=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Nov 13 22:02:34 2024
    AWUS01 KWNH 132202
    FFGMPD
    TNZ000-KYZ000-INZ000-ALZ000-ILZ000-MSZ000-140400-

    Mesoscale Precipitation Discussion 1155
    NWS Weather Prediction Center College Park MD
    501 PM EST Wed Nov 13 2024

    Areas affected...MS River Valley into northern MS, western TN/KY,
    southwestern IN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 132200Z - 140400Z

    SUMMARY...Training thunderstorms across the lower MS/OH Valleys
    will be capable of 1 to 2+ in/hr rainfall rates and localized
    totals up to 3 inches through 04Z. Isolated flash flooding may
    occur as a result.

    DISCUSSION...Infrared satellite and radar imagery showed scattered
    showers and thunderstorms across the lower OH and MS Valleys into
    portions of central MS/western AL as of 2130Z. Forcing for ascent
    included lift ahead of a mid-upper level trough moving east
    through the central/southern Plains, with cells near and east of a
    low level (925-850 mb) confluence axis located across the lower MS
    Valley, which also extended northward into the lower OH Valley
    although not as strongly when compared to locations farther south.
    Low level warm advection was also contributing to heavier rainfall
    across the IN/KY border, located at the leading edge of 50-60 kt
    850 mb winds via VAD wind and short term RAP forecast data.
    Instability was somewhat limited however, with 500 to 1000 J/kg
    MLCAPE confined to central MS and elevated CAPE in excess of 500
    J/kg in pockets farther north into western KY via 21Z SPC
    mesoanalysis data.

    Water vapor imagery showed the mid to upper level trough over the
    central Plains acquiring a negative tilt which wil continue east
    into the overnight. Out ahead, diffluent flow across the lower OH
    Valley will aid in ascent with the slow eastward moving axis of
    low level confluence likely allowing for repeating/training rounds
    of heavy rain which could allow rates to reach into the 1-2 in/hr
    range through early overnight.

    To the south, across central/northern MS into western TN, locally
    higher instability should support greater intensity rainfall with
    ascent aided within the right entrance region of a 100-110 kt
    upper jet max located east of the advancing upper trough. The axis
    of low level confluence located in MS/western TN is expected to
    translate slowly but steadily toward the east over the next few
    hours which should limit training potential, however, periods of
    short-term training will still be possible, including the
    potential for more organized cells due to the combination of
    greater instability and favorable shear profiles. Rainfall rates
    of 1 to 2+ in/hr cannot be ruled out along with isolated areas of
    flash flooding through 04Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7OHFwLbNh11sOpNmvwiFeD7aeQcr4aO1WoVQgLU7WPVyU2fYz_h7LYtEB3Ox3Uk0p2DJ= SxMwR_xY7W8XO8rqLXmkJxM$ for graphic product...

    ATTN...WFO...BMX...HUN...IND...JAN...LMK...MEG...OHX...PAH...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 38778598 38258572 37498613 35788696 34348750=20
    32798866 32829016 33219054 34799016 36148939=20
    37438836 38618692=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Nov 14 02:56:08 2024
    AWUS01 KWNH 140256
    FFGMPD
    FLZ000-ALZ000-MSZ000-140830-

    Mesoscale Precipitation Discussion 1156
    NWS Weather Prediction Center College Park MD
    955 PM EST Wed Nov 13 2024

    Areas affected...Eastern MS...Much of AL...Far Western FL
    Panhandle...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 140255Z - 140830Z

    SUMMARY...Intense thunderstorms capable of a quick sub-hourly 1-2"
    near the front pose mainly urban flash flooding threat, while
    slower moving more scattered supercells within the Coastal Plain
    may result in a axis or two of 3-4" totals with similar localized
    flash flooding concerns through early overnight period.=20

    DISCUSSION...GOES-E WV suite depict slightly below average closed
    low crossing IA/MO with a well defined cold front/warm conveyor
    belt system across the Lower Ohio, Western Tennessee River Valleys
    extending south into MS where it is interacting with enhanced deep
    layer moisture and remnant low level circulation energy of ex-TC
    Rafael. CIRA LPW and RAP analysis denote enhanced tropical
    moisture and higher than normal theta-E air extending northward
    along a core of 30-35kt 850 southerly low-level jet. However, the
    deepest moisture and unstable air remains further south, generally
    in the lower 2/3rds of eastern MS into western AL, with maximum
    unstable air of 2000-2500 J/kg along the central Gulf Coast.=20
    Strong height-falls and right entrance ascent to 3H 100 kt Jet in
    the central MS Valley is providing the oblique but sufficient
    intersection with the cold front to generate convective cells from Starkville/Columbus MS southward to the tail of the
    front/inflection near the apex of the remnants of Rafael east of
    McComb. Given the stronger LLJ/divergence aloft remains displaced
    from best moisture/instability, cells still remain potent with
    capability of generating 1-1.5" total though with waning
    instability, updrafts continue to diminish from north to south
    over the next few hours. Still, there are urban targets along
    this track and with the sub-hourly totals near or over 1hr FFG
    particularly north and west AL and west central MS remains at low
    end risk for localized flash flooding for the next few hours.

    Further south, slightly backed flow as a result of the sheared
    inflection from ex-Rafael, moisture/instability axis is extended a
    tad eastward. Effective bulk shear is stronger to the north but
    given stronger SBCAPEs and backed low level flow, the potential
    for widely scattered supercells remains possible. Slower eastward
    propagation combined with natural slowing of rotating cells,
    allows for increased duration. Combined with broader updraft and
    enhanced directional convergence at the base of the updrafts,
    greater moisture flux of higher surface to 850mb moisture
    (gnerally 1.5"-1.75 per CIRA LPW through 700mb) will increase
    rainfall efficiency and localized duration. Rates of 2-2.5"/hr
    with localized spot of 3"+ possible in 1-2 hours pose a flash
    flood risk, especially given recent above average rainfall per
    AHPS and lowered FFG values in S AL. However, currently the best
    candidate cells is along/just south of Mobile Bay and in Greene
    county MS moving into Washington AL. As such, flash flooding
    remains possible through the early overnight period as well across
    S AL into far W FL panhandle.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!65FWgPo9OegZLuChIQEmJWRU1VncI7-KOLiEe1jSEbUXsAKI5p6t-XGTHad_VgZdlOlP= ghtJxuufFgiQ4y6sjTUHibM$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34268695 34178620 33838592 33308574 32408606=20
    31518649 30568702 30258757 30218794 30368823=20
    30738837 31038898 31348964 32108965 33258859=20
    33948776=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 18 21:57:06 2024
    AWUS01 KWNH 182157
    FFGMPD
    MSZ000-LAZ000-TXZ000-190400-

    Mesoscale Precipitation Discussion 1157
    NWS Weather Prediction Center College Park MD
    455 PM EST Mon Nov 18 2024

    Areas affected...Far Southeast TX...Southwest to Central LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 182200Z - 190400Z

    SUMMARY...An increase in coverage of showers and thunderstorms can
    be expected going into the evening hours. Heavy rainfall rates and
    potentially some areas of cell-training may foster some localized
    potential for flash flooding.

    DISCUSSION...As a deep upper-level trough pivots northeastward
    through the central Plains and toward the Midwest, a cold front
    will be gradually approaching the northwest Gulf Coast region.
    This front will be interacting with a very moist and increasingly
    unstable airmass out ahead of it this evening, and the result is
    expected to be an increase in the coverage of heavy showers and
    thunderstorms.

    PWs are quite high right now across southeast TX with values near
    or slightly above 2 inches, and these magnitudes are as much as 2
    to 3 standard deviations above normal for this time of the year.
    Meanwhile, MLCAPE values have risen to as much 1000 to 1500 J/kg
    and thus a moderate level of buoyancy has already pooled ahead of
    the front with the aid of daytime heating.

    A fairly strong southerly low-level jet of 30 to 40+ kts will be
    maintaining somewhat enhanced moisture transport off the Gulf of
    Mexico ahead of this front this evening. This coupled with the
    level of instability and favorable bulk shear should yield
    relatively organized bands or clusters of convection, including
    potentially some supercell activity, that will be capable of
    producing rainfall rates of 1 to 2 inches/hour. Initially the
    activity will be more focused over areas of far southeast TX, but
    should in time concentrate increasingly over southwest to central
    LA.

    Some of the more organized activity may involve some cell-training
    as the convection becomes aligned with the deeper layer mean flow,
    and this may result in the potential for locally excessive totals.
    The 12Z/18Z HREF guidance supports some 2 to 4 inch rainfall
    amounts with isolated heavier totals. A localized and mostly urban
    flash flood threat will exist as these bands of convection come
    through this evening.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6jucQIqEYwpxCvflmYFiKiE8VFtMqgbz0oaNbKbL_kmV0P55GzA3aCGc1dkx8VLC1nES= J4HizpGEPbfo3Q_5v0bbbow$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 32289212 32109155 31229155 30039244 29619285=20
    29709339 29649395 29909426 30469430 31049394=20
    32059292=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Nov 19 13:44:14 2024
    AWUS01 KWNH 191344
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-191900-

    Mesoscale Precipitation Discussion 1158
    NWS Weather Prediction Center College Park MD
    843 AM EST Tue Nov 19 2024

    Areas affected...Eastern LA...Southern MS...Southern AL...Far
    Western FL Panhandle...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 191345Z - 191900Z

    SUMMARY...Highly anomalous deep moisture and strength of flux
    allowing for efficient rainfall production with progressive
    pre-frontal trough. Embedded slower moving rotating updrafts will
    enhanced localized rainfall totals of 3-5" resulting in possible
    flash flooding.

    DISCUSSION...GOES-E WV suite depicts a large scale closed low
    dominating the northern Plains with negative tilt lower scale wave
    moving through the western Great Lakes, this is driving a very
    strong mid to upper level jet across the Mississippi Valley which
    in turn is spurring an very broad and strong low-level jet out of
    the Tropics into the central Gulf of Mexico intersecting the
    central Gulf Coast. CIRA LPW shows nose of 1-1.25" surface to
    850mb starting to near the southern TN boarder while as broad as
    central LA to western FL Panhandle. Combined with 40-45kts of
    southerly 850mb winds and 60-90 degrees of directional
    convergence; brings moisture flux values into the 99th and maximum
    percentile rankings over a vast area of the Deep South.

    An embedded shortwave/inflection can be analyzed through depth
    across S MS at the broad left entrance of the 120kt polar jet
    across AR/N MS, but also a weak diffluence region across S MS/AL
    in the wake of an exiting sub-tropical jet streak that is rounding
    the downstream large scale ridge into the Southern Appalachians.=20
    So while the height-falls are driving the cold front forward,
    there is weak surface to 850mb wave in S MS that is backing
    low-level flow and increasing flux convergence in that region, as
    well as further upstream in the coldest tops/highest unstable air
    across the mouth of the MS River and northern Gulf of Mexico. The
    instability gradient is along the Gulf Coast and as a result
    strongest cells/tops to -83C have been measure and with moisture
    values of 2.5-2.75", rates of 3"+/hr are possible across SE LA for
    the next hour or so. Near the surface inflection, weaker
    instability but solid flux convergence and increased bulk shear
    will allow for short-term efficient rainfall production to 2"/hr;
    with the vast majority falling in a sub-hourly manner given
    forward progress. This should result in possible flash flooding
    for urban and prone areas across E LA into S MS/S AL over the next
    few hours as the pre-frontal convergence zone slides east.=20

    As the morning progresses, bulk shear values increase over 40kts
    along and east of the inflection as it slides slower to the east
    in the further enhancing right entrance (increasing to 130-140kts)
    300mb jet. This will slow the frontal zone as well, and allow for
    some modest/weak instability to build back west to the boundary.=20
    Embedded rotating updrafts have a higher probability of occurring
    and with backed/increased directional moisture flux and reduced
    forward speed/propagation... downdrafts with capability to produce
    2.5-3"/hr rates may occur. Recent HRRR and 00z Hi-Res CAMs hint
    at this solution across the lower 2-3 rows of counties in
    MS/AL...combine this localized increase of 2-4" with the preceding
    progressive but intense showers on the pre-frontal trough and
    localized 3-5" totals become increasingly possible. Given the
    bulk of unstable air remains offshore, there is some reduction in
    confidence that updrafts will be strong enough to overcome the
    increased bulk shear to support these increased rates. However,
    the potential remains and would be the most likely driver to
    potential flash flooding events even into rural areas where FFG
    values of 3-4"/3hrs are more representative of soil conditions.=20=20
    As such, flash flooding is considered possible through the morning
    into early afternoon.


    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!82ah6Q-ckqRNkevsaGmwb3_q2Kwc4cqt7J5U3jZ97nTD6YePil4ppAX3h0_tzJL-7b3d= Z06AH1XwYUP9HIoSnMGcCRc$ for graphic product...

    ATTN...WFO...BMX...JAN...LIX...MOB...TAE...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 32648645 32208539 30938530 30128581 30188632=20
    30098773 29628864 29068883 28878931 29139023=20
    30578966 31758890 32518776=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Nov 19 20:03:20 2024
    AWUS01 KWNH 192003
    FFGMPD
    CAZ000-ORZ000-WAZ000-200630-

    Mesoscale Precipitation Discussion 1159
    NWS Weather Prediction Center College Park MD
    302 PM EST Tue Nov 19 2024

    Areas affected...Coastal Ranges of WA, OR and Northwest CA...

    Concerning...Heavy rainfall

    Valid 192000Z - 200630Z

    SUMMARY...Approach of occluded/cold front into WA/OR after 00z;
    start of prolonged moderate rainfall with strong Atmospheric River
    into SW OR/NW CA...

    DISCUSSION...GOES-W shows a classic evolution of a rapidly
    deepening 'bomb' cyclone just north of 45N132W, with impressive
    comma-head baroclinic shield expanding along the NW and N side
    while a clear slot/descending branch over the SW and southern
    hemispheres. Central pressures have gone from 1014mb to estimated
    955mb from OPC in the last 24hrs. A broad sub-tropical jet cirrus
    canopy with subtle ridging at the apex of the cold front
    42.7N129.5W indicates the anticyclonic rotor of the nose of the
    140kt jet directed toward the central OR coast. Clearing aloft,
    has allowed a view of narrow convective elements along the
    occluded portion of the front where steep lapse rates/CAA aloft
    support a narrow ribbon of 500-750 J/kg of SBCAPE. CIRA LPW shows
    sfc-700mb layers remain very narrow stretched along/ahead of the
    cold front, before broadening to a broader wedge of slightly above
    average moisture values south of 38N and west of 134W,
    approximately delineating a warm front. Enhanced 700-500
    moisture hugs the entire length of the mid to upper level jet and
    portion of the cold front (WSW to ENE orientation) that parallels
    (generally west of 130W). As such, total PWats of 1-1.25"
    southwest of the warm front are showing very high moisture flux on
    60 to 90kts of 850mb southwesterly flow helping to build IVT
    values of near 900-1000 kg/m/s.

    This front will continue to advance quickly toward the coast over
    the next few hours with similar orientation/northward expansion of
    the warm front. Further strengthening of the occluded low will
    bottom out toward mid to upper 940mb range but start a cyclonic
    loop reducing the surface to boundary layer impetus and expand the
    occluded front in a northwesterly manner. As such, elevated
    convection will reduce in forward speed reaching the coast and
    with further narrowing influences and upper-level jet expanding
    further eastward into the central OR...convective elements will
    become more fractured in nature only to increase orographic ascent
    light rainfall from 1/20th to .1" per hour with scattered streaks
    of .33-.5"/hr resulting in spotty 1-1.5" totals along favored
    southwest facing coastal ranges from central OR northward.

    Further south, the leading edge of heavy rainfall/WAA should be
    arriving in the 03-06z time frame toward Southwest Oregon and
    Northwest California. IVT values in the 400-500 range will
    increase toward 700 kg/m/s by 06z. Weakly unstable air near the
    triple point and just upstream along the cold front in the warm
    sector could see enhancement of rates from .5-.75"/hr along or
    just offshore by 03z. HREF 1"/hr probability reach 50% along the
    coast by 06-09z, though 1"/3hr values are over 75% with spots
    offshore near 100% nearing the NW CA coast. At this point, there
    is not likely to be sufficient coverage/intersection with coastal
    locations to result in excessive rainfall/flash flooding...though
    may become more of a risk after 06z.

    As such, will leave the hazard tag as only Heavy Rainfall expected
    for this MPD; but this rainfall south of central OR will only set
    the stage for upcoming likely significant rainfall across the area
    over the next few days. Please keep attune to further MPDs, AHDs
    from the National Water Center and flooding/hydrological
    advisories and statements from local forecast offices over the
    coming days.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-aoHmH-pg9_tbypJXyH5IpgccCd57z5Fbcvw0YTle1efs_OIdqJmrTmfGQpuSwemuzuD= E2CC-hYKQhjX9vo5iH--CfA$ for graphic product...

    ATTN...WFO...EKA...MFR...PQR...SEW...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 48362483 47992415 47312359 46222336 44762359=20
    43682404 42632396 41762381 41132348 40532340=20
    40082363 39962415 40302456 40942483 41312460=20
    42102453 42852471 43562456 45212426 46672449=20
    47422475 47872490 48102498=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Nov 20 13:09:27 2024
    AWUS01 KWNH 201309
    FFGMPD
    CAZ000-ORZ000-202100-

    Mesoscale Precipitation Discussion 1160
    NWS Weather Prediction Center College Park MD
    806 AM EST Wed Nov 20 2024

    Areas affected...Northern California... Far Southwest Oregon...

    Concerning...Heavy rainfall

    Valid 201300Z - 202100Z

    SUMMARY...Solid, persistent Atmospheric River to continue
    throughout the morning into afternoon. Typical .25-.33"/hr rates
    may occasionally tick up to .5" for an hour or so occasionally
    with localized embedded pulses across Southwest facing terrain.=20
    Solid 2-4" for terrain with 1-2" for lower slopes/valleys by 21z.

    DISCUSSION...GOES-W SWIR and regional RADAR mosaic, shows the back
    edge of the atmospheric river nearing the OR/CA boarder as the low
    to mid-level drying under the core of the upper-level jet
    continues to press the occluded front across W WA through to the
    SW OR coast. The triple point appears in a traditional location
    just north of Cape Mendocino before it jumps south as the front is
    expected to reach the CAPE over the next few hours. While the
    near record deep cyclone continues to slowly wobble north, there
    remains still a bit of height-falls to allow for the front to
    continue a slow sag southward. Well upstream, a subtle shortwave
    near 35N and 140W is starting to amplify with downstream
    baroclinic leaf forming between 140 and 130W; but that is well
    away off, but will likely start to have some influence with
    localized shortwave ridging and finally stall the southward
    progression of the front, likely between 21-00z.=20

    Southward drift relative to the coast remains a few miles an hour,
    the core of 50-65kts of slightly cyclonic 850mb flow into
    southwest facing orography will shift from S Humbolt county
    currently, through Mendocino, likely reaching Sonoma and far
    northern Marin county by 18-21z. With exiting of stronger
    height-falls, winds will tapper but only slightly and remain at
    50kts in the 850mb layer. CIRA LPW and RAP analysis show core of
    highest sfc-700mb is now nosing into the coast and rain-rates are
    likely to increase from the .25-.33" to .5"/hr at that nose for a
    few hours before slipping south (with lingering .25-.5"). HREF
    .5"/hr probability remains well above 75%, with a secondary maxima
    along the lower slopes of the northern Sierra Nevada Range. The
    strength of the WAA will likely keep freezing levels lifting up
    from 2000 to 5000 ft throughout the day. Allowing the lower
    slopes to see similar rainfall rates/impacts nearing 2-4" by 21z.=20
    Valleys will obviously see much less, but still beneficial 1-2"
    are probable (with exception of directly in rain-shadow of the SW
    facing peaks).

    As the AR plume, reaches its southward extent in the 18-00z time
    frame, winds will still further slack, but PW will be increasing
    as deep layer flow becomes unidirectional and each layer
    contributes to near 1.5" (still well offshore); basically, as the
    strength of flow decreases it will be bolstered by increased total
    moisture and so rates are likely to remain fairly steady
    throughout with only those localized embedded pulses reaching
    above .5"/hr. While the soils continue to further saturate, with
    increasing run-off as it does so; overall rates still do not
    likely reach flash flooding concerns quite yet, but localized
    slower rise flooding and nuisance/urban flooding will remain
    probable.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-NpsoHZsM_OUATdSdbSPD3yFgX8RZicD4HuiKTwQaIY1LQgQKrtdKEVYNtLSPWdFY0i2= xVOZWeZWUOprtv22DV40tsM$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...STO...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 43012444 42922411 42582386 42142365 41592353=20
    41102336 41032265 40992258 40992209 40622192=20
    40152181 39602136 39232098 38702111 38332155=20
    37832268 38392350 39202397 39972440 40582462=20
    41222436 41822441 42262459 42652467 42972457=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Nov 20 20:30:32 2024
    AWUS01 KWNH 202030
    FFGMPD
    CAZ000-210600-

    Mesoscale Precipitation Discussion 1161
    NWS Weather Prediction Center College Park MD
    329 PM EST Wed Nov 20 2024

    Areas affected...Northern California...

    Concerning...Heavy rainfall

    Valid 202030Z - 210600Z

    SUMMARY...Strong, persistent heavy rainfall signal continues into
    north-central coastal Range and starting to bleed over to the
    northern Sierra Nevada range with times of .5-.75"/hr rates and
    additional 3-4" totals by 06z.=20

    DISCUSSION...GOES-W WV suite depicts a weak baroclinc leaf with
    transverse banding lifting northeast toward and starting to
    intersect with the SW Oregon coast, this is indicative of a
    broadening right entrance to the polar jet and short-wave ridging
    across northern California. As such, the forward progression of
    the front has fully stalled with weak rain-cooled support pressing
    the pre-frontal convergence/isentropic band across Sonoma/Santa
    Rosa counties at this time. The upstream edge of the divergence
    pattern aloft well-offshore is helping to spur a weak surface low
    along the front which will help lift the best moisture flux
    convergence axis northward after 23-00z with some increased
    southerly flow at the coastline, shifting the axis back to
    Menodcino county later in the valid time period (03-06z).=20

    Recent surface observations have seen dew-points rising through
    the San Francisco Bay and filtering into the Sacramento Valley,
    suggesting the warm front has over-topped or is near over-topping
    the coastal range. CIRA LPW hints at this as well with .5-.75" at
    the sfc/850mb layer pressing through the north-central CA coast.=20
    LPW also denotes better alignment through depth and so moisture
    totals are reaching 1.3" and nearing 1.5" just upstream off-shore.
    Total IVT ranges are about 750-900 kg/m/s along and just offshore,
    given said moisture and continued solid 50-60kts of fairly
    orthogonal 850mb flow in the core of the PW plume. As such,
    .5"/hr rates in the coastal range are increasingly probable
    supported by 50-75% neighborhood probability along the coastal
    range wavering north/south with the passing surface inflection
    toward 03z. Totals across the coastal range vary from 2-4.5" and
    soils are starting to fully saturate. FFG values along the spine
    are about 1.5"/3hrs and given the recent saturation, it is
    becoming increasingly plausible of exceedance but probably
    probability still remain just below threshold.=20

    As mentioned, deeper moisture is filtering through the Sacramento
    Valley, though cooler and drier air remains coincident with the
    front range, this further intensifies the isentropic ascent plane
    increasing verticality of of the showers. Core of the plume still
    appears directed at the Butte/W Plumas county slopes, and HREF
    probability of 1"/hr reach 15-20% suggesting a spot or two for a
    few hours are likely to reach .75"/hr of rainfall, peaking in the
    23-01z time frame. Even IVT values are in the 600+ kg/m/s range
    supporting this potential.Persistence of southwesterly warm-air
    advection will press freezing levels steadily up slope as well,
    broadening the area of moderate to heavy rainfall in steeper
    terrain. Similar but slightly higher 1.5-2"/3hr FFG values exist
    across this area and while there is increased potential for higher
    intensity rates, the duration of moderate to heavy rainfall
    pre-cursory to this surge has been limited relative to the coast.=20
    While a spot or two of FFG exceedance is possible, it will need to
    be monitored closely...but will continue to maintain a Heavy
    Rainfall tag for this MPD valid time.

    Further north toward Cape Mendocino into the SW slopes of the
    Trinity Range...
    The core of the moisture will continue to be focused south, but
    given proximity to the stationary front/triple point, convergence
    should be maximized to allow for similar occasional upticks to
    .5"/hr. Given this area has the climatologically wetter climate
    and higher natural FFG values, the risk for flooding will continue
    to be better accommodated than further south. Though and
    additional 2-3" rainfall expected; this further saturation will
    result in greater run-off further setting the stage for expected
    activity over the next coming few days.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9xDAmHd0dfUfszK6USAAuGP2uXiKZFEHFeccEVhVueDyl15euGpcO2pRhLV0bGHSAjo9= jRsvBSK4K2yv0Y6fPc8nx7I$ for graphic product...

    ATTN...WFO...EKA...MTR...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 41782411 41612388 41312362 40982347 40982270=20
    41072204 40152159 39422087 38702061 38422091=20
    38292172 38102232 37872287 38332328 38832377=20
    39622397 40022422 40352452 40642443 41242428=20
    41672428=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Nov 21 06:01:35 2024
    AWUS01 KWNH 210601
    FFGMPD
    CAZ000-211800-

    Mesoscale Precipitation Discussion 1162
    NWS Weather Prediction Center College Park MD
    100 AM EST Thu Nov 21 2024

    Areas affected...Northern California

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 210600Z - 211800Z

    SUMMARY...Nearly stationary atmospheric river will maintain heavy
    rainfall across northern CA through Thursday morning with
    increasing concerns for widespread areal flooding and possibly
    some burn scar flash flooding.

    DISCUSSION...The latest GOES-W Airmass RGB satellite imagery in
    conjunction with CIRA-ALPW data shows a well-defined atmospheric
    river and an associated front currently stalled over northern CA
    and the adjacent offshore waters extending southwestward off the
    West Coast. Strong warm air advection and moisture transport
    focused in close proximity to this front continues to overrun
    northern CA with rather widespread moderate to heavy rain
    impacting the region.

    Strong low to mid-level southwest flow around the south side of a
    powerful deep layer cyclone west of Vancouver Island will be
    locked in place overnight and through Thursday morning which will
    maintain enhanced atmospheric river activity over northern CA.
    Multiple weak waves of low pressure are expected to ride
    northeastward along the front over the next 6 to 12 hours which
    will take aim on the northern CA coastal ranges, and this will be
    facilitated by some backing of the mid to upper-level flow as
    additional shortwave/jet energy digs through the base of the
    larger scale trough offshore of the West Coast.

    Enhanced 850/700 mb moisture flux coupled with the deeper layer
    warm air advection pattern and orographic ascent/upslope flow over
    the higher terrain of northern CA will focus a persistence of
    moderate to heavy rain, with IVT magnitudes north of the Bay Area
    reaching 500 to 750+ kg/m/s. This will support elevated rainfall
    rates which based off the 00Z HREF guidance should occasionally
    reach well into the 0.50" to 0.75"/hour range. Some isolated rates
    potentially exceeding 0.75"/hour will be possible and especially
    over southern parts of Humboldt County where the southwest-facing
    slopes will see stronger orographic ascent coupled with very close
    proximity of the aforementioned front.

    The persistence of these elevated rainfall rates over the next 6
    to 12 hours will likely result in additional rainfall amounts by
    18Z (10AM PST) Thursday morning of 3 to 5 inches over the coastal
    ranges and the foothills of the northern Sierra Nevada, with some
    isolated 6+ inch amounts possible. These rains will be in addition
    to the already several inches of rain that have fallen for the
    event, and thus isolated some storm total amounts by late Thursday
    morning may well be 10+ inches. Lesser amounts of as much as 1 to
    3 inches will generally be expected for the interior valleys
    including the northern Sacramento Valley.

    Expect increasing concerns for widespread areal flooding impacts
    from the additional rainfall going through Thursday morning, and
    this may include some concerns for burn scar flash flooding at
    least locally. Debris flow and landslide activity will be a
    notable concern as well from these heavy rains.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9BjNe-FW4HxpKd13oWUWc_JNgylrROGd6XTEv4pWKbm3bvcktYTNiMqJ079UYAML0jex= TIjq5wZE6gguTaoK9-EWBdE$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...STO...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 41972347 41602315 41142289 41142210 40672151=20
    40082122 39472046 39052031 38842061 38542159=20
    38122193 37882259 38322329 39262410 40662456=20
    41842417=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Nov 21 17:31:47 2024
    AWUS01 KWNH 211731
    FFGMPD
    CAZ000-220400-

    Mesoscale Precipitation Discussion 1163
    NWS Weather Prediction Center College Park MD
    1230 PM EST Thu Nov 21 2024

    Areas affected...Northern California...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 211730Z - 220400Z

    SUMMARY...Remarkably static and intense AR moisture flux
    continuing to compound rainfall totals. Spots of add'l 3-6"=20
    totals expected through 04z ahead of next enhanced surge
    associated with deepening cyclone. Soils are nearly fully
    saturated so greater run-off is expected. Flash flooding remains
    possible.

    DISCUSSION...GOES-W Airmass and RAP analysis shows post-frontal
    deep dry air mass with red hues converting quickly to yellows and greenish-blues along and south of the front depicts strength of
    the front and ability to increase thermal wind along and south of
    the boundary though a large depth of the atmosphere. This
    unidirectional flow through depth is expected to remain though the
    next 9 to 12 hours directed at the Redwood Coastline and
    continuing to infiltrate well into northern California and the
    northern Sierra Nevada and Trinity Ranges...continuing similar
    evolution to unfold.

    This will be changing into the 03-06z period...GOES-W WV suite
    denotes a short-wave rounding the base of the global trough just
    east of 40N140W, which will be spurring rapid cyclogenesis over
    the next 12-24hrs. This will strengthen and amplify the flow
    nearing the coast, but that is for subsequent MPD issuance. Its
    influence, however, is starting to be felt in other downstream
    fields; including upper-level jet starting to split/ridge a bit
    across coastal OR and peripherally N CA. This will provide broad
    right entrance ascent from the exiting jet streak across the
    region and a very weak surface wave(s) are noted near Cape
    Mendocino into SW OR; low level winds appear to be responding with
    slightly backed flow especially along and east of the coastal
    range, further enhancing deep moisture flux through the northern
    Sacramento Valley and increasing orographic ascent (while further
    increasing freezing levels above nearly all peaks minus Shasta by
    the end of the valid time).=20=20

    CIRA LPW analysis shows a small split in the low level moisture
    further upstream, likely associated with the approaching shortwave DPVA/cyclogenesis. This enhanced area however, has solid
    isentropic slope through the 700-500mb layer that is currently
    intersecting far NW CA and overlaid with the leading surface to
    850 (and 850-700mb) slug of moisture from Cape Gorda through the
    San Francisco Bay (and up through the Sacramento Valley). This is
    resulting in solid core of 1.25-1.5" with embedded spots just over
    1.5". The strength of the moisture flux in the sfc-850mb (about
    .6-.75") on steady 45-50kt winds is solidly within the 95-99th
    percentile of CIRA LPW moisture flux values. This matches with
    consistent and remarkably broad 600 kg/m/s ticking up to 700
    kg/m/s in the core directed at S Mendocino/N Sonoma county. This
    will result in consistent .33"/hr rates with occasional .5"+/hr
    spurts in the southwest facing topography of the Coastal Range.=20
    Spots of additional 3-6" totals are expected and given 6-12" that
    have fallen in spots, soil saturation has reached 90% with spots
    over that. This will result in increased run-off and may spur
    mudslides and debris flows, especially in/near recent burn scars.=20
    As such, will continue to tag this MPD as flash flooding
    possible...though it remains more the duration of the rate that is
    driving the flooding conditions.

    A bit less consistent with a slow northward intersection with the
    northern Sierra Nevada Range of 500-600 kg/m/s, but slightly
    increased moisture flux convergence due to cyclonic acceleration
    through the gap of the Bay, should see similar rates and totals in
    strongest orographic ascent (Butte/Plumas county). OAK 12z RAOB
    showed near daily record of 1.25" TPW and that continues to
    increase with approaching core of moisture through the gap to
    indicate how anomalous the deep moisture is within the central
    valley. Slow sfc to 850mb backing of the flow will redirect
    orientation of the plume toward the eastern Trinity Range toward
    00z, reducing orthogonal flow into the Sierra Range. Still,
    swaths of 3-5" from Butte to Tehama and 2-3" into Shasta county
    are expected.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!47mgUUzyezbC5IOK_B6T_CgFjJXAY9hExwobLZoQgLdiY8DG_zBvSSJ8WaUpY1aUJWJN= pe2rEFldNv6fk3tbi2uKR5w$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 41582391 41562347 41322293 41382250 41362231=20
    41262177 40722153 40212113 39462076 39072106=20
    39122139 39462177 39692222 39332243 38902229=20
    38412237 38212291 38522340 38822370 39272392=20
    39742400 40212441 40592447 41092422=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Nov 22 04:01:42 2024
    AWUS01 KWNH 220401
    FFGMPD
    CAZ000-ORZ000-221600-

    Mesoscale Precipitation Discussion 1164
    NWS Weather Prediction Center College Park MD
    1100 PM EST Thu Nov 21 2024

    Areas affected...Northern California...Southwest Oregon

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 220400Z - 221600Z

    SUMMARY...Strong atmospheric river activity will continue to
    impact areas of northern CA overnight and into early Friday while
    gradually refocusing farther north back into portions of southwest
    OR. Widespread areal flooding concerns will continue, and there
    will also still be a possibility for some localized burn scar
    flash flooding impacts.

    DISCUSSION...The latest GOES-W GeoColor satellite imagery is
    showing the rapid deepening of a new area of low pressure offshore
    of the West Coast as strong shortwave energy rounds the base of
    the persistent larger scale upper-level trough. This low pressure
    center will strengthen over the next 6 to 12 hours and move to a
    position southwest of Vancouver Island by later Friday morning. As
    this occurs, the long duration, multi-day atmospheric river that
    continues to impact northern CA will advance a bit farther north
    and edge back into areas of southwest OR which will be the result
    of a backing of the deeper layer flow across the region and the
    northward advance of a warm front. By very early Friday morning, a
    cold front will then begin to arrive across coastal areas of
    southwest OR and northwest CA.

    Enhanced low to mid-level southwest flow out ahead of this cold
    front will continue to drive areas of persistently heavy rain
    given the level of moisture transport and warm air advection
    coupled with upslope flow/orographic ascent over the higher
    terrain. The 850/700 mb moisture flux anomalies are forecast to
    peak between 3 and 5 standard deviations above normal by around
    12Z (4AM PST) across coastal areas of northwest CA and southwest
    OR and the IVT magnitudes are forecast to locally peak in between
    750 and 1000 kg/m/s. While the highest values of IVT will be along
    the immediate coast, some of these elevated IVT magnitudes are
    forecast to spread inland including the northern Sacramento Valley.

    The 00Z HREF guidance suggests rainfall rates will occasionally
    reach 0.50" to 0.75"/hour, with potentially some spotty rates in
    the 0.75" to 1.0"/hour late tonight as peak IVT magnitudes arrive
    ahead of the cold front. Additional rainfall totals going through
    early Friday morning are expected to reach 3 to 5 inches, with
    isolated heavier amounts not out of the question. Given the
    persistence of the rainfall, and level of soil saturation and high
    streamflows already from this multi-day atmospheric river event,
    there will continue to be concerns for widespread flooding going
    through Friday morning. This may again include concerns for some
    burn scar flash flooding impacts at least locally.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4amqt4Yia4ywGGBmpYQ5syqEWjlez0Y0p1eEDtF4ZeILjefM_XxtmjRYS7L5njN9j6-o= R0agJvqPCaATEVyykVr1LXU$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...REV...STO...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 43542413 43432352 42482323 41812272 41672224=20
    41692162 41402136 40982140 40402082 39812057=20
    39322086 38962179 38232215 38022260 38282320=20
    39062390 39812426 40672459 42002459 43102467=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Nov 22 16:45:20 2024
    AWUS01 KWNH 221645
    FFGMPD
    CAZ000-230400-

    Mesoscale Precipitation Discussion 1165
    NWS Weather Prediction Center College Park MD
    1144 AM EST Fri Nov 22 2024

    Areas affected...cenral to northern CA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 221643Z - 230400Z

    SUMMARY...The atmospheric river will continue to gradually shift
    southward across north-central CA today and early tonight. While
    the magnitude of moisture flux will be lower than earlier today,
    locally significant impacts will remain possible where areas of
    training allow rainfall rates in excess of 0.5 in/hr. Additional
    rainfall through 04Z of 3 to 7 inches for the northern Sierra
    Nevada and localized totals of 2-4 inches for the Coastal Ranges
    are anticipated.

    DISCUSSION...16Z surface observations showed that a northward
    moving surface low continued to deepen roughly 250 miles west of
    the northern OR coast, with an attached occluded/cold front now
    inland across northern CA. GOES West water vapor imagery showed
    the strengthening mid to upper-level reflection of this surface
    low with the associated upper low moving inland across the Pacific
    Northwest. IVT values have weakened from near 1000 kg/m/s earlier
    this morning near the coastal OR/CA border but remained of a
    moderate intensity in the 600-700 kg/m/s range per short term
    model forecast data. While the intensity of the atmospheric river
    has decreased, there are indications upstream in water vapor
    imagery that short periods of stalling may occur with the moisture
    axis, along with a temporary increase in IVT values later this
    afternoon and early evening. While subtle inflections were noted
    in water vapor imagery within the southwesterly flow pointed at
    CA, which could allow for brief training, a more notable shortwave
    impulse was observed near 35N 140W which could result in a longer
    period of training potential.

    As this mid-level shortwave impulse near 140W continues to advance
    toward the east, RAP guidance indicates some amplification within
    the base of the broader parent closed low and slowing/stalling of
    mid-upper level height falls across the central CA coast. At the
    surface, a weak surface wave along the cold front is forecast to
    develop and approach the CA coast which will result in some minor
    increase in IVT values (up to 800 kg/m/s) and slowing/stalling of
    the plume over the San Francisco metro region with 850 mb winds
    intensifying to near 60 kt along the coast. The best indication
    for stalling will be in the 21Z-03Z time frame.

    Downstream across the Great Valley into the Sierra Nevada, 700 mb
    winds up to ~70 kt are expected later today with upslope
    enhancement favoring the greatest likelihood of 0.5 to 1.0 inch of
    rain in an hour or less. Additional rainfall totals through 04Z of
    3-7 inches are expected for the Sierra Nevada along with localized
    2-4 inch totals for the Coastal Ranges. Urban flooding impacts
    will be possible as well given overlap with the San Francisco and
    Sacramento metro regions and the addition of 1 to 2 inches, though
    rates are likely to remain below 0.5 in/hr outside of terrain due
    to negligible forecast instability.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9M6z_0wuTofaY4LB0_ojO6STfSKvkNKxKeGkkE-nBG6bfN1s7925Pl2uPNa2e32fHeem= CATXbgPjIVTW2hAz_zYK13M$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...REV...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 41662174 41602146 41102119 40502072 39572017=20
    39262006 38712026 38232078 37692133 37022163=20
    36822200 37132258 37822319 38812384 39602360=20
    40532302 41182266 41562216=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 23 04:18:02 2024
    AWUS01 KWNH 230417
    FFGMPD
    CAZ000-231500-

    Mesoscale Precipitation Discussion 1166
    NWS Weather Prediction Center College Park MD
    1115 PM EST Fri Nov 22 2024

    Areas affected...Portions of Central and Northern CA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 230415Z - 231500Z

    SUMMARY...Strong multi-day atmospheric river event gradually
    beginning to wane across central and northern CA, but flooding
    concerns will continue into Saturday morning.

    DISCUSSION...The long duration, multi-day atmospheric river
    impacting central and northern CA is generally past peak at this
    point and will be weakening in intensity going through Saturday
    morning. However, there will continue to be sufficient levels of
    additional rainfall for additional flooding concerns overnight.

    GOES-W Airmass RGB satellite imagery along with CIRA-ALPW data
    shows the atmospheric river axis along with an associated frontal
    boundary aligned in a southwest to northeast fashion across the
    Bay Area and extending inland across the Central Valley and the
    adjacent windward slopes of the central and northern Sierra
    Nevada. A wave of low pressure is noted riding northeast along the
    front, and this coupled with stronger upper-level jet
    dynamics/forcing advancing inland is still maintaining a corridor
    of stronger IVT magnitudes and thus some enhanced rainfall rates.

    IVT magnitudes are currently on the order of 700 to 800 kg/m/s
    just south of the Bay Area and are in between 500 and 700 kg/m/s
    across the Central Valley. Rainfall rates associated with this are
    still reaching upwards of 0.50" to 0.75"/hour on occasion across
    the coastal ranges and into the some of the orographically favored
    upslope areas of the Sierra Nevada. As the cold front gradually
    advances east and inland across the region, the high 850/700 mb
    moisture flux anomalies and related IVT magnitudes will begin to
    weaken, and this will eventually allow the rainfall rates to
    subside.

    The 00Z HREF guidance maintains high probabilities though of
    seeing 0.50"+/hour rainfall rates going through about 09Z (1AM
    PST) down across Santa Cruz, Santa Clara and Monterey Counties
    before subsiding. Farther inland, with the enhanced IVT magnitudes
    and upslope flow just ahead of the front still impacting the
    foothills of the Sierra Nevada, these 0.50"+/hour rainfall rates
    should persist through 12Z (4AM PST) across these areas and
    including Butte and Yuba Counties southward down through Tuoloumne
    and Mariposa Counties.

    Locally an additional 2 to 4 inches of rain will be possible with
    locally heavier amounts, and these additional rains are expected
    to maintain areal concerns for flooding going into early Saturday
    morning before the rainfall rates taper down. Some additional
    debris flows, rock and landslide activity, and perhaps an isolated
    concern for burn scar flash flooding will be possible overnight.
    Conditions should improve substantially Saturday morning as the
    front passes through the region and the atmospheric river impacts
    gradually come to an end.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4fKb18QgT9BSU13-3IlGEnq8f5EFxNcKGJOLaeIfbgoYxUkvXDF1YnL67zR2_J6CELQi= sThJk5SihYatPr-S-Qz3KDY$ for graphic product...

    ATTN...WFO...HNX...LOX...MTR...REV...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 40912135 40612096 40162058 39262043 38181971=20
    37651919 37031889 36661921 36302017 35812051=20
    35502107 35862167 36482218 37332260 38212285=20
    39342226 40452191 40832163=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Nov 26 04:15:47 2024
    AWUS01 KWNH 260415
    FFGMPD
    CAZ000-261615-

    Mesoscale Precipitation Discussion 1167
    NWS Weather Prediction Center College Park MD
    1114 PM EST Mon Nov 25 2024

    Areas affected...Portions of Central and Southern CA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 260415Z - 261615Z

    SUMMARY...Moderately strong atmospheric river to continue
    overnight and through Tuesday morning across portions of the
    central and southern CA coastal ranges, San Joaquin Valley, and
    southern Sierra Nevada. Some areal flooding concerns and a low-end
    burn scar flash flood threat will exist.

    DISCUSSION...The GOES-W Airmass RGB satellite imagery in
    conjunction with CIRA-ALPW data shows a rather well-defined and
    moderately strong atmospheric river advancing inland across
    coastal areas of central and southern CA, the San Joaquin Valley
    and into the higher terrain of the southern Sierra Nevada.

    So far, the heaviest rainfall rates have been in the foothills of
    Fresno and Tulare Counties where some occasional rainfall rates of
    0.50"+/hour have already been observed. The moisture transport
    over the coastal ranges and into the interior foothills is
    relatively strong with IVT magnitudes reaching as high as 500 to
    750 kg/m/s, and this is associated with 850/700 mb moisture flux
    anomalies of 3 to 4 standard deviations above normal.

    There is a rather substantial subtropical moisture connection to
    this atmospheric river with PWs that are running anywhere from 2
    to 4 standard deviations above normal, and CIRA-ALPW showing the
    deeper layer moisture axis extending well offshore of the West
    Coast all the way down to near 30N 140W where there is close
    proximity of a deeper layer trough. Embedded within this moist
    southern stream flow are multiple shortwave impulses interacting
    with a frontal zone and there has been at least some weak surface
    wave activity traversing this front, including one wave that has
    advanced inland to the northeast of Monterey.

    Some additional increase in IVT values are forecast overnight, and
    especially in the 06Z to 12Z time frame as additional stronger
    energy from offshore arrives, and this should promote some
    additional localized increase in rainfall rates. The coastal
    ranges of Monterey and San Luis Obispo Counties may see rainfall
    rates increase into the 0.25" to 0.50"/hour range on occasion.
    However, with the spillover of stronger moisture transport into
    the foothills of the southern Sierra Nevada, and with favorably
    orthogonal orientation of the flow into the terrain, the rainfall
    rates here below snow level should occasionally reach into the
    0.50" to 0.75"/hour range with possibly a couple instances of
    rates higher than this which is supported by the 00Z HREF guidance.

    Additional rainfall amounts going through Tuesday morning may
    reach 1 to 3 inches for the coastal ranges, and as high as 3 to 6
    inches for the foothills of the southern Sierra Nevada. Given the
    persistence overnight and into early Tuesday morning of heavier
    rainfall rates and the corresponding storm totals, there may be
    some areal flooding concerns along with at least a low-end threat
    for some burn scar flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4S86pssxoqB_q2s94wSJQmSTivjmgVP9UzqieyBN3u1R0YzB5GMO8A3Gz8GF6ABMOYWQ= SN36r8X53JCqAUI7Fpt0_X4$ for graphic product...

    ATTN...WFO...HNX...LOX...MTR...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 37841961 37471911 36941866 36351843 35881835=20
    35581837 35451868 35721934 35511987 35201997=20
    34761977 34532004 34582066 35352097 35722133=20
    36332183 36852153 37232057 37722011=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Dec 9 17:06:42 2024
    AWUS01 KWNH 091706
    FFGMPD
    MSZ000-LAZ000-092304-

    Mesoscale Precipitation Discussion 1168
    NWS Weather Prediction Center College Park MD
    1206 PM EST Mon Dec 09 2024

    Areas affected...Southeast LA and Far Southern MS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 091704Z - 092304Z

    SUMMARY... A narrow band of showers and storms training across
    southeast LA into MS containing hourly rainfall rates up to 2" at
    times could produce areas of flash flooding through this
    afternoon. Any flash flood risk is expected to be localized and
    confined to urbanized locations.

    DISCUSSION... Upper shortwave crossing over the western Gulf
    Coast, as evident by GOES-16 mid-level WV, ahead a of deeper
    positively-tilted longwave trough extending from the Upper Midwest
    to the central Great Basin are aiding in enhance lift along the
    central Gulf Coast. Strong west-southwest flow at the mid and
    upper levels along the central and western Gulf Coast are
    maintaining a moist environment with analyzed PWs of 1.7-1.9"
    centered across south-central and southeast LA. These PW values
    also near the 90th climatological percentile per the 00z ECENS.
    Uniform west-southwest flow through the column will also support
    the training potential into this afternoon until the better
    forcing shifts eastward by this evening.

    Instability will be a limiting factor as MUCAPE remains around
    500-1000 J/kg, which for this part of the country struggles to
    produce rainfall rates above FFG. 3-hour FFG of 3-5" exists across
    much of the region, but are lower near Baton Rouge and Lafayette
    due to prior rainfall. 12z HREF and 15z HRRR guidance seem to have
    an ok handle on current trends and highlight a low chance for
    exceeding 3" per 6 hours by this evening within the MPD area. If
    training occurs over low-lying or urban regions for an extended
    period, localized flash flooding is possible.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Ua6quaahsrqkzhmkj3WqcRhB5bVObQ6f4qoNdWMD4P1mWRNdlQNBAVGh26W39UYyqpt= AzvV1okY2UYluhPW0fgXzpg$ for graphic product...

    ATTN...WFO...LCH...LIX...MOB...

    ATTN...RFC...LMRFC...NWC...

    LAT...LON 30938954 30748893 30318894 29998953 29569081=20
    29349194 29679223 30229177 30769057=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Dec 9 21:59:11 2024
    AWUS01 KWNH 092159
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-100257-

    Mesoscale Precipitation Discussion 1169
    NWS Weather Prediction Center College Park MD
    458 PM EST Mon Dec 09 2024

    Areas affected...Parts of Southeast LA, Southern MS, and Southwest
    AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 092157Z - 100257Z

    SUMMARY... A weakening line of showers and storms as well as
    reforming convection upstream over south-central LA may lead to
    additional chances for localized flash flooding this evening along
    sections of the central Gulf Coast.

    DISCUSSION... Same shortwave responsible for the breakout of
    morning convection across southern LA is now crossing the central
    Gulf Coast and entering the Southeast, while strong uniform
    southwesterly flow continues to advect tropical moisture from the
    eastern Pacific per GOES-West ADV LPW. PWs remain in the 1.6-1.9"
    range per SPC's mesoanalysis and around the 90th climatological
    percentile. These elevated PW values continue to advect further
    eastward and across AL, but with instability remaining mostly
    meager. SBCAPE values have climbed to above 1000 J/kg across
    south-central LA mainly due to diurnal heating, which will wane in
    the next few hours. However, speed maxes noted in GOES-East ML WV
    exiting northern Mexico within the deep tropical moisture stream
    imply convection may continue to linger a few hours past sunset.

    This combination of elevated moisture, strong uniform
    southwesterly flow, and remaining instability pool will lead to
    additional chances for localized training thunderstorms capable of
    containing hourly rainfall rates up to 2"/hr through around 9 pm
    CT. A corridor of 3-5" of rainfall has already fallen per MRMS in
    a SW-NE oriented line along the northern shores of Lake
    Pontchartrain and southwestward. Otherwise, additional localized
    corridors of 1-1.5" have already occurred. Therefore, even though
    3-hr FFG remains widely above 2.5" there could be localized areas
    more susceptible to flash flooding with 2-3" additional totals.
    Urban locations will be most at risk within the broader isolated
    flash flooding threat stretching from southern LA to southern MS.

    Farther east into southern AL, a continuous band of rainfall
    containing hourly rates around 1" is expected to continue within a
    corridor of enhanced atmospheric moisture and very low
    instability. This region may see more widespread rainfall amounts
    above 1.5", but falling at lower rates. Any flash flood risk for
    AL is considered low, with urban and poor drainage locations most
    at risk for isolated impacts.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_5mD1sgdjdxSJQUq--ZU_lFvtM-hwSmOEBRUzFgHv9etbNUToQBgD0D22VOt_sV5YVQq= _eYBHEVqLVb4zGcYLULQXZA$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 31828764 31668652 30968662 30388839 29879017=20
    29609171 29979218 30519198 31059089 31578904=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Dec 10 04:26:15 2024
    AWUS01 KWNH 100426
    FFGMPD
    FLZ000-GAZ000-ALZ000-MSZ000-101000-

    Mesoscale Precipitation Discussion 1170
    NWS Weather Prediction Center College Park MD
    1125 PM EST Mon Dec 09 2024

    Areas affected...southern AL, southwestern GA, northern FL
    Panhandle

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 100423Z - 101000Z

    SUMMARY... Localized flash flooding will be possible over southern
    AL, southwestern GA into northern portions of the FL Panhandle.
    Rainfall rates of 1-2 in/hr with localized totals of 2-4 inches
    may occur.

    DISCUSSION...An axis of training showers and embedded
    thunderstorms has resulted in a narrow axis of 2-4 inches of rain
    over southwestern AL since roughly 12Z. Radar imagery from 04Z
    showed that a WSW to ENE axis of moderate to heavy rain continued
    to affect southern AL but with slow eastward progression. The
    heavy rain was occurring near a low level convergence axis, which
    was located just above the surface and extended from the
    northwestern tip of the western FL Panhandle across the southern
    AL/GA border. Precipitable water values of 1.5 to 1.8 inches and
    generally weak instability near 500 J/kg were supporting localized
    rainfall rates of 1-2 in/hr at times. Water vapor imagery showed
    weakly diffluent flow over the region and ascent may be aided by
    lift occurring within the right-entrance region of a RAP
    forecast/developing 130 kt jet max over northern AL/eastern TN.

    Southerly to southwesterly low level flow is forecast to maintain
    over the region through the night along with 500-1000 J/kg
    ML/MUCAPE just south of the convergence axis, which should
    continue to slowly translate east over the next few hours ahead of
    an upstream upper trough over the western U.S. and resultant
    mid-level height falls. While overall weakening is expected as the
    low level convergence axis loses definition, pockets of short term
    training may be enough to support additional 1-2 in/hr rates at
    times from southern Al into southwestern GA and the northern FL
    Panhandle through ~10Z. Also, additional shower redevelopment will
    be possible toward 10Z back to the west, ahead of a cold front to
    be approaching from the Lower Mississippi Valley.

    Due today's rainfall, flash flood guidance is 2-3 inches in 3
    hours across northern portions of the MPD threat area. The
    potential for an additional 2-4 inches may cause localized flash
    flooding over urban or otherwise sensitive locations of the region.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9YLOaOjknNUwA86BtvGPdc8o5iaR99r4j6RkzaBQchx1OroHDV00el0DeOobp5ncHnkL= _9gprbuo8pSa4tKtur2mr54$ for graphic product...

    ATTN...WFO...BMX...FFC...MOB...TAE...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 32778527 32478442 31658451 31158486 30838560=20
    30738682 30738789 31198846 31808806 32498670=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Dec 10 10:20:19 2024
    AWUS01 KWNH 101020
    FFGMPD
    ALZ000-MSZ000-LAZ000-101615-

    Mesoscale Precipitation Discussion 1171
    NWS Weather Prediction Center College Park MD
    519 AM EST Tue Dec 10 2024

    Areas affected...southern LA into south-central MS and western AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 101018Z - 101615Z

    SUMMARY...Showers and embedded thunderstorms will increase this
    morning across southern LA/MS/AL. Rainfall coverage and intensity
    should increase through 16Z and areas of training will be capable
    of producing 1-2 in/hr rainfall rates. Flash flooding will be
    possible, especially where overlap occurs with rainfall from
    Monday.

    DISCUSSION...Radar and GOES East satellite imagery from 10Z showed
    a SW to NE oriented zone of widely scattered showers with embedded thunderstorms translating toward the east across southern LA into
    south-central MS. These showers were located along a near surface
    convergence axis located out ahead of a cold front, which draped
    from southern AR into southeastern TX. MLCAPE was fairly weak over
    LA/MS (500-1000 J/kg per 10Z SPC mesoanalysis data) but shower
    activity was located just to the west of an axis of precipitable
    water values that contained 1.5 to 1.7 inches.

    As broad lift begins to overspread the Lower MS Valley, out ahead
    of a large, positively tilted, upper trough axis over the
    Southwest, the coverage and intensity of showers/thunderstorms
    along the eastward progressing low level convergence axis will
    increase. This should also be true as the convergence axis reaches
    higher precipitable water values to the east along with forecasts
    of increasing instability with daytime heating. An upper level jet
    max over the eastern TX/OK border, with GOES East DMVs having
    sampled 120-130 kt between 07-08Z near 250 mb, is expected to
    continue to increase in magnitude as it translates downstream
    toward the MS River through the morning. Locations within the
    right-entrance region of this upper jet max are expected to see
    enhanced lift through late morning. Mean steering flow from the
    southwest will parallel the axis of forcing allowing for training
    of heavy rain at times with 1-2 in/hr becoming more likely later
    this morning as the axis of heavy rain shifts east.

    While expected rainfall through 16Z is likely to fall primarily to
    the north of a stripe of heavy rain (2 to 5 inches) which fell
    across portions of the central Gulf Coast on Monday, localized
    convective development near the Gulf Coast...or closer to the
    source of higher instability...could overlap with these more
    hydrologically sensitive areas to generate flash flooding. Farther
    north, any areas of flash flooding that develop should remain
    localized atop low lying and/or urban areas.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8VIX2kgJs2zzn24siebz7LfZftG3fwtvEp4o3p_Fq8aeifb8uHeRdwA2Z-msOBIuPTeM= Y5ft_Gp15KtBwN_PRYjOYFE$ for graphic product...

    ATTN...WFO...BMX...JAN...LCH...LIX...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 33068836 32588751 31838799 30219007 29529181=20
    29679238 30139264 31089168 32638948=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Dec 10 15:31:20 2024
    AWUS01 KWNH 101531
    FFGMPD
    GAZ000-ALZ000-MSZ000-LAZ000-102130-

    Mesoscale Precipitation Discussion 1172
    NWS Weather Prediction Center College Park MD
    1030 AM EST Tue Dec 10 2024

    Areas affected...Parts of the Deep South and Southeast

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 101530Z - 102130Z

    SUMMARY... Increasing coverage of showers and thunderstorms
    through this afternoon will be capable of containing hourly rates
    up to 2"/hr and 6-hourly totals over 3", while likely training
    over similar areas. This will lead to scattered flash flooding
    potential, mainly for urban and low-lying locations

    DISCUSSION... Current satellite, radar, and surface observations
    display a developing southwest-northeast oriented axis of showers
    and thunderstorms extending from eastern LA to central AL. These
    showers and thunderstorms are forming in advance of a deep upper
    trough (-1.0 to -1.5 standardized anomaly per 00z ECENS)
    stretching from the Upper Midwest to the Southern Rockies. This
    trough is aiding in strong uniform southwesterly flow advecting
    anomalous moisture throughout the column with a source region of
    the eastern Pacific, visible via GOES-West ADV LPW. Actual PW
    values of 1.5"-1.7" currently spans from eastern LA to central GA,
    but these values are forecast to expand throughout the day into
    the Southeast in response to strengthening mid and upper level
    flow as the the aforementioned trough takes on more of a neutral
    tilt over the central U.S.

    Radar and GOES-East visible satellite this morning depicts and a
    few subtle areas of convergence extending to the northeast of the
    approaching cold front. One area impacting Birmingham, AL and a
    separate more noticeable axis to the south over Montgomery, AL and
    the I-65 to I-85 corridor. These areas of convergence are most
    likely to display training storms within the deep uniform
    southwesterly flow, with greater instability (500-1000 J/kg)
    advecting into the southern line. Overall, CAMs and 06z HREF
    guidance display that hourly rates are not expected to exceed 2"
    outside of very localized locations, but that 6-hourly totals
    could exceed 3" and this would top the 6-hr FFG. So areas
    experiencing training thunderstorms will be most at risk for
    excessive rainfall as opposed to impacts from individual cells.

    Overall, if these amounts are realized it is expected that
    scattered low-lying and urbanized locations could experience rapid
    water runoff and flash flooding impacts, particularly after 18z
    along the I-85 and I-65 corridors of AL.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9I0Lt1rnPx9qCAo9zkE6kisJU6T2p8DxE5PKBP-g4294KOZjc8QtecrsXJ5kPF0yaCJM= NEGcZ5UU0Ls0nhxvVmVupF0$ for graphic product...

    ATTN...WFO...BMX...FFC...JAN...LIX...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34148494 33898413 33208394 32328501 31338706=20
    30698864 30408964 30619019 31059021 31738971=20
    32528879 33258766 33848634=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Dec 11 06:07:29 2024
    AWUS01 KWNH 110607
    FFGMPD
    VAZ000-NCZ000-SCZ000-GAZ000-111205-

    Mesoscale Precipitation Discussion 1173
    NWS Weather Prediction Center College Park MD
    106 AM EST Wed Dec 11 2024

    Areas affected...Piedmont to Blue Ridge foothills of GA/SC/NC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 110605Z - 111205Z

    SUMMARY...There will be some potential for lower end flash or
    urban flooding across the Piedmont of GA/SC/NC into the foothills
    of the Blue Ridge Mountains through 12Z. Elements of training
    rainfall will be capable of producing 1 to 1.5+ in/hr rates with 3
    to 6-hour totals of 2-3 inches.

    DISCUSSION...0530Z radar imagery across the southeastern U.S.
    showed a broad swath of mostly stratiform rainfall extending from
    central GA into the Carolinas, though some embedded thunderstorms
    were observed within a broken convective line extending from
    western GA to the Gulf Coast where MLCAPE was estimated to be
    500-1000 J/kg (05Z SPC mesoanalysis). Precipitation was occurring
    in advance of a cold front with the convective line along a narrow
    axis of pre-frontal convergence near the surface. MRMS rainfall
    rates have recently been peaking near 1 in/hr, such as along the
    GA/SC border just south of Columbus.

    While much of this rain has been beneficial to the region given
    below average rainfall over the past few weeks, there will likely
    be an uptick in rainfall intensity heading through the morning
    hours for locations in the Carolinas. As an upper trough axis,
    observed on water vapor imagery just west of the MS River,
    continues to advance eastward, continued amplification of the
    downstream low level flow will likely result in increased moisture
    transport and modest instability increases into the Carolinas
    through 12Z. In addition, while instability is not expected to be
    a significant contributing factor to enhancing rainfall, a
    strengthening upper level jet is likely to enhance lift over the
    Blue Ridge and Piedmont later this morning. GOES East DMVs sampled
    170 kt near 250 mb over the upper OH Valley at 05Z and some
    additional strengthening is likely farther south, ahead of the
    through axis becoming neutrally tilted over OK/AR on current water
    vapor imagery, forecast to become negatively tilted later this
    morning. Increasingly divergent and diffluent flow over the
    southeastern U.S. may help to compensate for weak instability and
    allow for rainfall rates of 1 to 1.5+ in/hr where heavier cores
    train along pre-frontal convergence axes through 12Z. With these
    heavier rates, potential for urban flooding or minor flash
    flooding will exist with perhaps 2-3 inches of rain in a 3 to 6
    hour window of time.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!42KVo-cuWdZA49WyXuK3cBlvwfFLJT3Fo_efugQTMp1x4HlfCgrYm430E7bLCQiYB5kI= th86gfq61e8Se2dVPOycHJM$ for graphic product...

    ATTN...WFO...CAE...FFC...GSP...RAH...RNK...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36627963 35477938 34228065 32668254 32128373=20
    32218460 32788480 34048402 35008291 36418123=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Dec 13 20:01:31 2024
    AWUS01 KWNH 132001
    FFGMPD
    CAZ000-ORZ000-140600-

    Mesoscale Precipitation Discussion 1174
    NWS Weather Prediction Center College Park MD
    300 PM EST Fri Dec 13 2024

    Areas affected...Northern California...Southwest Oregon

    Concerning...Heavy rainfall

    Valid 132000Z - 140600Z

    SUMMARY...An approaching storm system accompanying a strengthening
    atmospheric river will result in an areal increase of excessive
    rainfall rates this afternoon and into tonight. Areas of flash
    flooding and landslides are possible.

    DISCUSSION...GOES-West satellite imagery shows a steady fire-hose
    of Pacific moisture being directed at the U.S. West Coast today
    with periods of rain well underway across northern CA and southern
    OR. As the afternoon unfolds, the approaching warm front and storm
    system will force southerly 925-850mb winds to accelerate into the
    far northern CA coast. The warm front's approach will also force
    freezing levels to rise as high as 5,000ft in some cases. This
    provides both a deeper warm cloud layer and would allow for higher
    elevations (up to around 5,000ft) to be at-risk for excessive
    rainfall rates. By 00Z, the triple-point of the frontal system
    will be tracking through the CA/OR border and the warm front will
    reside along the CA Coastal Range. A surge in 850mb moisture flux
    along the northern CA coast will accompany an IVT >750 kg/m/s that
    surpasses the 99th climatological percentile according to NAEFS.
    This robust IVT is the catalyst for a >12hr period for excessive
    rainfall from as far north as southwest OR to as far south as some
    of the northern Bay Area suburbs overnight.

    12Z HREF probabilistic guidance shows high chance probabilities
    70%) for >0.5"/hr rainfall rates around the Eureka area as early
    as 21Z. These probabilities then spread as far north as the OR/CA
    coastal border between 00-03Z. By 03Z, the cold front will be on
    approach and the northern CA coast will become placed within the
    storm's warm sector. Low-end MUCAPE values (generally <200 J/kg)
    could be available for potential convective enhancement in
    northern CA tonight, while the strong SW flow aloft supports
    strong upslope enhancement into the Trinity/Shasta Mountains
    between 03-06Z tonight. These two areas could see rainfall rates
    approach 1"/hr in some cases.

    Overall, through ~06Z Saturday, additional rainfall totals of 2-4"
    are expected within most of the highlighted region with localized
    totals surpassing 5" possible. The 12Z HREF depicts
    low-to-moderate chance probabilities (30-50%) for 12-hr QPF >5"
    along the coast near and south of Eureka, as well as in the
    southwestern facing slopes of the Trinity/Shasta Mountains.
    Previously saturated soils have recovered to some extent given the
    drier than normal stretch of weather over the past couple weeks,
    which should help limit the areal extent for potential flash
    flooding. That said, the atmospheric parameters mentioned above
    are more than enough to support the potential flash flooding and
    landslides in parts of northern CA this afternoon and into
    tonight.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4qLvtWeaBcIOYHZkoGSpo2fqD1WRjZoZ7yQJcmzH6-Uedhy7O7s0XLSR8fnL2zcKeXvT= NoWtsLIC1SZ_CJNrFGFsldM$ for graphic product...

    ATTN...WFO...EKA...MFR...STO...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 42442432 42422394 42172361 41792363 41342343=20
    40972324 40832293 41082230 40862213 40252285=20
    39652302 39112306 38872348 39072392 39622409=20
    40142453 40582460 41482437 42082453=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Dec 14 05:01:06 2024
    AWUS01 KWNH 140501
    FFGMPD
    CAZ000-141500-

    Mesoscale Precipitation Discussion 1175
    NWS Weather Prediction Center College Park MD
    1200 AM EST Sat Dec 14 2024

    Areas affected...Northern and Central California....

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 140500Z - 141500Z

    SUMMARY...Initial surge of deep moisture/typical Atmospheric River
    will given way to approaching stronger cyclogenesis/flux
    convergence with potetial of .75-1"/hr localized showers that may
    induce localized flash flooding particularly in/near urban
    locations around San Francisco Bay after 11z.

    DISCUSSION...GOES-W WV suite depicts a mature strong closed low
    along 130W near 46N that has driven an occluded/cold front
    through the coastal range of W WA/OR. Solid shortwave ridge
    within the upper-level cirrus canopy denotes the left exit of the
    130kt 3H jet streaking northward, while the right entrance exists
    at the trailing edge of the cold front resulting in a weak surface
    to 850mb wave/inflection along/just north of Cape Mendocino. CIRA
    LPW denotes this feature with an enhanced moisture pocket of .6"
    and .4" with the respective sfc-850 and 850-700mb layers before
    connecting back to the main core of the SW to NE oriented warm
    conveyor/AR plume. This plume currently intersects the Redwood
    Coast from Cape Mendocino to near the entrance to the San
    Francisco Bay. Enhanced convergence and weak cooling aloft has
    seen some steepening of lapse rates near the surface inflection
    back near the Cape, with RADAR indicating some enhanced linear
    filaments of convective still remaining but ushering themselves
    ashore likely with .5"/hr rates resulting in best opportunity for
    short-term flooding concerns. However, the main core of the AR
    will continue with solid 45-50kt fairly orthogonal ascent
    resulting in 700-800 kg/m/s of IVT that will slowly drift
    southward over the next 4-6hrs resulting in average .33 to .5"/hr
    rates across the Redwood Coast toward the Napa Region. Additional
    totals of 2-3" are likely through 12z as the core of the AR shifts
    ashore into the central Valley and lower slopes of the Northern
    Sierra Nevada range.

    Possible Flash Flooding after 10-15z in Central California...
    GOES-W WV suite also depicts the core of a strong mid to low level
    cyclone developing just west of 130W about 36-37N quickly
    approaching. Upstream strong digging of the trough is
    strengthening the descending branch of the mid to upper level jet
    rapidly deepening the cyclone. The strong vorticity advection is
    expected to peak over the next 3-4hrs just west of the central CA
    coast with near negative tilt as a 130-140kt jet streak rounds the
    base of the larger scale trough from 09-12z. Low level flow will back/strengthen and flux will steadily increase. Additionally,
    CAA will help to steepen mid-level lapse rates and potential for
    250-500 J/kg of MUCAPE will accompany the enhanced moisture flux.=20
    Hi-Res CAMs continue to suggest convective streets/elements with
    capacity of .75-1"/hr rates likely to focus where the cold front
    sags/flattens which looks to be trending near Sonoma county, but
    with height-falls/forward propagation along/ahead of the DPVA will
    enhance through San Francisco Bay toward 12z. 00z HREF
    probability of 1"/3hr is nearly 100% while 1"/hr peaks around
    50-60% at 12-13z near the mouth of the Bay; providing enhanced
    confidence for possible incidents of flash flooding in/near the
    urban locations surrounding the Bay (initially north side before
    15z). Localized totals of 1-2.5" are possible with convective
    areas near the Bay though spots of 3-5" are also likely along SW
    facing orographic peaks in the Trinity Range, Coastal Range of
    Mendocino/Lake and Napa counties and lower slopes of Tehama/Butte
    county by 15z.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7BT1hUO_UzJjqIeszCnUrh0hrk4ZaqXFMBmM5FzZ5NmdukTWliA6qstx3gYkW6dKSULT= U4Zlw_yYYOOcqerdhNP4cU0$ for graphic product...

    ATTN...WFO...EKA...MTR...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 41372412 41312379 40962356 40822328 40672266=20
    40702194 39892160 39332095 39012071 38642080=20
    38232113 37302130 36662155 36422192 36792243=20
    37392272 38002312 38592356 39072384 39742401=20
    40012425 40322450 40762436 41032427=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Dec 17 03:03:52 2024
    AWUS01 KWNH 170303
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-OKZ000-170830-

    Mesoscale Precipitation Discussion 1176
    NWS Weather Prediction Center College Park MD
    1002 PM EST Mon Dec 16 2024

    Areas affected...Southern Arkansas...Northwest Mississippi..Adj
    portionsOK, TX, LA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 170300Z - 170830Z

    SUMMARY...The potential for continued back-building of weakening
    but training showers may present a low-end scattered incident or
    two of flash flooding through the overnight hours.

    DISCUSSION...GOES-E WV suite denotes an elongated trough/stream
    intersection extending from northeast Texas across the Delta
    Region of the MS River toward the southern Ohio Valley toward the
    tail end of the more amplified exiting flow across the Lower Great
    Lakes. GOES-AMVs confirm RAP analysis of this intersection
    extends the length of the broad right entrance to the 70-90kt 3H
    jet across the TN/OH valley. A small inflection/wave is highly
    divergent across NE TX providing the enhanced ascent pattern noted
    with strong cirrus filaments along the northern edge of the
    convective clusters across NE TX, AR into N MS/SW TN. The deep
    unidirectional flow extends back to central TX, where moisture is
    generally confluent before veering into solid isentropic ascent
    toward the upper level jet entrance. As such, CIRA LPW and RAP
    analysis show an enhanced pool of moisture starting to near 1.5"
    with the vast majority below 850mb.

    Surface analysis shows defined sagging cold front across AR, that
    is starting to sharpen, with warm sector southerly flow providing
    weak but sufficient surface convergence from 5-10kts. Strong
    convection with some weak QLCS features generally training along
    the boundary/deep layer moisture interface are fed upstream by
    pool of 1000-1250 J/kg of MUCAPE before diminishing rapidly toward
    N MS. Rates of 1.5-1.7"/hr are probable given moisture/unstable
    air and with training profiles may allow for streaks of 2-3"
    totals, though eastward along the line will see enhanced
    southeastward propagation. While soil conditions are fairly
    dry/generally recepible; they are starting to go a bit dormant and
    rates may be sufficient for localized pooling/enchained run-off.=20
    As such flash flooding is considered possible.=20=20

    While upstream convection appears to becoming a bit more fractured
    due to slightly weaker flow, the upper-level divergence/outflow
    channel is suggestive/supportive of back-building/isentropic
    ascent. Additionally, this mid-level wave is supporting some
    shortwave ridging across SW to south-central AR and backing
    propagation vectors to be be more northward allowing for greater
    potential for training cells through the next 4-5 hours. Hi-Res
    CAMs are inconsistent in the evolution overall convective activity/coverage...given the weakened upstream convergence, but
    ones that do have stronger convergence do depict a higher
    potential for training/back-building signal near areas that have
    already received the higher rainfall resulting in initial flash
    flooding warning. Confidence is high contingent on the evolution
    and so the risk for continued flash flooding across Texarkana
    toward the central LA/AR border is also considered possible
    through 09z (as signals further diminish through the entire hi-res
    CAM suite).

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4JL0cz_VHm3h9p4tVjTc76TK83nt1BoJs5dsXu1ORbV9cyx5DbBbMIFhfgvCHAe5i5sJ= CN4gz7US5su4YfGLjs8bzDY$ for graphic product...

    ATTN...WFO...JAN...LZK...MEG...SHV...

    ATTN...RFC...ABRFC...LMRFC...NWC...

    LAT...LON 34649054 34488968 33928946 33409022 33069166=20
    32919259 32909333 32849406 33109473 33359479=20
    33799453 33989415 34199346 34409209=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Dec 17 22:04:14 2024
    AWUS01 KWNH 172204
    FFGMPD
    ORZ000-WAZ000-181000-

    Mesoscale Precipitation Discussion 1177
    NWS Weather Prediction Center College Park MD
    503 PM EST Tue Dec 17 2024

    Areas affected...western WA into northwestern OR

    Concerning...Heavy rainfall

    Valid 172202Z - 181000Z

    SUMMARY...Areas of heavy rainfall will continue to affect western
    WA into northwestern OR through tonight. While high rainfall rates
    will not not be constant over the next 6-12 hours, rates will
    occasionally surpass 0.5 in/hr and locally approach 1 in/hr into
    the favored terrain leading to an additional 2-5 inches of rain
    through Wednesday morning.

    DISCUSSION...GOES West water vapor imagery at 21Z showed a
    vorticity max embedded within a broader mid-upper level trough
    axis near 41N 141W, tracking toward the east and preceded by a
    130-150 kt upper level jet. A cold front was analyzed at the
    surface out ahead of the upper trough with a surface wave near 42N
    135W. An atmospheric river was noted with peak PWAT values of 1.2
    to 1.3 inches on CIRA Advected TPW imagery and RAP analysis data
    ahead of the cold front to the west of WA/OR. PWAT values along
    the coast, near the mouth of the Columbia River, were just below
    1.2 inches via GPS data, but when combined with southwesterly 850
    mb winds of 40-50 kt, IVT values were estimated to be near 700
    kg/m/s along the southern WA/northern OR coast. Downstream
    rainfall rates into the northern OR Coastal Ranges have already
    been observed in the 0.5 to near 1.0 in/hr range from earlier
    today, but radar/satellite imagery indicated the heaviest rain was
    shifting north into western WA.

    Water vapor imagery does not suggest the base of the upper trough
    is amplifying any more to the south and may even be beginning to
    lift slightly north. A general E to ENE motion to the upper trough
    is forecast by RAP guidance through the overnight which will
    continue to translate the greatest magnitude of IVT values
    northward across western WA, with the peak axis focusing primarily
    into Vancouver Island just after 00Z, perhaps clipping far
    northwestern Clallam County in WA. Peak rainfall rates along the
    WA Coastal Ranges into the Olympics within the northward shifting
    IVT axis should reach into the 0.5 to 0.8 in/hr range, perhaps
    isolated values near 1.0 in/hr. A temporary lull in heavy rain is
    expected for much of the Pacific Northwest just after 00Z followed
    by another surge as the upper trough and surface cold front
    approach overnight. From roughly 06Z onward, IVT values are
    forecast to surge to near 1000 kg/m/s along the WA/OR coast via
    recent RAP guidance, but only last for an hour or two at that
    magnitude. The overnight surge is likely to produce rainfall rates
    in the 0.5 to 0.8 inch range with localized values near or in
    excess of 1.0 in/hr.

    Additional rainfall totals of 2-4 inches are likely to occur
    through 09Z for the WA Coastal Ranges into northwestern OR, along
    with the upslope regions of the WA Cascades. Isolated totals in
    excess of 5 inches cannot be ruled out, especially in any favored
    southwest facing slopes of the Olympics where the duration of
    higher rainfall rates is expected to be the longest. Gauges showed
    24 hour totals of 1-2 inches for the Coastal Ranges and Cascades
    so far, with localized maxima near 3 inches. Earlier collaboration
    with the National Water Center and NWM output suggests flooding
    should be isolated at best, partially due to dry antecedent
    conditions, but 48 hour rainfall totals of 5-7 inches through
    Wednesday morning will likely support notable rises on area
    creeks/streams.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-E06sBTiKv_1XE9fjB-Sa5EcS8WulePp0i71Bzc_2R7jrYf7wCg9heGD1yHABLvMe-a7= 6QL8Ggj5rYHY1DZKV4_0uSQ$ for graphic product...

    ATTN...WFO...OTX...PDT...PQR...SEW...

    ATTN...RFC...NWRFC...NWC...

    LAT...LON 49102238 49072164 48862117 48662101 48372094=20
    48102088 47782096 47562096 47322103 47122107=20
    46952103 46782107 46562129 46332135 46172137=20
    45982159 45782159 45592169 45472197 45512216=20
    45702243 45852246 46072267 46182270 46422248=20
    46632258 46742255 46872228 46962223 47042238=20
    47012275 46822305 46672311 46502308 46332320=20
    46272340 46112344 45962345 45672333 45552337=20
    45382341 45282347 45172354 44982347 44792356=20
    44722384 44982433 45492455 46732462 48242509=20
    48442453 48282397 48302321 48622290 48872289=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Dec 17 22:51:19 2024
    AWUS01 KWNH 172250
    FFGMPD
    FLZ000-180400-

    Mesoscale Precipitation Discussion 1178
    NWS Weather Prediction Center College Park MD
    550 PM EST Tue Dec 17 2024

    Areas affected...east coast of FL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 172248Z - 180400Z

    SUMMARY...Localized flash/urban flooding will be possible along
    the eastern FL Peninsula over the next few hours. Slow cell
    movement and/or training will be capable of 1 to 3 in/hr rainfall
    rates which may generate isolated excess runoff within the urban
    corridor.

    DISCUSSION...Radar imagery from KMLB and infrared satellite
    imagery through 2230Z showed scattered thunderstorms occurring
    along the east coast of FL between Cape Canaveral and Port Saint
    Lucie, streaming in from the east following the mean low to
    mid-level easterly flow between 10-20 kt. Surface dewpoints in the
    lower 70s have contributed to anomalous mid-December moisture with
    precipitable water values between 1.5 and 1.8 inches (90th
    percentile) with 1500-2000 J/kg MLCAPE observed on the 22Z SPC
    mesoanalysis.

    Cells were located just north of a weak mid-upper level vorticity
    max observed on water vapor imagery over south-central FL, along a
    persistent west-east convergence axis seen in fading visible
    imagery offshore of the east coast. Mean easterly winds in the low
    to mid-levels have supported repeating cells with short-term
    training, with observed rainfall rates of 1-2 in/hr near Vero
    Beach. While recent cloud top cooling on satellite imagery has
    appeared to migrate generally just offshore, redevelopment and
    westward translation of heavy rain looks to continue a short-term
    urban/flash flood threat from southern Brevard County into St.
    Lucie County along the coast where an additional 2-4 inches will
    be possible on a highly localized basis through ~01Z.

    Indications are that these cells will weaken after 00Z as boundary
    layer stabilization occurs with nocturnal cooling, with cells
    shifting more offshore or perhaps dissipating. While the HRRR
    hasn't been doing well with the ongoing placement of cells, there
    are indications in recent HRRR guidance that the activity could
    refocus a bit farther south sometime in the 00-03Z time frame.
    Similar potential for slow movement and/or training will exist is
    development does get going farther south later tonight. Any areas
    of flash flooding are expected to remain localized with potential
    for a quick 2-4 inches over the next few hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5Q_aGikNvzafCzBZkLacufk8V7gRB8rgpd-NiBBSPYDk2FeZhieib_YkAuz--L98hVCe= yJGOyht5Bs8lDtVQwfvAzcU$ for graphic product...

    ATTN...WFO...MFL...MLB...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 28308046 27768008 26657985 26118002 26178029=20
    26258043 26628045 27058049 27558065 28018077=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Dec 18 03:51:44 2024
    AWUS01 KWNH 180351
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-180920-

    Mesoscale Precipitation Discussion 1179
    NWS Weather Prediction Center College Park MD
    1050 PM EST Tue Dec 17 2024

    Areas affected...Southeast OK...South-central MO...Far Northeast TX...Arkansas...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 180350Z - 180920Z

    SUMMARY...Another round of elevated occasionally training
    showers/thunderstorms with capability of 1.5"/hr and localized
    totals of 2-3". Intersection with recently saturated increasingly
    dormant soil conditions may result in increased localized run-off
    and low-end flash flooding potential overnight.

    DISCUSSION...03z surface analysis depicts an older polar boundary
    draped across the Red River Valley, S Arkansas into the TN River
    Valley. CIRA sfc to 850 LPW shows return moisture from the western
    Gulf of Mexico streamed northward across central TX, then angling
    northwest across much of AR while ascending across/above the
    boundary into the 850-700mb layer. Total PWat values are in the
    1.25 range, but sharpening upper-level polar trough across the
    Central High Plains is increasing flow through the layers into the
    30-40kt range through 700mb while sharpening the isentropic
    boundary as the northern stream cold front presses further south
    and east over the next few hours. Modest, mid-level drying and
    lingering steeper lapse rates along with the near surface
    moisture/heating is providing solid MUCAPE over the boundary with
    values of 1500-2000 J/kg spreading across SE OK. Additionally to
    the strengthening low level convergence/isentropic ascent; the
    right entrance of the 100 kt jet is dropping southeast providing
    solid divergence and evacuation to developing elevated convection
    (while also moving into broadly diffluent region across S MO/AR
    into the MS Valley).

    Current GOES-E 10.3um and regional RADAR mosaic depict numerous
    narrow core cells breaking out in two SW to NE orientated bands
    across E OK and north-central AR. Coverage will increase and
    updrafts will broaden to support 1.25-1.5"/hr rates occasionally
    increasing to 2"/hr randomly and widely scattered in nature. Deep
    layer flow while not ideally unidirectional, will support cross
    track/repeating particularly over the first 2-4 hours before the
    stronger flow/height-falls aloft increase forward cell motions and
    increase southeastward cell propagation. This should allow for a
    few scattered incidents of 2-3" totals across E OK/W AR and
    perhaps even further downstream; which is likely to align with
    areas that missed out on the moderate/heavy rainfall a few days
    ago; but FFG values of 1.5"/hr and 2-3"/3hrs are well within
    range. Still there are some overlaps along the edges of
    south-central MO and eventually SW AR to south-central AR...that
    may be more susceptible given soil saturation values per NASA
    SPoRT at or above 65-70% in the 0-40cm layer. Also considered,
    flash flooding is possible, but given rates and totals are at the thresholds...any flash flooding is likely to be on the lower end
    and scattered in nature with highest potential in urban locales.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9k0OktekT6-4MAB-s6CmNq1zWrJWc0ukpHtcoOWW2wcxIkYIgfPTxAYzKsNIDQVsEgyO= NeeMQe8udUjNq2_YpnhJcBs$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SGF...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 36789162 36309120 35499120 34769177 33929358=20
    33409564 33519674 34139694 34849641 36019480=20
    36739300=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Dec 18 06:30:50 2024
    AWUS01 KWNH 180630
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-181130-

    Mesoscale Precipitation Discussion 1180
    NWS Weather Prediction Center College Park MD
    129 AM EST Wed Dec 18 2024

    Areas affected...Southeast MO...Northeast AR...Southern
    IL...Northwest TN...Western KY...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 180630Z - 181130Z

    SUMMARY...Warm advective showers/thunderstorms likely to expand in coverage/intensity toward early morning. Training/repeating
    across wet/dormant grounds with low FFG suggest spots of 2-3" may
    result in localized flash flooding conditions.

    DISCUSSION...06z Surface analysis shows southerly return flow
    across MS and W AL northward into W TN has pressed the warm front
    into SW KY with lower 60s and upper 50s Temps and Tds starting to
    trickle in through the MS Valley. Aloft, CIRA LPW and VWP network
    show and increasing moisture plume on 30-35kts of 850-700mb WAA
    across AR into the Tri-Rivers area bringing overall deeper layer
    moisture values over 1.25" with short-term totals likely to near
    1.5" about 09z. The combining streams, low level WAA profile with
    modest lapse rates aloft have seen a steady increase in CAPE with
    500-1000 J/kg analyzed across SE MO/NE AR at this time also to
    focus into a nice SW to NE plume of 1000 J/kg by 09zZ into S IL/W
    KY. As such, regional RADAR and GOES-E SWIR show scattered
    thunderstorms W KY/E TN with greater cooling towers across SE MO
    into NE AR with some tops reaching -60 to -65C; under increasing
    influence of right entrance ascent/evacuation aloft of 100kt 3H
    jet over N MO/N IL.

    Given the strength of flux and available moisture, cores can be
    capable of intense short-term rates with hourly totals of
    1.25-1.5" given progressive/faster cell motions. Orientation of
    cell development to the mean flow along with the scattered
    downstream development (and heavier cells across NW TN/SW KY
    earlier this evening) will allow for repeating over grounds that
    already have 0-40cm soil moisture ratios well above normal (95+
    percentile) over 60%. Hourly FFG values only further decrease
    from west to east with hourly values of 1.5"/hr and 2-2.5"/3hrs
    reducing to 1" and 2-2.5", respectively across central KY/TN.=20=20

    Toward 12z, overall low level profile will continue to align SW-NE
    and increase LLJ strength into the 35-45kt range. This should
    allow for the scattered cells to orient into a longer linear
    convective line from NE to SW though eastward propagation will
    increase reducing the potential for training...all considered
    scattered incidents of flash flooding are possible through the
    morning toward daybreak.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!40Ie6Zq5yf8uB3MWqhWVGlCzKo9snejZAtX0MOTAzCi4qiOLLicShXJEzclSO_LIt0TM= IH5zPZN3bVkbZs6gL20vIaE$ for graphic product...

    ATTN...WFO...LMK...LZK...MEG...OHX...PAH...

    ATTN...RFC...LMRFC...NCRFC...OHRFC...NWC...

    LAT...LON 38218612 37798561 37208571 36798642 36078824=20
    35469063 36109101 36699093 37299000 37878855=20
    38198741=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Dec 18 09:16:23 2024
    AWUS01 KWNH 180916
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-OKZ000-181400-

    Mesoscale Precipitation Discussion 1181
    NWS Weather Prediction Center College Park MD
    415 AM EST Wed Dec 18 2024

    Areas affected...Southern Arkansas...Adj SE OK/NE TX/N LA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 180915Z - 181400Z

    SUMMARY...Flattening convective line shows potential for training
    over the next few hours while crossing saturated soils from recent
    heavy rainfall across southern AR.

    DISCUSSION...Recent GOES-E 10.3um and regional RADAR trends
    suggest upwind edge of best isentropic convergence across SE OK
    has seen a recent uptick in convective development. WV suite
    depicts the right entrance of a speed max in the cirrus across
    central OK at this time. This is resulting a downstream shortwave
    ridging and flattening of the 500-1000mb thickness ridge allowing
    for a more eastward propagation of the convective line likely over
    the next few hours. CAPE analysis fields suggest highest theta-E
    axis is ideally oriented for the isentropic ascent along the Red
    River Valley. Cooling tops below -65C suggests stronger updrafts
    and deeper moisture flux/rainfall production. CIRA LPW places .6
    to .75" sfc-850mb moisture with additional 850-700mb layer over
    .3-.5" allowing for totals of 1.25" to 1.4"; given 30-35kts of
    flow; flux convergence will support rates of 1.5-1.75" and given
    the orientation may allow for 1-2 hours of training before the
    core of height-falls across W OK/NW TX dig more and start to
    accelerate the cold front south and eastward and reduce the best
    ascent angle to the front from the LLJ. As such a streak or two
    of 1.5-2.5" totals remain probable across Texarkana and southern
    Arkansas.

    Unfortunately, heavy rainfall last evening has reduced upper level
    soil capacity across this area with NASA SPoRT 0-40cm saturation
    ratios well above normal in the 65-75% range. So believe FFG
    values may have likely recovered too fast and grounds may be more
    susceptible to increased run-off and potential for localized flash
    flooding. By no means will the rainfall totals be great enough
    for sizable areal coverage and/or magnitude of flash flooding, but
    the potential remains sufficient for an incident or two to occur
    through mid-morning across S Arkansas.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8ImBU7gdw3rEfK9MDyfI6Z8EhZJG1sGH7v7E9YKCKFHrFJ-g4cmmyOqL0Ji0NIw6JTO0= tOWh3VyxLlWscqrydoWoCH8$ for graphic product...

    ATTN...WFO...JAN...LZK...SHV...

    ATTN...RFC...ABRFC...LMRFC...NWC...

    LAT...LON 34969203 34799153 34209115 33829110 33209133=20
    32859199 32859382 33179485 33789516 34319482=20
    34629404 34939286=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Dec 18 11:00:51 2024
    AWUS01 KWNH 181100
    FFGMPD
    TNZ000-KYZ000-181600-

    Mesoscale Precipitation Discussion 1182
    NWS Weather Prediction Center College Park MD
    600 AM EST Wed Dec 18 2024

    Areas affected...Central Kentucky into Western Tennessee...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 181100Z - 181600Z

    SUMMARY...Progressive convective line with embedded intense
    downdrafts capable of 1-1.5"/hr and quick 1.5-2.5" totals across
    low FFG values suggest widely scattered incident or two of flash
    flooding remain possible through late morning.

    DISCUSSION...RADAR mosaic and GOES-E 10.3um EIR show a progressive
    convective line with slight uptick of vigor over the last hour or
    so as the deep layer moisture flux/convergence aligns with
    remaining instability axis across central KY back to SW TN. Core
    of highest theta-E air remains across W TN with 500-1000 J/kg of
    CAPE that decreases slowly northeastward into central KY. GOES-E
    WV suite shows polar upper-level trough has made main push east
    and southward out of the Plains toward the MS Valley. Broad
    divergence along the right entrance to the downstream jet streak
    through the Great Lakes continues to maintain solid large scale
    ascent while maintaining strength of the the LLJ across Arkansas
    into the TN River Valley. Surface moisture in the mid-50s,
    combined with the strong moisture flux convergence along the
    leading edge of the convective line will continue to support
    intense sub-hourly rain-rates in the range of 1.5-1.75"/hr though
    duration is likely to limit totals to 1-2" with perhaps up to an
    additional .5" within the broadening moderate precipitation
    shield.

    The progressive nature should limit overall totals; however, the
    line is moving into overall lower FFG values of 1-1.5"/hr and
    1.5-2"/3hr which remain possible of being locally exceeded.=20
    Overall coverage and magnitude of flash flooding is likely to be
    limited on the low end of exceedance. However, the potential for
    flash flooding will remain possible until about 15-18z when
    instability is nearly fully exhausted and moving into a more
    stable, lower temperature/moisture environment through the
    Cumberland Plateau.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6Md3hLJdhA941mUTQUxMeabtvfSbT989k_pMKdrhV7sY6s-q7FvjZyQEIAl93dn1fJGc= uVyrtBADLr2uMtqlro30JKE$ for graphic product...

    ATTN...WFO...JKL...LMK...MEG...OHX...PAH...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 38218366 37728326 36728462 35918596 35478705=20
    35168826 35198946 35638955 36428855 36958775=20
    37918608 38188508=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Dec 24 02:12:52 2024
    AWUS01 KWNH 240212
    FFGMPD
    CAZ000-ORZ000-241410-

    Mesoscale Precipitation Discussion 1183
    NWS Weather Prediction Center College Park MD
    911 PM EST Mon Dec 23 2024

    Areas affected...Northern CA into Southwest OR

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 240210Z - 241410Z

    SUMMARY...An atmospheric river moving into northern CA and
    southwest OR will bring an increase in rainfall coverage and
    intensity tonight into early Tuesday. Rainfall rates locally as
    high as 0.5" to 1" in an hour may result in some flood risk.

    DISCUSSION...This is a fairly progressive system, which will limit
    the magnitude of rainfall totals and flood risk. However this is
    also a dynamic system with a strong upper jet and deep mid level
    trough moving inland. These features will help enhance ascent and
    also allow for some weak instability along the front supporting
    low topped convective elements locally enhancing rainfall rates.
    The 18z HREF neighborhood probabilities of exceeding 0.5" in an
    hour increase and expand in coverage ~04z across southwest OR and
    northwest CA and peak in the 60-90% range from 06z-12z, with the
    higher probabilities shifting southward with time. There are even
    some 1" an hour probabilities showing up, peaking ~40% in the King
    Range between 06z and 08z. The last few runs of the HRRR also
    shows peak hourly rain ~0.75-1" along a narrow band from the King
    Range into far southwest OR between ~04z and 08z. These rates
    decrease some as the low topped convective line moves inland away
    from the slightly higher instability just offshore, but both HREF
    probabilities and recent HRRR runs still support localized
    rainfall exceeding 0.5" in an hour inland. Despite the progressive
    nature of this system, the potential for these aforementioned
    higher rates does introduce some risk of rock and land slides long
    with minor flooding of urban and other flood prone areas.
    Antecedent rainfall has resulted in above average soil saturation
    and near to above average streamflows, making the flood risk a bit
    higher than it otherwise would be for such an event.=20

    Guidance also suggests we may see anther uptick in rainfall rates
    around 12z over the northern Sacramento Valley and adjacent
    foothills. A combination of enhanced low level convergence driven
    by stronger southerly flow up the valley, and slightly higher=20=20
    instability values over the valley by this time, supports this=20=20
    uptick in rainfall rates potentially towards 1" in an hour. These
    higher rates will likely be fast moving by this time, and so the=20
    heaviest rain at any one location should not last more than an=20=20
    hour or so. This will help limit impacts, although rates could be
    high enough to still result in some localized flood concerns.
    There is a chance rainfall rates between 0.5" and 1" in an hour
    could move over the Park burn scar around 12z. Rainfall rates of
    this magnitude could result in debris flows, so while confidence
    in rates reaching these magnitudes remains low, observational
    trends will need to be monitored closely late tonight into Tuesday
    morning.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4eSVyvBEISJtm2Pp2s5Uusl5WFNV6pSi3sVPQ6FGzsRFy5CL5U2_IJSkY2yzAZpq4KuM= FkOxjEfRzT2GBGEDAt48HEw$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...STO...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 42842444 42652390 42122329 41652327 41392245=20
    41312189 40772164 40382141 40052118 39932108=20
    39662122 39702164 40012206 39792264 39202259=20
    38592274 38302316 38482348 38712368 38982389=20
    39782438 40242463 41152454 42102450 42642462=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Dec 24 13:25:56 2024
    AWUS01 KWNH 241325
    FFGMPD
    CAZ000-242200-

    Mesoscale Precipitation Discussion 1184
    NWS Weather Prediction Center College Park MD
    825 AM EST Tue Dec 24 2024

    Areas affected...Eastern Central Valley & Lower Slopes of Sierra
    Nevada of California...

    Concerning...Heavy rainfall

    Valid 241330Z - 242200Z

    SUMMARY...Quick hitting AR is starting to weaken, but 1-1.25" of
    upslope along lower slopes of central and southern Sierra Nevada
    will continue to pose a heavy rainfall threat into the afternoon.

    DISCUSSION...GOES-W WV suite shows the very strong cyclone that
    spurred the strong moisture advection and strong winds with this
    Atmospheric River has lifted north and is making landfall
    along/north of Vancouver island into central BC. However, the
    base of the longer wave trough remains off-shore and is pressing
    eastward toward the central CA coast. Weak sub-tropical ridging
    just NE of the right entrance of the polar jet (see upstream wedge
    of mid to upper level strato-cu with west-east transverse banding
    signture) well south, generally parallel to Cape Conception.=20=20
    CIRA LPW shows a severing of the core of the AR plume about this
    location as well; combine this with slowly deminishing winds and
    the AR IVT values are and expected to continue to reduce over the
    next 6-9 hours, with a continued bifurcation of the moisture plume
    near surface and mid-levels broadening post-frontally. 13z
    surface analysis depicts the cold front starting to push though
    the southern portion of the northern Valley, though low level flow
    remains backed across the northern Valley. Residual deep moisture
    and steepening lapse rates will allow for increasing instability
    and recent HRRR suggests a few lingering convective cores remain
    possible across the Valley moving southeastward post-frontally and
    intersecting the already saturated lower slopes of Tehama, Butte
    and Yuba counties with potential of spotty .5-1" additional totals
    to maintain ongoing flooding concerns in the area.

    The main AR core along/ahead of the cold front had an excellent
    broad, higher reflectivity core that resulted in .5-1"/hr rates
    but that continues to weaken with the aforementioned reduction of
    moisture and flux. Still, the leading edge will have solid
    moisture and fairly orthogonal intersection with the lower slopes
    of the central and southern Sierra Nevada Range with .75-1" total
    PWat and 35 reducing to mid-20kt flow to allow for .5"/hr reducing
    to .25"/hr rates for 1-3 hours resulting in quick .75-1.25"
    totals. This may near the naturally lower FFG values (.5-.75"/hr
    or .75-1"/3hr) of within the complex/steeper terrain with a very
    low but non-zero risk of widely scattered exceedance; though the
    probability does not rise to FF possible category and will
    consider this a Heavy Rainfall discussion and likely last MPD for
    this event as the front rapidly presses through the Sierra Nevada
    after 21z.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5TIbpStOrameMt-4LqYaC6SYsiivdq3C1ktByVq2Je6Ylbz9ryj49UqPiLWrsfe4tuSL= AmPUffAoGofCkvl6d1KZZgc$ for graphic product...

    ATTN...WFO...HNX...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 40842182 40332159 39872129 39402079 38882053=20
    38312021 37771978 37311927 36931884 35961832=20
    35551828 35161864 35101903 35451942 36021972=20
    36652015 37312038 37812088 38452114 39162152=20
    39702195 40092221 40392241 40692236=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Dec 24 14:04:58 2024
    AWUS01 KWNH 241404
    FFGMPD
    ARZ000-TXZ000-OKZ000-241930-

    Mesoscale Precipitation Discussion 1185
    NWS Weather Prediction Center College Park MD
    904 AM EST Tue Dec 24 2024

    Areas affected...North/Northeast Texas...Portions of SE OK & SW
    AR...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 241405Z - 241930Z

    SUMMARY...Increasing convective activity with potential of
    1.5"+/hr rates with back-building and short-term training
    potential may exceed FFG, especially near urban centers resulting
    in possible localized flash flooding.

    DISCUSSION...GOES-E 10.3um loop shows convection breaking out
    along the frontal zone across North Texas into the Red River
    Valley with steady increasing lightning detection within most
    active cores, particularly along the upstream edge. Surface
    analysis denotes a weak surface low near F02 with stationary front
    meandering through the Red River with northern stream cold front
    slowly dropping southwest across eastern portions of the Big
    Country back through the Concho Valley; south of which, returning
    Gulf moisture is starting to encroach with reinforcing shot of
    enhanced theta-E with mid 60s Tds in the southern Triangle lifting
    north as well. CIRA LPW shows a slug of detached mid-level
    moisture from the Pacific stream pooled along the frontal boundary
    in association with a weak shortwave over northeast OK. GOES-E WV
    suite also denotes, core of northern stream upstream larger scale
    wave is starting to dig across the Central High Plains;
    effectively strengthening the low level flow to further enhanced
    deep moisture convergence over the midday into afternoon hours.=20
    This has resulted in a 500-1000mb thickness ridge over E TX that
    is supporting a veered propagation vector field that will align
    with deeper layer steering for at least a few hours across the Big
    Country into Northeast Texas providing a solid potential for 1)
    training of convection but 2) increasing upstream moisture
    convergence and steepening lapse rates (with modest mid-level
    drying from the southwest) to support increasing instability and
    convergence for development/backbuilding.=20

    In the short-term, the cells are converting modest instability
    with MLCAPE increasing to about 500-1000 J/kg along the upwind
    edge with downstream cells likely becoming a bit more elevated
    with MUCAPE pool of 500 J/kg to maintain more scattered/isolated
    cells into SW AR with time. Solid deep layer convergence and
    total PWats of 1.25" (though bulk of .75"+ at sfc/850mb layer)
    will allow for some intense rainfall production. RADAR estimates
    of 1.5"/hr have already be observed with potential for additional
    capacity if the training/repeating corridor saturates through
    depth.

    A balance of unidirectional SSW steering and some outflow/cold
    pool propagation southeastward may reduce ideal training setup
    given weaker instability totals, but risk of 2-3" totals in 2-3
    hours may result in localized flash flooding. This only increases
    in proximity to DFW urban corridor, where risk goes up and may be
    the only location that these totals may overcome the higher FFG
    given drier 30-50% soil saturation environment along and east of
    I-35...though saturation increases toward the Texarkana region,
    hence the inclusion of the area at this time. As such, a incident
    or two of flash flooding is considered possible in the near-term.=20


    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_0Q92CWVPg1fjm9lGxImqhznbTs7LPIRekyUZg4JCUizngcJcy2cG-pCf62ScdIFVIjE= ApfoMoqXUQ4VO-_ZsLljK8Q$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 34729428 34249336 33499368 32819472 32049641=20
    31759835 32379852 33159788 33879686 34449568=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Dec 24 18:51:39 2024
    AWUS01 KWNH 241851
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-250030-

    Mesoscale Precipitation Discussion 1186
    NWS Weather Prediction Center College Park MD
    150 PM EST Tue Dec 24 2024

    Areas affected...Northeast Texas...Southwest Arkansas...Northwest
    Louisiana...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 241850Z - 250030Z

    SUMMARY...A low-end threat of flash flooding continues with slow
    southeastward drift of frontal zone within favorable training/
    back-building regime.

    DISCUSSION...18z Surface analysis shows a triple point of digging
    cold front and retrograding sliver of dry line near BBD. A cold
    front connects up to a surface wave near Denton before flattening
    further into the Red River Valley just north of Texarkana.
    GOES-Visible imagery shows the effective warm sector with field of
    cu across the majority of E TX, becoming more dense closer to the
    coast given slightly higher Tds in the mid 60s and Temps nearing
    upper 70s; with the exception of a pocket of low level stratus
    that impeded filtered solar radiation across the Hill Country
    generally west of HLR/EDC/T20/BEA. The western Gulf return
    moisture flow is solid east of this shallow stratus with 20-25kts
    of flow increasing toward 30-35kt nearing the front. However,
    there is a bit of veering that has slightly reduced deep layer
    convergence, likely in continued response to the exiting shortwave
    across NW AR and an associated diffluence wedge of 3H ascent
    across north Texas. This continues to support isentropic
    slantwise ascent across the DFW metro into NE TX in proximity to
    the frontal boundary and the convergence is maintaining some
    convective cells into northeast TX, though weaker lapse rates due
    reduce MUCAPE values below 750 J/kg before reaching SE OK/SW AR
    where broader moderate shield precipitation continues.

    Recent RADAR mosaic and GOES-E Visible shows some upstream
    redevelopment in the core of the peak MLCAPE maxima on the NE side
    of the stratus where mid-level SWly flow is providing mid-level
    drying and increased lapse rates; near Hamilton county to Bosque
    county where values are slowly increasing from 1000 J/kg to 1500
    J/kg with further heating. Moisture flux/pooling in/near the
    boundary will aid low-level convergence to support rainfall
    production with capability of 1.5"+/hr rates similar to this
    morning's bout that could occasionally tick up to 2"/hr IF
    prolonged training deepens moisture profile in depth. As cold
    pool generation may overcome due to evaporative cooling; it will
    be a storm scale interaction balance and most likely be widely
    scattered in nature and limited in duration and therefore
    coverage. Still, this may result in localized 2-3" totals in
    less than 2-3 hours. Unlike earlier this morning, the line of
    convection is less likely to track through larger urban, more
    hydrophobic ground conditions and rainfall totals are are the
    lower end of exceeding the slightly higher FFG in the region.=20
    Still, an isolated case of FF still remains possible.

    Downstream into far NE TX/SW AR...
    Instability is likely to continue to be the limiting factor but
    stronger isentropic ascent and with increasingly confluent
    850-700mb moisture streams may allow for a broader shield
    precipitation to form with occasional embedded convective cores
    that ramp up run-off in the short-term. Increasingly deeper
    cyclogenesis should also enhanced WAA/moisture flux to the region
    that this activity may increase toward end of daylight hours with
    rates of 1-1.5"/hr scattered within the deeper unidirectional
    steering flow. Similar 2-3" totals may exist and while not as
    flashy in nature given the longer duration; isolated flooding
    conditions may evolve though 00z across NE TX into SW AR where
    soil saturation values are more average to slightly above average
    per NASA SPoRT 0-40cm RSM fields.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9W_4Km_meX7XjyHBudaT4ZRzje7Nt7oiosYUguFSu0i2-PU2qCspQKMl-jCRV2_Ee7vV= RNcKvVR8VUqy5oX31McLl_A$ for graphic product...

    ATTN...WFO...FWD...SHV...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 34009441 33639344 32849310 32149370 31639564=20
    30989700 31119823 31889820 32599750 33519600=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Dec 25 00:34:05 2024
    AWUS01 KWNH 250033
    FFGMPD
    LAZ000-TXZ000-250600-

    Mesoscale Precipitation Discussion 1187
    NWS Weather Prediction Center College Park MD
    733 PM EST Tue Dec 24 2024

    Areas affected...east-central/southeastern TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 250030Z - 250600Z

    SUMMARY...A few areas of flash flooding, especially across urban
    locations, will be possible through 06Z for portions of east-central/southeastern TX. Rainfall rates of 2 to 3 in/hr are
    expected but should remain localized.

    DISCUSSION...00Z surface observations showed a complex depiction
    of effective boundaries in place over central and eastern TX, but
    with two of the more significant features driving ongoing
    convection being a wavy stationary front and southward extending
    trough axis south of the DFW metroplex and the leading edge of
    higher theta-e air which extended from near RWV to GLS.
    Thunderstorms were scattered across the region but have recently
    been increasing along/ahead of a pre-frontal trough axis/wind
    shift located east of I-35 and extending to just south of SSF. SPC
    mesoanalysis showed uninhibited MLCAPE of 500-1500 J/kg within the
    warm sector of the wavy stationary front to the north, and 2000+
    along the middle to lower TX coast. Anomalous moisture (PWATs 1.0
    to 1.4 inches) combined with favorable instability/shear profiles
    have allowed for organized cells with slower cell motions than the
    deeper-layer mean wind of 15-25 kt. One of these slower cells
    resulted in observed 2-3 in/hr rainfall rates in a southeastern
    Houston suburb ending 2330Z with MRMS showing occasional/spotty
    rates in the 2-3 in/hr since 21Z over north-central TX.

    As the base of a mid to upper-level trough continues to amplify
    over central TX early tonight while translating eastward, forcing
    will be aided by diffluent flow downstream over eastern TX.
    Thunderstorms are likely to continue expanding near the southward
    extending trough axis over east-central TX within the reservoir of
    instability as well as near the quasi-stationary fronts over
    northeastern and southeastern TX. Mean/unidirectional southwest
    flow is likely to allow for some training and repeating cells with
    increasing 850 mb winds overnight (up to ~25 kt) possibly
    supporting slower cell movement and brief backbuilding. Localized
    2-3 in/hr rainfall rates will be likely with isolated 2-3 hour
    rainfall totals of 3-5 inches possible.

    While soils have been fairly dry over this portion of TX over the
    past couple of weeks and FFG values are fairly high (3-5 inches in
    3 hours), overlap of heavy rain with any urban areas will
    exacerbate flash flood potential due to poor drainage of these
    potential higher rates. A few areas of flash flooding will be
    possible, but the threat is expected to remain relatively
    localized.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-M72DAobPLmIhD3qOMgraYugFl6_6YsSHFXYQOW4cO0fOt8RNy_yOJE7iEgTmbQZ9GQb= 5OaACXjPjHbWotmP9jG6qb4$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...LCH...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 32609438 32559392 32129359 31049383 29779491=20
    29189635 28709829 29119879 30659714 31539649=20
    32149586 32479506=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Dec 25 06:04:34 2024
    AWUS01 KWNH 250604
    FFGMPD
    TXZ000-251200-

    Mesoscale Precipitation Discussion 1188
    NWS Weather Prediction Center College Park MD
    103 AM EST Wed Dec 25 2024

    Areas affected...Southeast TX, including Middle and Upper TX Coast

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 250600Z - 251200Z

    Summary...Flash flooding remains possible overnight with localized
    rainfall rates of 1-3"/hr and additional short-term totals as high
    as 3-5" (favored in the vicinity of Victoria and around the Middle
    TX Coast).

    Discussion...A digging shortwave trough is driving a complex of
    thunderstorms over portions of Southeast TX, gradually moving
    towards the Middle and Upper TX Coast. Peak rainfall rates have
    generally ranged from 1-2"/hr, though occasionally have peaked
    between 2-3"/hr along the southern end of the complex (per MRMS
    estimates). The mesoscale environment is characterized by ML CAPE
    of 500-1750 J/kg, precipitable water values of 1.2-1.4 inches
    (near the 90th percentile for late December, per CRP sounding
    climatology), and deep layer (0-6 km shear) of 25-50 kts (with
    both instability and shear maximized in the vicinity of Victoria).

    Going forward, the expectation is for the complex of thunderstorms
    to remain active until near dawn, particularly along the southern
    portions of the complex. Not only is this the best environment for
    discrete convection, but supercells have already favored this area
    with bunkers right motions supporting slow storm motions (10-15
    kts). With both the strongest and slowest convection near the
    Middle TX Coast, the highest localized totals of 3-5" are possible
    here (per 00z HREF 40-km probabilities for 3" exceedance of
    30-50%, as well as more recent runs of the HRRR indicating totals
    near 5"). Farther north (including the greater Houston metro
    area), lower instability and a stronger cold pool should support
    weaker and faster storm motions, generally limiting additional
    totals to the 1-2" range.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6yI9FnMjRfliJHO1AgUChmY7PJv3qFXeb6DtnVXuVPConpX-9354XnRHjm7cJEPIGE1y= n-z-dHGCYjoZH5TvTpfGOs0$ for graphic product...

    ATTN...WFO...CRP...EWX...HGX...LCH...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 30979476 30979413 30629412 29899440 29399466=20
    28959495 28439573 27929684 28799819 29419813=20
    29939697 30449603 30769531=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Dec 25 17:03:35 2024
    AWUS01 KWNH 251703
    FFGMPD
    ORZ000-WAZ000-260300-

    Mesoscale Precipitation Discussion 1189
    NWS Weather Prediction Center College Park MD
    1202 PM EST Wed Dec 25 2024

    Areas affected...Western WA...Western OR...

    Concerning...Heavy rainfall

    Valid 251700Z - 260300Z

    SUMMARY...Strong deepening dynamics will back winds toward more
    favorable orographic ascent by 19-20z and increase rainfall
    efficiency to near .5"/hr in favored spots by 00-03z. Runoff will
    likely increase stream flows, but flooding is not expected quite
    yet except for the most vulnerable/traditional locations.

    DISCUSSION...GOES-W WV suite shows a compact shortwave crossing
    the Southeast Gulf of AK at the far southeast edge of the global
    scale trof that has been dominating the Bering Sea. The compact
    wave as a solid negative tilt to it associated with a broad strong
    polar Pacific Jet with a 150-170kt 250mb streak supporting solid
    low level strengthening wind profile with a strong warm front
    starting to press eastward with 700-500mb moisture flux & WAA
    resulting in lighter showers across W WA and NW OR at this time.=20
    Low level winds continue to strengthen with 40-50kts at 850-700mb
    per LGX VWP but remaining mainly parallel to the coast, but
    increasing reflectivity and polar microwave passes suggest warm
    front is approaching quickly and will veer the wind profile toward
    21z across W WA and W OR. This will be accompanied by the core of
    the sub-tropical moisture stream; with leading 850-700mb moisture
    advected on 60-70kts of flow with IVT values increasing from 400
    kg/m/s toward 600 kg/m/s. Upslope component on the SW facing
    Olympics and Willapa Hills will see first brunt with .33"
    increasing to near, occasionally reaching .5"/hr rates by 00z=20
    when winds start to peak near 80kts from the SW and IVT peaks near
    850-900 kg/m/s. Rainfall totals of 1.5-2.5" by 03z, are likely to
    fully saturate the remaining capacity of the upper soils.=20
    Currently, much of the area is about 70-80% capacity through 40cm
    and while a lot, this is above average in the 70th percentile near
    the coast but increasing toward 75-80th percentile in the higher
    elevations and further inland. As a result, increased run-off
    will be channeled to the streams; and while this is a strong AR,
    the duration is not expected to be long to result in any sizable
    flooding but increase stream flows in preparation for subsequent
    AR surges over the following days.

    As the front passes winds will slacken and veer to more due west
    and much of NW WA will be out of the core of the AR moisture plume
    with .5-.75" PWATs...while shifting into W OR with 1 to nearing
    1.25" total PWats. This will maintain stronger rates in the
    coastal range of W OR for a few more hours before the next
    wave/lifts northward later on Thursday morning. Still by 03z,
    west facing orography in NW OR will experience 1-2.5" of rain even
    to the tops of the peaks, while .5-1" totals are expected in the
    lower valleys (less than .25" in traditional shadowed locations.=20
    Similarly, a good soaking and setting the stage for a likely
    active pattern of AR pulses though the weekend; however flooding
    is not likely to be an issue with exception of the most susceptible/traditionally flooded areas.=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!63vZsNSo0SPkto2ZrbQyGX2WJrtCI8bhV8c3R_XIBrhaaKP1qCVuF8-99Dy7psvvqQ-i= zaXcC8QSeEM7PLM8UuUHVrA$ for graphic product...

    ATTN...WFO...MFR...PQR...SEW...

    ATTN...RFC...NWRFC...NWC...

    LAT...LON 48462444 47932366 47282319 46322307 44672328=20
    43912349 43612382 43492435 43922463 44862442=20
    45692426 46592439 47372467 47862493 48182502=20
    48312497=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Dec 26 03:02:40 2024
    AWUS01 KWNH 260301
    FFGMPD
    CAZ000-ORZ000-WAZ000-261500-

    Mesoscale Precipitation Discussion 1190
    NWS Weather Prediction Center College Park MD
    1000 PM EST Wed Dec 25 2024

    Areas affected...Western WA...Western OR...Far Northwest CA

    Concerning...Heavy rainfall

    Valid 260300Z - 261500Z

    SUMMARY...Atmospheric river activity continues across the Pacific
    Northwest with areas of heavy rain expected to persist into early
    Thursday morning before weakening.

    DISCUSSION...GOES-W Airmass RGB satellite imagery shows a strong
    shortwave trough amplifying offshore of the Pacific Northwest, and
    this is driving a rapidly deepening area of low pressure near 45N
    131W. This approaching low center along with a strong upper-level
    jet on the order of 130 to 150+ kts at 250 mb will continue to
    drive a well-defined atmospheric river into the Pacific Northwest
    overnight with a gradual southward shift of the higher PW axis/IVT
    core by early Thursday morning as a cold front gradually arrives
    and begins crossing the region.

    IVT magnitudes are expected to peak over the next 3 to 6 hours
    across the coastal ranges of far southwest WA, western OR and far
    northwest CA with values impressively reaching as high as 800 to
    1200 kg/m/s. However, the offshore energy and attendant cold front
    is quite progressive and thus these enhanced IVT parameters are
    not expected to persist for too long. The IVT values are forecast
    by the 18Z GFS and 12Z ECMWF to steadily weaken by 12Z as the cold
    front advances inland along with the corridor of stronger low to
    mid-level flow.

    Rainfall rates overnight are forecast to generally be on the order
    of 0.25" to 0.50"/hour with occasional 0.50"+ rates expected for
    especially the southwest facing slopes of the coastal terrain. The
    most recent HREF guidance suggests portions of southwest OR and
    far northwest CA will generally have the highest probabilities of
    seeing these rates, with peak rates potentially here reaching as
    high as 0.75"/hour as the cold front arrives later in the night.

    By early Thursday morning, the rates are forecast to be weakening
    overall, but there will be some post-frontal instability and
    persistence of onshore flow to keep shower activity going that may
    foster some additional brief heavy rainfall rates. A consensus of
    the latest HREF guidance supports additional rainfall totals on
    the order of 2 to 4 inches going through early Thursday morning
    (15Z/7AM PST) across the orographically favored higher terrain,
    and especially the coastal ranges.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8M49YNk1dZh0T4I6mLeXxA08cPYpvQHh3Td323rWZpzqOpGY-HOXXE4-RDpq1HIAuSTx= yjBfKQ0ENUv6OEEPMdRPsBE$ for graphic product...

    ATTN...WFO...EKA...MFR...PDT...PQR...SEW...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 47872325 47542211 46972182 46442176 45442171=20
    44512185 43832202 43142230 42212222 41632232=20
    41052297 40082311 39822346 40102428 41142453=20
    42522470 44752434 46162436 47322425=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Dec 26 14:01:54 2024
    AWUS01 KWNH 261401
    FFGMPD
    TXZ000-OKZ000-261930-

    Mesoscale Precipitation Discussion 1191
    NWS Weather Prediction Center College Park MD
    901 AM EST Thu Dec 26 2024

    Areas affected...Northern Texas...Southeastern Oklahoma...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 261400Z - 261930Z

    SUMMARY...Warm advective wing of highly dynamic cyclogenesis
    already breaking out elevated convection. Continued increasing
    moisture flux and slow instability advection to increase rainfall
    rates to 1.5"/hr crossing areas of recent heavy rainfall.=20
    Short-term training elements pose risk of localized possible flash
    flooding.

    DISCUSSION...A very strong and sharp shortwave can be seen moving
    out of the Texas Panhandle into western OK. A strong digging
    100kt jet parallel to the Front Range of the Rockies decelerates
    sharply before rounding a slowly negatively tilting trof across
    the Big country then rapidly accelerating into 100-105kt SSW jet
    across the MOKSAROK placing much of northeast Texas into a very dynamic/favorable upper-level pattern for rapid evacuation and
    strengthening low level flow...as noted by transverse banded
    activity across the Big Country. Deep layer moisture has been
    limited to the Gulf; but recent CIRA LPW suite denotes that the
    strengthening low level jet in response to the height-falls is
    advecting increasing moisture and higher theta-E across central TX
    toward the region.

    The nose of the MUCAPE axis has recently nudged into the area of
    ascent with 500 to 750 J/kg being analyzed; and as such, recent
    convective towers have been forming along the northeast edge of
    the Hill country with active increasing lightning detected.=20
    Strong WAA pattern from the SW through 700-500mb, indicates the
    strong steering pattern; but with the low level moisture and WAA
    response, redevelopment along the effective boundary slowly
    lifting northeastward across N TX, will allow for some convective
    elements to have a training profile. This training/back-building
    potential is likely to be the main key/driving factor to localized
    flash flooding as well as crossing areas recently saturated from
    prior rainfall two days ago. NASA SPoRT 0-40cm denotes a sharp
    gradient of soil saturation along I-35, becoming 50-65% saturated
    toward northeast TX; however, AHPS 7 day anomaly shows those
    deeper saturation may extend a county or two further west;
    increasing the potential to intersect with the heavy rainfall.

    Cells are likely to be a bit more moisture starved given limited
    mid to upper level moisture and the training is likely to help
    over come it. However, the strength of ascent and focused
    convergence in banded convective lines may allow for .5"/hr to
    increase to 1.5"/hr throughout the late morning into early
    afternoon hours with increased moisture flux. As such, streaks of
    1-3" totals are probable through the morning with slow
    northeastward expansion of the WAA. This places the rates and
    totals near or slightly above the lowered FFG values across the
    area of concern into SE OK; so localized exceedance is possible
    with increased potential in and around the urban DFW corridor.=20=20
    As such, flash flooding is considered possible.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7-lwxPQ-ppsZeC5-MLk-uR9jROzDzUapNNWF7iakQfIoO1oPbEoLcDJr0cI4ugbnYljw= Txlo75z-qsOIWKVuiuEnTVY$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 34969605 34879539 34399470 33709458 32999468=20
    32499532 32069612 31599769 31689832 32309881=20
    33299863 34219764 34679693=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Dec 26 16:42:23 2024
    AWUS01 KWNH 261642
    FFGMPD
    TXZ000-262230-

    Mesoscale Precipitation Discussion 1192
    NWS Weather Prediction Center College Park MD
    1141 AM EST Thu Dec 26 2024

    Areas affected...East Central and Southeast Texas...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 261645Z - 262230Z

    SUMMARY...Increasing convection is developing along confluence
    lines within the strengthening warm conveyor belt. Upstream
    moisture flux/instability advection likely to aid in storm-scale
    backbuilding resulting in periods of training. Rates increasing
    from 1.25 toward 2"/hr by 21z will allow for localized spots of
    2-4" in the next 6 hours. Localized flash flooding will be
    possible.

    DISCUSSION...A highly dynamic setup is trying to rapidly evolve an strengthening thermodynamic environment conducive of strong
    thunderstorms with intense rainfall potential for this evening.=20
    However, in the interim, smaller pockets of unstable air and
    strong dynamic ascent patterns will produce widely scattered cells
    that will have the capability of producing locally 2-4" totals by
    22z and may induce localized flash flooding.

    GOES-E WV suite shows a highly amplified upper level pattern with
    dual jets flanking a weakly negative tilt orientation across the
    Red River Valley into central TX; the upstream jet across E NM is
    about 110-120kts decelerating and descending across the Hill
    country before rounding the base and entering a broad
    strengthening 100 kt jet entance across much of central TX into E
    OK, though broader diffluence is supportive of divergence aloft
    across the Mid-Texas Gulf Coast into SE TX. attm. The old
    stationary boundary extends from near Ardmore to west of DFW metro
    toward Austin and just west of BEA/NOG under influence of the
    highly unstable western Gulf of Mexico. The strengthening LLJ
    aligns with the natural confluence of the western Gulf and is
    surging deeper moisture/instability along a rising warm coastal
    front through the Coastal Plain at this time; intersecting with
    the old surface boundary near KT20. This LLJ will act as a solid
    warm conveyor belt with embedded N-S confluence lines until the
    main upper-level height-falls and effective mid-level cold front
    presses south and eastward into the evening hours. The building
    heat from slightly clearing skies has brought temps in the low 70s
    with similar high 60s and low 70s Tds and increasing MLCAPEs to
    1500-2000 J/kg with the warm front. Convergence from
    southeasterly surface low should provide sufficient convergence
    for scattered thunderstorm development. Recent Lightningcast
    products have been rapidly increasing signals throughout the warm
    sector with a few cells even further north into east-central TX;
    with expected further expansion with further surface
    heating/instability growth.

    Cells that do develop will be ingesting solid 1.25-1.5" total PWat
    air within 30-35kt increasingly confluent flow, which should
    support back-building environment. Given the 850-700mb warm
    sector low-level shear profiles will support solid bulk shear
    values for organized updrafts with some rotation, further
    increasing moisture flux convergence and loading in the lower
    profile for efficient rainfall production. Rates of 1.25"/hr will
    increase to near 2"/hr over the next 6 hours and while coverage is
    likely to be more scattered in nature initially, the backbuilding
    and favorable orientation of convergence bands to the mean
    steering will allow for short-term periods of localized training
    to allow for some localized spots of 2-4"; with greater
    probability initially closer to the coast and along the rising
    warm front. This may intersect areas that received 2-4" of rain
    two days ago, as NASA SPoRT 0-40cm soil saturation ratios are
    modestly high particularly north and east of the Houston Metro,
    but there were some spots southwest that show 200-400% above
    normal precip anomalies on AHPS. With all this considered
    scattered incidents of flash flooding are considered possible
    before evening but will be increasing with time (and after 22z)
    across the area of concern.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!83k89vQkL0se-6SxlNfGWD-VH7qKLS8PCzmL9AIX5ULv-DJljqIl3izLKVzxx1HlQKCv= ZErtIX9-PAavlPWwysaZmIk$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...LCH...SHV...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 32249475 31939413 31449382 31059379 30229390=20
    29509439 28239651 28449693 29519697 30789716=20
    31529678 31979601 32219541=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Dec 26 18:57:14 2024
    AWUS01 KWNH 261856
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-270100-

    Mesoscale Precipitation Discussion 1193
    NWS Weather Prediction Center College Park MD
    156 PM EST Thu Dec 26 2024

    Areas affected...Northeast TX...Southeast OK...Far Southwest AR...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 261900Z - 270100Z

    SUMMARY...Reducing instability, rainfall efficiency; but slower
    moving cells with some training pose spots of 2-3" and widely
    scattered possible flash flooding through evening.

    DISCUSSION...The window for excessive rainfall inducing localized
    flash flooding is starting to close due to multiple factors; one
    being convection moving into areas of higher FFG, though still
    equally saturated in the 0-40 cm layer with NASA Sport RSM still
    in the 60-70% range. The second is reducing moisture flux and
    available instability. Yet, a training steering profile still
    remains as well as potential for stationary cells near the
    pivoting deep layer cyclone over Northern Texas toward 00z.

    Currently, regional RADAR mosaic and GOES-E suite of imagery show
    the decaying convection along the effective 850-700mb warm front
    across NW LA/SW AR angling back to the developing deep layer pivot
    of the cyclone over the central Red River Valley between North and
    Northwest Texas. Strong height-falls as the upper-level jet and
    5H trough swing more negative tilt across central to northeast
    Texas; the effective 850mb cold front is aligning to the surface
    and is pressing much faster eastward to the south. A mid-level
    dry slot/descent channel is starting to pinch in proximity to
    Falls, Robertson and Bell county and the LLJ is starting to take a
    more branched appearance as the confluent flow increases
    convective activity along the trailing convergent southwesterly
    flow and effectively severs the best deep layer moisture transport
    along and ahead of the effective 850mb advancing front.=20

    Currently, the window is still open and MUCAPE values 750 J/kg
    nosing toward 1000 J/kg are still within access and ascend through
    the western branch of the TROWAL to maintain/promote convective
    activity across the Heart of Texas region. The southerly backing
    30kt flow is supporting 1.25" total PWats mainly below 700mb to
    providing solid flux convergence for efficient rainfall production
    for the next few hours with rates of 1-1.25" slowly diminishing
    with time. Deep layer steering at the nose/left rotor of the
    developing dry slot may allow for cells to angle sufficiently for
    some short-term SW to NE training from Freestone/Navarro county
    region to Red River/Cass counties over the next 4-6 hours. As the
    dry slot severs the connection rates will drop below 1"/hr and
    overall totals will reduce to less than the rising FFG values in
    far NE TX, reducing the potential for low-end flash flooding
    conditions.

    A secondary risk may start to occur near the pivot of the deep
    layer cyclone as it crosses North Texas toward 00z. Steepening
    lapse rates and remaining modest pooled moisture and convergent
    flow along the southeast quadrant may spark a few narrow core
    convective cells. Deep layer steering will be near zero near the
    center of the low, allowing for Subtle Heavy Rainfall Signature
    (SHaRS) events with 1-1.5"/hr rates falling over areas having
    recently experienced prolonged moderate shield precipitation
    across the Red River Valley and across into S OK. These would be
    very spotty in nature, but the intensity of the rates in such a
    small area could pose a localized flash flooding risk as well.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6UeAJSEdlBDof7NCT1FAGCfMmd71AcYjg4AgLFxxQkSypyZ3Uumopuv5xMQCBmxZvgts= T2blZsW2fz5MmAwGwxQv8HU$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 34419525 34109433 33619364 32979395 32289460=20
    31229645 32409692 33729715 34299646=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Dec 26 23:58:58 2024
    AWUS01 KWNH 262358
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-270500-

    Mesoscale Precipitation Discussion 1194
    NWS Weather Prediction Center College Park MD
    658 PM EST Thu Dec 26 2024

    Areas affected...southeastern TX into western LA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 262356Z - 270500Z

    SUMMARY...Training and repeating of thunderstorms will continue a
    flash flood threat from southeastern TX into western LA through
    05Z. Rainfall rates of 1-2 in/hr and localized totals of 2-4
    inches can be expected.

    DISCUSSION...Regional radar imagery at 2330Z across the South
    showed a line of thunderstorms extending from northwestern LA into
    the Piney Woods of southeastern TX with a second line extending
    from Jasper/Newton counties to roughly Matagorda Bay. These storms
    were occurring just ahead of a pre-frontal trough/wind shift
    located east of a cold front moving through east-central TX. SPC
    mesoanalysis data from 23Z showed PWATs of 1.4 to 1.7 inches
    coincident with the thunderstorm axis and MLCAPE of 500-2000 J/kg
    from the central TX/LA border to the mid TX coast. Favorable shear
    profiles ahead of a potent mid-level vorticity max (over north TX)
    have supported supercells with enhanced rainfall rates while mean
    steering flow from the southwest has resulted in areas of training
    and/or repeating rounds of heavy rain from the northern TX/LA
    border into the southeastern TX Coastal Plain.

    Over the next 3-5 hours, the best upper level support (PVA, upper diffluence/divergence) will shift eastward from the Arklatex into
    northern LA/southern AR. However, RAP forecasts of instability
    show only a small pocket of 500-1000 MUCAPE just ahead of the
    mid-level low center which should be steadily tracking east
    through the first half of tonight. Due to lower instability
    profiles, a lower end flash flood threat will exist for these
    northern locations where strong forcing will should be balanced by
    a fairly progressive translation of heavy rain toward the east and
    limited instability.

    Farther south, a lack of height falls for the Gulf Coast region
    should result in a slower eastward progression of heavy rain. It
    is here where greater instability is forecast to reside within the
    warm sector (500-1500 J/kg MLCAPE). 850 mb winds of 40-60 kt from
    the southwest and similarly oriented mean steering flow will allow
    for areas of training and repeating thunderstorms capable of 1-2
    in/hr (perhaps locally above 2 in/hr) due to a slower eastward
    progression to the axis of thunderstorms. 2-4 inches of rain over
    a roughly 2 hour window is expected to result in a couple of areas
    of flash flooding through 05Z from southeastern TX into western LA.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-CVMsN44zV6cl5EGyQ9kxK4q073aGWwSlZREmXdpQRwVl8YWclCSHggBiLiwR3Lwqe2B= _T9ceaMmzLObBgV_elWJF50$ for graphic product...

    ATTN...WFO...HGX...JAN...LCH...LZK...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 33949177 33509109 32649100 31619139 30769200=20
    29699292 29499407 29039513 29219549 30059521=20
    31439447 32449392 33769307=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Dec 27 02:46:32 2024
    AWUS01 KWNH 270246
    FFGMPD
    CAZ000-ORZ000-271200-

    Mesoscale Precipitation Discussion 1195
    NWS Weather Prediction Center College Park MD
    945 PM EST Thu Dec 26 2024

    Areas affected...Southwest OR...Northern and Central CA

    Concerning...Heavy rainfall

    Valid 270245Z - 271200Z

    SUMMARY...New atmospheric river surge arriving overnight will
    bring additional rounds of heavy rainfall and potentially some
    localized flooding and runoff concerns.

    DISCUSSION...The latest GOES-W Airmass RGB satellite imagery shows
    a new shortwave trough amplifying offshore of the West Coast which
    will drive a new area of cyclogenesis overnight. The developing
    low center will arrive across the coastal ranges of northwest OR
    and southwest WA by early Friday morning. To the south of this low
    center will be a renewed deep layer fetch of Pacific moisture that
    will overrun the coastal ranges down the coast, and especially
    across southwest OR and into northern and central CA.

    A warm front offshore of the West Coast will be approaching as
    rather strong IVT magnitudes encroach on the region. Enhanced low
    to mid-level flow around the southern flank of the shortwave
    trough will drive IVT values upwards of 750 to 1000 kg/m/s at
    least for several hours (generally between 03Z and 09Z) as the
    warm front arrives and advances inland. Later tonight and toward
    12Z, the low center entering the Pacific Northwest will drive a
    cold front inland across the coastal ranges.

    PWs are forecast to reach as high as 1 to 1.25+ inches, and
    reaching locally as high as 2 to 3+ standard deviations above
    normal with the greater anomalies forecast to set up in the 06Z to
    12Z time frame down across the Bay Area. Even areas a bit farther
    south down the coast around Monterey are expected to see a notable
    increase in PWs overnight as this latest atmospheric river surge
    arrives.

    The latest HREF guidance shows rather high probabilities of seeing
    at least a few hours of potential 0.50"+/hour rainfall rates
    impacting the orographically favored terrain from southwest OR
    down through northwest CA and also portions of the Bay Area in the
    06Z to 12Z time frame. Some of these heavier rains may also at
    least locally spillover into the far northern Sacramento Valley
    and the foothills of the northern Sierra Nevada, but generally the
    heaviest rates should be across the coastal ranges. This will
    coincide with the strongest window of forcing from warm air
    advection and higher IVT parameters. After 12Z, the rates should
    diminish rather substantially as the energy associated this latest
    system advances rapidly inland.

    Additional rainfall totals going through 12Z (4AM PST) Friday
    morning are expected to reach 2 to 3 inches with isolated heavier
    amounts possible. Given the wet antecedent conditions, these
    additional rains may result in some localized flooding concerns
    and this will include some urban flooding potential around the Bay
    Area tonight.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8784PPpwQjwvhq15F2dET7JKppLElsnfqNyj9XokRKUxZ74gHfsylSnY2rK2uCnw_wQK= 8WHCS1WHNlAuclfAjx9eiDQ$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...REV...STO...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 43142392 42382323 41932229 41422172 41052171=20
    40552133 40062088 39642075 39182077 39102137=20
    40002199 39922247 39572247 38952222 38262196=20
    37342135 36822148 36582193 36972258 38182341=20
    39262412 40792456 41792449 42912460=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Dec 27 05:02:00 2024
    AWUS01 KWNH 270501
    FFGMPD
    MSZ000-LAZ000-ARZ000-271100-

    Mesoscale Precipitation Discussion 1196
    NWS Weather Prediction Center College Park MD
    1201 AM EST Fri Dec 27 2024

    Areas affected...Southwest and Central LA...Western and Central MS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 270500Z - 271100Z

    SUMMARY...A broken axis of heavy showers and thunderstorms will
    continue to foster a localized threat for some flash flooding
    overnight across portions of southwest to central LA through
    western and central MS.

    DISCUSSION...The latest GOES-E IR satellite imagery shows a
    vigorous shortwave trough and compact low center transiting the
    Lower MS Valley which continues to foster a rather well-organized,
    but broken axis of heavy showers and thunderstorms. The activity
    has waned somewhat over the last couple of hours as the stronger
    mid and upper-level dynamics begin to lift away from the area of
    greater instability pooled closer to the Gulf Coast, but the
    low-level flow remains rather strong and convergent. In fact, the
    area VWP data continues to show a 40 to 50+ kt low-level jet
    surging northward up toward the Mid-South from the Gulf Coast and
    this is maintaining a corridor of strong moisture transport and
    convergence along and just ahead of a cold front.

    MUCAPE values of 1000 to 1500 J/kg are still noted across areas of
    southwest LA which taper down to 500 to 1000 J/kg across central
    LA and into far southwest MS. The level of effective bulk shear
    that is in place remains quite strong and is locally exceeding 50
    kts which is still favoring a fair degree of convective
    organization with the band of thunderstorms including some
    supercell structures. These stronger cells will continue to have
    the capability of producing very heavy rainfall rates that will
    locally reach 1.5 to 2.5 inches/hour, and this will be aided by
    PWs of near 1.5 inches and the aforementioned low-level jet.

    The 00Z HREF guidance suggests that some southwest to northeast
    training of these more organized cells may still occur at least
    locally going through the overnight hours, with some spotty swaths
    of 2 to 4 inch rainfall totals possible. As a result, the
    convective activity is expected to still foster a localized threat
    for some flash flooding and especially within any of the more
    urbanized corridors.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8AYKJQYCJzdlGJ1DnlsKVi-y-Vy0y68r4TY_Gx05VUkCCrk_D2j8_DfV9ZoNz4PbNAeT= _RwPP91ja-S6tHrJH66gD4o$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MEG...SHV...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 33929018 33838931 33338915 32638945 32049000=20
    31549046 30729121 29619243 29509306 29759358=20
    30539289 31749210 33299114=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Dec 28 01:23:12 2024
    AWUS01 KWNH 280123
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-280630-

    Mesoscale Precipitation Discussion 1197
    NWS Weather Prediction Center College Park MD
    822 PM EST Fri Dec 27 2024

    Areas affected...southern MS/AL into far western FL Panhandle

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 280121Z - 280630Z

    SUMMARY...A threat for training will be heightened across southern
    MS into southern AL and far western FL through at least 06Z. The
    potential for localized flash flooding from rainfall rates in the
    1-3 in/hr range will exist.

    DISCUSSION...Regional radar imagery across the central Gulf Coast
    at 0115Z showed a SW to NE oriented axis of thunderstorms
    stretching from the southern coast of MS into central AL. A second
    axis, with only a widely scattered coverage of cells, was present
    from the offshore waters south of the MS/AL border into portions
    of far southern AL. The environment along and southwest of a
    stationary front extending through southern MS/AL contained
    500-1500 J/kg MLCAPE and 1.5 to 1.7 inch precipitable water values
    (per 01Z SPC mesoanalysis and 00Z LIX sounding). Low level
    confluent flow just above the surface was a main driver in the
    ongoing axis of convection but lift within the right-entrance
    region of a departing 100 kt upper level jet streak over the OH
    Valley may also be contributing to ascent across the Deep South.

    As a shortwave and associated jet energy continue to pull away
    from the region tonight, greater synoptic lift will be weakening
    but the low level confluent flow is expected to remain from far
    southern MS into southern/central AL with a gradual eastward
    translation with time. Instability and moisture parameters will be
    supportive of 1-3 in/hr rainfall rates where cells train. Since
    FFG values are fairly high (3 to 5 inches in 3 hours), the flash
    flood threat should be localized in nature and likely more of an
    issue if areas of training focus atop metropolitan regions, such
    as Mobile and/or Pensacola. The threat for training and high
    rainfall rates is expected to continue until at least 06Z tonight.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!71r839v-_5o6dtr2UdHh9onJgc9ohvM9fxCJDVTYt_8v3LXApt3JgWDndezxxRnFZZol= iUnEg7_i9-z7XwsrVrnv4E8$ for graphic product...

    ATTN...WFO...BMX...LIX...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 32348685 32208624 31688638 30998660 30228731=20
    30058834 29998926 30158951 30418953 30928893=20
    31778810 32168757=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Dec 28 03:07:44 2024
    AWUS01 KWNH 280307
    FFGMPD
    CAZ000-ORZ000-281300-

    Mesoscale Precipitation Discussion 1198
    NWS Weather Prediction Center College Park MD
    1007 PM EST Fri Dec 27 2024

    Areas affected...Southwest OR...Northwest CA

    Concerning...Heavy rainfall

    Valid 280305Z - 281300Z

    SUMMARY...The latest in a series of atmospheric river surges will
    be arriving overnight across southwest OR and northwest CA with a
    new round of focused heavy rain over the coastal ranges.

    DISCUSSION...The GOES-W Airmass RGB satellite imagery shows
    another strong shortwave trough gradually approaching the Pacific
    Northwest which will be favoring the arrival of a new area of
    deepening surface low pressure near Vancouver Island by early
    Saturday morning. To the south of this low center evolution, a
    renewed deep layer surge of Pacific moisture and associated
    atmospheric river activity will be overrunning the coastal ranges
    of southwest OR and northwest CA.

    Strong low to mid-level westerly Pacific flow overnight will allow
    a warm front to approach the region and advance quickly inland
    across northern CA, with a trailing cold front that will then
    gradually begin to cross the coastal ranges by early Saturday
    morning. IVT magnitudes will rise rather sharply over the next
    several hours across especially southwest OR and far northwest CA,
    including Coos, Curry and Del Norte Counties, with values
    increasing to over 750 kg/m/s by 06Z.

    Enhanced warm air advection and moisture transport into the
    orographically favored terrain will likely result in rainfall
    rates approaching and locally exceeding a 0.50"/hour. The 18Z HREF
    guidance shows elevated probabilities (50 to 70 percent) of this
    occurring with potentially some brief 0.75"/hour rates occurring
    as the IVT values peak overnight just ahead of the approaching
    offshore cold front.

    The IVT magnitudes will then be dropping off in the 09Z to 12Z
    time frame which will allow for the rainfall rates and shower
    activity to at least diminish early Saturday morning, but the
    aforementioned cold front that arrives will also be tending to
    slow down which will keep the front in close proximity to the
    coastal ranges of northwest CA through Saturday morning.

    Additional rainfall amounts going through 12Z of 2 to 4 inches are
    likely for especially the coastal ranges of southwest OR and
    northwest CA, with isolated heavier amounts. Given the already wet
    antecedent conditions and high streamflows, these rains are
    expected to foster at least some localized concerns for runoff
    problems and flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5S2qpY0yCgrlh_Xu6QoJd_NKFF2_brL_2Dv6RidVoWup7OYz2RXzF2_zPVJ7mN5N1bJ2= MNpWRLOtTJjCB_69u5oY1Dw$ for graphic product...

    ATTN...WFO...EKA...MFR...PQR...STO...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 43822300 43242210 42362196 41802203 41332170=20
    40812165 40012113 39812140 40222251 39862285=20
    39442332 39442397 40012446 40372455 41322425=20
    42042466 42782479 43542448=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Dec 28 04:12:43 2024
    AWUS01 KWNH 280412
    FFGMPD
    FLZ000-ALZ000-MSZ000-281010-

    Mesoscale Precipitation Discussion 1199
    NWS Weather Prediction Center College Park MD
    1111 PM EST Fri Dec 27 2024

    Areas affected...Southern MS...Southwest AL...Far Western FL
    Panhandle

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 280410Z - 281010Z

    SUMMARY...Extremely heavy rainfall associated with training
    showers and thunderstorms is expected over the next several hours
    just north of the Gulf Coast involving portions of southern MS,
    southwest AL and the far western FL Panhandle. Flash flooding is
    already occurring locally and is expected to continue overnight,
    including growing concerns for major urban flash flooding.

    DISCUSSION...The latest GOES-E IR satellite imagery in conjunction
    with dual pol radar shows a corridor of extremely heavy shower and
    thunderstorm activity impacting portions of Harrison and Jackson
    Counties in southern MS, along with Mobile and Baldwin Counties in
    southwest AL. The convection over the last hour has been growing
    further in organization with cooling convective tops (as low as
    -65C) and the activity showing well-defined cell-training and
    backbuilding characteristics.

    This convection is being driving by moist, convergent and unstable
    low-level flow advancing north in close proximity to a warm front.
    This coupled with a focused axis of moisture convergence and
    divergent flow aloft is likely to foster a continuation of locally
    concentrated and slow-moving showers and thunderstorms with
    cell-training concerns going well into the overnight hours.

    MLCAPE values of near 1000 to 1500 J/kg have been pooling across
    the central Gulf Coast region, and the 00Z RAOB from LIX along
    with the latest CIRA-ALPW imagery shows a rather deep column of
    moisture in place with PWs of 1.5 to 1.7 inches. This coupled with
    as much as 30 to 40 kts of effective bulk shear, and the proximity
    of the warm front should favor organized convection capable of
    producing rainfall rates as high as 2 to 3 inches/hour with the
    strongest cells.

    A look at the 00Z HREF guidance suggests additional rainfall
    totals going through dawn may reach as high as 4 to 8 inches, and
    some localized totals approaching 10+ inches cannot be ruled out
    given the enhanced backbuilding and cell-training concerns. Flash
    flooding is already occurring, and there will be major urban flash
    flooding concerns overnight along areas close to I-10. Areas near
    and just to the north of a line from Biloxi, MS to Mobile, AL and
    potentially edging east into the far western FL Panhandle north of
    Pensacola will need to be very closely monitored overnight for a
    threat for locally significant flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Qif0ATdGfBHQYG_-1XDQqcfOslfa8rthM-HBDYZchRAaFAnAyLl9bPt88Te02ozUMxq= 1vdC7YvcR7BpPAdFtrREfTo$ for graphic product...

    ATTN...WFO...LIX...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 31348709 31028674 30638688 30358737 30258835=20
    30378905 30668907 30958868 31278787=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Dec 28 10:28:47 2024
    AWUS01 KWNH 281028
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-OKZ000-281625-

    Mesoscale Precipitation Discussion 1200
    NWS Weather Prediction Center College Park MD
    525 AM EST Sat Dec 28 2024

    Areas affected...Northern and Eastern TX...Northern LA...Southern
    AR...Western MS

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 281025Z - 281625Z

    SUMMARY...Showers and thunderstorms will begin to rapidly develop
    and expand in coverage by mid to late morning. Heavy rainfall
    rates and wet antecedent conditions will promote increasing
    concerns for flash flooding with time.

    DISCUSSION...The early morning GOES-E Airmass RGB satellite
    imagery shows a mid to upper-level shortwave trough amplifying east-southeastward out of the southern High Plains and advancing
    toward the Red River Valley of the South. Increasingly divergent
    flow aloft and strengthening shear parameters interacting with the
    poleward transport of moisture and instability up across central
    and eastern TX will set the stage for rapidly developing clusters
    of strong thunderstorms in the 12Z to 15Z time frame across areas
    of north-central to northeast TX, with development also then
    taking place farther east in close proximity to a warm front over
    into areas of northern LA, southern AR and possibly western MS.

    This warm front will be an important focus for convection going
    toward midday as a strengthening and increasingly convergent
    southerly low-level jet reaches 30 to 40+ kts in response to
    surface low pressure deepening upstream across north-central TX.
    Already there is as much as 1500 to 2500 J/kg of MLCAPE noted over south-central to southeast TX and southern LA which will be
    lifting north over the next several hours. The convection should
    rather quickly become organized with combinations of multicell and
    supercell thunderstorms evolving and growing upscale in a west to
    east fashion as stronger upstream forcing arrives in conjunction
    with the strengthening low-level jet.

    PWs increasing to 1.25 to 1.5 inches coupled with the instability
    and strengthening shear will likely favor the stronger storms by
    late morning producing rainfall rates as high as 1 to 2
    inches/hour, and there will likely be increasing concerns for some
    cell-merger activity and cell-training near the aforementioned
    warm front. Warm sector convection farther south over areas of
    eastern TX will also begin to initiate and evolve by late morning
    which will be capable of producing enhanced rainfall rates.

    Some rainfall totals of 2 to 4 inches will be possible with the
    morning activity, and with the antecedent conditions quite wet
    with elevated streamflows across much of eastern TX and into the
    Arklatex region, these rainfall amounts are expected to increase
    the threat of flash flooding. This will include an urban flash
    flood threat from near the Dallas-Fort Worth metropolitan area
    eastward over toward Shreveport. More organized coverage of strong thunderstorms (with notable severe weather concerns) along with
    heavy rainfall and flash flooding will evolve beyond this period,
    and expect more MPDs to be issued accordingly.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4VtrFGxZhdszbz1jCtUQenIjnmV5Yv_41ZrfofGKSvnuqTtrlMLn2MDutfGbQSXldjpg= WH3kujPoD34PLZAZ7XFXOh8$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...JAN...LCH...LZK...OUN...SHV...
    TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 34119456 34059309 33929136 33259058 32489072=20
    31899145 31649230 31249413 30429588 30309690=20
    30749739 31419742 31839807 32239820 33089740=20
    33699638 33979555=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Dec 28 17:05:21 2024
    AWUS01 KWNH 281705
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-282230-

    Mesoscale Precipitation Discussion 1201
    NWS Weather Prediction Center College Park MD
    1204 PM EST Sat Dec 28 2024

    Areas affected...eastern TX, northern LA, southern AR,
    northwestern MS

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 281700Z - 282230Z

    SUMMARY...Areas of training heavy rain, with rates of 1-3 in/hr,
    will affect portions of eastern TX into northern LA, southern AR
    and perhaps far northwestern MS through 22Z. Rainfall totals of
    3-5 inches in 2-3 hours will be possible across a SW to NE
    oriented axis, overlapping TX/LA/AR.

    DISCUSSION...Regional radar imagery at 17Z showed scattered to
    widespread thunderstorms from the AR/LA border into northeastern
    TX. Convection extended roughly near/north of a stationary front
    which was analyzed WSW from the MS/AR border into eastern TX at
    17Z. Convection transitioned into a QLCS with southeastward bowing
    observed across I-20 in eastern TX. Meanwhile, an upstream NNE to
    SSW axis of thunderstorms was pressing east along I-35 between ACT
    and SAT, located just ahead of a pre-frontal trough/dryline. 30-40
    kt of SW 925-850 mb flow was advecting moisture northward through
    southeastern TX into the stationary front which marked a gradient
    in MLCAPE with roughly 500-1500 J/kg along the boundary via 16Z
    SPC mesoanalysis data.

    As a potent mid-level shortwave continues to advance east from
    central TX today, downstream forcing will increase as an upper
    level jet max becomes better defined over eastern OK, placing
    right-entrance ascent over the Arklatex to Lower MS Valley. Low
    level winds may also increase a little more into the afternoon
    ahead of the upper trough axis. Thunderstorms are expected to
    continue to expand in coverage ahead of the advancing convective
    line near I-35 with low level convergence near the stationary
    front aligning with mean SW steering flow to support
    training/repeating cores of heavy rain. PWAT coverage of 1.5
    inches and greater is forecast to expand across the region,
    coupled with more than sufficient instability and favorable shear
    to promote organized cells. Thunderstorms will be capable of
    producing 1 to 3 in/hr rainfall rates due to training and
    repeating rounds could amount to 3-5 inches of rain in a 2 to 3
    hour period.

    The greatest concern for training and the heaviest rainfall totals
    through 22Z will be in the vicinity of the stationary front from
    northeastern TX into northern LA/southern AR and perhaps far
    northwestern MS. Farther south, while the convective line near
    I-35 is likely to remain progressive from west to east, additional
    development ahead of the line and periods of short term training
    within the convective axis may still promote a threat for flash
    flooding across portions of southeastern TX into western LA.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4i5B_CGCd0spZ74-7xxxyMPvLmBC7c-caEj4poEVxog-A1lcfgRu45FBPALHA4_OinGV= Q7HFihBaK-K5Mr1ZVIIl3wA$ for graphic product...

    ATTN...WFO...FWD...HGX...JAN...LCH...LZK...MEG...SHV...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 34599115 34399049 33749063 32799145 31879208=20
    30719287 30099476 30589647 31169716 31819719=20
    32369670 32679535 33579389 34119247=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Dec 28 21:45:14 2024
    AWUS01 KWNH 282144
    FFGMPD
    TNZ000-MSZ000-LAZ000-MOZ000-ARZ000-TXZ000-290330-

    Mesoscale Precipitation Discussion 1202
    NWS Weather Prediction Center College Park MD
    444 PM EST Sat Dec 28 2024

    Areas affected...far southeastern TX into lower/middle MS Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 282142Z - 290330Z

    SUMMARY...An axis of training heavy rain is expected to produce
    scattered areas of flash flooding from far southeastern TX into
    the lower/middle MS valley through 03Z. Rainfall rates of 1 to 2
    in/hr (locally higher) are expected.

    DISCUSSION...Regional radar imagery at 0415Z showed a NE to SW
    oriented axis of thunderstorms tracking slowly toward the east
    from southeastern AR into LA and far southeastern TX. Cell speeds
    were slowest in the vicinity of a quasi-stationary front that was
    analyzed from western TN/northwestern MS into southeastern AR,
    with a surface low becoming better defined along the front roughly
    35 miles west of Monroe, LA. South of this low, a cold front was
    moving southeast/east but cells ahead of the front were more
    intense than those to the north with generally colder cloud tops,
    greater lightning frequency and higher MRMS hourly rainfall
    estimates. This was due to the numerous coverage of cells
    (including supercells) along/ahead of the cold front near the
    lower Sabine River to the MS River, with mergers and brief
    training coupling with greater individual cell organization. SPC
    mesoanalysis data from 21Z showed 1500 to 2500+ J/kg MLCAPE in
    place from the LA/MS border into the southeastern TX Coastal
    Plain.

    Water vapor imagery showed that a strong shortwave trough over
    east-central TX was beginning to take on a negative tilt.
    Increasing diffluence and divergence aloft, downstream of the
    shortwave, will overspread the lower and middle MS Valley through
    the late evening. As this happens, the surface low over northern
    LA is expected to organize and track northward up the MS River
    Valley. The southward extending cold front will pick up speed and
    sweep southeastward across southeast TX and LA. While the forward
    speed of the cold front will limit flash flood potential across TX
    and portions of LA, multiple rounds with cells in the pre-frontal environment/mergers and brief training will still pose an isolated
    flash flood threat for these regions.

    Farther north, slow movement of the quasi-stationary front and
    increasing low level moisture transport ahead of the organizing
    surface low will wrap moisture back to the west, north of the low,
    with an expected longer duration of rainfall rates of 1-2 in/hr
    and perhaps the highest additional rainfall totals for the region
    through 03Z, on the order of 2 to 4+ inches from near the MS River
    into northwestern MS and southwestern TN. FFG values are lower for
    these northern areas 2-3 inches in 3 hours, and therefore, flash
    flooding appears likely.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9w36jnmzsUfUSBYucW5z_D40yqswbGnGbSTvNPgSoLjqC8xkC7mD_LsX7otRtyPAodcm= egr8NDaV1b8KScbomMakKBI$ for graphic product...

    ATTN...WFO...HGX...JAN...LCH...LIX...LZK...MEG...SHV...

    ATTN...RFC...LMRFC...SERFC...WGRFC...NWC...

    LAT...LON 36228927 36068867 35498838 34708850 33298883=20
    32028940 30369057 29339295 29559483 30789473=20
    31489371 32869292 33719206 35299093 36088987=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Dec 29 02:33:43 2024
    AWUS01 KWNH 290233
    FFGMPD
    FLZ000-TNZ000-ALZ000-MSZ000-LAZ000-290830-

    Mesoscale Precipitation Discussion 1203
    NWS Weather Prediction Center College Park MD
    931 PM EST Sat Dec 28 2024

    Areas affected...Central Gulf Coast...Mid-South

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 290230Z - 290830Z

    SUMMARY...Strong to severe thunderstorms associated with an
    eastward advancing QLCS will continue to foster some potential for
    areas of flash flooding going into the overnight hours.

    DISCUSSION...The latest GOES-E IR satellite imagery in conjunction
    with dual-pol radar shows a well-defined QLCS continuing to
    advance off to the east across large areas of the Mid-South with
    an extension essentially from northern MS south-southwestward down
    into southeast LA. This continues to be associated with a strong
    mid-level trough ejecting out of the Lower MS Valley and lifting
    toward the Mid-South as it gradually takes on a neutral to
    slightly negative tilt. Enhanced deep layer ascent and shear
    continues to interact with a strong southerly low-level jet of 40
    to 60+ kts and this will continue to drive a well-organized axis
    of convection downstream across much of the South going through
    the overnight hours.

    MLCAPE values of 1500 to 2500 J/kg are noted across southeast LA
    into far southern MS, and this coupled with higher PWs reaching
    over 1.5 inches should tend to drive heavier rainfall rates across
    this area with the more organized convective cells that will be
    crossing this region over the next several hours. The convection
    in general across the central Gulf Coast region including
    southeast LA, southern MS and southern AL may tend to take on more
    of a southwest to northeast orientation going through 06Z which
    will facilitate some areas of cell-training.

    Farther to the north, the instability does drop off rather
    considerably, and especially for areas up across northern MS,
    northern AL and through middle TN, but with such strong dynamical
    forcing crossing this region, there should still be at least some
    broken QLCS activity that fosters heavy rainfall. This portion of
    the overall convective axis is certainly more progressive though
    which will tend to keep the overall rainfall potential a bit more
    limited.

    Rainfall rates with the stronger and more organized storms, and
    especially the supercell activity closer to the central Gulf
    Coast, will still be capable of reaching 1.5 to 2.5 inches/hour.
    For areas that do see cell-training, some additional rainfall
    amounts of 2 to 4 inches will be possible overnight. This may
    drive at least some pockets of flash flooding and especially
    around the more sensitive urban corridors.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!66qJBdcM3qSWnWivv0F8k5hcl4Ewq1Kk7lTRWu4iMEUXLiuVSl6OCxLGAI7I6L6dgqMn= -S6pPSdzuszfomkmTBntI2U$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LCH...LIX...MEG...MOB...OHX...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 35668714 35168590 33308571 31228642 30218757=20
    29908868 29528996 29249100 29469199 30089196=20
    30999050 32408972 34238929 35248854=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Dec 29 04:26:57 2024
    AWUS01 KWNH 290426
    FFGMPD
    CAZ000-ORZ000-291625-

    Mesoscale Precipitation Discussion 1204
    NWS Weather Prediction Center College Park MD
    1125 PM EST Sat Dec 28 2024

    Areas affected...Southwest OR...Northern CA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 290425Z - 291625Z

    SUMMARY...Increasing rainfall rates associated with strengthening
    atmospheric river activity will be impacting southwest OR and
    northern CA overnight and through early Sunday morning. The wet
    antecedent conditions and additional rains will promote concerns
    for urban and small stream flooding, including a low-end flash
    flood threat for any sensitive burn scar locations.

    DISCUSSION...The latest surface analysis shows a warm front across
    northern CA and with an offshore extension of this to a developing
    surface low near 43N 130W. A cold front then extends well
    southwest away from the low center. The low center will be
    deepening overnight as it lifts northeastward toward the Pacific
    Northwest overnight in conjunction with an amplifying shortwave
    trough. The attendant warm front will slowly lift north with time,
    but this coupled with deep layer southwest flow should still help
    to focus a well-defined atmospheric river into the coastal ranges
    of southwest OR and northwest CA.

    GOES-W GeoColor satellite imagery shows the southwest extension of
    moisture offshore of the West Coast, and the latest CMORPH2 and
    NESDIS Blended Rain Rate data shows a pool of heavier rainfall
    rates kust offshore in association with the advance of stronger
    low to mid-level IVT magnitudes. The IVT values should increase to
    750 to 1000 kg/ms/s in the 06Z to 12Z time frame across portions
    of Coos, Curry, Del Norte and Humboldt Counties going from north
    to south across southwest OR and northwest CA as the core of the
    strong low to mid-level flow arrives ahead of the offshore cold
    front and the south side of the aforementioned low center.

    Enhanced warm air advection, moisture transport and orographic
    ascent should favor rainfall rates increase to as much as 0.5" to
    1.0"/hour across these coastal ranges. Rainfall rates may also
    approach and briefly exceed a 0.50"/hour for some of the adjacent
    terrain and counties extending inland into southern parts of the
    OR Cascades and also down into the Shasta/Sisikiyou ranges of
    northern CA including also eventually parts of the northern Sierra
    Nevada early Sunday morning. Some of the heaviest overall rates
    should tend to be associated with the final arrival and passage of
    a cold front, and there may be some convective elements associated
    with the front that will enhance the rainfall rates.

    After the cold front passes through, the rates will then quickly
    slacken, but additional rainfall totals over the next 6 to 12
    hours are forecast to reach as high as 3 to 6+ inches for the
    favored coastal ranges, and with as much as 1 to 3 inches
    elsewhere. Some of these heavier rains may also reach down the
    coast into the Bay Area Sunday morning.

    Given the wet antecedent conditions and high streamflows, these
    additional rains are likely to increase the concern for areas of
    urban and small stream flooding, and there may be at least a
    localized flash flood threat should some of these heavier rainfall
    rates overlap any of the more sensitive burn scar locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8dOWZUGZOi6H9JYNkcqb2e7NJkXCb7ced17aC56rmajOFfoUdP0hiVS36up0JBynBsbt= KlEz6OyACTuHTemwR1GXNhc$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...PDT...PQR...REV...STO...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 44712205 44262132 43742131 43252177 42792210=20
    42532272 42132301 41792271 41522238 41502185=20
    41262169 41012151 40382131 39562038 39022023=20
    38822057 39092111 39682161 40372216 40452237=20
    40322278 39782256 39342255 38702206 38012172=20
    37282169 36972215 37352271 38142330 39372423=20
    40592459 41602465 42482464 43212459 43962399=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Dec 29 15:35:32 2024
    AWUS01 KWNH 291535
    FFGMPD
    FLZ000-291945-

    Mesoscale Precipitation Discussion 1205
    NWS Weather Prediction Center College Park MD
    1034 AM EST Sun Dec 29 2024

    Areas affected...FL Keys

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 291533Z - 291945Z

    SUMMARY...There is increasing potential for torrential rainfall to
    impact the FL Keys over the next few hours. Rainfall rates of 2 to
    4 in/hr will be possible, though significant uncertainty remains
    with the evolution of rainfall.

    DISCUSSION...15Z visible satellite and local radar imagery from
    KBYX showed a WSW to ENE axis of thunderstorms about 10 miles
    north of the lower and middle FL Keys. The storms were slow
    moving, located along a long-lived outflow boundary which has been
    slowly dropping south over the past few hours. The environment was
    favorable for organized cells with 40+ kt effective bulk shear and
    500-1000 J/kg MLCAPE and about 2 inches PWAT (SPC mesoanalysis and
    12Z KEY sounding). KBYX estimated rainfall rates were 2-4 in/hr
    across the offshore waters of FL Bay. Area surface observations
    along the Keys showed southerly winds of 10-20 kt with gusts to
    near 30 kt, within a broadly confluent low level wind pattern just
    above the surface, allowing overrunning of the slow moving outflow
    boundary with cells generally training from west to east. There
    were embedded mesocyclones with a fairly large mesocyclone/mesolow
    located about 15 miles northwest of MTH. Upper level flow was
    diffluent ahead of a southern stream upper jet max over the Gulf
    of Mexico.

    While hires models are unable to handle the mesoscale details of
    the ongoing convective axis, loops of satellite/radar suggest the
    outflow will continue to slowly sink south with heavy rain
    impacting the Keys over the next 1-2 hours. Cyclonic flow around
    the mesolow northwest of MTH may cause the outflow to
    progressively sink south through the lower Keys over the next
    couple of hours, with only a glancing blow of heavy rain to land
    areas. However, this scenario is only speculation and continued
    upstream convective development and strong southerly flow may
    offset any stronger southward push of outflow, allowing for
    stalling and torrential rainfall to persist a bit longer. Even if
    rainfall overlaps the island chain for "only" an hour or two, that
    could still result in several inches of rain which may produce
    flash flooding.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4oDjM0fuHCSNj41GNcQFnIb3blAd1UEH4n_WyjmZbN8Ui77WR-eRpPF4Z7D5bG_NrfFP= a0rlnDyna1OEd9MAtfaPTas$ for graphic product...

    ATTN...WFO...KEY...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 25258024 24738027 24338119 24408180 24688195=20
    24878117=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jan 9 21:56:19 2025
    AWUS01 KWNH 092155
    FFGMPD
    TXZ000-100400-

    Mesoscale Precipitation Discussion 0001
    NWS Weather Prediction Center College Park MD
    454 PM EST Thu Jan 09 2025

    Areas affected...Upper Texas Coast

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 092200Z - 100400Z

    SUMMARY...Blossoming convection may briefly train along portions
    of the Upper Texas coast this evening. Rainfall rates around
    1.5"/hr are possible in urbanized communities and could lead to
    localized flash flooding in poor drainage areas.

    DISCUSSION...Deepening low pressure along the Texas coast is
    located beneath the divergent right-entrance region of a robust
    ~160kt 250mb jet streak over the Middle Mississippi River Valley
    this afternoon. Farther west, an anomalous upper trough over
    northern Mexico contains 500mb heights as low as the 1st
    climatological percentile according the NAEFS. Onshore flow will
    increase at low levels this evening as high pressure over the Ohio
    Valley and the deepening surface low along the Texas Coast tighten
    the surface pressure gradient. In fact, southerly 850mb winds of
    40-50kts around 00Z this evening are above the 99.5 climatological
    percentile per NAEFS. These atmospheric parameters are playing a
    role in the development of an IVT surpassing 1,000 kg/m/s, which
    are values above the maximum observed IVT levels in the CFSR
    database per NAEFS.

    As the low-level wind field strengthens, surface-925mb FGEN will
    also strengthen as low-level winds draw PWs up to 1.75" ahead of
    the storm. Rainfall rates will increase in intensity this evening
    to the north of the warm front, as well as the western flank of
    the storm's circulation. Area averaged HRRR soundings from the
    Houston metroplex to Galveston show >98% saturated soundings from
    the surface to 300mb and warm cloud layers as deep as 12,000ft.
    This supports favorable warm rainfall processes, but the one big
    ingredient that is lacking is instability. Moisture advection and synoptic-to-mesoscale forcing alone would support hourly rainfall
    rates of 1"/hr rainfall rates, but the HRRR shows as much as 250
    J/kg of MUCAPE present along the Upper Texas coast. It is here
    where hourly rainfall rates may approach 1.5"/hr with low chances
    (5-10% via the 12Z HREF) for rainfall rates of >2"/hr.

    NASA SPoRT-LIS in the sfc-10cm and sfc-40cm soil depths are
    running drier than normal with some locations in moderate drought
    according to the latest drought monitor. This atmospheric setup is
    one where most of the observed rainfall will be more beneficial
    than harmful. That said, locally excessive rainfall rates may lead
    to localized flash flooding tonight in areas that feature a
    greater concentration of non-permeable surfaces. Any minor
    flooding or ponding may also be harder to identify for motorists
    with the heaviest rainfall rates arriving after sundown.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6WuwYvpJCKhEATb070Liy1Kuaz0SAUjCpSHY6BLIYNSZFUo__rWPTiO-Q7PN2edyhkNT= Rl3AkQy2cmPVUwEZCbtSnw0$ for graphic product...

    ATTN...WFO...HGX...LCH...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 29949414 29599410 29139464 28519559 28559607=20
    28819626 29089625 29489589 29849525=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jan 13 05:29:06 2025
    AWUS01 KWNH 130529
    FFGMPD
    ALZ000-MSZ000-LAZ000-131027-

    Mesoscale Precipitation Discussion 0002
    NWS Weather Prediction Center College Park MD
    1228 AM EST Mon Jan 13 2025

    Areas affected...southeastern Louisiana into southern Mississippi
    and southwestern Alabama

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 130527Z - 131027Z

    Summary...Isolated/low-end flash flood potential exists as shallow
    convection continues to redevelop/train across the discussion
    area.=20

    Discussion...Over the past 2-4 hours, a focused area of convection
    has trained along an axis extending from near Morgan City to near
    Laplace and Lake Pontchartrain. The convection is favorably
    oriented parallel to fast (60-80 kt) southwesterly flow aloft and
    is also being maintained by focused convergence on the nose of
    30-kt 850mb flow. Stout convergence is maintaining this
    convection despite modest instability. Training convection was
    resulting in a few spots of 0.5-1 inch/hr rain rates that have
    persisted long enough for MRMS rainfall estimates exceeding 3
    inches per six-hours. MRMS also depicts peak rainfall/FFG ratios
    now exceeding 0.6 in spots beneath the training band.

    Also somewhat concerning is the fact that models/CAMs suggest that
    the sustained convergence resulting in the convection should
    persist across areas west of New Orleans for at least another
    couple hours, further contributing to localized runoff/flood
    potential especially in western suburbs of New Orleans Metro.=20
    Over time, the axis of heavier rainfall should translate eastward
    in tandem with peak 850mb flow, with a few spots of isolated
    flood/runoff problems extending toward Northshore Lake
    Pontchartrain and adjacent areas of southern
    Mississippi/southwestern Alabama over the next 2-4 hours or so.=20
    This threat should remain isolated, but may become enhanced where
    heavier rain rates can affect any urban/low-lying areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5lgj6_24p6wF6tyyVzp9KfTlxr-vAa1kZJ22IwlhC8WBE9JViKvc4uF2BemgDzRy8QhS= QRgbkMFzgMA3Zc4jIei9jZs$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 31418904 31418809 30988783 30648822 30028936=20
    29888975 29659086 29649184 30129186 30689116=20
    31089015=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jan 26 19:06:52 2025
    AWUS01 KWNH 261906
    FFGMPD
    CAZ000-270105-

    Mesoscale Precipitation Discussion 0003
    NWS Weather Prediction Center College Park MD
    205 PM EST Sun Jan 26 2025

    Areas affected...Southern California

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 261905Z - 270105Z

    SUMMARY...Locally heavy showers and a few thunderstorms arriving
    over the next several hours may result in localized areas of burn
    scar flash flooding, including debris flow activity. This will
    include the Eaton, Palisades, Hurst, Franklin, Bridge and Hughes
    fire areas.

    DISCUSSION...GOES-W satellite imagery shows an upper-level low
    continuing to drop south toward southern CA, with coastal surface
    low pressure helping to facilitate an increase in low-level
    onshore flow into the Transverse and Peninsular Ranges. The flow
    is modest, but the uptick in Pacific moisture coupled with
    gradually steepening mid-level lapse rates and divergent flow
    aloft via DPVA is driving broken coverage of moderate to locally
    heavy shower activity.

    Additional shortwave energy rounding the base of the upper low
    will overspread the coastal ranges this afternoon, including much
    of the broader Los Angeles Basin. This coupled with a slight
    increase in diurnally driven instability and orographic ascent
    should help facilitate an increase in rainfall rates. In fact,
    there has already been some lightning activity noted with recent
    low-topped convection that has impacted Ventura County, and radar
    imagery shows convection tending to intensify just offshore of Los
    Angeles County which will be moving inland soon. This is where
    some MUCAPE values of 250+ J/kg are noted in the latest RAP
    analysis.

    The 12Z HREF guidance favors occasional rainfall rates locally
    reaching or exceeding a 0.25"/hour with some of the stronger
    convective elements that materialize over the next several hours.
    However, with the slight increase in instability and pulse nature
    of the convective threat, it is possible that there could be as
    much as a 0.25" of rain in as little as 15 to 30 minutes. The
    latest guidance suggests some spotty 6-hour rainfall totals
    reaching upwards of 1 inch where some of this activity persists
    over the foothills of the terrain including the San Gabriel and
    San Bernadino Mountains.

    Given the significant sensitivities on the ground with the ongoing
    wildfire activity and/or recently burned areas, these rains may be
    sufficiently heavy enough, at least on a localized basis, to
    result in some debris flow/mudslide activity and related flash
    flooding concerns. The Eaton, Palisades, Hurst, Franklin, Bridge
    and Hughes burn scar areas in particular will need to be closely
    monitored for impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!53YZ0QmbT34wxoA1C2YMl_sXNG14x0HdATKan4Qquj7yxKUoUmHjETLGk1wc_3hwLdq4= tI_pP8L1bTMokH8WkTqy3os$ for graphic product...

    ATTN...WFO...LOX...SGX...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 34861989 34761923 34681885 34521836 34381780=20
    34271702 33761663 33271688 33101720 33241756=20
    33491792 33601830 33841860 34041918 34291960=20
    34422014 34662028=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jan 27 02:06:58 2025
    AWUS01 KWNH 270206
    FFGMPD
    CAZ000-270805-

    Mesoscale Precipitation Discussion 0004
    NWS Weather Prediction Center College Park MD
    906 PM EST Sun Jan 26 2025

    Areas affected...Southern California

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 270205Z - 270805Z

    SUMMARY...An uptick in shower and thunderstorm activity is
    expected through the evening hours across coastal portions of
    southern California. This may result in localized areas of burn
    scar flash flooding, including debris flow activity. This will
    include the Eaton, Palisades, Hurst, Franklin, Bridge and Hughes
    fire areas.

    DISCUSSION...GOES-W satellite imagery continues to show a deep
    layered low dropping south just off the southern CA coast. Some
    cooling of cloud tops is noted over coastal Santa Barbara county,
    resulting in a modest uptick in rainfall rates. As of 01z, water
    vapor imagery continues to depict mid and upper level dry air
    further south over Los Angeles county, likely helping limit shower
    coverage and intensity. However, as the low continues to drop
    south, we should see a gradual moistening of the column, along
    with a steepening of lapse rates. These factors should promote an
    uptick in shower (and isolated thunderstorm) activity over coastal
    areas of Ventura, Los Angeles and Orange counties as the evening
    progresses. In fact as of 02z just beginning to see an uptick in
    shower activity and slight cooling in IR imagery over Los Angeles
    County.

    Recent HRRR runs and the 18z HREF are supportive of an uptick in
    shower coverage and rainfall rates between 02z and 12z. HREF
    probabilities of exceeding 0.5" in an hour increase into the
    20-40% range. The 23z HRRR depicted hourly rainfall around 0.75"
    just offshore, although the 00z HRRR is back closer to 0.5" an
    hour for peak rates. Both the HREF and HRRR focus the majority of
    these higher rates just offshore where the weak instability should
    stay focused. However, while the better coverage of these higher
    rates should remain just offshore, do anticipate we will see some
    0.5"-0.6" an hour rainfall make it onshore on a localized basis
    anytime between ~02z and 12z.

    For the most part this forecast rainfall will only result in
    localized minor flooding of urban and low lying areas. However,
    more significant impacts are possible over recent burn scar areas,
    particularly over Los Angeles County. Confidence on these more
    significant impacts remains low, however with the expected uptick
    in shower coverage and intensity this evening, the threat of
    significant impacts is higher than it was earlier this afternoon.
    The Eaton, Palisades, Hurst, Franklin, Bridge and Hughes burn scar
    areas in particular will need to be closely monitored for debris
    flow impacts this evening into the overnight hours.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4uDbQG2HQ3AXj8bza6JbxE_3NsjrpFL5VCim8O4HzhHqpTV4u8UDgWZJQs1a_ZIc2wmp= mkTgB9Us3LpwC15hDi3sH1k$ for graphic product...

    ATTN...WFO...LOX...SGX...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 34651835 34431817 34301774 33981760 33631762=20
    33451786 33571821 33631832 33991925 34322034=20
    34382049 34642044 34551947 34561934 34611884=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jan 30 01:46:49 2025
    AWUS01 KWNH 300146
    FFGMPD
    ARZ000-TXZ000-OKZ000-300644-

    Mesoscale Precipitation Discussion 0005
    NWS Weather Prediction Center College Park MD
    845 PM EST Wed Jan 29 2025

    Areas affected...Parts of North Texas and Southeast OKlahoma

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 300144Z - 300644Z

    SUMMARY...Increasing shower and thunderstorm activity is underway
    and is expected to continue into the late evening across portions
    of northern Texas and southeast Oklahoma which results in an
    increasing risk of flash flooding through 0630Z.

    DISCUSSION...Composite image of area 88D reflectivites from early
    this evening showed shower and thunderstormn activity growing in
    areal coverage with embedded heavy rainfall already moving through
    portions of the urbanized Dallas-Ft Worth metropolitan area.=20
    Given the approach of a trough in the southern stream along with a
    surface cold front...the trend for increasing coverage and
    rainfall intensity is expected to continue through at least 0630Z
    leading to increased risk of flash flooding.

    Recent HRRR runs and the 18z HREF are supportive of increasing
    coverage of showers and thunderstorms overnight as low level flow
    becomes southerly in the 20 to 35 kt range and begins to draw
    moisture northward from the Gulf. However...the models have
    already been proven to be too slow to develop heavy rainfall
    rates. Rainfall rates from the most active convection should
    generally be in the 1 to 1.5 inch range although isolated 2 inch
    per hour rates can not be entirely ruled out with some potential
    for 2 to 4 inches possible.

    Concern for flash flooding is greatest in urban areas and where
    storms have a chance to train...with flooding more in low lying
    areas in more rural areas.

    Bann

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6RSuJnuptgV9-xdqjF6cijpCseCo3G956WMpp8TGA3eVxuaKhKWo-mAMwAdeG9yIQKOc= gagUSGQqnwQfU5ZP1VZ0RrY$ for graphic product...

    ATTN...WFO...EWX...FWD...LZK...OUN...SHV...SJT...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 35289442 34329402 32469591 31239713 30439775=20
    30989861 32489814 34389658=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jan 30 05:45:08 2025
    AWUS01 KWNH 300544
    FFGMPD
    TXZ000-OKZ000-301043-

    Mesoscale Precipitation Discussion 0006
    NWS Weather Prediction Center College Park MD
    1243 AM EST Thu Jan 30 2025

    Areas affected...North-Central to Northeast TX...Far Southeast OK

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 300543Z - 301043Z

    SUMMARY...Heavy showers and thunderstorms will continue through
    the overnight hours. Areas of cell-training will continue to pose
    concerns for flash flooding and especially around the more
    urbanized locations. This will include the Dallas-Fort Worth
    metropolitan area.

    DISCUSSION...The latest GOES-E IR satellite imagery in conjunction
    with dual-pol radar shows a southwest/northeast oriented band of
    heavy showers and thunderstorms impacting areas of north-central
    to northeast TX, including especially the southern and eastern
    portions of the Dallas-Fort Worth (DFW) metropolitan area.

    All of the convection is being driven by the interaction of
    shortwave energy ejecting northeast across the southern Plains out
    ahead of the deep closed low over the Southwest, and with the
    pooling of at least modest instability and favorable southerly
    moisture transport out ahead of a frontal zone. MUCAPE values
    across much of central to northeast TX have risen to as much as
    1000 J/kg with the aid of a southerly low-level jet of 30 to 40+
    kts, and the CIRA-LVT values in the SFC-850 mb layer have been
    increasing steadily over the last few hours which is reflective of
    the increasing low-level moisture transport.

    The flow aloft is quite divergent based off the GOES-E IR/WV data
    and this should continue to promote a stronger low-level jet
    response going through the overnight hours with enhanced warm air
    advection along with favorable moisture and instability transport
    for heavy rainfall. There has been some cell-training noted with
    the convection over the last couple of hours and portions of the
    DFW metroplex have already received 2 to 3+ inches of rain with
    rainfall rates with some of the stronger cells reaching 1.5+
    inches/hour.

    Over the next few hours, the focus for the strongest axis of
    convection and heavy rainfall should tend to remain over the
    southern and eastern sides of the broader DFW metroplex, with some
    localized expansion of convection expected off to the northeast
    toward areas of the Arklatex, but mainly concentrated over areas
    of northeast TX and far southeast OK.

    Additional rainfall amounts of 2 to 4 inches are forecast
    overnight with isolated heavier totals possible where any
    cell-training tends to persist. Given the heavy rainfall that has
    already occurred over the last few hours, and these additional
    totals, flash flooding is likely overnight with the more urban
    locations the most susceptible to impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7Uv1FVTO6kNQSACLqRdyU4m03fCcfknashKVouQS9FXbudzYYCfAIwO3RmYkc5y8sR8q= 4dSTJ9xm3Jq-hVo_-dioFDs$ for graphic product...

    ATTN...WFO...FWD...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 33999460 33289472 32549572 31759694 31499786=20
    31699820 32269791 33179691 33949544=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jan 30 09:22:54 2025
    AWUS01 KWNH 300922
    FFGMPD
    ARZ000-TXZ000-OKZ000-301520-

    Mesoscale Precipitation Discussion 0007
    NWS Weather Prediction Center College Park MD
    421 AM EST Thu Jan 30 2025

    Areas affected...Central to Northeast TX...Southeast OK...Western
    and Central AR

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 300920Z - 301520Z

    SUMMARY...The threat for areas of flash flooding will continue
    this morning from broken bands of heavy showers and thunderstorms
    which will occasionally be capable of training over the same area.

    DISCUSSION...The latest GOES-E IR satellite imagery along with
    dual-pol radar continues to show broken areas of heavy shower and
    thunderstorm activity impacting areas of central to northeast TX
    through southeast OK and more recently into areas of western AR.

    Strong warm air advection with the aid of a strengthening
    south-southwest low-level jet of 30 to 50 kts continues to work in
    tandem with modest instability, but rather strong moisture
    convergence for sustainable convection. The flow aloft remains
    rather divergent out ahead of a deeper layer low center slowly
    ejecting east out into the southern High Plains, and this along
    with a triple point low center over northern TX is further helping
    to concentrate a corridor of rather strong forcing.

    MUCAPE values remain generally around 1000 J/kg with PWs close to
    1.5 inches, and this coupled with at least moderate shear should
    continue to support some rainfall rates with the stronger storms
    reaching as high as 1.5 inches/hour. This has been realized over
    much of the DFW metroplex already where cell-training overnight
    has yielded rainfall totals of as much as 2 to 5 inches.

    As shortwave energy ejects off to the northeast across the
    Arklatex region this morning, the overall axis of stronger warm
    air advection and moisture transport should also translate off to
    the northeast. This will help to maintain locally heavy showers
    and thunderstorms along an axis that will still tend to linger
    over northeast TX and southeast OK, but should move well
    downstream into areas of western and central AR going through the
    morning hours.

    Given the locally heavy rainfall rates and periodic cell-training
    concerns, additional rainfall totals of as much as 2 to 4 inches
    are expected which is also supported by the 00Z HREF guidance and
    recent HRRR runs. Some of these rains will be falling over areas
    that have already seen locally heavy rainfall overnight, so
    additional areas of flash flooding will generally be likely this
    morning and especially over the more urbanized areas.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ZQehYyNkVq3vDFLKDg74s0Azc8Jcq8SamPVbRiiYZI4a181TMTI4Rg1VcBklN6Hxhh9= u-kRalLjnzNhSWDyCxIcasw$ for graphic product...

    ATTN...WFO...FWD...LZK...MEG...OUN...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 36009200 35839128 35319103 34489198 33439396=20
    32349544 31579663 31269764 31619826 32429817=20
    33229756 34439598 35469410 35849292=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jan 30 15:34:56 2025
    AWUS01 KWNH 301534
    FFGMPD
    TNZ000-KYZ000-ILZ000-MSZ000-MOZ000-ARZ000-TXZ000-OKZ000-302130-

    Mesoscale Precipitation Discussion 0008
    NWS Weather Prediction Center College Park MD
    1033 AM EST Thu Jan 30 2025

    Areas affected...ArkLaTex into mid-MS Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 301532Z - 302130Z

    SUMMARY...Areas of flash flooding appear likely to continue from
    portions of the ArkLaTex into the mid-MS Valley through 21Z. Flash
    flood coverage is expected to be scattered with peak rainfall
    rates of 1-2 in/hr and additional totals of 2-4 inches are likely
    over the next 6 hours.

    DISCUSSION...Widespread areas of moderate to heavy rainfall were
    ongoing as of 15Z across northeastern TX into central AR and the
    MO Bootheel. While peak rainfall rates over the past few hours
    have dropped below 1 in/hr, the steady rainfall over the region
    since just before midnight has resulted in 3 to 5 inches of
    observed rainfall from northeastern TX into the Ouachita Mountains
    and the I-40 corridor. A strong low level jet was present from the
    ArkLaTex into western AR with VAD wind plot observed speeds of
    50-60 kt. Low level warm air advection to the north of a surface
    warm front (which extended W to E across southern AR) was focusing
    repeating rounds of moderate to heavy rain from SW to NE along an
    elevated convergence axis which was located between 925-850 mb
    from northeastern TX into the northwestern half of AR.

    While elevated instability to the north of the warm front was, and
    is expected to remain, weak (<500 J/kg) through the early
    afternoon, steady rain with rates occasionally peaking above 1
    in/hr should maintain areas of flash flooding from portions of the
    ArkLaTex into the mid-MS Valley over the next 3-6 hours. As a
    powerful closed low over the southern/central High Plains
    continues to slowly advance eastward during the afternoon, the low
    level jet is forecast to maintain its intensity while gradually
    translating eastward. Diffluent flow aloft and the slow moving to
    nearly stationary elevated axis of convergence will continue to
    allow for repeating rounds of heavy rain with occasional rates of
    1+ in/hr (but less than 2 in/hr) where pockets of relatively
    higher instability coincide with training echoes of heavy rain.
    Additional rainfall of 2-4 inches can be expected from portions of
    southwestern AR into northeastern AR and the adjacent MS Valley.
    Due to fairly low flash flood guidance values, flash flooding is
    considered likely.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6pDT3mKLeC3Lx-xR0A--qt9EQ6LYvz1vztxsgzxRgcoq9N1K6r0u4rlXBtPHZyUI6B5P= efYtnkAJhPWWh_oplYOSad0$ for graphic product...

    ATTN...WFO...FWD...LSX...LZK...MEG...OHX...PAH...SGF...SHV...
    TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...OHRFC...NWC...

    LAT...LON 37388967 37298861 37068807 36648778 36248786=20
    35598849 34619099 33649280 33179405 33249540=20
    34009560 35969379 37079202=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jan 30 22:03:34 2025
    AWUS01 KWNH 302203
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-310200-

    Mesoscale Precipitation Discussion 0009
    NWS Weather Prediction Center College Park MD
    502 PM EST Thu Jan 30 2025

    Areas affected...mid-MS Valley into lower/middle OH Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 302200Z - 310200Z

    SUMMARY...Areas of moderate to heavy rain will maintain a flash
    flood threat from northeastern AR/southeastern MO into the lower
    and middle OH Valleys and much of western and central KY through
    at least 02Z. Hourly rainfall of 0.5 to 1.0 inches will be
    possible along with 3 hourly rainfall up to 2 inches.

    DISCUSSION...A broad area of moderate to heavy rainfall extended
    from near the MO Bootheel into the lower OH Valley as of 2130Z.
    This area of rainfall has been translating northeastward during
    the day and has been responsible for peak hourly rainfall up to
    about 1 inch from the eastern AR/MO border into western KY and
    northwestern TN since ~18Z. While hourly rainfall totals have not
    been too high given MUCAPE has largely remained below 500 J/kg,
    3-hour rainfall totals of 2 to 3+ inches have resulted in numerous
    reports of flooding and flash flooding from southwestern to
    northeastern AR.

    The heaviest rainfall has been occurring at the nose of a 50-60 kt
    low level jet measured between 925-850 mb, which has been
    overrunning a surface warm front lifting north across AR and
    northern MS. The axis of greatest low level moisture transport is
    likely to continue to slowly shift east into KY/TN over the next
    few hours with an elevated convergence axis aloft focusing from
    near the MO Bootheel into the lower OH Valley. The orientation of
    this low level convergence axis will be parallel to the mean
    steering flow, allowing for repeating rounds of moderate to heavy
    rain.

    While instability is likely to remain limited into the late
    evening/early overnight hours, forcing will remain strong in the
    form of low level warm air advection and convergence beneath a
    strengthening area of upper level divergence located within the
    right-entrance region of a 150-160 kt upper level jet max centered
    over OH/PA/NY. Peak hourly rainfall of 0.5 to 1.0 inches and
    3-hourly rainfall of 1-2 inches may result in additional flash
    flood concerns across downstream locations along the OH Valley as
    these rains fall on top of locations that have already picked up 2
    to 3+ inches of rain since this morning. Embedded within this
    threat could be an isolated spot or two with higher end
    runoff/flooding depending on local hydrologic conditions.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_WfeXhkUoEcRdU2jQCUfJEVb89Eaqg1ZGQYuJA1_DpAdmS-upWdTLbPLYGO5d1LDBdZx= HPDxtoLrEc-3uVEsyc_L5_A$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...JKL...LMK...LSX...LZK...MEG...
    OHX...PAH...

    ATTN...RFC...LMRFC...NCRFC...OHRFC...NWC...

    LAT...LON 38848597 38598485 38008385 37228401 36768481=20
    36528671 36118840 35438943 35109024 35369091=20
    36259103 37329028 38618767=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jan 31 02:03:28 2025
    AWUS01 KWNH 310202
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MSZ000-MOZ000-ARZ000-310600-

    Mesoscale Precipitation Discussion 0010
    NWS Weather Prediction Center College Park MD
    901 PM EST Thu Jan 30 2025

    Areas affected...Portions of Kentucky and Tennessee

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 310200Z - 310600Z

    SUMMARY...Areas of moderate to heavy rain will maintain a flash
    flood threat across portions of the lower and middle OH Valleys
    and much of KY through at least 06Z. Hourly rainfall of 0.5 to 1.0
    inches will be possible along with 3 hourly rainfall up to 2
    inches.

    DISCUSSION...A broad area of moderate to heavy rainfall extended
    along and east of the Mississippi River into the Ohio and
    Tennessee Valley as of 0145Z. This area of rainfall has been
    translating northeastward during the afternoon and early evening
    and has been responsible for peak hourly rainfall up to about 0.75
    inch in eastern AR/MO border into western KY. MUCAPE has largely
    remained below 500 J/kg but that was enough to support 3-hour
    rainfall totals of 1.5 to 3 inches earlier.

    The heaviest rainfall has been occurring at the nose of a 50-60 kt
    low level jet measured between 925-850 mb, which has been
    overrunning a surface warm front lifting north across northeast
    Arkansas and far southern Tennessee at 00Z. The axis of greatest
    low level moisture transport is likely to continue to slowly shift
    east into KY/TN through late evening with an elevated convergence
    axis aloft focusing activity into the western lower OH Valley. The
    orientation of this low level convergence axis will be parallel to
    the mean steering flow, allowing for repeating rounds of moderate
    to heavy rain.

    While instability is likely to remain limited into the late
    evening/early overnight hours, forcing will remain strong in the
    form of low level warm air advection and convergence beneath a
    strengthening area of upper level divergence located within the
    right-entrance region of a 135-150 kt upper level jet max centered
    over OH/PA/NY from 00Z soundings. Peak hourly rainfall of 0.5 to
    1.0 inches and 3-hourly rainfall of 1-2 inches may result in
    additional flash flood concerns across downstream locations along
    the OH Valley...with the greatest concern for excessive rainfall
    at locations where these rains fall on top of locations that have
    already picked up 2 to 3+ inches of rain since this morning.
    Embedded within this threat could be an isolated spot or two with
    higher end runoff/flooding depending on local hydrologic
    conditions.

    Bann

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6AZrqa0rA0VEncquGN1STgxmYga5xVTkj-dm30YilLetOxvMSuYZwHR0OkwE17w4VfiI= Yziu9BoDUX_K83OjKn28WP0$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...MEG...OHX...PAH...RLX...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 38658585 38458319 37408284 36798460 35488777=20
    34838867 34818982 35518999 37188904 38108772=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Feb 1 19:17:41 2025
    AWUS01 KWNH 011917
    FFGMPD
    CAZ000-020700-

    Mesoscale Precipitation Discussion 0011
    NWS Weather Prediction Center College Park MD
    217 PM EST Sat Feb 01 2025

    Areas affected...central to northern California

    Concerning...Heavy rainfall

    Valid 011915Z - 020700Z

    SUMMARY...Heavy rain will develop across north-central CA this
    afternoon and especially tonight. Rainfall will be steady but with
    hourly totals increasing to over 0.5 inches, especially for the
    northern Sierra Nevada tonight. 12 hour totals of 3 to 6+ inches
    can be expected for the northern Sierra Nevada with 1 to 3 inches
    for the Coastal Ranges.

    DISCUSSION...A big picture view of Blended Total Precipitable
    Water (PW) and MIMIC Total PW showed a southwest to northeast
    oriented axis of PW values in excess of 1.5 inches streaming
    across HI to about 36N, and extending east to about 127W,
    weakening with eastward extent to the West Coast. Land-based GPS
    data from 18Z showed that PW values of greater than 1 inch
    extended from northern Mendocino County to Santa Barbara County
    with a max near 1.25 inches centered around San Francisco Bay and
    eastward into the lower Sacramento River Valley. The values within
    the core of the moisture axis are well over 200 percent of normal
    via the blended imagery.

    Placement of a low ot mid-level low over British Columbia and
    ridge centered about 600 miles west of the northern Baja Peninsula
    has allowed for a funneling of these anomalous moisture values
    into the CA coast. A powerful (191 kt at 250mb via 12Z SLE
    sounding) zonally oriented upper level jet was sandwiched between
    the low to the north and high to the south, with no significant
    movement of these two features forecast through early tonight.
    Recent GFS, RAP and other guidance are good agreement with the
    arrival of a corridor of stronger 850 mb winds (40-50 kt) arriving
    into Sonoma and Marin counties over the next 1-2 hours, oriented
    perpendicular to the coastline along and just south of a east-west
    oriented quasi-stationary front extending offshore of the central
    CA coast. Some backing of low level flow toward the southwest is
    expected across the Valley into the foothills of the Sierra
    Nevada. With the increase in low level flow and a subtle increase
    in PW values (up to ~1.4 inches), IVT magnitude is expected to
    peak between 800-900 kg/m/s from just north of San Francisco Bay
    into the southern Sacramento Valley in the 21Z-02Z time frame. The
    surge will be short-lived however and poor low and mid level lapse
    rates should limit instability to near zero for coastal and inland
    locations through the first half of tonight with rainfall
    intensity largely driven by wind speed and orographic lift.

    Steady light to moderate rain was ongoing across the coast and
    Sierra Nevada of north-central CA as of 18Z but should increase in
    magnitude over the next 6 hours, especially into the upslope
    regions of the Sierra Nevada where orographic ascent will be
    maximized given 700 mb winds peaking in the 70-80 kt range just
    after 00Z. 12 hour rainfall totals of 1 to 3 inches are expected
    for the Coastal Ranges from just north of San Francisco Bay to
    just south of 40N and 3 to 6+ inches for the Sierra Nevada from
    roughly Amador to Butte counties. While rainfall through 07Z is
    not expected to produce impacts from flooding, heavy rain will
    continue through the night with potential for flooding and higher
    rain rates to increase prior to 12Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5dIiGAeulu1rxK0zydcPEuCyMtNZXnx8os26hae-z-rkAXFPgV4aUFw3fciXn_7RGhfq= v6P58ylRb53IJTNahh-6NHU$ for graphic product...

    ATTN...WFO...EKA...HNX...MTR...REV...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 40442163 40302137 40112102 39882047 39442017=20
    38772012 38181972 37901960 37541946 37371955=20
    37521991 37722010 38022037 38332090 38262158=20
    37982207 37892261 37972305 38372341 38722374=20
    39002387 39362397 39652383 40062346 40262297=20
    40412231=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Feb 2 07:01:41 2025
    AWUS01 KWNH 020701
    FFGMPD
    NVZ000-CAZ000-021900-

    Mesoscale Precipitation Discussion 0012
    NWS Weather Prediction Center College Park MD
    200 AM EST Sun Feb 02 2025

    Areas affected...Northern California

    Concerning...Heavy rainfall

    Valid 020700Z - 021900Z

    SUMMARY...An atmospheric river aimed at northern California will
    continue to produce heavy rain with rates between 1/4 and 3/4
    inches per hour possible.

    DISCUSSION...An atmospheric river aimed at northern California
    will continue to advect tropical moisture from near Hawaii
    northeastward into the state today. The moisture has a tropical
    connection due to an expansive area of high pressure located off
    southern California joining forces with a cold core low off
    Vancouver Island to squeeze the moisture into a relatively narrow
    corridor (atmospheric river). PWATs between 1 and 1.25 inches are
    associated with the moisture plume. This is 4 sigma above the
    climatological normal as well as within the 90th to 95th
    percentile compared to a 30-year average of PWATs for the area.
    IVT values from CW3E GFS and EC guidance are around 800 kg/ms.
    Over the past 24 hours, Anywhere from 1 to 4 inches of rain have
    fallen across northern California, with the highest values in the
    Sierras around and west of the Lake Tahoe region. NASA Sport soil
    moisture imagery shows much of the surface soil layer has
    saturated significantly compared to 24 hours ago, so most of the
    rain that falls from here should convert to runoff.

    Radar imagery shows a plume of rainfall occurring over much of far
    northern California with rates generally between 1/10 and 1/4 inch
    per hour ongoing. These rates are confirmed by the numerous
    weather stations set up across northern California. A stationary
    front draped over northern California (not shown) delineates the
    remarkable surface convergence occurring within this atmospheric
    river, with winds off the coast of Crescent City 20 kts out of the
    north, and winds both off the coast of Mendocino as well as up the
    northern Sacramento Valley are 20 kts out of the south. This
    remarkable convergence is adding to the overall lift within the
    atmosphere along the front, with almost all of the rain occurring
    north of the front.

    As a potent upper level shortwave approaches the coast over the
    next 12 hours, HiRes models are in good agreement as to a slight
    increase in rainfall rates in far northern California over the
    next 4 hours or so, followed by a gradual southward drift of the
    rainfall plume towards Point Arena and the northern Sacramento
    Valley. Rainfall rates may locally increase to as high as 3/4
    inches per hour. Along the coast, rates should diminish through
    the predawn hours, with the rainfall tapering from north to south
    through the morning. Expect 3-6 inches of rain for much of the
    northern Sierras through 19Z, 2-4 inches of rain for the northern
    Coastal Ranges, and lesser amounts within the Sacramento Valley
    along the I-5 corridor and to the immediate lee (east) of the
    coastal ranges.

    Mudslides and rock slides are possible in the foothills and
    mountains below 6,500 feet where the precipitation remains all
    rain. Localized flooding is possible in the areas where the
    heaviest rain occurs over flood-sensitive and low-lying areas.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5Y4MMwOjNyUN8M1ASjGdGoHdQd6EJBF4AQTmwo1AvwSuAu3qu99oohaY-xe_RHQ_mUMv= 9zgJEkNuqis28DNtP29-2pg$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...REV...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 41902181 41862023 41252007 39932011 39391980=20
    38501957 38312007 38352115 39352158 40282212=20
    40012270 39472270 38732243 38352235 38622251=20
    38122328 38932398 39432394 40012417 40472452=20
    40982421 41562316=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Feb 2 19:37:00 2025
    AWUS01 KWNH 021936
    FFGMPD
    CAZ000-030700-

    Mesoscale Precipitation Discussion 0013
    NWS Weather Prediction Center College Park MD
    236 PM EST Sun Feb 02 2025

    Areas affected...northern California

    Concerning...Heavy rainfall

    Valid 021935Z - 030700Z

    SUMMARY...Moderate to Heavy rain will continue over the northern
    Sierra Nevada throughout the next 6-12 hours while a second round
    of moderate to locally heavy rain develops for the northern
    Coastal Ranges this evening. While locally higher totals will be
    possible on an isolated basis, additional rainfall totals of 3 to
    5 inches are expected for the northern Sierra Nevada into the
    southern Cascades and an additional 1 to 2 inches for the northern
    Coastal Ranges through 07Z.

    DISCUSSION...Eastern Pacific view of total precipitable water (PW)
    showed a relatively narrow axis of values greater than 1 inch
    extending from near the triple point of an occluded cyclone 36N
    138W (which showed up well in visible satellite imagery), ENE to
    the northern CA coast. Gauge observations have shown peak hourly
    rainfall totals in the 18Z hour of 0.1 to 0.2 inches for the
    northern Coastal Ranges and 0.25 to locally in excess of 0.5 in/hr
    for the northern Sierra Nevada. 24 hour totals near 9 inches have
    been reported just east of Chico in the Sierra Nevada with up to
    roughly 4 inches for the northern Coastal Ranges. Reports of
    flooding thus far have been limited and primarily focused across
    southern portions of the region on either side of I-80 in the
    Sierra Nevada and between San Pablo Bay and Santa Rosa via local
    storm reports.

    Confluent mid-level flow between a mid-level low over southwestern
    Canada and a low amplitude longwave trough centered near 145W
    along with a ridge over the Baja Peninsula will keep zonal flow
    focused from the northern CA and OR coastline, eastward into the
    central U.S. through the overnight. At the surface, a shallow but
    well-defined stationary front, co-located with the moisture axis,
    will essentially remain in the same place over the next 6-12 hours
    (slow northward drift), with low level winds varying within the
    plume between 40-50 kt in the 850-700 mb layer. Some subtle
    strengthening of 850 mb winds will be possible toward 00Z ahead of
    the leading edge of a weak mid-level shortwave expected to near
    the West Coast at 00Z, but IVT values are forecast to remain in
    the 400-600 kg/m/s range through 06Z Monday across northern CA.

    No significant changes to peak rainfall rates are expected for
    northern CA through 06Z, but additional light to moderate rainfall
    (perhaps locally heavy) is expected into the northern Coastal
    Ranges later this evening with the approach of the offshore
    mid-level impulse. Additional peak rainfall totals of 1-2 inches
    for the Coastal Ranges and 3-5 inches for the northern Sierra
    Nevada are likely over the next 12 hours but given rainfall rates
    will remain somewhat modest, it is the long duration of this
    rainfall event that will be noteworthy. At least through 06Z
    tonight, additional flooding impacts are expected to remain
    isolated with rainfall rates remaining under more critical
    thresholds.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4n3AZcPfTSdqmNWbK_ffJ6tUgbACVgJ7QSgoq4mOymxc8QfMd6TnHX7t1gN3EeZjfQhd= wbRivGG_nTd2zxNA-mPbQZ4$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...REV...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 41932111 41782055 41352037 41122043 40772058=20
    40382047 39872026 39282015 38942034 38772068=20
    38712095 38892118 39192143 39482163 39782182=20
    40032213 40082244 39972271 39512264 39282247=20
    38962222 38592215 38302216 38122234 38132269=20
    38222311 38502358 38832386 39182406 39592417=20
    40192451 40602421 40832377 40892338 40932300=20
    41122267 41302234 41712170=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Feb 2 23:04:29 2025
    AWUS01 KWNH 022304
    FFGMPD
    CAZ000-030200-

    Mesoscale Precipitation Discussion 0014
    NWS Weather Prediction Center College Park MD
    603 PM EST Sun Feb 02 2025

    Areas affected...Shasta County / northern CA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 022302Z - 030200Z

    SUMMARY...A narrow and focused band of heavy rain is expected to
    result in a localized area of flash flooding for portions of
    Shasta County in and around the Redding metro area. Peak hourly
    rainfall of 1-2 inches will be possible with localized additional
    totals of 3-5 inches through 02Z.

    DISCUSSION...Local radar imagery from KBBX at 2240Z showed a
    narrow band (just 2-4 miles wide) of stationary heavy rain
    occurring just south of downtown Redding, CA. This band has been
    present for the past 2 to 3 hours and has resulted in 4 to 6
    inches of rain, most of which has occurred since 20Z. These
    rainfall reports have been sourced from a number of
    Wunderground.com observations with the band just recently shifting
    south to Redding Regional Airport.

    The band of heavy rain was located along an axis of strong
    surface/near-surface convergence co-located with a
    quasi-stationary front that extended SW to NE across the northern
    Sacramento Valley. Weak instability may be present with RAP
    estimates of near 100 J/kg. Little change to the pattern on the
    regional scale is expected to keep the quasi-stationary front in
    roughly the same position over the next few hours though some
    minor wavering of the rainfall axis is expected over the next
    couple of hours along with possible weakening of the little
    instability that could be in place. Given the presence of this
    band of heavy rain across the I-5 corridor near Redding and into
    the higher terrain of eastern Shasta County, a localized area of
    flash flooding appears likely with this band. Due to the highly
    mesoscale nature of this feature, confidence is below average in
    its longevity but it seems likely to persist for at least another
    1-2 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4FAue9RTzh4i5PUpyW3cLxsADkEMcSbETXUz06rF_bbTk_yK60JiUQSPa9-OGZO58C4g= VO04DZVPTarVWNVVISBa5BE$ for graphic product...

    ATTN...WFO...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 41082185 40972166 40772163 40642187 40262256=20
    40462268 40972208=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Feb 3 02:14:14 2025
    AWUS01 KWNH 030213
    FFGMPD
    CAZ000-030700-

    Mesoscale Precipitation Discussion 0015
    NWS Weather Prediction Center College Park MD
    913 PM EST Sun Feb 02 2025

    Areas affected...Redding Area of Shasta County

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 030212Z - 030700Z

    SUMMARY...Heavy rain associated with a convergence band over
    Shasta County, CA will continue into tonight. Flash flooding will
    be possible in addition to the ongoing areal flooding.

    DISCUSSION...An impressive WSW-ENE convergence band that set up at
    the head of the Sacramento Valley near Redding and Anderson, CA
    continues to be the source of heavy rain this evening. A strong
    southerly low level jet (LLJ) with winds of over 40 kts at 850 mb
    continues along the Sacramento Valley, with surface stations south
    of the band reporting winds as high as 20 kts south of the band.
    The band had been nearly stationary over Anderson, CA or just
    south of Redding, but trends have been for the band to crawl
    northward with time. Guidance shows very little if any
    instability, so this band is likely being forced by the strong
    convergence in the area from the combination of the strong
    southerly flow with the LLJ hitting a stationary front in that
    same area, as well as localized upslope as the terrain of the
    Sacramento Valley forms an arc, or upside down U, allowing for
    southerly flow to become focused and converge in the Redding area.
    Surface observations show there has been over 1.7 inches of rain
    in the last 3 hours, and 2.5 inches of rain in the last 6.

    HiRes guidance is in good agreement that the front and convergence
    band will remain in place for at least the next several hours, if
    not throughout the overnight (HRRR). With rates as high as an inch
    per hour possible, expect continued areal flooding and possible
    flash flooding in those areas where the convergence band interacts
    with the terrain to focus the rain water into narrow streams,
    creeks, and channels. Urban areas in and around Redding may also
    locally increase the flash flooding threat.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9eS4LoJC5rkLYwpzCDlGSmDkq3NN8Fuul9JOKPgas3J0LLhDLgP0FQpPCjCFg8iwYp73= zgSNm_NPyE4BnVj4BcMxRqs$ for graphic product...

    ATTN...WFO...EKA...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 40792205 40692191 40492197 40422224 40402259=20
    40332288 40452290 40542276 40662255 40742235=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Feb 3 07:03:14 2025
    AWUS01 KWNH 030703
    FFGMPD
    CAZ000-031900-

    Mesoscale Precipitation Discussion 0016
    NWS Weather Prediction Center College Park MD
    202 AM EST Mon Feb 03 2025

    Areas affected...Northern California

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 030702Z - 031900Z

    SUMMARY...Steady rain will continue into northern California today
    with localized convergence bands of heavy rain embedded within the
    broader atmospheric river. Localized rates over 1 inch per hour
    and flash flooding possible.


    DISCUSSION...Heavy rain associated with the ongoing atmospheric
    river will continue through the day today. Just in the past 24
    hours, rainfall amounts locally exceeding 6 inches have fallen
    around and just south of the Redding area. This caused flooding in
    several areas as noted by the local storm reports. For now the
    band that caused that flooding around Redding has diminished in
    intensity. However, many of the ingredients that led to the band's
    formation remain in place. A stationary front remains in the area
    acting as a convergence boundary between the colder air to its
    north and the warmer air and southerly flow to its south. A
    southerly low level jet from 850 to the surface remains strong
    moving up the Sacramento Valley, with winds to 40 kts at 850 and
    20 kts as noted by several stations in the Sacramento Valley south
    of the area of rain. This low level jet and the orientation of the
    terrain are locally enhancing convergence at the northern end of
    the Sacramento Valley around Redding, as noted by localized
    increased in the radar reflectivities around that area. Meanwhile,
    plumes of moisture continue to move into the northern California
    coast, where their initial uplift by the northern coastal ranges
    are also responsible for heavier rains.

    The jet stream remains largely zonal extending hundreds of miles
    west out into the Pacific. The upper low to the north and the high
    to the south continue to put the squeeze on the moisture plume,
    increasing upper level winds and narrowing the moisture into a
    100-200 mile wide corridor that is the atmospheric river. During
    the day today, the upper low helping direct the jet stream will
    retrograde west. This will begin to reorient the atmospheric river
    from its current westerly flow to a southwesterly flow. This will
    allow the atmospheric river to begin to drift southward down the
    coast, while remaining in place over much of interior northern
    California. This reorientation may also work to support the low
    level jet, as the wind flow becomes more parallel with the
    mountains.

    HiRes guidance is in agreement that rainfall rates should remain
    largely steady through the early morning, though again embedded
    heavier bands remain very possible, especially at the northern end
    of the Sacramento Valley. Where any bands form, localized flash
    flooding in addition to the ongoing areal flooding cannot be ruled
    out. A subtle surface low will approach the coast around 18Z,
    likely enhancing the rainfall rates area-wide from west to east
    and could cause additional flooding into the afternoon. Expect
    another 2-4 inches of rain into the northern Sacramento Valley
    through 19Z with 1-3 inches of rain expected elsewhere in the
    highlighted area.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7nIjQKs2tSVxxpcQYGLU-voXabZlkuB003nbt11vwnS7sz9ePTpazwWKCbA1blSCz4CG= gVYQhD9XiSdz8mYMgIlR4qQ$ for graphic product...

    ATTN...WFO...EKA...MFR...REV...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 41912071 41622024 41282032 40912043 40342055=20
    39872043 39302035 39182094 39862145 40172184=20
    40302233 39802263 39442263 39162262 38912281=20
    38832334 38902386 39432391 39712388 40082424=20
    40392454 40732441 41102419 41622357 41882317=20
    41852176=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Feb 3 17:58:07 2025
    AWUS01 KWNH 031757
    FFGMPD
    CAZ000-040600-

    Mesoscale Precipitation Discussion 0017
    NWS Weather Prediction Center College Park MD
    1256 PM EST Mon Feb 03 2025

    Areas affected...Northern California & San Francisco Bay Area...

    Concerning...Heavy rainfall

    Valid 031800Z - 040600Z

    SUMMARY...AR continues though orientation will become more NE-SW
    with time as weak height-falls and shortwave press slow moving
    cold front southwest toward the Redwood Coast of California and
    increasing rainfall potential with some embedded convective
    elements possible with hourly rates of .33-.5".

    DISCUSSION...18z surface analysis depicts an atypically well
    defined surface front across NW NV into the northern portions of
    the CA Sierra Nevada into the southern slopes of the Trinity
    mountain and toward a weak surface wave near Cape Mendocino.=20
    Strong southerly veering to southwesterly flow through the
    northern Valley continues to intersect and ascend with moderate
    moisture into the upper 40s/lower 50s in Tds. Cold air into SW OR
    allows for a fairly steep isentropic ascent pattern to maintain
    light to moderate rainfall across the rim of mountains across the
    northern Valley with snow levels still above most but the highest
    peaks of the terrain. As such, prolonged .15-.25"/hr rates are
    likely to continue for a few more hours before the orientation of
    the AR/plume changes with the advance of the front; generally with
    a fulcrum/pivot point of the plume centered in N CA near
    Shasta/Siskyou county line.

    GOES-W IR and WV suite show a defined shortwave comma
    east-southeast of the 40N130W benchmark continuing to advance
    rapidly northeast under the influence of the rapidly exiting 150kt
    jet streak and associated right entrance region. As the
    ascent/shortwave-ridge pattern passes with this entrance region,
    influence of surface to 850mb northwesterly flow will allow for
    eastward progression of the well defined frontal zone. CIRA LPW
    sfc-850mb layer shows the stark moisture difference across the
    boundary with solid .5" over-topped by .25-.3" at 850-700mb and
    further solid core of subtropical moisture already at 700-500mb along/downstream of the shearing shortwave to further increase
    total moisture to over 1" nearing 1.25" intersecting the Redwood
    Coast southeast of Cape Mendocino. The shortwave is expected to
    further elongate/shear while reaching the NW CA coast by 00-02z
    period and the associated cold front intersection with the coast
    will drop southeastward. Forty-five to 60 degrees of sfc-850
    25-35kt confluent flow will support IVT to increase slowly from
    300-400 to 400-600 kg/m/s as the core of deepest moisture overlaps
    after 00-06z. Some mid-level CAA may support very weak vertical
    development given 50-150 J/kg possible; though driving mechanism
    is likely to be more low level convergence and orographic ascent
    across the Coastal Range. Typical .25-.33"/hr may occasionally
    increase to .5"/hr across S Mendocino county into Sonoma county
    after 00z. Scattered showers may extend into the Bay and Santa
    Cruz mountains late in the period (03-06z), though rates are not
    likely to be sizable for any flash flooding with exception of most
    susceptible urban locations.

    ...Northern Valley/Lower Slopes of Sierra Nevada...
    Southerly flow will veer to more southwesterly and increase
    orographic ascent toward perpendicular as the shortwave/DPVA
    crosses the region after 00z. Solid remaining moisture in the
    valley will ascent and present solid potential for .25-.5"/hr
    rates resulting in spotty totals of 2-2.5" by 06z. Given recent
    heavy rainfall and increased upper soil saturation increased
    run-off will occur resulting in areal expansion of increased
    riverine stream flows.

    All locales and rates are likely to be below critical values for
    any flashy style flooding and so will keep the tag on this
    discussion at Heavy Rainfall but will continue to monitor for any
    highly localized issues that may unfold.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5NT9hdA1JDhaj4Y1NVc-AQ5Osz_eKHK8Hq3u18ZgRFhg6FFoR-LJP0Siff8Lgcpr-N_u= S4j1gv4W9wxECn3Yf4sNI44$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 41412218 41392159 41082138 40842145 40682170=20
    40402166 40062151 39822115 39602081 39192055=20
    38772036 38372059 38532160 38292196 37802207=20
    37182183 36892198 36952237 37972305 38442344=20
    38962384 39722393 40052434 40502446 40972405=20
    40732365 40942346 40832288 41112243=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Feb 4 05:57:39 2025
    AWUS01 KWNH 040556
    FFGMPD
    NVZ000-CAZ000-041800-

    Mesoscale Precipitation Discussion 0018
    NWS Weather Prediction Center College Park MD
    1256 AM EST Tue Feb 04 2025

    Areas affected...Central and Northern California

    Concerning...Heavy rainfall

    Valid 040600Z - 041800Z

    SUMMARY...Heavy rain associated with the ongoing atmospheric river
    may locally reach rates to 1 inch per hour with any convective
    banding and heavier showers through mid-morning.

    DISCUSSION...The primary AR has shifted into the Bay Area and
    northeast through Sacramento this evening. For most areas, the
    rain is generally light to moderate, producing 1/10 to 1/4 inch
    per hour rates. The higher 1/4 inch per hour rates are largely on
    the windward (southwest-facing) sides of the coastal ranges and
    the Sierras. Onshore flow to 40 kt at 850 continues into the Bay
    area. Upon moving inland the flow shifts to southerly as it tracks
    along the foothills of the Sierras up the Sacramento Valley. This
    low level jet has been the primary driver of the moisture
    advection producing locally heavier rains in the form of
    convergent bands and enhanced upslope rainfall activity over the
    past few days. Since the LLJ isn't going anywhere, these local
    "flare-ups" of heavier rain will continue through the overnight
    and into Tuesday morning.

    The band is expected to shift south of the I-80 corridor by around
    10Z/2am PST based on all of the latest HiRes guidance. This will
    leave the I-80 corridor from San Francisco through Sacramento in
    off-and-on shower activity. The band will taper a bit as it stalls
    out generally from a Monterey to Modesto line through the rest of
    the overnight and into Tuesday morning. For far northern
    California, the area is in a much needed break right now in most
    areas, though very light rain and higher elevation snow continues
    north of Redding. This break in the rain will continue through at
    least sunrise as noted by the relative lack of higher cloud cover
    off the coast of California on the graphic.

    The next low is following swiftly behind this latest round.
    Guidance has shifted significantly northward in the latest runs.
    Thus, now expect another round of heavy rain to impact much of the
    Sacramento Valley, including the hard-hit Redding area. This
    heavier rain will arrive with the next low around 15Z/7am PST. IVT
    values with the low will increase to around 750 kg/ms according to
    CW3E interpolations of the GFS along the coast. The low will be
    supported by a quickly-advancing zonal jet stream moving in from
    the Pacific, so northern California will be in the left exit
    region of that jet. The surface low will thus be supported by
    favorable upper level dynamics. The heavy rain will be further
    supported by the strengthening LLJ in the Sacramento Valley, which
    will intensify in response to the approaching low and increasing
    pressure gradient. It's likely that any 1 inch per hour rates with
    any convergent bands will occur from mid-morning on due to the
    additional moisture and advection.

    Any resultant flooding from the heavy rain will likely be confined
    to urban areas and flood-prone streams and creeks.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!59G7LOfcoquUdQ5I44TLMUtD7kBqieQZlczqOHpWckco43BIlk7w5Dc1x577hsedxg-G= epVnUC0EIUZOlvbjghhm55A$ for graphic product...

    ATTN...WFO...EKA...HNX...MFR...MTR...REV...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 41642113 41392063 40972019 40202000 39102000=20
    38591974 38091969 37492045 37112124 36902191=20
    36992236 37492259 37812264 37972309 38182304=20
    38992387 39512390 39902398 39952396 40322377=20
    40672325 41062280 41582213=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Feb 4 18:13:43 2025
    AWUS01 KWNH 041813
    FFGMPD
    CAZ000-050600-

    Mesoscale Precipitation Discussion 0019
    NWS Weather Prediction Center College Park MD
    111 PM EST Tue Feb 04 2025

    Areas affected...Northern and Central California

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041800Z - 050600Z

    Summary...Localized flash flooding is possible with additional
    1-3"+ rainfall totals through 06z. Localities most likely to
    realize isolated flash flooding from additional 3-5" totals are
    along the northern foothills of the Sierras and the Santa Lucia
    Range.

    Discussion...Another round of moderate to heavy precipitation is
    underway across portions of northern and central CA, driven by a
    mid-level vort max leading an anomalous shortwave trough pivoting
    into the Pacific Northwest (along with synoptic uplift provided by
    upper-level divergence via the left exit region of a 130+ kt jet
    streak). The 12z HREF indicates an additional 1-3"+ of QPF through
    06z, with localities along the northern foothills of the Sierras
    and the Santa Lucia Range most at risk of localized flash flooding
    (with the highest chances for 0.5"+/hr rates and additional totals
    of 3-5", per the 12z HREF 40-km neighborhood probabilities for
    0.5" exceedance and ensemble agreement scale 0-100 km of 3.0"
    exceedance, respectively). The HRRR has also been among some of
    the wettest guidance, suggesting banded rainfall capable of
    0.5-1.0"/hr rainfall rates extending into the lower elevations of
    coastal regions (such as Santa Rosa and San Francisco). This seems
    plausible, given the location of the surface boundary and the
    uptick in low-level moisture flux convergence already underway per
    SPC RAP analysis (along with the favorable synoptic environment
    and total precipitable water values of 1.2"+ near the max moving
    average, per OAK sounding climatology). Please consult local NWS
    products for up-to-date information on flood hazards.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-3MqJeUTsCEduFm2c40d3KhB_DpG4USTTrHVrqWRBE724la5up9LZmQrMY6CbeVvHZIQ= fGwsoLslMkDywPsQgzK1dI4$ for graphic product...

    ATTN...WFO...EKA...HNX...LOX...MFR...MTR...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 41232226 41182197 40922182 40512171 40212157=20
    39972125 39732092 39032065 38462016 37751965=20
    37391947 36991909 36571882 36321867 36041878=20
    36251903 36631941 36891963 37191985 37412019=20
    37602049 37522078 37372103 37082126 36702152=20
    36472146 36212119 35892084 35482062 35302078=20
    35362137 35772195 36402232 37162279 37802305=20
    38442338 38742315 39122321 39412339 39792365=20
    40072361 40452342 40812310 40972275 41122236=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Feb 6 05:58:01 2025
    AWUS01 KWNH 060557
    FFGMPD
    MDZ000-VAZ000-WVZ000-OHZ000-KYZ000-061154-

    Mesoscale Precipitation Discussion 0020
    NWS Weather Prediction Center College Park MD
    1256 AM EST Thu Feb 06 2025

    Areas affected...much of West Virginia, far northeastern Kentucky

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 060554Z - 061154Z

    Summary...A gradual uptick in excessive runoff potential is
    expected especially in central/eastern West Virginia through 12Z.
    Local 1-2 inch rainfall totals are expected.

    Discussion...Areas of light to moderate rainfall have developed
    across much of the discussion area since 03Z, with several
    observations of 0.5-1 inch rainfall totals noted. In addition to
    the recent rainfall, an upstream scenario is favoring repeated
    rainfall with heavier rates through 12Z, including: 1) upstream
    shortwave energy encouraging updrafts across western KY/TN, 2)
    increasing low-level flow impinging on a low-level boundary
    near/along the KY/TN border, and 3) 40-60 knot low-level flow,
    which was increasing instability/MUCAPE from west to east across
    Kentucky and vicinity. The net result of this pattern is a
    gradual increase in convective elements along a west-east axis
    from western Kentucky through the discussion area. Nearly
    continuous rainfall should occur through 12Z in most areas, with
    spots of 0.25-0.5 inch/hr rain rates and 1-2 inch rainfall totals
    expected.

    These rainfall totals should fall across areas of wet soils from
    antecedent rainfall over the past month from eastern KY into the
    central Appalachians. FFG thresholds are generally in the 1
    inch/3-hour range and are potentially lowering given ongoing
    rainfall. The regime should support a few areas of
    runoff/flooding especially across sensitive terrain in
    central/eastern West Virginia.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8u5tbUgiwIZheyNTPlzDMifhCAMlBdj6Hb5O6QBIEXw_tPWEV3CBwUTr2jl5tQFtN51T= MZwco3xcbOTNj646mYFQZLk$ for graphic product...

    ATTN...WFO...ILN...JKL...LWX...PBZ...RLX...RNK...

    ATTN...RFC...MARFC...OHRFC...NWC...

    LAT...LON 39377916 39007889 38137978 37548077 37458241=20
    37928337 38258350 38538317 38878224 39208068=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Feb 16 00:46:52 2025
    AWUS01 KWNH 160046
    FFGMPD
    OHZ000-TNZ000-KYZ000-INZ000-ILZ000-MSZ000-MOZ000-ARZ000-160645-

    Mesoscale Precipitation Discussion 0042
    NWS Weather Prediction Center College Park MD
    745 PM EST Sat Feb 15 2025

    Areas affected...Lower MS Valley into the Mid-South and OH Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 160045Z - 160645Z

    SUMMARY...Widespread flash flooding with damaging and
    life-threatening impacts will continue as showers and
    thunderstorms continue to train locally over the same area and
    focus heavy rainfall totals.

    DISCUSSION...The latest GOES-E IR satellite imagery along with
    dual-pol radar shows widespread and well-organized showers and
    thunderstorms impacting much of the Lower MS Valley with a
    northeastward extension up across portions of the Mid-South and
    the OH Valley. Strong shortwave energy is crossing the Arklatex
    and will be rapidly lifting northeastward into the OH Valley
    overnight. As it does so, the energy will be interacting with a
    moist and moderately buoyant airmass continuing to surge
    northeastward from the Lower MS Valley.

    This airmass is characterized by MUCAPE values of as much as 1000
    to 1500 J/kg and PWs approaching 1.5 inches which is also being
    aided by the persistence of a powerful 50 to 60+ kt southwest
    low-level jet. Radar imagery shows a QLCS currently evolving from
    eastern AR up across western TN and western KY with some embedded
    supercell convection. The better thermodynamics are situated from
    southeast AR through northern MS and into western TN and this
    should provide convective sustenance through the remainder of the
    evening hours as the overall QLCS activity advances off to the
    east.

    While the southern flank of the overall convective footprint this
    evening should become increasingly progressive as a cold front
    arrives from the west, there will still be notable concerns for
    training showers and thunderstorms for several more hours farther
    off to the northeast in close vicinity of a warm front lifting
    north through the OH Valley.

    Rainfall rates with the stronger storms over the next several
    hours will still be capable of reaching 1.5 to 2 inches/hour with
    the strongest of cells. Additional rainfall amounts going through
    06Z may reach as high as 2 to 4 inches with isolated heavier
    amounts not out of the question.

    Many areas have already received 2 to 4 inches of rain since early
    this morning, and the extremely sensitive ground conditions with
    saturated soils and ongoing widespread areas of flash flooding
    coupled with the additional rainfall, will pose concerns for
    potentially Flash Flood Emergency level impacts with damaging and life-threatening conditions. This situation will continue to be
    closely monitored.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-u7CK8MFFfh285T7L6vQEdWwmFqgQ4JozDgaBI4lhPBu2Yio0WTPIyifjGyhjkKWHNON= Qc75AzU5U893xOknW4FalYw$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...LZK...MEG...MRX...OHX...PAH...
    RLX...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 38918407 38398319 37498313 36788408 36358516=20
    35508719 34558970 34249121 34669174 35549119=20
    36728984 37428858 38068736 38868545=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Feb 15 17:02:22 2025
    AWUS01 KWNH 151701
    FFGMPD
    VAZ000-WVZ000-152300-

    Mesoscale Precipitation Discussion 0039
    NWS Weather Prediction Center College Park MD
    1200 PM EST Sat Feb 15 2025

    Areas affected...Central Appalachians and Portions of the VA
    Piedmont

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 151700Z - 152300Z

    SUMMARY...Heavy rainfall moving into the central Appalachians and
    adjacent areas of the VA Piedmont coupled with areas of melting
    snow will set the stage for areal flooding and possible flash
    flooding going through the afternoon hours.

    DISCUSSION...The latest radar imagery shows moderate to heavy
    rainfall along with locally some mixed precipitation that is in
    the process of changing to rain advancing east across the central
    Appalachians with southern WV and southwest VA seeing generally
    the heaviest corridor of higher rainfall rates. The rainfall is
    associated with strong warm air advection and moisture transport
    into the region which is being aided by a southwest low-level jet
    of 40 to 50 kts.

    Instability is generally non-existent, but the level of isentropic
    ascent and low-level frontogenetical forcing is quite strong and
    is supporting rainfall rates of a 0.25" to 0.50"/hour. Meanwhile,
    heavier rains are noted locally upstream over areas of central and
    eastern KY which will be advancing eastward this afternoon, and
    with an additional strengthening of the low-level jet expected
    this afternoon, somewhat heavier rates that may exceed a
    0.50"/hour will be possible over areas of southern WV down through
    southwest VA. Some very modest intrusion of elevated instability
    may arrive toward this evening that may also support a few
    thunderstorms capable of producing these heavier rates.

    The 12Z HREF guidance suggests additional rainfall amounts of as
    much as 1 to 2+ inches by early this evening. These rains coupled
    with warmer temperatures and a melting snowpack over some of the
    higher terrain, and already high streamflows, will favor an
    increasing concern for areal flooding and potentially some flash
    flooding where these heavier rainfall rates can focus and persist.
    Conditions will continue to be closely monitored over the next
    several hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9CXcnsAJgEF_8dcauc9YTCzQK2Ukg73QSPRiGtp6YqQvqygLqPd4dqwi8v6lfNypQH5a= JsyKzLS8e6_RN0Yz9pC3E8A$ for graphic product...

    ATTN...WFO...LWX...MRX...RLX...RNK...

    ATTN...RFC...LMRFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 38808007 38567930 38127898 37597888 37007910=20
    36707971 36598126 36708187 37698188 38258235=20
    38578216 38798126=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Feb 15 18:59:03 2025
    AWUS01 KWNH 151856
    FFGMPD
    TNZ000-KYZ000-ILZ000-MSZ000-MOZ000-ARZ000-160055-

    Mesoscale Precipitation Discussion 0040
    NWS Weather Prediction Center College Park MD
    155 PM EST Sat Feb 15 2025

    Areas affected...Lower MS Valley into the Mid-South and OH Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 151855Z - 160055Z

    SUMMARY...Flash flooding will become more expansive and
    significant going into the early evening hours as heavy showers
    and thunderstorms organize and train over the same area. Some of
    the flash flooding is expected to be extremely dangerous and
    life-threatening.

    DISCUSSION...Strong shortwave energy ejecting east out across the
    southern Plains will be encroaching on the Lower MS Valley this
    afternoon and will be interacting with a moist and increasingly
    unstable airmass which coupled with strengthening shear profiles
    will set the stage for expanding clusters of strong to severe
    thunderstorms. This is likely to include a combination of
    multicell and supercell convection which will be embedded within
    an environment conducive for yielding very heavy rainfall rates.

    GOES-E visible satellite imagery shows a notable increase in cloud
    street activity across LA/MS and through central and southern AR
    which is indicative of an increasingly unstable boundary layer.
    Diurnal heating via solar insolation has allowed for MLCAPE values
    to increase to 1000 to 1500 J/kg, and these values will continue
    to increase over the next few hours. A quasi-stationary front is
    draped from the Arklatex northeastward into northern MS and far
    southwest TN with multiple waves of low pressure noted along it.
    Meanwhile, a powerful southwest low-level jet is in place reaching
    upwards of 50 to 60+ kts and this is yielding very strong moisture
    transport from the Gulf of America up across the broader Lower MS
    Valley and Mid-South region with PWs that have now increased to
    1.3 to 1.5 inches.

    As thunderstorms continue to develop and organize over the next
    several hours, there will be rainfall rates capable of reaching
    1.5 to 2 inches/hour with the stronger cells. Cell-merger and
    cell-training concerns will increase by later this afternoon and
    this evening with potentially some QLCS-related training of storms
    possible in the 21Z to 00Z time frame from south-central to
    northeast AR into the MO Bootheel, northwest TN and far southwest
    KY. This is favored by a consensus of the 12Z HREF and the 16Z to
    18Z runs of the experimental WoFS guidance which shows a
    combination of multicell, supercell and QLCS-driven convection
    heading into the evening hours.

    Additional rainfall amounts of as much as 3 to 6 inches are
    expected within the corridors of greatest cell-training which
    currently is being most favored across northeast AR into the MO
    Bootheel, northwest TN and far southwest KY going through 00Z.
    Given that some of these areas already have flash flooding
    ongoing, the additional rains are likely to foster extremely
    dangerous and life-threatening flash flooding conditions by this
    evening, with Flash Flood Emergency level impacts possible. As
    conditions evolve this evening, additional MPDs will be issued to
    address this high-impact event.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5sDaEqb8kaaqOtjNqI9qjq4Zfoa4R4X76DNCTY7jrCBOcSZPwnFV4Z8bjoJSYUeH8OqW= QlIa7Da_Ddzeh7AkvK07zns$ for graphic product...

    ATTN...WFO...LMK...LZK...MEG...OHX...PAH...SGF...SHV...

    ATTN...RFC...ABRFC...LMRFC...OHRFC...NWC...

    LAT...LON 37798645 37448527 36658564 36088783 34629061=20
    33119252 33099332 33889348 35589251 36809080=20
    37528852=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Feb 15 19:50:41 2025
    AWUS01 KWNH 151947
    FFGMPD
    VAZ000-WVZ000-OHZ000-TNZ000-KYZ000-INZ000-160145-

    Mesoscale Precipitation Discussion 0041
    NWS Weather Prediction Center College Park MD
    246 PM EST Sat Feb 15 2025

    Areas affected...Portions of the OH/TN Valleys and Central
    Appalachians

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 151945Z - 160145Z

    SUMMARY...Locally significant flash flooding is expected going
    into the evening hours from persistent heavy rainfall over
    saturated soils.

    DISCUSSION...The latest GOES-E IR satellite imagery along with
    dual-pol radar shows an expansive area of heavy rain continuing to
    advance west to east across central and eastern KY and into
    southwest VA and southern WV. The activity continues to be
    associated with strong warm air advection which is being aided by
    a powerful southwest low-level jet of 40 to 60+ kts overrunning a
    strong frontal zone.

    This is driving very strong moisture transport with magnitudes in
    the SFC/850 mb layer of as much as 320 kg/m/s aiming across much
    of western and central TN and toward southern KY as seen in the
    experimental CIRA-LVT (Layered Vapor Transport) imagery. Some very
    modest instability with MUCAPE values of as much as 100 to 250
    J/kg is noted over the region and this has been supporting some
    occasional elevated convective elements.

    Over the next several hours heading into the evening, there will
    continue to be a west to east axis of heavy rainfall given the
    level of strong isentropic ascent and frontogenetical forcing, but
    as a warm front lifts north with time, this band of heavy rainfall
    should also gain latitude with the rain eventually getting into
    more of north-central to northeast KY and central WV.

    The rainfall rates should be able to at least occasionally reach
    into the 0.50" to 0.75"/hour range, and especially with any
    stronger convective elements that continue to materialize. These
    rates and overall persistence of heavy rainfall should support
    additional rainfall totals by early this evening of 1 to 2 inches
    with locally higher amounts.

    Many areas have ongoing areal flooding and flash flooding, and
    with extremely sensitive/saturated soil conditions and very high
    streamflows, much of the additional rainfall will lead to
    immediate runoff and potentially support significant flash
    flooding for some locations. This will include areas of the
    central Appalachians for locations that currently also have a
    melting snowpack and thus added water runoff concerns.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_x0dK2JV4HgGIM65ux75coVlDb0zP0EKlMSOCYp6OUxNID4h2UFh_3Lze1FX9vfrroeP= NMzW9UPAY6yLbhgB4ivmMHs$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...LWX...MRX...OHX...RLX...RNK...

    ATTN...RFC...LMRFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 38868096 38507991 38007962 37197993 36698093=20
    36348411 36568591 37358642 37988611 38578432=20
    38848255=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Feb 16 01:21:39 2025
    AWUS01 KWNH 160121
    FFGMPD
    TNZ000-ALZ000-MSZ000-LAZ000-ARZ000-160720-

    Mesoscale Precipitation Discussion 0043
    NWS Weather Prediction Center College Park MD
    820 PM EST Sat Feb 15 2025

    Areas affected...Northern LA...Central and Northern MS...Western
    and Northern AL...Middle TN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 160120Z - 160720Z

    SUMMARY...Heavy showers and thunderstorms will be sweeping across
    the region over the next several hours which may produce some
    areas of flash flooding, with especially the more urbanized
    locations at risk for potential runoff problems.

    DISCUSSION...Radar and satellite imagery shows an evolving QLCS
    crossing through areas of eastern AR through western TN, with more
    broken clusters of organized convection including a few supercells
    down across areas of northern LA which is beginning to move into
    areas of western MS.

    The airmass downstream of the current convection is moist and
    moderately buoyant with MLCAPE values of 1000 to 1500 J/kg locally
    and PWs of near 1.5 inches. However, a substantial amount of shear
    remains in place ahead of the strong shortwave and attendant
    frontal system crossing the Lower MS Valley. A very strong
    low-level jet of 50 to 60+ kts remains a key player in driving
    enhanced moisture/instability transport and this will sustain the
    convective threat well into the overnight hours as a cold front
    approaches and eventually crosses the region.

    Rainfall rates associated with the QLCS and more discrete
    supercell activity over the next several hours will likely reach
    as high as 1.5 to 2 inches/hour, and there may be at least some
    occasional cell-merger and cell-training activity that will
    support some locally excessive rainfall totals that may reach 2 to
    4 inches.

    NASA SPoRT data shows antecedent soil conditions on the moist side
    across much of the region given the heavy rainfall that occurred a
    few days ago. This coupled with the locally heavy convective rains
    over the next several hours may pose at least some concern for
    areas of flash flooding. However, generally the more urbanized
    locations will be at greatest risk for runoff problems and impacts
    heading into the overnight hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_dh-UctBjAzaR5XuVslTA7kCWT2U17Uy4b4tnD0KR7Ikw5OL3TSB6yB3TtpYwMlaiFlY= TmhjBMfPKLhR7eOGB3-TFn0$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LCH...LIX...LZK...MEG...MRX...
    OHX...SHV...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36018588 35688528 34408623 32918779 31708932=20
    31109076 31149210 31389265 31909290 32679249=20
    33559157 34289031 35008825=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Feb 16 02:04:02 2025
    AWUS01 KWNH 160202
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-OHZ000-KYZ000-160800-

    Mesoscale Precipitation Discussion 0044
    NWS Weather Prediction Center College Park MD
    901 PM EST Sat Feb 15 2025

    Areas affected...Portions of the OH Valley and Central
    Appalachians

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 160200Z - 160800Z

    SUMMARY...Locally significant and life-threatening flash flooding
    will continue into the overnight hours with additional Flash Flood
    Emergency level impacts possible from additional rounds of heavy
    rainfall, with the central Appalachians continuing to see the
    greatest risk of this.

    DISCUSSION...The latest radar imagery continues to show an
    expansive area of heavy rainfall impacting areas of mainly
    north-central to northeast KY through central WV and down into
    areas of south-central VA. The activity continues to be associated
    with strong warm air advection which is being aided by a powerful
    southwest low-level jet of 40 to 60+ kts surging up through the
    OH/TN Valley region and into the central Appalachians.

    Very strong transport continues as a result which coupled with
    enhanced isentropic ascent and frontogenetical forcing continue to
    yield heavy rainfall rates generally in the 0.25" to 0.50"/hour
    range with some occasionally heavier rates where some embedded
    elevated convective elements focus. Some very modest instability
    with MUCAPE values of as much as 100 to 250 J/kg is noted over the
    region and this continues to favor at least some transient pockets
    of convection.

    A warm front continues to gradually lift north into the OH Valley
    and central Appalachians and this is allowing for the overall
    heavy rainfall shield to gain latitude. Going into the overnight
    hours, rainfall rates should still be capable of reaching a
    0.50+"/hour locally and especially with the aforementioned pockets
    of elevated convection. Additional rains of as much as 1 to 2
    inches will be possible over the next 6 hours, with areas closer
    to the OH River involving northeast KY and southern OH seeing
    potentially 2 to 3 inches given heavier rainfall approaching from
    western KY including some stronger pockets of even stronger
    convection.

    Given the additional rainfall and ongoing widespread focus of
    areal flooding and flash flooding, significant and
    life-threatening flash flooding is likely to continue with
    additional potential for Flash Flood Emergency level impacts. This
    will especially be the case over portions of the central
    Appalachians where there have already been a total of 4 Flash
    Flood Emergencies issued since early this afternoon.
    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Fg8Ag0Kz6_p6CldtRGTmShLNnTzxgtRFgJQKMCYiQiuItEFTm3kwmTWjaghChzH9c0f= cMRalbMI6zKUo33LWwfq1OI$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...LWX...PBZ...RLX...RNK...

    ATTN...RFC...MARFC...OHRFC...NWC...

    LAT...LON 39878106 39677973 39037917 38167920 37658001=20
    37598196 37648310 37888390 38408422 39038417=20
    39528328 39768232=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Feb 16 04:34:27 2025
    AWUS01 KWNH 160432
    FFGMPD
    PAZ000-WVZ000-OHZ000-KYZ000-INZ000-161000-

    Mesoscale Precipitation Discussion 0045
    NWS Weather Prediction Center College Park MD
    1132 PM EST Sat Feb 15 2025

    Areas affected...southwestern to eastern OH into western PA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 160430Z - 161000Z

    SUMMARY...Localized flash flooding will be possible from portions
    of southwestern OH into eastern OH and western PA through 10Z.
    Peak rainfall rates between 0.50 and 0.75 in/hr may occur but most
    locations should see lower rates. Still, the addition of 1-2
    inches of rain over a relatively short period of time atop
    sensitive ground conditions may result in localized flash flooding.

    DISCUSSION...Regional radar imagery at 04Z depicted an area of
    higher reflectivity moving east-northeastward into
    southwestern/central OH, just north of MPDs #42 and #44. While
    bright banding accounts for these higher reflectivity values with
    surface temperatures only in the 30s and 40s, ground observations
    have reported peak rainfall rates of about 0.25 to 0.50 inches
    (locally higher) to the west and north of Cincinnati within the
    last hour. This axis of precipitation is related to a
    strengthening zone of low level frontogenesis (850-700 mb),
    located north of an approaching surface low in KY, connected to a quasi-stationary front that extended through eastern KY into
    north-central WV. SPC mesoanalysis data from 04Z indicated less
    than 100 J/kg MUCAPE to the north of the front into OH. Strong
    divergence aloft was also present over the region, given the
    position of a 180+ kt upper level jet max located over MI and Lake
    Huron, placing OH within its favorable right-entrance region.

    Short term RAP forecasts indicate the surface low over KY will
    steadily track northeastward over the next several hours, allowing
    the front to lift north as a warm front through 09Z. This movement
    will cause the strong axis of frontogenesis to also lift north
    while weak MUCAPE (up to 150 J/kg or so) moves into southeastern
    OH and western PA between 06-09Z. Bands of heavy rain are expected
    within the broader precipitation shield with occasional rates as
    high as 0.50 to 0.75 in/hr. Additional rainfall of 1 to 2 inches
    is expected to occur through 10Z from southwestern OH into eastern
    OH and western PA. While this region of the Midwest has escaped
    the ongoing significant rains and flooding to the south, soils
    remain sensitive with low FFG values of only 1 inch in 3 hours
    across the upper OH Valley. Localized flash flooding may result
    due to an additional 1-2 inches of rain over a fairly short period
    of time.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7BAiGOy8kEX0Z4HBYlIicO-KDRnqegYnHBg7SBqOeCHPk2w6XUgTeWNieeac3ajxg3Uv= trfZBU7hi5iGPucbXayZgAw$ for graphic product...

    ATTN...WFO...CLE...CTP...ILN...PBZ...RLX...

    ATTN...RFC...MARFC...OHRFC...NWC...

    LAT...LON 41607951 41217861 40217943 39797989 39858054=20
    39788209 39048425 38888491 39668496 40678319=20
    41268145=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Feb 16 06:41:24 2025
    AWUS01 KWNH 160641
    FFGMPD
    VAZ000-NCZ000-WVZ000-TNZ000-KYZ000-161230-

    Mesoscale Precipitation Discussion 0046
    NWS Weather Prediction Center College Park MD
    140 AM EST Sun Feb 16 2025

    Areas affected...Cumberland Plateau into central Appalachians

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 160639Z - 161230Z

    SUMMARY...Despite an expected weakening trend in rainfall
    intensity, additional rainfall over a 2-3 hour window will impact
    locations of the central Appalachians hard hit on Saturday. Up to
    an inch of rain is expected in some locations with rates of 0.25
    to 0.5 in/hr. These rains are expected to exacerbate ongoing
    flooding concerns.

    DISCUSSION...0630Z radar imagery showed that a squall line
    extended SSW from southern TN (between I-65 and I-24) into
    northwestern AL. An inflection along the line was noted over
    southern TN with an inferred low level vorticity max to its west.
    North of the inflection point, the convective line was weaker but
    still has had a history of producing hourly rainfall in excess of
    1 inch over Middle TN since 04Z. The convective line has begun to
    outpace many of the 00Z hires models, most notably over AL, likely
    not properly capturing the influence of the mesoscale vorticity
    max.

    Going forward, instability will be a limiting factor to higher
    rainfall rate potential across the "northern" locations of eastern
    KY, southern WV and western VA. However, recent hires models may
    be slightly downplaying rainfall rate potential from the
    Cumberland Plateau into the central Appalachians. Current thinking
    is that 0.25 to 0.50 in/hr will be possible from eastern KY into
    southern WV and western VA with locally higher rates farther south
    over eastern TN where up to a couple hundred J/kg of CAPE may be
    present to locally boost rainfall intensity. However, heavy
    rainfall duration will be limited by the progressive movement of
    the convective line across TN.

    Farther north into eastern KY, southern WV and western VA, poorer
    organization of the line will be somewhat offset by a longer
    duration of rainfall, about 2-3 hours is when a majority of the
    expected rainfall will fall. Portions of this region have received
    heavy rainfall over the past 24 hours and have ongoing/widespread
    significant flooding. Up to an additional inch of rain may fall
    across these sensitive locations which will act to exacerbate
    existing flooding concerns.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4tfc1TY4BPoPr3mT0SExna_-HdVTbXyjJ7Lx8pDjG2Kd9NnJHBU1PtteAsY_pIjgmpr_= j5g0qjkAmSOkRRfFrLxPxJQ$ for graphic product...

    ATTN...WFO...JKL...MRX...OHX...RLX...RNK...

    ATTN...RFC...LMRFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 38398034 38327990 37977999 37388020 36928005=20
    36508149 36288219 35728344 35498470 35698554=20
    36188547 36918424 37558322 37988274 38278199=20
    38368112=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Feb 16 07:33:57 2025
    AWUS01 KWNH 160733
    FFGMPD
    PAZ000-WVZ000-OHZ000-KYZ000-INZ000-161030-

    Mesoscale Precipitation Discussion 0047
    NWS Weather Prediction Center College Park MD
    233 AM EST Sun Feb 16 2025

    Areas affected...upper OH Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 160730Z - 161030Z

    SUMMARY...Moderate to heavy rain will continue to translate east
    through the upper OH Valley in the short term with an additional
    inch of rain through 1030Z. Renewed flash flooding is expected.

    DISCUSSION...0730Z radar imagery showed a leading linear segment
    of heavy rain moving through eastern KY, followed by a stratiform
    region of moderate to heavy rain over eastern KY. As a low level
    vorticity max advances northeast from Middle TN, an 2-3 hour long
    duration of stratiform moderate to heavy rain is expected to
    advance into eastern KY, southern OH and eventually portions of
    western WV. In addition, preceding the stratiform region will be a
    leading line of showers with embedded thunderstorms which have had
    a history of 0.25 to 0.50 in an hour but with a 0.25 inch or more
    in 15 minutes over eastern KY.

    As the entire envelope of rain translates toward the
    east/northeast, additional totals up to about an inch are expected
    through 1030Z, with a likelihood of renewed flash flooding or a continued/worsening of ongoing flooding concerns occurring from
    heavy rain which fell over the past 24 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6BP8PzyRHNEKpvsqNiFF7Yyyibfz9nGkUd5w_1SazcpiI6Buo5H2cC0t0gEgqrf8pdsJ= SNCWbBtxqXXKNUUPknncq0Q$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...PBZ...RLX...

    ATTN...RFC...OHRFC...NWC...

    LAT...LON 40038127 39908038 39558035 39178062 38228193=20
    37628302 36958397 36798457 36938503 37448531=20
    38198528 39078473 39758323 39958210=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Feb 12 09:28:38 2025
    AWUS01 KWNH 120928
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-121526-

    Mesoscale Precipitation Discussion 0029
    NWS Weather Prediction Center College Park MD
    427 AM EST Wed Feb 12 2025

    Areas affected...much of Louisiana, central/southern Mississippi,
    and a small part of east Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 120926Z - 121526Z

    Summary...Convective bands will continue to increase and grow
    upscale into clusters and lines while moving eastward across the
    discussion area. A few areas of 1-2 inch/hr rain rates are
    expected, which should pose a flash flood risk especially near
    sensitive areas.

    Discussion...Over the past hour or so, radar mosaic imagery has
    depicted a distinct uptick in convective activity across east
    Texas and Louisiana. The increase in convection is likely tied to
    a dramatic increase in southerly 850mb flow along the Sabine River
    Valley (into the 40-60 kt range) along with attendant
    convergence/ascent. The eastward movement of a distinct mid-level
    shortwave trough and steep lapse rates aloft were also
    contributing factors to the increase in convection. Most storms
    are elevated above a cool stable boundary layer, although mergers
    and growth into linear segments with localized training have
    already been observed near/just east of Lufkin, where spots of 1
    inch/hr rain rates were already estimated via MRMS.

    These convective trends are expected to continue, with
    observations and CAMs both suggestive of upscale growth into one
    or two dominant complexes that move eastward across the region.=20
    Many cell mergers are anticipated and localized training will
    remain a distinct possibility. These factors should contribute to
    occasional 1-2 inch/hr rain rates at times as storms move eastward
    through the discussion area. These rates should approach FFG
    thresholds - especially along an axis from Lufkin to Greenville to
    Columbus where prior rainfall has contributed to wet soils and
    <1.5 inch/hr FFG thresholds. Prolonged rainfall along and south
    of this axis (i.e., greater than 1 hour of heavy rainfall) may
    also result in flash flooding. This threat is expected to persist
    through 15Z, with occasional convective redevelopment in east
    Texas indicated in the models throughout the morning.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7lIa7zzacsrpPgW07lPFC80pQTiBIi1dUIuuMNf9dXQ_UvaMihtl4fGGQ3H3scWSq11f= CVF68sukC-fDK3-OoZLRXG4$ for graphic product...

    ATTN...WFO...HGX...JAN...LCH...LIX...MEG...SHV...

    ATTN...RFC...LMRFC...SERFC...WGRFC...NWC...

    LAT...LON 33888837 33218839 32128857 31239008 30539215=20
    30489469 31609498 32489388 33409101 33838960=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Feb 12 15:27:20 2025
    AWUS01 KWNH 121519
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-122031-

    Mesoscale Precipitation Discussion 0030
    NWS Weather Prediction Center College Park MD
    1018 AM EST Wed Feb 12 2025

    Areas affected...Lower Missisippi Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 121518Z - 122031Z

    Summary...Showers and thunderstorms will expand in coverage and
    begin to train from SW to NE through the afternoon. Rainfall rates
    in excess of 1"/hr will become more common, which through training
    may produce 2-3" of rain. This could lead to instances of flash
    flooding.

    Discussion...The regional radar mosaic this morning depicts two
    areas of heavy precipitation spreading across portions of the Gulf
    Coast and lower Mississippi Valley states. A meandering stationary
    front analyzed by WPC draped from northern MS into eastern TX is
    providing focus for a corridor of convection, while a more broad
    warm front slowly lifting across LA/MS is helping to spawn warm
    advection showers and isolated thunderstorms. In general, rainfall
    rates this morning have been between 0.25 and 0.5 inches per hour,
    but a few embedded 1"/hr cells have recently been observed via
    MRMS radar estimates. This has produced locally 2-3" of rain in
    the past 6 hours, and a few flood advisories are currently in
    effect.

    As the morning progresses into the afternoon, upstream troughing
    across the Central Plains will amplify, with synoptic ascent
    becoming enhanced across the region through height falls, PVA, and
    an intensifying jet streak aloft. Together, this will help lift
    the warm front more steadily northward, leading to greater
    instability drawing northward and impinging into the stationary
    front. This is reflected by impressive moisture transport vector
    convergence later this morning, especially from northern LA into
    northern MS. As CAPE climbs to 500-1000 J/kg, this will support
    more widespread convective rain rates which the HREF indicates
    have a 20-40% chance of exceeding 1"/hr, with short term rain
    rates potentially eclipsing 2"/hr as shown by the HRRR 15-min
    fields. Storm motions will remain quick on 850-300mb winds of
    40-60 kts, but organization along this boundary and some
    backbuilding into TX will support training. This suggests that
    despite the fast motion of individual cells, some areas may pick
    up 2-3" of rain.

    The soils across this region are generally saturated as noted via
    NASA SPoRT 40cm soil moisture that is around the 90th-95th
    percentile. This has reduced FFG to just 1-2"/3 hrs, or less, in
    many areas, for which the HREF suggests has a 20-50% chance of
    exceedance in the next few hours. This is further reflective of
    the isolated potential for flash flooding into this afternoon.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5eDLGJEwOksezvhbZNpBWprRz3gZUBB61rszsHvK2Q2fLtc_mwlEocph5LRwhyUAkwSs= tbV3sRDDzZmp40aMZ8EYLHo$ for graphic product...

    ATTN...WFO...JAN...LCH...LZK...MEG...SHV...

    ATTN...RFC...LMRFC...SERFC...WGRFC...NWC...

    LAT...LON 34238926 33958850 33368831 33048848 32578930=20
    32039023 31339199 31039338 31069381 31169418=20
    31549474 32279439 32789356 33479207 33969096=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Feb 12 20:27:20 2025
    AWUS01 KWNH 122026
    FFGMPD
    ALZ000-MSZ000-LAZ000-130215-

    Mesoscale Precipitation Discussion 0031
    NWS Weather Prediction Center College Park MD
    326 PM EST Wed Feb 12 2025

    Areas affected...Lower Mississippi Valley through Northern Alabama

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 122024Z - 130215Z

    Summary...Showers and thunderstorms rapidly blossoming within a
    warm sector will expand in coverage and intensify through the
    afternoon. These thunderstorms will lift northward and then train
    SW to NE ahead of a cold front, with rainfall rates as much as
    2-3"/hr. This could lead to instances of flash flooding.

    Discussion...The regional radar mosaic across the Gulf Coast this
    afternoon depicts rapidly expanding and intensifying thunderstorms
    along and just south of a warm front from LA to the FL Panhandle.
    This convection is expanding within a pronounced warm sector
    characterized by favorable instability (MLCAPE 1000-2000 J/kg) and
    elevated PWs (1.6 to 1.8 inches) according to the SPC
    mesoanalysis. Additionally, recent VWPs from the region indicate
    modest low-level veering but with strong inflow, supporting large
    updrafts capable of producing intense rainfall rates. This is
    being analyzed by recent MRMS 15-min rainfall as high as 0.75"
    (3"/hr rates), resulting in rising CREST unit streamflow values
    across parts of LA and MS. Upstream of this fresh convection, a
    wave of low pressure and attendant cold front are analyzed by WPC
    crossing from TX into LA, along which additional thunderstorms are
    occurring with current FFWs.

    As the afternoon progresses into the evening, the environment
    should become increasingly unstable as the plume of 1000-2000 J/kg
    MLCAPE surges as far north as Birmingham, concurrent with elevated
    PWs being drawn northward. This plume of robust thermodynamics
    will be advected on 850mb inflow that is progged to reach 50+ kts,
    resulting in 850-700mb moisture flux that may exceed 5 sigma
    according to the SREF. Additionally, increasing synoptic lift
    within the RRQ of an intensifying jet streak will support an
    expansion of convection into the evening, with thunderstorms
    likely aligning along or just ahead of the convergence axis of the
    approaching cold front as it squeezes the warm sector. This
    alignment will rapidly enhance the flash flood risk, as training
    of cells along the boundary will offset the limiting storm speed
    of 40-60kts.

    The HREF suggests that coverage of rainfall rates exceeding 1"/hr
    will expand, and the HRRR 15-min progs suggest rainfall intensity
    may produce 0.75 to 1 inch of rain in as little as 15 minutes.
    These rates themselves could cause instances of flash flooding,
    but where training occurs, more than 3" of rain is possible,
    enhancing the flash flood risk. The most likely locations for any
    flash flooding will be across urban areas as soil moisture in
    southern LA, MS, AL is drier than normal according to NASA SPoRT.
    However, training of these intense rain rates could quickly
    overwhelm even the drier soils, so flash flood instances are
    possible anywhere across the discussion area into this evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7HS20P0xpH_2YeArlrAwCpCkIcjONWRgMCzQPbWsAxBFJQAM3nSAqEdYjgbLbHzZEWoP= UGLjng9UesXPUWDHdCY15PE$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LCH...LIX...MEG...MOB...SHV...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34828712 34538627 33658599 32878613 32308688=20
    31708793 31268939 30989077 30979206 30969237=20
    31009261 31569255 32349167 34568837=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Feb 12 20:31:47 2025
    AWUS01 KWNH 122031
    FFGMPD
    ALZ000-MSZ000-LAZ000-130215-

    Mesoscale Precipitation Discussion 0031...Corrected
    NWS Weather Prediction Center College Park MD
    331 PM EST Wed Feb 12 2025

    Corrected for updated graphic

    Areas affected...Lower Mississippi Valley through Northern Alabama

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 122024Z - 130215Z

    Summary...Showers and thunderstorms rapidly blossoming within a
    warm sector will expand in coverage and intensify through the
    afternoon. These thunderstorms will lift northward and then train
    SW to NE ahead of a cold front, with rainfall rates as much as
    2-3"/hr. This could lead to instances of flash flooding.

    Discussion...The regional radar mosaic across the Gulf Coast this
    afternoon depicts rapidly expanding and intensifying thunderstorms
    along and just south of a warm front from LA to the FL Panhandle.
    This convection is expanding within a pronounced warm sector
    characterized by favorable instability (MLCAPE 1000-2000 J/kg) and
    elevated PWs (1.6 to 1.8 inches) according to the SPC
    mesoanalysis. Additionally, recent VWPs from the region indicate
    modest low-level veering but with strong inflow, supporting large
    updrafts capable of producing intense rainfall rates. This is
    being analyzed by recent MRMS 15-min rainfall as high as 0.75"
    (3"/hr rates), resulting in rising CREST unit streamflow values
    across parts of LA and MS. Upstream of this fresh convection, a
    wave of low pressure and attendant cold front are analyzed by WPC
    crossing from TX into LA, along which additional thunderstorms are
    occurring with current FFWs.

    As the afternoon progresses into the evening, the environment
    should become increasingly unstable as the plume of 1000-2000 J/kg
    MLCAPE surges as far north as Birmingham, concurrent with elevated
    PWs being drawn northward. This plume of robust thermodynamics
    will be advected on 850mb inflow that is progged to reach 50+ kts,
    resulting in 850-700mb moisture flux that may exceed 5 sigma
    according to the SREF. Additionally, increasing synoptic lift
    within the RRQ of an intensifying jet streak will support an
    expansion of convection into the evening, with thunderstorms
    likely aligning along or just ahead of the convergence axis of the
    approaching cold front as it squeezes the warm sector. This
    alignment will rapidly enhance the flash flood risk, as training
    of cells along the boundary will offset the limiting storm speed
    of 40-60kts.

    The HREF suggests that coverage of rainfall rates exceeding 1"/hr
    will expand, and the HRRR 15-min progs suggest rainfall intensity
    may produce 0.75 to 1 inch of rain in as little as 15 minutes.
    These rates themselves could cause instances of flash flooding,
    but where training occurs, more than 3" of rain is possible,
    enhancing the flash flood risk. The most likely locations for any
    flash flooding will be across urban areas as soil moisture in
    southern LA, MS, AL is drier than normal according to NASA SPoRT.
    However, training of these intense rain rates could quickly
    overwhelm even the drier soils, so flash flood instances are
    possible anywhere across the discussion area into this evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5MQOgaXrGVUoKPJkQubelxBuZyrEYS24uHQXIN3l7yhjsj_2rwva_5FCBl-uLT7SYJgF= n5-HZtHsTQA859vPlm0_hRI$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LCH...LIX...MEG...MOB...SHV...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34828712 34538627 33658599 32878613 32308688=20
    31708793 31268939 30989077 30979206 30969237=20
    31009261 31569255 32349167 34568837=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Feb 13 02:21:54 2025
    AWUS01 KWNH 130221
    FFGMPD
    NCZ000-GAZ000-TNZ000-ALZ000-MSZ000-LAZ000-130820-

    Mesoscale Precipitation Discussion 0032
    NWS Weather Prediction Center College Park MD
    920 PM EST Wed Feb 12 2025

    Areas affected...Portions of Eastern LA...Southern MS...Much of
    AL...Southeast TN...Northern GA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 130220Z - 130820Z

    SUMMARY...Heavy showers and thunderstorms will continue to impact
    the South overnight with concerns for high rainfall rates and
    cell-training. Additional areas of flash flooding are likely which
    will include the more sensitive urban corridors.

    DISCUSSION...The latest radar and satellite imagery continues to
    show a well-organized convective outbreak evolving across the
    South with multiple bands of strong to severe convection,
    including supercells, that are focusing corridors of locally
    enhanced rainfall. A strong southwest low-level jet of 40 to 50+
    kts continues to advance up across eastern LA through southern MS,
    with it nosing up into areas of western and central AL. This is
    fostering strong moisture transport along with the arrival of a
    moderately buoyant airmass characterized by MUCAPE values of 1000
    to 2000 J/kg.

    Strong low to mid-level veering flow with height continues to
    yield enhanced shear profiles favorable for supercells and these
    more organized storms out ahead of an approaching cold front and
    in vicinity of a warm front lifting northeast across the Southeast
    have been tending to locally train over the same location this
    evening.

    Over the next few hours, areas of southern MS through central AL
    in particular will continue to see cell-training and cell-merger
    concerns as the convection attempts to evolve a bit more into a
    QLCS which will still include embedded supercell concerns. By late
    this evening and going well past midnight, areas of northwest GA
    will begin to see more of the concentration of heavier convective
    rainfall.

    The evening CAM guidance, including the HRRR and the experimental
    WoFS supports an additional 2 to 4 inches of rain with isolated
    heavier amounts possible where the corridors of more organized
    cell-training occurs, and this will be aided by rainfall rates of
    generally 1 to 2+ inches/hour.

    Some areas of flash flooding are already occurring, and the
    additional rains over the next several hours should yield
    additional areas of flash flooding. This will include especially
    the more sensitive urban areas, which by later in the night may
    include the Atlanta metropolitan area.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_3fNJtQJjYRscRkNcMOzrGhXFAUr56rJ10qzqoCtWZNkR97j4WNaN_fsQhuz9NB-qHqL= UURXVMq2s7XddsY3-NVIKYs$ for graphic product...

    ATTN...WFO...BMX...FFC...GSP...HUN...JAN...LIX...MOB...MRX...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 35448488 35208370 34498325 33368365 31778605=20
    30328893 29919032 30629034 32228877 33658741=20
    34978636=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Feb 13 05:45:44 2025
    AWUS01 KWNH 130544
    FFGMPD
    CAZ000-131740-

    Mesoscale Precipitation Discussion 0033
    NWS Weather Prediction Center College Park MD
    1244 AM EST Thu Feb 13 2025

    Areas affected...portions of northern, central and southern CA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 130543Z - 131740Z

    SUMMARY...Areas of heavy rain will overspread a sizable portion of
    northern to south-central CA through 18Z Thursday ahead of an
    approaching occluded cyclone. Some locations may see hourly
    rainfall in excess of 0.5 inches for several hours with the
    greatest potential for high rates along the Santa Lucia Range. 12
    hour rainfall totals of 3 to 5+ inches are likely within areas of
    favored terrain and heavy rain may produce areas of flooding/flash
    flooding within urban areas and/or sensitive burn scars.

    DISCUSSION...Loops of GOES West water vapor imagery through 05Z
    showed a strengthening closed mid to upper-level low centered near
    42N 134W. A strong, zonally oriented 250 mb jet axis was located
    across 36N 140W, south of the closed low, with winds in excess of
    150 kt located as far east as 134W per GOES West DMW vectors. The
    location of the upper level jet max west of the upper trough axis
    indicated the longwave trough was digging southward, but the
    parent closed low appeared to be generally moving toward the east.
    A ribbon of moisture streamed from west to east across the eastern
    Pacific Ocean along a cold front connected into an occluded
    cyclone over the eastern Pacific. TPW and LPW imagery showed that
    the plume of moisture extended thousands of miles back to the
    west, originating in the tropical west-central Pacific. However,
    anomalous moisture was already located just off of the CA coast
    with 00Z soundings from OAK and VBG showing PWAT values between
    the 90th percentile and climatological max for mid-February. Warm
    advection rainfall was already occurring in advance of the warm
    front analyzed southeastward toward the south-central CA coast,
    roughly 60 miles west of the coast of Monterey County.

    As the closed low continues to advance off toward the east over
    the next 6-12 hours, the attendant cold front is forecast to
    steadily advance east and southeast, reaching the northern coast
    of CA around 12Z. IVT values will steadily increase across the
    central CA coast through 12Z peaking between 800-900 kg/m/s in the
    vicinity of San Francisco. IVT values will remain above 600 kg/m/s
    for a good portion of the central to south-central CA coast for
    several hours with 850 mb winds peaking between 50-60 kt. The
    orientation of the 850 mb flow is expected to be perpendicular to
    the coast from North Bay to Point Conception.

    Hourly rainfall in excess of 0.5 inches will become likely in and
    around the higher terrain of San Francisco Bay by 09Z, perhaps
    lasting for 3-5 hours. Farther south, hourly rainfall may reach 1
    in/hr along the Santa Lucia Range given the favorable orthogonal
    orientation of the low level flow to the axis of the mountain
    chain. Downstream into the Sierra Nevada, snow levels are expected
    to be near 7000 ft which will result in rainfall impacts to
    potentially extend up to a relatively high elevation. Hourly
    rainfall in excess of 0.5 inches may exceed 6 hours in duration
    for portions of the central Sierra Nevada and Santa Lucia Range.
    Sub-hourly rainfall rates over 0.25 inches in 15 minutes will be
    possible within area of orographic ascent and boosted by weak
    instability, though CAPE values are forecast to remain focused
    below ~4 km AGL and stay below 250 J/kg by a majority of the most
    recent guidance prior to 18Z.

    12 hour rainfall totals through 17/18Z are expected to peak in the
    3 to 5 inch range for the Coastal Ranges into the upslope regions
    of the central Sierra Nevada, through higher totals may occur
    within the Santa Lucia Range given a favorable low level wind
    orientation. While flooding/flash flooding will be possible, it is
    expected to remain on the low end of the scale and may be focused
    across urban areas or perhaps lingering sensitivity on any area
    burn scars.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5Xmh9Oowt5YmUjifd4UFwIY0mxZaT2flnAljU8G1GJgFwfOn4sGM2mM1sT_wTJ33SY2v= mCQsmDq9al77Us9izFuTJMQ$ for graphic product...

    ATTN...WFO...EKA...HNX...LOX...MTR...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 40782243 40652194 40112164 39712119 39512070=20
    39232058 38912037 38572025 38051987 37581950=20
    37421919 37171914 37021903 36751880 36571874=20
    36271862 35941838 35501850 35381881 36001952=20
    36032012 35642002 35171970 34622061 35212158=20
    35932251 37862346 39302456 39972518 40592460=20
    40532360 40662277=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Feb 6 08:23:03 2025
    AWUS01 KWNH 060822
    FFGMPD
    WVZ000-OHZ000-KYZ000-061321-

    Mesoscale Precipitation Discussion 0021
    NWS Weather Prediction Center College Park MD
    322 AM EST Thu Feb 06 2025

    Areas affected...northern/central Kentucky

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 060821Z - 061321Z

    Summary...At least minor/isolated flash flood potential should
    continue through 13Z or so as upstream convection near the
    Mississippi/Ohio River confluence migrates eastward through the
    discussion area.

    Discussion...Persistent, repeating convection along an axis from
    near Lexington, KY to near Huntington, WV has produced several
    areas of 1-1.75 inch rainfall totals over the past 3-6 hours
    despite relatively quick movement. The rainfall associated with
    these storms has wet soils considerably across the region, with
    most recently updated FFG thresholds lowering into the 0.25-0.75
    inch/hr range and MRMS Flash responses suggestive of at least
    isolated, minor flooding and runoff issues existing along that
    corridor.

    Convection upstream of this region is causing some concern that
    perhaps another uptick in flash flood potential might occur
    between 09-13Z. This convection is expected to expand due to 1)
    forcing for ascent aloft associated with mid-level vort maxima
    across IL/IN, 2) fast low-level flow impinging on a warm front in
    western KY, and 3) increasing MU/SBCAPE across the region. CAMs
    generally follow suit with this thinking, suggesting another round
    of potential training convection entering the Lexington/Huntington
    axis between 10-13Z with possible 0.25-0.75 inch/hr rain rates.=20

    Should this potential materialize as forecast, isolated flash
    flood potential can be expected especially in the 10-13Z timeframe.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Dbq6sRFf-TmWAgKxEN9tpF57_2A46cfFrfpBZfR6GDUtFhpx-71Wt25V371NY16Y7ly= aHQuREIgM8AVbkSlD_tx01g$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...RLX...

    ATTN...RFC...OHRFC...NWC...

    LAT...LON 38728286 37988244 37468285 37208508 37498620=20
    38138567 38578468=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Feb 6 13:00:36 2025
    AWUS01 KWNH 061300
    FFGMPD
    VAZ000-WVZ000-KYZ000-061830-

    Mesoscale Precipitation Discussion 0022
    NWS Weather Prediction Center College Park MD
    800 AM EST Thu Feb 06 2025

    Areas affected...South-central & Eastern KY...Southern WV... Far
    Western VA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 061300Z - 061830Z

    SUMMARY...While intensity and coverage is on a downward trend, a
    few cells will remain capable of intense rain rates of
    1.25-1.5"/hr over saturated soils for scattered incident or two of
    flash flooding through the remainder of the morning.

    DISCUSSION...GOES-E WV suite shows the core of the triggering
    shortwave energy along the base of the broader synoptic trough has
    slid across central Ohio with trailing tail crossing northern KY
    along/ahead of the approaching 130+kt flat upper-level jet. This
    orientation continues to provide solid broad scale ascent with
    DPVA south and eastward across the area of concern, accompanied by
    solid divergence to maintain ongoing convective activity across
    the warm sector. Surface and VAD wind profiles also denote the
    speed and directional confluence/convergence supporting the active
    line of cells with about 30-45 degrees of convergence in both
    10-20kts of sfc and 50 to 60kts of 850mb flow. Additionally, this
    confluence zone continues to align with diminishing but
    sufficient unstable air mass with mid-60s temps over upper 50s/low
    60s Tds and modest lapse rates for 750-1000 J/kg of SBCAPE across
    south-central to southeastern KY reducing across WV to below 500
    J/kg.

    As such, overall trends have been toward slightly warming tops;
    however, there remain some stronger/broader updrafts with weak
    rotation across southern KY to tap all the available low level
    moisture (over 1.25" total PWats), to allow for some remaining
    efficient rainfall with sub-hourly rates resulting in some totals
    over 1-1.25" in quick duration. Instability and rates will
    diminish through the morning, but west to east cell motion and
    inflow from the southeast into increasing terrain should help for
    some orographic enhancement as well to maintain a low-end
    scattered threat for intense rates.=20

    While orientation of the convergence/convective line has become
    more oblique to the mean steering flow, reducing the capability
    for much higher totals from training noted overall; the soil
    conditions across E KY into S WV/W VA remain cold and highly
    saturated with NASA SPoRT LIS 0-40cm soil ratios well over 75%
    with some spots near 90% in higher terrain that may still have or
    recently just lost the majority of snow pack. As such, FFG values
    are very low (1-1.5"/hr) naturally and with little capacity for
    uptake especially in remaining sub-hourly intense rates...even has
    they diminish with reducing instability into late morning,
    incidents of flash flooding will remain possible.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4QeDRkGcVP3I_A0OHqJcVfoqVaN09OCm6L59ruCauiCi-ZP8B0HE2_GPbwyy0ITJEJdY= XHekTKSHT7OVBkq_Z6OdEhs$ for graphic product...

    ATTN...WFO...JKL...LMK...MRX...RLX...RNK...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 38778098 38658043 38308041 37908075 37228132=20
    36698199 36628406 36738564 37078586 37408487=20
    38088309 38468188=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Feb 6 14:44:06 2025
    AWUS01 KWNH 061444
    FFGMPD
    CAZ000-070300-

    Mesoscale Precipitation Discussion 0023
    NWS Weather Prediction Center College Park MD
    943 AM EST Thu Feb 06 2025

    Areas affected...Coastal Ranges, Sacramento Valley and Lower
    Slopes of Sierra Nevada in California

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 061500Z - 070300Z

    SUMMARY...Compact, quick moving storm with anomalous moisture flux
    to affect mainly coastal ranges at first but by late afternoon
    transition to more convective localized convective showers with
    training potential. Given rates up to .5"/hr, locally 2-3" totals
    are possible in favored orography.=20

    DISCUSSION...GOES-W WV suite denotes a compact, increasingly
    well-defined southern stream shortwave and associated surface low
    near 38N and 128W lifting east-northeast with expanding baroclinic
    shield downstream starting to cover much of northern California.
    This wave/low will continue to strengthen and occlude further
    throughout the day as northern upstream persistent upper-low
    finally swings southeast and provides further DPVA and sharpens
    the entrance region to the strengthen upper-level jet streak;
    while steepening lapse rates with cold advection aloft (mainly
    affecting northern CA later in the forecast period, after 00z),
    prolonging the onshore flow and potential for locally heavy
    rainfall.

    RAP analysis/forecast shows strong warm advective pattern
    approaching the central California coast with southerly 30kt 850mb
    winds veering to 50-65kts in the 17-19z period. The nose of the
    LLJ is also accompanied by the core of a narrow warm
    conveyor/moisture axis with 1-1.25" total PWats (though CIRA LPW
    suggests this is mainly below 700mb) and trends continue to direct
    it centered from Monterey Bay southward along the Santa Lucia
    Range. IVT values appear to be 600-700 kg/m/s and given
    orthogonal ascent to the southern Santa Cruz and Santa Lucia
    range, rates of .33-.5"/hr are likely to commence with the arrival
    of the warm front around 17-18z and continue for 5-6hrs, with a
    very slow southward drift of the core of the LLJ/moisture axis.=20
    This magnitude of moisture flux is about 5 standard anomaly above
    normal even in the wet season. As such, localized totals of 2-3"+
    are probable along the range. Later in the afternoon, the plume of
    moisture sags south and rounds Cape Conception around 00z, winds
    will slowly be diminishing to about 30kts at 850mb; there is some
    more oblique (45-60 degrees) of orographic ascent in the
    mid-levels, but southerly surface flow will not increase until
    after the forecast period as the cold front rounds the bend. So
    at this time there is mixed signals to potential for sizable rates
    over the fresh burn scars across the eastern Transverse Ranges, so
    while not completely improbable for flash flooding/mudslides by
    03z, we will be monitoring closely for potential for a targeted
    MPD if conditions increase/warrant it later into this
    evening/overnight.

    Meanwhile, further north the western branch of the TROWAL will
    provide ample moisture flux wrapping north of over the
    surface-850mb low to feed surface upslope forcing to allow for
    moderate rainfall with .25-.33" rates along the coastal ranges
    north of the San Francisco Bay; which should slowly expand
    eastward through into the lower slopes of the Trinity to northern
    Sierra Nevada Ranges. As the upper-level northern stream DPVA
    swings southeast, providing some cooling aloft and steepening
    lapse rates, it will also help to sharpen the
    deformation/convergence zone across NW CA as the surface low
    transitions from coastal to northern central Valley from 23-01z.
    An uptick in convective activity with slight reduction in forward
    speed may result in spotty .33-.5"/hr rates across the
    Redwood/Lost Coast resulting in localized totals of 2-3" by 03z as
    well, this should remain more of a heavy rainfall risk as the
    older burn scars are less susceptible, but an isolated
    creek/stream with quick rise is not completely out of the picture
    given soil conditions remain above average in the 80-95
    percentiles even for this time of year given recent rainfall.=20

    Bottom-line, this quick hitting/strong moisture flux is highly
    anomalous even in the wet season but the overall rates and totals
    still generally remain below flash flooding concerns and will hold
    with a 'heavy rainfall' tag at this time; however will convective
    trends closely for any potential targeted MPDs and flash flooding conditions.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_m8IGq-VPPGXEQyevjqhrrzrpAKV7GP0muBc3Y085SJcZwXQPsBVIx3odYIwSQaiWOVe= yRxGb-5-ycijb610wIr1vsI$ for graphic product...

    ATTN...WFO...EKA...HNX...LOX...MTR...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 40862210 40712184 40432167 40082152 39602087=20
    39172059 38832038 38522027 38141999 37601966=20
    37271940 36881906 36511880 36191865 35951876=20
    36131904 36361928 36671951 37201977 37752022=20
    38092079 37922118 37852141 37492161 37032143=20
    36472092 35972040 35722025 34981988 34761927=20
    34551873 34071906 34331984 34422053 34812083=20
    35452118 36102182 37532286 38292338 39092396=20
    39782422 40382392 40422342 40172319 39972297=20
    39912271 40212264 40582251 40842237=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Feb 6 21:59:44 2025
    AWUS01 KWNH 062159
    FFGMPD
    VAZ000-WVZ000-TNZ000-KYZ000-INZ000-070357-

    Mesoscale Precipitation Discussion 0024
    NWS Weather Prediction Center College Park MD
    458 PM EST Thu Feb 06 2025

    Areas affected...portions of KY and southwest VA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 062157Z - 070357Z

    Summary...Showers and thunderstorms within a saturated atmospheric
    column over saturated soils are expected to lead to hourly rain
    totals to 1.5" and local amounts to 3". This could lead to flash
    flooding over saturated soils and urban areas.

    Discussion...Recent radar imagery shows quick-moving but scattered
    showers and thunderstorms forming and moving through western KY at
    the present time. They are elevated in nature and forming on the
    back side of a frontal zone with a few surface waves on the south
    side of a broad shortwave trough in the Great Lakes, utilizing
    500-1000 J/kg of MU CAPE. Other activity to the southeast is much
    closer to the surface front. At the moment, the flat wave in
    western TN is closest to the back edge of the convection.=20
    Precipitable water values of 0.75-1.25" lie across the region
    within a cool air mass, leading to almost complete saturation.=20
    Effective bulk shear is ~50 kts, which is enough for both linear
    convective organization and mesocyclone formation.

    Flash flood guidance values are fairly low, roughly 1" in three
    hours -- within the past 24 hours, 1-3" of rain fell in this area.
    With the expectation of 0.5"+ an hour totals, possibly as high as
    1.5" in an hour, expected over the next several hours as the
    storms propagate generally east-southeast parallel to thickness
    lines, flash flood guidance exceedance could occur in scattered
    spots where cells can train/two or more mesocyclones can align.=20
    The progressive frontal boundary and quick cell movement should
    keep rain amounts from getting exceptionally high. Hourly totals
    to 1.5" with local amounts to 3" are the expectation, which could
    lead to flash flooding in urban areas and over saturated soils and
    hilly topography.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4hjqNsAz6I_CgvsCe2AdIOO_gfHq22emXLJFkkxZcrzBwWbHk8xyOFB25QZTRoWSnQ43= PyYx9RdN4MljM43fwdPmtzI$ for graphic product...

    ATTN...WFO...JKL...LMK...MRX...OHX...PAH...RLX...RNK...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 38228453 37108114 36598259 36368416 36528789=20
    38218643=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Feb 7 03:18:43 2025
    AWUS01 KWNH 070318
    FFGMPD
    NVZ000-CAZ000-070916-

    Mesoscale Precipitation Discussion 0025
    NWS Weather Prediction Center College Park MD
    1017 PM EST Thu Feb 06 2025

    Areas affected...much of California

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 070316Z - 070916Z

    Summary...Flood/flash flood potential should continue on at least
    an isolated basis through 09Z/1a PST. An additional 1-2 inches of
    rainfall is expected along windward locations of the Sierra, and
    locally higher amounts cannot be ruled out.

    Discussion...Flood/flash flood potential is expected to continue
    through at least 09Z this evening. Persistent lift associated
    with an upstream mid-level wave west of Oregon continues to
    support scattered to widespread shower activity across the region.
    Additionally, strong southerly low-level flow (40-50 knots at
    850mb) continues to support local terrain enhancement to rain
    rates across windward locations of the Sierra, where hourly rain
    rates nearing 0.25 inch were noted per MRMS near/southeast of
    Redding. These rates have contributed to isolated flash flooding
    and mudslides. This regime is expected to persist for several
    more hours, with additional rainfall accumulations of 1-2 inches
    expected. Wet (and moistening) ground conditions and ongoing
    rainfall is expected to continue to foster at least isolated
    instances of excessive runoff/flood impacts.

    Around/after 09Z, models suggest the low-level flow enhancing
    rainfall rates this evening will begin to weaken slightly.=20
    Moderate to heavy rainfall should still remain in the area,
    although a gradual decrease in the overall coverage of the
    heaviest rainfall should commence. A gradual lessening of the
    flash flood risk is also expected during this timeframe.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7sio6R-zD-MkEH7oU-5ZcgLLWkA77ovXv8xNE8-FPjMaKLIzGgMa50aRkvVG02OrovOx= fRjlFcDlzwbRkCjqOCf6qRI$ for graphic product...

    ATTN...WFO...EKA...HNX...MFR...MTR...REV...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 41242187 40582099 39452012 38001937 37381921=20
    37161927 37201984 38132077 38812152 38512191=20
    37612172 36792147 36512163 37682257 40012355=20
    40912315 41172265=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Feb 7 03:49:46 2025
    AWUS01 KWNH 070349
    FFGMPD
    CAZ000-070948-

    Mesoscale Precipitation Discussion 0026
    NWS Weather Prediction Center College Park MD
    1048 PM EST Thu Feb 06 2025

    Areas affected...portions of southern California

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 070348Z - 070948Z

    Summary...Increasing onshore flow is interacting with the
    Transverse Ranges in southern California to produce scattered
    showers and locally heavy rainfall. Rainfall totals of 0.25-1
    inch are possible through 10Z/2am and beyond. Excessive runoff
    and debris flows are a distinct possibility - especially near
    sensitive areas of variable terrain and near burn scars.=20

    Discussion...Over the next several hours, a strong low-level
    cyclone (currently centered near Eureka) will migrate
    northeastward toward Oregon. As this occurs, strong southwesterly
    low-level flow will increase across portions of southern
    California especially near terrain-favored coastal ranges. Moist
    air (characterized by 1-1.1 inch PW values) will accompany the
    increasing flow and become forced over the Transverse Ranges,
    resulting in areas of orographically enhanced moderate to heavy
    rainfall. This process is already underway, with spots of 0.2-0.4
    inch/hr rain rates already observed west of Los Angeles in the
    past hour very near Malibu and Castaic. These trends are expected
    to continue, and a roughly 6-12 hour window of heavier rainfall
    potential will exist across the discussion area continuing into
    the overnight hours (perhaps through 12Z-15Z Friday).

    These areas of heavy rainfall will occur in areas of sensitivity
    from both terrain and burn scars from recent fires across the
    region. As a result, areas of flooding and debris flows are
    possible. Rainfall totals of 0.25-1 inch are probable through
    10Z, with locally higher amounts (exceeding 1.5 inches) possible
    in terrain-favored areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8xHNefkHYP3_lJgJJICRRL1GK8_LbVx7lSPiJ3pel_wzghsP-I4EeifkSzULBluoOydH= JBQwRntAtlaAIl5l-aQqq0E$ for graphic product...

    ATTN...WFO...HNX...LOX...SGX...VEF...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 35242052 35241936 35121841 34921756 34291731=20
    33971765 34001857 34512041 34842065=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Feb 13 08:17:57 2025
    AWUS01 KWNH 130817
    FFGMPD
    FLZ000-GAZ000-ALZ000-131345-

    Mesoscale Precipitation Discussion 0034
    NWS Weather Prediction Center College Park MD
    317 AM EST Thu Feb 13 2025

    Areas affected...FL Panhandle into southeastern AL and central GA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 130815Z - 131345Z

    SUMMARY...A low probability threat for flash flooding due to
    training will exist from the FL Panhandle into southeastern AL and
    central GA through ~13Z. The threat will carry the potential for
    rainfall rates in the 1-2 in/hr range within any areas of training.

    DISCUSSION...Radar imagery at 08Z showed that a SW to NE oriented
    axis of thunderstorms extended from the western FL Panhandle into
    north-central GA. These thunderstorms were located out ahead of a
    cold front and trends over the past few hours have shown a
    weakening of the portion of the line over southwestern AL in favor
    of strengthening of a new line out ahead, which was currently
    crossing the western FL Panhandle. Recent infrared satellite/radar
    trends through 08Z showed yet another line beginning to organize
    about ahead of the existing convective axis, ~85 miles south of
    Mobile Bay.

    The environment within the warm sector was characterized by 500 to
    1500 J/kg MLCAPE from the warm frontal position along the AL/GA
    border to just south of the Gulf Coast along the FL Panhandle.
    Flash flood guidance was lowest to the north (2-3 inches in 3
    hours) and highest in western FL (4+ inches in 3 hours). The
    greatest potential for high rainfall rates, near or even in excess
    of 2 in/hr, will exist within the better instability across
    southern locations.

    Water vapor imagery showed a longwave trough over the central U.S.
    advancing east, but with the base of the trough lifting north,
    from OK to the MS Valley. This deamplification along the southern
    end of the upper trough favors a gradual weakening trend of 850 mb
    wind magnitude and of convective intensity over the AL/GA/FL
    tri-state region. However, lingering instability and sufficient
    low level moisture transport could allow for training if the
    convective axis to the south continues to expand north and meets
    with the ongoing northern portion advancing to the east at a
    somewhat faster pace. While the general movement should be a
    progressive eastward movement at 25-30 kt, There is a low end
    chance that alignment of the heavy rain axis/axes will allow for a
    brief period of training, which could contain rainfall rates of
    1-2 in/hr, and local 2-3 inches of rain over a 2 to 3 hour window.
    Localized flash flooding could result, but again, this threat
    appears to be fairly low and recent CAM guidance does not support
    much in the way of a flash flood threat over the next 3-5 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7s8IP4xI0b1AYsqAUAimeiOmfPECkOXtCWqYtuKrqVX6k26DOppC74qbJEl_8Iojm-yn= PIyiCfeNtY13adK3mY0lnso$ for graphic product...

    ATTN...WFO...BMX...CAE...CHS...FFC...JAX...MOB...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 33618302 33498228 33078167 32528146 31768171=20
    30898320 30198408 29568500 30128734 31088690=20
    32538513 33028448 33508380=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Feb 13 17:27:35 2025
    AWUS01 KWNH 131726
    FFGMPD
    CAZ000-140300-

    Mesoscale Precipitation Discussion 0035
    NWS Weather Prediction Center College Park MD
    1225 PM EST Thu Feb 13 2025

    Areas affected...Coastal Central and Southern
    California...Foothills of Sierra Nevada...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 131730Z - 140300Z

    SUMMARY...Strong Cyclone and atypically broad Atmospheric River
    will have potential for .75"/hr rates and localized totals of 3-5"
    in favored orographic ascent. Flash flooding is likely, especially
    in lower FFG of Southern California. Significant flash flooding
    may be possible in/near fresh burn scars.=20

    DISCUSSION...GOES-W WV suite depicts a broad, fairly symmetric
    closed low just off the NW coast of California continuing to bowl
    ESE likely crossing the coastline much later tonight. This low is
    atypically deep with the 90th to 95th percentile, but in
    combination with fairly cold/stronger ridging downstream has
    resulted in an atypically broad subtropical moisture plume with
    1.25-1.5" total PWat values along upstream along/ahead of the
    height-falls and associated cold front. GOES-W Vis/IR suite
    denotes a stark cloud line with slightly anafrontal to the
    southeastward cold front and moisture surge. Within the thick
    stratus plume, 850-700mb flow is in the 50-65kt range and is
    currently orthogonal to the Santa Lucia and Diablo Ranges,
    presenting strong IVT/orographic convergence along the range.

    ...Central California/Sierra Nevada Foothills...
    The IVT values are 4-5 standard anomaly units above seasonal
    average and range about 700-900 kg/m/s. Rates have been slowly
    increasing, with 3hr totals reaching 1-1.25" but will likely
    increase with an additional .5-.75"/hr for maybe 1-2 hours as the
    plume shifts southeastward. Totals already have reached 3-4" in
    the Santa Cruz and northern Santa Lucia resulting in rapid stream
    rises and some localized reports of flash flooding. The
    additional 2-3" over the next few hours will likely result in
    spots of 4-6" totals and continue the flash flooding risk.=20=20

    Additionally, the plume has saturated the sub-cloud environment in
    the San Joaquin Valley to allow for rain to reach the ground as
    the core of the plume presses onshore. The warm front will press
    through to the foothills and help to increased the depth of
    orographic ascent resulting in spots of .75-1"/hr rates before
    becoming very heavy snow at or above 7000Kft. This will decrease
    with the passage of the plume/cold front and the flux will reduce
    accordingly resulting in scattered shallow convective cells and
    bands may aggravate the area given those steepening lapse rates,
    which may have intense but brief cores of heavy rainfall/small
    hail/graupel.

    ...Southern California...
    Unlike further north, there is precedent moist airmass in place
    across the California Bight/Channel Islands, surface to 700mb
    values are above normal and total PWats are in the 1-1.25" range.
    Currently, the warm front has progressed through the highest
    terrain of the Transverse Range and winds are veering slightly
    while increasing. This will allow for short-term increase in
    orographic ascent across the Transverse (particularly east) and
    Peninsular Ranges prior the main core of the AR/cold front later
    this evening. Rates of .25-.33"/hr will increase as winds slowly
    uptick from 15-20 to 30kts by 00z below 7500 Kft across the
    ranges. Spots of 1-1.5" are probable to pre-soak the windward
    facing topography.=20=20

    A few hours prior to 00z, the cold front and AR will round Cape
    Conception and winds will have solid veered profile with depth
    with 40-50kts of 850-700mb flow fairly orthogonal to the range. A
    few hi-Res CAMs suggest 100-250 J/kg may be present from slightly
    higher theta-E air in place allowing for a subtle but important
    uptick in vertical development that should result in .75"/hr rates
    with spotty potential of 1"/hr. The growing concern here, is
    while the plume is less orthogonal to the terrain the breadth of
    the AR will allow for increased duration of exposure to the higher
    flux. As such, below freezing levels, spots of 3-4" are probable
    across the western Transverse Range by 03z and likely to be
    similar toward the eastern and Peninsular Ranges thereafter. It
    is not out of the realm of possibility that spots of 5" are
    possible and heavy rainfall will extend to the coast with .5"/hr
    rates and totals over 1-1.5" resulting likely flash flooding
    conditions through the evening even for urban locations.=20=20

    This is of particular concern given recent burn scars are going to
    be less tolerable to any rates over .50"/hr let alone any
    potential crossings of .75-1"/hr. It is too early to be certain
    about any particular canyon/scar, but given hourly rates and
    overall totals there is a sizable possibility for significant
    flash flooding/debris flows in or near these scars and avoidance
    of this prone areas is strongly advised. Please keep close
    attention to local statements/warnings from WFO Los Angeles, state
    and local emergency managers. It is possible a subsequent
    targeted MPD may be required to address ongoing rainfall trends.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5Jo-Vnr9C7RceznyxJQj2mzaqf1eMMqjQu8gci3RUa33MtzZyNzLc3-bkHz0P8kSr9kP= RHKQXeh5NFj5hCkzyP5N6vM$ for graphic product...

    ATTN...WFO...HNX...LOX...MTR...SGX...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 39472072 39042072 38382025 37511965 37171934=20
    36811897 36291868 35631855 35491870 35611899=20
    36381942 37042017 37252083 36982108 36442068=20
    35832027 35381997 35141959 34871927 34721872=20
    34681829 34651797 34351744 34271688 33721646=20
    33041646 32571633 32541676 32521721 32761767=20
    32821887 33141955 33592012 34292057 35002087=20
    35632142 35912176 37062251 37762270 38112257=20
    38602206 39002160 39242125=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Feb 14 02:17:15 2025
    AWUS01 KWNH 140217
    FFGMPD
    CAZ000-141200-

    Mesoscale Precipitation Discussion 0036
    NWS Weather Prediction Center College Park MD
    916 PM EST Thu Feb 13 2025

    Areas affected...Coastal Southern California...Foothills of the
    SIerra

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 140200Z - 141200Z

    SUMMARY...The ongoing Atmospheric River event will continue into
    the early hours of Saturday, with the threat of .50-.75"+ hourly
    rainfall rates across portions of Southern California and into the
    western upslope of the Sierra. Flash flooding will remain likely
    across Southern California, especially across recent burn scar
    areas, and possible in the foothills of the Sierra. The flash
    flooding threat will be diminishing from west to east across
    Southern California after 0200 UTC as a cold front moves steadily
    east, but should perist to near 1200 UTC in the Sierra Foothills.

    DISCUSSION...The latest GOES-W satellite imagery shows the broad
    mid to upper level trof along the west coast pushing steadily
    inland. An axis of anomalous PW values..2 to 2.5+ standard
    deviations above the mean, and 850-700 mb moisture flux anomalies
    of 3 to 5+ standard deviations above the mean, will continue on
    the southeast side of this upper trof, along and ahead of the
    associated cold front pushing steadily eastward across Southern
    California this evening. Surface analysis at 0000 UTC indicates
    this front having pushed to the southeast of Santa Barbara and
    extending eastward just south of Sandburg and Edwards AFB.=20=20=20
    There is good consensus in the latest hi res guidance on the
    timing of the primary heavy rain areas in the vicinity of this=20
    front pushing across Southern California this evening. HREF
    neighborhood probabilities are high, 90%+, for hourly rain totals
    of .50"+/hr along and ahead of the front, but drop to generally
    less than 25% for 1"+/hr, reflective of the progressive nature of
    this front. This progression will lead to a sharp cutoff in the
    flash flood threat as the front passes. However, until this
    occurs, flash flooding will remain likely across Southern
    California, especially over recent burn scar regions.=20

    ..Foothills of the Sierra Nevada...
    While the primary anomalous PW axis will remain across Southern
    California this evening, persistent west southwesterly low level
    upslope flow level will continue to impact the foothills of the
    Sierra into early Saturday. HREF neighborhood probabilities for
    .50"+/hr rainfall amounts are not as high or continuous as areas
    across Southern California. but do depict potential for localized
    heavy amounts and the potential for flash flooding issues.=20
    Simulated hi res radars do show potential for cells to be much
    slower moving and train in the upslope regions of the Sierra. In
    areas of training, additional hourly amounts of .50-.75"+ and
    additional totals of 2-3" are possible through early Saturday
    morning.
    =20

    Oravec

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!89MFGru-sN9tQMcyudE5FAOdDpRlLChT9anMRUAZeQHCenuXZAVsnylGh7z6d0rV3Mh9= Cq58UMkl4T356xrp3V4SigM$ for graphic product...

    ATTN...WFO...HNX...LOX...PSR...SGX...STO...VEF...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 39932145 39242074 38191983 38101991 37181925=20
    36221856 35051825 34711787 34711774 34451696=20
    34351684 33951639 32951616 32321669 33011746=20
    33041754 33101769 33441803 33491825 33951871=20
    34411857 35511890 36741990 37352017 38572095=20
    39722147=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Feb 8 07:41:33 2025
    AWUS01 KWNH 080741
    FFGMPD
    VAZ000-WVZ000-OHZ000-KYZ000-081340-

    Mesoscale Precipitation Discussion 0027
    NWS Weather Prediction Center College Park MD
    240 AM EST Sat Feb 08 2025

    Areas affected...much of West Virginia and a small part of eastern
    Kentucky

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 080740Z - 081340Z

    Summary...At least minor/isolated runoff issues could develop in
    the next few hours as moderate rain moves in from central/northern
    Kentucky through 14Z.

    Discussion...Strong convergence on the nose of a 40-kt low-level
    jet over western Kentucky has aided in development of moderate
    rainfall generally along an axis from near Louisville to near the
    WV/KY border near Pikeville. Within this axis, the persistence of
    rainfall has allowed for MRMS-estimated areas of 0.10-0.30 inch/hr
    rain rates to materialize. The axis was also parallel to robust
    westerly flow aloft (supporting persistence), and recent radar
    mosaic imagery indicates upstream shower activity near the MS/OH
    River confluence poised to move through areas currently affected
    by moderate rainfall. The net result of this pattern is a fairly
    prolonged period of light to moderate rainfall eventually
    extending into West Virginia, with 0.75-1.25 inch rainfall totals
    expected through 14Z across the discussion area.

    Despite modest rain rates, soils are wet across the area from
    recent rainfall and FFG thresholds are 1) ~0.25 inch/hr and 2)
    less than 1 inch/3-hr across parts of the region (especially in
    hillier terrain in eastern WV). These thresholds and recent flash
    flood events suggest that ground conditions are extremely
    sensitive. The moderate rainfall moving in from Kentucky should
    persist for several hours, resulting in at least isolated
    instances of excessive runoff/flooding. The uptick in flood risk
    should persist in the 0830Z-1400Z timeframe and beyond as
    low-level convergence strengthens across the area through the day.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_gr4qwKw5K5jYf9hzwSVfd5OU0gHU4AZ65N0702g3mo6SY0OyiHomCv70lD39JquYytq= XuS7c2SyHio4hQsMcSo5XK8$ for graphic product...

    ATTN...WFO...ILN...JKL...LWX...PBZ...RLX...RNK...

    ATTN...RFC...MARFC...OHRFC...NWC...

    LAT...LON 39108015 39037954 38687946 38157973 37708021=20
    37518090 37498204 37568309 38528343 38888208=20
    38988118=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Feb 15 07:22:34 2025
    AWUS01 KWNH 150722
    FFGMPD
    TNZ000-KYZ000-ILZ000-MOZ000-ARZ000-151315-

    Mesoscale Precipitation Discussion 0037
    NWS Weather Prediction Center College Park MD
    220 AM EST Sat Feb 15 2025

    Areas affected...northeastern AR across MS Valley into KY and TN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 150717Z - 151315Z

    SUMMARY...The threat for flash flooding will steadily increase
    over the next 3-6 hours from northeastern AR, across the MS Valley
    and into KY and TN. Training and repeating rounds of rain will
    produce peak hourly rainfall of 0.5 to 1.5 inches and 6 hour
    totals of 1 to 2 inches, locally as high as 3 inches.

    DISCUSSION...Scattered showers and elevated thunderstorms were
    observed to be increasing in coverage over portions of the lower
    and middle MS Valleys in association with strong low level warm
    air advection. 850 mb winds were from the S to SW, peaking around
    70 kt in southern MO (per VAD wind data). Layered PW imagery
    showed the rapid northward return of moisture from the eastern
    half of TX into the lower MS Valley (surface to 700 mb layers),
    allowing for the swift development of MUCAPE from west to east as
    dewpoints in the lower layers of the troposphere increase,
    allowing parcels to make use of relatively steep 700-500 mb lapse
    rates (6-7 C/km).

    Regional radar imagery at 07Z showed a persistent region of
    elevated convection from northeastern AR into northwestern TN,
    co-located with an axis of moisture flux convergence located at
    the leading edge of low level moisture return. Alignment of this
    axis and the mean steering flow from the WSW has caused training
    and repeating rounds of heavy rain to affect portions of
    northeastern AR into far northwestern TN. Local Wunderground
    rainfall network observations have shown 0.3 to 0.6 inches of rain
    within 30 minutes and one report as high as 0.7 inches in 30
    minutes, just south of the MO Bootheel from ~06Z.

    Expectations are for continued low level warm air advection to
    maintain the trend of increasing MUCAPE values toward the east,
    supporting elevated thunderstorms into central KY/TN later this
    morning. RAP forecasts indicate little latitudinal movement of the
    elevated zone of low level convergence over the next several hours
    and additional upstream development is anticipated over AR in the
    12-15Z window as forcing for ascent increases ahead of an
    approaching shortwave trough axis which extended from the central
    High Plains into the Desert Southwest at 07Z. Repeating rounds of
    showers and thunderstorms will continue through the morning with
    periodic episodes of training which will translate into locally
    high rainfall rates.

    Soil moisture across a large portion of the region is above
    average due to recent rainfall and/or snow melt. As a result, FFG
    values are low, with less than 2 inches in 3 hours along the KY/TN
    border and less than 2.5 inches in 3 hours closer to the MS River.
    While this MPD is tagged with flash flooding "possible", the
    threat is only expected to increase over the region during the
    daytime hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_LKzuenuFE5n5GFxs7T9W29CMESBylqN1j8oHhWN0qhcWfw7cdPyRqwFnLJlnpYxzdkU= PZuwZc4Uo9CGdNvPzJ_r8YM$ for graphic product...

    ATTN...WFO...JKL...LMK...LZK...MEG...MRX...OHX...PAH...SGF...

    ATTN...RFC...ABRFC...LMRFC...OHRFC...NWC...

    LAT...LON 37398765 37278539 36858434 36188435 35808534=20
    35518752 35158996 34769206 35459269 36329152=20
    37068991=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Feb 9 02:06:44 2025
    AWUS01 KWNH 090206
    FFGMPD
    VAZ000-WVZ000-OHZ000-KYZ000-090804-

    Mesoscale Precipitation Discussion 0028
    NWS Weather Prediction Center College Park MD
    906 PM EST Sat Feb 08 2025

    Areas affected...southern West Virginia, far eastern Kentucky

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 090204Z - 090804Z

    Summary...Fast-moving showers could produce a quick 0.25 inch of
    rainfall across the discussion area through 05-06Z. Extremely
    sensitive ground conditions suggest potential for
    efficient/excessive runoff and impacts during this timeframe.

    Discussion...Forcing/ascent along and ahead of a cold front has
    aided in development of a couple bands of convection extending
    from Parkersburg to Huntington to Somerset, KY. These showers
    were in a marginal environment in terms of instability, although
    ~100 J/kg MUCAPE appears to support updrafts along and ahead of
    the front. Quick movement (from 70 kt mean steering flow) has
    limited rain rates so far, although recent MRMS data suggests
    pockets of 0.1-0.2 inch/hr rates near Jackson, KY over the past
    hour.

    These showers will move toward portions of the discussion area
    that are extremely sensitive to any additional rainfall. NASA
    SPORT soil moisture values are near 100% across the area amid
    plenty of antecedent rainfall (including 1-1.5 inch totals in the
    past 24 hours). FFG thresholds generally range from 0.25-0.5
    inch/hr, but are near zero in a few spots. Several impacts were
    also reported this from this morning's round of rainfall.=20
    Incoming rainfall along/ahead of the front may result in an uptick
    in excessive runoff and flood potential through 07Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6CEl1e3dRVBZoJxLJsa61bKoSMJFD78rTxWcNS0IlUX6QYExwTPlGoyKjjoYiqi6dcik= Vqkxvao6vBmbl3PUftyaBpo$ for graphic product...

    ATTN...WFO...JKL...LWX...PBZ...RLX...RNK...

    ATTN...RFC...MARFC...OHRFC...NWC...

    LAT...LON 39258120 39198015 38957938 38497951 37768007=20
    37438073 37308138 37478217 38198265 38988194=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Feb 15 13:34:02 2025
    AWUS01 KWNH 151332
    FFGMPD
    VAZ000-WVZ000-TNZ000-KYZ000-INZ000-MSZ000-MOZ000-ARZ000-151930-

    Mesoscale Precipitation Discussion 0038
    NWS Weather Prediction Center College Park MD
    830 AM EST Sat Feb 15 2025

    Areas affected...Portions of the OH/TN Valleys and Mid-South

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 151330Z - 151930Z

    SUMMARY...An expansive axis of heavy showers and thunderstorms
    with strong cell-training concerns will be promoting a widespread
    flash flood threat over the next several hours across portions of
    the OH/TN Valley region and Mid-South.

    DISCUSSION...The latest GOES-E IR satellite imagery shows an
    expansive areas of heavy shower and thunderstorm activity
    impacting areas of eastern AR up across central and western TN and
    much of central and southern KY. Light to moderate stratiform
    rains are noted north of here closer to the OH River and also into
    the central Appalachians.

    The convection that is organizing is associated with strong warm
    air advection which is being aided by a powerful southwest
    low-level jet of 50 to 60+ kts overrunning a strong frontal zone.
    This is driving very strong moisture transport which is showing up
    in an impressive fashion with the experimental CIRA-LVT (Layered
    Vapor Transport) imagery as it is depicting SFC/850 layer LVT
    magnitudes of 300+ kg/m/s. Meanwhile, a nose of MUCAPE values on
    the order of 500 to 1000 J/kg is now oriented up across central to
    northeast AR through western TN and western KY and this is helping
    to facilitate the broader axis of elevated convection.

    Over the next several hours, very strong warm air advection and
    moisture transport will continue to support organizing bands of
    convection that will be aligned with the deeper layer mean flow
    and thus will be conducive for a substantial level of
    cell-training. Increasing CAPE values with time along with
    strengthening shear profiles will support stronger convective
    elements that will yield increasingly heavy rainfall rates.

    Rainfall rates with the stronger storms may reach as high as 1 to
    1.5 inches/hour at least going through midday, but with
    significant cell-training concerns, this may result in some
    rainfall amounts by early afternoon alone of 2 to 4 inches. The
    latest CAM guidance suggests areas of western/northern TN through
    southern KY will have the heaviest totals going through the 18Z to
    20Z time frame, with somewhat lesser amounts farther north.

    Given the extremely sensitive/saturated soil conditions and
    already elevated streamflows for many locations, these rainfall
    totals over the next several hours are likely to begin resulting
    in widespread flash flooding. Additional MPDs will be issued this
    afternoon to update what should evolve into a high-impact and
    life-threatening flash flood event in time.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9YBX9aJ4KgA8Z4iKzzTmNqcBfe8AW-uZDjSAoMlL6IbG7HtnQ7qDKHisENvc779BvUjO= SUH7voR82zaHIzanXz9Ys10$ for graphic product...

    ATTN...WFO...JKL...LMK...LZK...MEG...MRX...OHX...PAH...RLX...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 38438386 37938214 36958191 36258289 35938480=20
    35578763 34359122 34619187 35219176 36318988=20
    37208813 38008597=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Feb 23 07:54:43 2025
    AWUS01 KWNH 230754
    FFGMPD
    IDZ000-CAZ000-ORZ000-WAZ000-231800-

    Mesoscale Precipitation Discussion 0049
    NWS Weather Prediction Center College Park MD
    253 AM EST Sun Feb 23 2025

    Areas affected...Coastal and Cascade Ranges of S WA, OR & Far
    Northwest CA & E WA/SE OR/N ID...

    Concerning...Heavy rainfall

    Valid 230800Z - 231800Z

    SUMMARY...Prolonged AR continues but very broad plume of moisture
    will start to focus ahead of next stronger cyclone/frontal push
    toward 18z. Deep moisture surges through the Columbia Plateau
    into E WA/N ID prepping the soils/increasing run-off ahead of next
    surge.

    DISCUSSION...GOES-W WV suite shows broad cirrus canopy associated
    with polar jet streak and deep atmospheric river extending from
    the eastern Pacific across W WA into S British Columbia into the
    entrance of the core jet streak that is about 150-160kts. The weakening/initial low level cyclone has occluded northward into
    the central BC coastal region with the front extending southward
    into/near the Cascade Range, while the warm front extends through
    the Columbia River Valley. CIRA LPW, particularly the sfc-850mb
    layer bares this evolution out very well with the cold front
    starting to sag/stall SW to NE just across the W WA angling back
    toward the next approaching stronger wave out near 150W. The
    plume remains very broad/wide from the W WA coast to the
    Lost/Redwood coast of northwest California with a solid slug of
    850-500mb centered on the NW Oregon coast extending back toward
    37-38N and 140W; both layers showing associated moisture flux
    values running well into 99th percentile for the 20 year record.=20
    As such, 1.25" TPW values intersect much of the coastline with
    weakly confluent 850-700mb flow angled from the SW about 30
    degrees off perpendicular, but given the depth has washed over the
    coastal range to to the Cascades. Still, within a broad ascent
    pattern in the exiting right entrance pattern provides a
    continuation of moderate rainfall rates of .25-.3"/hr, slowly
    reducing from north to south across the WA Cascades through the
    early morning (but remaining solid further south across OR). This
    should result in 2-4" totals across the coastal and Cascade ranges
    of Oregon to 18z; with 1.5-2.5" across WA early through 15z.

    ...Eastern Washington/N Idaho...
    As noted above, the broad plume is broad and deep enough to wash
    over the coastal range and has begun to fill the Columbia river
    Valley into the Plateau region. IVT values of 300-400 kg/m/s will
    increase to near 500-600 kg/m/s along 30-45kts of gap flow through
    the Plateau into the foothills and eventually higher terrain of SW
    WA/NE OR and then toward the Clearwater Range by 12z. Total PWat
    values are starting to increase above .75" which would place 90+th
    percentile moisture for the date at OTX and GFS/ECMWF flux values
    at 3-5 standard anomaly values across the area. While total
    moisture is much less than coastal positions, rates of .15-.2" may
    occasionally reach .25"/hr with steadily increasing freezing
    levels with all but the highest peaks along the ID/MT boarder and
    further south across the Blue/Wallowa and Salmon River Ranges
    likely to experience more rain than snow/wintry mix. As such
    spots of 1-2" totals are expected by 18z. Given the rates are low
    and prolonged, this will more likely pre-soak the soils with
    slowly increasing run-off values with this particular surge of
    moisture...but there is more to come that may be more likely to
    result in localized flooding concerns.

    ...Southwest Oregon/Northwest California...
    As the jet streak exits the broader wave of deep moisture will
    remained focused across much of OR into NW CA. As the trailing
    edge to the prior forcing backs ahead of the next stronger
    approaching shortwave/developing low level cyclone/pressure trough
    toward 18z, westerly winds will increase into the 45-50kt range
    becoming ever so slightly more orthogonal to the boreal rain
    forests of SW OR/NW CA. IVT values over 700 kg/m/s combined with
    slightly steeper orography will allow for rain-rates to exceed
    .5"/hr, occasionally reaching .75"/hr starting around 09-10z.=20
    This will be prolonged for about 6-9hrs and potentially result in
    localized spots of 4-6". This is not atypical for these
    rain-forests but still strong enough for increased run-off and low
    end flooding potential before the core of the narrowing AR plume
    starts to shift northward with strengthening warm air advection
    after 15z.=20

    There will remain some timing/uncertainty to the width of the core
    of the heavy rainfall surge toward 18z and a subsequent MPD will
    be required at that time to provide additional details for the
    main surge of heaviest rainfall/highest impacts to this longer
    duration AR event.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7owdNXCQ66se1jmlJbzZ-zMyLYjnzALvV8uQUYrQ9mpQtR3nsZjcZBrTRdwd0abJF_5m= 4ApWn2jy_KJ6iZZehzfp6xA$ for graphic product...

    ATTN...WFO...EKA...MFR...MSO...OTX...PDT...PQR...SEW...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 48291746 48071637 47651595 46901558 46161514=20
    45641539 45411657 45271772 45431937 45052090=20
    44302149 42912179 42092223 41482268 40702308=20
    40742421 41462419 42772465 43782437 44932423=20
    45852415 46742425 47082388 46662330 46602249=20
    47772185 47952108 46582112 46142070 46221911=20
    47281863 47891828=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Feb 22 20:21:35 2025
    AWUS01 KWNH 222021
    FFGMPD
    CAZ000-ORZ000-WAZ000-230820-

    Mesoscale Precipitation Discussion 0048
    NWS Weather Prediction Center College Park MD
    320 PM EST Sat Feb 22 2025

    Areas affected...Pacific Northwest

    Concerning...Heavy rainfall

    Valid 222020Z - 230820Z

    SUMMARY...Atmospheric river conditions arriving across the Pacific
    Northwest will bring heavy rainfall in across the coastal ranges
    and into the windward slopes of the Cascades later today and
    tonight.

    DISCUSSION...A series of offshore shortwave impulses lifting
    northeastward toward British Columbia over the next 6 to 12 hours
    will be bringing an offshore frontal system toward the coastal
    ranges of western WA and western OR along with strong atmospheric
    river conditions.

    The latest GOES-W WV suite along with CIRA-ALPW and experimental
    LVT data shows a very well-defined trans-Pacific fetch of deep
    moisture extending from just offshore of the Pacific Northwest
    southwestward all the way down to northwest of Hawaii with notable
    tropical origins of some of the moisture transport. Multiple
    low-amplitude shortwave impulses are embedded within this
    atmospheric river channel, and this will help to facilitate strong
    warm air advection and onshore flow into especially the coastal
    ranges of western WA and western OR along with the windward slopes
    of the Cascades by later today and continuing into the overnight
    period that will drive locally enhanced rainfall amounts.

    PW anomalies are forecast to rise to 2 to 3+ standard deviations
    above the climatological mean by 00Z and continue at this level
    through tonight as a strong southwest low to mid-level jet sets up
    and persists just offshore and overruns the higher terrain of the
    Pacific Northwest. In fact, the 850/700mb moisture flux anomalies
    are forecast to rise to as much as 3 to 5+ standard deviations
    above normal, with one peak this evening by around 00Z and then
    another later tonight as the arrival of each shortwave impulse
    corresponds to a stronger low to mid-level wind field.

    Given the enhanced deep layer warm air advection and moisture
    transport along with some of its tropical origin, the rainfall
    rates are expected to be efficiently high. The 12Z HREF guidance
    shows high probabilities of seeing 0.50" to 0.75"/hour rainfall
    rates across the Olympic Peninsula in the 21Z to 00Z time frame,
    with portions of the southwest WA coastal range also seeing
    elevated probabilities of these rates toward early this evening.
    Areas farther east into the windward slopes of the Cascades and
    farther south across coastal OR and gradually coastal northwest CA
    should see rates easily reach into the 0.25" to 0.50"/hour range
    with rates occasionally over a 0.50"/hour.

    Over the next 12 hours, some rainfall totals are expected to reach
    as high as 3 to 5+ inches over the higher terrain and especially
    the favored coastal ranges and upslope areas of the Cascades with
    lesser amounts over the adjacent interior valleys/terrain-shadowed
    locations. Generally these initial rains are not likely to cause
    much in the way of any flooding threat aside from potentially some
    localized urban and small stream runoff concerns where the heavier
    and more persistent rates set up. However, additional heavy
    rainfall beyond this period going into Sunday will gradually raise
    the flooding threat.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Bcn8atyisx4Hf-E9XQot4K2cLaj04bBNcljUCuWosTXrq0j5Uxuq4UDLpO2N8fDN-3m= XFr0k6riV0DfUzAGFmmzU_c$ for graphic product...

    ATTN...WFO...EKA...MFR...OTX...PDT...PQR...SEW...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 49162120 48902067 48122052 47472075 47002120=20
    46402119 45762157 45192153 44712176 44052168=20
    43342208 42402211 42282262 42932320 42792371=20
    42262360 41472341 40742345 40022393 40282454=20
    41532441 43062470 44952423 46622433 47972464=20
    48332411 48092348 47562304 47682238 48692234=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Feb 23 18:27:33 2025
    AWUS01 KWNH 231827
    FFGMPD
    CAZ000-ORZ000-WAZ000-240625-

    Mesoscale Precipitation Discussion 0050
    NWS Weather Prediction Center College Park MD
    125 PM EST Sun Feb 23 2025

    Areas affected...Pacific Northwest

    Concerning...Heavy rainfall

    Valid 231825Z - 240625Z

    SUMMARY...An atmospheric river resurgence this afternoon and
    evening will bring a new round of heavy rainfall to the Pacific
    Northwest and especially for the coastal ranges and windward
    slopes of the Cascades.

    DISCUSSION...The latest GOES-W WV suite shows a negatively tilted
    upper-level trough in between 40-50N and approaching 130W with an
    occluded low center near 48N 142W. This energy will gradually
    advance off to the northeast toward the Pacific Northwest and
    British Columbia over the next 6 to 12 hours which will bring a
    resurgence of stronger atmospheric river conditions back across
    the region this afternoon through this evening.

    A warm front that is currently oriented west to east across the
    Columbia River basin will lift back northward with time as a
    strong low to mid-level jet surges northeastward ahead of the
    approaching offshore surface low and upper-level trough axis. This
    will bring a resurgence of strong warm air advection and moisture
    transport into the coastal ranges from far northwest CA up across
    western OR and western WA through this evening.

    IVT magnitudes are already increasing again across coastal
    northwest CA and much of western OR and will be well into the 600
    to 800+ kg/m/s range this afternoon through early this evening as
    the offshore cold front approaches the region. These IVT values
    will increase up across western WA as well, with magnitudes here
    generally rising back as high as 400 to 600 kg/m/s.

    PW anomalies of 2 to 3+ standard deviations above normal are
    forecast through this evening ahead of the cold front and this
    coupled with 850/700 mb moisture flux anomalies of 3 to 5+
    standard deviations above normal should favor rainfall rates
    reaching as high as 0.50" to 0.75"/hour. The heaviest rates should
    tend to be focused across the OR coastal ranges and there is some
    low-end potential for rates to even approach 1.0"/hour with
    arrival of the strongest IVT parameters and forcing later this
    afternoon. Enhanced IVT spillover into the windward slopes of the
    Cascades should support at least spotty areas of a 0.50" to
    0.75"/hour rates here, but the rates overall should tend to be
    somewhat more modest farther north into western WA with lower IVT
    values and lower PWs by comparison to western OR.

    A cold front will advance inland by late this evening and this
    will then allow for another break in the overall atmospheric
    regime with rates once again then coming back down. However, at
    least over the next 6 to 12 hours, expect additional rainfall
    amounts of as much as 2 to 4 inches for western OR and 1 to 3
    inches for western WA. These rains may bring additional concerns
    regionally for runoff problems including small stream and urban
    flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!93hHJZr0qetLo277TEuzyb-znKxZjhbG7rVHDOjABuldxUbC_x0FdY6w5DyCIQ6HRfAU= tj3FZEQvAuW0v1Bzdcj-ImY$ for graphic product...

    ATTN...WFO...EKA...MFR...OTX...PDT...PQR...SEW...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 49162120 48902067 48362056 47722062 47212097=20
    46512092 46222066 45892047 45722076 45502126=20
    45052150 44542152 43992163 43622194 42852201=20
    42442228 42462303 42222342 41652354 41792441=20
    43062470 44172437 46192417 47572457 48052414=20
    48012332 47762313 47512270 47632198 48432212=20
    49032186=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Feb 24 20:25:36 2025
    AWUS01 KWNH 242025
    FFGMPD
    ORZ000-WAZ000-250815-

    Mesoscale Precipitation Discussion 0051
    NWS Weather Prediction Center College Park MD
    324 PM EST Mon Feb 24 2025

    Areas affected...WA/OR Coastal Ranges into Cascades

    Concerning...Heavy rainfall

    Valid 242022Z - 250815Z

    SUMMARY...Areas of heavy rain will return to the WA and OR Coastal
    Ranges and downstream into the Cascades later today/tonight. While
    peak rainfall rates may reach/exceed 0.5 in/hr on an isolated
    basis, they are much more likely to remain in the 0.2 to 0.4 in/hr
    range. 12 hour rainfall of 1-2 inches, locally 3+ inches, is
    expected through 08Z.

    DISCUSSION...GOES West water vapor imagery at 20Z showed a
    well-defined closed low centered just west of 130W near 45N. This
    upper low had been strengthening this morning but appears to be
    nearing maturity. At the surface, an occluded cyclone was depicted
    through visible satellite imagery with the WPC 18Z surface
    analysis showing a central pressure of 978 mb and this intensity
    is likely close to peak strength. The triple point was located
    just near the mouth of the Columbia River and what is left of an
    earlier axis of warm advection precipitation was lifting north
    through central WA. Meanwhile, radar imagery showed a band of
    rain, associated with the approaching cold front, moving just past
    the Willamette Valley into the Cascades. The diffluent left exit
    region of a mid-upper level jet streak was also located over the
    lower Columbia River Valley, likely enhancing lift and enhancing
    precipitation intensity.

    Short term forecasts from the RAP suggest the closed low will
    maintain a similar intensity through about 03Z prior to filling as
    it moves toward southern Vancouver Island. The cold frontal band
    will continue to steadily move inland through 00Z, followed by a
    lull in precipitation intensity outside of instability driven
    showers due to steepening mid-level lapse rates tied to the
    approach of the closed low aloft. RAP forecasts show MLCAPE up to
    ~500 J/kg along the OR coast through the early overnight.

    As the deep low level low nears the coast, a period of strong 850
    mb onshore flow is expected to be directed into the coast of
    northern OR into southern WA, with 850 mb wind speeds of 70-80 kt
    in the 03-09Z time frame from the SW to WSW. While snow levels
    will be dropping to ~3500 ft behind the cold front across the
    Pacific Northwest, the u-component of the 850 mb wind will be
    60-70 kt into the Coastal Ranges and 30-45 kt into the Cascades
    with a strong orographic component and steady rainfall of 0.2 to
    0.4 in/hr, locally up to 0.5 in/hr possible.

    While rainfall rates will not be exceptionally high, the addition
    of 1 to 2 more inches, perhaps as high as 3 inches through 08Z, is
    expected. Due to widespread 3 to 6 inch rainfall totals across the
    region over the past 48 hours, additional rainfall may bring
    additional localized concerns for runoff problems including small
    stream and urban flooding.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!55bhW1vo4IQzGsDuIMw_NE5Diu18eoFsJYr2p46l6W9gZLhpJIff3SS_BrqRHC7dYc7W= TAHvAhW86MrVVwQRIVZuG1s$ for graphic product...

    ATTN...WFO...PQR...SEW...

    ATTN...RFC...NWRFC...NWC...

    LAT...LON 47912425 47842399 47612365 47572333 47602310=20
    47032293 46942263 47022225 46962195 46652177=20
    46332188 45982181 45652168 45362178 44972186=20
    44622201 44442224 44442248 44492262 44712279=20
    44852288 44902310 44862327 44742334 44652339=20
    44492349 44402379 44472410 44582428 44962430=20
    45732423 46472429 47062450 47622455 47802452=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Feb 25 07:50:55 2025
    AWUS01 KWNH 250750
    FFGMPD
    ORZ000-WAZ000-252000-

    Mesoscale Precipitation Discussion 0052
    NWS Weather Prediction Center College Park MD
    250 AM EST Tue Feb 25 2025

    Areas affected...Lower Foothills of Western Washington & Far
    Northwest Oregon...

    Concerning...Heavy rainfall

    Valid 250800Z - 252000Z

    SUMMARY...Reducing rainfall rates to .25-.3"/hr and spots of
    additional 2-3" adds to streamflows/ongoing river flooding within
    western facing foothills of Cascades/Olympics, as well as much of
    the Coastal Range.

    DISCUSSION...GOES-W WV shows an textbook symmetric deep layer
    fairly broad cyclone just west of the entrance to the Juan de Fuca
    strait, which is accompanied by a sub 985mb surface low. While
    the cyclone is starting to fill well past peak maturity, a subtle
    lobe of vorticity and associated jet streak is rounding the base
    of the cyclone resulting in broadening diffluent/divergent
    downstream flow across W WA increasing westerly surface to 700mb
    flow. Given onshore surface winds are gusting over 50 mph that
    increase to 70kts by 700mb slowly veering from WSW to W over the
    next few hours, is solidly orthogonal to the SW slopes of the
    Olympics and while moisture is limited due to the deep cold air
    through depth, total PWats of .75" and the strength of winds will
    continue to result in solid rainfall rates of .25 to .3"/hr in the
    lower slopes before the freezing levels about 3Kft.=20

    The upper-low will continue to spin down but approach the coastal
    range maintaining the strong moisture flux with very slow
    reduction with the winds. The Willapa Hills will take the
    greatest brunt of flux closer to the track of the low and best
    orthogonal flow to support .25-.3"/hr for about 9-12 hours which
    will allow for an additional 2-3"+ though spots along the NW
    Oregon Coastal Range in Clatsop and Tillamook counties will see
    slightly reduced rates, but still potent for 1-2.5" totals. Given
    soil conditions are already nearly fully saturated per NASA SPoRT
    LIS product suggesting 85-95% saturation through 40cm, most will
    continue to run off and maintain already increased stream rates
    and flooding conditions in downstream rivers, yet rates are not
    likely to result in rapid rises.

    Downstream into the Cascades, the slopes increase rapidly with
    only limited areas of the lower foothills below freezing levels,
    with much of the moisture above to fall as snow. Still, similar
    1-3" totals in the lower foothills extend mainly north of the
    Columbia river in the Washington Cascades with best rates up to
    .25"/hr likely as the core of the upper-level low crosses later
    this morning into early afternoon (15-20z), ending the prolonged
    atmospheric river event.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6ptxx-izneKiuT-T8bFrjZRyS9DoqHxEXlQ07Odyat_BSgRIPD4ILhc2sCWd-4sVOrHW= _qSY2GUrh7Sqs3iNsogBibM$ for graphic product...

    ATTN...WFO...PQR...SEW...

    ATTN...RFC...NWRFC...NWC...

    LAT...LON 48942200 48742184 48432150 47742151 47592157=20
    47042186 46692232 46322237 46232248 46172269=20
    45992307 45572326 44912345 44722383 45082410=20
    46302409 47572444 48352474 48232423 47882394=20
    47502371 47432326 46852323 46682282 46812275=20
    47032231 47492197 48092192 48412207 48792219=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 9 09:21:36 2025
    AWUS01 KWNH 090921
    FFGMPD
    FLZ000-GAZ000-ALZ000-091520-

    Mesoscale Precipitation Discussion 0053
    NWS Weather Prediction Center College Park MD
    520 AM EDT Sun Mar 09 2025

    Areas affected...Far Southern GA...FL Panhandle into Northern FL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 090920Z - 091520Z

    SUMMARY...Locally training clusters of heavy showers and
    thunderstorms this morning may result in isolated areas of flash
    flooding.

    DISCUSSION...The latest GOES-E IR satellite imagery along with
    dual-pol radar shows clusters of heavy showers and thunderstorms
    gradually expanding in coverage across portions of the central and
    eastern Gulf Coast region as southerly warm air advection and
    moisture transport interacts with a quasi-stationary front
    extending east from a wave of low pressure just east of New
    Orleans, LA. A modest low-level jet of 20 to 30+ kts is focused
    out ahead of this low pressure wave, with the primary nose of this
    situated up into the FL Panhandle region where PWs are gradually
    increasing along with instability.

    MIMIC-PW data shows the pooling of 1.5 to 1.75 inch PWs currently
    near the central Gulf Coast with the latest RAP analysis showing
    MUCAPE values of 500 to 1000+ J/kg. However, the 3-hour MUCAPE
    differentials are on the order of +400 to +600 J/kg across far
    southern AL through the western part of the FL Panhandle and this
    is where some of the more organized clusters of convection have
    been developing over the last couple of hours.

    As a positively-tilted mid-level trough and associated closed low
    continues to eject east out of the southern Plains and toward the
    Lower MS Valley this morning, there will be a gradual increase in
    downstream upper-level divergence along with a corresponding
    subtle increase in the low-level jet. This coupled with proximity
    of the front across especially the FL Panhandle vicinity should
    help facilitate a further expansion and organization of convection
    in a general west to east fashion which will bring a concerns for
    locally training showers and thunderstorms.

    The HRRR has been generally trending wetter over its last few
    model runs, and the HRRR coupled with the 00Z NSSL-MPAS guidance
    support rainfall rates of 1 to 2 inches/hour, with sufficient
    levels of cell-training to generate totals of as much as 3 to 5
    inches by late this morning. These rains will be falling over
    areas that are relatively dry based off the latest NASA SPoRT soil
    moisture data, but given some of the wetter model trends overnight
    along with the latest radar and satellite data, it will be
    possible that enough rain falls this morning for some isolated
    areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7cN8Er7gbxvXCCMp6l_QuyuQC4cX6fjOzVtsEC9BrtCMgIaUDHU75Hlm2yR0n6uZcY5p= jO9Ed7vKZG3lOUDkT_h6eM8$ for graphic product...

    ATTN...WFO...JAX...MOB...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 31198337 31148199 30858134 30458130 30138148=20
    30008205 29898300 29848401 29668506 29908550=20
    30268609 30308699 30608721 30878690 31038587=20
    31088475=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 9 15:34:07 2025
    AWUS01 KWNH 091534
    FFGMPD
    FLZ000-GAZ000-ALZ000-092132-

    Mesoscale Precipitation Discussion 0054
    NWS Weather Prediction Center College Park MD
    1133 AM EDT Sun Mar 09 2025

    Areas affected...portions of north Florida/Florida Panhandle and
    southern Georgia

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 091532Z - 092132Z

    Summary...Flash flood potential should continue through 21Z/5p EDT
    today as showers and thunderstorms repeat over areas that have
    received 1-2.5 inches of recent rainfall.

    Discussion...The flash flood risk across northern Florida and
    adjacent areas of southern Georgia continues. Latest radar mosaic
    imagery indicates scattered coverage of thunderstorms moving from
    west to east along an axis extending from near Pensacola to near
    Jacksonville. This axis is collocated with a nearly stationary
    baroclinic zone, with localized ascent along that axis occurring
    along the nose of 25-30 knot low-level jet centered over the
    north-central Gulf just southeast of New Orleans. Flow aloft
    remains parallel to the axes of convergence/heaviest rainfall,
    supporting continued training/repeating convective activity.=20
    Moist thermodynamic profiles (1.5+ inch PW) and elevated
    instability (around 1000 J/kg MUCAPE) continue to support robust
    updrafts with local rain rates of 1-2 inches/hr at times beneath
    training convection.

    The ongoing meso-to-synoptic scale pattern supporting heavy rain
    is expected to persist through at least 21Z today. Some question
    exists regarding convective coverage given slight ridging aloft
    ahead of a positive tilt mid-level wave centered over northeast
    Texas, although general consensus (supported by models and
    observations) is that enough convective coverage will continue to
    foster training and occasional 1-2 inch/hr rain rates. Some of
    these rates will fall on wet soils from prior rainfall over the
    last 3-6 hours, promoting localized runoff. Localized totals
    exceeding 3 inches through 21Z cannot be ruled out.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9veAP3tFSullh2E8hoKhzT9euHwmG4wO47cksP5TLNtUOWzbVzVBVgWg_cmH-SvF-0TY= 1W2gmBPKbK-f1DuzgWUk08Q$ for graphic product...

    ATTN...WFO...JAX...MOB...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 31488330 30958141 29928135 29718329 29818531=20
    30188715 30888635=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 9 21:35:44 2025
    AWUS01 KWNH 092135
    FFGMPD
    FLZ000-GAZ000-100334-

    Mesoscale Precipitation Discussion 0055
    NWS Weather Prediction Center College Park MD
    535 PM EDT Sun Mar 09 2025

    Areas affected...northern Florida and far southern Georgia

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 092134Z - 100334Z

    Summary...Scattered convection continues to pose an isolated flash
    flood threat while migrating eastward across the discussion area.=20
    Another 1-3 inches of rainfall are possible through 03Z/11p EST
    tonight.

    Discussion...Over the past couple hours, a gradual uptick in
    convective coverage has been noted across the western and central
    Florida Panhandle. This increase in convective coverage is likely
    tied to a few factors, including: 1) subtle geopotential height
    falls ahead of an advancing mid-level wave near the ArkLaTex, 2)
    the inland advection of warm/moist air that can support more
    surface-based convection, and 3) continued convergence on the nose
    of 30-kt southwesterly low-level flow over the central Gulf. The
    increase in coverage along with modest training/repeating has
    resulted in a few areas of 3 inch rainfall totals since 15Z, with
    much of that tally happening in a 2-hour window. Rainfall was
    wetting soils and resulting in lower FFG thresholds especially in
    and north of the I-10 corridor in the central Florida Panhandle
    (near the Tallahassee area). These factors suggest an uptick in
    flash flood potential in the short term.

    The meso-to-synoptic scenario should continue to foster areas of
    heavy rainfall through 03Z. Deep moist convergence should remain
    focused along the Florida Panhandle for the next 3-6 hours as
    forcing for ascent associated with the mid-level wave approaches
    the region. Additional convection should migrate eastward into
    southeastern Georgia and northeastern Florida over time.=20
    Localized 3 inch totals through 03Z remain possible beneath
    training/repeating convective axes. Isolated instances of flash
    flooding are expected as a result.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_pKdQfdqHQpCQEiJRYXMfLh5ME0F9tG0zNqyX7FtHfalbr71_61zH2ofmEpr8FlJPm3T= b4NWA5vtjXA2crJClLNNs-Y$ for graphic product...

    ATTN...WFO...JAX...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 31318282 30958161 29748222 29658522 29978586=20
    30658635 30988469=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Mar 10 03:01:50 2025
    AWUS01 KWNH 100301
    FFGMPD
    FLZ000-GAZ000-100900-

    Mesoscale Precipitation Discussion 0056
    NWS Weather Prediction Center College Park MD
    1100 PM EDT Sun Mar 09 2025

    Areas affected...Southern GA...FL Panhandle to Northeast FL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 100300Z - 100900Z

    SUMMARY...Locally training showers and thunderstorms are forecast
    to continue into the overnight hours with additional concerns for
    flash flooding.

    DISCUSSION...The latest radar imagery shows a band of very heavy
    showers and thunderstorms impacting the Big Bend of FL through
    northeast FL, with an emphasis over the last couple of hours on
    parts of Dixie, Lafayette and Taylor Counties. The convection is
    well aligned with a quasi-stationary front draped across the
    region and is being driven by focused low-level moisture
    convergence and the pooling of instability ahead of a wave of low
    pressure transiting the northeast Gulf of America. Meanwhile,
    scattered bands of heavy showers and thunderstorms are also seen
    redeveloping across areas of the FL Panhandle and up across
    southern GA to the north of this front.

    PWs of 1.5 to 1.75 inches are in place along the front along with
    MUCAPE values of about 1000 J/kg. There is a southwest low-level
    jet of 30 to 40 kts helping to favor the moisture and instability
    transport, and with rather divergent flow aloft noted out ahead of
    an approaching mid-level trough, there should continue to be a
    focus well into the overnight hours for additional showers and
    thunderstorms that should generally track in a west-southwest to
    east-northeast fashion.

    Overall, the heaviest rainfall threat at least for the next few
    hours should continue to be in vicinity of the Big Bend of FL, but
    areas downstream toward northeast FL including the greater
    Jacksonville area may also potentially see additional heavy
    rainfall amounts from some of these stronger showers and
    thunderstorms. The 00Z HREF guidance also maintains a threat for
    locally heavy rains across southern GA with sufficient levels of
    elevated instability and forcing expected to remain in place for
    additional small-scale bands of convection going into the
    overnight hours.

    Rainfall rates with the stronger storms will be capable of
    reaching 1.5 to 2 inches/hour, and additional rainfall totals
    overnight may reach as high as 3 to 4+ inches. This will yield an
    additional concern at least locally for flash flooding, with the
    more urbanized locations generally at greatest risk for seeing
    impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!60T8bdQo2_4hnlREzM4XsNH5K2rP0jLfF4D4-Hd1fZoYSH2SQjr2N3nsTqziOKd2MLx1= 3GjvRChr80iSTGYGciAjIYk$ for graphic product...

    ATTN...WFO...CHS...JAX...TAE...TBW...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 31858202 31708113 31338105 30808125 29938125=20
    29748153 29508198 29408313 29848371 29908454=20
    30298508 30988488 31638356=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Mar 11 20:21:51 2025
    AWUS01 KWNH 112021
    FFGMPD
    CAZ000-120215-

    Mesoscale Precipitation Discussion 0057
    NWS Weather Prediction Center College Park MD
    421 PM EDT Tue Mar 11 2025

    Areas affected...Coastal Southern California...Eastern Channel
    Islands....

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 112020Z - 120215Z

    SUMMARY...Convective elements capable of .5-.75"/hr rates and
    totals up to 1" pose localized possible flash flooding conditions
    particularly in urban/rocky sloped ground conditions.

    DISCUSSION...GOES-W Visible imagery continues to show a band of
    convective cells along the northeast quadrant of the deep layer
    cyclone. An embedded lobe of vorticity is rounding the southern
    base of the low providing subtle but sufficient diffluence aloft
    across the southeastern California Bight with slowly increasing
    DPVA to further enhanced vertical development. WV suite also
    suggests core of upper-level low and cold air advection is
    filtering in steepening the lapse rates with MUCAPE reaching
    500-750 J/kg within the band. Low level confluent response along
    the band and ample surface to 850mb of .5-.6" per CIRA LPW
    combines to support .75-.9" total PWats within/below the
    steepening lapse rates. Cells have a healthy cauliform appearance
    with boiling overshooting tops along the upstream edge; given
    helicity of 100 m2/s2 and sfc-1km shear in the 15-20kt range, weak
    rotation may be further supporting moisture flux into the cores of
    the cells as they advance northeastward. Given all the
    parameters, cores of the cells will be capable of .5-.75"/hr
    rates.

    The uncertainty will continue to be the intersection with land
    areas before the window of opportunity reduces as the vorticity
    center rotates through reducing effective ascent pattern in
    3-6hrs. In the short-term, the upstream forcing should allow for upstream/back-building of cells slowing forward propagation, but
    once the DPVA passes through, cell motions could increase to
    20+kts, limiting totals. As such, cell cores are likely to
    intersect San Clemente, potentially far eastern Catalina islands
    with chance of up to 1" totals (HREF probs of 20-25%); however,
    there is greater uncertainty toward reaching Orange county and
    eastern San Diego county. Still, if cell maintain convective
    vigor (as suggested by recent HRRR and RAP solutions), even .5"/hr
    rates would be near the FFG values in the area; so while localized
    scattered incident or two of flash flooding is considered possible
    through 03z.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9QwItwWK0CVQJx-eQ_IvljRdXm0E8e-F73XKWm_oZYUC3P-ZmiyPEvotO0L2UdoN3B3m= L524sOk8LPxPbnuSN_ux3gQ$ for graphic product...

    ATTN...WFO...LOX...SGX...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 33831750 33681704 33201664 32611654 32351696=20
    32301741 32611822 33091863 33781836=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Mar 12 15:46:26 2025
    AWUS01 KWNH 121546
    FFGMPD
    CAZ000-130300-

    Mesoscale Precipitation Discussion 0058
    NWS Weather Prediction Center College Park MD
    1145 AM EDT Wed Mar 12 2025

    Areas affected...Northwest to Central California...

    Concerning...Heavy rainfall

    Valid 121545Z - 130300Z

    SUMMARY...Progressive cold front/moisture flux to produce 1-2"
    totals in 4-6 hours, particularly only coastal ranges and lower
    foothills of the Sierra Nevada Range.=20

    DISCUSSION...GOES-W WV suite depicts a broad cold larger scale
    trough across the northeast Pacific with a leading northwesterly
    surge of colder air undercutting the base generally a degree or
    two south of the 40N130W benchmark. This is resulting in some
    negative tilt to the base of the trof with downstream responses
    noted in the expanding baroclinic shield cloud in the diffluence
    aloft to the northeast nearing Cape Mendocino. This is starting
    to buckle the surface front and enhanced surface to low level
    cyclogenesis near 39N and 127W backing low level flow and
    increasing the low level jet to 50kts within the broader
    isentropic ascent into the upper-level evacuation zone. Total
    moisture is not particularly impressive with this atmospheric
    river with surface to 850mb CIRA LPW in the .5" range, however,
    the narrow ribbon of mid to upper-level moisture is fairly
    vertically aligned along/ahead of the cold front to support
    reduced drying and perhaps some seeding from the mid-levels to
    keep RH values higher than average in the band.

    Still, the cold air advection is solid/strong resulting in a
    fairly progressive frontal zone push from west to east. Initial
    core of the pre-frontal LLJ is starting to interact with the
    Lost/Redwood near and south of Cape Mendocino. The surface low
    will track throughout the period into the Cape region and
    potentially allow for additional surges of steepening lapse rates
    for secondary convergence bands with weaker/narrow updrafts
    intersecting the coastal region through the remainder of the day.=20
    Rates should remain at or below .5"/hr averaging around .25" and
    support 1.5-2.5" totals in favored orographics, but will come of
    little concern given the rain forest nature to the area. However,
    as the cold front presses through, strong 40-50kts of flow will
    intersect the coastal ranges toward the San Francisco bay through
    21z. As the cyclone continues to deepen, the directional
    convergence along the front will go from 30-45 degrees up to 60-75
    degrees increasing the overall convergence. The undercutting
    upper-level shortwave may also have some peripheral influence of
    steepening lapse rates aloft for some increased vertical ascent to
    these convergence/ascent parcels allowing for narrow scattered
    updrafts along the front with .25 to locally/occasionally reaching
    near .5"/hr with 12z HREF .5"/hr probability values vacillating
    around 30-50% changes north of the Bay through 21-22z time period.
    =20

    ...Central Californian coasts/Central Valley...
    As the front drops south past the San Francisco Bay, the winds
    will continue to be strong but also orient more favorably to the
    Santa Cruz and eventually Santa Lucia ranges with near
    orthogonality through solid depth in the 21-00z time period. The
    IVT strength will be peaking toward 500 kg/m/s with 850-700mb flow
    starting to weaken slightly due to displacement southward from the
    peak cyclogenesis...but still in the 40-50kt range. The
    combination of flux to steeper terrain will result in .5"/hr rates
    being more likely, but given the southward translation of the cold
    front may only result in 1-3 hours and overall totals are more
    likely to be near 2-2.5", but an isolated 3" is not completely out
    of the picture. HREF probability is over 80% for much of the
    period along the Santa Lucia from 23-02z, though never even
    reaches 10% for 1"/hr.

    The moisture surge will have also filtered through the lower
    terrain gap of the Bay and shower activity will also likewise
    increased through the central valley into the lower foothills of
    the Central Sierra Nevada. Similarly, favored, nearly orthogonal
    ascent will support .25-.33"/hr rates. Totals of 1.5-2"+ may
    result in increased runoff, but more likely beneficial in all but
    the most prone areas. Forward progression will continue with the
    front, likely reaching Southern California/Cape Conception after
    03z.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9wSFTaHPHgEaMtQ9LPhHbeJKNAuzNgnahkhk9ORXzVDu2-Q_CtdDGjTbt-TAXv5Z1HW4= _dyWAy9m8u6k0of2KtDHU0U$ for graphic product...

    ATTN...WFO...EKA...HNX...LOX...MTR...STO...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 41272379 40622330 40412284 40062178 39442086=20
    38272024 37511972 36702069 35812059 35162041=20
    34582037 34442061 35362112 36182194 37652263=20
    38432348 38782376 39122387 39692401 40072450=20
    40822442 41202419=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Mar 13 02:06:03 2025
    AWUS01 KWNH 130205
    FFGMPD
    CAZ000-131405-

    Mesoscale Precipitation Discussion 0059
    NWS Weather Prediction Center College Park MD
    1005 PM EDT Wed Mar 12 2025

    Areas affected...portions of southern California

    Concerning...Heavy rainfall

    Valid 130205Z - 131405Z

    Summary...A frontal band will translate from west to east across
    southern California coastal ranges, resulting in 1-2 inch rainfall
    totals - highest in terrain-favored areas. This rainfall will
    affect burn scars across the region, posing a risk of runoff,
    flash flooding, and debris flows through at least 13Z/6a PDT.

    Discussion...A strong Pacific cold front (currently located near
    KPRB/Paso Robles, CA and KSBP/San Luis Obispo) was making steady
    southeastward progress over the past several hours, and will
    continue to do so across the discussion area through 13Z. Along
    and west of the front, areas of convection have produced 0.5-1
    inch of rain over the past 3 hours - highest along coastal areas
    between San Francisco and San Luis Obispo within the Santa Lucia
    Range. Minor flooding has also occurred across Alameda County.
    These rainfall rates will continue to spread southeastward in
    tandem with the front, while potentially increasing as depicted by
    CAMs as the rainfall band reaches the Transverse Ranges and
    adjacent areas near Los Angeles Metro through 06-12Z (11p-5a PDT)

    As these rates spread southeastward, they will encounter fresh
    burn scars from recent fires across the region. These and other
    sensitive areas will promote runoff along with the potential for
    flash flooding and debris flows. Models/obs indicate that a 3-5
    hour period of moderate to heavy rain will affect the region, with
    peak flash flood risk potential occurring in the 08Z-12Z (1a-5a
    PDT) timeframe around the Los Angeles metro and adjacent areas of
    the Tranverse Ranges. The risk will peak farther southeast toward
    San Diego and adjacent mountainous areas in the 12-14Z (5a-7a PDT)
    timeframe. Storm totals of 1-2 inches are expected (locally
    higher in terrain-favored areas), and peak hourly rain rates
    should mostly remain in the 0.5-0.75 inch range, locally higher.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9l63Z6R_esTVdrCecbqOAtG3lr6pabvSCrQmDjG1DDk7QWEkBZ39gano74qcppqcUoRa= xE81mbjsCZVb5r5_TWGABXY$ for graphic product...

    ATTN...WFO...HNX...LOX...SGX...VEF...

    ATTN...RFC...CNRFC...NWC...

    LAT...LON 35732024 35711942 35461831 35081719 34491661=20
    33541642 32851661 32601709 32941746 33571821=20
    33871899 34142000 34632080 35342090=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 16 08:51:49 2025
    AWUS01 KWNH 160850
    FFGMPD
    CAZ000-ORZ000-162049-

    Mesoscale Precipitation Discussion 0071
    NWS Weather Prediction Center College Park MD
    450 AM EDT Sun Mar 16 2025

    Areas affected...portions of western and southwestern Oregon

    Concerning...Heavy rainfall

    Valid 160849Z - 162049Z

    Summary...Persistent rainfall is expected to continue to pose a
    risk for flooding and localized flash flooding. Another 2-5
    inches of rainfall are possible through at least 21Z today.

    Discussion...The ongoing regime supporting heavy rainfall
    continues, and very little has changed over the past 12 hours.=20
    60-70 knot low to mid-level flow remains oriented perpendicular to
    the Oregon Coast and Cascades, promoting orographic lift and
    continued rainfall amid 500-750 kg/m/s integrated water vapor
    transport values. 0.1-0.3 inch hourly rain rates have persisted,
    resulting in 1-3.5 inch rainfall totals over the past 24 hours -
    highest across southwestern Oregon coastal ranges. This regime
    will continue to persist most of the day, with only a slow
    southward shift in the low/mid-level jet axes and attendant
    precipitation maxima. Another 2-5 inches of rainfall are expected
    areawide - with highest rainfall totals expected across
    southwestern Oregon (coastal ranges in particular). This
    long-duration rainfall event will result in a gradual increase in
    flood potential. Streamflows across the region are already above
    average, further supporting the idea of enhanced/efficient runoff
    with additional rainfall as the day progresses.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9_R1rtv4cWvOsKkuAhgMCqYmvk2VRaKACoS8WhomDFPAYR4Sy_h44tfRCTUx2DXzNCOT= 43UXf_z6Jag2VRPzox0q970$ for graphic product...

    ATTN...WFO...EKA...MFR...PDT...PQR...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 44892238 44782181 44212150 43242174 42422193=20
    41972324 42032432 42822462 43952437 44222390=20
    44522317=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 16 12:54:26 2025
    AWUS01 KWNH 161254
    FFGMPD
    SCZ000-GAZ000-161552-

    Mesoscale Precipitation Discussion 0072
    NWS Weather Prediction Center College Park MD
    853 AM EDT Sun Mar 16 2025

    Areas affected...portions of far southeast GA and SC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 161252Z - 161552Z

    Summary...A training band of heavy rain is expected to continue to
    lead to hourly totals to 3" with storm totals to 5". This could
    lead to flash flooding.

    Discussion...A bow echo along a convective line in central SC
    combined with another mesocyclone near Millen GA have held up
    convection across portions of southeast GA and SC. Hourly rain
    totals to 3" and local amounts of 5" have been indicated by radar
    imagery within this band. Precipitable water values of
    1.50-1.75", MU CAPE of 500-1000 J/kg, effective bulk shear near 50
    kts, and fairly unidrectional flow with height have fostered the
    development of this band.

    The 06z HREF guidance suggests that this band should persist for
    no more than a few hours. For QPF volume, the 00z ARW appears to
    have captured this best, though it's too far northeast with the
    footprint. The mesocyclone near Millen GA should force forward
    propagation of the band later this morning. Until then, expect
    the threat of hourly rain totals to 3" with local amounts to 5"
    being possible across portions of extreme southeast GA and SC.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!71azd5URerDFRbC3ND0wAvIdIG0g7GkqDj-d3LTDbGgep7Jd6SHNokwY_JH284ueH-xI= 17KwPtUI_oPWzddtfm5psXg$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 33988040 33308001 32918085 32728216 33318182=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 16 20:43:33 2025
    AWUS01 KWNH 162043
    FFGMPD
    CAZ000-ORZ000-170730-

    Mesoscale Precipitation Discussion 0073
    NWS Weather Prediction Center College Park MD
    442 PM EDT Sun Mar 16 2025

    Areas affected...Southwest Oregon...Northern California...

    Concerning...Heavy rainfall

    Valid 162045Z - 170730Z

    SUMMARY...Flooding risk reducing as cyclone makes landfall and
    warm conveyor belt presses quickly southward to intersect coastal
    range and northern Sierra Nevada Foothills with heavy rainfall.

    DISCUSSION...Southwest Oregon has been experiencing prolonged
    moderate rainfall for over 24hrs at this point with large areas of
    4"+ totals across much of the area of Coos, Douglas, Josephine and
    northern Jackson counties and spots in the boreal rain forests of
    Curry county in the 8-10" ranges. Longer duration flooding has
    been going in atypical locations with the prolonged heavy
    rainfall. The strong onshore moisture flux will be ending in the
    next hour or so, but a strong surface wave can be seen with a
    secondary one further west along an old occluded front. Steeper
    lapse rates due to CAA aloft and some modest retention of moisture
    along the boundary may allow for some scattered shower activity to
    cross SW OR along the occluded front into the stationary front
    that crosses into central OR. Rates up to .25-.33"/hr are
    possible but will be more scattered in nature and may result in
    those ranges of totals in a sub-hourly manner. This is not likely
    to further contribute to enhanced flooding, but will slow its
    ending for a few more hours.=20=20

    Further south...GOES-W Visible imagery shows the cold front and
    more directed atmospheric river/warm conveyor belt has started a
    southward progression. The core of .75-.9" total PWat continues
    to be advected from strong 40-50kt 850mb winds allowing for IVT
    values to remain at 650-700 kg/m/s near the triple point that is
    near the OR/CA coastline and southeastward. Upper-level
    height-falls will continue to support increasing south and
    eastward propagation of the cold front and therefore
    onshore/upslope moisture flux. Occasional rates of .33-.5"/hr are
    possible especially along the steepest inclines of the northern
    Sierra Nevada foothills, but duration of moderate rainfall is
    likely to be limited to a few hours and likely only result in
    spotty totals of 1.5-3" in traditional locations in Butte, Tamaha
    and Yuba counties. Coastal Ranges are more likely to see
    1.5-2.5", reducing to .75-1.5" by the time the plume further
    weakens (wind speeds down to below 35kts) and IVT values fall
    below 400 kg/m/s...nearing the mouth of San Francisco Bay between
    03-06z. A secondary weaker band of scattered showers will wrap
    around the surface low as it translates east and affects the NW
    California after 00z as well, adding another .5-.75" for the
    totals. Bringing the overall event to close in the early morning
    hours tonight.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5nnx9kBXfO4owThSuTG3TcFLcpoLPpnuE59scDkR7fjNIfb7IZmLoD24j9WynYUVfjKv= xqr-e-TbeJ15Le6vVwyrdY8$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...STO...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 43762376 43402333 42922284 42092262 41122202=20
    39922140 39382078 38672050 38392087 38572132=20
    39852189 40562243 39762260 38632211 38022277=20
    38442338 39022398 39812419 40592462 41122434=20
    41812430 42392466 42882466 43412443 43742423=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 16 21:59:01 2025
    AWUS01 KWNH 162158
    FFGMPD
    VAZ000-NCZ000-170400-

    Mesoscale Precipitation Discussion 0074
    NWS Weather Prediction Center College Park MD
    558 PM EDT Sun Mar 16 2025

    Areas affected...Northeast NC...Southeast VA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 162200Z - 170400Z

    SUMMARY...Continuation of stronger cells capable of 1.5-2"/hr
    rates with upstream redevelopment probable resulting in possible
    streets of 3"+ totals and localized flash flooding conditions.

    DISCUSSION...RADAR mosaic depicts a cluster of stronger elongated
    updrafts in proximity to the I-95 corridor tracking through an
    area that had already seen an earlier round wetting the grounds
    with spots of .75-1.5" as far north as Petersburg/Wakefield, VA.
    These cells are aided by a divergence maxima rounding the cyclonic
    edge of a fairly laminar upper-level jet. This pattern is
    expected to remain similar with a very slow eastward progression;
    as such, 500-1000 thickness ridge resides along/just east of the
    I-95 corridor and with solid 45-50kts of moist 850mb flow, there
    is ample potential for additional upstream redevelopment.=20=20
    Alignment of the moisture axis and instability axis appears to be
    fairly stable in placement as well with upstream well of 1000-1500
    J/kg of MLCAPE to the west and 1.5 to 1.75" of total PWats
    eastward. Solid deep layer confluence is providing the upstream
    convergence to allow for back-building/redevelopment. However,
    the updraft strength is offset a bit being on the gradient of the
    instability axis, resulting in inconsistent, narrow updrafts but
    stronger cloud base moisture flux allows for efficient loading to
    support 1.5-2"/hr rates. Lengths of the updrafts should allow for
    an hour or so of training for streaks of 1.5" with each
    pulse/round of convection moving northward.

    Stronger convergence along the cold front as the base of the trof
    drifts eastward is likely to occur after sunset and likely spell=20
    the last round, this may be after 04z (the end valid time of this
    message) and trends will need to be continually monitored for
    additional training and longer duration totals of 3-4" when all is
    over earlier tomorrow morning. Area has been fairly dry and FFG
    values are high (especially further east in the Coastal Plain);
    however, given each round slowly infiltrated and saturates the
    upper soils reducing it for the next round. While, an incident or
    two of flash flooding is possible, it is more likely to be
    isolated, lower-end with greatest risk of higher magnitude of
    flooding in urban locations such as Raleigh, Rocky Mount, Emporia,
    Petersburg and the Hampton Roads vicinity of SE VA.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5iY5coMLNs81Tr5eQT0UFxE04VIqjH8-mHIs9W4KB6MNGOWjJEA0ZHVJVXa-ktQ6kJzE= XvY4ZQOIjalgGcDRcMqw_Sc$ for graphic product...

    ATTN...WFO...AKQ...MHX...RAH...

    ATTN...RFC...MARFC...SERFC...NWC...

    LAT...LON 37897661 37867619 37297617 36797596 36597603=20
    36207647 35347760 35007846 35417909 36347852=20
    37367736=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 16 22:48:04 2025
    AWUS01 KWNH 162247
    FFGMPD
    NCZ000-SCZ000-GAZ000-170400-

    Mesoscale Precipitation Discussion 0075
    NWS Weather Prediction Center College Park MD
    647 PM EDT Sun Mar 16 2025

    Areas affected...Central SC...South-central NC...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 162245Z - 170400Z

    SUMMARY...Expanding thunderstorms within favorable repeat/training
    environment pose possible isolated incidents of localized flash
    flooding into early overnight period.

    DISCUSSION...Regional RADAR and GOES-E VIS/EIR loops show
    destabilization and convective growth across the Piedmont of
    central SC starting to move into central NC. Clear skies
    throughout the day allowed for increased insolation and temps to
    rise into the upper 70s, low 80s along a tight deep layer moisture
    gradient. However, surface low level confluence with
    southwesterly flow intersecting with SSW 10-15kts of flow backed a
    bit off the coastal Plain is providing sufficient moisture
    convergence given Tds into the low to mid 60s. That flux and
    solid updraft strength is supporting 1.5"/hr rates. Deep layer
    steering does support fast cell motions, however, it is fairly
    ideally aligned with the low-level convergence axis to allow for repeating/training, though slow eastward propagation is expected,
    spots of 2-2.5" totals in 1-2 hours which is close to exceeding
    the FFG values mainly along the Fall-line and the axis of
    saturated soils from this morning's heavy rainfall from Allendale
    county to Orangeburg county to N Dillon county where 1hr FFG
    values are 1.5-2" and 3hr are 1.5-2.5".=20

    There is some uncertainty in potential for favorable back-building
    environment especially toward the GA/SC line. Stronger forcing
    near the southeast base of the rounded upper-level (500 to 300 mb)
    jet should support divergence aloft and weak DPVA to aid low level
    inflow for back-building; however, drier air infiltrating aloft
    also looks to be mixing downward and overall Pwats are decreasing
    upstream suggestive of drier air mixing and increasing eastward
    propagation limiting training/repeating potential.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6dVV0h7LxCbuKBuOcrFbI-UdTFgw93lAczQB7HCq95kV_2qK-BA_XAcPQduZYi1jHgo0= phmMPnTxOpmwQefHRxLyLtM$ for graphic product...

    ATTN...WFO...CAE...CHS...GSP...ILM...RAH...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 35777959 35627911 35257877 34747884 34347905=20
    33907955 33158060 32738168 33088194 34098138=20
    34578106 35518014=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Mar 17 02:25:03 2025
    AWUS01 KWNH 170225
    FFGMPD
    NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-DCZ000-170824-

    Mesoscale Precipitation Discussion 0076
    NWS Weather Prediction Center College Park MD
    1024 PM EDT Sun Mar 16 2025

    Areas affected...portions of the Mid-Atlantic

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 170224Z - 170824Z

    Summary...Gradually deepening convection will migrate
    northeastward across the discussion area for the next several
    hours. Rates of 1-2 inches/hr are expected - highest across
    eastern Maryland into the DelMarVa. Isolated flash flooding is
    possible in this regime.

    Discussion...Several atmospheric factors are combining to result
    in increasing convective coverage and heavy rainfall across the
    discussion area, including: 1) convergence along a surface cold
    front extending from Charlottesville, VA to near Lancaster, PA, 2)
    strong low-level flow/warm advection, which was maintaining deeper
    convection near/east of Richmond, VA while also maintaining ~500
    J/kg SBCAPE and 1-1.5 inch PW ahead of the front, 3) advancing
    mid/upper level vorticity (and ascent) from troughing centered
    over the Ohio Valley and central Appalachians.

    As these features continue to evolve slowly eastward over the next
    few hours, axes of heavier rainfall will continue to spread
    east/northeastward along and ahead of the aforementioned cold
    front. Spots of 1 inch/hr rain rates can be expected at times
    nearer the front, while heavier rainfall (including 2-2.5 inch/hr
    rain rates) could occur out ahead of the front as is currently
    being estimated near/east of Richmond, VA. FFGs across the
    discussion area are lowest across the DC-to-Philadelphia I-95
    corridor (0.5-1.0 inch/hr) and these thresholds could be eclipsed
    on an isolated basis over the next 2-4 hours as the front makes
    its way eastward through the region. Heavier rain rates are
    expected east of I-95 toward the DelMarVa, although it appears
    that ground conditions/FFGs are a bit less sensitive in these
    areas, suggestive of more isolated flash flood potential. 2-3
    inch rainfall totals are expected across the DelMarVa through 08Z
    tonight, with lighter totals expected elsewhere.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7Ce5av1YTI927ZG7X7fk5468shHGtUbotqmqvLvoedAIbDL3bVJ0yI5ANf6KErC3x2Ph= W1OxS8Q4GPh1UU3jnDhLs7E$ for graphic product...

    ATTN...WFO...AKQ...CTP...LWX...PHI...RNK...

    ATTN...RFC...MARFC...NWC...

    LAT...LON 40787539 40437427 39587434 38027549 37357691=20
    37677889 38807814 40237663=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Mar 17 04:46:08 2025
    AWUS01 KWNH 170445
    FFGMPD
    VAZ000-NCZ000-170900-

    Mesoscale Precipitation Discussion 0077
    NWS Weather Prediction Center College Park MD
    1244 AM EDT Mon Mar 17 2025

    Areas affected...northeastern North Carolina into southeastern
    Virginia

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 170444Z - 170900Z

    Summary...Deep convection continues to develop across North
    Carolina and stream north-northeastward into southeastern
    Virginia. 1-2 inch/hr rain rates persist in the strongest
    activity. This regime should continue for at least another 3-4
    hours, posing a continued risk of flash flooding.

    Discussion...Convection has continued to refire along a surface
    trough extending from just east of Richmond, VA to just east of
    Raleigh, NC over the past couple hours. This trough has allowed
    for convective development to remain oriented generally parallel
    to deep south-southwesterly flow aloft, allowing for substantial
    training in a few locales. Additionally, 1.5+ inch PW values and
    500 J/kg SBCAPE supports efficient rainfall processes with the
    ongoing storms. Ascent from upstream mid-level troughing
    continues to result in ascent/height falls over the trough as
    well. These factors support continued, SSW-NNE oriented training
    bands of storms for the next 2-4 hours or so.

    Over time, eastward translation of the surface trough and
    mid-upper forcing will lead to an eventual end of heavy rainfall
    potential - most likely after 08-09Z. Between now and then,
    concern exists that these training convective bands could
    eventually make it in to populated, sensitive areas of
    southeastern Virginia where lower FFGs (around 1 inch/hr) could
    result in a few areas of flash flooding. It is not out of the
    question for rain rates to double those lower values (generally
    extending from near Richmond southeastward through Virginia Beach)
    and lead to locally significant impacts.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Y2go9nfNkgnIXmUE6p5CsTdp6lYfOFWqV83E671QGmN4vdHIn9_sfKnoBF5s5mDutI1= rQSOJlbJj7BPykGub9s1shI$ for graphic product...

    ATTN...WFO...AKQ...MHX...RAH...

    ATTN...RFC...MARFC...SERFC...NWC...

    LAT...LON 37587690 37067613 36627606 36017677 35477799=20
    36767811 37557755=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 15 08:24:40 2025
    AWUS01 KWNH 150824
    FFGMPD
    ALZ000-MSZ000-151122-

    Mesoscale Precipitation Discussion 0060
    NWS Weather Prediction Center College Park MD
    423 AM EDT Sat Mar 15 2025

    Areas affected...northeastern Mississippi and northwestern Alabama

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 150822Z - 151122Z

    Summary...Localized 1.5-2.5 inch/hr rain rates should continue for
    the next couple hours or so. Convective evolution thereafter is a
    bit uncertain. Isolated flash flooding is possible.

    Discussion...A dominant, right-moving supercell has persisted for
    several hours while reaching Itawamba County, Mississippi near the
    MS/AL border. This supercell has maintained broad rotation within
    a moist and strongly sheared airmass. Convection immediately
    upstream (along and north of its gust front) has enabled a
    scenario for localized training and rain rates approaching 2
    inches/hr from near Okolona, MS northeastward to near Fulton, MS.

    As his lead supercell progresses into Alabama, increasing
    convective coverage has materalized upstream in areas near Tupelo,
    Columbus, and Greenwood. The cells are embedded within strong,
    broadly confluent 850mb flow exceeding 45 knots areawide, which
    continues to maintain moist/unstable thermodynamic profiles in the
    immediate wake of the supercell. It appears that this confluent
    low-level jet structure should be maintained for mutliple hours
    this morning despite 1) departing forcing for ascent with a
    mid-level vort max moving away toward the upper Midwest and 2)
    renewed mid-level troughing across Texas that should result in a
    gradual backing of 850mb flow.

    The ongoing supercell along the MS/AL border should eventually
    weaken as it reaches less stable air especially across north-central/northeastern Alabama. Upstream convection, however,
    should continue to support localized runoff issues as 1-hour FFG
    thresholds (in the 1.5-2 inch range) are approached by localized repeating/training cells across the discussion are through the
    morning - especially in areas that have already had rainfall.=20
    Isolated flooding is possible, although this event appears to be
    perhaps the beginning of a more synoptically evident flash flood
    event expected to unfold later today/tonight.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7eCMpjSSgxklFtbZy5khg8whhCUDdbCxFysQ5KngdLyj_VimEKCIqmbL2B7FmnAwhFAD= 7iMELL4PgcC3C1toe7e7W1s$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...MEG...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34998775 34638646 34078673 33678809 33918976=20
    34758916=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 15 08:38:46 2025
    AWUS01 KWNH 150838
    FFGMPD
    ALZ000-MSZ000-151122-

    Mesoscale Precipitation Discussion 0060
    NWS Weather Prediction Center College Park MD
    437 AM EDT Sat Mar 15 2025

    Areas affected...northeastern Mississippi and northwestern Alabama

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 150822Z - 151122Z

    Summary...Localized 1.5-2.5 inch/hr rain rates should continue for
    the next couple hours or so. Convective evolution thereafter is a
    bit uncertain. Isolated flash flooding is possible.

    Discussion...A dominant, right-moving supercell has persisted for
    several hours while reaching Itawamba County, Mississippi near the
    MS/AL border. This supercell has maintained broad rotation within
    a moist and strongly sheared airmass. Convection immediately
    upstream (along and north of its gust front) has enabled a
    scenario for localized training and rain rates approaching 2
    inches/hr from near Okolona, MS northeastward to near Fulton, MS.

    As this lead supercell progresses into Alabama, increasing
    convective coverage has materalized upstream in areas near Tupelo,
    Columbus, and Greenwood. The cells are embedded within strong,
    broadly confluent 850mb flow exceeding 45 knots areawide, which
    continues to maintain moist/unstable thermodynamic profiles in the
    immediate wake of the supercell. It appears that this confluent
    low-level jet structure should be maintained for multiple hours
    this morning despite 1) departing forcing for ascent with a
    mid-level vort max moving away toward the upper Midwest and 2)
    renewed mid-level troughing across Texas that should result in a
    gradual backing of 850mb flow.

    The ongoing supercell along the MS/AL border should eventually
    weaken as it reaches less stable air especially across north-central/northeastern Alabama. Upstream convection, however,
    should continue to support localized runoff issues as 1-hour FFG
    thresholds (in the 1.5-2 inch range) are approached by localized repeating/training cells across the discussion are through the
    morning - especially in areas that have already had rainfall.=20
    Isolated flooding is possible, although this event appears to be
    perhaps the beginning of a more synoptically evident flash flood
    event expected to unfold later today/tonight.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4kA5R-nTAYdqcnuZSVxKc7CLoymXMlueBEuDFgRhC6J5yx9FvJI17HxkWFUVMzJXfnS9= bmsX-xqX1Sl_gXjmZScFA6k$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...MEG...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34998775 34638646 34078673 33678809 33918976=20
    34758916=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 15 11:30:41 2025
    AWUS01 KWNH 151130
    FFGMPD
    TNZ000-MSZ000-LAZ000-ARZ000-151700-

    Mesoscale Precipitation Discussion 0061
    NWS Weather Prediction Center College Park MD
    730 AM EDT Sat Mar 15 2025

    Areas affected...Northern Louisiana, Northwestern Mississippi, &
    Western Tennessee

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 151129Z - 151700Z

    SUMMARY...Training cells along a stationary upper level boundary
    will likely pose a flash flooding threat through the morning with
    rates locally exceeding 2 inches per hour. Flash flooding is
    likely.

    DISCUSSION...A very dynamic scenario is unfolding across
    northwestern Mississippi this morning as a stationary upper level
    boundary acts as a forcing mechanism for storms that are already
    forming. Low level SSE flow is advecting plentiful Gulf moisture
    characterized by dew points near 70 degrees and SBCAPE values over
    2,000 J/kg into the region. At 850mb, a south-southwesterly LLJ
    has strengthened to near 50 kts, which will keep a steady supply
    of moisture advecting into the front. Meanwhile a potent shortwave
    across northeast Texas is approaching the region, which will add
    even more forcing. This will both strengthen the storms training
    along the front and broaden the precipitation shield over the
    area, meaning many areas will not see a break in the rainfall.

    1-hr FFGs in this region are generally between 1.5 and 2.5 inches,
    which will both come down with the early morning convection
    already breaking out, and with the later additional forcing will
    support even stronger convection capable of rates exceeding 2
    inches per hour. This will support widely scattered to numerous
    instances of flash flooding across this region. Despite recent dry
    weather, the long-duration of the training convection across this
    region should easily overcome these FFG values. While each
    individual cell will move rather rapidly to the northeast across
    this area, the high likelihood that multiple cells producing heavy
    rainfall will move over any one location under the line of storms
    will compound any flooding and rises in streams and creeks rather
    rapidly.

    Urban flash flooding will be a significant concern as these storms
    set up very near metro Memphis, though likely staying just south
    and east of the city. Expect the southern and eastern suburbs to
    be hard-hit with multiple inches of rain through the morning.

    The line of training storms is likely to remain in roughly the
    same place through the morning based on many of the CAMs guidance
    into the early afternoon until both the upper level shortwave and
    attendant surface cold front push through and shift the storms off
    to the east. This discussion will be updated as the situation
    evolves.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_5HHhRDdgRo8t5NqeiouNdOmh4EPxcRsY94ub6gJ8DUkOHw5DL79hu5sOW6OO7mB_JwL= PHDjrB-y_X0F9KE_5RWUGcg$ for graphic product...

    ATTN...WFO...JAN...LZK...MEG...OHX...SHV...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36408824 36138749 35118829 34788860 34038936=20
    31619205 31649320 32649244 33719163 34739068=20
    36118922=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 15 13:22:32 2025
    AWUS01 KWNH 151321
    FFGMPD
    GAZ000-TNZ000-ALZ000-151630-

    Mesoscale Precipitation Discussion 0062
    NWS Weather Prediction Center College Park MD
    920 AM EDT Sat Mar 15 2025

    Areas affected...Northeastern Alabama, Far Northwestern Georgia,
    and Southeastern Tennessee

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 151319Z - 151630Z

    SUMMARY...Training cellular convection over northeastern Alabama
    may cause a localized flash flooding risk as they advect
    northeastward into the Chattanooga Metro.


    DISCUSSION...Cellular convection that has been largely stationary
    across northeastern Alabama this morning has been advecting
    northeastward into the Chattanooga Metro area this morning.
    Southeasterly surface flow characterized by dewpoints in the 50s
    is largely orthogonal to the northeastward moving and oriented
    line of convection. This has been feeding the storms and
    contributing to their persistence. The upper levels feature a
    bifurcated jet streak, with the storms in the middle of the
    bifurcation. It's possible the southern arm is contributing to
    upper level lift being in the divergence region of the jet.

    Much of the CAMs guidance suggests this area of storms will shift
    off to the north and join up with the line of storms well to its
    west over the next few hours. However, that remains to be seen, as
    the forcing would support the storms remaining in place. Following
    a persistence forecast, over the next few hours, heavier cells
    will be moving over the Chattanooga metro, which due to urban and
    terrain concerns poses a higher localized flash flooding risk.
    Most of the instability is west of the storms, with the
    southeasterly inflow not advecting much into the storms. Thus,
    there is some chance the storms fall apart on their own, but as
    that hasn't happened yet, the flash flooding threat will persist
    for the next few hours. At the very least, this offset of
    instability from the inflow should continue to limit the strength
    and maximum rainfall potential of the storms.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8mgvyMuJcn2-fNlM-3kPTK3NR5GcSLFrpfLYhsaijjuto0MX9J5U-5AtZQgL05dJGAt9= MxvhoQMMFQID5WhjD9kgCDg$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...MRX...OHX...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 35748504 35588457 35168472 34748494 34158542=20
    34048613 34088651 34828709 35388651=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 15 16:45:53 2025
    AWUS01 KWNH 151644
    FFGMPD
    TNZ000-KYZ000-ALZ000-MSZ000-LAZ000-152230-

    Mesoscale Precipitation Discussion 0063
    NWS Weather Prediction Center College Park MD
    1244 PM EDT Sat Mar 15 2025

    Areas affected...Northern MS...Northwest AL...Western to Middle TN...South-Central KY...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 151645Z - 152230Z

    SUMMARY...Strong, highly efficient rotating thunderstorms capable
    of 1.5-2"/hr rates likely to train for a hour or so as the line
    slowly advances eastward. Subtle buckles in the QLCS may result
    in further enhanced duration with a spot or two of 4-5" possible.=20
    Rates and totals are likely to result in scattered to numerous
    incidents of flash flooding to accompany severe weather risk.

    DISCUSSION...GOES-E WV suite depicts secondary upper-level low
    deepening across OK/N TX with lower scale shortwave resulting in
    some negative tilting. This results in broadening of dual jet
    structure with very impressive downstream baroclinic shield across
    the Mid-MS Valley into Lower Ohio Valley denoting the very strong
    divergence aloft, especially in proximity to 130kt 250H jet streak
    exiting over N IL into LP of MI. The wedge of diffluence across
    the area of concern will provide strong large scale ascent to
    maintain the well above average low level wind flow; 850mb 50-65kt
    southerly with backed sfc to boundary layer 20+ kt flow pumping
    higher theta-E air across E MS/AL into southern Middle TN with Tds
    increasing from low 60s to upper-60s/low 70s. Mid-level EML has
    been mixing out, but has allowed for increasing unstable air mass
    (2000-2500 MLCAPE) along the sharp pre-frontal pressure trough
    from W TN back to a developing surface wave in NE LA. Overall the
    strength of the low level flow and solid low level moisture (up to
    1.5" TPW) resulting in highly anomalous flux values near 3-3.5 Std
    Dev from normal and generally about 1000+ kg/m/s of IVT.

    As such, very strong, broad and likely rotating updrafts will
    further enhancing localized moisture flux due to isallobaric flow
    but also strong convergence to add about .5"/hr to general
    updrafts. WoFS solutions continue to have many of the runs
    supporting .3-.5"/5 minute rates with this broader cores allowing
    for increased duration and hourly totals of up to 2"/hr. So any
    given storm may overwhelm urban/prone flooding locations even if
    isolated or along/ahead of the main line. The greater concern,
    particularly further north where deeper mean flow will allow for
    more of pivot point to develop for the longer line of cells,
    should increase potential for SW to NE training convection,
    especially near/downstream of the surface wave as it lifts from NE
    LA across central MS to Middle TN.

    Current surface observations and RADAR mosaic suggest a weak
    WAA/isentropic boundary across south-central Middle TN eastward
    toward the southern Cumberland Plateau due to earlier convection.
    WoFS, HRRR and RAP rapidly refreshing guidance all suggest, this
    boundary will maintain with a buckle noted in the SB/MLCAPE fields
    though MUCAPE will support elevated convection downstream across
    northern Middle TN into south-central KY. As such, this
    inflection near the MS/TN/NW AL border continues to be highest
    potential for those longer duration/training events with 4-5"
    totals possible through 22z...slowly lifting northeastward across
    Middle TN into the later evening hours. This also overlaps with
    rainfall reduced FFG values and will likely result in scattered to
    numerous incidents of flash flooding this afternoon into early
    evening. Scattered incidents are likely further north into KY
    where FFG and instability are lower; as well as south into central
    MS where cells will be stronger, but duration is likely to be
    lower and FFGs a bit higher.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6ZunH1fZ5lizEHjEz_LL0-V-fh5nX6MlqJl6Dj25tXUpVt2WUpoBFRZ_K2-GwNxLW1QR= LIf3igJylnBuPn6SlBJ0tf4$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LMK...MEG...OHX...PAH...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 37528646 37418538 36678505 35748543 34328659=20
    32888788 32158867 31798983 32109095 33489055=20
    34948934 36448791=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 15 18:51:18 2025
    AWUS01 KWNH 151850
    FFGMPD
    OHZ000-INZ000-152230-

    Mesoscale Precipitation Discussion 0064
    NWS Weather Prediction Center College Park MD
    249 PM EDT Sat Mar 15 2025

    Areas affected...Central and Eastern Indiana into Adj. Northwest
    Ohio...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 151850Z - 152230Z

    SUMMARY...A very narrow band of thunderstorms ideally oriented to
    the moisture gradient and deep layer steering flow and of
    sufficient length for training to exceed lower FFG values in the
    region suggest an incident or two of localized flash flooding is
    possible.

    DISCUSSION...GOES-E WV overnight into early this morning noted the
    strong cyclone across the Upper Great Lake region resulted in a
    strong, elevated mixed layer (EML) extending well northwest into
    the Ohio River Valley and central Great Lakes region, with
    dust/soil and smoke particulates noted with it in the visible
    imagery. This mixed layer has a surface reflection noted by a
    frontal/dewpoint gradient across central IL into NW IND, with 40s
    quickly becoming upper 50s and mid 60s across central and southern
    IND. Clear skies this morning provided short-duration but ample
    insolation for instability to build with SBCAPEs reaching near
    1000-1500 J/kg mainly along and south of the boundary.

    The WV suite also notes a broadening baroclinic shield of high
    cirrus moving across the area associated with a broadening
    diffluent region across the Ohio River Valley as a 130kt 250mb jet
    streak continues to wrap along the interface of the older cyclone
    and the approaching strengthening one from the Southern Plains.=20
    This has provided strong divergence aloft along the broad right
    entrance region of the jet and in turn lead to the acceleration
    and backing of the low level jet across the TN Valley into the
    region. Southerly winds intersecting with the SW to NE gradient
    within the area of surface based instability provided sufficient
    moisture convergence to generate thunderstorms along and south of
    this axis within the area of deeper surface to boundary layer
    moisture. Initial thinking was the cores of updraft would be
    narrow given limited instability/surface heating. Strong steering
    flow would also result in quicker SSW to NNE cell motion and the
    probability of intersection of narrow updrafts would be limited.=20
    However, recent trends note the stronger heating and moisture flux
    convergence has resulted in slightly broader up/downdrafts while
    also expanding longer along the convergence axis. Combined with
    nearly parallel deeper layer steering and all 3 components are
    start to result in a narrow axis of intense thunderstorms with
    hourly rates of 1-1.5"/hr.=20

    Given the length is about 80 miles, there is solid potential for
    spots of 1.5-2" totals within 1-2 hours. FFG values are already
    low from slower green-up with 1hr values between 1-1.5 and 3hr
    values less than 2" along the training axis. As such, localized
    flash flooding is considered possible, even if only a few
    neighboring watersheds are impacted. The risk for flash flooding
    is likely to be limited in time given quick erosion of remaining
    downstream unstable area and may only exist for a few more hours
    before weakening.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_UivbsJzSPcg_k9OS7bFSpmk5XzP2UNVT1RHNVTblUqpFgwUKiN8sZnwlFcXLBFksmHQ= e5xLrnDHs6iNGoOdX9t6ecQ$ for graphic product...

    ATTN...WFO...ILN...IND...IWX...

    ATTN...RFC...OHRFC...NWC...

    LAT...LON 41248449 40808418 39948506 38878650 39058701=20
    40478589 41238521=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 15 20:46:48 2025
    AWUS01 KWNH 152046
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-160230-

    Mesoscale Precipitation Discussion 0065
    NWS Weather Prediction Center College Park MD
    446 PM EDT Sat Mar 15 2025

    Areas affected...Eastern LA...Southeast MS...Southern AL....

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 152045Z - 160230Z

    SUMMARY...Lines of rotating cells are starting to congeal into a
    more single line and starting to advance eastward. Better
    alignment of moisture and instability axis will retain moisture
    flux to support up to 2"/hr rates; however, a more easterly
    component may reduce some training and therefore flash flooding
    will become more scattered in nature over higher FFG.=20

    DISCUSSION...GOES-E WV suite depicts core of negative tilt
    shortwave has swung through Arkansas into the middle MS valley,
    this has resulted in low level veering and alignment of the
    moisture and instability axis across E LA into S MS. Currently,
    merging cells across the best confluence in S MS is resulting in
    higher than average rainfall rates (to other cells) due to
    slightly backed flow downshear of surface low near BTR. Moisture
    flux of 20-25kts of low 70s Tds and 2000-2500 J/kg of MLCAPE will
    maintain strong updrafts and efficient low level moisture flux
    convergence for rates of 2"/hr, perhaps as high as 2.5-3" for very
    short periods when isallobaric flow increases with cycling of updrafts/supercells.=20

    Upper-level flow is starting to increase with overspreading of WSW
    3H jet over 110kts, increasing easterly propagation component to
    the convective line. This will reduce training in the longer
    period, so supercells will continue to remain efficient along the
    line with streets of 2-3" totals possible. Combined with the
    generally higher FFG values across S MS/AL and E LA, flash
    flooding should become more scattered/isolated in nature as the
    line increases forward speed. However, there are numerous prone
    urban centers, particularly along I-10 that may be quickly
    over-whelmed by 1-2" sub-hourly totals if directly impacted by the
    leading broad downdrafts. As such, flash flooding is considered
    possible across the area of concern. An additional MPD will be
    issued subsequent to discuss higher likelihood flooding conditions
    further north.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!47acq6U6UiFDtOn5lz9LnQ7bSRAEohWdHH8qHVXCHooew4f0BdlG2iwOFFw53xlugh5a= 2eMIAF4cfO_voMfiU4v6nrw$ for graphic product...

    ATTN...WFO...BMX...JAN...LIX...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 33398592 32748566 31788611 31128717 30488834=20
    29839028 30519073 31999005 32718931 33318745=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 15 21:29:17 2025
    AWUS01 KWNH 152129
    FFGMPD
    GAZ000-TNZ000-KYZ000-ALZ000-MSZ000-160315-

    Mesoscale Precipitation Discussion 0066
    NWS Weather Prediction Center College Park MD
    528 PM EDT Sat Mar 15 2025

    Areas affected...Middle & Eastern TN...Northeast MS...Northern
    AL...Northwest GA...South-Central KY...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 152130Z - 160315Z

    SUMMARY...Multiple lines of thunderstorms with moderate shield
    precipitation between crossing already saturated/low FFG soil
    conditions, likely to continue flash flooding risk through to
    early overnight period.

    DISCUSSION...A very complex surface pattern exists across the
    middle MS Valley due to the back to back strong upper-level
    shortwaves. This continues through depth with the EML from the
    prior stronger closed low being modified by earlier convection
    this morning across E TN/N MS; while a secondary dry slot is
    starting to manifest across AR in the wake of the secondary
    shortwave now maturing across S MO. As such, surface moisture
    though worked over, remains across E TN/W KY/N MS with TDs still
    in the upper 50s/lower 60s. However, strong LLJ in response to
    the shortwave has allowed for the western branch of low level
    moisture and warming at the boundary layer to wash through and
    with steepening lapse rates from the new EML; an expanding area of
    MUCAPE is developing across NE MS and W Middle TN in the wake of
    the stronger cells further east. As such, there is an expectation
    of the stronger forcing along the cold front and lifting surface
    low across N MS to expand elevated thunderstorms along the leading
    edge further into W Middle TN. MUCAPEs of 500-1000 J/kg will
    increase over the next few hours and feed cells and given strong
    low level moisture flux convergence allow for increasing rainfall
    potential with 1-1.5"/hr rates possible. This is going to fall on
    areas already saturated/flooded by earlier rounds of thunderstorms
    (see below) and likely to exceed the compromised FFG values at or
    below 1.5 at 1-3 hour time periods.

    Ahead of this new development, the initial storms continue to
    press eastward across E Middle TN into the Cumberland Plateau as
    well as extending back as a pre-frontal convective line across N
    AL and NE MS. A broad shield of moderate precipitation is likely
    to continue between these two lines maintaining flooding
    conditions through the late evening/early overnight period.=20=20
    Cells to the east are starting to weaken a bit, with reducing
    lightning mainly has area has only received advected higher
    theta-E air from central AL/NE GA given cloud cover inhibiting
    insolation throughout the day. Still, there is weak but
    sufficient MUCAPEs into E TN and far S KY to maintain some. A
    spot or two of 3-4" remains possible organization over the next
    few hours. Rates of 1-1.5"/hr are probable given the broad,
    strong LLJ pumping 1.5-1.75" TPW (mainly below 700mb) on 50+kts of
    850mb southerly flow/WAA. As such, rainfall pattern will show
    broad area of 2-3" across much of the eastern half of TN and
    northern AL where multiple rounds will cross with embedded
    weakening but intense showers to overtake those lower FFG
    values/saturated soils in the region keeping flash flooding likely
    through much of of the evening into early overnight period; but a
    spot or two of 3-4" may result in considerable or even significant
    flash flooding possible.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9BAOaS0GR8qN_Lw5l6zu_8ndMnqMO_QKRe3gr0a_a7eWDmIYEO2pGoZ15D8wpzhZB-H9= YbKfZSHxeuDjH6T-pjLeEpY$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...JAN...JKL...LMK...MEG...MRX...
    OHX...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 37158440 36498387 35568421 34458484 33638532=20
    33158642 32408895 32688965 33928905 35528824=20
    36368765 36728673 37148538=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 15 23:13:49 2025
    AWUS01 KWNH 152313
    FFGMPD
    CAZ000-ORZ000-160915-

    Mesoscale Precipitation Discussion 0067
    NWS Weather Prediction Center College Park MD
    713 PM EDT Sat Mar 15 2025

    Areas affected...Southwest Oregon...Far Northwest CA...

    Concerning...Heavy rainfall

    Valid 152315Z - 160915Z

    SUMMARY...Persistent solid, relatively unwavering moist onshore
    flow to bring average .25"/hr & up to .5"/hr rates; resulting in
    localized totals of 4-5" in Coastal Range of SW Oregon and 2-3"
    across lower slopes of southern Oregon Cascades.=20

    DISCUSSION...GOES-W WV suite shows classically anti-cyclonically
    curved strong upper-level jet with axis starting to near the
    Oregon coast in the next hour or so. A highly sheared
    vorticity/shortwave center along the northwest edge of the axis
    will slide northeast into WA and leading nose of enhanced low to
    mid-level moisture plume will reach the south-central to southwest
    Oregon coastline. Winds will veer to SWly and increase from
    40/45kts to 50-60kts by 03z. Visible imagery loop shows moisture
    axis as well defined mid-level clouds with a line of enhanced, but
    still shallow verticality that extends from near the ridge apex at
    126W to 39N136.5W and 35.5N141W aligned with both the enhanced
    moisture and surface to boundary layer convergence/confluence
    axis. Very slow eastward advancement of the axis will retain
    consistency in placement between N Coos to S Curry county in
    Oregon for the next 9-12hrs. IVT values of average of 500 will
    peak toward 750 kg/m/s throughout the late evening into early
    morning hours. Combine this with favored orographic ascent will
    allow for current .15-.25"/hr rates to increase to .33" to
    occasionally .5"/hr rates in the SW OR boreal rain forest for that
    duration.

    This should result in localized 4-5" totals across SW Oregon,
    while downstream, the moisture will be slightly reduced having
    wrung out on the Coastal Range, but rates of .25-.33"/hr across
    the Southern Oregon Cascades may allow for spots of 2-3" totals by
    12z. This will be fairly focused and solid, given the location is
    fairly accepting of these rainfall totals, increased run-off
    should feed rivers but not likely result in rapid
    run-off/inundation. As such, will leave this Atmospheric River as
    Heavy Rainfall tag at this time.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5zSf8W_nkpEGKMSaxA5uhOGgHaTwtXSPZidNkJWNTvODKinYFpU2Mr5iSP1OoZab4pEn= BPgvyOul0YIfudJS1Vkn3OU$ for graphic product...

    ATTN...WFO...EKA...MFR...PQR...

    ATTN...RFC...CNRFC...NWRFC...NWC...

    LAT...LON 44932234 44342219 43732228 43082226 42512226=20
    42642271 42482332 41762335 41632368 41912437=20
    42562454 43202456 43962431 44422419 44622389=20
    44412352 44242311 44732266=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 16 02:10:15 2025
    AWUS01 KWNH 160209
    FFGMPD
    GAZ000-ALZ000-160600-

    Mesoscale Precipitation Discussion 0068
    NWS Weather Prediction Center College Park MD
    1008 PM EDT Sat Mar 15 2025

    Areas affected...east-central Alabama into
    west-central/northwestern Georgia

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 160207Z - 160600Z

    Summary...A cluster of intense convection was producing areas of
    1-2.5 inch/hr rain rates just south of the Birmingham Metro area.
    Some concern exists that this activity could persist eastward,
    eventually reaching the Atlanta Metro area through 04Z/midnight
    EDT.

    Discussion...Deep, intense convection has materialized throughout
    a strongly sheared, unstable warm sector across
    central/southwestern Alabama today. More recently, a cluster of
    strong storms (including LEWPs/bows and trailing/training
    convection) has produced a localized area of 1-2.5 inch/hr rain
    rates just south of Birmingham over the past 1-2 hours. These
    rates were approaching FFG thresholds (generally in the 2-inch/hr
    range), and areas of at least minor excessive runoff are apparent
    given MRMS Flash responses across the region.

    Some concern exists that this complex will persist northeastward,
    likely crossing the AL/GA border region by 03Z and reaching
    portions of the Atlanta Metro area through/after 04Z. The extent
    of the flash flood threat may be mitigated by weaker downstream
    instability (upper 50s F surface dewpoints contributing to only
    around 500 J/kg MUCAPE), which could weaken updraft intensity.=20
    However, current convective organization and strong shear should
    maintain heavier downpours downstream into northwestern Georgia
    and result in at least a few areas of 1 inch/hr rainfall rates -
    potentially affecting populated areas such as Atlanta Metro.=20
    Given the scenario, at least an isolated flash flood threat should
    evolve with this convective cluster through 06Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6PkgW2rrRmHcCDSXjUmR1bBndN5Ha0sfrL1oFVZ-5d3mQFMLQT_odohRJTK106XMbTuo= ega-CxuyvNF2pZP_4Qx8dwg$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34518516 34418416 33868353 33298349 32998378=20
    32578531 32368759 33128757 34098620=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 16 03:27:30 2025
    AWUS01 KWNH 160326
    FFGMPD
    VAZ000-TNZ000-KYZ000-160925-

    Mesoscale Precipitation Discussion 0069
    NWS Weather Prediction Center College Park MD
    1125 PM EDT Sat Mar 15 2025

    Areas affected...middle/eastern Tennessee into central Kentucky

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 160325Z - 160925Z

    Summary...Flash flood potential continues across large portions of
    Tennessee and Kentucky. This risk should gradually end from west
    to east as a surface trough migrates eastward across the area
    through 09Z.

    Discussion...Widespread heavy rainfall for much of the day has wet
    soils and caused many reports of flash flooding today especially
    across Middle Tennessee. 2-7 inch storm total amounts have
    fallen, and flash flood guidance depicts widespread areas of
    near-zero hourly thresholds from far northwestern Alabama through
    north-central Kentucky at the latest update. Meanwhile,
    widespread rainfall continues to occur. Most of the rainfall is
    light in nature and related to a strong convective MCS centered
    over Alabama. A narrow corridor of stronger convection has
    redeveloped from near Nashville to Huntsville, however, that
    contains areas of 1 inch/hr rain rates at times. This corridor of
    stronger convection likely represents the end of the heavy
    rainfall threat as it shift eastward across the discussion area
    through the early overnight hours as only lighter/isolated shower
    activity is noted to its west.

    Between now and 09Z, another 0.5-1 inch of rainfall can be
    expected areawide (with locally higher amounts). These rainfall
    totals will exacerbate ongoing flooding and perhaps lead to
    additional runoff problems in sensitive areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9dN27J2wElsZ0LJKjflZPrbFzsvJ7zDOs7MCr5Bq9ZmTYbn3GXJVizrxZ1i4jQ9mXhbk= 48RZ5tme3tJFwH3cbpWvU2o$ for graphic product...

    ATTN...WFO...HUN...ILN...JKL...LMK...MRX...OHX...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 38698453 38528347 37578314 36048367 35078458=20
    35028645 35758673 36858638 38318563=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 16 05:41:23 2025
    AWUS01 KWNH 160541
    FFGMPD
    GAZ000-ALZ000-160840-

    Mesoscale Precipitation Discussion 0070
    NWS Weather Prediction Center College Park MD
    140 AM EDT Sun Mar 16 2025

    Areas affected...a small part of southeastern Alabama and
    southwestern Georgia

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 160540Z - 160840Z

    Summary...Localized training of storms on the southwestern flank
    of a linear MCS near Columbus could pose a localized flash flood
    risk over the next couple hours.

    Discussion...Scattered to numerous thunderstorms have grown
    upscale into an extensive linear segment from near La Grange to
    Columbus, GA over the past couple hours. On the southwestern
    flank of this MCS, scattered convection continues to increase in
    coverage and intensity generally in the area of Troy and
    Andalusia, AL. These storms are in a very strongly sheared, moist
    and unstable environment with minimal capping. Additionally,
    surface wind vectors suggest strong, focused convergence along the
    southwestern end of the linear MCS that, when combined with nearly
    2 inch PW values, should support areas of training/backbuilding
    especially within the stronger instability across southeastern
    Alabama. Areas of 2-2.5 inch/hr rain rates have been estimated on
    the southwestern flank of the MCS (southwest of Columbus), and
    short term trends suggest that heavy rainfall should continue in
    this area for at least another couple hours until a surface trough
    (extending along I-65 from Montgomery to Evergreen) translates
    eastward through the area later tonight.

    The mesoscale pattern could support an instance or two of flash
    flooding as rainfall totals approach FFG thresholds (generally in
    the 2.5 inch/hr and 3 inch/3-hr range) over the next couple hours.
    An additional 2-3 inches of rainfall cannot be ruled out in the
    wake of the initial MCS. Weaker surface-based instability over
    Georgia should mitigate the eastward extent of the flash flood
    risk.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6mEZyfPIG80kwjuD4vnYA886Ysn63JTQ9nX8dTa7J3dXElvIf8YGal2xt3OqGplQ3jY2= WWrRlmJ6H3RHHhq8mQB9Jro$ for graphic product...

    ATTN...WFO...BMX...FFC...MOB...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 32408483 31968419 31168462 31188599 31418651=20
    32288564=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 23 14:27:24 2025
    AWUS01 KWNH 231427
    FFGMPD
    WAZ000-240230-

    Mesoscale Precipitation Discussion 0078
    NWS Weather Prediction Center College Park MD
    1026 AM EDT Sun Mar 23 2025

    Areas affected...Northwest Washington....

    Concerning...Heavy rainfall

    Valid 231430Z - 240230Z

    SUMMARY...Prolonged onshore moisture flux across Olympics and
    lower Foothills of northern WA Cascades may result in spots of
    3-5" totals, given over .33"/hr average rates. Saturated grounds
    and some snow melt may increase run-off increasing stream flows.

    DISCUSSION...GOES-W WV suite depicts a strong upper-level jet
    across the northeast Pacific/southern Gulf of Alaska crossing
    central BC before extending southeast into the southern Canadian
    Rockies resulting in solid ridging across the Pacific Northwest
    with apex of the ridge just west of the coast. This allows for
    moderate divergence aloft across southwest BC/northern WA which is
    expected to persist through much of the day today allowing for
    solid westerly onshore, ascending flow into this divergent area.=20
    The southern edge of a warm front has reached the NW WA coast and
    is aiding in the ascent/WAA which has started to increase over the
    last hour or so across the Olympics. Additionally, this leading
    pulse has brought increased low to mid-level moisture via a very
    broad atmospheric river plume with sfc-850mb LPW values in the
    .5-.6" range with a dual core 850-700mb flow of .25-.3", though
    the northern plume/fetch is longer more directed toward southern
    Vancouver Island and the NW tip of WA. As a result, 1-1.2" total
    PWats are expected being fluxed with 35kts increasing to 50+kts
    toward 18-21z. Overall IVT values will increase from 400-450
    kg/m/s currently peaking at 650-700 kg/m/s toward 21-00z...then
    leveling out around 500 kg/m/s for the rest of the evening into
    the overnight.=20=20

    The plume's orientation will remain steady through this surge of
    moisture flux and favorably intersect the Olympic range with rates
    of .15"/hr currently to increase to near/just over .5"/hr in the
    best orographic ascent by 18z. The core of the flux will be
    north into southern Vancouver Island, but will then slide toward
    the northern WA Cascades through the late afternoon/early evening
    increasing rates of .25-.33", perhaps occasionally reaching .5"/hr
    at the peaks. The depth of warm air will result in freezing
    levels lifting above all but the highest peaks. This has a
    combination of those high rates but also rain upon snow.=20
    Temperatures are not going to be significantly over freezing, so
    melt may be a bit slow, but will contribute to run-off. Soil
    saturation values are very high (or even 100% due to snow pack),
    so much of the water from rainfall will run-off too increasing
    potential for above average stream flow but not likely to rise
    fast enough for rapid-rise/flash flooding.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7u5LhiU2H0T2GdeZ8a0qufxxSFrwQchurSmg0fp_8FpNZ0CDyOeeFItU1Ry6XEvV_GMI= UmW2gV4K632D0NIAFMNNgdA$ for graphic product...

    ATTN...WFO...SEW...

    ATTN...RFC...NWRFC...NWC...

    LAT...LON 49132248 49112172 48982125 48322116 47602148=20
    47452178 48022208 48152248 48042298 47812312=20
    47472321 47272338 47212383 47322417 47592451=20
    47942466 48362485 48432447 48222370 48432313=20
    48772304 49092285=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 23 22:06:13 2025
    AWUS01 KWNH 232206
    FFGMPD
    TNZ000-ALZ000-MSZ000-ARZ000-240400-

    Mesoscale Precipitation Discussion 0079
    NWS Weather Prediction Center College Park MD
    605 PM EDT Sun Mar 23 2025

    Areas affected...Western & Middle TN...Northern MS...Northwest
    AL...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 232205Z - 240400Z

    SUMMARY...Multiple rounds of intense showers/thunderstorms with
    rates of 1-1.5"/hr may allow for a few streets of repeating cells
    and 2-3" localized totals nearing/exceeding FFG values resulting
    in possible widely scattered incidents of low-end flash flooding,
    particularly near urban centers.

    DISCUSSION...GOES-E WV suite depicts a strong, compact short-wave
    across N IL/S WI moving quickly east with a lower-scale
    wave/mid-level trough accelerating eastward into the upper-Ohio
    River Valley. This is accompanied by a strong upper-level jet
    streak that has rounded the base of the main trof with solid right
    entrance ageostrophic response across the lower Ohio Valley
    providing strong divergence along and south into the Tennessee
    River Valley.=20

    Surface and LLJ has responded with increasing Southwesterly flow
    fluxing higher theta-E air northward with Tds into the upper 50s
    and lower 60s. Filtered insolation and mid-level steepening lapse
    rates have made the area modestly unstable with MLCAPE nosing
    across W KY into W TN over 1000-1250 J/kg, along and ahead of
    solid cold front. Additionally, GOES-E Vis and sfc to boundary
    layer streamlines suggest a confluence axis between deeper Gulf
    moisture from the Western Gulf and return from the central/eastern
    Gulf becoming increasingly confluent across central MS to NE MS
    into Middle TN. With conditionally unstable air, this has been
    sufficient to break out weaker but slowly increasing convective
    activity across Middle TN... with some convection/flux convergence
    supporting rates of .5-.75", which is expected to increase over
    the next few hours. Forward propagation is likely to limit
    overall totals with any individual cell, but could be stage
    setting for later development.

    As the line expands, cells will have capability for
    back-building/flanking line development that is probable to align
    with strong/fast steering flow resulting in some accidental
    training. However, further upstream cold front is starting to
    advance with solid 90 degree convergence along the leading edge
    southwesterly LLJ/moisture plume. Cells will expand in coverage
    and width and should be capable of 1-1.5"/hr rates as they
    advance, with similar very fast (40+ kt) forward speed, likely
    limiting overall rainfall totals. Hence, any flash flooding
    potential will require these cells to traverse areas already
    affected by 1-2" totals with earlier rounds. If so, 2-4hr spot
    totals of 2-3" are possible. This is in range of the lower FFG
    values over the TN valley (1.5-2"/hr & 2-3"/3hr). As such, a few
    widely scattered instances of flash flooding are considered
    possible particularly after 00z and in/near urban settings.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5qS4wqKO0XRxof-tpw08nyp5JjttqzzEKkAI-JFPw30tXIEzHdpdsUsi4_LyUGI1LFvE= ooBcRUDKd0DxmmOzIwDWIKM$ for graphic product...

    ATTN...WFO...BMX...HUN...MEG...OHX...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36488810 36478551 35158602 34288698 33908848=20
    34009006 34279071 34979061 35638953=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 23 22:57:51 2025
    AWUS01 KWNH 232256
    FFGMPD
    MSZ000-LAZ000-ARZ000-240430-

    Mesoscale Precipitation Discussion 0080
    NWS Weather Prediction Center College Park MD
    656 PM EDT Sun Mar 23 2025

    Areas affected...Northern LA...Southern AR...Central MS...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 232300Z - 240430Z

    SUMMARY...Strong moisture flux convergence with initial convective
    development will allow for very quick moisture loading and strong
    downdrafts capable of quick 2"/hr rates (15-minute totals of
    1-1.5" psbl). As cold front moves east, interaction with older
    warm sector convection may allow for localized repeating/training
    and spot totals of 2-3" in 1-2hrs resulting in possible flash
    flooding.

    DISCUSSION...GOES-E Visible/10.3um and RADAR mosaic denote
    scattered destabilization occurring across the warm sector mainly
    along the Lower Mississippi River Valley at the intersection of
    the nose of instability axis (2500-3000 J/kg) of MLCAPE that
    extends from the Heart of Texas into northeast LA and the nose of
    the deepest sfc to 850mb moisture core (LPW of .8-.9") across
    south-central LA into northeast LA. This boundary layer moisture
    is quickly advancing northward toward a southward pressing/well
    defined (steep isentropes) that is bisecting AR from NE to SW.=20
    These cells are expected to be slower moving but with steering
    more northward toward the frontal zone before effective bulk shear
    increases due to stronger flow aloft across the Delta Region into
    the Bootheel of MO. The collision of the air masses is likely to
    result in rapid convective development along the front from NW MS
    across S AR into N LA and eastern TX mainly in the 01-02z time
    frame. There has been solid signal throughout the day toward this
    time frame, but trend in the HRRR is a bit earlier and more
    focused resulting in very strong moisture flux loading to the
    line. Stronger mid-level dry air will likely aid stronger
    downdrafts due to mixing but given loading is expected to have
    heavy rainfall totals in quick sub-hourly amounts.=20=20

    Experimental HRRR 15-min estimates 1-1.25" at onset around 0130z
    become near 1.75" by 02-03z across N LA. Hourly totals of 2-2.5"
    seem plausible given weaker overall steering before cold
    front/outflow boundaries begin to organize and advance eastward.=20
    While soil moisture is about 45-55% (in all but the braided
    portions of the MS River...65+% there), this is running in the
    10-15th percentile, suggesting upper-soils may initially not allow
    much infiltration). Still, the spotty/smaller areal coverage may
    limit the overall magnitude of flash flooding suggesting highly focused/localized at least initially across S AR/N LA for spotty
    possible flash flooding. It is only later toward 04-06z with
    some organization and potential west to east training that
    localized totals may reach 2-4" through 06z. 18z HREF and recent
    HRRR runs support the best probability to be in proximity to the
    AR/LA/MS intersection and points east-northeastward. Confidence
    is increasing toward possible scattered incidents of flash
    flooding through this time period before cells become too
    scattered/progressive generally after 06z, but will continue to
    monitor trends closely.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7hIGogkyekcaPFZ5mQuNuFDncu-1T3xDaKXSDtqWIBkgl9Xr33WqK0aQHxJBgQFIzTQH= TN2pU1KMFLkxjA2r89twVmg$ for graphic product...

    ATTN...WFO...JAN...LZK...MEG...SHV...

    ATTN...RFC...LMRFC...SERFC...WGRFC...NWC...

    LAT...LON 34389006 34318925 34248863 33868836 33378837=20
    32958857 32398922 32039070 31829179 31709325=20
    31989383 32779367 33569269 34099146=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Mar 24 04:21:59 2025
    AWUS01 KWNH 240421
    FFGMPD
    ALZ000-MSZ000-LAZ000-241020-

    Mesoscale Precipitation Discussion 0081
    NWS Weather Prediction Center College Park MD
    1221 AM EDT Mon Mar 24 2025

    Areas affected...northern LA into central MS and western AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 240420Z - 241020Z

    Summary...Periods of training thunderstorms may produce areas of
    isolated to widely scattered flash flooding through 10Z across
    portions of northern LA, central MS and western AL. Peak rainfall
    rates between 1-3 in/hr and spotty totals of 2-4 inches are
    expected through 10Z.

    Discussion...04Z regional radar imagery showed a WSW to ENE line
    of thunderstorms that extended from northern LA into northern AL.
    This line formed earlier within an axis of pre-frontal confluence
    and has since become the dominant area of convection across the
    Lower Mississippi Valley. Farther north, closer to the cold front
    itself, were a few scattered thunderstorms, mainly located in TN.
    04Z SPC mesoanalysis data showed the environment from northwestern
    AL to northern LA contained 500 to 1500+ J/kg MLCAPE (highest to
    the west over northern LA) and 1.2 to 1.5 inches of PWAT.

    Expectations are for the line of storms to continue advancing
    southeastward, ahead of the cold front and along the leading edge
    of rain-cooled outflow which has since formed behind the advancing
    line. While storm motion should remain progressive and not pose a
    significant threat for flash flooding, the environment is, and
    will continue to be, capable of producing 0.5 to 1.0 inches of
    rain in 15 minutes given forecasts of lingering instability over
    the next several hours. Where convective orientation matches the
    mean steering flow from the WSW, training will produce 1-2 in/hr
    rates, perhaps exceeding 2 inches in an hour. The result will be
    spotty 2-4 inches of additional rainfall through 10Z, although the
    higher end of that scale is considered a much lower probability of
    occurrence. Given relatively high flash flood guidance values
    (especially over southern portions of the MPD threat area), any
    areas of flash flooding that develop will likely be tied to areas
    of poor drainage, particularly those of urban nature.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5iNlAJLMPBL0LowdHFEYBBf6NSLZE3NmvkpPJCf1XN80ciwOnFlAfZocorpASxeUuuTZ= 5vLHHIRe69SoHcrcizDE3oM$ for graphic product...

    ATTN...WFO...BMX...JAN...MEG...MOB...SHV...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 33898746 33168677 32388762 31658960 31399127=20
    31559306 32459350 32829180=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Mar 24 13:00:54 2025
    AWUS01 KWNH 241300
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-241659-

    Mesoscale Precipitation Discussion 0082
    NWS Weather Prediction Center College Park MD
    900 AM EDT Mon Mar 24 2025

    Areas affected...coastal Mississippi, southeastern Louisiana, far
    southwestern Alabama

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 241259Z - 241659Z

    Summary...A couple of linear convective complexes are merging and
    could pose an isolated flash flood threat over the next 2-3 hours
    from New Orleans Metro eastward through Mobile, AL.

    Discussion...Radar mosaic imagery depicts a couple of linear
    convective complexes across the discussion area: 1) extending
    along an east-west axis from near Mobile, AL to just north of
    Baton Rouge, LA that was moving slowly southward and 2) a
    faster-moving complex approaching an axis from Hammond to Morgan
    City, LA. The orientation of these complexes has fostered some
    localized training/repeating, with 1-1.5 inch/hr rain rates noted
    per MRMS on a spotty/localized basis. These rates are generally
    below FFG thresholds, although some concern exists that as the
    convective complexes continue to merge, areas of 1+ inch/hr rain
    rates could materialize across more urbanized areas of the region
    (generally from New Orleans proper to Mobile) and cause
    spotty/isolated flash flooding to materialize. This threat
    appears to be highest along the Mississippi Gulf Coast over the
    next couple hours.

    Both of the linear complexes are progressive enough to suggest
    that most of this morning's isolated flash flood threat should end
    during the 16Z/11am CDT hour.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_sSfTvyit0fsLPPkcLyhhxiqZLlLuSS5ctoiw9pr19Q5N0fWB7y1XZrpyltdpsig9m2E= 5St-nugHTgro9SwwZt9Ep34$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 31488818 30878748 30398748 29798898 29369018=20
    29539131 30369107 31189086 31448943=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Mar 25 18:28:02 2025
    AWUS01 KWNH 251826
    FFGMPD
    FLZ000-260025-

    Mesoscale Precipitation Discussion 0083
    NWS Weather Prediction Center College Park MD
    225 PM EDT Tue Mar 25 2025

    Areas affected...Southeast FL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 251825Z - 260025Z

    SUMMARY...Heavy showers and thunderstorms expanding over southeast
    FL may result in some urban flash flooding over the next few hours.

    DISCUSSION...The latest GOES-E visible satellite imagery in
    conjunction dual-pol radar shows the development and expansion of
    heavy shower and thunderstorm activity over southeast FL, with an
    emphasis on Miami-Dade County. Cooling cloud tops are noted in a
    southwest to northeast fashion from over and west of Homestead and
    stretching northeast into the Miami metropolitan area.

    A combination of a front settling gradually south down the FL
    Peninsula coupled with localized seabreeze convergence near the
    urban corridor will facilitate additional convective development
    this afternoon. A moderately moist and unstable environment is
    already in place with MLCAPE values of 1500+ J/kg and PWs of 1.5+
    inches. This coupled with 30 to 40+ kts of effective bulk shear
    will favor slow-moving and relatively organized convective cells
    capable of producing rainfall rates of 1.5 to 2.5 inches/hour.
    Some localized storm totals going through early this evening of 3
    to 5 inches will be possible.

    While FFGs are very high, these rains are expected to impact
    portions of the highly urbanized/populated urban corridors from
    Homestead northward up to Fort Lauderdale and possible even West
    Palm Beach as the activity further expands in coverage. As a
    result, a concern for urban flash flooding will exist over the
    next several hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6fezOdQZdpWSnZPkSSd7WX3xSI_FOMCiYoS75JXtNKoRd0-L7Phtqc4hqKdVD0huC7Z9= 2lNVrYtUewlHRm9qsaj5Hk4$ for graphic product...

    ATTN...WFO...MFL...MLB...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 26988032 26918004 25998000 25398033 25278061=20
    25448082 25938057 26498039=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Mar 26 04:30:15 2025
    AWUS01 KWNH 260430
    FFGMPD
    ARZ000-TXZ000-OKZ000-261015-

    Mesoscale Precipitation Discussion 0084
    NWS Weather Prediction Center College Park MD
    1229 AM EDT Wed Mar 26 2025

    Areas affected...south-central OK into northern TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 260428Z - 261015Z

    SUMMARY...Repeating and training of thunderstorms from south
    central OK into portions of northern TX may produce localized
    flash flooding later tonight. Potential for 2 to 4 inches along
    with rainfall rates of 1 to 2 in/hr (locally higher) will exist
    through 10Z.

    DISCUSSION...A combination of GOES East infrared satellite and
    regional radar imagery at 04Z showed widely scattered
    thunderstorms from northeast of DAL to south of OKC. Cloud tops
    were generally warming over TX but new development was occurring
    across south-central OK where low to mid-level moisture transport
    was allowing for generally weak instability to build northward
    from the Red River, north of a quasi-stationary front analyzed
    over northern TX. The new development was occurring at the nose of
    a 30-35 kt 850 mb low level jet as sampled by VAD wind data at
    KDYX and KFWS, about 10-15 kt stronger than F000 and F001 hour RAP
    guidance suggests.

    Nocturnal strengthening of the low level jet is expected to
    continue through ~06Z with a max axis between SPS and GYI,
    supporting the overrunning of the quasi-stationary front. A
    relatively small pocket of elevated instability between 500 and
    1500 J/kg is forecast by the RAP to be in place from between I-20
    and I-40 on either side of I-35 over the next several hours, but
    should lower in magnitude toward 12Z.

    Thunderstorms are expected to continue to increase in coverage
    over south-central OK over the next 1-3 hours, with mean steering
    flow aligned roughly parallel to the surface front, repeating
    cells along with instances of training are expected. However, any
    clustering of thunderstorms may result in more of a southward
    propagation of cells into the inflow layer. Sufficient speed shear
    exists for some organized thunderstorms and elements of training
    heavy rainfall could result in rates of 1-2 in/hr, though earlier
    convection near Dallas in southern Collin County was responsible
    for ~1 inch of rain in 15 minutes, so 1-2 inches in less than 1
    hour will certainly be possible tonight. Dry antecedent conditions
    and high flash flood guidance should limit any flash flood
    concerns to urban areas or otherwise sensitive, poorly draining
    locations. 2-4 inches will be possible on a localized basis
    through 10Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7yir3J56soxSS-WTlk0RRuhnRmeEBBntW-T8chuI9ezLR2FYrpUV5D0v_OxihHksyxMk= SwLYT73PzJO9zk3vZN3nmsQ$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 35359778 34899659 34079496 33429390 32739422=20
    32789547 33469733 34739858 35199836=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Mar 26 17:15:53 2025
    AWUS01 KWNH 261715
    FFGMPD
    TXZ000-262315-

    Mesoscale Precipitation Discussion 0085
    NWS Weather Prediction Center College Park MD
    115 PM EDT Wed Mar 26 2025

    Areas affected...South-Central and Deep South TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 261715Z - 262315Z

    SUMMARY...Developing and expanding clusters of heavy showers and
    thunderstorms are expected through this afternoon. Very heavy
    rainfall rates and locally slow cell-motions will support an
    increasing flash flood threat.

    DISCUSSION...The midday GOES-E satellite imagery shows a
    well-defined mid-level shortwave trough ejecting east across
    northwest mainland Mexico which will begin to cross the Rio Grande
    Valley by later today. Increasingly divergent flow aloft ahead of
    these height falls along with some smaller scale vort energy will
    be gradually overspreading the lower Rio Grande Valley and
    adjacent areas of south-central TX and will be interacting with an
    increasingly moist and unstable airmass.

    MLCAPE values over much of the region are already locally on the
    order of 1500 to 2000 J/kg, with PWs of 1.5 to 1.75 inches.
    Persistent low-level south-southeast flow will continue to bring
    moisture up across much of southern TX in general going through
    the afternoon hours, and the latest CIRA-ALPW and MIMIC-TPW data
    sets show notable concentrations of deeper and more anomalous
    moisture advecting into the lower Rio Grande Valley ahead of the
    upstream mid-level height falls/shortwave energy.

    This will set the stage for developing and expanding clusters of
    heavy showers and thunderstorms going through the afternoon hours.
    The convective cells in this moistening environment should become
    increasingly efficient and will be capable of producing very high
    rainfall rates considering the level of instability and some
    uptick in updraft helicity parameters.

    The 12Z HREF guidance suggests the stronger and more organized
    convective cells may be capable of producing 2 to 3 inch/hour
    rainfall rates. A combination of multicell and some isolated
    supercell structures are generally expected to evolve over time,
    and some of the cells that become more deeply rooted are expected
    to potentially become very slow-moving with cell-motions a bit to
    the right of the deeper layer mean flow. This will support some
    locally enhanced rainfall totals, with some rainfall totals by
    early this evening of 3 to 5+ inches possible.

    Antecedent conditions are very dry, but with such high rainfall
    rates and potential for slow cell-motions, the threat for flash
    flooding will be increasing with time. Additional MPDs will likely
    be required this evening to further address the excessive rainfall
    threat going into the overnight hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4aPFlnQ_WWQm9hc6kTt-06RSX7IdGQfndG2Vwt8UA4aR2YV7FEW9O1vcMKua9pksn0_Q= EPjdyCFI2HiIQV1Rz1KgAYQ$ for graphic product...

    ATTN...WFO...BRO...CRP...EWX...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 29289749 28919687 28229668 27529713 27149726=20
    26709731 26009720 25929757 26109820 26369895=20
    26729931 27479964 27839989 28240022 28800007=20
    29279882=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Mar 26 23:19:59 2025
    AWUS01 KWNH 262319
    FFGMPD
    TXZ000-270518-

    Mesoscale Precipitation Discussion 0086
    NWS Weather Prediction Center College Park MD
    719 PM EDT Wed Mar 26 2025

    Areas affected...portions of south Texas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 262318Z - 270518Z

    Summary...Areas of heavy rainfall continue to move slowly across
    the discussion area, with redevelopment of deep/intense convection
    noted along/just west of the Rio Grande recently. Flash flood
    potential (locally significant) should continue through 05Z/11p
    CDT and likely beyond.

    Discussion...Over the past 6 hours, scattered to numerous
    thunderstorm activity has produced areas of 1-5 inch rainfall
    amounts - highest northwest of Corpus Christi and northwest of
    McAllen. Prior dry conditions and high FFGs suggested that these
    rainfall totals have likely resulted only minimal impacts so far,
    though wetting soils should gradually result in the region
    becoming more susceptible to flash flooding as additional rainfall
    develops across the region tonight.

    Meanwhile, radar/satellite mosaic imagery indicates
    redeveloping/strengthening convection along and either side of the
    Rio Grande Valley, with additional strengthening storms located
    just north of Corpus Christi. Wind fields aloft have strengthened
    across the discussion area in tandem with better ascent/lift,
    which is the likely culprit for the recent increase in convective
    coverage. Increased wind shear has enabled a few of the
    convective structures toexhibit right/deviant motion with speeds
    as slow as 5-10 knots and rain rates exceeding 2 inches/hr.

    Over time, concern exists that convection near the Rio Grande
    could grow upscale into one or more convective complexes. These
    complexes will move very slowly while continuing to exhibit
    embedded rotation and occasional cell mergers that should enhance
    rain rates. Localized areas of 3-5 inch rainfall totals are
    expected, and significant flash flooding could become a great
    concern if higher rain rates were to materialize in
    sensitive/urbanized portions of the discussion area.

    A secondary concern for upscale growth/backbuilding exists
    near/just north of Corpus Christi where low-level confluence
    exists on the northern extent of 20-25 kt 850mb flow. A few of
    these areas have already experienced 2-5 inch rainfall totals
    today. Additional rainfall could result in flash flooding
    especially if a more persistent convective band could become
    established.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6rl1j1YZhZDJqe53V_RjJH2MXwSfghCpBfsOtGddV2TNxyeRFOEiI-lCNUsmSupXuQq2= kaxU-Zb1wQ7Hr3gbZt1RxVU$ for graphic product...

    ATTN...WFO...BRO...CRP...EWX...HGX...SJT...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 30599832 30329724 29809654 29259617 28569631=20
    27869674 27099719 26499730 26349770 26379853=20
    26649920 27329952 28049993 28730053 29050080=20
    29620131 30180112 30559991=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Mar 27 05:12:02 2025
    AWUS01 KWNH 270511
    FFGMPD
    TXZ000-271100-

    Mesoscale Precipitation Discussion 0087
    NWS Weather Prediction Center College Park MD
    111 AM EDT Thu Mar 27 2025

    Areas affected...Deep South Texas...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 270515Z - 271100Z

    SUMMARY...Highly uncertain convective environment with ample
    moisture, persistence of moderate to heavy rainfall may result in
    possible localized flash flooding potential through early morning.

    DISCUSSION...A very complex dynamic environment remains across
    much of southern Texas this evening. An elongated mid-level
    trough axis exists generally along 30N with multiple weaker
    vorticity rolls ebbing and shearing with influence of changing
    lower-level moisture/instability field feeding back through
    convective feed-back and latent heat release. WV suite denotes
    favorable right entrance ascent pattern with anticyclonic curved
    transverse banding features moving downstream into E TX/N LA;
    while left exit favorable divergence ascent pattern is expected to
    replace and further support indirect thermal circulation and back
    low level flow from southeast to easterly to strengthen isentropic
    ascent, perhaps triggering additional development as noted west of
    Zapata county along the western moisture gradient at 700-500mb and
    traced well in the CIRA LPW layers. It can be also noted the new
    convection is ascending along the veered sfc to 850mb and then
    further 850mb to 700mb from southeast to south-southwest,
    respectively. Additionally, RADAR and SWIR loop suggest a weak
    MCV from older convection just west of NW Webb county, moving east
    may be affording additional strengthening of the southerly turning
    of the winds.

    Overall, the more southerly flow intersects with the dying
    outflow/convective line across south Texas, that has laid out
    fairly orthogonal to the strengthening low level flow. Cell
    motions will be more northward, though this boundary and the
    effective bulk shear in the 35-40kt range is suggestive of greater
    cell organization for enhancing low level moisture flux into the broadening/rotating updrafts. Rapid refresh models like the
    RAP/HRRR have started a trend toward this convective mode, which
    in turn, trends to increased longevity. Overall deep layer
    moisture remains solid with .75-1", sfc to 850mb LPW values along
    the Lower Rio Grande, over-topped with .4-.6" in 850-700mb, though
    hints of some dry air mixing along that western gradient of dry
    air pressing eastward may result in some entrainment, but should
    also aid in steepening lapse rates for increasing some instability
    for deeper/stronger updrafts, though proximity to modest 700-500mb
    moisture allows for the total column to remain near or slightly
    above 1.75"; higher to the southeast nearer the Gulf source.=20=20
    However, there has been some mixing/overturning from the initial
    convection to leave the instability field more scattered and
    pocketed in nature; likely resulting in some uncertainty on the
    persistent vigor of the updrafts. However, there are remains of
    1500-2000 J/kg of CAPE mainly south of the River, that should
    allow for cells capable of rates over 2"/hr for an hour or so and
    scattered within the area of concern.

    Cell motions will increase potential for flanking line
    development/repeating with a more eastward component for the
    stronger/rotating cells and more north-northeastward for weaker
    ones. As a result the environment for intersection/repeating is
    going into the storm-scale interactions which are notoriously
    difficult to assess/forecast and so confidence is not very high in
    incidents of flash flooding; especially given the area of best
    overlap/signal of heavy rainfall is generally north and across the
    rural and naturally higher FFG values of Zapata,Jim Hogg, Brooks,
    and Kenedy counties. However, proximity of the boundary further
    south may be poorly resolved in the guidance nearer the urban
    areas north of the river, and the earlier rainfall in Starr and S
    Jim Hogg counties may receive an additional 2-4" locally inducing
    flash flooding. All considered, the risk of flash flooding
    remains possible through the early morning hours across Deep south
    Texas.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4rC0G-FOvh2aQdHX2I-yG6TMcHBTxX2b_Mg8p-FVIsNYVWrN_Jl-BdQzArh3JGCZL1dJ= ROIhuOotL9O3bzRCctJeKlM$ for graphic product...

    ATTN...WFO...BRO...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 27149894 27059845 26849767 26809716 26069705=20
    25809737 25999773 25989800 26169857 26389909=20
    26749934 27089943=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Mar 27 14:22:10 2025
    AWUS01 KWNH 271422
    FFGMPD
    TXZ000-271900-

    Mesoscale Precipitation Discussion 0088
    NWS Weather Prediction Center College Park MD
    1020 AM EDT Thu Mar 27 2025

    Areas affected...Lower Rio Grande Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 271420Z - 271900Z

    SUMMARY...Some expansion of heavy showers and thunderstorms are
    expected through this morning and into the early afternoon hours.
    Heavy rainfall rates and locally slow cell-motions will foster a
    threat for additional flash flooding concerns.

    DISCUSSION...A mid-level trough continues to gradually advance
    east across the southern High Plains and adjacent areas of
    northern mainland Mexico with multiple embedded vort centers seen
    in GOES-E IR/WV satellite imagery ejecting out of the base of it
    toward the lower Rio Grande Valley.

    Radar imagery shows one band of convection that has slowly
    progressed through Deep South Texas over the last few hours, with
    the core of this activity now situated over far northeast Mexico.
    However, there is redevelopment seen farther northwest to the
    southeast of Laredo involving Zapata, Jim Hogg, and Starr
    Counties. This convection is generally forming along a weak
    instability gradient that is also aligned along an inverted
    surface trough which is gradually attaining sufficient
    baroclinicity to be classified as a weak stationary front.

    Despite rather modest instability parameters with MLCAPE values of
    500 to 1000 J/kg, there will likely be some gradual recovering of
    instability with time across Deep South Texas to the southeast of
    this weak frontal zone which will strengthen the overall
    instability gradient. This coupled with ejecting vort energy and
    the left-exit region of an upper-level jet streak from northern
    Mexico across the lower Rio Grande Valley will likely tend to
    support and sustain the redeveloping areas of convective activity
    with some gradual expansion off to the northeast expected with
    time.

    PWs are generally in the 1.5 to 1.7 inch range across the area,
    and this coupled with the instability should be capable of
    favoring convection with 1 to 2 inch/hour rainfall rates going
    through the morning and early afternoon hours. The latest hires
    CAM guidance is handling the ongoing activity very poorly, so
    confidence is generally quite low, but given the latest convective
    trends, some additional rainfall totals going through early
    afternoon may reach 2 to 4 inches with isolated heavier amounts
    not out of the question given slow cell-motions.

    Given some of the heavier rainfall from overnight and early this
    morning, and thus the moistening up of the soil conditions, these
    additional rains over the next several hours may result in some
    additional flash flooding concerns.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7yGQbC0BOQX8nuGEbtr0eD5gL0LsuaytCRvB9lG0U3-n6-eCMJWmsg8izXHpTmssRSNH= oPC9bApWRWf4IRsWdzlWu0U$ for graphic product...

    ATTN...WFO...BRO...CRP...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 27619834 26959776 26359713 25829719 25959804=20
    26459909 27159953 27609918=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Mar 27 18:58:42 2025
    AWUS01 KWNH 271858
    FFGMPD
    TXZ000-280057-

    Mesoscale Precipitation Discussion 0089
    NWS Weather Prediction Center College Park MD
    257 PM EDT Thu Mar 27 2025

    Areas affected...Deep South TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 271857Z - 280057Z

    SUMMARY...A strong and well-organized QLCS gradually settling down
    through Deep South TX will be capable of producing very heavy
    rainfall rates and a general likelihood for flash flooding heading
    into the early evening hours.

    DISCUSSION...GOES-E IR satellite imagery in conjunction with
    dual-pol radar shows a well-defined QLCS gradually settling
    eastward down across Deep South TX. This convective complex is
    being strongly favored by the ejection of left-exit region
    upper-level jet dynamics across the lower Rio Grande Valley
    downstream of a deeper layer trough crossing northern Mexico and
    parts of the southern High Plains.

    This energy is also interacting with a quasi-stationary frontal
    zone and the pooling of a modestly unstable airmass characterized
    by MLCAPE values of near 1000 J/kg. While instability is rather
    modest, there is a rather favorable shear environment for a
    continuation of organized convection over Deep South TX with
    stronger mid-level winds helping to support as much as 40+ kts of
    effective bulk shear. Some additional uptick in diurnal heating
    over the next few hours should support some additional boundary
    layer destabilization and this coupled with a convergent and moist
    low-level south-southeasterly jet of 30 to 40 kts should support
    convection with high rainfall rates capable of reaching 2 to 3
    inches/hour with the stronger storms. In fact, the latest
    CIRA-ALPW data shows a notable surge/wave of higher PWs/moisture
    concentrated in the SFC/850 mb layer lifting northwest out of the
    Bay of Campeche and taking aim on Deep South TX. Speed convergence
    associated with this in conjunction with the implied stronger
    moisture transport will further enhance the rainfall rate
    potential over the next few hours.

    The 12Z HREF guidance along with numerous runs of the HRRR
    continue to struggle with the details and evolution of the ongoing
    convective activity more regionally over southern TX. Accounting
    for the current activity, the HRRR is closest from a convective
    mode/object perspective, but is way too slow with its evolution.
    Basically the HRRR 00Z to 06Z/Fri QPF signal is likely to occur
    more over the next 6-hours based on the latest satellite and radar
    trends.

    High rainfall rates and rather slow cell-motions with the QLCS
    evolution should favor additional rainfall amounts of as much as 3
    to 5 inches, and especially where any transient areas of
    cell-training can occur. Given the wet antecedent conditions from
    earlier heavy rainfall, these additional rains are likely to cause
    additional areas of flash flooding heading into the early evening
    hours, and this will include the Brownsville vicinity.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9lJw7qhr-YditUF01Jsskdf0F1HyOx-VligRuIWX7GghXyGUKavp5zBbEsD-Qg8grHcs= y4kj0RwOjuo95XTSHkADn00$ for graphic product...

    ATTN...WFO...BRO...CRP...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 27509751 27429722 26879728 25919702 25739713=20
    25959801 26199884 26569899 27159840=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Mar 28 00:39:58 2025
    AWUS01 KWNH 280038
    FFGMPD
    TXZ000-280636-

    Mesoscale Precipitation Discussion 0090
    NWS Weather Prediction Center College Park MD
    837 PM EDT Thu Mar 27 2025

    Areas affected...south Texas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 280036Z - 280636Z

    Summary...Locally significant flash flood potential should
    continue through 06Z/1am CDT.

    Discussion...A very slow-moving cluster of deep, intense
    convection continues to make progress across Deep South Texas
    while producing multiple hours of 1-3 inch/hr rain rates. These
    rates have falling in populated areas near McAllen and Harlingen,
    prompting significant impacts.=20

    Radar mosaic imagery indicates the leading edge of a cold pool
    extending from just north of Brownsville west-southwestward along
    and just south of the Rio Grande River. Meanwhile, mesoanalyses
    and satellite imagery indicate renewed convective development
    across portions of northeastern Mexico associated with a mid-level
    shortwave trough centered near 27.3N, 101.4W. Steep lapse rates
    aloft were located just west of the ongoing complex and much of
    northern Mexico as well.

    While the heavy to extreme rain rates currently being observed
    just north of Brownsville may shift offshore over the next couple
    hours, the combination of a trailing/lingering outflow boundary
    near the Rio Grande and upstream ascent/instability from
    aforementioned lapse rates should result in a continued threat of
    at least elevated convection over the next 3-6 hours. The
    heaviest rainfall threat will be modulated by the southward shift
    of the outflow boundary - should this boundary drift back to the
    north into south Texas, a renewed threat for 2+ inch/hr rain rates
    could materialize and raise continued, significant flash flood
    potential. At least areas of 1-2 inch/hr rain rates are expected
    with deep convection given the upstream instability and lift -
    even with elevated convective activity. Ground conditions are
    inundated with significant impacts being reported amid near-zero
    FFGs from Harlingen westward to Rio Grande City. Additional
    rainfall will likely exacerbate those impacts.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5p028T9sL6KQXZnanMNZMTqQdWg8mAvmVIXWa_cm3sm3lHjz3ELz06uE-otCSh8jSDmD= 0U54iXplbl5S9GWvSUC6cGI$ for graphic product...

    ATTN...WFO...BRO...CRP...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 27539856 27469744 26169691 25879768 26469918=20
    27129935=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Mar 28 04:58:59 2025
    AWUS01 KWNH 280457
    FFGMPD
    TXZ000-281000-

    Mesoscale Precipitation Discussion 0091
    NWS Weather Prediction Center College Park MD
    1256 AM EDT Fri Mar 28 2025

    Areas affected...Lower Rio Grande Valley and Lower Texas Gulf
    Coast...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 280500Z - 281000Z

    SUMMARY...Strong MCV, providing ascent for another round of strong thunderstorms capable of 2"+/hr rates to further compound ongoing
    significant flash flooding across the Rio Grande Valley. Heavy
    rainfall likely to expand northward toward Corpus Christi urban
    areas over the next few hours as well, with possible flash flooding

    DISCUSSION...GOES-E WV shows strong vorticity center/MCV currently
    along the south-southwest side of the larger scale stationary
    upper-level low crossing over the Rio Grande into Webb county.=20
    These height-falls have once again backed the low level flow off
    the very moist/unstable western Gulf that had filtered across
    Tamaulipas and into eastern Nuevo Leon state in Mexico. CIRA LPW
    shows surface to boundary layer moisture nearing 1" fluxed on
    30-35kts toward the flanking line, allowing for increased
    instability of 1000-1500 J/kg (narrow and skinny profiles) while
    this is leading to confluence through the ascent layer in the
    850-500mb layer. CIRA LPW suggests an additional third to half
    inch and quarter to third of an inch in those mid-levels to
    support overall depth of 1.75 to near 2" along the Gulf coast. So
    once again, strong moisture flux convergence aided by unstable air
    has developed into a squall line with cells likely to increase
    from 1.25 to 1.5-2"/hr as the line reaches deeper moisture further
    east. Additionally, the southerly moist flow is expanding
    scattered isentropically forced cells between the exiting
    convective cluster and the approaching line. These more scattered
    cells will be a tad shallower, but with solid flux should be still
    prolific in rainfall capability even if more scattered/random in nature...adding .5-1" prior to the main line. This WAA appears to
    be trending northward toward relatively drier locations and may
    start to stall/flatten to southwest steering as it nears the coast
    across N Kenedy, Kleberg and Nueces county. Spots of 2-3" are
    possible across this northern area that may initiate some
    localized flash flooding concerns, especially near the Corpus
    Christi urban areas that are particularly prone to intense rates.

    Additionally, upper level jet diffluence remains extreme across
    far southeast TX and the lower Rio Grande Valley with 60-70kt
    speed max jet lifting northward across south Texas, while the core
    of the sub-tropical jet streak is fairly flat (west to east)
    across northeast Mexico into the Gulf. This is over 90 degrees of
    diffluence maintaining solid evacuation of convection as it moves
    eastward to areas already flooded. This should also allow for
    slowing of forward propagation as well as with strengthening of
    the low level inflow for flanking line back-building across the
    Lower Rio Grande Valley. Additional 3-5" totals across already
    flooded areas; likely to maintain flash flooding conditions with
    some significant flash flooding/emergency conditions to be
    possible with this next round. Localized totals over 10" are
    likely to become reality across a broader area of lower Rio Grande Valley.=20=20

    While it is hopeful that after this MCV/forcing wave moves
    through, the environment will clear out; however, there remains
    quite a bit of uncertainty, as south-southeasterly flow of the
    western Gulf is likely to be maintained through the peak of the
    diurnal surge after prior to day break (08-10z). Intersection
    with lingering outflow boundaries may still trigger additional
    development, but will update the MPD later this morning to address
    this concern.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-N-vDMrM6XC5gGT-Vh-2RmbLUIA-IWY7v3ZuEyPzRzoDnmQUMCzTFhqN2TzdpDopnGwJ= SVcWJD7TLFVF_FGg6OeyNKk$ for graphic product...

    ATTN...WFO...BRO...CRP...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 28039762 27789713 27029738 26529721 25969710=20
    25799726 25919782 26109845 26259881 26489914=20
    26749915 27249867 27579831=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Mar 28 09:12:29 2025
    AWUS01 KWNH 280912
    FFGMPD
    TXZ000-281400-

    Mesoscale Precipitation Discussion 0092
    NWS Weather Prediction Center College Park MD
    511 AM EDT Fri Mar 28 2025

    Areas affected...Lower Rio Grande Valley of Texas...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 280915Z - 281400Z

    SUMMARY...A few more hours of showers/thunderstorms repeating
    across already flooded locations. Additional 1-3" totals
    possible, continuing flooding conditions through day break.

    DISCUSSION...GOES-E WV suite depicts core of MCV/vorticity center
    lifting north-northeast across South Texas with a trailing
    shortwave rounding out the bottom of the filling mid to upper
    level trough that has been persistent across central TX over the
    past few days. In the process the progressive squall line has
    moved into the northwest Gulf, but with some weak DPVA upstream,
    low-level winds have returned to south/southeast from the surface
    to boundary layer off the western Gulf. GOES-E 3.9um SWIR loop
    showed low level stratus at the leading edge of the return
    moisture, modest instability field lifted north but along
    weakening winds into the 15-25kts range from 925mb VWP in the
    area. Veered flow across 850-700mb with weak WAA allowed for some
    convection to refocus and build across Hildalgo to W Cameron
    county. Weaker flux of still ample deep layer moisture of 1.75-1.9
    Total PWat and 1000 J/kg, support rates up to 1.5"/hr but given
    the veered steering flow aloft will once again allow for cells to
    train ENE across significantly flooded areas with an additional
    1-3" totals expected, likely to maintain ongoing flooding
    conditions.

    Hi-Res CAMs continue to struggle with the placement and timing of
    the evolution of the convection. However, early HRRR runs showed
    a similar evolution through the Lower Rio Grande Valley but had
    been about 2 to 2.5 hours too slow with the timing of the squall
    line and the ongoing redevelopment. Still, the evolution seems to
    be the best handle on the situation, as such there most recent run
    has backed off a tad, suggesting the convergence and ascent
    pattern may be weakening with greater surface to boundary layer
    winds turning eastward across the Northwest Gulf over the next 3-5
    hours finally giving the area of concern a break from these
    repeated rounds. Given the run to run variability and poor
    performance from other CAMs, not fully confident that additional
    convection may maintain at the trailing edge of the low level
    confluence of the larger cyclonic circulation as it lifts
    northeast across Northeast Texas later this morning as hinted by
    the recent RAP runs.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9r039ww4ec7ioPgjc0BaxaDY5z-eJ8qZZfvOl-7Ncf1gzzlQ41znwbiDnB1-tJWM694W= ENbXJdwOluvoDuKnE-LEeFI$ for graphic product...

    ATTN...WFO...BRO...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 26969773 26889732 26519720 25989709 25799730=20
    25969771 25979800 26129846 26339890 26659872=20
    26909818=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Mar 28 18:12:48 2025
    AWUS01 KWNH 281812
    FFGMPD
    LAZ000-ARZ000-TXZ000-290010-

    Mesoscale Precipitation Discussion 0093
    NWS Weather Prediction Center College Park MD
    211 PM EDT Fri Mar 28 2025

    Areas affected...Eastern TX...Far Western LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 281810Z - 290010Z

    SUMMARY...A localized threat for some flash flooding will exist
    going through the early evening hours from heavy showers and
    thunderstorms that may train over the same location.

    DISCUSSION...The early afternoon GOES-E visible satellite imagery
    shows an increasingly expansive CU/TCU field over eastern TX as
    vigorous mid-level shortwave/vort energy lifting northeastward
    interacts with a surface trough and the pooling of modest boundary
    layer instability. MLCAPE values are on the order of 500 to 1000
    J/kg with a seasonably moist environment characterized by PWs of
    1.5 to 1.75 inches.

    Radar does show a band of showers and thunderstorms organizing in
    a general south to north fashion over far eastern TX, and as
    additional diurnal heating/solar insolation contributions to
    further boundary layer destabilization this afternoon, there
    should be some additional expansion of convection which should
    tend to become locally well-organized given the presence of 30 to
    40+ kts of effective bulk shear. This will include a convective
    threat to the middle and upper TX coast and the greater
    Houston/Galveston metropolitan area.

    The 12Z HREF guidance shows 50 to 70 percent probabilities of 1 to
    2 inch/hour rainfall rates with the storms this afternoon, and
    some localized exceedance of 2 inch/hour rates will be possible
    especially for areas of far eastern TX just west of the LA border
    where the axis of stronger instability and relatively stronger
    surface moisture convergence is expected to be focused.

    Given concerns for some localized cell-training, some storm total
    amounts by 00Z (7PM CDT) may reach as high as 3 to 5 inches. FFG
    values across the region are rather high, but the HREF guidance
    does suggest some low end probabilities of exceedance which
    suggests a localized concern for flash flooding with an emphasis
    generally on the more urbanized locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4DhSf5ZuFUL6CbDwtUmz1GNmJBEXHXQ-9JjNoS51qiaJZGo1hr3MPnBVPVysW1AFUPks= qgc95sChMxDL4DpcXmOg54I$ for graphic product...

    ATTN...WFO...CRP...HGX...LCH...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 33089412 32769304 31189288 29729373 28859497=20
    28499554 28399633 28699661 29309630 30539529=20
    32419473=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 29 20:07:25 2025
    AWUS01 KWNH 292006
    FFGMPD
    MSZ000-LAZ000-300005-

    Mesoscale Precipitation Discussion 0094
    NWS Weather Prediction Center College Park MD
    405 PM EDT Sat Mar 29 2025

    Areas affected...Southeast LA...Far Southwest MS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 292005Z - 300005Z

    Summary...Showers and thunderstorms are expanding and intensifying
    over south-central LA. While a fair amount of uncertainty remains,
    training cells with maximum hourly rainfall rates of 2-3"/hour
    will support an increasing flash flood threat (possibly
    significant) this afternoon.

    Discussion...Radar and Day Cloud Phase imagery this afternoon
    continues to depict expanding thunderstorm thunderstorm coverage
    along the Central Gulf Coast. As this activity matures, radar
    estimates hourly rainfall rates of 1.8-2.8"/hour are occurring
    within the most intense cores.

    This uptick in coverage and intensity is likely in response to 1)
    increasing insolation across the region, 2) the approach of an
    offshore MCV, and 3) a broad north-south oriented 850 hPa
    convergence axis. Near the convection, mesoanalysis estimates of
    1500 J/kg MLCAPE (in a saturated and "skinny" profile), PWAT of
    1.6-1.7", and 20 kts of effective bulk shear suggest cells should
    maintain enough organization to realize the moist and unstable
    environment. Over the next several hours, expect areas downstream
    to fill in where cumulus is showing increasing increasing
    development, and train as the slow moving forcing aligns with the
    mean flow.

    With all of this said, there remains a fair amount of uncertainty
    amongst the CAM suite with how the convection evolves through
    tonight. However, through 0z, the 12z HREF suite depits increasing probabilities of 6 hour QPF exceeding the 10 to 100 year ARI,
    generally focused over Southeast LA (45% and 35%, respectively).
    This suggests an increasing threat of flash flooding over the next
    several hours, some of which could be significant -- particularly
    over vulnerable urban areas.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4iMuny3Z9uhyr0FEWrVQznNFwuihUBrpiMIrTar7riSpSiYdcX7nLFxYV2E5SXbPNclD= 7SBwEKFtnwAKwmP6IJ8k8CY$ for graphic product...

    ATTN...WFO...LCH...LIX...MOB...

    ATTN...RFC...LMRFC...NWC...

    LAT...LON 31069021 30728892 29788903 29539047 29699186=20
    30059252 30619249 30989160=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 29 20:16:11 2025
    AWUS01 KWNH 292014
    FFGMPD
    MSZ000-LAZ000-300005-

    Mesoscale Precipitation Discussion 0094...Corrected
    NWS Weather Prediction Center College Park MD
    414 PM EDT Sat Mar 29 2025

    Corrected for Typos in discussion

    Areas affected...Southeast LA...Far Southwest MS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 292005Z - 300005Z

    Summary...Showers and thunderstorms are expanding and intensifying
    over south-central LA. While a fair amount of uncertainty remains,
    training cells with maximum hourly rainfall rates of 2-3"/hour
    will support an increasing flash flood threat (possibly
    significant) this afternoon.

    Discussion...Radar and Day Cloud Phase imagery this afternoon
    continues to depict expanding thunderstorm coverage along the
    Central Gulf Coast. As this activity matures, radar estimates
    hourly rainfall rates of 1.8-2.8"/hour are occurring within the
    most intense cores.

    This uptick in coverage and intensity is likely in response to 1)
    increasing insolation across the region, 2) the approach of an
    offshore MCV, and 3) a broad north-south oriented 850 hPa
    convergence axis. Near the convection, mesoanalysis estimates of
    1500 J/kg MLCAPE (in a saturated and "skinny" profile), PWAT of
    1.6-1.7", and 20 kts of effective bulk shear suggest cells should
    maintain enough organization to realize the moist and unstable
    environment. Over the next several hours, expect areas downstream
    to fill in where cumulus is showing increasing development, and
    train as the slow moving forcing aligns with the mean flow.

    With all of this said, there remains a fair amount of uncertainty
    amongst the CAM suite with how the convection evolves through
    tonight. However, through 0z, the 12z HREF suite depits increasing probabilities of 6 hour QPF exceeding the 10 to 100 year ARI,
    generally focused over Southeast LA (45% and 35%, respectively).
    This suggests an increasing threat of flash flooding over the next
    several hours, some of which could be significant -- particularly
    over vulnerable urban areas.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6kN1J_PuhyzdL6t3BxiCJM0tmiDO1r9tfCNO_aN_IzySBPlID5OHsmsUxQ0XmNE1CnqV= Lrwknf5DeFuAk1hvcUyzpWc$ for graphic product...

    ATTN...WFO...LCH...LIX...MOB...

    ATTN...RFC...LMRFC...NWC...

    LAT...LON 31069021 30728892 29788903 29539047 29699186=20
    30059252 30619249 30989160=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 30 15:40:41 2025
    AWUS01 KWNH 301540
    FFGMPD
    FLZ000-ALZ000-MSZ000-301938-

    Mesoscale Precipitation Discussion 0095
    NWS Weather Prediction Center College Park MD
    1138 AM EDT Sun Mar 30 2025

    Areas affected...Far Southern MS...Southwest AL...Far Western FL
    Panhandle

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 301538Z - 301938Z

    SUMMARY...Relatively slow-moving and occasionally backbuilding
    areas of very heavy showers and thunderstorms will pose a
    localized threat of flash flooding going through the early to
    mid-afternoon hours.

    DISCUSSION...GOES-E IR satellite imagery shows a cluster of
    cooling convective cloud tops associated with heavy showers and
    thunderstorms across portions of far southern MS and stretching
    eastward into southwest LA and the western parts of the FL
    Panhandle. The convection which has become rather organized over
    the last hour is mainly associated with a low-level convergence
    axis with proximity of a well-defined instability gradient.

    MLCAPE values of 1000 to 1500 J/kg and PWs of 1.5 to 1.7 inches
    are in place across the area which are contributing to rainfall
    rates reaching upwards of 2 inches/hour with the stronger cells.

    Some localized backbuilding of these cells are noted and
    especially over parts of Harrison and Jackson Counties in southern
    MS. However, stronger convective cells are also slowly evolving
    into areas of southwest AL as well. Given the cooling cloud top
    trends, there should tend to be some persistence of these cells
    over the few hours, and there will be concerns for additional
    backbuilding and/or training of cells in the near-term given the
    deeper layer mean flow.

    The 12Z HREF guidance including some of the recent HRRR guidance
    suggests as much as an additional 3 to 4 inches of rain with
    locally higher amounts. Given ongoing convective trends and
    additional rainfall potential in the near-term, additional
    localized areas of flash flooding will be possible and this will
    include a threat for some urban impacts rather close to the
    Mobile, AL area, and especially areas north and west of here over
    the next couple of hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!88WA6OD9oqEFl1w1avYnNz_7N_xsPoUgO-Fdd_HC8nxbBqTxm8EGFiRkDXjP5bVA3q__= ujsuVkTAPp13KcgO-M0TohU$ for graphic product...

    ATTN...WFO...LIX...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 31378778 31258683 30788654 30458694 30358760=20
    30368842 30698898 31138872=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Mar 30 18:24:51 2025
    AWUS01 KWNH 301824
    FFGMPD
    FLZ000-ALZ000-MSZ000-302323-

    Mesoscale Precipitation Discussion 0096
    NWS Weather Prediction Center College Park MD
    223 PM EDT Sun Mar 30 2025

    Areas affected...Far Southern MS...Southwest AL...Western FL
    Panhandle

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 301823Z - 302323Z

    SUMMARY...Very heavy rainfall continues to impact areas of far
    southern MS, southwest AL and the western part of the FL
    Panhandle. Extremely heavy rainfall rates persisting over the
    region with locally backbuilding and training cells will yield
    areas of locally significant/considerable flash flooding over the
    next few hours.

    DISCUSSION...GOES-E IR satellite imagery continues to show a
    cluster of strong cold-topped convection with numerous
    overshooting tops over areas of the central Gulf Coast region
    extending from far southern MS eastward across southwest AL and
    into the western FL Panhandle. The convection continues to be
    anchored along a general north/south convergence axis and within a
    well-defined instability gradient.

    MLCAPE values of 1000 to 1500 J/kg and PWs of 1.5 to 1.75 inches
    are in place across the area which coupled with some occasional
    mesocyclone activity has been yielding extreme rainfall rates of 2
    to 4 inches/hour with the stronger cores. Already there are
    Radar-QPE values across parts of Jackson County of 8 to 10 inches
    where significant backbuilding of convection has occurred.

    Very strong overshooting top activity has yielded some cloud top
    temperatures recently to near -70 C and there has been an overall
    expansion of convection over the last few hours to include more
    areas of southwest AL and the western FL Panhandle. The GOES-E
    visible satellite imagery shows some low-level cloud street
    activity upstream over southeast LA and southern MS as a
    destabilizing boundary layer couples with moist southwest flow.
    This low-level feed of moisture and instability should continue to
    support the downstream convective clusters, with a favorable
    backbuilding environment continuing at least in the short term.

    Additional rainfall totals of 3 to 6+ inches are expected given
    the very high rainfall rates and convective mode going through
    early this evening. The recent HRRR guidance has been supporting
    this, and additional areas of flash flooding are likely which will
    include locally significant/considerable urban flash flooding
    impacts. The Mobile metropolitan area will need to continue to
    closely monitor this activity for enhanced rainfall and flash
    flooding concerns over the next few hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!97y4yS4B8xvjC4kmwc2NgFDY5G7NE8uDIj7fw--El0wAP1fbMFFFCL-rqA_0jMqNvWPo= HF7za1J1YohLonWGn85qaTM$ for graphic product...

    ATTN...WFO...LIX...MOB...TAE...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 31338653 31008611 30598623 30358667 30258801=20
    30258931 30748918 31278787=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Mar 31 02:30:21 2025
    AWUS01 KWNH 310230
    FFGMPD
    VAZ000-TNZ000-KYZ000-ALZ000-MSZ000-ARZ000-310800-

    Mesoscale Precipitation Discussion 0097
    NWS Weather Prediction Center College Park MD
    1029 PM EDT Sun Mar 30 2025

    Areas affected...Central & Eastern KY...Western & Middle
    TN...Northern MS...Northwest AL...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 310230Z - 310800Z

    SUMMARY...QLCS starting to have bowing segments that will result
    in a few streaks of enhanced moisture convergence and increased
    heavy rainfall duration resulting in streaks of 2-4" totals and
    possible localized flash flooding.

    DISCUSSION...Regional RADAR mosaic denotes solid and broadening
    squall line across central KY angling back across W TN into far
    northeast AR. Maturing bowing segments are starting to arch out
    with meso-low/inflections noted in the north near Henry county, N
    KY and Christian/Tocd counties in S KY and generally flattening
    near the tail of sufficient deeper layer convergence/mid-level
    forcing from the exiting shortwave across central IND. Modestly
    broad wedge axis of unstable air remains in place along/ahead of
    the line with 500 along the Ohio River back to 2000 J/kg MLCAPE
    across N MS/W TN attm. Moisture is not particularly deep, through
    the layer, but the strength of flux on 40kts of confluent boundary
    layer to 850mb flow has resulted in 1.25-1.5" total PWat values.=20
    Given the strength of the convergence both in speed and direction
    through depth intersecting with outflow boundaries will support
    solid rates of 1.5-2"/hr with bulk falling in initial 15 minutes
    (HRRR and WoFS sub-hourly rates suggesting 1.25/15 minutes with
    .35-.5"/5 minutes rates, respectively).

    While the broad post-squall shield precipitation is increasing,
    especially further north toward better divergence aloft, overall
    totals are likely to be around that 1.5-2" range, which remains
    slightly below even 1hr FFG values across KY (which are higher
    south). However, given these bowing segments and embedded
    inflections are helping to back sfc to boundary layer flow with
    oriented outflow boundaries, orthogonal to the flow, isentropic
    ascent will increase downstream and increase duration in proximity
    of these inflections, allowing for localized 2-3" streaks to form
    along the QLCS, as well as the tail end cells where forward
    steering flow is weaker across W TN/N MS. WoFS 90th percentile
    have some suggestions of totals nearing 4" across N Middle TN,
    which seems plausible. Still 3hr totals of 3" would pose possible
    flash flooding even into the southern portion of the MPD area of
    concern (though 3+ to 4" would make it more probable). As such,
    most locations will not see flooding concerns, but there is enough
    of a signal and trends to suggest a few streaks will result in
    flash flooding through early morning.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_Dlp-AeuNUkFkJlNKzpWnEBpHwKhb9-PpUlIRugJipmdYcfc01QVbsKnw8MzjoE4Bx2x= 0ocA-wSkgzmS-6Kn9JWtxOU$ for graphic product...

    ATTN...WFO...HUN...JKL...LMK...MEG...MRX...OHX...PAH...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 38268398 37908305 37108282 36388380 35388543=20
    34658724 34338937 34609036 35349034 36128917=20
    36708833 37838627 38238537=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Mar 31 03:22:38 2025
    AWUS01 KWNH 310319
    FFGMPD
    MSZ000-LAZ000-TXZ000-310900-

    Mesoscale Precipitation Discussion 0098
    NWS Weather Prediction Center College Park MD
    1118 PM EDT Sun Mar 30 2025

    Areas affected...Eastern Texas...Western Louisiana...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 310320Z - 310900Z

    SUMMARY...A favorable back-building environment/slow cell
    propagation will give way to broader warm advection off the
    western Gulf resulting in expanding convective cluster into the
    middle overnight period. Rates of 2-2.5"/hr and spots of 3-4"
    totals across recently saturated grounds pose possible localized
    flash flooding to continue through early morning.=20

    DISCUSSION...03z Surface analysis depicts a well defined front
    stretching from the Delta region of E AR across toward Texarkana
    before sagging south across central TX. A pool of enhanced low
    level moisture exists through the Sabine River Valley nosing
    toward the frontal zone with Tds in the lower 70s and some return
    moisture off the western Gulf supporting 1.5-1.75" total PWats.=20
    Aloft, GOES-E WV suite denotes a 3H 90kt speed max tracking across
    OK before cyclonically curling northeast across AR/S MO; while the
    sub-tropical jet axis dives south across the Rio Grande and
    southern TX, providing a strong divergence pattern aloft. This
    combination of factors has resulted in a few thunderstorms near a
    weak surface to boundary layer low near TYR. While winds are
    weak, boundary layer inflow is out of the W and SW per upstream
    VWP noting solid inflow and ability of convection to backbuild
    over the last hour or so. This is noted well in the cycling
    overshooting tops in 10.3um EIR as well, limiting forward
    propagation of the heavy rainfall cores. While dry/cooler air
    aloft is supporting hail generation, there is ample moisture flux
    to support 2"/hr rates; and localized spots of 2-4" are already
    starting to be estimated. While not particularly confident due
    to edge of the convective domain, recent WoFS solutions suggest
    back-building cells may even be capable of 4-6" totals per 50th to
    90th percentile totals.=20

    The favorable divergence should be slackening over the next 3-5hrs
    to reduce this potential back-building. However, this will come
    with the diurnal increase in southwesterly flow off the western
    Gulf with increased warm-advection after 06-07z. Combined with
    eastward approach of stronger shortwave/general height-falls,
    convective over-turning is expected further south and east.=20
    Moisture flux convergence into the cells will be prolific with
    Pwats nearing 2.0" and confluent 25-30kt 850mb flow will support
    2-2.5"/hr rates. Slow forward propagation is expected allowing
    for spot totals of 3-4". Overall, the area has been quite
    saturated with 0-40cm percentiles over 85% per NASA SPoRT and
    saturation ratios of 65-80% across the area of concern/convective
    development. As such, spots of flash flooding are likewise
    considered possible through early morning across W and SW LA.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-SSsD5Z2tjugsUFtSK5xsbjr_lzPqsj0NIZfzcvpF53G9M7ZfEaTLZDve8eAHjDms3-R= wcIumUPH1UlCt6Z7NUBvZ14$ for graphic product...

    ATTN...WFO...HGX...JAN...LCH...LIX...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 32589312 32329195 31969154 31139137 30189160=20
    29679216 29799335 29749454 30029489 31019526=20
    31989506 32529448=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Mar 31 07:13:41 2025
    AWUS01 KWNH 310713
    FFGMPD
    MSZ000-LAZ000-ARZ000-311200-

    Mesoscale Precipitation Discussion 0099
    NWS Weather Prediction Center College Park MD
    312 AM EDT Mon Mar 31 2025

    Areas affected...Northeast LA...Southern AR....Northern MS...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 310710Z - 311200Z

    SUMMARY...Favorable training profile for strong thunderstorms
    capable of 2"+/hr rates. Localized totals of 2-4" in 2-3hrs pose
    possible localized flash flooding over the next few hours.

    DISCUSSION...GOES-E 10.3um and regional RADAR mosaic has shown
    consistent strong development that has maintained itself across S
    AR, starting to spread downstream into NW MS, with additional
    upstream overshooting tops breaking through the cirrus canopy over north-central LA. GOES-E WV and AMV suite shows a strong speed
    max starting to round the southeast quadrant of a larger scale
    trof through the Ozarks providing solid divergence aloft. RAP
    forecasts are expected for the jet to further enhance the
    downstream right entrance region across the central MS Valley
    maintaining solid divergence across the lower Delta Region into N
    MS over the next few hours. At the surface, a slowly forming
    surface low along a stalled portion of the main front has locally
    backed surface to boundary layer flow tapping enhanced moisture
    and unstable airmass out of the MS Valley. Tds in the low 70s and
    MLCAPE to 1500 J/kg combined with the convergence downstream of
    the surface low will maintain inflow/flux convergence to further
    expand convective development over the next few hours. Veering
    mid-level flow above the boundary layer is also providing
    850-700mb moisture flux from a pool of enhanced moisture upstream
    to increase rainfall efficiency and likely limit cold pool
    development.

    Deep layer steering is also generally parallel to the boundary to
    support moderately lengthy axis for training over the next few
    hours. As such, a streak of enhanced rainfall with 2-4" totals
    should extend from S AR into northern MS. This aligns with a
    localized minimum in FFG values along the river and northeastward
    where 1/3hr FFG values of 1.5-2" & 2-3" have a solid potential of
    been exceeded in spots along the training axis. In the longer
    term maintenance of the line of convection will be determined on
    upstream development over central LA and points south. If
    clusters develop, inflow/flux of moisture/unstable air is likely
    to be disrupted, but until then there is a good possibility of an
    incident or two of localized flash flooding through early morning.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5VrUXOTKumSFvhfkvikkPBun-IArAQjVjGr3cr4JLzCa_PXtafYErBxlZM1K4-z67cN7= HutoKbkwkHCH6iwdVu9KehI$ for graphic product...

    ATTN...WFO...JAN...LZK...MEG...SHV...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34858901 34268829 33388846 32878936 32679035=20
    32589159 32609252 32819306 33349308 34369101=20
    34729014=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Mar 31 08:27:37 2025
    AWUS01 KWNH 310826
    FFGMPD
    MSZ000-LAZ000-TXZ000-311400-

    Mesoscale Precipitation Discussion 0100
    NWS Weather Prediction Center College Park MD
    425 AM EDT Mon Mar 31 2025

    Areas affected...Southern LA...Far Southeast TX...Southwest MS...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 310830Z - 311400Z

    SUMMARY...Merging clusters with quick 2-3" totals and intersection
    with recently flooded/nearly saturated soils pose localized
    scattered incidents of possible flash flooding/rapid inundation
    through Monday morning.

    DISCUSSION...Regional RADAR mosaic shows a mature cluster to wedge
    of thunderstorms across the northern Piney Woods of E TX into
    north-central LA starting to become increasingly progressive
    toward the southeast given strengthening cold pool from earlier
    storms as well as height-falls/shortwave trough passing across the
    area currently. Additionally, diurnally driven onshore
    flow/strengthening of the western Gulf low-level jet has recently
    lead to broad WAA isentropic ascent from the Sabine River eastward
    into SW LA. Deep layer moisture and confluent low-level flow
    accelerating into the approaching line of convection will result
    in very strong moisture flux convergence and cell mergers over the
    next few hours. Given total PWats of 1.75" and doubling within
    the low-level column should increase efficiency to support rates
    of 2-2.5"/hr with perhaps an isolated 3"/hr rate total.=20
    Southeastward propagation should limit duration, but widely
    scattered spots of 2-3" totals are likely to occur.

    The random scattered may overlap with recently flooded locations
    over the last few days and may reaggravate flooding given limited
    infiltration expected. NASA SPoRT 0-40cm soil saturation are well
    above average (into the 90th percentiles) with ratios above
    70-75%. Additionally, the high rates should traverse a few prone
    cities of Baton Rouge, Lafayette, and eventually New Orleans and Biloxi/Gulfport toward 14-15z posing urban rapid inundation
    flooding possible as well.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9xz7nrpBLMqRrsvQu8ef5bfmpSXxKDiVR4DdcoWegR_lOaNZesiTKZD0Gk5h79RDOxvK= u2Wh1fTxzNuV4S_rVDURKhY$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MOB...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 32229098 32118951 31828886 31338859 30998847=20
    30558853 29908895 29388970 29259051 29279145=20
    29469234 29719310 29919382 30529429 31199452=20
    31629377 32159228=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Mar 31 09:58:20 2025
    AWUS01 KWNH 310956
    FFGMPD
    NCZ000-GAZ000-TNZ000-ALZ000-311500-

    Mesoscale Precipitation Discussion 0101
    NWS Weather Prediction Center College Park MD
    556 AM EDT Mon Mar 31 2025

    Areas affected...Northern AL...Northwest
    GA...South-central/Southeast TN...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 311000Z - 311500Z

    SUMMARY...Multiple rounds of repeating thunderstorms capable of
    2-3" totals may result in isolated incidents of flash flooding
    into early morning hours.

    DISCUSSION...GOES-E WV suite shows convective line across
    Middle-TN is starting to reduce southeastward progression between
    the exiting of the main shortwave across the Great Lakes and the
    approaching wave across the Ozarks. Upstream convective complex
    is starting to feedback with developing outflow jet with
    transverse banding features noted across the Mississippi River
    Valley. VWP suite shows 700-500 steering flow is becoming
    increasingly parallel to the orientation of the old convective
    line across southern TN, while GWX 925-850mb flow shows some
    backed inflow obliquely intersecting the old outflow
    boundary/convective line across NW to north-central AL; with weak
    southerly surface to boundary layer flow proving some flux of
    remaining unstable, moist air across northern AL.=20

    As such, GOES-E 10.3um and Regional RADAR shows an uptick in
    convective vigor along and downstream of the approaching shortwave
    energy in N MS into NW AL. Narrow MLCAPE axis of 1000-1750 J/kg
    remains across the area of concern to feed the development as well
    as maintain approaching stronger cells across N MS. Given the
    aforementioned steering flow supporting parallel flow to the
    boundary, there is an increasing chance of a few hours of
    training/repeating convective cores ahead of the main line and
    approaching cold front. While deep layer moisture is more limited
    than further upstream, solid low level Tds in the mid to upper 60s
    and solid 80-100% RH values through 850-700mb along the axis
    should allow for efficient rainfall production with limited loss
    to evaporation. So with overall Total PWats around 1.5-1.6";
    rates of 1.75"/hr occasionally reaching 2"/hr are possible. With
    one to two hours of repeating with very slow southeastward
    propagation of the line, spots of 2-3" totals are becoming more
    likely.

    Soils are not as dry as locations to the south and east, with
    average soil saturation around 55-60% through 40cm, FFG values
    across the area are near/at the limits of these hourly rates and
    totals. However, given the average nature of the soils, perhaps
    infiltration will be fairly solid to keep flash flooding risk
    limited to typically prone areas and urban locations or isolated
    spots over the FFG. All in all, a spot or two of flash flooding
    is considered possible, if training conditions are ideal
    downstream of MPD 99 in AL/S TN/NW GA.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7GwCPeEscaJZ1Zqv9fhiwj9INUFtuYWHYIRaHLIJDZH2onh38HqSWmsxGEVeG6fcxLCh= evumTvBbd6yd5T5CUqy1eY4$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...MRX...OHX...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 35808471 35668418 35308406 34848426 34478470=20
    34088539 33708637 33238811 33738822 34468812=20
    34938800 35158752 35408644 35658534=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Mar 31 21:56:25 2025
    AWUS01 KWNH 312155
    FFGMPD
    NYZ000-NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-DCZ000-010354-

    Mesoscale Precipitation Discussion 0102
    NWS Weather Prediction Center College Park MD
    555 PM EDT Mon Mar 31 2025

    Areas affected...Northern Mid-Atlantic and Northeast

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 312154Z - 010354Z

    Summary...Repeating of cells containing hourly rainfall rates of
    1.5-2"/hour at times could support a few instances of flash
    flooding this afternoon and evening, mainly over urbanized areas.=20


    Discussion...Radar and Day Cloud Phase imagery show convective
    initiation is well underway over portions of the northern
    Mid-Atlantic and Northeast ahead of a lee-side trough and cold
    front. Recent mesoanalysis estimates suggest modest MLCAPE values
    of 500-1000 J/kg and 35-45 kts of effective bulk shear have
    materialized in the pre-frontal airmass to support increasing
    organization as this activity matures.

    Over the next few hours, expect thunderstorm coverage to continue
    expanding along the lee trough, and beneath increasing
    right-entrance region forcing overspreading the region. While
    individual cell motions will be progressive (40-45 kts), effective
    shear vectors oriented parallel to the lee-trough and front will
    support repeating of individual cells as the activity grows
    upscale. Eventually, this repeating should be interrupted as cold
    pools congeal and the activity begins to accelerate eastward
    tonight. Before then, however, the repeating nature of these cells
    containing rainfall rates upwards of 1.5-2"/hour could lead to a
    few instances of flash flooding. Through 3z, HREF neighborhood
    probabilities depict a high (40-80%) chance of at least 2" of
    rainfall across the highlighted area, with an embedded 25-30%
    chance of at least 3" also noted just north of Philadelphia. While
    the area has been quite dry as of late, the this output suggests a
    few instances of flash flooding could result this afternoon,
    especially given the urban footprint of the region.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8TYDuCfDZBfiekq1vsT_SiVM-YyqKbLPP5cxN4pVFwbXrHsB9SIVAjJwtq8IdauFg6qb= Y9bhklNHxX5D-wvBR6kCJxU$ for graphic product...

    ATTN...WFO...AKQ...ALY...BGM...CTP...LWX...OKX...PHI...

    ATTN...RFC...MARFC...NERFC...NWC...

    LAT...LON 41567440 41497377 40877383 40167452 39477524=20
    38217627 38107744 39157779 40327655 40907560=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 2 01:29:51 2025
    AWUS01 KWNH 020129
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-020725-

    Mesoscale Precipitation Discussion 0103
    NWS Weather Prediction Center College Park MD
    929 PM EDT Tue Apr 01 2025

    Areas affected...northeastern KS into MO River Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 020126Z - 020725Z

    Summary...Training of cells from SW to NE may result in localized
    flash flooding from portions of northeastern KS into the middle MO
    River Valley. Rainfall rates of 1-2 in/hr within areas of training
    will be common and there will be potential for 2-4 inches through
    07Z.

    Discussion...Regional radar imagery has shown an increase over the
    past 1-2 hours in the number of showers/thunderstorms over the
    central Plains, out ahead of a deepening surface low located
    between RSL and K82 at 01Z. An already strong 850 mb low level jet
    of 40-50 kt was observed over central KS/OK with rapid low level
    moisture transport underway into the central Plains, resulting in
    a 500 to 1000 J/kg MUCAPE increase over southeastern NE into
    eastern KS since 22Z (via SPC mesoanalysis). 00Z blended TPW
    imagery showed modest moisture over KS/NE with PW values of 0.7 to
    0.9 inches, but these values are likely to continue increasing
    through the early overnight with the continued advection of
    moisture.

    850 mb winds are forecast to notably strengthen through 06Z over
    OK/KS to over 70 kt locally, yielding increasing MUCAPE along and
    west of the Missouri River, with 1000-2000 J/kg becoming common by
    04-06Z via recent RAP forecasts. Increasing ascent ahead of an
    approaching shortwave trough near the Four Corners region will be
    accompanied by strengthening diffluence and divergence aloft as a
    powerful jet stream rounds the base of the trough and ejects out
    into the central Plains through 06Z. Convection is expected to
    rapidly expand in intensity over central to northeastern KS over
    the next 1-2 hours.

    In addition, strengthening low level convergence at the nose of
    the low level jet is expected to set up over northeastern KS from
    SW to NE (consistent RAP signal in 925-850 mb layer), oriented
    nearly parallel to the expected mean steering flow of individual
    cells, supporting the potential for training. Rainfall rates of
    1-2 in/hr will be likely within areas of training and localized
    2-4 inch totals through 07Z may support isolated flash flooding.

    The HRRR has been persistent in forecasting locations from near
    Salina to the MO/NE border for heavy rain. The 00Z WoFS guidance
    also indicates these same locations with 40-60 percent
    probabilities of exceeding 2" through 06Z. However, dry antecedent
    conditions will likely limit flash flood coverage to urban
    locations or otherwise locally sensitive terrain.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6yeemBWHM5RMysyHocDa7wgVNVZZRAbQuibsN60gBN61HPIV9Z265xr_1W8F3f1Ii2Q2= jyPFzFboCccPHPuJkOB0sic$ for graphic product...

    ATTN...WFO...DMX...EAX...GID...ICT...OAX...TOP...

    ATTN...RFC...ABRFC...MBRFC...NWC...

    LAT...LON 41129452 40769397 40249387 39349503 38509745=20
    38689834 39349822 40279690 40939563=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 2 06:29:56 2025
    AWUS01 KWNH 020629
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-021200-

    Mesoscale Precipitation Discussion 0104
    NWS Weather Prediction Center College Park MD
    229 AM EDT Wed Apr 02 2025

    Areas affected...Northeast KS...Northwest MO...Far Southeast
    NEB...Far Southwest IA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 020630Z - 021200Z

    SUMMARY...A few more hours of training thunderstorms capable of
    1.5-1.75"/hr rates and localized totals of 3"+ continuing flash
    flooding risk. However, veering flow will result in increasing
    forward cell motions limiting overall totals and flooding risk
    eastward into N MO.

    DISCUSSION...Surface and RAP analysis fields show maturing surface
    to 850mb low across south-central NEB continuing to pivot slowly
    with expanding warm sector across eastern KS, spreading into
    western MO. Pressure falls have been backing warm sector flow/LLJ
    proving solid moisture and unstable air advection toward the
    frontal zone. Isentropic ascent has been redeveloping
    thunderstorms along a WSW to ENE line from Salina to Manhattan
    toward St. Joseph. The prolonged isentropic ascent from low level
    moisture convergence from the warm sector has resulted in
    saturating the deep profile for rainfall rates to reach 1.75-2"/hr
    over the last few hours resulting in a streak of 2-4" totals and
    long swath of MRMS FLASH unit stream flows reaching 400 cfs/sqmi
    from central KS into NE KS. While the warm sector remains
    unstable with MLCAPEs of 2000 J/kg, the upper-level shortwave axis
    is swinging from weak positive to neutral transferring
    cyclogenesis further southwest along the cold front and resulting
    in increasing height-falls. As such, LLJ is starting to veer
    slightly as the initial surface wave matures/occludes over the
    next 2-3 hours reducing orthogonal upglide. As the cold front
    advances eastward, there will be increasing convective development
    southward with increased forward propagation, reducing duration of
    heavy rainfall and capability of saturating the deeper layer
    profile.=20

    As a result, the best training will still occur across NE KS into
    far NW MO with rates of 1.5-1.75"/hr totals expected. Spots
    already receiving 1-2" may still reach 3"+ totals. FFG values
    decrease steadily east and north with 1.5"/1hr and 2-2.5"/3hrs are
    still in the realm of being exceeded in the shorter term though
    likely decreasing steadily further eastward into south-central
    IA/north-central MO. Strong up/downdrafts capable of a quick
    1-1.5" sub-hourly total are still within a low possibility of
    inducing some flooding concerns especially near urban centers and
    traditionally prone flooding areas, but the progressive nature
    should limit it to those locations only through the morning.=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8yLBRa_lL_djpBXbO78aU_pgHa3ksqlwXVn2DiKc9GU3_eZdlEgBAiTLgf6JKvfK1qdD= hneY2MgjuyVbw0aPzs8do1E$ for graphic product...

    ATTN...WFO...DMX...EAX...OAX...TOP...

    ATTN...RFC...ABRFC...MBRFC...NCRFC...NWC...

    LAT...LON 40989315 40739264 40179248 39639269 39199314=20
    38889380 38609485 38489601 38989700 39649673=20
    40399590 40859437=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 2 19:54:34 2025
    AWUS01 KWNH 021954
    FFGMPD
    KYZ000-INZ000-ILZ000-MOZ000-ARZ000-030100-

    Mesoscale Precipitation Discussion 0105
    NWS Weather Prediction Center College Park MD
    353 PM EDT Wed Apr 02 2025

    Areas affected...northern AR into southeastern MO, southern IL and
    western IN

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 021952Z - 030100Z

    Summary...Areas of training are likely to develop across portions
    of northern AR into southeastern MO, southern IL and western IN
    over the next few hours as an axis of thunderstorms builds north
    and slowly translates eastward. Localized 2-4 inch totals are
    expected (locally higher).

    Discussion...Numerous thunderstorms were ongoing at 1945Z from the
    southern OK/AR border into and across the Ozarks, just ahead of an
    outflow reinforced cold front. Strong southerly 850 mb winds of
    50-60 kt were in place from the lower MS Valley into the lower OH
    Valley ahead of a longwave upper trough anchored over the western
    U.S., aiding the northward transport of moisture/instability into
    the Midwest.

    As one shortwave lobe over MN continues to lift north this
    evening, weak mid-level height falls over the middle to upper MS
    Valley will transition to near neutral height falls down across
    the Mid-South as shortwave ridging was evident in water vapor
    imagery over KS/OK. This large scale pattern will likely result in
    only slow eastward movement to the boundary from southern MO into
    western AR. Largely unidirectional flow from the SW in place ahead
    of the cold front/outflow will promote short term areas of
    training along with repeating cells. Strong low level flow
    overrunning convective induced outflow will allow for the
    continued regeneration of thunderstorms and rainfall rates of 1-2
    in/hr (locally higher). A few locations within areas of training
    could see 2-4 inches of rain (locally higher) through 01Z with at
    least isolated to widely scattered areas of flash flooding
    becoming likely.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4nb0Qiw5SHP0TTWIoUPXoa9JwVKrpaALGqeJ0rfGf4nYa5AxnNC2T1uf070SpI_5MSHG= zriOg13e15HaCbKGP1nsIjc$ for graphic product...

    ATTN...WFO...ILX...IND...LSX...LZK...MEG...PAH...SGF...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NCRFC...OHRFC...NWC...

    LAT...LON 40158729 39028726 37758834 35349074 34749336=20
    35429385 37359227 38999067 40018870=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 2 22:47:00 2025
    AWUS01 KWNH 022245
    FFGMPD
    TNZ000-KYZ000-ILZ000-MSZ000-LAZ000-MOZ000-ARZ000-TXZ000-OKZ000-030400-

    Mesoscale Precipitation Discussion 0106
    NWS Weather Prediction Center College Park MD
    644 PM EDT Wed Apr 02 2025

    Areas affected...ArkLaTex into mid-MS Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 022244Z - 030400Z

    SUMMARY...There are growing concerns for an axis of heavy
    rain/flash flooding to develop from near the ArkLaTex into western
    TN/KY through 04Z. Peak rain rates of 2-3 in/hr will be likely
    within axes of training, most likely across AR to the MS River.

    DISCUSSION...22Z surface radar imagery and surface observations
    depicted an elongated axis of thunderstorms stretching from
    southwestern IL into southwestern AR. A cold front/outflow
    boundary combination was located at the leading edge of the
    thunderstorms and visible satellite/radar imagery showed cloud
    streets and developing thunderstorms feeding into AR from the
    south within 50-60 kt of flow at 850 mb (per area VAD wind plots).
    The environment ahead of the cold front was moderately unstable
    and very moist with MLCAPE of 2000 to 3000+ J/kg and PWATs of 1.7
    to 1.9 inches per a special 20Z SHV sounding and 22Z SPC
    mesoanalysis data.

    Due to a lack of height falls over the Mid-South, south of an
    advancing mid-level shortwave over the upper MS Valley, the
    outflow (effective cold front) is forecast to steadily advance
    eastward into the lower OH Valley over the next 3-6 hours, while
    the southern end of the boundary stalls across the ArkLaTex. The
    resultant orientation should align with the mean steering flow
    from SW to NE. As robust low level moisture transport and
    pre-frontal cells intersect the boundary, coverage of
    thunderstorms should increase from near the ArkLaTex into eastern
    AR and eventually into western TN/KY over the next several hours.
    Areas of training will have the potential to produce 2-3 in/hr
    rainfall rates and depending on the persistence of training over
    any given location, some higher end rainfall totals (4+ inches)
    could materialize.

    Flash flooding appears likely within this setup and should overlap
    of training occur with any urban centers, locally significant
    flash flooding could occur.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!87rQbXWChLFISaUYEuig2aBZ3ZgIUeq0zAQazBHlEiii96a4XxPPlpOvQbUGmz7zZ6Oo= rMhpSP5l5YOPngyrx6T2YS4$ for graphic product...

    ATTN...WFO...FWD...JAN...LZK...MEG...OHX...PAH...SHV...

    ATTN...RFC...ABRFC...LMRFC...OHRFC...WGRFC...NWC...

    LAT...LON 37438778 37018735 35378873 34359049 33259241=20
    32659396 32699536 33329565 33769524 34659337=20
    35029237 36189057 36958900=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Apr 3 00:00:38 2025
    AWUS01 KWNH 030000
    FFGMPD
    OHZ000-KYZ000-MIZ000-INZ000-ILZ000-030555-

    Mesoscale Precipitation Discussion 0107
    NWS Weather Prediction Center College Park MD
    759 PM EDT Wed Apr 02 2025

    Areas affected...Lower OH Valley into IN, western OH into
    southeastern MI

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 022358Z - 030555Z

    SUMMARY...Areas of training are expected to shift into much of IN
    and portions of southeastern MI/western OH through 06Z. Rainfall
    rates of 1-2 in/hr will be possible within areas of training and
    flash flooding will be possible. However, by 06Z or so, rainfall
    intensity is expected to decrease as instability lowers,
    especially for northern locations.

    DISCUSSION...2330Z radar imagery showed that a pre-frontal axis of
    convection extended from far southwestern MI into southeastern MO,
    with embedded mesoscale vortices/bowing segments, but with an
    overall movement toward the east. The environment along and ahead
    of the elongated line of thunderstorms contained 500 to 1500+ J/kg
    MLCAPE and anomalous PWATs at or above the climatological max for
    early April via SPC sounding climatology. In addition to
    increasing upper jet induced divergence aloft, continued low level
    moisture advection within 50-60 kt of 850 mb flow has allowed
    instability to increase over the past few hours, and as a result,
    convective organization has increased over eastern IL into
    northwestern IN since 21Z/22Z. There have been occasional
    instances of training where line orientation has matched the mean
    steering flow, supporting hourly rainfall of 1.0 to 1.5 inches
    over IL into northwestern IN.

    Recent runs of the RAP suggest that CAPE values over IL/IN are
    near their peak for the evening/night and over the next several
    hours, a general downward trend in CAPE is expected with the onset
    of nocturnal cooling, not including minor increases in instability
    over southeastern MI and western OH due to low level moisture
    advection. As the cold front/outflow boundary continues to advance
    east, the ongoing axis of thunderstorms will follow with a general
    progressive movement but there will be embedded areas of training
    as different embedded speeds within the line setup short term
    areas of training. The threat for short term training will
    translate into much of IN and portions of southeastern MI and
    western OH over the next few hours, but with an expectation for
    weakening rainfall intensity toward 06Z as instability fades.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_666p51CeHBYO_OG0vfKqJg8_rFcx8AyZ2eiQYsHo8c_id_oAF9WnokNVf5uc7c8A4DU= cgeQjlQPWg9wlPvkGsvMGuE$ for graphic product...

    ATTN...WFO...CLE...DTX...GRR...ILN...ILX...IND...IWX...LMK...
    LOT...PAH...

    ATTN...RFC...LMRFC...NCRFC...OHRFC...NWC...

    LAT...LON 42838266 42458251 41798282 41458233 39988349=20
    38758468 38008569 37288720 37308865 38198878=20
    40268733 41768595 42718414=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Apr 3 05:35:24 2025
    AWUS01 KWNH 030535
    FFGMPD
    TNZ000-KYZ000-ALZ000-MSZ000-ARZ000-031130-

    Mesoscale Precipitation Discussion 0108
    NWS Weather Prediction Center College Park MD
    133 AM EDT Thu Apr 03 2025

    Areas affected...Mid-South into the TN Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 030530Z - 031130Z

    Summary...Continued scattered to numerous flash flooding with
    rebuilding and backbuilding convection resulting in additional
    2-5" localized totals.

    Discussion...A large line of thunderstorms (QLCS) extends from the
    Lower Great Lakes and OH Valley to the Ark-La-Tex, and the segment
    of the line across West/Middle TN into north MS continues to stall
    with favorable conditions for backbuilding in the near term.
    Ongoing deep convection continues to produce rainfall rates of up
    to 1-2"/hr with ample upper-level divergence in the vicinity of
    the right-entrance region of a large upper-level jet streak. The
    mesoscale environment from north MS to West/Middle TN is
    characterized by SB CAPE of 750-1500 J/kg, precipitable water
    values of 1.3-1.7 inches (near the max moving average, per BNA
    sounding climatology), and effective bulk shear of 55-65 kts. With
    the stalling of the QLCS in this extraordinary environment, given
    a 40-50 kt low-level jet ushering in continued strong moisture
    transport and resulting deep layer moisture flux convergence,
    renewed convection with heavy rainfall is expected.

    Looking at a consensus of the latest hi-res models, an additional
    2-5" of rainfall appears likely across portions of north MS into
    West/Middle TN. While the bulk of this rainfall is expected over
    areas that have received little to no rainfall so far, some
    portions of West TN have already received some heavy rainfall (up
    to 1-3"). Given the current presentation of radar (with impress
    discrete cell signatures reforming in the MS Delta), models may be underestimating the intensity and persistence of cells which may
    backbuild farther north into northeast AR and far West TN.
    Continued scattered to numerous areas of flash flooding are
    likely, and some flooding may become significant in urban areas
    where cells effectively backbuild.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7hfyUf4n7PFOgilrSP4UMqtOuH9yF3kHFRx1lsp8kbmFEgNWua5KgA8xXCiFYxDuv6fr= SP0Ey46nQBq4Cun8RgiQklE$ for graphic product...

    ATTN...WFO...HUN...JAN...LMK...LZK...MEG...OHX...PAH...

    ATTN...RFC...ABRFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 37018687 36798638 36438652 36098678 35818667=20
    35608671 35348709 35048751 34998757 34938769=20
    34668816 34318892 34028976 33959022 33879069=20
    34039183 34269269 34499294 34759274 35139219=20
    35379119 35519058 35658999 35898946 36218884=20
    36468816 36868754=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Apr 3 11:08:16 2025
    AWUS01 KWNH 031107
    FFGMPD
    TNZ000-KYZ000-ALZ000-MSZ000-MOZ000-ARZ000-031705-

    Mesoscale Precipitation Discussion 0109
    NWS Weather Prediction Center College Park MD
    706 AM EDT Thu Apr 03 2025

    Areas affected...Mid-South

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 031105Z - 031705Z

    SUMMARY...Additional repeating rounds of heavy showers and
    thunderstorms going through midday will continue to favor a
    regional threat of flash flooding across the Mid-South.

    DISCUSSION...Early morning GOES-E IR satellite imagery shows an
    axis of heavy showers and thunderstorms tending to repeat/train
    over the same locations across portions of the Mid-South as a
    moist and unstable airmass continues to lift north from the Gulf
    Coast region.

    A moderately buoyant airmass is noted in particular from southeast
    AR through northern MS and into a small portion of middle TN with
    MLCAPE values of 1000 to 2000 J/kg. Areas off to the northeast
    here going up into southeast KY are more stable by comparison with
    CAPE values generally under 1000 J/kg. Area VWP data though shows
    an impressive southerly low-level jet reaching on the order of 40
    to 50+ kts and this is yielding sustainably strong moisture
    transport.

    The combination of this moisture and instability in conjunction
    with a well-defined convectively enhanced surface boundary and
    divergent flow aloft should favor sustainable clusters of
    convection this morning which will tend to be aligned with the
    deeper layer mean flow and thus will promote convective cells repeating/training over the same area.

    The thermodynamic environment will promote rainfall rates with the
    stronger convective cores reaching 1 to 2 inches/hour and
    especially considering the level of shear (effective bulk shear of
    50+ kts) which will favor pockets of strong and organized
    updrafts. The PWs are generally on the order of 1.5 to 1.6 and
    this will support these high rainfall rates as well and especially
    with the strength of the low-level jet.

    Additional rainfall totals going through midday should reach on
    the order of 2 to 4 inches with isolated heavier amounts possible.
    The heaviest of these rains this morning should tend to be over
    central and eastern AR through northwest MS and the western half
    of TN where there is better pooling of instability. Flash flooding
    is already occurring over many of these areas, and additional
    flash flooding is expected through midday.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7Glh58uNZgPDObmYUVJtlqpyrRk27cJF0CuE5_ucCZFEdDUnIaSexig1NfcpKBjt7cIP= OCeUkKIElIczbu5AUaaK_5U$ for graphic product...

    ATTN...WFO...HUN...JKL...LMK...LZK...MEG...MRX...OHX...PAH...

    ATTN...RFC...ABRFC...LMRFC...OHRFC...NWC...

    LAT...LON 37758373 36908347 35968525 35448668 34688896=20
    34119130 34059300 35039302 36139050 36798830=20
    37608587=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Apr 3 11:51:51 2025
    AWUS01 KWNH 031150
    FFGMPD
    ARZ000-TXZ000-OKZ000-031748-

    Mesoscale Precipitation Discussion 0110
    NWS Weather Prediction Center College Park MD
    749 AM EDT Thu Apr 03 2025

    Areas affected...Northern TX...Southeast OK...Western/Central AR

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 031148Z - 031748Z

    SUMMARY...Expanding clusters of heavy showers and thunderstorms
    wil tend to further organize this morning and should favor at
    least some scattered areas of flash flooding, including an urban
    flash flood concern.

    DISCUSSION...A deep layer trough over the Four Corners region
    continues to channel a strong upper-level jet along with embedded
    vort energy out across the southern Plains and toward the broader
    lower MS Valley region. This energy is interacting this morning
    with a moist and unstable southerly low-level jet of 30 to 40+ kts
    across areas of northern TX and southeast OK which is yielding
    several clusters of organized and very cold-topped convective
    clusters.

    A substantial amount of the convection is elevated in nature to
    the north of a quasi-stationary front, and generally rooted within
    a corridor of MUCAPE values of 1000 to 2000 J/kg. However, notably
    higher instability parameters are seen farther south and east into
    the warm sector south of the front. This instability coupled with
    the moist low-level jet and strong vertical shear is promoting
    high rainfall rates and especially with several severe-mode
    supercell structures that are evolving across northern TX to the
    west of the Dallas-Fort Worth metropolitan area and also locally
    across southeast OK.

    Strong upper-level jet energy crossing the southern Plains over
    the next several hours will provide an expansive area of deeper
    layer ascent and shear that will combine with the favorable
    thermodynamic environment for sustinable and well-organized
    convective clusters. Heavy rainfall is expected locally, and the
    rainfall rates are expected to reach 1.5 to 2.5 inches/hour with
    the stronger cells.

    Some occasional cell-merger activity and localized cell-training
    will be possible, and rainfall totals going through midday may
    reach an additional 3 to 4+ inches. These rains will be falling
    locally on some areas that saw heavy rain yesterday including
    parts of northeast TX, southeast OK and western/central AR.
    Therefore, with relatively moist antecedent conditions in place
    here and additional rains likely to arrive this morning, some
    scattered areas of flash flooding are generally likely. Adjacent
    areas of northern TX are a bit more conditionl with the flash
    flood threat, but there will be concern for urban flooding impacts
    should these stronger storms impact some of the larger
    metropolitan areas.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4Y8GZBLcveXpj8IEbv24DJyE-o_wtGlRTDkTfvTgVtJfauzaS1mqXvY3klqhro2a1RMn= DcoHkf2cDNtb4QNuuUhcQM0$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...SJT...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 35929347 35839213 34859170 34129250 33339421=20
    32719611 32439748 32389891 33269930 34209824=20
    35129607=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Apr 3 17:10:22 2025
    AWUS01 KWNH 031709
    FFGMPD
    TNZ000-KYZ000-INZ000-ALZ000-ILZ000-MSZ000-MOZ000-ARZ000-032307-

    Mesoscale Precipitation Discussion 0111
    NWS Weather Prediction Center College Park MD
    108 PM EDT Thu Apr 03 2025

    Areas affected...Mid-South into the OH Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 031707Z - 032307Z

    SUMMARY...There will be increasing concerns through the afternoon
    and early evening hours for increasingly significant and
    life-threatening flash flooding from repeating rounds of heavy
    showers and thunderstorms.

    DISCUSSION...The early afternoon GOES-E IR satellite imagery in
    conjunction with radar shows an extensive axis of heavy shower and
    thunderstorm activity becoming a bit better organized and aligned
    in a southwest to northeast fashion from central AR northeastward
    through western TN and into areas of southern KY.

    Compared to earlier this morning, the overall convective
    orientation has been tending to gain some latitude as subtle
    mid-level height rises over the Southeast U.S. becomes more
    apparent and fosters a stronger poleward transport of warm air
    advection and moisture transport ahead of the deeper layer
    troughing over the central and southern Rockies. The airmass south
    of a well-defined frontal boundary over the Mid-South has become
    moderate to strongly unstable with MLCAPE values of 1500 to 2500
    J/kg and remains quite moist with a southerly low-level jet of 30
    to 40+ kts. The latest CIRA-ALPW data shows a substantial pooling
    of moisture in the SFC/700mb layer with notably strong
    concentrations noted from southern AR through northern MS.

    The concern going through the afternoon and early evening hours
    will be the gradual expansion and organized nature of heavy shower
    and thunderstorm activity over areas that have already seen heavy
    rainfall and flash flooding over the last 12 to 24 hours.
    Streamflows across the region continue to increase and with
    locally saturated soil conditions in place, the additional
    rainfall signal that is coming out of the 12Z HREF guidance
    suggests a growing concern for high-impact flash flooding.

    Rainfall rates are expected to increase to as much as 1.5 to 2.5
    inches/hour with the stronger storms, and especially over areas of central/eastern AR, northwest MS, and western TN where the
    instability nosing over the aforementioned front is a bit
    stronger. By early this evening, some additional rainfall totals
    of as much as 3 to 5 inches will be possible. Flash flooding is
    already ongoing across areas of western and middle TN, and with
    the additional rains, significant and life-threatening impacts are
    expected to gradually occur.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5FwRbRnet63ia_JlOGnqsGOLdEjyOfjYWp1aFGTgiuvIqEiCJMBaGlzpwCdf1sEYYhMj= yIKTGWvfNjmPEzMiRKRBhZM$ for graphic product...

    ATTN...WFO...HUN...JAN...JKL...LMK...LZK...MEG...MRX...OHX...
    PAH...

    ATTN...RFC...ABRFC...LMRFC...OHRFC...NWC...

    LAT...LON 38458369 37868287 37078375 36028580 34928810=20
    34019061 34069213 34889248 35529183 36219041=20
    37058855 38158573=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Apr 3 18:03:21 2025
    AWUS01 KWNH 031802
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-OKZ000-040000-

    Mesoscale Precipitation Discussion 0112
    NWS Weather Prediction Center College Park MD
    201 PM EDT Thu Apr 03 2025

    Areas affected...Arklatex into the Mid-South

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 031800Z - 040000Z

    SUMMARY...Heavy showers and thunderstorms should tend to expand in
    coverage this afternoon and become locally concentrated over parts
    of the Arklatex region and into the adjacent areas of the
    Mid-South. Areas of flash flooding are likely, and locally
    significant impacts will be possible.

    DISCUSSION...A deep layer trough over the Four Corners region
    continues to channel a strong upper-level jet along with embedded
    vort energy out across the southern Plains and toward the broader
    lower MS Valley region. Early morning convective clusters have
    advanced well off to the east-northeast, but the upstream energy
    this afternoon will be continuing to interact with a moist and
    increasingly unstable airmass pooled across eastern TX and through
    the lower MS Valley in close proximity to a frontal zone. The
    result will be redeveloping and expanding coverage of heavy
    showers and thunderstorms.

    The latest surface analysis shows a wave of low pressure lifting
    through northeast TX which will be gradually lifting off to the
    east-northeast over the next several hours along the
    aforementioned front. A southerly low-level jet of 40 to 50 kts
    will be in place ahead of this low center, and there will be a
    corridor of strong low-level moisture convergence that will
    facilitate upscale growth of convection that will likely become
    locally concentrated and focused by later this afternoon. Strong
    instability near and south of the front with MLCAPE values of 2000
    to 3000 J/kg and rather strong shear parameters will also be key
    ingredients for organized convection.

    Recent runs of the HRRR guidance along with the 12Z NSSL-MPAS
    guidance suggests areas of far northeast TX and southern AR will
    tend to be the primary focus for heavy rainfall going through
    early this evening, with convection potentially also training over
    the same area. Rainfall rates with the stronger storms may reach
    as high as 2.5 inches/hour. Some of these rains though will also
    be advancing into downstream areas of the Mid-South currently
    covered by MPD #111.

    Some additional storm totals by early this evening may reach as
    high as 3 to 5 inches, and especially where any cell-training
    occurs. Given the wet antecedent conditions overall and additional
    totals, flash flooding is likely, and there may be some locally
    significant impacts which will include an enhanced urban flash
    flood concern.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4PRh506P9DTJKKPFHI7XH21kt5Ujeh97P0njN6oEddzwS6cqmp4yJ2kzmRwufLPkz4MB= GVkowHWQQ63FoIJMLiIJ6U0$ for graphic product...

    ATTN...WFO...FWD...JAN...LZK...MEG...SHV...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 35179115 34908998 34408966 33959007 33539089=20
    33129221 32779322 32199434 32069546 32639606=20
    33479549 34449410 35039273=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Apr 3 20:10:06 2025
    AWUS01 KWNH 032008
    FFGMPD
    WVZ000-OHZ000-KYZ000-040105-

    Mesoscale Precipitation Discussion 0113
    NWS Weather Prediction Center College Park MD
    408 PM EDT Thu Apr 03 2025

    Areas affected...upper OH Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 032006Z - 040105Z

    SUMMARY...Repeating and brief training of cells could result in
    localized flash flooding across far eastern KY into WV and far
    southern OH over the next few hours. Additional rainfall of 1-2
    inches will be possible through 01Z, falling atop 1-2 inches of
    rain which fell over the past 12 hours.

    DISCUSSION...Regional radar imagery and cooling cloud tops on GOES
    East infrared imagery has shown an increase in rainfall intensity
    across eastern KY over the past 2 hours, attributed to increasing
    instability. Mostly clear skies located south of an outflow
    boundary (located from south of SME, east-northeastward into
    south-central WV between CRW and BKW) have allowed MLCAPE to
    increase into the 500 to 1000+ J/kg range over southeastern KY as
    roughly 30 kt of southwesterly 850 mb flow overruns the boundary.
    Average cell motions have been fast with ~40 kt from the WSW,
    limiting rainfall over any given location, but that rainfall has
    been intense with 0.3 to 0.5 inches in 15 minutes observed.

    A flash flood concern may expand eastward into WV through the
    early evening as instability increases into the southern half of
    WV, through the continued advection of low level moisture and at
    least brief additional heating under clearing skies in southern
    WV. Some backing of low level flow is forecast by the RAP and as
    moist/unstable air continues to overrun the rain-cooled boundary,
    additional storms are expected to form upstream in KY and advance
    downstream into WV. There will likely be some repeating cells and
    perhaps some brief training although uncertainty remains on the
    degree of training into the evening. Given 1 to 2 inches of rain
    which impacted western and central WV over the past 12 hours, an
    inch or two of additional rainfall through 01Z may result in some
    localized flash flooding atop sensitive grounds.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!83ODIoNtyyHDZpeHeYyS4PH3dAxGa2NLQBVuHdICwwSWc5hGEYJouWjLQKpTcM_W6foM= k4ITTYwFn1cMTMx5pmBomgc$ for graphic product...

    ATTN...WFO...ILN...JKL...RLX...

    ATTN...RFC...OHRFC...NWC...

    LAT...LON 39448128 39378022 38597991 38048112 37668250=20
    37778307 38418362 38918296=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Apr 3 23:25:55 2025
    AWUS01 KWNH 032325
    FFGMPD
    WVZ000-OHZ000-TNZ000-KYZ000-INZ000-ILZ000-MSZ000-MOZ000-ARZ000-040500-

    Mesoscale Precipitation Discussion 0114
    NWS Weather Prediction Center College Park MD
    725 PM EDT Thu Apr 03 2025

    Areas affected...lower/middle MS Valley into OH Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 032323Z - 040500Z

    SUMMARY...Additional rainfall of 1 to 3 inches over the next 6
    hours is expected to continue areas of flash flooding from the
    lower/middle MS Valley into the OH River Valley. Peak rainfall
    rates of 1 to 1.5 in/hr (locally up to 2 in/hr possible) are
    likely at times which will overlap, at least partially, with areas
    that have ongoing flooding from heavy rainfall over the past 24
    hours.

    DISCUSSION...Regional radar imagery at 23Z showed scattered
    thunderstorms over TN/KY, mostly north of a stationary front
    analyzed from northwestern MS into Middle TN and eastern KY. A
    greater coverage of thunderstorms was noted back to the west over
    AR and southeastern MO, having originated back near the ArkLaTex
    around 19Z. It appears the clusters of storms over AR/MO were
    located ahead of a subtle low to mid-level shortwave, just nosing
    into southwestern AR at 21Z, best identified in LPW imagery in the
    850-700 mb and 700-500 mb layers.

    The low to mid-level shortwave is likely to track northeastward
    within southwest flow, allowing thunderstorms to spread
    northeastward from AR/MO into the OH Valley overnight. Southerly
    850 mb winds of 40-50 kt are forecast to overspread
    western/northern TN into KY as the shortwave feature moves east,
    maintaining an overrunning component of the stationary
    front/outflow boundary combination over TN/KY. Elements of
    training will be possible and sufficient elevated instability will
    exist to support rainfall rates of 1 to 1.5 in/hr (locally up to 2
    in/hr possible) within axes of training that develop.

    The result will be an additional 1 to 2 inches (perhaps as high as
    3" in isolated spots) through 05Z, resulting in continued areas of
    flash flooding. It seems the bulk of the heavy rainfall threat
    over the next 6 hours will fall north of the axis of heaviest
    rainfall that fell over the past 24 hours, but some overlap along
    the northern edges (northwestern TN into western/central KY) will
    likely occur. These additional rains will exacerbate ongoing
    flooding that is occurring across numerous locations of the MS
    Valley into TN and KY.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-GtEasy6cbb83SbUu4XzvZQY7pkhTbBfcCwtm-XuQZgkv6-rsJ_V80CNjmokbsIXabHo= vGakHxy_ruTA3MR3yIHoEPc$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...JKL...LMK...LSX...LZK...MEG... OHX...PAH...RLX...SGF...

    ATTN...RFC...ABRFC...LMRFC...NCRFC...OHRFC...NWC...

    LAT...LON 39558447 39288337 38518236 37998357 37348474=20
    36158627 35048842 34839010 34969138 35239235=20
    37009071 38108911 39198578=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 4 00:19:22 2025
    AWUS01 KWNH 040019
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-OKZ000-040500-

    Mesoscale Precipitation Discussion 0115
    NWS Weather Prediction Center College Park MD
    818 PM EDT Thu Apr 03 2025

    Areas affected...ArkLaTex into central/eastern AR

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 040014Z - 040500Z

    SUMMARY...While near term flash flooding appears likely over the
    next 1-2 hours from central to eastern AR, uncertainty remains
    back toward the southwest in the vicinity of the ArkLaTex. There
    is some potential for thunderstorms to develop in this region and
    track northeastward into areas of AR over the next few hours,
    reinvigorating a threat for flash flooding across the region.

    DISCUSSION...00Z radar imagery showed scattered thunderstorms over
    central and eastern AR, advancing toward the northeast with little
    in the way of redevelopment back to the southwest. The activity
    was occurring north of a well-defined stationary front that
    extended SW across southern AR into northeastern TX.

    Rainfall rates of 1 to perhaps 2 in/hr will remain possible,
    maintaining the flash flood threat over central/eastern AR for
    another 2 hours or so. This activity is occurring ahead of a low
    to mid-level shortwave noted in LPW imagery with drying in the
    850-700 mb layer in its wake.

    While some weak subsidence is likely occurring in the wake of the
    convective activity moving through AR, moderately strong and
    uninhibited MLCAPE of 2000 to 3000+ J/kg was estimated just south
    of the stationary front over eastern TX into northern LA (via SPC
    mesoanalysis data from 00Z). A forcing mechanism is uncertain
    however and 850 mb winds are forecast by the RAP to weaken from
    their present 30-40 kt to 20-30 kt through 06Z and some weak
    subsidence is likely occurring over the region in the wake of the aforementioned shortwave. Nonetheless, the environment is quite
    unstable and sufficiently moist to support thunderstorms with
    potential for heavy rain.

    Should convection initiate in the next 1-2 hours, there will be
    potential for rainfall rates of 1-2 in/hr, with storm movement
    toward the northeast into portions of the region that have been
    hit with heavy rain over the past 24-48 hours, possibly reigniting
    a threat for flash flooding. However, the threat appears to be
    lowering given the near onset of nocturnal cooling at the surface
    and lack of visible triggers.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_Lj8hPqgQobWkP1sGxNKaXJoXLC7zWfNeY5j7HL6L3yBsXfWTrEGwYazUmurySBCdcEE= Idkgwsda8UFfRyTOmZAk0lg$ for graphic product...

    ATTN...WFO...LZK...MEG...SHV...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 35219184 35099086 34539046 33079260 32209480=20
    32469541 33629469 34659346 35099257=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 4 05:22:18 2025
    AWUS01 KWNH 040520
    FFGMPD
    WVZ000-OHZ000-TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-041115-

    Mesoscale Precipitation Discussion 0116
    NWS Weather Prediction Center College Park MD
    119 AM EDT Fri Apr 04 2025

    Areas affected...Mid-South to the OH/TN Valleys

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 040515Z - 041115Z

    Summary...Continued heavy rainfall with rates up to 1.5"/hr will
    lead to additional 6-hour totals of 2-5". Scattered to numerous
    instances of flash flooding are likely.

    Discussion...Clusters of convection continue to slowly backbuild
    across portions of the Lower MS Valley, mainly over the Ozarks and
    Delta of AR, arcing northeastward into the OH/TN Valleys with the
    deep layer flow. A broad low-level jet (35-55 kts at 850 mb) is
    providing seemingly unending strong moisture transport into a
    narrow, clearly defined axis of overrunning/frontogenesis (also
    ideally in the right-entrance region of a 140+ kt jet streak over
    southeastern Canada). The mesoscale environment is characterized
    by MU CAPE of 250-1000 J/kg, precipitable water values of 1.3-1.6
    inches (near the max moving average, per BNA sounding
    climatology), and deep layer (0-6 km) shear of 60-80 kts.

    Northeasterly deep layer flow will support a relatively narrow
    axis of repeating heavy rainfall over the next 6 hours, with a
    consensus of hi-res CAMs (00z HREF suite) suggesting additional
    localized totals of 2-4" (with rates generally capped at 1.5"/hr
    due to instability being somewhat limited). This heavy rainfall is
    expected to occur over areas that have already seen as much as
    3-7" of rainfall over the past 24 hours (per NSSL estimates).
    Given all of the recent heavy rainfall, it will not take much
    additional rainfall to cause continued or renewed flooding, as
    Flash Flood Guidance (FFG) is indicated to be 1.0" or less for the
    bulk of the region. With hi-res models (00z HREF) indicating
    relatively high odds for localized 2" exceedance (40-km
    neighborhood probabilities of 20-50%), scattered to numerous
    instances of flash flooding are considered likely. Should these
    2-5" streaks of rainfall occur over particularly sensitive
    terrain, flooding may be locally significant.=20=20

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8ulu3UvCykHbl4Zvh12J1sW7Atyp4-CZTiRU-DkPzrKP4NQITkS6py9dd7Ph0NKyah6e= ZQh6mbE_Ckb4gkxGZOiHvS0$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...LZK...MEG...OHX...PAH...RLX...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 39248266 39138199 38748173 38188196 37928239=20
    37428322 36898454 36678539 36368647 35848783=20
    35308941 35209041 35709107 36908981 37788809=20
    38428664 38758553 38998447 39118361=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 4 05:29:34 2025
    AWUS01 KWNH 040529
    FFGMPD
    WVZ000-OHZ000-TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-041115-

    Mesoscale Precipitation Discussion 0116...Corrected
    NWS Weather Prediction Center College Park MD
    128 AM EDT Fri Apr 04 2025

    Corrected for DISCUSSION ERROR

    Areas affected...Mid-South to the OH/TN Valleys

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 040515Z - 041115Z

    Summary...Continued heavy rainfall with rates up to 1.5"/hr will
    lead to additional 6-hour totals of 2-5". Scattered to numerous
    instances of flash flooding are likely.

    Discussion...Clusters of convection continue to slowly backbuild
    across portions of the Lower MS Valley, mainly over the Ozarks and
    Delta of AR, arcing northeastward into the OH/TN Valleys with the
    deep layer flow. A broad low-level jet (35-55 kts at 850 mb) is
    providing seemingly unending strong moisture transport into a
    narrow, clearly defined axis of overrunning/frontogenesis (also
    ideally in the right-entrance region of a 140+ kt jet streak over
    southeastern Canada). The mesoscale environment is characterized
    by MU CAPE of 250-1000 J/kg, precipitable water values of 1.3-1.6
    inches (near the max moving average, per BNA sounding
    climatology), and deep layer (0-6 km) shear of 60-80 kts.

    Northeasterly-directed deep layer flow will support a relatively
    narrow axis of repeating heavy rainfall over the next 6 hours,
    with a consensus of hi-res CAMs (00z HREF suite) suggesting
    additional localized totals of 2-4" (with rates generally capped
    at 1.5"/hr due to instability being somewhat limited). This heavy
    rainfall is expected to occur over areas that have already seen as
    much as 3-7" of rainfall over the past 24 hours (per NSSL
    estimates). Given all of the recent heavy rainfall, it will not
    take much additional rainfall to cause continued or renewed
    flooding, as Flash Flood Guidance (FFG) is indicated to be 1.0" or
    less for the bulk of the region. With hi-res models (00z HREF)
    indicating relatively high odds for localized 2" exceedance (40-km
    neighborhood probabilities of 20-50%), scattered to numerous
    instances of flash flooding are considered likely. Should these
    2-5" streaks of rainfall occur over particularly sensitive
    terrain, flooding may be locally significant.=20=20

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!65jeMKewRQbbm6f8Sc1OzS0H7NWyCscsuXNwaNnmBf5yuNmOhC0rp6mCrBIoV5xm8iKW= H3_oXoiBGms7WCvmQyTpTZo$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...LZK...MEG...OHX...PAH...RLX...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 39248266 39138199 38748173 38188196 37928239=20
    37428322 36898454 36678539 36368647 35848783=20
    35308941 35209041 35709107 36908981 37788809=20
    38428664 38758553 38998447 39118361=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 4 11:04:32 2025
    AWUS01 KWNH 041104
    FFGMPD
    VAZ000-WVZ000-OHZ000-TNZ000-KYZ000-INZ000-ILZ000-MOZ000-041530-

    Mesoscale Precipitation Discussion 0117
    NWS Weather Prediction Center College Park MD
    703 AM EDT Fri Apr 04 2025

    Areas affected...Portions of the Ohio Valley and Central
    Appalachians

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 041103Z - 041530Z

    SUMMARY...Widespread areas of areal flooding and flash flooding
    will continue through the early to mid-morning hours with locally
    considerable impacts as additional rounds of heavy showers and
    thunderstorms arrive. Some improvement expected by late morning.

    DISCUSSION...The early-morning GOES-E IR satellite imagery along
    with dual-pol radar shows an extensive axis of cold-topped
    convection associated with heavy showers and thunderstorms
    impacting large areas of Kentucky with an eastward extension of
    this down into areas of western and southern West Virginia. The
    convection continues to be supported by a south-southwest
    low-level jet of 30 to 40+ kts with a nose of modest instability
    characterized by MUCAPE values of as much as 500 to 1000 J/kg.

    A somewhat complicated frontal structure is in place as well with
    a surface frontal boundary situated across middle Tennessee and
    into the central Appalachians with an inverted trough back to the
    northwest of this over Kentucky that is more reflective of a
    rather strong 850/925 mb front. The convergence along this feature
    coupled with strong warm air advection and moisture transport over
    the surface boundary is contributing to the extensive axis of
    convection that still currently remains in place.

    PWs across the region are generally on the order of 1.5 to 1.7
    inches which is running about 2 standard deviations above normal
    for this time of the year, and this continues to favor heavy
    rainfall rates with aid from the low-level jet. Some rainfall
    rates with the current activity continue to be upwards of 1 to 2
    inches/hour, with some of the heaviest rates seen over central and
    southern Kentucky and coinciding with the colder convective tops.

    A series of very low-amplitude vort impulses embedded within the
    stronger deeper layer west-southwest mid-level flow will tend to
    support some sustenance of the convection at least for the next 2
    to 3 hours, but the 06Z HREF guidance generally suggests an
    overall weakening trend of the convection by later this morning as
    this energy advances downstream and away from the region.
    Additional rainfall amounts of 1 to 3 inches can be expected prior
    to this.

    Regardless, extremely sensitive soil conditions along with high
    streamflows will support generally any additional rainfall going
    right into runoff, with areal flooding and flash flooding likely
    to continue this morning which will include locally considerable
    impacts on the ground.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5Fznc_x1McqQxNPWHnplxKufBF9opAbQWow7JJhAz7Q7psbzXESMyqNSHDL4uqVKT0Gy= FhujT9pj9qC5If6c5iWgQWo$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...MEG...MRX...OHX...PAH...RLX...
    RNK...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 39148251 38998040 38028020 37068290 36598543=20
    36118826 36268923 36888916 37498816 38018666=20
    38658487=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 4 12:33:33 2025
    AWUS01 KWNH 041233
    FFGMPD
    ILZ000-MOZ000-ARZ000-OKZ000-KSZ000-041831-

    Mesoscale Precipitation Discussion 0118
    NWS Weather Prediction Center College Park MD
    832 AM EDT Fri Apr 04 2025

    Areas affected...Eastern OK...Western and Northern AR...Southern
    MO

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041231Z - 041831Z

    SUMMARY...Organizing clusters of heavy showers and thunderstorms
    will pose at least some concern for pockets of flash flooding
    going through midday.

    DISCUSSION...The early-morning GOES-E WV suite shows a vigorous
    mid-level trough gradually ejecting east out into the southern
    High Plains which is interacting with a moist and unstable airmass
    surging northward up into the Arklatex region and broader lower MS
    Valley region along with proximity of a quasi-stationary front. A
    strong southerly low-level jet of 30 to 40+ kts is overrunning
    this front which is yielding substantial warm air
    advection/isentropic ascent and a nose of elevated instability up
    across areas of eastern OK, northern AR and southern MO.

    Already there is a large cluster of strong to severe thunderstorms
    impacting especially northeast OK and northwest AR where very cold
    convective tops to about -75 C are noted. The convection is being
    aided by strong kinematics with strong effective bulk shear
    parameters (50 to 60+ kts) in place coupling with the nose of
    elevated instability with MUCAPE values of 1000 to 2000+ J/kg.

    This convection is expected to remain well-organized through the
    midday time frame with the convection likely becoming more
    pronounced eventually into areas of southern MO, but with
    additional development impacting areas of eastern OK and western
    to northern AR going into the early afternoon hours. This will be
    supported by some further strengthening of the low-level jet
    (reaching as high as 40 to 50 kts) up across eastern OK and
    western AR by early this afternoon ahead of the upstream height
    falls.

    The aforementioned front will be lifting north as a warm front
    with time, and this coupled with proximity of an inverted surface
    trough poleward of the front will yield substantial low-level
    convergence and forcing for convection. While there will be a
    well-defined severe mode to the convection over the next several
    hours, there will be sufficient levels of heavy rainfall that
    pockets of flash flooding may begin to materialize. This will be
    aided by 1 to 2 inch/hour rainfall rates and some rainfall totals
    through 18Z (1PM CDT) of as much as 2 to 4 inches. The more=20
    sensitive locations for runoff concerns should tend be over the
    Ozark Plateau. However, there will also be urban runoff
    considerations for flash flooding as well.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!738EzVqskWXfNmic-InLYm7NPBYcti281QVL6D2CbzgZMNYt1bjIkYgK7s1ZSaPA_cj5= NlCFZiGcVeOow7gYyteXgqM$ for graphic product...

    ATTN...WFO...ICT...LSX...LZK...MEG...OUN...PAH...SGF...SHV...
    TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NCRFC...NWC...

    LAT...LON 37889085 37598974 36888920 36178999 35259323=20
    34289432 34239542 34889594 35729655 36499615=20
    37319440 37769268=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 4 15:14:04 2025
    AWUS01 KWNH 041513
    FFGMPD
    MOZ000-ARZ000-OKZ000-042000-

    Mesoscale Precipitation Discussion 0119
    NWS Weather Prediction Center College Park MD
    1112 AM EDT Fri Apr 04 2025

    Areas affected...Central to Northeast OK...Far Northwest
    AR...Southwest MO

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 041510Z - 042000Z

    SUMMARY...Increasingly concentrated areas of very heavy shower and
    thunderstorm activity is occurring over northeast OK, far
    northwest AR and into areas of southwest MO. Flash flooding is
    likely with locally considerable impacts over the Ozark Plateau
    going through mid-afternoon.

    DISCUSSION...Radar and satellite trends show an increasingly
    concentrated southwest to northeast axis of very heavy showers and thunderstorms across portions of central to northeast OK,
    northwest AR, and into southwest MO.

    There are strong cell-training concerns setting up across this
    region as the convection becomes aligned with the deeper layer
    mean flow and also in close proximity to a well-defined 850/925 mb
    convergence axis/front. Additionally, there is a well-defined
    elevated instability gradient in place here with MUCAPE values of
    as much as 1000 to 2000 J/kg. Facilitating the overall heavy
    rainfall footprint continues to be the nose of a 30 to 40+ kt
    low-level jet which should further strengthen a bit over the next
    few hours which will yield stronger moisture transport into the
    region for convective sustenance and also enhanced rainfall rate
    potential.

    Rainfall rates of as much as 1.5 to 2.5 inches/hour will be
    possible with the stronger storms, but with increasingly
    well-established cell-training concerns, there may be as much as 4
    to 6 inches of rain that occurs by mid-afternoon. None of the
    current 12Z HREF guidance, nor the recent HRRR solutions, have a
    good handle of the ongoing activity. Based on the
    repeating/training signature of cooling convective cloud tops over
    eastern OK, it appears that an organized level of convection will
    certainly continue in the near-term.

    Flash flooding has already started locally, but a more regional
    and higher level of flash flooding impacts can generally expected
    to occur soon, and especially for areas of the Ozark Plateau.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5hBlg23FMRW-uk3586EhmJn2OPHs3FRGHSkqR2KmkuCazBiDilTl66yG0G-Rj8chB_OZ= myMiqQuTGlx8PUH0aYSvFJI$ for graphic product...

    ATTN...WFO...OUN...SGF...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NWC...

    LAT...LON 37689214 37289195 36799275 35959445 35299551=20
    34579645 34799679 35629628 36229565 36859477=20
    37229404 37669286=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 4 15:47:11 2025
    AWUS01 KWNH 041546
    FFGMPD
    VAZ000-WVZ000-OHZ000-KYZ000-INZ000-ILZ000-MOZ000-042000-

    Mesoscale Precipitation Discussion 0120
    NWS Weather Prediction Center College Park MD
    1145 AM EDT Fri Apr 04 2025

    Areas affected...Portions of the OH Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 041545Z - 042000Z

    SUMMARY...Additional pockets of heavy rainfall may continue
    through early this afternoon across areas of western and central
    KY, with areas farther east across eastern KY and southern WV
    seeing a continued slow improvement. Additional areas of areal
    flooding and flash flooding will continue though in the near-term.

    DISCUSSION...Radar imagery continues to show a west to east axis
    of moderate to locally heavy rain associated with showers and
    thunderstorms continuing to focus across the region to the north
    of a returning warm front. Warm air advection/isentropic ascent
    over this boundary along with the proximity of an elevated
    instability gradient is a factor in maintaining the convective
    threat and this continues to be aided by a persistent
    south-southwest low-level jet of 30 to 40 kts.

    The 12Z HREF guidance insists that the threat for heavy rains over
    areas downstream involving eastern KY and southern WV should wane
    going into the afternoon hours, however, there may still be some
    localized persistence of convection with localized cell-training
    concerns for areas of central and western KY including areas
    closer to the OH River. A northward advance of some of the
    convection is also expected to occur over southern IL and southern
    IN which will need to be closely monitored.

    Rainfall rates with the stronger storms still lingering over
    western KY, and also overspreading parts of southern IL and
    southern IN may exceed 1 inch/hour, with some additional spotty
    rainfall amounts here of up to 2+ inches going through
    mid-afternoon. All of these additional rains will only act to
    prolong and exacerbate the ongoing areal flooding and flash
    flooding situation across this portion of the OH Valley.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4qPgw1VzB_zkfCBGqefUftHfJyl9naMVoclp1EdovrKVSoAJj3BfTIA6jdl4RuOQdt_B= Xs0ohtICtWH0jSR58nmVB60$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...JKL...LMK...LSX...MRX...PAH...
    RLX...

    ATTN...RFC...LMRFC...NCRFC...OHRFC...NWC...

    LAT...LON 38868629 38798425 38378207 37578121 37158228=20
    37228348 37298580 37188869 37628964 38328920=20
    38708816=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 4 18:52:06 2025
    AWUS01 KWNH 041852
    FFGMPD
    TNZ000-KYZ000-ILZ000-LAZ000-MOZ000-ARZ000-TXZ000-OKZ000-050050-

    Mesoscale Precipitation Discussion 0121
    NWS Weather Prediction Center College Park MD
    251 PM EDT Fri Apr 04 2025

    Areas affected...Arklatex...Ozark Plateau...Lower MS
    Valley...Lower OH Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 041850Z - 050050Z

    SUMMARY...Numerous areas of heavy showers and thunderstorms will
    continue to evolve going into the evening hours, with concerns for cell-training, and locally very heavy rainfall totals. Numerous to
    widespread areas of flash flooding, including significant and
    life-threatening impacts, are expected to gradually occur going
    into the evening hours.

    DISCUSSION...The early-afternoon GOES-E IR/WV suite shows a
    vigorous mid-level trough continuing to gradually eject east out
    across the southern High Plains which is interacting with a very
    moist and strongly unstable airmass surging northward ahead of it
    involving the Arklatex/Lower MS Valley and portions of the Lower
    OH Valley.

    The latest surface analysis shows an area of low pressure becoming
    a bit better defined across far northeast TX with a warm front
    extending northeast from there up across central AR, northwest TN,
    and into southern KY. Strong warm air advection is surging
    poleward of this front with the aid of a south-southwest low-level
    jet of 40 to 50+ kts. GOES-E visible satellite imagery shows a
    substantial amount of solar insolation helping to destabilize the
    warm sector over the Lower MS Valley and Mid-South, and the latest
    RAP analysis a broad area of MLCAPE values into the 2000 to 3000
    J/kg range. Farther to the north, a lot of this CAPE coupled with
    strong isentropic ascent is yielding a corridor of locally
    enhanced elevated convection currently across northwest AR,
    southwest to central MO, and in a more broken fashion farther off
    to the east into parts of the Lower OH Valley.

    Flash flooding is already ongoing over sizable portions of the
    Ozark Plateau from elevated training convection with rainfall
    rates into the 1 to 2 inch/hour range. However, over the next few
    hours, a much more substantial outbreak of strong to severe
    convection including supercell clusters should evolve over parts
    of the Lower MS Valley and especially the Arklatex region.
    Enhanced instability and strong shear low-level shear parameters
    will be key to this.

    Rainfall rates will be increasing to as much as 2 to 3 inches/hour
    with the stronger and more organized supercell structures, and the
    concern by this evening with be a setup conducive for convection
    training over the same area in close proximity to the
    aforementioned wave of low pressure and related orientation of the
    front. A trailing part of this front will extend down into areas
    of northeast TX, with the northeast extension lifting up into the
    Lower OH Valley.

    Very heavy rainfall totals are likely by this evening, with parts
    of northeast TX through west-central and northern AR likely seeing
    as much as 3 to 5 inches of rain with isolated heavier totals
    possible. The heavy rains with somewhat lesser totals will also
    likely impact areas of southern MO. Given the rainfall totals and
    wet antecedent conditions, numerous to widespread areas of flash
    flooding, including significant and life-threatening impacts, are
    expected to gradually occur heading into the evening hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6R-AfvbxfA3EC4tOOR5sYz7d-C3asUM26WG6qeE4Ew-OUSpuqAOwYxVKBWsj3by8WnYK= tlIKCU7-aQKUtPg1iV0Rbrw$ for graphic product...

    ATTN...WFO...FWD...LSX...LZK...MEG...OUN...PAH...SGF...SHV...
    TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NCRFC...OHRFC...WGRFC...
    NWC...

    LAT...LON 38848910 37778816 36738896 35739043 34379228=20
    32599413 32059512 32049620 32729687 33909669=20
    35719526 38249194=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 4 21:13:09 2025
    AWUS01 KWNH 042113
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MSZ000-MOZ000-ARZ000-050210-

    Mesoscale Precipitation Discussion 0122
    NWS Weather Prediction Center College Park MD
    512 PM EDT Fri Apr 04 2025

    Areas affected...western TN into KY and far southern IN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 042108Z - 050210Z

    SUMMARY...Brief training of scattered thunderstorms will pose a
    possible risk of isolated to widely scattered areas of renewed
    flash flooding across saturated soils of western TN into KY and
    the OH Valley through 02Z. While storm coverage is a bit
    uncertain, rainfall rates of 1-2 in/hr will be possible if/where
    cells are able to repeat/train.

    DISCUSSION...Visible satellite and radar imagery across the OH
    Valley at 21Z showed scattered thunderstorms, some organized
    supercells, from western TN into portions of southern KY. The
    cells were located along or south of a slow moving warm front
    which was analyzed WSW to ENE from the MO Bootheel into southern
    KY. While better forcing and thunderstorm coverage was located
    well to the west of this region (northeastern TX into southern
    MO), sufficient instability, daytime heating, frontal convergence
    and subtle/weak remnant boundaries from prior convection were
    helping to develop storms south of the front.

    Storm motions for most cells should be from the SW to WSW between
    30-40 kt, not a major concern for flash flooding and expectations
    are for cell coverage to remain scattered through the evening.
    However, there is some low-end potential for additional cell
    development on the heels of existing cells to set up a window for
    short term training from SW to NE. Given the highly sensitive,
    saturated soils from 4 to as much as an estimated 10 inches of
    rain over the past 48 hours, the potential for another quick 1-2
    inches could result in isolated to widely scattered flash flooding
    into the evening hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-s0RpwNCXZfkQfdlIuu5LbI6WDR5-gy51CWFUPr9soveKbHvmWUOLpIiX94JFVeCgvlK= ZwhqidXL2jjsNt-ppBQ3Jx0$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...MEG...MRX...OHX...PAH...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 38498606 38478456 37968313 37658271 37178297=20
    36518443 36098633 34958869 35098962 35728981=20
    36828929 37808796=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 5 00:22:10 2025
    AWUS01 KWNH 050022
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-050615-

    Mesoscale Precipitation Discussion 0123
    NWS Weather Prediction Center College Park MD
    821 PM EDT Fri Apr 04 2025

    Areas affected...northeastern TX, ArkLaTex, into central AR

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 050019Z - 050615Z

    SUMMARY...Training of thunderstorms and flash flooding is likely
    to continue from northeastern TX into central AR over the next few
    hours. Rainfall rates within axes of training will contain 1-3
    in/hr rates (but locally higher cannot be ruled out). Additional
    rainfall totals of 3 to 6+ inches may occur within a narrow axis
    from northeastern TX into southwestern AR through 06Z, potentially
    causing considerable to life-threatening impacts.

    DISCUSSION...00Z radar imagery showed a slow moving cluster of
    heavy rain over northeastern TX, from north of I-20 into
    southwestern AR. Colder cloud tops in GOES East infrared imagery
    showed a classic appearance of a strongly divergent and diffluent
    pattern in the upper levels. Observed rainfall rates within this
    cluster have exceeded 3 in/hr at times and produced 5 to 6+ inches
    of rain in the vicinity of Lindale, TX since ~21Z. This cluster of thunderstorms was located along and just ahead of a slow moving
    cold front, attached to a surface low in far southwestern AR. A
    warm front extended northeastward from the low into far
    southeastern MO and was being overrun by a strong 40-50 kt low
    level jet.

    The surface low is forecast to move northeastward into
    north-central AR by 06Z, beginning an eastward push to the front
    over central AR, but with little movement south of the AR/TX
    border. As this occurs, the core of the 850 mb jet axis is
    expected to nudge eastward to the MS Valley, but heavy rain
    along/ahead of the front should remain a flash flood concern due
    to training. Moderately strong MLCAPE values of 2000-3000 J/kg
    (00Z SPC mesoanalysis) should lower a bit due to nocturnal
    cooling, but remain more than sufficient for strong updrafts and
    heavy rainfall production. Alignment of the front with the deeper
    layer steering flow and only a slow eastward translation will set
    up a dangerous pattern for very heavy rain on a localized basis
    with potential for 2 to 3+ in/hr rates and 3 to 6+ inches of rain
    over the next 6 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!80hdqKdN75RYAE95dB8wXfQ7tyDFZkyDyWiogcqXJ3i5MP-DVlqtiZfcSo3Uix2LjJEM= _9F7Wl7lPQ743ys8ezZCNp4$ for graphic product...

    ATTN...WFO...FWD...LZK...SHV...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 35649226 35459160 34609170 33439282 32139408=20
    31629519 32249561 33349493 34149447 34679376=20
    35179315=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 5 01:34:27 2025
    AWUS01 KWNH 050133
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-050725-

    Mesoscale Precipitation Discussion 0124
    NWS Weather Prediction Center College Park MD
    933 PM EDT Fri Apr 04 2025

    Areas affected...northern AR across mid MS/lower OH Valleys into
    central IN

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 050132Z - 050725Z

    SUMMARY...Numerous to widespread flash flood coverage is expected
    to affect locations from northern AR into and across the mid
    MS/lower OH Valleys into central IN through 07Z. An elongated axis
    of heavy rain with embedded training is expected to produce a
    broad swath of 1 to 3 inch rainfall totals with embedded maxima
    over 5 inches possible.

    DISCUSSION...Regional radar imagery at 01Z showed an axis of heavy
    rain that extended from the ArkLaTex into central IL/IN with a
    large number of ongoing flash flood warnings and reports. Within
    this axis were areas of training from SW to NE with MRMS-derived
    hourly rainfall maxima of 1 to 2 inches (locally higher) since
    21Z. A surface low was analyzed over southwestern AR, with a
    quasi-stationary front extending northeastward into the lower OH
    Valley, before turning eastward along the KY/TN border. A strong
    850 mb jet axis of 40 to 55 kt was present just ahead of the
    surface low, streaming anomalous precipitable water values of 1.5
    to 1.7 inches north-northeastward from the western Gulf and
    ascending over the strongly defined baroclinic zone over the
    Mid-South. Unidirectional flow in the low to mid-levels above the
    LFC has, and will continue to support, areas of training overnight.

    Short term forecasts take the warm front northward within the
    highly amplified large scale flow over the lower 48 and form a
    surface low along the front, expected to reach east-central IL at
    06Z. Strong ascent will continue ahead of the low and lifting warm
    front with continued areas of training containing rainfall rates
    of 1-2 in/hr (locally higher), supported by 500 to 1500+ J/kg
    MUCAPE. Aiding ascent will be the right entrance region of a
    strengthening anitcyclonically curved upper level jet max over the
    upper Great Lakes. A broad axis of heavy rain is likely to extend
    from central AR into IL/IN with a gradual eastward translation,
    ahead of the cold front and with possible eastward bowing segments
    of the line, allowing for locally enhanced training/high rainfall
    rates just south of the bowing segments. Convective orientation
    will often match the mean steering flow, supporting prolonged
    periods of training that will gradually shift off toward the east
    into portions of the lower OH Valley which have received very
    heavy rain over the past 24-48 hours. Numerous to widespread
    coverage of flash flooding is likely through 07Z with locally
    significant impacts possible across a few locations.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!95-tfsyPL9x22f_NUxd8Mvhnp6SCNwmNNRzpvSVyLLa4UD3Sp1vT4I23n6f91th7_DQg= UsaVaMwSz6_n83TcxsomfhU$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...LMK...LSX...LZK...MEG...OHX...
    PAH...SGF...

    ATTN...RFC...ABRFC...LMRFC...NCRFC...OHRFC...NWC...

    LAT...LON 40448738 40308540 38828509 37328674 36208886=20
    35029067 35219201 36079193 38378992=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 5 07:11:42 2025
    AWUS01 KWNH 050711
    FFGMPD TNZ000-KYZ000-INZ000-ILZ000-MSZ000-LAZ000-MOZ000-ARZ000-TXZ000-OKZ000-05130=
    0-

    Mesoscale Precipitation Discussion 0125
    NWS Weather Prediction Center College Park MD
    310 AM EDT Sat Apr 05 2025

    Areas affected...Ark-La-Tex through the Mid-South

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 050700Z - 051300Z

    Summary...Convection to continue with rainfall rates of 1-3"/hr
    and 6 hour localized totals of 3-6". Numerous to widespread flash
    flooding to continue.

    Discussion...A blocking pattern on the synoptic scale continues to
    allow for a persistent region uplift via favorable upper-level
    divergence. At the surface, convective initiation usually occurs
    in the vicinity of the quasi-stationary front (in this case also
    accompanied by strong frontogenesis). These storms have a steady
    supply of moisture from the Gulf via an unusually strong and
    persistent low-level jet (30-50 kts at 925-850 mb). Going forward,
    the corridor most favored to receive heavy rainfall is
    characterized by MU CAPE of 1250-1750 J/kg, a ribbon of near
    record high precipitable water of 1.6-1.9 inches (well above the
    max moving average for LZK, as a 2.0" reading has never been
    recorded in April), and deep layer (0-6 km) shear of 40-60 kts.

    Looking ahead, a hi-res model consensus suggest a narrow corridor
    of 3-6" of rainfall is possible over the next 6 hours as the front
    remains stalled in a highly favorable environment for renewed
    convection capable of producing rainfall rates of 1-3"/hr. The 00z
    HREF indicates high probabilities (50-70%) for localized 3"
    exceedance (40-km neighborhood) from southwest AR through far
    western TN and the MO Bootheel. While it is a good thing that the
    bulk of the heavy rainfall over the past 24 hours has occurred to
    the west of the main area of concern (though some portions of the
    Ark-La-Tex are among those that have already received 3"+), 6 hour
    Flash Flood Guidance values still generally range from 2.0-3.0".
    As a result, continued numerous to widespread flash flooding is
    likely. Should some of the more extreme depictions of localized
    5"+ totals occur (as shown by more recent HRRR runs as well),
    significant, life threatening flash flooding will be possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4OWJSAQ9t69iVFfJhpDM-sksI1kTn1EHqLQqAkfvJcUkJhEdjWdEpkf0OTQg6ga4AuKy= j0kCHSadVehZGC7lpzN7ogg$ for graphic product...

    ATTN...WFO...LZK...MEG...OHX...PAH...SGF...SHV...

    ATTN...RFC...ABRFC...LMRFC...NCRFC...OHRFC...NWC...

    LAT...LON 37998815 37618751 36748746 36048839 35668889=20
    34869011 34289110 33799202 33169337 32999405=20
    33149447 33709474 34379432 34909361 35659255=20
    36319153 36819079 37488950=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 5 10:53:04 2025
    AWUS01 KWNH 051052
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-051600-

    Mesoscale Precipitation Discussion 0126
    NWS Weather Prediction Center College Park MD
    650 AM EDT Sat Apr 05 2025

    Areas affected...Central to Northeast TX...Eastern OK...Western AR

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 051050Z - 051600Z

    SUMMARY...Heavy showers and thunderstorms impacting areas of
    central to northeast TX and southeast OK will advance into
    west-central to southwest AR, favoring a continued likelihood of
    flash flooding, including significant and life-threatening impacts.

    DISCUSSION...The early morning GOES-E IR satellite imagery shows
    an elongated complex of cold-topped convection advancing across
    areas of central to northeast TX and up across southern and
    eastern OK. Convection is also seen redeveloping ahead of this
    into areas of west-central AR. The convection is being strongly
    forced by the gradual ejection of stronger height falls across the
    southern Plains in association with a mid-level trough.

    A quasi-stationary front with multiple waves of low pressure
    riding northeast along it remains draped in a southwest to
    northeast fashion from central TX northeastward across central AR.
    As the upstream height falls and axis of DPVA continues to advance
    east, this boundary along with the pooling of moderate to strong
    instability should continue to favor well-organized clusters of
    convection with very heavy rainfall potential.

    MUCAPE values are on the order of 1500 to 2500 J/kg along the
    front, and there is a southerly low-level jet of 30 to 40+ kts
    continuing to favor strong moisture flux convergence parameters.
    The latest RAP analysis shows a stronger corridor of this
    currently across northeast TX up into southeast OK and areas of
    west-central AR where convection recently has grown upscale with
    cooling convective tops.

    The antecedent conditions are extremely sensitive over areas of
    far northeast TX and much of western AR where very heavy rainfall
    and locally high-impact/catastrophic flash flooding has already
    occurred over the last 6 to 12 hours. Sensitivities on the ground
    are also noted over eastern OK with a substantial lowering of FFG
    values compared to 24 hours.

    Additional rainfall amounts going through the mid to late-morning
    hours may reach 2 to 4 inches with isolated heavier amounts which
    is supported by recent HRRR solutions and the experimental WoFS as
    well. Some of the heaviest rainfall at least for the next couple
    of hours should tend to be over far eastern OK and into western AR
    where substantial Low-level forcing is currently in place.

    Expect numerous to widespread areas of flash flooding to continue
    this morning, with locally significant and life-threatening flash
    flooding impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4l2yqdDHE367UPseM7cDidQNpbnCD2iRWQDCrJYjOl65D01yjUcogme9IvthDwbk1PfR= ykLmMMOtzDqwYJydjGhF_9Q$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 36369375 35959288 35059257 33729311 32449450=20
    31829568 31689673 32549738 33999678 35889516=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 5 11:34:06 2025
    AWUS01 KWNH 051132
    FFGMPD
    VAZ000-WVZ000-OHZ000-TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-051730-

    Mesoscale Precipitation Discussion 0127
    NWS Weather Prediction Center College Park MD
    731 AM EDT Sat Apr 05 2025

    Areas affected...Portions of the OH Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 051130Z - 051730Z

    SUMMARY...Additional rounds of heavy showers and thunderstorms
    moving into the OH Valley this morning over extremely
    sensitive/saturated and locally flooded ground will further
    enhance runoff concerns and flooding this morning.

    DISCUSSION...Radar imagery shows a couple of bands of heavy
    showers and thunderstorms advancing east across areas of western
    KY and also western TN, with an axis of weaker and more fragmented
    convection downstream across central and eastern KY which is
    starting to move into parts of southwest WV.

    The surface analysis shows a well-defined outflow boundary/front
    across the region with a persistent southwest low-level jet of 30
    to 40 kts overrunning this boundary and facilitating sustainable
    isentropic ascent and transport of moisture and instability over
    it. However, the best nose of instability with MUCAPE values of
    500 to 1000 J/kg is situated over western TN and this is likely
    going to be the area that sees some of the more organized
    convection persisting through the morning hours.

    One complicating factor to the forecast for rainfall this morning
    though is the fact that there is some evidence of an MCV advancing
    east across western KY, and this vort energy may continue to
    interact with the low-level jet and outflow boundary in a manner
    that may help to sustain the convective threat for a few more
    hours downstream into areas of central and eastern KY. The
    rainfall rates with this will likely be on the order of 1 to 1.5
    inches/hour at most with the strongest cells, but the fact that
    these additional rains will be falling over areas that are either
    already flooded, or have at least very sensitive/saturated soil
    conditions, suggests that additional areal flooding and flash
    flooding concerns will occur over these areas.

    The bigger and more significant concerns for high-end flash
    flooding and life-threatening impacts this morning though will be
    back across western TN and will be connected to upstream heavy
    rainfall/flash flooding concerns evolving back into
    central/eastern AR where there is a growing threat of significant cell-training. Recent runs of the HRRR guidance suggest heavy
    training rainfall over central and eastern AR will impact western
    TN. Very high rainfall rates here of 2+ inches/hour will be
    possible, with additional rains locally of 2 to 4+ inches by
    midday over western TN. The additional downstream rains over KY
    should tend to be more into 1 to 2 inch range.

    Expect areal flooding and flash flooding to continue with locally
    significant and life-threatening impacts as these additional rains
    arrive over the next several hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-cLPD_GDRvtB48xhx_7yzbwEo3MFGEDxdfWq31hwZnAD9txO2ynZHNJ0qXai6HVB7J6Q= gfmRJlUdFvYiKSOpeQEx03s$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...MEG...MRX...OHX...PAH...RLX...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 38918449 38828204 37438196 36308489 35478827=20
    35838980 37088921 38048747=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 5 13:17:02 2025
    AWUS01 KWNH 051316
    FFGMPD
    TNZ000-KYZ000-ILZ000-MSZ000-LAZ000-MOZ000-ARZ000-TXZ000-OKZ000-051915-

    Mesoscale Precipitation Discussion 0128
    NWS Weather Prediction Center College Park MD
    915 AM EDT Sat Apr 05 2025

    Areas affected...Arklatex...Lower MS Valley...Mid-South...Lower OH
    Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 051315Z - 051915Z

    SUMMARY...Training areas of very heavy showers and thunderstorms
    over the next several hours are expected across large areas of
    central and eastern AR and also parts of western TN. High-end
    flash flooding with life-threatening and locally catastrophic
    impacts will likely set up over the next several hours across
    these areas. This is a particularly dangerous situation.

    DISCUSSION...A particularly dangerous situation is expected to
    begin to unfold over the next several hours across areas of
    central and eastern AR and potentially into western TN as a band
    of slow-moving and training showers and thunderstorms with high
    rainfall rates impacts this region. Already the mid-morning GOES-E
    IR satellite imagery and area dual-pol radars show an extensive
    area of convection impacting large areas of the Arklatex with an
    eastward extension of this into portions of the Mid-South and
    Lower OH Valley.

    The convection continues to be driven by the gradual ejection of
    mid-level troughing/height falls across the southern Plains with
    downstream interaction with a moist and unstable 30 to 40+ kt
    southerly low-level jet and proximity of a strong frontal zone.
    Multiple waves of low pressure continue to transit the front which
    is yielding locally focused areas of low-level convergence and
    forcing and this is with an already divergent flow pattern aloft.
    MUCAPE values along the front which extends from southwest to
    northeast AR are on the order of 1000 to 2000 J/kg along with a
    substantial block of vertical shear with effective bulk shear
    values of 50+ kts overrunning large areas of the Lower MS Valley
    and Mid-South.

    The HRRR guidance shows the low-level jet becoming increasingly
    convergent and strengthening to 50+ kts by late this morning from
    far eastern TX up through southern AR with a substantial corridor
    of speed convergence suggested along the nose of this across
    central and eastern AR and into western TN. The moisture transport
    will be very strong, and the latest CIRA-ALPW data shows very
    strong SFC/850 mb LVT (Layered Vapor Transport) values of 320+
    kg/m/s lifting up across the western Gulf Coast region which will
    advance north through the Lower MS Valley by midday and through
    this afternoon. The PWs are forecast to be 1.75+ inches and the
    level of forcing, moisture transport and instability should
    support locally extreme rainfall rates of 2 to 3+ inches/hour.

    Extensive cell-training with these high rainfall rates is the
    major concern over the next several hours, with potential
    additional rainfall totals of as much as 4 to 6+ inches possible
    by mid-afternoon. Saturated soil conditions included areas that
    are already flooded will see enhanced impacts from these rains
    which may include multiple large cities extending from Texarkana,
    AR northeastward to Dyersburg, TN. This is particularly dangerous
    situation with with concerns for Flash Flood Emergency level
    impacts going through mid-afternoon.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-BhH9G-ZmCxiqRHn0PiJVw6byh-WhR6Pg8asL4B-cpi_S5jdNEcf-7jnMRSCrSvGflIo= h8xPwp0PWUV3KiqMR8HI1h4$ for graphic product...

    ATTN...WFO...LSX...LZK...MEG...OHX...PAH...SGF...SHV...

    ATTN...RFC...ABRFC...LMRFC...OHRFC...NWC...

    LAT...LON 37508810 36988764 35838834 34759000 34229102=20
    33379260 32569373 32739468 33249472 34499433=20
    35429358 36019280 37149070 37488942=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 5 19:16:35 2025
    AWUS01 KWNH 051916
    FFGMPD TNZ000-KYZ000-INZ000-ALZ000-ILZ000-MSZ000-LAZ000-MOZ000-ARZ000-TXZ000-06011=
    5-

    Mesoscale Precipitation Discussion 0129
    NWS Weather Prediction Center College Park MD
    315 PM EDT Sat Apr 05 2025

    Areas affected...Lower MS Valley...Mid-South...Lower OH Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 051915Z - 060115Z

    SUMMARY...Widespread flash flooding with continued areas of
    training showers and thunderstorms will continue over the Lower MS
    Valley, Mid-South and Lower OH Valley going into the evening
    hours. High-end flash flooding with life-threatening and locally
    catastrophic impacts will continue to be a likelihood.

    DISCUSSION...Areas of extremely heavy rainfall will continue to
    unfold over the next several hours as an elongated axis of
    slow-moving and training showers and thunderstorms with high
    rainfall rates impact large areas of the Lower MS Valley,
    Mid-South and portions of the Lower OH Valley. The latest GOES-E
    IR satellite imagery shows a very large and impressively
    cold-topped convective canopy over the region, with dual-pol radar
    showing some of the strongest convection and heaviest rainfall
    rates associated with a QLCS stretching from southeast AR up
    across western TN. Rainfall rates with this feature are well into
    the 2 to 3 inch/hour range, and there has been at least some southwest/northeast oriented training of this band of severe
    convection.

    No major changes to the large scale pattern are noted as the
    convection continues to be driven by the gradual ejection of
    mid-level troughing/shortwave energy across the southern Plains
    with downstream interaction with a very moist and unstable 40 to
    50+ kt southerly low-level jet focused along and out ahead of a
    strong frontal zone. Multiple waves of low pressure continue to
    transit the front which is yielding locally focused areas of
    low-level convergence and forcing within an area that is broadly
    divergent aloft.

    MLCAPE along and south of this front and also a nearby outflow
    boundary off to the east are on the order of 2000 to 3000 J/kg.
    Enhanced shear profiles remain in place with robust 0-3km bulk
    shear values of 50 to 60 kts which is favoring highly organized
    and severe-mode convection including supercell development. This
    very unstable/sheared environment coupled with very strong
    moisture transport will continue to favor extremely heavy rainfall
    rates in the 2 to 3 inch/hour range going through this evening as
    the overall convective axis gradually settles down to the south
    and east.

    The experimental WoFS and HRRR guidance support additional
    rainfall totals of as much as 3 to 6+ inches. Some of these
    additional rains will locally overlap with areas of the Mid-South
    and Lower OH Valley that are extremely sensitive and experiencing
    ongoing flooding. This includes parts of eastern AR, western TN
    and much of western KY. However, farther down to the south into
    northern LA, far southeast AR and northern MS, the antecedent
    conditions are notably drier with much higher FFG values.

    Therefore, the high-end threat for significant flash flooding and
    locally catastrophic impacts will continue to be over areas a bit
    farther north, inclusive of multiple major metropolitan areas that
    will see extreme rainfall potential. Areas farther south will be a
    bit more conditional with the threat, but will also still likely
    see flash flooding concerns with potential for significant impacts
    given the extreme rainfall rate potential. Additional localized
    Flash Flood Emergency level impacts overall remain a threat
    heading into the evening hours, and this situation will continue
    to be closely monitored.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_Fnn6fJQ5whc6VQMHy1b3neaQVWPSoDMkQCUmixC0VGJUJ3YCzw0D_ewIeYIVPJ6sOct= 7OspbwYmv0reS7mTHgr2mBM$ for graphic product...

    ATTN...WFO...HUN...ILN...IND...JAN...LMK...LSX...LZK...MEG... OHX...PAH...SGF...SHV...

    ATTN...RFC...ABRFC...LMRFC...NCRFC...OHRFC...SERFC...WGRFC...
    NWC...

    LAT...LON 38838648 38688465 37738437 36768538 35568736=20
    34398894 33149048 32299154 31699282 31479380=20
    31699485 32199497 33259453 34599348 36059201=20
    37209047 38198882=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 5 22:46:30 2025
    AWUS01 KWNH 052245
    FFGMPD
    MSZ000-LAZ000-TXZ000-060430-

    Mesoscale Precipitation Discussion 0130
    NWS Weather Prediction Center College Park MD
    644 PM EDT Sat Apr 05 2025

    Areas affected...Southeast Texas and Southwest Louisiana

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 052244Z - 060430Z

    SUMMARY...Inflow convection into the much more robust showers and
    storms over northern Louisiana has been intensifying over the past
    few hours. Daily record precipitable water in the column is
    supporting convection with very efficient warm-rain processes.
    Localized rainfall rates to 2 inches per hour are expected. Flash
    flooding is possible, especially in urban areas, small streams and
    creeks, and other flood-prone, low-lying areas.

    DISCUSSION...An impressive low level jet is advecting incredibly
    moist air from the Gulf northward on 40-45 kt southerly winds from
    925 through 850 mb. This has pushed PWATs into record territory at
    Lake Charles. The storms are being driven by a very slow moving
    upper level low and associated surface cold front that are
    providing ample lift to support storms that have been producing
    rainfall rates to 2 inches per hour near and just northeast of
    Houston. This surface based convection will continue into the
    evening hours as none of the ingredients supporting very heavy
    rainfall will be abating. Further, recent heavy rainfall across
    the bayous of Louisiana have lowered the thresholds needed for
    flooding caused by these storms as they slowly track east across
    far southeast Texas and southwest Louisiana.

    CAMs guidance has struggled by underdoing both the coverage and
    rainfall intensity of these storms so far. However, there is
    reasonable agreement that the heaviest rainfall over the next 6
    hours (for southeast Texas and southwest Louisiana) will be across
    the southeasternmost counties in Texas and the southwesternmost
    parishes of Louisiana. Additional inflow convection may develop
    further east towards central Louisiana and Baton Rouge later
    tonight in response to the eastward movement of the convection
    further north, but there's considerably more uncertainty for the
    eastern half of the MPD area.

    Given the storms from Houston north and east have developed into a
    training pattern with additional storms forming on the front edge
    of the line near Houston, this pattern of training is likely to
    continue into the evening hours given the very slow movement of
    the parent cold front causing these heaviest storms. Flash
    flooding is possible with these training storms, especially in
    southeast Texas closest to the heaviest storms. Impacts are most
    likely in urban areas around and the eastern suburbs of Houston,
    in already full streams and creeks, and flood-prone low-lying
    areas.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7biR7nHxootvLUv5Wj5Z8zVrTIJhXtlWsjMklbNl1sH6mP0x7whwBUtUF1JntcuPPYOh= Gq1DwLoM9ZR7vhc6R8e2SXo$ for graphic product...

    ATTN...WFO...HGX...JAN...LCH...LIX...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 31909174 31829127 31619117 30809146 30139184=20
    29549215 29579267 29769335 29629425 29169496=20
    29459553 29979542 30519524 30859508 31239487=20
    31579467 31579464 31449396 31549321 31859239=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 5 23:41:25 2025
    AWUS01 KWNH 052341
    FFGMPD
    VAZ000-NCZ000-WVZ000-OHZ000-TNZ000-KYZ000-060530-

    Mesoscale Precipitation Discussion 0131
    NWS Weather Prediction Center College Park MD
    741 PM EDT Sat Apr 05 2025

    Areas affected...Southern Appalachians and Mid-to-Upper Ohio
    Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 052340Z - 060530Z

    SUMMARY...Storms racing eastward at the nose of a robust low level
    jet will likely cause additional flash flooding due to
    rainfall rates up to 1.5 inches per hour occurring over areas hard
    hit by recent heavy rainfall. Flash flooding likely.

    DISCUSSION... The leading edge of a robust low level jet will
    continue to feed weakening storms as they race eastward towards
    the southern Appalachians and portions of the mid-to-upper Ohio
    Valley. While the storms with the heaviest rainfall rates will
    remain at the leading/eastern edge of the precipitation shield,
    they will be able to overcome low FFGs from heavy rainfall this
    past Wednesday and Thursday to further aggravate ongoing river and
    stream flooding. Rainfall amounts of 1-3 inches are broadly
    expected, which in turn will cause additional flash flooding,
    especially in low-lying, urban, and small creeks and streams.

    Rates with the leading line of storms are generally up to 1.5
    inches per hour. Given areal hourly FFGs between 3/4 and 1 inch
    per hour in much of eastern Kentucky, West Virginia and far
    southern Ohio, the leading line should induce additional flash
    flooding as they move through. The plume of rainfall behind the
    storms will persist for a few hours following the initial line of
    storms which will further aggravate flooding as the newly risen
    streams and creeks likely overflow their banks.

    The storms are encountering an environment that is increasingly
    hostile to them, so they should continue weakening as they press
    eastward into eastern Kentucky and West Virginia. The weakening of
    the LLJ to 15-25 kt as well as MUCAPE values only up to 1,000 J/kg
    should support the continued weakening of the storms. However,
    much more potent moisture and instability further southwest but
    upwind along the line should allow the moderate rainfall (with
    rates generally below an inch per hour) to persist well into the
    evening hours.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8UKUIH8WltSq-jzU__W6rUpl3XX2lsuaIgdVx04bSYLx5gZIRfR2y5BNvOZgBVnEQo3-= thuonAf3Z-V3kUAC31jM_vs$ for graphic product...

    ATTN...WFO...GSP...ILN...JKL...LMK...MRX...OHX...RLX...RNK...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 39448169 39408134 38898066 38308049 37588058=20
    36688144 36058257 35668630 36018650 36478574=20
    36768530 37428447 38168426 38608446 38628445=20
    38868472 38868354 38938312 39068256 39238211=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 6 00:44:00 2025
    AWUS01 KWNH 060043
    FFGMPD
    TNZ000-ALZ000-MSZ000-LAZ000-ARZ000-060630-

    Mesoscale Precipitation Discussion 0132
    NWS Weather Prediction Center College Park MD
    843 PM EDT Sat Apr 05 2025

    Areas affected...Portions of the Mid-South from Northern Louisiana
    through Southern Tennessee

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 060042Z - 060630Z

    SUMMARY...Strong convection producing rates to 2.5 inches per hour
    and training storms are likely to cause new flash flooding in many
    areas that have been spared much rain from previous days. Flash
    flooding likely with considerable flash flooding probable in areas
    that have not received much rain in previous days.

    DISCUSSION...Training storms moving NNE along a very slow moving
    cold front are drawing abundant Gulf moisture from an impressively
    robust 50 kt LLJ streaming parallel to the front. Individual cells
    associated with the training storms have a history of producing
    rainfall rates to 2 inches per hour. With the end of the diurnal
    period, the typical strengthening of the LLJ should support the
    strongest cells intensifying further through the evening as they
    are very efficiently using warm rain processes to result in these
    very high rainfall rates.

    CAMs guidance has been very slow with these storms further to the
    north, but the lack of eastward progress in this portion of the
    South has been in decent agreement in the CAMs, which supports the aforementioned strengthening of the storms as the LLJ
    reintensifies.

    Fortunately, all of the storms with the highest rainfall rates now
    have moved south and east of the areas that have been hit hardest
    by the heavy rains over the past 3 days. Thus, they are moving
    over areas now with significantly higher FFGs and soils that are
    far more capable of absorbing at least some of the heavy rainfall
    before it converts to runoff as compared with areas north and west
    in the stratiform rain. Northern and western areas of the MPD area
    that have moved to stratiform rain have been hard hit in recent
    days, and the stratiform rain, while much lower in overall rates,
    will still completely convert to additional runoff, and will
    contribute to continued flash flooding.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!69riJZDaqZsZK_E6UBGr6WJWmsnSF-M0MFzUmARbtzItppYrh5BkKCU2sPdfWWfrVEON= Vc64N_XMFDYfHrcfTKPtql4$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LZK...MEG...MRX...OHX...SHV...

    ATTN...RFC...LMRFC...OHRFC...SERFC...WGRFC...NWC...

    LAT...LON 36058677 35878615 35568538 35108553 33898660=20
    32828815 32278975 32209091 31849229 31749325=20
    31959365 33179259 33929149 35698928=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 6 01:28:23 2025
    AWUS01 KWNH 060127
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-060530-

    Mesoscale Precipitation Discussion 0133
    NWS Weather Prediction Center College Park MD
    927 PM EDT Sat Apr 05 2025

    Areas affected...Lower Ohio and Mid-Mississippi Valleys

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 060126Z - 060530Z

    SUMMARY...Stratiform rain with rainfall rates up to a half inch
    per hour is prolonging ongoing life-threatening flash flooding
    across northeast Arkansas, northern Tennessee, and western
    Kentucky.

    DISCUSSION...An area of stratiform rain on the northern and
    western edge of the moisture plume and convection producing
    incredibly heavy rainfall across northern Louisiana, Mississippi,
    and southern Tennessee will continue to weaken and dissipate from
    northwest to southeast through the evening hours. Heavy rain is no
    longer expected in this area, but the stratiform rain ongoing in
    this area is likely to continue for the next several hours for
    southern and eastern portions of this MPD area, and should end
    within the next hour of northern and western areas.

    This stratiform rain is producing rainfall rates of up to a half
    inch per hour, and for many areas is less than a quarter of an
    inch per hour. While this alone would not be discussion-worthy,
    given the many reports of a foot or more of rain over the past 3
    days, much of which fell earlier today, even this light rain is
    prolonging ongoing life-threatening flash flooding across much of
    this region. As the convection causing the stratiform rain shifts
    to the south, so too will the stratiform. FFGs in this entire MPD
    region are less than a half inch per hour, and in many areas under
    a quarter of an inch per hour, so even this rain is sufficient to
    prolong and in some areas perhaps worsen ongoing flooding. Drier
    air impinging on the precipitation shield from the north should
    continue eroding the precipitation shield, which will finally
    fully and completely end this historic rainfall event across this
    area.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7unvdMqqVXhPOOh1hp9eEUl5K-TOvsZJnKeOjoVCwRbOHwrXU3Z_XABvI74UJaA8vxNA= 852aRTGZboelW2eTltQMZfo$ for graphic product...

    ATTN...WFO...ILN...LMK...LZK...MEG...OHX...PAH...

    ATTN...RFC...ABRFC...LMRFC...OHRFC...NWC...

    LAT...LON 38798478 38758475 38528444 38078433 37488448=20
    36968508 36148647 36098690 36018851 35568966=20
    34899052 34839053 34359118 33749192 33539240=20
    33729268 34449212 35259166 35569142 36089088=20
    36489021 36888923 37428821 37678763 37898714=20
    38208641 38628553 38798509=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 6 07:33:29 2025
    AWUS01 KWNH 060732
    FFGMPD
    GAZ000-ALZ000-MSZ000-LAZ000-061330-

    Mesoscale Precipitation Discussion 0134
    NWS Weather Prediction Center College Park MD
    331 AM EDT Sun Apr 06 2025

    Areas affected...southeast LA and south-central MS into
    north-central AL

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 060730Z - 061330Z

    Summary...Rainfall rates of 1-2"/hr will lead to localized totals
    of 2-4". Scattered instances of flash flooding are likely.

    Discussion...A QLCS is slowly traversing the Southeast this
    morning, with the most intense convection located across much MS
    and moving into AL. Rainfall rates have been as high as 1-2"/hr in
    this area, and those rates are expected to continue with a
    mesoscale environment characterized by ML CAPE of 500-2000 J/kg,
    precipitable water values of 1.4-1.7 inches (near the max moving
    average, per JAN sounding climatology), and deep layer (0-6 km)
    shear of 50-60 kts.

    A consensus of hi-res models suggests that short term (3-6 hour)
    localized totals of 2-4" can be expected, which is likely to at
    least locally continue to eclipse associated Flash Flood Guidance
    (FFG) of 2.5-3.0". While the line of convection is relatively slow
    to move eastward, thankfully it continues to gradually move into
    areas of MS/AL that are much drier are capable of handling heavy
    rainfall. Scattered (to possibly numerous) instances of flash
    flooding are considered likely.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8ylv84Z1m-jjtUsN3NR1DXMO2sMrW6n_iy0xVZQrUFNEhDa0Q0hHODKoQAkY6iaOCjZD= Q80OMObHBP20UnqJgIqbU0s$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...JAN...LIX...MEG...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34928531 34518496 33808559 32978664 32128740=20
    31338814 30128945 29759009 29979071 30449143=20
    31119156 32279055 33708896 34578737 34898632=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 6 12:37:03 2025
    AWUS01 KWNH 061236
    FFGMPD
    FLZ000-GAZ000-ALZ000-MSZ000-061835-

    Mesoscale Precipitation Discussion 0135
    NWS Weather Prediction Center College Park MD
    836 AM EDT Sun Apr 06 2025

    Areas affected...much of central/southern Alabama into western
    Georgia

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 061235Z - 061835Z

    Summary...A couple of slow-moving MCS continues to produce several
    areas of 1-2.5 inch/hr rain rates across west-central Alabama and
    far southeastern Mississippi. These trends are expected to
    continue eastward across the discussion area, posing isolated to
    scattered flash flood potential especially in low-lying and
    sensitive areas.

    Discussion...A couple of slow-moving linear convective segments
    (one from GAD to TCL and another from near MEI to PIB) were
    migrating slowly eastward across the discussion area this morning.
    The linear segments are oriented largely parallel to fast flow
    aloft, with propagation being the primary driver for eastward
    movement. Additionally, the pre-convective airmass (characterized
    by 1.5+ inch PW values, strong low-level shear, and ~1000 J/kg
    MLCAPE) was supporting efficient rainfall processes, with 1-2.5
    inch/hr rain rates focused across western AL and southeastern MS
    nearer the strongest instability. These rates were approaching
    FFG thresholds especially along the BHM/TCL corridor where ~2
    inch/hr rain rates and urban land surfaces were resulting in local
    peaks in MRMS Flash responses. Higher FFGs south of that area
    were resulting in more isolated flash flood potential in the short
    term.

    Over the next 6 hours or so, MCSs should continue eastward
    progress across the discussion area, although some slowing of
    speed may occur with mid/upper forcing remaining well west of the
    area. Surface heating ahead of the MCSs may also provide
    opportunity for open-warm-sector initiation that may support more
    opportunities for cell mergers through the afternoon hours. The
    greatest concern for flash flooding will reside south of I-20 and
    north of I-85 (generally from Birmingham to Montgomery to Auburn)
    where rain rates are most likely to exceed local FFG through 18Z.

    Farther northeast, convection should reach the Atlanta Metro area
    and portions of northern Georgia, but storms seem to be outpacing
    the northeastward extent of the most unstable air across Alabama.
    Isolated flash flooding is possible in this regime as storms reach
    Atlanta by around 15Z or so.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!45s0Hvi48YIxX4L6P5bHqj_CCqLKMfODNcOaxVWSpgjjRoPlOpzcIAfN3JT-M8Pb1O5u= CDTAA-4prmjhVrjOkP7q7a0$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...JAN...MOB...TAE...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34458520 34248383 33328378 32418436 31588540=20
    30968719 30858838 32658852 33668756=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 6 18:25:09 2025
    AWUS01 KWNH 061825
    FFGMPD
    FLZ000-GAZ000-ALZ000-MSZ000-LAZ000-070023-

    Mesoscale Precipitation Discussion 0136
    NWS Weather Prediction Center College Park MD
    224 PM EDT Sun Apr 06 2025

    Areas affected...coastal Mississippi, southern Alabama, and
    southwestern Georgia

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 061823Z - 070023Z

    Summary...Scattered convective bands will continue to promote
    occasional training across the discussion area through 00Z/8p EDT.
    1-2.5 inch/hr rain rates can be expected with the most vigorous
    and training convection. Occasional instances of flash flooding
    remain possible.

    Discussion...Over the past couple hours, a linear MCS has
    exhibited limited/localized convective training while resulting in
    several spots of 2+ inch/hr rain rates northeast through southwest
    of Montgomery. This MCS remains oriented favorably for localized
    training as it migrates toward the Auburn and Columbus areas.=20
    These storms will likely maintain their intensity through at least
    the AL/GA border with local 2 inch/hr rain rates continuing.=20
    Instability is a bit weaker in Georgia, which could result in the
    onset of a weakening trend with storms as they move toward the
    Macon vicinity.

    Farther upstream, trailing, but diffuse outflow was located
    generally from Montgomery west-southwestward to areas just
    southeast of Hattiesburg. Additional showers/thunderstorms
    continue to persist along and south of this outflow generally from
    coastal areas of Mississippi northeastward to Montgomery. A few
    updrafts were also noted on the southwestern flank of the
    aforementioned MCS near Montgomery. These trends will continue,
    with localized areas of backbuilding and training promoting 2
    inch/hr rain rates at times and localized spots of 4+ inch amounts
    through 00Z this evening. Given rain rates and the overall FFG
    spatial profile across the discussion area, flash flood potential
    appears to be maximized in urbanized/sensitive areas and in spots
    that can experience greater than 1-2 hours of training, deep
    convection.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!46JctrMCaWOGj-m2C0VETVgpQJpnfrZ9i8GImeVaxYy7Db-Ph7ZFk-MAXawpHDlxLqQa= inkIm7CqFKJKhDOZEz5gtIU$ for graphic product...

    ATTN...WFO...BMX...FFC...JAN...LIX...MOB...TAE...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 33478451 33478369 32708348 31538453 30848620=20
    30188822 30148950 31238915 32018854 32898634=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 6 23:15:47 2025
    AWUS01 KWNH 062314
    FFGMPD
    FLZ000-ALZ000-MSZ000-070410-

    Mesoscale Precipitation Discussion 0137
    NWS Weather Prediction Center College Park MD
    712 PM EDT Sun Apr 06 2025

    Areas affected...Coastal MS...Southern AL...Western FL Panhandle

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 062310Z - 070410Z

    SUMMARY...Training bands of showers and thunderstorms will
    continue through the evening hours which will include locally
    significant and life-threatening flash flooding concerns from
    extreme rainfall rates.

    DISCUSSION...GOES-E IR satellite imagery shows an extensive axis
    of cold-topped convection impacting portions of coastal MS through
    southwest AL. This corridor of heavy shower and thunderstorm
    activity is embedded within a divergent flow regime aloft with a
    combination of right-entrance region upper jet dynamics and
    shearing vort energy interacting with a moist and unstable
    south-southwest low-level jet.

    The latest area VWP data shows a convergent low-level jet on the
    order of 30 to 40+ kts with some of the strongest moisture
    convergence magnitudes situated across coastal MS/AL and the far
    western parts of the FL Panhandle. MLCAPE valyes of 1500+ J/kg are
    noted across this region with relatively strong shear parameters
    (effective bulk shear of 40+ kts) still favoring organized
    updrafts and a sustainable axis of convection.

    Significant concerns for cell-training will exist through the
    evening hours as this convection tends to maintain itself out
    ahead of a cold front slowly approaching from the west. While the
    overall instability may begin to slowly decrease in magnitude,
    there will likely still be sufficient low-level
    forcing/convergence and modest jet support aloft for convection to
    continue over the next several hours albeit perhaps occasionally
    in a broken fashion. Smaller scale bands of training convection
    are expected to continue though locally.

    Given the thermodynamic and kinematic environment, and level of
    moisture transport off the Gulf, the rainfall rates will continue
    to be locally extreme in nature, with rates as high as 2 to 4
    inches/hour. Already areas around the Mobile, AL metropolitan area
    and adjacent suburbs have been seeing these high rates over the
    last couple of hours. In fact, just in the last hour, the Downtown
    Mobile (KBFM) ASOS reported 3.17 inches of rain!

    The latest HRRR guidance suggests high-end rainfall potential
    going through the mid to late-evening hours, with additional
    rainfall totals of 4 to 6 inches possible, with isolated heavier
    amounts. The 12Z ARW/ARW2 solutions of the HREF suite have a
    similar footprint, but are likely a bit too far to the north
    considering the latest observational trends.

    Given these solutions and the latest radar and satellite trends,
    it seems rather likely that some portions of southwest and
    southern AL in particular, and the far western parts of the FL
    Panhandle will have a period of extreme rainfall over the next few
    hours at least.

    Consequently, flash flooding is likely to continue through the
    evening hours, including potentially significant and
    life-threatening impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6tJnoky9b0kBloIYnqTHjGEexeGoxM-sjB5J2mUVJThqY_OzF6nQArzpr7h1KiUc0lgw= z7Nk5H9SnxJfYkzIemOSPaM$ for graphic product...

    ATTN...WFO...BMX...LIX...MOB...TAE...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 31878642 31848563 31178560 30548641 30208782=20
    30138870 30438895 31008836 31618709=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 6 23:16:10 2025
    AWUS01 KWNH 062316
    FFGMPD
    FLZ000-ALZ000-MSZ000-070410-

    Mesoscale Precipitation Discussion 0137
    NWS Weather Prediction Center College Park MD
    715 PM EDT Sun Apr 06 2025

    Areas affected...Coastal MS...Southern AL...Western FL Panhandle

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 062310Z - 070410Z

    SUMMARY...Training bands of showers and thunderstorms will
    continue through the evening hours which will include locally
    significant and life-threatening flash flooding concerns from
    extreme rainfall rates.

    DISCUSSION...GOES-E IR satellite imagery shows an extensive axis
    of cold-topped convection impacting portions of coastal MS through
    southwest AL. This corridor of heavy shower and thunderstorm
    activity is embedded within a divergent flow regime aloft with a
    combination of right-entrance region upper jet dynamics and
    shearing vort energy interacting with a moist and unstable
    south-southwest low-level jet.

    The latest area VWP data shows a convergent low-level jet on the
    order of 30 to 40+ kts with some of the strongest moisture
    convergence magnitudes situated across coastal MS/AL and the far
    western parts of the FL Panhandle. MLCAPE values of 1500+ J/kg are
    noted across this region with relatively strong shear parameters
    (effective bulk shear of 40+ kts) still favoring organized
    updrafts and a sustainable axis of convection.

    Significant concerns for cell-training will exist through the
    evening hours as this convection tends to maintain itself out
    ahead of a cold front slowly approaching from the west. While the
    overall instability may begin to slowly decrease in magnitude,
    there will likely still be sufficient low-level
    forcing/convergence and modest jet support aloft for convection to
    continue over the next several hours albeit perhaps occasionally
    in a broken fashion. Smaller scale bands of training convection
    are expected to continue though locally.

    Given the thermodynamic and kinematic environment, and level of
    moisture transport off the Gulf, the rainfall rates will continue
    to be locally extreme in nature, with rates as high as 2 to 4
    inches/hour. Already areas around the Mobile, AL metropolitan area
    and adjacent suburbs have been seeing these high rates over the
    last couple of hours. In fact, just in the last hour, the Downtown
    Mobile (KBFM) ASOS reported 3.17 inches of rain!

    The latest HRRR guidance suggests high-end rainfall potential
    going through the mid to late-evening hours, with additional
    rainfall totals of 4 to 6 inches possible, with isolated heavier
    amounts. The 12Z ARW/ARW2 solutions of the HREF suite have a
    similar footprint, but are likely a bit too far to the north
    considering the latest observational trends.

    Given these solutions and the latest radar and satellite trends,
    it seems rather likely that some portions of southwest and
    southern AL in particular, and the far western parts of the FL
    Panhandle will have a period of extreme rainfall over the next few
    hours at least.

    Consequently, flash flooding is likely to continue through the
    evening hours, including potentially significant and
    life-threatening impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8aUsSa2dTP_AHq7EO7N8Aq2tXA_gAcZVx_K_0MLLpfulMOMnD8YT15GBvhT9AvzVGDJd= NJwMezGPybElErU79s7iAEY$ for graphic product...

    ATTN...WFO...BMX...LIX...MOB...TAE...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 31878642 31848563 31178560 30548641 30208782=20
    30138870 30438895 31008836 31618709=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Apr 7 11:15:52 2025
    AWUS01 KWNH 071115
    FFGMPD
    FLZ000-GAZ000-ALZ000-071630-

    Mesoscale Precipitation Discussion 0138
    NWS Weather Prediction Center College Park MD
    715 AM EDT Mon Apr 07 2025

    Areas affected...Central FL Panhandle...Southwest GA...Far
    Southeast AL...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 071115Z - 071630Z

    SUMMARY...Slow moving pre-frontal band with embedded training
    cores pose localized 2-4" totals in 1-3 hours. Flash flooding
    possible.

    DISCUSSION...GOES-E WV suite depicts a broad right entrance region
    of to 130+kt 3H Jet across the area of concern as the jet lifts
    through the central Ohio Valley in the next few hours. A weak
    surface low across NW GA is shepherding along a slow moving cold
    front that now extends southward across SE AL into the far W FL
    panhandle into the central Gulf. Along/ahead of the boundary the
    instability axis is nosed northward into SW GA with 500+ MLCAPE as
    far north as Columbus, GA increasing to 1500+ along the central
    Gulf Coast, this while the moisture axis remains pooled mainly
    through depth along and just anafrontal. However, there is a
    viable overlap location along a pre-frontal surface to boundary
    layer wind confluence and pressure trough. The combination of
    factors as resulted in sufficient convective development of a
    broadening band of thunderstorms from Washington county, FL to
    Houston county, AL toward Calhoun county, GA. Moisture through
    depth results in 1.75" total PWats, however, sfc-850mb LPW
    supported by low 70s Tds suggest the bulk of that is being fluxed
    into the confluent line at 15kts near surface to 35kts near cloud
    base with solid 15-30 degrees of confluence.

    As such, rates of 2"/hr occasionally ticking up to 2.5" are
    becoming more common along the line into SE AL. Furthermore, the
    flow above the boundary layer is providing fairly unidirectional
    flow for training nearly parallel to the slow advancing frontal
    zone. This allows for increased duration, especially as upstream
    redevelopment is occurring well into the Gulf. While the front
    is providing some slow eastward propagation this may allow for 1-2
    hours of heavy rainfall and may result in localized 2-4" totals,
    with highest totals more likely near the stronger flux and higher
    unstable air near the Gulf, though potential to extend further
    inland is expected as instability axis is forecast to shift
    northward as well. FFG values seem to decrease from coast inward
    to SW GA, to pose a similar potential of exceedance though the
    line...but not continuously so. As such, flash flooding is
    considered possible and likely to be widely scattered to scattered
    in nature, and per usual greater near urban and traditional prone
    locations.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!52qAP3rEyJJrL85feL7OzqOLlVvvwVwnMQ7s2AlsmfdL4VZaY7X4h4_rew0hJt3yQdIJ= _cndTreoUIhC1Ri87nZOTcQ$ for graphic product...

    ATTN...WFO...FFC...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 33078300 32688277 31288362 30238431 29638483=20
    29828542 30168584 30388616 31208554 31878483=20
    32848365=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Apr 14 19:16:26 2025
    AWUS01 KWNH 141916
    FFGMPD
    MDZ000-VAZ000-WVZ000-OHZ000-KYZ000-INZ000-150115-

    Mesoscale Precipitation Discussion 0139
    NWS Weather Prediction Center College Park MD
    316 PM EDT Mon Apr 14 2025

    Areas affected...West Virginia, southern Ohio, northern/eastern
    Kentucky

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 141915Z - 150115Z

    Summary...Scattered convection will produce areas/spots of 1
    inch/hr rain rates at time, posing a risk of isolated flash
    flooding through 04Z this evening.

    Discussion...Over the past hour, scattered convection has
    developed from Bloomington to near Cincinnati. These cells were
    on the northeastern extent of an axis of 1000-2000 J/kg SBCAPE and
    were also along and just ahead of a surface front that was making
    steady eastward progress across the Ohio Valley. Convection was
    already oriented parallel to steering flow aloft - with localized
    training noted just south of Cincinnati already prompting
    MRMS/local radar estimates of 0.75 inch/hr rain rates in a few
    spots.

    Through the afternoon, convection will mature and increase in
    coverage, with supercellular wind profiles, moderate instability,
    and continued orientation parallel to mean flow aloft supporting
    localized areas of training. Occasional areas of 1 inch/hr rain
    rates are expected, which could fall over sensitive areas and
    prompt isolated flash flooding. Areawide FFGs are in the 1-1.5
    inch/hr range and should be approached on an isolated basis where
    the most focused/pronounced training could occur. Convection
    should move quickly eastward over the discussion area due to fast
    flow aloft, with flash flood potential increasing over West
    Virginia from the 22Z/5pm timeframe onward. CAMs also indicate
    potential for convective development southwestward along the front
    (across Kentucky) that could produce brief/spotty flash flooding
    if localized convective training can materialize.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9uU820pM34VCL-hWsHDfNgOYr24p-v7klbH-lAsGpbVIoEL812TyUPBzJXtxwu9aJvVS= beq_Xilin9A0D5ddG5RR_WA$ for graphic product...

    ATTN...WFO...ILN...IND...JKL...LMK...LWX...PBZ...RLX...RNK...

    ATTN...RFC...MARFC...OHRFC...NWC...

    LAT...LON 39798072 39207927 38027965 37388120 37008451=20
    37258573 37998577 39388566 39748379=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Apr 17 18:57:54 2025
    AWUS01 KWNH 171857
    FFGMPD
    WIZ000-MNZ000-IAZ000-180035-

    Mesoscale Precipitation Discussion 0140
    NWS Weather Prediction Center College Park MD
    256 PM EDT Thu Apr 17 2025

    Areas affected...western IA/MN border into southern MN/western IA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 171853Z - 180035Z

    Summary...Isolated flash flooding may develop during the late
    afternoon hours from far northwestern IA into southern MN and
    western WI. Rainfall rates of 1-2 in/hr are expected with brief
    training which could allow for some 2 to 3 inch totals through 01Z.

    Discussion...18Z surface observations showed a surface low located
    over west-central MN near BDH with a cold front trailing
    southwestward into NE across the MO River and a warm front
    extending south-southeastward in IA. Surface observations over
    northwestern IA/southwestern MN have shown a dewpoint rise of ~20
    degrees over the past 6 hours, owning to rapid low level moisture
    transport via 30-40 kt of 850 mb winds present over IA/MN out
    ahead of the cold front. The increase in low level moisture
    combined with daytime heating has led to MLCAPE values of
    1000-1500 J/kg via 18Z SPC mesoanalysis data.

    Visible satellite and radar imagery showed convective initiation
    has occurred along the warm front in Sibley County with convection
    likely to expand in intensity and coverage through the remainder
    of the afternoon in the warm sector as the surface low and
    attendant cold front advance downstream. Clear skies on visible
    imagery and continued low level moisture advection are likely to
    increase instability from current values across downstream
    locations along the MN/WI border through 00Z. The portion of the
    cold front closest to the surface low will track eastward more
    quickly than the portion over the MO Valley, which when combined
    with pre-frontal convection, may allow for brief training of
    storms from SW to NE. With any areas of training, the environment
    is supportive of rainfall rates of 1-2 in/hr which may allow for
    isolated 2-3 inch totals through 01Z. Despite dry antecedent
    conditions, flash flood guidance values are only 1-2 inches per
    hour and ~1.5 to 2.5 inches in 3 hours. Localized flash flooding
    will be possible into the early evening but the greatest threat
    will likely be with with any urban overlap of heavy rain.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8EAXMFPDTVnqFpID0U66H6YvxOHD5dQ9OQ7EH6Ya7eYjyaKp31gnXj9FuuimB73slG-j= Lt2LqqJ-j4ldryAcNgnX3XM$ for graphic product...

    ATTN...WFO...ARX...DLH...DMX...FSD...GRB...MPX...

    ATTN...RFC...MBRFC...NCRFC...NWC...

    LAT...LON 45939305 45839185 45299052 44738999 44139044=20
    43929128 43749264 43239439 43359620 44079631=20
    45299515=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 19 02:23:07 2025
    AWUS01 KWNH 190223
    FFGMPD
    ILZ000-MOZ000-ARZ000-OKZ000-KSZ000-190821-

    Mesoscale Precipitation Discussion 0141
    NWS Weather Prediction Center College Park MD
    1022 PM EDT Fri Apr 18 2025

    Areas affected...eastern Oklahoma through southern/east-central
    Missouri

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 190221Z - 190821Z

    Summary...Several instances of flash flooding are possible through
    08Z/3am this morning as convective coverage increases along/ahead
    of a front through the discussion area.=20

    Discussion...Over the past hour, rapid thunderstorm development
    has materialized both along and just northwest of a surface cold
    front extending from near PVJ/Pauls Valley, OK northeastward to
    near Joplin and Springfield, MO. The storms were located in a
    steep mid-level lapse rate environment, with ~7C/km H7-H5 rates
    and 1.25-1.4 inch PW values supporting strong, quickly evolving
    updrafts. The orientation of the initiating front parallel to 50+
    kt mean flow aloft was allowing for this initial convection to
    train and produce spots of 1 inch/hr rain rates (especially in
    northeastern Oklahoma), supporting localized flash flood potential
    in the short term.

    With time, continued evolution of convection into combinations of lines/clusters and even supercells will allow for areas of
    propagation to the right of mean flow. Local rain rates of 1-1.5
    inch/hr are expected, which should approach hourly FFG thresholds
    (in the 1.5 inch/hr range - lowest in Missouri) over time. The
    tendency for storms to grow upscale and propagate eastward may
    help to mitigate a larger-scale flash flood risk tonight, although
    isolated to scattered instances of runoff are still expected where
    convective training is more pronounced. This risk will spread
    northeastward into more of Missouri beginning from 03Z onward and
    perhaps reach portions of Saint Louis and vicinity in the 07-10Z
    timeframe.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6ZUX32AyGcovsmm4U9pjKN1-2GU2Gd03b-N7foR5LYecVDm7Oo_n8BqPMBEnxxOfaPgY= mB5W8M_hGJ_uLhxQOafwATg$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...LZK...OUN...SGF...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NCRFC...NWC...

    LAT...LON 39079119 38529009 37659028 35739330 34069712=20
    34359777 35499688 36779552 38229352=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 19 08:28:21 2025
    AWUS01 KWNH 190826
    FFGMPD
    MOZ000-ARZ000-OKZ000-191225-

    Mesoscale Precipitation Discussion 0142
    NWS Weather Prediction Center College Park MD
    426 AM EDT Sat Apr 19 2025

    Areas affected...northeastern Oklahoma, northwestern Arkansas, far
    southern Missouri

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 190825Z - 191225Z

    Summary...Areas of 1-3 inches of rainfall have occurred, with
    heaviest totals estimated near Rogers, AR. Upstream thunderstorm
    activity should lead to a continued, but localized flash flood
    threat for the next few hours.

    Discussion...Training thunderstorms have produced localized areas
    of 1-3 inches of rainfall along an an axis from just south of
    Muskogee, OK to just west of Branson, MO since 05Z. The heaviest
    totals within this axis have fallen near Rogers/Springdale, AR per
    MRMS estimates. Moderate MRMS Flash responses are suggestive of
    runoff issue in a few areas and also highlights the sensitivity of
    local ground conditions.

    Recent radar mosaic imagery suggests that additional rainfall will
    occur across this axis over the next 2-4 hours or so. A very
    loosely organized convective complex extends from Muskogee
    east-northeastward through Carroll County, AR that is oriented
    favorably for training/repeating and local rain rates of 1
    inches/hr at times. Additionally, newer convection has
    materialized near Oklahoma City that should migrate toward the
    discussion area by around 11Z at the earliest. A break in
    convective activity exists between these storms and the
    aforementioned Muskogee/Carroll MCS, however, which suggests that
    there may be a brief temporal window for excessive runoff to
    subside some before heavy rainfall re-enters the area. Flash
    flooding remains possible in this regime through at least 12Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6TGfurpS73GyPmaSM3oivBB60scu1N8bo8SAA19Q4-s1AiZOJvJy0t0-4KKSFEOTVkq8= nBe67AtSv46Wcu30CNG6Uwg$ for graphic product...

    ATTN...WFO...LZK...SGF...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NWC...

    LAT...LON 37329207 37069125 36719136 36019221 35229397=20
    35139538 35779561 36359513 36909374=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 19 09:22:19 2025
    AWUS01 KWNH 190921
    FFGMPD
    TXZ000-OKZ000-191319-

    Mesoscale Precipitation Discussion 0143
    NWS Weather Prediction Center College Park MD
    520 AM EDT Sat Apr 19 2025

    Areas affected...portions of north/central Texas, far southern
    Oklahoma

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 190919Z - 191319Z

    Summary...A linear convective complex may slow its forward speed
    this morning, prompting an increase in rain rates and a
    conditional flash flood threat.

    Discussion...Convection initially over west Texas has grown
    upscale into a lengthy linear complex extending from Mineral Wells
    to Brady. This complex continues to remain strong due to its
    organization (mature cold pool), steep lapse rates aloft
    (exceeding 7.5C/km), 2000 J/kg MLCAPE, and strong low-level flow
    within the pre-convective environment. The orientation of the
    complex was parallel to southwesterly flow aloft, although
    eastward propagation has held rain rates in check (generally less
    than 1-1.5 inches/hr) so far this morning.

    Some concern exists, however, that this convective band may slow
    its forward progress this morning. Mid/upper troughing continues
    to deepen across Arizona, with falling geopotential heights across
    the discussion area along with a very slight backing of flow
    aloft. The right-ward propagation of the complex was also
    resulting in movement away from stronger mid/upper forcing for
    ascent. This slowing trend is hinted at in some CAMs, although
    uncertainty exists due to poor handling of cold pool/mesoscale
    dynamics.

    Should this slowing trend commence, rain rates beneath the MCS
    should increase and prompt isolated flash flood potential.=20
    Underlying FFGs are quite high though (>2.5 inch/hr) with dry
    soils noted per NASA Sport soil moisture data. Isolated flash
    potential would persist for as long as the MCS maintains its
    intensity. Impacts around the Dallas/Fort Worth metro area cannot
    be completely ruled out.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-5fDOUB7fxm-8kjfYYDzTHcZ4biXBnOgwRuHf_p73-guwmPNv9t9CXJ61YpsYs5YARw5= NcPquMZtvDOVgItB8eJiTiY$ for graphic product...

    ATTN...WFO...FWD...OUN...SJT...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 34069677 33899552 32429590 31409764 31009912=20
    31229966 31999933 32669877 33789763=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 19 11:37:58 2025
    AWUS01 KWNH 191137
    FFGMPD
    MOZ000-ARZ000-OKZ000-191700-

    Mesoscale Precipitation Discussion 0144
    NWS Weather Prediction Center College Park MD
    737 AM EDT Sat Apr 19 2025

    Areas affected...Northwest AR...Southwest MO....Far Eastern OK....

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 191135Z - 191700Z

    SUMMARY...Another round of strong thunderstorms crossing recently saturated/flooded grounds increasing the potential for flash
    flooding through early morning.

    DISCUSSION...10z Surface analysis depicts a complex analysis with
    old outflow boundaries/mixed air with exiting meso-high across MO
    into NE OK. To add to the complexity, a sharpening upper-level
    right jet entrance region is lifting north across central OK into
    E OK/W KS resulting in falling pressures downstream across SW MO
    backing low level flow and increasing deep layer moisture flux
    convergence. This shortwave DPVA/Upper-level divergence ascent
    pattern is noted well in the GOES-E WV suite, with numerous
    overshooting cooling tops breaking through the cirrus canopy
    across E OK starting to encroach on SW MO/NW AR. CIRA LPW backed
    up by RAP analysis denotes a slug of enhanced deep layer moisture
    up to 1.75", along and downstream of the shortwave to increasing
    rainfall production/efficiency over the next few hours. Early
    morning convection limiting factor is typically lack of
    instability; however, a well of mid 70s Temps over mid to upper
    60s Tds and solid lapse rates does support along stream
    instability with SBACAPEs of 1000-1500 J/kg from SE OK to
    W-central AR, likely to be advected northward across the old
    outflow boundary/cold front. The source is not very large and may
    limit coverage and/or duration of convective activity but should
    be sufficient to support 1.5-2"/hr rates.

    The growing concern is the overlap/intersection with already
    saturated/flooded ground conditions across NW AR and so potential
    of an additional 2-3" (mainly in less than 1-1.5hrs) will likely
    result in flash flooding conditions in a few spots, but the
    expansion of the area/source of instability will allow for
    southward and eastward propagation an may expand the areal
    coverage for flash flooding over the coming hours. Further
    diurnal stabilization toward late morning will likely reduce
    intensity with loss/usage of remaining unstable air and
    coverage/intensity should decrease toward 16-17z and into
    south-central MO/northeast AR.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5wjEgPOcun6IIk5wKgeLwfqk7XzBAg9KVnLkwOe46TajoRX8scNBdzJ3MuyiN9u3qteg= 7faW3qEvrHpzFTMtHtikkuY$ for graphic product...

    ATTN...WFO...LZK...SGF...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NWC...

    LAT...LON 37189238 37069184 36809132 36249113 35729134=20
    35189203 34799318 34609408 34529487 34579543=20
    34979555 35969508 36699454 37099363=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 19 12:22:43 2025
    AWUS01 KWNH 191222
    FFGMPD
    OHZ000-KYZ000-INZ000-ILZ000-191720-

    Mesoscale Precipitation Discussion 0145
    NWS Weather Prediction Center College Park MD
    822 AM EDT Sat Apr 19 2025

    Areas affected...Southern IL...Southern IND...Adj Portions of
    Northwest KY...Ext Southwest OH...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 191220Z - 191720Z

    SUMMARY...Limited instability, but favorable repeat/training,
    solid moisture and fairly saturated soils pose a possible widely
    scattered flash flooding incident or two through morning.

    DISCUSSION...Regional RADAR denotes a line of broken convective
    cells with a pair of stronger wave like convective elements
    crossing Southern IL and into Southern IND, along the leading edge
    of sagging cold front from stronger exiting wave across the
    central Great Lakes into Ontario. This orientation is aligning
    with deeper layer unidirectional steering flow along a
    sharp/dominant ridge over the Southeast. Deep layer moisture
    steaks along this boundary with total PWats up to 1.5", mainly
    below 700mb. While RAP/HRRR suggests waning/limited instability,
    there is solid remaining low level heating, with weak nearly
    moist-adiabatic lapse rates but enough to eek out about 500 J/kg
    enough to main ongoing convection. Additionally, 12z surface
    analysis notes stronger below boundary layer convergence
    particularly upstream with push of dying MCV/MCS energy across IL
    increasing surface convergence from weak confluence (30 degrees)
    further downstream to nearly opposition across S IL with weak
    surface wave near MDH/HSB. As such, stronger cells will likely
    continue to support .5-.75" in 15-30 minutes as noted by
    observations. This generally matches the 15-minute totals from
    the HRRR which has been fairly good in timing/orientation with the
    past few runs.

    The length of the confluence/convergence with the weak but
    sufficient instability may allow for repeating/training elements
    over the next few hours to support some localized spots of 1-1.5"
    totals. Very slow southward sag of the boundary/training zone
    will start to cross the strong soil saturation gradient across the
    region where even with a bit of time to dry out, soil saturation
    values remain near 60-70% in the upper 40cm; so with quick burst
    of .5"/15 mins, with some maintained moderate shower activity
    afterward. FFG values are 1.5"/hr which may suggest sub-hourly
    totals may be nearing a critical value especially if they have
    rebounded too quickly given recent high flooding. As such,
    reduced infiltration is considered possible for a widely scattered
    incident or two of flash flooding/ponding conditions particularly
    in urban areas and near prone flashy bluffs.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_pDnkmHo8fKRUap2zK478Y41e5JW4ZCdsWNZ2uze10Tota0giqvb15pXR3vnr5HN-vfq= maHZgvuHsAqTOxGWiik0GdI$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...LMK...PAH...

    ATTN...RFC...LMRFC...NCRFC...OHRFC...NWC...

    LAT...LON 39838459 39378422 38968445 38188600 37468776=20
    37158868 37308932 37888931 38578835 38918761=20
    39248702 39618608 39818537=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 19 21:31:50 2025
    AWUS01 KWNH 192131
    FFGMPD
    TXZ000-OKZ000-200245-

    Mesoscale Precipitation Discussion 0146
    NWS Weather Prediction Center College Park MD
    530 PM EDT Sat Apr 19 2025

    Areas affected...west-central TX into east-central OK

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 192130Z - 200245Z

    Summary...Repeating and training of cells over west-central TX
    will pose at least a localized but increasingly likely flash flood
    threat over the next several hours. The flash flood threat is
    expected to expand northeastward into northern TX and east-central
    OK after 00Z. Rainfall rates of 1-2 in/hr will be likely and
    totals in excess of 4 inches through 03Z will be possible.

    Discussion...Surface observations and radar imagery from 21Z
    showed 3 or 4 supercells between MAF and SJT located near a
    quasi-stationary front with movement toward the northeast.
    Additional development was occurring northeast of these stronger
    cells. The cells were located near and northeast of a triple point
    low located just east of FST within a very unstable but modestly
    moist environment with 2000-4000 J/kg MLCAPE and PWATs near 1 inch
    (via recent SPC mesoanalysis data). Cell coverage will increase
    over the next few hours as forcing for ascent increases ahead of
    an approaching mid-level low over western NM and as continued low
    level moisture advection into/across the Red River helps to boost
    instability.

    Individual cells are likely to continue a northeastward motion
    following the deeper-layer mean flow and frontal orientation but
    organized supercells are likely to move right of the mean wind.
    There will likely be elements of short term training as cell
    alignment matches the steering flow but as cells advance off
    toward the northeast, additional development is expected near the
    triple point as low level southerly/southeasterly flow advects
    unstable airmass back into the region.

    Beyond 00Z, 850 mb winds are forecast to increase over
    central/eastern TX above 40 kt, increasing low level moisture
    northward across the Red River with pockets of CIN eroding across
    OK (via recent RAP forecasts) likely supporting convective
    development and expansion through 03Z. Given similarly oriented
    storm motions and boundary orientation at the surface, training is
    expected to become increasingly likely. Rainfall rates of 1-2
    in/hr are expected to develop with areas of flash flooding
    becoming likely. Potential for localized totals greater than 4
    inches will exist and may overlap with the northern edge of 1-2
    inches of rain which fell over the past 24 hours over portions of
    TX/OK.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6QK-IFBxP_faYCThfe5DdxiQNub2Eeq7nuHf7c24BVknH3dtNaZy_P4aFGY5BPb0kLp2= IQ_D9P2ISE8mXfw7ZETkTK0$ for graphic product...

    ATTN...WFO...FWD...LUB...MAF...OUN...SJT...TSA...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 35669666 35639576 35269554 34579577 33069725=20
    32169859 31650003 30690195 30730263 31280247=20
    32370115 33459966 34869821=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 20 02:43:36 2025
    AWUS01 KWNH 200243
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-KSZ000-200800-

    Mesoscale Precipitation Discussion 0147
    NWS Weather Prediction Center College Park MD
    1042 PM EDT Sat Apr 19 2025

    Areas affected...west-central TX into northeastern OK into
    adjoining portions of KS/MO/AR

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 200240Z - 200800Z

    SUMMARY...Training of heavy rain will continue over the next
    several hours with a particular focus from areas of northern TX
    into southeastern OK. Peak/localized rainfall rates over 3 in/hr
    cannot be ruled out and an additional 3 to 6 inches may overlap
    with locations that have picked up 2 to 4 inches within the past
    2-3 hours. Considerable flash flooding with life-threatening
    impacts will be possible.

    DISCUSSION...Radar imagery over TX/OK showed a SW to NE oriented
    axis of thunderstorms which extended from west of San Angelo, TX
    to just north of Ardmore, OK. Supercells were embedded within the
    axis and a general SW to NE movement of cells was allowing for
    training and high rainfall rates. Recent reporting stations from Wunderground.com showed 3 to 6 inches of rain has fallen in
    Montague County in northern TX since earlier today with rainfall
    rates locally at or in excess of 3 in/hr between Bowie and Nocona
    over the past 1-2 hours. Most of the convection was located along
    or north of a frontal boundary draped across the southern Plains,
    attached to a surface low just northeast of Fort Stockton.

    The LLJ was measured by a few VAD wind plots in central TX at or
    above 50 kt from the south and this southerly flow was overrunning
    the baroclinic zone in place. Steering flow pointed toward the
    northeast, or roughly parallel to the surface boundary, was
    allowing for training and repeating cells. Additional
    strengthening of the LLJ (~10 kt) is expected over the next few
    hours ahead of a cold front extending southwest from the surface
    low near Fort Stockton, forecast to sweep eastward over the next 6
    hours. The surface low is forecast to track northeastward toward
    the Red River overnight with strong ascent ahead of an ejecting
    mid-level closed-low approaching from NM.

    Training will continue with a particular focus for higher end
    flash flooding possible from portions of northern TX into
    southeastern OK. Recent WoFS output has shown high probabilities
    (70 to 90+ percent) for 3+ inches extending from northwest of Fort
    Worth, across the Red River near I-35 into southeastern OK between
    Ardmore and McAlester. 50th percentile values from the 02Z WoFS
    showed a stripe of 3-4 inches across this zone and 90th percentile
    values (reasonable spot maxima) were 5-6 inches. Portions of the
    region over northeastern OK into adjoining areas of KS/MO/AR
    received heavy rain early this morning and are more sensitive to
    runoff from additional heavy rain, with an additional 2-4 inches
    possible across these northern areas of the MPD threat area.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9gpJbSa5-KNCzrfBTjBFoyuOJeRbHSAxBEJhkqpr48ZReyBOfuHjDvOD9Oha5290X_1j= TYkseKB6nNGpmN2TKkUFMKE$ for graphic product...

    ATTN...WFO...FWD...LUB...MAF...OUN...SGF...SJT...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 37069474 36699427 36169407 35419451 34049574=20
    33079686 32479782 31739910 30830191 31200255=20
    32350138 33639939 35429726 36739566=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 20 07:37:56 2025
    AWUS01 KWNH 200737
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-KSZ000-201335-

    Mesoscale Precipitation Discussion 0148
    NWS Weather Prediction Center College Park MD
    337 AM EDT Sun Apr 20 2025

    Areas affected...north-central Texas northeastward into the
    Missouri Ozarks

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 200735Z - 201335Z

    Summary...Flash flood potential continues from far north-central
    Texas through eastern Oklahoma. Some of this potential should
    spread into far northwestern Arkansas and southern Missouri as
    well.=20

    Discussion...Three linear convective complexes have materialized
    and picked up forward progress along an axis extending from near
    Joplin, MO south-southwestward through Ardmore, OK to near
    Stephenville, TX and Del Rio, TX. Because of the increase in
    forward speed and upscale growth, the spatial extent of 1 inch/hr
    rain rates have lessened substantially over the past two hours,
    with only localized pockets noted per MRMS across southeastern
    Oklahoma and west-central Texas. Nevertheless, these rates are
    falling on areas of lowered FFGs from prior rainfall over the past
    24-36 hours. MRMS Flash responses also remain elevated from
    Jacksboro to Ardmore and near Muskogee. The orientation of
    ongoing MCSs will allow for rainfall to repeat across these areas,
    preventing any recovery from earlier flash flooding in these areas
    and potentially worsening runoff in some spots.

    The ongoing MCSs should continue to move eastward, but models
    suggest potential for stalling of forward progress especially
    across eastern OK/northwestern AR as a closed upper low hangs back
    over New Mexico. The slowing MCSs and areas of convective mergers
    should allow for continued flash flood potential especially in
    areas that received prior heavy rainfall. Again, FFGs remain
    lowered from eastern OK into northwestern AR from 3-8 inches of
    antecedent rain, and 1-1.5 inch/hr rain rates should continue at
    least on a spotty basis for the next 3-6 hours across the
    discussion area.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-U1RJgmAj7dXOJ7TLrRdG9B8hi9c6_l8zuIKYDkQG4oTQRsRNPyGJUaxGejs4sDkRzC_= iONFyol8VrfMt_hW3J-Kots$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SGF...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NCRFC...WGRFC...NWC...

    LAT...LON 38009189 37309158 36289193 35639271 34299488=20
    33119599 32899779 33159847 34069822 34929741=20
    36579591 37579364=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 20 15:25:58 2025
    AWUS01 KWNH 201525
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-202115-

    Mesoscale Precipitation Discussion 0149
    NWS Weather Prediction Center College Park MD
    1125 AM EDT Sun Apr 20 2025

    Areas affected...Eastern OK...Northwest AR...Southwest
    MO...Southeast KS...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 201525Z - 202115Z

    SUMMARY...Recharging thermodynamic enivorment and strong forcing
    starting to initiate scattered convective activity capable of
    intense rain-rates (1-1.5"/hr) across saturated soils conditions
    possible to result in renewed flash flooding conditions locally.

    DISCUSSION...GOES-E WV suite depicts about 1.5 standard deviation
    deep closed low centered across SW OK continuing to lift
    northeastward with a negative tilt orientation extending across
    the Red River Valley. The suite along the RADAR mosaic also
    denotes the southern stream shortwave/MCV from last evening's
    convective complex remains at the western gradient of the warm
    conveyor belt in southwest MO lifting north-northeastward. The
    pair support a stronger 1008/9mb surface low across central OK
    with a warm front extending eastward across southeast OK while a
    progressive cold front is undercutting through northeast TX. The
    Ozarks/Boston Mountains along with worked over surface environment
    breaks the frontal zone across NE OK toward a weakness in the
    surface pattern across SW MO associated with the aforementioned
    shortwave.

    The interaction with these waves and strong dynamics (DPVA and
    right entrance ascent pattern) across E OK is strengthening and
    backing low level warm sector and sharpening the FGEN fields
    across central to northeast OK into SW OK. VWP suite shows
    southerly flow strengthening to 40-50kts through 700mb advecting
    the conditionally unstable airmass across E TX/W AR where breaks
    in cloud cover are bringing temperatures into teh low 70s with
    increasing surface Tds into the mid 60s resulting in SBCAPEs over
    1000 J/kg. Given the advective environment/strong backing flow
    and isentropic ascent downstream of the height-falls; moisture
    convergence/FGEN is strengthening across E OK attm.=20=20

    As such, regional RADAR depicts increasing shallow convective
    coverage across Coal/Hughes/Creek county axis with more widely
    scattered activity further northeast along the WAA/FGEN axis into
    SW MO. Total PWats of 1.25, steadily increasing toward 1.5" and
    vertical development should support rates of 1-1.5"/hr with bulk
    falling in less than 30 minutes. Forward propagation is likely to
    initially limit overall totals initially to 1-1.5", but will be
    falling across compromised soil conditions likely to exceed the
    lowered FFG values (.75-1.5"/hr), the forward speed/coverage of
    the rainfall may be limited and only result in re-aggravating
    flash flooding conditions across the area; however, as the
    afternoon progresses, increased heating/convective vigor will
    increase coverage allowing for broader coverage particularly along
    a SW to NE axis near the triple point as it lifts across NE OK,
    far SE KS, SW MO where training/repeating will occur where SWly
    steering flow is more parallel to the FGEN axis. This is also
    where FFGs are further compromised below .5"/hr likely resulting
    in broader areas of flash flooding into the mid-afternoon.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7p7E-w_gRtyoJqAWg-X5ohvJU_BPEKgD8jpwiVzfZyv5d3jgrL7OflBf_Oy6XiwAsceK= bYOi78V9u94eoxeSq1VCufk$ for graphic product...

    ATTN...WFO...EAX...ICT...OUN...SGF...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NWC...

    LAT...LON 38819352 38499282 37759260 37279277 36549330=20
    35549393 34999446 34649485 34139579 34439655=20
    35459673 36269662 37029605 38269479 38689419=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 20 20:28:16 2025
    AWUS01 KWNH 202027
    FFGMPD
    WIZ000-ILZ000-MOZ000-IAZ000-210220-

    Mesoscale Precipitation Discussion 0150
    NWS Weather Prediction Center College Park MD
    427 PM EDT Sun Apr 20 2025

    Areas affected...MO into eastern IA and far western IL

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 202026Z - 210220Z

    Summary...Heavy rain will translate north-northeast from MO into
    IA through 02Z with embedded rainfall rates of 1-2 in/hr due to
    training. Flash flooding is expected (especially across wet
    antecedent conditions) from an additional 2-3 inches, although 3+
    cannot be completely ruled out.

    Discussion...20Z surface observations placed a triple point
    surface low along the southern KS/MO border with a cold front
    extending southward from the low into western AR and a warm front
    extending ENE across central MO. An inverted trough extended north
    from the triple point low through western MO into central IA with
    an attached surface low near CDJ. A convective line was
    propagating eastward ahead of the cold front through southwestern
    MO into a region of saturated soils due to 4 to 8 inches of rain
    over the past 2 days. Farther north, surface convergence along the
    inverted trough and slightly elevated low level convergence at the
    nose of 35-50 kt 925-850 mb winds were aiding the placement of a
    SW to NE axis of thunderstorms extending across north-central MO,
    with periods of training ongoing.

    As a potent mid-level shortwave tracks northeastward from the
    central KS/OK border to the east-central IA/MO border over the
    next 6 hours, the triple point low will follow a similar path with
    low level convergence sustaining thunderstorms ahead of the
    inverted surface trough in a SW to NE fashion (at least early on).
    Increasing divergent and diffluent flow aloft within the right
    entrance region of an upper level jet streak over western IA will
    overlap the low level convergence yielding strong ascent. Steering
    flow oriented SSW to NNE will support training along this low
    level convergence axis ahead of the triple point low with rainfall
    rates of 1-2 in/hr. Farther south, closer to the warm front's 20Z
    position, additional rainfall should be lighter due to the
    progressive nature of the convective line, with perhaps an
    additional 1 to 1.5 inches max over the next few hours.

    The greater concern for flash flooding will be over central MO due
    to recent heavy rain, followed by locations from northern MO into
    eastern IA where training is likely to produce an additional 2-3
    inches along a fairly narrow axis. While a lack of recent rainfall
    has northern MO into southern IA with limited soil moisture values
    per NASA SPoRT imagery, flash flood guidance is as low as 1.5 to
    2.5 inches in 3 hours and is likely to be surpassed in a few
    locations.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4iZwCzsOU28YRCv-ryi1RghtsXfAieEaTm8mZirYUzjFahLb77Q3yXQeIGU9Wh7IOZE-= 2YDK19ajMOGYVYxrzsOEDc0$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...EAX...LSX...SGF...

    ATTN...RFC...ABRFC...MBRFC...NCRFC...NWC...

    LAT...LON 42959099 41549071 39919100 38339169 37689236=20
    37249332 37319402 37749442 38639448 39329435=20
    40759361 42909264=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 20 23:09:56 2025
    AWUS01 KWNH 202308
    FFGMPD
    TXZ000-210435-

    Mesoscale Precipitation Discussion 0151
    NWS Weather Prediction Center College Park MD
    708 PM EDT Sun Apr 20 2025

    Areas affected...middle/upper TX Coastal Plain

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 202306Z - 210435Z

    SUMMARY...Isolated flash flooding will be possible from training,
    slow movement and/or backbuilding thunderstorms along portions of
    the TX Coastal Plain through early tonight. Rainfall rates could
    exceed 2 to 3 in/hr resulting in storm total rainfall of 3 to 6
    inches.

    DISCUSSION...Visible satellite and radar imagery showed a line of
    scattered thunderstorms extending from eastern TX to the middle TX
    coast, located along a trough axis positioned ahead of a cold
    front/dryline which extended SSW from northeast TX into the
    southern Coastal Plain. The environment was supportive of heavy
    rain with PWATs of 1.7-1.9 inches, MLCAPE of 2000-2500 J/kg and
    effective bulk shear of 25-40 kt (22Z SPC mesoanalysis).

    Over the past few hours, cell motions have been averaging 20-25 kt
    toward the NE (similar to the 0-6 km AGL mean wind), parallel to
    the initiating trough axis, although slower motions were observed
    south of 29 degrees N, where shear values were weaker. Cells to
    the south were less numerous but have had a history of
    backbuilding and rainfall rates of ~1 inch in 15 minutes across
    portions of eastern Victoria County.

    MLCAPE of at least 1000-2000 J/kg with little to no CIN is
    forecast by the RAP to persist across the TX Coastal Plain beyond
    sunset along with some degree of continued convection. While bulk
    shear values are forecast to lower from south to north with a
    departing mid-level shortwave over KS/MO, there may remain a
    narrow zone where sufficient shear exists for at least
    quasi-organized cells where low level inflow remains modest along
    the middle to upper TX coast after 00Z. The combination of slowing
    cell motions with a continued (though modest) influx of low level
    moisture may be enough to sustain a cell or two with slow net
    movement (backbuilding/training) which could result in localized
    heavy rain with 3 to 6 inches possible.

    However, this threat is considered to be very isolated in nature
    and given dry antecedent conditions from a lack of rainfall over
    the past two weeks, any impactful threat of heavy rainfall would
    likely remain isolated and urban in nature.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Xwum2D-HNNvpNkuhJ1VMI4cungmctJ4h9_IkFKXekp1mIMO9FuWFgVAwGCaVVcEUoNj= BcuU_IhmnOccn2CnGoDtkhc$ for graphic product...

    ATTN...WFO...CRP...EWX...HGX...LCH...SHV...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 31499497 31249426 29809509 28639650 28679709=20
    29419670 30369581=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Apr 21 04:30:20 2025
    AWUS01 KWNH 210428
    FFGMPD
    LAZ000-TXZ000-211026-

    Mesoscale Precipitation Discussion 0152
    NWS Weather Prediction Center College Park MD
    1227 AM EDT Mon Apr 21 2025

    Areas affected...western Louisiana, southeastern Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 210426Z - 211026Z

    Summary...Isolated flash flood potential will continue through at
    least 10Z/5a CDT.

    Discussion...Flash flood potential continues across the region.=20
    04Z radar mosaic imagery depicts scattered, slow moving clusters
    of thunderstorms along an axis from just south of Shreveport to
    just northwest of Houston. The axis of convection was collocated
    with an axis of confluent 850mb flow, with thunderstorms being
    maintained by an airmass characterized by 1.5-1.8 inch PW values,
    1000 J/kg MLCAPE, and weak convective inhibition. Ascent aloft
    associated with a mid-level wave continues to depart the region,
    which has resulted in slower storm motions (from weaker wind
    fields aloft) and occasional heavy rain rates lasting for 1-3
    hours, resulting in local areas of 2-4 inch rainfall totals.=20
    These totals have impacted portions of Shreveport Metro, prompting
    impacts earlier tonight.

    Models/observations suggest that the current trends will continue,
    with areas of 2-5 inch rainfall totals occurring beneath heavier
    and most persistent convection through 10Z this morning. The
    confluence axis and attendant thunderstorm activity may develop
    slowly southward during this period as well. FFGs are quite high
    (~4 inch/3-hrly rates) across the region, suggesting that heavier
    rainfall may need to occur across sensitive and/or urban ground
    conditions for any substantial impacts to materialize.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9rpuMnsWVoUVWykel--mceOdkwKFz_L81jMyUAVG6use6GRbzk_LfkXqfHKz3J7R9WEq= YcpZCeOH9suzl_J0Gr_ikfc$ for graphic product...

    ATTN...WFO...HGX...LCH...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 32819266 32029230 30659348 29299519 28829635=20
    29619631 30229592 31809459 32599358=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Apr 21 09:52:53 2025
    AWUS01 KWNH 210952
    FFGMPD
    LAZ000-TXZ000-211400-

    Mesoscale Precipitation Discussion 0153
    NWS Weather Prediction Center College Park MD
    552 AM EDT Mon Apr 21 2025

    Areas affected...southeast Texas, far southwest Louisiana

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 210950Z - 211400Z

    Summary...Local/spotty flash flood potential should continue for
    at least another 2-3 hours.

    Discussion...Convection continues to fire along an 850mb
    confluence axis extending from north-central Louisiana through
    southeast Texas. Along and ahead of this confluence axis, 1000
    J/kg MLCAPE and 1.7 inch PW values were combining with favorable
    kinematics for slow-moving storms with locally extreme rain rates.
    In fact, MRMS estimates approximately 6.5 inches of rain in
    southern Tyler County over the past 3 hours. Nearby convection
    has also produced 1-2 inch/hr rain rates at times. Recent radar
    mosaic imagery also depicts an uptick in weaker convection from
    Tyler County westward and southwestward through Colorado County,
    suggestive of a continued flash flood threat in these areas over
    at least the next 2-3 hours.

    Convective coverage becomes a bit less certain after 13Z or so.=20
    Although confluence will remain in place across the discussion
    area through that time, RAP/SPC Mesoanalyses depict
    weakening/slackening 850mb flow east of the confluence zone that
    could cause existing updrafts to struggle against conditional
    instability aloft. The timing of this scenario is a bit
    uncertain, however, and recent CAMs maintain convection across the
    discussion area (perhaps propagating and/or developing toward
    coastal areas) through at least 15-16Z or so. This area will be
    re-evaluated for any continuing flash flood potential (and another
    MPD) after ~13-14Z or so.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8RJo606zd1WMJtEDznN4AR8V65bPUpR3N7_K2A6-J_IjRzYSPsetddO13LsdWa3tKqDf= uRoXyBEla7OZeNXFq18V7EQ$ for graphic product...

    ATTN...WFO...HGX...LCH...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 31669341 31289269 30569280 29899379 29159515=20
    28739615 29059666 29829618 30479560 31419444=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Apr 21 14:01:10 2025
    AWUS01 KWNH 211401
    FFGMPD
    TXZ000-211900-

    Mesoscale Precipitation Discussion 0154
    NWS Weather Prediction Center College Park MD
    1000 AM EDT Mon Apr 21 2025

    Areas affected...Coastal Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 211358Z - 211900Z

    Summary...Showers and thunderstorms will continue through early
    afternoon across the Upper and Middle Texas Coasts. Rainfall rates
    in excess of 1"/hr mcould reach 3"/hr at times, leading to
    rainfall of 2-3" with locally up to 5". This may cause instances
    of flash flooding.

    Discussion...The regional radar mosaic this morning shows a line
    of showers and thunderstorms extending from near Corpus Christi,
    TX northeast towards Beaumont, TX. This convection is blossoming
    along a slow moving cold front analyzed by WPC which will continue
    to sag very slowly southward towards the Gulf Coast through the
    aftn. Rainfall rates this morning have already been estimated via
    local radars of 2-3"/hr, resulting in 3-5" of rain in a few areas
    in the vicinity of Houston, and these scattered intense rates are
    likely to continue through the aftn.

    As the front sags southward, it will encounter weak but onshore
    850mb flow of 10-15 kts. While this is modest, it will be
    sufficient in the presence of PWs that are 1.6 to 1.7 inches,
    above the 90th percentile according to the SPC sounding
    climatology, to produce intense moisture advection and convergence
    into the boundary. This will combine with the approach of the LFQ
    of a subtropical jet streak extending across northern Mexico to
    enhance ascent, and the simulated radar from the morning CAMs
    suggest storms will persist for many more hours. As instability
    climbs to 2000-3000 J/kg later today, the organization of
    convection may become more diffuse, but still widespread enough
    that mean cloud layer winds from SW to NE will result in short
    duration training. With HREF 2"/hr probabilities peaking above
    40%, and the HRRR 15-min accumulated precipitation fields
    indicating short-duration rain rates above 3"/hr possible, this
    could cause 2-3" of rain with locally higher amounts as much as 5"
    into the aftn.

    Soils across the region are generally drier than normal according
    to the NASA SPoRT 0-40cm soil moisture anomalies, and this is
    reflected by both 1-hr and 3-hr FFG that are generally 3-4 inches.
    Despite that elevated FFG, the HREF indicates a 10-30% chance of
    exceedance. This suggests at least an isolated flash flood risk,
    but the greatest potential will be where any slow moving storms
    can train or linger across urban areas where infiltration capacity
    is lower.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9nrl5y5qCVdpT6p-Pt2fvcmz3jaTMBr23716sfzWqAHXpnlHmuUjG7f2OoIHI5LcqKTz= bTDXgkXuuC6B57uLE_5XUFc$ for graphic product...

    ATTN...WFO...CRP...HGX...LCH...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 30839475 30829407 30359376 29789402 29449468=20
    28979541 28599606 28209661 27879695 27529725=20
    27269743 27309773 27739780 28739691 30359540=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Apr 21 21:09:45 2025
    AWUS01 KWNH 212109
    FFGMPD
    MSZ000-LAZ000-220110-

    Mesoscale Precipitation Discussion 0155
    NWS Weather Prediction Center College Park MD
    508 PM EDT Mon Apr 21 2025

    Areas affected...southern MS into southeastern LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 212107Z - 220110Z

    Summary...Training/backbuilding cells will continue a flash flood
    threat for portions of southeastern LA into southern MS through
    01Z. Localized high rainfall rates in excess of 3 in/hr will be
    possible.

    Discussion...Visible satellite and regional radar imagery at 2045Z
    showed scattered thunderstorms extending from south-central MS
    into southeastern LA, with low level moisture feeding an unstable
    (1000-2000 J/kg MLCAPE) and moist (1.5 to 1.7 inch PWATs) airmass
    into the region via southerly 10-15 kt 925-850 mb winds. Given
    similarly oriented and slightly weaker deeper layer steering flow,
    elements of training and backbuilding have been observed near
    downtown New Orleans and the I-10 corridor to the west. Several
    reports of rainfall rates exceeding 1 inch in 15 minutes and 3
    inches per hour have been observed in this area of LA.

    Aloft, initiation was augmented by lift ahead of a subtle
    shortwave aloft over the western Gulf and an upper level jet max
    crossing northern Mexico and southern TX, with divergence and
    diffluence focused over the lower MS Valley. Similar broader scale
    flow and ascent will remain in place over the next few hours with
    continued potential for training/backbuilding existing across a
    wider region than just the New Orleans metro, though coverage of
    very high rainfall rates may be limited in scope.

    While flash flooding is ongoing across portions of southeastern
    LA, some uncertainty exists with the longevity of cells over the
    New Orleans metro given the potential for exhausting of
    instability. The development of additional flash flood producing
    rainfall across other locations is also a bit uncertain. While the
    setup favors rainfall rates over 3 in/hr expanding to the west and
    north of New Orleans, high flash flood guidance of 3 to 4+ inches
    per hour is in place for southern portions of the lower MS Valley
    so any additional flash flooding may be limited to urban locations
    where infiltration of water will be slowed.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8G6OZzvNq_ldcFlbDDjLfH4OGZv-aEDF8ByEBpIae-8YgYwJz-7j091BHtc47XqD7DcW= 4Bq_34cWEAIsE-a7Fjgu76A$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MOB...

    ATTN...RFC...LMRFC...NWC...

    LAT...LON 32959013 32958936 32668890 31998885 30738906=20
    29918927 29439021 29599150 29899210 30629233=20
    31419172 32239112=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Apr 22 00:11:58 2025
    AWUS01 KWNH 220011
    FFGMPD
    ALZ000-MSZ000-LAZ000-220530-

    Mesoscale Precipitation Discussion 0156
    NWS Weather Prediction Center College Park MD
    810 PM EDT Mon Apr 21 2025

    Areas affected...northeastern LA into central MS/AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 220009Z - 220530Z

    SUMMARY...Isolated flash flooding will be possible over the next
    3-5 hours from northeastern LA into central MS and central AL.
    Potential will exist for training and rainfall rates of 2-3 in/hr
    with totals up to 5 inches, although coverage of these higher
    rainfall totals should be quite limited if they do occur.

    DISCUSSION...Scattered to numerous thunderstorms were ongoing from
    the central LA/MS border into central MS and western AL at 00Z,
    near and south of a quasi-stationary front. SPC mesoanalysis data
    from 23Z showed MLCAPE across the region was 1000-1500 J/kg with
    1.5 to 1.8 inches of precipitable water. Water vapor imagery
    showed a shortwave over northern LA, beginning to advance
    northeastward into MS, and recent cooling of cloud tops near
    Natchez, MS may be a result of ascent ahead of the advancing
    shortwave.

    Farther east, existing convection along the MS/AL border has
    produced a rain-cooled boundary within the warm sector of the
    stationary front and subtle enhancement of 925-850 mb winds ahead
    of the shortwave are forecast through 03Z which should support
    increased overrunning of the front and rain-cooled outflow
    boundary. Per radar imagery, mean storm motions were off toward
    the northeast at 10 to 20 kt (locally higher), quasi-parallel to
    initiating boundaries which could promote some training and brief
    backbuilding of storms over the next few hours. Favorably
    diffluent flow aloft was, and will continue to be, in place within
    the broad left-exit region of a jet max positioned over
    south-central TX, which should aid with lift across the lower MS
    Valley and just downstream.

    While the environment is moist, diurnal cooling and convective
    overturning will contribute to some loss in instability overnight,
    which means coverage of convection may be near its max at the
    present time across the broader LA/MS?AL region. Nonetheless, some
    flash flood threat will continue into the first half of the
    overnight with rates of 2-3 in/hr easily attainable within the
    favorable environment with potential for additional development.
    However, limited coverage of these higher rates and generally high
    flash flood guidance for the region should limit the areal extent
    of any flash flooding that might develop.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-2JeLoNx706_syp8m3NMuRmrtoFgkj1r70crNPp-wAC4r7VpCeruDXQi5Cy68u-7Gj4G= 71LaZa1oTNAnsR-m16lWLkA$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LCH...LIX...MEG...MOB...SHV...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34028735 33748629 32798640 31858799 31458898=20
    30729009 30769152 31229190 31999192 32839120=20
    33508968=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Apr 22 11:59:14 2025
    AWUS01 KWNH 221159
    FFGMPD
    TNZ000-ALZ000-MSZ000-221800-

    Mesoscale Precipitation Discussion 0157
    NWS Weather Prediction Center College Park MD
    758 AM EDT Tue Apr 22 2025

    Areas affected...portions of north-central AL and northeast MS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 221200Z - 221800Z

    Summary...Additional scattered totals of 2-4" are likely and may
    overlap accumulations of 2-3" from early this morning/overnight.
    Isolated to scattered instances of flash flooding are possible.

    Discussion...Convection has been percolating over the past several
    hours over northwestern AL into far northeast MS, in the vicinity
    of a weak, stalling surface front and low pressure. While not
    overly impressive synoptically, a weak shortwave aloft is noted
    with an associated 50-60 kt (mini) jet streak, providing just
    enough divergence aloft to support sustained convection (with 0-6
    km shear of only about ~20 kts). Meanwhile, the low-levels are
    becoming increasingly supportive of sustaining convection as well,
    as weak 925-850 mb moisture transport has prevented convection
    from becoming outflow dominate with 3-hr change in ML CAPE of
    50-150 J/kg (resulting in current ML CAPE of 250-750 J/kg).
    Precipitable water of 1.5" (above the 90th percentile, per BMX
    sounding climatology) has supported occasional rainfall rates to
    1.0-1.5"/hr (per MRMS estimates, as the peak rainfall rates have
    occurred in observation sparse areas).

    Going forward, there's a good chance that some of the recent
    trends of backbuilding convection will continue, as upwind
    propagation vectors in the vicinity of the convection are 5 kts or
    less (taking into account the mean storm flow and opposite flow of
    the 850 mb jet). In addition, storm motions are also relatively
    slow (10-15 kts), so the combination of backbuilding and
    appreciable individual cell residence time may occasionally
    support hourly rates/totals on the order of 2-3"/hr. Overall the
    00z/06z CAMs are struggling with the depiction of convection in
    the region, though the 00z FV3 is an outlier in depicting 2-4"
    totals through 15-18z (though this may be displaced too far
    south). More recent HRRR runs (since 06z) are doing a better job
    depicting convection in the correct location, though still
    probably a bit too weak given the trends (only showing highly
    isolated totals of 2"+). Thinking additional scattered totals of
    2-4" are likely through 18z, and much of this could occur over
    areas that have already seen 2-3" this morning. Given that the
    realization of any flash flooding is dependent on localized
    training of convection with overall weak forcing and relatively
    high uncertainty, isolated to scattered flash flooding is
    considered possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!97Lv8b8STAMVV_JHxr01esYhoO9LORUL1A8q8z52-EZzkGZOXizU2p6BlJVGlNy2Wc8d= AbwTHczKTG5GoT7HJFE34Mo$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...MEG...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 35158589 34028607 33268695 32578762 32408843=20
    32518937 33068950 33568943 34238915 34708760=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Apr 22 22:22:58 2025
    AWUS01 KWNH 222222
    FFGMPD
    ALZ000-MSZ000-LAZ000-TXZ000-230300-

    Mesoscale Precipitation Discussion 0158
    NWS Weather Prediction Center College Park MD
    621 PM EDT Tue Apr 22 2025

    Areas affected...Southern LA...Southern MS...West central AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 222221Z - 230300Z

    Summary...Scattered to numerous slow moving thunderstorms, some
    with rainfall rates exceeding two inches per hour, are likely to
    continue through the evening hours. Some instances of flash
    flooding will be possible where cells become most persistent.

    Discussion...Convection continues to develop and persist south of
    a weak, stalling surface front and wave of low pressure. Regional
    Doppler radars are indicating multi-cellular clusters with some
    back-building convection, with the most impressive radar
    signatures just north of the Interstate 10 corridor in
    south-central Louisiana, and a second area slow dropping south
    near the MS/AL border. Enhanced-V signatures on GOES visible and
    infrared satellite is also apparent, and thus evidence that these
    cells are becoming anchored in place for an hour or more in some
    cases. MRMS rainfall estimates of 2+ inches per hour have been
    observed, and although flash flood guidance values are generally
    high across most of the outlook area, this could be enough to
    cause some flooding issues in poor drainage and urban areas.

    The latest CAM guidance suite generally agrees on the idea of
    scattered QPF maxima of 2-4 inches through 10 pm local time, with
    most of this falling within a two-hour time period in any given
    location. HREF exceedance probabilities of flash flood guidance
    are relatively low, but probably higher in reality given what is
    currently happening. Once these multi-cell clusters become more
    outflow dominant later this evening, the flooding threat with
    these cells should diminish.

    Hamrick

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9VJorr0aPCRxno_U1sseDK1brsJ-HQX-GiSAGx8bN17zlE1GOXMLggLkdlYIlUeNmNip= bC1oKRAgskMQKrv9Tq49cPE$ for graphic product...

    ATTN...WFO...BMX...JAN...LCH...LIX...MOB...SHV...

    ATTN...RFC...LMRFC...SERFC...WGRFC...NWC...

    LAT...LON 33228908 33228842 32648804 31418847 30768898=20
    30518954 30469060 30209165 30189221 30369306=20
    30969371 31529342 31779267 31849210 31879112=20
    32239035 32718970=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 23 02:29:20 2025
    AWUS01 KWNH 230228
    FFGMPD
    TXZ000-OKZ000-KSZ000-230700-

    Mesoscale Precipitation Discussion 0159
    NWS Weather Prediction Center College Park MD
    1027 PM EDT Tue Apr 22 2025

    Areas affected...Northwest TX...Western OK

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 230227Z - 230700Z

    SUMMARY...Slow moving thunderstorms are expected to persist over
    southern portions of the Texas Panhandle and extending to
    west-central Oklahoma through 7Z tonight. Cell mergers and cell
    training may lead to some instances of flooding.

    DISCUSSION...Regional Doppler radars continue to indicate both
    supercells and multi-cell clusters that have had a history of
    heavy rainfall over the past few hours that have developed ahead
    of the dry line. In addition, GOES-16 infrared satellite imagery
    shows expanding cold anvil canopies with the convective complexes,
    especially so with the MCS over the southern Texas Panhandle where
    the flash flood threat is greatest over the next several hours.
    Rainfall rates with the strongest and most persistent convection
    will likely exceed two inches per hour at times, increasing the
    threat of flash flooding in those areas.

    The latest CAM guidance suite is likely a little undergone with
    forecast QPF totals through 7Z, although the FV3 is on the higher
    end of the guidance. There will likely be some 2-4 inch totals on
    a localized basis, with much of this falling in a two hour time
    period for any given location. This activity is expected to
    gradually become more progressive as the MCS matures and moves
    eastward.

    Hamrick

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!69fkd65H5_vuI8g3O56S8XNSq9PA_mz6PWWQ5zIAmVdlIOF5vlVLy9QGF6JCR7DPkYaF= GGrT-RlbgKhvQABe-i1pfUI$ for graphic product...

    ATTN...WFO...AMA...DDC...LUB...MAF...OUN...SJT...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 37149929 36899837 36109799 35009821 34109857=20
    33529909 33009981 32590098 32530215 32840277=20
    33240300 33900300 34420263 35010172 35740079=20
    36660004=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 23 06:29:23 2025
    AWUS01 KWNH 230627
    FFGMPD
    TXZ000-231100-

    Mesoscale Precipitation Discussion 0160
    NWS Weather Prediction Center College Park MD
    227 AM EDT Wed Apr 23 2025

    Areas affected...portions of central Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 230626Z - 231100Z

    Summary...An eastward-moving convective complex is spreading
    0.5-1.5 inch/hr rain rates across the Texas Hill Country
    currently. On its present track, this complex could reach the
    Austin/San Antonio Metropolitan Corridor and pose a risk of
    isolated, urban flash flooding in the next couple hours or so
    (through 09Z/4am CDT).

    Discussion...Convection across southwest Texas and the Hill
    Country has managed to grow upscale into an eastward-moving
    complex, with persistence well beyond that indicated by most prior
    model guidance. This complex is being maintained by considerable
    mid-level organization and a mature cold pool that continues to
    propagate into a gradually more moist and unstable downstream
    airmass (1.5 inch PW, 2000 J/kg MLCAPE). The complex is currently
    on the eastern edge of stronger low-level flow/shear, which lends
    some uncertainty with regard to eastward persistence. However,
    recent NAM/RAP low-level wind fields are progged to increase
    modestly across the discussion area through 09Z. This, combined
    with weak convective inhibition downstream suggests that heavier
    downpours could make it into the Austin/San Antonio Metropolitan
    Corridor by around 09Z/4am CDT or so.

    If this complex can hold together, areas of 1-1.5 inch/hr rain
    rates should affect urbanized areas and pose an isolated risk of
    flash flooding. This risk should mainly focus around urbanized
    and low-lying/sensitive locations, as nearby FFGs/soil moisture
    profiles indicate less-sensitive ground conditions especially east
    of the Austin/San Antonio areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!92bSGB7MsIfxlXOfhH7K6Y9G6z_R8kOec2n6d8bMxoyOtgXuGgmZ5RstDwY6PQgqUnrd= lYOROYJD2PDiQJfsl6EfNks$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...SJT...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 31239839 31089742 30189660 29279677 28809790=20
    29190010 29760095 31129922=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 23 17:43:36 2025
    AWUS01 KWNH 231743
    FFGMPD
    NCZ000-SCZ000-232341-

    Mesoscale Precipitation Discussion 0161
    NWS Weather Prediction Center College Park MD
    143 PM EDT Wed Apr 23 2025

    Areas affected...southeast NC & northeast SC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 231741Z - 232341Z

    Summary...Organized thunderstorms are forming across southeast NC
    and coastal SC with some showing signs of backbuilding/limited
    movement. Hourly rain totals to 2" with local amounts to 4" are
    possible, which would be problematic in urban areas.

    Discussion...A frontal boundary lies across the region, oriented
    east-northeast to west-southwest, with a weak/elongated wave near
    Lake Waccanaw NC, which has shifted southwestward since 12-15z
    based on surface observations. Precipitable water values are
    ~1.3-1.4". ML CAPE across the region appears to be drifting
    southwest, with values of 500-1500 J/kg on both sides of the
    front, which should increase another 500 J/kg or so this
    afternoon. Effective bulk shear of 25-35 kts is organizing the
    storms.

    The 12z HREF indicates that the heavy rain threat increases
    through the afternoon, with the highest rain rates shifting
    southwest with time, which fits recent trends in the ML CAPE pool
    and RAP mass fields regarding the weak frontal wave's expected
    future movement. Recent backbuilding on radar is expected to
    continue over the next several hours. Hourly rain totals should
    maximize in the 2" range, with local amounts to 4" possible. The
    guidance shows a reasonable signal for heavy rain in this region,
    with a similar signal. Soils are sandy in this region, which when
    combined with minimal rainfall over the past couple of weeks has
    led to high flash flood guidance values. Any issues are expected
    to be urban, given the expected hourly and overall totals.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4T_ajSQ1-VUK47W6_KDMX7BqVWldPLCAWJitNzA6kPicZs7cPMRFv42WDBh4JcbLmqW0= aFi2yZa1CRLNB6Xw4Ok6eIM$ for graphic product...

    ATTN...WFO...CAE...CHS...ILM...MHX...RAH...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 34977727 34687693 34307759 33797790 33807835=20
    33687873 33107917 33127980 33988006 34647916=20
    34887820=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 23 18:42:08 2025
    AWUS01 KWNH 231842
    FFGMPD
    ALZ000-MSZ000-LAZ000-ARZ000-TXZ000-OKZ000-240100-

    Mesoscale Precipitation Discussion 0162
    NWS Weather Prediction Center College Park MD
    241 PM EDT Wed Apr 23 2025

    Areas affected...Ark-La-Tex and East TX through southern and
    central MS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 231900Z - 240100Z

    Summary...Increasing convective coverage through the late
    afternoon and evening with relatively slow storm motions will
    result in widely scattered hourly totals of 1-2". Localized
    repeating of efficient rainfall rates may result in 3-6 hour
    totals as high as 3-5" (highest chances in the vicinity of the
    MS/LA border region). Isolated/localized flash flooding is
    possible.

    Discussion...Diurnally driven showers and thunderstorms are
    increasing in coverage (once again) this afternoon across a
    relatively weakly forced, moderately unstable and moist
    environment from the Ark-La-Tex through southern and central MS.
    One cluster of scattered to numerous is occurring across portions
    of southern MS and southeast LA, while another is occurring closer
    to the Ark-La-Tex. Most storms have been relatively shallow thus
    far (due to some capping between 850-600 mb), but updrafts in the
    vicinity of the MS/LA border have begun to reach the LFC in the
    past hour or two. Meanwhile, cloud cover associated with remnant
    MCVs (from overnight convection across TX) has moved into the
    Ark-La-Tex and points south, which has largely suppressed deeper
    updrafts (so far). DPVA in association with these MCVs may help to
    eventually organized convection (along with associated remnant
    upper-level divergence associated with the MCVs, as well as being
    on the periphery of modest divergence in association with the left
    exit region of a subtropical jet streak near the TX and Mexico
    border). The commonality between both areas is relatively weak
    southerly low-level flow (primarily guiding storm motions) with
    925-850 mb winds between 10-20 kts (and upwind propagation vectors
    as weak as 5 kts, generally towards the southeast). In addition,
    PWATs generally range from 1.3-1.7 inches (near 90th percentile)
    with ML CAPE of 1000-2000 J/kg. Slower storm motions with the
    potential for localized backbuilding, outflow boundary collisions,
    and cell mergers should present the potential for localized
    repeating of 1-2" rainfall rates/hourly totals.

    While individual CAMs (including the 12z HREF, 06z RRFSe, and
    hourly HRRR/RRFS) all seem to depict varying degrees of randomized
    scattered coverage of highly localized 2-5" totals, some
    interesting tidbits can be gleaned from the post-processed
    statistical output. Both ensemble suites depict high odds (40-80%)
    for localized 2" exceedance (per 40-km neighborhood method) and
    medium odds (20-50%) for localized 3" exceedance. While 2"
    exceedance probs are widespread across the region, there is
    distinct clustering in the vicinity of the MS/LA border region for
    3" exceedance probs (with the HREF lagging the RRFSe for the
    relevant time frame, indicating 21z-03z peak vs. 18z-00z peak).
    While 3-6 hour FFGs typically range from 3.0-5.0", prior days
    rainfall has resulted in localized sensitivities with FFGs as low
    as 2.0-3.0". Isolated/localized flash flooding is possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7leZU0rL5bUXzXVrRLZEWZWLOkWRkmhmOtL6qeUB42OpL-fUK9HRMGJAAxnOjLZPWZZs= KtXnvOF4DGd8y1Xh8SB3mVI$ for graphic product...

    ATTN...WFO...BMX...FWD...HGX...JAN...LCH...LIX...LZK...MOB...
    SHV...

    ATTN...RFC...ABRFC...LMRFC...SERFC...WGRFC...NWC...

    LAT...LON 33919418 33849314 33779211 33529139 33649055=20
    33638952 33288826 32258830 31098873 30588987=20
    30369082 30119156 30149201 30589314 30169409=20
    31129511 31949546 32549618 33399584 33729488=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 23 18:46:05 2025
    AWUS01 KWNH 231845
    FFGMPD
    MOZ000-KSZ000-NEZ000-240044-

    Mesoscale Precipitation Discussion 0163
    NWS Weather Prediction Center College Park MD
    245 PM EDT Wed Apr 23 2025

    Areas affected...northeast KS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 231844Z - 240044Z

    Summary...Showers and thunderstorms are increasing in coverage and
    intensity across northeast KS. Hourly rain totals to 1.75" and
    local overall totals to 4" are possible over the next several
    hours, which would challenge modest flash flood guidance values.

    Discussion...ML CAPE has been increasing while CIN has been
    increasing across eastern KS, which is leading to a convective
    uptick across northeast KS in the vicinity of a front.=20
    Precipitable water values are near 1", and ML CAPE has risen to
    just over 2000 J/kg. Effective bulk shear remains under 25 kts,
    at the moment. There have been signs of backbuilding and cell
    mergers north of Randolph KS as of late, and the convective
    pattern is slowly growing.

    The mesoscale guidance suggests two pulses of activity -- one
    early, which is ongoing near the mesoscale warm front, and one
    later on toward the end of the MPD period which appears to be
    caused by convection along the mesoscale cold front which edges
    eastward. Inflow at 850 hPa is forecast to increase, which should
    lead to effective bulk shear increasing to 25+ kts and increasing
    convective organization with time. Assuming some hail
    contamination, hourly rain totals to 1.75" are ongoing due to
    backbuilding and cell mergers, and there's no reason to expect
    that to change much over the next several hours. This leads to
    the idea that the mesoscale guidance is too low on overall
    rainfall amounts. Moistening of the atmosphere locally should
    raise the precipitable water values above 1.25". Overall rain
    totals should maximize around 3-4", which would challenge the
    modest flash flood guidance values in the area. Any flash
    flooding would be isolated to widely scattered.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-zVn48V_Ux1xp2tktEU9p1x7YqeA_W6d5MkCMNybACj-kO4xHxkLdHQVGhX7ncAStcnr= B8gousFspoCTrolmajQHmv4$ for graphic product...

    ATTN...WFO...EAX...GID...ICT...OAX...TOP...

    ATTN...RFC...ABRFC...MBRFC...NWC...

    LAT...LON 40109594 39789510 39139510 38579664 38599781=20
    39289783 40069758=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 23 19:29:11 2025
    AWUS01 KWNH 231929
    FFGMPD
    SCZ000-GAZ000-240127-

    Mesoscale Precipitation Discussion 0164
    NWS Weather Prediction Center College Park MD
    328 PM EDT Wed Apr 23 2025

    Areas affected...portions of eastern GA and southern SC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 231927Z - 240127Z

    Summary...Thunderstorms with heavy rainfall have formed across
    portions of eastern GA and southern SC. Hourly rain totals to 2"
    with overall totals to 5" are possible.

    Discussion...An effective front is helping to foster increasing
    convection from eastern GA across southern SC near and east of a
    weak wave. Precipitable water values of 1.3-1.4" lurk in this
    region, as well as ML CAPE of 1000-2000 J/kg and effective bulk
    shear of ~30 kts. Water vapor imagery appears to show the region
    at the base of a mid-level shortwave moving through the southern
    Appalachians. Radar imagery shows hourly rain totals near 2" as
    of late due to either cell mergers or backbuilding, which should
    be the maximum expected in this environment. The highest local
    overall total has been in the 5" range, which is also the maximum
    expected.=20

    The 18z RAP shows increasing convergence along the boundary,
    particularly in southeast GA, over the next couple hours while the
    weak wave recedes to the west-southwest. The 12z HREF shows the
    potential of heavy rainfall in this area for the next five hours.=20 Thereafter, CIN should develop after sunset and help shut down
    convection. Until then, hourly totals to 2" and overall totals to
    5" are anticipated. Flash flood guidance values are high as there
    hasn't been much rainfall over the past week or two. Any flash
    flood issues that arise are expected to be in urban areas.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!67DyTSWjLVaGHv2l3q3H4RIF0RaL4BmwhQF9cT0_01ySvIyFSCKFziBhfN60nuPyyvKm= r5_jCqrVdI0y3FPpMgcWMso$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 33738123 33668043 32987959 32038095 32358231=20
    32698297 33128336 33448294 33678205=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 23 22:07:35 2025
    AWUS01 KWNH 232207
    FFGMPD
    OKZ000-KSZ000-COZ000-240406-

    Mesoscale Precipitation Discussion 0165
    NWS Weather Prediction Center College Park MD
    607 PM EDT Wed Apr 23 2025

    Areas affected...portions of western KS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 232206Z - 240406Z

    Summary...Thunderstorms are increasing in coverage in and near
    western KS. Hourly rain amounts to 1.75" with local totals to 4"
    are possible.

    Discussion...The atmosphere in western KS is warming and becoming
    uncapped (decreasing CIN) this afternoon as warm air advects in
    from the south and southwest within the southern and southeast
    quadrant of a retrograding circulation apparent on radar imagery
    just southwest of Goodland KS. Precipitable water values are
    0.91" per Goodland's 21z sounding, moist for the High Plains. ML
    CAPE of 1500-2500 J/kg lies across the region. Effective bulk
    shear is 25-40 kts, which is enough to organize convection
    linearly in a confluent way from the southwest.

    Expectations are for increasing coverage for the next few hours
    before activity attempts to accelerate east to northeastward. The
    mesoscale guidance has been showing upward trends in their QPF
    since 12z across this region. Interestingly, the mesoscale warm
    front in western KS isn't expected to make much additional headway
    northward, per recent RAP guidance, though ML CAPE does overrun it
    some distance to the north. Hourly rain amounts to 1.75" with
    local totals to 4" appear possible where cells train or merge or
    where occasional mesocyclones form and try to align. There's a
    wide range in the flash flood values across western KS, though the
    area has been dry the past couple of weeks. Any flash flooding is
    more likely to be in urban areas.=20=20

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7kstM5zEixMFgkbLcggjGsbUwC5upH5jYdIme9AJE3K1DonxdqP3mTGtgN9AaIKlotGj= NRtXBEMGSP1gCgJUJu_m7OY$ for graphic product...

    ATTN...WFO...AMA...DDC...GID...GLD...PUB...

    ATTN...RFC...ABRFC...MBRFC...NWC...

    LAT...LON 39870111 39629940 37769975 36880117 36800291=20
    38110314 38840244=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 23 23:56:01 2025
    AWUS01 KWNH 232355
    FFGMPD
    MSZ000-LAZ000-ARZ000-240454-

    Mesoscale Precipitation Discussion 0166
    NWS Weather Prediction Center College Park MD
    755 PM EDT Wed Apr 23 2025

    Areas affected...in and near portions of western & northern MS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 232354Z - 240454Z

    Summary...Thunderstorms with some level of organization should
    persist in and near portions of western and northern MS in the
    short term. Hourly rain amounts up to 2.5" with local amounts to
    5" are possible until thunderstorms fade this evening/tonight.

    Discussion...The mesoscale pattern in and near MS is chaotic, with
    a grand boundary collision coming shortly as the outflow
    boundaries from the cold pools near the LA/AR border, southwest
    TN, and eastern MS meet near the lower portion of the MS River
    Valley. Upstream, a strong shortwave is moving by the ArkLaTex,
    eastward into the region enhancing upper level divergence.=20
    Precipitable water values are 1.25-1.5". ML CAPE is 1000-2000
    J/kg, but CIN has set in near the LA/AR border and the central
    MS/AL border where temperatures have fallen below 70F. Effective
    bulk shear is around 25 kts, allowing some storms to attain some
    level of organization, but there are a lot of cell mergers
    apparent in recent radar imagery. Recent hourly rain amounts have
    been up to 2.5" in several spots near the MS/LA border as well as
    near Tchula MS.

    While there are some location differences between the 18z HREF and
    12z RRFS probabilities of 0.5"+ of rain in an hour, they point to
    the region of highest instability between the various outflow
    boundaries. After 00z, there should be a slow waning in coverage
    of the heavy rainfall, due to both increasing CIN and decreasing
    ML CAPE in and near western and northern MS after all the outflow
    boundaries collide and the atmosphere stabilizes. Until then,
    hourly rain amounts to 2.5" with local totals to 5" remain
    possible, which could exceed flash flood guidance values and be
    most problematic in urban areas.

    Roth=20

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!77SPtgatE5YpErfP9df76jPRGvSCGpLK5E782E-SN-PU1J1HGztd_NvgbyTuVl_itvlf= OJA8XCyMIVejpfdL-nzLGa0$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MEG...SHV...

    ATTN...RFC...LMRFC...NWC...

    LAT...LON 34578912 33718927 33168965 32479048 31869051=20
    30869034 30469124 31049186 31679261 32299220=20
    33079141 33509102=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Apr 24 09:16:22 2025
    AWUS01 KWNH 240914
    FFGMPD
    LAZ000-241400-

    Mesoscale Precipitation Discussion 0167
    NWS Weather Prediction Center College Park MD
    514 AM EDT Thu Apr 24 2025

    Areas affected...south-central LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 240912Z - 241400Z

    Summary...Slow moving showers and thunderstorms will pose an
    isolated flash flood threat to portions of south-central LA over
    the next 3-5 hours. Slow cell movement with potential for 2 to 3+
    in/hr rates will exist.

    Discussion...Local radar imagery from KPOE and neighboring sites
    showed a relatively small and largely warm-topped cluster of
    showers and thunderstorms over south-central LA at 09Z. Rainfall
    over the past few hours over LA has produced an outflow boundary
    which extended 20-30 miles south of and roughly parallel to I-10
    from near Lake Charles to near Abbeville. Modest low level flow
    atop this boundary and low level speed convergence (seen via VAD
    wind plots at 925 mb and 850 mb) appeared to be contributing
    factors in the location of the cluster of heavy rain, factors not
    being modeled well by recent RAP runs. Enhanced divergence within
    the left-exit region of an upper level jet max over south-central
    TX into the western Gulf was also possibly aiding with lift across
    the region.

    While this cluster has been in place for several hours in some
    form, there are growing concerns for slowing of cell movement
    given recent radar trends. Continued overrunning of the
    rain-cooled boundary is expected to continue over the next 3-5
    hours with components of slow moving/backbuilding/training
    allowing for localized heavy rainfall to continue across
    south-central LA. The environment is forecast to remain mostly
    unchanged over the next 2-3 hours and additional potential for 2
    to 3+ in/hr rainfall rates will remain along with localized storm
    totals over 5 inches possible in a relatively short period of
    time. These high rainfall rates will be most concerning with any
    overlap of urban or other areas with poor drainage.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8xydkvqgJw6N_oHudG9lbPun5o1hx_Bigy_e9qfIKhxomhd60fAYnsXG48W7COMhWDuK= dEkuqQpXjdRhhYGoQzppQsA$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...

    ATTN...RFC...LMRFC...NWC...

    LAT...LON 30999214 30969128 30849089 30459061 29939068=20
    29779159 29919251 30219280 30699269=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Apr 24 10:15:08 2025
    AWUS01 KWNH 241014
    FFGMPD
    TXZ000-241500-

    Mesoscale Precipitation Discussion 0168
    NWS Weather Prediction Center College Park MD
    613 AM EDT Thu Apr 24 2025

    Areas affected...northwestern to west-central TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 241011Z - 241500Z

    Summary...Rainfall rates of 1 to 2 in/hr (locally higher) within
    areas of training could produce localized flash flooding from 2-4
    inches of rain through 15Z over northwestern to west-central TX.

    Discussion...The merging of two convective clusters across northwest/west-central TX may lead to localized flash flooding
    over the next 3-5 hours. Regional radar imagery at 0945Z showed a
    largely forward propagating linear convective line from
    west-central OK into west-central TX north of SWW. A second
    (smaller and weaker) convective line was observed to the south,
    over west-central TX from DYS to BBD. The western-most edges of
    both convective lines were in the process of merging just north of
    I-20 in the vicinity of DYS. 850 mb VAD winds showed 30 to 40 kt
    from the south at KSJT and KDYX, overrunning the outflow
    associated with the stronger, northern convective cluster with
    recent slowing along its western end.

    Mean steering flow was from the SSW to SW at 15-20 kt, and of
    similar orientation to the 850 mb flow across northwestern to
    west-central TX, allowing for short-term training. Expectations
    are for the northern complex to continue advancing toward the
    southeast, following short term Corfidi vector forecasts. The
    orientation of the two systems is expected to evolve like a
    zipper, with merging of the two outflows advancing a burst of
    convection from west to east. Merging and short term training will
    likely support rainfall rates of 1 to 2 in/hr (locally higher) and
    short term rainfall totals of 2-4 inches through 15Z and these
    rains may produce localized flash flooding. While an expected
    weakening of the low level jet through the remainder of the
    morning hours may allow for an overall weakening, modest
    diffluence aloft and lingering instability of ~1000 J/kg may allow
    for convective maintenance for at least another 2-4 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_SsciM_Ua-mjzwCWvKm7QpC7IlBo7CGMGRieLpcAISNLoo78aywX001glk6JVckde8-T= owgvJJVyHshXbg1uKSfOXUQ$ for graphic product...

    ATTN...WFO...FWD...LUB...OUN...SJT...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 33669858 33569779 33199732 32749713 32309745=20
    32119815 32109919 32390041 33030060 33409993=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Apr 24 14:01:12 2025
    AWUS01 KWNH 241401
    FFGMPD
    LAZ000-241800-

    Mesoscale Precipitation Discussion 0169
    NWS Weather Prediction Center College Park MD
    1000 AM EDT Thu Apr 24 2025

    Areas affected...southeast LA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 241400Z - 241800Z

    Summary...Localized flash flooding likely to continue and possibly
    expand to localities farther east (including the New Orleans
    metro) with additional isolated totals of 3-5" possible.

    Discussion...A persistent cluster of thunderstorms from overnight
    has grown into a mini MCS this morning, though GOES-East infrared
    imagery indicates only sporadic cold cloud tops with a relatively
    unimpressive appearance. Radar imagery tells a much different
    story, as shallow updrafts have been incredibly persistent with
    relatively slow storm motions (KHDC VWP indicating 10-20 kt
    low-level flow), backbuilding along the southern and southwest
    flanks, and upwind propagation towards the southeast (into the
    low-level flow). With SPC's SFCOA analysis indicating PWATs of
    1.5-1.7 inches (near the 90th percentile, per LIX sounding
    climatology) and a reservoir of 500-1000 J/kg of ML CAPE directly
    to the south and southeast, there are concerns that this small
    convective complex will persist through the mid-morning to
    mid-day. Crucially, the influence of the left exit region of a
    subtropical jet streak (near 75 kts at 250 mb centered over South
    TX) is providing both 20-25 kts of effective bulk shear and
    enhanced upper-level difluence and lift. The persistence of the
    convection (with the aforementioned occasional cold cloud tops
    breaking through) suggests that the shear will continue to at
    least irregularly support deep convection, and this feedback loop
    allows for more rising motion and increased divergence aloft to
    support further new updrafts and initiation. Localized areas with
    the most efficient backbuilding and repeating of 1-3"/hr rainfall
    rates has resulted in estimated hourly totals of as much as 2-4"
    per MRMS (with KLFT recording back to back hours of 2.34" and
    2.41" of rainfall earlier this morning). Past 6-hour MRMS
    estimates indicate scattered totals of 3-6" (with some of the
    heaviest and largest areas in the vicinity of the Lafayette and
    Baton Rouge metro areas).

    Hi-res CAM suites from 00z failed to capture virtually any of this
    activity, though more recent hourly runs of the HRRR and RRFS have
    done a much better job initializing and persisting convection
    (with the RRFS notably catching on to this trend much earlier than
    the HRRR). Analyzing these most recent model runs (10z onward)
    going forward, the output QPF suggests the potential for
    additional 3-5" localized amounts. As detailed above, the
    short-term trends and current mesoscale environment supports these
    amounts, and the heaviest amounts should continue to shift towards
    the east with upwind propagation (potentially putting the New
    Orleans metro area into greater threat over the next several
    hours). Ongoing flash flooding (some significant and life
    threatening) is likely to continue, possibly spreading eastward to
    areas that have seen little to no rainfall thus far.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5N9wt-OBb_mHc8SOlveQ8_orqihjzyBNmMnvotN0YMlp3nwwm_S4HY4wVzVzxOFhjss1= eIM2-KxOG8zkn_QiXAtouDw$ for graphic product...

    ATTN...WFO...LCH...LIX...

    ATTN...RFC...LMRFC...NWC...

    LAT...LON 30989140 30879083 30709028 30388974 29808987=20
    29449035 29639090 29799159 29979225 30789197=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 25 18:40:39 2025
    AWUS01 KWNH 251839
    FFGMPD
    TNZ000-ALZ000-MSZ000-251840-

    Mesoscale Precipitation Discussion 0175
    NWS Weather Prediction Center College Park MD
    840 AM EDT Fri Apr 25 2025

    Areas affected...portions north-central MS into northwestern AL
    and Middle TN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 251240Z - 251840Z

    Summary...Intensifying thunderstorm activity will support 3-6 hour
    localized totals as high as 3-5" through midday. Isolated to
    scattered instances of flash flooding are possible.

    Discussion...A cluster of thunderstorms is becoming more intense
    and organized this morning over portions of the MS Delta,
    supported by a mid-level shortwave/trough and enhanced low-level
    convergence (southerlies from the Gulf and westerlies over the
    Ark-La-Tex). While the influence of the subtropical jet to the
    southwest is waning relative to the past few days, the
    aforementioned shortwave is providing ample diffluence aloft as
    the area is situated between the polar and subtropical jets. Per
    SPC's SFCOA analysis at 12z, the mesoscale environment is
    characterized by SB CAPE of 500-1500 J/kg over MS (with 500 J/kg
    or less over north AL and Middle TN, but anticipated to increase),
    PWATs of 1.4-1.8 inches (between the 90th percentile and max
    moving average, per JAN sounding climatology), and effective bulk
    shear near 20 kts. The combination of moderate instability, highly
    anomalous moisture, and sufficient bulk shear should continue to
    maintain relatively organized convection.

    Hi-res CAMs are in relatively good agreement with regard to
    expected localized amounts going forward, with both the 06z HREF
    and 00z REFS probability-matched mean QPF indicating localized
    totals as high as 2-3" (though the exact placement of these higher
    totals varies quite a bit, as evidenced by 06z HREF and 00z REFS
    Ensemble Agreement Scale 1" exceedance probabilities of 10% or
    less). More recent runs (since 06z) of the HRRR have been quite a
    bit more robust with QPF, indicating totals as high as 3-5"
    through 18z (and the latest observational trends are supportive of
    this, as convection is beginning to locally train from southwest
    to northeast over portions of the MS Delta with MRMS hourly
    estimates near 2.5"). With much of this QPF expected to fall in as
    little as a 3-hr period, associated FFGs generally range from
    1.5-3.0" (with 6-hr FFGs ranging from 3.0-5.0"). Isolated to
    scattered instances of flash flooding are possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4HV3v4pPP987NOVoFP8ZRSND8srVIJVosByvDaE5xv-cqIRjgNUL4e72jc_TVoCx-gUY= eQtrHTxNW75JIIpJ8tU3joI$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...MEG...OHX...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 35918727 35678623 34918587 33648730 32838905=20
    32829082 33449104 34069020 34408980 35308870=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 25 18:46:07 2025
    AWUS01 KWNH 251845
    FFGMPD
    ALZ000-MSZ000-LAZ000-260030-

    Mesoscale Precipitation Discussion 0176
    NWS Weather Prediction Center College Park MD
    245 PM EDT Fri Apr 25 2025

    Areas affected...Northeast LA...Southern MS...Southwest AL...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 251845Z - 260030Z

    SUMMARY...Clusters of slow moving thunderstorms in proximity to
    older MCV across E MS may result in multiple rounds of intense
    rainfall potentially resulting in widely scattered spots of 2-4"
    inches inducing possible focused flash flooding.

    DISCUSSION...Regional RADAR mosaic denotes an older mid-level MCV
    along the southwestern flank of the main upper-level trough
    exiting through the Lower Ohio Valley. The subtle outflow jet to
    the north continues to provide broad scale ascent to maintain the
    vorticity center. In the lower levels, this has resulted in solid moisture/instability advection across the central Gulf within
    solid WAA regime providing strong moisture flux convergence along
    and downstream of the MCV. Instability axis of 1000 J/kg across
    central AL increases toward 2000 J/kg (MLCAPE) across the I-10
    corridor from central LA toward southern AL providing solid
    additional buoyancy for broader overturning even upstream along
    the trailing southwest flank of the MCV/confluence axis. Deep
    layer moisture lags a bit to the west of the instability with
    1.5-1.7" total PWat Valleys but proximity and solid surface Tds
    values in the lower 70s to allow for efficient rainfall production
    for the cells. The combination should allow for rates of
    1.5-2"/hr.

    Cells in the warm sector of the wave will remain slow moving
    waiting for the upstream forcing/inflow may result in hour or so
    duration. Minus a small zone of reduced FFG across E MS north of
    Meridian, FFG values are likely not to be exceeded given totals of
    2-2.5" with the first round. However, given increasing density of
    coverage, potential for mergers and a secondary bout of similar
    intense rates may result in more scattered areas reaching 2-3.5"
    over a 3hr period and potentially result in localized incident or
    two of flash flooding.

    Further southwest across E LA/SW MS, winds are likely to respond
    with confluent veering as the MCV continues to press eastward.=20
    500-1000mb thickness suggestion some increased spread and
    therefore reduced propagation vectors toward the southeast though
    the late afternoon into evening hours. Additionally, any outflow
    boundary is more probable to orient NW to SE and be a bit more
    orthogonal to the veered low level flow resulting in some
    potential for back-building, though with weaker/weakening flow
    convergence may become more scattered in nature. Slower cell
    motions at the trailing edge, also suggest increased duration for
    spots of 2-4" here as well. Proximity to I-10 and urban locales
    that dot along it, further increase potential for possible
    incidents of flash flooding as well.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_vByYc_g22sQd655tAbs9W3PESykLNxpuPF20vxHQsOm4nUgJSvpBakwr-YnB74OMgyW= -YJ_syZ94oasKLzqI8HlXbQ$ for graphic product...

    ATTN...WFO...BMX...JAN...LIX...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 33578771 33268690 32528676 31868722 31248809=20
    30548963 30439051 30589140 31419153 31969013=20
    33028910 33448844=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 25 19:17:33 2025
    AWUS01 KWNH 251917
    FFGMPD
    GAZ000-TNZ000-ALZ000-252300-

    Mesoscale Precipitation Discussion 0177
    NWS Weather Prediction Center College Park MD
    316 PM EDT Fri Apr 25 2025

    Areas affected...portions of northern AL and southern Middle TN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 251910Z - 252300Z

    Summary...Thunderstorms initiating along a gust front with the
    potential for training with associated flash flood threat of 1-2"
    localized totals.

    Discussion...A gust front from earlier cells this morning has
    begun to initiate new convection, along a line from just west of
    Birmingham to Huntsville. The mesoscale environment along and out
    ahead of this line is characterized by ML CAPE 500-1000 J/kg,
    PWATs of 1.3-1.6 inches (near or above the 90th percentile, per
    BMX sounding climatology), and effective bulk shear of 15-20 kts.
    Hourly rainfall estimates (per MRMS) are already approaching an
    inch, and the 850-300 mb mean flow is nearly parallel to the line
    of developing storms. In addition, upwind propagation vectors
    suggest only limited forward propagation towards the east, which
    may increase residence time of training storms.

    Latest HRRR runs seem to be initializing the position of the gust
    front fairly well, and indicate 1-2" localized totals (through
    23z) along an apparent training axis. The 12z HREF suggests
    somewhat higher totals are possible, indicating 20-30% chances for
    localized 2" exceedance (per 40-km neighborhood exceedance
    probabilities). Lastly, the experimental RRFS and REFS depict
    similar solutions as well (with 2" exceedance probabilities from
    the 06z REFS also being 20-30%).

    Rainfall totals over the past 3 days across the region generally
    range from 1-3", and NASA SPoRT-LIS 0-1 m soil moisture indicates
    values above the 90th percentile for much of the area. These wet=20
    antecedent soil conditions suggest that localized instances of
    flash flooding are possible along this axis of storms.

    Churchill/Shieh

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-U_RLt0TnGx40yDrouEv__3XgG0OyHG4y6ATzKHaa8Djx9NmQmIm7XEUn79pclyXK4Uv= qvDCMHS8ntEzmj9HpSTYmq0$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...MRX...OHX...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 35578579 35078490 33808564 33118663 33118778=20
    33328794 33608767 34328716 34718697 35168678=20
    35458648=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 25 19:34:23 2025
    AWUS01 KWNH 251934
    FFGMPD
    GAZ000-TNZ000-ALZ000-252300-

    Mesoscale Precipitation Discussion 0177
    NWS Weather Prediction Center College Park MD
    316 PM EDT Fri Apr 25 2025

    Areas affected...portions of northern AL and southern Middle TN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 251910Z - 252300Z

    Summary...Thunderstorms initiating along a gust front with the
    potential for training with associated flash flood threat of 1-2"
    localized totals.

    Discussion...A gust front from earlier cells this morning has
    begun to initiate new convection, along a line from just west of
    Birmingham to Huntsville. The mesoscale environment along and out
    ahead of this line is characterized by ML CAPE 500-1000 J/kg,
    PWATs of 1.3-1.6 inches (near or above the 90th percentile, per
    BMX sounding climatology), and effective bulk shear of 15-20 kts.
    Hourly rainfall estimates (per MRMS) are already approaching an
    inch, and the 850-300 mb mean flow is nearly parallel to the line
    of developing storms. In addition, upwind propagation vectors
    suggest only limited forward propagation towards the east, which
    may increase residence time of training storms.

    Latest HRRR runs seem to be initializing the position of the gust
    front fairly well, and indicate 1-2" localized totals (through
    23z) along an apparent training axis. The 12z HREF suggests
    somewhat higher totals are possible, indicating 20-30% chances for
    localized 2" exceedance (per 40-km neighborhood exceedance
    probabilities). Lastly, the experimental RRFS and REFS depict
    similar solutions as well (with 2" exceedance probabilities from
    the 06z REFS also being 20-30%).

    Rainfall totals over the past 3 days across the region generally
    range from 1-3", and NASA SPoRT-LIS 0-1 m soil moisture indicates
    values above the 90th percentile for much of the area. These wet=20
    antecedent soil conditions suggest that localized instances of
    flash flooding are possible along this axis of storms.

    Churchill/Shieh

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8H0tZCjGAkuYGNcEepY6SJ4-Ho3-2yu_iHFrnMD-4vwvWr-UKKgqLCvvBCSuqJVAsSwd= VoESYXG1whgbf0debKwh5ls$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...MRX...OHX...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 35578579 35078490 33808564 33118663 33118778=20
    33328794 33608767 34328716 34718697 35168678=20
    35458648=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Apr 25 19:59:02 2025
    AWUS01 KWNH 251958
    FFGMPD
    PAZ000-WVZ000-OHZ000-260130-

    Mesoscale Precipitation Discussion 0178
    NWS Weather Prediction Center College Park MD
    358 PM EDT Fri Apr 25 2025

    Areas affected...Northern Ohio...Northwest Pennsylvania...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 252000Z - 260130Z

    SUMMARY...Unseasonable moisture allowing for shallow but efficient
    showers and thunderstorms with 1"/hr rates and potential for
    repeats and totals over 2", resulting in possible scattered flash
    flooding.

    DISCUSSION...CIRA LPW and RAP analysis shows strong warm conveyor
    belt extending along and ahead of broad large scale trof across
    the Mississippi Valley into Lower Ohio/Tennessee Valley.=20
    Southwesterly 850mb flow and core of 1.5" TPW noses northward
    across east-central IND into northern Ohio with increasing speed
    convergence as 30kts of 850mb flow reduce to 10-15kts across the
    area of concern. CIRA LPW percentile on the anomalous moisture
    denote a broad area of 95-99th in the surface to 850mb layer (Tds
    in the lower 60s) with a bit more focused 95-99th in the 850-700mb
    layer across northern OH. Filtered sunshine through broken cirrus
    has brought temperatures in the mid-70s resulting in increasing
    unstable environment with MLCAPE axis of 1000 J/kg along a similar
    west to east axis at the nose of the LLJ/speed convergence. As
    such, regional RADAR shows increasing convection, while
    overshooting tops/CBs below -60C are breaking out across northwest
    OH into north-central ahead of DPVA downstream of shortwave trough
    energy crossing central IL/IND attm.=20

    So, while instability is not extreme for broad updrafts, the
    overall coverage of these cores will increase into the afternoon.
    Combine this with orientation of the cores along the instability
    axis is fairly parallel to the deeper layer WSW to ENE steering
    and may support some scattered repeating of cells. Rates of
    1"+/hr are probable so localized totals of 2"+ in 1-3hrs may
    result in localized exceedance of FFG values which are generally
    1-1.5"/hr and <2"/3hrs across the area of concern. As such,
    scattered incidents of flash flooding is considered possible
    through the evening hours.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9R7uAVG39AqR_GgyzNHoocEpXj6N-mLrsgtVJEF9AZUKlLdQ_zutQBTkRo8879qjakSG= qGXJFCKtMHG7l40ela-YtlA$ for graphic product...

    ATTN...WFO...CLE...ILN...IWX...PBZ...

    ATTN...RFC...NCRFC...OHRFC...NWC...

    LAT...LON 42128004 41587964 40837906 40367935 40258095=20
    40108247 40088414 40398468 41128467 41428446=20
    41598400 41708288 41498233 41938083=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 26 00:40:41 2025
    AWUS01 KWNH 260040
    FFGMPD
    TXZ000-NMZ000-260600-

    Mesoscale Precipitation Discussion 0179
    NWS Weather Prediction Center College Park MD
    839 PM EDT Fri Apr 25 2025

    Areas affected...Texas Panhandle and Cap Rock...Adj East-Central
    NM...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 260040Z - 260600Z

    SUMMARY...Upscale growth from individual supercells toward
    clusters and small complexes is expected to increase rainfall
    efficiency and expand areas of intense rainfall rates/totals
    through early overnight period. Spots of 3-5" are possible and
    more incidents of flash flooding will be likely.

    DISCUSSION...00z Surface analysis denote a surface low WNW of
    Clovis with slowly retrograding dry line extending southward
    across SE NM toward ROW/ATS and CNM. A strong and steepening
    frontal zone extends from the low northeastward toward the
    Canadian River Valley northeast of AMA to BGD and HHF before
    sagging southward again across central OK. Low level moisture
    continues to stream eastward and while sfc Tds have remained in
    the upper 50s/low 60s, the depth of moisture continues to increase
    as PWat values have risen a few tenths in the last few hours,
    though still remain greatest/pooled along and south of the frontal
    boundary through the upper Red River valley where values are over
    1.5". VWP shows LLJ is starting to increase from 850 to 700mb
    with that moisture return with lower winds increasing into the
    lower 30 kt range from the southeast but southerly flow at 700 is
    about 20-25 kts.=20

    As such, moisture flux convergence from 850-700mb is starting to
    maximize along the front and convective activity has perked up in
    the last hour or so, expanding across toward the surface low in
    eastern NM. While KDP/ZDR suggests large hail currently remains
    main threat, there is expanding moderate to heavy rainfall
    signatures as the overall near storm profile continues to
    moisten/saturate especially in the lowest levels. This will
    increase rainfall efficiency from supporting 1-1.5"/hr rates
    currently toward 2"/hr after night fall occurs.=20

    Additionally, RAP forecast along with some suggestion in GOES-E WV
    loop (and AMVs) suggest a broadening diffluent region toward the
    jet occurring over the TX Panhandle. This is expected to expand
    with increasing divergence aloft through 06z as it slowly shifts
    eastward. This will further enhance confluent low level moisture
    flux toward other developing clusters into a few smaller
    complexes. Slow forward cell motions and storm scale interactions
    suggest cell mergers and increased duration at given locations.=20
    As such, there remains a solid signal of spots of 3-5" totals and
    given recent rains and FFG values of 1.5-2"/hr and 1.5-3"/3hrs it
    is considered likely that localized flash flooding concerns will
    continue into early overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5N-0sd9vPVk7VcgHHY2ft_IoFztZyOTqiK5qvnXTzVnrFGLctrqf1E959b2UNU0BUlYQ= zDMEdZ4Ytjcxzmv3pmpe7VA$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 35930148 35800077 35360033 34710017 33860040=20
    33380094 33410180 33760301 34100340 34880381=20
    35380318 35800230=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 26 01:11:03 2025
    AWUS01 KWNH 260109
    FFGMPD
    NYZ000-PAZ000-WVZ000-OHZ000-260615-

    Mesoscale Precipitation Discussion 0180
    NWS Weather Prediction Center College Park MD
    908 PM EDT Fri Apr 25 2025

    Areas affected...Northeast OH...Northwest PA...WV Stovepipe...Far
    Southwest NY...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 260115Z - 260615Z

    SUMMARY...Localized widely scattered convective cells capable of
    producing 1"/hr rates with a low-end risk of 1-2" totals to
    continue to pose isolated incident or two of possible flash
    flooding overnight.=20

    DISCUSSION...GOES-E WV suite depicts an anti-cyclonically curved
    cirrus shield indicative of right entrance positive
    ascent/divergence across the Ontario peninsula into the Lake Erie
    region. Nose of well above average (95th-99th percentile)
    moisture feed/LLJ or warm conveyor belt has been persistent from
    the southwest aided by orographic ascent through the western
    Allegheny Plateau. Some remaining conditionally unstable air with
    500-750 J/kg of CAPE appears to be aiding remaining convective
    cores across far NE OH into NW PA at this time with some cycling
    of cooling tops noted in 10.3um EIR. Given 1.25-1.4" Total
    PWats...rates of 1"/hr still remain observed though likely to
    downturn slightly over the next few hours with further loss of
    surface heating. Still orientation of convection is broad enough
    in the WAA regime and fairly parallel to the deeper layer steering
    to support some short-term repeating/training potentially
    resulting in a spot or two of 1.5-2" totals in 1-2 hours. Given
    complex terrain, these rates and totals are in the range of the
    1-1.5"/hr and/or 1-2"/3hr FFG values to be exceeded. As such,
    localized flash flooding remains possible.=20

    While the instability will be decreasing due to low level heating,
    the main mid to upper level trough remains upstream with CAA aloft
    likely to steepen mid-level lapse rates to maintain weak CAPE of
    250-500 J/kg. As such, there will remain potential for weaker
    .25-.5"/hr rate showers along/ahead of the cold front crossing the
    area. This may aggravate some areas that were near or just
    exceeding FFG and result in increased runoff through the overnight
    period past 06z with streaks of an additional .5-1".

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_IxUaTP-0-xqiaFTsxUZaerFGjq2DlIb8QrUij8E-ZLjQEFpw9hNKqQOIDCQi7Ised8o= 6FPBHy_FiRcUUjiv0eEUAM4$ for graphic product...

    ATTN...WFO...BUF...CLE...CTP...PBZ...

    ATTN...RFC...MARFC...NERFC...OHRFC...NWC...

    LAT...LON 42547841 42207786 41497774 40667823 40037945=20
    39758064 39858135 40218170 40948194 41388187=20
    41918102 42417952=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 26 01:41:41 2025
    AWUS01 KWNH 260141
    FFGMPD
    NCZ000-SCZ000-GAZ000-260600-

    Mesoscale Precipitation Discussion 0181
    NWS Weather Prediction Center College Park MD
    941 PM EDT Fri Apr 25 2025

    Areas affected...Northern GA...Upstate SC...Western NC...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 260140Z - 260600Z

    SUMMARY...Progressive, but intense line moving through rugged
    terrain poses a possible localized flash flooding concern through
    early overnight period.

    DISCUSSION...GOES-E 10.3um loop shows a rapidly cooling and
    upstream expanding line of thunderstorms across northeastern GA
    with additional cooling noted along the southwestern edge of the
    older outflow boundary moving out of AL into western GA. RAP
    analysis supported by surface observations shows some remaining
    elevated temperatures in the mid 70s to a few low 80s across the
    northern portion of the state. Tds in the mid 60s and steepening
    lapse rates aloft continue to support a pocket of 1000-1250 J/kg
    of CAPE along/ahead of the convergence line. Additionally,
    surface to boundary layer winds have backed and increased
    orthogonality to the line to further increase convergence and
    updraft strength. Deep layer moisture lags the instability axis
    slightly, but confluent low level flow of 15-20kts, help flux
    convergence with PWats reaching about 1.5".

    RADAR trends show some northeast cell motions within the line,
    especially further north to subtly increased heavy rainfall
    duration, as such, rates of 1.5-2"/hr have already been estimated
    across the northeast and spots of 2-3" are possible as the line
    crosses the area. Given complex terrain and lower FFG values, a
    spot or two of exceedance suggest flash flooding is possible.=20=20
    Also of note, the line is in the process of crossing the Atlanta
    metro, which is also prone to such rates given impermeable
    surfaces. Otherwise, the progressive nature will likely limit
    overall flooding risk to lower end and isolated to widely
    scattered in nature through early overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6HXsN-0KAo9swWJQALG0aDlKrtzTCE9zTO14Zktbk6FEzuy58DLOF5sVAuvwmOWL1rnL= 3UDoxav0N78Mg_NHrrmYJIY$ for graphic product...

    ATTN...WFO...CAE...FFC...GSP...MRX...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 35718287 35628228 34938165 34058166 33498243=20
    33138311 32838375 32828452 33058496 33768494=20
    34288456 35368357=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 26 06:23:50 2025
    AWUS01 KWNH 260622
    FFGMPD
    TXZ000-OKZ000-NMZ000-261030-

    Mesoscale Precipitation Discussion 0182
    NWS Weather Prediction Center College Park MD
    222 AM EDT Sat Apr 26 2025

    Areas affected...TX Panhandle into northwestern TX/southwestern OK

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 260620Z - 261030Z

    SUMMARY...Areas of flash flooding will be likely from portions of
    eastern NM into and across the TX Panhandle into northwestern
    TX/southwestern OK. Slow movement of heavy rain cores will be
    capable of producing rainfall rates of 2 to 3+ in/hr as the threat
    gradually builds east over the next 3-4 hours.

    DISCUSSION...06Z radar imagery from the TX Panhandle showed an MCS
    with an embedded MCV attempting to become better organized over
    the TX Panhandle near Amarillo. MLCAPE and MUCAPE values were
    estimated to be 1000-2000 J/kg (higher values to south), PWATs of
    1 to 1.5 inches and effective bulk shear values of 30+ kt (via SPC
    mesoanalysis data). This environment has been supportive of
    organized supercells with varying motions and spotty very heavy
    rain with observed rainfall rates locally in excess of 3 in/hr.
    Individual cell organization has become a bit poorer near/north of
    a quasi-stationary front but farther south, a supercell was noted
    west of I-27 near Earth and the environment remains capable of
    organized cells. In addition, the heavy rainfall threat was
    maintaining significance with cooling still noted on infrared
    cloud tops. 850 mb winds were southeasterly at 25-35 kt over the
    southern Panhandle, advecting moisture and instability into the
    convective complex over the Panhandle.

    Forecast Corfidi Vectors suggest a general eastward motion to the
    MCS should continue in the short term through additional
    convective development is probable along convergence tied the
    southward sagging frontal boundary over northwestern TX and
    moderately strong low level flow into the boundary where
    uninhibited instability was present. The result will be an
    expansion of convective coverage with embedded elements of
    training, slow and erratic individual cell motions and merging of
    heavy rain cores which will likely result in continued high
    rainfall rates, possibly exceeding 3 in/hr. Portions of
    northwestern TX have received heavy rain over the past 3 days and
    are locally more susceptible to flash flooding from heavy
    rainfall.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9FasTZT8hSZNys83Q55tj1gpLu1TNcgIGzk4q43Et76ulQh67muG8MGCz96yIf48QuNP= Q1JnIQ-DVt_7GWg2M3THYfQ$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...OUN...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 35589989 35339903 34709859 33839904 33580005=20
    33660195 33730291 33890411 34900414 35520234=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 26 10:17:09 2025
    AWUS01 KWNH 261015
    FFGMPD
    TXZ000-OKZ000-NMZ000-261500-

    Mesoscale Precipitation Discussion 0183
    NWS Weather Prediction Center College Park MD
    615 AM EDT Sat Apr 26 2025

    Areas affected...TX Panhandle into southwestern/central OK

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 261013Z - 261500Z

    SUMMARY...Flash flooding is likely to continue across portions of
    the TX Panhandle into northwestern TX and southwestern OK over the
    next few hours. Peak rainfall rates of 2-3 in/hr and peak
    additional totals of 3 to 6 inches will be possible.

    DISCUSSION...Radar mosaic and infrared satellite imagery at 0945Z
    showed an MCS advancing slowly eastward across the TX Panhandle
    into southwestern OK. Embedded thunderstorms were located along
    and north of a wavy quasi-stationary front which extended westward
    across northern TX, just south of the Red River, into the southern
    TX Panhandle and eastern NM. A couple of forward propagating
    segments were observed toward the southeastern edge of the MCS (in
    the vicinity of Childress), located south of an eastward advancing
    MCV near Pampa. VAD wind plots showed 35 to 46 kt of southerly
    flow over west-central to central TX which backed to a
    southeasterly direction near the Red River, supporting the robust
    transport of low level moisture northward atop the surface front.

    The training and repeating nature of cells along and north of the
    front have supported peak rainfall rates of 2-3 in/hr across
    southern portions of the TX Panhandle within the unstable
    environment. The front marked the northern edge of 500-1500 J/kg
    MLCAPE with 1000+ J/kg MUCAPE located north of the front via the
    09Z SPC mesoanalysis.

    As the MCV over the TX Panhandle continues to advance eastward
    into western OK over the next few hours, continued convection
    enhanced through warm air advection will spread eastward beneath
    convectively influenced diffluent flow aloft. Meanwhile, scattered thunderstorms in the wake of the MCV over the western TX Panhandle
    are expected to continue to congeal as they advance eastward and
    eventually bow southeastward into the low level inflow layer with
    periods of training. Some of the heaviest rain is expected to
    occur south of the MCV track where new thunderstorm development
    ahead of the advancing southeastern flank of the MCS should setup
    a prolonged period of heavy rain with additional totals of 3 to 6
    inches possible through 16Z, most probable over portions of
    southwestern OK or perhaps far northwestern TX.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_Aq53z0gQ7BaFo9NR_l5lsTuHDO4qmlAU_t8gUxZ1tn0WHo2vsro8iVeU_0mn2jqj0qn= Q7euJh7B1LvBxntf3b91OWw$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...OUN...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36249818 35819712 34999736 33889853 33659943=20
    33710086 33810202 34010268 34240320 34860353=20
    35430296 36000126=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 26 14:47:47 2025
    AWUS01 KWNH 261447
    FFGMPD
    TXZ000-OKZ000-262100-

    Mesoscale Precipitation Discussion 0184
    NWS Weather Prediction Center College Park MD
    1046 AM EDT Sat Apr 26 2025

    Areas affected...portions of Northwest TX into North TX and
    south-central OK

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 261500Z - 262100Z

    Summary...Scattered instances of flash flooding are likely to
    continue and expand in association with a mature MCS/MCV with
    additional localized totals of 3-6" expected (most likely from
    Norman/OKC southwestward into portions of North TX). Localized
    significant and life threatening flash flooding is possible.

    Discussion...A mature MCS (mesoscale convective system) has
    progressed southeastward out of the TX Panhandle and northwestern
    OK from overnight into the morning, resulting in 6-12 hour
    localized rainfall totals of 3-6 inches. The leading edge of the
    squall line has reached a quasi-stationary surface boundary draped
    from the southern Permian Basin eastward along and near the Red
    River of the South. Some of the heaviest totals have occurred in
    association with a well-defined MCV (mesoscale convective vortex)
    and accompanying RIJ (rear-inflow jet), producing localized 3-6"
    totals in the vicinity of Lawton, OK over just the past 3 hours
    (with hourly totals as high as 2-3"). Most recent observational
    trends support continued training and repeating of cells with
    1-3"/hr rainfall rates along and near the path of the MCV/RIJ
    (which should progress towards the northeast at near 20 kts within
    the southwesterly mid-level flow). While instability is somewhat
    limited on this trajectory (though MU CAPE of 500-1000 J/kg
    extends northeast into the OKC/Norman metro area), the dynamics of
    the MCV (as well as the influence of the right-entrance region of
    a 90 kt polar jet streak over the Middle MS Valley) are providing
    ample diffluence aloft with effective bulk shear of 30-40 kts.
    Along the southern and southwestern flanks of the MCS, much more
    ample instability (gradient of 1000-2000 J/kg of SB CAPE) with
    appreciable low-level (850 mb) moisture transport via 20 kt LLJ
    (low-level jet) should continue to support localized rainfall
    rates of 1-2"/hr. Training and repeating of cells moving west to
    east along the combined gust front and quasi-stationary boundary
    may support excessive rainfall farther south into northwest TX as
    well.

    Primarily relied on hourly runs of the HRRR and experimental RRFS
    since 06z, which are in remarkably good agreement (hour-to-hour
    and between the two separate models). Additional 3-6 hour totals
    as high as 3-6" are expected, though generally occurring to the
    south and east of where prior rainfall has occurred (though some
    additional overlap is possible, resulting in combined totals of up
    to 8" in some localities from south of Norman, OK to the southwest
    along and near I-44 to the Red River of the South). Very wet
    antecedent conditions (with NASA SPoRT-LIS 0-1 m soil moisture
    anomalies at or above the 90th percentile) have resulted in 3-6
    hour FFGs (flash flood guidance) of 2.0-3.0 inches, suggesting
    that additional scattered instances of flash flooding are likely
    (and could locally be significant and life threatening,
    particularly if these higher-end totals occur over metro areas).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7dh7aFHyBpfxJKjPKhZ1sow3WOq8VPkGTc7P0t0bKdbP9t0JJcYcqqDf7CuNVDhy5yya= qQ4KARA0ETRWFEmOzWfnZhE$ for graphic product...

    ATTN...WFO...FWD...LUB...MAF...OUN...SJT...TSA...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36039651 35389590 34409620 33529759 32869861=20
    32500005 32770224 33670264 34060208 34250107=20
    34410000 35019889 35439824 35849754=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Apr 26 20:24:27 2025
    AWUS01 KWNH 262024
    FFGMPD
    ARZ000-TXZ000-OKZ000-270200-

    Mesoscale Precipitation Discussion 0185
    NWS Weather Prediction Center College Park MD
    423 PM EDT Sat Apr 26 2025

    Areas affected...Eastern OK...Western AR...Adj Far Northeast TX...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 262025Z - 270200Z

    SUMMARY...Slow moving thunderstorms in warm sector ahead of dying
    MCV to support 1.75-2"/hr rates and scattered spots of 2-4"
    totals. While FFG values are high, an isolated incident of flash
    flooding or two may be possible.

    DISCUSSION...Last night's MCS continues to decay with some
    remaining ongoing fractured convective activity along the leading
    edge where DPVA intersects some elevated unstable energy across
    east-central OK eventually into NW AR. The main MCV is nearly
    fully occluded and is shearing out as it moves NNE along the KS/OK
    boarder. However, mid-level jet streak over the Red River, likely
    in larger scale synoptic diffluent region of the 3H jet is
    starting to strengthen the effective triple point mid-level
    circulation and develop a newer MCV across south-central OK. This
    wave as strengthened low level flow across northeast TX advecting
    higher low 70s sfc Tds and some warmer air within the clear sector
    to support 2500 J/kg of MLCAPE across SE OK toward Texarkana.=20

    The sharp frontal zone has resulted in weak directional low level
    confluence along its axis and new thunderstorms are developing
    south of the main old stationary front further north across SE OK.
    These WAA induced cells have solid bulk shear for updraft
    rotation to support increased localized moisture flux convergence
    along the pooling q-axis due to isallobaric influence. As such,
    moisture loading along with slowed forward propagation is allowing
    for efficient low level rain-fall production with 1.75-2"/hr rates
    becoming increasingly probable over the next few hours. ENE cell
    motions may allow for some cross tracks for the most intense
    downdrafts and spots of 2-4" are considered possible through the
    evening hours, particularly along and south of the surface front
    into central western AR.=20

    NASA SPoRT LIS products denote the area of concern is mainly
    aligned with RSM 0-40cm at average or slightly below average in
    the 45-50% range. This also aligns with the higher FFG values
    across the region, so even with the intense rainfall, it still may
    be difficult to exceed those values, especially further south and
    east near the Red River Valley where 3"/hr and 4"/3hr is
    apparently required to induce FF. Still, the overall organization
    and prolific history with the overall system and favorable
    moisture/instability environment still hints at one or two
    isolated low-end flash flooding incidents may still remain
    possible through this evening.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_oKDg3__20k9e8DyvugMLiYjJjVqnvLQCo3sK4tDhN4g9cljquwEyIEOiQf5YTdYpMzA= a2tbwI3IZ3vcAayci_jZ190$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...NWC...

    LAT...LON 36159508 36079443 35879395 35599355 35049318=20
    34039305 33559373 33559511 33689672 34399705=20
    34899629 35539564 35929543=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 27 22:51:57 2025
    AWUS01 KWNH 272251
    FFGMPD
    MTZ000-WYZ000-280430-

    Mesoscale Precipitation Discussion 0186
    NWS Weather Prediction Center College Park MD
    650 PM EDT Sun Apr 27 2025

    Areas affected...Northwest WY...South-central MT...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 272250Z - 280430Z

    SUMMARY...Increasing convective activity along/south of sharp
    stationary deformation zone will allow for slowly increasing
    rainfall rates and localized totals up to 2" through early
    overnight period. Rain over snow pack will further increase
    runoff and the potential for flooding conditions.

    DISCUSSION...An anomalous deep closed low across the Great Basin
    has a strong vorticity center rotating along the northeastern
    quadrant across the north-central Rockies of WY and ID. Both GOES
    WV suites show a highly divergent mid to upper-level pattern
    across southern MT enhancing the deformation shear axis from
    central ID across SW to central MT. A similarly sharp 500-1000
    thickness ridge extending across SE MT to the northern High
    Plains, suggestive of very slow propagation vectors and convergent
    deep layer steering flow along the downshear side of the deep
    upper-low in the area of concern. Strong dynamic ascent will
    need to overcome limited instability warm/moist air in the lower
    profile and utilize slant-wise ascent toward the deformation zone.
    However, a ribbon of low to mid-level moisture has been trying to
    bleed through the terrain of south-central MT into northwest WY
    with Tds into the low 40s supporting .25 to .5" low level PWat
    values.=20

    As the main forcing lifts north an 850-700mb cyclone is deepening
    across northern WY which has further strengthened low level
    northeasterly flow convergent with southerly flow along/ahead of
    the synoptic cold front starting to press through W WY/E UT at
    this time. So solid moisture flux will continue from the east and
    deeper source throughout the evening into the early overnight
    period. Already, the deep layer convergence is utilizing
    available moisture with convective towers seen breaking through
    the cirrus canopy across south-central MT with increasing
    lightning noted. Given the stationary deformation zone and
    increased convergence, cell motions will be limited or even
    stationary with potential of increasing upstream mergers
    throughout the evening. So while intensity of .25-.5"/hr is
    expected (with some HREF probability nearing 50% for 1"/hr rates,
    driven mainly by the NAM-Nest) these rates are falling in
    proximity to some warming snow pack that will also add to the
    runoff and potential flooding concerns through the evening with
    localized totals of 1-2" possible. Even where snow has melted,
    NASA SPoRT 0-40cm soil saturation values are running well above
    normal and over 70-80% across areas north of YNP. As such,
    localized flooding is considered possible through the evening into
    early overnight hours.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_7trUiFzDZpdFHVCPwZIM83ppYryUyQRRhtOIDLZs72pgPSCQ5aGJYYx-4XZC61TNV4I= ZVaYMRSxOdfLAyZLOEcaukY$ for graphic product...

    ATTN...WFO...BYZ...RIW...TFX...

    ATTN...RFC...MBRFC...NWC...

    LAT...LON 46790966 46640866 46060778 45300753 44850810=20
    44120844 43910862 43860911 44090974 44481043=20
    44781126 44911207 45341225 45801200 46321153=20
    46631078=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 27 23:32:59 2025
    AWUS01 KWNH 272332
    FFGMPD
    SDZ000-MTZ000-WYZ000-280500-

    Mesoscale Precipitation Discussion 0187
    NWS Weather Prediction Center College Park MD
    731 PM EDT Sun Apr 27 2025

    Areas affected...Sotheast MT...Western SD...Northeast WY...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 272330Z - 280500Z

    SUMMARY...Slow moving increasingly efficient thunderstorms capable
    of 1"/hr and spots of 1.5-2.5" totals in less than 3hrs posing
    possible localized incidents of flash flooding

    DISCUSSION...Surface analysis at 23z, shows a deepening sub-1000mb
    surface low between BYG and GCC in northeast WY bulging eastward
    along the western edge of the Black Hills before dropping south
    through the NEB panhandle toward secondary wave near TOR. Surface
    Tds of mid to upper 50s are wrapping around and through the Black
    Hills and trying to draw westward along and north of the bulge
    across SE MT. Full heating along/ahead of the wave and solid DPVA
    aloft from approaching upper-level trough within the eastern
    quadrant of the deep upper low over the Great Basin and the low
    level moisture is resulting in solid instability numbers, even to
    1500 J/kg as far west as Big Horn county, MT. As such,
    convergence along the bulging dry line and easterly flow north of
    the low has lead to a cluster of strong severe thunderstorms
    across SE MT. While hail is main concern, there is ample moisture
    flux to support increasing rainfall production.

    Given proximity to a sharp 500-1000 thickness ridge and generally
    weaker steering flow in proximity to a sharp deep layer
    deformation zone across central to northeast MT, even though
    organization, cells will be slow moving allowing for .5"/hr rates
    to slowly increase toward 1"/hr rates in the coming hours as deep
    layer moisture flux increases Total Pwats from .75-1" to 1-1.25".
    Below average/early season FFG values are within reach for
    1-1.5"/hr and 1-2"/3hrs across SE MT into the Black Hills of SD.=20
    Eventually cold pools should generate and low level flow will veer
    in proximity to the dry line bulge and cell motions/propagation
    will become more easterly, still duration may allow for some spots
    of 1.5-2.5" totals though early overnight period across the area
    of concern and so isolated incidents of flash flooding are
    considered possible.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_dWBXY2a-da0RBsxxrHmcTpieg-WWRvgIZgxRxxO3c8OQ25IRj8jr3wCOD_LwxRVqKoa= BjFEi3MTXhnBq02N5xOjnak$ for graphic product...

    ATTN...WFO...BYZ...GGW...UNR...

    ATTN...RFC...MBRFC...NWC...

    LAT...LON 47780660 47600599 46880600 46390542 45730365=20
    44950276 44130242 43500324 43640421 44500518=20
    44790632 44930698 45120728 45750749 45900757=20
    46450817 46790850 47160826 47450764=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Apr 27 23:36:20 2025
    AWUS01 KWNH 272336
    FFGMPD
    SDZ000-MTZ000-WYZ000-280500-

    Mesoscale Precipitation Discussion 0187...Corrected
    NWS Weather Prediction Center College Park MD
    735 PM EDT Sun Apr 27 2025

    Corrected for Southeast MT in Areas Affected Line

    Areas affected...Southeast MT...Western SD...Northeast WY...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 272330Z - 280500Z

    SUMMARY...Slow moving increasingly efficient thunderstorms capable
    of 1"/hr and spots of 1.5-2.5" totals in less than 3hrs posing
    possible localized incidents of flash flooding

    DISCUSSION...Surface analysis at 23z, shows a deepening sub-1000mb
    surface low between BYG and GCC in northeast WY bulging eastward
    along the western edge of the Black Hills before dropping south
    through the NEB panhandle toward secondary wave near TOR. Surface
    Tds of mid to upper 50s are wrapping around and through the Black
    Hills and trying to draw westward along and north of the bulge
    across SE MT. Full heating along/ahead of the wave and solid DPVA
    aloft from approaching upper-level trough within the eastern
    quadrant of the deep upper low over the Great Basin and the low
    level moisture is resulting in solid instability numbers, even to
    1500 J/kg as far west as Big Horn county, MT. As such,
    convergence along the bulging dry line and easterly flow north of
    the low has lead to a cluster of strong severe thunderstorms
    across SE MT. While hail is main concern, there is ample moisture
    flux to support increasing rainfall production.

    Given proximity to a sharp 500-1000 thickness ridge and generally
    weaker steering flow in proximity to a sharp deep layer
    deformation zone across central to northeast MT, even though
    organization, cells will be slow moving allowing for .5"/hr rates
    to slowly increase toward 1"/hr rates in the coming hours as deep
    layer moisture flux increases Total Pwats from .75-1" to 1-1.25".
    Below average/early season FFG values are within reach for
    1-1.5"/hr and 1-2"/3hrs across SE MT into the Black Hills of SD.=20
    Eventually cold pools should generate and low level flow will veer
    in proximity to the dry line bulge and cell motions/propagation
    will become more easterly, still duration may allow for some spots
    of 1.5-2.5" totals though early overnight period across the area
    of concern and so isolated incidents of flash flooding are
    considered possible.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ZdCcDG0wQ7mqaRM0Cb_ygwg4LgT6RyszKTP5aK-iZZDLXG-LYMNSc9qCMmQv85wtuLK= fp7lJjaQZ3zrJCF5QZZudJc$ for graphic product...

    ATTN...WFO...BYZ...GGW...UNR...

    ATTN...RFC...MBRFC...NWC...

    LAT...LON 47780660 47600599 46880600 46390542 45730365=20
    44950276 44130242 43500324 43640421 44500518=20
    44790632 44930698 45120728 45750749 45900757=20
    46450817 46790850 47160826 47450764=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Apr 28 04:35:51 2025
    AWUS01 KWNH 280435
    FFGMPD
    NEZ000-SDZ000-NDZ000-280930-

    Mesoscale Precipitation Discussion 0188
    NWS Weather Prediction Center College Park MD
    1235 AM EDT Mon Apr 28 2025

    Areas affected...NE/SD border into central/northern SD

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 280432Z - 280930Z

    Summary...Widely scattered instances of flash flooding will be
    possible from the NE/SD border into central/northern SD and far
    southeastern ND through 09Z. Short term training of organized
    cells and areas of heavy rain will support 1 to 2 in/hr rainfall
    rates and localized totals near 3 inches.

    Discussion...04Z surface observations placed a triple point low
    just southeast of Pine Ridge, SD with a trailing cold front
    co-located with line of thunderstorms extending southward through
    western NE. A cyclic supercell was located east of the surface low
    in Cherry County, NE along a warm front with elevated
    thunderstorms north of the warm front into south-central SD. The
    frontal cyclone was related to a large closed mid/upper low
    crossing the Intermountain West, with highly favorable upper level
    jet induced divergence and diffluence across the central SD/NE
    border. SPC mesoanalysis data showed anomalous moisture in place
    over SD with PWATs between 1 and 1.2 inches and MLCAPE was
    estimated to be between 500 to 1500 J/kg along the central SD/NE
    border with elevated instability of 1000 to 1500+ extending
    northeastward into east-central SD.

    The track of the surface low is forecast by the RAP to advance
    into central SD by 09/12Z with advection of low level moisture and
    strong lift helping to erode the capping inversion seen on the 00Z
    ABR sounding. The ABR sounding indicated 700-500 mb lapse rates of
    9.1 C/km which should support strong updrafts into the overnight.

    Deeper layer steering flow form the SW will allow for some areas
    of short term training as the triple point low and related fronts
    advance into SD over the next few hours, with low level
    convergence aligned with cell motions. Rainfall rates of 1-2 in/hr
    are expected which could produce some 2 to 3+ inch totals and
    widely scattered instances of flash flooding given flash flood
    guidance values of 1.5 to 2.5 inches in 3 hours present across
    much of SD.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5cYUUL5zCaVh5UImT3CU_Mf4ctEypeD3r7xOMxaEXnmp_HU9I50TXGIJJjBZgMr9qlKQ= 9AYvvgrEuT76FFbHdRBJZak$ for graphic product...

    ATTN...WFO...ABR...BIS...FGF...FSD...LBF...OAX...UNR...

    ATTN...RFC...MBRFC...NCRFC...NWC...

    LAT...LON 46179863 46129736 45199698 44029708 42799796=20
    43000005 42950195 43240265 44290188 45560021=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Apr 28 05:46:47 2025
    AWUS01 KWNH 280545
    FFGMPD
    SDZ000-NDZ000-MTZ000-281140-

    Mesoscale Precipitation Discussion 0189
    NWS Weather Prediction Center College Park MD
    145 AM EDT Mon Apr 28 2025

    Areas affected...western ND/SD border

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 280544Z - 281140Z

    SUMMARY...Isolated flash flooding will be possible in the vicinity
    of the western ND/SD border from slow movement of heavy rain over
    the next 3-6 hours. Rainfall rates occasionally exceeding 1 in/hr
    are expected to lead to spotty 2-3 inch totals through 12Z.

    DISCUSSION...GOES East infrared imagery and lightning data showed
    the slow eastward movement of a small cluster of thunderstorms
    which was located near the tri-state region of MT/ND/SD at 0520Z.
    A combination of 700 mb VAD wind plots, 850-700 mb LPW imagery
    along with RAP analysis data showed the upper level reflection of
    two surface lows over the High Plains. Using 700 mb as a
    representative level, the low centers were located over
    southeastern MT and southwestern SD, with a general weakness in
    the 850-300 mb steering flow near and southeast of the tri-state
    region. MUCAPE of approximately 500-1000 J/kg was in place from
    the eastern MT/WY border into the western ND/SD border via 05Z SPC
    mesoanalysis data.

    The weakness in the deeper layer flow is forecast by the RAP to
    maintain and perhaps deamplify the winds even more through 12Z
    across the region (as low as 5 kt). The weakness aloft will
    continue to allow for slow movement of heavy rain cores from along
    and east of the MT/ND/SD intersection into southwestern ND and
    northwestern SD. Instability values are likely to weaken as lower
    levels of the atmosphere cool in the wake of the stronger low over
    SD which is forecast to track northeastward, resulting in moisture
    wrapping around to the north and west of the low into an elongated commahead/deformation zone which will contain embedded heavy
    rainfall rates.

    The potential for hourly rainfall of 1 to 1.5 in/hr will be
    greatest through ~08Z, after which point the reduction in
    instability values should reduce rainfall intensity to a more
    steady/longer duration rainfall event. Through ~12Z, spotty
    additional rainfall totals of 2-3 inches will be possible which
    may support some isolated flash flooding.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_YM1yTafQONHrX6asL4cCmxvF6rHm5elBnRCKS1KoMRZ4qfUzSFtX5ibjcrCuWZPSoGW= uqe4GAagXgT8zpbaXfPOJA4$ for graphic product...

    ATTN...WFO...ABR...BIS...BYZ...UNR...

    ATTN...RFC...MBRFC...NWC...

    LAT...LON 46360150 45950026 45390049 45060185 44990334=20
    45260426 45930437 46270349=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Apr 28 09:04:10 2025
    AWUS01 KWNH 280902
    FFGMPD
    MNZ000-SDZ000-NDZ000-281500-

    Mesoscale Precipitation Discussion 0190
    NWS Weather Prediction Center College Park MD
    501 AM EDT Mon Apr 28 2025

    Areas affected...southeastern ND into northwestern MN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 280900Z - 281500Z

    SUMMARY...Steady rain with embedded rain rates of 0.5 to about 1
    in/hr are expected to affect portions of southeastern ND into
    northwestern MN through 15Z. While rainfall intensity should
    remain relatively low, total rainfall 1 to 2 (locally 2+) inches
    may result localized areas of runoff.

    DISCUSSION...0850Z water vapor imagery and MRMS reflectivity
    showed the manifestation of a low to mid-level vorticity max over
    east-central SD, slowly advancing toward the NNE. Anomalous
    moisture was present with recent GPS data indicating 1.0 1o 1.1
    inches near FSD, with northward extrapolation using SPC
    mesoanalysis and sounding climatology data, suggests moisture
    across the Red River of the North was over the 90th percentile.
    GOES East derived winds and short term RAP forecasts highlighted
    an 80-100 kt jet max positioned over northeastern CO into central
    NE with left-exit region induced diffluence and divergence over SD.

    As the low to mid-level low/vort over central SD moves north,
    favorable ascent will overspread eastern ND into western and
    northern MN within a SW to NE oriented deformation zone which is
    expected to slowly pivot over eastern ND. 850 mb winds to the east
    of the main surface low will continue to advect anomalous moisture
    northward which will wrap back into the cold conveyor
    precipitation axis where weak instability (up to 500 J/kg) should
    be present per recent RAP forecasts. The combination of the
    anomalous moisture, strong ascent and weak instability should be
    enough to support localized rainfall rates of 0.5 to about 1 inch
    per hour at times, with a longer duration heavy rainfall axis
    impacting southeastern ND into northwestern MN through 15Z.
    Localized totals within this axis of 1-2 inches are expected, and
    localized totals in excess of 2 inches will be possible along with
    localized flash flooding given possible exceedance of the 1,3 and
    6-hour FFG.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-9kdz3Ql0hBEblXSPiW_A5YnrZBL6XNpk0DCR8FwTSeclGVOVuKsbsTpwVbvipmjCkYy= 2skUT_X8Vv7GZAOWO94MGkY$ for graphic product...

    ATTN...WFO...ABR...BIS...FGF...

    ATTN...RFC...MBRFC...NCRFC...NWC...

    LAT...LON 48139576 47819517 47039572 46129752 45639924=20
    45820012 46460006 47019919 47849716=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Apr 29 00:12:23 2025
    AWUS01 KWNH 290012
    FFGMPD
    WIZ000-MNZ000-IAZ000-290411-

    Mesoscale Precipitation Discussion 0191
    NWS Weather Prediction Center College Park MD
    811 PM EDT Mon Apr 28 2025

    Areas affected...northern Iowa, southeastern Minnesota, western
    Wisconsin

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 290011Z - 290411Z

    Summary...Isolated flash flooding could occur as a convective
    complex migrates eastward across the region tonight.

    Discussion...Scattered convection that had initially developed
    across southwestern Minnesota has grown upscale into loosely
    organized linear segments, with a bow structure noted southwest of
    Eau Claire, WI. Southwest of this bowing segment, cells were
    gradually maturing along an axis from near Rochester, MN
    southwestward to north-central Iowa near Emmetsburg. Trailing
    convection southwest of the bow has exhibited a favorable setup
    for convective training. Cooler surface temperatures (in the 50s)
    northwest of the training axis is indicative of a maturing cold
    pool that could interact favorably with southwesterly 850mb flow
    to maintain convergence and new updrafts streaming into the
    training axis for another 2-3 hours or so. This scenario should
    help to maintain ongoing 1-1.5 inch/hr rain rates (estimated per
    MRMS) where convective training is most pronounced, leading to
    isolated spots of FFG exceedence and flash flooding.

    This scenario should be relatively short-lived, however. Models
    suggest that 850mb flow will veer gradually to westerly through
    03-04Z, which should act to limit training potential by decreasing
    convergence along the edge of the aforementioned cold pool. As
    long as convective training persists, isolated flash flooding will
    be possible.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_-_EKBTA_c9I3YiqutjyEpLuLz3wnz_-0PU0yWbMQa8f-HNujL6G00n0WJf1PsDMtF0S= W-8kiQnJVpRW0UmEgUBHrok$ for graphic product...

    ATTN...WFO...ARX...DMX...GRB...MPX...

    ATTN...RFC...NCRFC...NWC...

    LAT...LON 45109092 44738987 43928987 43299109 43089444=20
    44229398 44909261=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Apr 29 00:40:35 2025
    AWUS01 KWNH 290040
    FFGMPD
    MOZ000-KSZ000-NEZ000-290639-

    Mesoscale Precipitation Discussion 0192
    NWS Weather Prediction Center College Park MD
    839 PM EDT Mon Apr 28 2025

    Areas affected...northeastern Kansas and vicinity

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 290039Z - 290639Z

    Summary...Areas of flash flooding have occurred near Manhattan,
    KS, and additional instances could continue for at least another
    2-4 hours. Spots of additional 1-4 inch rainfall totals are
    expected.

    Discussion...Between 22Z and 00Z, trailing convection has
    developed upstream of a lead supercell currently about 25 N of
    Topeka, KS. These cells were redeveloping just north of trailing
    outflow behind that lead supercell (extending across Manhattan and
    areas southeast of Salina). This axis also happens to be
    collocate with a dryline extending through Salina to just east of
    Omaha, NE. Surface winds have remained backed across
    central/southeastern Kansas ahead of this complex. This scenario
    has enabled focused convergence of updrafts from south of Salina
    through Manhattan on to areas north of Topeka, with spots of 2
    inch/hr rain rates estimated per radar. The stationary nature of
    the boundaries and their orientation parallel to steering flow
    aloft suggests a continued threat of flash flooding for at least
    another 2-3 hours.

    Although some uncertainty exists with respect to the persistence
    of ongoing convection across the discussion area, continued
    convective training appears probable for the next 3-6 hours across
    northeastern Kansas. Both synoptic and mesoscale features are not
    expected to change much through 06Z, with only subtle
    southward/rightward movements of outflow and training axes based
    on local convective evolution. At least 1 inch/hr rain rates are
    expected in this regime as long as convective training remains
    pronounced. Local areas of 2-4 inch totals could occur where
    training is most pronounced.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_wZC2CZ-6MRkeFD2Wsjhg3qrgqOEOdN61247glka5ilR3N9vWTSFfwNLtXWLEeknJmVj= xlFs7zDLgOB9MkQD3o3Yeq4$ for graphic product...

    ATTN...WFO...EAX...ICT...OAX...TOP...

    ATTN...RFC...ABRFC...MBRFC...NWC...

    LAT...LON 40319338 39849303 39429316 39039392 38699577=20
    38279705 38269769 38999783 39829637 40299453=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Apr 29 12:31:48 2025
    AWUS01 KWNH 291231
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-291700-

    Mesoscale Precipitation Discussion 0194
    NWS Weather Prediction Center College Park MD
    830 AM EDT Tue Apr 29 2025

    Areas affected...Northeast OK...Far Southeast KS...Southwest
    MO...Far Northwest AR

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 291230Z - 291700Z

    SUMMARY...A strong complex of showers and thunderstorms will
    continue to advance off to the east over the next few hours. A
    concern for isolated areas of flash flooding will continue.

    DISCUSSION...GOES-E IR satellite imagery shows a mature,
    cold-topped MCS advancing eastward across central to northeast OK
    and into far southeast KS. The convection is focusing in close
    proximity to a wave of low pressure riding northeastward up along
    a strong frontal zone, with a corridor of rather strong moisture
    convergence in place. Additionally, there is a fair amount of
    instability in place at least in a somewhat elevated fashion with
    MUCAPE values of close to 2000 J/kg.

    A southwest low-level jet of 30 to 40 kts should tend to help
    sustain the convective complex at least for a few more hours as it
    advances downstream into areas of southwest MO and possibly far
    northwest AR. The PW environment is somewhat moist with values of
    around 1.5 inches, and this coupled with the organized nature of
    the convection should tend to favor rainfall rates continuing to
    reach well into the 1 to 2 inch/hour range.

    The latest hires model guidance suggests some localized 2 to 4
    inch rainfall totals may be possible where at least some brief
    cell-training occurs in close proximity to the aforementioned
    front.

    This will be occurring over areas of the Ozark Plateau that are
    rather moist from an antecedent conditions perspective.
    Streamflows especially across southwest MO are generally running
    above normal this morning, and these additional rains may favor
    some more efficient runoff concerns. Thus, at least an isolated
    threat of flash flooding will continue to be attached to this
    convective complex over the next few hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_YtAHwLIxvYXDoB8u53nWX34dYblkr38RB1FnHtjtADXvc4XSoSrZ1y__Raze2mg_rUs= sjYNOrD_g3qdFIMNh9KGVZk$ for graphic product...

    ATTN...WFO...ICT...LZK...OUN...SGF...TSA...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NWC...

    LAT...LON 37979386 37939220 36989202 36279334 35829505=20
    35659624 35929694 36519683 37289562=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Apr 29 19:29:58 2025
    AWUS01 KWNH 291929
    FFGMPD
    OHZ000-KYZ000-INZ000-ILZ000-MOZ000-300127-

    Mesoscale Precipitation Discussion 0195
    NWS Weather Prediction Center College Park MD
    329 PM EDT Tue Apr 29 2025

    Areas affected...southeastern Illinois, southern indiana, far
    northern Kentucky, and southwestern Ohio

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 291927Z - 300127Z

    Summary...Isolated spots of flash flooding are possible as a
    convective complex migrates from southern Illinois across the
    discussion area through 01Z/8pm CDT.

    Discussion...Strong convection has aligned in a mostly linear
    fashion across southern Illinois from near Mount Vernon to near
    Cape Girardeau. This complex was moving east at around 30-35
    knots. More recently, radar mosaic imagery has depicted lead
    cells developing out ahead of the main linear complex in more of a
    east-west orientation (parallel to flow aloft). These cells have
    merged with the main complex, allowing for localized prolonging of
    heavier rainfall and rates peaking at around 1.5-2 inch/hr (per
    MRMS), which has locally exceeded hourly FFG. A couple instances
    of flash flooding have been reported near the cell mergers over
    the past 30-60 minutes or so just southwest of Nashville, IL.

    The overall regime will shift eastward across the discussion area,
    traversing the Ohio Valley and adjacent areas of IL/IN/KY and
    southwestern OH through 01Z. The regime is expected to continue
    to produce spots of 1.5 inch/hr rain rates that could result in
    localized flash flooding at times especially where cell mergers
    are most frequent. Current trends suggest that the greatest flash
    flood risk should enter southern Indiana after around 21Z or so,
    and southwestern Ohio after around 23-00Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-PuPv9n1SfeNeI19PsPJWwp3xX5up8hR_o-DnjFLVmA4dQqmjJVPyfHj5E1NZ_5vJIsN= T2JNipLAfGfb--nHNPntg4Q$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...JKL...LMK...LSX...PAH...

    ATTN...RFC...LMRFC...NCRFC...OHRFC...NWC...

    LAT...LON 39618410 39078322 38478345 37728508 36998796=20
    36928939 37888971 38888916 39318789 39608588=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Apr 29 19:39:46 2025
    AWUS01 KWNH 291937
    FFGMPD
    TXZ000-OKZ000-300135-

    Mesoscale Precipitation Discussion 0196
    NWS Weather Prediction Center College Park MD
    336 PM EDT Tue Apr 29 2025

    Areas affected...West-Central to Northwest TX...Southwest to
    Central OK

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 291935Z - 300135Z

    SUMMARY...Considerable development and expansion of heavy showers
    and thunderstorms can be expected over the next several hours
    going into the evening time frame. Areas of flash flooding will
    become likely in time due to heavy rainfall rates and storm totals
    along with locally sensitive soil/streamflow conditions.

    DISCUSSION...The mid-afternoon GOES-E visible satellite imagery
    shows convection beginning to initiate across areas of western TX
    in close proximity to the dryline, with additional agitated CU/TCU
    development noted off to the northeast near a stationary front
    situated over northwest TX and into southwest and central OK. In
    fact, there is a cluster of stronger convection evolving over
    central OK to the south of the Oklahoma City metro area which is
    near the intersection of the front and a nearby long-lived outflow
    boundary.

    The warm sector airmass across the southern Plains near these
    boundaries is quite unstable with MLCAPE values of 2000 to 2500+
    J/kg in place with the aid of strong diurnal heating and a
    moisture-laden boundary layer with surface dewpoints in the mid to
    upper 60s. A substantial amount of shear is already in place with
    effective bulk shear values of 50 to 60+ kts noted, and this
    coupled with the favorable thermodynamic environment will set the
    stage for developing and expanding clusters of heavy showers and
    thunderstorms over the next few hours.

    Given the arrival of subtle height falls from the west in
    association with a deep upper trough over the Southwest, and with
    some additional strengthening of the low to mid-level wind field,
    the convection should grow upscale heading into the evening hours
    with well-organized convection focusing near the dryline and
    especially the front/outflow boundary locations. This will include
    supercell thunderstorm activity with potential for cell-mergers
    and potentially some smaller scale QLCS evolution in time.

    The environment will be rather moist by this evening across the
    region and especially over northern TX and into southern OK where
    PWs should increase to near or above 1.5 inches and this will be
    running a solid 2 standard deviations above normal. This coupled
    with the kinematic and thermodynamic environment should help
    support rainfall rates as high as 1.5 to 2.5"/hour with the
    stronger convective cores, and especially any supercells.

    In time, the upscale growth along with concerns for cell-mergers
    and localized cell-training will favor some storm totals by early
    this evening of 3 to 5 inches. The heaviest rainfall totals are
    expected to be over areas of northwest TX into southwest and
    south-central OK and this closely aligns with the current WPC D1
    ERO depiction of a Moderate Risk of excessive rainfall. Areas of
    flash flooding are expected to gradually become likely across
    these areas, and especially given elevated soil/streamflow
    sensitivities.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_c1eevdiFtS-0Cwz6NjADVsbGIGzBbVl9q2QZNdUHRDAADw_Sufx18Piy8FaE1z9zc1H= M29cIQgMWgk5RcT8C7jD3j4$ for graphic product...

    ATTN...WFO...FWD...LUB...MAF...OUN...SJT...TSA...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36489622 36179484 35469462 34559520 33889625=20
    33269753 32199944 31610038 30810235 30700312=20
    30960329 31850260 32510223 33110226 33680167=20
    34340032 35129907 36029763=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Apr 29 22:47:00 2025
    AWUS01 KWNH 292245
    FFGMPD
    PAZ000-WVZ000-OHZ000-KYZ000-INZ000-300244-

    Mesoscale Precipitation Discussion 0197
    NWS Weather Prediction Center College Park MD
    644 PM EDT Tue Apr 29 2025

    Areas affected...northern Kentucky, southeastern Indiana, southern
    Ohio, portions of West Virginia

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 292244Z - 300244Z

    Summary...Loosely organized convective clusters continue to
    migrate eastward and produce spots of 1 inch/hr rain rates. These
    trends are expected to continue through/after sunset, posing a
    risk of isolated flash flooding.

    Discussion...Scattered convection has developed in earnest across
    portions of southwestern Ohio and Kentucky out ahead of a MCS over
    southern Indiana. Heavier rain rates associated with this
    convection have decreased somewhat - mainly due to a lesser degree
    of organization of the convection compared to just a couple hours
    ago. Nevertheless, spots of 1 inch/hr rain rates continue to be
    estimated per MRMS as cells merge/train on a localized basis.=20
    Storms are being maintained by a moist, uncapped, and unstable
    airmass characterized by 1.6 inch PW values and ~1500 J/kg MLCAPE
    away from cold pools. Additionally, 25-35 kn westerly flow was
    allowing for efficient recovery of the airmass across Ohio in the
    wake of a strong MCS that traversed that area, indicating
    potential for eastward persistence of storms into OH/WV through
    the early evening.

    Cells should also gradually move into areas with slightly lower
    FFG thresholds (around 1 inch/hr across the discussion area)
    compared to areas upstream in Indiana/Illinois. Thus, an
    isolated/localized flash flood threat should continue through the
    early evening hours as clusters of convection migrate eastward -
    especially in sensitive/low-lying areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7QwIooTYNiv3BCw5v-kuJACsWOkQSZZmVXqL9egLaSv3MgCUEQNOz2rBDsgPoL4GWkRj= RBmIfTZYB7NNBtEk7F1EaMw$ for graphic product...

    ATTN...WFO...CLE...ILN...IND...JKL...LMK...PBZ...RLX...RNK...

    ATTN...RFC...OHRFC...NWC...

    LAT...LON 40478361 40328101 39728000 38687995 37818132=20
    37308363 37508554 38738552 40168479=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 30 01:29:26 2025
    AWUS01 KWNH 300128
    FFGMPD
    ARZ000-TXZ000-OKZ000-300727-

    Mesoscale Precipitation Discussion 0198
    NWS Weather Prediction Center College Park MD
    927 PM EDT Tue Apr 29 2025

    Areas affected...west Texas into much of Oklahoma

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 300127Z - 300727Z

    Summary...Flash flood threat continues across the discussion area
    through 07Z and beyond. Significant impacts are expected
    especially across western north Texas and vicinity.

    Discussion...Over the past 1-2 hours, a general uptick in
    convection has been noted across much of Oklahoma and western
    north Texas in tandem with 1) an increase of southerly low-level
    flow across much of the southern Plains and 2) the complicated
    evolution of a mature supercellular cluster currently just near
    Wichita Falls. Most of the convection has been slightly elevated
    atop a cool/stable layer, but the aforementioned supercellular
    cluster appeared to root near a remnant outflow from earlier
    convection, with its complex evolution resulting in a few areas of
    2-4 inch rainfall totals extending from just southeast of Lubbock
    to near Seymour over the past 3-4 hours. Convection continues to
    grow upscale into a mix of lines and cells while also moving
    through sensitive/wet ground conditions from prior extreme
    rainfall across western north Texas and southwestern Oklahoma.=20
    Occasional instances of flash flooding are expected with this
    activity (extending into central/south-central Oklahoma) over the
    next 2-4 hours.

    Although a very brief break in precip coverage is apparent across
    west Texas currently, 1) 40-45 knot 850mb flow across southwest
    Texas, 2) nearly stationary surface boundaries, and 3) apparent
    ascent over the TransPecos will result in another round of renewed
    convection across west Texas that will migrate east-northeastward
    across sensitive areas that have received abundant rainfall over
    the past week (western North Texas into southern/central
    Oklahoma). Potential exists for a significant, widespread flash
    flood event to unfold across these areas over the next 6 hours and
    beyond.=20

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_EIqktVdM0CRvzyjj4rYoFAmAjCXJjqyLTxoXsMbYyfBf9JdT9Sq0TjJYb2qgG465eB2= 7rGGx0vcbf6vCruvIcgV3_8$ for graphic product...

    ATTN...WFO...AMA...FWD...LUB...MAF...OUN...SJT...TSA...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36559630 36539492 35869448 34909480 34029556=20
    33249716 32539920 31130148 31390243 33050238=20
    34280149 34979995 36019812=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 30 12:46:34 2025
    AWUS01 KWNH 301246
    FFGMPD
    TXZ000-OKZ000-301500-

    Mesoscale Precipitation Discussion 0201
    NWS Weather Prediction Center College Park MD
    612 AM EDT Wed Apr 30 2025

    Areas affected...northwestern TX into central/northeastern OK

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 301011Z - 301500Z

    SUMMARY...Scattered to numerous coverage of flash flooding is
    expected from portions of northwestern TX into central and
    northeastern OK through 15Z. Rainfall rates of 1-2 in/hr (locally
    higher) are likely to impact portions of the region which have
    recently received heavy rainfall, potentially leading to significant/considerable impacts.

    DISCUSSION...Radar imagery at 10Z showed a forward propagating
    line segment which extended from southwestern OK into northwestern
    TX, located along and north of a quasi-stationary front which
    draped southwestward from southern OK into the western Permian
    Basin of TX. Peak MRMS-derived hourly rainfall with the advancing
    line has generally been 1-2 inches. Over southern OK, a band of
    training resulted in 2 to 5 inches of rain from northern Wilbarger
    County, TX to Stephens County, OK, out ahead of the advancing line
    segment. In addition, immediately in the wake of the forward
    propagating line segment was an additional/small cluster between
    MAF and LBB, slowly advancing eastward.

    While some minor weakening of low level winds is expected over the
    next few hours with the diurnal cycle, 25-45 kt of flow at 850 mb
    is likely to maintain robust clusters of thunderstorms from
    northwestern TX into central/northeastern OK over the next 3-5
    hours. While line segments are expected to generally propagate
    toward the east, there will be instances of training within the
    line segments where orientation matches the SW to NE oriented
    deeper layer steering flow. Rainfall rates of 1-2 in/hr will be
    likely (locally higher) with an additional 2-4 inches through 15Z
    for portions of the region. Due to areas of ongoing flash flooding
    from recent heavy rainfall, scattered to numerous occurrences of
    flash flooding are expected and locally significant/considerable
    flooding could affect locations on either side of the Red River
    which have picked up 4+ inches of rain over the past 12 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8MAzfF1wXQgr7WueA7_e4Z9aRC6qVPzNVzFJ6tklIk3XhCWBTaZbJKICFxSLG7MUWxt9= gkxQC-7DvxNU89dmrfZxvmA$ for graphic product...

    ATTN...WFO...FWD...LUB...MAF...OUN...SJT...TSA...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36369678 35909572 35239553 34019604 32449740=20
    31839848 31689945 31680041 31910100 32160138=20
    32310186 32550216 32960214 33430166 33780050=20
    34809961 35819813=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 30 14:02:37 2025
    AWUS01 KWNH 301402
    FFGMPD
    ARZ000-TXZ000-OKZ000-302000-

    Mesoscale Precipitation Discussion 0202
    NWS Weather Prediction Center College Park MD
    1000 AM EDT Wed Apr 30 2025

    Areas affected...Central and Northern TX...Eastern OK...Far
    Western AR

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 301400Z - 302000Z

    SUMMARY...Very heavy showers and thunderstorms will be impacting
    much of central and northern TX and into portions of eastern OK
    and far western AR going through the mid-afternoon hours. Areas of
    significant and life-threatening flash flooding are expected which
    will include a notable urban flash flood threat to multiple
    metropolitan areas including Dallas-Fort Worth and adjacent
    suburbia.

    DISCUSSION...The early morning GOES-E IR satellite imagery in
    conjunction with dual-pol radar shows an elongated axis of very
    heavy shower and thunderstorm activity focused across areas of
    central and northern TX and extending well into areas of southern
    and eastern OK. The convection is well organized and generally
    focused along a quasi-stationary front with multiple waves of low
    pressure riding east-northeast along it.

    A look at the latest RAP analysis shows MLCAPE values of 1000 to
    1500+ J/kg already pooled up along the front, with an increasingly
    moist warm-sector airmass continuing to advance north into the
    boundary with aid from a southerly low-level jet of 40 to 45+ kts.
    3-hour MLCAPE differentials of +400 to +600 are already noted
    along an axis from central TX to southeast OK along the corridor
    of more convergent and moist low-level flow, and the combination
    of higher surface dewpoints and diurnal heating will favor a
    steady increase in instability over the next several hours.

    The southern flank of the convective axis in particular from
    central to northeast TX is expected to be particularly potent with
    very high rainfall rate potential going forward as a combination
    of strengthening thermodynamics and rather strong low to mid-level
    shear (0-3 km bulk shear of 40 to 45 kts) favor enhanced/efficient
    updrafts with substantial moisture convergence/water-loading
    through the cloud-bearing layer. Rainfall rates of 2 to 3
    inches/hour are likely in these areas.

    Areas from especially the Mineral Wells to Dallas-Fort Worth
    metropolitan corridor along with the adjacent suburbs of northern
    TX (including the Denton to Sherman corridor) are expected to see
    some of the heaviest rainfall rates and totals going through
    mid-afternoon with as much as 3 to 5+ inches of rain possible
    where localized corridors of cell-training occurs.

    However, areas farther north into eastern OK are expected to see
    additional heavy rainfall as a strong upstream MCV approaches and
    interacts with the pooling of moisture/instability surging up
    across southeast OK in close proximity to the aforementioned
    front. Areas from Durant through McAlester and the Stigler
    vicinity will likely see additional heavy rainfall totals of as
    much as 2 to 4+ inches through this nowcast period.

    Areas of significant and life-threatening flash flooding are
    expected going through the mid-afternoon hours, and this will
    include notable urban flash flooding concerns given the high
    rainfall rate potential along with locally sensitive antecedent
    conditions.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5arosPIwo0JxCv4WSt4E3f2qT0ZCm2ioDwv5j60E1Q2YrS4EHbMobOzJ1jfgWTuz5WbC= jJkWCcjG6aqQAOhgXE_YCOc$ for graphic product...

    ATTN...WFO...FWD...LUB...LZK...OUN...SHV...SJT...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 36609514 36199387 33929391 32249596 31619879=20
    31840029 32580048 33959863 35529709=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Apr 30 19:27:39 2025
    AWUS01 KWNH 301927
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-010125-

    Mesoscale Precipitation Discussion 0203
    NWS Weather Prediction Center College Park MD
    325 PM EDT Wed Apr 30 2025

    Areas affected...Central to Northeast TX...Far Southwest AR...Far
    Northwest LA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 301925Z - 010125Z

    SUMMARY...A complex of heavy showers and thunderstorms will
    continue to gradually settle south and east going through the
    afternoon and early evening hours. Intense rainfall rates and
    storm totals will likely promote additional areas of flash
    flooding which will include locally considerable/significant urban
    flash flooding impacts.

    DISCUSSION...The afternoon GOES-E visible satellite imagery shows
    a substantial amount of CU/TCU development across central to
    northeast TX out ahead of a well-defined and long-lived MCS that
    has been transiting northern TX and eastern OK over the last
    several hours. The warm-sector airmass with the aid of strong
    diurnal heating and a moisture-laden boundary layer with surface
    dewpoints in the upper 60s to low 70s is affording MLCAPE values
    as high as 1500 to 3000 J/kg. This includes the Austin to Waco
    corridor on northeastward up into the Tyler and Longview vicinity.

    A combination of strong instability and enhanced moisture flux
    convergence with the aid of a southerly low-level jet of 40 to 50
    kts will continue to favor a well-organized southern flank of the
    larger scale convective mass. The convergent nature of the moist
    low-level wind field and with favorable low to mid-level shear
    profiles (0-3 km bulk shear of 30 to 40 kts) should continue to
    sustain enhanced convective cores with rainfall rates reaching as
    high as 1 to 3 inches/hour.

    The concern going into the evening hours will be the increasing
    threat for the southwest flank of the convective line to begin
    slowing down as upstream mid-level height falls begin to
    increasingly overspread the broader southern Plains region, and
    with the deeper layer flow becoming more aligned with the leading
    edge of the surface cold pool/outflow boundary orientation.
    Cell-training concerns with backbuilding convection may extend in
    time as far southwest as the Austin metropolitan area itself, but
    greater short-term concerns are expected along the Waco to Tyler
    corridor and stretching east through Tyler and Longview. Some of
    the convection will also advance into far southwest AR and
    northwest LA, but generally the heaviest rainfall should be for
    areas farther down to the southwest over central to northeast TX.

    Recent runs of the HRRR/RRFS guidance and also the experimental
    WoFS indicate potential for as much as 3 to 6 inches of rain where
    the greatest cell-training concerns set up, and this will promote
    additional areas of flash flooding with a concern at least locally
    for considerable/significant urban flash flooding impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Uxh8F4G4WVKve7VdDUzMV8SxxjdxMM54Y7QlaXv6HZeu32842o5oB_xYj8hvsheO8ZB= i8bpEOrjQJe_jd4fBqjCKpk$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...OUN...SHV...SJT...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 34059415 33699330 32959312 32199366 31049538=20
    30359680 30319798 30969847 31949822 33459674=20
    34019538=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu May 1 01:22:25 2025
    AWUS01 KWNH 010121
    FFGMPD
    LAZ000-ARZ000-TXZ000-010720-

    Mesoscale Precipitation Discussion 0204
    NWS Weather Prediction Center College Park MD
    920 PM EDT Wed Apr 30 2025

    Areas affected...central/east Texas and far western Louisiana

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 010120Z - 010720Z

    Summary...Areas of flash flooding remain possible along and ahead
    of an elongated, southward-moving MCS. 1-2 inch/hr rain rates
    remain likely, which could cause flooding issues especially in
    sensitive/urban areas.

    Discussion...An elongated MCS continues to migrate slowly
    southward and is currently located along an axis from near Temple
    to Shreveport. Individual cells/clusters within the broader MCS
    are initiating closer to stronger mid-level instability across
    central Texas and migrating eastward, resulting in extensive
    training and multiple areas of 1-2 inch/hr rain rates at times.=20
    Heavier rain rates have persisted for multiple hours, resulting in
    spots of 2-5 inch rainfall totals (per MRMS radar estimates) These
    rain rates have resulted in scattered impacts (especially between
    Waco and Tyler). These rates are exceeding FFG thresholds on a
    spotty basis, as 3-5 inch/hr FFG thresholds are prevalent across
    much of Texas east of I-35 and south of I-20.

    The ongoing convective scenario supporting flash flooding should
    continue to translate southward over the next 4-6 hours. However,
    flash flood potential should become progressively more isolated as
    a result of 1) continued high FFG thresholds south of the ongoing
    MCS, and 2) veering/weakening 850mb flow, which should ultimately
    result in less convergence/convective coverage within the MCS.=20
    Flash flooding remains possible especially where heavier rain
    rates (exceeding 1 inch/hr) 1) reside over local areas of multiple
    hours and/or 2) fall over urban/sensitive ground conditions.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7IJ6HI6asb4UBFCBoCHm6UG6O1Cnbp0FzpzPSjg4qLP4GKZhyeYh16E5tXbUqI39Yxy3= CmlzRbSS_JhNKxfSZ7vNGc0$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...LCH...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 33139422 32769326 31569314 30239367 29619561=20
    29439804 31009834 31819751 32579605=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu May 1 21:53:30 2025
    AWUS01 KWNH 012153
    FFGMPD
    TXZ000-020351-

    Mesoscale Precipitation Discussion 0205
    NWS Weather Prediction Center College Park MD
    553 PM EDT Thu May 01 2025

    Areas affected...portions of southwest into central Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 012151Z - 020351Z

    Summary...Isolated, slow-moving thunderstorms are capable of local
    2-3 inch/hr rain rates, which could result in a few areas of flash
    flooding. Later this evening, a complex emanating from near the
    Rio Grande should also foster an isolated flash flood risk.

    Discussion...In the past hour or so, explosive thunderstorm
    development has occurred on an isolated basis along an axis from
    near Killeen, TX west-southwestward to near Del Rio. The updrafts
    are breaching the cap within a zone of focused convergence along a
    dryline near that same axis. Although wind fields aloft are
    westerly at around 20-35 knots, cells have exhibited slow
    right-moving, supercellular tendencies that have supported local
    rain rates of 2-3 inches/hr (estimated per MRMS/local radar).=20
    These rates are falling in areas of local FFGs in the 1.5-2.5
    inch/hr range (lowest near Killeen and surrounding areas that
    received 2-3 inch rainfall amounts yesterday night), suggestive of
    isolated flash flood potential near the slowest-moving convection.

    Ongoing activity is expected to continue to remain isolated and
    confined to areas near/south of the dryline this evening.=20
    Eventually, convection over northern Mexico (southwest of Del Rio)
    is expected to grow upscale and form an eastward-moving complex
    that will move through a pool of very strong instability across
    the discussion area and provide another opportunity for heavy
    rainfall - especially in western portions of the discussion area
    (Del Rio to perhaps San Antonio and vicinity late). Totals could
    be locally higher where cell mergers occur. The ongoing scenario
    supports at least an isolated flash flood threat across the
    discussion area thhrough the evening.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!75_ZViJMHzk25RmhjBbfsxXiOCCgIpWakpSNFuErSxeYpogwQW7Cfzgg6Vl7I9cHpxl8= OJxA3ydtFtRx3_Fo1PnnmLI$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...MAF...SHV...SJT...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 31979462 31529426 30799497 29709757 28689999=20
    29010078 29370133 29810215 30250135 31519920=20
    31959700=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 2 00:29:00 2025
    AWUS01 KWNH 020027
    FFGMPD
    TXZ000-020225-

    Mesoscale Precipitation Discussion 0206
    NWS Weather Prediction Center College Park MD
    826 PM EDT Thu May 01 2025

    Areas affected...portions of central Texas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 020025Z - 020225Z

    Summary...Heavy rainfall continues to pose a locally signficant
    flash flood risk - especially northwest through northeast of
    Austin, TX metro.

    Discussion...A combination of supercellular and outflow-dominant
    clusters have produced rain rates of 2-3 inches per hour and
    nearly 7 inches in 3 hours along an axis from near Burnet/Buchanan
    Dam eastward to near Hearne, TX. Recent radar imagery indicates a
    gradual increase in both 1) the presence of outflows spreading
    away from heavier cores near this activity and 2) overall
    convective coverage. These trends were occurring amid a modest
    increase in low-level flow, which has helped to maintain an influx
    of moist (1.5 inch PW) and strongly unstable (4000 J/kg MLCAPE)
    air into the storms.

    Though the exact evolution is still a bit uncertain, some concern
    exists that upscale growth could both 1) allow for a longer
    duration of heavier precipitation into the evening than depicted
    by most CAMs that 2) ultimately spreads impacts closer to
    populated areas such as Austin and College Station. Given the
    magnitude of rain rates (2+ inches/hr), these impacts could become
    significant.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5xBDbz2oyG0PhaoPfAXCyK8jXvCMqNtW7yvaw-eAWXWV46OsfxHpnwSA1WX4vQDrolLq= igLW9XjfOgUNz3ekf64O1rQ$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...SJT...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 31349847 31219647 31039519 30479483 29889519=20
    29479706 29969943 31079950=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 2 02:19:08 2025
    AWUS01 KWNH 020218
    FFGMPD
    TXZ000-020700-

    Mesoscale Precipitation Discussion 0207
    NWS Weather Prediction Center College Park MD
    1017 PM EDT Thu May 01 2025

    Areas affected...Rio Grande Valley of Southwest TX....

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 020215Z - 020700Z

    SUMMARY...A few more hours of intense rainfall with cell
    collisions and localized 2"/hr and totals to 4" continuing
    possible flash flooding concerns through early overnight period.

    DISCUSSION...RADAR mosaic and lightning mapping loop shows
    maturing cold pool across Uvalde/Kinney county with an arching
    bowing segment from a developing MCV near Medina county back
    toward a strong super-cell feature near Zavala county before
    angling back toward maturing complex of cells along the Serranias
    del Burro west of Maverick county. Surface analysis shows the dry
    line rapidly retreating up the Rio Grande toward the lower Pecos
    therefore shifting all forcing to maintain convection along/ahead
    of the convective outflow. CIRA LPW shows the nose of a very deep
    anomalous moisture surge through the Rio Grande with Sfc-850mb
    values over .75" with supportive 850-500mb helping to support
    1.5"+ totals advected on increasing backed southwesterly flow up
    the river valley.

    A pool of remaining conditionally unstable but slowly capping
    instability with 2500-3000 J/kg of CAPE is also being ingested to
    the line to help support vigorous thunderstorms for a few more
    hours at least. As such, saturating lower profiles should
    maintain some rainfall efficiency with reduction lost to hail
    production with each hour. Given the flux, rates of 2-2.5"/hr are
    probable and likely for the next few hours slowly diminishing with stabilization and slowing intensity of the cold pool/forward flank
    isentropic ascent. Given this though, storm scale
    interactions/collisions become more probable resulting in
    localized intense bursts and spots of 3-4" in 1-2hrs given slowed
    forward progress.=20=20

    While Hi-Res CAMs show quick devolution of the complex, they are
    also reduced in assimilation of coverage/intensity of ongoing
    convective environment, particularly the HRRR which as a tendency
    to rapidly diminish ongoing cells in a stabilizing
    environment...much faster than reality. As such, the threat of
    cells propagating southeast to east-southeast with intense rates
    capable of inducing scattered flash flooding remains possible
    through the early overnight period. across Southwest TX and the
    Rio Grande Valley.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4_DraB7OiQL6fna4_cLnb51Wom-EqPXgPfT_88ddU_mk-6FowF-eSxh6jiL9Ch5d7AaB= JFielt9asX6xpzotL9FJikA$ for graphic product...

    ATTN...WFO...CRP...EWX...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 29569861 29429829 28839804 28299806 27939841=20
    27729899 27679962 27890002 28320045 28630069=20
    28840071 28970050 28900023 29019989 29439959=20
    29549926=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 2 03:02:15 2025
    AWUS01 KWNH 020301
    FFGMPD
    TXZ000-OKZ000-020900-

    Mesoscale Precipitation Discussion 0208
    NWS Weather Prediction Center College Park MD
    1100 PM EDT Thu May 01 2025

    Areas affected...Central & Southern OK...Adj. TX Panhandle and Northwest/Northern TX...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 020300Z - 020900Z

    SUMMARY...Another round of thunderstorms crossing highly saturated
    soil conditions likely to result in scattered flash flooding
    conditions overnight.

    DISCUSSION...A subtle fast moving shortwave enhanced/maintained by
    right entrance jet max across southern KS is providing solid DPVA
    to develop a bowed band of elevated convection racing across the
    northern Texas Panhandle. The overall height-falls from the
    larger scale digging trough seen well in GOES-E WV across the
    northern Central Plains has resulted in rapidly responding LLJ
    across central and eastern TX as VWP has increased to near 50kts
    at DYX and are starting to reach the 30kts at FDR with CIRA LPW
    showing rapid of the SFC-850mb dry slot (with Tds now in the 60s
    and even low 70s) across north-central TX and EML noted in
    850-700mb is reducing/retreating to the west in CIRA LPW.

    This increasing moisture flux at the surface still remains
    easterly in nature, but slow veering is expected through the
    boundary layer in the next few hours. This will start to ascend
    across a well defined deep layer isentropic boundary that bisects
    OK from near the MO/AR intersection south of OKC/Norman toward LTS
    and through the northern Cap Rock from CDS to PVW. While the dry
    air is helping lapse rates and instability profiles initially, the
    increasing moisture flux from the south will eventually increase
    rainfall potential after 07-08z. However, initial thunderstorms,
    even elevated along the front will have sufficient low level flux
    to support 1-1.5"/hr rates in proximity to the boundary. Deep
    layer steering should allow for some training/repeating to further
    enhance rainfall totals before rainfall rates/efficiency is
    expected to increase later.=20

    Normally, 1.5-3" totals would be fine, especially in the expected
    faster moving environment; however, upper soil conditions remain
    highly saturated with 0-40cm ration of 70-75% across much of OK
    and Northwest to Northeast TX which is near record values as NASA
    SPoRT percentiles are in the 98th+ percentile across a vast area,
    with active flooding along many rivers including the Red River and
    nearby tributaries. As such, even though FFG values have
    "rebounded" to 1.5"/hr or 2-2.5"/3hrs, the probability of
    infiltration is very low and nearly all rainfall will be runoff
    and as such, near convective cores, scattered incidents of flash
    flooding are considered likely through the overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9WqZlIY8Blz7NMYSpgkVKo_JrAfbMlEmBmZRzcZ3xesDZYKL8-95bY3h8EA1woY1qK9P= nV4KmHBzQzgnuTUB_w2ZTrY$ for graphic product...

    ATTN...WFO...AMA...FWD...LUB...OUN...TSA...

    ATTN...RFC...ABRFC...NWC...

    LAT...LON 36439613 36209503 35409444 34979458 34139565=20
    33859740 33859965 34210068 35660041 36029814=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 2 08:24:39 2025
    AWUS01 KWNH 020824
    FFGMPD
    ARZ000-TXZ000-OKZ000-021430-

    Mesoscale Precipitation Discussion 0209
    NWS Weather Prediction Center College Park MD
    423 AM EDT Fri May 02 2025

    Areas affected...South-Central & Eastern OK...Far Northern
    TX...Northern AR...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 020830Z - 021430Z

    SUMMARY...Fast moving, but intense cores capable of 1"/15-30
    minutes and localized totals of 2-3.5" crossing saturated ground
    conditions likely to continue scattered flash flooding incidents
    through early morning.

    DISCUSSION...GOES-E 10.3um loop shows expanding cooling complex
    along the Red River in SW OK/NW TX. RADAR mosaic shows a more
    detail to the driving forces, with fast moving S/W almost MCV like
    mid-level circulation across northwest OK with a bowed arch of
    elevated thunderstorms angling southward with some 700mb boundary
    starting to activate west to east downstream of the SW into the
    sharpening right entrance of the 300mb jet. WV suite notes that
    the larger scale main vorticity center is sharpening the overall
    height packing and the jet is starting to accelerate to 100kts.=20
    This is providing solid divergence aloft along and downstream to
    maintain the wave, while simultaneously continuing to keep the
    broad (nearly Texas wide) 40-50kt 850mb low level jet streaming
    northward. Upstream edge is starting to angle/veer more
    southwestward, potentially expanding back-building of the flanking
    line of the developing convective complex near a weak closing
    1007/8mb surface low near KCWC.

    A main surface front continues to bisect the state into NW AR,
    though a subtle either southern stream or wake pressure trof
    exists south of it and south of the Red River connecting to a weak
    low near DEQ and southeast angling surface trof across S AR. Both
    are enhancing surface to boundary layer moisture convergence and
    isentropic ascent, eventually tapping a solid remaining well of
    2000-3000 MUCAPE. While moisture flux into the boundaries
    continues to help pool total moisture to 1.25-1.5", the orthogonal
    ascent and strong convergence is increasing rates to 1.5-2"/hr.=20
    As such, strong thunderstorms will continue to be maintained
    across much of southern OK; however,the veered eastern edge of the
    LLJ is starting to ascend over that southern boundary, utilizing
    the instability axis over central AR and breaking out
    thunderstorms across generally in the vicinity of I-40. Deep
    layer steering through much of the WAA regime may reduce some
    cross track/repeating in the near term, but as the shortwave
    approaches may flatten for increasing repeat/training environment
    as is ongoing across southern OK.

    So with increased duration, spots of 2-3.5" totals are possible
    along the boundaries. This alone is likely to exceed FFG in the
    region, but those values may have rebounded much too quickly given
    other soil saturation signals from NASA SPoRT. 0-40cm ratios
    across most of the area of the MPD are over 70-75%, though the
    lowest areas in central to northeast AR are still well over 60%
    and are above normal with the vast majority of OK, NW and W AR in
    the 90th percentile. As such, limited infiltration suggests that
    much rainfall over saturated grounds and elevated stream flows
    will likely continue flash flooding concerns throughout the late
    overnight through early morning day break.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7lNvr8BhJntG__3RUn8RJdFUjvfug-tIKslsjUN6oGC29oalLF7f7YgyIy1FGBe5pY1H= lcGZZIGPrK2ixThaOUvGSKw$ for graphic product...

    ATTN...WFO...FWD...LZK...MEG...OUN...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 36439462 36389273 36149122 35759043 35489020=20
    35009038 34629092 34449164 34459321 34359444=20
    33469635 33389821 33929857 35189715 36059633=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 2 18:11:00 2025
    AWUS01 KWNH 021810
    FFGMPD
    LAZ000-TXZ000-030000-

    Mesoscale Precipitation Discussion 0210
    NWS Weather Prediction Center College Park MD
    209 PM EDT Fri May 02 2025

    Areas affected...portions of central and eastern TX through
    western LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 021800Z - 030000Z

    Summary...Convection will continue to proliferate this afternoon,
    likely resulting in scattered totals of 3-5" (and locally higher)
    through the evening. Scattered to numerous instances of flash
    flooding are possible, and may be locally significant in more
    sensitive terrain and metro areas.

    Discussion...Convection is beginning to proliferate across
    portions of eastern TX, as 20-30 kts of southerly to southeasterly
    low-level (925-850 mb) moisture transport combines with relatively
    moist, cool air aloft (700-500 mb) originating from convection
    over the northern Sierra Madre Oriental range yesterday (as is
    clear from CIRA advected layered precipitable water imagery).
    While this region just north and east of the Houston metro area is
    the current core of the highest moisture content (PWATs near 1.8",
    per SPC's SFCOA analysis, which is well above the 90th percentile
    per LCH sounding climatology), the broader region from the Heart
    of TX northeastward to the Ark-La-Tex is characterized by PWATs of
    1.4-1.8", SB CAPE of 2000-4500 J/kg (with a tight gradient along
    the northern extent due to relatively stable outflow from an MCS
    near the Red River of the South overnight), and effective bulk
    shear of 25-40 kts. Shear is resulting from a dual jet structure
    that is somewhat phased, providing ample divergence aloft within
    the left-exit region of a subtropical jet streak (near the
    TX/Mexico border) and on the outer periphery of a right-entrance
    region of a polar jet streak (centered over the Great Lakes).

    Convection is anticipated to continue to proliferate, likely
    growing upscale to the north and west as the afternoon progresses.
    Relatively broad surface to low-level convergence should become
    more defined over time, reinforced by the aforementioned outflow
    sagging south (along with a quasi-stationary front lagging just
    behind with additional ongoing convection inbetween). Recent
    hi-res guidance (12z HREF suite) is in rather good agreement
    concerning the potential for excessive rainfall, indicating
    relatively high odds (40-70%) for localized 3" exceedance and
    somewhat elevated odds (15-25%) for localized 5" exceedance (per
    12z HREF 40-km neighborhood exceedance probabilities). Subsequent
    HRRR and experimental RRFS hourly runs (since 12z) support the
    earlier ensemble guidance, consistently indicating the potental
    for 6"+ localized totals over the next 6 hours (through 00z).

    While scattered 3-5" totals (with locally higher amounts) are
    likely, corresponding Flash Flood Guidance (over a 3-6 hour
    period) largely encompasses the same range (3.0-5.0"). This
    suggests that scattered to numerous instances of flash flooding
    are possible (though not guarenteed). The situation is more
    concerning for sensitive terrain, including eastern portions of
    the TX Hill Country into the Heart of TX (including the San
    Antonio and Austin metro areas) where FFGs are as low as 2.0-3.0",
    and perhaps most concerning for portions of the Houston/Galveston
    metro into the Golden Triangle region of southeast TX (where HREF
    exceedance probs are maximized). Should higher totals occur over
    more sensitive areas, significant to life threatening flash
    flooding is possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7QYwxzKqJcY2TZlclXwM356aOX_msIpb5Ij50AkD2-sotN2-OdcFdTLwnvJz50ar27kq= V7CUrfHpcQqC1UHMUPhz5Lc$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...LCH...SHV...SJT...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 32889352 32289295 31439295 30139323 29739402=20
    29369579 29069721 29449899 30889914 31409846=20
    31579720 31959577 32289510 32609454=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 2 18:40:12 2025
    AWUS01 KWNH 021839
    FFGMPD
    TNZ000-ALZ000-MSZ000-LAZ000-ARZ000-030037-

    Mesoscale Precipitation Discussion 0211
    NWS Weather Prediction Center College Park MD
    238 PM EDT Fri May 02 2025

    Areas affected...Portions of the Lower MS Valley and Mid-South

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 021837Z - 030037Z

    SUMMARY...Showers and thunderstorms with heavy rainfall rates will
    be capable of producing isolated to widely scattered areas of
    flash flooding this afternoon and evening.

    DISCUSSION...A low-amplitude shortwave trough traversing portions
    of the lower OH Valley and Mid-South will be interacting with a
    moist and unstable airmass pooling along and just ahead of a
    frontal zone and will be favoring an expansion of heavy showers
    and thunderstorms over the next several hours.

    MLCAPE values of 1500 to 2500 J/kg are in place across northern LA
    through through northern MS/AL and into middle TN. Coinciding with
    this is as much as 30 to 40 kts of effective bulk shear, and this
    should yield a combination of multicell and occasional supercell
    convection. Given the moist environment with PWs approaching and
    locally exceeding 1.5 inches, and organized character of the
    convection, the rainfall rates should be rather high and capable
    of reaching 1.5 to 2 inches/hour.

    Some cell-merger activity is expected as the convection evolves
    over the next several hours, with multiple convective clusters
    likely materializing by this evening. Colliding outflow boundaries
    will be a facilitator of this as well. This coupled with locally
    slow cell-motions in general may allow for some of the rainfall
    totals to reach as high as 2 to 4+ inches, and this is consistent
    with a consensus of the latest hires model guidance.

    Given the relatively moist antecedent conditions and high rainfall
    rates, there a concern for isolated to widely scattered areas of
    flash flooding. The bigger concern generally will be for the more
    sensitive urbanized locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-xmxM_9lHwfIZTHzCYDF5q8hzCyses-xFYtMIq6SWKBkM4mhUm3IUjQUJzujEHRMoUHz= 1UmjpAwyNgvM7_sv_qvutT0$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LCH...LZK...MEG...MRX...OHX...
    SHV...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36488617 36328520 35598491 34718610 33938733=20
    32828936 31869089 30979224 30899295 31869279=20
    32709305 33089270 33989115 34808968 35608826=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 3 00:01:50 2025
    AWUS01 KWNH 030001
    FFGMPD
    LAZ000-TXZ000-030600-

    Mesoscale Precipitation Discussion 0212
    NWS Weather Prediction Center College Park MD
    800 PM EDT Fri May 02 2025

    Areas affected...Portions of South-Central and Southeast
    TX...Southwest LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 030000Z - 030600Z

    SUMMARY...Locally heavy showers and thunderstorms will continue
    through the evening hours. Additional scattered areas of flash
    flooding will continue to be possible where slow cell-motions and
    cell-mergers yield enhanced rainfall totals.

    DISCUSSION...The early-evening GOES-IR satellite imagery along
    with dual-pol radar shows broken areas of heavy showers and
    thunderstorms focusing along and just ahead of a slow-moving cold
    front settling down across south-central to southeast TX.

    Over the last couple of hours, there has been a trend toward
    locally more organized convection and colder cloud tops in a
    broken fashion from near Del Rio eastward to the southern suburbs
    of the Austin metropolitan area. Meanwhile, farther east into the
    southeast TX coastal plain and adjacent areas of southwest LA,
    clusters of convection continue to persist here while slowly
    advancing eastward.

    A substantial pool of instability is pooled across much of
    southern TX in close proximity to the front with MLCAPE values of
    2500 to 3500 J/kg in place along with about 40 to 50 kts of
    effective bulk shear. This coupled with at least modest low-level
    south to southeast flow into the front should sustain the
    convective threat going through the evening hours.

    Slow cell-motions and cell-merger activity will continue to be a
    short-term concern which given the moist/unstable environment
    should continue to support rainfall rates of up to 2 inches/hour.

    Additional rainfall amounts through the evening hours may reach as
    high as 2 to 4 inches with isolated heavier totals. This will
    continue to promote additional concerns for scattered areas of
    flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5uDo8rnc5HSgBUjKVpkyiGFwAHlzbYEKBespbsu5NCWDanJx3joHSagtJnBF9DbcLaQA= U8RjJmxWZDrqSJGzX6ZjqFI$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...LCH...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 31369425 31349316 30799235 29999275 29629423=20
    28949612 28459847 28540037 29440139 29900117=20
    30099909 30569712 31099543=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 3 02:29:02 2025
    AWUS01 KWNH 030227
    FFGMPD
    ALZ000-MSZ000-LAZ000-030830-

    Mesoscale Precipitation Discussion 0213
    NWS Weather Prediction Center College Park MD
    1026 PM EDT Fri May 02 2025

    Areas affected...Southeast LA...Southern MS...Southwest AL...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 030230Z - 030830Z

    SUMMARY...A few clusters of stronger thunderstorms with localized
    storm mergers/interactions to increase localized spot totals to
    2-3" and low-end possible flash flooding with increased potential
    magnitude if intersecting larger urban areas.

    DISCUSSION...GOES-E WV suite shows broad, strong southwesterly
    upper-level flow across Texas into the Southeast and eastern Ohio
    Valley along/ahead of stron closed low in the Central Plains.=20
    Embedded within it are a few stronger southern stream shortwave
    features enhanced/maintained by right entrance jet ascent
    patterns. One in particular exists across north-central MS moving
    quickly northeast; it is within the wake of another exiting across
    the Cumberland Plateau. This has resulted in low level convective
    activity to have bowed out eastward across N AL now starting to
    move quickly across N GA into the southern Appalachians. The tail
    end, under influence of the MS wave has angled back westward and
    is acting as an effective warm front from pre-frontal
    southwesterly flow and strengthening warm advection regime. As
    such, increased istentropic ascent of moderately unstable and
    moist air denoted by 1500 MLCAPE and 1.25-1.5" slug of enhanced
    moisture. As such a cluster of enhanced cooling tops can be seen
    over west-central AL. This cluster is slowly propagating eastward
    in a col in steering flow. This is likely to increase duration and
    storm scale interaction/mergers over the next few hours. With
    occasional rates of 1.5-1.75", localized totals of 2-3" are
    probable and may result in localized FF given the locally lower
    FFG values in the area.

    Southwestward across southern MS/LA... the fast moving shortwave
    across central MS has been resulting in increased height-falls and southeastward propagation of the active convective/effective
    pre-frontal convergence line. New activity continues to grow and
    cool within 10.3um GOES-E IR loop from eastern MS back to central
    LA where orientation once again begins to be more flat,
    east-northeast to west-southwest. Still, strong convergence and
    increased deep layer moisture up to 1.75" may allow for very
    intense downdrafts with spots of sub-hourly 1.5-2" as the line
    advances southeastward. FFG values are quite high and unless
    these cells traverse the larger urban centers across I-10/12,
    flash flooding will be less likely, but still non-zero through the
    overnight period.

    Of increasing interest is the MS and AL coastal counties, mainly
    after 06z, but a few cells have already begun to develop in the
    vicinity of far SE LA. CIRA LPW, particularly in the sfc to 850mb
    layer shows a narrow but strongly enhanced axis of moisture that
    can be traces along the western edge of a recent sub-tropical
    ridge as return flow from the Northern Caribbean tropical moisture
    source. This can be tracks through 850-700mb and totals are
    1.5-1.7" with a recent uptick as the return flow becomes
    convergent/confluent on the northwest edge of the sub-tropical
    ridge axis. This convergence into the southwesterly flow ahead of
    the approaching trof, further taps the higher theta-E of the Gulf
    too, with WAA development. This is expected to expand/rapidly
    develop near the diurnal peak of convection near 07-09z,
    intersecting with the approaching line from the northwest.=20
    Overall totals prior to 09z may not be significant, yet (likely
    peaking after 09z) the start in proximity to the coastal urban
    centers still may pose low end flash flooding and trends will be
    watched closely for subsequent MPD(s).

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_PtIFxtChj7ZM32_ZWkvIg7m0J5uetM8VXZZqRd2RzAQ5aOWSGfU4LucLousGT6atZ-9= sFQfxGIc6puhbwkrWCwofPo$ for graphic product...

    ATTN...WFO...BMX...JAN...LCH...LIX...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 33648696 33388651 33028634 32018679 31268750=20
    30308795 30208896 29828951 29789068 29959182=20
    30379235 31029202 31529096 32178988 32938889=20
    33488795 33638745=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 3 07:36:12 2025
    AWUS01 KWNH 030736
    FFGMPD
    FLZ000-ALZ000-031300-

    Mesoscale Precipitation Discussion 0214
    NWS Weather Prediction Center College Park MD
    335 AM EDT Sat May 03 2025

    Areas affected...Coastal Alabama...Western Panhandle of Florida...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 030735Z - 031300Z

    SUMMARY...Slow moving/stationary coastal thunderstorms to be swept
    up from west to east through early morning with main pre-frontal
    convective line. Highly localized 2-4" totals are possible in
    proximity to urban centers posing possible rapid inundation
    flooding.

    DISCUSSION...Regional RADAR mosaic depicts a mature convective
    line with a few bowing segments continuing to march southeastward
    across southwest AL into far southeast LA with strong
    meso-high/cold pool helping its advancement. A weak surface wave
    appears to have formed in proximity to southern MS, which seems
    plausible given strength of onshore southerly to southwesterly
    flow. Strong frictional convergence at the coast at the nose of
    an enhanced but narrow moisture plume from the mouth of the MS
    river turning more southwest to northeast toward the AL/W FL
    coastline continues to feed an expanding (eastward) convective
    line at the coast. Surface to 700mb moisture per CIRA LPW show
    values of 1.5 to 1.7" being fed by 15-25kts of flow. Warm Gulf
    air in the upper 70s to low 80s and modest steepening lapse rates
    support solid 1500-2000 J/kg of MLCAPE to maintain the stronger
    updrafts. The combination supports cells capable of 1.5-2"/hr
    along the warm advective/frictionally forced cells. While
    pre-frontal convective line is advancing sweeping up/merging along
    the way, this should result in 2-3 hours of solid rainfall prior
    to the main line sweeping through. As such, localized totals of
    3-4" are possible.=20=20

    There is a potential factor that may limit flooding impact that
    would be related to strength of cold pools from initial convection
    pressing outflow boundaries off-shore resulting in best
    convergence and downdrafts to be also offshore. Current trends
    suggest this is occurring more upstream and nearer the mixing of
    the EML downward with the main-line convection. So while the
    soils are very sandy and likely to support solid infiltration, the
    vast urban locations along I-10 from Mobile to Panama City will
    have large impermeable surfaces even up to the shoreline; and as
    such rapid inundation flooding may be possible over the next
    4-6hrs as the main line sweeps through.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-g3JI-d4aOcymSOaieVA6ljwjuWfKKzRO67QyiKkQC3TvB13PzyEWFyW698RGPQffEOd= hJB_C7K0DcwjEW_l83dHHJk$ for graphic product...

    ATTN...WFO...MOB...TAE...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 31008721 30998635 30908573 30268593 30328644=20
    30298699 30218751 30248828 30878832 30998805=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 3 18:49:19 2025
    AWUS01 KWNH 031849
    FFGMPD
    NCZ000-GAZ000-TNZ000-KYZ000-ALZ000-MSZ000-040048-

    Mesoscale Precipitation Discussion 0215
    NWS Weather Prediction Center College Park MD
    248 PM EDT Sat May 03 2025

    Areas affected...Portions of the TN Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 031848Z - 040048Z

    SUMMARY...Bands of heavy showers and thunderstorms will be
    impacting portions of the TN Valley going through the afternoon
    and evening hours. Some localized potential for flash flooding
    will exist where the stronger and more organized storms occur, and
    especially with somewhat moist antecedent conditions.

    DISCUSSION...The early afternoon GOES-E visible satellite imagery
    shows convection developing and expanding in coverage across areas
    of eastern MS up through northern AL and into middle TN. Despite
    some cloud cover which has tempered the boundary layer
    destabilization process, there has been a sufficient level of
    diurnal heating to foster MLCAPE values of near 1000 J/kg across
    eastern MS and into northern AL, with lesser values noted up
    across middle TN.

    A cold front meanwhile continues to edge off to the east as a
    deeper layer trough and closed low pivots across the middle MS and
    lower OH Valley region. The pooling of moisture and instability
    ahead of this front this afternoon and evening should continue to
    favor a general increase in the coverage of convection, although
    the activity should tend to be oriented in linear bands aligned
    with the deeper layer southwest flow across the broader TN Valley
    region.

    Additional boundary layer instability through solar insolation
    coupled with fairly strong moisture convergence near the front
    should help yield pockets of heavier rainfall rate potential that
    may reach as high as 1 to 2 inches/hour. PWs are seasonably moist
    with values of 1.2 to 1.4 inches and there is a sufficient level
    effective bulk shear (30 to 40 kts) to favor some level of
    stronger updrafts/organization for some of these heavier rainfall
    rates to materialize.

    Hires model solutions generally favor as much as 2 to 4 inches of
    rain with the stronger storms and where any brief cell-training
    occurs given the linear nature of the convection. Some localized
    1-hour and 3-hour FFG exceedance may occur as a result, and some
    locations over the broader TN Valley region did see heavy rainfall
    yesterday which has led to some moistening of the soils along with
    higher streamflows. As a result, some localized potential for
    flash flooding will exist going through the afternoon and evening
    hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7EtQmXZXqbXR8RUP2LHqsVL0HqYhd2s2e84_W4kNxEHm-KM7VjZWFeZZPBRNpRDWthBE= n93eO-qD7O1_3LEHfi4YQVI$ for graphic product...

    ATTN...WFO...BMX...FFC...GSP...HUN...JAN...JKL...LMK...MEG... MOB...MRX...OHX...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36798491 36768379 36238345 35048410 33338559=20
    32598673 32248813 32508895 33188908 34398750=20
    36038601=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 4 18:21:44 2025
    AWUS01 KWNH 041820
    FFGMPD
    NYZ000-NJZ000-PAZ000-042320-

    Mesoscale Precipitation Discussion 0216
    NWS Weather Prediction Center College Park MD
    220 PM EDT Sun May 04 2025

    Areas affected...Northeast PA...Northwest NJ...Southeast NY

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041820Z - 042320Z

    SUMMARY...Some concentrations of showers and thunderstorms are
    expected this afternoon across areas of northeast PA, northwest NJ
    and into adjacent areas of southeast NY. Persistence of locally
    heavy rainfall rates may be enough to cause some areas of flash
    flooding.

    DISCUSSION...The large scale pattern across the Eastern U.S.
    features a deep layer cyclone over the OH Valley with an occluded
    surface low structure and a stationary front that extends east
    across central to eastern PA and into southern New England. A
    relatively deep warm/moist conveyor belt is noted along the East
    Coast with an axis of 1.25 to 1.5 inch PWs oriented south to north
    from the Delmarva up across eastern PA and much of NJ.

    Cloud cover so far today has been keeping boundary layer
    instability limited, but there is a pool of MUCAPE values on the
    order of 1000 J/kg which is being aided by a southerly low-level
    jet of 20 to 30 kts and the broader warm advection regime along
    the East Coast. As it is, this coupled with convergent flow into
    the aforementioned frontal zone along with some orographic ascent
    over the higher terrain has been yielding some recent uptick and
    expansion of heavier shower activity.

    Some modest shear is noted across the region which coupled with
    some additional uptick in boundary layer instability should favor
    the potential for some additional convective expansion with some
    increase in thunderstorm activity. The latest CIRA-ALPW data shows
    rather concentrated moisture in the 850/500 mb layer and this
    should tend to favor greater rainfall efficiency with the
    convective cells that evolve this afternoon.

    Rainfall rates may reach as high as 1.5"/hour with the stronger
    convective elements and there may be some localized
    persistence/training of these cells that yield some rainfall
    totals of 2 to 4 inches. Some of the rainfall across parts of
    northeast PA, northwest NJ and southeast NY over the last 12 to 24
    hours has at least started the process of moistening up the soil
    conditions somewhat despite very dry longer-term antecedent
    conditions. The rainfall this afternoon near especially some of
    the higher terrain may be enough to encourage some runoff problems
    with a threat for some areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7KOm-wGo_pfx8zDm3qfj2ktRqMErXDH34y1a5qtT_hxYPnt7351SJSgdcHuQ0bce5Jle= x8gKX-mMNmDDL_eLMAEbYbY$ for graphic product...

    ATTN...WFO...ALY...BGM...CTP...OKX...PHI...

    ATTN...RFC...MARFC...NERFC...NWC...

    LAT...LON 42537392 42337345 41687359 41017412 40527492=20
    40667587 41187574 42197480=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 4 18:34:33 2025
    AWUS01 KWNH 041834
    FFGMPD
    TXZ000-NMZ000-050030-

    Mesoscale Precipitation Discussion 0217
    NWS Weather Prediction Center College Park MD
    233 PM EDT Sun May 04 2025

    Areas affected...southeast and central NM and adjacent portions of
    TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041830Z - 050030Z

    Summary...Increasing shower and thunderstorm coverage will likely
    result in localized rainfall rates of 1-2"/hr with 3-6 hour totals
    up to 2-3". Isolated instances of flash flooding are possible.

    Discussion...A deep layer (700-200 mb) closed low is very slowly
    shifting southeastward over Southern CA, southwestern AZ, and far
    northwestern Mexico. An associated phased jet streak (~110 kts @
    200 mb) is progged to shift rapidly northeastward into southwest
    NM over the next several hours in association with DPVA from the
    aforementioned closed low, providing ample lift via divergence and
    diffluence within the idealized left-exit region of the jet streak
    over portions of southwestern NM by 21z. Additionally, an
    impressive pool of instability (SBCAPE of 1000-2500 J/kg) has
    built to the south over the past several hours, centered over far
    West TX (though 500-1000 J/kg has already built farther north as
    well). PWATs are a bit less impressive, ranging from 0.5-0.8"
    (still well below the typical PWAT during the height of the
    monsoon season, though highly anomalous for early May as indicated
    by ELP sounding climatology around the 90th perentile), though
    modest low-level moisture transport (via 20-25 kt LLJ @ 925-850
    mb) could bring PWATs to as high as 1.0" (near record daily values
    at ELP).

    Hi-res CAMs are in good agreement concerning the development of
    convection this afternoon, and some deeper convective cells are
    already starting to develop prior to 18z. Given the presence of
    equally anomalous effective bulk shear (30-40 kts, near the 90th
    percentile), convection is expected to become organized into
    discrete and semi-discrete clusters with localized rainfall rates
    expected to reach 1-2"/hr (particularly with any supercells that
    develop). Storm motions near 20 kts should generally limit
    residence time over any one location, though limited backbuilding
    (particularly just north and downwind of the Sacramento Mountains
    where convergence is locally enhanced from differential heating)
    may result in localized 3-6 hour totals of 2-3". These expected
    isolated totals are near the associated FFGs (at 1, 3, and 6 hour
    intervals), and sub-hourly (15-min) totals as high as 0.50-0.75"
    (as indicated by the HRRR) may also drive a localized flash flood
    threat with the limited infiltration ability of dry desert soils.
    Isolated instances of flash flooding are possible, particularly in
    sensitive or low-lying areas (such as burn scars and dry washes).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_96BeVrpUQgP00lQgyqFLiW0XBUkP_rVpXQxloVljj3MsYXTZp3VkJt4x7DPo3uaH0UY= dk5ROzugEYwaHl-qS8sDaxU$ for graphic product...

    ATTN...WFO...ABQ...EPZ...LUB...MAF...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36330501 36210418 35490367 35130330 34390300=20
    33670286 32470277 31580311 31590475 32520548=20
    33100610 33780693 35500690 36200635=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 4 19:04:10 2025
    AWUS01 KWNH 041902
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-050100-

    Mesoscale Precipitation Discussion 0218
    NWS Weather Prediction Center College Park MD
    301 PM EDT Sun May 04 2025

    Areas affected...Portions of Eastern CA...Northwest AZ...Southern
    NV

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041900Z - 050100Z

    SUMMARY...Scattered slow-moving showers and thunderstorms across
    portions of eastern CA, northwest AZ and southern NV today will
    pose a concern for isolated pockets of flash flooding.

    DISCUSSION...The midday GOES-W WV suite shows a rather anomalous
    deep layer trough/closed over the Southwest U.S. which is forecast
    to move very slowly off to the east this afternoon. Cold 700/500
    mb temperatures are promoting steeper mid-level lapse rates and
    this coupled with strong boundary layer heating via solar
    insolation is already contributing to MLCAPE values of 500 to 1000
    J/kg.

    GOES-W visible satellite imagery meanwhile already shows areas of
    shower and thunderstorm activity developing and expanding over
    some of the higher terrain and adjacent deserts with some of the
    more notable cells situated over northwest AZ and edging into
    southern NV around the northeast flank of the mid-level closed
    low. Somewhat stronger southeast flow/shear across these areas is
    seen in the latest RAP analysis, and these stronger wind fields
    may tend to promote somewhat strong cellular organization.

    The PW environment for this time of the year is rather anomalous
    with PWs of locally 0.7 to 0.9 inches and this is 2 to 3 standard
    deviations above normal. Much of the moisture concentration is in
    the mid-levels of the column, but with the available instability
    and persistence of these convective cells, there may be some
    convective cells that are capable of producing rainfall rates of
    up to 1.0 to 1.25 inches/hour. Much of this rain could fall in as
    little as 30 minutes with the stronger and more organized cells.

    The 12Z HREF guidance led especially by the NAM-conest supports
    these rainfall rates, with some storm total potential of up to 2
    inches going through this afternoon. As a result, a few isolated
    areas of runoff concerns and flash flooding cannot be ruled out.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7jsiFueUTM6zjTVBmvw0DaP6LwTHPxG1dHOmvlEnixt8AkRL0OXuFNUj85eqFLqLP1Sq= A56ADuquhbcmY7-hTskCEiQ$ for graphic product...

    ATTN...WFO...FGZ...PSR...SGX...SLC...VEF...

    ATTN...RFC...CBRFC...CNRFC...NWC...

    LAT...LON 37331443 36921363 35781303 34501328 33751401=20
    33401505 33331636 33991687 34581624 35501580=20
    36381593 37121557=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 4 19:11:04 2025
    AWUS01 KWNH 041910
    FFGMPD
    FLZ000-042300-

    Mesoscale Precipitation Discussion 0219
    NWS Weather Prediction Center College Park MD
    309 PM EDT Sun May 04 2025

    Areas affected...Southeast Mainland FL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041905Z - 042300Z

    Summary...Localized training of 1-3"/hr rainfall rates may result
    in isolated 5"+ totals over the next several hours. Localized
    flash flooding is possible.

    Discussion...Deep convection has initiated over the past couple of
    hours over southeast FL, spurred by enhanced moisture convergence
    at the surface from southeasterly (onshore) flow from the Atlantic
    and rain cooled outflow from an earlier low of convection to the
    west. The mesoscale environment is characterized by SBCAPE of
    2000-2500 J/kg, PWATs of 1.7-1.9" (near the 90th percentile, per
    MFL sounding climatology), and deep layer shear of 30 kts (near
    the 75th percentile). Given recent observational trends, limited backbuilding/training appears possible in the vicinity of the
    Miami and Ft Lauderdale metro areas, with MRMS indicating hourly
    rates/totals of 1-3" with the stronger convective cells. Given the
    increasingly favorable mesoscale environment and very supportive
    parameter space (with hi-res CAMs also signaling the potential for
    localized 5" exceedance with 12z HREF 40-km neighborhood
    probabilities of 15%), localized flash flooding is possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_BxV9E0Zx5b-4QINBiGrDg0fdeq-fGqPxtsyIcZ1C-y6silZ_0rR3fwJ2r_rWOlwaZXR= ymgz02oltPbts1kiTqZPYL8$ for graphic product...

    ATTN...WFO...KEY...MFL...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 26568033 26557988 25797993 25188024 25568066=20
    25998045 26448048=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 4 23:04:37 2025
    AWUS01 KWNH 042304
    FFGMPD
    MEZ000-MAZ000-NHZ000-VTZ000-CTZ000-NYZ000-NJZ000-PAZ000-050502-

    Mesoscale Precipitation Discussion 0220
    NWS Weather Prediction Center College Park MD
    702 PM EDT Sun May 04 2025

    Areas affected...Northeast PA...Central to Southeast NY...Portions
    of Southern New England

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 042302Z - 050502Z

    SUMMARY...Concentrations of heavy and slow-moving showers will
    continue into the evening hours across portions of northeast PA,
    central to southeast NY and parts of southern New England. A
    threat for some flash flooding will continue given localized
    persistence of some of the heavier showers.

    DISCUSSION...Generally no change to the earlier MPD reasoning
    across the region. The large scale pattern across the Eastern U.S.
    features a deep layer cyclone over the OH Valley with an occluded
    surface low structure and a stationary front that extends east
    across central to eastern PA and into southern New England. A
    rather deep warm/moist conveyor belt continues to only slowly
    shift eastward with time along the East Coast, but continues to
    channel an axis of 1.25 to 1.5 inch PWs northward up toward areas
    of the northern Mid-Atlantic and southern New England.

    Radar imagery shows an area of slow-moving but locally heavy
    shower activity impacting areas of northeast PA through parts of
    central and southeast NY where recently there has been some
    rainfall rates reaching upwards of 1 to 1.5 inches/hour based on
    MRMS data. Meanwhile, with aid of the broader warm air advection
    regime, an axis of locally heavy rainfall is also noted from
    eastern NY over into far northwest MA, southern VT and southern
    NH. Much of the rainfall in general across the region is being
    aided by a combination of frontogenetical forcing and elevated
    instability. The best instability is along the front itself with
    areas of central and eastern PA seeing MUCAPE values of 500 to
    1000 J/kg.

    Some persistence of locally heavy shower activity with some
    cell-training concerns will continue into the evening hours across
    the region with rainfall rates still capable of reaching 1 to 1.5
    inches/hour where stronger convective elements near the front
    materialize. Some additional rainfall amounts of 2 to 3 inches
    will be possible locally. As a result, some additional localized
    runoff problems and flash flooding will be possible.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6ULHUzrxS2td6LtE2y5M5QBgytxA_aZ4B9cbbIBmnTpwPyYEe03qtSjl4qkavv5we0Y2= mnwA_ZlaGyXMv7DguogPcM0$ for graphic product...

    ATTN...WFO...ALY...BGM...BOX...BTV...GYX...OKX...PHI...

    ATTN...RFC...MARFC...NERFC...NWC...

    LAT...LON 43517287 43507113 43117078 42667137 42447252=20
    41417381 41147528 41367594 42057599 43007480=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 4 23:39:37 2025
    AWUS01 KWNH 042339
    FFGMPD
    PAZ000-MDZ000-WVZ000-OHZ000-050437-

    Mesoscale Precipitation Discussion 0221
    NWS Weather Prediction Center College Park MD
    738 PM EDT Sun May 04 2025

    Areas affected...Portions of Northern WV...Western PA...Far
    Northeast OH

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 042337Z - 050437Z

    SUMMARY...A couple of bands of slow-moving, but heavy showers and
    thunderstorms may result in a few localized areas of flash
    flooding through the early to mid-evening hours.

    DISCUSSION...The latest radar imagery shows a couple of bands of
    heavier showers and thunderstorms materializing across northern WV
    and western PA as a pool of late-day instability remains focused
    near a very slow-moving frontal occlusion. This is all associated
    with the deep layer cyclone pivoting slowly across the OH Valley.

    RAP data shows a corridor of favorable low-level moisture
    convergence along the frontal occlusion coinciding with as much as
    1000 J/kg of MLCAPE. Relatively divergent flow aloft around the
    northeast quadrant of the deep layer trough/closed low over the OH
    Valley is also yielding at least some modest deep layer ascent.

    GOES-E IR satellite data has been showing some additional
    convective cloud top cooling over the last 30 to 45 minutes and
    this has been coinciding with MRMS data showing some increase in
    rainfall rates, with some of the stronger storms yielding rates up
    to close to 1 inch/hour.

    Over the next few hours, expect a couple of relatively slow-moving
    bands of convection to continue to pivot across portions of
    northern WV, western PA and possibly getting into far northeast OH
    with at least some brief cell-training concerns that could yield
    rainfall totals upwards 1.5 to 2.5 inches. This may be enough to
    exceed the 1-hour and 3-hour FFG values locally. Therefore, a few
    localized areas of runoff problems and flash flooding will be
    possible.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6EO--QMCXgH_LExtfV52mbSZRtA2FBJENwRVtK14jMGtf7HZJtWIONfT_AUnD6hcoUwn= pBTKWafbITuQUixMqJBH79M$ for graphic product...

    ATTN...WFO...CLE...CTP...LWX...PBZ...RLX...

    ATTN...RFC...MARFC...OHRFC...NWC...

    LAT...LON 41938036 41567967 40667912 39277940 38837986=20
    38948031 39348035 40188042 40988069 41468110=20
    41908097=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 5 00:31:07 2025
    AWUS01 KWNH 050031
    FFGMPD
    TXZ000-COZ000-NMZ000-050630-

    Mesoscale Precipitation Discussion 0222
    NWS Weather Prediction Center College Park MD
    830 PM EDT Sun May 04 2025

    Areas affected...Central and Eastern NM...Portions of the Western
    TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 050030Z - 050630Z

    SUMMARY...Clusters of showers and thunderstorms will continue
    through the evening hours across areas of central and eastern NM
    and edging out into parts of western TX. Heavy rainfall rates will
    continue to promote a concern for widely scattered areas of flash
    flooding.

    DISCUSSION...The late-day GOES-E IR satellite imagery shows
    several broken clusters of heavy showers and thunderstorms with
    cold convective tops impacting areas central and eastern NM into
    parts of far western TX.

    There continues to be as much as 1000+ J/kg of MUCAPE pooled
    across much of central to southeast NM which coupled with
    relatively moist low-level southeast flow should tend to maintain
    the convective threat well through the evening hours. Divergent
    flow aloft associated with left-exit region upper-level jet
    dynamics downstream of an upper trough/closed low over the
    Southwest is also yielding a corridor of deeper layer ascent for
    more sustainable clusters of convection.

    Rainfall rates with the stronger convective cells should continue
    to be on the order of 1 to 1.5 inches/hour over the next several
    hours, with some localized orographic ascent/upslope flow over the
    higher terrain favoring some of these higher rates.

    A combination of some cell-mergers and cell-training may foster
    some storm total amounts of as much as 2 to 4 inches which is
    generally favored by a consensus of the latest hires model
    guidance. This may result in some additional widely scattered
    areas of flash flooding which may occur near some locally
    sensitive burn scar locations or dry washes.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5FRLX6G8TlwU2vn9xR9JQFRAdj6CCr6qotUODNkSbsXMdAwk7Ddb2ePPECIIb6dyV_uM= yC4AKcc7Cl9VjSLhRF_B4H0$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...MAF...PUB...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 37110471 36770348 35520268 33950207 32790196=20
    31890254 31730357 32220446 32920496 34270577=20
    35150681 36220683 36870611=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 5 02:22:20 2025
    AWUS01 KWNH 050221
    FFGMPD
    AZZ000-050730-

    Mesoscale Precipitation Discussion 0223
    NWS Weather Prediction Center College Park MD
    1020 PM EDT Sun May 04 2025

    Areas affected...Southwest to south-central Arizona...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 050220Z - 050730Z

    SUMMARY...Very narrow updrafts in proximity to anomalously
    deep/moist upper-low will remain slow moving for highly focused
    areas of .75-1.5" totals and possible flash flooding.

    DISCUSSION...GOES-W WV suite and 00z RAOB analysis depicts a
    fairly stacked anomalously deep (2.5-3.5 Std. Dev.) upper low
    centered just west of the Lower Colorado River northeast of
    Blythe. Similarly atypical moisture values exist though the deep
    low with total PWats of .75-1". RAP analysis denotes the slow
    downward trend/loss of unstable air (given loss of solar
    insolation), but an axis of steeper mid-level lapse rates but
    solid upper-40s to low 50s Tds exists across the Sonoran Desert
    toward Sun Valley and the western edges of the Mogollon Rim.=20
    General, southwest to southerly confluence in the low to
    mid-levels is providing sufficient convergence to result in some
    new destabilization/convective development in that axis from east
    of Yuma toward central Maricopa into southwest Yavapai county.=20
    The limited 500-750 J/kg CAPE and modest, even if anomalous,
    moisture is resulting in narrow updraft/downdraft cores.

    The key toward intense rain-rates and excessive rainfall potential
    is the orientation to a steering flow col within that SW-ENE
    confluence zone as the upper-low slowly wobbles/re-forms eastward.
    As such, 15-20kts of cloud base in flow of increasing moisture
    should support increased duration of .5-.75"/hr rates potentially
    resulting in localized totals up to 1.5". Given desert/hard-pan
    ground conditions, highly focused flash flooding may result and is
    considered possible through the next few hours as the cells
    exhaust/seek out the remaining instability patches.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6MnkT-lixCg6lOMDSJq5brlZIqLWIPPYF_ZtxhQYEnj5JwRO6bQJwH1PSwwCY7LRCwIr= leYeWfe0DITiCv8F0SSbX5g$ for graphic product...

    ATTN...WFO...FGZ...PSR...TWC...VEF...

    ATTN...RFC...CBRFC...NWC...

    LAT...LON 34951338 34831238 34271126 33721115 32941162=20
    32321235 31841298 32131404 32401446 32951423=20
    33421390 33631383 34521396=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 5 07:22:15 2025
    AWUS01 KWNH 050720
    FFGMPD
    TXZ000-NMZ000-051300-

    Mesoscale Precipitation Discussion 0224
    NWS Weather Prediction Center College Park MD
    319 AM EDT Mon May 05 2025

    Areas affected...Northern & Eastern New Mexico...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 050720Z - 051300Z

    SUMMARY...Continued risk of regenerative thunderstorms along the dryline/surface front. Deep layer steering may support
    training/repeating locally for streaks of 2-3" totals and possible

    DISCUSSION...GOES WV suite depicts very deep (3-3.5 Std. Dev.)
    closed low generally centered in the Lower Colorado River Valley
    and is currently reorienting as very strong shortwave energy
    rotates around the western to southwestern edge of current center.
    This is elongating the overall low favorably across eastern AZ
    into much of NM to support strong divergent/diffluence pattern
    with 100-120kt jet streak rounding the base of the upper-low in NW
    Old Mexico. In also supporting/broadening updraft strength for
    any convection that does develop, it is has be strengthening solid
    moisture return through the Rio Grande and Pecos Valley through
    the southern High Plains. Strong easterly and confluent
    southeastern flow at 15-20kts exist across much of north-central
    to southeast NM.

    CIRA LPW denotes deepest moisture remains upstream across the
    western TX panhandle through the Guadeloupe Mtns with nose of
    .5-.75" sfc-850mb wedge trying to filter in. Concurrently, the
    850-700mb layer from the southeast on 35-40kts of flow (per VWP)
    is reaching .5"...reaching near 1" totals across southeast NM.=20
    EML's are steepening lapse rates to support sufficient lapse rates
    to support 500-1000 MUCAPE pooling along the stationary frontal
    boundary toward a surface low in the northern Rio Grande Valley
    north of ONM. As such, orographic ascent and localized
    convergence is sparking widely scattered thunderstorms in the
    vicinity of the frontal zone. Weak isallobaric pressure falls aid inflow/maintenance of updrafts for a few hours to over-come the
    strong effective bulk shear in the weakly unstable environment.=20
    As such, steering flow in diffluent pattern supports short-term
    training of the updrafts oriented more south to north across
    northern NM, while more SW to NE in the vicinity of the Sacramento
    Range into eastern NM. Rates of .75"/hr and 1-2 hours of
    repeating, may support localized totals of 1.5-2.5" and given
    dry/hard ground conditions has the potential to exceed the lower
    FFG values (1-1.5"/hr, 1-2.5"/3hrs).=20

    Eventually, shortwave energy will round the base and the
    associated jet will increase southwesterly flow and the frontal
    zone will start to lift east and northeast with further enhanced
    moisture flux convergence along the leading edge. This should
    help to expand overall coverage, but may limit the increased
    duration locally into the early morning hours. Isolated incidents
    of flash flooding remain possible through morning.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-EtUO_usx9PKwfcJ9pFCg0QvDAvjTAqT1L5Yom4s2sZwuoB7ZRrTKMDi9OurgtFJnyNe= 12YdwnWHsxDlpqeM0sfq4DU$ for graphic product...

    ATTN...WFO...ABQ...EPZ...LUB...MAF...

    ATTN...RFC...ABRFC...CBRFC...WGRFC...NWC...

    LAT...LON 36580528 36200420 35510344 34880312 33440283=20
    32370321 32280446 32710530 33670611 34260672=20
    34810764 35550787 36190745 36580654=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 5 18:03:54 2025
    AWUS01 KWNH 051803
    FFGMPD
    TXZ000-060000-

    Mesoscale Precipitation Discussion 0225
    NWS Weather Prediction Center College Park MD
    203 PM EDT Mon May 05 2025

    Areas affected...central TX to middle/upper TX coast

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 051802Z - 060000Z

    SUMMARY...Repeating and short term training of cells across
    central TX to the middle/upper TX coast may result in localized
    flash flooding through 00Z. Peak rainfall rates could be as high
    as 2-3 in/hr with isolated totals in excess of 4 inches.

    DISCUSSION...1730Z radar imagery showed a cluster of thunderstorms
    near Austin on either side of I-35, with an average cell movement
    off toward the northeast at 30-40 kt. Some new cell development
    has been observed south of ongoing cells, allowing for brief
    training with MRMS-derived rainfall of 1.0-1.5 in/hr over eastern
    Travis into Bastrop County. This area of storms was elevated,
    being forced by low level warm advection to the north of a wavy
    warm front at the surface, extending west to east across
    south-central TX. Layered PW imagery showed these storms were
    positioned along the northern edge of a surface to 700 mb moisture
    axis, drifting northward through central TX. SPC mesoanalysis and
    RAP guidance showed MUCAPE of 1000-1500 in the vicinity of Austin.

    925-850 mb winds were from the south-southeast to southeast across
    the surface warm front at 20-30 kt (VAD wind plots) from central
    to southern TX and are forecast by the RAP to translate eastward
    toward Houston through 00Z. Steering flow should take ongoing
    thunderstorms toward the northeast with more organized cells right
    of the mean wind. Meanwhile, additional development is likely to
    fill in between the ongoing activity and the surface warm front
    which is expected to lift north during the afternoon. Overrunning
    of the front and low level convergence on the nose of stronger low
    level flow (which may align with steering flow at times) will
    favor repeating cells with short term training and potential for
    rainfall rates of 2-3 in/hr. Flash flooding will be possible with
    storm totals over 4 inches on a localized basis which will pose a
    risk of flash flooding, with the greatest threat over urban
    locations due to relatively high 3-hr flash flood guidance values
    of 3 to 5 inches.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_P0YKSKTL1gBtls5rF98gmbdey2EVPC3rWrgH2gGbCZnOs0wj-JR92VvuRDltHfx9usZ= H9YRdgB0Dr9f3m-5LimiX_c$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...LCH...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 31119726 31079636 30629535 30219460 29649428=20
    29089435 28779486 28549571 28469634 28469740=20
    28909836 29479873 30169871 30869804=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 5 18:49:25 2025
    AWUS01 KWNH 051849
    FFGMPD
    NYZ000-PAZ000-MDZ000-VAZ000-WVZ000-OHZ000-060045-

    Mesoscale Precipitation Discussion 0226
    NWS Weather Prediction Center College Park MD
    248 PM EDT Mon May 05 2025

    Areas affected...portions of northern Mid-Atlanitc and central
    Appalachians to Lake Erie

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 051846Z - 060045Z

    SUMMARY...Training of showers and thunderstorms from the northern
    mid-Atlantic and central Appalachians to the southern shore of
    Lake Erie may result in isolated to widely scattered areas of
    flash flooding through the early evening. Rainfall rates of 1-2
    in/hr are expected.

    DISCUSSION...Visible satellite and regional radar imagery from
    1830Z showed scattered showers and thunderstorms extending from
    northern VA into northern MD, northwestward into PA, western NY
    and eastern OH. These showers/storms were located northeast of a
    closed mid to upper-level low over the OH Valley with low level
    southeasterly flow advecting moisture northwestward across the
    region. Broadly diffluent flow aloft was in place to the northeast
    of the closed low, helping increase synoptic scale lift over the
    region. Blended TPW imagery showed that PW values ranged from ~1.4
    inches to the southeast over northern MD to ~0.7 inches over
    eastern OH. SPC mesoanalysis data from 18Z showed MLCAPE was
    generally weak at 500-1000 J/kg with cloud cover or lower moisture
    values limiting instability to some degree.

    However, flash flood guidance values across a large portion of the
    region were about 1.0 to 1.5 inch/hr or slightly less and
    similarly oriented low level and mean steering flow wind vectors
    were supportive of repeating cells. While 925-850 mb winds were
    generally weaker than the mean steering flow, low level axes of
    confluence will support lines of showers/thunderstorms with a
    tendency for cell repeating and short term training. The
    environment is supportive of 1-2 in/hr rainfall rates and some
    indications from the RAP support a minor increase in the low level
    flow toward 00Z which could help increase the threat for
    backbuilding cells. The flash flood threat is expected to be
    isolated to widely scattered in nature through 01Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5oAZZoUG6T6lXFWX2bavNkkIop7hDyh3OEZYuiq2yvTJqWYyxIdpojuROOjp1jn922bT= V5YYqct6A3hLdFr_6NuhPeQ$ for graphic product...

    ATTN...WFO...BUF...CLE...CTP...LWX...PBZ...RLX...

    ATTN...RFC...MARFC...NERFC...OHRFC...NWC...

    LAT...LON 42437874 41107743 40007715 39257740 38697812=20
    38777907 39138020 39888046 40198103 40628153=20
    41728134 42258003=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 5 19:27:47 2025
    AWUS01 KWNH 051926
    FFGMPD
    NYZ000-PAZ000-MDZ000-VAZ000-WVZ000-OHZ000-060045-

    Mesoscale Precipitation Discussion 0226
    NWS Weather Prediction Center College Park MD
    323 PM EDT Mon May 05 2025

    Areas affected...portions of northern Mid-Atlanitc and central
    Appalachians to Lake Erie

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 051846Z - 060045Z

    SUMMARY...Training of showers and thunderstorms from the northern
    mid-Atlantic and central Appalachians to the southern shore of
    Lake Erie may result in isolated to widely scattered areas of
    flash flooding through the early evening. Rainfall rates of 1-2
    in/hr are expected.

    DISCUSSION...Visible satellite and regional radar imagery from
    1830Z showed scattered showers and thunderstorms extending from
    northern VA into northern MD, northwestward into PA, western NY
    and eastern OH. These showers/storms were located northeast of a
    closed mid to upper-level low over the OH Valley with low level
    southeasterly flow advecting moisture northwestward across the
    region. Broadly diffluent flow aloft was in place to the northeast
    of the closed low, helping increase synoptic scale lift over the
    region. Blended TPW imagery showed that PW values ranged from ~1.4
    inches to the southeast over northern MD to ~0.7 inches over
    eastern OH. SPC mesoanalysis data from 18Z showed MLCAPE was
    generally weak at 500-1000 J/kg with cloud cover or lower moisture
    values limiting instability to some degree.

    However, flash flood guidance values across a large portion of the
    region were about 1.0 to 1.5 inch/hr or slightly less and
    similarly oriented low level and mean steering flow wind vectors
    were supportive of repeating cells. While 925-850 mb winds were
    generally weaker than the mean steering flow, low level axes of
    confluence will support lines of showers/thunderstorms with a
    tendency for cell repeating and short term training. The
    environment is supportive of 1-2 in/hr rainfall rates and some
    indications from the RAP support a minor increase in the low level
    flow toward 00Z which could help increase the threat for
    backbuilding cells. The flash flood threat is expected to be
    isolated to widely scattered in nature through 01Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7ash_-YrVg9-HmJOfkJNSKwXzW6mVwXXl1y78FanFERR4KeCRFwGXVp981GV7fwADlFJ= wMa5Jxe3gm5I0s6RlRrAnhs$ for graphic product...

    ATTN...WFO...BUF...CLE...CTP...LWX...PBZ...RLX...

    ATTN...RFC...MARFC...NERFC...OHRFC...NWC...

    LAT...LON 42437874 41107743 40007715 39257740 38697812=20
    38777907 39138020 39888046 40198103 40628153=20
    41728134 42258003=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 5 22:39:36 2025
    AWUS01 KWNH 052239
    FFGMPD
    PAZ000-MDZ000-VAZ000-NCZ000-DCZ000-WVZ000-060300-

    Mesoscale Precipitation Discussion 0227
    NWS Weather Prediction Center College Park MD
    638 PM EDT Mon May 05 2025

    Areas affected...portions of eastern VA into the DMV and far
    eastern WV

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 052235Z - 060300Z

    Summary...Training convection will be capable of hourly totals of
    1-3" with short-term (3-hr) totals as high as 2-4". Isolated to
    scattered instances of flash flooding are possible (and may be
    locally significant in sensitive urban/mountainous terrain).

    Discussion...Radar and GOES-East satellite imagery indicate the
    proliferation of convection across portions of eastern VA/NC over
    the past several hours, moving fairly rapidly (~25 kts) towards
    the N-NE within nearly unidirectional flow on the eastern
    periphery of a large, deep layer (850-200 mb) closed low centered
    over IL/IN/KY. The mesoscale environment in the vicinity and
    downstream of the aforementioned convection is characterized by
    SBCAPE of 1000-2000 J/kg, PWATs of 0.8-1.3" (between the 75th and
    90th percentile, per IAD sounding climatology), and deep layer
    (0-6km shear) of 20-40 kts (per 22z SPC SFCOA analysis). The
    strongest cells have been capable of impressive instantaneous
    rainfall rates of 3-5"/hr (per MRMS estimates), which has resulted
    in estimated hourly rainfall totals of up to 2.5" (where deeper
    convective cells have been able to occasionally train, mainly to
    the east of I-95 in eastern VA).

    Recent hi-res CAMs have not handled the evolution of convection
    particularly well, and recent observational trends (including
    continued overshooting/cooling cloud tops via GOES-East imagery)
    suggest that localized hourly totals of 1-3" will continue to
    manifest farther north (into the more sensitive DMV region) with
    storm propagation (as a pool of 1500-2000 J/kg of SBCAPE remains
    untapped). While both of the hourly updating CAMs (HRRR/RRFS) are
    handling the convection poorly, the 18z HREF suite does still give
    a good idea of the potential for excessive rainfall through 03z
    (with 40-km neighborhood probabilities for 2" and 3" exceedance of
    20-30% and ~10%, respectively). Given locally sensitive terrain
    (per FFGs as low as 0.75-1.50" and 1.50-2.50" for 1-hr and 3-hr
    periods, respectively) over urbanized terrain along and near I-95
    and over portions of the Appalachians in the vicinity of northern
    VA, western MD, and far eastern WV, isolated to scattered
    instances of flash flooding are possible (and may be locally
    significant, should 2-4" totals occur over the most sensitive
    localities).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6dfyBFfZ7lIgNjsTCMzn8e7-k6qb3VAuAVNx0xL5na-fLggLrUtAcLowcrkE6wezFkVC= SbWHtIKcv95cd5dDCOkUzKI$ for graphic product...

    ATTN...WFO...AKQ...CTP...LWX...RAH...

    ATTN...RFC...MARFC...SERFC...NWC...

    LAT...LON 39827743 39597667 39037647 37767669 36447699=20
    36217739 36777738 37437742 38277778 39617833=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 6 02:48:04 2025
    AWUS01 KWNH 060247
    FFGMPD
    TXZ000-NMZ000-060830-

    Mesoscale Precipitation Discussion 0228
    NWS Weather Prediction Center College Park MD
    1047 PM EDT Mon May 05 2025

    Areas affected...Central & Eastern NM...Cap Rock & Northern
    Permian Basin of TX...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 060245Z - 060830Z

    SUMMARY...Streaks of thunderstorms with repeating flanking line
    development will become increasingly efficient with moistening
    profiles. Increasing rates to 1.5-1.75" with 1.5-3" totals
    resulting in widely scattered incidents of possible flash flooding.

    DISCUSSION...GOES WV continues to show fairly static deep upper
    low across east-central AZ with trof extending southward as
    stronger 120-130kt 250mb jet undercuts it resulting in broad
    downstream diffluence across the Southern High Plains into W TX.=20
    An embedded vorticity center can be seen near the SW Heel of NM
    starting to sharpen, ready to lift northeastward providing even
    further mid to upper level forcing through strong DPVA. As a
    result a strong 995-6 surface low exists in the vicinity of the
    Davis mountains with a strong 50-60 Td gradient across it in less
    than a few miles. This dryline extends north toward an
    intersection with old stationary front between CNM and GDP (which
    extends along the Sacramento Mtns toward ABQ and southeastward
    across the Pecos Valley toward ECU/ERV. Isallobaric response in
    the lowest levels is supporting very strong convergence along the
    axis of both the dry line and stationary front providing very
    solid moisture and instability transport, with 40-50kts of
    southeasterly flow off the Rio Grande Valley into the W Texas
    Panhandle; PWs are trickling into the 1.25" range and capped 2000+
    J/kg CAPE (a subsequent MPD may be required if/when cap breaks
    across southern Permian/Pecos River Valley).

    North of the front/dryline intersection, flow is backed further
    out of the east-northeast to northeast at similar 20-40kts from
    surface to boundary layer. The flux into the front is pooling to
    .75-1" PW and support a narrow ribbon of 1000 J/kg as far north as
    ABQ. As such, strong thunderstorms have been developing along the
    stationary front and given deep layer steering, have been lifting
    north (further west) and northeast (across the northern Permian
    Basin to southern Cap Rock).=20

    Given the upstream forcing remains upstream, the surface response
    has locked the front and these localized convergence maxima to
    support back-building or flanking redevelopment that generally
    follow similar paths. Initially, large hail and gusty winds have
    been the primary factor, but the continued flux and rainfall has
    been locally moistening the profile and increasing rainfall
    efficiency. Combine this with continued expanding divergence
    aloft, upscale growth into clusters and 'wedges' in satellite
    appearance will increase, though the source/redevelopment regions
    will decouple as the DPVA and FGEN ascent lifts north and
    northeast. As such, rates up to 1.5"/hr will become possible and
    with training/repeating, streaks of 1.5-3" will become more likely
    across north-central NM into the Cap Rock.=20

    AHPS 7-10 precipiation anomalies show much of these areas have
    seen well above normal rainfall (200-400%) and NASA SPoRT 0-40cm
    soil saturation graphics denote this as well rising into the
    70-80th percentiles, especially further north and east across the
    Cap Rock into the Big Country. As such, scattered incidents of
    flash flooding should become possible through the overnight
    period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6PKildUX1RhiAHTlcMe9ccRmpalpVifABwVk08lPLvwyKfNKcyUYuNQJlLxz22CWuTJS= wc46mBXOFov0C6cHXb7mjyE$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...MAF...SJT...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 36450534 36050360 34950147 34260051 33360001=20
    32649996 32180013 31740065 31700321 32100423=20
    33790521 34500562 35210638 36040636=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 6 05:07:54 2025
    AWUS01 KWNH 060507
    FFGMPD
    TXZ000-060930-

    Mesoscale Precipitation Discussion 0229
    NWS Weather Prediction Center College Park MD
    107 AM EDT Tue May 06 2025

    Areas affected...Stockton & Edwards Plateau of Western Texas...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 060505Z - 060930Z

    SUMMARY...Continued risk of regenerative thunderstorms along the dryline/surface front. Deep layer steering may support
    training/repeating locally for streaks of 2-3" totals and possible

    DISCUSSION...GOES WV suite depicts very deep (3-3.5 Std. Dev.)
    closed low generally centered in the Lower Colorado River Valley
    and is currently reorienting as very strong shortwave energy
    rotates around the western to southwestern edge of current center.
    This is elongating the overall low favorably across eastern AZ
    into much of NM to support strong divergent/diffluence pattern
    with 100-120kt jet streak rounding the base of the upper-low in NW
    Old Mexico. In also supporting/broadening updraft strength for
    any convection that does develop, it is has be strengthening solid
    moisture return through the Rio Grande and Pecos Valley through
    the southern High Plains. Strong easterly and confluent
    southeastern flow at 15-20kts exist across much of north-central
    to southeast NM.

    CIRA LPW denotes deepest moisture remains upstream across the
    western TX panhandle through the Guadeloupe Mtns with nose of
    .5-.75" sfc-850mb wedge trying to filter in. Concurrently, the
    850-700mb layer from the southeast on 35-40kts of flow (per VWP)
    is reaching .5"...reaching near 1" totals across southeast NM.=20
    EML's are steepening lapse rates to support sufficient lapse rates
    to support 500-1000 MUCAPE pooling along the stationary frontal
    boundary toward a surface low in the northern Rio Grande Valley
    north of ONM. As such, orographic ascent and localized
    convergence is sparking widely scattered thunderstorms in the
    vicinity of the frontal zone. Weak isallobaric pressure falls aid inflow/maintenance of updrafts for a few hours to over-come the
    strong effective bulk shear in the weakly unstable environment.=20
    As such, steering flow in diffluent pattern supports short-term
    training of the updrafts oriented more south to north across
    northern NM, while more SW to NE in the vicinity of the Sacramento
    Range into eastern NM. Rates of .75"/hr and 1-2 hours of
    repeating, may support localized totals of 1.5-2.5" and given
    dry/hard ground conditions has the potential to exceed the lower
    FFG values (1-1.5"/hr, 1-2.5"/3hrs).=20

    Eventually, shortwave energy will round the base and the
    associated jet will increase southwesterly flow and the frontal
    zone will start to lift east and northeast with further enhanced
    moisture flux convergence along the leading edge. This should
    help to expand overall coverage, but may limit the increased
    duration locally into the early morning hours. Isolated incidents
    of flash flooding remain possible through morning.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_N5fE4wFHlpDy96aRX6nu7dP0VdlmSqvAb_Yw_c5WL_QNHt1YAOzA3rEqzY6z0l5Je8t= xE_-6y1JfoCsrcGbzSqoLFg$ for graphic product...

    ATTN...WFO...EWX...MAF...SJT...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 32369992 32079938 31449903 30729857 30019832=20
    29339841 29129956 29160073 29750195 29830241=20
    31290348 31600310 31720173=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 6 05:58:30 2025
    AWUS01 KWNH 060556
    FFGMPD
    NYZ000-PAZ000-061100-

    Mesoscale Precipitation Discussion 0230
    NWS Weather Prediction Center College Park MD
    155 AM EDT Tue May 06 2025

    Areas affected...Central PA...West Central Upstate NY...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 060555Z - 061100Z

    SUMMARY...Additional 1-2" of rainfall in 1-2 hours across recently
    saturated soils and low FFG pose possible localized flash flooding
    over next few

    DISCUSSION...GOES-E WV shows an eastward extension of the deep
    upper low, extending across WV into central MD providing increased
    downstream DPVA ascent and a localized increase in low level WAA
    across MD into central PA. 05z surface analysis shows the cold
    front remains fairly banked up along the front range/Blue Ridge of
    the Appalachians into central PA connecting to a triple point
    south of BFD, with warm front bisecting PA just north of SEG
    toward the Lehigh Valley. Along with the slight increase in LLJ
    to 30kts, increased low level moisture is bringing back 1.0-1.25"
    total PWats and some weak instability about 250-500 J/kg. Solid
    southwesterly flow along/behind the cold front further strengthens
    FGEN ascent through the area. As such, recent RADAR and 10.3um
    EIR show increasing shallow convective cells across the
    Mason-Dixon line from RSP to DMW, but extend northward through
    much of the warm sector in central PA.=20

    Deep layer steering along/ahead of the cold front will support
    training of cells; with 1"/hr rates, so with length supportive of
    1-2 hours of training across a narrow axis. This may result in an
    additional 1-2" in less than 2hrs across areas that already had
    some heavy rainfall this afternoon, especially further north into
    south-central NY. The combination over saturated ground
    conditions and 1-3hr FFG values of .5-1.25 and .75 to 2,
    respectivly; suggest flash flooding may be possible through the
    remainder of the overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-8E8PW1DctycXKrVsVpd_vZmgHagG0EasYre2KnqTLi3IRhMNVCwo-EnfuHBRiQU2hY5= 2uceGZ-a4oCqFIZwB6JsG6Q$ for graphic product...

    ATTN...WFO...BGM...BUF...CTP...

    ATTN...RFC...MARFC...NERFC...OHRFC...NWC...

    LAT...LON 42997787 42947738 42617691 42077658 41467649=20
    40697655 40457662 39757688 39907774 41387840=20
    42187861 42717843=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 6 08:00:55 2025
    AWUS01 KWNH 060800
    FFGMPD
    TXZ000-OKZ000-061400-

    Mesoscale Precipitation Discussion 0231
    NWS Weather Prediction Center College Park MD
    400 AM EDT Tue May 06 2025

    Areas affected...TX Big Country through Hill Country...Adj Ext
    Southweset OK...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 060800Z - 061400Z

    SUMMARY...Broad area of ascent across much of TX ahead of
    anomalously deep closed low exiting the Southwest. Scattered
    incidents of flash flooding possible with localized 2-3" totals
    across recently saturated grounds/low FFG.=20

    DISCUSSION...GOES-E WV shows core of 3-3.5 Std Dev. closed low is
    finally starting to translate eastward given upstream kicker
    resulting in very broad downstream diffluence/divergence area to
    shift out of the High Plains into the Big Country and eastern
    Edwards Plateau. A convectively reinforced shortwave is starting
    to shear along the northeast quadrant of the low and pivot into E
    NM still providing an axis of 700mb isentropic ascent/WAA channel
    to maintain elevated convection/broadening moderate shield
    precipitation across the Rolling Plains into the Big Country and
    Red River Valley. Activity is scattered and generally lighter
    with occasional embedded cores capable of 1"+/hr rates but
    increased duration over greatest saturated soil conditions (where
    precip anomalies are 300-500% of normal and remain in the upper
    90th percentiles of saturation). As such, limited infiltration
    will result in some enhanced run-off, but likely be limited in
    coverage to those random/scattered elevated cores.

    Southward into the Edwards Plateau/Hill Country...
    A broad/strong axis of DPVA ahead of the main height-falls is
    maintaining the 999mb low near/south of MAF, the stationary front
    is starting to lift northeast as a warm front ahead of the low and
    the dry line across the Western TX Panhandle is shifting eastward
    increasing moisture convergence ahead of it. Warm moist winds out
    of the Rio Grande Valley continue to advect 1.3-1.5" total PWats
    (loaded mainly below 850mb) will continue to be highly confluent
    even as they veer more southerly/southwesterly over the next few
    hours. Higher unstable air with MUCAPE of 2000+ j/kg will
    isentropically ascend across the front and maintain stronger thunderstorms/clusters along the boundary as they shift eastward.=20
    Rates of 2"/hr are probable, though 1.5" may fall in 15-30 minutes
    given 06z HRRR forecast and given some upstream cells may allow
    for two rounds and/or flanking line repeating/training resulting
    in spots of 2-3.5" totals mainly near/just north of the front
    across the Edwards Plateau toward the Hill country. This area has
    experienced less heavy rainfall than further north, so soil ratios
    are much more supportive of infiltration, but the shear intense
    rates have a solid probability to result in scattered incidents of
    flash flooding through daybreak.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7jvy40uk_yP6qavLrS7B8BTO2TlHZvozSU9W7QSATtW51-SLaPcRVIgE48RDaXPMvNd_= 1v873evK1qD3ceg9b2Wuy_E$ for graphic product...

    ATTN...WFO...EWX...FWD...LUB...MAF...OUN...SJT...

    ATTN...RFC...ABRFC...WGRFC...NWC...

    LAT...LON 34689941 34119755 32869680 31409681 31019684=20
    30319715 29989767 29939885 30480069 30920171=20
    31550195 32830212 34090165 34610071=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 6 13:35:59 2025
    AWUS01 KWNH 061335
    FFGMPD
    TXZ000-061931-

    Mesoscale Precipitation Discussion 0232
    NWS Weather Prediction Center College Park MD
    935 AM EDT Tue May 06 2025

    Areas affected...South-Central and Eastern Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 061331Z - 061931Z

    SUMMARY...Increasing thunderstorm coverage, including scattered
    supercells, along a lifting warm front are expected to congeal
    with thunderstorms from an eastward moving cold front to produce
    locally 3"+ rainfall amounts. Flash flooding is possible with the
    potential for locally considerable impacts through early this
    afternoon should the heaviest rainfall occur over vulnerable urban
    locations.

    DISCUSSION...GOES-E WV depicts clearly a deep closed low sliding
    over the southern High Plains and producing broad ascent
    throughout the south-central U.S., amplified by the nose of a
    110kt upper jet reaching over the Concho Valley per the 12z RAP
    analysis. At the surface, a lifting warm front is evident in
    recent METAR observations throughout southern and eastern TX,
    between Austin and San Antonio at 12z. It is along and just north
    of this boundary where the greatest potential for discrete
    supercells are possible before quickly merging with an approaching
    line of storms along the advancing cold front through 17z-19z.
    MRMS highlights current storms of producing locally up to 2"/hr
    rainfall rates, but as these storms expand, these rates will
    likely cover a larger area and more likely to lead to flash
    flooding impacts. However, as this line moves further into eastern
    TX by midday, eastward progression will slow as flow becomes more
    uniform out of the west-southwest along a stalled out boundary,
    supporting back-building cells. This places areas near College
    Station on eastward toward the TX-LA as having the greatest
    potential for locally considerable impacts. It is this area where
    the 06z HREF depicts 20-40% chances for 3"+ amounts through 18z,
    with heavy rainfall likely continuing after 18z.

    Recent HRRR runs highlight hourly totals of 1-4" through 19z,
    which would occur within somewhat compromised terrain and where
    FFG of 1-3" per 1-hr and 2-4" per 3-hr exists. This seems
    reasonable given the current radar representation and environment
    given the widespread 1.6-1.9" PWATs.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_sKp8n-_lEUQ1ndcNPGAbBu9V6SjnW0wAQiPckGXesc-S7ZqaGS6YwrPty21mIlV4j7v= -C4i0rZvbrGGcT6IS6HXeTA$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...SHV...SJT...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 32079586 31999507 31479479 30729510 29959613=20
    29569780 29659907 30049937 30589896 31429763=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 6 15:03:58 2025
    AWUS01 KWNH 061502
    FFGMPD
    ARZ000-TXZ000-OKZ000-062101-

    Mesoscale Precipitation Discussion 0233
    NWS Weather Prediction Center College Park MD
    1102 AM EDT Tue May 06 2025

    Areas affected...Northern Texas and Southern/Central Oklahoma

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 061501Z - 062101Z

    SUMMARY...Broad area of moderate rainfall with embedded
    thunderstorms and heavier rates could lead to scattered flash
    flooding with more widespread nuisance flooding through this
    afternoon.

    DISCUSSION...Strong ascent continues east of the closed low moving
    over the southern Rockies/High Plains, while a squall line pushes
    eastward across Texas. Ahead of this squall line, some scattered
    supercells are possible within an elevated warm sector and MUCAPE
    of 1,000-2,000 J/kg. Rainfall rates per MRMS have generally
    remained below 1.5"/hr, but this area along the Red River Valley
    has experienced saturated ground conditions as of late. NASA SPoRT
    LIS 0-40 cm soil moisture percentiles are generally in the 70-95th
    range (lower in northeast TX and southeast OK). The longer
    duration of moderate to heavy rainfall (pockets of 1-2"/hr)
    expected through this afternoon could lead to localized flash
    flooding where terrain and ground conditions are most susceptible.
    However, even where flash flooding does not occur, nuisance
    flooding and ponding of water in fields/near roads is possible.

    Recent HRRR runs depict 3-hrly totals up to 1.5" possible in the
    highlighted MPD area, with some locations already recording
    0.5-1.0" since 12z. 3-hrly FFGs in the area are less than 2.5"
    from a line between DAL and OKC on westward, with eastern sections
    of the MPD highlighted by 3-hrly FFGs of 3-4". PWATs over the 90th climatological percentile extend northward to the Red River, with
    values over 1.7" into north-central TX ahead of the squall line.
    Storms developing in this region of better moisture and strong
    southern 850mb flow of 40-50kts in eastern TX will surge northward
    overriding a mid-level warm front and add to the heavier mostly
    stratiform rainfall through this afternoon with embedded
    convection leading to the isolated flash flooding threat.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9B6RyaImxVjtm_rl5c2NVrCOKRqLJV7RCP9EAg9HiM7eL_6loYdf1QLCvdsUxZTAN5Y9= zn6ERw2ALiY27yiVNUzEu58$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 35749821 35669728 35289629 34679517 33979440=20
    33049444 32309547 31729684 31179826 31569863=20
    32439795 33399804 34689881 35379879=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 6 16:27:59 2025
    AWUS01 KWNH 061626
    FFGMPD
    NYZ000-NJZ000-PAZ000-MDZ000-062225-

    Mesoscale Precipitation Discussion 0234
    NWS Weather Prediction Center College Park MD
    1226 PM EDT Tue May 06 2025

    Areas affected...Northern Mid-Atlantic into the Interior Northeast

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 061625Z - 062225Z

    SUMMARY...Developing convection this afternoon is expected to
    repeat over areas of the Northeast and Mid-Atlantic where recent
    rainfall has lowered flash flood guidance. Isolated rainfall
    totals over 2 inches could lead to scattered areas of flash
    flooding, with the most likely impact along the NY-PA border and
    nearby areas.

    DISCUSSION...A closed low over the Upper Ohio Valley continues to
    churn and usher in broad southerly flow along the East Coast.
    PWATs are highest along the immediate East and into New England,
    where values range from 1.0-1.2" and near the 90th climatological
    percentile, but the greater mix of instability and shear exists
    just to the west from central New York to northern Maryland. Here,
    GOES-E visible imagery depicts broken cloud cover allowing for
    SBCAPE to increase over 1,000 J/kg in southeast PA, which
    coincides with where the deepest convection has developed over the
    last hour.

    Thunderstorms are expected to continue building (although
    scattered in nature) over the next few hours as instability
    continues to grow and expand northward. However, a focus in
    convection is possible along a weak frontal boundary/convergence
    axis. All of this activity will become more widespread in
    northeast PA/southern NY by about 20z once a shortwave rounding
    the base of the upper trough very quickly pushes over the recent.
    This increased ascent may allow for rainfall rates to approach
    2"/hr and broader coverage of moderate rain, but more importantly
    impact areas prone to flash flooding due to recent rainfall. NASA
    SPoRT LIS 0-40 cm soil moisture is above 98th percentile for much
    of northern PA and NY. This goes along with 3-hr FFG under 2"
    (even as low as 1" in localized areas). The 12z HREF highlights
    impressive probabilities for exceeding this FFG along the PA-NY
    border just west of Binghamton by 21z this afternoon. Will
    continue to monitor rainfall rates in case the need for more considerable/significant language is needed this afternoon.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-zNr3KN6SDSE3JVMvQf89LMxtvDfaG9b8QSlF8tlYXJ27koKS-_KrG0f7Nw3b8vVNQKI= 0XNDivRwfvuLdpmKBO-7DY8$ for graphic product...

    ATTN...WFO...ALY...BGM...BUF...CTP...LWX...OKX...PHI...

    ATTN...RFC...MARFC...NERFC...NWC...

    LAT...LON 43647667 43467564 42937467 41957436 40827468=20
    40007534 39507640 39807705 40867721 41787734=20
    42837786 43467764=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 6 19:00:32 2025
    AWUS01 KWNH 061900
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-070059-

    Mesoscale Precipitation Discussion 0235
    NWS Weather Prediction Center College Park MD
    259 PM EDT Tue May 06 2025

    Areas affected...Eastern Texas and Louisiana

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 061859Z - 070059Z

    SUMMARY...Organized line of thunderstorms with hourly rates up to
    3 inches expected to continue sliding eastward while additional
    merging cells along a warm front increase the potential for 5 inch
    totals, likely resulting in areas of flash flooding.

    DISCUSSION...GOES-E CH9 WV loop this afternoon depicts a
    picturesque upper low churning over the southern High Plains with
    an expansive area of increased ascent extending to the east and
    north, with a well-organized line of thunderstorms entering
    eastern TX along a cold front. Additionally, a surface warm front
    extends eastward from the squall line across southern LA, with
    low-to-mid 70s dew points south of the front and 60s north. PWATs
    continue to creep upward and are generally 1.7-2.0" in the
    highlighted area, but will continue to rise above 2.0" across a
    larger region of the central Gulf Coast per the RAP. The 06z ECWMF
    highlights these values as exceeding the 99th percentile when
    compared to climatology.

    Rainfall totals up to 3 inches have been observed from this line
    near Round Rock, TX and are expected to maintain or increase in
    intensity through this evening given the increasing moisture and
    daytime instability being advected northward. Helping this
    northward advection is a potent 40-50kt 850mb jet extending into
    eastern TX as of 18z.

    Recent HRRR runs support the potential for hourly rates up to 3
    inches and 5 inch totals, with the 12z HREF highlighting
    widespread 20-50% chances for 3-hrly totals greater than 3 inches
    in the MPD area. Although, the HRRR has been developing too much
    leading convection compared to current radar data. Outside of the
    eastern extent of the Texas Triangle, where 3-hrly FFGs are under
    3 inches, much of LA does have elevated FFG that could inhibit the
    initial impacts of heavy rainfall. However, for southern sections
    of LA along the warm front, thunderstorms are anticipated to
    remain less progressive and oriented more west-east (similar to
    the mean wind) by this evening. Current convection near Baton
    Rouge shows this potential for slow-moving warm frontal storms
    that may continue and congeal with the approaching line. Scattered
    flash flooding is likely within this area, with greatest potential
    for significant impacts where convection is slower to progress on
    the southern flank from east-central TX through central LA.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-We7JFvC5PFF4_SXBouUY-5YNdCX72TI3auSt4vVsjxP_mBdDrWVhnm6KBf_JWkZnUsw= FXB_NfnIRJ93335YRP7QMxw$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...JAN...LCH...LIX...SHV...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 33209438 33169319 32189208 31309121 30619057=20
    30039088 29969184 29989302 29949431 29799642=20
    30279701 31309620 32449527=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 6 22:34:06 2025
    AWUS01 KWNH 062233
    FFGMPD
    NYZ000-NJZ000-PAZ000-070400-

    Mesoscale Precipitation Discussion 0236
    NWS Weather Prediction Center College Park MD
    633 PM EDT Tue May 06 2025

    Areas affected...central NY to PA/NJ border

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 062230Z - 070400Z

    SUMMARY...Isolated to widely scattered areas of flash flooding
    will remain possible across a broad section of Upstate NY down to
    the PA/NJ border through 04Z. Peak hourly rainfall up to 1.0-1.5
    inches (especially early on) will be likely on an isolated basis.

    DISCUSSION...Radar imagery at 2230Z showed that a broken line of showers/thunderstorms extended from near Syracuse to the NY/PA/NJ
    border. A mesoscale axis of low level convergence to the west of
    Syracuse has resulted in a localized area of hourly rainfall in
    excess of 2 inches (north of Skaneateles) with surrounding
    locations in and around central NY to northeastern PA, in the 1-2
    inch range (in 60 minutes). Water vapor imagery showed a
    well-defined, negatively tilted shortwave trough swinging toward
    the north over eastern PA, to the east of a mid to upper-level low
    center over northwestern PA. Flow ahead of this feature was
    strongly diffluent, aiding in lift within a weakly unstable
    airmass (500-1000 J/kg MUCAPE), though infrared cloud tops have
    been warming over the past hour.

    Through 04Z, the shortwave spoke is forecast to lift northward
    into central NY, sending the broken convective line toward the
    north and east into the Catskills and Hudson Valley. There is a
    low end threat for south to north training as the line advances
    east, though advection of drier and more stable air into the
    region from the southwest should lessen this the heavy rain/flash
    flood threat with time over eastern portions of NY.

    Over central NY, weaker deeper layer mean flow will continue to be
    supportive of slower movement of heavy rain cores with the ongoing
    axis west of Syracuse expected to advance off toward the northeast
    over the next couple of hours. Meanwhile additional heavy rain may
    move in from the south through 04Z with peak rainfall rates
    lowering into the 0.5 to 1.0 in/hr range as instability diminishes
    with the loss of daytime heating. An additional 1-2 inches of rain
    (locally a little above 2 inches over central NY) is expected on a
    localized basis which may linger the flash flood threat for
    another few hours over northern PA/NJ into NY.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_LvscJ0LH-UgyPdloWrQuY7y05MIaWEhDEJIGMQ_pYpb6LHRx8KqcVMcpWRivSBxpmce= GgvFt0X17xKLAfj9WEjC7ag$ for graphic product...

    ATTN...WFO...ALY...BGM...BTV...BUF...CTP...OKX...PHI...

    ATTN...RFC...MARFC...NERFC...NWC...

    LAT...LON 44567573 44147450 43527391 42747368 41367401=20
    41047446 41057510 41407572 41577626 41877770=20
    42487817 43287778 44027718 44467636=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 6 23:25:36 2025
    AWUS01 KWNH 062325
    FFGMPD
    AZZ000-NVZ000-CAZ000-070500-

    Mesoscale Precipitation Discussion 0237
    NWS Weather Prediction Center College Park MD
    724 PM EDT Tue May 06 2025

    Areas affected...eastern CA, southern NV, western AZ

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 062323Z - 070500Z

    SUMMARY...An increasing coverage of thunderstorms across portions
    of eastern CA, southern NV and western AZ over the next 2-4 hours
    will be capable of flash flooding. Rainfall of 0.25 to 0.50 inches
    in 15 minutes and storm totals of 1-2 inches are expected on a
    spotty basis.

    DISCUSSION...GOES West water vapor imagery placed a closed
    mid-level low over south-central NV at 23Z, advancing slowly to
    the south. The approach of this low and its southern elongation
    into CA has allowed low level winds to shift from a northerly
    direction this morning to southwesterly to its south, increasing
    low level theta-e values into the lower Colorado River Valley. The
    combination of surface heating and low level moisture advection
    has increased MLCAPE values into the 500-1000 J/kg range from
    southern NV into eastern CA and western AZ via the 23Z SPC
    mesoanalysis. Visible satellite and radar imagery showed a few
    thunderstorms along the NV/AZ border, co-located with severe and
    flash flood warnings. Visible satellite imagery also showed
    developing cumulus over eastern CA with a few early thunderstorms
    over the Mojave Desert.

    Continued low level moisture advection into eastern CA and western
    AZ is expected to allow for marginal increases in an already
    highly anomalous moisture axis (standardized PW anomalies of +3 to
    +4). Mean westerly deeper layer flow of roughly 10 kt from the
    west will be co-located with similarly oriented and slightly
    stronger 700 mb winds which will be likely to support repeating
    cells and brief upwind propagation of cells. Rainfall rates within
    this environment should be easily capable of producing 0.25 to
    0.50 inches of rain in 15 minutes or less, which could result in
    some flash flooding of low lying areas and normally dry washes.
    Storm total rainfall of 1 to 2 inches is expected through 05Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_vfrOuTSTuZgQ-GHE-ivVTl3OphkUUwxyfxnNfyUUGizRv3bkOVdE4RQ_dz8I94WsHce= E2p9xS2vDy1dJ_bBFPPiV5I$ for graphic product...

    ATTN...WFO...FGZ...PSR...VEF...

    ATTN...RFC...CBRFC...CNRFC...NWC...

    LAT...LON 36511331 36321268 35751210 35141165 34561186=20
    33541272 33011382 33031480 33761571 34501618=20
    35261582 35671479 36481378=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 7 01:12:36 2025
    AWUS01 KWNH 070112
    FFGMPD
    ALZ000-MSZ000-LAZ000-ARZ000-TXZ000-070700-

    Mesoscale Precipitation Discussion 0238
    NWS Weather Prediction Center College Park MD
    911 PM EDT Tue May 06 2025

    Areas affected...southeastern TX into LA and central/southern MS

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 070110Z - 070700Z

    SUMMARY...Areas of heavy rain will continue a significant flash
    flood threat across portions of south-central LA into MS through
    07Z. Hourly rainfall in excess of 3 inches will be possible along
    with additional rainfall of 5 to 8 inches. These higher end
    rainfall totals could result in life-threatening conditions.

    DISCUSSION...Radar mosaic imagery at 0045Z depicted widespread
    thunderstorm coverage from western MS into central and southern
    LA, with a narrow tail of thunderstorms extending into the TX
    Coastal Plain. A weakening bowing segment was observed to be
    crossing into western LA with warming cloud tops over the past
    hour while a persistent area of cooling cloud tops has been
    observed from near JAS (far southeastern TX) to near and south of
    AEX (south-central LA), co-located with the low level overrunning
    via ~50 kt of 850 mb flow. The region from Newton County to
    Beauregard Parish has experienced hourly rainfall in excess of 3
    inches since 21Z and has MRMS-derived rainfall of 4-6 inches over
    the past 3 hours ending 00Z.

    As a pair of convectively induced mesoscale circulations, located
    on either side of the southern AR/MS border, advance toward the
    northeast within the 700-500 mb flow, the axis of strongest 850 mb
    flow will slowly advance east toward the LA/MS border through 06Z.
    While some weakening of the low level flow is anticipated, the
    northern portion of the convective cluster should advance into MS,
    while the southwestern flank will be slower to advance downstream,
    being met by developing thunderstorms atop the front and
    rain-cooled air over southern/southwestern LA. Training of heavy
    rainfall axes will continue to be capable of hourly rainfall in
    excess of 3 inches beneath a strongly diffluent flow pattern
    aloft.

    23Z and 00Z WoFS guidance showed a small region of 40 to 70+
    percent probabilities of 5+ inches over portions of south-central
    LA into southwestern MS over their 6-hr forecast range. Using the
    90th percentile output as a reasonable localized high-end of
    additional rainfall potential, 7 to 8 inches could fall over
    portions of south-central LA into southwestern MS. These rains
    could result in locally considerable to life-threatening flash
    flooding through 07Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5KvbH6KyYdXaEI4BJ3SYIUlQ0NGVWIFaENOeKFRvjmaYcL7R2nUdfe9UObPxozDAKxkr= 7NOGiCQoCKZjKZ4GDySURV4$ for graphic product...

    ATTN...WFO...BMX...HGX...JAN...LCH...LIX...MOB...SHV...

    ATTN...RFC...LMRFC...SERFC...WGRFC...NWC...

    LAT...LON 33678915 32628814 31348806 30648844 29938955=20
    29529136 29479306 29539384 29429464 29759479=20
    30529442 31439328 33139156 33569059=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 7 06:45:08 2025
    AWUS01 KWNH 070644
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-071300-

    Mesoscale Precipitation Discussion 0239
    NWS Weather Prediction Center College Park MD
    243 AM EDT Wed May 07 2025

    Areas affected...Central Gulf Coast...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 070700Z - 071300Z

    SUMMARY...Mature MCS starting to weaken with reduced inflow, but
    embedded intense rates of 2"/hr will continue to over-run frontal
    zone and repeat over saturating soils along I-10 maintaining
    likely rapid inundation flooding concerns through daybreak.

    DISCUSSION...GOES-E WV suite shows very large, anomalous closed
    low over the Southern Plains with large mature MCS well displaced
    at the far eastward extent of its influence. Given the broadening
    of the larger cyclone, the mid to upper-level forcing is
    diminishing as the jet slowly reduces in speed and responding
    winds in the lower levels continue to weaken in turn. While they
    are weakening, the strength and orientation remain sufficient to
    maintain the complex throughout the remainder of the overnight
    period with ideal split in dual jet structure with 100 kt jet
    lifting northeast across NE TX into TN, while the subtropical jet
    (60-70kt) ridges ideally, bending southeastward across the western
    to central Gulf providing excellent divergence/evacuation for to
    maintain the MCS.

    The MCS's MCV is over eastern-MS but is slowly shearing along the
    SW to NE flow and low level winds are veering across the central
    Gulf, reducing orthogonality of LLJ to the leading squall line
    across S MS into far SE LA. Source of greatest instability and
    enhanced moisture also resides upstream into the northwest Gulf,
    so the fast moving, but intense rain-rates will further reduce
    overall totals crossing into S AL/W FL though scattered incidents
    of sub-hourly 1.5-2" remain possible and urban flooding concerns
    remain.

    The greater concern remains upstream across western LA into
    central LA, where outflow from aforementioned bow is starting to
    lay flat west to east southeast LA, and perhaps align with the
    slowly sagging cold front. Currently, surface to boundary layer
    flow remains orthogonal to the boundary-combining front; but 850mb
    flow is already veering less orthogonal out of the SW to WSW. The
    jet is also expected to reduce in magnitude from 30kts toward
    15kts by 10z, reducing upglide ascent. Given the Gulf remains
    very warm, MLCAPEs of 2000-3000 J/kg will remain with deep moist
    profile support 2-2.25" total PWats. So while flux may reduce,
    the unstable environment will support scattered development from
    SW LA across south-central LA with capability of 2"/hr rates.=20
    Cells will once again cross saturated/flooded areas and maintain
    ongoing flooding conditions through morning, with slow improvement
    as scattered cells further reduce to isolated. Still pockets of
    additional 3-4" totals are probable through 12z and so flooding
    remains likely especially along of I-10 in LA.=20

    Note: Low level flow environment is going to slack for a time
    toward the end of the valid time; however, there is an upstream
    shortwave that will trail the right entrance of the exiting
    upper-level jet streak AoA 12z and appears to be triggering
    convection west of the Lower Rio Grande Valley currently; this
    will slide eastward and increase lower level flow/convergence
    again with another shot of thunderstorms. Will continue to
    monitor those trends closely.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6aKIpgWB3RtxG-We4i4LuB0Kxg2gwwiQMiQUe5d2tQO0QhHK3OWgvtDBrbc0wkoiDQrx= Uv4OHBbemTT4k2L6O_hSZ2o$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MOB...TAE...

    ATTN...RFC...LMRFC...SERFC...WGRFC...NWC...

    LAT...LON 31948811 31928756 31708670 30978638 30348665=20
    30038832 29588882 28978910 28938994 28999089=20
    29179129 29399197 29629301 29699363 30019361=20
    30419304 30899189 31349021 31828881=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 7 11:19:51 2025
    AWUS01 KWNH 071119
    FFGMPD
    LAZ000-TXZ000-071505-

    Mesoscale Precipitation Discussion 0240
    NWS Weather Prediction Center College Park MD
    719 AM EDT Wed May 07 2025

    Areas affected...Middle to Upper Texas Coasts

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 071118Z - 071505Z

    SUMMARY...Repeating heavy rain along stationary front over Middle
    to Upper Texas Coasts this morning. Embedded intense rates of
    2"/hr will continue over the next few hours with localized
    additional rain >4" and flash flooding possible immediately inland
    from the coast, but south of Houston proper.

    DISCUSSION...Ample Gulf moisture has surged back over the coast
    along a stationary front stretching from Matagorda Bay to the
    coastal border with Louisiana. Deep layer SWly flow around an
    centered over western OK is parallel to a stationary front along
    the coast which is limiting previous progression into the Gulf.
    This analysis is not seen in recent RAP runs which depict the
    front having pushed into the Gulf. So the 2" PW axis remains along
    the coast where the heavy rain is occurring. This moisture,
    combined with 2000 J/kg MUCAPE has allowed a line of heavy
    thunderstorms to develop.

    The SWly flow will allow motion in the orientation of the activity
    as fresh air moves in from the Gulf allowing redevelopment. KHGX
    has 1hr rainfall estimates of 1.5-2"/hr near Matagorda Bay to
    southern Brazoria County. Redevelopment ahead of a multi cell
    cluster just north of Matagorda Bay at 11Z, associated with a
    surface low, will continue allowing repeating heavy activity and
    the potential for 4" locally through about 14Z. This area has high
    FFG, so any flash flooding should be limited to urbanized areas.
    Since the front is quite strong, expect the heaviest activity to
    remain south of Houston proper, but should a concern for the
    Galveston area until the surface wave passes, shunting activity
    into the Gulf.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8SQNAKllMapIppT-eBOrPiOtp9w_sXB27hiOCgaLyrJyX2V9ZJdnew30CgQTsPdK2ssD= myYd3bPGNVZ4FG_PPvzsSCk$ for graphic product...

    ATTN...WFO...CRP...HGX...LCH...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 29829384 29679382 28949496 28489622 28909658=20
    29399543 29699465=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 7 12:54:11 2025
    AWUS01 KWNH 071254
    FFGMPD
    LAZ000-TXZ000-071805-

    Mesoscale Precipitation Discussion 0241
    NWS Weather Prediction Center College Park MD
    853 AM EDT Wed May 07 2025

    Areas affected...Southern Louisiana

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 071250Z - 071805Z

    SUMMARY...Continued repeating heavy rain through midday for far
    southern Louisiana. The focus is pushing into the Gulf, so the
    flash flood threat is considered possible, including for New
    Orleans.

    DISCUSSION...A stationary front remains over southern Louisiana,
    though outflow is noted from regional radar as pushing into the
    Gulf. There remains a heavy rain focus along the frontal boundary
    south of I-10 with rainfall rates around 1.5"/hr from KLCH and
    KHDC. This is despite IR GOES imagery depicting warming cloud tops
    over the past couple of hours.
    There is quite a PW gradient over southern LA with values of 1.75
    to 1.9" south of I-10 with an east-west gradient to instability
    with more over southwest LA (1500-2000 J/kg) vs southeast (around
    1000 J/kg). Deep layer SWly flow around 25kt with upwind
    propagation to the east will keep activity moving along the
    frontal boundary to in or near New Orleans over the next few hours.
    Southwest LA has been spared from the heavy rain of the past day,
    so this activity is moving into less susceptible areas (though
    NOLA is perpetually susceptible). The main flash flood threat
    through midday is for urbanized areas.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8H4X-GGB03tGW4Unu-S0YcXi5ZhWcY1HXPTD2CEfoOWP21S3iY3LlgGsXTRd83nQdg8d= Qy1nNOrA21L-PtNzZEtMNWs$ for graphic product...

    ATTN...WFO...LCH...LIX...

    ATTN...RFC...LMRFC...WGRFC...NWC...

    LAT...LON 30199118 30139021 30168943 29938900 29528952=20
    29098988 28979079 29319211 29519320 29599375=20
    29809393 30029345 30169261=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu May 8 17:24:28 2025
    AWUS01 KWNH 081724
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-082322-

    Mesoscale Precipitation Discussion 0242
    NWS Weather Prediction Center College Park MD
    122 PM EDT Thu May 08 2025

    Areas affected...portions of the Lower Ohio Valley and Tennessee

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 081722Z - 082322Z

    Summary...Slow-moving showers and thunderstorms are producing
    spots of 1-1.5 inch/hr rain rates at times across southern
    Illinois. These rates should continue, with storms translating
    slowly eastward toward central Kentucky and Middle Tennessee
    through 23Z/6p CDT.

    Discussion...A combination of factors was contributing to a
    focused area of convective development across western areas of the
    discussion area (from southern IL through northwestern TN) over
    the past couple hours: 1) insolation/surface destabilization
    occurring beneath a slow-moving mid/upper low over Missouri and 2)
    convergence along a synoptic front extending from near SAR
    east/northeast to ILN. Mid-level flow fields are relatively weak,
    resulting in slow-moving and weakly organized convection that has
    exhibited multiple cell mergers at times. Moisture/instability
    profiles are supporting areas of 1-1.5 inch rain rates beneath the
    most persistent convection and merging cells, which was resulting
    in areas of FFG exceedance especially where heavier rates have
    persisted for more than an hour.

    Models/obs suggest that the area of convection will gradually
    translate eastward mainly across Kentucky and Tennessee over the
    next 6 hours or so. Occasional cell mergers/spots of FFG
    exceedance are expected on an isolated basis. The combination of
    both propagation and newer downstream development of convective
    activity suggests that a modest increase in flash flood potential
    should occur from western Kentucky eastward through the I-65
    corridor, with central KY/middle TN risk peaking from 19Z onward.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4fCaYm9r0ehHkR4D9l6qqwC_5q7d8tDwYx0CkCOgAFh7NQs0zbI5vhWrbNC0-JfsdeLx= 5L4WgRG7ZH8HeV9vbfa1kFk$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...JKL...LMK...LSX...MEG...OHX...
    PAH...

    ATTN...RFC...LMRFC...NCRFC...OHRFC...NWC...

    LAT...LON 39278510 36568497 35828675 35698910 36469000=20
    37109006 37798970 38798762=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu May 8 20:33:31 2025
    AWUS01 KWNH 082033
    FFGMPD
    MEZ000-MAZ000-NHZ000-RIZ000-VTZ000-CTZ000-NYZ000-NJZ000-PAZ000-090130-

    Mesoscale Precipitation Discussion 0243
    NWS Weather Prediction Center College Park MD
    432 PM EDT Thu May 08 2025

    Areas affected...southern NY into southern/central New England

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 082030Z - 090130Z

    Summary...Isolated to widely scattered areas of flash flooding
    will be possible across parts of southern NY into southern/central
    New England through late evening. Hourly rainfall of 1-2 inches
    with localized totals between 2 and 3 inches will be possible with
    activity likely diminishing in coverage and intensity after
    sunset.

    Discussion...20Z visible satellite and radar imagery showed
    scattered showers and thunderstorms in the vicinity of a wavy
    stationary front analyzed from coastal ME into southern
    NY/northern NJ. Earlier breaks in cloud cover and daytime heating
    have allowed for the development of weak instability (MLCAPE up to
    and locally in excess of 500 J/kg along the front over southern
    New England via SPC mesoanalysis). GPS data showed PWATs were
    modest, hovering near 1 inch but cell motions should be a bit
    slower, somewhere between 10-20 kt from the southwest.

    The coverage of showers and thunderstorms is expected to increase
    within the corridor between the front and a sea breeze boundary
    over southern CT into RI over the next couple of hours. The front
    is also forecast by the RAP to sweep southward, west of a surface
    low in east-central MA. Cell mergers, subsequent outflow and brief
    training with similar cell movement and boundary orientations
    could support a few spots with hourly rainfall between 1-2 inches
    and perhaps storm totals between 2 and 3 inches prior to expected
    dissipation after the loss of daytime heating.

    The expected total rainfall is certainly on the low side, but it
    may fall somewhat quickly atop a region of the Northeast which has
    seen 200 to 400+ percent of average rainfall over the past 7 days,
    leaving soil moisture values above average. This fact, combined
    with the urban nature of the region and rush hour could result in
    isolated to widely scattered instances of flash flooding over the
    next 3-5 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!87id6Yox9IhGQA9HdHtf3d_vLLf1C6f81DsThCFm63wkFilMFkRxMEhyLrC0EKCFEKV9= 4GX2HSU5d-3iJR46ZAZywZ8$ for graphic product...

    ATTN...WFO...ALY...BGM...BOX...GYX...OKX...PHI...

    ATTN...RFC...MARFC...NERFC...NWC...

    LAT...LON 43377142 43217065 42647056 41757136 41257259=20
    40927338 40577412 40657450 40757467 40967485=20
    41227493 41747460 42637294=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 9 00:16:03 2025
    AWUS01 KWNH 090015
    FFGMPD
    TXZ000-090345-

    Mesoscale Precipitation Discussion 0244
    NWS Weather Prediction Center College Park MD
    814 PM EDT Thu May 08 2025

    Areas affected...southern TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 090012Z - 090345Z

    SUMMARY...Localized flash flooding will be possible across
    portions of southern TX with high rainfall rates of 2-3 in/hr and
    isolated totals of 3-5 inches over the next 2-4 hours.

    DISCUSSION...Radar imagery through 00Z showed an uptick in
    thunderstorm coverage to the northwest of Corpus Christi across
    the I-37 corridor where outflows were merging. Upstream, a pair of
    thunderstorm clusters were advancing toward the ESE from the Rio
    Grande between Eagle Pass and Laredo, co-located with an MCV-like
    feature, as well as a cluster just east of I-35 near Cotulla. The
    environment over southern TX was unstable with 500-2000 J/kg
    MLCAPE although pockets of CIN were present near the coast from
    earlier storms via SPC mesoanalysis data.

    It appears probable that lift out ahead of the east-southeastward
    advancing circulation/convective clusters to the west and
    divergent/diffluent flow aloft, will continue to encourage
    convective development downstream. Following a general ESE motion
    over the next 2-4 hours will support cell mergers and occasional
    slow propagation which could support high rainfall rates of 2-3
    in/hr and perhaps localized totals of 3-5 inches through ~04Z over
    portions of southern TX. Due to relatively high FFG values across
    southern TX, any flash flooding that develops would likely be tied
    to impervious surfaces tied to towns/cities within the path of the
    advancing clusters of heavy rain.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6KB8RRc3fnDIWuIC2LQoVX5D0kGRB3lGvSlUEWloEYUuAae8J6BPPBS64skxZMEN9VDh= rHMH93A0OSkO0bOlOr8RvVc$ for graphic product...

    ATTN...WFO...BRO...CRP...EWX...

    ATTN...RFC...WGRFC...NWC...

    LAT...LON 28999961 28779793 28609693 28279665 27789692=20
    26899732 26859836 26909945 27399975 27860010=20
    28160046 28590042=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 9 03:11:34 2025
    AWUS01 KWNH 090311
    FFGMPD
    NCZ000-SCZ000-GAZ000-TNZ000-090700-

    Mesoscale Precipitation Discussion 0245
    NWS Weather Prediction Center College Park MD
    1110 PM EDT Thu May 08 2025

    Areas affected...southwestern NC, northwestern SC and northern GA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 090300Z - 090700Z

    Summary...Continued localized rainfall rates up to 1-2"/hr may
    train and repeat over the same areas over the next several hours,
    likely resulting in isolated to scattered instances of flash
    flooding (with short-term totals of up to 3-5").

    Discussion...Ongoing convection over the TN/NC/GA/SC border region
    is tending to align in a west-to-east training axis, along an
    effective low-level front (most pronounced at 1000-925 mb, per
    SPC's SFCOA 02z analysis, but also apparent from 925-700 mb). This
    low-level convergence is being driven by inflow/moisture transport
    from the S-SW (10-20 kts from 925-850 mb), which is isentropically
    ascending over rain-cooled outflow from earlier storms (and is
    most apparent in the surface theta E gradient which ranges from
    336K to the south to 324K to the north across the MPD).
    Significant upper-level divergence is complementing the low-level
    convergence, as the region is located near a phased jet structure
    in the right-entrance region of a ~90 kt jet streak centered near
    the Delmarva and the left-exit region of an increasingly defined,
    broader jet streak spanning much of the Deep South (with the
    latter becoming more of the primary influence over time).
    Otherwise, the mesoscale environment is characterized by MUCAPE of
    500-1000 J/kg (plenty sufficient on its own, and possibly
    underselling the influence of slantwise instability via isentropic
    ascent), precipitable water values of 1.1-1.4 inches (between the
    75th and 90th percentile, per GSO sounding climatology), and
    effective bulk shear of 30-40 kts.

    While convection should have the tendency to propagate towards
    towards the southeast over the course of the night (out of the MPD
    area and into sandy soils beyond the fall line into the coastal
    plain of SC/GA), there may be a several hour period where
    convection trains from west-to-east near the aforementioned
    effective front (as the upwind propagation vector, subtracting the
    850 mb flow from the mean flow of the cloud bearing layer,
    supports more due easterly storm motions parallel to the effective
    front, as observational trends indicate backbuilding of cells over
    the GA/TN/NC border region). Some of the most recent hi-res
    guidance (00z ARW/ARW2 and select recent runs of both the HRRR and
    experimental RRFS) indicate the potential for localized 3-5"
    totals (driven by rainfall rates of up to 1-2"/hr, per both
    observational trends and hi-res model data). With FLASH CREST unit
    flow data already indicating localized instances of flash flooding
    ongoing, expect areal coverage of flash flooding to expand over
    the next several hours (with isolated to scattered instances of
    flash flooding being likely, given 3-hr FFGs generally ranging
    from 2.0-3.0" and the increasing likelihood of training
    seagmants).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4_Jt7mYsymeIj8vFAihyPIwAgiiRq7m7doaZpWVaYwt19kPJ-VVpS9FacR02mtsnY5oU= wUMwCuLdsP2BL2ibItKfuMU$ for graphic product...

    ATTN...WFO...CAE...FFC...GSP...MRX...RAH...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 35638217 35548068 35247990 34538040 34098097=20
    33728220 33988352 34338519 34818538 35098492=20
    35328380=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 10 19:22:27 2025
    AWUS01 KWNH 101922
    FFGMPD
    ALZ000-MSZ000-110120-

    Mesoscale Precipitation Discussion 0250
    NWS Weather Prediction Center College Park MD
    321 PM EDT Sat May 10 2025

    Areas affected...Central/Eastern MS...Western /Central AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 101920Z - 110120Z

    SUMMARY...Some focused areas of heavy rainfall from slow-moving
    and locally training showers and thunderstorms may result in at
    least isolated areas of flash flooding heading through the
    afternoon and early evening hours.

    DISCUSSION...The latest GOES-E visible satellite imagery shows a
    fair amount of clearing across central and southern AL with strong
    solar insolation ensuing. This is destabilizing the boundary layer
    with the latest RAP analysis showing a nose of MLCAPE values of
    500 to 1000 J/kg already nosing up around the northeast flank of
    surface low pressure over eastern MS.

    The greater instability is over much of southern AL, but with
    additional surface heating and convergent deep layer flow
    associated the slow-moving upper-level low/trough over the South,
    there should be a corridor of higher instability that wraps up
    across areas of central AL and into eastern MS which will be in
    close proximity to a frontal occlusion.

    Slow-moving bands of heavy showers and thunderstorms are expected
    to evolve over the next several hours which will be supported by
    divergent flow aloft around the northeast flank of the closed low
    and the presence of frontal convergence and increasingly favorable thermodynamic environment.

    Rainfall rates of 1 to 2 inches/hour are likely with the stronger
    convective cells, and with slow cell-motions and some training
    concerns, there may be some rainfall totals of 3 to 4 inches that
    materialize with potential for spotty heavier amounts. This is
    generally consistent with the 12Z HREF guidance which shows a 40%
    to 60% chance of 6-hour rainfall totals exceeding 3 inches across
    portions of west-central AL, with somewhat lower probabilities
    into eastern MS.

    Given the moist antecedent conditions that are in place and these
    additional rainfall totals going through the early evening hours,
    at least some isolated areas of flash flooding will be possible.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5bzox7HEe9SRMJoOJek5nXeEKsflhzJYE_YpTLDDpxADiviCG7Ua5ZQubEz9Bw8sSTUH= vnIHOVIqIwDOI8gkNGIXRog$ for graphic product...

    ATTN...WFO...BMX...JAN...MEG...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 33908817 33668730 32918671 32118670 31848758=20
    32368861 32079004 32219078 33019082 33529025=20
    33848945=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 10 22:22:12 2025
    AWUS01 KWNH 102221
    FFGMPD
    GAZ000-110420-

    Mesoscale Precipitation Discussion 0251
    NWS Weather Prediction Center College Park MD
    620 PM EDT Sat May 10 2025

    Areas affected...Central GA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 102220Z - 110420Z

    SUMMARY...Slow-moving supercellular MCS cluster over central GA
    may result in sufficiently high enough rainfall rates for some
    isolated flash flooding concerns this evening.

    DISCUSSION...A long-lived supercellular MCS cluster moving
    gradually through central GA continues to remain very
    well-organized and has been tending to gradually track a tad to
    the right over the last few hours as it begins to interact with a
    warm front draped west to east across the region.

    Much of the convection is aligned with a rather strong instability
    gradient with as much as 1500 J/kg of MLCAPE pooled along the
    front. Meanwhile, there is favorable shear in place with 0-3 km
    effective bulk shear values of 30 to 40 kts which is playing a
    role in maintaining the supercell character of the convective
    mass. PWs across the region are quite moist with values of as much
    as 1.6 to 1.7 inches and this is running a solid 1.5 to 2 standard
    deviations above normal.

    Rainfall rates are impressively high with dual-pol radar showing
    hourly rainfall totals reaching 1.5 to 2.5 inches. The slow
    cell-motions overall with this activity are yielding heavier
    3-hour totals that have been on the order of 3 to 4+ inches based
    on MRMS data.

    Over the next few hours, the HRRR and RRFS guidance suggest a
    continuation of well-organized clusters of strong convection
    impacting areas of central GA with high rainfall rates that are
    likely to still reach 1.5 to 2.5 inches/hour. The HRRR guidance
    this evening in particular shows some back-building cells around
    the southwest flanks of the convection in association with a
    persistently moist southerly low-level jet of 30 to 40 kts, and
    this may help drive small-scale focused areas of heavier rainfall
    amounts that may reach 5+ inches.

    The 18Z HREF and 12Z REFS ensemble suites both suggest at least
    low-end probabilities (20% to 30%) of seeing the 3-hour FFG values
    exceeded going through 03Z/11 PM EDT. Therefore, at least an
    isolated threat for flash flooding is expected to exist this
    evening across central GA, with the more urbanized locations at
    greatest risk for impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4EXeqx2txJ9LjwExBFkX8L-ph7QLv6NombxP22FJV4jHUoQAHF591i3PpAhrj2JnJ681= kqqYG-RYeI9OQXYdnAoCeM0$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 33608236 33228194 32548200 31958269 31748353=20
    31718430 32268464 33188397 33578319=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 9 17:17:12 2025
    AWUS01 KWNH 091717
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-092215-

    Mesoscale Precipitation Discussion 0246
    NWS Weather Prediction Center College Park MD
    116 PM EDT Fri May 09 2025

    Areas affected...Southeastern Louisiana and the Central Gulf Coast

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 091715Z - 092215Z

    SUMMARY...Heavy rain threat for southeast Louisiana through the
    central Gulf Coast continues through this afternoon. Convergence
    of ongoing activity over southern Louisiana that should lift
    northeast raises a localized flash flooding threat for vulnerable
    areas including Lafayette, Baton Rouge, New Orleans, and Mobile.

    DISCUSSION...A positively tilted upper trough over the Mid-South
    this afternoon is providing broad scale moisture advection to the
    Central Gulf Coast. A pair of surface lows over southwest and
    southeast LA have slow-moving heavy thunderstorms that are
    producing 2-3" in two hours per regional radar and rain gauges.
    Continued low level 15-20kt southerly flow between these features,
    MLCAPE of 500-1000 J/kg, and lift from the right entrance region
    of an 80kt jet to the north should allow further development to
    the east/north which includes the I-10 corridor and vulnerable
    metro areas.
    This area has seen 2-5" rainfall over the past few days with
    saturated soil helping vulnerability to extend somewhat beyond the
    typical vulnerable urban areas from Lafayette to Mobile. Flash
    flooding is considered possible through this afternoon with
    additional threats this evening as the system slowly shifts east.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6lgD9AHtQs1kP2SuZ2Cs0-dpGYAHCKR2GdmZrbRJczfbfRYdLoyz8GRCum46ue79gM6W= 5WckfwUznojRbEbbJe-GvPk$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 31028791 30868695 30338721 30058826 29898918=20
    29448957 29179016 29549171 29999255 30449211=20
    30669095 30809024 30938888=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 9 20:19:46 2025
    AWUS01 KWNH 092017
    FFGMPD
    FLZ000-GAZ000-ALZ000-100115-

    Mesoscale Precipitation Discussion 0247
    NWS Weather Prediction Center College Park MD
    416 PM EDT Fri May 09 2025

    Areas affected...FL Panhandle...Far Southwest GA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 092015Z - 100115Z

    SUMMARY...Slow-moving thunderstorms across portions of the FL
    Panhandle and far southwest GA over the next several hours may
    result in isolated areas of flash flooding.

    DISCUSSION...The latest radar imagery continues to show several
    slow-moving areas of thunderstorms across portions of the FL
    Panhandle and far southwest GA. The convection has been forming
    over the last couple of hours in close proximity to a frontal zone
    draped across the region. A rather substantial pool of moisture
    and instability is focused along this boundary with MLCAPE values
    of locally near 1500 J/kg and PWs of 1.6 to 1.8 inches.

    An upper-level trough upstream approaching the central Gulf Coast
    will tend to favor some downstream upper-level divergence
    downstream over the FL Panhandle going through the remainder of
    the afternoon and into the early evening hours. This coupled with
    the favorable thermodynamic environment should tend to favor
    convective sustenance over the next several hours near the front
    where this is also a corridor of at least modest moisture
    convergence.

    There will be some potential for backbuilding and training of
    convective cells, and especially with some modest increase in the
    low-level flow expected near the front. The presence of
    smaller-scale cold pools/outflow boundaries will also tend to act
    as secondary catalysts for regenerating convective cells.

    Recent RRFS guidance has been tending to handle the ongoing
    convective cells rather well, and suggests some localized 3 to 5
    inch rainfall totals going through early this evening which will
    be supported by rainfall rates of up 2 to 2.5 inches/hour.

    Isolated areas of flash flooding will be possible as a result and
    especially if any of these stronger storms and heavier rainfall
    rates focus over the more urbanized locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6S39g1jTilYW1hSyyOiUBx7BDpsR9RRGNv3D8FIg2HPmTgOw-nv9hQILHvGnWGOz5qCe= koBR8IRBMK3CAtNgtzq_EIM$ for graphic product...

    ATTN...WFO...JAX...MOB...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 31108480 30988355 30768312 30478315 30258435=20
    30208561 30398702 30858723 31058636=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 10 06:05:12 2025
    AWUS01 KWNH 100604
    FFGMPD
    FLZ000-ALZ000-MSZ000-101200-

    Mesoscale Precipitation Discussion 0248
    NWS Weather Prediction Center College Park MD
    203 AM EDT Sat May 10 2025

    Areas affected...portions of far southern AL/MS into the FL
    Panhandle

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 100600Z - 101200Z

    Summary...Localized rainfall rates of up to 2-3"/hr may result in
    short-term totals of 5"+ through 7am CDT. Isolated instances of
    flash flooding are possible (and could be locally significant over
    more sensitive low-lying and metro areas).

    Discussion...A deep layer (surface to 500 mb) vertically tilted
    cut-off low is becoming more convectively active over the past few
    hours near the low-level (surface to 850 mb) center (just offshore
    southeast LA and southern MS). GOES-East infrared imagery depicts
    cooling cloud tops in association with this recent deep
    convection, though a rainband farther east (within the core of the
    warm conveyor belt) has maintained more impressive cold cloud tops
    with occasional overshooting tops. Both areas of convection are
    only just beginning to come ashore, though lapse rates remain
    unimpressive both in the vicinity of the convection and well
    onshore of both areas (max 2-6 km lapse rates of less than 7deg
    C/km). That said, a corridor of increasing instability (+300-600
    J/kg) is evident over the past several hours in association with
    the convection near the core of the low-level center (with little
    change so far in instability farther east into the FL Panhandle).
    CIRA composite advected layer precipitable water (PWAT) imagery
    depicts a clear increase in low-level PWAT (sfc-850 mb and 850-700
    mb layers), pivoting around the center of the low-level
    circulation (with both NEXRAD VWP and GOES Derived Motion Wind
    Vectors (DMW) indicating 15-25 kt flow around a well-defined
    surface circulation from an ideally placed ~330z ASCAT pass).
    Total PWATs range from 1.7-1.9 inches (between the 90th percentile
    and max moving average, per LIX sounding climatology), and
    low-level moisture transport and convergence (iscentropically
    ascending) is also being complemented by upper-level diffluence
    (also evident in NEXRAD VWP and GOES DMW between 400-250 mb) with
    deep layer (0-6 km) shear of 30-50 kts.

    The latest hi-res guidance (00z HREF suite, 18z REFS suite, and
    more recent runs of both the HRRR and RRFS) generally indicates
    the potential for extreme localized rainfall rates (2-3"/hr) with
    resulting isolated totals of 3-6"+ through 12z. The spatial
    disparities in these high QPF totals are relatively wide, but have
    come into better agreement (with 00z guidance onward) in depicting
    the greatest potential for localized 5"+ totals in the vicinity of
    the low-level center (confined to far southern portions of MS/AL,
    possibly extending into the far western FL Panhandle). This is
    consistent with the most recent observational trends, and 00z HREF
    40-km exceedance probabilities for 5" are indicated to be as high
    as 10-20% (with corresponding 100-yr ARI exceedance probabilities
    of 5%). Given the high uncertainty in the manifestation of these
    localized extreme rainfall rates/totals (which are largely
    conditionally dependent on localized backbuilding of convection
    near the low center), isolated instances of flash flooding are
    considered to be possible. Given the proximity to relatively
    sensitive low-lying and urbanized metropolitan areas (with 3-6
    hour Flash Flood Guidance as low as 1.5-2.0"), locally significant
    flash flooding is also possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4IwHcuJaidVMrh3-h8vB5amiBRsLWyUx5QUfof5c6c67F5wN5s7RgdhJTfIW49aXw5w5= vCEGlp7VOPbfPrbzIZT0-60$ for graphic product...

    ATTN...WFO...LIX...MOB...TAE...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 31188815 31148755 31018700 30838646 30788588=20
    30688535 30578502 30398468 30088453 29828468=20
    29588498 29708537 30048582 30268632 30278684=20
    30238745 30238749 30198859 30228915 30548913=20
    30878871=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 10 17:58:06 2025
    AWUS01 KWNH 101757
    FFGMPD
    FLZ000-GAZ000-ALZ000-102256-

    Mesoscale Precipitation Discussion 0249
    NWS Weather Prediction Center College Park MD
    156 PM EDT Sat May 10 2025

    Areas affected...Florida Panhandle into Alabama and Georgia

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 101756Z - 102256Z

    SUMMARY...Repeating thunderstorms moving north from the eastern
    Florida Panhandle into Alabama and Georgia rest of this afternoon
    may result in localized flash flooding.

    DISCUSSION...A multi-cell thunderstorm cluster with hourly
    rainfall rates of 1.5-2"/hr has developed from the eastern FL
    Panhandle through far southeast AL per regional radar. This
    activity expanded in the past couple of hours from an isolated
    supercell in a renewed warm conveyor belt lifting from the Gulf
    east of an upper low centered over southern MS. PW of 1.75" and
    MLCAPE >1500 J/kg in this axis will enable further development.
    Strong southerly flow from the Gulf around 35kt and a warm frontal
    boundary across this axis will allow this development to continue
    to be along the axis, causing repeating heavy thunderstorms and
    thus a flash flood risk.

    Recent HRRR runs depict a risk of 2-4" rainfall over the next few
    hours. Areas in the eastern FL Panhandle received 3-5" rainfall
    since last night where vulnerability is greater. Areas in
    southeast AL/southwest GA have only received around an inch of
    rain over the past week and are less vulnerable. Localized flash
    flooding will be possible where the most repeating occurs and over
    more urbanized locations.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6v2Of1QKyUsGiQVxQasG5djFuXW-5FiQn-JiuEL1vbyS9JUyzfIH2by-rIHK_9oApbcC= BF6AYr7kb-JLgam2nLru60w$ for graphic product...

    ATTN...WFO...BMX...FFC...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 32938504 32498415 31098441 29608515 30198600=20
    30888589 31978595 32728564=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 11 11:33:34 2025
    AWUS01 KWNH 111133
    FFGMPD
    FLZ000-GAZ000-ALZ000-111530-

    Mesoscale Precipitation Discussion 0252
    NWS Weather Prediction Center College Park MD
    732 AM EDT Sun May 11 2025

    Areas affected...Florida Panhandle into Southeast Alabama

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 111132Z - 111530Z

    SUMMARY...
    Locally heavy rainfall with rates over 3 inches per hour remain
    possible through the morning as training storms line up along a
    stationary front. Ongoing flash flooding likely to worsen...

    DISCUSSION...
    A surface stationary front and a large nearly stationary upper
    level low will act as the forcing mechanisms for continued deep
    convection over a portion of the Florida Panhandle into
    southeastern Alabama this morning. The front is drawing very moist
    air with PWATs to 1.8 inches northward on a 20-30 kt SSE flow at
    850. A shortwave rounding the southeastern periphery of this low
    is likely further enhancing convective development as the storms
    take advantage of convective instability caused by a very dry air
    mass aloft overtopping the very moist air mass near the surface.

    The latest HRRR runs are capturing the current convective setup
    across this region fairly well, and suggest for the next 4 hours
    or so that the training line of storms will continue moving almost
    due north into the Florida Panhandle and continuing into
    southeastern Alabama. A few other CAMs suggest that the storms may
    drift east with time, but the rate of eastward movement is
    uncertain and so far hasn't materialized yet...though developing
    convection offshore to the east of the line may try to drift west
    and merge with the storms, likely disrupting the training, even if
    temporarily.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6Qx4T2Dt7eNyw0jDLWUrpjPC1bzRw5q8wkFXji2OlPVWrNpTn2jH6AYeCgC_6m20mmkp= 1bc7Pf433r1SEiqeOxPJKrM$ for graphic product...

    ATTN...WFO...BMX...MOB...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 32018570 31928516 31858506 31598478 30698458=20
    30208466 29638485 29638525 29958549 30188589=20
    30368639 30378634 30738631 31198627 31858610=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 11 15:33:03 2025
    AWUS01 KWNH 111532
    FFGMPD
    SCZ000-GAZ000-112131-

    Mesoscale Precipitation Discussion 0253
    NWS Weather Prediction Center College Park MD
    1131 AM EDT Sun May 11 2025

    Areas affected...Eastern Georgia into Southwestern South Carolina

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 111531Z - 112131Z

    SUMMARY...
    A slow-moving line of training thunderstorms has developed across
    eastern Georgia. Flash flooding will be possible as rainfall rates
    with the strongest cores up to 3 inches per hour.

    DISCUSSION... A nearly stationary line of storms has developed
    across eastern Georgia in a north-south line. A moisture gradient
    has set up in a pseudo dry line but in the mid levels based on 850
    mb SPC mesoanalysis. On the dry side the dewpoints are as low as
    6C over central Georgia, whereas on the moist side they're as high
    as 13C. Thus, this is a robust gradient of moisture over the area.
    The storms have formed on the moist side of that gradient, which
    appear unlikely to move much over the next several hours. This
    will support the potential for multiple hours of heavy rain over
    the area.

    HRRR and RRFS model simulations of reflectivity suggest the storms
    will persist into the afternoon hours across this area, although
    the behavior of individual heavy rain cores will vary through this
    period. One of the biggest points of uncertainty is how the line
    of convection will behave once the storms entering far southern
    Georgia from the Florida Panhandle reach the latitude of the line
    of storms in eastern Georgia. Assuming the mid-level dry line
    weakens or dissipates as the storms tracking from Florida
    approach, this should diminish the local forcing allowing the
    storms to stay in place, resulting in an overall weakening of the
    storms and a lessening flash flood threat. However, the RRFS
    suggests that with daytime heating in full swing, that more storms
    may form along the coast and result in a new training line
    potentially linked to the sea breeze or the frictional gradient
    along the coast resulting from the predominant onshore
    southeasterly flow.

    While 12Z FFGs in the area of these training storms are around 3
    inches in an hour and 4 inches in 3 hours, the latter criterion
    could very well be exceeded with the persistence of thses storms
    over the next few hours. Flash flooding is possible.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_Oe3WXUCUFQaahADO9ociChMaAxsZC1GLrH26bZKgdabaOUdu7XkMBHVOf-OqpxgawPf= giZemuLia3jKuIYmtmn32nA$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...JAX...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 33888267 33868195 33528151 33078117 32518097=20
    32028124 31188169 30938256 31538343 32088362=20
    32448358 32968346 33448303=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 11 19:33:27 2025
    AWUS01 KWNH 111932
    FFGMPD
    ALZ000-MSZ000-120130-

    Mesoscale Precipitation Discussion 0254
    NWS Weather Prediction Center College Park MD
    331 PM EDT Sun May 11 2025

    Areas affected...Central to Southeast MS...Central and Western AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 111930Z - 120130Z

    SUMMARY...Developing bands of showers and thunderstorms will tend
    to expand in coverage going through early this evening. Some
    cell-training with heavy rainfall rates and also moist antecedent
    conditions will favor a threat for isolated to scattered areas of
    flash flooding.

    DISCUSSION...The mid-afternoon GOES-E visible satellite imagery
    shows a developing CU/TCU field across much of central to
    southeast MS and through western AL as diurnal heating/solar
    insolation work to destabilize the boundary layer in close
    proximity to a frontal occlusion. In fact, LightningCast data
    coupled with radar imagery does show convective initiation taking
    place with a few small-scale bands of convection beginning to
    organize over eastern MS and western AL

    A deep layer trough/closed low continues to pivot across the lower
    MS Valley, and this deep layer cyclonic flow coupled with the
    improving thermodynamic environment should support developing and
    expanding bands of convection going through the early evening
    hours.

    MLCAPE values have risen to as much as 1000 to 1500 J/kg with
    3-hour CAPE differentials of 600+ J/kg and this coupled with an
    expected increase in moisture convergence near the frontal
    occlusion should set the stage for convection that will be capable
    of producing rainfall rates of 1 to 2 inches/hour along with
    concerns for cell-training given the unidirectional deep layer
    cyclonic flow.

    The most recent 12Z HREF guidance along with recent HRRR and RRFS
    solutions support the potential for some bands of convection to
    produce rainfall amounts through early this evening of 2 to 4
    inches. These rains coupled with the moist and locally wet
    antecedent conditions will favor a setup that may yield isolated
    to scattered areas of flash flooding and especially where any
    cell-training occurs.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!40BjZmTCG-9k0PUnZylJS3HLlMlPI7F1UH2yybxvcJhEmxLuuA96ZBvrUiEJdAZB7IeN= QVFwNqII89Kx2OxixplWu0A$ for graphic product...

    ATTN...WFO...BMX...JAN...MEG...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34438949 33938803 32938714 32168694 31398723=20
    31078770 30928820 31138885 31718922 32348971=20
    33519061 34159056=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 11 20:58:24 2025
    AWUS01 KWNH 112057
    FFGMPD
    SCZ000-GAZ000-120255-

    Mesoscale Precipitation Discussion 0255
    NWS Weather Prediction Center College Park MD
    456 PM EDT Sun May 11 2025

    Areas affected...Portions of Central and Eastern GA...SC Midlands
    and Lowcountry

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 112055Z - 120255Z

    SUMMARY...Scattered areas of flash flooding will be likely going
    through the early to mid-evening hours from locally slow-moving
    and training showers and thunderstorms.

    DISCUSSION...The latest radar and satellite imagery shows an
    expansive area of heavy showers and thunderstorms impacting areas
    of central/eastern GA and through western/central SC as a deep
    layer southerly conveyor belt of warm and moist air lifts into the
    Southeast U.S. and interacts with a stationary front draped west
    to east across southern GA and the SC Lowcountry.

    The deep layer moisture transport is well-defined around the
    eastern flank of a deep layer trough/closed low over the lower MS Valley/western Gulf Coast region and has tropical origins with
    moisture seen in CIRA-ALPW advancing north up from Central America
    and the western Caribbean Sea across the eastern Gulf Coast region
    and into the Southeast U.S. PW values are 1.75+ inches which are a
    solid 2 to 2.5 standard deviations above normal, and the latest
    850/700 mb moisture flux anomalies are as much as 2 to 4 standard
    deviations above normal.

    This moisture transport and warm air advection will continue to
    support strong isentropic ascent across central and eastern GA and
    the SC Lowcountry through this evening which combined with
    moderate instability near the aforementioned front will support
    areas of organized convection with heavy rainfall rates. MLCAPE
    values across areas of southeast GA are still on the order of 1500
    J/kg with a strongly convergent low-level flow pattern in place
    given proximity of the front. However, the recent convective
    activity has resulted in some lowering of CAPE values over the
    last few hours.

    Nevertheless, expect sufficient levels of forcing and instability
    to continue going into the evening hours for additional rounds of
    heavy showers and thunderstorms which will be capable of producing
    rainfall rates of up to 1.5 to 2.5 inches/hour with the stronger
    convective cores, and especially with the efficient/moist deep
    layer tropical origins of the moisture transport.

    Areas of far eastern GA and possibly getting into areas of the SC
    Lowcountry will need to be closely monitored this evening for
    areas of notable cell-training as the convection here should be
    stronger and more focused with alignment also with the deeper
    layer steering flow. A wave of low pressure traversing the
    stationary front will be a key player in driving this threat.

    Some additional rainfall totals may reach 3 to 5+ inches
    (supported be HRRR and RRFS solutions), and given the rainfall
    that has already occurred, there will likely be scattered areas of
    flash flooding. This will include an urban flash flood threat,
    with even major metropolitan areas well to the north including
    Atlanta, GA and Columbia, SC potentially seeing some urban
    flooding concerns from heavy rainfall.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-PQNebJgmP1ejftQdPTKYsNq38Pe_C5zhc11_orRsASTcEKKmm_MlpI0cl_96R4J4cha= O7Ln1hUrQxIGMPBkSrABizo$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...JAX...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 34338150 34078036 32928007 32298059 31808105=20
    31278122 31168179 32068257 32358384 33058499=20
    33688492 33888415 33718258=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 12 01:31:43 2025
    AWUS01 KWNH 120131
    FFGMPD
    TNZ000-ALZ000-MSZ000-ARZ000-120730-

    Mesoscale Precipitation Discussion 0256
    NWS Weather Prediction Center College Park MD
    930 PM EDT Sun May 11 2025

    Areas affected...Northwest to Central MS...Central and Southern AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 120130Z - 120730Z

    SUMMARY...Bands of showers and thunderstorms will continue into
    the overnight hours across areas of northwest to central MS along
    with adjacent areas of central and southern AL. Concerns for
    cell-training with heavy rainfall rates will pose a threat for
    scattered areas of flash flooding.

    DISCUSSION...The early evening GOES-E IR satellite imagery shows
    an elongated southeast/northwest axis of relatively cold-topped
    convection continuing to impact areas of central and southern AL
    up across central to northwest MS. The bands of convection which
    are linear in nature remain concentrated rather close to a frontal
    occlusion and are persisting within a moist and moderately
    unstable airmass with the aid of divergent flow aloft around the
    northeast flank of the deep layer trough/closed low over the lower
    MS Valley.

    MLCAPE values remain locally on the order of 1000 to 1500 J/kg
    with PWs of near 1.5 inches, and this coupled with some modest
    shear parameters has been supporting rainfall rates of 1 to 2
    inches/hour with the stronger convective cores.

    There is a fair amount moisture convergence noted near the
    aforementioned frontal occlusion, and this coupled with the
    orientation of the convection with the deeper layer cyclonic flow
    should continue to yield linear convective structures that will be
    conducive for cell-training.

    The latest hires model guidance led by the HRRR and the RRFS
    collectively support as much as an additional 2 to 4 inches of
    rain going through 06Z (1AM CDT). The additional rains are
    expected to largely fall on areas that have seen recent rainfall,
    and thus with moist/wet antecedent conditions in place, there will
    continue to be a concern for scattered areas of flash flooding
    going into the overnight hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_S-7MAxSPke3GGhNJFikWZviEcceWn2e7YQ5cSsQEH7acwGWDohIE35xjVUZmDtlFu86= SMupNjXu7PuUylyaeQlBq80$ for graphic product...

    ATTN...WFO...BMX...JAN...MEG...MOB...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 35148972 33888795 33428640 32868585 31808589=20
    31348657 31368781 31568850 31848912 32498973=20
    33519061 34799086=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 12 02:23:18 2025
    AWUS01 KWNH 120221
    FFGMPD
    SCZ000-FLZ000-GAZ000-120820-

    Mesoscale Precipitation Discussion 0257
    NWS Weather Prediction Center College Park MD
    1020 PM EDT Sun May 11 2025

    Areas affected...Central and Southeast GA...SC Midlands and
    Lowcountry

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 120220Z - 120820Z

    SUMMARY...Additional rounds of heavy showers and thunderstorms
    overnight will continue to promote concerns for scattered areas of
    flash flooding heading into the overnight hours.

    DISCUSSION...The latest radar and satellite imagery is showing new
    rounds of heavy showers and thunderstorms lifting up across
    northern FL and stretching up across areas central to southeast GA
    and into far southern SC. This again is being supported by a deep
    layer southerly conveyor belt of warm and moist air lifting into
    the Southeast U.S. while interacting with a quasi-stationary
    frontal zone draped across far southern GA and up across coastal
    areas of SC.

    The deep layer moisture transport remains well-defined around the
    eastern flank of a deep layer trough/closed low over the lower MS Valley/western Gulf Coast region and continues to have tropical
    origins with moisture seen in CIRA-ALPW advancing north up from
    Central America and the western Caribbean Sea across the eastern
    Gulf Coast/FL Peninsula and into the Southeast U.S. coastal plain.
    00Z RAOB data shows PWs generally near or a little above 1.75
    inches which is 2 to 2.5 standard deviations above normal.

    This moisture transport and warm air advection will continue to
    support strong isentropic ascent across eastern GA and the SC
    Lowcountry going into the overnight hours which coupled with the
    frontal convergence and pooling of instability along it will favor
    additional concentrated areas of convection with heavy rainfall
    rates.

    MLCAPE values across coastal areas of GA and the SC Lowcountry are
    on the order of 1000+ J/kg and are being aided by cyclonic
    low-level flow off the warmer waters of the nearby Gulf Stream.
    Favorable shear parameters are in place too, and thus the
    environment will be conducive for some organized convective cells
    with high rainfall rates capable of reaching 1.5 to 2.5
    inches/hour.

    The recent runs of the HRRR/RRFS guidance and also the 18Z
    HREF/12Z REFS ensemble solutions support the potential for
    additional rainfall totals reaching 3 to 5 inches. This will
    support a continued threat for scattered areas of flash flooding
    heading into the overnight hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8WF7wnE_Vld1EJtp-iCOc0LihFjsIFoY6V_v5duHBRtQTw_psBDB8h2ni18qM8AzdxFg= 052o9i4SQ4SmUHBvMcGbRzA$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...ILM...JAX...TAE...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 34348071 33827990 32817999 32108053 31468104=20
    30578150 30468233 30788297 31638315 33048272=20
    34058190=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 12 07:36:03 2025
    AWUS01 KWNH 120734
    FFGMPD
    ALZ000-121100-

    Mesoscale Precipitation Discussion 0258
    NWS Weather Prediction Center College Park MD
    333 AM EDT Mon May 12 2025

    Areas affected...portions of eastern AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 120730Z - 121100Z

    Summary...Continued hourly rainfall totals of up to 1-2" are
    likely to result in localized 2-3" accumulations over the next
    several hours. Isolated to scattered instances of flash flooding
    are possible.=20

    Discussion...Persistent boundary layer moisture flux convergence
    just to the north of the triple point of a vertically stacked,
    deep layer (sfc-200 mb) cut-off low/cyclone is maintaining a
    cluster of thunderstorms across east-central AL (with MRMS
    estimating localized hourly totals as high as 1-2" at times). The
    convection has become increasingly linearly organized from
    south-to-north within the deep layer mean flow, backbuilding
    towards the triple point where 20-30 kts of low-level (primarily
    near the 925 mb isobaric surface/295K isentropic surface) is
    providing locally enhanced convergence/lift. In the mid- to
    upper-levels (400-250 mb), broad diffluence (within the left-exit
    region of a ~100 kt jet streak) and a distinct potential vorticity
    max upstream should continue to promote large scale lift and
    convective longevity. The mesoscale environment is characterized
    by ML CAPE of 250-1000 J/kg (and increasing by ~200 J/kg over the
    past several hours), precipitable water values of 1.3-1.5 inches
    (between the 75th and 90th percentile, per BMX sounding
    climatology), and effective bulk shear of 20-40 kts.

    Given the favorable environment and recent observational trends,
    the expectation is that isolated to scattered 1-2" hourly totals
    will continue over the next several hours, and the potential
    exists for localized training/repeating of these heavy rainfall
    rates. Hi-res CAMs (recent hourly runs of the HRRR and RRFS)
    insist that this activity will shift abruptly towards the
    northeast over the next 2-3 hours (as the low-level flow is
    expected to veer over the next couple of hours, largely cutting
    off the locally enhanced moisture transport/convergence). Even so,
    this will likely result in 2-3" of isolated to scattered rainfall
    totals through 10-11z (falling to the north and east of the
    Montgomery and Birmingham metro areas where MRMS estimates 1-2" of
    rainfall has occurred over the past several hours). Antecedent
    soil conditions are quite wet, with accompanying 3-hr Flash Flood
    Guidance (FFGs) generally range from 1.5-2.5" (as NASA SPoRT-LIS
    0-1m soil moisture remains well above the 90th percentile across
    the region). Isolated to scattered instances of flash flooding are
    possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_J_SPlRrOXtcghp3L4_NDB5gp-OB0sKIYbLllyz9vOPrylqtZzfDLiBT4AysRcBSK3X-= 4bO7GdHADcPyymcyRHtOpMI$ for graphic product...

    ATTN...WFO...BMX...HUN...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34278653 34188564 33388533 32158541 32018580=20
    32278604 32718625 33268647 33758657=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 12 11:13:50 2025
    AWUS01 KWNH 121113
    FFGMPD
    FLZ000-121600-

    Mesoscale Precipitation Discussion 0259
    NWS Weather Prediction Center College Park MD
    713 AM EDT Mon May 12 2025

    Areas affected...South Florida...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 121115Z - 121600Z

    SUMMARY...Compact MCS with rates of 2.5-3"/hr and some training
    elements may result in quick 3-5" totals and rapid inundation
    flooding IF collocates with urban areas over next few hours.

    DISCUSSION...CIRA LPW and surface observations depict a sharpening moisture/dewpoint gradient along and southeast of Biscayne Bay,
    with values in the Sfc-850mb layer near .7" while south across the
    FL straits near/over 1-1.1". This is supporting an isentropic boundary/effective warm front developing due to increasing
    southwest to southeast 15-25kt confluence along/ahead of NNE to
    SSW convective band crossing the central Keys. This allows for an
    effective triple point to exist across the Everglades along the Monroe/Miami-Dade county line. The strength of the moisture convergence/confluence and higher surface theta-E air to support
    SBCAPEs of 2000-2500 J/kg will support the rapidly cooling CB tops
    below -65C. Cells along the effective warm front have sufficient
    bulk shear to be rotating increasing moisture flux convergence for
    rainfall efficiency to greater than 2.5"/hr. Isolated, narrower
    updraft cells will exist along and northeast of the triple point
    through the length of the warm conveyor belt that extends north to
    just east of Cape Canaveral. Cells will be less efficient within
    the broader moderate shield precipitation given reduced available
    instability.

    There remains great uncertainty in the evolution/track of the MCV
    and therefore the triple-point and warm frontal convection.=20
    Dynamically biased Hi-Res CAMs (ARW, Nam-Nest, HRRR, RAP) suggest
    a continued northeastward track of the MCV lifting the heavy
    rainfall/triple point corridor northeastward across urban
    Miami-Dade/Broward. However, thermodynamically biased guidance
    (RRFS, ARW2, etc) suggest higher theta-E release in the mid-levels
    and increased outflow and forward propagation out across the Gulf
    stream east, resulting in a more moderate broad shield
    precipitation to occur over the urban corridor. RADAR trends
    would support the latter, reducing the overall risk of heaviest
    rainfall to the near-offshore from Biscane Bay, eastward, but the
    former cannot be fully ruled out. Currently, the greatest risk
    appears to be in the Homestead/southern Dade urban areas lifting
    northeast toward downtown Miami with spots of 3-5" possible over
    the next 1-3 hours.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5coNZZSMvoioPfi3TcX1DHsgzScETln8Jv5VrLC5CtjPnaTzvP3qXzn2W3yJvYGn9Z3t= 76hTgMMw1GB2BWw3AbqKe7g$ for graphic product...

    ATTN...WFO...KEY...MFL...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 26918021 26707996 26068001 25638009 25218026=20
    24968056 25018090 25198112 25668102 26148062=20
    26768049=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 12 19:28:55 2025
    AWUS01 KWNH 121927
    FFGMPD
    ALZ000-MSZ000-130025-

    Mesoscale Precipitation Discussion 0260
    NWS Weather Prediction Center College Park MD
    326 PM EDT Mon May 12 2025

    Areas affected...Central and Eastern MS...Western and Central AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 121925Z - 130025Z

    SUMMARY...Slow-moving showers and thunderstorms this afternoon
    with locally heavy rainfall rates up to 1.5 inches/hour coupled
    with moist antecedent conditions will pose an isolated threat for
    flash flooding.

    DISCUSSION...The latest GOES-E Day Cloud Phase RGB satellite
    imagery is showing the gradual expansion and continued initiation
    of showers and thunderstorms across central and eastern MS and
    adjacent areas of western and central AL. The convection is
    largely developing underneath the deeper layer closed low
    gradually pivoting eastward across the Gulf Coast states.

    Cooler mid-level temperatures coupled with boundary layer heating
    over the last several hours has facilitated MLCAPE values of as
    much as 1000 to 1500 J/kg, and this coupled with cyclonic low to
    mid-level flow should foster some increase in convective coverage
    going through the remainder of the afternoon.

    The environment is relatively moist with PWs generally close to
    1.25 inches, but with the available instability and slow
    cell-motions underneath the upper low, some hourly rainfall
    amounts of up to 1.5 inches will be possible. This is consistent
    with the 12Z HREF guidance which suggests some additional storm
    totals by early this evening reaching as high as 2 to 4 inches
    where the cells tend to locally anchor themselves.

    Given the moist antecedent conditions from recent heavy rainfall,
    these additional rains over the next several hours may pose an
    isolated threat for flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-9BSivFSyq4By7qv9PRu-GMcCDwbOoEOoMoiFTIsKvd-AoxrbzqhqNVMsW5NGRBOEkir= 0nTDzHp48z3FTx7oIHSU5pM$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...MEG...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 34598819 34578700 34248643 33718628 33068720=20
    32618952 32789082 33529100 34128995=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 12 21:36:56 2025
    AWUS01 KWNH 122136
    FFGMPD
    FLZ000-130035-

    Mesoscale Precipitation Discussion 0261
    NWS Weather Prediction Center College Park MD
    535 PM EDT Mon May 12 2025

    Areas affected...Southeast FL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 122135Z - 130035Z

    SUMMARY...A band of heavy showers and thunderstorms will be
    approaching the urban corridor of southeast FL over the next
    couple of hours. As this activity crosses the region early this
    evening, and urban flash flood threat will exist.

    DISCUSSION...The latest GOES-E IR satellite imagery along with
    regional radar data shows a band of heavy showers and
    thunderstorms gradually crossing south FL, with the activity
    gradually encroaching on the I-95 urban corridor of southeast FL.

    The activity has been intensifying over the last hour with cooling
    convective tops noted, and this intensification trend is being
    facilitated by rather strong low-level moisture convergence and a
    moderate to strongly unstable airmass characterized by MLCAPE
    values of 1500 to 2000 J/kg. Meanwhile, it is very moist with PWs
    of 2.0 to 2.25 inches which is locally 3+ standard deviations
    above normal.

    Rainfall rates with the approaching convective band are expected
    to be very high considering a well-defined deep tropical airmass
    and robust instability. Some rainfall rates may be capable of
    reaching 2 to 3 inches/hour, with even some sub-hourly rainfall
    totals of as much as 1.5 inches in just 20 to 30 minutes possible.

    The convection is moving fairly slowly, but steadily off to the
    east, and should advance into the I-95 urban corridor of southeast
    FL from West Palm Beach down to Fort Lauderdale and the Miami
    metropolitan area within the next 1 to 2 hours. Given the high
    rainfall rates and relatively slow cell-motions, some rainfall
    totals by mid-evening could reach 3 to 4 inches.

    These additional rains coupled with local sensitivities from the
    rainfall that occurred this morning will pose a concern for flash
    flooding over the next few hours. However, even the high rainfall
    rates alone impacting the I-95 corridor of southeast FL this
    evening will drive a notable urban flash flood threat.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Xg6sWsvXY4qY09efCUo_CbCtYAexn5UKyxJaBvLrn5bZK6xj1XsxcJh_nj2TJkmxa7e= UyEhxSk_Bll6Bru4kjXiKOs$ for graphic product...

    ATTN...WFO...KEY...MFL...MLB...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 27468013 26727992 25888000 25238035 25388079=20
    26308052 27428054=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 12 23:50:00 2025
    AWUS01 KWNH 122349
    FFGMPD
    NCZ000-SCZ000-GAZ000-TNZ000-130548-

    Mesoscale Precipitation Discussion 0262
    NWS Weather Prediction Center College Park MD
    748 PM EDT Mon May 12 2025

    Areas affected...Central to Northeast GA...Upstate SC...Western NC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 122348Z - 130548Z

    SUMMARY...Scattered areas of flash flooding may materialize this
    evening from areas of slow-moving and locally training showers and thunderstorms.

    DISCUSSION...The early-evening GOES-E IR satellite imagery along
    with regional radars shows some general increase in the coverage
    of shower and thunderstorm activity across areas of central to
    northeast GA which some linear structures becoming better defined
    and also coinciding with some cooling convective tops.

    A weakening frontal system is traversing the Southeast U.S. out
    ahead of a deeper layer trough/closed low over the Gulf Coast
    states, but there is a pool of moderate instability currently
    situated up across areas of central to northeast GA with MLCAPE
    values of 1000 to 1500 J/kg. Coinciding with this is a belt of
    effective bulk shear values of 30 to 40 kts and there has been an
    increase in the general organization of these cells over the last
    hour.

    The experimental WoFS guidance from the 20Z through 22Z runs has
    been rather insistent on there being some potential this evening
    for some north/south bands of convection that will be capable of
    training over the same area. Recent HRRR runs have been hinting at
    the same type of convective mode and potential for localized
    cell-training.

    Rainfall rates with the stronger storms will likely be capable of
    reaching 1.5 to 2 inches/hour given their level of organization
    and slow movement, and there may be some storm totals that could
    locally reach 3 to 4+ inches by midnight as these storms lift
    generally northward through northeast GA, portions of upstate SC,
    and also eventually western NC.

    Given the moist antecedent conditions and heavy rainfall potential
    in the near-term, there may be some scattered areas of flash
    flooding that materialize this evening.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4shPj7Yi4n01bHOoBrVwp8A_732lDSua5i-tWyoL1a4vbBnTJrO2YJaoEWKYTEr8WqK-= dcopQVf0GS94YqniOW2Np5U$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...JAX...MRX...RNK...

    ATTN...RFC...LMRFC...OHRFC...SERFC...NWC...

    LAT...LON 36478179 36068129 34078121 32668132 31908159=20
    31608216 31898263 33198284 33878289 34738292=20
    35488294 36168248=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 13 14:42:08 2025
    AWUS01 KWNH 131442
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-131915-

    Mesoscale Precipitation Discussion 0263
    NWS Weather Prediction Center College Park MD
    1041 AM EDT Tue May 13 2025

    Areas affected...northern/western VA into WV/MD Panhandles

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 131439Z - 131915Z

    SUMMARY...Localized flash flooding may develop across portions of
    central to western VA into the central Appalachians through 19Z.
    Periods of steady rain with embedded hourly rainfall of 0.5 to 1.0
    inches (locally in excess of 1 inch) can be expected with
    localized 3-hr totals of 2-3 inches.

    DISCUSSION...1430Z GOES East water vapor imagery showed a slow
    moving closed mid-level low centered over KY/TN with a negatively
    tilted shortwave spoke rotating into NC. Flow aloft ahead of this
    feature was becoming increasingly diffluent over the northern
    Mid-Atlantic region with a jet streak noted on GOES East DMV (~70
    kt) over south-central VA. Lower level winds were oriented from SE
    to NW with 850 mb wind speeds of 25-45 kt (highest from southern
    Chesapeake Bay into northwestern MD), a favorable orthogonal
    orientation for upslope enhancement into the axis of the Blue
    Ridge and central Appalachians.

    While instability was limited, central VA into east-central WV was
    positioned along the gradient in RAP forecast instability with
    MLCAPE of 1000+ J/kg to the southwest developing early in the
    afternoon. Favorable divergence and diffluece aloft will accompany
    embedded mesoscale vortices within the broader stratiform
    precipitation shield, likely help to enhance rainfall rates along
    with periods of short term training. Factoring in upslope
    enhancement due to terrain, periods of hourly rainfall between 0.5
    and 1.0 inches will be likely at times late this morning into the
    afternoon with localized hourly rainfall in excess of 1 inch
    possible. The steady nature of the rainfall with occasional
    enhancement to rainfall intensity is expected to support 2-3
    inches of rain within a 3 hour period which may result in
    localized areas of flash flooding.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4uz4ytRo_taTdQ6D8wyy1zgG3jcJLAIZeZb4rZ1BEX3kW6UAcbEayJQxl5kJsIbNSGer= qzJsyssRhC034gj6sByQ0RI$ for graphic product...

    ATTN...WFO...AKQ...CTP...LWX...PBZ...RLX...RNK...

    ATTN...RFC...MARFC...OHRFC...NWC...

    LAT...LON 40437845 39777762 38197733 37357806 37467920=20
    38257964 39447985 40227936=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 13 18:16:37 2025
    AWUS01 KWNH 131816
    FFGMPD
    PAZ000-VAZ000-WVZ000-OHZ000-132245-

    Mesoscale Precipitation Discussion 0264
    NWS Weather Prediction Center College Park MD
    216 PM EDT Tue May 13 2025

    Areas affected...western VA into WV and the upper OH Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 131813Z - 132245Z

    SUMMARY...Scattered thunderstorms are expected to expand from
    portions of western VA into WV and adjoining areas of southeastern
    OH and southwestern PA through 23Z. Hourly rates within the
    afternoon storms are expected to exceed 1 in/hr at times due to
    short term training.

    DISCUSSION...Visible satellite and radar imagery at 18Z showed a
    region of scattered thunderstorms from central WV into western VA
    near I-64. These storms were located ahead of a shortwave trough
    moving north from northeastern TN into western NC, part of a
    larger closed mid-level low centered over KY/TN. The region was
    also situated southwest of a broad region of overcast skies where
    daytime heating has combined with modest moisture to support
    instability. The environment near this region of thunderstorms
    contained 500-1500 J/kg MLCAPE with weakly anomalous precipitable
    water values with low level flow from the southeast at 10-20 kt
    over western VA, but with weaker magnitudes over central WV.

    The main concern for flash flooding is due to the expectation of
    additional convective development ahead of the shortwave trough
    within clear skies (unstable environment). While a general
    movement of thunderstorms toward the north or east is expected,
    unidirectional flow from the south to south-southeast will be
    supportive of short-term training axis of heavy rain, capable of
    generating hourly rainfall 1 to 1.5 inches (perhaps locally higher
    but likely staying below 2 inches). These instances are expected
    to be isolated to widely scattered but would be in excess of
    hourly flash flood guidance which is near 1 inch per hour over
    this region of the central Appalachians.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7Xuvk6gN6MMtXSPXK19CH4hYN-I5VIhYLOF-9Y2RSoZJcD9jWzZFCTQTVz99Ictmjf6k= D9G4Fcmweo-KYuh8W02YUYg$ for graphic product...

    ATTN...WFO...LWX...PBZ...RLX...RNK...

    ATTN...RFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 40138083 39918020 39127989 38357957 37727941=20
    37317987 37158134 37458181 38178224 38758226=20
    39318201 39728164 40038123=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 13 19:45:02 2025
    AWUS01 KWNH 131944
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-140100-

    Mesoscale Precipitation Discussion 0265
    NWS Weather Prediction Center College Park MD
    343 PM EDT Tue May 13 2025

    Areas affected...South-central PA...Western MD...Eastern WV...Far
    Northwest VA...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 131945Z - 140100Z

    SUMMARY...Continued moderate rainfall with occasional weak
    embedded convective elements within strong orthogonal upslope
    ascent regime. Localized spots of additional 1.5-2.5" totals
    possible within broader .5-1" average by early overnight.

    DISCUSSION...A strong moist dynamic environment across the
    Allegheny section of the larger Allegheny Plateau in far NE WV, W
    MD into south-central PA is expected to persist through the
    evening with a very slow south to north advancement along the
    ridge lines. Highly anomalous warm conveyor belt with nearly all
    CIRA LPW layers at or above the 95th percentiles with maxima at
    the lowest sfc-850. Combine this with persistent, nearly
    orthogonal 35-40kts of 925-700mb winds per VWP is resulting in IVT
    values over 600-700 kg/m/s even without support of increased
    vertical potential from insolation. As a result localized totals
    have already been over 2-4" throughout the day in E WV/W MD and
    starting to reach 2-3" across Somerset county in PA. Slightly
    lower vertical exposure across the Blue Ridge, still spots of
    1.5-2.5" have been observed. Additional rainfall will compound
    and expand ongoing flooding concerns through the complex terrain
    through 00z.

    GOES-E WV suite shows broad closed low across the Ohio Valley,
    though an eastward extension of the low/vorticity maxima is
    lifting across SW VA/S WV at this time, surface winds are backing
    in response to the height-falls and the 850mb trof is sharpening
    increasing directional convergence from more westerly return flow
    intersecting the 30-40kt WCB flow. Additionally, best diffluent
    region of the upper-level jet is starting to lift northward ahead
    of the 850mb trof with apex of the split along the Allegheny ridge
    as noted in the broad cirrus shield (starting to evacuate Northern
    VA/E WV. While there will be some insolation, the timing is
    likely limited across and north of I-64; with strong instability
    gradient noted in RAP analysis. Still, with the DPVA approaching
    and some temps rebounding into the low to mid-70s, modified
    sounding across central VA would support 500-1000 J/kg of MLCAPE
    that could be utilized in further ascent on the 850mb convergence
    line. Upstream convection along Albemarle/Augusta can be seen
    developing in this instability axis and with 700-500mb flow veered
    a bit, the cells should track NNW into the most affected areas
    with localized enhancements to the WCB moisture flux to support
    .5-1"/hr rates for embedded convective elements through the
    complex terrain.

    Rapid refresh guidance (HRRR/RRFS/WoFS) are inconsistent in
    placement, as expected, but continues to support those embedded
    additional 1.5-2.5" totals within a broader field of .5-1" totals,
    likely to maintain on going flooding, slowly expanding coverage
    northward of flooding risk through the early overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7JuH7uIBN6Hk4gtCv49xg0SFGrGWdlXSzPyAf3UafcT3ldJyuLUcVihS8kR9-UGT6qGG= pEfuEAU1HlG0B0IGqmo0Gtg$ for graphic product...

    ATTN...WFO...CTP...LWX...PBZ...RLX...

    ATTN...RFC...MARFC...OHRFC...NWC...

    LAT...LON 41277830 41187740 40827691 40267683 38947785=20
    38107867 38167922 38757974 39667966 40617905=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 13 21:59:12 2025
    AWUS01 KWNH 132159
    FFGMPD
    VAZ000-WVZ000-140300-

    Mesoscale Precipitation Discussion 0266
    NWS Weather Prediction Center College Park MD
    558 PM EDT Tue May 13 2025

    Areas affected...Western Virginia & Adj portions of Eastern WV...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 132200Z - 140300Z

    SUMMARY...Significant flash flooding event starting to unfold
    across central VA.

    DISCUSSION...21z surface map depicts a highly confluent flow
    strengthening a focus for very slow moving/stationary band with
    training elements aligning into terrain. As noted in MPD 265, an
    eastward extension of the upper-level trof continues to sharpen
    across SW to S VA, supporting lee-cyclogenesis in the vicinity of
    ROA to FVX. Earlier afternoon convection/moderate shield
    precipitation has aided the strengthening of a surface ridge
    extension through the northern Shenandoah Valley which further
    helps to anchor the strengthening band of convective activity from
    Nottoway to Augusta county, VA. Surface Tds in the upper 60s to
    lower 70s remain located along the southwestern gradient of the
    warm conveyor belt, delineated well by warm status clouds in the
    1.6um near IR channel. Solid insolation across NC and southeast
    VA shows a pocket of unstable air with an axis fo 2000 J/kg SBCAPE
    along and south of the confluence band to maintain/focus the
    convective development.

    Recent Visible imagery, RADAR mosaic and lightning detection show
    the strengthening/expanding nature to the entire convective line,
    though the apex near the Blue Ridge continues to focus best
    convergence due to the upslope. Total PWats of 1.3-1.5" and flux
    at the cloud base should support rates of 1.5"/hr, increased
    duration will support 1.5-3hrs of duration with slow northward
    propagation and may result in localized 3-4" totals by 01z,
    maintaining flash flooding conditions, where locally significant
    flooding remains possible with a spot or two of 5"+ possible (in
    line with recent 90th percentile for WoFS 20-21z solutions.=20

    Additionally, a band of scattered storms are lifting north with
    the 700-500mb trof axis across SW VA toward the area, this will
    expand the risk of flash flooding southwestward within the terrain
    where heavy rainfall today has sizably reduced the FFG values
    below 1"/hr and 1.5"/3hr. As such, even as they pass fairly
    quickly with 1-2" totals may trigger localized flash flooding
    upstream, before potentially merging with the line and finally
    ejecting it more northeast into more stable air near and north of
    the Potomac River Valley.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!44aKQ3CFTO1oae-1CEiijb2JyLhnRDWqepZb9dSY0U689bxvzkJy87DSyFsUXdVLq7IL= KkpZWdHx4UGkz0S2VliX13o$ for graphic product...

    ATTN...WFO...AKQ...LWX...RNK...

    ATTN...RFC...MARFC...SERFC...NWC...

    LAT...LON 39047869 39037806 38587754 38067742 37607751=20
    37197762 37027792 37197853 37287912 37327958=20
    37477997 37887990 38347956 38717925=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 14 03:17:42 2025
    AWUS01 KWNH 140317
    FFGMPD
    PAZ000-MDZ000-VAZ000-DCZ000-WVZ000-140800-

    Mesoscale Precipitation Discussion 0267
    NWS Weather Prediction Center College Park MD
    1116 PM EDT Tue May 13 2025

    Areas affected...Blue Ridge Mountains across much of VA and into
    MD/WV/PA, east into portions of the DMV

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 140300Z - 140800Z

    Summary...Rainfall rates of 0.5-1.0" (and locally higher) are
    expected to continue over areas that have already received 2-5".
    Scattered instances of flash flooding are likely to continue (with
    locally significant to catastrophic impacts possible across
    portions of the Blue Ridge Mountains).

    Discussion...Areas of stratiform rainfall with 0.5-1.0"/hr rates
    continue across much of VA and into adjacent portions of MD/WV/PA,
    generally along and to the east of the Blue Ridge Mountains.
    Embedded convective elements occasionally produce hourly rates in
    excess of 1" (per MRMS) estimates, and this is problematically
    occurring over areas that have already received 2-5" rainfall
    totals over the past 12-24 hours (with some localities in the
    vicinity of Shenandoah National Park receiving the bulk of that
    amount over the past 3-6 hours, with multiple Flash Flood
    Emergencies currently in effect). Deep cyclonic flow with a
    northwestward translating mid-level vorticity max and accompanying
    diffluence aloft looks to maintain synoptic scale lift and
    upper-level support, while moderate to strong low-level moisture
    transport (most prominent at 925 mb with 30-40 kt flow) via the
    persistent warm conveyor belt directed SE-ESE across the DMV
    maintains lower-level support/convergence. While instability is
    beginning to wane over much of the region (-200 to -800 J/kg of
    MUCAPE over the past 3 hours), buoyancy remains sufficient (MUCAPE
    of 100-500 J/kg) to sustain embedded convective elements (in
    addition to terrain forcing along the Blue Ridge itself).

    Given the aforementioned wet antecedent conditions (with Flash
    Flood Guidance over 3-6 hours generally ranging from 1.0-2.0", and
    locally even below 1.0") and the expected continued rainfall rates
    of 0.5-1.0" (and locally higher) over the next several hours,
    scattered instances of flash flooding are likely to continue (and
    may be locally significant to catastrophic).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6C544q-j0CS5Fqexn-dky9GR_2eMLXIcVhVcs5SmIyBCwsPTFFSNAgnnqdMy6F-R8_3f= jylB6TYnng06ebUqru3UAR0$ for graphic product...

    ATTN...WFO...AKQ...CTP...LWX...PBZ...RNK...

    ATTN...RFC...MARFC...OHRFC...NWC...

    LAT...LON 40417842 40337806 40177774 40047742 39957731=20
    39827714 39677699 39417689 39037691 38777699=20
    38337724 37577752 37397815 37647857 38047870=20
    38597871 39387876 39557892 39707931 40027923=20
    40337893=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 14 15:58:27 2025
    AWUS01 KWNH 141557
    FFGMPD
    PAZ000-MDZ000-VAZ000-NCZ000-WVZ000-142100-

    Mesoscale Precipitation Discussion 0268
    NWS Weather Prediction Center College Park MD
    1157 AM EDT Wed May 14 2025

    Areas affected...Central Appalachians

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 141556Z - 142100Z

    Summary...Showers and thunderstorms will expand in coverage and
    intensify through the afternoon across the Central Appalachians.
    Rainfall rates of 1-2"/hr are expected, which could result in 2-3"
    of rain in a few areas. This rain atop saturated soils could cause
    instances of flash flooding.

    Discussion...The GOES-E Day-Cloud distinction RGB imagery late
    this morning indicates fresh updrafts beginning to expand across
    northern NC and into parts of southern VA. These updrafts are
    resulting in intensifying showers and isolated thunderstorms noted
    via the regional radar mosaic, and are occurring in a region of
    expanding lightning cast probabilities above 30%. This suggests
    that destabilization is rapidly occurring, which is reflected by
    the SPC RAP analysis showing that CIN has eroded and SBCAPE has
    climbed to as high as 1000 J/kg. Within this environment, forcing
    for ascent is increasing downstream of a potent shortwave, clearly
    noted in WV imagery, lifting northward within a synoptic trough
    oriented NW to SE across the region. Downstream of this trough
    axis, winds veer through the column which is helping to both
    transport higher moisture northward (PWs measured around 1.2
    inches which is close to the 90th percentile for the date) and
    force orographic lift as sfc-925mb winds lift out of the SE,
    leading to an even more impressive overlap of thermodynamics and
    ascent by this aftn.

    The high-res CAMs are in good agreement that clusters of
    thunderstorms will continue to develop and move slowly northward
    on 0-6km mean winds of around 10 kts. These storms will likely
    intensify through the aftn as SBCAPE reaches as high as 1500 J/kg,
    which will be acted upon by the approaching shortwave and
    continued orographic/upslope low-level ascent. This favorable
    environment will support rainfall rates for which both the 12Z
    HREF and 00Z REFS indicate have a 40%-50% probability for
    exceeding 1"/hr, with the HRRR suggesting a threat for more than
    0.5"/15min at times (>2"/hr rates). Although bulk shear will
    remain weak at 20 kts or less, some repeating clusters of storms
    are possible, lengthening the duration of heavy rain which could
    lead to pockets of event-total rainfall reaching 2-3" in some
    areas.

    Although convection will generally remain scattered outside of
    small clusters, flash flooding will be a concern beneath any heavy
    rain producing cells today. This is due primarily to these
    excessive rain rates moving across extremely saturated soils from
    24-hr rainfall as much as 3-6". This has compromised FFG to as low
    as 0.5" to 1" in 3 hours, for which the HREF and REFS both
    forecast a 50-60% chance of exceedance, highest from the Blue
    Ridge of VA northward into the Potomac Highlands and Allegheny
    Mountains.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9-LiTbH9UdaoulASgam8FMpozb9ZbK3Cx0_HDNyK6MID1CASzJZmcX8shHr_UfSSPFrg= H683c8ecMNC3RWE84mKJSoA$ for graphic product...

    ATTN...WFO...AKQ...CTP...LWX...PBZ...RLX...RNK...

    ATTN...RFC...LMRFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 40277930 40047856 39297808 38207806 37227848=20
    36747909 36357980 36308022 36398097 36758134=20
    37578125 38808083 39778047=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 14 17:34:34 2025
    AWUS01 KWNH 141734
    FFGMPD
    VAZ000-NCZ000-142300-

    Mesoscale Precipitation Discussion 0269
    NWS Weather Prediction Center College Park MD
    133 PM EDT Wed May 14 2025

    Areas affected...Eastern North Carolina and Virginia

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 141733Z - 142300Z

    Summary...Showers and thunderstorms will increase in coverage
    through the afternoon and lift slowly northeast. Rainfall rates
    may exceed 2"/hr at times within this convection, leading to
    pockets of 2-3" of rain or more. This could cause flash flooding,
    especially over urban areas or more sensitive soils.

    Discussion...The regional radar mosaic this afternoon shows
    rapidly expanding coverage of showers and isolated thunderstorms
    from the Piedmont of North Carolina through the Tidewater Region
    of Virginia. This convection is blossoming in response to
    increased ascent through a variety of forcing including a wave of
    low pressure and accompanying stationary front, the Piedmont
    Trough, and a potent shortwave/vorticity maxima noted on the
    GOES-E WV imagery. Together, these are producing deep layer ascent
    into favorable thermodynamics characterized by PWs of 1.4-1.5
    inches, around the 90th percentile at both KMHX and KWAL, with
    MLCAPE measured by the SPC RAP analysis now exceeding 1500 J/kg.
    At the same time, a plume of higher sfc-850mb and 850-700mb noted
    in the CIRA LPW product is surging across Cape Fear, and this will
    additionally enhance moisture/thermodynamics as it lifts northward
    on minimally veered SW sfc-500mb flow. Rainfall rates within this
    developing convection have already been estimated via KRAX and
    KAKQ to exceed 1.5"/hr.

    As the aftn progresses, shower and thunderstorm coverage will
    likely become more widespread as reflected by available CAM
    simulated reflectivity, with intensity also peaking later this
    aftn and into the evening. The HREF and REFS rainfall rate
    probabilities feature a 60-80% chance of exceeding 1"/hr, and
    about a 20% chance of exceeding 2"/hr. Although mean 0-6km winds
    should remain modestly progressive at 15-20 kts to the northeast,
    Corfidi vectors collapse to around 5 kts, which when combined with
    a surge of greater thermodynamics approaching from the south
    suggests short term training/backbuilding is probable to enhance
    the duration of these rain rates. This storm motion collapse could
    also occur along the sea breeze or stationary front, providing
    additional impetus for heavy rainfall accumulations, locally
    exceeding 2-3" of rain.

    Much of this region has been wet the past 7 days as reflected by
    AHPS rainfall departures of 150-300% of normal, leading to 0-40cm
    soil moisture that exceeds the 98th percentile. This has
    compromised FFG to as low as 1"/1hr and 1.5"/3hrs, lowest across
    southeast and south-central VA which is where HREF 3-hr FFG
    exceedance probabilities are highest. Any short term training of
    these intense rain rates, especially across these more sensitive
    soils of VA, or atop any urban areas, could result in instances of
    flash flooding into this evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5-PGRic5prtyeemOf5k_ebIL4TseZozVJycRWJMxj921jxF0khf06ifnj9WkHCaMTS5i= NozWHoq9D-QBdZVCs9nFaLo$ for graphic product...

    ATTN...WFO...AKQ...MHX...RAH...RNK...

    ATTN...RFC...MARFC...SERFC...NWC...

    LAT...LON 38067718 38007684 37817658 37347631 36787594=20
    36537599 36167620 35757654 35447697 35217753=20
    35107807 35427858 35677902 35877944 36027975=20
    36257993 37017938 37667847 37927776=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 14 20:29:54 2025
    AWUS01 KWNH 142029
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-OHZ000-150100-

    Mesoscale Precipitation Discussion 0270
    NWS Weather Prediction Center College Park MD
    429 PM EDT Wed May 14 2025

    Areas affected...Northern WV...Southwest PA...Adj Eastern OH...
    Far Western MD...Far Northwest VA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 142030Z - 150100Z

    SUMMARY...Slow moving, scattered to regionally dense narrow core
    convective cells capable of 1-1.5"/hr rates/totals over complex
    and recently saturated soils pose localized/focused flash flooding
    potential through evening.

    DISCUSSION...Recent GOES-E Visible loop shows broad area of
    congested cu/Tcu across northern WV into far SW PA/Garrett county
    MD become more numerous and increasing in vertical depth. Area
    has been confined to the north and northeast given prolonged
    stratus deck limiting peak heating. Surface Tds in the upper
    50s/low 60s remains well above normal and with modest mid-level
    lapse rates, SBCAPEs have risen to 1500 J/kg to help
    develop/maintain convective vigor for the next few hours. GOES-E
    WV loop and RAP analysis denotes decaying upper-level low has
    sheared from NW to SE with core of vorticity across the Piedmont
    of NC/S VA with a secondary lobe back toward N OH, this has
    resulted in broad northeastward lift of the trof, but also
    resulted in slowing of the mid-level steering to less than
    15-20kts. This should allow for strong cells to develop and
    collapse within a 1-2 hour period with locally intense rain-rates
    up to 1-1.5".

    While localized, the overall density of the narrow cores is fairly
    close in proximity, that as new development produces outflow and
    seeks out remaining unstable parcels for additional development,
    proximity may allow for isolated spots to have a second intense
    pulse with overall spotty totals perhaps reaching 2", with highest
    probability over NE WV into SW PA, as further north remains more
    stable given the lack of heating this afternoon. Given these
    intense rates over complex terrain naturally with lower FFG;
    recent heavy rainfall in spots over the last day or so as further
    reduced the capacity of soils, with increased run-off likely. As
    such, scattered incidents of flash flooding are considered
    possible through late evening/early overnight as instability is
    exhausted.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5y3GBp-wWsDsjYStz99xzTB4Jsc7IQJSYXpbRjk44mgYA7joYS-mC4A8IyYPKSR2rl-D= _86UJu0HiFYEnBlUKUgByVg$ for graphic product...

    ATTN...WFO...LWX...PBZ...RLX...RNK...

    ATTN...RFC...MARFC...OHRFC...NWC...

    LAT...LON 40788042 40427977 39717944 39077858 37977931=20
    37978049 38858081 39368114 39778148 40568117=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 14 21:49:56 2025
    AWUS01 KWNH 142149
    FFGMPD
    MDZ000-VAZ000-WVZ000-150300-

    Mesoscale Precipitation Discussion 0271
    NWS Weather Prediction Center College Park MD
    549 PM EDT Wed May 14 2025

    Areas affected...Northern Virginia...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 142200Z - 150300Z

    SUMMARY...Intense thunderstorms capable of 1.5-1.75"/hr
    rates/totals within slow/chaotic cell motions regime resulting in mergers/collisions and localized 2+" totals in vicinity of
    saturated ground conditions likely to induce focused/localized
    incidents of flash flooding through early overnight period.

    DISCUSSION...GOES-E Visible/EIR and regional RADAR mosaic show
    convective evolution is a bit faster than Hi-Res CAM solutions
    suggest in timing. Overall, recent HRRR solutions continue to be
    consistent with other 12/18z Hi-Res CAMs with evolution of
    convective activity/coverage across northern Virginia; however,
    typical to slower timing bias appears to be unfolding at this time.

    Strong vorticity center at southeastward end of
    elongating/shearing upper-level trough from the Great Lakes/Upper
    Ohio Valley is being reinforced by convective activity feeding
    back into the circulation across south-central VA. A slow
    north/northeastward lifting of the wave is supporting weak
    cyclogenesis across central VA, as well as strengthening
    northeasterly flow out of the relatively stable air out of
    Maryland, further reinforcing FGEN from the surface wave near KCHO
    across the western Northern Neck into the Middle Neck before
    angling northward across the Delmarva. As a result, there is a
    strong stability gradient along the Potomac River, making
    potential for heavy rainfall reduced north of it. Weak but
    sufficient low level/boundary layer southeasterly flow is
    providing solid moisture of 1.5"+ north of the vorticity center
    into NoVA. A few hours of solid clearing skies have resulted in
    temps rising into the mid to upper 70s, resulting in increasing
    SBCAPEs over 1000 J/kg toward 2000 J/kg near the tidal Potomac
    River.

    With the vorticity center strengthening, DPVA and modest expansion
    of divergence aloft into strengthening entrance to 30-40kt 3H jet
    streak over PA will continue to support upper-level evacuation for
    developing convective cells/clusters. Additionally, steering flow
    through 500mb will support northwest then westward motion of cells
    across NoVA and with storm influences, may result in slow, chaotic
    motions allowing for increased residency for any given cell.=20
    While wind speeds will be relatively weak at 5-10kts for inflow,
    directional convergence will aid in raising rainfall
    efficiency/potential with 1.5-1.75"/hr rates possible. Given slow
    motions and narrow up/downdrafts, intense cores of 2"+ totals
    remain possible, especially later this evening as cells interact
    with increased terrain across the Blue Ridge.

    Recent significant rainfall further west toward the terrain, has
    sizably reduced FFG values that even 3hr FFG values are less than
    1" increasing the potential for near zero infiltration supporting
    high runoff and likely flash flooding incidents. Further east
    toward I-95, grounds are also have deeper wetness, with ratios in
    the 60-75%, but may have more capacity that all but the highest
    totals/intense rates over 1.5" may result in flash flooding. As
    such, incidents of flash flooding are considered likely, but
    coverage is likely to be wide spread and locally focused.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!49AqB-LZf7dWSZCssukD0vreZbNMMatm13jez-eUS9C61rOxiPjsk87l7leOwx7UX0dz= iwfQ-TYdp4wElpvCdmRr0A0$ for graphic product...

    ATTN...WFO...AKQ...LWX...

    ATTN...RFC...MARFC...NWC...

    LAT...LON 39577796 38977729 38777706 38217655 38007636=20
    37487651 37267713 37727817 38357918 39167886=20
    39567842=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 14 23:55:45 2025
    AWUS01 KWNH 142355
    FFGMPD
    NEZ000-SDZ000-150449-

    Mesoscale Precipitation Discussion 0272
    NWS Weather Prediction Center College Park MD
    754 PM EDT Wed May 14 2025

    Areas affected...Central SDak...Northern & Central NEB Sand
    Hills....

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 142349Z - 150449Z

    SUMMARY...Expanding convective cluster with very strong moisture
    flux convergence, stationary downdrafts and some training elements
    suggest spotty 3-4" totals in the Sand Hills and 1.5-2" totals in
    Central SDak. Both may pose a few isolated to widely scattered
    incidents of rapid inundation flooding.

    DISCUSSION...GOES-East and West WV suite shows a pair of strong
    embedded shortwave features (E ID and Northern CO/S WY) carving
    out the broaden north-south synoptic trough over the northern
    Rockies and northern High Plains. The pair have helped to provide
    a strong deep layer convergence zone across the Dakotas generally
    around 101-102W with CIRA LPW denoting pooled mid-level moisture
    along and eastward with well above normal 1.25" total PWat values.
    With the main shortwave exiting the WY/CO Rockies, a downstream
    boundary layer to 700mb low is stacked across west-central NEB
    near LBF, with a strong confluent LLJ streaming from the
    southeast. This LLJ has ample anomalous low level moisture being
    advected on 20-30kts with low 60s at the surface and 40-50s into
    the boundary layer resulting in 1.3" total PWat, but the flux is
    very strong with nearly 90 degrees of directional convergence
    along the shear axis across the Sand Hills into the Dakotas.

    Moderately unstable air has helped to develop convection
    throughout the late afternoon/early evening across Ziebach to
    Jackson county in SDak, with recent increase in vigor noted.=20
    Rates of .5"/hr have steadily increased with some spots nearing
    1". The concern is the deep layer steering has allowed for
    training elements along it resulting in spots of 1-2" totals
    starting to accumulate. Slow eastward propagation is expected but
    will have to wait for a hour or two until height-falls shift the
    convergence eastward. Instability will also be waning through
    that time period, so there is a narrow N-S axis for these
    increased totals. Localized spots of 1.5-2"+ are at the tipping
    point of 1-3hr FFG values in the area, so a few localized spots
    may be exceeded resulting in some flash flooding conditions in the
    next 3 hours.

    Further south into the Sand Hills, soil conditions can infiltrate
    a higher volume of water quickly; however, the very strong
    moisture flux convergence along with 1500-2000 J/kg of instability
    advected will continue to support strong/broadening updrafts.=20
    This has been particularly impressive in S Cherry county and has
    been expanding northward and southward along a stationary front.=20
    Large hail signatures have over-estimated rainfall rates, but the
    amount of flux is likely supporting 1.5"+/hr rates as noted by an
    observation of 1.2"/hr in Mullen, NEB. Further saturation of the
    deep layer profile will further enhance rates to near 2"/hr in
    spots. Strong height-falls from the ejecting shortwave are
    resulting in nearly stationary cell motions as pull west is
    counteracted by propagation vectors to the east-northeast. As a
    result, local totals are likely nearing exceeding 2-2.5"; with an
    additional 2-2.5" possible in spots. As such localized 3-4+"
    totals may occur locally. FFG values suggest infiltration through
    the sandy soils should take most of these totals, but the shear magnitude/volume across areas may still result in localized
    flooding/ponding especially near roads/urban locations. As such,
    flooding is considered possible across north-central NEB too, but
    areas along/surrounding the Sand Hills will be prone for flooding
    in south-central SDak before the expanding complex forward
    propagates in earnest toward 03-04z.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9CUKk6Szq98yjI5KKspiJnhLapAmolslMfMretFmje_2Wax_04tEDoSSberuXxsear9h= CaXVbhW5I1jjfVJ9kSYt7sw$ for graphic product...

    ATTN...WFO...ABR...FSD...LBF...UNR...

    ATTN...RFC...MBRFC...NWC...

    LAT...LON 45790120 44130068 43739926 43269878 42519867=20
    41879904 41010090 41100215 41710251 42210192=20
    42700170 43700197 44340201 45090212 45710191=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu May 15 18:40:32 2025
    AWUS01 KWNH 151840
    FFGMPD
    VAZ000-WVZ000-160015-

    Mesoscale Precipitation Discussion 0273
    NWS Weather Prediction Center College Park MD
    239 PM EDT Thu May 15 2025

    Areas affected...eastern WV into western VA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 151838Z - 160015Z

    Summary...Showers and thunderstorms are expected to develop over
    the higher terrain of eastern WV into western VA within the next
    1-3 hours. While movement of cells should be generally
    progressive, exceedance of very low flash flood guidance (FFG) may
    result in spotty runoff issues atop sensitive grounds.

    Discussion...Visible satellite imagery at 1815Z showed an
    expanding field of cumulus with increasing vertical development
    over the central Appalachians of eastern WV to the Blue Ridge
    Mountains of western VA. This region was located behind a
    departing mid to upper-level trough over the northern Mid-Atlantic
    coast within a WNW flow aloft. While the deeper moisture axis was
    located over the western Atlantic, weakly anomalous precipitable
    water (PW) values of approximately 1.0 to 1.3 inches remained via
    area GPS PWs and a special 17Z sounding from RNK, with some
    contribution to the low to mid-level layer coming from the
    southwest via LPW imagery. Daytime heating has also contributed to
    500 to ~1500 J/kg MLCAPE across the region via SPC mesoanalysis
    data and the RNK sounding.

    Continued heating of the elevated heat source(s) will likely
    contribute to convective initiation within the next 1-3 hours,
    based on satellite trends and short term RRFS/HRRR forecasts.
    Effective bulk shear values of 35 to 45 kt combined with the
    instability values should support some organized cells, capable of
    higher rainfall efficiency. Individual cell motions are expected
    to be fairly progressive toward the E to SE at 15-25 kt, but
    potential for 0.5 to 1.0 in/hr rates will exist and considering
    potential for mergers (perhaps slightly higher rates) could yield
    1-2 inches through 00Z. While this is not a typical flash flood
    setup for the region, conditions on the ground are hyper-sensitive
    due to recent heavy rain with FFG values as low as 0.25 to 0.5
    inches in an hour in some locations, with much of the outlooked
    area containing FFG below 1 in/hr.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_xEb0cDxAc32sQoAaxfnSJGBjezE5lpDVI8tKOAVeiBpgA8vgwXFyTmVvb-PkhsVVzo0= iMPJZud7l4MiCgbuDBO2Kp8$ for graphic product...

    ATTN...WFO...AKQ...LWX...PBZ...RLX...RNK...

    ATTN...RFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 39187838 38867798 37887823 37307895 37328029=20
    37688069 38248069 38728009 39077944=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu May 15 19:47:39 2025
    AWUS01 KWNH 151947
    FFGMPD
    NCZ000-160100-

    Mesoscale Precipitation Discussion 0274
    NWS Weather Prediction Center College Park MD
    346 PM EDT Thu May 15 2025

    Areas affected...Eastern North Carolina...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 151945Z - 160100Z

    SUMMARY...Lingering deep moisture and slow, potentially multiple
    cell/repeating tracks crossing recently saturated grounds pose
    scattered incident or two of flash flooding this evening.

    DISCUSSION...19z Surface and RAP analysis denotes a pool of
    lingering enhanced deep layer moisture across eastern NC that has
    had near full isolation throughout the day resulting in quite
    unstable environment. Sfc Tds in the low 70s with low to upper
    80s extending from the VA/NC line south to a few 90s near
    Lumberton, NC; and modest 7 to 7.5C/km lapse rates have resulted
    in a pool of MLCAPE over 3000 J/kg across the area of concern.=20=20
    Surface analysis shows a broad surface trof from upstate NC toward
    a weak low near DAN/GSO with the Fall-line trough extending
    southward through central SC; stronger winds from SC at 10-15kts
    slow in proximity to the temperature gradient increasing flux
    convergence.=20

    GOES-E Visible loop shows enhanced convergence lines with the
    sea-breeze, but overall general congestus across central NC is
    starting to bubble to a few TCu/CBs near RAH. Deep layer
    850-700mb southwesterly flow will veer a bit more with slightly
    confluent streamlines across the state in proximity to the surface
    trof and low. Isolated cells will build to be scattered through
    the evening, but given updraft strength and flux capability of TPW
    AoA 1.5", should support 1.5-1.75"/hr rates. Cell motions of
    10-15kts will help with duration and may support some spots of
    enhanced rainfall. As cells become more clustered toward the east
    into the late evening (potentially locked to terrain due to
    bay/sea-breeze boundaries), there are increased chances of
    localized 2-3" totals.=20

    Normally, soils would support these rates, but given recent
    400-600% of normal rainfall across portions of E NC per AHPS, and
    soil saturation ratios above the 98th percentile in the range of
    65-80% (greater along and east of I-95), FFG values may have
    rebounded a bit too quickly but 3hr FFG value of 2.5-3" are still
    in range of some exceedance, the risk of limited infiltration and
    rapid inundation flooding is considered possible.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!98_8g15ot8znuugGKkTQ43XlbPTbDGOIuR9S-WWaffEBDew1o3gxBCr0w36eg2ubVN88= z54NxlJ5vkwB9IuFJRu14MQ$ for graphic product...

    ATTN...WFO...AKQ...MHX...RAH...

    ATTN...RFC...SERFC...NWC...

    LAT...LON 36547686 36407611 35967578 35637586 35177663=20
    34867736 34897829 35077906 35397933 35867943=20
    36387884 36517783=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 16 11:37:49 2025
    AWUS01 KWNH 161137
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-161630-

    Mesoscale Precipitation Discussion 0275
    NWS Weather Prediction Center College Park MD
    737 AM EDT Fri May 16 2025

    Areas affected...Northeast Arkansas through Central Kentucky

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 161134Z - 161630Z

    Summary...Repeating heavy thunderstorms continue developing from
    northeast Arkansas through central Kentucky this morning. While
    movement of cells remains progressive, cell mergers and repeating
    activity makes flash flooding possible.

    Discussion...Numerous supercells have developed ahead of a
    stationary front over northeast Arkansas, the Missouri Bootheel
    and western Kentucky. Gulf-sourced moisture (PW of 1.8") is
    pooling along the front with higher instability (MUCAPE >2000
    J/kg) and powerful deep layer WSWly flow (60kt) allowing for heavy
    repeating cells. Rainfall up around 1.5" in the past hour as been
    estimated from the heaviest cells which have large hail. The 09Z
    RRFS is decent with its current depiction with a diurnal increase
    in coverage through the rest of the morning. Flow parallel to the
    front will allow repeating storms.

    Flash flood guidance is 1.5 to 2" per hour, so flash flooding
    should be limited to where repeating heavy activity occurs.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_1tfTVs699s6-4k1XkAri7sZh3oy2tit-HTTPl7u9WuYCx97jRqUIb4InJAemZ043UsC= ao5rsCLZN5J1gYraksY2HTA$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...LZK...MEG...OHX...PAH...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 38448437 37168364 36478611 35728928 35169145=20
    35639212 36189161 36758983 37338844 38108616=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 16 14:09:13 2025
    AWUS01 KWNH 161407
    FFGMPD
    NJZ000-PAZ000-DEZ000-MDZ000-161905-

    Mesoscale Precipitation Discussion 0276
    NWS Weather Prediction Center College Park MD
    1007 AM EDT Fri May 16 2025

    Areas affected...Southeast Pennsylvania Through New Jersey

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 161406Z - 161905Z

    Summary...Organized thunderstorms progress to the northern
    Mid-Atlantic coast through the early afternoon. 1.5"/hr rainfall
    rates could cause localized flash flooding, particularly over
    urban areas such as Philadelphia and Wilmington, DE.

    Discussion...Mesoscale convective system (MCS) progressing over
    Pennsylvania will continue to move ESE over a low amplitude trough
    extending up the Eastern Seaboard. Gulf-sourced moisture, with PW
    of 1.5" (2 sigma over normal) spreading up from the Southeast is
    riding over a warm front extending from southern PA through the
    Delaware Bay. Instability is sufficient (around 1000 J/kg) along
    the frontal boundary with a notable decrease below 500 J/kg over
    central New Jersey which is directly downstream of the activity.
    However, upscale growth is seen in IR imagery with continued
    cooling in the core of the system over east-central PA.

    Hourly CAMs (HRRR and RRFS) have struggled with intensity and
    timing of this system. However, given the sensitivity of the large
    urbanized areas downstream of the MCS and history of leading cells
    adding to rainfall impacts, there is a localized flash flood risk
    through mid-afternoon.

    Additional risk for heavy rain in the Mid-Atlantic later this
    afternoon and evening will continue to be monitored.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Ih3aHS-OCGz35h_OQuVdxf-bCcH3P9x1surIhyxWpeJQ6xG4Z-xYmJiRuLzQp6UhlY5= sDKXFRXK-2ASt0bRuc0AxSo$ for graphic product...

    ATTN...WFO...BGM...CTP...OKX...PHI...

    ATTN...RFC...MARFC...NWC...

    LAT...LON 41027647 40697470 40247370 39357414 39157460=20
    39487556 40097709 40627752=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 16 15:24:21 2025
    AWUS01 KWNH 161524
    FFGMPD
    VAZ000-NCZ000-WVZ000-OHZ000-TNZ000-KYZ000-162015-

    Mesoscale Precipitation Discussion 0277
    NWS Weather Prediction Center College Park MD
    1123 AM EDT Fri May 16 2025

    Areas affected...South-Central Appalachians

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 161519Z - 162015Z

    Summary...Risk of repeating heavy thunderstorms across the
    south-central Appalachians this afternoon. Fast motion to these
    storms will continue, so flash flooding is possible where cell
    mergers and repeating of the heaviest activity occurs.

    Discussion...Numerous supercells embedded in a quasi-linear system
    east of a stationary front will continue to develop and shift east
    over the south-central Appalachians this afternoon. Gulf-sourced
    moisture (PW of 1.7 to 1.9") is pooling ahead of the front with
    higher instability MLCAPE 1500 to 2500 J/kg) and powerful deep
    layer WSWly flow (50 to 60kt) allowing for heavy repeating cells.
    Peak hourly rainfall estimates of 1.0 to 1.5" per hour continue in
    the heaviest cells which also have hail present. The RRFS
    continues to have a decent handle on this regional activity
    especially compared to recent HRRRs which are too late with
    activity. The 13Z RRFS indicates potential for 3" over the next
    few hours which is reasonable given the repeating threat from flow
    parallel to the front.

    Flash flood guidance decreases east from KY with terrain with
    three-hour values of 1.5 to 2" decreasing to as low as 1". Given
    the axis of higher instability continuing through the crest of the Appalachians, there is a notable threat for flash flooding in
    spite of the fast cell motion.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5n6lhpSV2aOGa-JlZUmxQ7UBI471RTs10LVLX_K2zJ5YPlFuQiUx-7HMOcOsVTfixl0w= p86S_Hbs6HlCrxD5CLx0IFo$ for graphic product...

    ATTN...WFO...JKL...LMK...LWX...MRX...OHX...RLX...RNK...

    ATTN...RFC...LMRFC...MARFC...OHRFC...SERFC...NWC...

    LAT...LON 38588107 38537968 37937903 37107891 36287983=20
    36208569 37638499 38308328=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 16 17:52:54 2025
    AWUS01 KWNH 161752
    FFGMPD
    MEZ000-NHZ000-170000-

    Mesoscale Precipitation Discussion 0278
    NWS Weather Prediction Center College Park MD
    152 PM EDT Fri May 16 2025

    Areas affected...Northern NH...North & Northwest ME...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 161800Z - 170000Z

    SUMMARY...Widely scattered but very slow moving thunderstorms with
    capability of 1.5"/hr and focused spots of 2-3" are possible,
    resulting in possible localized flash flooding.

    DISCUSSION...Well before arrival of eastern edge of very
    broad/deep layered cyclone across the Great Lakes, a surge of
    enhanced moisture sourced from the tropics/sub-tropics a week or
    so ago lifted northward across northern New England and has
    lingered in place. Total moisture values of 1.25-1.3", mainly
    loaded from the surface to 700mb as noted by upper 50s low 60s
    Tds, and 850-700mb CIRA LPW within the 95th-99th percentile (for
    the running mean over the last 20 years). Combined with solid
    clear skies and ample insolation throughout the day ahead of forcing/approaching cirrus deck, CAPEs have risen to 1000-1500
    J/kg across the area of concern.=20=20

    VWP and RAP analysis shows recent switch of boundary layer (850mb
    winds) to the south with values increasing to 15kts. Given weak
    capping, this has been sufficient convergence in proximity to
    higher terrain/upslope to break out isolated to widely scattered
    convection over the last few hours from the Presidental Range
    through the northern deep woods of Maine with a few cells reaching
    -45 to -50C. GOES-E WV suite shows vorticity center at mid-level
    intersection of weak warm conveyor belt lifting northeast but will
    be also peeling more northward over the next few hours this will
    bring some weak favorable upper-level divergence ascent pattern to
    help maintain convection but also result in further expansion of
    the 500-1000mb thickness ridge. With mean steering flow being
    weak at 5-10kts, this further helps to reduce forward propagation
    vectors, with some hints in Hi-Res CAMs that retrograding cells
    may occur toward the north and northwest with the approaching
    height-falls. This should support longer localized duration and
    with increasing convective coverage, higher potential for cell
    interaction and mergers. Given mild moisture flux and
    instability rates of 1.25-1.5" are possible. As such, localized
    widely scattered incidents of 2-3"+ may occur especially with any mergers/repeating through the late afternoon.

    While the area is remote/low population, it is fairly rugged and
    FFG values (minus the localized maxima near/north of Laconia, NH)
    of 1-1.5"/hr & 1.5-2" are well within range of being exceeded
    within/near the cores of these cells, and as such an incident or
    two of localized flash flooding is considered possible through
    00z.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Oi-V1B6cMaJw-S1ygvQDOCiF6RGiwOu8jcPzcGVUN2Jlti_30umJ-1MzUz1dPxzsj0I= hNeb1gjzgj9x6xfUhlBTh2U$ for graphic product...

    ATTN...WFO...CAR...GYX...

    ATTN...RFC...NERFC...NWC...

    LAT...LON 47496897 47196785 46306773 45596830 44856964=20
    43667092 43857186 44997123 45997052 47216964=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 16 22:05:11 2025
    AWUS01 KWNH 162204
    FFGMPD
    KYZ000-INZ000-ILZ000-170330-

    Mesoscale Precipitation Discussion 0279
    NWS Weather Prediction Center College Park MD
    604 PM EDT Fri May 16 2025

    Areas affected...Much of Kentucky...Adj Southern IL/IND...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 162200Z - 170330Z

    SUMMARY...Individual cells likely to expand and become more
    linearly oriented, tracking through areas already saturated.=20
    Additional 2-3" totals (in 1-3hrs) over the 1-3" from this
    morning, may result in scattered incidents of flash flooding into
    early overnight period.

    DISCUSSION...Initial cluster of super-cells is tracking through S
    IL entering western KY at this time, with additional development
    along the unstable areas surrounding them. Further expansion of
    the cluster is expected over the next few hours as cells continue
    to march through broad nose of 30-40kt southwesterly LLJ.=20
    Environment across western and central KY has nicely rebounded
    with temperatures into the mid 80s over upper 60s/low 70s Tds,
    while insolation was limited as dense high-CB anvils obscure the
    ground, instability has built back to well sufficient levels to
    maintain strong buoyancy through the late evening/early overnight
    period as cells rapidly race eastward. Strong moisture flux into
    the broad super-celll updrafts have increased rainfall efficiency
    over the last few hours with quick 1-1.5" sub-hourly totals
    estimated and some .75-1" totals noted upstream in SE MO.=20

    Initial convection will continue to expand and feed along the
    eastern edge of the LLJ with 1.5" total PWats feeding in, but
    overall the LLJ will narrow and veer ever so slightly, to become a
    bit more oblique to the outflow boundaries and allow for
    isentropic ascent/convergence along the flanking lines. Deep
    layer steering, while very strong and mean winds over 60kts, will
    slowly orient a bit more parallel to the updrafts supporting some
    short-term training of the flanking cells. 18z HRRR 15-minute
    rain totals occasionally reach 1.25-1.5" with the line as it
    progresses and as such spots of 2-3" are expected (generally
    aligning with 20-21z WoFS 50th to 90th percentile totals). Slow
    southward propagation will expose much of western and central KY
    to this additional heavy rainfall. This is of greater concern
    given the 1-3" totals that fell this morning. NASA SPoRT 0-40cm
    soil ratios got as high as 80-85% and FFG values reduced to less
    than 1.5"/hr across much of the area of concern with spots below
    .75"/hr into the more rugged terrain of central to eastern KY.=20

    Additionally, secondary development is probable along the cold
    front that has lagged the initial development with some continued
    heating and return moisture/instability flux through the MS River
    Valley. Additional upstream development, may further aid
    scattered repeating, further exacerbating any flooding conditions.
    So all considered, while severe weather is primary threat,
    especially across the next few hours; heavy rainfall will present
    sufficient totals to result in possible scattered incidents of
    flash flooding as well.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5FQSdt0kihQS_ChSagzFC57PMrZtSy4bQ9EHiIDINbgDX2_qtt-38mQgYH1igcKLCvj0= 5YULwxTj5m_CQcy9xxXLsi4$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...PAH...RLX...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 38728491 38528337 37868269 37288308 37048399=20
    36878565 36758699 36678874 37108912 37648864=20
    38148754 38538625=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 17 01:13:00 2025
    AWUS01 KWNH 170112
    FFGMPD
    TNZ000-KYZ000-MOZ000-ARZ000-170415-

    Mesoscale Precipitation Discussion 0280
    NWS Weather Prediction Center College Park MD
    912 PM EDT Fri May 16 2025

    Areas affected...Northeast AR...Northwest/Northern Middle
    TN...Bootheel of MO...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 170110Z - 170415Z

    SUMMARY...Upstream redevelopment and flattening steering flow
    support training environment for increasingly efficient rainfall
    producing thunderstorms.

    DISCUSSION...Regional RADAR and GOES-E 10.3um EIR loop shows line
    of severe/enhanced V overshooting top signatures continue to
    back-build along/ahead of the slowly advancing cold front across
    SE MO into NW AR. Strong speed shear aloft shows narrow wedge but
    fairly undirectional steering flow, generally parallel to the
    developing line along the front. Surface inflow of low to mid 70s
    Tds on 15-20kts of flow, veers to 45kts out of the WSW at 850mb,
    increasing moisture flux convergence to the updrafts. The deeper
    aligning LLJ is also increasing overall moisture values from 1.5
    toward 1.7/1.8" in total PWat values. As such, rainfall
    efficiency is increasing with rates currently reaching 1.5"/hr but
    will start climbing toward 2"/hr. Combine this with short-term
    training profiles and localized totals of 2-4" are becoming
    increasingly possible, especially as mature cells to the north
    increase cold pool geneation and propagate more south of due east
    into the path of these upstream developers.

    Cells are along the south and southwest edge of areas that
    received heavier rainfall this morning and FFGs reflect this
    ranging to aroudn 1.5"/hr and 2-2.5"/3hrs. Further south of the
    area of concern where recent drier conditions have existed, FFG
    values are about a 'category' higher at 2-2.5"/hr and
    2.5-3.5"/3hrs.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-MvhQmWbvnKieiVcTNm4NLzjOA9PrXTJ_nS_2j2MXN0W3qKV5mkp4mwadYxqCVnrbkaw= --iQqcc9E-pv1_H6kokxe6U$ for graphic product...

    ATTN...WFO...LZK...MEG...OHX...PAH...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 36658931 36618829 36608773 36568530 36118555=20
    35548893 35299096 35639184 36249136 36609015=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 17 03:18:24 2025
    AWUS01 KWNH 170316
    FFGMPD
    VAZ000-WVZ000-OHZ000-TNZ000-KYZ000-MOZ000-ARZ000-170915-

    Mesoscale Precipitation Discussion 0281
    NWS Weather Prediction Center College Park MD
    1115 PM EDT Fri May 16 2025

    Areas affected...Portions of the OH/TN Valleys

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 170315Z - 170915Z

    SUMMARY...Strong to severe thunderstorms will continue into the
    overnight hours across portions of the OH/TN Valleys, and will be
    capable of also producing heavy rainfall totals. A combination of
    cell-mergers and cell-training with moist antecedent conditions
    will maintain a threat for scattered areas of flash flooding.

    DISCUSSION...A well-organized severe weather outbreak continues to
    unfold across areas of southern OH down through especially central
    to southwest KY and northwest TN as a deep layer closed low
    advances east across the upper Midwest and sends a cold front
    southeastward into a very moist and unstable airmass.

    MLCAPE values this evening remain locally quite high across
    especially central KY through western TN with values of 2000 to
    3000 J/kg in place. This strong instability continues to work in
    tandem with enhanced shear profiles with 50 to 70+ kts of
    effective bulk shear to support supercell convection with an
    evolution into multiple linear bands/QLCS of activity over the
    next several hours as the broader convective threat advances
    eastward.

    The onset of nocturnal cooling will be initiating a gradual
    stabilization of the boundary layer and thus introducing some
    low-level CINH, but the hires model guidance suggests some
    intensification of the southwest low-level jet to as much as 50+
    kts by 06Z. This should maintain a strong degree of moisture and
    instability transport up across especially central and northern TN
    through central and eastern KY that will be conducive for
    maintaining a corridor of well-organized convection with heavy
    rainfall rates.

    Rainfall rates with the stronger and more organized cells will be
    capable of reaching 2 inches/hour, and with some likelihood for
    seeing cell-merger activity and cell-training, some additional
    rainfall totals of 2 to 4 inches will be possible. This is
    consistent with the 00Z HREF guidance, and it should be noted that
    recent HRRR runs overall appear to be locally a bit underdone with
    its QPF potential considering the high rainfall rates and
    cell-training concerns.

    The antecedent conditions across much of the region are quite
    moist, and some areas saw heavy rainfall just within the last 12
    to 18 hours. As a result, the additional rainfall amounts may
    result in scattered areas of flash flooding overnight.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6PWZMbL2SI6-aVebvdYnKT9Bm1kg1Wi4pF_DChZcHM7ZcaMU4nlY3I25chwg2XN5i0H4= _WPFeVs7jaH2vQ9BxK1ri8o$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...MEG...MRX...OHX...PAH...PBZ...
    RLX...RNK...

    ATTN...RFC...LMRFC...OHRFC...NWC...

    LAT...LON 39848076 38698000 37528106 36408303 35738505=20
    35418803 35718965 36508976 37168760 37818589=20
    38548465 39618286=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 17 16:40:02 2025
    AWUS01 KWNH 171638
    FFGMPD
    NHZ000-VTZ000-NYZ000-172230-

    Mesoscale Precipitation Discussion 0282
    NWS Weather Prediction Center College Park MD
    1238 PM EDT Sat May 17 2025

    Areas affected...northeastern NY into VT/NH

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 171636Z - 172230Z

    SUMMARY...Localized to widely scattered instances of flash
    flooding will be possible from northeastern NY into north-central
    New England through early evening. While the majority of cells are
    expected to be progressive, cell alignment will occasionally favor
    areas of short term training, capable of producing 1-2 inches of
    rain in an hour or less.

    DISCUSSION...16Z visible satellite and radar imagery showed
    scattered thunderstorms from eastern Lake Ontario into the
    Adirondacks, in the wake of a preceding swath of
    showers/thunderstorms advancing through VT. The storms over
    northeastern NY were located just downstream of the leading edge
    of a mid-upper level closed low centered over Lake Huron, within
    the diffluent left exit region of a 90-110 kt upper level speed
    max located just south of the closed low. The environment over
    northeastern NY into VT contained 500-1000 J/kg MLCAPE and 1.1 to
    1.4 inches of precipitable water per 16Z SPC mesoanalysis data.

    Daytime heating in the wake of overcast skies departing toward the
    east from VT (and eventually parts of NH) should allow for an
    expansion of CAPE across the region with 500-1500 J/kg likely from
    eastern NY into central/north-central New England over the next
    2-4 hours. Forecast stalling of a warm front over southern NH
    should limit the northeastward extent of instability and therefore
    rainfall intensity over eastern NH at least through late
    afternoon. A mixture of storm types will be possible given
    sufficient shear and instability but individual cells are expected
    to average 25-35 kt from the southwest. The concern for flash
    flooding will come from multiple rounds of cells over the same
    location and/or brief alignment of cells with the mean wind to
    support short term training. These scenarios could allow for 1-2
    inches of rain in an hour, or even as short as 15-30 minutes,
    given the strong ascent ahead of the upper low. 1-2 inches of rain
    (perhaps localized 3 inch totals) will be capable of localized to
    widely scattered flash flooding through 22Z. However, the coverage
    of these higher rainfall totals should stay somewhat limited
    across the region.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-7EM3pHbT7goWxmX10YGl1NPzHOPV8cGSEUpYB-UnBbR_Yct8s7eVOu09P55KJnodLJs= jsL5Un_9piRR3fgAOEN0WF4$ for graphic product...

    ATTN...WFO...ALY...BGM...BTV...BUF...GYX...

    ATTN...RFC...NERFC...NWC...

    LAT...LON 45217212 44987141 44247144 43467192 42777243=20
    42747308 42967348 43157380 43177476 43227535=20
    43217581 43417609 43667612 43967584 44407513=20
    45057386=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 18 05:17:00 2025
    AWUS01 KWNH 180515
    FFGMPD
    MSZ000-ARZ000-180913-

    Mesoscale Precipitation Discussion 0283
    NWS Weather Prediction Center College Park MD
    114 AM EDT Sun May 18 2025

    Areas affected...Portions of Central AR

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 180513Z - 180913Z

    SUMMARY...Some clusters of locally repeating/training showers and
    thunderstorms south of Little Rock and into the Pine Bluff
    vicinity may continue for a few more hours and result in a
    continuation of at least an isolated urban flash flood threat.

    DISCUSSION...The latest GOES-E IR satellite imagery along with
    regional radar shows a couple of clusters of cold-topped
    convection impacting areas of central AR. There is evidence of a
    modest MCV traversing the region which is interacting with the
    proximity of stationary front and a moist/unstable airmass pooled
    along it.

    Despite the increase in boundary layer CINH associated with
    nocturnal cooling, there remains as much as 2000 to 3000 J/kg of
    MUCAPE which coupled with a modest southerly low-level jet of 20
    to 30 kts overrunning the front continues to help favor some
    active convection across the region.

    The southwest flank of the overall MCS has been characterized by
    some cooling convective tops over the last couple of hours as this moist/unstable airmass continues to lift into the region in an
    elevated fashion. Over the next few hours, the convection will be
    capable of locally repeating/training over the same location, with
    areas south of Little Rock and especially near the Pine Bluff area
    seeing the greatest threat of this.

    Rainfall rates with the stronger storms will be capable of
    reaching 1.5 to 2.5 inches/hour, and some isolated additional
    totals of 3 to 4 inches will be possible. A localized urban flash
    flood threat will exist as a result.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5EGZlEQIqtiQPOA4W2rDRvnMOVaF0TkyXnOxmOS7c5IlSLNl5ZJmc0IRe_6pjlmaNd27= USnMxNDbEoa3YtoeZdsVhcg$ for graphic product...

    ATTN...WFO...JAN...LZK...MEG...

    ATTN...RFC...ABRFC...LMRFC...NWC...

    LAT...LON 34649207 34419083 33939089 33779169 33959293=20
    34249333 34569308=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 18 21:52:19 2025
    AWUS01 KWNH 182150
    FFGMPD
    TXZ000-OKZ000-190300-

    Mesoscale Precipitation Discussion 0284
    NWS Weather Prediction Center College Park MD
    549 PM EDT Sun May 18 2025

    Areas affected...Northwest and North TX into far southern OK an

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 182150Z - 190300Z

    Summary...Rapidly growing thunderstorms near a bulge in the
    dryline may result in rainfall rates as high as 2-3"/hr (and
    short-term totals of 3-5" with localized backbuilding). Isolated
    to scattered instances of flash flooding are possible.

    Discussion...Thunderstorms are rapidly initiating late this
    afternoon along a bulge in the dryline in the vicinity of Abilene,
    TX, near a maximum in surface-based instability (with 21z RAP
    analysis indicating 3000-5000 J/kg of SBCAPE across the greater
    North TX region). Convection should rapidly grow upscale in this
    mesoscale environment, which is also characterized by precipitable
    water values of 1.5-1.9 inches (between the 90th percentile and
    max moving average, per FWD sounding climatology), and (equally
    anomolous) deep layer shear of 50-60 kts. GOES-East water vapor
    imagery suggests a subtle shortwave trough near Midland, TX may be
    contributing to enhanced lift, and an associated ~100 kt jet
    streak (embedded within the broader phased jet structure) may also
    be ideally situated to the north (providing enhanced upper
    divergence via the right-entrance region). Storm mode may
    initially favor splitting supercells (relatively straight
    hodographs) with bunkers right vectors favoring much slower ENE
    motion (~25 kts) relative to the mean wind (~45 kts). With
    rainfall rates as high as 2-3"/hr anticipated, any backbuilding
    and training could result in significant short-term (3-6 hour)
    localized totals. This is expected to drive the greatest localized
    flash flood threat to the west of the DFW metro area (though
    upscale development into an MCS may allow for upwind propagation
    towards the ESE, and backbuilding along the western flank could
    bring training of heavier totals farther east into the DFW metro
    area).

    Hi-res CAMs are in relatively good agreement with regard to
    convective initiation along the (very well modeled) bulge in the
    dryline, though resulting QPF does vary quite dramatically. Some
    of the stronger solutions suggest the potential for 3-5" totals
    (mainly the FV3 and RRFS, the later of which has outlier solutions
    of 5"+ with some of the hourly runs). Taking a more probabilistic
    approach with the HREF and RRFSe ensemble systems (18z and 12z
    runs, respectively), a 40-km neighborhood method suggests a chance
    (15-30%) of 3" exceedance and a slight chance (10-20%) of 5"
    exceedance. These probability maxima are mostly concentrated to
    the north and west of the DFW metro areas, but an upwind
    propagating MCS could bring the threat of these totals into the
    DFW metro (and surroudning) area as well. Isolated to scattered
    instances of flash flooding are possible (and could be locally
    significant should backbuilding of convection manifest).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Xx0ler_E1yqiuvG2mxWyG8iBYDFiP8mCnHnL_bZRSp2KrYpMX8Nl4JGsNYNnXOUUIBU= HMescxKkMwd_B6P1O_on_j0$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...SJT...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 34319646 33889576 32839560 31459626 31109773=20
    31270024 32290012 33869946 34309805=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 19 02:24:00 2025
    AWUS01 KWNH 190223
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-190600-

    Mesoscale Precipitation Discussion 0285
    NWS Weather Prediction Center College Park MD
    1023 PM EDT Sun May 18 2025

    Areas affected...Central to Southeast NE...North-Central to
    Northeast KS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 190220Z - 190600Z

    SUMMARY... Scattered to numerous clusters of strong to severe
    thunderstorms will pose an increasing threat for isolated to
    scattered areas of flash flooding over the next few hours.

    DISCUSSION...The mid-evening GOES-E IR satellite imagery shows
    scattered to numerous areas of heavy showers and thunderstorms
    impacting much of central to southeast NE and into north-central
    to northeast KS. Very cold cloud tops are associated with the
    activity and there continues to be an array of supercell activity
    embedded within the larger scale convective envelope across the
    central Plains region.

    Ejecting height falls associated with a deep layer trough over the
    central Rockies will continue to advance gradually east over the
    Plains which will encourage the persistence of a strong south to
    southeast low-level jet of 40 to 60 kts over the region going into
    the overnight period. The low-level jet is overrunning a
    well-defined frontal zone and is yielding strong moisture and
    instability transport with a corridor of enhanced isentropic
    ascent poleward of the front.

    MUCAPE values across southern NE through eastern KS in close
    proximity to the front are as high as 1500 to 2500 J/kg and with
    strong effective bulk shear values of 50+ kts favoring
    well-organized clusters of convection. This setup should continue
    over the next few hours going through at least 06Z (1AM CDT), and
    with the enhanced moisture transport and convergence near the
    front, there will an environment conducive for additional
    cell-mergers and some cell-training.

    Rainfall rates are expected to locally reach 2.5 to 2.5
    inches/hour, with some additional storm totals of 3 to 4+ inches
    going through 06Z (1AM CDT). While antecedent conditions across
    the region are generally dry, the arrival of heavy convective
    rainfall along with the localized persistence of it over the next
    few hours will support a concern for isolated to scattered areas
    of flash flooding. The more urbanized locations in particular will
    be more sensitive to this threat.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9nCF6knr4PxQF8kVSnqwbBA6k5lLXCeNU12CoNUtdIfivBZ8YTx7mWeMWKhzYsYLaeU1= TpGnvn9WruDpSqPaxazBXVI$ for graphic product...

    ATTN...WFO...EAX...GID...LBF...OAX...TOP...

    ATTN...RFC...ABRFC...MBRFC...NWC...

    LAT...LON 42179992 41909763 41139609 39839494 38909459=20
    38629512 38799628 39969918 40820108 41770129=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 19 04:53:06 2025
    AWUS01 KWNH 190451
    FFGMPD
    MOZ000-KSZ000-191030-

    Mesoscale Precipitation Discussion 0286
    NWS Weather Prediction Center College Park MD
    1250 AM EDT Mon May 19 2025

    Areas affected...Far Southeast KS...Southwest MO

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 190450Z - 191030Z

    SUMMARY...Showers and thunderstorms may become a bit more
    concentrated over the next few hours over areas of far southeast
    KS and into southwest MO. Heavy rainfall rates and locally
    repeating cell-activity may result in sufficient rainfall totals
    for scattered areas of flash flooding overnight.

    DISCUSSION...Strong warm air advection with enhanced low-level
    moisture transport along with proximity of a strong elevated
    instability gradient is expected to set the stage for heavy shower
    and thunderstorm activity becoming a bit more concentrated over
    the next few hours across areas of far southeast KS and into
    southwest MO. This is all focusing well ahead of a deep layer
    trough edging out into the central Plains as a warm front
    gradually lifts northward across the region.

    A sharp instability gradient is noted in a northwest to southeast
    fashion across eastern KS down through far southwest MO and into
    northwest AR where this front is located, and there is as much as
    1500 to 2500 J/kg of MUCAPE along the boundary. This coupled with
    strong shear profiles and the nose of a 30 to 40+ kt southerly
    low-level jet has been yielding increasingly concentrated areas of
    heavy showers and thunderstorms over the last couple of hours.

    Given some additional nocturnal enhancement in the low-level jet
    overnight, this convection may attain some greater coverage and
    organization with MCS development/evolution possible near the warm
    front. The convection should tend to advance off to the east with
    time, with some east-southeast motion possible along the
    instability gradient if convection grows upscale into an MCS
    overnight.

    The 00Z hires model CAMs are generally in terrible agreement with
    respect to the convective details overnight, but recent GOES-E IR
    satellite imagery is showing cooling cloud tops over especially
    far southeast KS, and this trend favor an expansion of convection
    into southwest MO in at least the near-term.

    Rainfall rates with the stronger storms may reach 1.5 to 2
    inches/hour, and some localized storm totals by dawn may reach 3
    to 4 inches. This will be supported by a conducive environment for
    some repeating cell-activity near the aforementioned warm front.
    Some scattered areas of flash flooding will be possible where
    these heavier rainfall totals set up.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Klv7UJElzFeOvudX46NcuY9Q_C-iJETPVuQLB-z7mQZSKEy4T3PMasWHLNiEpSw8Qw6= 3QBQOLqLxxgnK4qKwc1lgl8$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...SGF...TOP...

    ATTN...RFC...ABRFC...LMRFC...MBRFC...NCRFC...NWC...

    LAT...LON 38719375 38439254 37839180 37339162 36739194=20
    36759328 37219449 37629502 38229513 38609459=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 19 05:42:31 2025
    AWUS01 KWNH 190542
    FFGMPD
    TNZ000-ALZ000-MSZ000-190940-

    Mesoscale Precipitation Discussion 0287
    NWS Weather Prediction Center College Park MD
    140 AM EDT Mon May 19 2025

    Areas affected...Northern MS and Northern AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 190540Z - 190940Z

    SUMMARY...A locally training band of showers and thunderstorms
    with high rainfall rates will continue to impact portions of
    northern MS while gradually moving east into downstream areas of
    northern AL over the next 2 to 3 hours.

    DISCUSISON...The latest radar imagery shows a broken band of heavy
    showers and thunderstorms traversing portions of northern MS
    (especially north of Tupelo) with an alignment north of a
    quasi-stationary front. This convection which is effectively a
    small-scale MCS has been rather long-lived at this point and
    continues to move east along a well-defined instability gradient
    pooled along the front.

    There continues to be as much as 1500 to 2000 J/kg of MLCAPE over
    areas of northeast MS through northern AL, and the convective mass
    will likely tend to be sustainable for at least a few more hours
    given favorable low-level moisture convergence nosing in along the
    southwest flank of the convection where warm air advcetion is more
    pronounced. Additionally, there is proximity of at least a weak
    MCV near the MS/TN border which should favor at least some modest
    mid-level forcing.

    Rainfall rates with this MCS have had a history of being quite
    high and upwards of 1.5 to 2.5 inches/hour. Over the next 2 to 3
    hours, the RRFS which has the best handle on this system (albeit a
    tad too far north), suggests an eastward extension of heavy
    convective rains that would allow for northern AL to be impacted.

    Some of these areas in general across northern MS and northern AL
    are quite moist from recent rainfall, and the arrival of as much
    as another 2 to 3+ inches of rain may allow for some runoff
    concerns and at least an isolated threat for flash flooding.

    This will especially be the case over northern AL where there is
    some locally higher/sloped terrain and thus potential for more
    efficient runoff given the high rainfall rates. Areas that will
    likely be impacted over the next 2 to 3 hours will include Muscle
    Shoals and eventually the Huntsville vicinity.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6RHvC0rpznoIBbk7DBnOZeZT79lcZCMUj_ebjgFNtpBftmrY9X_oU-BE89KIKfhXI_xR= SoNrjNxPcDM1s9NeWZ8ze0Q$ for graphic product...

    ATTN...WFO...BMX...HUN...MEG...OHX...

    ATTN...RFC...LMRFC...SERFC...NWC...

    LAT...LON 35068805 35068653 34918569 34388579 34158810=20
    34258924 34488983 34848987 35038910=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 19 06:32:03 2025
    AWUS01 KWNH 190631
    FFGMPD
    MOZ000-IAZ000-NEZ000-191030-

    Mesoscale Precipitation Discussion 0288
    NWS Weather Prediction Center College Park MD
    231 AM EDT Mon May 19 2025

    Areas affected...Southeast NE

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 190630Z - 191030Z

    SUMMARY... Heavy showers and thunderstorms will continue to impact
    areas of southeast NE for a few more hours which will maintain a
    threat of isolated to scattered areas of flash flooding. The more
    urbanized locations will be at greatest for any impacts.

    DISCUSSION...GOES-E IR satellite imagery along with the regional
    radar mosaic shows an expansive clustering of heavy showers and
    thunderstorms over southeast NE which continues to be driven by a
    strong warm air advection pattern downstream of an upper-level
    trough ejecting out across the central Plains.

    Enhanced moisture and instability transport with aid from a south
    to southeast low-level jet of 40 to 60 kts continues to surge over
    a warm front. MUCAPE values 1000 to 2000 J/kg remain in place, and
    the strong isentropic ascent/frontogenetical forcing on the
    poleward side of the warm front will help to maintain the
    organized elevated convective threat for at least a few more hours.

    Rainfall rates will continue in the near-term to be as high as 1.5
    to 2 inches/hour, and there will still be a threat for some
    localized small-scale linear bands of convection that train over
    the same area. This may yield some additional spotty rainfall
    amounts of 2 to 4 inches.

    The additional rains over the next few hours will maintain a
    threat for isolated to scattered areas of flash flooding with much
    of this concern focus around the more urbanized locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8ppNkW8ARl_FcmcBoGMLPKuYGoe24tSiO4PH51muFFbIH1CPv4olLvINsQAlp77Hk011= diXE4_fCbtUhVaMqaE_Bb7M$ for graphic product...

    ATTN...WFO...EAX...GID...OAX...

    ATTN...RFC...MBRFC...NWC...

    LAT...LON 41899722 41709633 41139555 40349543 40109603=20
    40089698 40299815 40719873 41329870 41799814=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 19 20:48:42 2025
    AWUS01 KWNH 192048
    FFGMPD
    MOZ000-IAZ000-KSZ000-200047-

    Mesoscale Precipitation Discussion 0289
    NWS Weather Prediction Center College Park MD
    447 PM EDT Mon May 19 2025

    Areas affected...eastern KS into northwest MO and far southern
    central IA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 192047Z - 200047Z

    Summary...Continued 1-2" hourly totals likely to train over the
    same areas, resulting in short-term (3-4 hour) rainfall totals of
    3-5". Scattered instances of flash flooding are likely.

    Discussion...Clusters of thunderstorms have rapidly developed and
    organized across eastern KS into northwest MO this afternoon,
    within an area of strong warm air advection (along a warm front
    and extending well into the warm sector of an associated cyclone).
    The mesoscale environment is characterized by MUCAPE of 2000-3000
    J/kg, PWATs of 1.4-1.8 inches (between the 90th percentile and
    daily max record, per TOP sounding climatology), and (equally
    anomolous) deep layer (0-6 km) shear of 50-60 kts. Storms are fast
    moving in this environment (generally following the 850-300 mb
    flow of 40-50 kts towards the NNE), but the tendency to orient
    parallel to the mean flow is resulting in highly efficient hourly
    rainfall totals of 1-2" (per MRMS estimates). Continued training
    of these efficient cells is likely, resulting in localized
    short-term (3-4 hour) totals of 3-5" (and supported by 12z HREF
    40-km neighborhood probabilities of 20-40% for 3-hr 3" exceedance
    through 00z). Scattered instances of flash flooding are likely.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9-PWbF8AIbhXy1oPXeNrpK2OygwWLLIYv-Z-iyZsEdpk9Rjo2ge80LkEhNtfDrHHD7yD= buhpGbSgtmAsbLoeS1EFGNE$ for graphic product...

    ATTN...WFO...DMX...EAX...ICT...SGF...TOP...

    ATTN...RFC...ABRFC...MBRFC...NWC...

    LAT...LON 40809422 40649294 38399355 37369473 37629577=20
    38789555 40049494=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 19 21:59:14 2025
    AWUS01 KWNH 192157
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-KSZ000-200200-

    Mesoscale Precipitation Discussion 0290
    NWS Weather Prediction Center College Park MD
    556 PM EDT Mon May 19 2025

    Areas affected...far North TX into much of central and eastern OK,
    adjacent portions of far northwest AR, southwest MO, southeast KS

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 192155Z - 200200Z

    Summary...Hourly rainfall as high as 2-3" to result in additional
    localized 3-6" through 02z (9pm CDT). Scattered instances of flash
    flooding are likely (and may be locally significant).

    Discussion...Discrete clusters of supercells are gradually
    becoming more prolific across far North TX into much of central
    and eastern OK, within a mesoscale environment characterized by
    SBCAPE of 2500-5000 J/kg, PWATs of 1.6-2.0 inches (near or
    exceeding the daily max value, per OUN/SGF sounding climatology),
    and deep layer (0-6 km) shear of 55-65 kts (above the 90th
    percentile). While storm motions are generally fast in this
    environment (with both the deep layer mean flow and bunkers right
    vectors 45-55 kts towards the NNE-NE), storms are increasingly
    organizing linearly with localized training of cells already
    resulting in some 2-3" totals (with MRMS and some local
    observations starting to indicate these totals in as little as an
    hour). As convection continues to organize with the approach of a
    potent shortwave trough over the TX Panhandle, expect convection
    to continue to proliferate and grow upscale with already
    substantial divergence aloft only further increasing (as the MPD
    region is within a very favorable placement between semi-phased
    subtropical and polar jet streaks). This may eventually result in
    somewhat slower (20-30 kt) storm motions more generally towards
    the east as convection begins to propagate upwind (towards the
    low-level jet, per the Corfidi vectors).

    Until convection organizes more linearly with meaningful eastward
    propagation, expect storms to continue to increase in coverage and
    result in additional localized training elements with additional
    localized totals as high as 3-6" possible (per hourly HRRR and
    experimental RRFS output, which has corrected westward in recent
    runs relative to the 12z HREF and 00z RRFS suites). Experimental
    WoFS 90th percentile of accumulated rainfall also agrees with this
    potential (and even indicates the potential for isolated 6"+
    totals north of the DFW metro area in far North TX with
    backbuilding towards the dryline with unimpeded strong low-level
    inflow from the Gulf). Scattered instances of flash flooding are
    likely (and may be locally significant, especially if 6"+ totals
    occur over sensitive localities that have seen as much as 2-3" of
    rain over the past 3-24 hours).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!59xDXd0SdSLI66eX_ARHnkHbV6RnZ4_HBJT9Y53aSEJp8Rhvy0pI1S--IA_0HcA9d4--= JCfcn5uqDK4XuhpkzzUzA7Y$ for graphic product...

    ATTN...WFO...FWD...ICT...LZK...OUN...SGF...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 37279552 36909358 35889340 34449471 33559584=20
    32919792 33419840 35279669 36669617=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 20 00:45:33 2025
    AWUS01 KWNH 200045
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-200430-

    Mesoscale Precipitation Discussion 0291
    NWS Weather Prediction Center College Park MD
    844 PM EDT Mon May 19 2025

    Areas affected...northeast KS, northwest MO, south-central IA, and
    far southeast NE

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 200040Z - 200430Z

    Summary...Continued thunderstorms (up to 1-2"/hr rates) within the
    warm sector of a nearby low pressure system will likely result in
    additional localized 2-4" totals through 0430z (1130 PM CDT).
    Scattered to numerous instances of flash flooding are likely (and
    may locally be significant in the vicinity of the Kansas City
    metro area).

    Discussion...Thunderstorms are once again expanding in coverage
    once again across portions of eastern KS, this time a bit farther
    west closer to the dryline (which is in the process of being
    overtaken by a lagging cold front). While much of the earlier
    convection has progressed north and east since the prior MPD,
    rainfall totals over the past 4 hours have been locally as high as
    1.5-5.0" (with the highest totals near and immediately north and
    northeast of the KC metro, where MRMS FLASH CREST unit streamflow
    indicating ongoing minor to moderate flooding, which has been
    gradually subsiding). Despite the earlier convection, the
    mesoscale environment remains supportive of heavy rainfall, with
    MLCAPE of 500-2500 J/kg, PWATs of 1.3-1.7 inches (above the 90th
    percentile, per TOP sounding climatology), and highly anomalous
    deep layer (0-6 km) shear of 50-60 kts. The recent convection
    along the dryline has been much slower to advance with localized
    backbuilding, but should start to propagate upwind (towards the
    ENE-E at 20-30 kts) as cold pools becoming more established (and
    eventually by the synoptic forcing of the cold front).=20

    The expectation is for localized 1-2"/hr rates to continue in this
    favorable environment, given observational trends and recent
    hi-res model data. This convection is likely to pass over the same
    areas that have recently received heavy rainfall, and may even
    locally train/repeat as well (as the mean 850-300 mb flow remains
    parallel to the dryline and ongoing convection). This should
    result in additional localized totals of 2-4" (as indicated
    consistently by runs of the HRRR since 20z, as well as the 50th
    percentile of accumulated rainfall from the experimental WoFS).
    Given 3-hr Flash Flood Guidance (FFG) of 2.0-3.0" (which largely
    doesn't take into account the recent rainfall), scattered to
    numerous instances of flash flooding are likely.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9vU_1Bw_WMlQLx0iMhaVTtrRKejjusIpoBJ-iLLr8HAXIAkd_EasNV5PsQqt3g_G_hgM= ZaES5oTOrL7-2gSiWQ9L-TY$ for graphic product...

    ATTN...WFO...DMX...EAX...ICT...OAX...TOP...

    ATTN...RFC...ABRFC...MBRFC...NCRFC...NWC...

    LAT...LON 41779594 41729509 41499419 40829308 40249281=20
    39219325 38399442 37769665 38329694 39449642=20
    40339680 40939678 41549652=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 20 02:03:47 2025
    AWUS01 KWNH 200203
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-200600-

    Mesoscale Precipitation Discussion 0292
    NWS Weather Prediction Center College Park MD
    1002 PM EDT Mon May 19 2025

    Areas affected...southeast OK, northwest and central AR, adjacent
    portions of far North TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 200200Z - 200600Z

    Summary...Linear convective system to continue producing hourly
    1-3" rainfall, additional localized 3-hr totals as high as 3-5"
    (through 05z, midnight CDT). Scattered to numerous instances of
    flash flooding are likely to continue, and may locally
    significant/life threatening.

    Discussion...Thunderstorms have undergone significant linear
    organization across portions of the Southern Plains, now moving
    gradually into the Lower MS Valley as the QLCS (quasi-linear
    convective system) propagates upwind to the E-ESE. The system has
    a history of producing very heavy rainfall (hourly rainfall as
    high as 2-3" with training/repeating segments), and some overlap
    with already hard hit areas is possible along the southwest flank
    (as has been consistently depicted by the experimental WoFS, still
    indicating the potential for hourly 2-3" totals near the Red River
    of the South). The mesoscale environment along and ahead of the
    convective system is characterized by MLCAPE of 1750-3500 J/kg
    (highest along and out ahead of the southwest flank), PWATs of
    1.7-2.0 inches (near the daily max moving average and record daily
    levels, per FWD and LZK sounding climatology), and tremendous deep
    layer (0-6 km) shear of 55-65 kts. Strong low-level moisture
    transport is being appropriately offset by divergence aloft
    (evident via GOES-East water vapor imagery, as the area remains
    ideally wedged between a semi-phased jet stream with subtropical
    jet along and south, and polar jet along and north). While CAMs
    have struggled with the rapid evolution of convection in this
    highly dynamic environment, observational trends (and most
    helpfully the rapidly updating experimental WoFS system) suggest
    that additional localized 3-5" totals are likely over the next few
    hours. Scattered to numerous instances of flash flooding are
    likely, and may be locally significant and life threatening (given
    3-hr Flash Flood Guidance as low as 1.5-2.0" and prior high totals
    partially overlapping the MPD).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_obl-6YcNFk9HM5yYk1s_xg7h9gDxuAyBo6BNj7PIMO5wp3UJFGie6VqtxAlcSzFJk0f= t7fCfZeVEwD4iLBuNqFUCSw$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SGF...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC...

    LAT...LON 36609217 36389116 35599154 34749251 33969369=20
    33519493 33369602 33479696 33579721 33979734=20
    34539667 35259583 35769516 36139470 36419423=20
    36559356 36589295=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 20 02:06:45 2025
    AWUS01 KWNH 200206
    FFGMPD
    INZ000-ILZ000-MOZ000-200705-

    Mesoscale Precipitation Discussion 0293
    NWS Weather Prediction Center College Park MD
    1005 PM EDT Mon May 19 2025

    Areas affected...Central and Southern MO...Central and Southern IL

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 200205Z - 200705Z

    SUMMARY...Increasing coverage of showers and thunderstorms with
    high rainfall rates along with areas of cell-training will likely
    result in scattered to numerous areas of flash flooding overnight.
    Locally significant and life-threatening urban flash flooding
    impacts will be possible.

    DISCUSSION...A well-organized band of heavy showers and
    thunderstorms with very cold convective tops continues to
    generally expand in coverage across central and southern MO with
    additional cells seen in radar imagery beginning to develop also
    farther east across eastern MO and small portions of western IL.

    All of this continues to evolve as a very strong warm-air
    advection pattern advances across the middle MS Valley and into
    the lower OH Valley with enhanced moisture and instability
    transport seen focusing up along and over a warm front. MLCAPE
    values are as high as 2000 to 3000 J/kg from central and southern
    MO through southern IL involving the warm sector, and the
    environment is very moist and strongly sheared with PWs of 1.6 to
    1.8+ inches and effective bulk shear values of 50+ kts. As a
    result, the convective mode is inclusive of supercell
    thunderstorms, and the latest radar shows a number of embedded
    supercells within the broader axis of convection.

    Over the next several hours, areas of significant cell-training
    will be a concern across areas of southern and eastern MO and into
    southern IL where radar trends along with recent hires model
    guidance supports the convection becoming increasingly aligned
    with the deeper layer southwesterly flow across the region.

    The latest HRRR, RRFS and experimental WoFS guidance all support
    high rainfall rate potential with the evolution of the supercell
    thunderstorm activity over the next few hours with rainfall rates
    reaching as high as 2.5 inches/hour, and this is certainly
    supported by the highly favorable thermodynamic and kinematic
    environment that is in place.

    Cell-training will likely favor some storm totals of 3 to 5 inches
    with isolated heavier totals to 6+ inches possible. This will
    likely result in scattered to numerous areas of flash flooding
    which will include the potential for significant and
    life-threatening urban flash flooding impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!66kuZVZ6W0BjlOXg3oPFMYzM38EtDM2KnSaaV6CzYZ3fWpFETgG2mSJduUdnVmA4_ezm= 7hcNUjDEnTNXU3BgWBAF1DU$ for graphic product...

    ATTN...WFO...ILX...LSX...PAH...SGF...

    ATTN...RFC...LMRFC...MBRFC...NCRFC...OHRFC...NWC...

    LAT...LON 40338905 39488773 37988803 36669033 36519312=20
    37399357 39109227 40159086=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 20 06:16:48 2025
    AWUS01 KWNH 200616
    FFGMPD
    TNZ000-MSZ000-ARZ000-TXZ000-OKZ000-201200-

    Mesoscale Precipitation Discussion 0294
    NWS Weather Prediction Center College Park MD
    216 AM EDT Tue May 20 2025

    Areas affected...Southeast OK into Central AR

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 200615Z - 201200Z

    SUMMARY...Showers and thunderstorms advancing east across
    southeast OK through central AR going through dawn will continue
    to support a threat for isolated to scattered areas of flash
    flooding.

    DISCUSSION...The latest GOES-E IR/WV suite along with regional
    radars show a broken axis of locally heavy showers and
    thunderstorms focusing across southeast KS through central AR. The
    overall convective trends over the last 1 to 2 hours has been
    tending to show some weakening of the activity over western and
    central AR, but with some upscale growth and cooling convective
    tops over southeast OK.

    Stronger shortwave dynamics ejecting east across KS/OK is helping
    to favor the redevelopment and expansion of convection closer to
    the Red River, and there remains a moist/unstable low-level jet of
    40 to 50 kts lifting up toward the broader Arklatex region. MLCAPE
    values are generally on the order of 1000 to 2000 J/kg with PWs
    locally near 1.5 inches, and this coupled with relatively decent
    shear profiles should maintain a convective threat through dawn
    that should be able to gradually move east back into areas of
    western and central AR.

    Expect some additional storms over the next few hours to be
    capable of 1 to 2 inch/hour rainfall rates, and with some
    localized repeating cell-activity, some additional rainfall totals
    through dawn may reach 2 to 3+ inches. Given some of the earlier
    rainfall, and potential for these rains to impact a few more
    urbanized locations, there will continue to be a threat for
    isolated to scattered areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!45iFJtRcqc5HE6CtYU1IyV8Q3amItxYRPRwiziYgMx67fHRRBaauXzngv_DcFhqBw3ji= fHKgXJzf2134johtAWfsG2U$ for graphic product...

    ATTN...WFO...FWD...LZK...MEG...SHV...TSA...

    ATTN...RFC...ABRFC...LMRFC...NWC...

    LAT...LON 35869043 34899027 34169153 33459388 33549513=20
    33969564 34369536 34829515 35269457 35739270=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 20 17:00:57 2025
    AWUS01 KWNH 201700
    FFGMPD
    VAZ000-WVZ000-OHZ000-TNZ000-KYZ000-202230-

    Mesoscale Precipitation Discussion 0295
    NWS Weather Prediction Center College Park MD
    100 PM EDT Tue May 20 2025

    Areas affected...Eastern KY...Northeast TN...Far Southwest
    WV/Western VA...Ext Southern OH...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 201700Z - 202230Z

    SUMMARY...Strengthening storms with history of quick 1-2" totals
    moving towards more hydrologically sensitive grounds and may
    result in an isolated to widely scattered incident or two of
    localized flash flooding.

    DISCUSSION...CIRA LPW depicts a western Gulf connected warm
    conveyor belt pressing eastward across the Cumberland and
    Tennessee River Valleys; though there is some tilting of the plume
    with 700-500mb starting to outpace/outrun the core of the surface
    to 850mb layer, but still a solid slug of 1.75" total PWats lay along/downstream of a corralling mid-level shortwave feature
    crossing into northern Middle TN; as such there is moisture flux
    trapping along the downshear angle northeast of the low along its
    expected path into central KY. An anchored surface front further
    sharpens ascent pattern as it bisects KY from FTK to DVK to JKL
    toward a surface inflection in SW WV. Additionally, last-night's
    pre-frontal convective trough has entered an area that has
    received solid insolation across Middle TN into central/eastern KY
    that an instability axis/bubble has formed with solid 2000 J/kg
    CAPE. Weakly backed mid-level flow ahead of the shortwave is
    enhancing weak confluence, deep layer convergence and instability
    advection to further enhanced thunderstorm activity. Cells
    near/downshear of the MCV near Allen county have increased
    rainfall efficiency to see a few observations at or just below
    1"/hr. This is expected to uptick slightly as updrafts broaden
    increasing that duration of the downdraft even just a few minutes
    for 1.5-2" totals to occur over the next 1-2 hours as the line
    continues a fairly progressive eastward march.

    The concern for isolated to widely scattered incidents of
    localized flash flooding only further increases due to more rugged
    terrain of the Cumberland Plateau and eventually the western
    slopes of the Appalachian Range. Additionally, NASA SPoRT 0-40cm
    relative soil moisture values remain elevated at 65-75% and
    therefore the lower FFG values of 1.5"/hr and 1.5-2.25"/3hrs are
    will within reach for minor exceedance (given duration/totals are
    likely to remain less than 3" with this progressive round). All
    considered localized flash flooding is considered possible this
    afternoon.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_X75e2fSTwI0T75wp1o4ayXg-BI0NU8OieXT6DURteTX7y-QuCQGCvbBIdk1emaOJTLo= OtscYtrjHDT9HG98KUjUdg0$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...MRX...OHX...RLX...

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 38978336 38828228 38448140 37768117 37168192=20
    36568236 35968363 35748472 35738567 36228610=20
    36788595 37698525 38788425=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 20 18:22:05 2025
    AWUS01 KWNH 201820
    FFGMPD
    ILZ000-IAZ000-202359-

    Mesoscale Precipitation Discussion 0296
    NWS Weather Prediction Center College Park MD
    220 PM EDT Tue May 20 2025

    Areas affected...Eastern Iowa...Northwest to Central Illinois...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 201819Z - 202359Z

    SUMMARY...Very slow moving thunderstorms, especially
    near/downstream of compact upper-low may produce localized 2-4"
    totals resulting in possible focused flash flooding incident(s).

    DISCUSSION...GOES-E Vis/10.3um EIR loops depict a compact
    upper-level low across far northeast MO. Relatively clear skies
    in proximity to the upper-low with ample low to mid-level moisture
    as noted in RAP analysis and CIRA LPW has built localized wedge of
    increased instability along the northeastern and eastern quadrants
    of the circulation across E IA and much of central to southern IL.
    SBCAPEs have risen to 2000 J/kg near the upper-low increasing
    steadily toward the southeast. Moderate northwest wrapping branch
    of the TROWAL shows sfc to 700mb PW around 1-1.25" with sfc Tds in
    the low to upper 60s. Strong deep layer convergence may be
    limited in wind speed at 20-25kts from 925-850, but directionally
    is more than sufficient to overcome weak capping for broad
    destabilization. Given this, modest rain-rates of 1.25-1.5" can
    be supported, the greater concern is very slow/stationary cell
    motions with forward (north, northeast and eastward) cell motions
    likely to be near zero along and downstream of the upper-low's
    path to the north-north east (allowing for 1-2 hours of heavy
    rainfall). As such spots of 2-4" totals are possible along the MS
    River in E IA and NW IL.

    Within the eastern/southeastern quadrant, deeper layer southwest
    to westerly steering will allow for increased cell motions of
    15-25kts toward the east across central IL, producing streaks of
    1-2" totals. This alone is not too concerning, however, given
    compact nature of the upper-low, there will be multiple bands of
    convergence allowing for a second round/repeat track of cells in a
    few hour time span. Narrower updrafts will make for intersection
    of storm tracks to be more random in nature though may result in a
    spot or two of 2-3" totals.

    Last evening's moderate rainfall has moistened the upper 40cm of
    soils with NASA SPoRT saturation ratios increasing to over 70%
    across central and E IA, as well as southern IL and brought
    central IL up to normal around 50%. As such, FFG values are a bit
    lower, near 1-1.5"/hr and 1.5-2.5"/3hrs. As such, localized
    exceedance is possible, though slightly higher near/along the
    upper-level low's track near the MS River. As such, a localized
    flash flooding incident or two is possible through late evening
    hours.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!98SFdPND8JK0l9clrcGygY1eqc-Fof8dzMJumkZ7Vc0mP5I2OBMuvsslOapLhdKBEiHR= x3JlfoSXGuVBeDXOcsymNzw$ for graphic product...

    ATTN...WFO...DVN...ILX...LOT...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 42329117 42309002 41948917 41438851 40588808=20
    39838844 39608915 39739004 39959030 40329047=20
    40519078 40629136 41089199 41769199=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 20 21:32:02 2025
    AWUS01 KWNH 202131
    FFGMPD
    TNZ000-KYZ000-210200-

    Mesoscale Precipitation Discussion 0297
    NWS Weather Prediction Center College Park MD
    530 PM EDT Tue May 20 2025

    Areas affected...portions of central and northern West/Middle TN
    into western and central KY

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 202130Z - 210200Z

    Summary...Training and repeating of 1-2"/hr rates may lead to
    localized totals of 2-3" (much of which will occur over relatively
    saturated soils) through 9PM CDT. Scattered instances of flash
    flooding are possible.

    Discussion...Semi-discrete severe thunderstorms are rapidly
    organizing linearly near (and just east) of the MS River (along
    the TN/AR/MO/KY border). This is occurring within a deeply
    unstable (2000-3500 J/kg of SBCAPE) warm sector, with the clearing
    cold front lagging significantly behind the line of storms (across
    eastern AR/southwest MO). Precipitable water along and ahead of
    the storms is between 1.5-1.9 inches, between the 90th percentile
    and record levels for the Nashville area (per BNA sounding
    climatology), and moderate to strong low-level moisture transport
    will transport these highly anomalous values northeast into the
    MPD region (with 925-850 mb flow of 35-45 kts). A semi-phased jet
    stream is providing sufficient diffluence aloft (though not ideal,
    within the right exit region of the broad jet streak), and ample
    deep layer (0-6 km) shear (50-60 kts) to organize updrafts into
    supercell structures (which are occurring both along and out ahead
    of the main line).

    The primary concern going forward with regard to flash flooding
    are for continued proliferation of convection to result in
    training and repeating elements along and out ahead of the main
    line. Notably, Flash Flood Guidance (FFG) across northern Middle
    TN into south-central KY is much lower than surrounding areas
    (1.5-2.0" over 3-hr), and this may contribute higher coverage (and
    greater potential for locally significant) flash flooding. MRMS
    QPE CREST unit streamflow indicates somewhat elevated activity in
    this region already, as NSSL QPE estimates 1.0-2.0" totals over
    the past 6 hours from an earlier line of storms.

    Hi-res guidance is in relatively good agreement with QPF through
    02z (9pm CDT), depicting localized 2-3" totals over the next 3-5
    hours (per 18z HREF and experimental 12z RRFSe PMM QPF, as well as
    the 90th percentile accumulated rainfall of the 19z and 20z runs
    of the experimental WoFS). Given the aforementioned wet antecedent
    conditions, this suggests 20-40% chances for FFG exceedance (per
    40-km neighborhood method of the 18z HREF and 12z RRFSe
    ensembles). Scattered instances of flash flooding are possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8KWYKChrGYjFMQVCsaqcrvSchhLS26ylgXMWZGbkzN0RVLwRgXU0BUhj6twJC6K0zEPA= Etc7X1uyHR7i8fsGmDu_unI$ for graphic product...

    ATTN...WFO...LMK...MEG...OHX...PAH...

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 37778649 37698540 37138513 36348524 36038574=20
    35758687 35338956 35958899 36528856 37148819=20
    37488745=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 21 01:58:16 2025
    AWUS01 KWNH 210157
    FFGMPD
    VAZ000-NCZ000-WVZ000-GAZ000-TNZ000-KYZ000-ALZ000-210530-

    Mesoscale Precipitation Discussion 0298
    NWS Weather Prediction Center College Park MD
    956 PM EDT Tue May 20 2025

    Areas affected...Portions of the TN Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 210155Z - 210530Z

    SUMMARY...Locally training showers and thunderstorms will continue
    through midnight across portions of the TN Valley. Additional
    concerns for isolated to scattered flash flooding will exist.

    DISCUSSION...The latest satellite and radar imagery shows a broken
    axis of heavy showers and thunderstorms extending from eastern KY
    down through middle and eastern TN and into northern AL.

    Overall, the airmass out ahead of this activity remains modestly
    buoyant with as much as 500 to 1000 J/kg of MLCAPE, and this
    coupled with effective bulk shear values of 50+ kts will continue
    to favor at least some organized convection with potential for a
    few supercells going through the midnight time frame. PWs across
    the region are moist too with PWs of 1.4 to 1.8 inches, but with
    the greatest moisture concentrations noted down across
    middle/eastern TN into northern AL.

    Rainfall rates will be capable of reaching 1.5 to 2 inches/hour
    with the stronger storms over the next few hours, and with radar
    showing some locally training of these cells, some additional
    storm totals with the overall band of convection may reach 2 to 3+
    inches. The most recent consensus of hires guidance including the
    HRRR, RRFS and the experimental WoFS support these rainfall
    amounts.

    Given the generally moist and sensitive soil conditions across the
    region, these additional rains going through midnight may result
    in some additional isolated to scattered areas of flash flooding.
    However, the convection and overall threat of heavier rainfall
    should tend to weaken after midnight.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5rjyOhWQ5M9bvnXw_ryV9AWYvz_piPagm-7AsJV7TEIpPVl5vU6Laiz-D6RXXa3Hrt2i= fCWB5jv1tT4ZA-jjIO-38Jw$ for graphic product...

    ATTN...WFO...BMX...FFC...GSP...HUN...JKL...MRX...OHX...RLX...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 38118373 37998233 36338257 34498433 33938629=20
    33958773 34418772 35348597 36318481=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 21 05:11:04 2025
    AWUS01 KWNH 210509
    FFGMPD
    GAZ000-210730-

    Mesoscale Precipitation Discussion 0299
    NWS Weather Prediction Center College Park MD
    108 AM EDT Wed May 21 2025

    Areas affected...Portions of Northern GA including the Atlanta
    Metropolitan area

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 210508Z - 210730Z

    SUMMARY...A band of heavy showers and thunderstorms will continue
    to settle gradually southeastward across areas of northern GA.
    These heavy rains will impact the broader Atlanta metropolitan
    area within the next 1 to 2 hours and may cause some urban flash
    flooding.

    DISCUSSION...The latest radar imagery shows a long-lived band of
    showers and thunderstorms approaching the Atlanta metropolitan
    area with heavy rainfall rates of 1 to 2 inches/hour. The
    convection continues to be maintained by the pooling of moisture
    and instability ahead of it.

    In fact, a southwest low-level jet of 30 to 40 kts is noted with
    as much as 500 to 1000 J/kg of MUCAPE. This coupled with some
    elevated effective bulk shear values (50+ kts) is still helping to
    foster some strong organized updrafts and will likely still favor
    some convective sustenance over the next couple of hours despite
    the battle with increasing boundary layer CINH/nocturnal cooling.

    Generally the shower and thunderstorm activity is rather
    progressive, but there may be sufficient levels of brief
    cell-training to yield some rainfall totals as high as 2 to 2.5
    inches before the band of convection exits the region off to the
    south and east and weakens.

    Given the urban environment that these rains will be falling over
    within the next 1 to 2 hours, there may be some runoff concerns
    and potential for at least localized flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4P-AULBDZcu6XfXzgJytui2Xj1QjbLHzE2pnlWyPZRRlDH2qYp8a34HtyqYnYlUKbPhD= Xi_ihp35Lut7Xgg7-il28_U$ for graphic product...

    ATTN...WFO...FFC...

    ATTN...RFC...ALR...NWC...

    LAT...LON 34248417 34218355 33818350 33498425 33488499=20
    33798516 34088476=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 21 06:28:37 2025
    AWUS01 KWNH 210626
    FFGMPD
    VAZ000-NCZ000-211130-

    Mesoscale Precipitation Discussion 0300
    NWS Weather Prediction Center College Park MD
    225 AM EDT Wed May 21 2025

    Areas affected...North-Central NC into South-Central VA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 210625Z - 211130Z

    SUMMARY...Locally slow-moving and repeating areas of showers and
    thunderstorms will be impacting portions of north-central NC and
    into south-central VA going through dawn. Isolated areas of flash
    flooding will be a concern as a result.

    DISCUSSION...Increasing warm-air advection and moisture transport
    riding up across the southern Mid-Atlantic region along with the
    arrival of a warm front will help to focus a gradual increase in
    shower and thunderstorm activity across north-central NC and
    especially south-central VA over the next few hours going into the
    dawn time frame.

    The latest surface analysis shows a front draped northwest to
    southeast across western and central NC and there is a pooling of
    elevated instability noted poleward of this boundary with MUCAPE
    values as high as 500 to 1000 J/kg nosing up through northern NC.
    A southwest low-level jet should becoming a bit better defined
    over the next few hours, and increasing to as much as 30 to 35+
    kts by 09Z (5AM EDT) across the region based on the latest RAP
    forecast.

    This will result in increasing isentropic ascent and a further
    expansion of elevated instability up into south-central VA.
    Meanwhile, the arrival of mid-level troughing/energy from upstream
    over the OH/TN Valley region is expected to be interacting with
    the front and should foster a developing wave of low pressure
    along as it lifts gradually northward very early this morning.
    This will yield a corridor of strong low-level convergence/forcing
    near the front which will favor additional concerns for areas of
    elevated convection to develop and become a bit more concentrated.

    The 00Z HREF guidance suggests the potential for rainfall rates
    with some of the elevated convection to reach as high as 1.5
    inches/hour. There may be some repeating cell-activity in a
    southwest to northeast fashion near an inverted surface trough
    north of the front, and that could support some totals by dawn of
    as much as 2 to 3+ inches. As a result, there may be some isolated
    concerns for flash flooding given more enhanced runoff potential.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6PMHzyXMGqTxPY0NYbbE2hpTC7xcRgMkL9w_DnLMkJxMXrY_qE4xHZ6UcsgA8D9-1_ai= bZ1uCCe6rvPjDvR3A-_k664$ for graphic product...

    ATTN...WFO...AKQ...RAH...RNK...

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37607716 36947679 36277833 36028016 36468049=20
    37017980 37547839=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 21 15:22:11 2025
    AWUS01 KWNH 211522
    FFGMPD
    LAZ000-TXZ000-212030-

    Mesoscale Precipitation Discussion 0301
    NWS Weather Prediction Center College Park MD
    1121 AM EDT Wed May 21 2025

    Areas affected...Southern Louisiana...Far Upper Texas Coast...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 211520Z - 212030Z

    SUMMARY...Highly efficient, slow moving thunderstorms with
    additional training and upstream development may result in
    localized 2-3"/hr rates and rapid inundation flooding is possible.

    DISCUSSION...An extremely moist deep layer profile exists along
    the frontal zone that is becoming coincident with the LA/Upper TX
    coastline. Total PWat values are over 2.25" with some suggestion
    of 2.5" values embedded along it. Initial convection has further
    sharpened the insentropic slope with 10-15kts of northeasterly
    flow opposed by 5-10 kts of due southerly flow across the front.=20
    Upper-level broad right entrance to 90kt 3H jet across
    east-central TX into northern LA is providing solid upper level
    divergence, which the convection is likely further enhancing to
    support additional development/organization over the next few
    hours. Given moisture, rates of 2.5-3"/hr are likely with the
    cores of the cells, which can be confirmed by last hour at LFT as
    well as surrounding observations near UofL-Layfette of 3" in the
    last hour as well...supporting localized rapid inundation
    potential.=20=20

    While the gradient of deep layer moisture/unstable environment
    basically aligns from I-10 to the coast, the steering flow is
    ideally orientened parallel to the front and moisture/instability
    graident to allow for favorable training environment. So given
    broad southerly flow/isentropic ascent convergence there are
    additional cells in the Upper TX coastal region with further
    congested cu west of Galveston Bay, hinting at continued expansion
    potential along/upstream for localized training environment
    throughout the rest of the morning/early afternoon hours from
    south of Houston to New Orleans. While Hi-Res CAMs suggest some
    dry air mixing to allow for southward propagation (cold pool
    generation), RADAR trends have not be aligned with this evolution
    but the risk should still remain along/south of I-10.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_fFy51LkxMH3PmueKRUzcGNlutVOHm1mK6VQpk4JFI_ChbbdzkV6n6Y67jaLck7vBZt5= -QQ6w2SOE43OhKcPQG9f8xk$ for graphic product...

    ATTN...WFO...HGX...LCH...LIX...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 30649023 30058986 29649004 29479139 29499251=20
    29629299 29699347 29059539 29529554 30169398=20
    30349339 30629173=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 21 18:06:42 2025
    AWUS01 KWNH 211806
    FFGMPD
    PAZ000-WVZ000-OHZ000-212200-

    Mesoscale Precipitation Discussion 0302
    NWS Weather Prediction Center College Park MD
    204 PM EDT Wed May 21 2025

    Areas affected...Northeast Ohio...Western Pennsylvania...Far
    Northern West Virginia...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 211800Z - 212200Z

    Summary...Isolated to scattered instances of flash flooding are
    possible, driven by localized hourly totals up to 1-2" and the
    potential for 3-hr localized totals in excess of 2".

    Discussion...Convection is blossoming this afternoon in the
    vicinity of the triple point of a surface cyclone, both within the
    warm sector/along the warm front and pivoting northwestward to the
    north of the center of the low. The mesoscale environment is
    characterized by a ridge of surface ThetaE of 330-336K,
    precipitable water of 1.0-1.2 inches (near the 90th percentile,
    per PIT sounding climatology), SBCAPE of 500-1500 J/kg, and deep
    layer (0-6km) shear of 35-55 kts. While current convection is
    moving at a decent clip within 30-40 deep layer (850-300 mb) flow
    (resulting in localized hourly maxima near 1.0", despite
    instantaneous rates as high as 2.0-2.5", per MRMS estimates),
    nearly unidirectional deep layer southwesterly flow (with 850 mb
    winds of 15-25 kts) could result in slower storm motions via
    upwind propagation should cold pools become more established (per
    upwind Corfidi vectors of 10-20 kts towards the east). Along with
    cell mergers and localized training segments, this may result in
    some localized hourly totals of up to 1-2" (as depicted by recent
    hourly HRRR and experimental RRFS runs, as well as the PMM of the
    12z HREF) with 3-hr totals 2"+ possible (per 12z HREF 40-km
    neighborhood probabilities of 20-30% for 2"/3-hr exceedance).
    Isolated to scattered instances of flash flooding are possible
    (with 12z HREF 40-km neighborhood probabilities for 1-hr and 3-hr
    FFG exceedance ranging from 30-40%, and generally maximized in the
    vicinity of the more sensitive Pittsburgh metro area).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!85oPV8A2K537IpIeK-9VoMAceI-sx7LtlSQSdFPcnRSgEiC8B2As97blEXYZmfFBeZ4Z= K7gj3PJ2z8Wr5nJjfgNq5y4$ for graphic product...

    ATTN...WFO...CLE...ILN...PBZ...RLX...

    ATTN...RFC...TIR...NWC...

    LAT...LON 42048009 41407950 40597928 39747949 39427978=20
    39178083 39368145 39728182 40208228 40558272=20
    40798300 41178314 41478284 41538235 41798142=20
    41908102=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu May 22 17:11:56 2025
    AWUS01 KWNH 221711
    FFGMPD
    TXZ000-OKZ000-222230-

    Mesoscale Precipitation Discussion 0303
    NWS Weather Prediction Center College Park MD
    111 PM EDT Thu May 22 2025

    Areas affected...Southern Oklahoma...Northern Texas....

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 221710Z - 222230Z

    SUMMARY...Maturing cluster thunderstorms continuing to back-build
    for a corridor of enhanced rainfall totals of 2-4"+. These cells
    may intersect recently saturated grounds to further increase
    potential for incidents of flash flooding through afternoon.

    DISCUSSION...16z surface analysis shows strong warm advection
    lifting primary/initial front northward mainly through the Big
    Country and northern Texas into the Red River Valley. This front
    is the leading edge of 70+ Tds toward the trailing edge of the
    secondary cold front that had stalled across central OK into AR.=20
    Stronger easterly flow, intersection of the frontal zones appeared
    to be the main focus of initial convective development across
    south-central OK. GOES-E WV suite denotes a weak mid-level
    weakness across central OK as well as a subtle cyclonically curved
    right entrance to the 70kt 3H jet (just west enough of stronger
    confluence over the Mississippi River). This divergence aloft
    has allowed for recent uptick/expansion of convective coverage
    further north into central OK.

    With surface pressure falls further west over the Cap Rock and
    backed low-level WAA, a ribbon of higher theta-E air is rotating
    around the western side of the complex supporting a wedge of
    increasingly unstable air. Isallobaric influence is resulting in
    surface turning to then ascend along the western, fairly
    stationary N-S outflow boundary. Visible imagery shows the ascent
    into the upwind side of the cluster allowing for additional
    upstream redevelopment, effectively anchoring the cluster. As
    such, localized rainfall efficiency is increasing through the
    initial cluster but also expanding northward with 1.5" rates,
    occasionally reaching 2"/hr, though hail is contaminating the rain
    rate estimates, local observations are starting to press 2" totals
    and with an hour or more time, localized spots of 4" are becoming
    increasingly possible (this is in line with RRFS, ARW/ARW2
    evolution which seem to have best handle on the evolution).=20

    Strong downstream convergence aloft is likely to limit eastward
    propagation and eventually dominating cold pools should press the
    best convergence further south into North Texas over the next 2-3
    hours, where best forcing in lower levels will continue to press
    westward, supporting upstream redevelopment and possible slow
    retrograding of the cluster with time. Unfortunately, the
    placement/tracks appear to be overlapping with areas that have
    received above normal rainfall over the last few days per AHPS.=20
    As such, localized FFG are reduced to about 2"/hr and 3"/3hrs.=20
    This further increases the potential for exceedance and possible
    further expansion and additional incidents of possible flash
    flooding through the afternoon.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_Uv2mqqWoUUIpk5a1jpB0LeWhTFz1VJxbQCKoEykMxIHrqNoPtV2cs3W7iu7_nWK_mYp= tdDl1QozSgkQSTV_neJ5sso$ for graphic product...

    ATTN...WFO...FWD...OUN...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 36359709 36339626 36059574 35319531 33969553=20
    32939596 32539729 32829838 33369869 34039834=20
    34459784 34879747 35299720 35969707=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 23 01:10:02 2025
    AWUS01 KWNH 230109
    FFGMPD
    TXZ000-230700-

    Mesoscale Precipitation Discussion 0304
    NWS Weather Prediction Center College Park MD
    908 PM EDT Thu May 22 2025

    Areas affected...TX Big Country into Hill Country

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 230105Z - 230700Z

    Summary...Localized hourly rainfall as high as 1-3" may result in
    some isolated 3-6" totals through 2AM CDT. A few instances of
    flash flooding are possible.

    Discussion...Convection has proliferated across the TX Big
    Country, in the vicinity of a weak surface low and an associated
    dryline and stationary boundary (the later of which has been
    bolstered and augmented by an earlier outflow boundary,
    originating from persistent deep convection over southern OK
    earlier this morning). MRMS indicates localized hourly rainfall of
    up to 1-2" over the past several hours in association with this
    convection, limited by relatively progressive storm motions of
    15-25 kts (as instantaneous rates are indicated to be as high as
    3-5"/hr). With the proliferation of convection over the past
    couple of hours, concerns are increasing for localized training
    and repeating near and south of the old outflow boundary. In
    addition, convection has been percolating downstream in the TX
    Hill Country, where much weaker deep layer mean flow (~10 kts) is
    allowing for localized hourly totals as high as 2-4" (per MRMS
    estimates). Besides the discrepancy in storm motions, the two
    areas have a similar parameter space with MUCAPE ranging from
    1000-2500 J/kg, precipitable water of 1.1-1.6 inches (between the
    daily mean and the 90th percentile, per FWD sounding climatology),
    and deep layer shear of 30-45 kts (increasing from south to north,
    with the greatest influence from the jet and associated northwest
    flow aloft near the Red River).

    While hi-res CAMs have struggled a bit overall with the robustness
    of the ensuing convection, the HRRR and experimental WoFS have
    done a decent job catching up with the evolution (by means of
    their rapid radar assimilation systems). The most recent HRRR runs
    (22z and 23z) depict localized totals of up to 3-5" through 07z,
    and the WoFS depicts localized totals as high as 4-7" (per 90th
    percentiule of accumulated rainfall from the 23z and 00z runs).
    While these two aforementioned areas of convection are expected to
    remain mostly separate, the northern line of storms should
    propagate meaningfully southeastward (upwind into the 15-25 kt
    low-level jet, by way of the Corfidi vectors) while shallower
    convection to the south meanders about (with some cells even
    drifting somewhat north within the low-level flow). With 3-hr
    Flash Flood Guidance generally ranging from 3.0-4.0" (and
    associated 18z HREF 40-km neighborhood probabilities of FFG
    exceedance ranging from 10-20%), isolated/localized instances of
    flash flooding are possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_HOccqQbjvrvAQLLdcr3BHisb5IcqYXiHKBcmJOdJvOij_DiTU_G4bZvZV2Af8vZUoPU= 8Z31rlnZwMZmzmMQ5csthcI$ for graphic product...

    ATTN...WFO...EWX...FWD...OUN...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 33459915 33239831 32729733 31549748 30919707=20
    30419712 30039758 29979902 30289992 30850032=20
    31620107 31960062 32230023 32490005 32949970=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 23 06:58:21 2025
    AWUS01 KWNH 230657
    FFGMPD
    TXZ000-231056-

    Mesoscale Precipitation Discussion 0305
    NWS Weather Prediction Center College Park MD
    257 AM EDT Fri May 23 2025

    Areas affected...portions of central Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 230656Z - 231056Z

    Summary...Isolated flash flood potential should persist for
    another 2-3 hours or so across central Texas and vicinity.

    Discussion...An intense cluster of thunderstorms has grown upscale
    through the night, with a favorable orientation for spots of 3-5
    inch/hr rain rates at times from Brown County, TX southward
    through Llano, County, Texas. These cells continue to be
    favorable environment for producing heavy rainfall (~3000 J/kg
    SBCAPE, 1.7 inch PW values, slow cell movement), although a slight
    weakening trend has been noted over the past half hour that is
    likely attributed to weakening low-level shear with southward and
    eastward extent. Despite these recent trends, the well-organized
    nature of the convection, presence of a mature cold pool, and weak
    downstream inhibition suggests that flash flood potential could
    continue on an isolated basis through 09Z-10Z or so - especially
    if cells can make it into the central Texas I-35 corridor while
    continuing their slow movement. Areas of 1-2.5 inch/hr rain rates
    remain likely at times through 09-10Z while deeper convection
    persists.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4lpK4KBSAKErboRwRAuPenFwwSzRC5Azzhy96g2BDYt-V2YrW8PM_ywabz-x-QmTOCvD= -4oZSgv_cBs_MgJEeIlhB_E$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31359842 30909741 30079702 28639716 28149913=20
    28770033 29740061 30450055 30689999 30609906=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 23 07:01:37 2025
    AWUS01 KWNH 230701
    FFGMPD
    TXZ000-231056-

    Mesoscale Precipitation Discussion 0305
    NWS Weather Prediction Center College Park MD
    301 AM EDT Fri May 23 2025

    Areas affected...portions of central Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 230656Z - 231056Z

    Summary...Isolated flash flood potential should persist for
    another 2-3 hours or so across central Texas and vicinity.

    Discussion...An intense cluster of thunderstorms has grown upscale
    through the night, with a favorable orientation for spots of 3-5
    inch/hr rain rates at times from Brown County, TX southward
    through Llano, County, TXs. These cells continue in a favorable
    environment for producing heavy rainfall (~3000 J/kg SBCAPE, 1.7
    inch PW values, slow cell movement), although a slight weakening
    trend has been noted over the past half hour that is likely
    attributed to weakening low-level shear with southward and
    eastward extent. Despite these recent trends, the well-organized
    nature of the convection, presence of a mature cold pool, and weak
    downstream inhibition suggests that flash flood potential could
    continue on an isolated basis through 09Z-10Z or so - especially
    if cells can make it into the central Texas I-35 corridor while
    continuing their slow movement. Areas of 1-2.5 inch/hr rain rates
    remain likely at times through 09-10Z while deeper convection
    persists.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_TREFCzR4mf2u0jWXv5LWb6BbIGF44wgBnJLtlehle7u-2E0sJeS25tI9HYUU4UBDIeO= J4kieA0iStwYFH__63MO5Ro$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31359842 30909741 30079702 28639716 28149913=20
    28770033 29740061 30450055 30689999 30609906=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 23 07:12:04 2025
    AWUS01 KWNH 230712
    FFGMPD
    TXZ000-231056-

    Mesoscale Precipitation Discussion 0305
    NWS Weather Prediction Center College Park MD
    311 AM EDT Fri May 23 2025

    Areas affected...portions of central Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 230656Z - 231056Z

    Summary...Isolated flash flood potential should persist for
    another 2-3 hours or so across central Texas and vicinity.

    Discussion...An intense cluster of thunderstorms has grown upscale
    through the night, with a favorable orientation for spots of 3-5
    inch/hr rain rates at times from Brown County, TX southward
    through Llano, County, TX. These cells continue in a favorable
    environment for producing heavy rainfall (~3000 J/kg SBCAPE, 1.7
    inch PW values, slow cell movement), although a slight weakening
    trend has been noted over the past half hour that is likely
    attributed to weakening low-level shear with southward and
    eastward extent. Despite these recent trends, the well-organized
    nature of the convection, presence of a mature cold pool, and weak
    downstream inhibition suggests that flash flood potential could
    continue on an isolated basis through 09Z-10Z or so - especially
    if cells can make it into the central Texas I-35 corridor while
    continuing their slow movement. Areas of 1-2.5 inch/hr rain rates
    remain likely at times through 09-10Z while deeper convection
    persists.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6-1nO1S90LzRhyfsWiT_jN799tZ3qsRaxsEz8ifKiGKSrC44_eTHwqYFL5qeUIIwu7fW= 99LUL7VkgLmLZRomwx5jQO4$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31359842 30909741 30079702 28639716 28149913=20
    28770033 29740061 30450055 30689999 30609906=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 23 15:59:11 2025
    AWUS01 KWNH 231559
    FFGMPD
    FLZ000-232200-

    Mesoscale Precipitation Discussion 0306
    NWS Weather Prediction Center College Park MD
    1158 AM EDT Fri May 23 2025

    Areas affected...Southeast Florida...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 231600Z - 232200Z

    SUMMARY...Slow moving very intense/efficient thunderstorms capable
    of 2.5-3"/hr rates and highly localized totals of 4-5"+ across
    urban corridor may result in rapid inundation flooding concerns
    through this evening.

    DISCUSSION...GOES-E Visible imagery, 15z surface observations and
    local VWP denote the old surface front/boundary is dissolving
    across southern Florida but vestiges of roll clouds and moisture
    gradient suggest it remains along/north of Grand Bahama and
    intersects with early morning sea-breeze along/just east of
    Broward county with the breeze boundary dropping south along the
    Keys. A secondary roll arc can be see SW of Collier
    county...suggesting the remaining front exists through the
    Everglades, though there is a weak vorticity center/twist in the
    cu field over western Palm Beach county which also matches up with
    925-850mb VWP and pooled/enhanced moisture pool. Td in the upper
    70s and total PWat values of 2" exist in the vicinity of the low
    with expanding cu field that has some suggestion of TCus starting
    to form. Given temps are nearing 90F, MLCAPEs are reaching 2000+
    J/kg along the eastern coast near the low/frontal zone.=20

    Destabilization is expected in the next 1-2 hours with this
    weakly convergence area and with the ample deep warm layer and
    moisture, rapid rainfall efficiency will rapidly increase with
    expanding thunderstorms. Deep layer flow is weak below 700mb but
    above, there should be enough westerly wind speed to support
    updraft outflow and some weakly organized cells for a few
    updraft/downdraft cycles increasing duration in vicinity of the
    urban corridor of SE Florida. Onshore flow should help to reduce
    eastward propagation (relative to similar cells that will develop
    along the SW FL coast). Given this rates of 2.5-3"/hr are
    possible, with 12z HREF probs of 3"/hr maximizing around 20-25%
    between 20-22z (2"/hr is near 45%); localized spots of 4-5" are
    possible in less than 1-3hrs possibly resulting in
    focused/localized rapid inundation flooding in the urban centers.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8ap2bN96LpgJxqTt9VvD_OBi_2sr22VHjYzpdG0tjXxAS3HB0wB_U-UCfiiAYOLaBvL8= iuSVy-P9FyqPtMmzPoyzTuw$ for graphic product...

    ATTN...WFO...MFL...MLB...

    ATTN...RFC...ALR...NWC...

    LAT...LON 27648050 27578036 27168019 26857999 26118003=20
    25698012 25468029 25458046 25788052 26118037=20
    26328033 26548043 26598045 27048070 27288078=20
    27538069=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 24 06:43:53 2025
    AWUS01 KWNH 240643
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-241242-

    Mesoscale Precipitation Discussion 0307
    NWS Weather Prediction Center College Park MD
    243 AM EDT Sat May 24 2025

    Areas affected...central through southeast Kansas, northeastern
    Oklahoma, southwestern Missouri, northern Arkansas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 240642Z - 241242Z

    Summary...Several rounds of thunderstorms should result in
    isolated to scattered flash flooding through 12-13z (7-8a CDT)
    this morning across the discussion area. Areas of 3-5 inch totals
    are expected, with heaviest totals from far northeast Oklahoma
    into southern Missouri and northern Arkansas.

    Discussion...Latest radar mosaic imagery depicts scattered
    convection with increasing coverage from southwest Kansas eastward
    to along the Missouri/Arkansas border near Flippin, AR. The
    storms are oriented parallel to west-northwesterly steering flow
    aloft while also focused on the nose of a broad 25-35 knot 850mb
    jet axis across Oklahoma. Steep mid-level lapse rates and strong
    shear aloft was enabling strong updrafts, while the orientation of
    low-level convergence was supporting training/repeating of cells
    especially across southern Missouri, where current estimates of
    2-4 inch rainfall totals were noted in a few areas over the past 6
    hours.

    The ongoing scenario favors a continued expansion of convection
    along the low-level convergence zone, with continued convective training/repeating resulting in scattered instances of flash
    flooding. Perhaps the greatest risk of excessive runoff will
    exist across far northeastern Oklahoma, southwestern Missouri, and
    northern Arkansas, where 1) the greatest duration of persistent
    deep convection will reside and 2) hilly/sensitive terrain exists,
    supporting flooding. Another 3-5 inches of rain is expected
    generally along an axis from Joplin, MO to Flippin, AR, with
    locally higher amounts possible.

    Farther upstream (across central Kansas), convection is slightly
    more progressive and FFGs slightly higher, suggestive of a more
    isolated flash flood threat compared to downstream areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-y8Y3h9C3QRncbB9oSJDjjLV_GJPj-OM3wrSeyge678rVH_mPxQEhetNFR5BfUAHsPUx= avQiE--uIsahayfQjB8GV5w$ for graphic product...

    ATTN...WFO...EAX...ICT...LZK...MEG...OUN...PAH...SGF...TOP...
    TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38709765 38479560 37669143 36099063 35319132=20
    35329453 35899682 37139798=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 24 06:56:37 2025
    AWUS01 KWNH 240655
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-241242-

    Mesoscale Precipitation Discussion 0307...Corrected
    NWS Weather Prediction Center College Park MD
    254 AM EDT Sat May 24 2025

    Corrected for graphic text and hatched area

    Areas affected...central through southeast Kansas, northeastern
    Oklahoma, southwestern Missouri, northern Arkansas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 240642Z - 241242Z

    Summary...Several rounds of thunderstorms should result in
    isolated to scattered flash flooding through 12-13z (7-8a CDT)
    this morning across the discussion area. Areas of 3-5 inch totals
    are expected, with heaviest totals from far northeast Oklahoma
    into southern Missouri and northern Arkansas.

    Discussion...Latest radar mosaic imagery depicts scattered
    convection with increasing coverage from southwest Kansas eastward
    to along the Missouri/Arkansas border near Flippin, AR. The
    storms are oriented parallel to west-northwesterly steering flow
    aloft while also focused on the nose of a broad 25-35 knot 850mb
    jet axis across Oklahoma. Steep mid-level lapse rates and strong
    shear aloft was enabling strong updrafts, while the orientation of
    low-level convergence was supporting training/repeating of cells
    especially across southern Missouri, where current estimates of
    2-4 inch rainfall totals were noted in a few areas over the past 6
    hours.

    The ongoing scenario favors a continued expansion of convection
    along the low-level convergence zone, with continued convective training/repeating resulting in scattered instances of flash
    flooding. Perhaps the greatest risk of excessive runoff will
    exist across far northeastern Oklahoma, southwestern Missouri, and
    northern Arkansas, where 1) the greatest duration of persistent
    deep convection will reside and 2) hilly/sensitive terrain exists,
    supporting flooding. Another 3-5 inches of rain is expected
    generally along an axis from Joplin, MO to Flippin, AR, with
    locally higher amounts possible.

    Farther upstream (across central Kansas), convection is slightly
    more progressive and FFGs slightly higher, suggestive of a more
    isolated flash flood threat compared to downstream areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9t77hMU9qKaGO04psibe9OYR7NakIsyhcVflkryF50w_GcXfOYDUSMx7zmwCG1ine3TD= 2fWPCHlyQhyyqQv0T9BHfMQ$ for graphic product...

    ATTN...WFO...EAX...ICT...LZK...MEG...OUN...PAH...SGF...TOP...
    TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38709765 38479560 37669143 36099063 35319132=20
    35329453 35899682 37139798=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 24 12:47:09 2025
    AWUS01 KWNH 241245
    FFGMPD
    TNZ000-MSZ000-MOZ000-ARZ000-OKZ000-KSZ000-241800-

    Mesoscale Precipitation Discussion 0308
    NWS Weather Prediction Center College Park MD
    844 AM EDT Sat May 24 2025

    Areas affected...Southeast KS and Eastern OK through the Ozarks

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 241244Z - 241800Z

    Summary...A sprawling MCS aligned north of a warm front will
    continue to dig southeast this morning while only slowly
    weakening. Rainfall rates of more than 2"/hr are likely at times,
    leading to 1-3" of rain with localized amounts above 4". This
    could cause instances of flash flooding.

    Discussion...The regional radar mosaic this morning shows a large
    swath of convection aligned WNW to ESE from southeast Kansas
    through the Ozarks and into western Tennessee. This convection is
    generally formed along the nose of a LLJ that is measured via
    regional VWPs of 30-35 kts from the SW, feeding into the clusters
    of thunderstorms to continue to fuel heavy rainfall rates
    estimated via local WSR-88Ds of 2-3"/hr at times. This convection
    is persisting just north of a warm front, so the LLJ is
    additionally lifting isentropically to produce ascent beyond the
    convergence along the nose of the LLJ. Additionally, an MCV is
    noted in the reflectivity moving into NW AR, with the accompanying
    convergence boundaries providing an additional impetus for
    strengthening areas of thunderstorms, although a bow echo
    developing

    Over the next few hours, the high-res CAMs are in good agreement
    that the developing bow echo will become the dominant feature as
    the LLJ begins to veer more out of the west, helping to sweep out
    the remaining convection from northwest to southeast. While this
    will result in faster general motion and a slow reduction in the
    flash flood potential, it will take several hours for everything
    to propagate southeast out of the area. Additionally, a convergent
    trailing tail west of this MCV/bow echo, noted already on
    reflectivity across SE KS, could result in some backbuilding and
    lingering heavy rainfall, despite more modest instability.
    Rainfall rate forecasts from the HREF and 15-min HRRR continue to
    indicate that 2"/hr or more are likely as everything dives
    southeast, although the heavier rates will likely be within the
    faster moving cells. Otherwise, there are moderate probabilities
    (20-40%) for rates exceeding 1"/hr along the convergent bands, and
    additional rainfall of 1-3" with locally more than 4" is expected.

    3-hr FFG across this area is generally 2-4", for which the HREF
    has a decreasing trend in potential for exceeding through late
    morning. However, where the rainfall rates are strongest near the
    MCV, or where multiple rounds can occur within the WAA downstream
    of the MCV/along any convergent bands, both the HREF and REFS
    suggest a 10-20% chance of exceedance, further indicating the
    continued potential for at least additional isolated flash
    flooding into the early aftn.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6twk8jaOYHowMlLwgESbuWirvoheBtWy26KWmZ3uLSFlTLJ8xh05itsuqM3PWkcVx8zf= Rjq_28bfv2BlMm-ZNhoVFW4$ for graphic product...

    ATTN...WFO...ICT...LZK...MEG...OUN...PAH...SGF...SHV...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 38129793 37889672 37559548 37349414 37049223=20
    36409057 35698979 34998938 34478944 34288987=20
    34279055 34309136 34449239 34369322 34239414=20
    34179495 34649580 35409653 36499697 37669796=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 24 17:18:55 2025
    AWUS01 KWNH 241718
    FFGMPD
    NEZ000-SDZ000-COZ000-WYZ000-242300-

    Mesoscale Precipitation Discussion 0309
    NWS Weather Prediction Center College Park MD
    118 PM EDT Sat May 24 2025

    Areas affected...Portions of the Central High Plains

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 241717Z - 242300Z

    Summary...Increasing coverage of showers and thunderstorms will
    spread across portions of the Central High Plains through this
    evening. Rainfall rates of 1+"/hr are possible at times, leading
    to rainfall of 1-2" with locally higher amounts where repeating
    cells occur. This may lead to instances of flash flooding.

    Discussion...The GOES-E visible satellite imagery this aftn
    depicts slow clearing of the low-overcast, resulting in a surge of
    increasing surface instability noted via the SPC RAP mesoanalysis.
    Within this destabilizing environment, updrafts are forming and
    strengthening as noted in the day-cloud phase RGB, and showers
    have begun to develop across eastern WY. This fresh convection is
    blossoming within a moistening column, aided by both upper level
    SW flow (clearly evident as well in the visible imagery) and
    underlying low-level SE flow which is pushing PWs to 0.7 to 0.9
    inches, above the 75th percentile according to the SPC sounding
    climatology. Embedded within the mid/upr SW flow, a shortwave is
    noted lifting across central WY, and this feature will enhance
    convective coverage into the afternoon, producing scattered to
    widespread showers and thunderstorms across the area.

    There may be two distinct modes of convection this aftn, but both
    have the potential to produce heavy rain rates. Across the
    Panhandle of Nebraska and much of SE Wyoming, the low-level
    upslope flow will provide the impetus for development. Storms in
    this vicinity will be generally slow moving as the low-level flow
    and upper level flow counteract, with storms forming along terrain
    boundaries, outflow boundaries, and differential heating
    boundaries, leading to potential backbuilding and training. The
    HREF rainfall rate probabilities for 1"/hr within this region peak
    above 25%, and this is supported by HRRR 15-min rainfall as much
    as 0.25-0.5 inches, so locally heavy rain with slower storm
    motions could produce 1-2" of rain with locally higher amounts in
    this area. Although soils are generally dry here as noted via NASA
    SPoRT observations, this could still result in isolated instances
    of flash flooding through the aftn.

    Farther to the north, the primary mechanism for development will
    be the progression of the embedded shortwave lifting into
    central/northern WY. The high-res CAMs are in good agreement that
    convection will become widespread as this forcing moves into the
    increasingly favorable thermodynamics. Storms here will likely
    organize in response to 30-45 kts of bulk shear, leading to
    clusters and possibly repeating rounds of rainfall with rates up
    to 1"/hr. FFG across South Dakota and northern Wyoming is lower,
    generally 1-1.5"/3hrs, for which both the HREF and REFS suggest
    has a 10-20% chance of being exceeded. While convection across
    this area will likely be moving more progressively to the east,
    isolated instances of flash flooding could still result.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7L7Bhc4Q3CUlvTaVOUtlI0VWuNSFXrp6Pc8Fw-AKKN4JF59f4ZmUGO0n5JY7PAFdd7-X= 00xyYHVhr7T5X5KXeuxuNzQ$ for graphic product...

    ATTN...WFO...BOU...CYS...LBF...RIW...UNR...

    ATTN...RFC...KRF...NWC...

    LAT...LON 44450414 44120356 43770277 43580233 43010212=20
    42660230 42430259 42000269 41250327 40980445=20
    41080553 42090618 43110598 44120570 44430506=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 25 03:48:36 2025
    AWUS01 KWNH 250348
    FFGMPD
    TXZ000-250746-

    Mesoscale Precipitation Discussion 0310
    NWS Weather Prediction Center College Park MD
    1147 PM EDT Sat May 24 2025

    Areas affected...portions of northwest Texas and the Texas South
    Plains

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 250346Z - 250746Z

    Summary...Isolated flash flood potential exists with slow-moving
    thunderstorms across the discussion area over the next 2-3 hours
    or so. Local rain rates exceeding 2 inches per hour may occur in
    a few areas through 07Z or so.

    Discussion...Initially high-based convective activity over the
    Texas South Plains has exhibited modest upscale growth and cold
    pool development while moving slowly east over the past couple
    hours or so. This has allowed for storms to reach slightly better
    moisture content and low-level shear (1.6 inch PW and 35 knots
    850mb flow), resulting in updraft persistence and heavy rainfall
    rates. Localized areas of 2-3 inch/hr rain rates have
    materialized just northwest of Jayton (Kent County) recently.
    Latest convective trends (exhibiting an uptick on convective
    coverage throughout the discussion area) suggests potential for
    somewhat greater longevity/persistence of convection than
    previously anticipated across the discussion area, with flash
    flood potential expected on at least an isolated basis over the
    next 2-3 hours or so.

    The heavier rainfall rates are falling in mostly rural portions of
    the discussion area. FFG thresholds are in the 2-3 inch/hr range
    and are being threatened where the most persistent convection has
    managed to evolve. These trends should continue for another 2-3
    hours or so.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6jRHTMMvP992bnR-tplyqr4QvxoNAVqY9iel-9K9-rvYi5NZoYFZ5hyauP6EzGYtGxx1= cTGKkpm1ZF-NAqE2m5RCV6o$ for graphic product...

    ATTN...WFO...FWD...LUB...MAF...OUN...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 34330000 33999854 33169852 32709952 32380079=20
    32430146 33220145 33590136 34120108=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 25 06:18:06 2025
    AWUS01 KWNH 250618
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-251216-

    Mesoscale Precipitation Discussion 0311
    NWS Weather Prediction Center College Park MD
    217 AM EDT Sun May 25 2025

    Areas affected...northern/centtral/eastern Oklahoma,
    southern/southeastern Kansas, southwestern Missouri, northwestern
    Arkansas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 250616Z - 251216Z

    Summary...Scattered clusters of thunderstorms will continue to
    expand in coverage across the discussion area, fostering
    development of ~2 inch/hr rain rates and and 2-3.5 inch rainfall
    totals through 12Z/7am CDT. These rain rates should result in a
    few instances of flash flooding.

    Discussion...Low-level flow has increased dramatically across
    Oklahoma this evening, resulting in a convergence zone generally
    along the OK/KS border. Storms have developed within this zone
    amid steep lapse rates aloft and strong instability (7C/km H7-H5
    and 1000-1500 J/kg MLCAPE). Individual storms within the
    convergence zone are exhibiting varied storm speeds/direction of
    movement amid a mix of elevated and near-surfaced based activity,
    resulting in a few cell mergers and prolonging of local rain
    rates. A few spots of 2-2.5 inch/hr rates have recently been
    observed just east of Ponca City.

    The storms are also expected to migrate generally eastward within
    the convergence zone toward areas that have received 1-6 inch
    rainfall totals over the past 24 hours - highest across
    southwestern Missouri. FFG thresholds across the discussion area
    are relatively low (1-2 inch/hr thresholds) - and exceedence of
    these thresholds are expected at times on a scattered basis
    through 12Z/7am CDT. Flash flooding is likely in this regime.

    Another potential scenario depicted/suggested by both models and
    observations is for mature, right-moving cells and/or clusters to
    migrate south/southeastward across eastern Oklahoma as cells
    mature through the night. This scenario would promote heavy
    rainfall across areas of east-central Oklahoma that have also
    received 3-5 inch rainfall amounts since last night and are
    sensitive to flash flooding (locales near Ada, McAlester, and
    Tulsa). Flash flooding is possible in these areas, but may take a
    few more hours to materialize (i.e., 09-12Z) compared to areas
    farther north and east.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8KREghq_1Zv9YChWDBinacOSRrXFSeN2cbXsp_8tkSX2pa8pWD_CEe0yVfGOds5U2Hbv= kVD0ua6CioIWkU-kazJj70U$ for graphic product...

    ATTN...WFO...ICT...LZK...OUN...SGF...SHV...TOP...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 38169680 37979466 37639310 36569245 35839289=20
    35299389 34489485 34619629 35579759 36519821=20
    38099843=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 25 12:05:08 2025
    AWUS01 KWNH 251205
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-251700-

    Mesoscale Precipitation Discussion 0312
    NWS Weather Prediction Center College Park MD
    804 AM EDT Sun May 25 2025

    Areas affected...South-Central Kansas through the Ozarks

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 251203Z - 251700Z

    Summary...Showers and thunderstorms will continue to train to the
    southeast for several more hours this morning. Rainfall rates
    within this convection will reach 1-2"/hr, at times higher,
    leading to pockets of rainfall that may exceed 3". This rain
    falling atop saturated soils may produce additional flash flooding.

    Discussion...The regional radar mosaic early this morning shows an
    impressive axis of showers and thunderstorms organized from
    central Kansas through northeast Arkansas. These storms are
    developing along the convergent nose of the LLJ which is measured
    via regional VWPs to be 30-40 kts, with weak impulses embedded
    within the mid-level flow contributing additional ascent. The
    primary storm mode within this area has been multiple clusters,
    organized through 40-50 kts of bulk shear as analyzed by the SPC
    RAP, helping to reinforce radar-estimated rain rates to above
    2"/hr as measured by local WSR-88Ds. On the western edge of this
    complex, an MCV is developing as noted within reflectivity, and it
    is this feature which will eventually sweep through from west to
    east, combining with the veering of the LLJ to bring a slow
    wane/end to the morning activity.

    During the next few hours, the high-res CAMs are in good agreement
    that, in general, activity will become more progressive to the
    east and begin to weaken. This will be due in part to the veering
    of the LLJ which will less efficiently transport the elevated
    thermodynamics south of the warm front into the region, while the
    MCV also sweeps through, with weak NVA in its wake suppressing
    additional ascent. Until this occurs, PWs of around 1.7 inches and
    MUCAPE around 2000 J/kg will support continued rain rates of
    1-2"/hr, with locally higher rates possible as reflected by HREF
    and REFS hourly-rain rate probabilities and the 15-min HRRR
    rainfall accumulations. This will lead to additional rainfall of
    1-3", with locally higher amounts possible where HREF exceedance
    probabilities rise to above 20% for 3"/6hrs.

    Although there is some spread both temporally and spatially among
    the guidance as to where the heaviest rain will occur the next few
    hours, the HREF EAS probabilities suggest the area from far SE KS
    through far NW AR has the greatest potential for heavy rain during
    the next few hours. This is also where 48-hr rainfall has been
    most prolific, 3-6", leading to FFG that is compromised to
    1.5-2"/3hrs due to exceptionally moistened soils. While flash
    flooding is possible anywhere within this area through late
    morning, these primed soils will be most susceptible to additional
    flash flooding.

    Later this afternoon, potentially after a break, additional
    convection is expected. While there is still uncertainty as to
    exactly where this will develop, it is likely that additional MPDs
    will be needed to address this threat.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_kG6UcP4P7JKLSHJyyFhw4xK0vh4umepX2Tyrr_Bl7XcdSrfawISXuYFdDBkCN3LhP7l= LkMuLvwdB7t1OXDkEuNHTM0$ for graphic product...

    ATTN...WFO...DDC...EAX...ICT...LZK...MEG...OUN...PAH...SGF...
    TOP...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 38639803 38479646 37959454 37499252 37179143=20
    36729089 36649090 36329078 35869082 35469139=20
    35259248 35409425 35769556 36439678 36909773=20
    37209833 37519870 38159880=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 25 15:29:43 2025
    AWUS01 KWNH 251529
    FFGMPD
    SCZ000-GAZ000-252130-

    Mesoscale Precipitation Discussion 0313
    NWS Weather Prediction Center College Park MD
    1129 AM EDT Sun May 25 2025

    Areas affected...Lowcountry of South Carolina, Southeast Georgia

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 251530Z - 252130Z

    Summary...Thunderstorms will expand and intensify across the
    Lowcountry of South Carolina and coastal plain of Georgia through
    the afternoon. These storms will move slowly and chaotically at
    times, allowing for 2-3"/hr rates to produce as much as 3-5" of
    rain. Flash flooding is possible.

    Discussion...The GOES-E day-cloud phase RGB late this morning
    shows rapid expansion and intensification of updrafts associated
    with increasing coverage of convection noted on the regional radar
    mosaic. This activity is blossoming in response to an MCV, likely
    a remnant from convection yesterday over the Ozarks, moving across
    South Carolina, while a shortwave and accompanying surface low
    tracks across Georgia. Additional forcing for ascent is being
    provided via convergence, both along a slowly advancing warm
    front, and through sea breeze interactions. This ascent is acting
    upon extremely favorable thermodynamics characterized by PWs
    analyzed by the SPC RAP of 1.7 to 1.9 inches, above the 90th
    percentile for the date, and expanding SBCAPE above 3000 J/kg.
    Where the strongest ascent is overlapping these most impressive
    thermodynamics, rainfall rates have been estimated via KCLX to
    exceed 2.5"/hr.

    As the afternoon progresses, the high-res CAMs are in good
    agreement that convection will expand across eastern GA and
    southern SC as forcing for ascent increases in response to the
    movement of the shortwave and warm front into the area. This will
    act upon thermodynamics that will remain extremely robust,
    supporting rainfall rates that may approach 3"/hr at times as
    noted via both HREF and REFS probabilities for 2"/hr exceeding
    30%. Although shear is minimal, which will likely limit storm
    organization, these rates could become problematic as storms track
    extremely slowly through the aftn. This will be due to generally
    weak 0-6km mean winds of just around 10 kts to the east, being
    impeded by the westward advance of the sea breeze boundary within
    the weakly forced environment. This will result in the collapse of
    Corfidi vectors to 5 kts or less, suggesting nearly stationary
    storms or chaotically moving storms. With rain rates expected to
    remain 2-3"/hr, this could produce 3-5" of rain in some areas.

    Rainfall across the region has been minimal as of late, reflected
    by both AHPS rainfall departures and NASA SPoRT soil moisture,
    which has resulted in elevated FFG that is generally 3"/1hr and
    4"/3hrs. Despite that, modest FFG exceedance probabilities do
    exist among the ensemble systems, further indicative of the
    intense rainfall potential. While flash flooding impacts will be
    most likely across urban areas, anywhere storms linger or repeat
    could experience flash flooding.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9DLkYv3UfhzPax8FzGSVG40XByARSD3hJqCbX4HLpyJJhPgsdAysjcKd2Sn_Lr55-5-s= WqoGaRBLj0MXQ9HNJu0W5IU$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...JAX...TAE...

    ATTN...RFC...ALR...NWC...

    LAT...LON 33568094 33538039 33397992 33247959 32987960=20
    32677989 32428023 32118065 31768098 31508131=20
    31458190 31458286 31628335 31908333 32368308=20
    32758280 33268215 33438162=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 25 17:00:12 2025
    AWUS01 KWNH 251700
    FFGMPD
    TNZ000-MSZ000-MOZ000-ARZ000-OKZ000-252200-

    Mesoscale Precipitation Discussion 0314
    NWS Weather Prediction Center College Park MD
    1259 PM EDT Sun May 25 2025

    Areas affected...Eastern Oklahoma through much of Arkansas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 251659Z - 252200Z

    Summary...Showers and thunderstorms will increase in coverage once
    again this afternoon and move across portions of Oklahoma and
    Arkansas. Rainfall rates of 1-2"/hr or more are expected, which
    could produce 2-3" of rain with locally higher amounts by this
    evening. Flash flooding is possible.

    Discussion...The combination imagery of the regional radar mosaic
    and Day-Cloud Phase RGB suggest the environment from the Southern
    Plains into the Lower MS VLY is becoming favorable for renewed
    convective growth. Updrafts noted in the RGB coincident with
    increasing Lightning Cast values suggest the environment is
    destabilizing, additionally reflected by SPC RAP MLCAPE of
    1000-3000 J/kg, and in some areas this is resulting in rapid
    uptick of reflectivity values associated with thunderstorms. While
    convection from this morning has primarily decayed, remnant
    outflow boundaries and the wavering stationary front are providing
    focus for ascent, which within the increasing instability and
    overlapped ~1.7 inch PWs, is resulting in renewed convection. This
    is most clearly evident along a boundary in the vicinity of Fort
    Smith, AR, but other cells blossoming from eastern AR to nearly
    the Red River Valley indicate the flash flood risk is steadily
    increasing this aftn.

    The high res CAMs, despite latitudinal differences in their
    simulated reflectivity, are all in agreement that coverage will
    expand quickly in the next few hours. This is supported by current observations, with more rapid growth likely as a shortwave tracks
    west to east overhead from OK. The latitudinal uncertainty
    reflected in the CAMs provides some challenge for the greatest
    flash flood risk location, but the HRRR, ARW2, and RRFS are more
    closely aligned, and south, of the other guidance, which is tied
    better to the current instability gradient. This is also supported
    by what should be a slight jog south of the stationary front as it
    gets pushed by remnant outflow boundaries. As thunderstorms
    develop, they should track progressively to the east on 0-6km mean
    winds of around 20 kts, but as they deepen and organize thanks to
    bulk shear of 30-40 kts, clusters will begin to track E/SE and
    repeat/train over the same areas. With rain rates progged by both
    HREF and REFS probabilities to exceed 2"/hr (20-40% chance), this
    will result in stripes of 2-3" of rain with locally higher amounts
    possible (20-30% chance).

    This region has been saturated by heavy rainfall. 48-hr rainfall
    from MRMS has been anywhere from 2 to 6 inches, leading to
    extremely compromised FFG as low as 0.5-1.5"/3hrs. This suggests
    that any of these heavy rates will quickly yield runoff, leading
    to potential instances of flash flooding through the aftn.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_v_l5HEX3go-cZVenFMuvBvN9Og1R9Q8um1oN-feJn-AiwUD5ZDpGK5OS8a4cVjhvr9g= No6safGxp7Kf7pxsWlOFKvg$ for graphic product...

    ATTN...WFO...LZK...MEG...OUN...PAH...SGF...SHV...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 36609089 36539035 36358994 36118963 35568958=20
    34679039 34099205 33959377 34069530 34169611=20
    34399644 34789655 35809605 36379524 36489359=20
    36539179=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 25 22:15:34 2025
    AWUS01 KWNH 252214
    FFGMPD
    TXZ000-OKZ000-NMZ000-260330-

    Mesoscale Precipitation Discussion 0315
    NWS Weather Prediction Center College Park MD
    613 PM EDT Sun May 25 2025

    Areas affected...northwestern TX into central OK

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 252211Z - 260330Z

    Summary...Localized to scattered areas of flash flooding are
    expected from portions of northwestern TX into central OK through
    03Z as a result of slow moving and training of thunderstorms. Peak
    rainfall totals of 3 to 5 inches are expected, although locally
    higher totals cannot be ruled out.

    Discussion...22Z radar imagery across TX and OK showed a few
    scattered thunderstorms over the southeastern TX Panhandle near a quasi-stationary front and just east of the southern Caprock
    Escarpment. Additional thunderstorms were noted over
    south-central OK, near/north of the front. Large MLCAPE values of
    3000 to 4000+ J/kg were estimated via the 21Z SPC mesoanalysis
    along with sufficient shear for organized cells and PWATs that
    ranged from ~0.7 inches near the I-27 corridor to 1.7 inches in
    east-central OK. A slow moving cell over Motley and Dickens
    counties has had a history of backbuilding toward the west along
    the boundary and additional cells were forming within the unstable
    environment nearby.

    Additional thunderstorms are likely to develop over the next few
    hours over the TX Panhandle into south-central OK, especially
    beyond 00Z with an expected increase in the low level jet (20 to
    40 kt by 03Z at 850 mb). In addition, RAP guidance supports the
    strengthening of an upper level jet max over OK/KS, placing the TX
    Panhandle into OK within the divergent and diffluent right
    entrance region after 00Z. Deeper layer mean flow is from the
    southwest but right and left splitting supercells will follow
    motions deviant from the mean wind with outflows and mergers
    resulting in some chaotic movement at times. An overall movement
    toward the east is expected of the expanding TX
    Panhandle/northwestern TX convection with eventual merging with
    activity into OK. Rainfall rates will vary but could contain peak
    rain rates in the 2-3 in/hr range. Flash flooding is considered
    likely on an isolated to scattered basis, especially if storms can
    overlap with recent heavy rain over portions of northwestern TX.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!90uWgDyKLH9TtxLjurgvBC3FxgMR4pMVJZ6CDGZvqJ88cm8XFRFYOrsHnh_l1A2rG4ah= 4MsbV5X2bDuDVHlYOkTY9Lg$ for graphic product...

    ATTN...WFO...ABQ...AMA...FWD...LUB...MAF...OUN...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35619821 35519731 35319668 35099637 34519628=20
    34229637 33919662 33579760 32689931 32330035=20
    32250150 32510225 33470231 33460334 33840398=20
    34360379 34690268 35090174 35329970=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun May 25 22:55:46 2025
    AWUS01 KWNH 252255
    FFGMPD
    ALZ000-MSZ000-LAZ000-ARZ000-TXZ000-OKZ000-260400-

    Mesoscale Precipitation Discussion 0316
    NWS Weather Prediction Center College Park MD
    654 PM EDT Sun May 25 2025

    Areas affected...lower MS Valley into northern AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 252254Z - 260400Z

    Summary...A few areas of flash flooding will be possible from near
    the Arklatex, across the lower MS Valley into northern AL through
    04Z. Rainfall rates of 1 to 2+ in/hr are likely along with 2-4
    inch totals (locally near 5 inches possible).

    Discussion...2230Z visible satellite and regional radar imagery
    showed a line of thunderstorms which extended from western TN into south-central AR, preceded by an elongated outflow boundary. An
    apparent MCV was identified over western TN, near the northern
    edge of the convective line. Scattered thunderstorms were ongoing
    south of the outflow from southern AR into north-central MS. To
    the east, another (slower moving) outflow boundary was located
    southwest and then west of a remnant MCV tracking through eastern
    TN. South of these outflows, the environment was very moist and
    unstable with 1500 to 4000+ J/kg MLCAPE and PWATs locally over 2
    inches in southern AR via 22Z SPC mesoanalysis data.

    While the main outflow boundary surging southward through AR and
    northern MS is expected to maintain a progressive movement toward
    the south, there could be some slowing/stalling along the western
    flank. Merging with cells preceding the outflow along with areas
    of brief training, especially along the western flank, may support
    a few areas of flash flooding over the next 3-5 hours. Aiding with
    ascent should be an increasingly diffluent regime in the upper
    levels along with divergence within the right entrance region of a
    jet max positioned to the north over the Midwest. 2 to 4 inches of
    rain (locally near 5 inches) is expected.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6oiodd3oUl6JW9t67JbcQCyOAXe5gHWIBW-bLHuaMJFwDNk8cDhKO4M-r4CWJz4tySwc= 8UnR3zBxEXGV4cwA4eyWoC0$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LZK...MEG...SHV...

    ATTN...RFC...ALR...ORN...TUA...NWC...

    LAT...LON 34998848 34888737 34818590 34198568 33718629=20
    33198763 32688876 32319080 32209226 32579389=20
    33129449 33759459 34249386 34429268 34529159=20
    34979006=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 26 03:10:59 2025
    AWUS01 KWNH 260309
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-260908-

    Mesoscale Precipitation Discussion 0317
    NWS Weather Prediction Center College Park MD
    1109 PM EDT Sun May 25 2025

    Areas affected...northern Texas, southern Oklahoma, southwestern
    Arkansas, northwestern Louisiana

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 260308Z - 260908Z

    Summary...Scattered to numerous thunderstorms are expected to
    continue moving slowly across the Red River Valley and vicinity
    tonight. Local amounts of 3-5 inch rainfall totals are expected.
    Several instances of flash flooding are likely.

    Discussion...Clusters of thunderstorm activity continue to slowly
    propagate eastward across portions of southwestern Oklahoma and
    portions of west-central Texas currently. These cells are mostly
    outflow dominant and in the process of further congealing amid
    relatively weak steering flow aloft (around 20 knots or so).=20
    Abundant moisture and instability downstream of these clusters
    (2000 J/kg MLCAPE and 1.5-1.7 inch PW values) should enable them
    to continue on their eastward trek for several hours. Gradually
    increasing 850mb flow across downstream areas of north
    Texas/southern Oklahoma through the night should also aid in their
    organization and persistence. Areas of 2 inch/hr FFG thresholds
    (locally lower) should be exceeded with the most persistent
    activity and any cell mergers, suggestive of a continued flash
    flood threat through the overnight hours.

    Radar mosaic imagery also indicates a gradually increase in
    convective activity across south-central Oklahoma. These cells
    are likely responding to increased ascent from strengthening
    low-level flow impinging on outflow/synoptic front near the Red
    River. As these cells continue to increase in coverage, they will
    eventually merge with incoming MCS(s) from the west, resulting in
    prolonged rainfall potential. Spots of 3-5 inch rainfall totals
    should fall in these areas on already wet grounds from antecedent
    rainfall, and potentially significant flash flood impacts cannot
    be ruled out.

    FFG thresholds are higher across much of north Texas, representing comparatively drier conditions that have persisted in the area
    over the past 1-2 weeks. Flash flood potential might be more isolated/conditionally tied to slow-moving cells/mergers that can
    prolong rainfall for longer than one hour and/or fall on sensitive
    ground conditions.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Q-DNL40N-TvWsixZzAGoqzF6GpgeHbhYAtK5Q1cY7ziEnoNd7o_HnWObWqKjsS0DCPA= vY1kgbyAz_lhTBzJmdNWArA$ for graphic product...

    ATTN...WFO...FWD...LUB...LZK...OUN...SHV...SJT...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35799712 35649521 34889410 33829334 33029292=20
    32459402 32139568 32199801 32590001 33350021=20
    34249945 35159884 35579843=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 26 03:59:25 2025
    AWUS01 KWNH 260359
    FFGMPD
    GAZ000-ALZ000-260758-

    Mesoscale Precipitation Discussion 0318
    NWS Weather Prediction Center College Park MD
    1158 PM EDT Sun May 25 2025

    Areas affected...east-central Alabama and west-central Georgia

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 260358Z - 260758Z

    Summary...Spotty/isolated flash flood potential exists for another
    2-4 hours or so.

    Discussion...Latest radar/observations depict a focused axis of
    convection very near an old outflow extending from near Gadsden,
    AL to just south of Atlanta, GA. These cells were moving
    relatively slowly while ingesting sufficient moisture and
    instability (1.5-1.6 inch PW/1000 J/kg SBCAPE) to produce spots of
    1-2.5 inch/hr rain rates (estimated per MRMS). These cells were
    also located along and ahead of an eastward-moving MCS over
    central Alabama. At the current rate of motion, the central AL
    MCS should overtake the preceding convection and reduce rainfall
    potential substantially after it's moved through (in the 04-08Z
    timeframe - latest with eastward extent). Until this happens,
    rain rates should approach FFG thresholds on at least an isolated
    basis, and local amounts of 3-3.5 inches cannot be completely
    ruled out.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6S4bFJHSPQWZ3wikte43bjEYHYtq1mdRThnnFQdLZsYqRHq7XP_kfpREswfrJDqtahTG= Fo5IKS1fLCTMW0UO45Mft7o$ for graphic product...

    ATTN...WFO...BMX...FFC...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34178605 33938485 33558380 32708374 32488537=20
    33098676=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 26 08:41:05 2025
    AWUS01 KWNH 260840
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-OKZ000-261438-

    Mesoscale Precipitation Discussion 0319
    NWS Weather Prediction Center College Park MD
    439 AM EDT Mon May 26 2025

    Areas affected...north/east Texas, north/central Louisiana,
    southwest Mississippi, southwest Arkansas, far southeastern
    Oklahoma

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 260838Z - 261438Z

    Summary...Flash flood potential should gradually increase across
    the discussion area as convective complexes traverse the region
    through 14Z/9am CDT this morning.

    Discussion...Flash flood potential is expected to concentrate
    along a couple of axes through 14Z this morning - 1) along and
    just ahead of an expansive linear complex extending from McCurtain
    County, OK west-southwestward through Mineral Wells, TX and 2)
    along a stalling outflow boundary extending from near Shreveport,
    LA east-southeastward to near Natchez, MS. Texas convection so
    far has been progressive, but cell motions have been slow enough
    for 1-2 inch/hr rain rates to materialize near the Dallas/Fort
    Worth Metroplex and pose primarily urban flash flood potential.=20
    These cells were gradually moving toward areas of higher FFGs
    (from central into eastern Texas), suggestive of a potentially
    lessening flash flood risk over time and with southeastward extent
    despite abundant moisture and instability in the pre-convective
    airmass. Local cell mergers and should also play a role in
    enhancing rain rates, and at least a few instances of flash
    flooding are likely especially in sensitive/urbanized areas.

    Farther east, a southward-moving outflow boundary from prior
    convection has stalled, with vigorous redevelopment along it
    boosting rain rates into the 1-2.5 inch/hr range in a few spots
    (including Shreveport Metro). The stalling boundary raises
    concern for prolonged heavy rain rates and localized totals
    exceeding 5 inches in spots through 14Z this morning - posing a
    threat for flash flooding especially in urban and sensitive
    locations. Portions of Louisiana (including Shreveport) could
    experience heavy rain from both the stalled outflow and the
    upstream Texas linear complex this morning.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7zTWtTEGey_T9pVK-D0XrnPNObWz31bcJxabnfL-kpgwsLFc2E_qWCmgoRwABtmOC2p9= aDJ8e16_mH28YGprD8x8_pc$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...JAN...LCH...LIX...LZK...OUN...
    SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 34389506 33999362 33159168 32049056 31249044=20
    30779125 30869408 30839796 31609862 32729881=20
    33249793 33919582=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 26 14:02:01 2025
    AWUS01 KWNH 261401
    FFGMPD
    MSZ000-LAZ000-ARZ000-261900-

    Mesoscale Precipitation Discussion 0320
    NWS Weather Prediction Center College Park MD
    1001 AM EDT Mon May 26 2025

    Areas affected...Northern LA...Western & Central MS...Southeast
    AR...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 261400Z - 261900Z

    SUMMARY...Intense squall line along/ahead of MCV/Cold Pool will
    track through areas having received heavy rainfall yesterday and
    again this morning. An additional 1" in 30 minutes followed by
    shield precip may reaggravate flooding conditions through early
    afternoon.=20

    DISCUSSION...Regional RADAR mosaic depicts a mature MCS with well
    defined boundary features, with a strong bow/squall line extending
    from the meso-low southwest of ELD along the state line
    southwestward into the Piney Woods before becoming oriented west
    to east across the Heart of TX. An effective warm front has been
    established along the outflow boundary from yesterday's complex
    across MS/AL. Solid southerly and southwesterly return flow from
    the Gulf brings Tds in the the mid-70s and with active scattered
    convection along it throughout the pre-dawn enhancing a meso-high
    across E MS; the gradient has sharpened increasing moisture flux
    convergence along it. Weakening low level flow has reduced
    convergence but localized clusters, such as the one near HEZ have
    allowed for focused convection to continue resulting in ongoing
    flash flooding conditions even prior to the line. As such,
    portions of southeast AR, Northeast LA and SW MS have seen
    generally 1-2" with those enhanced hot-spots to 4", reducing
    capacity of the upper soil column.=20=20

    VWP shows a slow reduction of the LLJ toward 25kts which is
    veering ahead of the squall line, but the forward speed driven by
    1016mb meso-high and northeast shifting MCV into SW AR,
    convergence will remain strong enough to maintain the northern
    (southeast propagating) portion of the line. Total moisture over
    2" and MUCAPE of 1000-1250 J/kg will allow to maintain solid
    rainfall production. Rainfall rates up to 1.5"/hr are probable,
    though only 15-30 minutes of duration will result in a quick
    .75-1" in such short duration over the saturated soils that will
    maintain any ongoing flash flooding or trigger a scattered
    incident or two along the path generally along I-20. Potential
    for flash flooding should reduce slightly toward central MS where
    soils have not been as compromised as locations further southwest,
    especially near Natchez, MS.

    It should be noted that additional new stronger development is
    probable along the downstream edge of the complex into S MS/AL
    toward afternoon but this is less certain in timing/placement and
    will watch trends closely for any additional MPD need.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-uCZ3I6sr9k0AIOc5b45KrubKEguzuPpBhC7dfCE5kHriCsNkqHRRxohb-UkRJAu-5UH= cGT8ZnGF2AfpPLsdDkjZxiQ$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...LZK...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 33639133 33229018 32738938 32128904 30988945=20
    30749001 31009111 31189214 31389305 31809355=20
    32499352 33579296=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 26 19:36:26 2025
    AWUS01 KWNH 261936
    FFGMPD
    TXZ000-OKZ000-270000-

    Mesoscale Precipitation Discussion 0321
    NWS Weather Prediction Center College Park MD
    335 PM EDT Mon May 26 2025

    Areas affected...north-central TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 261935Z - 270000Z

    Summary...Rainfall rates of 1-2 in/hr will be possible across
    portions of north-central TX over the next few hours. These rains
    may overlap with portions of northern TX which received heavy rain
    over the past 24 hours, allowing for increased sensitivity to
    additional rainfall.

    Discussion...1915Z satellite and radar trends showed a small
    cluster of thunderstorms expanding just west of the DFW Metroplex
    near a quasi-stationary front, which roughly paralleled I-20 from
    near DYS to TYR. Infrared cloud tops have been cooling and
    coverage has been increasing over the past hour. The storms were
    located along the northeastern gradient in instability with about
    500 to 1500 J/kg MLCAPE. Meanwhile, locations to the east had less
    than 100 J/kg and locations to the southwest were over 2000 J/kg
    (via 19Z SPC mesoanalysis data). RAP model analyses and VAD wind
    data showed a narrow corridor of stronger 850 mb winds of 20-25
    kt, extending from near KGRK to the NNW toward I-20, intersecting
    the frontal boundary and resulting in lift.

    Short term forecasts from the RAP suggest the narrow corridor of
    850 mb winds will continue to provide lift near the front and
    resulting rain-induced outflow near the I-20 corridor, with mean
    storm movement toward the northeast to east. This motion will
    likely allow for overlap of heavy rain into portions of northern
    TX which picked up 2-4 inches of rain late Sunday night into this
    morning through 00Z. The addition of another 2-3 inches over the
    next 3-4 hours may result in renewed flash flood concerns for the
    region. While there is a definitive minimum in instability to the
    east of the DFW Metroplex, some replenishment of instability is
    likely in the short term with low level moisture returning, though
    there remains uncertainty in rainfall intensity to the east of the
    Metroplex through early evening.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_dt3v-0nB4xmvphN9Jwlc0LLUhse8iUyxyzBXlyKwHHBZXF6S7K0ppk9oS_HBZ_2kSMG= GPYd2mnbsg9eAIsBr7HlxvA$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 33969720 33859654 33799567 33559535 33159522=20
    32409540 32059635 32419755 32699844 33029889=20
    33419879 33759829 33899779=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon May 26 22:04:34 2025
    AWUS01 KWNH 262204
    FFGMPD
    TXZ000-270245-

    Mesoscale Precipitation Discussion 0322
    NWS Weather Prediction Center College Park MD
    604 PM EDT Mon May 26 2025

    Areas affected...central TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 262201Z - 270245Z

    Summary...Thunderstorms are expected to expand in coverage through
    the evening, possibly resulting in flash flooding over portions of
    central TX, including the TX Hill Country. Rainfall rates will
    vary but could be as high as 2-3 in/hr.

    Discussion...Local radar imagery over west-central TX at 2130Z
    showed a strong supercell over Menard County, tracking toward the
    southeast at 15-20 kt with additional cells feeding in from the
    south. These storms were located along an outflow boundary that
    extended from the the middle/upper TX coast, northwestward to a
    stationary front that was analyzed northeast from a triple point
    low near OZA. SPC mesoanalysis data showed the cells were within a
    very unstable environment with 3000-4000 J/kg MLCAPE, with roughly
    5000 J/kg located southward, closer to the Rio Grande. VAD wind
    data from KEWX showed 850 mb winds of ~20 kt from the SE,
    emanating from a moisture rich environment where Blended TPW
    imagery showed 2+ inches of PWAT over south-central TX to the
    middle TX coast.

    These cells were forming out ahead of the southeastern edge of a
    an upper trough moving from NM into West TX. Given the largely
    uninhibited environment in place near/south of the outflow and in
    the vicinity of the triple point low along with larger scale
    forcing ahead of the upper trough, additional cells are likely
    across portions of the Edwards Plateau through 00Z.

    This type of environment favors supercells whose motions can be
    somewhat unpredictable due to storm scale influences, possibly
    leading to slower movement with enhanced rainfall efficiency with
    mesocyclones, allowing for at least a localized flash flood
    threat. Beyond the localized threat, there are indications for at
    least a modest increase in the low level flow beyond 00Z which
    could support a greater coverage of storms into the late evening
    and early overnight, with cell movement toward the east but
    potential upstream development leading to training and a greater
    flash flood risk. This threat for later in the night will continue
    to be monitored but there is at least a near-term flash flood
    concern from ongoing cells, mergers and slow movement.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6nCLXvX1ON5q8vsqdQjWWy8khzT-w9Erc4ysnjBnXk7n3cvDNzBg03A900Ayj5mfAgDA= X-hCITpU2h_rwqL2GsGAcjQ$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31939871 31749784 31209721 30359723 29299789=20
    29059920 29300076 29690141 30590150 31150080=20
    31520001=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 27 02:59:55 2025
    AWUS01 KWNH 270256
    FFGMPD
    TXZ000-270700-

    Mesoscale Precipitation Discussion 0323
    NWS Weather Prediction Center College Park MD
    1056 PM EDT Mon May 26 2025

    Areas affected...south-central TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 270253Z - 270700Z

    Summary...Thunderstorms are expected to expand in coverage through
    the evening, possibly resulting in flash flooding over portions of
    central TX, including the TX Hill Country. Rainfall rates will
    vary but could be as high as 2-3 in/hr.

    Discussion...Local radar imagery over west-central TX at 2130Z
    showed a strong supercell over Menard County, tracking toward the
    southeast at 15-20 kt with additional cells feeding in from the
    south. These storms were located along an outflow boundary that
    extended from the the middle/upper TX coast, northwestward to a
    stationary front that was analyzed northeast from a triple point
    low near OZA. SPC mesoanalysis data showed the cells were within a
    very unstable environment with 3000-4000 J/kg MLCAPE, with roughly
    5000 J/kg located southward, closer to the Rio Grande. VAD wind
    data from KEWX showed 850 mb winds of ~20 kt from the SE,
    emanating from a moisture rich environment where Blended TPW
    imagery showed 2+ inches of PWAT over south-central TX to the
    middle TX coast.

    These cells were forming out ahead of the southeastern edge of a
    an upper trough moving from NM into West TX. Given the largely
    uninhibited environment in place near/south of the outflow and in
    the vicinity of the triple point low along with larger scale
    forcing ahead of the upper trough, additional cells are likely
    across portions of the Edwards Plateau through 00Z.

    This type of environment favors supercells whose motions can be
    somewhat unpredictable due to storm scale influences, possibly
    leading to slower movement with enhanced rainfall efficiency with
    mesocyclones, allowing for at least a localized flash flood
    threat. Beyond the localized threat, there are indications for at
    least a modest increase in the low level flow beyond 00Z which
    could support a greater coverage of storms into the late evening
    and early overnight, with cell movement toward the east but
    potential upstream development leading to training and a greater
    flash flood risk. This threat for later in the night will continue
    to be monitored but there is at least a near-term flash flood
    concern from ongoing cells, mergers and slow movement.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7sg9zYosmAk-rVtAupeJVZ4zIKjblOwzw1aLNpbBRoTB3ohKnJYcGI5tT6L3b5ylo1_v= nojnA0GCdPhruQos53t3sGk$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30749673 30119625 29319668 28799794 28609890=20
    28669968 29000056 29430091 29860111 30150099=20
    30390044 30229912=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue May 27 14:04:05 2025
    AWUS01 KWNH 271403
    FFGMPD
    GAZ000-ALZ000-MSZ000-272000-

    Mesoscale Precipitation Discussion 0324
    NWS Weather Prediction Center College Park MD
    1002 AM EDT Tue May 27 2025

    Areas affected...Southern and Eastern MS...Central AL...Northwest
    GA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 271400Z - 272000Z

    SUMMARY...Heavy showers and thunderstorms with some cell-training
    concerns will favor a threat for isolated to scattered areas of
    flash flooding going into the afternoon hours.

    DISCUSSION...A broken QLCS continues to advance off to the east
    this morning across portions of central and southern MS which is
    expected to advance downstream into areas of western and central
    AL through midday. However, recent radar and satellite trends
    already show an expansion of convection out ahead of the main QLCS
    activity, and in general, GOES-E IR satellite imagery shows an
    axis of cooling convective tops from central MS through
    west-central AL.

    The airmass will be destabilizing with time for many downstream
    areas of western and central AL and also into northwest GA going
    through the early afternoon hours. This coupled with the arrival
    of the convectively-enhanced shortwave traversing the lower MS
    Valley and interaction with a moist southwest low-level jet of 30+
    kts nosing up across eastern MS through central AL should favor a
    general expansion of convection over the next several hours.

    PWs rising to over 1.75 inches and the destabilizing boundary
    layer will contribute to an uptick in rainfall rates. The
    relatively organized nature of the convective cells will be
    capable of yielding some rainfall rates of as much as 1.5 to 2
    inches/hour which is supported by the 06Z HREF guidance.

    The overall convective footprint in satellite and radar imagery
    suggests a concern for cell-training going into the afternoon
    hours and some of the HREF guidance supports some rainfall totals
    of as much as 2 to 4+ inches going through mid-afternoon.

    Locally wet antecedent conditions from recent rainfall are
    reflected in lower FFG values, and the latest NASA SPoRT soil
    moisture data in conjunction with USGS streamflow data suggest
    sensitivities that will contribute to elevated runoff concerns. As
    a result, isolated to scattered areas of flash flooding will be
    possible where these heavier rainfall amounts occur over the next
    several hours. This will include potential for some urban flash
    flooding impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8WU29EKXNicUu-9aXdUoIIrmzM1N2O9VFctLyEeVJxS7_ZzPrEWQw_zYF2NAO46_CMjs= M1uN4vGhum8uzBZu1aUiHpw$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...JAN...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34568441 33578375 32708470 31878642 31178844=20
    31038973 31429027 32369010 33158882 33998708=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 28 08:48:20 2025
    AWUS01 KWNH 280848
    FFGMPD
    TXZ000-281300-

    Mesoscale Precipitation Discussion 0325
    NWS Weather Prediction Center College Park MD
    447 AM EDT Wed May 28 2025

    Areas affected...portions of central and south Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 280846Z - 281300Z

    Summary...Deep convection has expanded in coverage across portions
    of central and south Texas over the past couple hours, with
    several areas of 1-2 inch/hr rain rates noted with some of the
    activity. Flash flooding is possible - especially if heavier
    downpours can fall in urbanized/sensitive areas through 13Z/8a CDT.

    Discussion...While a mature MCS over portions of south Texas has
    struggled to maintain its organization this morning, newer
    convection has materialized in a cluster just northwest of San
    Antonio and along the Texas Gulf Coast near Corpus Christi. The
    environment supporting these storms is plenty moist and unstable
    (1.75 inch PW and 2000 J/kg MLCAPE, respectively), supporting deep
    convection with efficient rain rates. Weak low-level shear has
    lead to mainly outflow-dominant storms, although some organization
    has been noted with the cluster northwest of San Antonio. Mergers
    associated with this activity has enabled spots of 1.5 inch/hr
    rain rates (estimated per MRMS) to develop.

    The eastward propagation of thunderstorms, presence of steep lapse
    rates aloft, and lack of convective inhibition suggests that many
    areas across central/south Texas should experience at least an
    inch of rainfall this morning. For most areas, these rates will
    fall well shy of FFG thresholds, although a few spots near
    Austin/San Antonio and Corpus Christi will still be susceptible to
    an urban flash flood threat. This threat should exist on an
    isolated/spotty basis through at least 13Z or so - gradually
    ending from west to east.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_zVP6hF3iYFwotOqwzfxjbaM4iRIAS-qmrPXai5iArBBej1q5ky8zmqD8pIE-b7TUuc9= EWrwTWNsgohZZ7wVOulWDCE$ for graphic product...

    ATTN...WFO...BRO...CRP...EWX...FWD...HGX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31329834 30949672 29969614 28719630 27239720=20
    26279746 26349833 26949929 27749958 29179963=20
    30979922=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 28 11:47:53 2025
    AWUS01 KWNH 281147
    FFGMPD
    TXZ000-281700-

    Mesoscale Precipitation Discussion 0326
    NWS Weather Prediction Center College Park MD
    746 AM EDT Wed May 28 2025

    Areas affected...Upper Texas Coast

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 281145Z - 281700Z

    SUMMARY...Approaching complex of thunderstorms producing 1-2"/hr
    rainfall rates may produce urbanized areas of flash flooding,
    especially around the Houston metro area.

    DISCUSSION...Vigorous thunderstorm activity along the Lower Texas
    Coast is propagating northeast along a 925mb theta-e gradient that
    is oriented SW-NE just south of I-10. The mean 925-850mb wind
    field over the western Gulf is out of the SE with these winds
    intersecting the nearby surface front located north of I-10 this
    morning. This persistent SE flow will overrun the frontal boundary
    and continue to act as a trigger for additional thunderstorm
    activity. RAP mesoanalysis shows between 1,000-2,000 J/kg of
    MUCAPE while PWs are steadily on the rise thanks to a southerly
    IVT that is on the order of 300-500 kg/m/s. This allows for PWs to
    rise above 1.75" along the Upper Texas Coast this morning with
    some isolated areas approaching 2.0". RAP soundings are also
    indicating highly saturated soundings and warm cloud layers up to
    12,000ft deep in some cases.

    The storms may extend farther inland to the north of I-10 as SErly
    850mb winds accelerate. However, the concern for rainfall rates
    2"/hr is most likely along and south of I-10 where there greatest
    instability is present. 06Z HREF probabilistic guidance shows a
    bullseye of 30-50% values for 3-hr QPF > 3-hr FFGs near the
    Houston metro late morning into early afternoon. As much as 1-3"
    of rainfall is anticipated with localized amounts as high as 4"
    possible within the highlighted threat region. These rates are
    also coming around the morning rush hour within a densely
    populated area. Flash flooding is possible this morning,
    particularly in the more urbanized communities and poor drainage
    areas of Southeast Texas.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5NRw0nW4xsPrE06Kvpf6pVD_kLiLeTds8DJWFRAAR6gjSlmBFVAQrEWL-xdtKsNQ91xn= XZ1k4p-mUqqny4JXeuLgK08$ for graphic product...

    ATTN...WFO...CRP...HGX...LCH...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30589540 30569445 30319400 29709393 29209433=20
    28639528 28369595 28589633 28949649 29469649=20
    29829654 30319632=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed May 28 18:28:14 2025
    AWUS01 KWNH 281827
    FFGMPD
    MSZ000-LAZ000-TXZ000-290025-

    Mesoscale Precipitation Discussion 0327
    NWS Weather Prediction Center College Park MD
    226 PM EDT Wed May 28 2025

    Areas affected...Upper TX Coast...Southern LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 281825Z - 290025Z

    SUMMARY...Locally heavy showers and thunderstorms with high
    rainfall rates will pose an isolated concern for flash flooding
    this afternoon. This will generally be more of an urban flash
    flood threat.

    DISCUSSION...GOES-E IR satellite imagery along with dual-pol radar
    shows a long-lived cold-topped MCS advancing across the upper TX
    coast and the adjacent offshore Gulf waters which will be moving
    into southwest LA over the next 1 to 2 hours. There is a rather
    well-defined MCV associated with this convection and this energy
    is expected to move inland across southern LA going into the
    evening hours.

    The airmass across southern LA has been destabilizing with MLCAPE
    values of 2090 to 3000 J/kg in place, and it is also very moist
    with PWs as high as 1.75 to 2 inches. There is some modest shear
    with about 30 kts of effective bulk shear, and the combination of
    this with the moderate to strongly unstable boundary layer will
    favor a likelihood of the aforementioned MCS at least maintaining
    itself as it begins to edge into southwest LA. However, with some
    additional heating via solar insolation over the next couple of
    hours, and with proximity of a seabreeze trough/convergence axis
    downstream of it across southern LA, there may actually be some
    further development and expansion of convective cells off to the
    east that may be rather slow-moving.

    HRRR and RRFS hires CAM solutions suggest a threat for rainfall
    rates to reach locally as high as 2 inches/hour, with some spotty
    storm totals by this evening that could reach up to 3 to 4+
    inches. This will tend to be favored more by some of the
    slow-moving pulse and multi-cell convection ahead of the MCS
    activity, but some of the totals in the northern comma-head region
    of the MCS may also potentially reach these levels.

    This suggests generally an isolated concern for flash flooding
    with much of this threat generally over the more urbanized
    locations inclusive of the I-10 corridor of southern LA.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!88-fOp4ULRWyC6-x0sSj90pcaO0ot9A3bzdnhsV5g9cxhzXITNmaOVig1-_HPsqlVy_4= BgUvbd8yNIsJEx5IPj0UMWs$ for graphic product...

    ATTN...WFO...LCH...LIX...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 30769212 30749081 30568966 30038962 29739047=20
    29619146 29489233 29729307 29779395 30059413=20
    30469353=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu May 29 00:39:34 2025
    AWUS01 KWNH 290039
    FFGMPD
    MSZ000-LAZ000-290338-

    Mesoscale Precipitation Discussion 0328
    NWS Weather Prediction Center College Park MD
    838 PM EDT Wed May 28 2025

    Areas affected...Southeast LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 290038Z - 290338Z

    SUMMARY...Additional clusters of heavy showers and thunderstorms
    will continue to impact southeast LA going through the evening
    hours. Areas of urban flash flooding will continue to be possible
    and especially around the New Orleans metropolitan area.

    DISCUSSION...The early-evening GOES-E IR satellite imagery along
    with dual-pol radar shows areas of heavy showers and thunderstorms
    moving across southeast LA with some signs of addition
    organization taking place within the last 30 to 45 minutes.
    Cooling cloud tops are noted with new clusters of convection, and
    this activity is generally moving off to the northeast in the
    direction of New Orleans and adjacent suburbia.

    All of this convection is connected to the persistence of a
    long-lived MCS which is less organized than earlier in the day,
    but continues to advance downstream while interacting with a very
    moist and moderately unstable airmass pooled across the central
    Gulf Coast region. The latest RAP analysis shows a well-defined
    instability gradient aligned in a southwest to northeast fashion
    across southeast LA, with MLCAPE values as high as 1500 to 2000
    J/kg. PWs are quite high and on the order of 1.8 to 2 inches, and
    this coupled with the instability will support rainfall rates of
    as much as 1.5 to 2.5 inches/hour with the stronger convective
    cores.

    Given the convective trends, this activity is likely to again
    impact areas around New Orleans, and some additional rainfall
    amounts here may locally reach 3 to 4 inches given some localized
    cell-training concerns before the activity advances off to the
    east later this evening. Additional concerns for urban flash
    flooding will exist over the next few hours as a result.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6XtgalyalxJUoHNWANvFIqkg5-qjbVP0K0E88QxZefnM1g09PLMs3U5SnqdHMX3VkvEQ= _MBJB-seXK9GKg7Wa6jl-Pg$ for graphic product...

    ATTN...WFO...LCH...LIX...

    ATTN...RFC...ORN...NWC...

    LAT...LON 30349025 30338956 29848948 29408997 29229072=20
    29619122 30019098=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu May 29 00:57:23 2025
    AWUS01 KWNH 290056
    FFGMPD
    TXZ000-OKZ000-KSZ000-COZ000-NMZ000-290555-

    Mesoscale Precipitation Discussion 0329
    NWS Weather Prediction Center College Park MD
    855 PM EDT Wed May 28 2025

    Areas affected...Far Southeast CO...Southwest KS...TX/OK
    Panhandles and Northwest OK

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 290055Z - 290555Z

    SUMMARY...Expanding clusters of showers and thunderstorms will
    continue to organize and grow upscale this evening. A combination
    of cell-mergers and some localized cell-training may lead to
    isolated areas of flash flooding.

    DISCUSSION...GOES-E IR satellite imagery shows expanding clusters
    of cold-topped convection across the central High Plains, with
    multiple supercells and some linear-mode activity impacting
    southeast CO, southwest KS and down into the TX/OK Panhandles. The
    convection is organizing in a moderately unstable and sheared
    environment with MLCAPE values of 1000 to 2000 J/kg and effective
    bulk shear values of as much as 40 to 50+ kts.

    Digging shortwave energy across the central High Plains is
    providing divergent flow aloft with DPVA in place, and this
    coupled with favorable thermodynamics and a nocturnally enhanced
    low-level jet overrunning a warm front should favor additional
    expansion and organization of convective clusters over the next
    few hours.

    The latest experimental WoFS along with multiple 18Z HREF members
    suggest cell-merger activity gradually favoring a more progressive
    MCS across the region with a southwest to northeast orientation by
    late this evening. This MCS evolution, which will involve a
    continued concern for some supercell activity, will drop
    southeastward across southwest to south-central KS and eventually
    well down across northwest OK which will include impacts also
    still across the TX/OK Panhandles.

    Rainfall rates with the stronger supercells may reach 1.5 to 2
    inches/hour, with some storm totals locally of 2 to 4 inches where
    a combination of any cell-mergers or brief cell-training occurs.
    Aside from the ongoing severe weather hazards, there may be a
    sufficient rainfall component to drive an isolated threat for
    flash flooding over the next several hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-hLE2nALBPq_k75a7PQkrSTGlnvY3J-WVgNMyqcZNdrtRJza5dl7_i_QeP7bai5bMCC6= fDeVPRWy7ZM4KgnGyLW8KTc$ for graphic product...

    ATTN...WFO...ABQ...AMA...DDC...ICT...OUN...PUB...

    ATTN...RFC...TUA...NWC...

    LAT...LON 38269894 37599771 36119800 35529937 35810157=20
    36730327 37610361 37910202 37860098=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu May 29 07:28:15 2025
    AWUS01 KWNH 290726
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-291150-

    Mesoscale Precipitation Discussion 0330
    NWS Weather Prediction Center College Park MD
    324 AM EDT Thu May 29 2025

    Areas affected...central to east-central Gulf Coast

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 290723Z - 291150Z

    SUMMARY...Localized flash flooding will be possible along coastal
    portions of MS/AL and the FL Panhandle over the next 3-4 hours.
    Efficient rainfall production from training of relatively small
    heavy rain cores may result in hourly rainfall of 2 to 3+ inches.

    DISCUSSION...07Z radar imagery across southeastern LA into MS, AL
    and the FL Panhandle showed scattered thunderstorms with embedded
    remnant MCVs and/or mid-level vorticity maxima. A vorticity max
    was located just north of Terrebonne Bay with thunderstorms
    expanding downstream near the southeastern LA coast and south of
    Mobile Bay in the vicinity of composite outflow.

    Radar imagery and surface observations indicated one area of
    convectively induced outflow aligned from SW to NE from the
    western FL Panhandle into the northern Gulf, with SPC mesoanalysis
    data showing 1000-2000 J/kg MLCAPE offshore (south of the
    composite outflow) and CIN northwest of the CAPE gradient. As the
    mid-level vorticity max advances northeastward over the next 3-6
    hours, advection of low level moisture is forecast by the RAP to
    erode CIN for locations near the coast from southeastern LA into
    the western FL Panhandle.

    Mean cell motions following the deeper-layer mean wind may support
    localized training into the western FL Panhandle as outflow slowly
    advances eastward over the next couple of hours. In addition, CIN
    eroding back to the west over coastal MS/AL may result in the
    development of thunderstorms by 12Z with some minor strengthening
    of 850 mb winds from the south, increasing the potential for short
    term training. Overlap of these potential heavy rainfall cores
    with urban areas or other locations with poor draining could
    result in localized flash flooding.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-onIruAfz0kgXWF8ijzMkaFARaWx5CvNBZZTMB6RRdhNPFGvFlPa1E_RhTYXf0DvV2QZ= 3wmPgftQxLpbu4y1GsAc9ms$ for graphic product...

    ATTN...WFO...LIX...MOB...TAE...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 30898675 30748582 30308521 29758554 29948658=20
    29468803 28718932 29139002 30348928 30848799=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu May 29 19:31:46 2025
    AWUS01 KWNH 291931
    FFGMPD
    NCZ000-SCZ000-GAZ000-300130-

    Mesoscale Precipitation Discussion 0331
    NWS Weather Prediction Center College Park MD
    330 PM EDT Thu May 29 2025

    Areas affected...Portions of the Southeast Coastal Plain

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 291930Z - 300130Z

    SUMMARY...Heavy showers and thunderstorms will continue to expand
    in coverage over the next few hours. High rainfall rates and
    locally slow cell-motions will favor an isolated flash flood
    threat which will generally be more urbanized in nature.

    DISCUSSION...A low-amplitude shortwave trough traversing the
    Southeast U.S. will be lifting up across the Southeast coastal
    plain going into the evening hours, and this energy interacting
    with a moist and unstable airmass pooled across the region will
    favor additional expansion of heavy showers and thunderstorms.

    MLCAPE values are as high as 1500 to 2500 J/kg with PWs of 1.75+
    inches and this coupled with a moderate level of effective bulk
    shear (30 to 35+ kts) will favor the overall convective footprint,
    and with rainfall rates that may reach as high as 1 to 2+
    inches/hour as convection generally grows upscale over the next
    few hours.

    These heavier rainfall rates are supported by the 12Z HREF
    guidance, and the latest CAMS also support a general concern for
    there to be some cell-merger activity and localized cell-training.
    Some of this will be fostered by proximity of some seabreeze
    convergence focusing convection ahead of the main arrival of the
    upstream shortwave energy, but the cell-motions will also be
    locally rather slow-moving.

    Rainfall totals by mid-evening may reach as high as 3 to 5 inches
    where the heavier and more focused areas of convection set up.
    This coupled with the high rainfall rates in general should tend
    to favor at least an isolated threat for flash flooding, which
    will primarily be a concern for the more urbanized locations. This
    may include the Columbia, SC metropolitan area in particular.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8REZgccIdKU1rVD2D4II5CRLOpHUXMapNXnGebDxim2QEr9TMRC8GXENGenWg1UCWLMw= rE_lvx7oKUbvPhIPrRRvly4$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...ILM...MHX...RAH...

    ATTN...RFC...ALR...NWC...

    LAT...LON 35997883 35797726 34887709 33897852 33267959=20
    32618107 33098227 34108234 35248088=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu May 29 21:58:13 2025
    AWUS01 KWNH 292156
    FFGMPD
    TXZ000-NMZ000-300355-

    Mesoscale Precipitation Discussion 0332
    NWS Weather Prediction Center College Park MD
    555 PM EDT Thu May 29 2025

    Areas affected...Southeast NM...Western and Central TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 292155Z - 300355Z

    SUMMARY...Clusters of showers and thunderstorms over southeast NM
    and southwest TX will continue to generally expand in coverage
    over the next few hours. A gradual increase in heavy rainfall
    rates is expected as this activity organizes further this evening,
    and this may result in isolated to scattered areas of flash
    flooding.

    DISCUSSION...The late-afternoon GOES-E visible satellite imagery
    shows expanding convective clusters over southeast NM and
    southwest TX as strong diurnal heating and corresponding boundary
    layer instability work in tandem with relatively moist low-level
    southeast flow and localized orographic ascent. All of this is
    occurring south of a cold front dropping southward down across the
    southern High Plains which will be an additional catalyst for
    convective development over the next several hours.

    MLCAPE values over much of central and western TX in particular
    are quite elevated with values of 2000 to 3000+ J/kg, although the
    latest RAP analysis does still show some pockets of MLCIN
    extending north/south from the Midland vicinity down through Fort
    Stockton. Any remaining CIN should gradually erode over the next
    couple of hours as additional surface heating occurs, and this
    will help set the stage for upstream convection consolidating over
    southeast NM and southwest TX to then advance off to the east and
    grow upscale into the very unstable/moist airmass pooled
    downstream.

    Aside from favorable thermodynamics, strong shear parameters are
    yielding a number of supercell thunderstorms already, and this
    threat will continue in the near-term as the activity consolidates
    into a least a broken MCS by this evening. Increasing low-level
    convergence along the front and also some nearby right-entrance
    region upper jet support will also be key players in driving the
    convective threat well through the evening hours for areas farther
    east across western and central TX.

    REFS/HREF suites of guidance show rather strong support for the
    stronger storms to produce rainfall rates well into the 1 to 2
    inch/hour range. A combination of slow cell-motions and
    cell-merger activity in the early stages of this evening's MCS
    development will support some rainfall totals reaching as high as
    3 to 4 inches. Both the REFS and HREF suites show elevated 3-hour
    FFG exceedance probabilities over portions of central and western
    TX this evening, and thus given the setup, isolated to scattered
    areas of flash flooding will be possible.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5si01hQNLYso09PYyybNDkMQUC5-N07Hx6vv7dCK0q22RE8_8YRsAdKgvOOJojIZqJpv= _YVjbvBsuNH30x8CwGF0IC8$ for graphic product...

    ATTN...WFO...ABQ...FWD...LUB...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 33620275 33440119 32859949 31929899 31149913=20
    30639985 30650167 31080354 31690432 32660445=20
    33330383=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu May 29 23:28:08 2025
    AWUS01 KWNH 292327
    FFGMPD
    NCZ000-300225-

    Mesoscale Precipitation Discussion 0333
    NWS Weather Prediction Center College Park MD
    725 PM EDT Thu May 29 2025

    Areas affected...Central NC

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 292325Z - 300225Z

    SUMMARY...Heavy showers and thunderstorms across central NC will
    continue through the mid to late-evening hours. Areas of flash
    flooding are likely and especially around the Raleigh-Durham
    metropolitan area and adjacent suburbs over the next couple of
    hours.

    DISCUSSION...Radar imagery shows showers and thunderstorms with
    heavy rainfall rates of 1.5 to 2.0 inches/hour impacting central
    NC as a shortwave impulse lifting up across the Southeast U.S.
    coastal plain interacts with a moist and unstable airmass pooled
    across the region.

    MUCAPE values are still locally on the order of 1000+ J/kg, and
    there are multiple small-scale outflow boundaries interacting with
    each other that are resulting in pockets of enhanced low-level
    convergence for additional convective development. The airmass is
    moist with PWs of near 1.5 inches, and this coupled with the
    remaining instability should still favor locally enhanced rainfall
    rates over the next couple of hours.

    There is also proximity of a warm front across central NC along
    with some modest right-entrance region upper-level jet dynamics
    that are helping to further facilitate the sustenance of
    convection at least in the near-term. Given the high rainfall
    rates and some cell-merger activity, expect some additional spotty
    rainfall amounts of 2 to 4 inches before sufficient boundary layer stabilization occurs for the activity to weaken later this evening.

    Areas of urban flash flooding are locally already occurring and
    will continue through the mid to late-evening hours givenj the
    high rainfall rates. This will include a near-term threat to the
    Raleigh-Durham metropolitan area which currently has heavy shower
    and thunderstorm activity situated to the west and south of the
    city.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-FX86hDq75fB1NIYMvO7VBoHoRkweFmjSRonOK_WAChZDyksQDdiWdFflkW2v2NDK-gY= zXq2F3Zb9MgB6e1RUhOzwS0$ for graphic product...

    ATTN...WFO...GSP...RAH...RNK...

    ATTN...RFC...ALR...NWC...

    LAT...LON 36507820 36287765 35847759 35507790 35327857=20
    35338008 35838044 36347951=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 30 04:35:07 2025
    AWUS01 KWNH 300434
    FFGMPD
    TXZ000-300900-

    Mesoscale Precipitation Discussion 0334
    NWS Weather Prediction Center College Park MD
    1234 AM EDT Fri May 30 2025

    Areas affected...west-central TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 300433Z - 300900Z

    SUMMARY...Localized to scattered areas of flash flooding will
    remain possible over the next 3-4 hours across west-central TX.
    Rainfall rates of 1 to 2 in/hr will be likely with spotty rates of
    2 to 3+ possible through 08Z.

    DISCUSSION...04Z radar imagery showed an elongated MCS over
    west-central TX, extending from south of FST to near DYS and COM.
    Southeasterly low level flow of 15-25 kt was located from southern
    TX into the convective complex with the stronger winds located
    closer to the Rio Grande and West TX, dropping off in magnitude
    with eastward extent. The source region of the southeasterly winds
    contained 1500-2500 J/kg MLCAPE and 1.3 to 1.8 inches of PWAT.
    Sufficient shear for organized cells was also present along and
    ahead of the MCS via 04Z SPC mesoanalysis data. While a cold front
    was dropping southward across the region, a cold pool also appears
    to be getting better organized with numerous outflow boundaries
    preceding the convective axis, with the MCS following a general
    movement toward the SE, into the moist and unstable inflow.

    This general movement is expected to continue over the next few
    hours with embedded peak hourly rainfall of 1-2 inches, although
    occasional embedded higher rates will be possible where brief west
    to east training develops. Training will be most likely along the
    southwestern flank of the complex where line orientation is more
    favored to align with the mean steering flow. The southwestern
    edge of the complex, located near the stronger low level flow, may
    also favor thunderstorm development just ahead of the advancing
    line due to the presence of the Hill Country terrain and a
    relative max in uninhibited instability as seen on SPC
    mesoanalysis data over the middle/lower Rio Grande Valley.
    Localized hourly rainfall of 2 to 3+ inches cannot be ruled out
    along with 2-4 inches of additional rainfall through 10 or 11Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9_LpUogQ6Na1GcCFPqH-Dhg9munRKPS1caZXVrmsRNKw3kWSPq4O3a-gnM-aWAy0nVp1= PPk98tAFMXArJPTzGsynfwg$ for graphic product...

    ATTN...WFO...EWX...FWD...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31979894 31939840 31599793 31199776 30469818=20
    29299908 28990028 29480148 29890315 30550324=20
    30790266 30850174 31030123 31470050 31700001=20
    31939945=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 30 09:25:36 2025
    AWUS01 KWNH 300925
    FFGMPD
    TXZ000-301300-

    Mesoscale Precipitation Discussion 0335
    NWS Weather Prediction Center College Park MD
    524 AM EDT Fri May 30 2025

    Areas affected...south-central TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 300923Z - 301300Z

    SUMMARY...A localized flash flood threat will continue for
    portions of south-central TX until about 13Z with peak hourly
    rainfall of 2 to just over 3 inches possible.

    DISCUSSION...09Z radar imagery over central to south-central TX
    showed a southward advancing convective line in the process of
    overtaking nearly a stationary cell over southeastern Kinney
    County where MRMS has estimated 3+ inches of rain in an hour. The
    cell formed on a surface convergence axis marking the leading edge
    of higher surface moisture and within a relative max in MLCAPE
    with SPC mesoanalysis data showing 3000 to 3500 J/kg centered over
    Kinney and Maverick counties. In the upper levels, flow was noted
    to be diffluent on water vapor imagery, likely contributing to
    lift over the region.

    The convective line is likely to continue advancing south over the
    next 2-4 hours, with embedded pockets of intense, efficient
    rainfall due to the combination of low level moisture from the
    Gulf and tropical moisture in the mid-upper levels emanating from
    Tropical Storm Alvin in the eastern Pacific. While the main low
    level convergence axis is being overtaken by the convective
    line...which should remain progressive...subtle areas of wind
    convergence were noted in surface observations between the Edwards
    Plateau and the lower/middle TX coast that could initiate new
    thunderstorms in advance of the convective line due to the
    unstable environment, which could allow for additional, but
    localized spots of 2 to 3+ in/hr rainfall given slow cell
    movement. There is also non-zero potential for west-east short
    term training falling atop scattered portions of the state that
    have received 200 to 400 percent of normal rainfall over the past
    week, which may increase the potential for runoff. Overall, the
    flash flood threat appears limited in scope, but a localized
    concern will linger for another few hours over portions of
    south-central TX.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5C2FzRdXN7Ca3wAGL9-G9ZhYwqcMttFKWCVJrQvabXsZTqVaifSkOD-7CWqUD-Rxh1LO= Uv6-t9sYDeDD_9SDVmrWfXQ$ for graphic product...

    ATTN...WFO...CRP...EWX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 29689729 28889688 28269864 28089972 28260030=20
    28830076 29190085 29380062 29499972=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 30 16:11:58 2025
    AWUS01 KWNH 301611
    FFGMPD
    PAZ000-MDZ000-WVZ000-OHZ000-302130-

    Mesoscale Precipitation Discussion 0336
    NWS Weather Prediction Center College Park MD
    1211 PM EDT Fri May 30 2025

    Areas affected...Northern WV...Western MD...Adj Southwest PA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 301610Z - 302130Z

    SUMMARY...Slow moving, repeating showers along stationary front
    downstream of strong/deep cyclone moving into more sensitive
    terrain/soil conditions coinciding with increasingly unstable
    environment. Rates may increase to 1.5"/hr and localized totals
    up to 2" are possible maintaining flash flooding potential through
    evening.

    DISCUSSION...GOES-W shows a very compact/symmetric and anomalously
    deep (2-3 std. dev from normal) tracking through the central Ohio
    River Valley, shifting northward. This is supporting a similarly
    deep 1002mb downstream low near southern OH, lifting northeast
    along a well defined and sharpening surface frontal zone. This
    front extends northeast toward Morgantown before angling along the
    Mason-Dixon line. Moist and weakly unstable environment has been
    advected on fairly strong upslope component into the central WV
    Appalachian Mtns and with strong cyclonic curvature from surface
    to 500mb, resulting in very strong moisture flux convergence and
    this is over-coming some mid to upper level drying above 700mb in
    the strong dry slot across KY/NE TN noted in CIRA LPW, limiting
    overall PWat totals to 1.25-1.4". Fairly deep warm cloud layer
    with the strong cyclonic curvature is resulting in a fairly
    efficient rainfall production with 1"/hr occurring along the
    downstream deformation/convergence zone; the breadth is along long
    enough for duration to reach about 60-90 minutes resulting in
    observations of 1.5-1.75"/3hr becoming more common.=20

    These rates/totals are at the threshold of the typically lower FFG
    values over the area, but NASA SPoRT LIS soil products suggest
    even greater saturation further upslope into central WV and MD
    with 0-40cm soil moisture values in the 70% which is clearly well
    above normal (85-90th percentiles). Given this scattered/focused
    incidents of flash flooding are possible near the cores of
    embedded convective elements along and downstream of the deep
    cyclone. The coverage/broaden of updraft cores should expand
    over the next 3-4hrs into NE WV/W MD and perhaps SW PA. GOES-E
    Visible loop shows breaks in cirrus canopy and have been clear
    into W MD for most of the morning, slowly increasing instability,
    along the northern edge of the dry slot within the TPW gradient,
    instability will increase to 750-1000 J/kg toward 18-20z. As
    cells deepen/broaden, localized totals up to 2" in 1-2hrs become
    possible.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-oTJ6DIbwbu_PNfIY0tGtfGAowEvecYGnsX3oIoCniYw6qjiLUMq2kJj9yBlnnjHvZAc= phL-wEoauNQZeV7IIlhPYNs$ for graphic product...

    ATTN...WFO...CTP...LWX...PBZ...RLX...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 40057864 39737823 39157854 38827917 38338031=20
    37958200 38348251 39088221 39568127 39888052=20
    39997956=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 30 21:46:12 2025
    AWUS01 KWNH 302144
    FFGMPD
    NYZ000-NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-DCZ000-WVZ000-OHZ000-310343-

    Mesoscale Precipitation Discussion 0337
    NWS Weather Prediction Center College Park MD
    543 PM EDT Fri May 30 2025

    Areas affected...Portions of the Central Appalachians and the
    Mid-Atlantic

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 302143Z - 310343Z

    SUMMARY...Heavy rainfall will become more concentrated heading
    through the evening hours across portions of the central
    Appalachians while also spreading across the interior of the
    northern Mid-Atlantic. Some embedded thunderstorm activity will
    favor enhanced rainfall rates, and scattered areas of flash
    flooding will become likely this evening.

    DISCUSSION...The latest GOES-E IR/WV suite shows a very strong
    shortwave trough amplifying across the OH Valley and into the
    central Appalachians, with a well-defined comma-head/deformation
    zone currently seen crossing through southeast OH, northern WV and
    southwest PA.

    This is driving a deepening wave of low pressure toward the
    Mid-Atlantic states, with recent surface observations showing a
    strengthening low center moving east-northeast across far northern
    VA to the east of KOKV and northwest of KIAD. A quasi-stationary
    front is seen oriented east of this low center across northern
    VA/southern MD and through the Delmarva region. The airmass ahead
    of this strong shortwave is modestly unstable, with warm-sector
    MLCAPE values of 500 to 1000 J/kg, but there is nose of elevated
    instability that is wrapping north of the front and into areas of
    eastern WV through northern MD and far southern PA.

    Over the next few hours, this elevated axis of instability will
    combine with strong DPVA, strengthening isentropic ascent, and a
    related corridor of enhanced frontogenetical forcing for an axis
    of heavy rainfall to move east out of the central Appalachians and
    across the northern Mid-Atlantic. Already radar and satellite
    imagery shows an axis of heavy rainfall with embedded strong
    thunderstorms impacting northern WV and southwest PA, with this
    activity moving east toward the MD/WV Panhandles.

    Meanwhile, downstream areas near the stationary front and into the
    warm sector will be seeing convection expand in coverage as better
    instability and strong shear profiles combine with backing
    low-level flow/surface convergence for an organized convective
    threat.

    The latest hires guidance including the 18Z HREF suite, the HRRR,
    and the experimental WoFS runs favors northern WV/southern PA and
    northern MD with the heaviest rainfall this evening with a focus
    on areas near and to the north of the surface low track. Rainfall
    amounts across this region of 3 to 4+ inches will be possible.

    However, areas of central and northern VA and into the Delmarva
    and eventually southern NJ will see bands of convection capable of
    producing rainfall rates of 1 to 2 inches/hour, with some spotty 2
    to 3+ inch rainfall totals possible here.

    Scattered areas of flash flooding are likely this evening, and
    this will include a threat to a few metropolitan areas including
    Washington, D.C., Baltimore, MD, Harrisburg, PA and Philadelphia,
    PA.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5C0lO_jdg_3w1ZKljP2pV-cdevq6SnWxhCvmGetT1PpsMfljS_8u3Vm4vzHbyou0kX63= d4tmPAqj5p3M0oErw055jYA$ for graphic product...

    ATTN...WFO...AKQ...BGM...CTP...LWX...OKX...PBZ...PHI...RLX...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 41187479 40607411 39567443 38427606 38137690=20
    38077809 38257902 38997961 39258052 39618097=20
    40208093 40677977 40717817 40867657=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 31 04:01:07 2025
    AWUS01 KWNH 310401
    FFGMPD
    MAZ000-CTZ000-NYZ000-NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-WVZ000-310930-

    Mesoscale Precipitation Discussion 0338
    NWS Weather Prediction Center College Park MD
    1200 AM EDT Sat May 31 2025

    Areas affected...far northern Mid-Atlantic into southern NY and
    southwestern New England

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 310357Z - 310930Z

    SUMMARY...Areas of heavy rainfall are expected to impact the far
    northern Mid-Atlantic region into southern NY and southwestern New
    England through 09Z, likely resulting in scattered areas of flash
    flooding. Embedded peak hourly rainfall of 1 to 2 inches is
    expected along with localized totals of 2 to 3 inches (perhaps up
    to 4 inches) through 09 to 10Z.

    DISCUSSION...0330Z radar imagery showed the heaviest rainfall
    occurring over southeastern PA/northern DE and southwestern NJ,
    near an apparent MCV located just northwest of ILG. MLCAPE from
    the 03Z SPC mesoanalysis was 500-1000 J/kg and PWs ranged from 1.2
    to 1.5 inches, with MRMS indicating hourly rainfall of 1-2 inches.
    Back to the west, a well-defined mid-level shortwave and comma
    head/deformation axis was located over the WV/MD panhandles.

    Ongoing heavy rain in the vicinity of the Philadelphia metro is
    expected to continue tracking northward over the next few hours
    into northern NJ and southern Upstate NY, following the mesoscale
    circulation and southerly flow ahead of the potent
    shortwave/closed low to the immediate west. Embedded hourly
    rainfall of 1-2 inches will follow the swath of heavy rain with
    embedded thunderstorms.

    Back to the west, there is good short term model agreement with
    the track of the shortwave into NJ through 10Z. A well-defined
    comma head/deformation axis will swing across the eastern PA/MD
    border containing another round of locally heavy rainfall. RAP
    forecasts indicate the potential for this axis to overlap with a
    small region of weak CAPE, perhaps as high as 500-1000 J/kg. Peak
    hourly rainfall with this second round of heavy rain could be near
    1 inch.

    Total rainfall through 09 or 10Z of 1 to 3 inches is likely with
    perhaps embedded totals near 4 inches. These rains will be falling
    atop portions of the densely populated urban corridor of I-95 and
    into the more sensitive terrain to the west of I-95. Scattered
    areas of flash flooding are considered likely.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8KHagQcfLY1syRefIcxRQW2H6qK_WPCmz7M54xCIF9k-Jpz13YRIHjF7cav4KNu_1zM2= 5EfarAk86QFt9Rty2SH1KSI$ for graphic product...

    ATTN...WFO...ALY...BGM...CTP...LWX...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 42447343 41887302 41297316 40557391 39887478=20
    39617602 39457686 39277774 39557852 40187849=20
    40617793 41277623 41747545 42317440=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 31 09:00:39 2025
    AWUS01 KWNH 310900
    FFGMPD
    MAZ000-NHZ000-VTZ000-CTZ000-NYZ000-NJZ000-PAZ000-311400-

    Mesoscale Precipitation Discussion 0339
    NWS Weather Prediction Center College Park MD
    500 AM EDT Sat May 31 2025

    Areas affected...northern NJ/southern NY into central New England

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 310858Z - 311400Z

    SUMMARY...The potential for localized flash flooding from an
    additional 1-3 inches of rain will exist from northern NJ/southern
    NY into central New England through 14Z. Peak hourly rainfall near
    1 inch will be possible.

    DISCUSSION...08Z surface observations showed an unusually strong
    surface low for late May of 987 mb located between Somerset and
    Morristown, NJ, tracking toward the northeast. Radar imagery and
    surface observations showed areas of heavy rain over northeastern
    PA, northern NJ and southern Upstate NY. Within this region, gauge
    reported hourly rainfall has generally peaked in the 0.5 to 1.0
    inch range, though it has been as high as 1.5 inches over western
    Morris County, NJ ending 08Z.

    Northern NJ had the highest area MLCAPE via 08Z SPC mesoanalysis
    data (up to 500 J/kg), wrapping in from the western Atlantic just
    north of the surface low. This region of northern NJ overlapped
    with low level convergence to the northwest of the surface to 850
    mb low and locally strong upper level divergence/diffluence within
    the left-exit region of an upper jet streak off of the
    Mid-Atlantic coast. Elsewhere, instability was limited which was
    limiting rainfall rates despite the robust forcing for ascent.

    Through ~14Z, the surface to 850 mb low will track into western CT
    via recent RAP forecasts, which will send the comma
    head/deformation axis northwest of the low into the lower Hudson
    Valley and western/central New England including the Berkshires
    and southern Green Mountains. While instability is forecast to
    remain rather low across this region and total PW is expected to
    lower a bit from present values, the similar SW to NE track and
    orientation of the low level precipitation axis may allow for
    additional rainfall totals of 1 to 2 inches (locally near 3
    inches) through 14Z. However, this area of the Northeast has not
    been as wet compared to locations farther south, so any instances
    of flash flooding should be isolated in nature.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_5xn1N7D_RhtPWVLqMlLFFbCFStl7IShW7aAxF5ESSVuyHtL92ZYxD8mOQvjoZGBfbex= s86cDFa9pvKwwRywtjPZlvM$ for graphic product...

    ATTN...WFO...ALY...BGM...BOX...BTV...GYX...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 44077228 43947186 43437159 42767165 42187179=20
    41717239 41337314 40957378 40637422 40297460=20
    40527509 41447500 42227443 43097337 43747283=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 31 14:00:13 2025
    AWUS01 KWNH 311400
    FFGMPD
    MEZ000-MAZ000-NHZ000-VTZ000-CTZ000-NYZ000-311905-

    Mesoscale Precipitation Discussion 0340
    NWS Weather Prediction Center College Park MD
    959 AM EDT Sat May 31 2025

    Areas affected...Hudson Valley into northern New England

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 311358Z - 311905Z

    SUMMARY...Risk for localized rainfall of two inches in three hours
    makes for a potential flash flood concern this morning for the
    Hudson Valley and southern Vermont/New Hampshire, then farther
    north through this afternoon

    DISCUSSION...983mb surface low now over western Mass is quickly
    lifting north-northeast. Bands of moderate rain are wrapping and
    pivoting around this low back over the central Hudson Valley and
    southern VT. Within this area, gauge reported hourly rainfall has
    generally peaked in the 0.5 to 0.75 inch range with upstream 3hr
    rainfall up to 2 inches in the Catskills.

    MUCAPE per the 12Z RAP is around 250 J/kg through this zone,
    rising to 500 J/kg east of the low in the warmer sector. Low level
    convergence to the northwest of the surface low and locally strong
    upper level divergence/diffluence within the left-exit region of
    an upper jet streak off of the Mid-Atlantic coast is aiding
    rainfall rates as well as topographic lift.

    Through ~20Z, the surface low will track through northern New
    England and produce a rainfall axis of 1 to 3 inches. However,
    this area of New England has not been as wet compared to locations
    farther south, so any instances of flash flooding should be
    isolated in nature.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-uI9hGt8gkv54chh2yiQho8xa3MbOqNx7bOAYJ8fxWcPWfKPcwbd5vK4qVkkB8txK5Mz= uWoPVNmpqFBft-zT1uUI3zc$ for graphic product...

    ATTN...WFO...ALY...BOX...BTV...GYX...

    ATTN...RFC...TAR...NWC...

    LAT...LON 45287145 45147089 43167114 42587244 41937347=20
    42407432 43747349 45057211=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 1 22:41:34 2025
    AWUS01 KWNH 012241
    FFGMPD
    NMZ000-AZZ000-CAZ000-020330-

    Mesoscale Precipitation Discussion 0341
    NWS Weather Prediction Center College Park MD
    640 PM EDT Sun Jun 01 2025

    Areas affected...Southern Arizona, far Southwest New Mexico

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 012240Z - 020330Z

    Summary...Showers and thunderstorms will expand in coverage and
    lift across southern Arizona/extreme southwest New Mexico this
    evening. Rainfall rates of 0.25" to 0.5" per hour are expected.
    Through repeated rounds, this could produce more than 1 inch of
    rain in some areas, leading to instances of flash flooding.

    Discussion...The GOES-E day-cloud phase RGB this afternoon shows
    an expansion of intensifying updrafts across the Sonoran Desert,
    lifting slowly into southern Arizona. This is collocated with
    expanding LightningCast probabilities, suggesting the environment
    is beginning to become more thermodynamically favorable for heavy
    rainfall. The SPC RAP analysis indicates that PWs have increased
    to 1.3 to 1.5 inches, well above the daily max at Yuma, AZ, and
    above the 99th percentile in the CIRA ALPW product, coincident
    with bubbles of SBCAPE within clearings that have reached 500-1500
    J/kg. Into this environment, forcing for ascent is increasing
    downstream of a potent upper low noted over the northern Baja
    Peninsula, with a mid-level convergence axis arcing to the NW near
    Tucson and Phoenix helping to focus development. The overlap of
    this impressive forcing into the robust thermodynamics is leading
    to rainfall rates that have been measured by MRMS as much as 0.75
    inhes just south of the international border.

    During the next few hours, the CAMs, including the RRFS, HRRR, 3km
    NAM, and UA WRF, all agree in an expansion northward of higher
    reflectivity, with additional development recurring over Mexico.
    This evolution is supported as forcing for ascent begins to
    increase through downstream divergence/height falls as the upper
    low pivots northeast from the Baja Peninsula. At the same time,
    the low-level southerly flow, while generally weak, will help
    advect greater moisture and stronger CAPE northward, additionally
    supporting the expansion and intensification of showers and
    thunderstorms. Any cells that become most intense could have rain
    rates above 1"/hr (10-20% chance) as shown by the HREF and REFS
    probabilities, with 15-min rainfall of 0.25 to 0.5 inches possible
    (HRRR). Although storm motions will remain generally progressive
    on 15-20 kts 0-6km mean winds, some organization and training is
    possible, especially along the convergence boundary, leading to
    total rainfall that may reach 1 to 1.5 inches in some areas.

    Much of AZ and NM have been extremely dry the past 30 days, which
    is manifesting as 0-10cm soil moisture from NASA SPoRT that is
    below the 5th percentile. However, this can actually enhance
    runoff initially within any more intense rainfall rates, so the
    risk for flash flooding is gradually beginning to increase. While
    the more intense convection is expected tonight and overnight,
    which will likely necessitate additional MPDs, during the next few
    hours at least an isolated risk will exist atop more sensitive
    terrain features, burn scars, and urban areas.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5-pFmvoAkHP6Z9hP003DeteToCi5zQCzxnBovjVekDrPpIrOt_5QKRCNsdp8d3JbdZWs= Sgiljf8Vo1hatQgvtO9NIZs$ for graphic product...

    ATTN...WFO...EPZ...PSR...TWC...

    ATTN...RFC...FWR...RSA...STR...NWC...

    LAT...LON 33261376 33221299 33181197 33081051 32670894=20
    32330859 31830856 31450875 31310904 31190949=20
    31141003 31221091 31351162 31481236 32151412=20
    32551480 32781474 33171422=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 2 04:34:45 2025
    AWUS01 KWNH 020433
    FFGMPD
    NMZ000-AZZ000-020900-

    Mesoscale Precipitation Discussion 0342
    NWS Weather Prediction Center College Park MD
    1232 AM EDT Mon Jun 02 2025

    Areas affected...central to eastern AZ

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 020430Z - 020900Z

    Summary...Showers and thunderstorms are expected to expand in
    coverage and intensity across central to eastern AZ over the next
    4-5 hours. Rainfall of 0.5 to 1.0 inches in an hour or less with
    repeating and training could result in a few instances of flash
    flooding.

    Discussion...GOES West imagery at 04Z showed a closed mid to
    upper-level low over the Baja California/Sonora border, about to
    move into southwestern AZ with a secondary subtle vorticity max
    moving north out of Pima County into south-central AZ. A RAP
    estimated 70-80 kt upper level jet streak was located over the
    northern Gulf of California, just southeast of the low's center,
    with divergent and diffluent flow downstream of the upper jet
    streak across a good portion of AZ. MRMS composite reflectivity
    and infrared satellite loops over the past 3 hours have shown
    waves of more intense rain/thunderstorms moving into southeastern
    AZ from Mexico (compared to earlier in the day) along with a
    number of embedded transient mesoscale circulations contained
    within. Recent gauge reports over eastern Santa Cruz County have
    shown between 0.5 and 0.7 inches of rain in an hour. SPC
    mesoanalysis data from 04Z showed MLCAPE of 500-1000 J/kg south of
    the AZ/MX border, but quickly dropping off to less than 500 J/kg
    into south-central and southeastern AZ.

    Over the next few hours, rounds of heavy rain will likely continue
    to move into southeastern and eastern AZ following the favorable
    upper level forcing ahead of the closed low along with instability
    and anomalous precipitable water values (1.45 inches at the TUS
    00Z sounding...well above the SPC sounding page's climatological
    max). Southerly to south-southwesterly flow at 700 mb (20-30 kt)
    along with deeper layer steering flow of the same orientation will
    support repeating and training cores of heavy rain at times,
    allowing for 0.5 to 1.0 inches in an hour or perhaps as short as
    30 minutes.

    Over central to south-central AZ, as the closed low center edges
    closer, RAP forecasts show MLCAPE increasing into the 250-750 J/kg
    range given an increase in low level moisture and cooling
    mid-level temperatures. This may allow for the development of a
    few thunderstorms by 08-09Z given DPVA, capable of hourly rainfall
    near 1 inch.

    Across both central to eastern AZ, a few areas of flash flooding
    may develop given overlap with areas of sensitive terrain, remnant
    burn scars, and/or urban centers.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5EFel7LqznqhVkm4NuMyIYXyG178WNCUCf7aBI8uJi3sZOq_sWXz0sR5OaCRtZ-GSjRA= 0eo2ys1j2nvLqm4tn0DwWzs$ for graphic product...

    ATTN...WFO...EPZ...FGZ...PSR...TWC...

    ATTN...RFC...STR...NWC...

    LAT...LON 35251122 34770987 33760912 32020894 31040934=20
    31091098 31431181 32121264 33981269 35091234=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 2 08:51:41 2025
    AWUS01 KWNH 020850
    FFGMPD
    AZZ000-NVZ000-CAZ000-021400-

    Mesoscale Precipitation Discussion 0343
    NWS Weather Prediction Center College Park MD
    449 AM EDT Mon Jun 02 2025

    Areas affected...southern NV, eastern CA, northwestern AZ

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 020848Z - 021400Z

    SUMMARY...A localized flash flood threat will set up for portions
    of western AZ, southern NV and far eastern CA over the next 4-5
    hours. Slow moving cells will be capable of producing a quick 0.5
    to perhaps 2 inches of rain.

    DISCUSSION...Over the past hour, GOES West infrared satellite and
    lightning imagery showed developing widely scattered showers and
    thunderstorms over western AZ. At 0830Z, a mid-level vorticity max
    was observed on GOES West water vapor imagery over central Mohave
    County, rotating WNW around a closed low centered to the south.
    While weak, CAPE has been on the rise as the closed low and its
    cold mid-level center, advance closer to the region with 08Z SPC
    mesoanalysis data showing roughly 500 J/kg MLCAPE from eastern CA
    into western AZ with slightly higher values of MUCAPE extending
    northward into southern NV. While a good portion of the area was
    estimated to be capped, CIN is weakening and surface dewpoints
    have been on the rise (5-10 F since 00Z) with 10-20 kt of
    southerly 850 mb flow up the Colorado Valley. Given northwest AZ's
    proximity to the closed low center, 850-300 mb mean layer winds
    are only 5-10 kt, indicative of the potential for very slow cell
    motions. Over the past 6-9 hours, layered PW imagery has shown a
    notable increase in moisture in the 850-500 mb layer, aiding in
    the recent expansion of instability.

    As convective inhibition continues to erode, additional cells are
    expected to form with the vorticity max and ahead of the closed
    upper low center in and around the tri-state region. The
    environment is supportive of small scale heavy rain cores which
    could produce roughly 0.5 inches of rain in 15-30 minutes, along
    with a spotty inch or two of accumulation. Overnight WoFS has been
    trending upward with rainfall potential and the 08Z cycle showed
    40-50 percent probabilities for 1+ inches over southern NV and
    30-40 percent to the east over central Coconino County. 90th
    percentile data (reasonable worst case scenario) indicated 2.3
    inches of rain through 14Z. The expectation of a few heavy
    rainfall cores around the region could result in isolated areas
    flash flooding in low-lying or other areas of poor drainage.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_laZi_FIacw5gB4EY1ALtFs72ksvXT_t3FUXWrzMROLgHPLRRKcZ1NL1KyviEN8Ki6A7= vkqYrYJUfQ5v_MrkHqWVVR4$ for graphic product...

    ATTN...WFO...FGZ...PSR...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 36671353 36481218 36131158 35501134 34281194=20
    33771300 33761401 34041464 34501509 35291540=20
    36061532 36601463=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 2 10:25:09 2025
    AWUS01 KWNH 021025
    FFGMPD
    FLZ000-021500-

    Mesoscale Precipitation Discussion 0344
    NWS Weather Prediction Center College Park MD
    624 AM EDT Mon Jun 02 2025

    Areas affected...central west coast of FL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 021023Z - 021500Z

    Summary...Localized/urban flash flooding will be possible along
    the west coast of FL, from roughly Tampa Bay to Naples through
    about 15Z. Spotty 3 to 5+ inch totals will be possible, with much
    of that potentially falling within a 1 to 2 hour window.

    Discussion...Regional radar and infrared satellite imagery at 10Z
    showed a west-east axis of thunderstorms extending from the
    eastern Gulf through the central FL Peninsula, located out ahead
    of a mid-level shortwave approaching from the central Gulf Coast.
    This region of FL was located within a low level confluent axis
    along a stationary front that extended from just south of Cape
    Canaveral to just south of Tampa Bay. While convergent 925-850 mb
    winds were fairly weak (up to ~10 kt), the environment over the
    central Peninsula contained 1000-2000 J/kg MLCAPE, 1.5 to 1.8
    inches of PW and estimated wet bulb zero heights just over 12 kft
    (via SPC mesoanalysis and RAP data), capable of efficient rainfall
    production. Several rain gauge reports near the coast between
    Tampa Bay and Charlotte Harbor have shown rainfall rates near 1
    inch in 15 minutes with 1-2 inch totals reported as of 10Z.

    Mean westerly flow and low dewpoint depressions at the surface
    will promote occasional instances of west-east training with
    minimal outflow generation over the next few hours, until daytime
    heating begins to alter the boundary layer and the continued
    approach of the upstream shortwave affects low level wind
    direction/speed, interfering with the convergence axis. Until that
    happens (~14 to 15Z), an isolated threat for flash flooding will
    occur within the urban corridor of the western Peninsula from
    roughly Tampa Bay to Naples, where localized potential for 3-5
    inches of rain will exist.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4hz0-YlbLdfbahyxJgLXOv4vyeuV6pL1Bg31DQCoDTWvUFXcDIYagTXF5GZGkdhT7du0= WRn-CYqNOvtlJWPXutGdfcQ$ for graphic product...

    ATTN...WFO...MFL...TBW...

    ATTN...RFC...ALR...NWC...

    LAT...LON 27798182 27628129 27308135 27058175 26438155=20
    26208202 26548254 27228294 27578280 27728248=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 2 16:44:55 2025
    AWUS01 KWNH 021644
    FFGMPD
    FLZ000-022242-

    Mesoscale Precipitation Discussion 0345
    NWS Weather Prediction Center College Park MD
    1243 PM EDT Mon Jun 02 2025

    Areas affected...portions of southern/southeastern Florida

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 021642Z - 022242Z

    Summary...Scattered to numerous thunderstorm activity is expected
    to develop through 22Z/6pm EDT this evening. These storms will be
    slow-moving, producing enough heavy rainfall in urbanized areas of
    southeastern Florida to promote flash flooding in a few areas.

    Discussion...Recent radar/satellite depicts deepening convective
    cores along the I-95 corridor from Fort Lauderdale to Homestead,
    FL currently. Additional storms were observed just south of the
    Florida Keys and near the Fort Myers area. These cells were
    developing in a strongly unstable environment (2000+ J/kg MLCAPE)
    with abundant moisture (2 inch PW values) supporting efficient
    rain rates as storms continue to strengthen/mature. Additionally,
    weak/modest wind fields aloft were contributing to slow and
    erratic storm motions across the region.

    As cells mature/deepen, a combination of mergers and erratic
    motions will eventually allow for 1-2 inch/hr rain rates to
    develop in a few spots across the urban south Florida I-95
    corridor. This corridor is sensitive to heavy rainfall and a few
    areas of urban flash flooding are expected. Rainfall totals
    exceeding 2 inches are also likely in much of the discussion area
    through 22Z/6pm EDT this evening, with spotty/isolated flash
    flooding expected elsewhere across the discussion area.

    Over time, mid-level flow may increase some ahead of an advancing
    mid-level wave over the northeastern Gulf of Mexico. While the
    resultant increase in shear could aid in a gradual increase in
    storm organization initially across southwestern Florida and
    vicinity, this evolution will likely not reduce the flash flood
    risk across the southern part of the state.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9VfOqdIXtFjAB9aF7tNj0WStYog0ToZ6NgEfAz1JR6cRBnWtTwpL9n6iVm9_pPwvqov-= 8_o8-ZOS3zWtgmqtWWHeH7E$ for graphic product...

    ATTN...WFO...KEY...MFL...MLB...TBW...

    ATTN...RFC...ALR...NWC...

    LAT...LON 27418138 27268040 26967991 25907998 24998041=20
    24548153 24618205 25148164 25638162 26298199=20
    26688210 26988209=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 2 21:45:44 2025
    AWUS01 KWNH 022145
    FFGMPD
    MNZ000-IAZ000-NEZ000-SDZ000-COZ000-030330-

    Mesoscale Precipitation Discussion 0346
    NWS Weather Prediction Center College Park MD
    545 PM EDT Mon Jun 02 2025

    Areas affected...Southwest to Northeast NEB...Far Northeast
    CO...Northwest IA...Far Southeast SD...Southwest MN...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 022145Z - 030330Z

    SUMMARY...Very strong, initially very slow moving thunderstorms
    with potential of upstream redevelopment/repeating may result in
    localized clusters of 3-4" totals and likely to result in
    incidents of flash flooding if outside of the Sand Hills.

    DISCUSSION...GOES-E Visible imagery shows a narrow channel of
    developing cumulus along and south of a well defined cold front
    extending from a surface low in western MN near AQP, southward
    toward the IA/MN/SDak state line before angling back southwest
    across the eastern side of the Nebraska Sand Hills before
    intersecting with another developing low in far northeast CO.=20
    This cu field denotes fairly impressive conditionally unstable
    ribbon of enhanced theta-E air with fairly rich low to mid-level
    moisture. MLCAPEs have risen to 2500-3000 J/kg from the low in MN
    toward southwest NEB, with sfc Tds pooled from mid-50s to low 60s.
    CIRA LPW and instability field also notes strong southerly LLJ
    and moisture/instability axis intersecting the frontal zone ahead
    of the CO low across Western KS to help feed thunderstorms into a
    convective complex later this evening.=20=20

    A strong, compact shortwave along the southeast edge of the larger
    broader synoptic scale trof that is dominant over the Northern
    High Plains, triggered stronger severe thunderstorms and a
    maturing cluster, small convective complex over west-central MN.=20
    Forward propagation of the complex will limit overall rainfall
    totals with cells, but in exiting the shortwave further stretches
    the 500-1000mb thickness ridge along the frontal zone. Solid
    moisture convergence/confluence along the front will increase and
    moisture convergence will start breaking out individual cells from
    northeast to southwest along the instability axis, as noted with a
    stronger initial cell entering NW IA at this time. The strong
    updrafts given surface to 850mb winds of 15-20kts and moisture of
    1.5"/hr will allow for efficient rainfall production along with
    some hail initially.

    As the thickness ridge further elongates, propagation vectors will
    continue to be less than 5-10kts and within a col of weakening
    mid-level flow...cell motions may be very slow initially,
    especially further southwest into northeast and central NEB. As
    such, cells may start to cluster and broaden in width, with rates
    of 1.5-2"/hr likely becoming more numerous between 23-01z.=20
    Stronger more orthogonal intersection upstream may result in
    greater efficiency there, but will eventually forward propagate
    eastward with better than normal steering flow orientation to
    result in some repeating. As such, localized pockets of enhanced
    rainfall totals along and south of the front may reach 3-4" with
    perhaps a very isolated 5" total occurring with best training/cell
    mergers.

    Hourly FFG along the southern and eastern edges of the Sand Hills
    and across into SW MN range from 1.5"/hr to 2-2.5"/3hrs. These
    values are likely to be exceeded in these local smaller
    cluster/pockets from 00-03z, with HREF neighborhood probability
    over 40-50% for 3" and even some 10-15% for 5". While most areas
    in the MPD area of concern will not receive these totals, it is
    likely to see a few incidents of flash flooding occurring,
    especially outside of the Sand Hills proper.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6I7nw_l2mITelr4EzVcLD1q_KhNMIiqnbtX44vkQrh1b9DalNoWo0IkTgQ8gmzuzEesv= LjAkGbybdgN-h2oioXjx_Mk$ for graphic product...

    ATTN...WFO...BOU...FSD...GID...GLD...LBF...MPX...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45109515 45019441 44419418 43549489 42189605=20
    41249743 40779851 40200038 40270231 41080248=20
    41650102 42109934 43149700 44179609 44939584=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 3 01:04:08 2025
    AWUS01 KWNH 030102
    FFGMPD
    AZZ000-NVZ000-030600-

    Mesoscale Precipitation Discussion 0347
    NWS Weather Prediction Center College Park MD
    902 PM EDT Mon Jun 02 2025

    Areas affected...Southern NV...Northwest AZ...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 030100Z - 030600Z

    SUMMARY...Clusters of thunderstorms starting to orient favorably
    for some repeating and potential for localized totals over 1" in
    short duration. Given hard ground conditions, incident(s) of
    flash flooding are considered possible.

    DISCUSSION...RAP analysis shows clusters of thunderstorms that
    developed along a fairly solid stationary front further north
    across eastern NV into central UT have developed potent enough
    cold pools/outflow boundaries. These boundaries along with
    forward propagation into a pool of deeper moisture and
    conditionally unstable environment into the Colorado River Valley
    have resulted in expanding and intensifying convective activity.=20
    GOES-W Visible imagery shows increasingly numerous overshooting
    tops entering Clark county, NV through Mohave county in NW AZ.=20
    Here MLCAPEs of 750-1000 J/kg remain in the fading solar input
    with low to mid 50s Tds across much of the lower Valley floors.=20
    Trapped 700mb moisture within western mid-level trof has
    relatively high 80% RH and total PWat values to 1.25" where
    terrain is lower. While there will remain sub-cloud evaporative
    loss, rates of 1"/hr are probable; though with forward/southward
    speed totals of .5" seem more common with the cores of the
    downdrafts.

    Hard ground conditions will allow for heavy runoff and minor
    flooding concerns; however, convective latent heat feed-back has
    helped to develop a solid 850-700mb circulation in proximity to
    the sagged western portion of the front in northern Lincoln
    county. Low level wind is starting to respond and strengthen from
    10kts toward 15-20kts with increased cyclonic curvature. As as
    result, flanking line convection into southern Nye county is
    orienting more NW to SE, parallel to the steering flow. Inflow
    from the southwest off the deserts may be a bit drier, but should
    be more orthogonal to help maintain some convective development.=20
    While still uncertain, there is some trend analysis that suggests
    some spots of training in proximity is possible as the overall
    cluster drops south then southeast. A spot or two of 1"-1.25"
    totals would certainly result in localized flash flooding
    concerns. Overall, the cluster/complex should track through the
    pool of instability for the next few hours into far southern NV/NW
    AZ, to maintain a low confidence but possible widely scattered
    focused incident or two of flash flooding this evening.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4WZurNb_hhtbASxzD4OcMXzWketQ-BWwekjYKyNI8jO_OuSgzKynVykZrPXmBTf1IDBP= hj9ixno456iD3bqCCf5u07U$ for graphic product...

    ATTN...WFO...FGZ...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 37441652 37421487 36951398 36641253 35721215=20
    34901250 34961394 35401473 36081546 36891650=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 3 04:25:49 2025
    AWUS01 KWNH 030425
    FFGMPD
    IAZ000-NEZ000-SDZ000-030840-

    Mesoscale Precipitation Discussion 0348
    NWS Weather Prediction Center College Park MD
    1225 AM EDT Tue Jun 03 2025

    Areas affected...eastern NE into western IA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 030424Z - 030840Z

    Summary...Areas of flash flooding will remain possible over the
    central Plains, especially over portions of eastern NE during the
    next couple of hours. Between roughly 07-08Z, the potential for
    flash flooding will begin to shift into western IA, though
    rainfall rates may be lowering by that point in time.

    Discussion...The merging of a line of thunderstorms moving south
    along a cold front and an eastward/northeastward advancing outflow
    boundary from western KS into southern NE resulted in a burst of
    very cold cloud tops over NE between 02-03Z, with 10.3 micron
    imagery from GOES East showing cloud tops near -80 C, and MRMS
    hourly rainfall of 2 to 3+ inches. Cloud tops have warmed a bit
    since then but strong to severe thunderstorms remained with
    locally heavy rain continuing over south-central NE. To the south,
    surface dewpoints ahead of the outflow were in the upper 60s to
    lower 70s over east-central KS and this low level moisture was
    surging northward toward southeastern NE in advance of the outflow.

    The well-defined cold front to the north will continue to advance
    southeastward over the next few hours, eventually meeting with the
    increasing low level moisture across the Missouri River Valley.
    The advection of low level moisture into the region will result in
    increasing instability, with recent RAP forecasts indicating
    1000-2000 J/kg MLCAPE into southeastern NE over the next couple of
    hours, along with decreasing convective inhibition.

    The main concern for additional flash flooding will come from a
    convectively induced vortex located northwest of GRI at 04Z, as it
    follows ENE through eastern NE and eventually reaches western IA.
    Rainfall rates of 1-2 in/hr are expected, although locally higher
    values will be possible, along with an additional 2 to 3 inches of
    rain on a localized basis.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6YK7JtEzNaZDlTTvDD3IWSRd2h8fvTW3ZLLgcdKdUP8CnH3ZNd-QB3Jc5OY_HvfcetCK= -Xvt5TYbLYMCDbdjxfbgSZI$ for graphic product...

    ATTN...WFO...DMX...FSD...GID...LBF...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43329482 42589467 41719526 40879628 40549783=20
    40719906 40580032 40800050 41380035 41759974=20
    42499769 43159641=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 3 05:27:55 2025
    AWUS01 KWNH 030526
    FFGMPD
    MOZ000-OKZ000-KSZ000-030930-

    Mesoscale Precipitation Discussion 0349
    NWS Weather Prediction Center College Park MD
    125 AM EDT Tue Jun 03 2025

    Areas affected...north-central to northeastern OK into
    southeastern KS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 030524Z - 030930Z

    Summary...Training of heavy rain from north-central and
    northeastern OK into southeastern KS may result in an isolated
    spot or two of flash flooding over the next 3-4 hours. Rainfall
    rates of 1-2 in/hr will be possible at times.

    Discussion...05Z radar imagery and surface observations showed an
    outflow boundary that arced from just west of EMP, southward into
    OK, then southwestward to near SWO and toward I-40. The portion
    over KS has been advancing eastward at 30-40 kt but the southern
    portion over OK has been slower to progress east, resulting in a
    SW to NE orientation of the boundary over northern OK, similar to
    the mean steering flow.

    A broken axis of thunderstorms was following the outflow with
    roughly 2000-3000 J/kg MLCAPE in place just ahead of it. The
    outflow boundary is expected to continue advancing east and
    southeast through KS/OK over the next few hours while a ~40 kt low
    level jet at 850 mb, oriented from the SSW, overruns the outflow
    allowing for continued thunderstorm developing and periods of
    short term SW to NE training. Within axes of training, rainfall
    rates of 1-2 in/hr will be possible and localized totals near 3
    inches through 09Z may occur over portions of
    north-central/northeastern OK into southeastern KS.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4cfO9KxznptzIK-L1mYgjKlnwJQBOleGL00Z4GDOx4SRkjDcFMrwFnDuuoKGPXFOyJ-q= X-NP4Kh0OXnNEglKE_aUwxA$ for graphic product...

    ATTN...WFO...ICT...OUN...SGF...TSA...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 37539459 36819470 36199549 35799668 35839758=20
    36199774 36539728 37529581=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 3 13:53:14 2025
    AWUS01 KWNH 031351
    FFGMPD
    MOZ000-OKZ000-KSZ000-031900-

    Mesoscale Precipitation Discussion 0350
    NWS Weather Prediction Center College Park MD
    951 AM EDT Tue Jun 03 2025

    Areas affected...Southern and Eastern KS...West-Central MO

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 031350Z - 031900Z

    SUMMARY...Heavy showers and thunderstorms will likely become more
    concentrated over the next several hours across portions of
    southern and eastern KS into west-central MO. Backbuilding and
    locally training convection will favor the potential for enhanced
    rainfall totals and thus concerns for scattered areas of flash
    flooding.

    DISCUSSION...The morning GOES-E IR satellite imagery shows a
    corridor of heavy showers and thunderstorms with cold convective
    tops impacting areas of eastern KS, with the activity beginning to
    move into areas of west-central MO. The activity is being
    sustained by a southwest low-level jet of 30 to 40+ kts out ahead
    of a cold front, and with the pooling of a favorably moist and
    unstable airmass. The ejection of a mid-level trough with
    favorably divergent flow aloft over the region is also a key
    player with the ongoing convective threat.

    PWs of near 1.75 inches are in place which are about 2 standard
    deviations above normal, and an instability axis is nosed up
    across eastern KS with MUCAPE values of as high as 1500 to 2000
    J/kg. Relatively strong low-level moisture convergence is noted,
    and the early-morning visible satellite imagery shows an expanding
    CU/TCU field down to the southwest of the current activity
    involving areas of south-central to southeast KS.

    Over the next few hours, there is likely to be the renewed
    development and expansion of convection across eastern KS and into
    west-central MO, with activity also likely developing down to the
    southwest into areas of south-central to southeast KS. This is
    consistent with the latest HRRR forecasts and also the 06Z HREF
    guidance which strongly support rainfall rates of 1 to 2
    inches/hour, with an environment conducive for backbuilding and
    locally training convective cells.

    Some rainfall totals through early this afternoon may reach 2 to 4
    inches with isolated heavier amounts possible where cell-training
    is maximized. The persistence of these rains may foster some
    scattered areas of flash flooding which will include a threat for
    some urban impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-wy9XlcHr2u5PWNjH8QduHIXBb-7hRYkgLTpTPbO1QDZgMgNDRhpvVbfbdR9AB8iPmpE= 4PrsHEsp_6YfexdvoHSGp1A$ for graphic product...

    ATTN...WFO...DDC...EAX...ICT...OUN...SGF...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39589338 38789297 38159397 37259619 36959759=20
    37249852 38189800 39339536=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 3 18:37:30 2025
    AWUS01 KWNH 031837
    FFGMPD
    MOZ000-OKZ000-KSZ000-040035-

    Mesoscale Precipitation Discussion 0351
    NWS Weather Prediction Center College Park MD
    236 PM EDT Tue Jun 03 2025

    Areas affected...Central and Northern OK...Southern and Eastern
    KS...Central to Northeast MO

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 031835Z - 040035Z

    SUMMARY...Heavy showers and thunderstorms with additional areas of
    flash flooding will continue into the evening hours across
    southern/eastern KS and into western/northern MO. Gradually this
    threat will settle down into central and northern OK. Given the
    high rainfall rates and localized persistence of the stronger
    storms, areas of significant and life-threatening flash flooding
    are expected.

    DISCUSSION...The midday GOES-E IR satellite imagery shows a
    southwest to northeast axis of heavy showers and thunderstorms
    impacting areas of south-central to northeast KS along with some
    adjacent areas of northwest MO. The activity continues to be aided
    by the persistence of a convergent moist/unstable low-level jet of
    30 to 40+ kts out ahead of a cold front. Relatively stronger
    mid-level forcing associated with an ejecting shortwave trough is
    interacting with MLCAPE values of as much as 1500 to 2500 J/kg and
    PWs of 1.75+ inches, and this has been resulting in a substantial
    amount of organization and persistence of convection over the last
    few hours.

    Already there has been locally considerable flash flooding
    impacting areas around Wichita and Emporia, and some rainfall
    totals locally since mid-morning of 5 to 7+ inches.

    Additional expansion of showers and thunderstorms are expected
    over the next few hours which will extend northeastward into more
    areas of western and northern MO to the southeast of a cold front.
    However, there will also be the development and organization of
    convection deep into the unstable warm sector involving central
    and northern OK where recent visible satellite trends indicate an
    increasingly agitated CU/TCU field. LightningCast data shows
    convection is imminent across these areas.

    Rainfall rates with the stronger storms heading into the evening
    hours will be capable of reaching 1.5 to 2.5 inches/hour, and some
    additional rainfall totals of as much as 3 to 6+ inches will be
    possible which is consistent with the latest HREF/REFS guidance
    and the HRRR solutions.

    Areas of flash flooding will continue, with a general increase in
    the coverage of flash flooding expected over the next several
    hours. Multiple major metropolitan areas will continue to be at
    risk for seeing significant and life-threatening flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-IAtjdWX4eJsMKO7JkRhRYe1Kgdu9_47k1LAU0g1-gm8g9kvqyBJXZ4n_4lCdSVSdXic= 4dq1D4q7T7gkDd4t8jcjQ5I$ for graphic product...

    ATTN...WFO...DVN...EAX...ICT...LSX...OUN...SGF...TOP...TSA...

    ATTN...RFC...KRF...MSR...TUA...NWC...

    LAT...LON 40379254 40109173 39399143 38459215 37309439=20
    35519679 35339838 36099884 37629783 38919648=20
    39789501 40169397=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 3 18:41:57 2025
    AWUS01 KWNH 031841
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-040040-

    Mesoscale Precipitation Discussion 0352
    NWS Weather Prediction Center College Park MD
    240 PM EDT Tue Jun 03 2025

    Areas affected...Southern and Eastern CA...Southern NV...Northwest
    AZ...Far Southwest UT

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 031840Z - 040040Z

    SUMMARY...Scattered areas of showers and thunderstorms will
    develop this afternoon across the broader Southwest U.S. which
    will be capable of producing locally heavy rainfall. Given the
    high rainfall rate potential, isolated to scattered areas of flash
    flooding will be possible.

    DISCUSSION...An anomalously moist airmass through the vertical
    column has pooled across large areas of the Southwest U.S. with PW
    anomalies that are near or at record levels for the date. This
    coupled with strong diurnal heating/surface-based instability by
    later this afternoon should result in a favorable environment for
    showers and thunderstorms to initiate and gradually expand in
    coverage.

    An upper-level low is seen in WV satellite imagery dropping
    southeastward offshore of southern CA, and this is yielding very
    steep mid-level lapse rates along with divergent flow aloft around
    its northeast flank which will further facilitate convective
    development over the next several hours.

    The steep mid-level lapse rates coupled with the boundary layer
    heating should facilitate SBCAPE values reaching as high as 1000
    to 2000 J/kg, with the greater CAPE fields likely focusing over
    northwest AZ and far southern NV. A combination of favorable
    thermodynamics along with localized orographics/terrain-induced
    circulations and even some modest shear over the region should
    yield scattered pulse to multi-cell thunderstorms which will be
    capable of producing rainfall rates of up to 1.5 inches/hour, with
    even some sub-hourly rates of 1 inch in 20 to 30 minutes possible.

    A look at the latest HREF/REFS guidance suggests some potential
    for 2 to 3+ inch rainfall totals where the storms become locally
    anchored near some of the terrain, and where any potential
    cell-merger activity occurs. This will allow for isolated to
    scattered areas of flash flooding to be possible. Some of the area
    burn scars will be at particular risk for impacts, along with dry
    washes and local slot canyon areas.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7bu_NYWF_fLMhfOJA9CCn2XRs97auo3iXgIJTXDFbIFwfiDH-HM3I2oZzWSQNmU3ggdK= pyQgv8KSZVa2R4-ubwYDFrE$ for graphic product...

    ATTN...WFO...FGZ...GJT...HNX...LOX...MTR...PSR...REV...SGX...
    SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 37651221 36921048 35121012 34211138 34271332=20
    34171475 33541551 32731573 32611686 33501754=20
    33991821 34441930 34672001 34892039 35482086=20
    35792094 36042033 35641929 35731865 36291858=20
    37401903 37631862 37011736 37561486=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 4 00:15:29 2025
    AWUS01 KWNH 040014
    FFGMPD
    NMZ000-AZZ000-UTZ000-NVZ000-CAZ000-040613-

    Mesoscale Precipitation Discussion 0353
    NWS Weather Prediction Center College Park MD
    814 PM EDT Tue Jun 03 2025

    Areas affected...southern California, southern Nevada, northern
    Arizona, far southern Utah, northwestern/north-central New Mexico

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 040013Z - 040613Z

    Summary...Mature thunderstorms continue to move slowly within an
    axis from near Los Angeles and the Transverse Ranges eastward to
    northwestern New Mexico. Spots of 0.5-1.25 inch/hr rain rates are
    exceeding FFG thresholds in local areas and causing excessive
    runoff/flood impacts. These impacts should continue on a
    scattered basis through at least 06Z/10p PDT.

    Discussion...Abundant surface heating, steep lapse rates aloft,
    and appreciable moisture content has enabled development of
    several clusters of slow moving thunderstorms across the
    discussion area this afternoon. The heaviest downpours have been
    concentrated across portions of the San Bernardino Mountains
    eastward to near Las Vegas and adjacent areas of northwestern
    Arizona, where PW values at or above an inch were noted via
    mesoanalyses. These cells have prompted occasional flash flood
    impacts over the last 3-6 hours as well. Models/CAMs suggest that
    these cells will be primarily diurnally driven and persist through
    just after sunset before weakening and decreasing in coverage.=20
    Flash flood potential is expected to continue during that time.

    Farther east, a more isolated threat for flash flooding exists
    across northern New Mexico. Here, moisture/PW values are
    comparatively lower (around 0.65 inch) and faster flow aloft has
    enabled slightly faster storm speeds, limiting the amount of
    rainfall in any one spot. Nevertheless, areas of 0.5 inch/hr rain
    rates should continue for another 3-5 hours or so (through 05Z/8p
    MDT) and may occur over burn scars and other sensitive terrain
    across the region. Eventually, nocturnal surface cooling should
    aid in decreasing storm intensity/coverage especially after dark.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5e9pyQVCwIArXpmvlTKWuxw3nrVrHw98niw9jpr7VX2hVazc9PZ_0dw4cyfQ2-P9MlRf= hz85YqqZmNzk0pbL6Hkb9gY$ for graphic product...

    ATTN...WFO...ABQ...FGZ...HNX...LOX...PSR...REV...SGX...SLC...
    VEF...

    ATTN...RFC...FWR...RSA...STR...TUA...NWC...

    LAT...LON 37871738 37811490 37311357 36791114 36900779=20
    36750563 36540468 35940491 35220636 34680802=20
    34330965 34551282 34031506 33041581 32631695=20
    33231751 33911848 34451950 34611902 35051831=20
    36361852 37371883=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 4 00:38:01 2025
    AWUS01 KWNH 040037
    FFGMPD
    TXZ000-OKZ000-040636-

    Mesoscale Precipitation Discussion 0354
    NWS Weather Prediction Center College Park MD
    837 PM EDT Tue Jun 03 2025

    Areas affected...southern/southeastern Oklahoma through north and
    central Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 040036Z - 040636Z

    Summary...Isolated flash flood potential should continue with
    scattered thunderstorm activity migrating southeastward across the
    discussion area through the night (06Z/1am CDT). Occasional
    instances of 2+ inch/hr rain rates are likely where cell mergers
    and training are observed.

    Discussion...Scattered thunderstorms have evolved into a series of clusters/loosely organized supercellular structures and linear
    segments extending from near Tulsa south-southwestward through Ada
    and southeast of Wichita Falls. Storms across northeastern
    Oklahoma have grown upscale and become quite progressive, with
    rain rates limited to around 1 inch/hr. Isolated flash flooding
    is possible in sensitive/low-lying areas in this regime.

    Farther southwest, clusters have exhibited less linear structure
    and have occasionally merged/backbuilt - prolonging heavy rain
    rates in local areas. Spots of 2-3 inch/hr rain rates were being
    estimated per MRMS near/southwest of Ada and also south of Wichita
    Falls. These rain rates were occurring in areas of 2-3.5 inch/hr
    FFG thresholds - highest with southward and southeastward extent.=20
    With already spotty/isolated coverage of the heavier rain rates
    moving into areas of slightly higher FFG, current thinking is that
    the ongoing flash flood risk should remain isolated and localized
    to sensitive/urban areas through the evening. CAMs/high-res
    guidance depict a potential focus for backbuilding/heavier rain
    rates across portions of north and west-central Texas through the
    overnight hours in tandem with a southward-moving synoptic front
    over the southern High Plains. The risk of 2+ inch/hr rain rates
    should persist through the night in this regime - potentially
    impacting areas near Dallas/Fort Worth, Waco, and perhaps Austin
    later tonight.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5XCku1DX0nLi8_CAqYvy7nZKF7QUmsJGQneAkIeh1Gbn5dkU2JLKqvI7ucQ9XG5RCWd9= fHf6U5wJBtMI-FKopVUS8qs$ for graphic product...

    ATTN...WFO...EWX...FWD...OUN...SHV...SJT...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 36579567 36289476 34829450 33319449 31859549=20
    31009631 30619754 30619894 31270027 32409953=20
    33519873 34589772 35479682 36369610=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 4 01:04:37 2025
    AWUS01 KWNH 040104
    FFGMPD
    ILZ000-MOZ000-ARZ000-OKZ000-KSZ000-040703-

    Mesoscale Precipitation Discussion 0355
    NWS Weather Prediction Center College Park MD
    904 PM EDT Tue Jun 03 2025

    Areas affected...southern/central Missouri, far northwest Arkansas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 040103Z - 040703Z

    Summary...A couple of progressive linear convective complexes will
    sweep through the region this evening, prompting occasional areas
    of 1-1.5 inch/hr rain rates on an isolated basis. These rates
    could result in a few areas of flash flooding - especially in
    typical sensitive/low-lying areas of the Missouri Ozarks.

    Discussion...Earlier convection across Kansas/northern Missouri
    has evolved into a couple of extensive linear segments - one
    extending from near Quincy, IL to near Sedalia, MO that intersects
    with a separate linear MCS across west-central Missouri through
    Joplin and Tulsa, OK. These linear complexes have become much
    more progressive compared to their earlier evolution, with 25-35
    kt storm motions generally limiting hourly rain rates to 1-1.5
    inch/hr in spots. Despite the downward trend in rain rates, some
    opportunity remains for training/repeating cells across central
    Missouri (near the intersection of the two linear complexes
    around/south of the Columbia area) and across far northeastern
    Oklahoma (where 1-1.75 inch/hr rain rates are more prevalent east
    of Bartlesville). The overall regime appears to be shifting
    eastward toward the Missouri Ozarks and vicinity, with terrain
    supporting occasional flash flood potential in low/sensitive
    spots. The downstream environment contains 1.5-1.9 inch PW values
    and 1500 J/kg MLCAPE - both supportive of efficient rain rates
    (occasionally exceeding 1 inch/hr) as storms move east.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8ByYPXRRSnfu_c27lD6bbhETAsPNodNoEP8VX-dTTFh0SNM7ZVnOGQk4D1V_s2HoWVhK= NmLH0YAw_jT6EEoROqKgEMg$ for graphic product...

    ATTN...WFO...EAX...LSX...LZK...PAH...SGF...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 39699213 39499106 39019056 38299066 37149094=20
    36359235 35839359 35929478 36479513 37209457=20
    38359388 39249298=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 4 06:08:02 2025
    AWUS01 KWNH 040607
    FFGMPD
    AZZ000-CAZ000-041030-

    Mesoscale Precipitation Discussion 0356
    NWS Weather Prediction Center College Park MD
    206 AM EDT Wed Jun 04 2025

    Areas affected...southern/desert CA into western AZ

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 040605Z - 041030Z

    Summary...Localized high rainfall rates may continue to produce a
    few areas of flash flooding from the desert regions of southern CA
    into portions of western AZ through 10Z. Peak rainfall rates of
    0.5 to 1.0 inches in 15-30 minutes will be possible.

    Discussion...Regional radar imagery and GOES West infrared
    satellite imagery through 0545Z showed scattered thunderstorms
    continued from the desert regions of southern CA into the
    southwestern edge of the Colorado Plateau through western AZ.
    While cloud tops were warming overall, some new cell development
    was noted near an outflow boundary pressing south through
    southeastern San Bernardino and eastern Riverside counties along
    with a few new cells showing up in Imperial County. Meanwhile in
    AZ, showers/thunderstorms have been slowly edging south atop a
    southward sagging outflow boundary which extended from northern
    Gila County, westward into La Paz County. Many of these cells in
    AZ have lost their vigor, but locally heavy rain continued in a
    couple of spots. Although instability was lowering, SPC
    mesoanalysis data showed these cells were occurring within 500 to
    1000 J/kg MLCAPE and anomalous PWs of 1 to 1.5 inches.

    A 700-500 mb upper low was centered just west of the northern Baja
    Peninsula and is forecast to slowly track eastward along with a
    northward extending trough. At least an isolated flash flood
    threat will remain with development along outflow, and while cells
    should be short-lived, there will be potential for peak rainfall
    rates of 0.5 to 1 inch in 15-30 minutes. Despite nocturnal cooling
    of the boundary layer, steep low to mid-level lapse rates will
    continue to support weak CAPE values overnight and increasing low
    level moisture with some return low level flow from the northern
    Gulf of California...out ahead of the 700-500 mb low...may support
    localized increases in CAPE over the next few hours, especially
    across portions of western AZ. Therefore, for the next 4-5 hours,
    a localized flash flood threat is expected to continue for
    portions of southeastern CA into western AZ.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6VJNNSMSqljyTgarX8u1q_W29dpmOZNhfLO1S200l26cdhDAad1dK_tCfbsxw9RRcU1j= 56oBGnVgPs-IQ8MrEya7C_s$ for graphic product...

    ATTN...WFO...FGZ...PSR...SGX...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 35441214 35371122 35081078 34651074 34161111=20
    34001147 33561273 33161377 32661434 32541507=20
    32491587 32611633 33021654 33601658 34081605=20
    34611531 35041382=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 4 08:04:08 2025
    AWUS01 KWNH 040803
    FFGMPD
    TXZ000-041330-

    Mesoscale Precipitation Discussion 0357
    NWS Weather Prediction Center College Park MD
    402 AM EDT Wed Jun 04 2025

    Areas affected...TX Hill Country to I-35 corridor

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 040800Z - 041330Z

    SUMMARY...Isolated to widely scattered instances of flash flooding
    will be possible through 13Z across portions of central TX. Heavy
    rainfall with potential for 1-3 inches in an hour but also
    sub-hourly rainfall of 1-2 inches in 30 minutes will be possible.
    These rates may impact the sensitive terrain of the Hill Country
    where locally heavy rain has fallen over the past week and
    possibly the I-35 corridor from near Temple to San Antonio.

    DISCUSSION...0730Z radar imagery showed a largely linear axis of
    thunderstorms extending WSW from McLennan County to southern
    McCulloch County. These storms were occurring along an outflow
    boundary and cold front advancing southward with some recent
    development toward the west, just south of San Angelo. The line
    has been mostly progressive over the past 3 hours but MRMS and
    gauge reports have indicated peak rainfall rates of 1.0 to 2.5
    inches in an hour and 1.0 to 1.5 inches in 15 minutes (vicinity of
    Goldthwaite and San Saba).

    Anomalous moisture of 1.5 to 2.0+ inches along with 1500-2500 J/kg
    MLCAPE were helping to fuel the high rates beneath a diffluent
    flow pattern in the upper levels. The cold front and outflow will
    both continue to sag southward through about 13Z across the Hill
    Country, at which point some slowing or stalling is forecast by
    short term guidance. The line of thunderstorms is expected to
    follow the boundary southward with some continued development
    toward the west as convective inhibition weakens due to low level
    moisture transport from the south. Meanwhile, possible weakening
    of rainfall intensity may occur to the east near I-35, given
    better orthogonal low level flow into the boundary will be in
    place for points west over the Hill Country and some recent
    warming of cloud tops has been observed over east-central TX.
    Locally high rainfall rates will continue at least an isolated
    flash flood threat across the Hill Country into the I-35 corridor
    through 14Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_anYHDsS_zWnwCd75Le8XZQNmkUKgJbsylSlSYD08du-gQZOld_acV83etyERhLecoEN= PZDUVFU67xosaM71UvC0Q6s$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31519757 31159714 30579712 29809753 29189851=20
    29129969 29240052 29830105 30600119 31170085=20
    31129957 31199896 31409840=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 4 09:48:08 2025
    AWUS01 KWNH 040948
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-041345-

    Mesoscale Precipitation Discussion 0358
    NWS Weather Prediction Center College Park MD
    547 AM EDT Wed Jun 04 2025

    Areas affected...southwestern MO into adjacent portions of OK/AR

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 040945Z - 041345Z

    SUMMARY...Localized SW to NE training may result in an isolated
    area or two of flash flooding in southwestern MO and perhaps
    adjacent portions of OK/AR through 14Z. Rainfall rates of 1-2
    in/hr are expected.

    DISCUSSION...Radar imagery at 0930Z showed a SW to NE axis of
    showers extending from Ottawa County in northeastern OK to Jasper
    County in southwestern MO. Local Wunderground observations just
    south of Joplin have indicated about 1 inch of rain in 30 minutes
    and generally peak totals of 1 to 2 inches. The storms were
    developing along a quasi-stationary front ahead of a subtle
    vorticity max over northeastern OK, as observed on 6.9 micron
    imagery from GOES East.

    09Z SPC mesoanalysis showed that the environment over southwestern
    MO had weak instability (< 500 J/kg MLCAPE) but contained high
    moisture with PWs between 1.7 and 1.8 inches. SSW low level flow
    and mean steering flow into the frontal boundary will continue to
    promote localized areas of SW to NE training over the next 1-3
    hours, but instability will remain weak. Additional development of
    showers could occur to the south, ahead of a surface low near MKO.
    SW to NE training but with a gradual eastward translation to the
    heavy rainfall axis is expected. This may result in localized
    flash flooding, especially if overlap occurs with recent heavy
    rain that fell near and north of I-44.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-ZU4yjHmnAfhNyUvRu1yO5x-zQC9YgGCrcvda0cJfHdEWYUB4x42iqGiZdObBKV-X5ho= n9E4UDqaA_I9hEhRHNN3vGI$ for graphic product...

    ATTN...WFO...SGF...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 38369286 38129220 37489249 36099389 35669447=20
    35669478 36189526 36839504 37849372=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 4 12:01:06 2025
    AWUS01 KWNH 041201
    FFGMPD
    FLZ000-041800-

    Mesoscale Precipitation Discussion 0359
    NWS Weather Prediction Center College Park MD
    800 AM EDT Wed Jun 04 2025

    Areas affected...southwestern FL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041200Z - 041800Z

    Summary...Showers and thunderstorms are increasing in coverage and
    intensity offshore, and should start moving ashore shortly.=20
    Hourly rain amounts to 3" with local amounts to 5" are possible,
    which would be problematic in urban areas.

    Discussion...An upper level low is noted in water vapor imagery in
    the northeast Gulf, south of Apalachicola. An area of scattered
    thunderstorms have formed offshore southwest FL which is slowly
    broadening and intensifying, while an outflow from overnight
    convection is approaching the convection's southeastern flank. As
    of this discussion's sending, hourly rain estimates are in the
    0.5-1" range to the northwest of Captiva. The synoptic surface
    wind field is light out to the east to southeast, while flow at
    850 hPa is south to southwest at 20-25 kts per VAD wind profiles
    and RAP forecasts, bringing effective bulk shear to 25 kts.=20
    Precipitable water values are around 2". ML CAPE values have been
    slowly rising along the immediate coast per SPC mesoanalyses,
    where skies are mostly clear as of this discussion's sending. For
    the moment, CIN is present inland. Offshore ML CAPE values are
    1000-1500 J/kg.

    Some additional increase in instability is expected before the
    showers and thunderstorms move inland. Should the convection
    continue increasing in coverage, which is implied by a modest
    increase in the Galvez-Davison index to 30 in the 15-18z time
    frame and recent radar trends, this would force the instability
    gradient to remain rather coastal. Given the effective bulk
    shear, some level of convective organization is anticipated, which
    should help with increasing hourly rain amounts if convection gets
    anchored to a coastal instability gradient, short periods of cell
    training, or cell collisions/mergers occur. The mesoscale
    guidance has isolated to widely scattered signals for 3-5" totals
    between Sarasota and Naples. Given the ingredients present,
    hourly rain amounts to 3" with local totals to 5" are possible,
    which would be most problematic in urban areas.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6DINYzn1E7d2wePx8FxKTNkWYNzrdSHt4yIEfi96RSP9R_Cu5DWebzj9vbSO_6kh70_2= _2U72Y7eygf1e3oz7HegB_o$ for graphic product...

    ATTN...WFO...MFL...TBW...

    ATTN...RFC...ALR...NWC...

    LAT...LON 28028238 27048159 26028146 25848180 26258210=20
    27838286=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 4 14:46:42 2025
    AWUS01 KWNH 041446
    FFGMPD
    SCZ000-GAZ000-042100-

    Mesoscale Precipitation Discussion 0360
    NWS Weather Prediction Center College Park MD
    1045 AM EDT Wed Jun 04 2025

    Areas affected...portions of coastal GA & SC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041500Z - 042100Z

    Summary...Narrow convective bands which can train for 1-2 hours
    are anticipated to increase in frequency late this morning into
    late this afternoon. Hourly rain amounts to 2.5" with local
    totals to 4" are possible, which could lead to issues in urban
    areas.

    Discussion...Water vapor imagery shows a pair of upper level
    circulations across east-central GA and south of Apalachicola FL.=20
    Their combined influence has brought a deep moisture plume into
    the region, with precipitable water values above 2". Inflow at
    850 hPa is ~20 kts per VAD wind profiles. Effective bulk shear is
    near 25 kts and ML CAPE of 1000-2000 J/kg are available near the
    upstream of the GA and southern SC coasts. Thus far this morning,
    a few very narrow, training bands of showers have led to hourly
    amounts of 1.5-2.5" and local amounts as high as 4".

    The expectation is for some increase in coverage of narrow rain
    bands with time as a surface trough sharpens and a surface low
    tries to develop near the GA coast this afternoon, which should
    amp up the 850 hPa inflow and effective bulk shear a little more.=20
    Slight increases in the Galvez-Davison index with time imply
    somewhat greater convective coverage with time as well. The
    mesoscale guidance, while it has a signal for heavy rainfall, may
    be seeming to underplay amounts per their relatively coarse (when
    compared to radar imagery) resolution. Hourly amounts to 2.5" and
    local totals to 4" remain possible where narrow convective bands
    can persist for 1-2 hours. A complicating factor in areas such as
    Charleston SC would be the tidal cycle, with high tide expected at
    2010z, which would potentially enhance any existing heavy rainfall
    issues. Issues are expected to be mainly constrained to urban
    areas.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-r5aQ_FAUKQZLTPJ-XZ0VXHitvMNr3fmdEouGD4sVH9UNcLOwScoJI1nQhHzVwJpimDJ= YGl8I53R6HZR9Q1kH5UDLmM$ for graphic product...

    ATTN...WFO...CHS...

    ATTN...RFC...ALR...NWC...

    LAT...LON 33247996 33087914 32128061 31738110 31858142=20
    32368137 32898076=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 4 16:12:39 2025
    AWUS01 KWNH 041612
    FFGMPD
    COZ000-NMZ000-AZZ000-UTZ000-NVZ000-CAZ000-042211-

    Mesoscale Precipitation Discussion 0361
    NWS Weather Prediction Center College Park MD
    1211 PM EDT Wed Jun 04 2025

    Areas affected...portions of the Southwest

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041611Z - 042211Z

    Summary...Showers and thunderstorms within an environment with
    increasing instability near the upper level trough could lead to
    hourly amounts to 1.5" with local totals to 3", which would be
    problematic in slot canyons, dry washes/arroyos, and burn scars.

    Discussion...An upper-level trough moving through portions of the
    Great Basin is leading to a moisture plume which stretches from
    northern AZ into southwest CO, with a 700 hPa trough fairly
    coincident to the upper level feature. To the south, a low-level
    circulation is apparent in GOES-18 Veggie Band imagery near the
    Lower Colorado River Valley which is also helping to maintain
    anomalously high moisture across the region. Precipitable water
    values range from 0.6" at higher elevations to 1.2" in lower
    elevations. Surface-based/ML/MU CAPE is showing an upward swing
    with daytime heating, albeit much earlier than usual, with MU CAPE
    of 500-1500 J/kg. Satellite imagery shows CIN eroding across
    eastern AZ, western NM, southern UT, and southwest CO. Effective
    bulk shear of 25-40 kts exists from southern and eastern AZ
    northeastward, which is leading to some convective organization
    with activity approaching the Four Corners.

    The 12z HREF probabilities of 0.5"+ jump upward and broaden across
    the area over the next couple hours. The MU CAPE currently
    available when combined with daytime heating should translate
    fairly soon into 1000-2000 J/kg ML CAPE. Given the moisture
    available, hourly rain amounts to 1.5" with local totals up to 3"
    appear to be the high bar. This degree of rainfall would be of
    most concern in urban areas, slot canyons, dry washes/arroyos, and
    near area burn scars. Rainfall-related issues appear to be
    isolated to widely scattered through 22z.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8hUjXV6T7Tuj7wYw0mqzfSME-c5-ZFcyxIl_MtNs7i19r3gkfV86d3t9x9uHL0HeVNWS= SRfJsAeAJ9x-iWST9hj1-lg$ for graphic product...

    ATTN...WFO...ABQ...FGZ...GJT...PSR...SLC...TWC...VEF...

    ATTN...RFC...FWR...RSA...STR...NWC...

    LAT...LON 38950817 35740681 33320984 33131151 34891536=20
    36491585 37921248=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 4 16:48:40 2025
    AWUS01 KWNH 041648
    FFGMPD
    ILZ000-MOZ000-ARZ000-OKZ000-042247-

    Mesoscale Precipitation Discussion 0362
    NWS Weather Prediction Center College Park MD
    1247 PM EDT Wed Jun 04 2025

    Areas affected...in and near southern Missouri & southwest
    Illinois

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041647Z - 042247Z

    Summary...Showers and thunderstorms are beginning to redevelop in
    and near southern Missouri. Hourly rain amounts to 2.5" with
    local amounts to 5" are possible, which would be problematic.=20
    Scattered areas of flash flooding are anticipated over partially saturated/compromised soils.

    Discussion...A wavy cold front stretches across the Great Lakes,
    Midwest, and southern Plains on the southeast flank of a longwave
    trough. Renewed shower and thunderstorm development has recently
    occurred across southwest MO, while other activity moves from
    southeast MO into southwest IL. Precipitable water values are
    ~1.8", ML CAPE is 500-2000 J/kg, and effective bulk shear is 25-35
    kts. The degree of effective bulk shear combined with fairly
    unidirectional flow with height out of the southwest have
    occasionally organized linear southwest-northeast bands near the
    front.

    The front is expected to slow down with time, which potentially
    increases the heavy rainfall/flash flood threat. The expectation
    is for increased convective coverage with time, though the
    mesoscale guidance isn't completely united in their vision as to
    where it would occur. The best overlap for heavy rainfall is
    across southern MO, where instability is greatest and where dew
    points are closest to 70F. However, places farther northeast in
    IL are experiencing an ongoing round of convection that could
    receive a second round in several hours. Northwest portions of
    the discussion area have received 1-4" of rain over the past 24
    hours, partially saturating soils. Hourly rain amounts up to 2.5"
    and local totals up to 5" are possible where cells train, merge,
    or an random mesocyclone develops.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4Y1VkfMQq3O3CbaTXrcJ9Eieyg52X0u5yduzCcAtYQYynDA2sVamT7MGRAcce77ChwPk= Z3eYWcoepQDhKwVcFz6upcg$ for graphic product...

    ATTN...WFO...ILX...LSX...LZK...PAH...SGF...TSA...

    ATTN...RFC...KRF...MSR...ORN...TIR...TUA...NWC...

    LAT...LON 40388960 39398851 38128917 36509119 36019421=20
    36519485 37979269=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 4 21:02:52 2025
    AWUS01 KWNH 042102
    FFGMPD
    INZ000-ILZ000-MOZ000-050201-

    Mesoscale Precipitation Discussion 0363
    NWS Weather Prediction Center College Park MD
    501 PM EDT Wed Jun 04 2025

    Areas affected...southern/east-central Missouri into
    central/eastern Illinois

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 042101Z - 050201Z

    Summary...A focused band of training convection has developed from
    east of Springfield, MO to near St. Louis over the past couple
    hours. The scenario will allow for localized spots of 2-5 inch
    rainfall totals to occur from east-central Missouri into central
    Illinois - raising concerns for a locally significant flash flood
    event especially near St. Louis Metro through 00Z.

    Discussion...Recent radar/observations depict an increase of
    convective intensity and coverage along a stalled synoptic front
    extending from near Springfield, MO to St. Louis to Champaign, IL.
    The increase in convective coverage is attributed to persistent
    convergence along the front and abundant sunshine/destabilization
    out ahead of the front, which has allowed for 2500 J/kg SBCAPE to
    develop amid 1.9 inch PW values near the storms.=20

    Of particular concern is the lack of indication that these storms
    will begin to propagate off their current axis of rainfall for at
    least the next couple hours or so. This will enable persistent
    training of convection to occur and support areas of 2-5 inch
    rainfall totals over the next 2-4 hours across portions of
    south-central to east-central Missouri. These heavy rain rates
    should pose a risk for locally significant urban flash flooding
    near St. Louis through 00Z/7p CDT.

    The bands of training convection are also expected to migrate east-northeastward across portions of Illinois and western Indiana
    through 02Z or so. Flash flooding is a distinct possibility in
    those areas as well given the propensity for storms to train in
    the moist/buoyant pre-convective environment.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6GFEC3zljXejqIs8tyW9rMiIBtA4bP_pTbzVrwmSG3YQQiBOf1KePKdCZt3MdBsHr0Pk= 751znBRoI-WzPc-dkPvJ96A$ for graphic product...

    ATTN...WFO...ILX...IND...IWX...LOT...LSX...PAH...SGF...

    ATTN...RFC...KRF...MSR...ORN...TIR...NWC...

    LAT...LON 41118667 40318634 39158671 38318827 36829154=20
    37039259 37869264 39099072 40398935 41038776=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 4 21:58:27 2025
    AWUS01 KWNH 042157
    FFGMPD
    COZ000-NMZ000-AZZ000-UTZ000-NVZ000-050355-

    Mesoscale Precipitation Discussion 0364
    NWS Weather Prediction Center College Park MD
    556 PM EDT Wed Jun 04 2025

    Areas affected...portions of the Great Basin and Four Corners
    region

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 042155Z - 050355Z

    Summary...Isolated/spotty flash flood potential will continue
    through peak heating hours this evening.

    Discussion...Scattered thunderstorms continue to move slowly
    across the discussion area, with localized areas of somewhat
    higher concentration of activity located across southern/eastern
    Utah and central New Mexico near Albuquerque. The storms remain
    in a favorable environment for locally heavy rainfall (exceeding
    an inch at times) due to their slow movement, 0.75-1 inch PW
    values, and steep mid-level lapse rates (exceeding 8C/km in most
    areas). Of particular concern through the next 6 hours are
    sensitive areas/slot canyons across southern Utah and burn scars
    across north-central New Mexico. Slightly faster steering flow
    aloft was noted over central New Mexico, which has resulted in
    somewhat faster storm speeds although spots of 1 inch/hr rates
    remain evident there per MRMS.

    Most of the storms across the discussion area expected to remain
    strongly tied to the diurnal cycle, with weakening/decreasing
    coverage expected to commence after 03Z or so.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!63rg36PGn9gN54gQ1CbJ6YB1MbqTGfTvE8e42i45_1JV-9hrj91rZMRiM9Ppz7n7ppnN= Y8oEnyxJC0vXyN_860pJTsE$ for graphic product...

    ATTN...WFO...ABQ...BOU...FGZ...GJT...LKN...PUB...SLC...VEF...

    ATTN...RFC...FWR...KRF...RSA...STR...TUA...NWC...

    LAT...LON 40070796 39630621 38360527 35510525 34530566=20
    33820760 33961124 34761382 36351616 37201646=20
    37961631 38621554 38881407 38841281 39521089=20
    39980964=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 5 05:00:20 2025
    AWUS01 KWNH 050500
    FFGMPD
    KYZ000-INZ000-ILZ000-MOZ000-051030-

    Mesoscale Precipitation Discussion 0366
    NWS Weather Prediction Center College Park MD
    1259 AM EDT Thu Jun 05 2025

    Areas affected...Southeast MO...Southern IL..Southwest to Central
    IND...Adj KY...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 050500Z - 051030Z

    SUMMARY...Increasing convective efficiency with clusters.=20
    Favorable orientation may allow for multiple repeating rounds
    resulting in widely scattered incidents of 2.5-3.5" totals and
    possible localized flash flooding.

    DISCUSSION...GOES-E WV along with RADAR mosaic denotes well
    defined shortwave/MCV crossing SE IL into west-central IND, with
    excellent anticyclonic outflow channeling to maintain MCV strength
    and therefore low level inflow. WV suite and RAP analysis also
    shows another subtle upstream shortwave, weak feature that can be
    seen in 850mb vorticity analysis near the MO Bootheel in Northern
    AR, moving even slower northeast. 850mb flow analysis shows
    return moisture channel across the TN Valley becoming
    convergence/confluent through the Tri-Rivers area of W KY
    intersecting with the frontal zone and outflow boundaries from
    initial convection. VWP shows 25-35kts of 925-850mb flow within
    the q-axis with 1.75-2" total PWATs stretched out across central
    IND back to the 850mb inflection in SE MO. This advection/q-axis
    has some remaining uncapped/weakly capped 1000-1500 J/kg of MLCAPE
    that can be utilized at those random intersections of deep layer
    moisture convergence near the boundaries. Additionally, 300-500mb
    flow is increasingly diffluent along th southeast side of the
    clustering providing solid ascent/outflow to maintain favorable
    ascent through the overnight period.=20

    As such, recent 10.3um EIR and RADAR mosaic shows increasing
    convective activity mainly along the upwind flanking line of the
    stronger outflow boundary from the original MCV across central IND
    back into S IL, as well as the best convergence in SE MO into S
    IL. Overall, moisture flux and vigor suggests increasing rainfall
    efficiency toward 1.5-2"/hr likely to evolve over the next few
    hours, particularly in the best unstable environment from MO to SW
    IND. Each cluster has solid potential for 1-2.5" totals...but
    deep layer steering between waves is flattening to support
    clusters repeating through the overnight period and may result in
    localized pockets up to 3.5" though most streaks/clusters of
    enhanced totals will be in the 2-3" range.

    Hydrologically, grounds are fairly average in soil moisture and
    therefor should up-take modest rainfall well with good
    infiltration. However, the rates near 2" are in the vicinity of
    the hourly FFG values, as well as the 3hr values ranging from
    2-3". This provides enough confidence for a few scattered
    incidents of possible flash flooding over the next 6hrs and
    matches up well with 00z HREF probability of 3"/6hr probability
    ranging up to 45% across potions of the highlighted area of
    concern.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4MK0OthzKFSTxx5XSaA6doI5tt8VJCuq_hiGxGDZ9KcKMPv6F54RrYSxZNRHURIjxHFU= TpJUNkijFIhNP0gOLOVwzfE$ for graphic product...

    ATTN...WFO...ILX...IND...LMK...LSX...PAH...

    ATTN...RFC...MSR...ORN...TIR...NWC...

    LAT...LON 39928640 39478601 38658610 38038669 37408752=20
    37188787 36988828 36708882 36699006 36589049=20
    36739102 37089099 37549037 38268901 38568846=20
    39158772 39858698=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 5 16:18:57 2025
    AWUS01 KWNH 051618
    FFGMPD
    NCZ000-SCZ000-052217-

    Mesoscale Precipitation Discussion 0367
    NWS Weather Prediction Center College Park MD
    1218 PM EDT Thu Jun 05 2025

    Areas affected...Central/Eastern NC and Northern SC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 051617Z - 052217Z

    Summary...Isolated to scattered flash flooding is possible this
    afternoon across portions of central to eastern North Carolina and
    northern South Carolina.

    Discussion...A surface low pressure is helping drive a heavy
    rainfall risk this afternoon across portions of central and
    eastern NC into northern SC. Close to and just north of the low
    center we are seeing very efficient warm rain processes in play,
    with PWs around 2", high freezing levels and a deeply saturated
    profile. This is allowing for hourly rainfall around 2" despite
    the less than impressive radar/satellite depiction. The low is
    expected to take more of an easterly turn this afternoon, and
    would expect this area of efficient rainfall to push east along
    with it through portions of central NC. The rainfall intensity
    will likely vary, with both upticks and downticks through the
    afternoon near the low center...but the environment will remain
    similar, and thus upwards of 2" an hour rainfall will remain
    possible at times.

    To the east and southeast of the low we are seeing increasing
    instability with daytime heating. This should support the
    expansion of some deeper convection over this corridor. These
    cells may tend to move quicker than the shallower convection near
    the low...but will still be capable of short duration heavy rates
    given the high PW airmass in place. Plus, certainly possible the
    warm front extending east from the low acts as a focus for at
    least some brief training.

    Overall, expecting an isolated to scattered flash flood risk to
    exist over the next several hours across portions of central to
    eastern NC. The HRRR has been struggling with the convective
    evolution this morning. Based on recent observational trends, it
    appears like the experimental RRFS and REFS may be handling this a
    bit better with regards to rainfall placement and magnitudes.
    Through 21z REFS neighborhood probabilities of exceeding 3" are
    40-70%, with 5" exceedance probabilities peaking at 10-20%. The
    probabilities of 2" in an hour increase to 40-70% early this
    afternoon as well. Given the placement of the warm front and
    instability axis, not expecting the rainfall axis to get much
    farther north than it currently is, and some backbuilding to the
    south (near the warm front) is possible as well.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4poGHp11DDA8Kh7HwH5czAuh5H0xJAMJcLQzZjETqU8tPpQk2ZAw641K4FPRnBIecs56= yyjXBARe-FaQe0YwcFbSh-M$ for graphic product...

    ATTN...WFO...CAE...GSP...ILM...MHX...RAH...

    ATTN...RFC...ALR...NWC...

    LAT...LON 36057932 35977850 35617813 35047760 34497778=20
    34157841 34167887 34387977 34668041 35008059=20
    35468061 35808045 35978003=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 5 17:42:57 2025
    AWUS01 KWNH 051742
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-052341-

    Mesoscale Precipitation Discussion 0368
    NWS Weather Prediction Center College Park MD
    142 PM EDT Thu Jun 05 2025

    Areas affected...Southern NV, Northwest AZ, Southwest UT and
    Southeast CA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 051741Z - 052341Z

    Summary...Increasing convection will lead to an isolated flash
    flood risk this afternoon across portions of the Southwest.

    Discussion...The focus for isolated flash flooding this afternoon
    appears to be across portions of southern NV, northwest AZ, far
    southwest UT and southeast CA. It is here where we are seeing the
    best overlap of instability and moisture today. Surface based CAPE
    is already over 1000 j/kg in spots, and forecast to increase
    towards 1500-2000 j/kg with mostly sunny skies helping
    destabilization. This is notably higher than the instability 24
    hours ago. PWs over this region generally range from 0.75" to
    1.25" and are a tad higher than 24 hours ago as well. This
    combination of increased instability and PWs should support
    intense rainfall rates in convection. While not widespread,
    probabilities from the HREF and REFS indicate that localized 1"+
    an hour rainfall is probable. Deep layer mean flow is only 5-15
    kts out of the west, allowing for just some slow eastward cell
    movements today. Cells should stay tied to terrain features long
    enough to produce locally heavy rainfall, and when they do move
    off the terrain brief cell mergers could locally enhance rainfall
    magnitudes.

    While widespread impacts are not anticipated, localized flash
    flooding is probable in this setup. Based on current radar and
    satellite trends the greatest convective coverage will probably be
    over northwest AZ...but there is a strong signal for isolated to
    scattered development shortly over southern NV as well. In fact
    neighborhood probabilities of exceeding 3 hr FFG get as high as
    60-80% in the experimental 06z REFS over southern NV. The risk
    over adjacent areas of CA is more conditional, but isolated cells
    may try to develop and/or propagate into this area later this
    afternoon. Southwest UT is a bit more uncertain, with ongoing
    showers impacting destabilization. But still a chance we get some
    stronger redevelopment over this corridor this afternoon as well.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_s372gQ_PLTmhwGVAl9VJI15IQotqoJBrrfYh0Bq3qZFXnv9SGFYi8eEn8F2iffMfo0D= z0CceIhCx0tBYfUu_Lg0IXg$ for graphic product...

    ATTN...WFO...FGZ...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 38381393 38301304 38071214 37351183 36421153=20
    35801157 35301190 34991289 34891410 34951476=20
    34651566 34611576 34581620 34971654 35481647=20
    36181616 36691595 37291577 37771522 38161460=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 5 18:42:27 2025
    AWUS01 KWNH 051842
    FFGMPD
    TXZ000-OKZ000-052241-

    Mesoscale Precipitation Discussion 0369
    NWS Weather Prediction Center College Park MD
    241 PM EDT Thu Jun 05 2025

    Areas affected...TX Panhandle into Southwest OK

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 051841Z - 052241Z

    Summary...A localized flash flood risk continues across portions
    of the Texas Panhandle into southwest Oklahoma.

    Discussion...Elevated training convection has resulted in a
    localized flash flood risk across portions of the TX Panhandle
    early this afternoon. This activity has not been well handled by
    any of the high res model guidance. This lowers confidence on
    convective evolution over the next few hours. Surface based
    instability and PWs are on the increase downstream of the current
    convective cluster, suggesting some threat that this activity
    maintains into the afternoon hours. Some more discrete cell
    development within the inflow of the cluster also suggests the
    potential for upscale growth into the afternoon hours. Both
    supercell and upwind propagation vectors are off to the southeast,
    generally aligned with the orientation of the cluster. Thus the
    combination of cell mergers and training suggests that isolated
    flash flooding could continue to be a concern along the track of
    this convection.

    Again confidence is lower than normal on the convective details
    over the next few hours. However recent IR satellite trends show
    enough persistence of the colder cloud tops to suggest some
    continued longevity of this convective cluster. Given the training
    orientation and possible cell mergers, a localized flash flood
    risk likely continues.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4dzGSl7CkGToASdWWOiRDTdNH_uEzkC-Fw7_No5E-qSYmfcBLy-JBRLMGU08aKrPyD22= 8iO93_aEybq3fSYOP4K0EiI$ for graphic product...

    ATTN...WFO...AMA...LUB...OUN...

    ATTN...RFC...TUA...NWC...

    LAT...LON 36110058 35969957 35949789 35479782 34729842=20
    34419929 34480017 34890067 35620098=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 5 19:43:34 2025
    AWUS01 KWNH 051943
    FFGMPD
    NYZ000-PAZ000-MDZ000-WVZ000-OHZ000-INZ000-060140-

    Mesoscale Precipitation Discussion 0370
    NWS Weather Prediction Center College Park MD
    341 PM EDT Thu Jun 05 2025

    Areas affected...Upper OH Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 051940Z - 060140Z

    SUMMARY...Scattered areas of showers and thunderstorms will
    continue to develop and generally grow upscale over the next few
    hours. Given relatively moist antecedent conditions and heavy
    rainfall rates of 1 to 2 inches/hour, some isolated areas of flash
    flooding will be possible this evening.

    DISCUSSION...The latest GOES-E satellite imagery shows a shortwave
    trough traversing the OH Valley which is interacting with a
    quasi-stationary front draped southwest to northeast from southern
    IN through northern OH, far northwest PA and southwest NY. A wave
    of low pressure is noted in surface observations near the IN/OH
    border, and a combination of relatively stronger low-level
    moisture convergence ahead of this wave along with modest DPVA
    should favor a general increase in the coverage of showers and
    thunderstorms over the next few hours.

    A moist and unstable boundary layer will support a favorable
    thermodynamic environment for convection to attain at least some
    loose organization with multi-cell convective clusters likely to
    evolve. MLCAPE values are locally near 1000+ J/kg with PWs of 1.2
    to 1.5 inches in place, with the better moisture overall situated
    over western PA, central and southern OH and down into northern KY
    where the nose of weak low-level southwest flow is noted ahead of
    the aforementioned front.

    Rainfall rates should be capable of reaching up to as much as 1.5
    inches/hour based on the latest hires model guidance including the
    12Z HREF guidance and the 06Z REFS. Some briefing training of
    cells ahead of the aforementioned wave of low pressure will
    support the potential for some localized 2 to 3+ inch rainfall
    totals going through this evening. The antecedent conditions are
    relatively moist, and with some urban sensitivities, the potential
    will exist for isolated areas of flash flooding over the next
    several hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!92X5OdkD_LpeeDkSWUalgu-PqA03B-JHfHN9Zh4SBtSt38ie3CK6EjJ5vJLaAwO43Mg_= aeXqNuI-RhijdLsh58rlivM$ for graphic product...

    ATTN...WFO...BGM...BUF...CLE...CTP...ILN...IND...IWX...PBZ...
    RLX...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 42977618 42487514 41667559 40907790 39867899=20
    39278045 39048250 39208377 39688514 40438558=20
    41168451 41158203 41998019 42757809=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 5 20:15:38 2025
    AWUS01 KWNH 052015
    FFGMPD
    TXZ000-NMZ000-060213-

    Mesoscale Precipitation Discussion 0371
    NWS Weather Prediction Center College Park MD
    413 PM EDT Thu Jun 05 2025

    Areas affected...Southeast NM into Southwest and West-Central TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 052013Z - 060213Z

    SUMMARY...Development and expansion of supercell thunderstorms
    going into the evening hours will likely tend to be slow-moving
    and will be capable of producing locally enhanced rainfall totals.
    Generally isolated areas of flash flooding will be possible with
    this thunderstorm activity this evening.

    DISCUSSION...The mid-afternoon GOES-E GeoColor satellite imagery
    shows a well-defined surface boundary/weak front situated across
    portions of eastern NM out through west-central TX. A substantial
    amount of instability is pooling along this boundary, and recent
    satellite imagery is showing the development of an extensive CU
    field across southwest to west-central TX and back into southeast
    NM. Convection has already initiated over the Davis Mountains, and
    additional development and expansion of convection is expected
    more broadly across the region going into the evening hours.

    Modest shortwave energy shearing out across the southern High
    Plains along with a belt of stronger mid-level flow/shear will
    combine with strong instability for supercell thunderstorms to
    develop over the next several hours, with discreet cells
    eventually merging/consolidating for some MCS evolution by later
    this evening. MLCAPE values of 3000 to 4000 J/kg are in place with
    as much as 50+ kts of effective bulk shear across southeast NM and
    parts of southwest TX east of the dryline, and some additional
    surface heating over the next 1 to 2 hours will help to further
    destabilize the region along and south of the aforementioned
    surface boundary.

    Aside from severe hazards associated with the supercells, rainfall
    rates will be capable of reaching 2+ inches/hour, and with the
    slow cell-motions, and potential for cell-mergers in time, some
    rainfall amounts of 3 to 4+ inches will be possible. Consequently,
    this will support a threat for at least isolated areas of flash
    flooding heading into the evening hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Dlu7-n_CyUWXdWj45gNQdRYSuf0V3GpyXGBtxKhanVZocRmPjSY-3cI09jt_yQ-CSbr= iA1SwJKLkYWLJJgFusTcwlo$ for graphic product...

    ATTN...WFO...ABQ...LUB...MAF...OUN...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 34560326 34190189 34010023 33139963 32199989=20
    31340123 30450193 29630289 29670389 30270453=20
    30920443 32200431 33290457 34220427=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 5 21:33:46 2025
    AWUS01 KWNH 052132
    FFGMPD
    TXZ000-OKZ000-KSZ000-COZ000-NMZ000-060330-

    Mesoscale Precipitation Discussion 0372
    NWS Weather Prediction Center College Park MD
    531 PM EDT Thu Jun 05 2025

    Areas affected...Eastern CO...Southwest KS...OK/TX Panahandles

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 052130Z - 060330Z

    SUMMARY...Heavy showers and thunderstorms will be organizing and
    expanding in coverage over the next several hours, with eventual
    MCS development likely over the southern High Plains. Isolated to
    scattered areas of flash flooding will be possible as the storms
    grow upscale and produce heavy rainfall rates.

    DISCUSSION...The mid-afternoon GOES-E IR/WV suite shows the
    shearing out of mid-level shortwave energy across the central and
    southern High Plains in general, and this energy coupled with
    localized orographics and proximity of a front should favor the
    expansion of convection over the next several hours. Already the
    most recent visible satellite and radar imagery shows
    thunderstorms initiating over to the east of the Front Range and
    also farther off to the southeast over southeast CO and far
    southwest KS where there is an area of low pressure helping to
    drive stronger low-level moisture convergence.

    A nose of MLCAPE values reaching 1500 to 2500 J/kg is seen in the
    latest RAP analysis along with effective bulk shear values of 30
    to 50 kts. With additional boundary layer destabilization expected
    in the near-term over southeast CO adjacent areas of southwest KS
    and the OK/TX Panhandles, a general increase in the coverage of
    convection should tend to occur from northwest to southeast as
    convection near and over the terrain advances downstream into the
    strongly favorable thermodynamic and kinematic environment.

    Eventually by later this evening there should be an environment
    conducive for merging convective clusters which will include a
    combination of multi-cell and supercell thunderstorms, and this
    will likely promote a stronger MCS evolution that will impact
    areas of especially southwest KS. A strengthening nocturnal
    southerly low-level jet over the aforementioned the front by later
    this evening will be a key contributor to the eventual MCS
    evolution via certainly strong warm air advection and moisture
    transport.

    Rainfall rates of 1 to 2 inches/hour are expected with the
    stronger storms, and with cell-merger activity likely, some spotty
    2 to 3+ inch rainfall totals are expected over the next few hours.
    However, by later this evening, the latest hires model guidance
    led by the 18Z HREF and 12Z REFS supports areas of southwest KS
    seeing heavier totals of 3 to 5 inches given the level of MCS
    organization that is expected.

    Isolated to scattered areas of flash flooding will be possible
    regionally as the convection continues to initiate, organize and
    expand in coverage heading into the evening hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7GyJorGDAXsLro2QlqzyDpLlnFkaoqrlNJ8GO2YK5gABx-8csbLZXpbijfepe253NHNk= YRjCcP-XmUSnU-mxMoJC48g$ for graphic product...

    ATTN...WFO...ABQ...AMA...BOU...DDC...GLD...OUN...PUB...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 40330409 40270300 39860230 38920094 38089869=20
    36759876 36140040 36230243 36990391 38380521=20
    39870512=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 5 23:27:37 2025
    AWUS01 KWNH 052326
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-060400-

    Mesoscale Precipitation Discussion 0373
    NWS Weather Prediction Center College Park MD
    725 PM EDT Thu Jun 05 2025

    Areas affected...Southern NV...Northwest AZ...Southern
    UT...Extreme Eastern CA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 052325Z - 060400Z

    SUMMARY...Showers and thunderstorms will likely continue to
    persist over the next few hours across portions of southern NV,
    extreme eastern CA, northwest AZ and southern UT. Additional
    isolated areas of flash flooding will be possible going into the
    evening hours as a result.

    DISCUSSION...The late-afternoon GOES-W visible satellite imagery
    shows multiple convectively reinforced outflow boundaries
    impacting the Southwest from ongoing small-scale clusters of
    convection. One axis of well-defined CU/TCU and embedded CBs
    exists across southern UT and into southern NV, with another one
    farther south over northwest AZ near the Mogollon Rim and over to
    the CA/NV border.

    In between these two outflow boundaries which are both generally
    settling slowly southward, there continues to be the pooling of
    instability with as much as 1000 to 1500+ J/kg of SBCAPE. In fact,
    the latest 3-hourly SBCAPE differentials has been showing
    localized increases (400+ J/kg) in instability over northwest AZ.
    Recent IR satellite imagery has been showing some additional
    cooling of the convective cloud tops over southern NV in
    particular, and the latest RAP analysis has also been indicating
    some modest effective bulk shear parameters showing up as an
    elongated mid-level shortwave trough/shear axis approaches the
    region from the northwest.

    The combination of lingering diurnally enhanced instability along
    with cooling cloud top trends and the aforementioned mid-level
    trough approaching the region suggests that the ongoing convection
    should tend to persist for at least a few more hours. A
    combination of orographic ascent and some potential for these
    outflow boundaries to interact with one another may also support
    potential for renewed convective development in the near-term.

    Some additional 1 to 2+ inch rainfall amounts will be possible
    with the stronger storms, and given the sensitivities on the
    ground around some of the local slot canyon areas (especially
    southern UT) along with any burn scars and the normally dry
    washes, there may be some additional isolated areas of flash
    flooding this evening.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4EACyrEbdoZbe-Xky5uQLRI3Jh6lEAFYCcdlcZh1nNPFWpa9VeLqOIz1hLqet5IFYeri= l4TghF_hU00nM8zvC0kiztg$ for graphic product...

    ATTN...WFO...FGZ...GJT...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 38551154 38461017 37761018 37011142 36341169=20
    35631153 34821169 34591240 34781365 34851463=20
    34991553 35521592 36281597 37051578 37671515=20
    38061409 38361289=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 6 00:49:02 2025
    AWUS01 KWNH 060048
    FFGMPD
    WVZ000-060330-

    Mesoscale Precipitation Discussion 0374
    NWS Weather Prediction Center College Park MD
    847 PM EDT Thu Jun 05 2025

    Areas affected...much of WV

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 060045Z - 060330Z

    Summary...Localized rainfall rates of 1-2"/hr may lead to
    continued or additional isolated to widely scattered instances of
    flash flooding.

    Discussion...A cluster of thunderstorms have been persistent
    across portions of southern WV over the past 2-3 hours, forming on
    the higher elevations of the central Appalachians and propagating
    upwind (against weak 700 mb flow from the west) into the New River
    Gorge region. While radar data is limited (KRLX down for radome
    replacement), GOES-East is indicating impressive cooling cloud
    tops along the western flank of the cluster, suggesting slow
    moving convection could continue for at least a couple more hours.
    Localized rainfall rates of 1-2"/hr may lead to continued or
    additional isolated to widely scattered instances of flash
    flooding (given 1-hr and 3-hr FFGs generally ranging from 1.5-2.0"
    and 2.0-2.5", repspectively).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5GC8COBtwmE5uj1AbuaKYsrfzycwrlOisrtxlpr-IGIoYRyEf0_EqbDpJxe7PqNS0F8T= SRcDwfyMTCf8X--9MThGVw0$ for graphic product...

    ATTN...WFO...RLX...RNK...

    ATTN...RFC...TIR...NWC...

    LAT...LON 38468087 38388044 38088051 37738098 37618184=20
    37778223 37988212 38218179 38418130=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 6 01:55:14 2025
    AWUS01 KWNH 060153
    FFGMPD
    TXZ000-OKZ000-060600-

    Mesoscale Precipitation Discussion 0375
    NWS Weather Prediction Center College Park MD
    953 PM EDT Thu Jun 05 2025

    Areas affected...Rolling Plains into TX Big Country

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 060152Z - 060600Z

    Summary...Localized rainfall rates of 1-2"/hr may lead to
    continued or additional isolated to widely scattered instances of
    flash flooding.

    Discussion...An intense, long-lived supercell is maintaining very
    impressive structure following significant impacts to the Lubbock
    and surroundings (including tornadoes, extreme straight line
    winds, giant hail, and flash flooding). The large cell is tracking
    ESE at 10-15 kts (following the expected bunkers right-mover
    vector), and the environment downstream is characterized by MUCAPE
    of 3000-4000 J/kg, PWATs of 1.4-1.6 inches (near or above the 90th
    percentile, using AMA, MAF, and FWD as proxy sounding
    climatology), and 40-60 kts of deep layer (0-6 km) shear. The
    low-level jet is already providing moderate moisture transport and
    warm air advection (20-30 kts at 850 mb), and will only strengthen significantly (to 30-40 kts) over the next 2-3 hours.

    Going forward with a deep layer mean wind of 25-30 kts (towards
    ENE) near and downstream of the intense convection (and more than
    sufficient instability and shear), organization into a larger MCS
    is possible (and should easily be maintained per MCS maintenance
    probabilities of 80-90%). Very intense rainfall rates up to
    2-3"/hr (and 1" in as little as 15-min, per MRMS) may result in
    isolated to widely scattered instances of flash flooding. Short
    term localized totals should be limited to 2-4", given Corfidi
    vectors imply 30-35 kt forward speed. Should upscale growth into
    an MCS not occur, then localized totals up to 5" may be possible
    with a slower moving supercell.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8xYZwLgSrniEeAG8yTAPC9K-6DYZMtUwS7Ax4MNLef22hIh_TsnfJnLBX6RKETMYuNrs= 6JKUUPs_fsxP1GPl5rmDOhE$ for graphic product...

    ATTN...WFO...FWD...LUB...OUN...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 34400118 34350016 34139863 33549841 33069869=20
    32960025 33120157 33460207 33910218 34280180=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 6 03:49:33 2025
    AWUS01 KWNH 060349
    FFGMPD
    TXZ000-OKZ000-KSZ000-COZ000-NMZ000-061000-

    Mesoscale Precipitation Discussion 0376
    NWS Weather Prediction Center College Park MD
    1148 PM EDT Thu Jun 05 2025

    Areas affected...southern KS, northern OK, far north TX Panhandle

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 060400Z - 061000Z

    Summary...Localized rainfall rates of 1-2"/hr may lead to
    continued or additional isolated to widely scattered instances of
    flash flooding.

    Discussion...An intense, long-lived supercell is maintaining very
    impressive structure following significant impacts to the Lubbock
    and surroundings (including tornadoes, extreme straight line
    winds, giant hail, and flash flooding). The large cell is tracking
    ESE at 10-15 kts (following the expected bunkers right-mover
    vector), and the environment downstream is characterized by MUCAPE
    of 3000-4000 J/kg, PWATs of 1.4-1.6 inches (near or above the 90th
    percentile, using AMA, MAF, and FWD as proxy sounding
    climatology), and 40-60 kts of deep layer (0-6 km) shear. The
    low-level jet is already providing moderate moisture transport and
    warm air advection (20-30 kts at 850 mb), and will only strengthen significantly (to 30-40 kts) over the next 2-3 hours.

    Going forward with a deep layer mean wind of 25-30 kts (towards
    ENE) near and downstream of the intense convection (and more than
    sufficient instability and shear), organization into a larger MCS
    is possible (and should easily be maintained per MCS maintenance
    probabilities of 80-90%). Very intense rainfall rates up to
    2-3"/hr (and 1" in as little as 15-min, per MRMS) may result in
    isolated to widely scattered instances of flash flooding. Short
    term localized totals should be limited to 2-4", given Corfidi
    vectors imply 30-35 kt forward speed. Should upscale growth into
    an MCS not occur, then localized totals up to 5" may be possible
    with a slower moving supercell.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5GNsShYOcy1o0aN_bgDBMW5QiWfLgxD_VK2h4RiBkz2aACOyMAUNtIiVqSmJ-2cyF2IW= 6vLq3REsFw1Xml1Jl0oCt38$ for graphic product...

    ATTN...WFO...ABQ...AMA...DDC...ICT...OUN...PUB...SGF...TSA...

    ATTN...RFC...TUA...NWC...

    LAT...LON 37969709 37729516 36079494 35889720 35939925=20
    36100057 36190191 36360312 37140265 37430215=20
    37600157 37710067 37819968 37899853=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 6 10:01:04 2025
    AWUS01 KWNH 061001
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-061400-

    Mesoscale Precipitation Discussion 0377
    NWS Weather Prediction Center College Park MD
    600 AM EDT Fri Jun 06 2025

    Areas affected...central and northeast OK into far southeast KS,
    southwest MO, and northwest AR

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 061000Z - 061400Z

    Summary...A mature mesoscale convective system (MCS) and an
    associated mesoscale convective vortex (MCV) is producing
    1.0-2.5"/hr rainfall and may result in additional 3-5" through 9AM
    CDT. Isolated to scattered instances of flash flooding are likely.

    Discussion...An MCS has matured overnight and is progressing
    through northern and eastern portions of OK at this hour. Very
    heavy rainfall accompanies this MCS (1-2" hourly totals), and
    particularly so ahead and downstream of a distinct MCV over far
    northeast OK (up to 2.5" hourly totals and 15-min totals up to
    1.5", per MRMS estimates). While the 30-40 kt low-level jet that
    is driving moisture transport and lift is expected to rapidly
    weaken (to 25 kts or less) over the next several hours, these
    rainfall rates will likely result in continued/additional isolated
    to scattered instances of flash flooding (given 1-hr/3-hr FFGs as
    low as 1.0-1.5" and 2.0-2.5", respectively). SBCAPE of 500-2500
    J/kg, PWs of 1.5-2.0" (between 90th percentile to near record
    values, per OUN and SGF sounding climatology), and effective bulk
    shear of 35-55 kts will sustain the heavy rainfall in the short
    term. 06z HREF 40-km neighborhood probabilities indicate 40-50%
    chances for 2"/1-hr exceedance, and 30-60% odds for 3"/3-hr
    exceedance (maximized over far northeast OK into adjacent portions
    of AR/MO).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Q_1Afec7JjLm1l2-99c6epwv_EwRFvqAuTkkSCqyBK47VNLTtQVgwmAmrjXgaBP1k1A= fu5dsJ0zAZHF7x8rh1r0uGM$ for graphic product...

    ATTN...WFO...ICT...OUN...SGF...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 37749333 37409254 35909386 34559644 35189815=20
    35579807 36039772 36459722 36639679 37049616=20
    37249522 37339450 37419418=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 6 11:52:05 2025
    AWUS01 KWNH 061152
    FFGMPD
    NYZ000-PAZ000-MDZ000-WVZ000-OHZ000-KYZ000-061750-

    Mesoscale Precipitation Discussion 0378
    NWS Weather Prediction Center College Park MD
    750 AM EDT Fri Jun 06 2025

    Areas affected...Central Appalachians...Northern
    Mid-Atlantic...Southern NY State

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 061150Z - 061750Z

    SUMMARY...Scattered showers and thunderstorms will generally tend
    to expand in coverage by midday across the central Appalachians,
    the northern Mid-Atlantic, and southern NY state. At least
    isolated areas of flash flooding will be possible given heavy
    rainfall rates and locally wet antecedent conditions.

    DISCUSSION...The early morning GOES-E WV suite shows a fairly
    well-defined shortwave impulse advancing east through the upper OH
    Valley which will be crossing gradually into the central
    Appalachians and northern Mid-Atlantic by midday. This energy
    coupled with a quasi-stationary front and multiple waves of low
    pressure riding northeast along it is already producing some
    locally heavy showers and thunderstorms across far eastern OH, the
    northern WV Panhandle and far western PA.

    While instability is quite modest with only about 500 to 750 J/kg
    of MUCAPE in place where the axis of convection is occurring, the
    diurnal heating cycle by later this morning through midday will
    facilitate stronger boundary layer instability. This coupled with
    local orographics and differential heating boundaries, along with
    a weak upper-level jet streak (associated with the aforementioned
    shortwave trough) should support a gradual expansion of convective
    activity that will encompass the central Appalachians and stretch
    northeastward across the northern Mid-Atlantic and southern NY
    state.

    The PW anomalies early this morning are running about 1.5 standard
    deviations above normal with CIRA-ALPW data showing rather strong concentrations of moisture in the 850/500 mb layer ahead of the
    shortwave impulse. This coupled with the increasing instability
    over the next several hours should favor increasingly efficient
    rainfall rates that by later this morning may reach 1.5+
    inches/hour.

    Cell-motions are forecast to be relatively slow, and with some of
    the activity capable of briefly training over the same area, some
    3-hourly rainfall totals of as much as 2 to 3 inches will be
    possible. Given the locally wet antecedent conditions that are in
    place, these heavier rainfall rates/totals may cause at least some
    isolated ares of flash flooding and this will include some urban
    flooding impacts as well.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!798xh1S2gP6gCHqZ3AkX_KyB5LRMvFDM0VMTe9p5-yhhxBmmuicIRxmYyDnzfCPSpHlU= ixYigMV85kKOKE0Vb0KtBOw$ for graphic product...

    ATTN...WFO...ALY...BGM...BUF...CLE...CTP...ILN...LWX...PBZ... PHI...RLX...RNK...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 43127592 42817468 42037441 41467499 40477713=20
    39197893 37678073 37748220 38738324 39908286=20
    40858186 41888015 42747773=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 6 14:06:38 2025
    AWUS01 KWNH 061406
    FFGMPD
    ARZ000-TXZ000-OKZ000-061800-

    Mesoscale Precipitation Discussion 0379
    NWS Weather Prediction Center College Park MD
    1005 AM EDT Fri Jun 06 2025

    Areas affected...Southeast OK...Western and Central AR

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 061405Z - 061800Z

    SUMMARY...A strong and well-organized MCS will continue to
    southeast through areas of southeast OK and into western and
    central AR. Additional areas of flash flooding in association with
    this will be possible.

    DISCUSSION...A long-lived, but still potent MCS continues to
    advance across portions of the southern Plains and into adjacent
    areas of the lower and middle MS Valley. Cold convective tops
    continue across especially southeast OK and the airmass out ahead
    of the MCS cold pool/outflow boundary remains moderately unstable
    in an elevated fashion with MUCAPE values of a much as 1000 to
    2000+ J/kg. A southwesterly low-level jet on the order of 30 to 35
    kts continues to help favor a moderately strong axis of moisture
    transport up across the region as well extending from the Red
    River Valley up through portions of central and northern AR.

    The early morning hires guidance led especially by the HRRR seems
    to be weakening the overall organization of the MCS a bit too fast
    given the current character of the convective cloud top canopy,
    with the RRFS guidance a bit more persistence.

    Some gradual weakening as a whole is expected to the MCS by later
    this morning as the leading edge of the convection advances
    farther downstream. However, the southwest flank of the MCS over
    southeast OK and potentially into western AR is exhibiting
    increasing signs for cell-training in the short-term (next 2 to 3
    hours) which will allow for heavy rainfall rates of 1 to 2
    inches/hour to potentially result in some 3-hour totals of 2 to 4+
    inches through midday before eventually weakening.

    Additional areas of isolated to scattered flash flooding will
    continue to be possible at least through midday with the southwest
    flanking line of the MCS activity.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4cR7XrRLixdOE8bwdaWEDfi28Tfjs5GiCuLCgQ5mHwawRSNwrZfAgaV4ON2Xs0ZUlYP5= XyI_fnLbkvgmmWv--h8HxeM$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 35449329 35239193 34229199 33779312 33669544=20
    33989684 34639653 34929571 35099448=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 6 15:22:18 2025
    AWUS01 KWNH 061522
    FFGMPD
    OHZ000-TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-062120-

    Mesoscale Precipitation Discussion 0380
    NWS Weather Prediction Center College Park MD
    1121 AM EDT Fri Jun 06 2025

    Areas affected...Portions of the Middle MS and Lower OH Valleys

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 061520Z - 062120Z

    SUMMARY...Areas of heavy showers and thunderstorms are expected to
    generally persist and expand in coverage going through the
    mid-afternoon hours from south-central to southeast MO into
    southern IL, along with adjacent areas of far southern IN, much of
    KY, and far northern TN. Heavy rainfall rates of up to 2
    inches/hour and concerns for cell-training will likely result in
    at least scattered areas of flash flooding.

    DISCUSSION...The late-morning GOES-E Airmass RGB satellite imagery
    in conjunction with radar shows a strong MCV advancing through
    southwest MO in association with a long-lived MCS that is
    advancing well off to the east across areas of the southern Plains
    and lower to mid-MS Valley region. This MCV though is also
    associated with an area of surface low pressure along a
    quasi-stationary frontal zone draped west to east across southern
    MO and into adjacent downstream areas of the OH Valley. A separate
    wave of low pressure is also noted over southeast MO.

    The airmass pooling along this front over the lower OH Valley
    ahead of these waves of low pressure and the mid-level energy
    aloft is rapidly destabilizing with strong solar insolation and
    surface heating. Already there are MLCAPE values of 1500 to 2500+
    J/kg pooled across much of the Mid-South with a nose of this
    advancing up into western and central KY.

    Over the next several hours, some increase in a southwest
    low-level jet (reaching 30+ kts) is expected across southeast MO
    through at least far southern IL and into western KY as the
    upstream MCV and related wave activity arrives. This will set the
    stage for stronger low-level moisture convergence and forcing
    along the front for a more organized and concentrated threat of
    heavy rainfall. However, downstream areas of far southern IN, much
    of KY, and far northern TN will also have a likelihood for
    scattered clusters of convection as favorable upper-level jet
    support near the front along with the boundary layer
    destabilization works to promote convective development.

    The airmass is quite moist with PWs running around 1.5 standard
    deviations above normal, and the increase in instability with some
    moderately strong effective bulk shear values of 30 to 40 kts
    should favor enhanced rainfall rates of up to 2 inches/hour. The
    latest 12Z HREF guidance and recent RRFS solutions show rather
    strong support for 2 to 4 inch rainfall totals with locally higher
    amounts possible where areas of cell-training take place.

    Expect a likelihood for scattered areas of flash flooding to occur
    going through the mid-afternoon hours, and this will be aided by
    locally moist antecedent conditions.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8j-4NfWH1TEZK8GT-5S97TyhZIvz-fPospdI50ntTdDNXoeQ2dzGWu2zAd-IRbIo0dnx= LLlhbM2pc-6l_YiNRJIMAy0$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...JKL...LMK...LSX...LZK...MEG... MRX...OHX...PAH...RLX...SGF...

    ATTN...RFC...KRF...MSR...ORN...TIR...TUA...NWC...

    LAT...LON 38938567 38738312 37508282 36568430 36168812=20
    36229032 36499232 37009369 37649390 38049320=20
    38399116 38678906=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 6 17:22:13 2025
    AWUS01 KWNH 061722
    FFGMPD
    MEZ000-MAZ000-NHZ000-VTZ000-CTZ000-NYZ000-NJZ000-PAZ000-062320-

    Mesoscale Precipitation Discussion 0381
    NWS Weather Prediction Center College Park MD
    121 PM EDT Fri Jun 06 2025

    Areas affected...Much of Central and Eastern NY...Central and
    Southern New England

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 061720Z - 062320Z

    SUMMARY...Showers and thunderstorms with heavy rainfall rates will
    expand in coverage this afternoon across especially central and
    eastern NY through much of central and southern New England.
    Scattered areas of flash flooding are likely, some of which may be
    locally significant.

    DISCUSSION...The midday GOES-E visible satellite imagery shows
    cloud cover and showers advancing across areas of central NY in
    association with a shortwave impulse. This energy coupled with
    proximity of quasi-stationary front and a destabilizing boundary
    layer along it will promote developing and expanding coverage of
    heavy showers and thunderstorms this afternoon across much of
    eastern New York through central and southern New England.

    MLCAPE values have risen to as much as 1000 to 2000+ J/kg across
    southeast NY through central and western CT, and also up across
    central and western MA. A nose of lesser instability is focused
    north of here up across southern VT/NH as well. Additional
    destabilization is expected over the next couple of hours as
    strong diurnal heating continues ahead of the approaching upstream
    energy. This warm sector airmass is also quite moist with PWs of
    1.5 to 1.6+ inches in place, and this pooling of moisture will be
    supported through the afternoon by a gradual increase in southwest
    low-level flow ahead of the shortwave impulse and as a wave of low
    pressure develops and transits the front across the interior of
    the Northeast.

    The 12Z HREF and 06Z REFS guidance supports locally very heavy
    rainfall rates reaching upwards of 2 inches/hour, and with
    convection also become locally concentrated/focused near some of
    the higher terrain of central and southern New England and
    especially southern VT, southern NH, and western and central MA.
    Some portions of southwest ME also based on recent HRRR guidance
    gets into some locally stronger concentrations of convection by
    early this evening as well.

    Given the approaching upstream wave and level moisture and
    instability that is in place, broken coverage of heavy showers and thunderstorms are likely with high rainfall rates that will be
    capable of some cell-training. As much as 3 to 5+ inches will be
    possible near some of the orographically favored terrain including
    the southern portions of the Green and White Mountains on down
    into the Worcester Hills and Berkshires. Elsewhere, areas away
    from the terrain and back into areas of eastern NY including the
    Hudson Valley and adjacent Catskills may see as much as 2 to 4
    inches of rain where storms become locally focused.

    Given the overall setup, and the relatively moist antecedent
    conditions, these rains are likely to cause flash flooding by
    later this afternoon which will likely continue into a part of the
    early evening time frame. Some locally significant flash flooding
    will be possible where the heaviest totals focus near areas of
    higher terrain.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_5ccycjOXBLhqTswYilucbubqSyweK-dbeClSfUCcms6psvtKsCk_r6ro_0AlujYbKq4= moHn2fDj9h2GBC3QRNQpnZY$ for graphic product...

    ATTN...WFO...ALY...BGM...BOX...BTV...GYX...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 44777023 44316968 43836979 43477027 42487119=20
    41747225 41257376 41317472 41807536 42317540=20
    43007489 43387466 43967447 44287353 44377242=20
    44667142=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 6 18:17:39 2025
    AWUS01 KWNH 061817
    FFGMPD NYZ000-NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-DCZ000-WVZ000-OHZ000-KYZ000-07001=
    5-

    Mesoscale Precipitation Discussion 0382
    NWS Weather Prediction Center College Park MD
    216 PM EDT Fri Jun 06 2025

    Areas affected...Central Appalachians into the Northern
    Mid-Atlantic

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 061815Z - 070015Z

    SUMMARY...Showers and thunderstorms will continue to locally
    expand in coverage through the afternoon and early evening hours.
    Isolated to scattered areas of flash flooding are likely from
    heavy rainfall rates and locally wet antecedent conditions.

    DISCUSSION...The early afternoon GOES-E visible satellite imagery
    along with dual-pol radar shows scattered to locally broken areas
    of heavy showers and thunderstorms already impacting southeast OH,
    much of WV, western MD and also southwest to northeast PA. Strong
    boundary layer heating continues locally which has allowed for
    MLCAPE values to rise to as much as 1000 to 1500 J/kg, with the
    better instability noted across southeast PA through northern NJ.
    However, secondary areas of 1000+ J/kg CAPE values are also noted
    across the western slopes of the central Appalachians in the wake
    of earlier convection.

    Heavy showers and thunderstorms will generally continue to advance
    east off the terrain of the Appalachians and Blue Ridge over the
    next few hours and get into at least the Piedmont areas of the
    northern Mid-Atlantic. There are some question marks about the
    I-95 corridor where some pockets of larger scale subsidence are
    noted given proximity of a surface low center off the Delmarva,
    but as this low pulls away, and additional surface heating takes
    place over the next few hours, the I-95 corridor from northern VA
    through northeast MD, southeast PA, and into central and northern
    NJ may also get into these areas of thunderstorms. Radar imagery
    shows a band of strong thunderstorms with high rainfall rates
    focused from near Harrisburg, PA down through Martinsburg, WV, and
    this band is associated with some evidence of a weak MCV/shortwave
    impulse.

    Ongoing recover of instability farther west over the central
    Appalachians and the western slopes of the terrain is occurring
    out ahead of a cold front, but with additional upstream shortwave
    energy approaching along with the influence of orographics,
    convection will be reloading across these areas going through
    early this evening.

    Rainfall rates with the stronger storms across the entire region
    will likely be 1 to 2 inches/hour, but with some additional spotty
    rainfall totals of as much as 2 to 3 inches going through early
    this evening. Given the impacts over areas that are already very
    moist on the ground, and also the concern for some urban impacts,
    isolated to scattered areas of flash flooding will generally be
    likely.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7mz0OZtuNSlhagVe1Mni9j0Yb8V2ZrpBiRGIRUqIZzkSOPuBHLPYm6d7xOoThzzJ42Dh= QwNakitSH09JOftHuUGCkyg$ for graphic product...

    ATTN...WFO...BGM...CLE...CTP...ILN...JKL...LWX...OKX...PBZ... PHI...RLX...RNK...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 41987566 41777473 41327390 40537389 39747517=20
    38767691 38047841 37438006 37228239 38398348=20
    39318287 40188147 41358002 41737872 41957725=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 6 21:32:15 2025
    AWUS01 KWNH 062132
    FFGMPD
    VAZ000-NCZ000-GAZ000-TNZ000-KYZ000-INZ000-070250-

    Mesoscale Precipitation Discussion 0383
    NWS Weather Prediction Center College Park MD
    531 PM EDT Fri Jun 06 2025

    Areas affected...Kentucky and Tennessee

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 062130Z - 070250Z

    SUMMARY...Additional rounds of heavy thunderstorms will shift east
    over Kentucky and much of Tennessee through this evening. Heavy
    rainfall rates of up to 2 inches/hour from repeating and merging
    cells makes a likely risk for flash flooding.

    DISCUSSION...A mesolow over western KY is accompanied by merging
    lines of heavy thunderstorms with additional scattered storms over
    central TN. This activity will continue to shift east in broad
    zonal flow with a noted impulse in water vapor imagery over
    western KY/TN. A separate wave of low pressure is along the a
    frontal boundary over southern MO.

    Low level WSWly flow around 20kt is maintaining elevated moisture
    with 2" PW (2 sigma above normal) pooled over western KY through
    central TN. Ample instability is present with MLCAPE of 1000-2000
    J/kg along and south of this moisture pool. The activity has
    become more perpendicular to the mean layer Wly flow, but new
    development ahead of the lines is allow for localized repeating
    cells. Enhanced rainfall rates of up to 2"/hr can be expected to
    continue which is in agreement with recent HRRR and RRFs runs.
    Localized rainfall of 2 to 4 inches is likely through 03Z with
    flash flooding considered likely.

    Recent development trends have generally been south of central KY
    which saw 1-2.5" rainfall this afternoon and is more vulnerable
    than the rest of the outlook area. There is a threat for isolated
    activity overnight, so further discussion may be needed for
    portions of the TN valley overnight.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8FQxpadhGXAguxseYKREE9hrczE6KG7MCj3tgouXcy0rZ6-XG_q6-dfpCiJ8_VAJ9CSN= MJW2tRm_ms1VrDAghDF7tW0$ for graphic product...

    ATTN...WFO...GSP...HUN...JKL...LMK...MEG...MRX...OHX...PAH...
    RLX...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 38098549 37638323 36618183 36058235 34998473=20
    35498785 36358851 37248789 37918737=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 6 22:30:15 2025
    AWUS01 KWNH 062230
    FFGMPD
    TXZ000-OKZ000-NMZ000-070428-

    Mesoscale Precipitation Discussion 0384
    NWS Weather Prediction Center College Park MD
    629 PM EDT Fri Jun 06 2025

    Areas affected...West Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 062228Z - 070428Z

    Summary...Supercells continue to develop over West Texas this
    evening with slow motion and repeating activity brings rainfall
    rates up to 2"/hr which should cause scattered instances of flash
    flooding, particularly for areas impacted by the storms last
    evening.

    Discussion...Scattered supercells will continue to develop along a
    surface trough set up west to east over the Caprock and through
    the Lubbock metro area. There is a notable risk for intense,
    long-lived supercells, much like last night in this same area due
    to an environment with SBCAPE of 4000+ J/kg, PW 1.4-1.6 inches
    (near or above the 90th percentile), and 50-60 kts of deep layer
    (0-6 km) shear. Low-level Sly flow of 15kt is providing fresh
    inflow which will only increase overnight as it intensifies into a
    low-level jet.=20

    Recent HRRRs are much to late with development in this area, but
    the RRFs is much more energetic and decent with the current
    depiction. The 6hr QPF from the RRFS is 2-4" in this west-east
    corridor and helps form the basis for this discussion (along with
    upscale growth to existing cells at this time. Congealing activity
    should allow for repeating heavy rain while upwind propagation
    should allow for longer duration of heavy rain. It is worth noting
    that giant hail is also a risk with this activity. Very intense
    rainfall rates up to 2-3"/hr would result in scattered flash
    flooding, particularly for urban environments like Lubbock and
    where the storms tracked last night which also intersected
    Lubbock. Scattered instances of flash flooding are considered
    likely for the outlook area.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6zXfNsLIhodgd1bjGIvbFLlLbW02M-SSlkggH4c89nFuWDKIsQ7c1rhjefzPO8hyVDRi= KPITkNfTrqALc1HKT5MIBQ0$ for graphic product...

    ATTN...WFO...ABQ...FWD...LUB...MAF...OUN...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 34320156 34329887 33109866 32820029 33150318=20
    34090327=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 6 23:15:28 2025
    AWUS01 KWNH 062314
    FFGMPD
    MEZ000-MAZ000-NHZ000-RIZ000-CTZ000-070230-

    Mesoscale Precipitation Discussion 0385
    NWS Weather Prediction Center College Park MD
    713 PM EDT Fri Jun 06 2025

    Areas affected...New England

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 062312Z - 070230Z

    SUMMARY...Heavy thunderstorms will continue to move east over
    mainly interior sections of New England this evening before
    dissipating near the coast. Further localized flash flooding is
    possible through 03Z.

    DISCUSSION...Narrow swaths of elevated instability (SBCAPE
    1500-2000 J/kg) persist east of a frontal zone and inland from the
    coast where a cool breeze has set up. Southerly flow ahead of the
    fronts is reinforcing moisture with PW up to 1.6". Recent HRRR and
    RRFS runs quickly diminish the activity shortly after 00Z, but the
    presence of the instability, particularly over interior CT and up
    the I-95 corridor into Maine warrants an additional note beyond
    the main period of flooding that occurred this afternoon over New
    England terrain back toward the Hudson Valley. Recent IR satellite
    scans do show a warming trend to cloud tops, so perhaps that trend
    will indeed continue as CAMs suggest. Still, an additional 2" is
    possible in places through this evening which could cause further
    localized flash flooding.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4rZ0-JSek5Xpjd9TQc0Ym3yvIk9yn3tkSyuGjijssjIVEIjOag1g11hI452845mxVbjK= PDclfzCmDw_6GhAqtkLwWx4$ for graphic product...

    ATTN...WFO...ALY...BOX...GYX...OKX...

    ATTN...RFC...TAR...NWC...

    LAT...LON 44867032 44556945 43857030 43077079 42557106=20
    42157137 41677169 41387308 41717323 42997172=20
    44347091=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 7 00:04:41 2025
    AWUS01 KWNH 070004
    FFGMPD
    TXZ000-OKZ000-KSZ000-COZ000-NMZ000-070602-

    Mesoscale Precipitation Discussion 0386
    NWS Weather Prediction Center College Park MD
    804 PM EDT Fri Jun 06 2025

    Areas affected...South-Central High Plains

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 070002Z - 070602Z

    Summary...Scattered supercellular activity over southeast Colorado
    into the Oklahoma Panhandle is expected to develop into a
    mesoscale convective system (MCS) rest of this evening and track
    southeast overnight. The flash flood threat will increase with
    this development, particularly as it crosses areas in southern
    Kansas which saw heavy thunderstorms last night. Localized flash
    flooding is likely through 06Z.

    Discussion...Supercells in southeastern CO have developed in a
    high shear (60kt 0-6km Bulk Shear)/moderate instability (1500-2000
    K/kg SBCAPE) environment. Further development between the two main
    cells just prior to 00Z is an indication of the expected MCS
    development tonight. The right side of this developing MCS will
    cross areas impacted by heavy rain this afternoon from a cell
    currently in the OK Panhandle and activity from last night over
    southern KS.

    Ample moisture is present in CO downstream of this activity with
    PW around 1". Further moisture will be provided as it moves into
    KS from the nocturnal low-level jet which the development should
    turn south into in spite of deep layer westerly flow in an overall
    zonal flow pattern over the central U.S. Heavy rainfall is
    expected with 1-2" hourly totals, and particularly where flanking
    axes become repetitive. Antecedent wet soils are present over
    southern KS and far southeast CO where heavy rain has fallen over
    the past day.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5_nt5J6gdwMbRU_hgYii8lGfh4lqFwwKzhYBStZmzUQSn6rM0dz7ZqRfMmLhPC4j7ZnU= dEU3ajBJ-etnE2rfdEEh_R0$ for graphic product...

    ATTN...WFO...ABQ...AMA...BOU...DDC...GLD...OUN...PUB...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39400205 38889968 37839869 35609888 36120083=20
    37030343 37650430 38700390 39310290=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 7 00:31:53 2025
    AWUS01 KWNH 070031
    FFGMPD
    WVZ000-OHZ000-KYZ000-INZ000-070600-

    Mesoscale Precipitation Discussion 0387
    NWS Weather Prediction Center College Park MD
    830 PM EDT Fri Jun 06 2025

    Areas affected...Central Ohio Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 070029Z - 070600Z

    SUMMARY...Slow moving rounds of heavy rain is expected to keep
    shifting east along a stalled frontal boundary from southern
    Indiana through the Cincinnati metro area this evening. Localized
    flash flooding is possible.

    DISCUSSION...A shortwave impulse in zonal flow will continue to
    shift east over the central Ohio Valley this evening. Deep layer
    WSWly flow will keep activity moving parallel to a stationary
    front draped just north of the Ohio River. Elevated moisture will
    be maintained with 1.75" PW (2 sigma above normal) with sufficient
    instability (SBCAPE around 1000 J/kg). Enhanced rainfall rates of
    up to 1.5"/hr can be expected to continue which is in agreement
    with recent HRRR and RRFS runs. Localized rainfall of 2 to 4
    inches is possible through 06Z with flash flooding considered
    possible.

    Much of this area has not received rainfall over the past day.
    However, the slow moving nature of this activity and the potential
    for another round overnight makes for a possible flash flood
    threat.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7wjxWFx4wU4ASYrmtvBUXoMmZTVDIhs-obdZ7RzOigFLwde2FsBUDyBnsnOUxthXUl73= jAjoPwvdteXb-yKcIRDvseM$ for graphic product...

    ATTN...WFO...ILN...IND...JKL...LMK...RLX...

    ATTN...RFC...TIR...NWC...

    LAT...LON 39618210 39018182 38548236 38328325 38298428=20
    38588585 39498581 39578437=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 7 04:52:17 2025
    AWUS01 KWNH 070451
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-KSZ000-070930-

    Mesoscale Precipitation Discussion 0388
    NWS Weather Prediction Center College Park MD
    1251 AM EDT Sat Jun 07 2025

    Areas affected...Southern KS...Far northwest TX
    Panhandle...Northern & Central OK...Adj SW MO/NW AR...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 070450Z - 070930Z

    SUMMARY...Expanding convective coverage as clusters grow upscale
    into a quick moving MCS. Sub-hourly 1-1.5" with potential for
    some repeating on southern flank results in scattered spots of
    3-4" totals. Given saturated grounds, localized incidents of
    flash flooding are likely.=20

    DISCUSSION...GOES-E 10.3um and RADAR mosaic depict multiple
    clusters of severe thunderstorms across portions of the eastern TX
    panhandle and west-central OK in advance of expanding linear
    convective complex across SW KS into the OK Panhandle. The latter
    has quick momentum at the leading edge of stronger larger scale height-falls/solid DPVA across N KS at the right entrance of an
    expanding/jet streak that is already 90kts across NEB at 300mb.=20
    The combination is providing very strong dynamic ascent and
    evacuation for developing convective line and MCV across
    west-central KS. As such strong WAA has been over-spreading much
    of OK into S KS from untapped very unstable environment with 3000
    J/kg of MLCAPE. The strong WAA at the nose of a broad weakly
    veered 25-30kt LLJ is providing the solid isentropic
    ascent/moisture convergence along a lingering deep layer moisture
    pool in OK which is sparking pre-linear MCS thunderstorms.

    With very broad up/downdraft channels and ample 2" total PWats,
    cells are becoming very efficient rainfall producers as severe
    capabilities slowly diminish. Sub-hourly totals of 1-2" have been
    observed even though deep layer steering allows for some
    progressive forward motions. These cells are setting the stage
    and further moistening the upper-layers of an already fairly
    saturated grounds, especially east of I-35. So it is possible
    even these pre-cursory cells may result in localized flash
    flooding conditions prior to the main line. Additionally,
    proximity to the southern edge of the moisture/instability, may
    allow for a favored alley for training given shifting too far
    south may see greater dry/stable air ingestion and favoring
    maintenance north of the gradient in south-central OK.

    RADAR trends show, strong vertical ascent along the leading edge
    of the linear complex into Pawnee/Stafford county KS, potentially
    further developing to edge of 700mb WAA ascent band north of the
    Flint Hills in east-central KS. Strengthening MCV under
    aforementioned strong upper-level support will allow for increased back-shearing of the complex with favorable mid-level inflow jet
    likely helping to maintain broad moderate shield precipitation in
    the northern rotor of the MCS near the MCV for prolonged moderate
    rainfall as well across central KS. However, increasing concern
    is along the southern rotor of the MCS where forward propagation
    vectors will be slightly reduced allowing for increased orthogonal
    exposure to the broad southerly LLJ. As such, flanking cells will
    have a greater potential for training but also having best
    moisture/instability flux for strongest updrafts capable of 2"/hr.
    This may result in a streak/swath of enhanced rainfall totals of
    3-4" across northeast TX panhandle and likely along/north of I-40,
    but with solid DPVA/expanding WAA, MCS will expand for broader
    area of enhanced rainfall potential into Northeast OK and
    eventually southwest MO/NW AR toward 10z. Forward propagation
    will likely limit significant totals but spots of 3-4" in less
    than 3hrs will exceed FFG values over this saturated ground (RSM
    0-40cm of 70-75%). As such, flash flooding is considered likely
    overnight.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5I4C4LpHxwRchMU4c7SmFWnpCtDN4OzEKtky1simUCjW2x-FINgi_FKB5BzLvcftTdbV= i3DYpwOpt3uWs3Aw-pqPHs0$ for graphic product...

    ATTN...WFO...AMA...DDC...ICT...OUN...SGF...TOP...TSA...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 38609681 38359567 37859488 37479445 36779412=20
    35649436 35079520 34889646 34919786 35029913=20
    35320023 36470222 37080177 37659982 38399875=20
    38579789=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 7 05:36:14 2025
    AWUS01 KWNH 070536
    FFGMPD
    VAZ000-WVZ000-OHZ000-KYZ000-INZ000-071100-

    Mesoscale Precipitation Discussion 0389
    NWS Weather Prediction Center College Park MD
    135 AM EDT Sat Jun 07 2025

    Areas affected...Southern OH...Central to Northeast KY...Much of
    WV...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 070535Z - 071100Z

    SUMMARY...Shallow but efficient slow moving cells capable of
    1.5"/hr with some potential repeating may result in widely
    scattered localized flash flooding conditions overnight.

    DISCUSSION...GOES-E WV suite depicts a broad west to east
    shortwave feature crossing near Cincinnati, OH with favorable
    vorticity advection supporting a weak surface to boundary layer
    wave in southeast OH along/south of a stagnant stationary front.=20
    Ample low level moisture in the mid to upper 60s and spots of low
    70s, while CIRA LPW shows a ribbon of enhanced moisture
    along/ahead of this wave bringing nearly moist/saturated profiles
    to support 1.75" total PWats. Some weak remaining unstable air
    remains with 250-500 J/kg of SBCAPE in the vicinity of the Ohio
    River and southward into eastern KY. As such, RADAR and 10.3um
    IR loop shows a few very shallow cells along of the wave in S OH
    as well as back in the trailing trof of the mid-level wave
    along/east of Louisville, KY.

    While weak, there are pockets of enhanced moisture convergence in
    the 10-15kts of veered low level flow to tap the weak instability.
    With the shallow updrafts, all of it are within the warm cloud
    layer, will result in highly efficient tropical like showers.=20
    Rates of 1.5-1.75" could be common over highly focused fairly
    narrow updrafts. The concern is the overall deep layer steering
    is unidirectional nearly west to east which also will contribute
    to an upslope component across E KY/WV over the next few hours.=20=20
    As such, narrow streaks of hour or two of training may support
    localized streaks of 1.5-2.5" over 1-3hrs across the area of
    concern. Given complexity of terrain, recent above average
    rainfall over S OH, N WV and soil saturation ratios in the 60-70%
    and isolated incident or two of flash flooding will continue to be
    possible through the overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!59vH941tSJub9Q0Hco0lIqH8JQrs_JYVtp37Tv6h1KkPWHWoyxJk2MmeOvpn834-6F0m= JGR5pOxnYEO2HjbwqKO0acY$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...PBZ...RLX...

    ATTN...RFC...TIR...NWC...

    LAT...LON 39707997 39537964 39197955 38677987 38038101=20
    37448208 36808358 36908489 37528538 38118588=20
    38538544 38698469 38838412 38988358 39258270=20
    39598157=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 7 07:36:14 2025
    AWUS01 KWNH 070736
    FFGMPD
    TXZ000-OKZ000-NMZ000-071130-

    Mesoscale Precipitation Discussion 0390
    NWS Weather Prediction Center College Park MD
    335 AM EDT Sat Jun 07 2025

    Areas affected...Texas Panhandle into Northwest Texas...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 070735Z - 071130Z

    SUMMARY...Persistent repeating convection tracking across similar
    areas of heavy rain/saturated grounds suggests possible flash
    flooding to continue for the next few hours.

    DISCUSSION...GOES-E and AMA/LBB RADAR mosaic show continued solid
    convective activity of elevated thunderstorms with some broader
    stronger rotating updrafts from Lamb to Cottle county Texas.=20
    Solid 925-850mb veered LLJ at 35-45kts from southeast to southerly
    continue to ascent across a similarly flat west to east outflow
    boundary a few counties south from earlier convection, continuing
    to be reinforced by the ongoing activity. This shallow cold pool
    continues to provide sufficient isentropic ascent and speed
    convergence to maintain moisture/instability flux to the line of
    cells. Recent 10.3um EIR loops has shown solid uptick in
    convective vigor, cloud top cooling and hard/bumpy tops suggestive
    of strengthening rainfall potential to accompany severe risks.=20

    Given deep layer steering flattens from just above 700mb and slows
    to 20-30kts, rainfall duration is starting to aid in overall
    rainfall accumulation over the last hour or two. Rates of 1.5"/hr
    given western edge of fairly deep layer moisture availability and
    flux; translating over similar 1hour FFG values in the 1-1.5"/hr
    range due to last few days, suggests additional spots of 2-3" over
    the next 3 hours may result in additional flash flooding incidents.

    GOES-E 7.3 Low-Level WV animation shows a weak circulation over
    northeast NM, with tightening temperature gradient likely in
    response to some outflow/gravity waves coming off active
    convection along the flanking line of the complex across the
    northern Panhandle. This tightening with further steepening of
    the lower level isentropes/frontal zone and in proximity of a well
    of enhanced capped MLCAPEs to 2500 J/kg, has seen newer convection
    develop along the NM/TX border. While this development isn't
    ideally aligned with convective line to the south, further
    expansion (and tendency to propagate south given undercutting
    outflow from the north) suggests training/potential for 1.5"/hr
    and spots of 2"+ totals in short-duration is expanding toward the
    northwest in the TX panhandle and adjacent NM...nearly ideally
    aligned with the localized minimum in FFG values. Further
    expanding the area of possible flash flooding incident or two over
    the next few hours.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-d-IaLsFNUx94p1dzDGfOQAmdwik4IpghVyekpdHzelC4gV_m_FkCVj5BegkKtTFJEWA= V8y_c2howmXpxPCgZxb5dYQ$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...OUN...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35600270 35380195 34429971 33979844 33519853=20
    33429969 33580147 33770223 34090277 34540311=20
    35380356=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 7 08:53:18 2025
    AWUS01 KWNH 070853
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-071430-

    Mesoscale Precipitation Discussion 0391
    NWS Weather Prediction Center College Park MD
    452 AM EDT Sat Jun 07 2025

    Areas affected...Northern AR...Northeast OK...Far Southeast
    KS...Southwest MO...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 070850Z - 071430Z

    SUMMARY...Progressive MCS with broad warm advective thunderstorms
    downstream should support opportunities for multiple rounds of
    heavy rainfall with rates up to 2"/hr and totals of 2-4" resulting
    in possible incidents of flash flooding.

    DISCUSSION...Mature MCS continues to race east-southeastward
    across the Flint Hills of south-central KS with very strong
    dynamics aloft to help maintain it as it progresses into the Ozark
    Plateau. Very strong divergence aloft within the right entrance
    to dual jet structure aloft along with latent heat release will
    continue support strong mid-level cyclogenesis. In response, VWP
    networks shows broad strengthening of the LLJ with solid veering
    through 700mb and winds of southwesterly components to over 30kts
    through depth continuing to advect very unstable (2500-3000 J/kg
    of MUCAPE) while also pooling deep layer moisture along the
    southeast quadrant of the MCV to 2-2.1".=20

    Given the cyclonic/isallobaric component, winds are also very
    convergent to support high moisture flux along and downstream of
    the MCV track. Currently, warm advective cells have developed well
    into north-central AR with rates of 1.5"/hr well in advance of the
    cells near the center with rates likely to be over 2"/hr. While
    cells along the effective warm front are moving more
    east-northeast relatively and are not ideally training with
    occasional breaks in intense rainfall rates; there will be
    multiple periods of heavy rainfall before capping it off with the
    cells near the effective triple point, followed by an hour or so
    of moderate broad shield precipitation. This will allow for a
    broad area of 2-3" totals across the 4 state corners into
    north-central AR toward 12z. Isolated spots on the line with
    greatest duration/intensity will likely see 3-4"+ totals and
    likely will drive incidents of flash flooding through daybreak.
    While the hydrology gets better further east toward the MS River
    Valley, the MCS is likely to maintain with similar rates/totals
    though incidents of flash flooding are more likely to be more
    scattered in nature relative to upstream in the Ozark Plateau

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6s5mozbPeAO_cwTyadC7xPFNKgZNLWZQOtaumSuz6qzi1-OppzHI007WRuOTKPUN1X-r= GFuJx7LH4R-ltfZZa-9EYrc$ for graphic product...

    ATTN...WFO...ICT...LZK...MEG...SGF...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 37829556 37749422 37409320 36989210 36529119=20
    36069049 35279033 34619113 34899383 35579612=20
    36369659 37289636=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 7 11:01:47 2025
    AWUS01 KWNH 071101
    FFGMPD
    MAZ000-NHZ000-VTZ000-CTZ000-NYZ000-NJZ000-PAZ000-071600-

    Mesoscale Precipitation Discussion 0392
    NWS Weather Prediction Center College Park MD
    701 AM EDT Sat Jun 07 2025

    Areas affected...Northeast PA...Central and Eastern NY...Central
    and Southern New England

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 071100Z - 071600Z

    SUMMARY...Broken areas of heavy showers and a few thunderstorms
    will continue through the morning hours across areas of northeast
    PA into eastern NY, and eventually spreading into parts of central
    and southern New England toward midday. Additional areas of flash
    flooding are likely given locally sensitive antecedent conditions.

    DISCUSSION...Recent cloud-top cooling is noted with a broken area
    of heavy showers and a few thunderstorms impacting areas of
    northeast PA into central and eastern NY. The activity is being
    focused by a shortwave impulse advancing into the Northeast out
    ahead a larger scale trough lifting through the OH Valley and
    central Appalachians. This energy is also interacting with a
    quasi-stationary front and helping to focus a wave of low pressure
    which is promoting isentropic ascent and frontogenetical forcing
    near the front for the locally heavier and concentrated areas of
    rainfall.

    Despite very modest instability profiles with only about 250 to
    500 J/kg of MUCAPE value, the vertical column is quite moist with
    PWs running a solid 1.5 standard deviations above normal, and
    CIRA-ALPW data showing strong concentrations of mid-level
    moisture. The recent cloud-top cooling suggests the current
    activity will likely continue in the near-term, and the latest
    upper-air analysis is showing some improving right-entrance region
    upper-jet dynamics over the region for ascent. This will
    compensate for the lack of instability over the next few hours and
    continue to favor at least broken ares of highly efficient
    rainfall and elevated rain rates.

    Rainfall rates may reach as high as 1.5 inches/hour with the
    strong convective cores, and with relatively slow cell-motions,
    some short-term rainfall rates at least by late-morning may reach
    2 to 3+ inches. While the activity over the next few hours will
    tend to be more focused over areas of eastern NY and down into the
    Poconos of northeast PA, areas of central and southern New England
    will also begin to see a threat of heavy rainfall by midday.

    The antecedent conditions in general across the region are rather
    sensitive, with locally elevated streamflows, and thus with the
    additional rainfall this morning, there will likely be concerns
    additional areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5byJrrhyihI_a7_sUgyPqnZphiL7rSTIMnzasNVARuOilsnneAjMY8B_nQFx7ZhfhcxK= dVmbZpCCR1-ywu3PtM0TwNw$ for graphic product...

    ATTN...WFO...ALY...BGM...BOX...BTV...GYX...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 43717394 43387208 42417198 41757275 41277372=20
    41067522 41777632 42897584=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 7 14:33:51 2025
    AWUS01 KWNH 071432
    FFGMPD
    MOZ000-KSZ000-NEZ000-071930-

    Mesoscale Precipitation Discussion 0393
    NWS Weather Prediction Center College Park MD
    1031 AM EDT Sat Jun 07 2025

    Areas affected...Far Southeast NE...Northeast KS...West-Central
    and Northern MO

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 071430Z - 071930Z

    SUMMARY...Concentrated areas of heavy showers and thunderstorms
    will be dropping down across northeast KS and into areas of
    west-central and northern MO over the next few hours with some
    gradual expansion in coverage. Areas of flash flooding will be
    possible which will include an urban flooding threat to the Kansas
    City and St. Joseph metropolitan areas.

    DISCUSSION...A well-defined and relatively compact shortwave
    trough ejecting east-southeast across southeast NE this morning is
    expected to gradually advance down across far northeast KS and
    northern MO going through the early afternoon hours. The dynamical
    nature of this system interacting with modest instability with
    MUCAPE values of 500+ J/kg should favor at least a sustenance of
    the current activity.

    However, as the diurnal heating cycle ensues over the next several
    hours, there will be downstream areas of especially west-central
    and northern MO that destabilize which will favor an environment
    conducive for convection to expand in coverage. This will further
    be facilitated by low-level convergence near a well-defined low
    center over northeast KS and also with a reloading/strengthening
    of a synoptic scale front across the region.

    The environment on a concentrated basis with the shortwave energy
    is rather moist and efficient, and rainfall rates with the
    convection over the next few hours should be rather high and
    capable of reaching 1.5 to 2 inches/hour. Given the rather slow
    cell-motions that are currently seen in radar imagery, some
    rainfall totals going through early this afternoon may reach 3 to
    4+ inches.

    This will tend to support a concern for some areas of flash
    flooding in a general sense, however, these heavy rains are likely
    to impact the Kansas City and St. Joseph metropolitan areas as
    well. Thus, there will also be an urban flooding threat over the
    next few hours as the heavier showers and thunderstorms arrive.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-X7SFVaQvKYZCM-h07XlCsRA3Q5DUXj73aoO9iF0cnj1ZJZ4ZMpSaKIeb0iD11IUc6qO= qiQyuFa8Z8-HPgrIjgCZE8g$ for graphic product...

    ATTN...WFO...EAX...LSX...OAX...SGF...TOP...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 40569574 40379385 39949208 38989191 38449300=20
    38669514 39329625 40049655=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 7 16:03:55 2025
    AWUS01 KWNH 071602
    FFGMPD
    MEZ000-MAZ000-NHZ000-RIZ000-VTZ000-CTZ000-NYZ000-NJZ000-PAZ000-072200-

    Mesoscale Precipitation Discussion 0394
    NWS Weather Prediction Center College Park MD
    1200 PM EDT Sat Jun 07 2025

    Areas affected...Far Northeast PA...Northern NJ...Southeast
    NY...Central and Southern New England

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 071600Z - 072200Z

    SUMMARY...Heavy rainfall will continue to overspread much of the
    northeast Mid-Atlantic region into central and southern New
    England going through the mid to late-afternoon hours. This will
    include some locally more concentrated areas of stronger
    thunderstorm activity with higher rainfall rates. Areas of flash
    flooding are likely considering the very moist and locally
    saturated soil conditions.

    DISCUSSION...An expansive axis of heavy rainfall in a southwest to
    northeast fashion continues to advance across southeast NY and
    into central and southern New England. The activity which includes
    some occasionally stronger thunderstorm activity continues to be
    strongly supported by an ejecting shortwave trough and associated
    wave of low pressure which is transiting a well-defined frontal
    zone across the Northeast.

    The latest GOES-E IR/WV satellite imagery shows an excellent
    corridor of upper-level jet divergence/forcing over especially
    central and southern New England with an expansive axis of cooling
    cloud-tops over the region. There continues to be a low-level
    frontogenetic response to this with the axis of heavy rainfall
    which has been very efficient this morning. Shallow, warm
    convective tops and frontogenetical forcing in the lower to
    mid-levels of the column have been yielding warm rain processes,
    and this showed up well in the 12Z ALY RAOB sounding which
    depicted a deep moist column with a tall/skinny CAPE profile.

    There should be a gradual uptick in the overall convective
    footprint of the heavy rainfall this afternoon across especially
    southern New England including the Boston, MA to Hartford, CT
    corridor and potentially edging south to near the New York City
    metropolitan area and adjacent areas of northern NJ by late
    afternoon. This will be supported by convergence along the
    aforementioned frontal zone, but also with an increase in
    diurnally driven instability. Cloud cover will tend to mitigate
    the amount of surface heating that does occur, but with an already
    very moist column, and the aforementioned low-level and
    upper-level support, there should be a gradual expansion of
    heavier showers and thunderstorms over the next several hours.

    Rainfall rates may reach as high as 1.5 inches to 2 inches/hour
    with the stronger cells, and the locally slow cell-motions and
    pockets of at least brief cell-training may support some totals by
    early this evening that reach 3 to 4+ inches. This is supported by
    the 12Z HREF and 06Z REFS guidance.

    The antecedent conditions are quite sensitive over the higher
    terrain of southern VT, southern NH and through central and
    western MA. Runoff here over the next few hours may be enhanced
    given the additional rains, and gradually heavier rainfall rates
    farther south and east may pose some urban flooding concerns.
    Overall, on a regional level, areas of flash flooding are likely.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4zyz2fNHQrNj5-6EzBlPX724UItKVK7zzsMlO1CFZPtKu2WHTKPaxkPDObDlKf4Rr6AK= yZUqQEvVW1o4fjPFj3TO9ss$ for graphic product...

    ATTN...WFO...ALY...BGM...BOX...BTV...GYX...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 44607027 44566903 43996893 42937041 41747132=20
    41217275 40987314 40527430 40537520 41047545=20
    41917467 42717390 43727193=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 7 16:06:51 2025
    AWUS01 KWNH 071606
    FFGMPD
    MEZ000-MAZ000-NHZ000-RIZ000-VTZ000-CTZ000-NYZ000-NJZ000-PAZ000-072200-

    Mesoscale Precipitation Discussion 0394
    NWS Weather Prediction Center College Park MD
    1206 PM EDT Sat Jun 07 2025

    Areas affected...Far Northeast PA...Northern NJ...Southeast
    NY...Central and Southern New England

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 071600Z - 072200Z

    SUMMARY...Heavy rainfall will continue to overspread much of the
    northeast Mid-Atlantic region into central and southern New
    England going through the mid to late-afternoon hours. This will
    include some locally more concentrated areas of stronger
    thunderstorm activity with higher rainfall rates. Areas of flash
    flooding are likely considering the very moist and locally
    saturated soil conditions.

    DISCUSSION...An expansive axis of heavy rainfall in a southwest to
    northeast fashion continues to advance across southeast NY and
    into central and southern New England. The activity which includes
    some occasionally stronger thunderstorm activity continues to be
    strongly supported by an ejecting shortwave trough and associated
    wave of low pressure which is transiting a well-defined frontal
    zone across the Northeast.

    The latest GOES-E IR/WV satellite imagery shows an excellent
    corridor of upper-level jet divergence/forcing over especially
    central and southern New England with an expansive axis of cooling
    cloud-tops over the region. There continues to be a low-level
    frontogenetic response to this with the axis of heavy rainfall
    which has been very efficient this morning. Shallow, warm
    convective tops and frontogenetical forcing in the lower to
    mid-levels of the column have been yielding warm rain processes,
    and this showed up well in the 12Z ALY RAOB sounding which
    depicted a deep moist column with a tall/skinny CAPE profile.

    There should be a gradual uptick in the overall convective
    footprint of the heavy rainfall this afternoon across especially
    southern New England including the Boston, MA to Hartford, CT
    corridor and potentially edging south to near the New York City
    metropolitan area and adjacent areas of northern NJ by late
    afternoon. This will be supported by convergence along the
    aforementioned frontal zone, but also with an increase in
    diurnally driven instability. Cloud cover will tend to mitigate
    the amount of surface heating that does occur, but with an already
    very moist column, and the aforementioned low-level and
    upper-level support, there should be a gradual expansion of
    heavier showers and thunderstorms over the next several hours.

    Rainfall rates may reach as high as 1.5 inches to 2 inches/hour
    with the stronger cells, and the locally slow cell-motions and
    pockets of at least brief cell-training may support some totals by
    early this evening that reach 3 to 4+ inches. This is supported by
    the 12Z HREF and 06Z REFS guidance.

    The antecedent conditions are quite sensitive over the higher
    terrain of southern VT, southern NH and through central and
    western MA. Runoff here over the next few hours may be enhanced
    given the additional rains, and gradually heavier rainfall rates
    farther south and east may pose some urban flooding concerns.
    Overall, on a regional level, areas of flash flooding are likely.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4R4grHp5Wg6GEP5i9dXmmHXEyxfS77bhDGbtcItE8WCmURe8VWe8X4GBL0uYzWSlHgxG= KlfJnDEaOhvnu8Z8xiy84qE$ for graphic product...

    ATTN...WFO...ALY...BGM...BOX...BTV...GYX...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 44607027 44566903 43996893 42937041 41747132=20
    41217275 40987314 40527430 40537520 41047545=20
    41917467 42717390 43727193=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 8 02:45:53 2025
    AWUS01 KWNH 080245
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-OKZ000-080800-

    Mesoscale Precipitation Discussion 0395
    NWS Weather Prediction Center College Park MD
    1044 PM EDT Sat Jun 07 2025

    Areas affected...Southern AR...Northern MS... Adj Northwest
    TX/Southwest OK...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 080245Z - 080800Z

    SUMMARY...Training, back-building thunderstorms within axis of
    enhanced moisture capable of 2-2.5"/hr rates and localized totals
    of 3-4" pose possible incident(s) of localized flash flooding
    overnight.

    DISCUSSION...GOES-E 10.3um EIR and Regional RADAR mosaic depict a
    west to east band of thunderstorms with a few cells starting to
    expand and cool below -65C. Cells are developing within a very
    favorable moisture/instability axis south of the main front. A
    surface Td gradient is well denoted with mid to upper 70s Tds
    within the higher theta-E axis from the Red River Valley across S
    AR into N MS/AL (while being 10 degrees cooler downslope of the
    Ozark Plateau in central AR. CIRA LPW also notes mid-level
    layers are at the trailing end of stronger shortwave over the Ohio
    Valley but the upstream wedge brings an axis of 2" total PWats
    through the area of concern. In the wake of the shortwave in IL,
    height-falls are starting to encroach from the northwest further
    tightening the gradient of moisture/instability and given cyclonic
    curl of weak (15-20kt) LLJ out of central TX has resulted in a
    solid confluence axis coincident providing deep layer convergence
    for convective development. Flow is fairly unidirectional
    parallel to the moisture/instability gradient to support some
    training/repeat potential. However, the weaker inflow from the
    west suggests, convergence will be stronger along the upwind side
    of deeper convective clusters/cells to support
    back-building/flanking line development. Propagation vectors,
    including Bunker's right mover vectors, suggest clusters will
    deflect just south of due east though enough overlap should exist
    for some training/repeating cells.

    Much like the convergence, the best instability air remains
    upstream across the OK/TX Red River Valley propagating into the
    clusters mainly in SW AR. MLCAPE values of 2500-3000 J/kg will
    remain available slowly expanding east into S AR over the next few
    hours. So strong updrafts and flux should support efficient
    rainfall production with 2-2.5"/hr rates possible. Given
    flanking development, potential for pockets/clusters of 3-4"
    totals are probable through the overnight period, with an isolated
    5" total possible. Hydrologically, the area of concern has been
    able to recover better than points north and NASA SPoRT LIS 0-40cm
    soil moisture has returned to average in all but far northern MS.=20
    Most values range in the 50%-60% saturation, so FFG values have
    also increased back to normal ranges, generally about 2.5-3"/hr
    and 4"/3hrs (2.5-3" in N MS). Given this, incidents of flash
    flooding are likely to be localized and widely scattered through
    the axis (though guidance/trends suggest SW AR as best potentail)
    and is considered possible.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!686R-YDvXgqUdtFCEo0klNkTomWyFD5muHgprm_vlVh7XoTLfrnBSIp8w2avC4Phny32= baTHzD5nzJ_2B_AL3amshnM$ for graphic product...

    ATTN...WFO...JAN...LZK...MEG...SHV...

    ATTN...RFC...ALR...ORN...TUA...NWC...

    LAT...LON 34909034 34798888 34288823 33418841 32958944=20
    32899195 32999383 33599495 33999507 34239482=20
    34519393 34639283=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 8 03:53:59 2025
    AWUS01 KWNH 080353
    FFGMPD
    VAZ000-WVZ000-OHZ000-KYZ000-INZ000-080900-

    Mesoscale Precipitation Discussion 0396
    NWS Weather Prediction Center College Park MD
    1153 PM EDT Sat Jun 07 2025

    Areas affected...Central and southeast IND...Southwest
    OH...Northeast KY...Western WV...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 080355Z - 080900Z

    SUMMARY...Scattered, focused but very intense warm cloud tropical
    showers capable of quick 1.5-1.75"/hr and totals up to 2.5" may
    result in possible flash flooding.=20

    DISCUSSION...GOES-E WV suite shows a pair of smaller scale
    shortwave features moving through the Ohio Valley at the eastern
    edge of the larger cyclonic synoptic trough over the Great Lakes.
    A stronger mid to upper level jet swings through the Lower Ohio
    into the TN River Valley, the short-wave axis continues to
    elongate/shear but also act as a deep layer speed convergence trof
    fro northwest IND across SW OH toward NE KY, with the base of the
    shear axis rotating eastward quicker. Deep layer moisture through
    the Ohio Valley remains well above average near 1.6-1.8" PWat. As
    the broad 20-25kt 850mb LLJ under-cuts, it is also advecting some
    weak mid-level drying to slightly steepen mid-level lapse rates
    and increase available instability toward 750-1000 J/kg in
    proximity to speed convergence axis. As such, smaller embedded
    fairly narrow updraft cores have been sprouting through the cirrus
    shield where some right entrance ascent/outflow has been
    increasing as the speed max exits to the northeast. Throughout
    the evening these shallow updrafts have been very efficient even
    with the above average moisture perhaps with some enhanced
    nucleation from ingested smoke particles in the warm cloud layer.=20
    Cells within the shear axis have also shown relatively slow cell
    motion with some remaining stationary for over an hour resulting
    in recent hourly observations of 1.25-1.5".=20

    Slow eastward shift of the shear axis with the base swinging
    through E KY/SW WV a bit quicker, may result in some very isolated
    spots seeing a repeating of these embedded shallow convective
    cells. As such, it cannot be ruled out a spot or t increase, with
    even recent hourly observations of 1.25-1.5" noted.wo of 2-2.5"
    totals may be possible. Still, the overall coverage is likely at
    the limit of inducing more than a few isolated incidents of flash
    flooding. However, hourly FFG of 1-1.5" and 3hr FFG values less
    than 2" dot the of concern and so there is sufficient potential
    for at least one or two possible incidents through early morning
    in/along the shear axis, particularly in narrow gullies/complex
    terrain within the Cumberland Plateau into central Appalachians.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_gHfN-X6UUolexQKvZLsszhNO-116VBf3HBuRFWqzcXkenLAXpKheQWLI5i2ceK8MMW7= gm5InkTNatx5bKGJKuK3uUI$ for graphic product...

    ATTN...WFO...ILN...IND...IWX...JKL...LMK...LOT...RLX...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 40958648 40858545 40488475 39868323 39608228=20
    39378156 38968077 38658067 37718115 37258201=20
    37348292 37598374 38108539 38318656 38898728=20
    39998751 40558743 40938706=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 8 06:47:06 2025
    AWUS01 KWNH 080646
    FFGMPD
    ALZ000-MSZ000-081200-

    Mesoscale Precipitation Discussion 0397
    NWS Weather Prediction Center College Park MD
    246 AM EDT Sun Jun 08 2025

    Areas affected...Central AL...East-central MS...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 080645Z - 081200Z

    SUMMARY...Expanding convective complex with favorable
    repeating/training elements suggest localized 2-4" totals and
    localized flash flooding is increasingly possible through early
    morning.

    DISCUSSION...GOES-E 10.3um EIR loops shows individual
    cells/overshooting tops continue to cool and expand westward along
    the flanking line. Cooling tops to -65 to -70C have expanded
    westward generally aligned with the collapse of the upstream cells
    in SE AR. 06z surface analysis along with VWP, suggests increased southwesterly flow from surface to boundary layer combined with
    forward flank cold pool is resulting in a more orthogonal ascent
    plane for convective expansion. GOES-WV and EIR also denotes a
    trailing boundary from exiting shortwave/mid-level trough can be
    seen extending across the Fall-line in SC across central GA before
    angling back northwest. SWIR and RADAR shows some downstream TCu
    developing along this axis; which also seems to align ideally from
    NW to SE with propagation vectors.

    RAP analysis shows a pool of uncapped 2000-2500 J/kg MLCAPE within
    the best streamlines into the expanding complex. Tds in the mid
    to upper 70s combined with a pool of 700mb enhanced moisture is
    resulting in localized PWats of 1.8 to 2", all adding into
    continued potential for 2-2.5"/hr rates. Expanding NW line should
    allow for longer duration of 2-3 hours, suggesting a swath of 2-4"
    is becoming more probable. Boundary layer inflow is currently
    peaking around 20-30kts, but is expected to diminish slowly toward
    12z, likely reducing convective strength as the complex rolls
    through central AL.=20

    Hydrologically, this complex as it tracks east-southeast is moving
    into an area of reduced FFG values with 1hr values of 2-3" (less
    than 2" near cities like Birmingham) and 3hr values are generally
    around 3-3.5". As such, places of ideal, greatest prolonged
    training are well within the possibility of exceedance and
    therefore, flash flooding is considered possible through 12z.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6h2dfuApWIR8a0OgAdP2H8Y6nzKltixtk0XLgTfPRbeMtzW-XlcUgyAAS13BYTxZWlok= NllMBeJ3p5L6gou6ECMqGlw$ for graphic product...

    ATTN...WFO...BMX...JAN...MEG...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34138859 33838705 33628573 32838543 32168556=20
    32338687 33068884 33658972 34098956=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 8 07:30:34 2025
    AWUS01 KWNH 080730
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-081300-

    Mesoscale Precipitation Discussion 0398
    NWS Weather Prediction Center College Park MD
    329 AM EDT Sun Jun 08 2025

    Areas affected...Texarkana...Northern LA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 080730Z - 081300Z

    SUMMARY...Continued upstream redevelopment and repeating across
    Texarkana to add additional 2-4" totals continuing to pose risk of
    possible localized flash flooding through early morning.

    DISCUSSION...GOES-E WV shows main shortwave across Ohio River
    Valley being pressed by stronger synoptic height-falls across the
    central Plains bleeding into the Ozark Plateau. This push
    continues to drive northwesterly flow/drier air to sharpen the
    stationary front across the Red River into the Delta Region of the
    Mississippi River Valley. Broad southerly to southwesterly
    surface to boundary layer flow across TX into N LA remains
    providing strong deep layer moisture convergence impinged against
    the front. Stronger cluster of cells moved right of the mean flow
    entering northern LA left a wake of 1.5-2.5" totals and cold pool
    angled from NW to SE crossing McCurtain county OK, Bowie county
    TX, and Miller county AR.=20

    Upglide ascent of 2000-2500 J/kg of MLCAPE and low to mid 70s Td
    air has resulted in additional upstream redevelopment with
    additional convergence up the Red River with scattered Tcu likely
    to further back-fill the downstream cells over the next few hours
    as well. However, flow is near or just past diurnal maxima and
    may be further veering reducing the orthogonal ascent/convergence
    with time. Still, Given ample deep layer moisture to 2" and slow
    southeastward repeating an additional 2-4" totals across SW AR
    into N LA remain possible maintaining a low-end potential for
    localized flash flooding through daybreak. Given remaining high
    FFG values and inconsistent convective coverage, flash flooding is
    still considered possible.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6gwX7n8loqAToh-kNs8cg_lfcsXnbUe29zBZQGomAUc-4mTUz1ZigK2GlM5qZXIimXaQ= 1lRmqhWqPu-map1JAFnPXQQ$ for graphic product...

    ATTN...WFO...JAN...LZK...SHV...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 34309478 34039353 33299168 32669124 32219162=20
    32319256 32769368 33239454 33749511=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 8 08:55:01 2025
    AWUS01 KWNH 080854
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-OHZ000-081500-

    Mesoscale Precipitation Discussion 0399
    NWS Weather Prediction Center College Park MD
    454 AM EDT Sun Jun 08 2025

    Areas affected...Southern OH...West Virginia...Northwest
    VA...Western MD...Adj Southwest PA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 080900Z - 081500Z

    SUMMARY...Slow moving, warm cloud heavy showers capable of
    1-1.5"/hr and locally 2"+ across complex terrain (or stationary
    near old upper low). Isolated flash flooding remains possible
    through daybreak.

    DISCUSSION...GOES-E WV suite depicts shortwave continuing to pivot
    and slowly shift eastward into west-central Ohio, while westerly
    flow continues to under-cut the shearing trough axis toward a new
    cyclonic rotor across southwest VA. As such, remaining slug of
    enhanced moisture continues to be advected upslope across E OH/WV
    wringing out the remaining 1.5-1.7" total PWats remaining in the
    western branch of the warm conveyor belt back to the old shearing
    out shortwave. Remaining pockets of 500-750 J/kg of CAPE will
    help to maintain a few localized stronger updrafts within the
    larger shield precipitation. Cores will continue to be relatively
    narrow but even shallow in nature will still have the capability
    of efficient warm cloud processes with rates/totals of 1-1.5"
    possible. Given the narrow gullies/terrain channels, this may
    result in localized flash flooding incidents across WV slowly
    shifting into W PA/W MD after 13-15z.=20

    Further west (Western and Central Ohio), near the inner core of
    the shortwave, strong directional convergence near the center may
    result in similar 1-1.5"/hr rates and spotty totals of 2"+ in a
    SHaRS (Subtle Heavy Rain Signature) type event due to near
    stationary cell motions. This is more likely over the next 1-3
    hours before the warm conveyor belt is severed by active
    convection downstream toward the new developing shortwave in the Mid-Atlantic.=20

    Shenandoah/Blue Ridge...
    WV suite shows solid anticyclonic shield with transverse banding
    features typical of right entrance ascent in proximity of central
    VA as the developing shortwave starts to stretch east of the
    Appalachians in the next few hours. Still with upstream shortwave
    energy and surface front banked up west of the ridge, surface to
    boundary layer winds will respond by backing and increasing toward
    20kts in the next few hours. Convection is already starting to
    develop across the Piedmont in response to the deep layer WAA, but
    winds banking in easterly upslope will take a few more hours to
    respond. However, as they do, they will be generally orthogonal
    with solid 1.5-1.75" TPW moisture flux into developing cells along
    the ridges tapping into weak unstable environment. Rates of
    1-1.5"/hr will be common here as well, but may see
    upstream/back-building cells for a few short-term repeating
    elements. Localized totals nearing 2" may result in focused
    incident or two of flash flooding especially given FFG values
    remain reduced across the area ranging from .75-1.5" over NW VA/E
    WV Panhandle and parts of W MD.=20

    In all three locations, flash flooding is not likely to be
    wide-spread nor with extreme totals over 2.5", however, given
    complexity of the terrain and a wet spring in most locations flash
    flooding is considered possible and scattered in nature.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8ezFTiP0q22-j6h4qfS2FU0ba0bhq84ahPVQAbLfvw8BkvT2pkDWd7tmzr4CWJHqh-Rv= iRnB9s5PLqTSio-NucyFGD0$ for graphic product...

    ATTN...WFO...ILN...LWX...PBZ...RLX...RNK...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 40428421 40348337 40168215 40197979 39647943=20
    39657824 39167776 38047849 37767884 37587980=20
    37618091 38268207 39138325 39648460 40168461=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 8 11:39:45 2025
    AWUS01 KWNH 081138
    FFGMPD
    ALZ000-MSZ000-081536-

    Mesoscale Precipitation Discussion 0400
    NWS Weather Prediction Center College Park MD
    736 AM EDT Sun Jun 08 2025

    Areas affected...Central and Easterm MS...Western and Central AL

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 081136Z - 081536Z

    SUMMARY...Areas of locally backbuilding and training thunderstorms
    with heavy rainfall rates of up to 2 inches/hour will continue for
    at least a few more hours across portions of eastern MS through
    western and central AL. Additional isolated to scattered areas of
    flash flooding are likely.

    DISCUSSION...The early-morning GOES-E IR satellite imagery shows
    notably divergent flow aloft associated with cold-topped
    convection across portions of eastern MS through western and
    central AL. Some of the more vigorous activity is noted over
    eastern MS in particular with cloud top temperatures as cold as
    -70C.

    This activity is embedded within a convergent low-level flow
    regime with a moderately buoyant airmass still situated across the
    region. MLCAPE values of as much as 1500 J/kg are in place, with
    the greater instability parameters over central and eastern MS.
    Additionally, there is as much as 40 to 50 kts of effective bulk
    shear playing a role in sustaining stronger updrafts and
    convective cores.

    The leading edge of the convection has propagated well downstream
    through central AL and is also generally losing latitude. However,
    the upstream activity over eastern MS has been showing strong
    backbuilding characteristics with downstream cell-training as
    well. The upwind propagation vectors in a narrow corridor across
    central and eastern MS are quite light, on the order of only 5 to
    10 kts at best, and with the convergent, moist and unstable
    low-level flow pattern in place, there may be additional
    convective development for at least a few more hours that also
    backbuilds and trains over the same area.

    Rainfall rates are already as high as 2 inches/hour, and with the
    ongoing repeating cell-activity, additional rainfall amounts of 3
    to 4+ inches are possible through late this morning. Given these
    additional rains, additional isolated to scattered areas of flash
    flooding are likely for the next few hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4IbhetcITzOj94SsN7SnBDJtGJpElb7ZwP5Uux9_T9kSOaFnEOaQ_XJlE283KvCY0QXk= qtYrK8p1F14u-N-Y49h-w7k$ for graphic product...

    ATTN...WFO...BMX...JAN...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 33648903 33478758 33208655 32838559 32388512=20
    31848530 31908625 32418834 32768920 33148999=20
    33528990=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 8 12:42:35 2025
    AWUS01 KWNH 081242
    FFGMPD
    LAZ000-ARZ000-TXZ000-081600-

    Mesoscale Precipitation Discussion 0401
    NWS Weather Prediction Center College Park MD
    841 AM EDT Sun Jun 08 2025

    Areas affected...Southwest AR...Northern LA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 081240Z - 081600Z

    SUMMARY...Backbuilding and training thunderstorms with heavy
    rainfall rates of 1 to 2 inches/hour continues to focus across
    southwest AR and is expectced to edge more into northern LA over
    the next couple of hours. Given the persistence of the early
    morning convection, and concerns for renewed development, isolated
    to scattered areas of flash flooding are generally likely.

    DISCUSSION...GOES-E IR satellite imagery shows notably divergent
    flow aloft across the broader Arklatex region in association with
    the ongoing convective activity. A band of very heavy showers and
    thunderstorms continue to impact areas of southwest AR and
    northern LA, with the convection continuing to feature cloud top
    temperatures as cold as -65C.

    Much like the convection farther downstream over MS/AL, this
    activity over AR/LA is focused with a moist, unstable and
    convergent low-level flow pattern with this convective cluster
    also near a front. MLCAPE values of 1500 to 2000 J/kg and
    effective bulk shear of 30 to 40 kts are both contributing to
    stronger redeveloping updrafts.

    PWs are on the order of 1.75+ inches, and with the level of shear
    and instability, rainfall rates are expected to continue to be
    well into the 1 to 2 inch/hour range, with some 2.5 inch/hour
    rates possible at least in the near term as these areas of
    stronger thunderstorms continue to persist.

    Backbuilding and training of convective cells across southwest AR
    and into northern LA are generally expected to continue at least
    into the late morning hours given the environment. Recent HRRR
    runs appear to generally be too quick to weaken this activity.
    However, the older 06Z run of the HRRR actually has a reasonably
    good handle of the convective footprint, and would suggest some
    persistence of the convective threat for a while longer.

    MRMS FLASH data has already been showing areas of 3-hour FFG
    exceedance over southwest AR, with CREST Max Unit Streamflow data
    showing elevated runoff near the town of Magnolia up through Hope.
    Additional rainfall amounts of 3 to 4+ inches are expected at
    least locally through late this morning, and this should favor
    isolated to scattered areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6QuDGAPqWIvy8KEaHKlz8wjUZVHYmAs2waHBkOtg3WJXRpcz1auXy-sy8X7FqRrfpuN6= gMC0xM8ajshU5VN5oO0Urp8$ for graphic product...

    ATTN...WFO...JAN...LZK...SHV...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 33719378 33459293 32869180 32179151 31909220=20
    32389331 33329413=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 8 16:12:06 2025
    AWUS01 KWNH 081612
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-OHZ000-082210-

    Mesoscale Precipitation Discussion 0402
    NWS Weather Prediction Center College Park MD
    1211 PM EDT Sun Jun 08 2025

    Areas affected...Portions of the Central Appalachians and Northern
    Mid-Atlantic

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 081610Z - 082210Z

    SUMMARY...Areas of moderate to heavy rainfall will continue
    through this afternoon with an expectation that scattered
    thunderstorms will develop and produce heavier rates. Given the
    moist and sensitive antecedent conditions, the additional rainfall
    is likely to result in some runoff problems and flash flooding.

    DISCUSSION...The midday GOES-E visible satellite imagery along
    with regional radar data shows areas of moderate to locally heavy
    rain falling over portions of western and southwest PA down
    through the MD/WV Panhandles and into northern VA. This rainfall
    is being driven by the arrival of a shortwave trough from the OH
    Valley which is promoting a northwest to southeast corridor of
    isentropic ascent and frontogenetical forcing along and just
    poleward of a warm front lifting gradually northeastward into the
    region.

    Meanwhile, solar insolation is seen taking place farther west
    across central and northern WV and western VA which is allowing
    for some CU/TCU development over the higher terrain. Surface-based
    instability is expected to continue to increase going through the
    afternoon hours, and with convergent flow along the front and
    orographic forcing over the higher terrain, there should be the
    development and gradual expansion of some heavier shower and
    thunderstorm activity over the next few hours. It should be noted
    that moist low-level southeast flow is expected to become better
    established into the Blue Ridge this afternoon as well, and this
    may yield some locally more concentrated areas of convection in
    these areas.

    The environment is pretty moist and the 12Z RAOBs at KPIT and KIAD
    showed 1.42 inch and 1.62 inch PWs respectfully which are at or
    just above the 90th percentile of daily climatology. This overall
    environment should favor at least above average rainfall
    efficiency across the region and especially with some of the
    forcing that will be occurring this afternoon in the warm layer of
    the column.

    Rainfall rates with the instability driven convective elements
    this afternoon from southwest PA down through northern VA will
    likely be quite high and capable of reaching 1.5 to 2 inches/hour.
    The 12Z CAM guidance suggests that some localized rainfall totals
    by this evening may reach as high as 2 to 3+ inches where some of
    the slower moving cells evolve.

    Given the wet antecedent conditions and high rainfall rates,
    isolated to scattered areas of flash flooding are likely.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4gCads1DEj_ivhAn6tQFEer7IwB5co9wce-7pbxIJ72pljVAewh5UyTyJNfYeNPNwFOD= a_q4Q6HNHZ5Em7cC4AH831A$ for graphic product...

    ATTN...WFO...AKQ...CLE...CTP...LWX...PBZ...RLX...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 41317974 41117866 40677788 39957717 38757715=20
    38037794 38227904 39408035 40708079 41228041=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 8 18:07:39 2025
    AWUS01 KWNH 081807
    FFGMPD
    TXZ000-OKZ000-090005-

    Mesoscale Precipitation Discussion 0403
    NWS Weather Prediction Center College Park MD
    206 PM EDT Sun Jun 08 2025

    Areas affected...TX/OK Panhandles into Northwest TX and Southwest
    OK

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 081805Z - 090005Z

    SUMMARY...Organizing supercell thunderstorms by mid-afternoon and
    gradual consolidation into a severe MCS by this evening may result
    in some scattered concerns for flash flooding where the cells to
    merge or locally train.

    DISCUSSION...The latest GOES-E GeoColor satellite imagery shows
    strong diurnal heating over the southern High Plains which is
    already favoring MLCAPE values as high as 2000 to 3000+ J/kg. A
    capping inversion which still remains in place will continue to
    steadily erode via additional surface heating over the next few
    hours.

    This will set the stage for well-organized and heavy showers and
    thunderstorms to develop near and to the south of a cold front
    dropping south toward the southern Plains, and also near and north
    of a retreating warm front situated farther south over western and
    northern TX. Already a northwest/southeast axis of elevated
    thunderstorms has developed over the last couple of hours over
    northwest TX given steep mid-level lapse rates.

    A highly sheared environment exists with effective bulk shear
    values of 30 to 50 kts in place, and these magnitudes are forecast
    to slowly increase through the afternoon hours. The combination of
    this and strong boundary layer instability will favor developing
    and expanding coverage of supercell thunderstorms by mid-afternoon.

    Aside from well-defined severe hazards, there will be a heavy
    rainfall component to the supercells considering the degree of low
    to mid-level moisture that is in place. The latest CIRA-ALPW data
    shows relatively enhanced moisture profiles from the surface up
    through the 700 mb level, and so many of the supercell
    thunderstorms will be capable of highly efficient rainfall rates
    that could reach 2 inches/hour.

    By early this evening, merging/consolidating supercell
    thunderstorms should lead the way for a severe MCS, but as this
    process occurs, there will be sufficient concerns for cell-mergers
    and cell-training such that some rainfall totals reach 2 to 4+
    inches.

    This may result in concerns for scattered areas of flash flooding
    which will include some localized urban impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_Dms-epohnvzfqk-7f01Fr3IdQDNLaIhg1PV2eKHWEY2vbRoaYJ04MqFxmim0LVFyTpI= Ys8X_BkQQfq8-ux3LAu8NYo$ for graphic product...

    ATTN...WFO...AMA...LUB...OUN...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 36960058 36509954 35759881 35019838 34079832=20
    33409886 33490002 34210078 34820146 35690220=20
    36250233 36830196=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 8 22:33:16 2025
    AWUS01 KWNH 082232
    FFGMPD
    PAZ000-MDZ000-VAZ000-DCZ000-WVZ000-090400-

    Mesoscale Precipitation Discussion 0404
    NWS Weather Prediction Center College Park MD
    631 PM EDT Sun Jun 08 2025

    Areas affected...southwestern PA into northern and eastern WV,
    northern VA, western MD, and DC

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 082230Z - 090400Z

    Summary...Short term localized totals of 2-4" likely to lead to
    isolated to scattered instances of flash flooding.

    Discussion...Showers and thunderstorms have been increasing in
    coverage over the past few hours in the vicinity of a warm front
    draped from southwestern PA through western MD, the WV Panhandle,
    northern VA. A shortwave trough will pivot through the area over
    the next several hours, providing additional lift via DPVA. The
    mesoscale environment is characterized by a SBCAPE gradient of
    500-2000 J/kg, precipitable water (PW) values of 1.4-1.7 inches
    (near the 90th percentile, per IAD sounding climatology), and
    effective bulk shear of 30-45 kts. MRMS estimates hourly rainfall
    totals as high as 1-2" in association with WSW-to-ENE training
    elements in the most intense multi-cell clusters, but fairly
    progressive storm motions (averaging near 20 kts) with more
    semi-discrete cells has tended to limit localized totals to 1".

    Going forward, there could be more substantial organization of
    convection going into the early evening hours given the overall
    favorable environment for heavy rainfall. The area of greatest
    concern in the near term is along the Blue Ridge Mountains from
    the eastern tip of WV southward to Shenandoah NP, as well as
    eastward into the DMV region. While hi-res models are not in the
    best agreement (with the HRRR in particular really struggling to
    properly initialize the the convection that is already ongoing),
    the best signal for heavy rainfall is located in this area (with
    fairly good agreement between the 18z HREF PMM and experimental
    12z REFS PMM, suggesting localized 2-3" totals). There was also a
    distinct uptick in the 18z HREF 40-km neighborhood 3" exceedance
    probabilities (largely due to the addition of the 18z NAM-nest),
    which indicate 30-50% odds for localized 3" exceedance (through
    03z). Given 3-hr FFG as low as 1.0-1.5" (mainly across northern
    sections of the MPD, including the aforementioned area of
    concern), isolated to scattered instances of flash flooding are
    likely. Convection should decrease substantially in coverage by
    03-04z with waning instability and increasing convective
    inhibition.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-mdYoAd0Hn_BrnMbqGyn2_P9vSuI-RA8SinqHC4y-e1RNcxsNaxZ57tvWMTsAXa-dH8-= fxWKHq3-neq0PTJwq8-qobQ$ for graphic product...

    ATTN...WFO...AKQ...CTP...LWX...PBZ...RLX...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 40287932 40237883 39887815 39487738 39107685=20
    38617697 38007695 37317740 37047812 37157854=20
    37567865 38277858 38867921 39168012 39768049=20
    40098017 40247979=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 9 00:27:25 2025
    AWUS01 KWNH 090026
    FFGMPD
    TXZ000-OKZ000-090600-

    Mesoscale Precipitation Discussion 0405
    NWS Weather Prediction Center College Park MD
    825 PM EDT Sun Jun 08 2025

    Areas affected...TX Panhandle into Northwest and North TX, Central
    and Southern OK

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 090025Z - 090600Z

    Summary...Localized hourly totals of 2"+ with 3-6 hour totals of
    3-5" likely to result in scattered instances of flash flooding.

    Discussion...Convection is rapidly proliferating across
    southwestern and central OK and the TX Panhandle into the Big
    Country within an extremely unstable environment (MU CAPE
    3000-5000 J/kg). While many cells remain discrete (mainly into the
    TX Big Country and North TX) with many splitting supercells and
    deviate cell motions, storms are becoming much more linearly
    organized over the TX Panhandle into western OK, as a cold pool
    becomes established within an area of broad low-level convergence
    (situated between a cold front near the OK/TX Panhandle border and
    a warm front just to the south). Precipitable water values range
    from 1.4-2.0" (between the 90th percentile and max moving average,
    per AMA/OUN/FWD sounding climatology), and deep layer (0-6 km)
    bulk shear of 40-60 kts (also near or above the 90th percentile).
    MRMS estimates indicate very heavy precipitation in association
    with the supercells (as much as 1" in 15-min), and hourly
    accumulations are as high as 1.5-2.5" (mostly in association with
    training convection where storms are organizing linearlly).

    A chaotic mix of storm modes will continue into the evening, as
    the developing MCS continues to grow upscale over the TX Panhandle
    into southwestern and central OK with splitting supercells and
    merging (possibly organizing into their own smaller clusters/bows)
    downstream into the TX Big Country and North TX. Eventually the
    MCS will become the dominant force and rapidly propagate into
    southern OK and North TX (with the upwind/downwind propagation
    vectors favoring ESE-SE movement at 30-50 kts), tracking over
    areas that will have already seen heavy precipitation from earlier
    discrete convection. Resulting localized 6-hr rainfall totals
    (through 06z) of 3-5" are expected (per 18z HREF PMM QPF) with the
    most favored corridor along and south of the Red River of the
    South (where 18z HREF 40-km neighborhood 3" exceedance
    probabilities range from 40-70%, shifted a bit south based on more
    recent hourly HRRR/RRFS data, as well as experimental WoFS data).
    Merging supercells and training elements will also be capable of
    2"+ hourly totals with corresponding HREF 1-hr FFG exceedance
    probabilities as high as 20-50%. Given both the extreme hourly
    rates and potential for 3-6 hour totals in excess of 3", scattered
    instances of flash flooding are likely.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7PuY86IVZnMuGVpfzrrdIxQvWlBrLbH_y1-spoByVky45f0XovAiLEHVcw8AXrYJ18RB= MgwL_tsGnAmIRSccpfJ9CwQ$ for graphic product...

    ATTN...WFO...AMA...FWD...LUB...MAF...OUN...SHV...SJT...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35680155 35440070 35429965 35499884 35689805=20
    34609564 32829475 31889619 31799831 32400042=20
    33150143 34150143 35360220=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 9 03:17:46 2025
    AWUS01 KWNH 090317
    FFGMPD
    VAZ000-NCZ000-090700-

    Mesoscale Precipitation Discussion 0406
    NWS Weather Prediction Center College Park MD
    1117 PM EDT Sun Jun 08 2025

    Areas affected...South-central to Southeast Virginia...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 090315Z - 090700Z

    SUMMARY...Continued limited flash flooding risk continues for a
    few more hours as remaining training cells approach southeast VA
    and more susceptible urban environment.=20=20

    DISCUSSION...GOES-E 10.3um and RADAR mosaic across the
    Mid-Atlantic shows a slowly stabilizing environment, particularly
    northward along the advancing occluded front from HGR/FDK MD into
    north-central VA toward the triple point near LKU. The warm front
    remains well defined cross the lower neck into Hampton Roads and
    out into the Atlantic through the mouth of the Chesapeake Bay.=20
    RAP analysis shows a well of 1000-1500 J/kg of MLCAPE along and
    east of the slowly advancing cold front out near the slopes of the
    Blue Ridge across south-central VA into southeast VA. However,
    VWP shows mid to upper level trof is starting to slide away
    further northeast but 850mb winds remain mildly convergence as
    down-sloping becomes more westerly and into the 20-25kt range. As
    such, a few convective cells remain across south-central VA and
    while there are some indications of cold pool/outflow, there is
    some upstream redevelopment on that low level convergence to keep
    activity going. Deep layer flow remains a bit north of ideally
    parallel to the orientation of the ongoing convection but still
    remains suggestive of training/repeat component as the cells
    continue to drift east.=20

    Total moisture of 1.75" and deep warm layer and flux for rainfall
    production helps to maintain solid efficiency for 1.5-1.75"/hr
    rates with length of training to support 1-2 hour duration for
    additional 1.5-3" totals over the next few hours. This is a the
    lower threshold of FFG values in the rural areas, however, if
    cells can maintain strength and tap remaining instability pockets,
    these rates/totals would pose a greater potentail for flash
    flooding across the urban locations from Richmond/Petersburg
    southeastward toward Norfolk and Hampton Roads. So while not the
    highest confidence it will given the stabilizing environment with
    loss of heating...the risk is sufficient for localized flash
    flooding to continue to be possible for the next few hours.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!51BV9I7SzZjyVQ3VKsMpcyrKrro_3Hrxdx8wnGGZ0JH4OgfvDf9kBSK-dYfHnLXB8_ki= YtsRcfwdUVnvu1lAofsMc08$ for graphic product...

    ATTN...WFO...AKQ...RNK...

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37857671 37637628 37077605 36847595 36567584=20
    36327595 36397697 36557779 36587861 36767934=20
    37157952 37427867 37637752 37747708=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 9 04:51:54 2025
    AWUS01 KWNH 090450
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-091030-

    Mesoscale Precipitation Discussion 0407
    NWS Weather Prediction Center College Park MD
    1249 AM EDT Mon Jun 09 2025

    Areas affected...Much of northern & Central TX...Northwest
    LA...Southwest AR...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 090450Z - 091030Z

    SUMMARY...Very large, progressive MCS. Greater duration of
    intense rain-rates along the warm advective wing on the northeast
    side as well as along the flanking line due to repeating pose best
    potential for 2-3" totals much in very short-duration.

    DISCUSSION...GOES-E WV suite shows a large dual clustered MCS
    across the Central Red River Valley back into the Rolling
    Plains/Big Country of Texas within a highly diffluent portion of
    the mid to upper-level flow at the base of a broad, strong
    synoptic low. This divergent pattern combined with a very
    moist/unstable environment has supported a strong MCV located at
    the northeast side of the complex in SE OK, quickly shifting
    east-southeast. Given the secondary explosive convective
    development a secondary weaker MCV can be seen further southwest
    near KMWL with a strong/broad bowing segement connecting the two
    features as an effective cold front ahead of the northern strong
    1013mb meso-high. Further upstream, left exit dynamics and
    southerly inflow from the Pecos river valley shows a third
    cluster/linear convective complex acting as a caboose to the
    overall complex, sweeping through with another strong burst of
    intense rainfall rates (though equally progressive given the
    downward mixing of strong flow aloft).

    Overall the deep layer flow with the diffluence as supported a
    very progressive southeastward propagation that is starting to
    limit overall duration of the most intense rain-rates. CIRA LPW
    and overall Total PWAT animation shows the complex is propagating
    into slightly drier overall environment through depth, though it
    continues to currently ingest 2-2.25" total PWats allowing for
    efficient rates over 2-3"/hr...yet, the quickness is generally
    limiting the initial burst to about 1-1.5" in 15-30 minutes, with
    broad moderate shield precip adding an additional .5-1" through
    the main line. However, southerly inflow on broad 20-25kt LLJ is
    advecting this drier and lower theta-E air, so rates should
    continue to diminish with greater dry air and forward propagation
    expected, reducing the overall flash flooding potential,
    especially as the convection moves off into the Heart of Texas and
    into NW LA where FFG values are over 2-2.5"/hr, making FF risk
    limited to urban areas.

    With that stated, there will remain two axes of increased rainfall
    duration: 1) Precursory to the squall line WAA downshear of the
    MCV center across NE TX into far NW LA/SW AR increasing overall
    duration and training. Expected totals of 2-3" are probable with
    an isolated spot of 4" possible. MCV may also slow and rotate
    northeastward further increasing duration of this training axis.=20
    2) The other is along the flanking line of the overall complex
    that is favorably oriented from WNW to ESE fairly parallel to the
    deep layer steering of the MCS. In addition, south to
    south-southwesterly isentropic ascent may help for additional
    development along the outflow boundary...though with lower
    unstable and moisture environment, extending the duration of
    thunderstorm activity and repeat/training will have the greatest
    potential for those 2-3" totals and continue scattered ongoing
    flooding in the southern Big Country into northeast Hill country
    as the trailing 'caboose' linear complex slides through out of the
    southern Rolling Plains.

    So all in all, the coverage of flash flooding will be reducing
    with a few axes of enhanced risk and given the ongoing flash
    flooding with upstream rainfall likely...flash flooding will
    remain likely through 10z, but reducing becoming more widely
    scattered in nature eventually becoming only an urban concern
    further south and east.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7iZ9QbBIW8NgwOmIRWKr69Fd02TdQRo2MD-wLx90BpK1HGllYPUNay--4nuOk1QAPLeE= 0s1vLBCqICnIDVyGfl54Lvs$ for graphic product...

    ATTN...WFO...FWD...HGX...LUB...LZK...MAF...SHV...SJT...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 34069465 33549339 33339303 32979215 32119211=20
    31679258 31579339 31259461 30729641 30989757=20
    31739974 32200062 32740093 33200032 33219972=20
    33099877 32919765 32949610 33329553 33909516=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 9 05:22:48 2025
    AWUS01 KWNH 090521
    FFGMPD
    FLZ000-ALZ000-MSZ000-091030-

    Mesoscale Precipitation Discussion 0408
    NWS Weather Prediction Center College Park MD
    121 AM EDT Mon Jun 09 2025

    Areas affected...Southern MS...Southern AL...Far Western FL
    Panhandle...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 090520Z - 091030Z

    SUMMARY...Stationary/slow moving clusters along old outflow
    boundary/theta-E gradient pose highly focused totals to 4"+ and
    possible widely scattered rapid inundation flooding overnight.

    DISCUSSION...04z Surface and RAP analysis shows a solid theta-E
    gradient across southern GA, southeast AL before dipping near
    Pensacola, FL before angling northwest into south-central MS with
    about 4-8 degrees making it subtle. However, total PWat analysis
    shows the feature much better with long strung out axis of 2"+
    total PWats seen well at the 850-500mb layers in CIRA LPW.
    Recent uptick in southwesterly surface to 850mb flow at 5-15kts
    results in sufficient isentropic ascent in small clusters (near
    the angle in far W FL) and utilizing the slightly uncapped 2000
    J/kg MLCAPE along the boundary. Upper level flow is generally
    weak, but with the approach of the stronger upper-level jet
    upstream in the Plains, is providing some deeper layer effective
    bulk shear into the 20-30kt range to provide some organization to
    the convective clusters to keep the downdrafts from collapsing in
    on the clustered updrafts. Given total PWats of 2" and sufficient
    15kt flux, rates of 2-2.5" have been seen in these clusters.=20
    Currently the line is still upstream enough that 500-1000
    thickness weak and therefore, upstream inflow is about equal to
    easterly steering flow to keep cells fairly stationary to weakly
    moving. New updrafts along weak outflow helps to expand the
    clusters (particularly further west into south-central MS), so
    isolated totals of 3-5" are becoming increasingly possible
    resulting in focused possible rapid inundation flooding.

    As the upstream MCS continues to barrel through eastern Texas, low
    level inflow will back a bit and WAA should expand convective
    initiation southern to west-central MS. This increase in inflow
    is also likely to increase forward cell motions toward the north
    likely reducing overall totals but increasing coverage of 1-3"
    totals in advance of the line. Will have to continue to monitor
    the area into the dawn time frame for subsequent MPDs.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5VbDJ44c3Rmz2iJAcrVXKwhNHGe5Pw8kVwV9suXhlnncytmYwmtK5OYyQnPtS7VPo78q= mZd6sc90VaeBfwjoG71E6uY$ for graphic product...

    ATTN...WFO...JAN...MOB...TAE...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 32608994 31938809 31768645 31388595 30698598=20
    30298622 30338699 30488782 30788833 31068944=20
    31559031 32149076=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 9 09:21:32 2025
    AWUS01 KWNH 090920
    FFGMPD
    ALZ000-MSZ000-LAZ000-ARZ000-091500-

    Mesoscale Precipitation Discussion 0409
    NWS Weather Prediction Center College Park MD
    519 AM EDT Mon Jun 09 2025

    Areas affected...Central MS...Southwest AL...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 090920Z - 091500Z

    SUMMARY...Training WAA convective cells with capability of 2"/hr
    rates and spots of 2-3"+ may result in possible localized
    incident(s) of flash flooding through early morning.

    DISCUSSION...Regional RADAR and surface observations show rapidly
    decaying MCS continuing to press eastward along the LA/AR border
    with outflow boundary starting to reach northeast LA where it
    intersects with slowly lifting frontal boundary that has had some
    active convection along it earlier this mornign across S MS.=20
    Surface to boundary layer winds are increasing with approach of
    the MCS and slightly increased WAA over the boundary breaking out
    more numerous updrafts across central MS connecting up to the
    lifting older cluster out of south-central MS. From 850-500mb,
    winds are fairly flat from west to east to allow for solid
    potential for training of these cells. CIRA LPW also denotes the
    weak amplifcation of the surface to 850mb moisture up the MS River
    Valley but also still pooled along the deeper layer boundary
    toward SW AL and active cluster in south-central AL as well. TDs
    in the mid-70s with 850-500mb moisture axis continue to support
    2-2.25" total PWats and with upstream faster flow associated with
    the MCS, propagation vectors have reduced to about 5kts and are
    supportive of backbuilding into the approaching outflow boundary.=20
    As such a few hours of efficient rainfall/training should allow
    for 2-3"+ totals across central MS.

    Slowly the cells will move into more senstive soil conditions from
    east-central MS into south-west AL from last evening's heavy
    rainfall, this may increase the potential for higher than normal
    run-off and incidents of flash flooding, but the air is drier
    aloft and more stable, and without very strong WAA to advect
    northward it may be more difficult to maintain stronger convection
    across this region, but at the same time, will not require as much
    rainfall totals (2-2.5" in 3-6hrs) than over the drier conditions
    of central MS. Either way, hourly rates and 3hour totals will be
    close enough to suggest localized incidents of flash flooding will
    be possible through early morning hours.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!49iAVeDqXzTLS09rM5rKAjVr573UgnYL74fGpAMblDT-x7fm-Iwr6ZcscrmThd3BdZSp= ySCU5-yh4-MIx4zdPyLsJR0$ for graphic product...

    ATTN...WFO...BMX...JAN...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 33649014 33468862 32828762 32548709 32258628=20
    31638628 31168664 31268799 31788932 32029021=20
    32289124 32859149 33449128=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 9 18:12:51 2025
    AWUS01 KWNH 091812
    FFGMPD
    NYZ000-PAZ000-WVZ000-OHZ000-092330-

    Mesoscale Precipitation Discussion 0410
    NWS Weather Prediction Center College Park MD
    212 PM EDT Mon Jun 09 2025

    Areas affected...eastern OH/western PA/western NY

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 091810Z - 092330Z

    Summary...A few areas of flash flooding will be possible from
    eastern OH into western/northwestern PA and western NY through
    early evening. Hourly rainfall of 1-2 inches are expected with
    localized totals of 2 to 3+ inches from short term training.

    Discussion...1745Z visible satellite and regional imagery showed
    developing showers and thunderstorms extending from central Lake
    Ontario into northwestern PA, along a pre-frontal trough axis/wind
    shift. Back to the west, additional activity was forming over
    central and eastern OH, just ahead of a slow moving cold front.
    Area 12Z soundings and GPS PWs indicated precipitable water values
    ranged from 1.2 to 1.5 inches within the warm sector from central
    OH to western NY and the 17Z SPC mesoanalysis showed MLCAPE of
    500-1000 J/kg from near Buffalo, NY to southern/eastern OH.

    Continued surface heating through a mixture of cloud coverage=20
    across the region and southwesterly low level advection of
    moisture will allow surface temperatures/dewpoints to come up a
    bit more through peak heating supporting RAP forecasts of MLCAPE
    by 21Z of 500-1500 J/kg for the MPD threat area. A mixture of
    storm types will be possible given sufficient shear/instability
    for organized convection but storm motions are expected to be
    roughly 30-40 kt for most of the region which should keep
    individual cells progressive. However, as the cold front slowly
    progresses eastward, pre-frontal convergence axes and
    storm-induced outflow boundaries are expected to align with the
    unidirectional flow from the SW, supporting periods of training.
    Hourly rainfall of 1-2 inches is expected within training and
    localized 2 to 3+ inch totals will be possible through about 00Z.
    Flash flood guidance is relatively low (1+ inches per 1 to 3
    hours) from portions of eastern OH into a good portion of PA and
    into areas of NY just north of the PA border. Exceedance of these
    lower FFG values will potentially lead to a few areas of flash
    flooding as storm coverage increases over the next few hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ZXUTkxpvlUH8KGv3x_3a6D9qEh_rRIlCe2DumB2r968SIP6VtdEzz9JN1uEkBZce_bX= n3g19xnWQGS3ibG_h565x2o$ for graphic product...

    ATTN...WFO...BGM...BUF...CLE...CTP...ILN...PBZ...RLX...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 43787671 43417592 42327661 40907872 40088075=20
    39748201 40238294 41298225 42437986 43407908=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 9 19:52:32 2025
    AWUS01 KWNH 091952
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-100150-

    Mesoscale Precipitation Discussion 0411
    NWS Weather Prediction Center College Park MD
    351 PM EDT Mon Jun 09 2025

    Areas affected...Central Gulf Coast

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 091950Z - 100150Z

    SUMMARY...Some isolated to scattered instances of flash flooding
    are possible into the early evening hours, especially across parts
    of southern AL where recent heavy rain has left soils saturated.

    DISCUSSION...The southwestern flank of old outflow boundary
    related to an MCV trekking across northern GA has stalled near the
    central Gulf Coast and is seeing continued cellular east-west
    thunderstorm development over the last few hours across southern
    MS/AL. Currently storms are struggling to produce rainfall rates
    over 1.5"/hr per MRMS, but these rates should increase as higher
    instability and PWATs advect into the region. SPC mesoanalysis
    highlights 4,000 J/kg of SBCAPE in the area near southern MS and
    southeast AL, which falls in the area of inflow towards developing
    storms as the column mean flow remains out of the west-southwest.
    This is also parallel to the linear orientation of storms and will
    promote some backbuilding and more widespread heavy rainfall as
    opposed to cellular activity due to the influence of a shortwave
    approaching the lower Mississppi Valley. PWATs are as high as 2"
    and the 18z RAP depicts these values increasing and expanding with
    time across the central Gulf Coast states this evening.

    Recent HRRR and experimental RRFS guidance is similar with respect
    to current convection, but differ with potential initiation
    southward closer to the Gulf Coast. The RRFS is likely overdone,
    but with the eventual convection also most likely greater in
    coverage than HRRR guidance given parameters available (HRRR
    suffers from a low-level dry bias). Additionally, soils remain
    saturated near the border of south-central AL and the far
    northwestern FL Panhandle where MRMS estimates an average of 2-5"
    of rain has fallen in the last 12 hrs. This results in an area of
    greatest concern for more widespread and impactful flash flooding.
    Otherwise, the remainder of the highlighted region more isolated
    instances of flash flooding are possible.


    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4BR4jsq545OsDMOgJeXhuzHlNlCETLmqgN0m3BjDqE1TDTwgroLnKKdZR_j0og48CZ2m= C4nGlGSJxai1xLsoy9TUPAw$ for graphic product...

    ATTN...WFO...JAN...LIX...MOB...TAE...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 31778695 31608621 31338587 30988614 30868705=20
    30758807 30508921 30568991 31009000 31488921=20
    31738820=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 9 21:01:52 2025
    AWUS01 KWNH 092101
    FFGMPD
    NMZ000-100300-

    Mesoscale Precipitation Discussion 0412
    NWS Weather Prediction Center College Park MD
    501 PM EDT Mon Jun 09 2025

    Areas affected...New Mexico

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 092100Z - 100300Z

    SUMMARY...Scattered showers and thunderstorms will continue for
    several more hours anchored near the terrain of the Southern
    Rockies, before activity begins to eject into the southern High
    Plains by 00z tonight.

    DISCUSSION...GOES-EAST infrared satellite imagery shows cooling
    cloud tops across northern NM over the last hour across much of
    northern NM and the terrain of the southern Rockies. Maximum
    hourly rainfall rates have been estimated per MRMS up to 2"
    briefly near Las Vegas, NM earlier this afternoon. This activity
    should continue through at least 00z centered over the higher
    elevations until activity congeals and a large cold pool develops,
    helping eject convection southeastward into the southern High
    Plains. Additionally, a shortwave diving across southern CA
    evident in GOES-East WV imagery will add to the ability for storms
    to continue sliding eastward once forward motion picks up.

    Sensitive terrain across the Sacramento Mts. and burn scars from
    the past few years remain the greatest concern for flash flooding
    as any storm will likely contain rainfall rates greater than
    0.5"/hr. PWATs per SPC's mesoanalysis are in the 0.75-1.0" range
    and MLCAPE of 500-1500 J/kg (greater in the High Plains). This is
    sufficient enough to maintain updrafts further until the growing
    cold pool takes over. NASA SPoRT-LIS 0-2 m relative soil moisture
    show much of northern NM in the 80-90th percentile, but with the
    central High Plains closer to average. FFG is as low as 1.5-2.0"
    for 3-hr in the highlighted area outside of burn scars, with
    recent HRRR guidance showing additional scattered 3-hrly totals
    around 1.5". This information leads to the potential for
    additional scattered flash flooding coverage into this evening.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!--kVV-qNvsnlPSCg4i3e_o5haCriyHHUmFgjyDBDRskDVkOT02vVH1vDwE8TzzSicfxy= XKRfCKJ0EX8ZZLKBEZVbAFQ$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 36990510 36970405 36550368 35950408 35260409=20
    34430357 33520385 32890453 32500515 32680576=20
    33220586 33670608 34050662 34510690 35170699=20
    35850694 36400667 36790605=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 9 23:23:28 2025
    AWUS01 KWNH 092323
    FFGMPD
    NYZ000-PAZ000-MDZ000-VAZ000-WVZ000-100520-

    Mesoscale Precipitation Discussion 0413
    NWS Weather Prediction Center College Park MD
    723 PM EDT Mon Jun 09 2025

    Areas affected...Portions of the Lower Great Lakes and Central
    Appalachians

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 092320Z - 100520Z

    SUMMARY...Ongoing thunderstorm activity ahead of an advancing cold
    front is expected to continue exhibiting brief training and likely
    producing additional isolated to scattered instances of flash
    flooding into at least the early overnight period. Maximum hourly
    amounts of 1-1.5" are most likely, but should occur within the
    very saturated and already flood-prone region of the central
    Appalachians.

    DISCUSSION...Latest radar, satellite, and surface observations
    indicate periods of heavy rainfall and numerous thunderstorms
    stretching from northwest PA into western NY, along with
    developing cells and scattered thunderstorms across central PA
    into WV and northern VA. These storms are all generally moving
    northeastward ahead of an approaching pair of cold fronts swinging
    across the Great Lakes. Meanwhile, easterly low-level flow off the
    Atlantic has produced an area of convergence along the central
    Appalachians extending from western VA along the Allegheny Mts
    through Upstate NY. This area of convergence could be a focus
    along sensitive terrain (1-hr FFG less than 1") for brief
    training/slow-moving storms and scattered flash flooding.

    PWs in the area are generally around 1.3-1.5", which isn't too
    spectacular and falls under the 90th climatological percentiles
    per the NAEFS ESAT. However, the strong southwesterly 850mb flow
    of 35-40 kts increase IVT above the 90th climatological percentile
    and could be what pushes the setup towards greater flash flooding
    potential for a few additional hours after sunset. Instability
    remains sufficient along this convergence zone with MLCAPE over
    1,000 J/kg, leading to the maintenance of updrafts due to the
    combined effective bulk shear in the area. Latest HRRR and
    experimental RRFS guidance depicts hourly totals up to 2" possible
    and 18z HREF probabilities for 3-hr totals greater than 2" as high
    as 40%. All of this within a region of the central Appalachians
    containing 1-hr FFG less than 1" and 3-hr FFG less than 2", as
    well as monthly rainfall running 200-300% above normal. These
    factors support the likelihood of additional isolated to scattered
    flash flooding, but with the magnitude of impacts potentially
    limited given the overall storm system is progressing eastward
    with time.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ThDQOe09jaiTiQ6WW3f6kzi2MOJvymk3fwPZ9k3lUC3mfTpZJirPre-3Os14FUKM2cM= DgZHl-p60loNrU8b5228ZeM$ for graphic product...

    ATTN...WFO...BGM...BUF...CTP...LWX...PBZ...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 44037585 43387535 41367669 39817749 39077824=20
    39127926 39677983 41007947 42567801 43737661=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 10 01:16:37 2025
    AWUS01 KWNH 100115
    FFGMPD
    TXZ000-NMZ000-100710-

    Mesoscale Precipitation Discussion 0414
    NWS Weather Prediction Center College Park MD
    914 PM EDT Mon Jun 09 2025

    Areas affected...Southeast NM into West-Central TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 100110Z - 100710Z

    SUMMARY...The combination of leading discrete cells and a
    developing MCS ejecting out of the NM High Plains will lead to the
    potential for scattered flash flooding and isolated rainfall
    totals of 2-4", mostly occurring within a few hours.

    DISCUSSION...A lingering outflow boundary/cold front extending
    across central TX towards the corner of southwest NM has already
    triggered convection in the form of discrete cells (some
    supercells) between Midland and San Angelo. Reflectivity values
    greater than 65 dBZ and hydrometeor classification depict these
    cells as primarily a hail/severe threat to start as opposed to
    heavy rainfall. However, given the slow motion of these cells and
    the eventual influence of an approaching MCS, flash flooding could
    become more of a concern into the early overnight hours.

    ML CAPE values of 2,000-3,000 J/kg remain in place along with east-southeasterly flow converging along the outflow/frontal
    boundary helping maintain a relatively moist column and PWs
    1.-1.5" (highest east near San Angelo in the highlighted area).
    This convergence promotes the greatest potential for longer
    duration rainfall and amounts that may exceed local FFG.

    3-hr FFG in the area is as low as 2-2.5" in local spots but
    generally as high as 3-4". This remains the limiting factor
    regarding confidence in flash flooding magnitude as well as the
    expected fast forward motion of the later MCS ejecting out of NM.
    However, coverage of heavy rainfall with amounts up to 4" where
    cells merge and/or on the northern and southern fringes of the MCS
    near any developing bookend vortices could trigger a few instances
    of flash flooding.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!67dXaBBc9SQ2iLzT0sX4G3-K5ozsP0tF8C3lLhZizsxMl2yoooYfMIZgt_G7_JFBBd3d= gXnpKwh7hbXdY3bznqsHoHU$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...MAF...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 34920343 34870257 33690162 32730096 31830044=20
    30980012 30880086 31490149 31930233 32110346=20
    32460407 33150428 34220398=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 10 02:12:29 2025
    AWUS01 KWNH 100212
    FFGMPD
    SCZ000-GAZ000-ALZ000-100700-

    Mesoscale Precipitation Discussion 0415
    NWS Weather Prediction Center College Park MD
    1011 PM EDT Mon Jun 09 2025

    Areas affected...East-central AL...Central GA...West-central SC...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 100210Z - 100700Z

    SUMMARY...A corridor of developing thunderstorms within a
    favorable training environment may pose a streak of 2-3" totals
    with an isolated 4" spot or two.=20=20

    DISCUSSION...GOES-E WV depicts an elongated trough along the East
    Coast States, with a few inflections noted toward the tail end
    across the Southeast. The lead wave is fairly strong and
    progressive exiting Upstate SC into central NC while the secondary
    wave is a big more elongated west to east across central AL. VWP
    shows deep layered unidirectional flow between the waves allowing
    for a favorable west to east training profile. RAP analysis along
    with CIRA LPW denotes the axis between the waves is increasingly
    confluent but also has allowed for increased theta-E air through
    depth for a narrow corridor of 1.75-2" total PWats, as well as
    axis of 1000-1500 J/kg of MLCAPE (favored toward 2000 J/kg
    upstream).

    Regional RADAR shows, old outflow/bowing segment from older
    convection crossing the AL/GA, in front/along the wave, surface to
    boundary layer winds appear to be increasing slightly with
    enhanced backed flow for convergence/ascent into the mid-level
    confluence axis. As such, EIR and RADAR show increasing
    convective activity with spotty stronger updrafts/cooling towers
    across central GA into West central SC. So, while the
    inflow/convergence is likely the most limiting factor, it is
    currently sufficient for cells capable of 1.5-2"/hr rates.=20=20

    Given the length of the corridor and likely consistent
    unidirectional flow to maintain training even through a narrow
    axis, there should be solid opportunity for training/repeating to
    allow for a streak or two of 2-3" in 1-3hrs with perhaps an
    isolated 4" spot or two; and while the ground conditions are
    relatively dry, especially toward the SC/GA line, these rates and
    potential totals have solid potential for isolated FFG exceedance
    and possible incident(s) of flash flooding over the next few
    hours.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4jQKAe_xI8NoO_mNKwuxAWS9XtxxTnxQMeAu6_Y8qnsHAvmraTVBkxy0LwWMcaKbvf7k= rLdpUq3w7BoPbMQqJXFDCbo$ for graphic product...

    ATTN...WFO...BMX...CAE...CHS...FFC...

    ATTN...RFC...ALR...NWC...

    LAT...LON 33868108 33428073 32928135 32698193 32278373=20
    32228479 32308558 32558594 32988591 33218511=20
    33598324 33818193=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 10 03:37:59 2025
    AWUS01 KWNH 100337
    FFGMPD
    NYZ000-NJZ000-PAZ000-100900-

    Mesoscale Precipitation Discussion 0416
    NWS Weather Prediction Center College Park MD
    1137 PM EDT Mon Jun 09 2025

    Areas affected...Eastern PA...South-Central NY...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 100335Z - 100900Z

    SUMMARY...Strong, efficient rainfall producing line of
    thunderstorms likely to continue flash flooding risk in complex
    terrain with spots of 2-3" probable.

    DISCUSSION...CIRA LPW along with RAP and surface analysis shows a
    pocket/narrow wedge of surface to 850mb moisture lifting north
    through N MD into south-central MD with overall totals reaching
    over 1.5" through full depth. The wedged stationary front that
    has been banked up through east-central PA has seen some
    sharpening as the cold air damning region over the
    Poconos/Catskills has seen a low level wind shift from the
    southeast further increasing moisture convergence as the
    initial/leading edge of the effective leading cold front maintains
    about a 20-45 degrees of convergence at the western edge of the
    warm conveyor belt/wedge of enhanced moisture. This higher,
    untapped unstable air continues to run about 500-750 J/kg with
    MUCAPE through the narrowing warm sector still about 250 J/kg into south-central NY.=20

    Aloft, the split in the upper-level jet/maximum diffluence
    continues to provide solid outflow in both directions and
    maintaining updraft strength though the eastern branch arch can be
    seen crossing the Potomac River just upstream which has been
    limited the upstream convective environment a bit more to allow
    for continued inflow across south-central PA. Additionally, as
    the base of the leading shortwave continues to peel northward
    across Lake Ontario, the trailing DPVA is providing a secondary
    push of convergence across north-central PA with new sprouting
    development in Tioga county lifting northward, so while
    instability is reducing, there is sufficient dynamics to maintain
    a risk of slowing eastward propagation cells across south-central
    NY near the surface wave/intersection of the lead/dying cold front
    at the peak of the warm conveyor belt.=20=20

    Throughout the line with total PWats to 1.5", 20-30kts of low
    level, strong convergent/confluent flow should continue to support
    stronger cells capable of efficient warm cloud processes and rates
    of 1.5" occasionally reaching 1.75"+/hr. Oblique cell motion
    toward the NNE and density of convective cores will allow for
    scattered training/repeating elements to increase over 1-2hrs for
    spots of 2-3" totals. Given complex terrain/naturally lower FFG
    values, incidents of flash flooding are likely to continue into
    eastern PA with the Poconos/Catskills at naturally higher risk for
    rapid flows in narrow channels/gullies.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_x61LFay-usRBSoxljti9TPZrQYleq3hQosjiH3DMAcITMbh-FTunpzAwFjVuFvAfpHP= 8vssGY5xzH1_sKZ8-uvp0gY$ for graphic product...

    ATTN...WFO...ALY...BGM...CTP...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 43117482 42607439 41847461 40887516 40117576=20
    39797614 39737660 39807792 40647760 42117689=20
    43097588=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 10 16:37:37 2025
    AWUS01 KWNH 101637
    FFGMPD
    LAZ000-TXZ000-102202-

    Mesoscale Precipitation Discussion 0417
    NWS Weather Prediction Center College Park MD
    1236 PM EDT Tue Jun 10 2025

    Areas affected...East-Central TX...West-Central LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 101636Z - 102202Z

    Summary...Periodic training/repeating of showers and thunderstorms
    with max rainfall rates of 2.5-3"/hr will drive an isolated flash
    flooding risk this afternoon.

    Discussion...Radar trends depict expanding convective coverage on
    a west-east axis over portions of East-Central TX and West-Central
    LA along a weak stationary front, downstream of a decaying MCS and
    associated MCVs south of the DFW Metro. Maximum estimated rainfall
    rates upwards of 2-2.5"/hour are noted within the most intense
    cores per single source radar and MRMS.

    Amid strong insolation, favorable midlevel lapse rates (7-7.5
    degrees), and PWATs of 1.8-2" (around the 90th percentile per SPC
    climatology), the environment is very favorable to support
    efficient warm rain production in the developing activity along
    the front, with hourly rainfall rates of 2.5-3"/hr possible at
    times. While effective shear is generally quite weak across the
    region, short term forecasts from the RAP suggest the approach of
    the MCVs could promote a corridor of enhanced shear oriented
    parallel to the boundary (20-30 kts) to support cell longevity and
    periods of repeating/training.

    As additional cells fill in and align with the upstream complex,
    both the HREF and RRFS PMM suggest localized rainfall totals of
    2-4" are possible along the front. While soil moisture anomalies
    within the affected region are generally around normal, the
    intense hourly rates combined with periods of repeating/training
    will support an isolated flash flood risk going through the
    afternoon.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-GW-sRjXvmcluTaZOuIQkmVsLvs49IQ7VNCkXws0PT4y3a1WTCHaS3MPRbXHgjN4wvBH= _vpIa9DIzXRzWB4E9fnD_No$ for graphic product...

    ATTN...WFO...FWD...HGX...LCH...LIX...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 32299605 31999432 31389217 30929180 30579214=20
    30639323 31019563 31459671 32069678=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 11 01:10:30 2025
    AWUS01 KWNH 110109
    FFGMPD
    TXZ000-110600-

    Mesoscale Precipitation Discussion 0418
    NWS Weather Prediction Center College Park MD
    908 PM EDT Tue Jun 10 2025

    Areas affected...middle Rio Grande Valley into south-central TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 110107Z - 110600Z

    Summary...Flash flood potential from locally high rainfall rates
    of 2 to 3 in/hr will set up over portions of the middle Rio Grande
    Valley into south-central TX through ~06Z.

    Discussion...GOES East infrared satellite and area radar mosaic
    imagery showed an MCS advancing south and east across the middle
    Rio Grande into northern Coahuila. Outflow was observed to be
    primarily advancing southeastward into northern Mexico and down
    the Rio Grande. The progressive nature of the outflow, advancing
    ~30 kt over the past 1-2 hours across Val Verde County, was
    limiting the flash flood threat. However, short term rainfall
    rates within the line of 1 to 1.5 inches in 30 minutes have been
    reported at times since 22Z.

    Southeast of the ongoing convective system was the presence of a
    remnant, increasingly diffuse, outflow boundary that extended from
    near San Antonio Bay WNW across the South Texas Plains toward Del
    Rio. Some localized convective development along this boundary has
    been noted across southeastern Val Verde into western Kinney
    counties over the past 30-60 minutes. SPC mesoanalysis data from
    00Z showed weak inhibition coupled with strong to extreme MLCAPE
    values of 3000 to 4000 J/kg along and south of the boundary, with
    lower CAPE values and modest to moderate inhibition to its north.
    The diurnal cycle along with the approach of an upper level
    shortwave over the western TX/Mexico border should support an
    increase in southerly 850 mb winds through 03Z, along the
    lower/middle Rio Grande Valley with recent RAP guidance supporting
    20 to 30 kt. Increasing upper divergence and diffluence ahead of
    the upper trough and low level convergence ahead of the advancing
    MCS and increasing low level jet may encourage additional cell
    development in advance of the progressive leading edge of the MCS
    in the vicinity of the remnant surface boundary over southern TX.
    The high CAPE/moisture environment along with relatively weak
    deeper layer mean flow could support a few slow moving cells, to
    be followed by a quick inch or two with the expected advancing
    convective line. Localized flash flood potential could result for
    portions of the middle Rio Grande Valley into south-central TX as
    a result.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4MklZ87qO4ZtWTE7P1gBV5ZPAojTBMtx3s8cVwtbQq8-PgjFQSQJCplx4P8IQGoJHK7_= svy-UJ6zkcylj8Jc436UPjs$ for graphic product...

    ATTN...WFO...CRP...EWX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30510048 30429988 30069896 29599843 29109845=20
    28599874 28119929 27970002 28100037 29050089=20
    29320124 29800147 30130134 30460093=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 11 05:30:45 2025
    AWUS01 KWNH 110530
    FFGMPD
    TXZ000-111100-

    Mesoscale Precipitation Discussion 0419
    NWS Weather Prediction Center College Park MD
    129 AM EDT Wed Jun 11 2025

    Areas affected...Central to Southern Texas...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 110530Z - 111100Z

    SUMMARY...Mature MCS likely to start weakening over next few hours
    but continue to have embedded very intense rain rates up to 2"/hr
    which may support localized totals to 3.5". Increasingly
    scattered incidents of flash flooding are still possible through
    morning.

    DISCUSSION...GOES-E 10.3um shows large MCC across the southeastern
    Edwards Plateau heading into the more hydrologically sensitive
    Balcones Escarpment. Cloud tops have been generally cooling on
    the periphery of the cloud shield, though the center continues to
    bubble with numerous over shooting tops colder than -75C. AMV/WV
    suite shows the upper-level vorticity center is starting to carve
    out some sort of broad closed low across the Pecos River Valley
    with a upstream speed max at 500-300mb rounding the southwest
    quadrant with a broad diffluent pattern noted over the core of the
    MCC. As such, latent heat release from the strong convection and
    solid outflow is rapidly strengthening an MCV just west of KSAT
    along the Balcones Escarpment. Surface temperatures still remain
    in the mid to upper 80s over mid 70s TDs supporting a narrow
    corridor of remaining significant 3000 J/kg CAPEs to maintain
    strong updrafts to further feed the MCV. Isallobaric wind
    response to the MCV is resulting in strong convergence along and
    downstream in the effective warm-advection wing of the cyclone
    across the eastern Hill country providing solid convergence to
    maintain scattered convection even where instability has reduced
    substantially northward into the Heart of Texas. Given slightly
    longer duration in weaker steering flow (within the southeast
    quadrant of the developing closed low aloft further west),
    localized pockets of 2-3" totals. Combine this with lowered FFG
    and saturated upper soils from last night's MCS, will keep
    potential for scattered possible incidents of flash flooding
    through the late overnight period.

    South of San Antonio into Southern Texas...
    Rates will remain strongest with the higher unstable, greater deep
    moisture (TPW to 2"+) along and southward along the bowing
    segment. However, given it will continue to be bowing out likely
    with some downward mixing from mid-level rear inflow jet...faster
    forward progress should limit overall totals likely to 1-1.5" in
    30-60 minutes. Given these rates will be over higher FFG of South
    Texas, the potential for flash flooding will be likely limited to
    urban centers and traditionally prone areas with those extreme
    short-term bursts. So while it is not completely a non-zero
    chance, the potential for FF, south of I-10 is much reduced.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7LVeQc-XfvkX2x1aP6ZjA0PlHnskdFZrUw5CB32dj7jBuqhwRe5fwyfdAeChSQL2edC2= pIIA93fktz2miJGTaGHvsvg$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32229696 31989610 31209593 29959673 28039753=20
    27499825 27379893 27529968 27819995 28969935=20
    29889954 30909995 31569946 32059829=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 11 18:23:55 2025
    AWUS01 KWNH 111823
    FFGMPD
    LAZ000-ARZ000-TXZ000-120007-

    Mesoscale Precipitation Discussion 0420
    NWS Weather Prediction Center College Park MD
    223 PM EDT Wed Jun 11 2025

    Areas affected...Eastern TX...Far Western LA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 111822Z - 120007Z

    Summary...Additional showers and thunderstorms are developing
    along and ahead of a persistent MCS in eastern TX. Training
    segments ahead of the MCS, and overlapping of heavy rainfall will
    drive additional scattered flash flooding this afternoon.

    Discussion...A complex forecast continues this afternoon as an MCS
    persists across Eastern TX, with leading thunderstorm segments
    exhibiting training characteristics further north in the over
    North TX into the Piney Woods Region of LA. Estimated hourly
    rainfall rates varied somewhat within this activity, between
    1.5-2"/hr (west of Lake Charles) and 3"/hr (near Shreveport).

    This uptick in coverage and intensity is likely due to the
    activity realizing a NW-SE oriented instability axis characterized
    by 1000-3000 J/kg MLCAPE, 2-2.3" PWATS, and 20-30 kts of
    southwesterly effective shear amid a variety of convergence
    boundaries analyzed across the region.

    Going forward, expect training and repeating of cells to drive
    scattered instances of flash flooding this afternoon and evening.
    Recent runs of the RRFS and HRRR maintain the best handle on the
    general placement and structure of the ongoing activity, and
    suggest additional rainfall totals of 2-5" can be expected.
    Locally considerable flash flooding impacts cannot be ruled out
    over areas which saw heavy rainfall earlier this morning.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-cARqypZkz9e3f5O0D3qEZqDVQmwcrIPTd9oAGPu9NHncpWNxbx1i_E0kQN5EzazxGkW= 7WjHDDAeBI9jgTXQLHRo-2w$ for graphic product...

    ATTN...WFO...FWD...HGX...LCH...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 33509527 33309407 32699359 31489332 29889297=20
    29369356 29499436 31069518 31549669 32269715=20
    33129645=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 11 21:34:55 2025
    AWUS01 KWNH 112134
    FFGMPD
    TXZ000-OKZ000-120315-

    Mesoscale Precipitation Discussion 0421
    NWS Weather Prediction Center College Park MD
    534 PM EDT Wed Jun 11 2025

    Areas affected...central TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 112131Z - 120315Z

    Summary...Slow moving storms atop portions of saturated soils are
    expected to produce locally heavy rain in excess of 3-5 inches
    over the next 3-6 hours for portions of central TX. Localized to
    scattered flash flooding is expected to result.

    Discussion...Water vapor imagery from GOES East showed a
    south-north elongated mid to upper-level low over west-central TX
    at 2115Z, slowly edging eastward. One of the embedded vorticity
    maxima was located halfway between BPG and ABI and a small cluster
    of slow moving thunderstorms has developed to its south and east.
    A general decrease in low to mid-level cloud cover since 17Z has
    helped with surface heating to the west of a broader shield of
    cloud cover over eastern TX. SPC mesoanalysis data from 21Z showed
    MLCAPE of 500-1500 J/kg over western and central TX with patchy
    but decreasing CIN along and west of I-35.

    RAP forecasts show the mid to upper-level trough and embedded
    vorticity maxima will slowly translate eastward over the next
    several hours. Additional convective development is likely over
    west-central TX in the short term, and over northern portions of
    the Edwards Plateau into portions of the I-35 corridor south of
    Forth Worth beyond sunset. While PWs are not as high as those over
    east TX, they are still about 1.5 to 2.0 inches (via SPC
    mesoanalysis) and slow cell movement of 10 kt or less beneath the
    upper low will promote locally high rainfall rates of 1-3 in/hr.

    Heavy rain over the past 72 hours has increased soil moisture and
    reduced FFG to less than 2.5 inches in 3 hours for many locations.
    While the coverage of slow moving rain rates should remain
    localized to scattered (at best), a fairly broad region of central
    TX will be under threat of localized flash flooding with 2 to
    3-hour totals of 3 to 5 inches possible through 03Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8DY1QUIkwGtfiWPwhIo6nk_rB7mBgFrNvxZnJl-CajmbjmT-CbydrISBr5Kv8TXYa7mI= cgbpiNR7yx5rI2ZIppSc60A$ for graphic product...

    ATTN...WFO...EWX...FWD...OUN...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 33939736 33759676 33419632 32749625 31639662=20
    30459774 30219949 30620036 31230061 31620069=20
    32140051 33099941 33669825 33829780=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 12 03:07:59 2025
    AWUS01 KWNH 120307
    FFGMPD
    TXZ000-120730-

    Mesoscale Precipitation Discussion 0422
    NWS Weather Prediction Center College Park MD
    1107 PM EDT Wed Jun 11 2025

    Areas affected...central TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 120304Z - 120730Z

    Summary...Areas of heavy rain from slow moving thunderstorms are
    likely to produce scattered areas of flash flooding across
    portions of central TX through 07Z. The threat of flash flooding
    is expected to increase toward the south with time and a few spots
    of 3 to 6+ inches may lead to significant/considerable impacts.

    Discussion...GOES East water vapor imagery showed the southern end
    of a mid to upper-level low over west-central TX along the
    northern end of the Edwards Plateau near the Colorado River at
    0230Z. Radar imagery showed scattered thunderstorms from the
    Edwards Plateau, northward to I-20 and as far east as I-35. MRMS
    hourly rainfall was topping out near near 4 inches just north of
    Waco while other cells to the west of I-35 and near I-20 showed
    peak hourly rainfall of 1-2 inches. The environment as sampled by
    the 00Z FWD RAOB and depicted on the 02Z SPC mesooanalysis showed
    modest mid-level lapse rates of 6.2 C/km, tall/skinny CAPE with
    500-1500 J/kg mixed layer instability and PWs that ranged from 1.7
    to 1.9 inches across the region. The 00Z FWD sounding also showed
    a wet-bulb zero height of 12.6 kft, indicative of the potential
    for warm rain processes.

    Over the next 3-5 hours, the southern lobe of the mid-level low
    will slowly edge east while 925-850 mb layer flow increases from
    southern to eastern TX into the 20 to 30+ kt range. Slow moving
    cells will continue across the region with the slowest motions
    closest to the mid-level low/trough placement...west of the
    Metroplex to just north of the Edwards Plateau. By 06Z (1 AM CDT),
    the increasing magnitude of the low level flow and low level
    convergence along its leading edge should allow for expanding
    convective development to focus farther southtoward San Antonio
    while slowly expanding east across the I-35 corridor. Cells will
    show a mixture of slow movement, back-building/training and
    merging which will be capable of 2 to 3+ in/hr rainfall.

    Given recent heavy rain and the expectation of localized
    additional totals of 3 to 6+ inches through 07Z to 08Z, scattered
    areas of flash flooding will be likely. 01Z and 02Z WoFS indicated
    the greatest potential for 3+ inches of rain over the following 6
    hours to be from near San Antonio, northward to just west of
    Austin (50-80 percent probs). In addition, 90th percentile data
    (reasonable worst case scenario) showed 10 to 12 inches of rain in
    some of these same locations. While 10 to 12 inches of rain may be
    a high bar to reach, even 50th percentile QPF values of 4-5 inches
    from the WoFS is noteworthy. These rains may lead to locally significant/considerable flash flood impacts, especially given the
    sensitive terrain of the TX Hill Country.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8YndtCGAs8KoCkAgOuZoFZR-gu-Fgd_InPfDR65XJRHG_XTfRp-j-Zl0TMax_ELjbBQb= oL9gywSBuQKOh6os3q1vc4A$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 33139750 32209651 30479643 29239715 28719821=20
    28699924 29249992 30859989 32009901 32969858=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 12 08:00:43 2025
    AWUS01 KWNH 120758
    FFGMPD
    TXZ000-121300-

    Mesoscale Precipitation Discussion 0423
    NWS Weather Prediction Center College Park MD
    358 AM EDT Thu Jun 12 2025

    Areas affected...TX Triangle region into the Middle and Upper TX
    Coast

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 120755Z - 121300Z

    Summary...Localized hourly rainfall totals as high as 3-4"
    expected to continue into mid-morning. Numerous instances of flash
    flooding are likely (some life threatening to locally extreme)
    with additional localized totals of 6"+ expected (with 8"+ amounts
    possible).

    Discussion...Clusters of thunderstorms are in the process of
    growing upscale into a mesoscale convective system (MCS) across
    western portions of the TX Triangle region, from the San Antonio
    area northeastward to near Waco. Storms are generally organizing
    linearly along the southern and eastern periphery of the
    established cold pool, where instability is greatest (1000-3000
    J/kg of SBCAPE) with increasing low-level moisture transport (in
    association with a strengthening nocturnal low-level jet with
    925mb winds of 25-30 kts from the SSE). PWs have also increased to
    a very impressive 1.9-2.3 inches, nearing daily max record levels
    (using CRP sounding climatology as a proxy). Localized hourly
    rainfall totals are estimated to be as high as 3-4" (per MRMS), a
    resulting of training (as deep layer steering flow is oriented
    nearly parallel to the cold pool boundary, due to the favorable
    placement of a mid-upper level low) and warm rain processes
    dominating (with wet bulb zero heights around ~13k feet). Storms
    training from west-to-east (along the southern edge of the cold
    pool) in the vicinity of San Antonio are particularly concerning,
    given the flooding sensitivities of the metro area. Meanwhile, a
    separate cluster of thunderstorms are growing in strength and
    coverage near the Middle TX Coast (where PWs are maximized) due to
    the strengthening low-level jet and associated warm-air
    advection/isentropic ascent.

    Storms should only continue to organize this morning, given the
    very favorable aforementioned environment (with differential
    divergence only increasing further over the next several hours).
    Hi-res models (both the 00z HREF and experimental 18z REFS
    ensembles) are in excellent agreement with both the expected
    magnitudes and placement of QPF with relatively high probabilities
    (40-60%) for both localized 5" exceedance (40-km neighborhood) and
    1" exceedance overlap (10-100 km Ensemble Agreement Scale). This
    corresponds with high FFG exceedance probabilities (up to 60-70%)
    and a decent chance (up to 25-35%) of locally exceeding 100-yr
    ARIs. Given this strong ensemble signal, localized 6"+ totals are
    expected (and it is notable that hourly HRRR/RRFS runs have been
    fairly consistent in depicting localized 8"+ totals, primarily
    between the Corpus Christi and Houston metros where repeating
    heavy rainfall is most likely). Numerous instances of flash
    flooding are likely, some of which are expected to be life
    threatening. Given the potential for 100-yr ARI exceedance,
    extreme instances of localized flash flooding are possible (with
    areas that do not typically flood at risk of experiencing flash
    flooding).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6DZOWV8JTor6182-ZxpoyfYaoFai91QBvupthK3DBZ1DNtJWghSvIB1PH6QwNHseSWq2= nCBg5hmAlLFXqBUNJ3MydBY$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...SHV...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32049643 31979551 31329461 29789487 29099531=20
    28689613 28389719 28619862 29179932 29799937=20
    30279846 30989817 31929747=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 12 13:01:47 2025
    AWUS01 KWNH 121301
    FFGMPD
    TXZ000-121802-

    Mesoscale Precipitation Discussion 0424
    NWS Weather Prediction Center College Park MD
    900 AM EDT Thu Jun 12 2025

    Areas affected...South-Central TX into the TX Piney Woods region

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 121300Z - 121802Z

    Summary...Flash flooding (some of which could be life threatening)
    will continue this morning as training thunderstorms containing
    localized hourly rainfall rates of 3-4" an hour continue.

    Discussion...An axis of training thunderstorms containing
    localized 3-4" an hour rainfall rates continues over South-Central
    TX along a well defined cold pool. Over the last 12 hours, these
    cells have resulted in prolific heavy rainfall amounts across the
    area, with localized amounts of 7-10" observed across
    South-Central TX into the Central TX Coastline. As highlighted in
    MPD 423, inflow characterized by 1500-3000 J/kg of MLCAPE, minimal
    CIN, 2-2.3" PWATs will continue to foster new cells upwind of the
    complex, which will train given the parallel orientation of the
    steering flow to the cold pool.

    As such, additional flash flooding is expected to continue through
    this morning and afternoon. Of note is that the HRRR and RRFS --
    which are handling the ongoing activity the best -- are around 1-2
    hours too slow with propagating the cold pool southward compared
    to radar observations, which could suggest the upper-end of their
    forecast rainfall amounts through 18z (7-8") are overdone.
    However, in light of ongoing impacts and potential for extreme
    3-4" hour rainfall rates, any additional rainfall will quickly
    translate to runoff. Life threatening flash flooding impacts
    remain possible atop areas hit hard earlier today, and over
    sensitive urban areas.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!__aj6jkVosj9m68XnO4KacRb0YmHUwUXRBlutGB_0mVEDydz3T5CKOUtxbmqM4UCF9Mf= XwAEkYe1oJwbzBpnrhBBWpA$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...LCH...SHV...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31469471 30969391 29989405 29319464 28669558=20
    28159725 28409872 28879936 29309932 29379876=20
    29419765 29729705 30389676 31029624 31389561=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 12 23:25:41 2025
    AWUS01 KWNH 122325
    FFGMPD
    MNZ000-SDZ000-NDZ000-130400-

    Mesoscale Precipitation Discussion 0425
    NWS Weather Prediction Center College Park MD
    724 PM EDT Thu Jun 12 2025

    Areas affected...northeastern SD into southwestern MN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 122323Z - 130400Z

    Summary...Localized flash flooding may occur over northeastern
    portions of SD into southwestern MN through 04Z. Rainfall rates of
    1-2 in/hr and localized totals of 2-3 inches are possible.

    Discussion...Recent radar imagery through 23Z showed the recent
    intensification of a thunderstorm over northern Spink County
    (south of Aberdeen) along with scattered showers extending from
    the eastern ND/SD border into central MN. These cells were
    elevated, located north of a wavy quasi-stationary front that
    extended westward into eastern SD, then southwestward into
    northwestern NE. Lift in advance of a 700-500 mb shortwave trough
    (extending from northeastern MT into western SD) and advection of
    low level moisture via a 20-25 kt 850 mb jet has allowed for an
    increase in MUCAPE north of the front, aiding in the recent
    intensification.

    850 mb winds are forecast to further strengthen a bit to near 30
    kt by 03Z from the eastern SD/NE border and northward to the
    front, according to recent RAP forecasts, allowing for potential
    upstream thunderstorm development. While instability will likely
    remain a modest 500-1000 J/kg over northeastern SD via short term
    HRRR/RAP forecasts, an observed GPS PW just east of the northern
    SD/MN border was 1.5 inches at 22Z, near the climatological max at
    ABR for mid-June. The mean steering flow of cells is expected to
    be from the WSW to W, roughly parallel to the frontal boundary to
    the south, which will support repeating rounds of heavy rain from
    west to east. Rainfall rates of 1-2 in/hr may occur at times and
    there will be the potential for 2-3 inches of rain through 04Z.

    This rain may overlap with locally hydrologically sensitive
    regions, including urban centers and portions of Brown and
    Marshall counties, which received locally heavy rain (up to 4
    inches) earlier today. Localized flash flooding could result from
    parts of northeastern SD into far southwestern MN through 04Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!77HmyaFbLjzuYrBy_F49UY2RfE7-0A4T8l6jh-1VIIl5o8lWbiugMoVq4hnScUlbA41D= MWbMjxF4ZU_-LNuFLolp_Fw$ for graphic product...

    ATTN...WFO...ABR...BIS...FGF...FSD...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45989717 45839581 45499528 44929549 44709668=20
    44639830 44569985 44980071 45630060 45959913=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 13 07:01:19 2025
    AWUS01 KWNH 130701
    FFGMPD
    WIZ000-MNZ000-SDZ000-NDZ000-131200-

    Mesoscale Precipitation Discussion 0426
    NWS Weather Prediction Center College Park MD
    300 AM EDT Fri Jun 13 2025

    Areas affected...south-central MN and some surrounding portions of
    far northeast SD, southeast ND, and western WI

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 130700Z - 131200Z

    Summary...Bands of slow moving heavy rainfall with localized
    hourly totals of 1-2" may result in 5"+ totals through 7am CDT.
    Isolated to scattered instances of flash flooding are likely (and
    may be locally significant).

    Discussion...Bands of slow moving heavy rainfall are taking shape
    early this morning across portions of far northeastern SD and
    south-central MN, in response to strengthening isentropic ascent
    (concentrated on 295-300K surface) amid veering low-level (925-850
    mb) flow. While the low-level jet is actually expected to weaken a
    bit over the next several hours (from 30-35 kts to 25-30 kts), the
    moisture transport (and more importantly the resulting isentropic
    ascent) will conversely become stronger and more pronounced (as
    the flow orients perpendicular to the isobars on the 300K
    isentropic surface). The resulting conditional symmetric
    instability (CSI) is driving the convective heavy rainfall threat
    this morning (even though MUCAPE of 250-500 J/kg is underselling
    the threat) with anomalously high wet bulb zero heights (~11k
    feet), 850 mb mixing ratios (~10 g/kg), and precipitable water
    (~1.5") all near the 90th percentile (per MPX sounding
    climatology).

    Hi-res CAMs have so far struggled to appropriately model what is
    ongoing, as impressive slow moving bands of heavy rainfall are
    indicated to be producing 15-min totals nearing 1" and hourly
    totals approaching 2" (per MRMS estimates). While modest low-level
    flow is producing these bands, the flow aloft within the layer of
    skinny CAPE from 700-500 mb is from the west at only about 10-20
    kts. These slow moving heavy rainfall bands will tend to train
    form west-to-east (while gradually lifting north a bit), and while
    some of the CAMs do hint at localized 2" hourly totals (primarily
    the ARW2 and NAM-nest) they're likely underestimating the scale of
    the potential (given ongoing observational trends, which are
    occurring meaningfully south and east of the main model signal).
    Even still, the post-processed statistical data from the 00z HREF
    is hinting at the relative high-end potential from this event with
    40-km neighborhood 6-hr probs for 3" and 5" exceedance of 25-45%
    and 5-15%, respectively. This corresponds with relatively high
    odds of 6-hr FFG exceedance (25-35%), as well as a chance (20-40%)
    of 10-yr ARI exceedance and a slight chance (up to 10%) for 100-yr
    ARI exceedance. Overall the HREF solutions are considered to be
    underestimating the threat, and therefore isolated to scattered
    instances of flash flooding are considered likely (and may be
    locally significant, given that training 1-2"/hr rainfall rates
    may result in localized 3-6 hour totals of 5"+).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9GeO2Y_p77Jj9o2SbODDn2-XHhR37R_OH3EPWgoHh1cIuV3EhMFJSjsO1IGuvGB0qT-J= TYOT9z_2w22QGOGiRuATaDY$ for graphic product...

    ATTN...WFO...ABR...ARX...BIS...DLH...FGF...FSD...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 46489497 46459367 46079266 45309223 44499244=20
    44089316 43979412 44399572 45099743 45719854=20
    46389765 46459629=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 13 11:17:50 2025
    AWUS01 KWNH 131117
    FFGMPD
    LAZ000-TXZ000-131716-

    Mesoscale Precipitation Discussion 0427
    NWS Weather Prediction Center College Park MD
    717 AM EDT Fri Jun 13 2025

    Areas affected...southern Louisiana, far southeast Texas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 131116Z - 131716Z

    Summary...A cluster of slow-moving storms have produced estimated
    4-6 inch rainfall totals near Lafayette, Louisiana this morning.=20
    This cluster is expected to very slowly evolve within a very
    unstable airmass, posing a risk for flash flooding through
    17Z/noon CDT.

    Discussion...Scattered thunderstorms have managed to evolve into a
    persistent, slow-moving cluster near Lafayette this morning. The
    storms are embedded in deep south-southwesterly steering flow of
    around 20-25 knots, but have managed to backbuild locally due to
    1) confluent 850mb wind fields evident via objective analyses, 2)
    a weak surface boundary extending from near Galveston, TX
    east-northeastward through Lafayette to near Hammond, LA, and 3)
    strong instability/weak inhibition along and south of that subtle
    boundary. Impressive moisture/instability content within the
    pre-convective airmass (2000 J/kg MLCAPE, 2 inch PW values) were
    contributing to impressive local rain rates exceeding 2.5
    inches/hr at times. With 4-6 inches of rain having already
    fallen, some impacts are likely with the ongoing activity in the
    short term.

    Through 17Z/noon CDT, the reinforcement of a surface/outflow
    boundary near the convection (due to cold pool formation) will
    likely enable continued development and training of cells. Some
    propagation of this cluster is expected, and both westward and
    eastward development of storms toward areas near Lake Charles and
    near/south of Baton Rouge can be expected. Another 3-5 inches of
    rainfall can be expected beneath the heavier, slower-moving
    thunderstorm bands as well. Locally higher amounts cannot be
    ruled out in a few spots.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8brUbtbNUCQexOiyQDMY6PJWizYuk4hFh28TcfdfEDKSg8D2K1Jtq_Jy87nnWU4uA2ZX= aECCbvGA9w68lP9Pz_sOiSM$ for graphic product...

    ATTN...WFO...HGX...LCH...LIX...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 30509132 30289060 29989016 29599001 29229034=20
    29169115 29539237 29659388 29469442 29779450=20
    30179381 30479252=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 13 17:10:31 2025
    AWUS01 KWNH 131709
    FFGMPD
    LAZ000-TXZ000-132137-

    Mesoscale Precipitation Discussion 0428
    NWS Weather Prediction Center College Park MD
    108 PM EDT Fri Jun 13 2025

    Areas affected...far southwest Louisiana, southeast Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 131707Z - 132137Z

    Summary...A few instances of flash flooding are possible for the
    next 2-4 hours (through 21Z) as slow-moving storms produce 1-3
    inch/hr rain rates across the discussion area.

    Discussion...Scattered convection has developed in earnest across
    areas near Beaumont and Lake Charles over the past couple hours.=20
    These storms are in a weakly sheared environment, with slow
    movement amid 2 inch PW values and 3000+ J/kg MLCAPE promoting
    rain rates of 1-2.5 inches/hr per MRMS. Storms are focused along
    a remnant outflow boundary extending from west-southwest to
    east-northeast across the region and a newer, stronger outflow
    boundary from south-central Louisiana that was currently near Lake
    Charles and propagating westward. These outflow boundaries will
    continue to encourage deep moist convection over the next 2-4
    hours over wet/sensitive ground conditions from prior rainfall
    over the past 48 hours. 2-2.5 inch/hr FFG thresholds are likely
    to be exceeded at times in this regime, and additional impacts to
    metro areas in the discussion area (i.e., Lake Charles, Beaumont,
    and eventually Houston) cannot be ruled out.

    At some point beyond 21Z/4p CDT, the expectation is that
    widespread convective overturning may temper the extent and
    intensity of convection along with resultant rain rates. Storms
    will mainly be outflow dominant given the weak low-level and deep
    shear across the discussion area. Between no

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!80gK5CFsjzotVDDdFn8D2Rins2BSrPtr11c-IPaZKv_A4fvVYQKUAG9nn1nUANK6ATxS= heW7p2APPVoX0sepZe4_Uvg$ for graphic product...

    ATTN...WFO...HGX...LCH...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 31109459 31089369 30649264 30059260 29659409=20
    29089601 29369649 30109621 30639552=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 13 17:30:53 2025
    AWUS01 KWNH 131730
    FFGMPD
    LAZ000-TXZ000-132137-

    Mesoscale Precipitation Discussion 0428
    NWS Weather Prediction Center College Park MD
    130 PM EDT Fri Jun 13 2025

    Areas affected...far southwest Louisiana, southeast Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 131707Z - 132137Z

    Summary...A few instances of flash flooding are possible for the
    next 2-4 hours (through 21Z) as slow-moving storms produce 1-3
    inch/hr rain rates across the discussion area.

    Discussion...Scattered convection has developed in earnest across
    areas near Beaumont and Lake Charles over the past couple hours.=20
    These storms are in a weakly sheared environment, with slow
    movement amid 2 inch PW values and 3000+ J/kg MLCAPE promoting
    rain rates of 1-2.5 inches/hr per MRMS. Storms are focused along
    a remnant outflow boundary extending from west-southwest to
    east-northeast across the region and a newer, stronger outflow
    boundary from south-central Louisiana convection that was
    currently near Lake Charles and propagating westward. These
    outflow boundaries will continue to encourage deep moist
    convection over the next 2-4 hours over wet/sensitive ground
    conditions from prior rainfall over the past 48 hours. 2-2.5
    inch/hr FFG thresholds are likely to be exceeded at times in this
    regime, and additional impacts to metro areas in the discussion
    area (i.e., Lake Charles, Beaumont, and eventually Houston) cannot
    be ruled out.

    At some point beyond 21Z/4p CDT, the expectation is that
    widespread convective overturning may temper the extent and
    intensity of convection along with resultant rain rates. Storms
    will mainly be outflow dominant given the weak low-level and deep
    shear across the discussion area.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4NA3V57CdURoU6XpbOVafLG8lyBrHSX9lipqQZqJfcO7ZWzG0AUpCFjUFx12gyOCBcC2= 7pKoF1EN3kmMjh9hPOIskg4$ for graphic product...

    ATTN...WFO...HGX...LCH...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 31109459 31089369 30649264 30059260 29659409=20
    29089601 29369649 30109621 30639552=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 14 00:30:26 2025
    AWUS01 KWNH 140030
    FFGMPD
    MDZ000-VAZ000-WVZ000-140559-

    Mesoscale Precipitation Discussion 0429
    NWS Weather Prediction Center College Park MD
    829 PM EDT Fri Jun 13 2025

    Areas affected...Central Appalachians....Southern DelMarVa

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 140029Z - 140559Z

    Summary...Periods of cell training along an increasingly defined
    cold pool should maintain the threat of scattered flash flooding
    through this evening.

    Discussion...Radar depicts an west-east axis of showers and
    thunderstorms growing upscale along an increasingly defined cold
    pool bisecting Central Virginia. Recent single source and MRMS
    hourly rainfall estimates show increasing rainfall efficiency
    within the most robust convective cores -- with localized 2-3" an
    hour rates noted over the last 30 minutes.

    Inflow characterized by 1.7-2.1" PWATs, 1500-2000 J/kg of MLCAPE
    (with minimal CIN), and deep warm cloud layers of 13,000-14,000
    feet, and 20-25 kts of effective shear will support additional
    convective clusters which could train/repeat given the parallel
    orientation of the steering flow to the emerging cold pool.

    Through 6z, the 18z HREF (supported by recent runs of the HRRR and
    RRFS) suggest the main corrior of concern will remain over
    North-Central Virginia. Probabilities of 6 hour QPF exceeding the
    10-100 year ARI in this region range from 20-30% and 10-25%,
    respectively. Additional scattered instances of flash flooding
    remain possible, some of which could be locally considerable.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7_9Af7xbdhiiX_t57DrbKE_Ucp1kkX7SM1qs9rix-DGVcyHJ3H5Xcovhyg8hv0ba5oFU= rHwTqm5eSaQzI7FtzDRfk1c$ for graphic product...

    ATTN...WFO...AKQ...LWX...RLX...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 38747781 38657683 38237636 37597677 37377741=20
    37327913 37728063 38278071 38498024 38487892=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 14 03:04:31 2025
    AWUS01 KWNH 140302
    FFGMPD
    TNZ000-MSZ000-ARZ000-140900-

    Mesoscale Precipitation Discussion 0430
    NWS Weather Prediction Center College Park MD
    1101 PM EDT Fri Jun 13 2025

    Areas affected...Central AR into northwest MS and southwest TN

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 140300Z - 140900Z

    Summary...Localized hourly totals of 1-2" expected to continue
    through the overnight hours, and training/repeating elements may
    lead to additional localized totals of 2-4" (on top of areas that
    have already seen as much as 2-4" in recent hours). Isolated to
    scattered instances of flash flooding are likely.

    Discussion...A deep layer (sfc-250 mb) cyclone is nearly
    stationary this evening over MO/IL, with deep layer cyclonic flow
    organizing bands of showers and thunderstorms along the southern
    periphery of the circulation. While heavy rainfall has generally
    been progressive within 20-30 kts of steering flow (850-300 mb),
    recent convective initiation to the southwest and south of the low
    center (concentrated mostly across northwestern and central AR) is
    allowing for localized elements of west-to-east training. This is
    resulting in localized hourly totals of up to 1-2" (with the
    highest totals confined just to the southwest of Memphis at the
    time of writing), per MRMS estimates. Low-level moisture transport
    is already on the rise in this area (mainly at 850 mb from the
    WSW), and should only become more robust closer to the surface
    over the next 3-6 hours (with strengthening isentropic upglide
    anticipated along the 300K surface as winds near 925 mb veer to
    the WSW and increase from 10-20 kts to 20-25 kts). In addition,
    the mesoscale environment is characterized by precipitable water
    values of 1.6-1.8" (and expected to increase to 2.0"+, between the
    90th percentile and max moving average per LZK sounding
    climatology), ML CAPE of 1000-2000 J/kg, and effective bulk shear
    of 25-35 kts.

    While the steering flow should continue to favor localized
    training and repeating of convection, upwind propagation vectors
    are also weak and variable in the vicinity of east-central AR into
    northwest MS and southwest TN. This is precisely where localized
    Flash Flood Guidance (FFG) exceedance is most likely to occur, as
    3-6 hour FFGs are as low as 1.5-2.5" (and in reality are likely
    even lower now, as this guidance applies to 00z and localized 2-4"
    totals have occurred since then with some local FLASH CREST unit
    streamflow response suggesting some minor flood impacts already
    ongoing). Looking ahead to the next 3-6 hours, additional heavy
    rainfall is expected along the base of the aforementioned deep
    low, with impacts most likely from Little Rock to Memphis and
    surroundings. Recent HRRR runs are in good agreement with this
    corridor, suggesting additional localized totals of 2-4" are
    possible (with continued potential for hourly totals up to 1-2").
    Isolated to scattered instances of flash flooding are likely.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Yz3QWHgHl8yBgvhFJmwIaKWJ0qxpj3iJlH-l0SDTdlngN8Fjm5OriqreI__9qXNVtfm= Vp1F9_itIZI_38LuWxyjYIA$ for graphic product...

    ATTN...WFO...LZK...MEG...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 35608908 34848878 34278981 34429176 35039300=20
    35379313 35579255 35499078=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 14 09:57:53 2025
    AWUS01 KWNH 140957
    FFGMPD
    OKZ000-KSZ000-141500-

    Mesoscale Precipitation Discussion 0431
    NWS Weather Prediction Center College Park MD
    556 AM EDT Sat Jun 14 2025

    Areas affected...south-central KS into north-central OK

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 140955Z - 141500Z

    Summary...Additional localized totals of 2-5" may result in
    isolated to scattered flash flooding through mid-morning.

    Discussion...A maturing MCS is forward propagating
    south-southeastward across portions of eastern KS this morning,
    producing hourly totals as high as 2.0-2.5" (with the help of
    convective initiation out ahead of the system). Farther south into north-central OK, convection has managed to initiate within a
    moderately capped environment (CIN 75-150 J/kg) due to weak
    moisture convergence along a quasi-stationary front. These storms
    are nearly stationary within weak steering flow, producing
    impressive localized hourly totals of up to 2-3". The mesoscale
    environment downstream of the MCS and in the vicinity of the OK
    storms is characterized by SBCAPE of 2000-3000 J/kg, precipitable
    water values of 1.6-1.8" (above the 90th percentile and near the
    max moving average, per OUN sounding climatology), and effective
    bulk shear of 15-20 kts.

    Although shear should be a somewhat limiting factor for storm
    organization, the mature MCS and associated MCV will likely
    continue to be sufficient forcing for continued longevity, given
    observational trends (despite MCS maintenance values of only
    20-40%, largely owing to the lack of shear and deep layer mean
    flow). CAMs are somewhat supportive of additional rainfall (while
    largely struggling with the OK convective initiation, in
    particular), as 06z HREF 40-km neighborhood probabilities for 3-hr
    and 6-hr FFG exceedance are around 15-25% (thru 15z). Additional
    localized totals of 2-5" are possible, and much of that is likely
    to fall within a period of only 1-2 hours.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-EyPxtMb02-tfX3vI-GrGhECHwGv1qVVOS1xOqmQs1r62_TM2QRzjSbqKtnHM2KrdlwP= hbJ4ov8oVxfa1hVCo0dc5VQ$ for graphic product...

    ATTN...WFO...DDC...GID...GLD...ICT...OUN...TSA...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39499929 39059834 38449758 37739689 36769642=20
    36129658 35469786 35519883 36539919 37410063=20
    37950082 38370048 39469980=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 14 13:10:07 2025
    AWUS01 KWNH 141310
    FFGMPD
    TXZ000-141708-

    Mesoscale Precipitation Discussion 0432
    NWS Weather Prediction Center College Park MD
    909 AM EDT Sat Jun 14 2025

    Areas affected...portions of southeast Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 141308Z - 141708Z

    Summary...A mesoscale complex has organized near Galveston and
    continues to propagate slowly westward toward areas near/south of
    Houston. These trends should continue over the next 2-4 hours or
    so, posing an isolated flash flood risk through 17Z/noon CDT today.

    Discussion..Convection that had initially formed over along and
    just offshore of the Texas coast has matured and formed a
    westward-moving cold pool that currently extends from near
    Downtown Houston southward to Lake Jackson. The storms are
    ingesting air from a very buoyant, weakly capped pre-convective
    environment (3000 J/kg MLCAPE, 2 inch PW). This moisture-rich
    environment and weak shear has fostered development of
    slow-moving, outflow dominant convection to materialize with spots
    of 2 inch/hr rain rates recently observed near Galveston and
    League City.

    Models/observations suggest that the westward-moving outflow
    associated with this complex will be the primary driver of any
    new/sustained convective development over the next 2-4 hours.=20
    This new development - along with areas/spots of 2-3 inch/hr rain
    rates should gradually develop westward and northwestward into
    additional inland parts of southeast Texas. The combination of
    wet soils from recent rainfall and urbanized/sensitive areas near
    Houston Metro suggest that flash flash flooding could occur on an
    isolated basis through the morning as convection evolves.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5M8thc-9DB8NgB6aCJ9ZMPwCmdV4KZC9i2KU6umfjdXrayixQXtZgyw8Vhawxm3tPP6V= xK-ej0evGK5uVnvu1-xkq1Y$ for graphic product...

    ATTN...WFO...EWX...HGX...LCH...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30959483 30359384 29629406 28789549 28989649=20
    29759671 30389640 30799587=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 14 17:47:38 2025
    AWUS01 KWNH 141747
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-142300-

    Mesoscale Precipitation Discussion 0433
    NWS Weather Prediction Center College Park MD
    146 PM EDT Sat Jun 14 2025

    Areas affected...portions of eastern Oklahoma through
    central/southwest Arkansas and far northeast Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 141746Z - 142300Z

    Summary...An intensifying convective complex over eastern Oklahoma
    will sweep through the discussion area and pose a risk of areas of
    1-2 inch/hr rain rates at times. These rates are expected to
    cause localized/isolated flash flood issues through 23Z/6p CDT.

    Discussion...Over the past couple hours, a linear MCS has
    materialized over eastern Oklahoma from near Muskogee to near Ada.
    Cells within this complex were moving east-southeastward at
    approximately 25-30 knots, which has mostly kept peak rain rates
    at around 1-2 inches/hr (just shy of FFG thresholds) so far this
    afternoon.

    As storms migrate downstream through the afternoon and early
    evening, a few considerations for increasing flash flood potential
    exist, including: 1) deepening convection ahead of the complex,
    which should allow for a few areas of mergers to prolong/increase
    rain rates above 2 inches/hr and 2) the orientation of the complex
    itself - which may allow for localized training on occasion. FFG
    thresholds should be breached in a few areas of this complex moves
    through, with low-lying/sensitive areas of particular concern for
    flash flooding.

    Over time, a few of these storms may reach areas just north/east
    of Little Rock that experienced 3-5 inch rainfall totals just a
    few hours ago. These areas may also be locally sensitive and
    prone to flooding.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9G_BsSIDoLxJhPZvUM2AVsLtHQKMlkdfbVjGW2Y7ZxpnETDMTbdPkk_lgO0wbWLHQRxQ= wR-NO6I2WyRbqVH8_rCudB8$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 36119511 36059402 35539176 34769128 33739158=20
    32959393 33609641 34339741 35069773 35569601=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 14 18:32:49 2025
    AWUS01 KWNH 141832
    FFGMPD
    OHZ000-KYZ000-INZ000-ILZ000-150030-

    Mesoscale Precipitation Discussion 0434
    NWS Weather Prediction Center College Park MD
    231 PM EDT Sat Jun 14 2025

    Areas affected...Portions of the OH Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 141830Z - 150030Z

    SUMMARY...Slow-moving showers and thunderstorms with high rainfall
    rates will likely support isolated to scattered areas of flash
    flooding going through the early evening hours.

    DISCUSSION...GOES-E visible satellite imagery along with area
    radars are showing a continued expansion of locally heavy showers
    and thunderstorms across large areas of the OH Valley, but with a
    bit more of a focus along a quasi-stationary frontal zone that is
    draped across the region.

    MLCAPE values have risen to as high as 1500 J/kg along and just
    south of this front extending from southeast IL through southern
    IN. Shear parameters are minimal, but the atmosphere is very moist
    with PWs of 1.6 to 1.8+ inches, and so the convective cells are
    capable of producing very high hourly and sub-hourly rainfall
    rates.

    The convection over the next few hours should generally continue
    to expand given a combination of the diurnal heating
    cycle/boundary layer instability, and also the slow approach of a
    wave of low pressure which is gradually traversing the front from
    the west. Cyclonic low-level flow into the aforementioned front
    should promote an environment where convection is at least
    relatively focused along and near this boundary. However, the
    steering flow is very weak with the 850/300 mb layer mean flow
    generally near or under 10 kts.

    This will promote slow cell-motions, and with the high moisture
    profiles in place, some convective cells may be capable of
    producing as much as 1.5+ inches in 30 minutes. Some spotty storm
    totals of as much as 2 to 4+ inches will be possible going through
    early this evening. The 12Z HREF and the 06Z REFS both depict
    rather elevated probabilities (locally 40 to 50+ percent) for
    seeing the 3-hour FFG exceeded across especially central/southern
    IN and parts of west-central OH given the moist antecedent
    conditions, and this area in particular may see notable concerns
    for flash flooding going through early this evening.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9JncnfDaR554Ytuw3YH9d_QzOUpBLRPoQ0NYmpuq_QgbwPWIy3fQLmbXZ_sBueXXpHro= dRUrS7r6hYWf6lUhB30B6RU$ for graphic product...

    ATTN...WFO...CLE...ILN...ILX...IND...LMK...LSX...PAH...RLX...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 40528323 40048239 39208261 38628387 37978618=20
    37308782 37438874 38108915 38828893 39508787=20
    40188558=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 14 19:42:11 2025
    AWUS01 KWNH 141942
    FFGMPD
    PAZ000-MDZ000-VAZ000-NCZ000-DCZ000-WVZ000-OHZ000-150140-

    Mesoscale Precipitation Discussion 0435
    NWS Weather Prediction Center College Park MD
    340 PM EDT Sat Jun 14 2025

    Areas affected...Upper OH Valley...Central
    Appalachians...Mid-Atlantic

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 141940Z - 150140Z

    SUMMARY...Scattered areas of flash flooding are expected to occur
    this afternoon and into the evening as heavy showers and
    thunderstorms develop and expand in coverage. Locally significant
    urban flash flooding impacts will be possible.

    DISCUSSION...The latest surface analysis shows a quasi-stationary
    front draped across the Mid-Atlantic region and stretching back up
    across the higher terrain of the central Appalachians and the
    upper OH Valley. A substantial amount of moisture is in place
    along this front with PWs in general across the region running
    nearly 2 standard deviations above normal.

    In fact, the 12Z RAOB data from KPIT and KIAD showed very moist
    soundings with PWs of 1.79" and 2.01" respectively. Tall, skinny
    CAPE profiles were noted as well, and thus the environment is
    conducive for highly efficient rainfall processes that could yield
    extreme rainfall rates as convection develops and expands in
    coverage over the next several hours. The airmass along and
    adjacent to the front continues to destabilize with the diurnal
    heating cycle, and MLCAPE values have risen to as much as 1000 to
    1500 J/kg on the warm side of the front across central WV and also
    across central to southeast VA.

    The increasingly concentrated axis of moisture and instability
    along and near the front, along with areas of locally more focused
    surface convergence should favor the regional development and
    expansion of heavy showers and thunderstorms over the next several
    hours. Some modest shear profiles and upper-jet aided
    ascent/divergence over the region should also facilitate this
    evolution with eventually broken clusters of convection
    materializing.

    Near-term convective development over the upper OH Valley and
    central Appalachians is expected with the aid of the front and
    also orographic ascent. However, by late this afternoon and this
    evening, the front itself from the MD/WV Panhandles on down
    through northern/central VA and eventually the Tidewater/Hampton
    Roads area of southeast VA should become quite active with
    convection impacting these areas.

    Rainfall rates may reach 2 to 3 inches/hour with the stronger
    storms given the moist/efficient environment that is in place, and
    some localized storm totals of 3 to 5+ inches are going to be
    possible given the relatively slow cell-motions that are expected.

    A combination of urban sensitivities and moist antecedent
    conditions in general will combine with the additional rainfall
    potential to support a notable threat of flash flooding going into
    the evening hours with at least scattered areas of flash flooding
    likely. Locally significant urban flash flooding impacts will also
    be possible if these heavier rains focus into the urban corridors.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9ZdF_BXZC-jracFekueYoO9JkMdHqj64jPXNE2vLfY8qIpgt_iSS3p16xpQ-62hCZ9or= Cbc1e65bAH6nU7jykWE8FoU$ for graphic product...

    ATTN...WFO...AKQ...CTP...GSP...LWX...PBZ...RAH...RLX...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 40847927 40557796 39957700 38917648 36987556=20
    36267629 36207854 35917986 35748123 36088172=20
    36988074 37918036 38638084 39678195 40568123=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 14 21:45:29 2025
    AWUS01 KWNH 142144
    FFGMPD
    MSZ000-LAZ000-150043-

    Mesoscale Precipitation Discussion 0436
    NWS Weather Prediction Center College Park MD
    543 PM EDT Sat Jun 14 2025

    Areas affected...New Orleans Metropolitan Area

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 142143Z - 150043Z

    SUMMARY...Heavy showers and thunderstorms impacting the broader
    New Orleans metropolitan area over the next few hours will
    continue to support an urban flash flood threat into the early
    evening hours.

    DISCUSSION...The latest radar imagery shows an axis of heavy
    showers and thunderstorms moving into the New Orleans metropolitan
    area including adjacent suburbia. The activity is focusing along
    the leading edge of an outflow boundary while interacting with a
    very moist and unstable airmass pooled across southeast LA.

    MLCAPE values of as much as 2000 to 3000 J/kg are in place with
    PWs of 2.0 to 2.25 inches. This suggests very high rainfall rate
    potential with these storms with potentially 1.5 inches of rain in
    as little as 30 minutes. Over the next few hours, slow
    cell-motions may support some spotty totals of 2 to 4+ inches.

    The activity may last into at least the early evening hours based
    on the latest HRRR and RRFS guidance, and given the urban
    sensitivities around New Orleans, these rains may result in
    additional areas of urban flash flooding heading through the early
    evening hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6AjeOYokZNcdYcJYvTHWzjBxEVMybvOpr2D-G2Kc7z39S4JR4hRXr2MRtCySQKr3qrlR= OUsTwSDuKpijSakRtkt_Ea0$ for graphic product...

    ATTN...WFO...LIX...

    ATTN...RFC...ORN...NWC...

    LAT...LON 30579003 30408947 29748979 29629064 29999098=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 14 23:52:48 2025
    AWUS01 KWNH 142352
    FFGMPD
    ALZ000-MSZ000-LAZ000-ARZ000-TXZ000-150300-

    Mesoscale Precipitation Discussion 0437
    NWS Weather Prediction Center College Park MD
    751 PM EDT Sat Jun 14 2025

    Areas affected...Portions of the Lower MS Valley and the Mid-South

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 142350Z - 150300Z

    SUMMARY...Multiple bands of heavy showers and thunderstorms will
    continue over the next few hours across portions of the Lower MS
    Valley and Mid-South from colliding outflow boundaries. A few
    additional areas of flash flooding will be possible this evening
    as a result.

    DISCUSSION...The latest GOES-E IR satellite imagery along with
    radar and surface data shows elongated bands of heavy showers and
    thunderstorms impacting areas of the Lower MS Valley and the
    Mid-South as convection continues to develop and locally expand in
    coverage as a result of colliding outflow boundaries.

    Areas that have not seen much in the way of convective overturning
    continue to be quite moist and unstable, with MLCAPE values as
    high as 2000 to 3000 J/kg with PWs near 2 inches. This is
    especially the case over northern MS and some parts of northern AL
    where the low-level flow is also rather convergent given the
    proximity of low pressure farther north over the Lower OH Valley.

    Expect heavy showers and thunderstorms to persist for a few more
    hours before the instability becomes sufficiently exhausted for
    the activity to begin weakening. Rainfall rates in the short-term
    may reach 1.5 to 2.5 inches/hour with some spotty totals of 3 to
    4+ inches where any cell-training occurs. Radar does show some
    cell-training occurring right now across areas of northern MS and
    northwest AL. This may foster a few isolated areas of flash
    flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_aygwZKEUQDi2lWciSkRwiM81719tnQGNxzH6LpTDTZVhG8UNvyL6slKlZ9rBdF7FUHH= yOcagm4zrLtMjFtP3xtE32w$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LZK...MEG...SHV...

    ATTN...RFC...ALR...ORN...TUA...NWC...

    LAT...LON 34728706 34558587 34098583 33588679 33228920=20
    32809344 32969464 33489445 34139182 34518907=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 01:34:49 2025
    AWUS01 KWNH 150134
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-OHZ000-150632-

    Mesoscale Precipitation Discussion 0438
    NWS Weather Prediction Center College Park MD
    933 PM EDT Sat Jun 14 2025

    Areas affected...Portions of the OH Valley...Central Appalachians
    and Mid-Atlantic

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 150132Z - 150632Z

    SUMMARY...Additional areas of slow-moving showers and
    thunderstorms are expected to continue to develop and locally
    persist into a portion of the overnight period. Given the high
    rainfall rate potential and slow cell-motions, additional
    scattered areas of flash flooding are expected.

    DISCUSSION...The latest surface analysis shows a quasi-stationary
    front still draped across the Mid-Atlantic region and stretching
    back up across the higher terrain of the central Appalachians and
    the upper OH Valley. 00Z RAOB data and the latest RAP analysis
    shows a substantial amount of moisture still remaining in place
    with PWs locally over 1.75 inches and with a moderate amount of
    instability pooled along the front with MLCAPE values of near 1500
    J/kg.

    Areas of central to northern VA are generally the most unstable,
    and there are pockets of locally strong low-level convergence near
    the front that should help maintain the ongoing convective threat
    across the region for a few more hours. Local orographics near the
    Blue Ridge and also deeper back into the high terrain of the
    central Appalachians will also facilitate areas of ascent for
    convection to redevelop and locally persist.

    Expect areas of slow-moving showers and thunderstorms to still be
    capable of producing rainfall rates of up to 2 inches/hour, and
    the slow cell-motions may yield some additional localized totals
    of 3 to 4+ inches. The most recent HRRR/RRFS guidance generally
    supports this.

    Given the additional rainfall potential and moist antecedent
    conditions overall, there should tend to be scattered areas of
    additional flash flooding going through the remainder of the
    evening and a part of the overnight period. This will include a
    localized urban flash flood concern as well.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!41lsI1pVeWgxcenTmksVQkJa-Gx7jUYJ3WmjT5keJQ2IJzo7oQv4M3UUkDy6rMYebUVi= tgXqlfuhFeYSaH9B8JzVrwY$ for graphic product...

    ATTN...WFO...AKQ...CTP...LWX...PBZ...RLX...RNK...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 40678047 40567966 39947837 38797727 38387668=20
    38077618 37737574 37427585 37347631 37577803=20
    38087958 38778059 39858121 40338116=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 04:12:38 2025
    AWUS01 KWNH 150338
    FFGMPD
    OKZ000-KSZ000-150940-

    Mesoscale Precipitation Discussion 0439
    NWS Weather Prediction Center College Park MD
    1137 PM EDT Sat Jun 14 2025

    Areas affected...much of north-central and northeast OK and
    portions of far south-central and southeast KS

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 150340Z - 150940Z

    Summary...Scattered instances of flash flooding are likely, driven
    by 3-6 hour rainfall totals of 3-6" (with the potential for
    localized 6"+ totals over portions of north-central OK).

    Discussion...Convection has initiated and gradually proliferated
    over the past few hours over portions of north-central OK and far
    south-central and southeast KS, in advance of a slow moving
    shortwave/remnant mesoscale convective vortex (MCV). The region is
    situated within an area of favorable northwest flow aloft, and the shortwave/MCV is providing 30-40 kts worth of deep layer (0-6 km)
    shear for convective organization and storm longevity. A
    substantial gradient of ML CAPE (500-3500 J/kg) is also situated
    over the area, paralleling a quasi-stationary surface boundary
    (quite evident in the surface thetaE gradient) that is draped from
    NNW to SSE from north-central OK southward to southeast OK.
    Tropospheric moisture content remains very highly anomalous,
    ranging from 1.7-2.1" (near the max moving average, per OUN
    sounding climatology). This is supporting highly efficient
    instantaneous rainfall rates of up to 3-5"/hr (per MRMS
    estimates), due to wet bulb zero heights around 13k-14k feet (also
    near the max moving average, per OUN sounding climatology). This
    is already allowing for localized hourly totals of 1-2" with
    ongoing convection (with modest cell motions of 10-20 kts), but
    these hourly totals could start to approach 3-4" as convection
    begins to backbuild towards the northwest. This backbuilding will
    be facilitated by a strengthening, veering low-level jet (LLJ),
    resulting in idealized isentropic lift near the 305K surface
    (along with warm air advection and increasing ML CAPE through the
    overnight hours).

    Hi-res CAMs are overall in quite good agreement concerning the
    convective evolution and resulting QPF overnight, suggesting
    localized 3-6" totals (and possibly even exceeding 6" in an
    isolated spot or two in north-central OK). While totals in this
    range may only meet or slightly exceed 6-hr Flash Flood Guidance
    (FFG), much of this QPF is likely to fall within a 3-hr period
    (per 00z HREF 40-km neighborhood 3"/3-hr exceedance probabilities
    of 20-50% between 06-09z). Between the 3-hr and 6-hr expected
    totals, probabilities of exceeding FFGs (per the HREF 40-km
    neighborhood exceedance probs) are between 30-60%. While it is
    likely that the most extreme totals will stay north of OKC and
    west of Tulsa (mitigating the impacts to large population
    centers), localized 5" exceedance (per HREF probs) is suggested to
    be as high as 25-35% (corresponding to 10-15% odds of 100-yr ARI
    exceedance). Experimental hourly RRFS runs since 18z have also
    consistently depicted this potential, concerningly even suggesting
    the potential for 7-9" localized totals. Given the very favorable
    environment for training heavy rainfall and the consistent hi-res
    signals, scattered instances of flash flooding are considered
    likely (with localized considerable flash flooding possible).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8SNRHZXJXg0ay_q7bKUjXWdZzvQ81ZhZa_jfasKpx8q8VYKBmVVDcxyVfmdYEvxuwaOn= VuUyS1t-V0w2tEB3i08wGVc$ for graphic product...

    ATTN...WFO...DDC...ICT...OUN...TSA...

    ATTN...RFC...TUA...NWC...

    LAT...LON 37589811 37459759 37409711 37429654 37559594=20
    37179535 36709488 36029476 35149593 35189727=20
    35689819 36489874 37199885 37579864=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 09:33:22 2025
    AWUS01 KWNH 150933
    FFGMPD
    OKZ000-151330-

    Mesoscale Precipitation Discussion 0440
    NWS Weather Prediction Center College Park MD
    532 AM EDT Sun Jun 15 2025

    Areas affected...Much of central OK

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 150930Z - 151330Z

    Summary...Additional localized 2-4" rainfall totals (at least
    partially overlapping with areas that have already seen 2-7"
    totals over past 7 hours) may contribute to continued isolated to
    scattered flash flooding.

    Discussion...A maturing MCS is continuing to produce healthy
    updrafts early this morning, as evidenced by persistent
    overshooting tops via GOES-East imagery and associated
    instantaneous rainfall rates as high as 3-5"/hr via MRMS
    estimates. This active convection is focused along the western and
    southern flanks of the established cold pool (which is highly
    pronounced on the 08z SPC RAP analysis surface thetaE plot), where
    ML CAPE of 500-2000 J/kg resides. Tropospheric moisture content
    remains impressive across this region (PWs of 1.4-1.8", near the
    90th percentile per OUN sounding climatology), though the LLJ and
    associated moisture transport is beginning to wane. Convection
    continues to backbuild to the northwest, and a slow moving
    shortwave/MCV is providing 30-40 kts of effective bulk shear
    (which seems to be significantly contributing to updraft
    longevity, despite an associated MCS maintenance parameter of only
    10-40% along the western flank of the system).

    While both the intensity of the MCS and the consistency of storm
    training has likely peaked with the waning LLJ and increased
    forward propagation of storms in the past hour, still expect some
    additional backbuilding and training to continue for 3-4 more
    hours. This favors at least some additional heavy rainfall for the
    greater OKC metro, where locally 2-3" of rainfall has already
    occurred with this system. Additional heavy rainfall may also
    continue to train to the north of OKC, where locally as much as
    6-7" of rainfall has occurred over the past 6-7 hours. Additional
    localized totals of up to 2-4" may occur (per 06z HREF PMM QPF, as
    well as subsequent HRRR and experimental RRFS QPF). Isolated to
    scattered instances of flash flooding are possible (particularly
    if these amounts occur over more sensitive areas, where locally
    considerable instances of flash flooding are possible).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_nFpD58aOjjsRSk69s4yRBFv-O3nLWEV53RIPFykhvKDkADlUdMAMG6uR1soq2fwuyaA= OlrF2j_rJ3tIk4ZWnarF-PQ$ for graphic product...

    ATTN...WFO...OUN...TSA...

    ATTN...RFC...TUA...NWC...

    LAT...LON 36959846 36809776 36599727 36319683 36009655=20
    35709625 35389592 34729569 34369613 34039708=20
    34049786 34379864 34779912 35059928 35739935=20
    36339937 36939927=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 12:46:22 2025
    AWUS01 KWNH 151246
    FFGMPD
    TXZ000-OKZ000-151644-

    Mesoscale Precipitation Discussion 0441
    NWS Weather Prediction Center College Park MD
    845 AM EDT Sun Jun 15 2025

    Areas affected...southern Oklahoma, north through northwest Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 151244Z - 151644Z

    Summary...A couple of mature convective complexes were merging and
    crossing the Red River of Oklahoma/Texas this morning. Spots of
    1-1.5 inch/hr rain rates should pose an isolated flash flood risk
    that should progressively become more isolated with time.

    Discussion...Recent mosaic imagery depicts a couple of merging
    convective complexes - one along the Red River from near Wichita
    Falls to near Durant, OK and another across far southwestern
    Oklahoma and the southeast Texas Panhandle near Childress. The
    complexes have gained forward speed through the morning, although
    several mergers have aided in 1-1.5 inch/hr rain rates within both
    complexes. These rain rates are generally lower than FFG
    thresholds areawide, with the greatest potential for impactful
    flooding existing in/near urban and sensitive locales over the
    past couple of hours.

    These general trends should continue to translate southward into
    more of north/central Texas this morning. 20 kt southwesterly
    850mb flow should continue to provide sufficient low-level shear
    for MCS maintenance while 1.5+ inch PW values and 1000-2000 J/kg
    of downstream MLCAPE supports robust, efficient updrafts. Areas
    of 1-1.5 inch/hr rain rates should continue with the complexes -
    again falling generally below FFG and limiting the spatial extent
    of flash flood potential to the most sensitive/urbanized spots.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!71y8DcbT55YApAgEdGP-Muc2DBNx-4TczWh5HFCPZeiagoaq7EDhEtdpIZnaHHabN4I9= EL-szN4iVpunhmuN9XVW45E$ for graphic product...

    ATTN...WFO...AMA...FWD...LUB...OUN...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35429905 34909730 34259641 32949623 32219664=20
    31739753 31909948 33100044 34530058 35409998=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 15:36:56 2025
    AWUS01 KWNH 151536
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-KYZ000-152133-

    Mesoscale Precipitation Discussion 0442
    NWS Weather Prediction Center College Park MD
    1135 AM EDT Sun Jun 15 2025

    Areas affected...portions of West Virginia, southwestern
    Pennsylvania, western Virginia, and eastern Kentucky

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 151533Z - 152133Z

    Summary...Thunderstorms will continue to increase in coverage
    today while producing spots of 1-1.5 inch/hr rain rates across the
    discussion area. These rates will support scattered flash
    flooding - especially across the central Appalachians - through
    22Z/6p EDT.

    Discussion...Recent radar/satellite imagery indicates sufficient destabilization across the discussion area to support deepening
    convection that was expanding in coverage. Mesoanalyses suggest
    that the convection was surface-based an in an environment
    characterized by 2000 J/kg SBCAPE and 1.8 inch PW values,
    supporting efficient rain rates with this activity. These cells
    were moving very slowly eastward - perhaps slowest across
    southwestern Pennsylvania amid a minimum in wind fields aloft.=20
    Slow cell movement was already allowing for a few spots of 1
    inch/hr rain rates to develop just south of Charleston, WV over
    the past hour.

    Ongoing convective trends are expected to continue through the
    afternoon, with pockets of insolation/destabilization aiding in
    sustained thunderstorm development amid weak vorticity maxima
    traversing the region aloft. The combination of weak low-level
    flow against central Appalachian terrain and a stationary boundary
    extending from southwestern Pennsylvania (Greensburg) southward
    through western Virginia (near Charlottesville) should also serve
    as an additional focus for convective development and persistent
    heavy rainfall. FFG thresholds happen to be lowest near the
    aforementioned boundary (<1 inch/hr), though instances of
    exceedence can be expected areawide in several locales through 22Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5BN9CdfmufgV11PHpNUNh1u-lojx2H6wU73AZiHaqQSe0HOtFtNvnsXwy7Xz6YUds0GY= s0i0I-a6KKh4NYPD4_T8FcM$ for graphic product...

    ATTN...WFO...AKQ...CTP...JKL...LWX...MRX...PBZ...RLX...RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 40557901 40087839 39057800 38247800 37677842=20
    37387950 36918209 37268354 37918311 38398230=20
    39418108 40258016=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 15:38:23 2025
    AWUS01 KWNH 151537
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-KYZ000-152133-

    Mesoscale Precipitation Discussion 0442
    NWS Weather Prediction Center College Park MD
    1137 AM EDT Sun Jun 15 2025

    Areas affected...portions of West Virginia, southwestern
    Pennsylvania, western Virginia, and eastern Kentucky

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 151533Z - 152133Z

    Summary...Thunderstorms will continue to increase in coverage
    today while producing spots of 1-1.5 inch/hr rain rates across the
    discussion area. These rates will support scattered flash
    flooding - especially across the central Appalachians - through
    22Z/6p EDT.

    Discussion...Recent radar/satellite imagery indicates sufficient destabilization across the discussion area to support deepening
    convection that was expanding in coverage. Mesoanalyses suggest
    that the convection was surface-based and in an environment
    characterized by 2000 J/kg SBCAPE and 1.8 inch PW values,
    supporting efficient rain rates with this activity. These cells
    were moving very slowly eastward - perhaps slowest across
    southwestern Pennsylvania amid a minimum in wind fields aloft.=20
    Slow cell movement was already allowing for a few spots of 1
    inch/hr rain rates to develop just south of Charleston, WV over
    the past hour.

    Ongoing convective trends are expected to continue through the
    afternoon, with pockets of insolation/destabilization aiding in
    sustained thunderstorm development amid weak vorticity maxima
    traversing the region aloft. The combination of weak low-level
    flow against central Appalachian terrain and a stationary boundary
    extending from southwestern Pennsylvania (Greensburg) southward
    through western Virginia (near Charlottesville) should also serve
    as an additional focus for convective development and persistent
    heavy rainfall. FFG thresholds happen to be lowest near the
    aforementioned boundary (<1 inch/hr), though instances of
    exceedence can be expected areawide in several locales through 22Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6JyBNWc_hqpvLo0oa2psanCcsU3oRrPTLv61DfO0x6UAhOhTOYfJCglkR8UoLMNK1dOl= r2UojUVRz-YfBTlXGsttGeA$ for graphic product...

    ATTN...WFO...AKQ...CTP...JKL...LWX...MRX...PBZ...RLX...RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 40557901 40087839 39057800 38247800 37677842=20
    37387950 36918209 37268354 37918311 38398230=20
    39418108 40258016=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 15:42:23 2025
    AWUS01 KWNH 151542
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-KYZ000-152133-

    Mesoscale Precipitation Discussion 0442...Corrected
    NWS Weather Prediction Center College Park MD
    1141 AM EDT Sun Jun 15 2025

    Corrected for graphic

    Areas affected...portions of West Virginia, southwestern
    Pennsylvania, western Virginia, and eastern Kentucky

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 151533Z - 152133Z

    Summary...Thunderstorms will continue to increase in coverage
    today while producing spots of 1-1.5 inch/hr rain rates across the
    discussion area. These rates will support scattered flash
    flooding - especially across the central Appalachians - through
    22Z/6p EDT.

    Discussion...Recent radar/satellite imagery indicates sufficient destabilization across the discussion area to support deepening
    convection that was expanding in coverage. Mesoanalyses suggest
    that the convection was surface-based and in an environment
    characterized by 2000 J/kg SBCAPE and 1.8 inch PW values,
    supporting efficient rain rates with this activity. These cells
    were moving very slowly eastward - perhaps slowest across
    southwestern Pennsylvania amid a minimum in wind fields aloft.=20
    Slow cell movement was already allowing for a few spots of 1
    inch/hr rain rates to develop just south of Charleston, WV over
    the past hour.

    Ongoing convective trends are expected to continue through the
    afternoon, with pockets of insolation/destabilization aiding in
    sustained thunderstorm development amid weak vorticity maxima
    traversing the region aloft. The combination of weak low-level
    flow against central Appalachian terrain and a stationary boundary
    extending from southwestern Pennsylvania (Greensburg) southward
    through western Virginia (near Charlottesville) should also serve
    as an additional focus for convective development and persistent
    heavy rainfall. FFG thresholds happen to be lowest near the
    aforementioned boundary (<1 inch/hr), though instances of
    exceedence can be expected areawide in several locales through 22Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8ToZW08JQZT_5QWx0keQiTIMhEOLuL9jP_9-Z3Gi-8iRpYkPMbApvk051D_0HNgKJmHC= QW6HV1Y6Rp6UEz2qr6X-XTo$ for graphic product...

    ATTN...WFO...AKQ...CTP...JKL...LWX...MRX...PBZ...RLX...RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 40557901 40087839 39057800 38247800 37677842=20
    37387950 36918209 37268354 37918311 38398230=20
    39418108 40258016=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 17:37:36 2025
    AWUS01 KWNH 151737
    FFGMPD
    MOZ000-OKZ000-KSZ000-152036-

    Mesoscale Precipitation Discussion 0443
    NWS Weather Prediction Center College Park MD
    136 PM EDT Sun Jun 15 2025

    Areas affected...southwestern Missouri and vicinity

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 151736Z - 152036Z

    Summary...A nearly stationary band of convection has materialized
    north through northwest of Springfield, MO with local 1-1.5
    inch/hr rain rates. Some potential exists for this band to persist
    for multiple hours, posing a flash flood threat.

    Discussion...Over the past hour or so, an east-to-west oriented
    band of deeper convection has organized just east of an MCV center
    near the KS/OK/MO border region. This band was also collocated
    with weak surface convergence over the region, with low-level
    southerlies over most of the Missouri Ozarks veering to easterly
    low-level flow across central/west-central Missouri. 1500 J/kg
    SBCAPE values and 1.6 inch PW values were promoting heavier rain
    rates with deeper convection along this confluence axis. These
    rates were approaching local FFG thresholds near 1.5 inch/hr -
    suggestive of an increasing flash flood threat in the short term.

    Over the next 2-3 hours, this band should move slowly, with local
    influences from cold pool generation playing a key role in the
    ultimate evolution of the band. Localized 3 inch rainfall totals
    cannot be completely ruled out - especially where rainfall is most
    persistent. These totals should result in a few instances of
    flash flooding especially in sensitive/low spots.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6nRn8jNE5BjAYQE6gQPnoZsph-G_B88ugHHWiXcVxzON6ITozYkpiTwYSDx0Vl63GJZ7= DkmDXhdLT3OT-8pR75gErXU$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...SGF...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38219328 38089169 37509136 36909294 36759472=20
    37109548 37739507 38019455=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 18:28:21 2025
    AWUS01 KWNH 151826
    FFGMPD
    VAZ000-NCZ000-160025-

    Mesoscale Precipitation Discussion 0444
    NWS Weather Prediction Center College Park MD
    226 PM EDT Sun Jun 15 2025

    Areas affected...Mid-Atlantic

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 151825Z - 160025Z

    SUMMARY...Heavy showers and thunderstorms will develop over the
    next few hours across central to southeast VA and into northeast
    NC. High rainfall rates and slow cell-motions will promote
    excessive rainfall totals and a likelihood for scattered to
    numerous areas of flash flooding going through early this evening.
    Considerable urban flash flooding with life-threatening impacts
    will be possible.

    DISCUSSION...The early-afternoon GOES-IR satellite imagery shows
    cooling convective tops over central WV through much of western VA
    as a very slow-moving mid-level shortwave trough advances east
    across the central Appalachians. Diurnal heating and resultant
    boundary layer destabilization is well underway ahead of this
    energy in vicinity of a well-defined stationary front draped from
    eastern WV down through southeast VA.

    MLCAPE values are already upwards of 1500 to 2500+ J/kg across
    central to southeast VA and through much of central to northeast
    NC. The airmass is also very moist across the region with PWs of
    1.75 to 2 inches, and the 12Z RAOB data from KIAD, KRNK and KGSO
    all showed very moist vertical columns with the KRNK and KGSO
    soundings in particular showing tally, skinny CAPE profiles. This
    once again suggests a highly efficient environment with extreme
    rainfall rate potential.

    Satellite imagery is showing a substantial amount of solar
    insolation ongoing on across south-central to southeast VA to the
    south of the front, and additional boundary layer destabilization
    is expected to couple with a combination of frontal convergence,
    and weak DPVA for the development and expansion of convection=20
    through the afternoon and early evening hours. Additionally,
    satellite and surface observations suggest that there may be a
    weak wave of low pressure developing along the front over
    south-central VA, and this may further yield a low-level focus for
    more concentrated/stronger convection over the next few hours.

    The latest 12Z HREF/06Z REFS guidance, along with the
    early-afternoon 17Z/1730Z WoFS guidance all suggest very high
    rainfall rate potential with 2 to 3 inch/hour rainfall rates
    possible with the stronger storms. The generally slow cell-motions
    and cell-merger concerns will foster concerns for some rainfall
    totals to reach 3 to 5+ inches going through 00Z (8pm EDT).

    Given the rainfall rates/totals, and sensitive antecedent
    conditions, scattered to numerous areas of flash flooding are
    generally expected over the next several hours. Considerable urban
    flash flooding will be possible, including significant to
    life-threatening impacts should these heavier rains materialize
    over the urban corridors and especially from Richmond to
    Petersburg over into the Hampton Roads vicinity. Areas of
    northeast NC from Roanoke Rapids to Elizabeth City also should be
    closely monitored for urban flash flooding concerns.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5AeCyIA4uZG8s0hyZyIhvidQnkyawsPHJ4eM3uI0tAWUCX9FxsYLVy7bcKizF2MHwPWP= l-xLKwgoaL191sSrXbb6Sbk$ for graphic product...

    ATTN...WFO...AKQ...LWX...MHX...RAH...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 38257797 37997749 37307635 36697576 36047563=20
    35507609 35547702 36087835 36377930 36668034=20
    37288034 37807967 38227882=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 18:57:34 2025
    AWUS01 KWNH 151856
    FFGMPD
    FLZ000-GAZ000-160000-

    Mesoscale Precipitation Discussion 0445
    NWS Weather Prediction Center College Park MD
    255 PM EDT Sun Jun 15 2025

    Areas affected...Portions of the Southeast U.S.

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 151855Z - 160000Z

    SUMMARY...Slow-moving heavy showers and thunderstorms will
    continue through the afternoon and early evening hours across
    southern GA into eastern portions of the FL Panhandle and through
    northeast FL. Isolated areas of mainly urban flash flooding will
    be possible.

    DISCUSSION...The latest GOES-E IR satellite imagery shows
    expanding clusters of heavy showers and thunderstorms across areas
    of southern GA into the FL Panhandle and northeast FL. The
    convection is focused generally near a weak inverted surface
    trough and in a weakly divergent flow regime aloft due to an
    upper-level trough near the Gulf Coast. Additionally, there is
    evidence of some seabreeze convergence more specifically attached
    to to the convective threat over northeast FL

    MLCAPE values of 2000 to 3000 J/kg and high PWs of locally over 2
    inches will support rainfall rates of 2 to 3 inches/hour with the
    stronger convective cores near the inverted trough axis. Slow
    cell-motions and a couple of cell-mergers may yield some spotty
    totals of 3 to 4+ inches going through early this evening. The
    latest HRRR and RRFS guidance supports this with some 12Z HREF
    guidance also favoring locally heavy rainfall amounts.

    A few isolated areas of mainly urban flash flooding will be
    possible as a result going through early this evening. Some areas
    that saw heavy rain yesterday may also be impacted which will
    introduce some localized runoff concerns.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4ujLAWZ7ayd4Fekz6g2lXfBTjze2QFfHDf_wJt4oHfq9PEPpkhPfsYrEZ8QPZ_V5vt64= hjO3iNTsYeLiIYoMA-xUJvY$ for graphic product...

    ATTN...WFO...CHS...FFC...JAX...TAE...

    ATTN...RFC...ALR...NWC...

    LAT...LON 32188313 32078195 31618142 31118129 30518136=20
    29488121 29468170 30118272 30218360 29748440=20
    29598502 30088551 31458463=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 20:04:47 2025
    AWUS01 KWNH 152003
    FFGMPD
    MOZ000-ARZ000-160202-

    Mesoscale Precipitation Discussion 0446
    NWS Weather Prediction Center College Park MD
    402 PM EDT Sun Jun 15 2025

    Areas affected...Southern MO...Central and Northern AR

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 152002Z - 160202Z

    SUMMARY...Showers and thunderstorms with high rainfall rates and
    slow cell-motions will pose a notable threat for scattered areas
    of flash flooding going into the evening hours.

    DISCUSSION...The afternoon GOES-E visible satellite imagery shows
    an expanding CU/TCU field across central and northern AR and areas
    of southern MO to the south of a band of broken showers and
    thunderstorms that areas already impacting portions of
    south-central MO to the north and east of Springfield. The
    convection is being strongly influenced by deep layer cyclonic=20
    flow associated with a nearly stationary low to mid-level low
    center over far northeast OK.

    This energy is also entangled along a quasi-stationary frontal
    zone and over the next few hours will be interacting with a
    moderately buoyant airmass pooled along it characterized by MLCAPE
    values of 1000 to 1500+ J/kg. Some of the greater instability is
    focused across central AR and with the cyclonic low to mid-level
    flow, there should be a gradual expansion of showers and
    thunderstorms over the next few hours down into northern and
    central AR.

    Rainfall rates with the convection should be capable of reaching
    1.5 to 2.5 inches/hour based on the 12Z HREF guidance, and with
    slow cell-motions going into the evening hours, there may be some
    localized storm totals of 3 to 4+ inches. In fact, recent HRRR
    guidance suggests some spotty 5 inch amounts may be possible
    across central AR early this evening from some areas of
    cell-training that occur.

    These rainfall amounts on top of moist antecedent conditions and
    near areas of more sensitive/rugged terrain involving portions of
    the Ozark Plateau will generally favor concerns for scattered
    areas of flash flooding. There also may be a notable urban flash
    flood threat if the convection can build far enough south and get
    into areas from Batesville on down through Little Rock and Hot
    Springs.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!49IBRrXnlptiXOf6M8z-UI4Q9Yb11Lnfg5Groj9n4L3EQnYRyLLLq27oT9EZ4hdb38lO= l7HA2L35Lk6zZrHv2as7Jho$ for graphic product...

    ATTN...WFO...LSX...LZK...MEG...PAH...SGF...SHV...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38169290 37759141 36599068 34759144 33869294=20
    33819418 34719434 36359337 37729382=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 20:19:30 2025
    AWUS01 KWNH 152019
    FFGMPD
    LAZ000-TXZ000-160117-

    Mesoscale Precipitation Discussion 0447
    NWS Weather Prediction Center College Park MD
    418 PM EDT Sun Jun 15 2025

    Areas affected...Southeast TX into western LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 152017Z - 160117Z

    SUMMARY...Isolated flash flooding is expected this afternoon
    across southeast Texas into western Louisiana with high
    instability and moisture resulting in intense rainfall rates.

    DISCUSSION...Recent SPC mesoanalysis depicts MLCAPE upwards of
    4000 j/kg and PWs as high as 2.2" over southeast TX into LA. This
    environment will be capable of very high rainfall rates likely
    resulting in an isolated flash flood risk this afternoon. Wind
    fields and shear are relatively weak, suggesting slow cell
    motions, but also mostly a pulse storm mode. This pulse nature of
    convection should overall limit the duration of heavier rainfall
    rates. However, an outflow boundary diving southward across the
    area should act as a focus for cell mergers over the next few
    hours, locally increasing duration and rainfall totals. Recent
    HRRR runs support localized totals over 3", and neighborhood
    probabilities of exceeding 3" from the 12z HREF are 40-60%.

    Given the wet antecedent conditions and elevated streamflows over
    most of this region would expect this rainfall to result in at
    least an isolated flash flood threat over the next several hours.
    Hourly rainfall of 2-3" appears probable in spots as the outflow
    drives cell mergers within the aforementioned highly unstable and
    moist airmass. The threat will be relatively short lived however,
    as the southward moving outflow should help clear things out from
    north to south by this evening.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4s2Csqn1qPzQ7ibWxoAzc0PA8Uf_nfNVrIocoY7M_pRBzl_6VQ2-4t7PRfEkQFtYykSF= lLrE5ldns0c8Jz50-PaCgns$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...LCH...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 32609459 32029380 31299329 30209352 29809439=20
    29449531 29239635 28569725 28719773 29299793=20
    30289800 30799742 31089664 31969575 32519533=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 21:06:26 2025
    AWUS01 KWNH 152106
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-OHZ000-KYZ000-160300-

    Mesoscale Precipitation Discussion 0448
    NWS Weather Prediction Center College Park MD
    505 PM EDT Sun Jun 15 2025

    Areas affected...Portions of the Upper OH Valley and Central
    Appalachians

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 152105Z - 160300Z

    SUMMARY...Slow-moving areas of very heavy showers and
    thunderstorms will continue into this evening across portions of
    the upper OH Valley and especially the central Appalachians.
    Numerous areas of flash flooding, including pockets of
    considerable to locally catastrophic impacts will continue over
    the next several hours. This is a life-threatening situation.

    DISCUSSION...The mid-afternoon GOES-IR satellite imagery along
    with radar imagery shows numerous areas of slow-moving and heavy
    showers and thunderstorms impacting southwest PA through southeast
    OH, eastern KY and large areas of WV, with this activity
    continuing to advance downstream into areas of western VA to the
    east of the Appalachians. The activity continues to be focused in
    connection with a slow-moving low to mid-level low center and
    trough drifting east across the central Appalachians which is also
    interacting with proximity of a stationary front.

    A very moist and moderately unstable airmass remains focused over
    the region, with PWs in the 90th to 95th percentile of
    climatology, and MLCAPE values still ranging in between 1000 to
    1500 J/kg with the aid of additional boundary layer heating.

    Additional rounds of slow-moving and heavy showers and
    thunderstorms are expected over the next several hours as cyclonic
    low to mid-level flow coupled with orographic ascent over the
    higher terrain of southwest PA down through central WV works to
    provide ascent. Locally focused areas of convergence near the
    front will also be a key facilitator for additional rounds of
    convection in the near-term.

    The latest HRRR/RRFS guidance supports up to an additional 2 to 4
    inches of rain, with isolated heavier amounts not out of the
    question given the very moist/unstable environment and orographic
    nature to a lot of the shower and thunderstorm activity.

    Numerous areas of flash flooding are already ongoing, and will
    continue into the evening hours, including pockets of considerable
    to locally catastrophic impacts. This life-threatening situation
    is expected to continue in the near-term.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9biiTJiVFRCvJBAwPYkMwwRhj8k04tlZc2ENXK-BWECgUDgqMpaIBjnH8LVqxW_XTfvq= AK3WQ7PRjE-DyQ3T3SkNNdY$ for graphic product...

    ATTN...WFO...CTP...ILN...JKL...LMK...LWX...MRX...PBZ...RLX...
    RNK...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 40877954 40537900 39527877 38547863 37787972=20
    37398062 37168242 37278404 37718457 38468439=20
    39218314 39978181 40788057=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 22:07:28 2025
    AWUS01 KWNH 152207
    FFGMPD
    TXZ000-NMZ000-160205-

    Mesoscale Precipitation Discussion 0449
    NWS Weather Prediction Center College Park MD
    606 PM EDT Sun Jun 15 2025

    Areas affected...Southeast NM...Southwest TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 152205Z - 160205Z

    SUMMARY...Slow-moving and locally anchored thunderstorms across
    portions of southeast NM and southwest TX will continue for at
    least a few more hours.

    DISCUSSION...Radar and satellite imagery shows slow-moving and
    locally anchored cold-topped thunderstorms across areas of
    southeast NM and southwest TX, with the convection focusing near
    some of the higher terrain generally southeast of the Sacramento
    Mountains. Moist and unstable low-level flow near terrain will
    tend to favor this activity over the few hours with some potential
    for this convection to organize upscale a bit more and then
    advance east potentially into adjacent areas of the far southern
    High Plains.

    Rainfall rates with these storms are expected to be high, and
    reaching as high as 1 to 2 inches/hour. The slow cell-motions and
    concerns for a few cell-mergers over the next couple of hours will
    support some isolated 3 to 4+ inch totals.

    Very little hires model guidance is properly handling the current
    activity, but the latest satellite and radar trends, especially
    with the level of recent cloud-top cooling suggests some
    persistence of the activity at least for a few more hours. Some
    areas of flash flooding will be possible with these cells given
    their slow movement and expected rainfall rates.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8j3vVNgSw1rWzjc_YGSFFZEET3eVW8HIJwOhu-QfZCevywGMfzxtIGE6LdoHx46-8wuE= AgjwhVMsSfsRSvpB1akMWMQ$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...NWC...

    LAT...LON 34600458 33860355 31910318 30440369 30130465=20
    30540557 31320556 32330545 33230579 34360591=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 22:52:59 2025
    AWUS01 KWNH 152252
    FFGMPD
    MDZ000-VAZ000-DCZ000-WVZ000-160150-

    Mesoscale Precipitation Discussion 0450
    NWS Weather Prediction Center College Park MD
    651 PM EDT Sun Jun 15 2025

    Areas affected...Northern VA...D.C....Southern MD

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 152250Z - 160150Z

    SUMMARY...Very efficient shower activity with locally high
    rainfall rates may cause some flash flooding concerns across
    portions of northern VA, D.C and southern MD over the next few
    hours.

    DISCUSSION...Radar imagery shows a few clusters of heavy shower
    activity beginning to impact areas of northern VA and southern MD
    along with areas just south of Washington D.C. The convection
    which is very efficient in nature with relatively warm tops and is
    embedded within a very moist vertical column with PWs of 1.8 to 2
    inches.

    There is some weak elevated instability (MUCAPE values of 500+
    J/kg) along with some isentropic ascent north of a stationary
    front and ahead of the upstream shortwave energy over the central
    Appalachians helping to facilitate this activity. Rainfall rates
    based on MRMS data are upwards of 1.5 to 2.5 inches/hour with this
    convection.

    Given these high rates and the slow cell-motions, some near-term
    totals over the next few hours may reach 3 to 4 inches. Given the
    generally wet antecedent conditions and urban sensitivities around
    the Washington D.C. metropolitan area, some flash flooding will
    certainly be a concern.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_5xad8J1EShpTiUsN_juiFnSmiX9zHxaIvLAcUv8sQ1unVjYX14jYwIPlmusOe3M2_Co= 9MCOq7mtbUoIDvOBZUMoIjw$ for graphic product...

    ATTN...WFO...AKQ...LWX...

    ATTN...RFC...RHA...NWC...

    LAT...LON 39207817 39107730 38707651 38187647 37857686=20
    37867715 38247787 38347849 38867857 39117856=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 15 23:35:57 2025
    AWUS01 KWNH 152335
    FFGMPD
    NDZ000-MTZ000-160535-

    Mesoscale Precipitation Discussion 0451
    NWS Weather Prediction Center College Park MD
    735 PM EDT Sun Jun 15 2025

    Areas affected...Portions of Central and Eastern MT

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 152335Z - 160535Z

    SUMMARY...Heavy showers and thunderstorms are expected to develop
    and grow upscale into a progressive convective complex this
    evening while advancing out across the MT High Plains.

    DISCUSSION...The late-day GOES-W visible satellite imagery shows
    convection initiating and expanding in coverage across central MT
    as a rather vigorous upstream shortwave trough approaches the
    region and interacts with an unstable boundary layer with MLCAPE
    values of 1500 to 2500 J/kg.

    Some MLCIN is still evident late this afternoon which may temper
    some of the initial stages of convective development, but as
    stronger forcing with the shortwave arrives and the low-level jet
    increases across southeast MT in close proximity to a developing
    wave of low pressure, there should be a considerable amount of
    upscale convective growth going into the evening hours.

    Supercell thunderstorms with notable severe weather hazards
    including large hail and damaging winds (please see SPC's WW #418
    and recently issued MD #1305 for more details) may also be capable
    of producing sufficiently heavy enough rainfall rates and totals
    over the next several hours for there to be at least some isolated
    areas of flash flooding. The PWs across the region are near the
    90th percentile of climatology, and with an increase in low-level
    moisture transport this evening, the rainfall rates may reach as
    high as 1 to 2 inches/hour.

    The environment this evening will be conducive for cell-mergers as
    the larger scale convective mass gradually takes on an MCS-related
    evolution and forward propagates downstream through eastern MT.
    Some rainfall totals of 2 to 4 inches will be possible as the
    event unfolds and convection locally becomes more concentrated,
    and this is supported by the 12Z/18Z HREF guidance. The HREF is
    also showing a corridor of rather high 1-hour and 3-hour FFG
    exceedance probabilities based on these totals.

    Therefore, the potential will exist over the next several hours
    for there to be at least some isolated areas of flash flooding in
    addition to the regional severe weather concerns.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4WxFmj--hot4-u_M4NgNv7Kfu7ddb83Dft7juoTw2mKNXuuAwzUTTvjH7pqx_k3wwhPl= 3-g8eAcmEcgN0416fMEqfAA$ for graphic product...

    ATTN...WFO...BIS...BYZ...GGW...TFX...

    ATTN...RFC...KRF...NWC...

    LAT...LON 48970768 48620591 48000473 47260400 46130407=20
    45380530 45370690 45670859 46231010 46991078=20
    47921055 48650945=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 16 00:36:29 2025
    AWUS01 KWNH 160036
    FFGMPD
    VAZ000-NCZ000-160635-

    Mesoscale Precipitation Discussion 0452
    NWS Weather Prediction Center College Park MD
    835 PM EDT Sun Jun 15 2025

    Areas affected...Central to Southeast VA...Central to Northeast NC

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 160035Z - 160635Z

    SUMMARY...Scattered areas of flash flooding will continue to be a
    threat going through midnight across areas of central to southeast
    VA, and especially central to northeast NC. Locally considerable
    urban flash flooding and life-threatening impacts will remain
    possible.

    DISCUSSION...The early-evening GOES-E IR satellite imagery shows a
    cold-topped convective mass continuing to evolve across areas of
    central to southeast VA, with some of the most vigorous activity
    including overshooting tops noted over parts of central to
    northeast NC. The convection continues to be focusing in close
    proximity to a stationary with a substantial pool of instability
    still pooled nearby. MLCAPE values are highest over much of
    central and eastern NC in general with values of 1500 to 2500+
    J/kg noted based on the latest RAP analysis.

    Convergent low-level flow nosing up across central to northeast NC
    over the next few hours to the south of the front will be a key
    facilitator of convection becoming more pronounced and focused
    across this region, with potentially some of this still capable of
    nosing up into southeast VA near the Hampton Roads vicinity.
    However, many areas of central VA have already largely been
    convectively overturned.

    PWs are a bit higher than they were around midday and are now
    upwards of 2 to 2.25 inches along the VA/NC border, and this
    coupled with the instability and modest shear profiles should
    easily favor rainfall rates reaching 2 to 3 inches/hour with the
    stronger cells. This is supported by the 23Z WoFS output which
    shows 50+ percent probabilities of seeing 2+ inch/hour rainfall
    rates across central to northeast NC over the next few hours.

    The 50th percentile of 23Z WoFS 6-hour QPF output shows a swath of
    2 to 4 inch rainfall totals across areas of central to northeast
    NC, with 90th percentile data showing spotty 6+ inch totals as a
    result of an environment conducive for cell-training.

    Lesser rainfall amounts at this point are expected farther north
    across southeast VA, but areas near Virginia Beach on down through
    Chesapeake may locally see a couple of additional inches of rain.
    However, generally the greatest focus of additional heavy rains
    and concerns for additional flash flooding should be across
    central to northeast NC based on the collective array of recent
    hires model guidance which also includes the HRRR and RRFS.

    Given the rainfall rates/totals, and locally sensitive antecedent
    conditions that remain in place, scattered areas of additional
    flash flooding will be likely going through midnight. And some
    locally considerable and life-threatening urban flash flooding
    impacts will remain possible.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_CxwtH_NO34SPxn5tZP0Em08jnf12L03pP5A841n-SOziwalz7tM3pfjUTjncHGkcEvc= qDxtm9Ir_AFyHG5xdyFtqBQ$ for graphic product...

    ATTN...WFO...AKQ...ILM...MHX...RAH...RNK...

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37627708 37417638 36927566 35837551 34987681=20
    34747769 34687877 34967929 35357936 36097916=20
    36548021 36948011 37137941 37107835 37327775=20
    37537748=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 16 01:52:57 2025
    AWUS01 KWNH 160152
    FFGMPD
    MOZ000-ARZ000-160730-

    Mesoscale Precipitation Discussion 0453
    NWS Weather Prediction Center College Park MD
    951 PM EDT Sun Jun 15 2025

    Areas affected...South-Central to Southeast MO...Much of Southwest
    to Central and Northeast AR

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 160150Z - 160730Z

    SUMMARY...Additional scattered areas of flash flooding are
    expected over the next few hours, which will include some urban
    flooding concerns as areas of slow-moving and locally training
    showers and thunderstorms continue to impact areas of
    south-central to southeast MO down through large areas of central
    to southwest AR.

    DISCUSSION...The evening GOES-E IR satellite imagery along with
    radar data shows broken bands of heavy showers and thunderstorms
    impacting parts of south-central to southeast MO, and especially
    down through central to southwest AR where there has recently been
    some notable cell-training of the activity. The convection is
    entrenched within a convergent low to mid-level flow regime around
    the southern flank of a deeper layer low center over the Ozark
    Plateau.

    The airmass remains very moist and unstable with MLCAPE values
    over portions of central to northeast AR on the order of 1500 to
    2500+ J/kg. PWs are as high as 2.0 to 2.25 inches and near the
    90th percentile of climatology. As a result, rainfall rates with
    the ongoing convection remain quite high with magnitudes of 2 to 3
    inches/hour with the stronger cells.

    Convergent flow over southeast through central AR and to a lesser
    extent up through southeast MO will continue to promote these
    slow-moving convective bands in the near-term. However, as
    instability gradually wanes, the activity by late this evening
    should weaken.

    The HRRR and RRFS guidance suggests locally an additional 2 to 4+
    inches of rain going through midnight, and these rains are
    generally expected to produce scattered areas of additional flash
    flooding. This will include concerns over the next few hours for
    some urban flooding impacts, and especially where any additional
    cell-training occurs before the activity weakens.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8L6gwf3kFEjO6o8azlz9SqSf1FkqoC8WIOv7fUZfRi1gPAkhhakz5so1ssQFJNz74XtW= dIPuUIC2u9o739ywc96fnhs$ for graphic product...

    ATTN...WFO...LSX...LZK...MEG...PAH...SGF...SHV...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 37449000 36808968 34819149 33799328 33839420=20
    34589416 36369254 37319106=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 16 05:58:35 2025
    AWUS01 KWNH 160556
    FFGMPD
    SDZ000-NDZ000-MTZ000-161100-

    Mesoscale Precipitation Discussion 0454
    NWS Weather Prediction Center College Park MD
    156 AM EDT Mon Jun 16 2025

    Areas affected...portions of southeastern MT into west-central ND
    and northwest SD

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 160555Z - 161100Z

    Summary...Localized hourly totals of 1-2" to continue, resulting
    in short-term (3-4 hour) totals of 2-4" (with higher isolated
    totals possible). Isolated to scattered flash flooding likely (and
    may be locally considerable).

    Discussion...A forward propagating mesoscale convective system
    (MCS) and associated mesoscale convective vortex (MCV) are
    translating eastward from MT into ND/SD at this hour. While the
    strongest convection is currently ongoing in a sparse
    observational environment (due to a lack of surface observations
    and poor radar coverage with the MRMS radar quality index near 0,
    given surrounding radars scanning around ~20k feet AGL), GOES-East
    1-min mesoscale sector imagery indicates persistent cold cloud
    tops with active overshooting tops (which are also apparent via
    MRMS with 30 dBZ echo tops persistently near ~60k feet). The
    mesoscale environment near and downstream of the MCS/MCV is
    characterized by ML CAPE of 1000-2000 J/kg, precipitable water
    values of 1.2-1.4" (between the 90th percentile and max moving
    average, per BIS sounding climatology), and significant deep layer
    (0-6 km) shear of 40-50 kts (also near the 90th percentile).
    Substantial differential divergence (850-250 mb) with a 25-35 kt
    low-level jet to the southwest (over central ND) providing
    moderate moisture transport and ample divergence aloft (via an
    idealized coupled right-entrance region and left exit region jet
    steaks) will continue to maintain an impressive MCS (with the
    aforementioned shear and instability combined with a 850-300 mb
    mean wind of 15-20 kts resulting in MCS maintenance probabilities
    of 60-70%). While accurate precipitation estimates are difficult
    to determine with the lack of quality near-surface radar data, the
    system has a history of localized 1-2" hourly totals (with some training/repeating of these amounts possible in the vicinity of
    the MCV).

    The 00z HREF members are in decent agreement going forward (0.5"
    exceedance 10-100 km neighborhood EAS probabilities of 30-45%
    through 09z), and more recent hourly runs of the HRRR and
    experimental RRFS are in even better agreement (generally
    indicating localized totals of 2-3", though some RRFS runs
    indicate isolated totals as high as 3-6"). Isolated to scattered
    instances of flash flooding are likely (with 40-km neighborhood
    HREF 3-hr FFG exceedance probs of 40-50%, which may be too low
    given RRFS output) and some flooding may be locally significant
    (as 3-hr 100-yr average recurrence interval QPF is indicating to
    be 2.5-3.0", having at least a 25% chance to be realized).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9COJHjkJIl7eW_uD21W0Q_8eZF2s8_PmJuAuZOXECS95hFDNW4EEx6sbRUxWvbCBtlmx= x3GYaIBJ9FKeRGWo9LvpkBw$ for graphic product...

    ATTN...WFO...ABR...BIS...BYZ...GGW...UNR...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 48700285 48700169 47930053 47319979 46429941=20
    45529958 45110147 45040319 45100527 45930532=20
    46970485 47530439 47950358=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 16 06:37:02 2025
    AWUS01 KWNH 160636
    FFGMPD
    NCZ000-161000-

    Mesoscale Precipitation Discussion 0455
    NWS Weather Prediction Center College Park MD
    236 AM EDT Mon Jun 16 2025

    Areas affected...portions of north-central NC

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 160635Z - 161000Z

    Summary...Locally considerable and life threatening flash flooding
    likely to continue for another few hours with additional 3"+
    totals possible over areas that have had 3-6" of rainfall over
    past 3-6 hours.

    Discussion...Convection is tending to backbuild late overnight in
    the vicinity of a stalled front over portions of northeastern NC.
    The mesoscale environment is characterized by sufficient ML CAPE
    of 500-1000 J/kg, highly anomalous precipitable water values of
    2.0-2.2" (near record levels, per GSO sounding climatology), and
    effective bulk shear of 20-25 kts. Moisture transport remains
    elevated from the W-WSW, nearly parallel to the deep layer
    (850-300 mb) steering flow (~20 kts), which is allowing for
    backbuilding from the Raleigh metro area eastward to Rocky Mount
    and Greenville. Some of these areas east of the Raleigh metro
    (which has been mostly dry so far) have picked up as much as 3-6"
    of rain over the past 3-6 hours. Flash flooding is already
    ongoing, the recent backbuilding trends (evident on both radar and
    infrared satellite imagery) may exacerbate or renew locally
    considerable flash flooding.

    While hi-res CAMs do not have a great handle on the situation
    (with both hourly HRRR and experimental RRFS runs struggling to
    properly initialize and model the ongoing storms), the 00z HREF
    does depict a concerning signal for significant additional
    accumulations (which is consistent with recent observational
    trends, especially considering locally wet antecedent conditions).
    The 00z NAM-nest solution in particular appears to be driving this
    HREF signal (as it depict localized totals as high as 4-7"),
    suggesting the potential for localized 3" and 5" exceedance
    (10-20% and near 10% odds, respectively, per 40-km neighborhood
    HREF exceedance probabilities). Isolated to scattered instances of
    flash flooding are likely, and locally considerable/life
    threatening flash flooding will be exacerbated with continued 1-3"
    hourly totals.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6IFFBw1cb0e5q1iBQCwFRbuLhF-69L85xP20aVpMoXQeyDZEuxTpzQEwMibgeOr8R7SD= LFGsayrevizsriDFH-oKEkg$ for graphic product...

    ATTN...WFO...AKQ...MHX...RAH...RNK...

    ATTN...RFC...ALR...NWC...

    LAT...LON 36277961 36267889 36057802 35997701 35637687=20
    35247723 35447903 35927975=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 22 05:32:22 2025
    AWUS01 KWNH 220531
    FFGMPD
    VTZ000-NYZ000-221130-

    Mesoscale Precipitation Discussion 0489
    NWS Weather Prediction Center College Park MD
    130 AM EDT Sun Jun 22 2025

    Areas affected...Northern and Central NY

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 220530Z - 221130Z

    SUMMARY...Strong convective complex over southeast Ontario will be
    arriving across northern and central NY over the next several
    hours. Some localized cell-training concerns are expected which
    may result in some areas of flash flooding early this morning.

    DISCUSSION...The latest GOES-E IR satellite imagery along with
    MRMS data shows a well-organized QLCS dropping down across
    southeast Ontario, with the convective mass associated with a
    strong shortwave embedded within deep layer west-northwest flow
    situated around the northeast flank of a deep layer subtropical
    ridge over the Midwest and Great Lakes region.

    Very cold convective tops are noted with the southwest flank of
    the convective complex, with some overshooting tops as cold as
    about -70C. Strong warm air advection and moisture transport
    associated with a 50+ kt southwest low-level jet is seen riding up
    across the lower Great Lakes region and far southeast Ontario, and
    there is a nose of strong elevated instability aimed into the
    southwest flank of the convective mass with MUCAPE values of 2000
    to 3000 J/kg.

    The robust moisture and instability transport into far southeast
    Ontario will begin overspreading areas of northern NY over the
    couple of hours as the shortwave energy approaches. This coupled
    with strong effective bulk shear values of 40 to 50+ kts will
    favor arrival of a well-organized band of convection, with the
    QLCS losing latitude and dropping southeastward across northern
    and eventually central NY going through early this morning.

    Rainfall rates with this activity as it has been traversing
    Ontario overnight have been well into the 1 to 2 inch/hour range,
    with some cell-training that has fostered storm totals of 2 to 4
    inches.

    As this activity arrives down across northern and central NY, the
    southwest flank of the convective mass may continue to be a focus
    for cell-training as some of the convection becomes aligned more
    parallel to the deeper layer steering flow. Similar rainfall rates
    and totals are expected as this QLCS arrives over the next several
    hours, and this may drive at least some areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!90hGePaoSpp5LcsF_fO6Mqd_Pe2sGOedy6UO8mH4JPJZvrEOn6znH5H7RbpBw9u37nRY= nXtsDeFevGYBmUd4F_etbVU$ for graphic product...

    ATTN...WFO...ALY...BGM...BTV...BUF...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 44977381 44537318 43167351 42377450 42337615=20
    42707711 43227723 43417673 43677638 44447591=20
    44967497=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 22 09:52:00 2025
    AWUS01 KWNH 220951
    FFGMPD
    NYZ000-NJZ000-PAZ000-221430-

    Mesoscale Precipitation Discussion 0490
    NWS Weather Prediction Center College Park MD
    550 AM EDT Sun Jun 22 2025

    Areas affected...Central/Southern NY...Northeast PA...Northwest NJ

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 220950Z - 221430Z

    SUMMARY...A strong convective complex over central NY will drop
    down into areas of southern NY, northeast PA and northwest NJ this
    morning. Locally significant cell-training concerns will exist,
    and this will likely support areas of flash flooding going through
    at least mid-morning.

    DISCUSSION...The latest GOES-E IR satellite imagery shows a strong
    cold-topped convective complex over central NY which is losing
    latitude and is expected to drop down into areas of southern NY,
    northeast PA and northwest NJ going through the mid-morning hours.

    This convection mass is being enhanced around its southwest flank
    where there is a strong and convergent westerly low-level jet of
    40 to 50+ kts, and this is yielding strong moisture and
    instability transport. A nose of MUCAPE values of 1000 to 2000+
    J/kg is seen arriving across much of western and central NY, with
    PWs locally up near 1.75 inches.

    A notable cell-training threat will exist over the next few hours
    across areas of central and southern NY in particular given the
    interaction of the westerly low-level jet with the convectively
    enhanced cold pool. The latest RAP analysis shows strong
    convergence around the western flank of the MCS, and with the
    upstream instability combined with isentropic ascent over the cold
    pool, there will be a likelihood for cell-regeneration over the
    next few hours in a general north-northwest to south-southeast
    fashion in behind the initial convective bow which will drive the
    cell-training threat.

    Rainfall rates with the ongoing activity across central NY have
    recently been upwards of 2 inches/hour based on MRMS data, and
    similar rates are expected at least for a few more hours. There
    are uncertainties with the character of this MCS as it approaches
    and overspreads areas of northeast PA and northwest NJ, but some
    cell-training concerns could potentially settle down into these
    areas as well. Overall, the latest hires CAM guidance is doing a
    poor job with respect to the placement and intensity of the
    convection as most of the solutions are too slow and also tending
    to weaken the activity too quickly.

    Going through mid-morning, some additional rainfall totals of 2 to
    4 inches along the path of the MCS will be possible, with isolated
    heavier amounts not out of the question given the cell-training
    concerns. Areas of flash flooding are already occurring in central
    NY, and with rather low FFG values in general across central and
    southern NY through northeast PA and northwest NJ, there will be a
    likelihood of seeing more flash flooding going through the
    mid-morning hours from these rains.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-scO5DMf6_J5cNLfgaJiGmfzhK_w5adIQJzu9BVk2DJgOgmVwcvbMz9vhOBwAutmie0U= jiP429lGM_KGwWcSEKWjE1E$ for graphic product...

    ATTN...WFO...ALY...BGM...BUF...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 43577562 43247443 42327375 41607384 41017477=20
    41287590 41827645 42497670 43217642=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 22 13:35:32 2025
    AWUS01 KWNH 221335
    FFGMPD
    MNZ000-NDZ000-221830-

    Mesoscale Precipitation Discussion 0491
    NWS Weather Prediction Center College Park MD
    934 AM EDT Sun Jun 22 2025

    Areas affected...Eastern North Dakota and Northwest Minnesota

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 221333Z - 221830Z

    SUMMARY...Slow moving heavy thunderstorms developing over eastern
    ND will continue to shift northeast, but backbuild into the
    southwesterly deep layer flow, prolonging rainfall duration.
    Localized flash flooding is possible through midday.

    DISCUSSION...Latest regional radar and satellite indicate rapid
    development of a thunderstorm complex over east-central ND along a
    low level trough above a stationary surface front and northwest of
    a surface low. Recent rainfall estimates from KMVX have reached 2"
    in Foster County in a little less than an hour. This is developing
    in a moist/unstable environment. A lobe of elevated moisture (PW
    up to 1.8" per the RAP) will continue shifting northeast over the
    Red River of the North valley through midday and there is a strong
    ML CAPE gradient SW to NE that exceeds 3000 J/kg east of the
    current activity.

    35kt deep layer SWly flow will keep advecting the moisture north,
    though upwind Corfidi vectors point east which should continue to
    allow backbuilding. Through midday, rainfall of 1-3" can be
    expected in a short time frame/near one hour. 1hr FFG decreases
    ahead of the current activity to below 2". Localized exceedance of
    FFG is expected to continue, making for a possible flash flood
    threat through midday.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9lF-Qb33x6N65pyajLEA4S_tT0z27ntmB3N__7hhYIltE7t9Z2pDwtThoK_GB5ygXGmr= vQxf0Z5nIO2k9DxQcKzWKDw$ for graphic product...

    ATTN...WFO...BIS...FGF...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 49029618 48289537 46179544 46929730 47309959=20
    48149933 49009832=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 22 15:37:01 2025
    AWUS01 KWNH 221536
    FFGMPD
    NYZ000-NJZ000-PAZ000-222030-

    Mesoscale Precipitation Discussion 0492
    NWS Weather Prediction Center College Park MD
    1136 AM EDT Sun Jun 22 2025

    Areas affected...Eastern Pennsylvania and West-Central New York

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 221535Z - 222030Z

    SUMMARY...A threat for repeating thunderstorms continues through
    the afternoon over portions of northeast PA and west-central NY
    where flash flooding is possible. This activity should remain west
    of the extreme rainfall from this morning in southern NY. However,
    areas south and west of there are vulnerable to flooding given the
    terrain and low flash flood guidance.

    DISCUSSION...A slow moving western front left over from extreme
    rainfall in southern NY is the focus for continued convection over
    west-central NY and northeast PA. Recent uptick in activity there
    has resumed 1"/hr rainfall (in Susquehanna Co PA) due to repeating
    development as upper level steering flow is nearly parallel to
    this front. Low level westerly flow has diminished from this
    morning, but remains around 25kt at 850mb per NEXRAD VAD Wind
    Profiles (such as KCCX).

    Pooled elevated moisture (PW around 2.0") and a strong gradient in
    MLCAPE will continue to allow further development through the peak
    diurnal hours. Cell-training will continue to be a threat in this
    rather static mesoscale pattern.

    A question remains as to how far west this activity develops. Over
    the past hour, the progression west has greatly slowed which means
    continued training is a threat and could grow more considerable as
    indicated by 12Z ARW2/FV3LAM/NAMnest. Given 1hr FFG is below 1.5"
    there is a localized flash flood threat that may yet expand in coverage/intensity if the training activity does stall.

    Going through the afternoon morning, additional rainfall totals of
    1 to 3 inches along this frontal zone, and thus flash flooding are
    possible.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7uatsuElLPeTHV-pUs3Ks0CQx1niQy5qJB0GzdozDli76jCVvTakiQz6EcHFwnKNydDZ= mWyQBZaOTQToiEl_JrV5Ntc$ for graphic product...

    ATTN...WFO...BGM...CTP...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 42767651 42537579 41887532 41047493 40467502=20
    40267563 40747653 41407679 42457730=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 22 20:19:05 2025
    AWUS01 KWNH 222019
    FFGMPD
    TXZ000-NMZ000-230217-

    Mesoscale Precipitation Discussion 0493
    NWS Weather Prediction Center College Park MD
    418 PM EDT Sun Jun 22 2025

    Areas affected...portions of far west Texas into eastern New
    Mexico

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 222017Z - 230217Z

    Summary...Scattered, slow-moving thunderstorms will continue to
    develop across portions of the TransPecos and southeastern New
    Mexico this afternoon. The combination of slow storm movement and
    cell mergers should allow for spots of 1-1.5 inch/hr rain rates to
    develop, likely prompting flash flooding in a few locales.

    Discussion...Scattered thunderstorm activity has materialized
    along a surface trough/dryline extending from near SRR/Alto, NM
    southward through KVHN/Van Horn, TX. The storms are in a
    marginally sheared environment (20 kts effective shear), but
    reside in a zone of persistent low-level convergence and
    orographic ascent especially across far west Texas. 1-1.4 inch PW
    values, slow storm movement, and occasional cell mergers will
    eventually lead to spots of 1-1.5 inch/hr rain rates as storms
    mature through the early evening. An increase in convective
    coverage is depicted by CAMs over the next 2-4 hours, which is
    reasonable given widespread deepening convective cumulus across
    the discussion area amid ~1000 J/kg MLCAPE.

    As convective coverage increases this afternoon, 1-1.5 inch/hr
    rain rates will fall on areas of sensitive/urban terrain. 1.5
    inch/hr FFG thresholds exist across most of the discussion area,
    which should be exceeded at times. Flash flooding is likely on an
    isolated to scattered basis through at least 02Z/9p CDT.

    Cook=20=20=20

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Tli1qtU_ms7-Cd62gqeOrC7r8HhS3Yxh8IOKl3Y2tZs7Rx9AKdC6liQ8ZAz_Czr8aAX= SFokChvMOzP9rM2JDMIt0rQ$ for graphic product...

    ATTN...WFO...ABQ...AMA...EPZ...LUB...MAF...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35830416 35680296 34770267 33090351 31040288=20
    29950259 29060323 30680499 31630606 33320608=20
    35260513=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 22 20:44:46 2025
    AWUS01 KWNH 222044
    FFGMPD
    NDZ000-222300-

    Mesoscale Precipitation Discussion 0494
    NWS Weather Prediction Center College Park MD
    443 PM EDT Sun Jun 22 2025

    Areas affected...central/northeastern North Dakota

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 222042Z - 222300Z

    Summary...A band of elevated convection has developed across
    central North Dakota, while obtaining a favorable orientation for
    training. Areas of 1-1.5 inch/hr rain rates can be expected while
    the band persists, prompting isolated flash flood potential.

    Discussion...In the past half hour or so, convection along an axis
    extending from 50 miles northeast of Bismarck to ~20 miles west of
    Langdon has exhibited increasing organization and training. This
    band of convection was elevated, but likely tied to strong
    convergence along an 850mb trough in the area. The region also
    resides on the western fringes of very steep lapse rates aloft,
    and its SSW-NNE orientation is favorably oriented to steering flow
    aloft for training. Areas of 1-1.5 inch/hr rain rates have
    already been observed within this band - especially just northeast
    of Bismarck.

    The temporal extent of this flash flood risk is a bit uncertain,
    with models not handling the ongoing training convection
    particularly well. At least 2-3 hours of convective training can
    be expected within this axis, resulting in spots of 3-4 inch
    rainfall totals through 22-23Z. The mesoscale organization of the
    complex may not persist beyond that point as the band lifts
    quickly north-northeastward into south-central Canadian provinces.
    Convective trends will be monitored for additional heavy rain
    potential beyond 23Z/6p CDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6dHjX62Ujp2c7YgScLGrE4Bx9KLq2BOKMXuxkfNZoxq1KLA2zMfmgfdbQxjASVQQgc27= ELlf8pvBWP5ieP_1o0T1fwk$ for graphic product...

    ATTN...WFO...BIS...FGF...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 49169903 49109803 48619789 47709860 46969994=20
    47020079 47580052 48030037 48789983=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 23 03:22:03 2025
    AWUS01 KWNH 230320
    FFGMPD
    TXZ000-NMZ000-230800-

    Mesoscale Precipitation Discussion 0495
    NWS Weather Prediction Center College Park MD
    1118 PM EDT Sun Jun 22 2025

    Areas affected...Southwest to West-Central TX...Southeast NM

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 230318Z - 230800Z

    SUMMARY...Locally slow-moving clusters of heavy showers and
    thunderstorms will continue into a portion of the overnight
    period. Some additional scattered areas of flash flooding will be
    likely from the high rainfall rates.

    DISCUSSION...The latest GOES-E IR satellite imagery is showing a
    few slow-moving convective clusters across portions of southwest
    TX and into southeast NM. The convection is embedded within a very
    moist and moderately unstable environment characterized by PWs of
    1.5 to 1.7 inches, and MLCAPE values of 1000 to 1500 J/kg.

    Some weak vort energy is noted in WV satellite imagery lifting
    northeastward across the region within the deeper layer southwest
    flow over the region, and this is providing for some localized
    stronger forcing/ascent for this activity. Cooling convective tops
    have been noted over the last hour, and based off MRMS data, some
    of the rainfall rates have been as high as 1.5 to 2 inches/hour.

    Over the next few hours, the slow cell-motions associated with the
    convection will favor some storm totals that may reach 3 to 4+
    inches, and this is supported by some of the 00Z HREF solutions.
    The HREF consensus generally supports the greater concentrations
    of heavy rainfall focusing over southwest TX where the guidance
    indicates somewhat stronger mid-level forcing/vort energy.

    Given the additional rainfall threat, some additional scattered
    areas of flash flooding are generally likely.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-QDjP1j0rIeJgBzvcmxgzkm5XJTCq46AavGrUWC14XCvgbNB9Sc2EDxo8WLUx2a7VzR0= UZS2qyi5HGzpzvZeVkRmSy8$ for graphic product...

    ATTN...WFO...ABQ...EPZ...LUB...MAF...

    ATTN...RFC...FWR...NWC...

    LAT...LON 34290281 34050204 32930211 31090324 29560370=20
    29530438 29860484 30460492 30940537 31440514=20
    32630402 33950347=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 16 11:29:34 2025
    AWUS01 KWNH 161129
    FFGMPD
    MNZ000-IAZ000-161530-

    Mesoscale Precipitation Discussion 0456
    NWS Weather Prediction Center College Park MD
    728 AM EDT Mon Jun 16 2025

    Areas affected...South-central to Southeast MN...North-central to
    Northeast IA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 161130Z - 161530Z

    SUMMARY...A few more hours of warm-advective thunderstorms with
    slow cell motions or weak training profile resulting in localized
    2-4" totals and possible flash flooding.

    DISCUSSION...RAP analysis denotes a small well of uncapped MUCAPE
    across south-central to southeastern MN into IA along the
    southeasterly periphery of a well defined surface warm front
    extending from a surface low/triple-point near ATY in eastern
    SDAK. Solid southerly flow intersects and veers becoming
    increasingly convergent through the upglide over the front to
    provide sufficient WAA to have maintained scattered convection for
    the past few hours. However, trends continue to support further
    rooting toward the front across Freeborn county slowly extending
    northward toward Sibley county, effectively along/parallel to the
    deeper layer steering flow. While the steering flow is weak to
    allow for fairly stationary cell motions, any motions generally
    are parallel to the frontal zone allowing for some
    cross-over/repeating of the cores of the cells. CIRA LPW along
    with RAP analysis denotes a 700mb wave and peak moisture pool
    across SE MN providing both the steering and the enhanced deeper
    layer moisture; though that is generally moderate to above average
    at about 1.5-1.7" in total. Inflow at cloud base is only about
    mid 60F Tds so efficiency is mid-level at about 1.5"/hr
    occasionally reaching 2" with pulses of WAA. Allowing for overall
    totals to be highly concentrated but starting to near 3" localized
    maxima.

    The greatest uncertainty remains on how long the favorable upglide
    can maintain give stronger upglide is likely to increased deeper
    layer cell motions and break up the more favored repeating
    environment, though even slight veering more westward in the
    lowest layers will also disrupt the setup. At this time, most
    guidance is traditionally slow with the upstream wave and have
    been suggesting a 15z disruption/end to ideal setup; however,
    typical model bias would suggest an hour or two faster and given
    upstream trends on the overall wave, this seems plausible. As
    such a few more hours can be expected likely expanding the 2-3"
    footprint with localized further increase to near 4" possible.=20
    Given FFG in the 1.5-2"/hr and 2-3"/3hr values, exceedance is
    probable and result in possible localized incident or two of flash
    flooding conditions through 15z before shifting southeast into NE
    IA with reduced overall totals.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8iRPBIRwNaYa_vct97pef8SaLqqBlfjgUUUocr6IgIzKe5tzpeNC5seJRK6CsYfAmk4N= FL4aaQioFUVbZ4iSjjo8ecw$ for graphic product...

    ATTN...WFO...ARX...DMX...MPX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 44839378 44129256 43669209 43079186 42759247=20
    42919314 43559390 44189415 44799420=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 16 14:02:38 2025
    AWUS01 KWNH 161402
    FFGMPD
    TXZ000-161900-

    Mesoscale Precipitation Discussion 0457
    NWS Weather Prediction Center College Park MD
    1001 AM EDT Mon Jun 16 2025

    Areas affected...Coastal South Texas...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 161400Z - 161900Z

    SUMMARY...Small MCC will continue to slowly drift southward with
    2-3"/hr rates and localized totals up to 5"+ resulting in
    continued flash flooding concerns through early afternoon.

    DISCUSSION...A small cluster of thunderstorms continues to grow
    upscale into a well formed/concentric Mesoscale Convective Complex
    across the lower TX coast. GOES-E WV suite shows the primarily
    forcing shortwave is between the two larger scale ridges west and
    east of it with a clear break in the mid-level westerlies to its
    north. Right entrance to a 25kt outflow jet to the south along
    the coast has been providing solid outflow aloft to maintain the
    MCV/shortwave especially given the mid-level latent heat release
    with this tropical-like complex. In the lower levels, the
    southerly Western Gulf LLJ has been providing solid flux
    convergence to the WSW to ENE outflow boundary across Corpus
    Christi Bay that has also taken on a N-S confluent orientation as
    far south as South Padre Island into NE Cameron county.=20=20
    Additionally, the mid-level outflow along the SW flank of the
    complex has been expanding a banding-like feature into N Kenedy
    county fairly orthogonal to the LLJ further enhancing convective
    complex. Given total PWats over 2.25" and 20-25kt of orthogonal
    inflow, the hourly rates of 2-3" are common and broadening in
    coverage.=20

    Very slow south-southwestward propagation is expected over the
    coming hours. Upstream instability remains more than sufficient
    with MLCAPEs already well over 2000 J/kg. Given the favorable
    upper-level environment for outflow, would expect this convective
    complex to maintain/expand southward along the coast with broad
    2-4" totals with localized 5-6" probable. Eventually, the western
    Gulf LLJ/WAA maximum will continue to slide north-northeast into
    the Upper Texas coast, likely to reduce some low-level convergence
    closer to the beaches, but still will provide solid flux to the
    complex. Additionally, this complex is also moving through very
    low population and very favorable soil conditions for
    infiltration, the shear amount in time will likely continue to
    produce flash flooding conditions through the noon-time hours into
    early afternoon.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4m-1AvGtE7uggz4CrsmEHWMsP8hZ1FmUpmmDejgp4iNz514MmrlWpx-owdkdg8rr9bEW= lMpGkp30eGBEcaFIoDct4h4$ for graphic product...

    ATTN...WFO...BRO...CRP...

    ATTN...RFC...FWR...NWC...

    LAT...LON 27599797 27599754 27379730 26869729 26139712=20
    26129762 26439818 26899826 27319820=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 16 16:43:12 2025
    AWUS01 KWNH 161643
    FFGMPD
    VAZ000-NCZ000-WVZ000-TNZ000-KYZ000-162200-

    Mesoscale Precipitation Discussion 0458
    NWS Weather Prediction Center College Park MD
    1241 PM EDT Mon Jun 16 2025

    Areas affected...Cumberland Plateau & Central Appalachians...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 161640Z - 162200Z

    SUMMARY...Weakly organized but efficient rainfall producing
    convective cells to increase in coverage/intensity over the next
    few hours resulting in widely scattered 1.5-2.5" totals and
    possible localized flash flooding.

    DISCUSSION...16z surface observations across the Cumberland
    Plateau into the central Appalachians show increasing temperatures
    into the mid to upper 70s with isolated 80s further south with
    very high dewpoints in the low to mid 70s across much of the area.
    Weak surface ridging along the western upslope of the Cumberland
    Plateau with mild troughing from N GA to W VA connects up to the
    surface frontal boundary around SW VA with a damming ridge across
    western and northwestern VA. As such, weak capping and sufficient
    convergence is breaking out thunderstorm activity particularly
    through the Cumberland Gap region of W KY/SW VA/NE TN, though
    additional bubbling Cu/TCu expand along the Smokey Mtn Ridge line
    to the south with increasing congestion south of the front in
    central WV.=20

    Total moisture of 1.75 to 2" is about 2-2.5 standard deviation
    from the mean at this time of year and given recent heavy rainfall
    has easily evaporated to further enhance rainfall potential.=20
    Given increasing instability toward 1000-1500 J/kg (MLCAPE),
    scattered updrafts should be fairly efficient with 13-14Kft of
    warm cloud layer processes to support 1.5"/hr rates with strongest
    cores perhaps up to 2". Deep layer westerly steering at about
    20kts will keep cells moving, but likely support sufficient
    duration for 1-2" totals. Secondary development along the upwind
    flanks of the outflow boundaries may allow for increased duration
    for short-term duration for a highly isolated 2.5" total. Given
    overall saturated ground conditions (all but south-central VA, per
    NASA SPoRT relative soil moisture values/percentiles) and complex
    terrain, above average runoff is expected and may result in widely
    scattered incidents of flash flooding increasing in coverage
    toward peak heating in the next 3-4 hours.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-4ZApocQ1Gm3csMyof-dHUyifJtqOp18ll0Te8Ho9phH-aJzxRTqi57FPMk-CTnZGpuF= IopP1_uH6xdeFJ1-RSbuFVk$ for graphic product...

    ATTN...WFO...GSP...JKL...LWX...MRX...RAH...RLX...RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 39098031 38887956 38607926 38077910 37267935=20
    36158050 35078284 35028406 35168515 36088450=20
    36658425 37338376 38028289 38578207 38788167=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 16 18:03:44 2025
    AWUS01 KWNH 161803
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-162330-

    Mesoscale Precipitation Discussion 0459
    NWS Weather Prediction Center College Park MD
    202 PM EDT Mon Jun 16 2025

    Areas affected...Western & Central KY...Southern IND...Southern
    IL...Southeast MO...Northeast AR...Adj. TN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 161800Z - 162330Z

    SUMMARY...Slow moving, efficient thunderstorms capable of 2-3" in
    1-2 hours pose localized flash flooding conditions, especially
    upstream over saturated ground conditions/low FFG.

    DISCUSSION...GOES-E WV suite shows a broad anticyclonic arch of
    high cirrus indicative of broad mid to upper level confluent flow
    to speed max over central Ohio Valley (generally 50kts). This
    results in a broad entrance region with favorable upper-level
    divergence to support/maintain an elongated shear axis from a
    stalled/shortwave feature across the eastern Ozark Plateau to a
    convectively reinforced short-wave crossing southern IL into
    southwest IND at this time. The combination of broad scale ascent
    has provided ample broken to dense mid to upper-level cloud
    features reinforcing surface front through differential heating
    across northeast AR into Western KY. Visible imagery also helps
    to denote the surface to 850mb low across N AR with front
    generally along the southern portion of the cloud line across SE
    MO, S IL into SW IND. Low level moisture remains above normal and
    into the low to mid 70s wrt dewpoint and CIRA LPW in the surface
    to 850mb within the Mississippi and Lower Ohio Valley nearing 1"
    in places. As such, a plume of 2"+ TPW exists across the area
    expanding eastward into western KY. Heating into the mid to upper
    80s will steadily increase instability over 1500 J/kg MLCAPE with
    SBCAPEs already over 3000 J/kg. As such, recent convective
    initiation has been quick and vigorous across S IL/W KY and will
    likely become quickly efficient in rainfall production given the
    flux through the core of the moisture plume. Rates of 2"/hr are
    likey though 15z HRRR hints that 15-minute totals may reach 1.5"
    given the overall efficiency/deep warm cloud processes.

    Deep layer flow should allow for cells to be fairly progressive
    especially east of the MS River valley and organized structures
    are likely to be clustered along and south of the frontal zone.=20
    Random upstream redevelopment has potential for repeating tracks,
    so spots of 2-3" totals are probable through the late
    afternoon/early evening. Cells near the surface to 850mb low are
    likely to be slower in eastward cell motions being a tad further
    west of the jet entrance with perhaps a cell getting lodged on
    some of the hills of the eastern Plateau given some favorable
    upslope. Additionally, FFG values are reduced upstream due to
    heavy rainfall last evening with 1hr values less than
    1.5"...though downstream in W KY are still between 1.5-2" with 3hr
    values in the 2-2.5" range. While the incidents of flash
    flooding are likely to be scattered in nature throughout the MPD
    area, the probability of FFG exceedance is likely and most
    probable upstream with lower FFG and slower cell motions (though
    lesser deep moisture/instability).

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8UQ39KEdni9YmN8qUQ_8y98AGhFSNpZ6viXOVbIgm9_h9OW_BhlfQFLYwUObpD3dsw4Z= q9wNOxCeH1WyJvnkZHnZXUQ$ for graphic product...

    ATTN...WFO...ILX...IND...LMK...LSX...LZK...MEG...OHX...PAH...
    SGF...

    ATTN...RFC...MSR...ORN...TIR...TUA...NWC...

    LAT...LON 39008653 38658541 38158488 37568483 36788544=20
    36538799 35749027 35339189 35679272 36239272=20
    37009205 37639098 38588915 38908806=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 16 18:24:09 2025
    AWUS01 KWNH 161824
    FFGMPD
    VAZ000-NCZ000-SCZ000-170022-

    Mesoscale Precipitation Discussion 0460
    NWS Weather Prediction Center College Park MD
    222 PM EDT Mon Jun 16 2025

    Areas affected...Southern Mid-Atlantic

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 161822Z - 170022Z

    SUMMARY...Heavy showers and thunderstorms will be developing and
    expanding in coverage through the afternoon and into the evening
    hours across much of the southern Mid-Atlantic region. Scattered
    areas of flash flooding are likely, which will include concerns
    for locally considerable urban flooding impacts.

    DISCUSSION...Surface observations show a quasi-stationary front
    draped once again across the southern Mid-Atlantic region and into
    the central Appalachians, with the 18Z METARs showing the front
    close to the VA/NC border and extending northwest up into eastern
    WV. Strong diurnal heating along and south of the boundary has
    allowed for the airmass across especially central and eastern NC
    to become very unstable with MLCAPE values of 2000 to 3000 J/kg.

    The low-level flow is very moist and rather convergent with PWs
    over the eastern half of NC running upwards of 2.0 to 2.25 inches.
    This coupled with additional surface heating over the next couple
    of hours along with convergence in close proximity to the front
    should favor the regional development and expansion of heavy
    shower and thunderstorm activity over the next few hours which
    will continue into the evening time frame.

    Rainfall rates are expected to once again be very high, with rates
    reaching as high as 2.5 inches/hour given the moist/unstable
    environment. The convection should tend to be a combination of
    slow-moving pulse and multi-cell convection, with some localized
    concerns for cell-training possible.

    The 12Z HREF supports some rainfall totals by 00Z (8pm EDT) of 3
    to 5 inches, and some recent RRFS solutions support this as well.
    Some areas of central and eastern NC saw rather heavy rainfall
    totals over the last 24 hours and are relatively sensitive. This
    combined with the additional rainfall, along with concerns for the
    more sensitive urban areas, including the Raleigh-Durham
    metropolitan area, suggests at least scattered areas of flash
    flooding are likely. Locally considerable urban flooding impacts
    will be possible going into the early evening hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_HWFy3AurrHzBtwgGBu-0U_ksnyj5hIrAq-csplnli80aa4_EwESsD4Nqont148gwvmW= fEYIFiBsy2dCNAuMpworpLs$ for graphic product...

    ATTN...WFO...AKQ...CAE...GSP...ILM...MHX...RAH...RNK...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 36997989 36737931 36537842 36427742 36457659=20
    36467588 35947551 35067581 34627769 34767938=20
    35138142 35418218 35828216 36198156 36518094=20
    36898035=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 16 18:40:02 2025
    AWUS01 KWNH 161838
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-162330-

    Mesoscale Precipitation Discussion 0459...Corrected
    NWS Weather Prediction Center College Park MD
    237 PM EDT Mon Jun 16 2025

    Corrected for FF Likely

    Areas affected...Western & Central KY...Southern IND...Southern
    IL...Southeast MO...Northeast AR...Adj. TN

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 161800Z - 162330Z

    SUMMARY...Slow moving, efficient thunderstorms capable of 2-3" in
    1-2 hours pose localized flash flooding conditions, especially
    upstream over saturated ground conditions/low FFG.

    DISCUSSION...GOES-E WV suite shows a broad anticyclonic arch of
    high cirrus indicative of broad mid to upper level confluent flow
    to speed max over central Ohio Valley (generally 50kts). This
    results in a broad entrance region with favorable upper-level
    divergence to support/maintain an elongated shear axis from a
    stalled/shortwave feature across the eastern Ozark Plateau to a
    convectively reinforced short-wave crossing southern IL into
    southwest IND at this time. The combination of broad scale ascent
    has provided ample broken to dense mid to upper-level cloud
    features reinforcing surface front through differential heating
    across northeast AR into Western KY. Visible imagery also helps
    to denote the surface to 850mb low across N AR with front
    generally along the southern portion of the cloud line across SE
    MO, S IL into SW IND. Low level moisture remains above normal and
    into the low to mid 70s wrt dewpoint and CIRA LPW in the surface
    to 850mb within the Mississippi and Lower Ohio Valley nearing 1"
    in places. As such, a plume of 2"+ TPW exists across the area
    expanding eastward into western KY. Heating into the mid to upper
    80s will steadily increase instability over 1500 J/kg MLCAPE with
    SBCAPEs already over 3000 J/kg. As such, recent convective
    initiation has been quick and vigorous across S IL/W KY and will
    likely become quickly efficient in rainfall production given the
    flux through the core of the moisture plume. Rates of 2"/hr are
    likey though 15z HRRR hints that 15-minute totals may reach 1.5"
    given the overall efficiency/deep warm cloud processes.

    Deep layer flow should allow for cells to be fairly progressive
    especially east of the MS River valley and organized structures
    are likely to be clustered along and south of the frontal zone.=20
    Random upstream redevelopment has potential for repeating tracks,
    so spots of 2-3" totals are probable through the late
    afternoon/early evening. Cells near the surface to 850mb low are
    likely to be slower in eastward cell motions being a tad further
    west of the jet entrance with perhaps a cell getting lodged on
    some of the hills of the eastern Plateau given some favorable
    upslope. Additionally, FFG values are reduced upstream due to
    heavy rainfall last evening with 1hr values less than
    1.5"...though downstream in W KY are still between 1.5-2" with 3hr
    values in the 2-2.5" range. While the incidents of flash
    flooding are likely to be scattered in nature throughout the MPD
    area, the probability of FFG exceedance is likely and most
    probable upstream with lower FFG and slower cell motions (though
    lesser deep moisture/instability).

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7l9PaXvJ-3mUClkVUOSDT5VIoG1TEjQ4JkP9VHyw7iyv5K8FFQuQFnafxN2yO8XvPMVm= 9oJf6Ev-Da7gHQ1Rs_nXBlY$ for graphic product...

    ATTN...WFO...ILX...IND...LMK...LSX...LZK...MEG...OHX...PAH...
    SGF...

    ATTN...RFC...MSR...ORN...TIR...TUA...NWC...

    LAT...LON 39008653 38658541 38158488 37568483 36788544=20
    36538799 35749027 35339189 35679272 36239272=20
    37009205 37639098 38588915 38908806=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 16 20:28:12 2025
    AWUS01 KWNH 162026
    FFGMPD
    LAZ000-TXZ000-170100-

    Mesoscale Precipitation Discussion 0461
    NWS Weather Prediction Center College Park MD
    426 PM EDT Mon Jun 16 2025

    Areas affected...Southeast TX...Far Southwest LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 162025Z - 170100Z

    SUMMARY...Slow-moving showers and thunderstorms with high rainfall
    rates over the next few hours may expand a bit more in coverage
    and pose concerns for isolated areas of flash flooding, and
    especially around the more urbanized locations.

    DISCUSSION...The mid-afternoon GOES-E visible satellite imagery
    along with regional radar data shows pockets of slow-moving and
    heavy showers and thunderstorms developing across portions of
    southeast TX and into far southwest LA. The activity is focusing
    along a convergence axis inland of the upper TX coast and out
    ahead of some weak shortwave energy advancing gradually into
    eastern TX.

    MLCAPE values over the region are locally as high as 3500 J/kg
    with PWs of around 2 inches, and this will be set the stage for
    some expansion of convection over the next few hours across
    especially southeast TX which may include the broader Houston
    metropolitan area.

    The 12Z HREF and 06Z REFS guidance both support some localized
    concentrations of slow-moving convective cells going through the
    late-afternoon and early evening hours. Rainfall rates are
    expected to be as high as 1.5 to 2.5 inches/hour, with some
    potential for localized storm totals by early this evening to be 3
    to 4+ inches.

    Some low to moderate probabilities (20 to 50 percent) of exceeding
    the 3-hour FFG are noted in the HREF and REFS guidance suites, and
    this suggests there may be at least an isolated concern for some
    flash flooding which in this case would primarily be a concern for
    the more urbanized locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-zw7MEO2muxVNT9xooq1-HD4hwaRR_XVj5LMxt6dusdsRLhjVyTYBf7HP1CK-Jd7LFkn= Vqvk9kZelIiRKtVAF5Cx7tc$ for graphic product...

    ATTN...WFO...HGX...LCH...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 30919460 30739351 29939315 29649414 29229511=20
    29029583 29269644 29799663 30269626 30619551=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 16 22:01:54 2025
    AWUS01 KWNH 162201
    FFGMPD
    VAZ000-NCZ000-WVZ000-170300-

    Mesoscale Precipitation Discussion 0462
    NWS Weather Prediction Center College Park MD
    600 PM EDT Mon Jun 16 2025

    Areas affected...Southeast WV...Southwest VA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 162200Z - 170300Z

    SUMMARY...Slow-moving showers and thunderstorms with very high
    rainfall rates are likely to result in at least scattered areas of
    flash flooding going through the evening hours. Some locally
    significant and life-threatening impacts are possible near areas
    of higher terrain.

    DISCUSSION...The GOES-E IR satellite imagery shows areas of
    slow-moving, but very efficient shower and thunderstorm activity
    impacting portions of southeast WV on down through southwest VA
    with an emphasis on some of the higher terrain of the central
    Appalachians, the adjacent Piedmont, and especially the Blue Ridge.

    A stationary front remains draped up against the eastern slopes of
    the higher terrain, with very moist low-level easterly flow aiming
    into the Blue Ridge. This combined with convection forming near
    and just west of the front within the instability pool over the
    higher terrain of central Appalachians is promoting a setup
    capable of yielding locally enhanced rainfall totals across the
    upslope areas of southeast WV and southwest VA.

    MLCAPE values over central and southern WV remain on the order of
    1000 to 1500+ J/kg, but PWs are locally near 2 inches, and the
    CIRA-ALPW data shows notably concentrated moisture in the 850/700
    mb layer where much of the stronger cloud-bearing ascent will be
    situated.

    Some of the 12Z HREF guidance and recent RRFS solutions are quite
    wet this evening, and support some slow-moving convective cells
    potentially anchoring themselves near the upslope areas of the
    Blue Ridge over the next few hours. Rainfall rates with the
    stronger ongoing storms are already as high as 2.5 inches/hour,
    and storms will continue to be capable of yielding these rates
    given the very moist/tropical vertical column that is in place.

    Given the concerns for slow-moving and orographically aided
    convection this evening near the front and the adjacent terrain,
    some rainfall totals may reach 3 to 5+ inches. This will likely
    result in at least scattered areas of flash flooding, with
    potential for locally considerable and life-threatening impacts
    given the potential for enhanced terrain-driven runoff and
    channeled flow away from the terrain.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5mY4DF4_oVCR7ZupSOG0dnEhaCh-8JVkHjvni8Z0c1f7GSvczk5zc3p65mlGKW4zmCfe= pgP-I_fvUDAUY-hfWq2beqs$ for graphic product...

    ATTN...WFO...LWX...RLX...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 38697975 38607937 38437919 38117915 37477923=20
    36647932 36447998 36628073 37078096 37728090=20
    38178064 38578021=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 16 23:31:11 2025
    AWUS01 KWNH 162331
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MSZ000-MOZ000-ARZ000-170530-

    Mesoscale Precipitation Discussion 0463
    NWS Weather Prediction Center College Park MD
    730 PM EDT Mon Jun 16 2025

    Areas affected...Portions of the Mid-South and OH Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 162330Z - 170530Z

    SUMMARY...Additional scattered to broken bands of showers and
    thunderstorms will continue to promote a threat for isolated to
    scattered areas of flash flooding going through the remainder of
    the evening hours.

    DISCUSSION...The late-day GOES-E IR satellite imagery along with
    radar shows an elongated and generally disorganized axis of
    showers and thunderstorms impacting areas of the Mid-South into
    the OH Valley. Some of the cooler convective tops over the last
    hour have been noted over areas of central and western KY,
    northwest TN, and parts of eastern AR where there has been a tad
    more low-level convergence along with a favorable thermodynamic
    environment for renewed rounds of convection.

    MLCAPE values more broadly across the region are generally still
    on the order of 1000 to 2000 J/kg, and the column remains very
    moist with PWs locally near or over 2 inches. For many areas, that
    is in the 90th percentile of climatology, and this has helped
    foster heavy rainfall rates with some of the bands of convection
    over the last few hours.

    The pattern across the region in the low-levels remains generally
    convergent along and south of a quasi-stationary front which also
    involves a wave of low pressure over northwest AR. However, aloft
    there is an elongated axis of mid-level vort energy which extends
    from the Lower MS Valley northeastward into the Lower OH Valley.
    Some modest deeper layer ascent is associated with this energy,
    and a combination of this with the front and also the
    moist/unstable boundary layer regime should support a continuation
    of scattered to broken bands of convection at least through the
    late-evening hours.

    Rainfall rates with the additional storms will still be capable of
    reaching 2 inches/hour, and with some localized pockets of
    cell-training, some of the additional rainfall totals going
    through midnight may reach 2 to 4 inches.

    Some additional isolated to scattered areas of flash flooding will
    be possible as a result, and especially with the moist antecedent
    conditions and local urban sensitivities.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4UgKdw8ohWSk-UqdNqY5cb06hVa2eoCIHcEo8JLMb0jiMVS3JHpJU7KCJTV9uOwhfV5N= TRMnwWn-r5dxPPjmTfyBmxk$ for graphic product...

    ATTN...WFO...ILN...JAN...JKL...LMK...LZK...MEG...OHX...PAH...

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 38438446 37528430 36668653 35398888 33909085=20
    34239171 36329047 37448897 38248681=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 17 00:33:50 2025
    AWUS01 KWNH 170032
    FFGMPD
    NCZ000-SCZ000-170500-

    Mesoscale Precipitation Discussion 0464
    NWS Weather Prediction Center College Park MD
    830 PM EDT Mon Jun 16 2025

    Areas affected...Central and Eastern NC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 170030Z - 170500Z

    SUMMARY...Heavy showers and thunderstorms will continue for at
    least a few more hours across areas of central and eastern NC.
    Additional isolated to scattered areas of flash flooding are
    possible.

    DISCUSSION...Very cold convective tops are noted with clusters of
    heavy showers and thunderstorms moving gradually east across
    central and eastern NC this evening. The convection remains
    embedded within a very moist and unstable boundary layer focused
    near and south of a stationary front.

    PWs of 2.0 to 2.25 inches, and MLCAPE values as high as 1500 to
    2500 J/kg are still in place based on the latest RAP analysis.
    Some modest shear with a belt of relatively stronger northwest
    mid-level flow is noted overhead as well and this coupled with the
    strong thermodynamics has been yielding some organization to the
    convection over the last couple of hours.

    Expect the areas of showers and thunderstorms to continue to
    advance off to the east with some loss in latitude as well over
    the next few hours, with some of the storms still capable of
    producing rainfall rates of 1.5 to 2.5 inches/hour with the
    stronger cells.

    However, the latest hires model guidance suggests that the
    activity should gradually weaken by late this evening as boundary
    layer instability gradually wanes. Some additional localized storm
    totals of 2 to 4 inches will be possible where the stronger storms
    focus at least over the next few hours.

    This may support some additional isolated to scattered areas of
    flash flooding which may also still include some localized urban
    flooding concerns.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5vfD60lU1gkMbXn8xUVKb5nvo9LJPsQs-cieKVWpfyhmKCqKGuiOAfYwH3bzCcyM-EH0= jKDa2rb7YI4IxRDJOcDKNxE$ for graphic product...

    ATTN...WFO...AKQ...GSP...ILM...MHX...RAH...RNK...

    ATTN...RFC...ALR...NWC...

    LAT...LON 36527902 36407820 36337749 36297702 36297649=20
    36167594 35767560 35347575 34877664 34587770=20
    34567894 34848003 35478039 36088048 36428021=20
    36417978=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 17 01:19:43 2025
    AWUS01 KWNH 170119
    FFGMPD
    MNZ000-170630-

    Mesoscale Precipitation Discussion 0465
    NWS Weather Prediction Center College Park MD
    918 PM EDT Mon Jun 16 2025

    Areas affected...Northeast MN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 170118Z - 170630Z

    SUMMARY...A strong MCS advancing across northeast MN will continue
    to drive concentrated and heavy areas of rainfall over the next
    few hours. Some additional areas of flash flooding will be
    possible.

    DISCUSSION...A strong cold-topped convective complex continues to
    ride northeastward up across northeast MN this evening in
    association with a compact shortwave trough and associated wave of
    low pressure. Strong shortwave dynamics interacting with a nose of
    focused elevated instability and warm air advection riding up
    toward northeast MN will favor the convection maintaining its
    organization through the remainder of the evening hours.

    Rainfall rates with the additional storms over the next 2 to 3
    hours will continue to be on the order of 1 to 2 inches/hour given
    the concentration of instability near what appears to be a
    tightening mid-level MCV southeast of Hibbing. Given some of the
    concentrated banded nature of the convection near the MCV feature,
    some of the additional rains may reach 3 to 4+ inches going
    through the late-evening hours which is supported by the latest
    RRFS guidance.

    The antecedent conditions are rather dry across the area, but with
    the latest radar/satellite trends and hires CAM guidance,
    additional areas of flash flooding will be possible.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9NhBpsH2Oi6i6fY09FUuBRCf6mzBxooprofAUx3sDDnewo6iYt2IQzPV3O_Zv0inIK8Z= zNdYZ4bUaD1ZDQTO3nL-9Nw$ for graphic product...

    ATTN...WFO...DLH...

    ATTN...RFC...MSR...NWC...

    LAT...LON 48259207 48229014 47918971 47449088 47089156=20
    47239229 47189297 47789305=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 17 04:09:49 2025
    AWUS01 KWNH 170408
    FFGMPD
    MDZ000-WVZ000-170900-

    Mesoscale Precipitation Discussion 0466
    NWS Weather Prediction Center College Park MD
    1207 AM EDT Tue Jun 17 2025

    Areas affected...northern WV into far western MD

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 170400Z - 170900Z

    Summary...Some persistence of 1.0-1.5" localized hourly rainfall
    amounts may allow for isolated instances of flash flooding.

    Discussion...Relatively weak low-level convergence and moisture
    transport in the vicinity of a quasi-stationary surface front and
    inverted trough of low pressure is maintaining a cluster of heavy
    showers and thunderstorms with efficient rainfall (1.0-1.5" hourly
    localized amounts, per MRMS) over northern portions of WV. The
    mesoscale environment in the vicinity of this cluster of
    convection is characterized by a maxima of surface based
    instability (SB CAPE of 500-1500 J/kg) with little to no
    convective inhibition, precipitable water values of 1.7-1.9 inches
    (near record levels, per PIT sounding climatology), and effective
    bulk shear of 25-30 kts. Low-level moisture transport is only
    expected to increase over the next few hours, as the pressure
    gradient tightens with a deepening low over the northern Great
    Lakes and an upper-level trough over the Mid-South both making
    their way eastward. Isentropic lift is expected to become more
    pronounced as a result (concentrated on the 300-305K surface,
    generally between the 900-800 mb isobaric surface), and this
    appears to be favorably offset by idealized divergence aloft in
    the vicinity of the right-entrance region of a 70 kt jet streak at
    250 mb (centered over north-central PA and arcing ESE-SE).

    While 00z hi-res CAM signals are rather limited (with the 00z HREF
    suite largely absent of QPF, with the exception of the 00z ARW),
    the hourly HRRR runs have started to initialize and pick up on the
    convection (02z more significantly so, depicting some 1-3"
    totals). While the HRRR seems to want to kill off the convection
    rather quickly, the 00z ARW indicates the potential for the
    persistence of ~1"/hr localized rates (with slow progression and
    backbuilding allowing for localized 2-3" QPF). Given the rather
    favorable aforementioned environment for heavy rainfall (with a
    particular focus on the highly efficient warm rain processes, as
    wet bulb zero heights are around 12k feet) with very sensitive
    terrain and wet antecedent conditions (1-3 hr FFGs of 1" or less).
    Isolated instances of flash flooding are possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-HlEH793x37spb6u4m2aRY_bwlaSZk-6C8SNRXPKGEeL23U4ShoHcm0icmWIhZbaGk6W= HA_cBO_MHqK44kHzSbUux9k$ for graphic product...

    ATTN...WFO...LWX...PBZ...RLX...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 39697956 39517895 38957909 39017986 39238091=20
    39498097 39668073=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 17 11:53:18 2025
    AWUS01 KWNH 171153
    FFGMPD
    KSZ000-171531-

    Mesoscale Precipitation Discussion 0467
    NWS Weather Prediction Center College Park MD
    752 AM EDT Tue Jun 17 2025

    Areas affected...Central KS...Far Northern OK

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 171152Z - 171531Z

    Summary...Convection has developed upstream of an intense bowing
    segment along the KS-OK border. Periodic training of these upwind
    cells containing max hourly rainfall rates of 1.5-2"/hr could
    support additional flash flooding this morning.

    Discussion...Radar depicts an axis of convection developing across
    Central KS, upstream of an intense bowing segment currently
    located along the KS-OK border. While this bowing segment is
    rapidly forward propagating, 2"/hr rainfall rates led to several
    reports of flash flooding in the Wichita area earlier, with
    additional reports received to the north in McPherson from the
    upstream activity.

    Objective analysis output suggests the environment in the wake of
    this bowing segment will support the maintenance of training cells
    for several more hours as a 30-40 kt nocturnal LLJ bisects a NW-SE
    oriented stationary front, which was parallel to the NW'ly
    effective shear vectors amid 2000-3000 MUCAPE and 1.4-1.7" PWATS.

    The HRRR suggests localized amounts upwards of 1.5-2.5" are
    possible through 15Z, in addition to the 2-3" estimated earlier.
    Thus, additional instances of flash flooding are possible where
    these cells can train before the nocturnal LLJ begins to weaken
    around 15z, particularly over the Wichita and McPherson areas
    currently experiencing flash flooding.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!__DuBJ5itTBL1Ma3F42q_ttOPJv4UYCEEKa_OEThcrkU6m4yNh_TlimHiwZq63wJa2Zx= 5VLhsjhrk0XIoExVPwYwTkI$ for graphic product...

    ATTN...WFO...DDC...GID...ICT...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39459879 38629718 37779656 37119678 37119769=20
    37779874 38959953=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 17 17:05:22 2025
    AWUS01 KWNH 171705
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-OHZ000-172303-

    Mesoscale Precipitation Discussion 0468
    NWS Weather Prediction Center College Park MD
    104 PM EDT Tue Jun 17 2025

    Areas affected...Eastern OH Valley...Central Appalachians

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 171703Z - 172303Z

    Summary...Repeating rounds of showers and thunderstorms containing
    rainfall rates exceeding 2"/hr at times are expected to produce
    scattered to numerous instances of flash flooding this afternoon
    -- some significant.

    Discussion...Recent trends in Day Cloud Phase RGB and
    LightningCast data suggest convection is developing over the Ohio
    River Valley and and Central Appalachians as steady moistening and
    insolation occur ahead of an approaching vort max in the
    Mid-South. A recent cluster of cells near Pittsburgh produced
    radar estimated rainfall rates of 1-2"/hr, prompting two Flash
    Flood Warnings.

    While this activity remains fairly scattered as of now,
    mesoanalysis, GPS, and earlier regional soundings show an
    increasingly unstable and saturated airmass available for these
    maturing cells to tap into, with 1000 J/kg of MLCAPE (with no
    CIN), 1.9-2" PWATs (above the daily max for many sites), and
    13,000-14,000 foot warm cloud depths. Individual cell motions will
    likely be somewhat progressive owing to 25-30 kts of effective
    shear across the region, but should assist with overall cell
    longevity.

    Going forward, the expectation is for coverage and intensity of
    cells to increase as the moistening and heating continues while
    the upstream vort-max slowly lifts into the Ohio Valley this
    afternoon. The overall setup should favor repeating rounds of
    thunderstorms along a SSW to NNE axis, with the HREF highlighting
    increasing probabilities of 1-2"/hour rainfall rates beginning
    around 17-19z. As these rates are realized, both the HREF and REFS
    neighborhood probabilities show a high likelihood (above 50%) of
    1-3 HR FFG exceedance through 22-23Z. However, even outside of
    the area of most intense rates, the combination of repeat rounds
    of thunderstorms and low FFGs (at or below 1") suggests scattered
    to numerous instances of flash flooding are likely -- some
    significant.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-rBBVyn0YYdkhwNFUUk7tKxGbgZvlRuCCS-y-sMehhR96j-vL8RONPLgQU8EhcQ_0x-w= X3KVXJsmCU0d-LKPAq8pNiY$ for graphic product...

    ATTN...WFO...AKQ...CLE...CTP...LWX...PBZ...RLX...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 41417891 40977746 39777721 38537752 37537917=20
    37268015 37648091 38698109 39728184 40428174=20
    41168042=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 17 18:34:42 2025
    AWUS01 KWNH 171833
    FFGMPD
    WVZ000-OHZ000-TNZ000-KYZ000-INZ000-ALZ000-MSZ000-180032-

    Mesoscale Precipitation Discussion 0469
    NWS Weather Prediction Center College Park MD
    233 PM EDT Tue Jun 17 2025

    Areas affected...OH Valley...TN Valley

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 171832Z - 180032Z

    Summary...Repeating rounds of showers and thunderstorms with
    2-2.5"/hr max rainfall rates are expected to produce isolated to
    scattered instances of flash flooding.

    Discussion...Regional radar mosaic highlights a corridor of
    expanding showers and thunderstorms along and ahead of a broad
    upper-trough and embedded vort-max located in the TN Valley.
    Downstream of this feature, a NE-SW oriented confluence axis was
    analyzed in the 925-850 hPa layer, which cells are generally
    organizing along.

    Very moist and unstable inflow characterized by 2-2.1" PWATs,
    eventually 1000-1500 J/kg MLCAPE (in a "tall-skinny" profile), and
    warm cloud depths of 13,000-14,000 feet should foster very
    efficient warm rain processes with 2-2.5"/hr max rainfall rates --
    although sub-hourly rates could be even higher on the storm scale
    with cell mergers.=20

    As storms expand in coverage this afternoon, the parallel
    orientation of the forcing to the steering flow should favor
    repeating and merging of cells, prompting isolated to scattered
    flash flooding across the area. Both the 12z HREF and REFS
    neighborhood probabilities highlight a moderately-high likelihood
    (35-50%) of 1-3 HR FFG exceedance as this activity matures through
    0z, with the centroid generally located over East-Central KY.
    However, even outside of this area, saturated soils per NASA SPoRT
    and reduced FFGs (.75-2"/hr) suggest isolated to scattered flash
    flooding is likely with scattered rainfall of 2-3" expected across
    the area.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4S0bhzzfycvCRr0UZjzQdZXOG2f9LbiaohCD2fdO05_DdC0KaJUJm4FWOwbn9TYxsPhF= MCg766BlaZyWaIKRqaKowNs$ for graphic product...

    ATTN...WFO...HUN...ILN...IND...JKL...LMK...MEG...MRX...OHX... PAH...PBZ...RLX...

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 40058326 39968210 39178139 38138152 37388241=20
    36808360 35938497 35128554 34578627 34478786=20
    35168888 36178899 38068702 39378505=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 17 18:35:51 2025
    AWUS01 KWNH 171835
    FFGMPD
    OKZ000-KSZ000-180015-

    Mesoscale Precipitation Discussion 0470
    NWS Weather Prediction Center College Park MD
    235 PM EDT Tue Jun 17 2025

    Areas affected...Southern Kansas...Adj. Far Northern Oklahoma...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 171835Z - 180015Z

    SUMMARY...Current training band of elevated cells likely to give
    way to stronger, slightly more progressive convective development
    further southwest that will track through areas saturated
    overnight resulting in 2-3" totals and possible flash flooding.

    DISCUSSION...In the wake of this morning's MCS, the overall flow
    field is muddled and trying to refocus on rapid surface to low
    level cyclogenesis across SW Kansas into the TX/OK Panhandles,
    with very strong backed surface to 850mb flow across much of
    western OK into south-central SW KS. However, from about
    800-700mb solid south to southwesterly flow at 30-40kts becomes
    strongly confluent/convergent along the former rear-inflow jet
    (arrow to the bow) of the dying MCS. Modified 12z soundings
    suggest modest remaining mid-level lapse rates to support MUCAPE
    of 1000-1500 J/kg for those convective cells. CIRA LPW shows a
    narrow band of enhanced moisture in the 850-700mb layer to suggest
    moisture flux is also supportive of efficient rainfall
    production/moisture loading for rates of 1.5-2"/hr (given deep
    layer TPW is over 1.75, and saturated in the sub-cloud layer to
    limit evaporative loss).

    Currently, favorable orientation of flow from 700-400mb is
    parallel to the CAPE gradient and convergence axis to support some
    slow eastward propagation for repeating/training; though trends in
    WV and Visible animations (along with VWP) suggests this will
    remain in the very short-term (about 1-2 hrs) as digging
    outflow/roll cloud further west is starting to become more
    orthogonal in the 925-850mb layer. 17z WoFS run suggests 1.5-3"
    totals along the training axis, utilizing the 50th-90th
    percentiles, which appears reasonable. Though daily totals are
    already over 5" per backyard obs in McPherson, KS.

    Additionally, the dry line appears to be bulging northeastward
    into NW OK further strengthening low level moisture convergence
    along the enhanced instability axis along the KS/OK boarder with
    MLCAPEs nearing 3000 J/kg (through still strongly capped). As
    such additional development on this roll cloud/convergence band
    will allow for additional development southwest of the mid-level
    rear-inflow band in central to eastern KS. Eventually, these
    stronger/broader rotating updrafts having increased moisture
    convergence to support 2-2.5"/hr rates (along with larger
    hail...see SPC MCDs for additional details) toward 23-00z and in
    proximity to the heavy rainfall axis from last evening's MCS
    generally near/along I-135/35. Similarly WoFS totals of 1-3" are
    possible quickly across south-central KS into the eastern Flint
    Hills by 00z, which is agreeable with the HRRR and at least the axis/evolutionary path of the RRFS, providing some additional
    confidence.=20

    All considering, local totals of 3" in 2-3hrs may lead to possible
    localized flash flooding, though if intersecting with Wichita
    metro; potential significantly increases given expected 2"+ rates.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7ieIGhXItnM0_1E3AiiepZWI1jZd34gTUqftVwm-TQx9MWhnC8VhBS0QVqQWGWKG55-r= wGCU3La_p4WesGjNIg3w6bc$ for graphic product...

    ATTN...WFO...DDC...ICT...OUN...SGF...TOP...TSA...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 38709779 38469636 37809488 36949467 36619510=20
    36599612 36689740 36879858 37029937 37369992=20
    37849986 38459873=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 17 19:17:55 2025
    AWUS01 KWNH 171917
    FFGMPD
    GAZ000-ALZ000-MSZ000-180030-

    Mesoscale Precipitation Discussion 0471
    NWS Weather Prediction Center College Park MD
    317 PM EDT Tue Jun 17 2025

    Areas affected...Southeast MS...Alabama...Northwest GA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 171915Z - 180030Z

    SUMMARY...Weakly organized convective cells congealing with
    potential for some localized repeating/mergers capable of 2"+/hr
    rates and localized totals 2-3" in about 3hrs may result in focus
    rapid inundation, particularly near urban centers.

    DISCUSSION...GOES-E WV suite shows the very slow moving and narrow
    positively tilted mid-level trough across the MS into TN/Lower
    Ohio Valleys. Embedded within are two meso-scale shortwave
    features that are directing/corralling convective activity into
    weakly organized linear features. The lead wave in southern
    Middle TN extends some wrap around southwesterly flow to bow out
    the deeper layer confluence zone eastward across N AL before it
    angles back southwest across west-central AL and southern MS
    toward the weaker trailing/tail-end wave near SW MS/NE LA. Deep
    layer moisture is well above average with values of 2-2.25"
    along/ahead of the deeper layer axis. Traditionally summer like
    temperatures in the mid 80s over lower to middle 70s Tds support
    ample CAPE over 2000 J/kg for stronger updrafts. Aloft, there is
    modest divergence along the eastern right entrance to the jet,
    especially given that it is also moderately anticyclonically
    arched for broad scale divergence to allow for modest outflow for
    a few up/downdraft cycles to help feed moisture flux into the
    increasingly confluent band of convection. Effective bulk shear
    values are 20-25kts to show some weak organization for linear
    features or propagation through outflow boundary/low level convergence/collisions with other outflows.

    Still, the overall 10.3um EIR loop and RADAR mosaic shows an
    overall broad coverage of these cells capable of short-term bursts
    of up to 2"/hr. This is particularly evident from Clarke, MS to
    Hale county, AL with a bit of deep layer steering for increased
    duration as cells have a few extra minutes of repeating/training
    given the north-northeast cell motion along the same oriented
    confluence axis. Additional incidents are probable to occur with
    time further north and east as the overall trof slowly slips
    eastward overall. Hydrologically, the rates up to 2"/hr are
    problematic across central AL into NW GA where 1hr FFG are at or
    below those rates. These cells are likely to cross larger urban
    centers with hydrophobic ground conditions that could be quickly
    overwhelmed by the short-term magnitude of heavy rainfall, but
    otherwise incidents of flash flooding are likely to be widely
    scattered an narrow in areal coverage/focus through the evening
    across the area of concern.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4n8NtknnqtpJcEOs-HGenrAnsOsx0lM-cwDHR_rN0AHqducfSoHRzHJ2mtHgwWi73BMj= bnCXOCe9WGgLq3HPT6SlFoA$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...JAN...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34958456 34758385 33548471 32548630 31618760=20
    31268835 31048917 31268998 31988999 33168892=20
    33658826 34288791 34408670 34868581=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 17 19:52:25 2025
    AWUS01 KWNH 171950
    FFGMPD
    ARZ000-180100-

    Mesoscale Precipitation Discussion 0472
    NWS Weather Prediction Center College Park MD
    350 PM EDT Tue Jun 17 2025

    Areas affected...Central Arkansas...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 171950Z - 180100Z

    SUMMARY...Slow moving cells capable of 2"/hr crossing recently
    saturated ground conditions and lowered FFG values, suggest
    possible re-aggravation of localized flooding conditions over the
    next few hours.

    DISCUSSION...GOES-E Vis/EIR and KLZK RADAR have shown recent
    development across the Ouachita Mountains through central AR.=20
    Surface, VWP observations and RAP analysis show a narrow but very
    unstable axis in the wake of the mid to upper-level trough that
    has crossed the Lower MS River and the approach of the old MCV
    from this morning's MCS across KS; where full insolation resulted
    in upper 80s Temps over mid to upper 70s Tds and along a subtle
    WNW to ESE return moisture axis from surface to 700mb per CIRA
    LPW. Air is very unstable within the axis with MLCAPEs over 3000
    J/kg. VWP and Visbible Cu streamers suggest 20kts of orthogonal
    warm air advection across this moisture axis providing convergence
    and weak isentropic gradient for ascent. As such, moisture flux
    of this high low level moisture (over 1.75") suggests efficient
    rainfall production.=20

    Given the strength of updrafts and orthogonal/unobstructed
    WAA/moisture flux, rainfall production of 2-2.5"/hr will remain
    possible with some weak DPVA to help maintain the strength of the
    southwesterly low level inflow for a few more hours as the MCV
    passes. Deep layer steering in the wake of the trough also
    supports movement perpendicular to the inflow/convergence axis to
    allow for possible repeating. However, with that stated, Hi-Res
    CAMs are very insistent in weakening environment and overall tops
    are warming and erroding (especially further east near the greater
    stability from early morning convection/overturning (temps in the
    upper 70s). Still, the placement of this convection is
    unfortunately aligned with an area that recently received heavy rainfall/flooding and FFG values remain depressed and prone to
    exceedance given 1hr values less than 2" and 3hr values less than
    2.5". Given this a spot or two of flash flooding is considered
    possible over the next few hours.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_WERQ3ZS2Han4lQHEVZ_iph58pKL7H2dw8lCMfI3pmCmJBxAPLbddOWM7cBRUOao3blP= zaJDDG2YX8oTdSYJ4zrgO4c$ for graphic product...

    ATTN...WFO...LZK...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 35139301 34949213 34719154 34359125 34029123=20
    33789138 33689186 33849268 34219353 34449393=20
    34829415 35129393=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 17 20:41:53 2025
    AWUS01 KWNH 172041
    FFGMPD
    MNZ000-IAZ000-NEZ000-SDZ000-180200-

    Mesoscale Precipitation Discussion 0473
    NWS Weather Prediction Center College Park MD
    441 PM EDT Tue Jun 17 2025

    Areas affected...Northwest IA...Northeast NEB...Far Southeast
    SDAK...Far Southwest MN...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 172040Z - 180200Z

    SUMMARY...Very slow/stationary cells along/north of deeper layer
    upper-low with favorable outflow to maintain cells. However,
    limited instability/moisture may limit overall coverage to be
    widely scattered, but highly focused with localized spots of 2-3"
    and flash flooding possible.

    DISCUSSION...GOES-E WV suite shows the core of the large
    scale/global trough is slowly shifting eastward across central to
    eastern NEB with and old smaller scale MCV preceding it across
    central IA. Developing convection along/north has very
    long/narrow anvils with cirrus tails expanding well downstream
    indicative of the very favorable right entrance divergence to the expanding/accelerating jet 90kt 3H jet over the eastern Dakotas
    into northern MN. Additionally, those larger mid-level waves
    produced extensive clouds across southeast NEB and central IA
    inhibiting solar heating this afternoon and sharpening the
    differential heating boundary and keeping instability generally
    through the Missouri River Valley an back toward the NEB
    Sandhills. Remaining pockets of 1500-2000 J/kg of MLCAPE will
    provide solid updraft strength for scattered coverage across the
    area of concern.=20

    Low level flow continues to provide some weak southerly moisture
    advection into the deeper layer deformation zone/axis across NW IA
    where Total PWat values are a modest 1.5" though convergence/flux
    will help to provide that boost for solid rainfall production at
    about 1.75"/hr. Given slow cell motions, some locations have
    already experienced over 3" resulting in localized flash flooding
    along the SDAK/IA state line. Weak cold pools are helping with
    some cell motions, weakly propagating southward into the 15-20kts
    of inflow and toward remaining pockets of instability. As such,
    further expansion of 2-3" areal coverage is possible to expand
    flooding conditions, particularly south into the flow and eastward
    along the deformation zone north of the MCV. As such, localized
    flash flooding remains possible this evening until instability is
    fully exhausted.

    Note: Similar evolution/cell development is occurring west across
    the Sand Hills, given very high FFG values and infiltration
    capability, have only expanded the western edge of the MPD area to
    the eastern edge these sandy soil areas.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5yRnPWNCZEoumjmpQaLQaFas1GSl_37ozpOAEWWRl3pVLfVbhGpsji75-b6Ll9vracIk= MBbCo7QiEUbfEObexERcYFM$ for graphic product...

    ATTN...WFO...DMX...FSD...MPX...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43699395 43629339 43349306 42959319 42709343=20
    42259417 41889497 41439602 41439694 42539797=20
    43399805 43639641=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 17 22:30:28 2025
    AWUS01 KWNH 172230
    FFGMPD
    PAZ000-MDZ000-VAZ000-DCZ000-WVZ000-OHZ000-KYZ000-180430-

    Mesoscale Precipitation Discussion 0474
    NWS Weather Prediction Center College Park MD
    629 PM EDT Tue Jun 17 2025

    Areas affected...Western/Central PA...Western/Central
    MD...DC...Southeast OH...WV...Western VA...Eastern KY...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 172230Z - 180430Z

    SUMMARY...Slow moving clusters of intense deep warm cloud rainfall
    production across saturated and steep terrain likely to see
    additional flash flooding incidents through early overnight
    period.

    DISCUSSION...22z surface analysis shows a slowing of the eastward
    advancement of the warm front across the Allegheny Plateau in
    Northern PA but better erosion of the low level stratus across
    central MD into south-central PA. However, with weak surface wave
    pressing east of the Appalachian Continental Divide, surface to
    boundary layer winds have increases along front int MD and
    northern VA resulting in dual moisture flux stream into the
    eastern portion of MPD area. Strong cluster near Fulton county,
    PA is likely to slow with the forward advancement of the front,
    but with solid upstream moisture flux streaming out of the Ohio
    Valley and then eastward, continued back-building upstream
    redevelopment environment will further expand the potential for
    intense rainfall. Total PWats over 2" are analyzed though both
    lower elevations but even with losing some vertical depth, values
    over 1.75" across much of the area of concern with maintained
    20-25kts of inflow and sufficient surface theta-E to keep
    saturated mid-level lapse rates still unstable with narrow skinny
    CAPE profiles should result in continued very efficient rainfall
    production with 2"/hr rates in the strongest cores.=20

    Aloft, solid right entrance divergence into 50-60kt jet over NY
    into New England will likely keep upslope strong though also
    support greater forward propagation of cells across SE OH, WV into
    W PA, but streaks of quick 1.5-2" in the rugged terrain is likely
    to result in localized flash flooding through the overnight.=20
    However, there is a sharpening SW to NE line of mid-level
    suppression north of the jet axis currently seen from just off
    Lake Erie in NE OH back toward NW OH/central IND. This is
    pressing southeastward with northern stream height-falls...and
    will likely further corral warm-cloud showers for better repeating
    potential across SE OH/WV as well. Recent Hi-Res CAMs including
    HRRR, RRFS and 19,20,21z WoFS strongly suggest best potential
    remains across SW to south-central PA with even some higher
    probabilities of locally exceeding an additional 3" inches in
    places. This may result in a possible incident or two of significant/considerable flash flooding, within the broader area
    of scattered likely flash flooding incidents.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6FL4VG3Y_yRnJpnDnNsFAG5SpxF6r675wqVQzhRLY-sWr0ZfcrL2sn-hGpccGijXGSwv= xxPJiOfEYVhtTa8j-s_GnvM$ for graphic product...

    ATTN...WFO...CTP...JKL...LWX...MRX...PBZ...PHI...RLX...RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 41627873 41417706 40837614 40227577 39747597=20
    39127655 38557764 38167860 37487991 37338024=20
    36818188 36688288 36748415 37258437 38388288=20
    38718261 39238223 40668093 40898047 41517953=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 18 00:17:56 2025
    AWUS01 KWNH 180017
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-180600-

    Mesoscale Precipitation Discussion 0475
    NWS Weather Prediction Center College Park MD
    817 PM EDT Tue Jun 17 2025

    Areas affected...Southeast KS...Northern OK...Far Southwest
    MO...Ext Northwest AR...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 180015Z - 180600Z

    SUMMARY...Strong, slow moving pre-frontal super-cells will grow
    upscale while upstream redevelopment on the main front will
    provide a secondary wave of intense rainfall likely to support a
    broad area of 2-3" with embedded spots of 6"+ likely resulting in
    flash flooding conditions through early overnight period.

    DISCUSSION...GOES-E WV suite depicts multiple smaller scale
    convective clusters and shortwave features within the broad
    cyclonic global trough the expands the breadth of the Northern and
    Central Plains. The main wave is lifting northeast across
    southern NEB and was the main driver of last evening's/this
    morning's MCS that saturated central and southern KS. In the wake
    a strong surface to 850mb cyclone has been evolving across the
    Texas Panhandle with well defined warm conveyor belt wrapping very
    deep moisture with strong advection across OK into southern KS
    pooling 1.75 to near 2" total PWats along the KS/OK boarder. With
    stronger EML mixing/bulging northeastward across SW OK, winds have
    backed more southerly and have interacted with leading outflow
    boundary from this afternoon's activity across south-central KS.=20
    A few large/broad updrafts continue to slowly advance across
    Sumner/Cowley into expanding into Bulter county. Cells are being
    fed by very unstable (4000+ J/kg MLCAPE) from northeast OK. WoFS
    5-min and HRRR 15 minute along with observations denote the strong
    moisture flux is support rates over 2.5"/hr with .5-.7" in 5
    minutes and 1.5"/15 minutes forecast from each model respectively.
    Steering flow is generally weak as secondary shortwave feature
    that has been convectively enhance is digging southeastward out of
    the Colorado High Plains. This will allow for clusters to further
    grow upscale while providing sufficient residency for 2-3"/hr
    totals within the cores. Strengthening LLJ may aid some
    southeastward propagation into the northern row(s) of Oklahoma.=20

    Additionally, the backed low level flow will have sufficient
    instability to develop another round of activity along the front
    as seen up toward the heavy rainfall axis across McPherson,
    Ellsworth counties, likely to build westward along the front in SW
    Kansas. Height-falls and surface outflow will support increased
    forward propagation mainly after 02-03z, adding an additional 1-2"
    totals and broadening the areal coverage of 2-3" totals across
    south-central KS, expanding into northern OK. Where the two
    clusters overlap likely near Osage, Kay, Sumner, Cowley, and
    Chautaqua county, there is increasing confidence in localized
    totals of 3-6" through 06z. WoFS signals have been very
    consistent run to run with the mean increasing to near 4-4.5"
    while the 90th percentile is becoming focused toward 7" maxima,
    while other rapid refresh guidance and Hi-Res CAMs are within that
    similar total range. As such, flash flooding is likely to occur
    across a large portion of the area of concern as the convective
    lines combine through the overnight period, while a few areas
    could see considerable to significant flash flooding conditions.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8WX__uF2ewsLZjX2-dICjNx3iwtkMmOq8PB3ivbpw60Gfpc24UpVy93-0e8eAEGCJQo4= XpSUNrjQHxUrHJ2Td61bNeY$ for graphic product...

    ATTN...WFO...DDC...EAX...ICT...OUN...SGF...TOP...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 38959749 38569555 38119445 37489376 36759371=20
    36129430 35749526 35609677 35819850 36219994=20
    36979943 37579881 38599879=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 18 06:18:28 2025
    AWUS01 KWNH 180618
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-181115-

    Mesoscale Precipitation Discussion 0476
    NWS Weather Prediction Center College Park MD
    217 AM EDT Wed Jun 18 2025

    Areas affected...much of OK into adjacent portions of far
    southeast KS, southwest MO, and northwest AR

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 180615Z - 181115Z

    Summary...Backbuilding convection may continue to train from
    west-to-east with localized hourly accumulations of 1.5-2.5".
    Isolated to scattered instances of flash flooding are possible.

    Discussion...A mature mesoscale convective system (MCS) with an
    impressive bow echo has made rapid eastward progress across
    northern OK over the past several hours, and more recently (over
    the past couple of hours) elevated convection rapidly initiated
    and proliferated in the vicinity of the rear inflow jet (RIJ). The
    west-east orientation of the elevated convection neatly resembles
    a "bow and arrow" mesoscale convective structure, as a strong
    low-level jet (LLJ) from the south is resulting in strong moisture transport/isentropic upglide (most prominently around the 925 mb
    isobaric surface and the 305K isentropic surface) over prominent
    cold pool resulting from the MCS (and aided by low-level
    frontogenesis with the close proximity of a front). The "bow and
    arrow" conceptual model favors an increasing flash flood threat,
    given the tendency with the lagging "arrow" convection to train
    from west-to-east (as convection is nearly parallel to both the
    850-300 mb mean flow, as well as the forward propagating Corfidi
    vectors). Should convection continue to backbuild, this could
    present a significant flash flood risk (with training cells
    producing localized hourly accumulations of 1.5-2.5", per MRMS
    estimates). Over the past hour or so, trailing convection has
    started to show a tendency of southward propagation (upwind into
    the LLJ, matching the associated Corfidi vectors quite closely),
    which may limit the flash flood threat somewhat (though this will
    eventually bring the trailing convection into the more populated
    OKC metro, additional backbuilding and a cessation of upwind
    propagation could ultimately be more problematic with regard to
    impactful flash flooding). In addition, convection may locally
    have a tendency to train along the north bookend vortex of the bow
    (near the OK/KS/MO border region), which has recently result in
    hourly totals to 2.0".

    Hi-res models have underestimated the intensity and scale of the
    backbuilding convection (as they tend to do with convection that
    is elevated in nature) across the 00z HREF suite, and hourly runs
    of the HRRR and experimental RRFS have not done much better. The
    HREF PMM QPF indicates the potential for localized 2-4" over
    east-central OK, and it seems reasonable to shift these totals and
    resulting post-processed exceedance probabilities (15-25% for 3"
    exceedance per 40-km neighborhood method) westward (based on the
    aforementioned observational trends). Convection may continue to
    backbuild for longer than expected in this environment with a
    large reservoir of 2000-3000 J/kg of MUCAPE (max 2-6 km AGL layer
    lapse rates of 8.0-8.5 degC/km) and impressive deep layer (0-6 km)
    shear of 40-50 kts. Precipitable water values are indicated to be
    1.7-2.0 inches (near the max moving average/record levels, per OUN
    sounding climatology). Isolated to scattered instances of flash
    flooding are considered possible (and may locally be significant,
    particularly if storms backbuild and train across the more
    populated core of central OK).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8yPPjHD9RtQWNUpZ8ILdNIXQk14QvZKD0t42GIDzFURtOOihOOK_zuIgoHCsvnK1GRiF= b1vbHj5wUiRMnC55Sv-JpRE$ for graphic product...

    ATTN...WFO...ICT...OUN...SGF...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 37739456 37259388 36609363 35939372 35149440=20
    34859536 34809712 35059853 35919931 36329939=20
    36479892 36569838 36519649 36889576 37539542=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 18 16:58:38 2025
    AWUS01 KWNH 181657
    FFGMPD
    NYZ000-NJZ000-PAZ000-MDZ000-VAZ000-DCZ000-WVZ000-182256-

    Mesoscale Precipitation Discussion 0477
    NWS Weather Prediction Center College Park MD
    1256 PM EDT Wed Jun 18 2025

    Areas affected...Eastern OH Valley...Northern Mid
    Atlantic...Interior Northeast

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 181656Z - 182256Z

    Summary...Shallow thunderstorms are gradually expanding in
    coverage and intensity across the Eastern OH Valley, Northern
    Mid-Atlantic, and Interior Northeast. Periods of repeating cells
    containing 1.5 to locally 2"/hr rainfall rates could support
    additional isolated flash flooding this afternoon in light of
    recent heavy rainfall in the region.

    Discussion...Day Cloud Phase RGB and LightningCast data suggest
    shallow thunderstorms across the Eastern OH Valley, Northern
    Mid-Atlantic, and Interior Northeast are intensifying as an
    extremely moist airmass destabilizes beneath eroding low-level
    clouds. The most persistent cells were initially roughly along
    I-80 in Western PA, which prompted several Flash Flood Warnings as
    they repeated over an area impacted yesterday and realized
    1.5-1.8"/hr rainfall rates per KCCX. Additional flooding was also
    noted near Buffalo, NY as an axis of cells stalled and trained
    overhead.

    As highlighted in the 12Z soundings from PIT and IAD, the airmass
    across the region remains very supportive for efficient warm rain
    production in these cells, with saturated profiles containing
    1.7-2.1" PWATs, 1000-2000 J/KG of MUCAPE, and warm cloud layers of 13,000-14,000 feet noted. Sufficient shear remains as well to
    support at least loosely organized multicellular storm modes, with
    20-35 kts depicted in recent mesoanalysis.

    Over the next several hours, a general trend of expanding
    multicells is expected as a weak shortwave over Western OH
    approaches from the west amid continued surface heating. Westerly
    steering flow should permit for periods of repeating cells,
    although storm coverage should remain more scattered compared to
    yesterday's event. As instability builds and additional cells
    form, both the HREF and REFS neighborhood probabilities show an
    increasing likelihood of at least 1"/hr rates and 1-3 HR FFG
    exceedance beginning around the 17-18z time frame. With FFGs in
    the region as low as .25-1.5", additional isolated flash flooding
    is possible as these cells expand and periodically repeat.

    Asherman=20=20

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6uRcE_EgBXsLRi5pJ0sbzuWgV4XEYN7K2asNVaGFLKdKlAqkR5vEYo0cyJ488jl06vw3= a70HyzBBPh5lllBNkrsXG7o$ for graphic product...

    ATTN...WFO...BGM...BUF...CLE...CTP...LWX...PBZ...PHI...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 42617863 42507757 41357647 40507484 39587600=20
    38627691 38617789 39237850 39597895 40118005=20
    40778037 41508026 42247970=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 18 18:02:04 2025
    AWUS01 KWNH 181802
    FFGMPD
    MIZ000-INZ000-WIZ000-ILZ000-190000-

    Mesoscale Precipitation Discussion 0478
    NWS Weather Prediction Center College Park MD
    201 PM EDT Wed Jun 18 2025

    Areas affected...Northeast IL (including the Chicago
    Metro)...Southwest MI

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 181800Z - 190000Z

    Summary...Intense convective complex is translating through IL.
    Scattered flash flooding -- some of which could be locally
    significant in/near the Chicago metro -- is possible this
    afternoon.

    Discussion...Intense convective complex continues to track across
    Central IL ahead of a well defined MCV located northeast of St.
    Louis. The leading corridor of cells was along a NW-SE axis, and
    generally forward propagating to the northeast at around 30-40
    kts, with an area of showers and thunderstorms wrapping around the
    northwest of the MCV, upstream of the forward propagating
    activity. Max rainfall rates within this complex were generally on
    the order of 1.5"/hr.

    Recent mesoanalysis and GPS data suggest a very moist and unstable
    airmass is advecting ahead of the complex, with 1.7-1.9" PWATS and
    3000-4500 J/kg of MLCAPE depicted in the pre-convective
    environment. Recent GOES-E DMW also placed the right entrance
    region of a jet streak over Lake Michigan and Wisconsin to further
    enhance forcing for ascent ahead of the MCV. As this complex
    translates northeastward within 40-50 kts of effective shear,
    multiple rounds of precipitation are possible in the MPD area from
    1) individual cells within the right entrance region of the jet
    streak, 2) along the leading edge of the forward propagating
    component and 3) beneath the northwest flank of the MCV.

    Over the next several hours, the HREF suggests increasing
    probabilities of 2"/hr rainfall rates as this repeating of
    precipitations occurs. Accordingly, scattered flash flooding may
    result with the HREF suggesting localized rainfall amounts of 2-4"
    may fall where these three rounds of precipitation can overlap.
    Localized significant flash flooding is possible in sensitive
    urbanized areas, including the Chicago metro.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_c3e9VqL6mdILTB0ccabE5kAdG9q2pzWJbWhDN8NMGVaFDbWGdLWh7lhddzJNCHTKwSK= XrJYzXylCmQoRpnUeG8TvWY$ for graphic product...

    ATTN...WFO...DVN...GRR...ILX...IWX...LOT...MKX...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 43698684 43628491 41858506 40788753 40498960=20
    41379028 43198864=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 18 20:35:22 2025
    AWUS01 KWNH 182035
    FFGMPD
    NYZ000-PAZ000-OHZ000-190200-

    Mesoscale Precipitation Discussion 0479
    NWS Weather Prediction Center College Park MD
    434 PM EDT Wed Jun 18 2025

    Areas affected...Western NY...Northwest PA...Extreme Northeast OH

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 182035Z - 190200Z

    SUMMARY...Flash flooding likely to continue as shortwave
    approaches helping to expand convective coverage which will remain
    slow moving and very efficient with 1.5-2"/hr rates and localized
    totals to 3"+.

    DISCUSSION...While the symmetric, mature main upper-low near
    southern Lake Michigan dominates the GOES-E WV suite, there
    remains a more subtle but similarly impactful compact wave
    crossing central Lake Erie currently. This wave is providing
    solid DPVA and enhanced west-southwesterly 20-25kts of inflow
    while corralling highly anomalous sub-tropical moisture across the
    Lower Great Lakes. A well defined surface front exists north of
    the Lakes in the Ontario Peninsula and just north of the St.
    Lawrence river Valley, but the cold lakes have provided strong
    differential heating boundaries to help develop strong
    thunderstorms earlier this afternoon. Given this upstream wave,
    cells have been very slow moving to the northeast with overall
    best motions driven by propagation/redevelopment along outflow
    boundaries which have become numerous across the area of concern
    (please see graphic for some deliniation).

    Given the deep moisture over AoA 2" in Total PWat and deep warm
    cloud layers near 12-14Kft; efficient rainfall production has
    resulted in 2"/hr rates and numerous incidents of flash flooding.
    This trend is likely to maintain itself through the next 3-4 hours
    as outflows intersect seeking out remaining pockets of 2000 J/kg
    unstable air pockets. Inflow from the southwest and some weak
    isallobaric response has limited cell motions and with broader
    slabs of ascent with merging boundaries/broader updrafts similar
    1.5-2"/hr rates are likely to expand and perhaps intersect/overlap
    with initial burst resulting in some localized totals to 3"+
    further inducing other localized incidents of flash flooding
    (especially in urban centers).

    As the evening progresses, stronger convergence along the
    shortwave trough axis now nearing the PA/OH state line, will act
    as final bout merging and sweeping up the remaining active
    convection. Simple mergers may further enhance sub-hourly rates.
    As such, scattered to numerous incidents of focused/localized
    flash flooding are considered likely through exhaustion of
    instability and/or shortwave moves through from west to east.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6EH5Ic01KSZo8ndipk2DzepOHfl6LQgQ7QlgDXImhodUE5V0FdxSiNqp-Q9TU8Ir8Pzj= ujENHkb-Ylopuv45dV0U1bY$ for graphic product...

    ATTN...WFO...BGM...BUF...CLE...CTP...PBZ...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 43617639 43217584 42617587 41987662 41567726=20
    41167831 40957936 40858030 41088068 41858061=20
    42447964 42897909 43387893 43407700=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 18 23:16:58 2025
    AWUS01 KWNH 182316
    FFGMPD
    WVZ000-OHZ000-TNZ000-KYZ000-INZ000-190430-

    Mesoscale Precipitation Discussion 0480
    NWS Weather Prediction Center College Park MD
    716 PM EDT Wed Jun 18 2025

    Areas affected...Southern OH...Central KY...Middle TN...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 182315Z - 190430Z

    SUMMARY...Increasing convective coverage capable of locally
    exceeding lower than normal hourly FFG due to well above normal
    soil saturation. Hourly 1-2" totals and some possible short-term
    storm scale interactions may allow for some isolated totals over
    2-3", resulting in widely scattered low-end incidents of flash
    flooding through early overnight period.

    DISCUSSION...RADAR mosaic depicts a mature, strong but very
    progressive squall line crossing eastern IND into OH. This line
    has been fairly consistent in producing .5-1.25" totals along its
    path through IND; however, this has not intersected areas of
    recent saturation until moving into southwest/southern Ohio.=20
    Here, 0-40cm relative soil saturation ratios are at or above 60%
    which is well into the 90th to 99th percentile per NASA SPoRT LIS
    products and this is more so south across much of KY into western
    and Middle TN.=20

    However, stronger surface to boundary layer convergence was
    slightly weaker and could not break the cap across much of the
    pre-frontal pressure trof/convergence boundary. Air remains very
    unstable with MLCAPE of 2500-3000 J/kg from Cincinnati across into
    Western TN. Ample moisture in the low to mid 70s (Tds) and total
    PWats of 1.75 to 1.9", suggest any thunderstorms to develop will
    have capability of producing 1.5-2"/hr rates. VWP and RAP
    analysis suggest as the MCV is lifting further north the winds had
    not been strong enough or have sufficient directional convergence;
    but recent trends suggest a slight increase in both wind speed as
    the LLJ diurnally strengthens and a slight increase of about 10-15
    degrees from 925-850mb has seen a steady southwestward expansion
    of the deep moisture convergence axis into western and middle TN.=20
    As such, individual cells have broken the cap through much of the
    line and continue to expand as they progress eastward.=20

    Further north into OH, stronger convergence/mature updrafts have
    been been outdone by forward speeds to result in hourly FFG
    exceedance, though as they reduce below 1.5" and forward
    progression reduces slightly further from the lifting
    shortwave/forcing increased duration suggests scattered incidents
    of exceedance are possible. Further south, deeper layer steering
    flow is a bit more west to east and slower by 5-10kts, also
    supporting increased duration. Stronger upstream LLJ/moisture
    convergence may also support flanking development within the storm
    scale environment to further increase overall duration. Similarly
    though, hourly rates of 1.5-2" are likely along the line with
    sub-hourly totals expected to be at or slightly above scattered
    along the line. As such, low-end flash flooding incidents are
    becoming increasingly possible through the late evening/early
    overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7OFUDBMGYjpw1V5tOuJZB-o5oYR3qQA9T73TnoqN69omVoVQ73dbVrDktZFeHaHUH4_t= dUfr4JMRYa4WRTZ_zJtw2WA$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...MEG...OHX...PAH...RLX...

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 39948284 39728209 39078151 38158205 37428310=20
    36678472 35418817 36328892 37788688 38748549=20
    39238484 39838404=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 19 05:11:15 2025
    AWUS01 KWNH 190511
    FFGMPD
    TNZ000-KYZ000-ALZ000-ILZ000-MSZ000-MOZ000-ARZ000-191030-

    Mesoscale Precipitation Discussion 0481
    NWS Weather Prediction Center College Park MD
    110 AM EDT Thu Jun 19 2025

    Areas affected...Central/Eastern AR...Central/Western
    TN...Southwest KY

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 190510Z - 191030Z

    SUMMARY...Some expansion of heavy shower and thunderstorm activity
    is expected over the next few hours. Some cell-training concerns
    are expected, and with high rainfall rates, some isolated areas of
    flash flooding will be possible.

    DISCUSSION...GOES-E WV suite shows a digging shortwave trough
    across the Midwest, with the leading edge of height falls
    impinging on the lower/middle MS Valley. This energy is beginning
    to interact with a strong instability gradient that is in place
    across central/eastern AR, western TN and parts of southwest KY.
    MLCAPE values are on the order of 1500 to 2500 J/kg locally, and
    despite the negative influence of boundary layer CIN, recent IR
    satellite imagery shows cooling convective tops becoming better
    established across eastern AR and into far western TN.

    A modest southwest low-level jet currently oriented across the
    region is expected to strengthen and become more convergent over
    the next few hours and reach 30 to 40+ kts. This will strengthen
    the moisture transport across the area, but will also foster
    stronger low-level forcing into an area that is already unstable.

    A combination of these factors will support some expansion of the
    current convective activity, with heavy showers and thunderstorms
    also becoming a bit better aligned with the deeper layer mean flow
    which will support a cell-training threat. PWs are quite moist
    with values of 1.8 to 2.0 inches based on 00Z RAOB soundings and
    recent GPS-derived data. The CIRA-ALPW data shows a substantial
    level of moisture concentrated in the mid-levels of the column
    where much of the vertical ascent will be taking place.

    This suggests convection capable of high rainfall rates that may
    reach 1.5 to 2.5 inches/hour which is generally supported by the
    00Z HREF guidance. However, with the cell-training concerns, some
    storm totals by dawn may reach 3 to 4+ inches. The HREF guidance
    does show some low-end FFG exceedance probabilities, and thus the
    expectation is that some isolated areas of flash flooding will be
    possible.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6x3IJ-5nN7igBJDozH4IRYtGn08iky7e3IScL7prcbP_D_VoIzRoSIKCel1r5Bk8-U45= iuQXZhYPpLbcCDwcoK7oeuE$ for graphic product...

    ATTN...WFO...HUN...LMK...LZK...MEG...OHX...PAH...

    ATTN...RFC...ORN...TIR...TUA...NWC...

    LAT...LON 37368825 37328650 36598599 35558663 34808852=20
    34389048 34589252 35559271 36148994=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 19 10:01:52 2025
    AWUS01 KWNH 191001
    FFGMPD
    TNZ000-ALZ000-MSZ000-ARZ000-191500-

    Mesoscale Precipitation Discussion 0482
    NWS Weather Prediction Center College Park MD
    600 AM EDT Thu Jun 19 2025

    Areas affected...Eastern AR...Southwest TN...Northern
    MS...Northern AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 191000Z - 191500Z

    SUMMARY...A well-organized band of heavy showers and thunderstorms
    will continue to pose a threat for some additional flash flooding
    going through the mid-morning hours.

    DISCUSSION...Early morning GOES-E IR satellite imagery shows a
    west to east oriented axis of heavy showers and thunderstorms
    extending from northeast AR through much of southwest TN and with
    a portion of the line losing latitude and edging into northeast MS
    and northern AL.

    The cold-topped convection has been showing a considerable amount
    of cell-training over the last couple of hours across southwest TN
    as the activity becomes aligned with the deeper layer steering
    flow. All of the convection continues to be facilitated by the
    pooling of a very moist and unstable airmass that is in place
    ahead of a shortwave trough advancing east toward the OH Valley
    and Mid-South. MLCAPE values are rather impressive early this
    morning across central to eastern AR and into southwest TN with a
    corridor of 2000 to 3000 J/kg of CAPE aligned with a convergent
    west-southwest low-level jet of 30 to 40 kts.

    This coupled with at least some modest shear will likely maintain
    the convective organization of this linear MCS for at least a few
    more hours. PWs are quite moist with values of 1.8 to 2.0 inches
    based on recent GPS-derived data, and the depth of moisture
    coupled with the instability and strength of the low-level jet
    should maintain high rainfall rates that will likely be on the
    order of 1.5 to 2.5 inches/hour.

    The latest hires CAMs suggest some additional training of
    convection may occur through mid-morning with the activity also
    gradually settling farther south. This will allow for more areas
    of eastern AR, northern MS and northern AL to get into some
    heavier rainfall potential. In general across the Mid-South, an
    additional 3 to 4 inches of rain will be possible, and this will
    include southwest TN where there will be concerns for some of
    these rains to impact the Memphis metropolitan area.

    Given the additional rainfall potential over the next few hours,
    some additional areas of flash flooding will be possible.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!__PQZVAc7m9l3XPWmUpSgYvESl4pTxh8ooWX-8ct4JKYvaUA2uKKz4Cv0g1ib_joNPJn= g4WAPY4qldNF9nrONsOJV7I$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LZK...MEG...OHX...

    ATTN...RFC...ALR...ORN...TUA...NWC...

    LAT...LON 35609036 35538830 35008631 34088633 33638759=20
    33628946 33849109 34299214 35259212=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 19 15:21:50 2025
    AWUS01 KWNH 191521
    FFGMPD
    ALZ000-MSZ000-ARZ000-191850-

    Mesoscale Precipitation Discussion 0483
    NWS Weather Prediction Center College Park MD
    1121 AM EDT Thu Jun 19 2025

    Areas affected...Southeast AR...North-Central MS...Western AL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 191520Z - 191850Z

    Summary...Periods of training and repeating thunderstorms within a
    persistent MCS will maintain the threat of isolated flash flooding
    for at least the next three hours.

    Discussion...Regional radar highlights a persistent MCS containing
    a forward propagating component across Eastern MS and
    North-Central AL, with upwind development occurring further west
    along a slow moving cold pool. The alignment of these cells was
    leading to periods of repeating and training across the
    highlighted area, with 1.5-2.6"/hr rainfall rates estimated within
    the most intense cells over North-Central MS.

    The development of new cells upstream is likely tied to a
    confluent low-level regime in the upwind portion of the cold pool
    interacting with a very moist and unstable airmass characterized
    by 2500 J/kg of MLCAPE (and minimal CIN), 1.8-1.9" PWATs, and
    20-25 kts of effective shear to support new development of loosely
    organized cells capable of continued 1.5-2.5"/hr rates.=20=20=20=20
    Both the HREF and REFS suggest this training and repeating
    activity will continue for at the next three hours -- albeit with
    some uncertainty regarding the persistence owing to how CAMs have
    struggled with the cold pool. However, the HREF and REFS suggest
    localized amounts of 2-3 inches remain possible through 18z, which
    could locally breach FFGs in the region and cause isolated flash
    flooding.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5mFJOs-EveGwM4s_VAQ7n4yIwmDh1ab-i84SQ1MZp7fF9Sg21bRODP--wA9DlvNRKU2I= Or2tiZdo-e8JA9Tkzu1Re5g$ for graphic product...

    ATTN...WFO...BMX...JAN...LZK...MEG...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34649171 34338950 33968828 33218711 32458722=20
    32168815 32488964 33669159=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 19 18:11:04 2025
    AWUS01 KWNH 191809
    FFGMPD NYZ000-NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-NCZ000-DCZ000-WVZ000-OHZ000-TNZ00= 0-KYZ000-200008-

    Mesoscale Precipitation Discussion 0484
    NWS Weather Prediction Center College Park MD
    208 PM EDT Thu Jun 19 2025

    Areas affected...Central Appalachians..Interior Northeast

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 191808Z - 200008Z

    Summary...Expanding coverage of brief but intense thunderstorms
    with sub-hourly rainfall rates upwards of .50-1"/15 min could
    cause isolated to scattered flash flooding this afternoon.

    Discussion...Trends in visible satellite imagery area depict an
    increasingly unstable PBL interspersed with intensifying clusters
    of thunderstorms ahead an upper-trough and cold front over the OH
    Valley.

    While this activity organizes, a strengthening jet-streak over the
    Interior Northeast is forecast to enhance southwesterly low-level
    flow into the warm sector and yield 1.7-2" PWATs, 1000-3000 J/kg
    of MLCAPE, and 30-40 kts of effective bulk shear across the region
    over the next few hours. Accordingly, storms should intensify into
    multicell clusters and supercells containing .5-1"/15 minute rain
    rates embedded within linear segments along an ENE-SSW axis ahead
    of the lee-trough and cold front -- refer to SPC MCD 1364 for the
    latest on the severe threat with these storms.

    While the scattered nature of the storms and progressive storm
    motions should limit a prolonged flash flood threat, brief
    training and repeating of these intense rates could easily breach
    the low .25-1"/hr FFGs across the region. As such, the HREF and
    REFS denote increasing probabilities of 1-3 HR FFG exceedance
    beginning around 18-19z, which suggests an increasing risk of isolated-scattered flash flooding going forward today.

    Asherman=20

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Bdmotk_OzDU9y-IVlXOkYLaAYyrOO725xTqPhsSZYgycWLao7WHU6MKZnsv8wNSg7pF= dM0CuarfZl7okdQdRZCJAbI$ for graphic product...

    ATTN...WFO...AKQ...ALY...BGM...BUF...CLE...CTP...GSP...JKL... LWX...MRX...OKX...PBZ...PHI...RLX...RNK...

    ATTN...RFC...ALR...ORN...RHA...TAR...TIR...NWC...

    LAT...LON 42997866 42497621 42227396 40077489 38377691=20
    36827942 35888163 36708295 39308143 42058012=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 19 18:27:51 2025
    AWUS01 KWNH 191826
    FFGMPD
    MSZ000-LAZ000-ARZ000-200000-

    Mesoscale Precipitation Discussion 0485
    NWS Weather Prediction Center College Park MD
    226 PM EDT Thu Jun 19 2025

    Areas affected...Central Arkasas...West-central Mississippi...Far
    Northern Louisiana...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 191830Z - 200000Z

    SUMMARY...Delicate balance of weak inflow and convergence to
    maintain thunderstorms in a favorable slow/repeating steering
    environment. Fairly saturated upper-soils may result in increased
    runoff and possible localized incident(s) of flash flooding.

    DISCUSSION...Regional RADAR mosaic depicts the main core of the
    outflow boundary from this morning's MCS continue to accelerate
    southward across eastern MS/western AL as the core of the cold
    pool presses south-southeastward starting to break out new
    convection along its leading edge. Upstream, however, the affects
    of the cold pool are much less as the overall larger scale
    forcing/shortwave slides northeast across the upper-TN Valley.=20
    Yet, the tail end of the cold front is hanging around with weak
    northwesterly flow and drier air helping to tighten the theta-E
    gradient across E OK into central AR. Temperatures are nearing
    90F whil Tds are in the mid to upper 70s, with ample pooled
    850-700mb moisture noted in CIRA LPW along the intersection of the
    outflow boundary to the cold front along the MS River. CIRA LPW=20
    does note that mid-level drying has mixed in across the region and
    the combination of slightly steeper lapse rates in this region has
    bumped up MLCAPEs to 3000-3500 J/kg.=20=20

    The key will be prolonged/sufficient low level inflow/convergence
    to maintain convective development. Currently, VWP at LZK/SHV and
    boundary layer cu tracers suggest 15-20kts of
    confluent/convergence across central AR to help spark the initial
    convective development. RAP analysis of bulk shear suggests
    proximity of the mid-level flow is sufficient for 20-25kts to
    maintain weak organization and while right entrance divergence is
    best maximized downstream across the convective cores east of the
    MS River, there should be enough tilt to allow for a few updraft
    cycles.=20

    As noted, total PWat values are AoA 2" with the weak inflow
    suggest solid moisture loading for 1.75-2"/hr rates, but updrafts
    may still be fairly narrow. However, with expected 10-15kts of
    upstream confluence flow into the boundary layer, convergence on
    outflows and deep layer steering along/just southeast of the
    frontal zone should allow for some repeating/training potential.
    Allowing for 2-3" localized totals. While FFG seems to have
    rebounded to normal/average values, the upper-soils remain fairly
    saturated at over 60% per NASA SPoRT LIS products which are well
    into the 90th percentile. This suggests, given the intensity of
    the rates, reduced infiltration and increased runoff potential.=20
    If the updrafts are broad enough, localized flash flooding is
    considered possible through the afternoon.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!73t4Php53iecAKRRi2iXTQBbsAIsJM_fLLQ2To9HVyuGtWM9kPQLPyAoyt_XpTnFFDxU= tI_NVvC2cfP_fD4ug76ZmWw$ for graphic product...

    ATTN...WFO...JAN...LZK...SHV...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 35059363 34839237 34409167 33469014 32818991=20
    32369058 33149241 33649331 34309422 34829424=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 19 19:22:47 2025
    AWUS01 KWNH 191920
    FFGMPD
    MEZ000-MAZ000-NHZ000-VTZ000-NYZ000-200100-

    Mesoscale Precipitation Discussion 0486
    NWS Weather Prediction Center College Park MD
    319 PM EDT Thu Jun 19 2025

    Areas affected...Interior New England...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 191920Z - 200100Z

    SUMMARY...Intense,efficient rainfall producing thunderstorms with
    capability of 1.5-2"/hr rates and some repeating further northeast
    into Maine, may result in localized 2-3" totals and possible
    incidents of flash flooding given complex/steep terrain.

    DISCUSSION...GOES-E WV suite shows a strong/fairly compact
    shortwave cyclone crossing the Lower Great Lakes with a broad jet
    streak across much of Quebec, resulting in favorable right
    entrance ascent downstream into Interior New England. RAP 500mb
    analysis shows a shortwave ridge axis through southern Quebec into
    VT and this seems to make a weak southern stream shortwave or
    remnant MCV-like feature matched with it. This wave seems to have
    supported a subtle 1001 wave along the stationary front near CWBW,
    and a weak surface trof appears within the Champlain Valley and
    seems to be a weak convergence zone that extends along the
    southern Adirondack Mtns into E NY. Surface Tds in the upper 60s,
    lower 70s expand across the area of concern toward a lifting warm
    front from CWHV to BNR to near Portland. Temperatures have risen
    to the mid to upper 80s across VT/N NH supporting MLCAPE rising
    into the 1000-1500 J/kg range. CIRA LPW and RAP analysis also
    confirms that moisture as pool along/downstream of this weak
    shortwave feature with total Pwats in the 1.75-2" range. The
    combination of factors suggest very heavy rainfall potential will
    exist with stronger updrafts crossing the area.

    Current RADAR shows steady increase along this convergence trof
    and though strongest convergence/moisture is north of the boarder,
    the potential for rainfall rates of 2"/hr are solid. The limiting
    factor to reaching those hourly totals will be duration and deep
    layer steering is fairly robust at 30-40kts. As updrafts broaden
    streaks of 1.5-2" totals are probable, though best probability for
    those totals remains in S Quebec near the low/frontal zone where
    convergence can be further maximized. However, eventually, those
    cells will cross back into northern Maine and if there are some
    repeating rounds (given upstream forcing remains strong, it seems
    possible), spots of 2-3" totals are possible.

    Irrespective of totals, the very intense quick burst of 1-1.5"
    across complex terrain (1hr FFG in 1.5-2" range) still should pose
    localized flash flooding risks...and any increase in duration due
    to storms scale interaction/terrain locking would obviously pose a
    greater risk, but given Hi-Res CAM solutions/evolution that
    evolution remains uncertain and lower confidence overall.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_pkZC73NZ8wjbZxFrOtyF5bTokhE-uYcfhblRfIpctdnqtNfbce4qGaUQ87dcxJUiA2r= ecgzNghach_tBzqWhF8gVi4$ for graphic product...

    ATTN...WFO...ALY...BTV...CAR...GYX...

    ATTN...RFC...TAR...NWC...

    LAT...LON 47456935 47446854 47216813 46426839 45846880=20
    44766973 44057114 42997229 42567369 42877469=20
    43487478 44287387 45077333 45077319 45177170=20
    45837075 46707025=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 20 00:30:54 2025
    AWUS01 KWNH 200030
    FFGMPD
    MEZ000-NHZ000-200600-

    Mesoscale Precipitation Discussion 0487
    NWS Weather Prediction Center College Park MD
    830 PM EDT Thu Jun 19 2025

    Areas affected...Northern Maine...Northern New Hampshire...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 200030Z - 200600Z

    SUMMARY...Strong squall line with up to 2"/hr rates with scattered
    upstream cells capable of repeating through areas affected
    initially. Localized totals to 2-3" by 06z, continuing risk for
    localized flash flooding into the early overnight period.

    DISCUSSION...RADAR starting to show squall line taking on more
    embedded bowing segments as the line reaches the lifting warm
    front across northern ME and the instability gradient. Subtle
    shortwave, weak height-falls driving the low level
    backed/convergent flow continues to lift northeast into the
    upriver portions of the St. Lawrence Seaway. As such, forward
    propagation speeds are starting to flatten the convective line
    allowing for increased heavy rainfall duration. Given total PWats
    still in the 1.75"+ range and ample remaining MLCAPE convective
    line is likely to maintain capability of 1.5-2"/hr rates and with
    increased duration of training, 1-2 hours may start to result in
    localized 2-3" totals along the band.

    While the deep layer moisture is exiting with the wave/drying
    slightly upstream, the LLJ is strengthening with winds increasing
    from 25-30kts toward 35kts, favoring upwind convergence. This may
    support flanking line/back-building development with time.
    Also, given the lingering west to east outflow boundary upstream
    is also orientating favorably for some increased orthogonal
    isentropic ascent in the upstream unstable airmass over NE NY into
    VT (as well as clusters in S Quebec near the surface boundary),
    will allow for additional development to potentially repeat across
    areas that have been recently saturated. As such, widely
    scattered/localized flash flooding remains possible through the
    early overnight period across Northern NH and ME.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7KRPftpJHxuycNIoO_CWAclCdjsqFHX5y2lpqMgEWzp3ZNCllrAM6bTII5bTJTiDsTKG= OuS7phihPTOMY_-shXw3LRY$ for graphic product...

    ATTN...WFO...CAR...GYX...

    ATTN...RFC...TAR...NWC...

    LAT...LON 46916783 45866769 45536779 45326825 44876933=20
    44457021 44287146 45027140 45357115 45567081=20
    46127039 46667004 46906933=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 21 02:03:51 2025
    AWUS01 KWNH 210202
    FFGMPD
    MIZ000-WIZ000-MNZ000-NDZ000-210800-

    Mesoscale Precipitation Discussion 0488
    NWS Weather Prediction Center College Park MD
    1001 PM EDT Fri Jun 20 2025

    Areas affected...eastern North Dakota, northern Minnesota,
    northwestern Wisconsin

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 210200Z - 210800Z

    Summary...Convection is expected to rapidly deepen and expand in
    coverage across the discussion area in the 03-08Z (10p-3a CDT)
    timeframe. These storms will exhibit mergers and localized
    training, with a risk of 2 inch/hr rain rates and a few areas of
    flash flooding.

    Discussion...Intense, deep convection has begun to quickly forward
    propagate eastward across southwestern South Dakota. Meanwhile,
    isolated cells have formed on the nose of strengthening low-level
    flow across eastern South Dakota, with supercellular structures
    noted near Jamestown, ND. These storms are exhibiting a limited
    flash flood risk at the moment, with fast storm motions across
    western North Dakota and isolated storm coverage in eastern North
    Dakota both limiting the spatial extent of any heavy rainfall. A
    few spots of 2 inch/hr rain rates near Jamestown could prompt
    isolated flash flood issues in the short term.

    Over time (more likely after 03Z/10p CDT), increasing low-level
    flow across the eastern Dakotas and strong speed convergence along
    the nose of that low-level flow across northern Minnesota will
    combine with strong instability (1500-4000 J/kg MLCAPE) to produce
    widespread thunderstorm activity. These storms should eventually
    concentrate along an axis from near/north of Fargo to ner Duluth.=20
    They'll also form in close enough proximity to promote occasional
    mergers and localized training, with spots of 2 inch/hr rain rates
    expected at times. Additionally, storms should eventually merge
    with upstream convection across North Dakota, providing further
    opportunity for prolonging of heavy rain rates at any one spot.=20
    Widespread 1-3 inch rainfall totals are expected beneath the
    convection, with local amounts of 5 inches possible where
    training/mergers are most pronounced. These rates will fall on
    areas of 1-2 inch/hr FFG thresholds (lowest along the ND/MN border
    and across northeastern Minnesota), with exceedence expected at
    times. Flash flooding is possible in this scenario.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Jy1OECamoSmfT4u0aW2Hzlx6jsyMA6UbK8afi-2qJMbkOjaMRnxQSJyh3fZX4dABMPr= 6Xnz7xYxQZmnqwjag3tXK5Q$ for graphic product...

    ATTN...WFO...BIS...DLH...FGF...GRB...MPX...MQT...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 48909458 48399232 47819106 47079065 45809004=20
    45429061 45729145 46589408 46639663 46399986=20
    46820093 47540036 47839969 48409860 48889700=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 23 20:33:58 2025
    AWUS01 KWNH 232032
    FFGMPD
    WIZ000-ILZ000-MNZ000-IAZ000-240231-

    Mesoscale Precipitation Discussion 0497
    NWS Weather Prediction Center College Park MD
    432 PM EDT Mon Jun 23 2025

    Areas affected...southeastern Minnesota, northeastern Iowa,
    central/southern Wisconsin, far northern Illinois

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 232031Z - 240231Z

    Summary...Scattered thunderstorms are increasing in organization
    and intensity across southeastern Minnesota and western Wisconsin,
    with areas of 1-1.75 inch/hr rain rates now being observed. These
    rates will promote isolated/spotty flash flood potential across
    the discussion area through 02Z/10pm CDT this evening.

    Discussion...Thunderstorms were increasing in coverage and
    intensity - especially across southeastern Minnesota where 1-1.75
    inch/hr rain rates were estimated per MRMS. The cells are
    embedded in deep southwesterly flow aloft along with weak/modest
    low-level shear, suggesting outflow-dominance and potential for
    multiple cell mergers to locally prolong rain rates. The cells
    are in a strongly unstable, moist airmass (3000 J/kg MLCAPE, 2
    inch PW values), supporting intense and efficient downdrafts and
    local rain rates exceeding 2 inches/hr. These rain rates will
    approach/locally exceed FFG thresholds, supporting isolated flash
    flood potential in the near term.

    Eventually, cells will further congeal into one or two
    forward-propagating convective complexes over the course of the
    afternoon. The upscale growth should allow for continued heavy
    rain potential along with more of a southward component of translation/development of heavy rain axes into more of southern
    Wisconsin, northeastern Iowa, and adjacent areas. The uncapped
    airmass southeast of ongoing convection and broad low-level confluence/convergence suggests that newer convection will merge
    with evolving complexes and aid in continued heavy rain potential,
    with spots of 2 inch/hr rain rates continuing. Isolated instances
    of flash flooding are expected through the evening as a result.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-m494f14f_IDXdcqs8x068e1qyax8IkhETHjSurrAhb-Dh3t0EwEJLtfNcaN9Wsi4ihU= aFOhNYumPMdFL-RZ7GaFUlQ$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...GRB...LOT...MKX...MPX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 44778792 43838768 43048803 42368880 41969068=20
    41649296 42329364 43279343 44019256 44679043=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 23 21:27:58 2025
    AWUS01 KWNH 232127
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-240326-

    Mesoscale Precipitation Discussion 0498
    NWS Weather Prediction Center College Park MD
    526 PM EDT Mon Jun 23 2025

    Areas affected...central/northeastern Kansas into central iowa

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 232126Z - 240326Z

    Summary...Scattered thunderstorms will gradually increase in
    coverage through 03Z/10p CDT across the discussion area. These
    storms will also gradually organize into bands fostering
    training/mergers, with rain rates exceeding 2 inches/hr at times.
    Flash flooding is expected on an isolated to scattered basis.

    Discussion...Scattered thunderstorms continue to expand in
    coverage 1) along and just north of a surface cold front extending
    from near Hays, KS to near Mason City, IA and 2) ahead of this
    front across much of central Kansas. The storms are embedded in
    deep southwesterly flow aloft, with marginal low-level shear
    contributing to loosely organized cells and clusters that are
    primarily outflow dominant in nature. Cells were drifting
    northeastward while merging, resulting in localized spots of 1
    inch/hr rain rates especially from central Kansas into
    southwestern Iowa. These rates are falling well below FFG
    thresholds (generally in the 2.5 inch/hr range), suggestive of an isolated/spotty flash flood risk in the near term (through 22Z or
    so).

    Over time, convective coverage should expand with continued
    surface heating and a weakly capped airmass. Meanwhile, 850mb
    flow should increase into the 25-30kt range while promoting
    convergence along the surface front. The strong southwesterly
    flow should also maintain both moisture (2+ inch PW values) and
    instability (3000 J/kg MLCAPE) Each of these factors support an
    increasing flash flood risk as areas of 2-3 inch/hr rain rates
    materialize. Sensitive/urbanized areas should experience the
    greatest flash flood risk in this scenario. Scattered storms
    should continue to grow upscale into bands promoting training and
    mergers, and development of one or two forward-propagating
    convective complex is likely especially from northeastern Kansas
    into southwestern Iowa. Isolated to scattered flash flooding is
    likely in this scenario.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9w9idsvK4vkaJsp-R3A420YwzqDK-j7FM6erI3URNlZs40zt8Cam0UIY7MlqXmMIbFX2= 27bnPdX326iNvtZl3ymLm9o$ for graphic product...

    ATTN...WFO...DDC...DMX...DVN...EAX...GID...ICT...OAX...TOP...

    ATTN...RFC...KRF...MSR...TUA...NWC...

    LAT...LON 42589334 42339222 41829171 40599262 38619539=20
    37499673 37219792 37269959 37660022 38380010=20
    39379885 40299814 41739523=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 23 21:43:51 2025
    AWUS01 KWNH 232143
    FFGMPD
    TXZ000-OKZ000-KSZ000-NMZ000-240342-

    Mesoscale Precipitation Discussion 0499
    NWS Weather Prediction Center College Park MD
    543 PM EDT Mon Jun 23 2025

    Areas affected...portions of the Texas Panhandle, Texas South
    Plains, southeastern New Mexico, far northwest Oklahoma, far
    southwest Kansas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 232142Z - 240342Z

    Summary...Scattered, slow-moving thunderstorms were drifting
    northward while occasionally merging, resulting in spots of 1-2
    inch/hr rain rates. These trends should continue for a few hours
    this afternoon, prompting an isolated flash flood risk especially
    in low-lying/sensitive areas.

    Discussion...Recent radar mosaic imagery depicts maturing
    convective cells in scattered fashion generally extending from
    Perryton, TX south-southwestward through Amarillo, Lubbock, and
    Hobbs, NM. These storms were drifting northward amid deep, but
    weak, southerly steering flow across the region. The storms were
    embedded in a very moist, unstable pre-convective environment,
    with ~2000 J/kg MLCAPE and 1.75-2 inch PW values contributing to
    strong updrafts and efficient rain rates. Weak shear and weak
    inhibition has enabled multiple outflow-driven cells to
    materialize, with several cell mergers and slow cell movement
    contributing to areas of 1.5-3 inch/hr rain rates in a few spots.
    Local FFGs are as low as 1.5 inch/hr in spots across the
    discussion area, suggestive of isolated flash flood potential
    currently existing in the most sensitive areas.

    These trends should continue through the evening hours as
    continued solar insolation promotes new updrafts/development in
    areas unaffected by current convection and outflows. Models
    suggest a diurnally driven convective threat, with gradual
    weakening of storms after sunset/02Z or so. The flash flood
    threat will likely be diurnally driven as well.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9ytSuizQuw-fdxJBu5_XB8t25iOUfBGEwdA4xnLh-ZD0tbRA1M2h8eZrFXr5FYnUFb9r= xVjHgFf-VJbs7vouFfFl1nc$ for graphic product...

    ATTN...WFO...ABQ...AMA...DDC...LUB...MAF...OUN...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 37479921 36939907 35939953 34080098 32490206=20
    31930264 32580374 33790408 35510295 36810141=20
    37439978=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 24 03:36:54 2025
    AWUS01 KWNH 240336
    FFGMPD
    TXZ000-NMZ000-240735-

    Mesoscale Precipitation Discussion 0500
    NWS Weather Prediction Center College Park MD
    1135 PM EDT Mon Jun 23 2025

    Areas affected...Southern NM...Southwest TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 240335Z - 240735Z

    SUMMARY...Clusters of heavy showers and thunderstorms will
    continue to pulse going into the overnight hours across portions
    of southern NM and into southwest TX. High rainfall rates and
    locally slow cell-motions will continue a threat for flash
    flooding.

    DISCUSSION...The latest GOES-E IR satellite imagery shows areas of
    cold-topped convection continuing to regenerate and locally
    persist across areas of southern NM and down into southwest TX.
    The environment remains very moist with PWs in the 90th to 95th
    percentile of climatology this evening. Despite the convection
    that has already occurred through the evening, there still remains
    pockets of instability with MLCAPE values locally over 1000 J/kg.

    There is some weak mid-level vort energy lifting slowly
    northeastward across far northern Mexico which may lift into
    southern NM and far southwest TX overnight, and this energy will
    likely support at least some sustenance of convection given the
    very moist environment and the lingering instability.

    The moisture concentrations in the mid and upper-levels of the
    vertical column are quite impressive based off the CIRA-ALPW
    analyses and this should favor rather efficient rainfall processes
    for additional high-end rainfall rates. Some rates with the
    stronger storms that persist over the next few hours may still be
    capable of reaching 2 inches/hour. The slow cell-motions will
    support additional rainfall amounts of 3 to 4+ inches.

    Additional areas of flash flooding will be possible, and this will
    especially be the case around some of the normally dry
    washes/arroyos and localized burn scar areas which are sensitive
    to heavy rainfall.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6GmEjehXi64hq1xaAqmgwG35h_BLjMYWj2FiHtIYIgpaf7GrWGmp-Xj24plTyXqJ_fs6= KtG3a77JVOQtFeMPty61tBg$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...NWC...

    LAT...LON 34230585 33900454 32800346 30990293 29490277=20
    29070342 29570448 30740551 31270620 32210700=20
    33530707=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 24 04:18:55 2025
    AWUS01 KWNH 240418
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-241000-

    Mesoscale Precipitation Discussion 0501
    NWS Weather Prediction Center College Park MD
    1217 AM EDT Tue Jun 24 2025

    Areas affected...Central/Eastern KS...Northwest MO...Southern IA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 240417Z - 241000Z

    SUMMARY...Areas of heavy showers and thunderstorms will continue
    overnight across portions of central and eastern KS, northwest MO
    and southern IA. Some additional concerns for flash flooding will
    exist from slow-moving cells and high rainfall rates.

    DISCUSSION...The latest GOES-E IR satellite imagery shows a
    southwest to northeast axis of broken shower and thunderstorm
    activity extending from central KS northeastward through northwest
    MO and into southern IA. The activity is focused along and south
    of a well-defined frontal zone with a very moist and unstable
    airmass pooled up along it. PWs of 1.75 to 2 inches, with MLCAPE
    values of 1000 to 1500 J/kg are noted along it.

    A rather convergent southwest low-level jet of 30 to 40 kts is
    focused in proximity to the front, and this should coupled with at
    least weakly divergent flow aloft should maintain a regional
    threat of heavy showers and thunderstorms going through the
    overnight hours.

    There will be additional storms capable of producing rainfall
    rates of 1.5 to 2.5 inches/hour based on the very moist
    environment along the front, and locally slow cell-motions and
    potential areas for some cell-training may allow for some spotty
    additional rainfall amounts of 3 to 5 inches.

    The 00Z HREF guidance is rather aggressive with some of the
    rainfall potential over the next several hours, and may be locally
    a bit overdone, but the environment near and south of the front
    should remain conducive for additional areas of heavy showers and thunderstorms. Some additional concerns for flash flooding will be
    possible as a result, and especially if any of these heavier rains
    can impact the more sensitive urbanized areas.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6lOlPDgyrx9pzE1UpcAhx8mWQInGxSn7TWM-dz_qLhqe7tK90GVcukyoo4LsZiRbE2Ki= 87xwrDFSIwJpPcrZU4ZkOUc$ for graphic product...

    ATTN...WFO...DDC...DMX...DVN...EAX...ICT...LSX...OAX...TOP...

    ATTN...RFC...KRF...MSR...TUA...NWC...

    LAT...LON 41699247 41249134 40229211 38769477 37969683=20
    37819855 38669881 40039606 41249448=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 24 09:42:28 2025
    AWUS01 KWNH 240942
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-241500-

    Mesoscale Precipitation Discussion 0502
    NWS Weather Prediction Center College Park MD
    540 AM EDT Tue Jun 24 2025

    Areas affected...Central/Northeast KS...Northwest MO...Southern IA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 240940Z - 241500Z

    SUMMARY...Additional rounds of heavy showers and thunderstorms are
    expected going through the mid-morning hours. Given the high
    rainfall rates along with cell-training concerns and the
    increasingly moist/wet antecedent conditions, the threat of flash
    flooding will continue.

    DISCUSSION...The early morning GOES-E IR satellite imagery along
    with dual-pol radar shows a broken axis of heavy showers and
    thunderstorms continuing to impact areas of central KS through
    northwest MO and into southern IA. Some of the coldest convective
    tops and heavier rainfall rates are along areas of the MO/IA
    border where MRMS data is showing rates upwards of 1.5 inches/hour.

    This activity is embedded within a moist and unstable airmass
    early this morning characterized by PWs of 1.75 to 2 inches, and
    with MUCAPE values of around 1000 J/kg. There continues to be a
    frontal zone draped in a southwest to northeast fashion across the
    area with multiple weak waves of low pressure riding northeast
    along it. Some weak vort energy is also noted in satellite
    imagery, with one vort over central KS and another one over
    southwest IA which are both contributing to some modest ascent
    over the region and thus facilitating convective sustenance.

    The 00Z REFS data suggests the ongoing activity may persist for a
    while this morning, with a setup that will locally favor
    repeating/training areas of convection. These areas of heavy
    showers and thunderstorms will be capable of yielding an
    additional 2 to 4+ inches of rain, with the heaviest amounts over
    northwest MO and southern IA.

    Given the rainfall that has occurred overnight, the antecedent
    conditions across the area are locally quite moist/wet, and thus
    with the additional rains this morning, the threat for areas of
    flash flooding will continue.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9KQ5T8zmZBIqtSI44KsE9wn-xT_Q6UG9i--l3QNJfCgX3Y1z4Vr3CPriu2SJutPwK_36= bQiCzPJBRzdT33ULLWALUKA$ for graphic product...

    ATTN...WFO...DMX...DVN...EAX...ICT...OAX...TOP...

    ATTN...RFC...KRF...MSR...TUA...NWC...

    LAT...LON 41649345 41569229 40769218 39219503 38299721=20
    38539798 39109751 40059611 41119482=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 24 14:45:56 2025
    AWUS01 KWNH 241444
    FFGMPD
    TXZ000-NMZ000-241900-

    Mesoscale Precipitation Discussion 0503
    NWS Weather Prediction Center College Park MD
    1044 AM EDT Tue Jun 24 2025

    Areas affected...West Texas into southeast New Mexico

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 241442Z - 241900Z

    Summary...Showers and isolated thunderstorms will expand across
    West Texas and Southeast New Mexico though the early afternoon.
    Rainfall rates may exceed 0.5"/hr, which through repeating rounds
    could produce over 1" of rainfall in some areas. Where these rain
    rates occur atop sensitive terrain features or burn scars, flash
    flooding may result.

    Discussion...The GOES-E Day-Cloud Phase RGB early this morning
    indicates a rapid increase in convective updrafts and paired
    increasing Lightning Cast probabilities. This is associated with
    deepening convection downstream of a shortwave lifting out of
    Chihuahua, Mexico within pinched 700-500mb flow out of the south.
    This flow is being squeezed along the periphery of an intense
    mid-level ridge centered over the Mid-Atlantic states and
    downstream of an amplifying trough over the Great Basin. 700mb
    temperatures have lowered about 2C during the past 24 hours,
    allowing for this more rapid uptick in convection, and rainfall
    rates have already been estimated above 0.5"/hr according to the
    KHDX radar in fresh development this morning.

    PWs across the region were measured this morning on the 12Z U/A
    sounding at KEPZ of 1.49 inches, well above the 90th percentile
    and near the daily record of the SPC sounding climatology. This PW
    is progged to surge to as high as 1.75 inches, and combine with a
    plume of instability approaching 2000 J/kg to fuel strong
    convection into the afternoon. Although the strongest echoes and
    accompanying rainfall may occur later today, through the next
    several hours the increasing deep layer lift (downstream of the
    shortwave and within the RRQ of an intensifying upper jet streak)
    will help push rainfall rates to 0.5-1"/hr according to both the
    HREF hourly probabilities and 1-hr rain rates from the UA WRF.
    Locally higher rainfall is even possible, as the HRRR 15-min
    rainfall reaches 0.5" before 19Z in isolated locations. With
    Corfidi vectors progged by the RAP to be just 5-10 kts, and in the
    presence of bulk shear increasing to 20-25 kts, even where
    rainfall rates are not most intense repeating rounds of
    showers/thunderstorms could cause 1-2" of rainfall.

    This area has been wet recently as noted by 7-day AHPS rainfall as
    much as 200-300% of normal, leading to 0-10cm soil moisture above
    the 98th percentile, and compromised FFG as low as 1-1.5"/3hrs.
    Although HREF exceedance probabilities are modest through the next
    several hours, it is possible that any of these more intense rain
    rates, if they do fall atop the more sensitive soils or vulnerable
    terrain and burn scars (especially around Ruidoso) could cause
    rapid runoff leading to flash flooding.

    Additional discussions for enhanced flash flooding potential will
    likely be needed for parts of these same areas, as well as
    downstream to the north, later this afternoon.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5iUU2XjpstSnoOYhxwgJYxGc5ULDIPu6z5dH0y9NPNHx9kHcKxriMVAWZiASSLuIZsHa= -oquvZqw9qLv7JjopB78UZI$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...NWC...

    LAT...LON 34210549 33830483 33340425 32640385 31170364=20
    30700377 30510398 30280464 30500538 31180624=20
    31720673 32370707 33220696 33870629 34190593=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 24 17:03:28 2025
    AWUS01 KWNH 241702
    FFGMPD
    COZ000-NMZ000-242300-

    Mesoscale Precipitation Discussion 0504
    NWS Weather Prediction Center College Park MD
    102 PM EDT Tue Jun 24 2025

    Areas affected...Central and Northern New Mexico, far southern
    Colorado

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 241701Z - 242300Z

    Summary...Showers and thunderstorms developing across New Mexico
    will expand and intensify through the afternoon. Rainfall rates
    may exceed 1"/hr at times, leading to 1-2" of rain with locally
    higher amounts possible. This may cause instances of flash
    flooding.

    Discussion...The regional radar mosaic late this morning shows
    rapidly expanding coverage of showers aligned with a surface
    trough axis across western New Mexico. This convection is
    blossoming in response to increasing ascent through low-level
    convergence and increasing upper diffluence as a jet streak pivots
    to the north. Thermodynamics are impressive across the region as
    well, with PWs analyzed by the SPC RAP of 0.8 to 1.2 inches (and
    measured on the KABQ 12Z U/A sounding of 1.12 inches, nearly a
    record), overlapping increasing SBCAPE of 1000-1500 J/kg. Recent
    shower activity from KABX WSR-88D has rapidly expanded coincident
    with cooling cloud tops reflective of deepening updrafts, yielding radar-estimated rainfall rates of 0.5"/hr.

    The CAMs are in good agreement that convection will continue to
    rapidly expand during the next few hours, and in fact the current
    activity is even more widespread than CAM initialization which
    appears to be running about 2 hours behind reality. This suggests
    that the impressive coverage of simulated reflectivity forecast by
    the CAMs is accurate, with the overlap of strong deep layer ascent
    maximizing over near record PWs leading to numerous thunderstorms
    by the aftn. As bulk shear increases to 20-30 kts, storms should
    organize into clusters and intensify even further, with HREF,
    REFS, and the UA-WRF indicating rainfall rates potentially
    eclipsing 1"/hr later today, with as much as 0.5" of rainfall
    occurring in 15-mins according to the HRRR. Although storms will
    form initially along the low-level convergent trough and across
    terrain, it is likely these clusters will move off to the
    northeast on 0-6km mean winds of 10-20 kts, with aligned Corfidi
    vectors indicating training of cells to produce 1-2" of rainfall
    with locally higher amounts.

    These intense rainfall rates, especially where they repeat/train,
    will pose an increasing flash flood risk through the afternoon.
    FFG across the area is elevated due to recent dry conditions,
    which limits HREF exceedance probabilities to just 5-10%. However,
    where any more pronounced training can occur, or should the
    strongest cells move atop sensitive terrain features, urban areas,
    or recent burn scars, rapid runoff leading to instances of flash
    flooding could result.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_12K0FKB0Trb3gvrfaEYs_Gnh8jnhyM6PaSfaUyWA5tFmVkBwaC7g3rtfTGlpcerobtD= ee1w8ucAB-uvlUWj8ImCSFg$ for graphic product...

    ATTN...WFO...ABQ...EPZ...GJT...PUB...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 37630508 37450464 37190429 36420431 35310434=20
    34640472 34230525 33970585 33970595 33580664=20
    33210731 33130781 33260806 34210815 35900780=20
    37040705 37590590=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 24 18:53:01 2025
    AWUS01 KWNH 241852
    FFGMPD
    TXZ000-OKZ000-NMZ000-250000-

    Mesoscale Precipitation Discussion 0505
    NWS Weather Prediction Center College Park MD
    252 PM EDT Tue Jun 24 2025

    Areas affected...West TX, High Plains of NM, far western TX
    Panhandle

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 241851Z - 250000Z

    Summary...Showers and thunderstorms will rapidly expand this
    afternoon across the High Plains of NM and surrounding areas.
    Rainfall rates in more intense cores will exceed 1"/hr, leading to
    localized rainfall totals of 2-3" or more. Flash flooding is
    likely.

    Discussion...The regional radar mosaic across the Southwest this
    afternoon shows a rapid expansion of showers and thunderstorms
    aligned from far West Texas northeast through the western
    Panhandle of Texas. This activity is building rapidly in response
    to impressive and intensifying deep layer ascent driven by a
    combination of height falls from an amplifying trough over the
    Great Basin, a favorably placed upper jet streak, and a potent
    MCV/convectively enhanced shortwave lifting out of Chihuahua,
    Mexico. This lift is acting upon extreme thermodynamics
    characterized by record PWs measured via regiona U/A soundings of
    1.4 to 1.6 inches overlapped with SBCAPE that has climbed to
    1000-2000 J/kg according to the SPC RAP analysis. With a large
    mid-level ridge anchored to the east, and the amplifying trough to
    the west, the region will remain pinched within moist flow
    allowing for ongoing convection to expand and intensify through
    the evening as reflected by available CAMs.

    Recent reflectivity from KFDX and KHDX WSR-88Ds has expanded
    rapidly in conjunction with a surge of Lightning Cast
    probabilities and deepening updrafts on the day-cloud phase RGB
    from GOES-E. This has manifested as radar-estimated rainfall rates
    as high as 1.5"/hr. Although storms have been generally of pulse
    variety with limited life spans due to weak bulk shear, some
    organization is occurring along a pronounced 850-700mb convergence
    axis as low-level winds weaken out of Texas. This, as well as the
    potent MCV emerging into West Texas, will help to focus
    thunderstorms over the High Plains of NM through the afternoon.
    Initially, fresh convection will move slowly as noted by weak
    winds in the sfc-600mb layer of regional soundings, but then
    eventually translate more rapidly northeast as they deepen. Still,
    Corfidi vectors will remain just 5-10 kts indicating that cells
    will generally move slowly today. With rain rates progged by both
    HREF and REFS ensembles to exceed 1"/hr (50-60% chance), and HRRR
    15-min rainfall as much as 0.5", this could result in 2-3" of rain
    with locally higher amounts through the evening.

    Parts of eastern NM and West Texas have been wet the past 7 days,
    with AHPS measuring rainfall departures that are as much as 300%
    of normal. This has lowered FFG to as low as 1-2"/3hrs, with much
    lower FFG likely across sensitive burn scars and terrain features.
    There is at least a 30-50% chance of exceedance of this FFG, and
    flash flooding is likely over more sensitive soils and urban
    areas. Should this heavy rain fall atop the most vulnerable areas,
    like the Ruidoso Complex, locally significant impacts are likely.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4dEE2h7MyQRmFd-wz1rKQSzbb140vqk0vv12d8Lh2Zo4Il3gPbnQxFdjJEb_X_7qAwH6= 2QhYw1x-o65AphocEErdBmE$ for graphic product...

    ATTN...WFO...ABQ...AMA...EPZ...LUB...MAF...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 36660298 36540251 36190215 35300242 34350288=20
    33130314 31800362 30860418 30670517 31130616=20
    31470655 31810675 32490660 33510612 34200568=20
    35360468 36380375=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jun 24 22:48:04 2025
    AWUS01 KWNH 242248
    FFGMPD
    NMZ000-AZZ000-250446-

    Mesoscale Precipitation Discussion 0506
    NWS Weather Prediction Center College Park MD
    647 PM EDT Tue Jun 24 2025

    Areas affected...Southwestern and central New Mexico

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 242246Z - 250446Z

    SUMMARY...Numerous showers and thunderstorms are impacting New
    Mexico this afternoon and containing hourly rainfall rates up to
    2.5". These storms are expected to continue through early tonight
    while potentially becoming more organized, likely leading to
    numerous additional instances of flash flooding and potentially
    significant local impacts.

    DISCUSSION...GOES19 IR satellite imagery depicts cooling
    cloud-tops associated with thunderstorms oriented
    northeast-southwest across New Mexico moving generally
    east-northeast under the influence of a large eastern U.S. upper
    ridge and western U.S. upper trough. This convergent flow is also
    allowing for plentiful amounts of atmospheric moisture content to
    continually pump into the region. PWs to remain elevated and above
    1.0" in the region, with maximum values along the New
    Mexico-Mexico border estimated over 1.6" per SPC's mesoanalysis.
    This is well above climatology and highlighted by both the GEFS
    and ECENS as exceeding the 95th climatological percentile. To
    summarize, any thunderstorms will have ample moisture to produce
    efficient rainfall rates of 1.5-2.5"/hr which in this part of the
    country can be particularly hazardous.

    MLCAPE values over 500 J/kg are widespread across central NM and
    higher south where values of 1000-2000 J/kg are being slowly
    advected northward along with an MCV in West Texas evident in
    visible satellite. The combination of increasing instability,
    convergent flow on the western periphery of an MCV, and high PWs
    leads to the likelihood of continued convection into the early
    overnight period, with thunderstorms also likely congealing along
    the primary confluence zone in central NM.

    Mountainous terrain, local burn scars, urbanized areas, and dry
    washes are most susceptible for flash flooding. Given the ongoing
    flash flood warnings in the area and the additional rainfall
    amounts locally to exceed 2", additional flash flooding is
    considered likely. Some significant impacts are also possible
    where renewed/developing convection overlaps with earlier rainfall
    associated with initial early afternoon thunderstorms

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!63bX0_HPse5-bkS0nVxK5lLAcq9ge0-GECSMqa9Em3_14U8G5j6bdyhBj_JMP2PduM8R= x6aYZ2n26dNZ4LbzJeZ8gYc$ for graphic product...

    ATTN...WFO...ABQ...EPZ...TWC...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 36930443 36120439 34730530 33250616 31960683=20
    31370757 31140869 31300972 31830979 33070882=20
    34460765 35890651 36820545=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 25 00:03:43 2025
    AWUS01 KWNH 250002
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-250400-

    Mesoscale Precipitation Discussion 0507
    NWS Weather Prediction Center College Park MD
    801 PM EDT Tue Jun 24 2025

    Areas affected...Far northeast KS, southeast NE, southern IA, and
    northern MO

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 250000Z - 250400Z

    SUMMARY...Scattered showers and thunderstorms moving from
    northeast Kansas into northern Missouri have the potential for
    rainfall rates of 1-2"/hr. These storms are moving into an area
    that experienced heavy rainfall earlier today and could spawn
    isolated instances of flash flooding.

    DISCUSSION...Recent radar and satellite observations depict mostly
    unorganized thunderstorms rounding the dominant eastern U.S. upper
    ridge and moving across the central Plains in an
    east-northeasterly direction south of a stationary front draped
    across central IA. Additionally, an outflow/low-level convergence
    boundary is analyzed south of this front and is the focus for the
    scattered thunderstorm activity of concern. MRMS shows hourly
    rates estimated up to 1.5-2.0" at times.

    Recent 22z HRRR run did not initialize this convection accurately
    compared to prior runs, with the experimental RRFS struggling to
    as well. This area of northern MO and southern IA falls on the
    southern periphery of the better moisture axis with PWs greater
    than 1.7" extending along the frontal boundary just to the north.
    However, an instability gradient noted by 2500-3000 J/kg of SBCAPE
    extends along the surface convergence zone and should be enough to
    maintain or grow updrafts within an area of 25-30kts of sfc-3km
    bulk shear. Therefore, it's possible storms maintain for several
    additional hours until instability weakens well after sunset.

    Parts of northern MO and southern IA experienced several inches of
    rainfall this morning (4-6") and FFG remains somewhat impacted as
    3-hr FFG remains below 2.5" in spots. Given the potential for
    storms to overlap these sensitive locations and locally intense
    rainfall rates of 1-2"/hr, isolated flash flooding is possible.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-YqAK2nReUAwowKySDnXIfLG34pWl_au-CPViECg22FY3GsAngUFLoJsFlpIbikY1ct6= oCOJS14rz8HNAU7YbzrS0B8$ for graphic product...

    ATTN...WFO...DMX...DVN...EAX...OAX...TOP...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 41309265 41119192 40699181 40159275 39649434=20
    39579520 39989560 40389544 40889477 41239357=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 25 00:47:37 2025
    AWUS01 KWNH 250047
    FFGMPD
    KSZ000-NEZ000-COZ000-250645-

    Mesoscale Precipitation Discussion 0508
    NWS Weather Prediction Center College Park MD
    846 PM EDT Tue Jun 24 2025

    Areas affected...Eastern Colorado through central Nebraska

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 250045Z - 250645Z

    SUMMARY...Organizing cluster of thunderstorms extending from
    eastern Colorado through southwestern portions of Nebraska is
    expected to gradually push northeastward while containing heavy
    rainfall rates potentially exceeding 2"/hr at times. Isolated to
    scattered instances of flash flooding are possible through early
    tonight.

    DISCUSSION...Recent surface observations, radar, and satellite
    trends depict an organizing thunderstorm complex exhibiting a
    somewhat slow northeast forward motion that has the potential to
    produce instances of flash flooding. MRMS estimates hourly
    rainfall rates up to 2.5"/hr near the border of southwest NE and
    northeast CO where the advancing line of storms out of CO is
    congealing with developing cells in the warm sector across
    southern NE.

    This area of thunderstorms falls within the RFQ of the 300mb upper
    jet racing out of the neutrally tilted western U.S. trough with
    its base in southern CA. This is providing ample divergence aloft
    and when combined with surface convergence along a frontal
    boundary, an ideal setup for thunderstorm growth. Southerly flow
    on the western periphery of the eastern U.S. upper high is also
    giving the region plenty of atmospheric moisture content to work
    with. PWs in the are over 1.5" and above the 95th climatological
    percentile per the 12z ECENS and GEFS. Therefore, rainfall rates
    are expected to be intense underneath the strongest updrafts and
    within developing mesoscale circulations created by merging cells.
    Recent CAMs depict the potential for rainfall totals up to 5" and
    the 18z HREF highlights 25 percent chances for at least 3" across
    a broad region in the highlighted MPD. 3-hr FFG is generally
    around 3", thus the potential for isolated to scattered flash
    flooding more likely in prone urban areas and low-lying areas near rivers/streams.=20

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_6ZheWlfpNxBg-IPc_t9xgysWualF5N1Q7fK90e16GzxcbvoAneg-XxQAWeHBc_qIsU4= kl2b3hkxp_Rj-dKIRD2kvqg$ for graphic product...

    ATTN...WFO...BOU...CYS...GLD...LBF...PUB...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 41870058 41520008 40620055 39160210 38510318=20
    38830376 39550326 40110302 41060294 41570248=20
    41830175=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 25 04:31:08 2025
    AWUS01 KWNH 250431
    FFGMPD
    TXZ000-NMZ000-251030-

    Mesoscale Precipitation Discussion 0509
    NWS Weather Prediction Center College Park MD
    1230 AM EDT Wed Jun 25 2025

    Areas affected...Central and Eastern NM...Southwest TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 250430Z - 251030Z

    SUMMARY...Heavy rainfall will continue overnight across areas of
    central and eastern NM down through southwest TX. A combination of
    heavier rainfall rates and slow-moving showers and thunderstorms
    will likely foster additional areas of flash flooding.

    DISCUSSION...The mid-evening GOES-E IR satellite imagery shows a
    slow-moving shortwave trough ejecting across western NM which is
    helping to drive a broader area of ascent downstream across much
    of central and eastern NM down through southwest TX. This is
    interacting with a very moist and unstable airmass and is
    currently sustaining a fairly large area of heavy shower and
    thunderstorm activity.

    PWs across the region are on the order of 1.3 to 1.5 inches which
    represents the 90th to 95th percentile of climatology. The 00Z EPZ
    RAOB showed a rather high WBZ level with a strong concentration of
    moisture in the mid and upper levels of the vertical column. This
    is further confirmed in CIRA-ALPW data which shows a very
    well-defined tropical connection of moisture lifting north from
    Mexico and up across the southern Rockies/High Plains around the
    western periphery of the subtropical ridge centered over the
    Eastern U.S.

    This very moist environment will favor highly efficient rainfall
    processes for enhanced rain rates. The latest RAP analysis shows a
    rather strong pool of instability currently over southeast NM with
    the aid of moist low-level southeast flow, and the MUCAPE values
    currently remain as high as 2000 to 3000 J/kg. This available
    thermodynamic energy coupled with the approaching shortwave
    trough, proximity of a weak MCV, and weak outflow-induced
    low-level forcing should maintain a solid threat for heavy showers
    and thunderstorms going well into the overnight hours. Localized
    orographic ascent near areas of high terrain, including the
    Sacramento Mountains will further enhance the convective potential.

    Rainfall rates with the stronger storms will likely be 1 to 2+
    inches/hour given the anomalously moist environment, and the
    relatively slow cell-motions may allow for some storm totals
    overnight to reach 2 to 4+ inches. Areas of flash flooding will be
    likely as a result, and there will be concerns overnight for
    notable arroyo flash flooding. Additionally, the burn scar complex
    (Blue-2, Salt, South Fork, and McBride) in the Sacramento
    Mountains will need to be carefully monitored for additional
    focused flash flooding concerns.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-nMEJJzWWb03U0-X1rrv491tKluIuvPx4lrGBnvZtvyCnskidgH0wAqmm1X3lc5mx7BI= ii_zbECZy3TL3voiEkJ6dHQ$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 36130397 36030307 34890321 33100407 31490443=20
    30870526 31170589 31400628 31750676 31880755=20
    32650771 33370725 34390640 35230542=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 25 06:58:19 2025
    AWUS01 KWNH 250657
    FFGMPD
    IAZ000-NEZ000-SDZ000-251255-

    Mesoscale Precipitation Discussion 0510
    NWS Weather Prediction Center College Park MD
    255 AM EDT Wed Jun 25 2025

    Areas affected...Central and Eastern NE...Western and Central IA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 250655Z - 251255Z

    SUMMARY...Multiple rounds of heavy showers and thunderstorms going
    through the early morning hours may produce sufficient rainfall
    for isolated to scattered areas of flash flooding.

    DISCUSSION...A shortwave impulse along with an attendant wave of
    low pressure along a front will continue to advance east going
    through the early morning hours and will drive a relative broad
    area of heavy shower and thunderstorm activity. Strong warm air advection/isentropic ascent with the aid of a southwest low-level
    jet of 30 to 40+ kts continues to surge poleward over a
    pre-existing outflow boundary across northern KS and northern MO
    and into closer proximity of the aforementioned front which
    extends across central to northeast NE and through north-central
    IA. This is yielding persistent moisture and instability transport
    ahead of the surface low and is favoring an elongated axis of
    elevated convection.

    MUCAPE values are on the order of 500 to 1000+ J/kg, with PWs that
    are locally 1.75 to 2 inches. These are generally in the 90th to
    95th percentile of climatology and are helping to favor high
    rainfall rates of 1.5 to 2 inches/hour with the stronger
    convective cells.

    Over the next several hours going through the early morning time
    frame, there should continue to be bands of heavy showers and
    thunderstorms advancing gradually off to the east and northeast
    across central to eastern NE and into western and central IA as
    the upstream shortwave energy and low center arrives. The
    low-level jet is forecast by the RAP guidance to gradually veer a
    bit with some additional strengthening of it at least through the
    predawn hours. This may favor some localized backbuilding and
    training of convection in time.

    The 00Z HREF and 18Z REFS data have some differences with respect
    to the placement of the heaviest rainfall over the next 3 to 6
    hours, with the HREF axis south of the REFS, but they both support
    additional high rainfall rates and some storm totals going through
    12Z (7AM CDT) that could reach 3 to 5 inches where more focused
    areas of cell-training occur.

    FFG values are generally rather high across most of the MPD area,
    but the HREF/REFS consensus shows some 20 to 40 percent
    probabilities of seeing the 3-hour FFG values exceeded and
    especially across western and central IA.

    As a result, the thinking is that there may be some concerns for
    isolated to scattered areas of flash flooding going through the
    early morning hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_oKyAqScDqt4nFYQ3Q1tv50_ylXgVLh6WSbgbMqCwDfRvlNMsufw54Lt2qTva8pj6ST6= sWLdWQ7l9ZF7b9wVXa-uqX0$ for graphic product...

    ATTN...WFO...DMX...FSD...GID...LBF...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 42999530 42999372 42529261 41799244 41299320=20
    40849516 40599696 40599859 40869923 41539922=20
    42279829 42819659=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 25 09:58:22 2025
    AWUS01 KWNH 250957
    FFGMPD
    TXZ000-NMZ000-251530-

    Mesoscale Precipitation Discussion 0511
    NWS Weather Prediction Center College Park MD
    555 AM EDT Wed Jun 25 2025

    Areas affected...Central and Southern NM...Southwest TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 250955Z - 251530Z

    SUMMARY...Some additional clusters of locally heavy showers and
    thunderstorms will be possible going into the morning hours which
    will maintain at least some potential for flash flooding.

    DISCUSSION...The predawn GOES-E IR satellite imagery along with
    dual-pol radar still shows some areas of locally heavy shower and
    thunderstorm activity impacting areas of central and southern NM
    along with far southwest TX. A slow-moving shortwave trough over
    the Southwest continues to slowly pivot eastward, and this is
    driving some right-entrance region upper-jet dynamics which
    coupled with the very moist and modestly unstable airmass across
    the region should favor a threat for these clusters of convection
    to persist into the morning hours.

    PWs across the region remain the same as earlier and are on the
    order of 1.3 to 1.5 inches which represents the 90th to 95th
    percentile of climatology. CIRA-ALPW data continues to show a deep
    layer tropical connection of moisture lifting north across Mexico
    and up across the southern Rockies/High Plains around the western
    periphery of the subtropical ridge centered over the Eastern U.S.

    The latest RAP analsyis shows MUCAPE values of 500 to 1000 J/kg
    locally over the region, and this coupled with the very moist
    environment and local ororgaphics should still favor some rainfall
    rates that may reach 1 to 1.5 inches/hour with the stronger cells.

    The 06Z HREF and 00Z REFS data suggests some potential for
    additional FFG exceedances going into the morning hours, with
    locally an additional 2 to 3 inches of rain possible going through
    15Z (9AM MDT) where the stronger remaining clusters of convection
    persist.

    Therefore, a threat for additional areas of flash flooding will be
    maintained at least over the next several hours. This will include
    locally enhanced runoff concerns for the normally dry
    washes/arroyos and any burn scar locations including for the
    Sacramento Mountains.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7K38a1kIEB2w34xBrMavFbZcIw1cFwiIyFHVKYnHfqsXWHiKgPP5LkNUC_jWIUqdUXef= MuVlHhOPNkkniu4OY_JHoKQ$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...NWC...

    LAT...LON 34810443 34410361 33090363 31500454 30930536=20
    31040579 31210604 31590672 31690776 31900802=20
    32480778 33230713 34120597=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 25 11:33:43 2025
    AWUS01 KWNH 251133
    FFGMPD
    WIZ000-MNZ000-IAZ000-SDZ000-NDZ000-251700-

    Mesoscale Precipitation Discussion 0512
    NWS Weather Prediction Center College Park MD
    732 AM EDT Wed Jun 25 2025

    Areas affected...eastern South Dakota, southern Minnesota, far
    northern Iowa

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 251132Z - 251700Z

    Summary...Showers and thunderstorms will steadily increase in
    coverage through the morning, focusing along an elevated boundary.
    Rainfall rates within the stronger convection will exceed 1"/hr,
    which through training could produce locally more than 3" of rain
    and instances of flash flooding.

    Discussion...The GOES-E IR imagery this morning shows an expansive
    area of cold clouds with continued cooling tops stretched from
    western SD through MN and IA. These cooling tops are associated
    with expanding showers and thunderstorms developing within
    pronounced ascent in the RRQ of a strengthening upper jet streak
    centered over Ontario, aided by both a shortwave lifting across SD
    and potent isentropic lift as the 850mb LLJ of 20-25 kts lifts
    northward over a surface warm front. Thermodynamics across the
    region are favorable for heavy rain as reflected by SPC RAP
    analyzed PWs of 1.5 to 1.8 inches, above the 90th percentile for
    the date, and MUCAPE around 1000 J/kg. This is supporting
    widespread rainfall rates of 0.5-1"/hr from regional radars, with
    expanding heavy rainfall occurring primarily along the nose of the
    LLJ/elevated 850mb boundary.

    During the next several hours, a wave of low pressure developing
    along the warm front across SD will help pinch the flow
    downstream, helping to accelerate the LLJ to offset the typical
    diurnal weakening of this feature. At the same time, the flow may
    back more prominently to the SE, helping to funnel even more
    intense thermodynamics into MN/SD (PWs over 2" coincident with
    1000 J/kg MUCAPE). The high-res CAMs indicate that convection may
    focus in two swaths - along the warm front itself - and then more
    impressively aligned to the elevated front where moisture
    confluence will be most intense and the enhanced ascent downstream
    of the shortwave will focus. Across this area, Corfidi vectors
    become aligned to the elevated front and sharply right of the mean
    0-6km winds, suggesting an enhanced training threat. With rainfall
    rates progged by the HREF and REFS to exceed 1"/hr (40-60%
    chance), this training will result in an axis of rainfall of 2-3"
    with locally higher amounts exceeding 4" as reflected by 6-hr
    HREF/REFS probabilities and PMM.

    Recent rainfall has been highly variable across this region as
    shown by NASA Sport 0-40cm soil moisture that is only above normal
    in some places, leading to FFG generally 1.5 to 3 inches in 3
    hours. HREF exceedance probabilities are 20-30% for these
    thresholds, indicating the increased risk for flash flood
    instances this morning anywhere in the region. However, the
    greatest risk will likely be in an east-west axis along the
    elevated front from far northeast SD through eastern MN.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7ZUaxsQT2De_-tE-nuOQ3_bEa9HOdzvEFNACArUtM8s-dBdv4LfiuTYRCn7zai-sh0Dh= rjXhy6iL7bvQ3kHx6dAngkE$ for graphic product...

    ATTN...WFO...ABR...DLH...DMX...FGF...FSD...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 46129639 46039406 45659283 44799290 43829334=20
    43239408 42929503 42859656 43199746 43589811=20
    44289898 44799938 45449921 45919813=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 25 16:54:46 2025
    AWUS01 KWNH 251654
    FFGMPD
    WIZ000-MNZ000-IAZ000-SDZ000-252300-

    Mesoscale Precipitation Discussion 0513
    NWS Weather Prediction Center College Park MD
    1254 PM EDT Wed Jun 25 2025

    Areas affected...northern IA, eastern SD, southern MN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 251700Z - 252300Z

    Summary...Showers and thunderstorms will gradually expand in
    coverage through the afternoon and intensify to support rain rates
    of 1-2"/hr. This could produce 2-3" of rain with locally higher
    amounts across wet antecedent soils. Flash flooding is possible.

    Discussion...The regional radar mosaic this afternoon shows an
    expansive area of stratiform rain across Minnesota. This
    precipitation is occurring in response to pronounced ascent within
    the RRQ of a strong jet streak to the northeast and persistent
    warm advection and isentropic ascent along the 850mb inflow axis.
    PWs across the region are impressive, analyzed by the SPC RAP to
    be 1.5 to 2.0 inches, with the limiting factor to rainfall
    intensity so far being the sharp instability gradient as SBCAPE
    above 250 J/kg is confined to areas south of the analyzed warm
    front. In general, the rainfall this morning has been of moderate
    intensity, but a few regions of training across IA, MN, and SD
    have resulted in 12-hr MRMS rainfall as much as 3-4 inches and
    saturated soils.

    During the next few hours, a wave of low pressure developing along
    the warm front will track northeast, leading to acceleration of
    the downstream low-level wind field. This will result in 850mb
    winds surging to 30-35 kts, forcing more pronounced isentropic
    ascent as the warm front lifts northward in response. At the same
    time, this will draw more intense thermodynamics northward, with
    PWs above 2 inches (a daily record if measured) and MUCAPE above
    1000 J/kg reaching as far north as the Twin Cities this evening.
    This will allow for a rapid expansion of convection as reflected
    by high res CAMs simulated reflectivity, and in this robust
    environment both the HREF and REFS suggest a high probability
    (60-70%) of rainfall rates exceeding 1"/hr, with 15-min rainfall
    from the HRRR potentially accumulating to 0.5 - 0.75 inches (brief
    3"/hr rates). Although 0-6km mean winds will remain progressive at
    20-25 kts, Corfidi vectors aligned to the warm front could produce
    2-3 inches of rain, with locally higher amounts above 4 inches
    possible.

    Rainfall already this morning, as noted above, has been locally
    3-4 inches, with widespread 0.5-1 inch also measured via MRMS.
    This has saturated the top soils across most of the area according
    to the HRRR, likely lowering FFG even beyond the analyzed
    1-2"/3hrs. Even in areas that have not been as saturated, HREF
    3-hr exceedance probabilities reach 20-30%, further suggestive of
    the increasing flash flood risk into this evening. However, the
    greatest potential for impacts will be across urban areas or
    beneath any longer-term training.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6Pg2UHEt3tlvhorApDLJ_LaL9xiX2f_7IFT-UYoPJjsR8ng3iEJXj1MXcQzROIt5EryC= 9XEs1PvDxXJ2V1UN8dulnpY$ for graphic product...

    ATTN...WFO...ABR...ARX...DLH...DMX...FSD...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45749319 45419178 44879111 44159113 43839138=20
    43339206 42759358 42599531 42819665 43359770=20
    43919788 44539711 44879628 45339504=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 25 19:57:35 2025
    AWUS01 KWNH 251956
    FFGMPD
    IAZ000-NEZ000-SDZ000-260155-

    Mesoscale Precipitation Discussion 0514
    NWS Weather Prediction Center College Park MD
    355 PM EDT Wed Jun 25 2025

    Areas affected...Central and northeast NE, far southeast SD, and
    far northwest IA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 251955Z - 260155Z

    SUMMARY...Developing thunderstorms are expected to increase in
    coverage this afternoon and early evening, while also training
    over similar areas across central and northeast Nebraska. Hourly
    rainfall rates up to around 2.5" are possible as well as the
    potential for rainfall totals up to 4-5", which would promote
    possible scattered instances of flash flooding.

    DISCUSSION...Cooling cloudtops are evident in GOES-East infrared
    satelitte this afternoon as thunderstorms form along a convergent
    surface trough/boundary south of a frontal boundary stretching
    across the Upper Midwest and northern Plains. Precipitable Water
    values are high in the region and are estimated between 1.7-2.0",
    which equates to above the 90th climatological percentile
    according to the 00z GEFS and ECENS. Additionally, moist southerly
    850mb flow of 20-25kts continues to funnel these elevated moisture
    values into the surface trough where thunderstorms can focus.

    The most important aspect of this setup is the upwind propagation
    vectors are parallel to this surface boundary and out of the
    southwest, which should promote training of thunderstorms. An
    instability gradient also rides along this boundary with SBCAPE
    values of 3000-4500 J/kg per SPC's mesoanalysis just to the south
    and in the inflow of these thunderstorms from south-central
    Nebraska to western Iowa.

    18z HRRR and 12z HREF seem to be handling the convection well so
    far and depict the potential for hourly rates locally up to 2.5"
    and scattered coverage of rainfall totals over 3". Maximum amounts
    could approach 5" by 02Z tonight if should better training of
    storms materialize. This area has seen rainfall lately with MRMS
    analyzing an area of around 3" in central Nebraska over the last
    24 hrs. 3-hr FFG is also relatively low and below 3", even as low
    as 1-1.5". Given the environmental setup and antecedent
    conditions, scattered instances of flash flooding are possible and
    most likely over urban regions, low-lying areas, and locations
    that saw heavy rain over the last 24 hrs.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6B_Y9p_f84qhpYdrtpRqh7T6PafJvwcWvHeX_CWBewcXXtiMs0LgpEqjk5fRI-qlV1cX= PHx6UX7z2-wZwDv3qqIMqr4$ for graphic product...

    ATTN...WFO...DMX...FSD...GID...GLD...LBF...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 42959656 42899532 42419492 41829571 41059727=20
    40169945 40360046 41240006 42359836=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 25 22:17:29 2025
    AWUS01 KWNH 252217
    FFGMPD
    WIZ000-MNZ000-IAZ000-260415-

    Mesoscale Precipitation Discussion 0515
    NWS Weather Prediction Center College Park MD
    616 PM EDT Wed Jun 25 2025

    Areas affected...Northern Iowa, Southeast Minnesota, and
    west-central Wisconsin

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 252215Z - 260415Z

    SUMMARY...Showers and thunderstorms are expected to continue
    through early tonight across portions of the Upper Midwest, while
    also containing intense rainfall rates up to 2"/hr and the
    potential for totals up to 4". These rainfall amounts may lead to
    scattered instances of flash flooding.

    DISCUSSION...A low pressure system was analyzed across southern
    Minnesota at 21z with an attached warm front extending eastward
    into western and southern Wisconsin while a cold front extended
    westward into southern South Dakota. Recent radar and satellite
    observations depict numerous strong to severe thunderstorms in the
    warm sector across southeastern Minnesota and into northern Iowa,
    with moderate to locally heavy stratiform rain north of the low
    pressure system and attached warm front. These thunderstorms are
    estimated to contain maximum hourly rainfall rates up to 2"/hr in
    localized spots and are moving generally east-northeastward.
    Instability is abundant across Iowa with SBCAPE values of
    4000-5000 J/kg as broad southerly flow helps place this
    instability perfectly in the inflow of ongoing storms. PWs also
    remain high and between 1.9-2.2" per SPC's mesoanalysis page,
    which would place it above the 90th climatological percentile.

    21Z HRRR and 20Z experimental RRFS differ somewhat in the exact
    location of heaviest amounts, but both agree on up to 4" of total
    rainfall from these storms. 6-hr FFG are around 2-4" so this
    plants a scenario where isolated to scattered instances of flash
    flooding are possible. The upwind propagation vectors do have a
    northwesterly component so while brief training of storms is
    ongoing across northern Iowa and southeast MN, these storms should
    become more progressive as we get into the late evening.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!65jnbVfWIvUprhnJ7gDLT2GDH9E1dVTXxeqSxEdMauFfvzZzh480LJP-Mjeq0rNg7d2k= 8PucvUm-zwAwydU_7yZVQlM$ for graphic product...

    ATTN...WFO...ARX...DMX...FSD...GRB...MKX...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45339175 44889028 44228951 43518968 42859122=20
    42449294 42219429 42299518 42769530 43409449=20
    44209363 45209285=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jun 25 23:58:04 2025
    AWUS01 KWNH 252356
    FFGMPD
    SDZ000-WYZ000-260555-

    Mesoscale Precipitation Discussion 0516
    NWS Weather Prediction Center College Park MD
    755 PM EDT Wed Jun 25 2025

    Areas affected...South-central into southwest South Dakota and far
    northeast Wyoming

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 252355Z - 260555Z

    SUMMARY...Slow moving thunderstorms along a stationary boundary
    are expected to merge with approaching convection ejecting
    eastward out of the High Plains this evening, with the potential
    for 1.5-2"/hr rainfall rates and scattered totals up to 4" across
    south-central South Dakota. This may lead to a few instances of
    flash flooding, particularly for areas with soils primed from
    previous rainfall today.

    DISCUSSION...A stationary boundary analyzed at 23Z draped across
    southern South Dakota has been aiding to anchor slow-moving storms
    in southwestern South Dakota this afternoon and should see
    convection continue, while also interacting with convection
    ejecting eastward from northeast Wyoming. MRMS depicts a few of
    these storms have produced anywhere from 1.5-3.0" this afternoon.

    Aside from the lifting mechanisms associated with the stationary
    boundary in the area, this part of the country remains in the RFQ
    of an upper jet streak and in an area of elevated PWs in the
    1.0-1.5" range (above climatology). Instability and effective bulk
    shear also remain modest with MLCAPE of 1000-2000 J/kg and
    effective shear of 40-50 kts in western SD. Therefore,
    thunderstorms should be able to maintain strength for several
    hours after sunset and should contain efficient rainfall rates to
    potentially lead to scattered flash flooding. The experimental
    RRFS and REFS seem to have somewhat better handle on current
    convection compared to other CAMs. The REFS also happens to have
    the highest probabilities for 3-hr rainfall amounts greater than
    3" by 06z tonight. These greatest chances occur within a region
    where 3-hr FFG in south-central South Dakota are in the 1.5-3"
    range. Given atmospheric and soil conditions as well as current
    radar trends, there exists the potential for isolated flash
    flooding chances early tonight.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7xRPBf3tA4vWBos6qybKaeni01YvYhj4ZsBmz2Dah6Yc-Lubk-BOCkDGxRjN5RWGQxdb= hcU_zMR6fE2Q5VXl8c4En-M$ for graphic product...

    ATTN...WFO...ABR...UNR...

    ATTN...RFC...KRF...NWC...

    LAT...LON 45130315 44530143 44009991 43669956 43239990=20
    43070141 43200338 43640420 44300447 44890422=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 26 01:46:52 2025
    AWUS01 KWNH 260145
    FFGMPD
    IAZ000-KSZ000-NEZ000-SDZ000-260745-

    Mesoscale Precipitation Discussion 0517
    NWS Weather Prediction Center College Park MD
    944 PM EDT Wed Jun 25 2025

    Areas affected...Much of central and eastern Nebraska, far
    northern Kansas, and western Iowa

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 260145Z - 260745Z

    SUMMARY...Ongoing thunderstorm activity combined with renewed
    convection tonight associated with an approaching upper shortwave
    trough is expected to continue the threat for scattered flash
    flooding. Additional rainfall totals in excess of 3" appear likely
    in spots, which should spawn new and renewed scattered instances
    of flash flooding across already saturated parts of central
    Nebraska into western Iowa.

    DISCUSSION...Overall setup remains similar to this afternoon and
    early evening with a well-defined outflow boundary depicted by
    GOES-EAST IR satellite imagery stretching from central Iowa into
    southern Nebraska, focusing convection overruning to the north
    while progressing northeastward. Meanwhile, an approaching upper
    shortwave over the central/northern High Plains is responsible for
    scattered convection currently over western Nebraska and eastern
    Colorado. This activity is expected to enter central Nebraska by
    about 04Z or so along with scattered thunderstorms maintaining
    along the instability gradient associated with the aforementioned
    outflow boundary.

    PWs remain elevated and in the 1.6-2.1" range (well above
    climatology), along with MLCAPE values of 1000-2000 J/kg.
    Meanwhile, mid-level southerly flow also remains modest around
    25-30 kts and should increase with time in response to the
    approaching shortwave and nocturnal low level jet. This should aid
    in isentropic ascent and greater coverage of intense rainfall
    rates. Latest HRRR, HREF, and experimental RRFS/REFS are all in
    line the potential for an additional 3" of rain over areas that
    have received 2-4" of rainfall over the last 24 hours per MRMS.
    FFG in this region depicts many areas with 3-hrly values under 2"
    and the 18z HREF has a stripe of 30-60 percent exceedence
    probabilities (although probably displaced a bit too far to the
    north given the latest southerly trends and sinking outflow
    boundary). For this reason, additional scattered flash flooding
    tonight is deemed likely.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5q5aAHo5jtn0N35EVSziHMQXrr0MRrchagREUGdhs1Fkohxze_y7_Bk9lay9jrgn3Waq= oO5Lw8Yln8NkX_2reUX8z0U$ for graphic product...

    ATTN...WFO...DMX...FSD...GID...GLD...LBF...OAX...

    ATTN...RFC...KRF...NWC...

    LAT...LON 42549705 42549530 41529504 40359693 39799887=20
    39800057 40320153 41250136 42019923=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 26 07:47:55 2025
    AWUS01 KWNH 260747
    FFGMPD
    IAZ000-NEZ000-SDZ000-261346-

    Mesoscale Precipitation Discussion 0518
    NWS Weather Prediction Center College Park MD
    347 AM EDT Thu Jun 26 2025

    Areas affected...much of Nebraska, western Iowa

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 260746Z - 261346Z

    Summary...Flash flood potential continues - especially near Grand
    Island, NE where 5-10 inches of rainfall has occurred over the
    past 12 hours.

    Discussion...Extensive flash flood impacts have occurred near
    Grand Island, NE earlier, where a couple of convective bands began
    to train over the region and produce 3-6 inches of rainfall over
    the past 6 hours. Since that time, upscale growth and slight
    weakening of convection across south-central Nebraska has enabled
    the heaviest rain to propagate just east of the Grand Island
    region.

    Unfortunately, an upstream mid-level impulse and convergence on
    the nose of 40-kt 850mb flow over Kansas to produce renewed
    convection across west-central Nebraska. These storms will allow
    for continued rainfall and perhaps another 1 inch of rain on top
    of prior significant rainfall, potentially exacerbating impacts
    near the Grand Island area. This additional rainfall risk will
    persist for at least another 3 hours or so (through 1030Z/5:30am
    CDT) until the upstream mid-level impulse passes the region.

    Additional rainfall will persist east of Grand Island through
    Columbus, Omaha Metro, and portions of western Iowa through 13Z/8a
    CDT. Rain rates should remain relatively low with this activity
    due to modest instability and appreciable (30-kt) movement,
    although prior rainfall (as much as 3-5 inches along this axis)
    have lowered FFG thresholds and made ground conditions
    sensitive/conducive for excessive runoff. Another 1-2 inches of
    rainfall along this axis could contribute to isolated/continued
    flash flooding this morning.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!660RDQVwhQ_JLiGJwL0-ycC7Ntvk-y0Ae1_dO8cUkgI72PGxXmyuryxESTa5kOtl_LaH= MAyEbw4WCLQwH0U7emlxWsI$ for graphic product...

    ATTN...WFO...DMX...FSD...GID...GLD...LBF...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43109403 42439339 41599368 40889554 40269810=20
    40150037 40600098 41470061 42119875 42659595=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 26 15:52:37 2025
    AWUS01 KWNH 261550
    FFGMPD
    WIZ000-MNZ000-IAZ000-NEZ000-262130-

    Mesoscale Precipitation Discussion 0519
    NWS Weather Prediction Center College Park MD
    1149 AM EDT Thu Jun 26 2025

    Areas affected...Northern & Western IA...Southern MN...Far Eastern
    NEB...Far Southwest WI...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 261550Z - 262130Z

    SUMMARY...Widely scattered elevated convection with some repeating
    elements will increase in coverage/surface rooting throughout the
    afternoon with 1.5-2"/hr rates and streaks of 2-3.5" totals over
    sensitive solids suggesting possible incidents of flash flooding
    by 21z.

    DISCUSSION...15z Surface analysis shows main surface low near
    Norfolk, NEB with well defined cold front dragging southwest into
    north-central KS east of Hill City; while downstream a pre-frontal
    pressure trof, generally along the core of the deeper layer
    moisture axis/warm conveyor belt extends from another weak low
    near CKP through Omaha/Council Bluffs into northeast KS and is
    well noted by alto-stratus deck with some isolated weaker
    convective cores where sfc to boundary layer convergence is
    maximized across western IA. East of that, clear skies in the
    warm sector extend to the surface front being strongly reinforced
    through differential heating with extensive low-stratus deck along
    the eastern MN/IA border into the Driftless area of SW WI.=20
    SBCAPEs are rising into the upper 3000s J/kg across the clearing,
    though solid southerly WAA/ moisture flux along the pressure trof
    of 35-40kts, isentropic ascent is starting to increase elevated
    convective development along and downstream of the DPVA from the
    upper-level trough. Combine this with highly favorable right
    entrance ascent/divergence across NW IA into south-central MN,
    convection will continue to develop/expand over the next few
    hours.=20=20

    Orientation of the frontal zone to the mean motion of the
    shortwave combined with the steepened isentropes further east,
    ascent pattern across north-central IA/southern-MN should see
    greatest convective development with stronger/broader updrafts.=20
    Combined with increasing flux convergence, efficient rainfall
    production will support rates of 1.5-2"/hr fairly quickly in the
    life-cycle. Additionally, the convergence axis will be broad and
    fairly parallel to the boundary and deeper layer flow to support
    some repeating cell motions/tracks. This will be key toward
    increased overall rainfall totals nearing 3-3.5" locally given
    individual cell motions may limit heavy rainfall duration to those
    1.5-2" hourly totals.=20

    Hydrologically, the area remains very saturated with much of IA
    and southern MN having 0-40cm relative soil moisture ratios within
    the 60-70% range, generally well into the 90th+ percentiles
    helping to have confidence that hourly FFG values of 1-1.5" and
    3hr at 1.5-2" within the area of concern. Combine this with the
    narrow axis of training cells from last night from Colfax/Dodge,
    NEB to Ida/Sac to Humbolt/Wright in IA and Fillmore, MN/Howard, IA
    further compromising upper-soil uptake. Scattered incidents of
    flash flooding will become increasingly likely toward 21z across
    the MPD area.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5_8mSO93A9qsx1cGZVRKMn6SzeJ1LMzQavB1wSmR622XxfJ7gW1yebX37K1_RhN1vL43= U9kCrmT0t150CfHH2NLjUbk$ for graphic product...

    ATTN...WFO...ARX...DMX...FSD...MPX...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 44909147 44539068 43729072 43139170 42659272=20
    41149501 40889599 41289672 41919666 42409646=20
    43649553 44249460 44879298=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 26 19:47:20 2025
    AWUS01 KWNH 261945
    FFGMPD
    NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-DCZ000-WVZ000-270145-

    Mesoscale Precipitation Discussion 0520
    NWS Weather Prediction Center College Park MD
    344 PM EDT Thu Jun 26 2025

    Areas affected...Mid-Atlantic

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 261945Z - 270145Z

    SUMMARY...Increasing number of thunderstorms will producing
    downpours containing hourly rainfall rates >2"/hr in some cases.
    Flash flooding is possible in impacted areas, especially areas
    with saturated soils and within more urbanized communities.

    DISCUSSION...The Mid-Atlantic is caught between a series of
    converging surface boundaries. A back-door cold front is
    approaching from the east, marching through the Delaware Valley
    and slowly making its way towards the northern neck of the
    Chesapeake Bay. To the north and west, a stationary front and the
    added help of a lake breeze off Lake Erie has triggered
    thunderstorms over northeast Ohio that are tracking southeast into
    western PA. Plus, strong surface based heating has been unfolding
    across the region that is causing a burgeoning field of
    cumulonimbus clouds along the Central Appalachians. The 12Z IAD
    RAOB showed a convective temp of 93F, which most areas from
    southeast PA on south through MD and into northern VA have all
    reached as of 19Z. Storms are initiating within an environment
    that is likely to have anywhere from 1,000-2,000 J/kg of MLCAPE
    and PWs that range between 1.75" from western and central PA to
    2.0" from the DC/Baltimore area on east to the northern DelMarVa
    Peninsula. Vertical wind shear soundings show generally weak shear
    aloft, making storm modes largely pulse-like in nature. However,
    outflow boundaries emanating from these first batch of storms will
    fire additional thunderstorms that congeal into larger clusters in
    parts of the Mid-Atlantic this evening.

    The 12Z HREF's probabilistic guidance is keying in on the greater
    DC/Baltimore metro area on north into the Lower Susquehanna Valley
    with the low-to-moderate chances (30-60%, highest probs in the DC
    metro area on east to the MD Eastern Shore) for >3" of rainfall
    between 21-03Z this evening. Farther west, thunderstorms
    propagating southeast from western OH will be a focus for
    additional thunderstorm development, as will areas along and north
    of I-80 where differential heating is becoming more pronounced.
    Some thunderstorms will be capable of producing >2"/hr rainfall
    rates given the available instability and moisture parameters,
    making places with sensitive soils (>80% 0-40cm soil saturation in
    northern WV, western and central PA) and heavier urbanized
    environments particularly susceptible to flash flooding this
    evening. Thunderstorm coverage should begin to fade after 03Z
    given the marginal vertical wind shear aloft and loss of daytime
    heating.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!44u1H162CiRzIW4v0puCGh5DcWdvRc6LmTYRYg6EhoYVUNk91MbCXcA34YBafbFdAMhp= d-vo7yqUw7nQpuTKnICS2gE$ for graphic product...

    ATTN...WFO...AKQ...BGM...CTP...LWX...PBZ...PHI...RLX...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 41827623 41367525 40217554 39507507 38347547=20
    37847628 37867748 37917902 38597966 40078014=20
    40907993 41327907 41587753=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 26 21:01:01 2025
    AWUS01 KWNH 262100
    FFGMPD
    WIZ000-MNZ000-IAZ000-270243-

    Mesoscale Precipitation Discussion 0521
    NWS Weather Prediction Center College Park MD
    459 PM EDT Thu Jun 26 2025

    Areas affected...Central WI...Northeast IA...Southeast MN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 262058Z - 270243Z

    SUMMARY...Thunderstorm coverage will increase along and north of a
    frontal boundary draped over southern WI this afternoon and
    evening. Repeating rounds of strong thunderstorms both along the
    frontal boundary and with assistance from approaching storms from
    the west may cause flash flooding.

    DISCUSSION...20Z surface analysis shows the location of the
    west-to-east oriented frontal boundary well, with a more organized
    complex of storms over southeast MN as a remnant MCV tracks
    towards central WI. Strong 925-850mb theta-e advection is underway
    over the Upper Midwest and will slowly inch the stationary front
    north as a warm front this evening. The influence of this
    low-level theta-e advection is evident in the increasing MUCAPE
    field in central WI as RTMA 3-hr trends show as much as 600-1,000
    J/kg MUCAPE increases over the past 3-hours alone. The Upper
    Midwest remains ideally positioned beneath the diffluent
    right-entrance region of a 250mb jet streak and PWs are steadily
    rising. By 00Z tonight, the highlighted region is expected to see
    PWs range between 1.75-2.0", which is generally above the 97.5
    climatological percentile per ECMWF ensemble guidance. With MUCAPE
    along the boundary near 2,000 J/kg, and even areas as far north as
    Green Bay likely to see up to 500 J/kg of MUCAPE, the stage is set
    for widespread thunderstorms that could contain up to 2"/hr
    rainfall rates.

    Aiding in the efficient rainfall production is the presence of
    vertical wind shear and helicity. Effective bulk shear values >40
    kts and effective SRH values >100 m2/s2 support thunderstorms
    potentially sustaining mesocyclones, which are very efficient
    rainfall producers. In addition, low-mid level RH values are
    averaging close to 90% and warm cloud layers per the 18Z RAP for
    this evening are pegged to be as deep as 13,000ft. West-Central WI
    also sports highly saturated soils with NASA SPoRT-LIS 0-40cm soil
    moisture percentiles well above the 90th percentile. As isentropic
    ascent and low-level moisture advection increase along and ahead
    of the approaching surface trough, there is the concern for
    repeated rounds of thunderstorms in parts of the region. Once the
    cold front approaches the region between 00-02Z, storm motions
    over central WI should be more continuous off to the north and
    east. Until then, however, there is a concern for training storms
    across portions of central WI, far southeast MN, and far northeast
    IA. Flash flooding is possible this evening, particularly in areas
    with sensitive soils and where storms train along and north of the
    frontal boundary in southern WI.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9PrKLtHq8DOxC7ZqVoyNuSVkYvemtuwUdcwVPlfGhdVUgq7Y8wicvr8DPXOXC1wWkZbY= QRfdjODtG7KwXdqHL0K5LVg$ for graphic product...

    ATTN...WFO...ARX...GRB...MKX...MPX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 45329101 45168840 44458740 43388785 43118856=20
    43048972 42779142 43249248 43759278 44959268=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 26 22:04:26 2025
    AWUS01 KWNH 262202
    FFGMPD
    PAZ000-WVZ000-OHZ000-KYZ000-270200-

    Mesoscale Precipitation Discussion 0522
    NWS Weather Prediction Center College Park MD
    601 PM EDT Thu Jun 26 2025

    Areas affected...Eastern OH...Northern WV Panhandle...Southwest PA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 262200Z - 270200Z

    SUMMARY...Ongoing clusters of storms to continue for the next
    several hours, prolonging the flash flood threat into this evening.

    DISCUSSION...Doppler radar shows scattered, slow-moving
    thunderstorms from southwest Ohio and along the Ohio River on east
    to far southwest Pennsylvania. The region does lie at the nose of
    an unusually strong 50kt ESErly 200mb jet located over the
    Southeast. This additional synoptic-scale influence is helping to
    provide some upper-level support in a setup that is otherwise
    heavily driven by daytime heating and nearby mesoscale boundaries
    (outflows, lake breeze off Lake Eire most notably). Storms will
    have as much as 2,000 J/kg of MLCAPE at their disposal through the
    remainder of the afternoon and into this evening. PWs are also
    ranging between 1.8-2.0", supporting the ongoing Excessive
    Rainfall rates being observed in central and southwest OH.

    Additional thunderstorms will likely come about as a result of
    outflow boundaries emanating from ongoing convection, as well as
    outflows colliding with other nearby outflow boundaries. Vertical
    wind shear is light, making these storms highly dependent upon
    cold-pool driven processes and congealing clusters of storms. With
    a couple more hours of daylight to go, more storms are likely to
    take advantage of the unstable/moist environment, as well as from
    the help of an anomalous 200mb jet streak aloft. Additional rounds
    of flash flooding are possible within the highlighted at-risk
    region through the remainder of this afternoon.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-UI0_WE3YdeAaBCDjVGjANfyRYBQFeXH5JajsrwAlwZTdOES9OzNsTm49MaLSml6A27O= tbOy6cI2LB89R-hplSgwzlo$ for graphic product...

    ATTN...WFO...CLE...ILN...IWX...PBZ...RLX...

    ATTN...RFC...TIR...NWC...

    LAT...LON 40848340 40828140 40528027 39738023 39118046=20
    38578168 38708279 38668375 39568409 40608399=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 26 22:58:06 2025
    AWUS01 KWNH 262256
    FFGMPD
    VAZ000-WVZ000-KYZ000-270300-

    Mesoscale Precipitation Discussion 0523
    NWS Weather Prediction Center College Park MD
    655 PM EDT Thu Jun 26 2025

    Areas affected...Southern & Central WV...Southwest VA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 262255Z - 270300Z

    SUMMARY...As rounds of slow moving strong thunderstorms continue
    to flare up this afternoon, additional areas of flash flooding are
    possible. Areas along steep terrain are most at-risk, as well as
    in low-lying valleys.

    DISCUSSION...Thunderstorms flaring up across southwest VA and
    southern WV have had a history of producing Excessive Rainfall
    rates with some elevated streamflow magnitudes evident in and
    around the Radford, VA area. The environment remains favorable for
    at least several more hours with mesoanalysis showing MLCAPE
    values between 1,000-2,000 J/kg and PWs of 1.7-1.9" for much of
    the highlighted area. These storms are also feeling the effects of
    a rather strong ESErly 200mb jet located over the Carolinas. These
    winds are unusual in terms of both strength its direction (ESE)
    which may be allowing for enhanced upper-level divergence over the
    region. Additional thunderstorm development will be largely due to
    outflow boundaries and congealing cold pools. The lack of
    sufficient vertical wind shear should keep these storms relatively
    short-lived (1-2 hours generally), but given the environmental
    parameters and some synoptic-scale support aloft, as much as 2-4"
    worth of rainfall could occur within the next few hours within the
    more intense storms. With that said, additional flash flooding is
    possible for the remainder of the afternoon and into this evening.
    Areas most at-risk are within low-lying valleys or along steep
    terrain.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4zH1lzES44c8WhQPNcoHxBUmakDdQj_gL4LajHoUlUdGRQj6MiOBPUM1mmo9otuxz60o= PoUzXPapyo8V70w4TgTLPhk$ for graphic product...

    ATTN...WFO...JKL...RLX...RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 39238006 38417985 37887970 37317950 36928001=20
    36948088 37148183 37698229 38398226 38728112=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 27 01:54:38 2025
    AWUS01 KWNH 270154
    FFGMPD
    MDZ000-VAZ000-DCZ000-270450-

    Mesoscale Precipitation Discussion 0524
    NWS Weather Prediction Center College Park MD
    952 PM EDT Thu Jun 26 2025

    Areas affected...Northern VA...Eastern MD

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 270150Z - 270450Z

    SUMMARY...Thunderstorms will continue across portions of northern
    VA and eastern MD for a few more hours. Hourly rainfall rates up
    to 2"/hr are possible with urbanized areas most prone to flash
    flooding.

    DISCUSSION...Outflow boundaries emanating from several different
    afternoon thunderstorm complexes have collided over northern VA,
    while a cold front races in from the DelMarVa Peninsula. This cold
    front is helping to ignite thunderstorms near Annapolis while the
    outflows have triggered storms from the southern Capital Beltway
    on west to the south of Interstate 66. The 00Z IAD RAOB shows
    depicts a more tropical air-mass aloft, highlighted by PWs of
    2.34" and MUCAPE >3,500 J/kg. This atmospheric setup is resulting
    in tropical-downpour rainfall rates with MRMS 15-minute
    radar-estimated rainfall rates ranging between 0.5-1.0" within the
    storms stretching from Routes 28 & 17 on east towards the MD
    Eastern Shore. The lack of vertical wind shear should ultimately
    lead to these cells dissipating within the next few hours.
    However, these storms are packing quite the punch with >2.0"/hr
    rainfall amounts likely to be realized in some of these areas. The
    flash flood threat continues across northern VA on east to the MD
    Eastern Shore this evening with the more urbanized communities
    within the "DMV" most at-risk for flooding should storms ensue
    over more densely populated locations.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-3uVZE8jo8fpOXVfUcofGTXdgVnK-OgMeMcVQbJm7ATeJrEqQF5NbhcCbTw4m8SkDQZ1= nCxzP2WssMx6sm3QhsL_Q30$ for graphic product...

    ATTN...WFO...AKQ...LWX...PHI...RNK...

    ATTN...RFC...RHA...NWC...

    LAT...LON 39157657 39157618 38967600 38677591 38467602=20
    38137631 37907662 37577726 37427752 37337803=20
    37397831 37517855 37707882 37827904 38027932=20
    38357925 38597901 38807864 38977821 39117766=20
    39127715=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 27 05:10:37 2025
    AWUS01 KWNH 270510
    FFGMPD
    MOZ000-KSZ000-270908-

    Mesoscale Precipitation Discussion 0525
    NWS Weather Prediction Center College Park MD
    109 AM EDT Fri Jun 27 2025

    Areas affected...northern/central Missouri

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 270508Z - 270908Z

    Summary...A complex of strong convection near/northeast of Kansas
    City was prompting training storms and areas of 1.5+ inch/hr rain
    rates. Flash flooding is possible as storms migrate from west to
    east across the discussion area through 09Z/4am CDT.

    Discussion...Over the past hour or so, convection along an axis
    from near Topeka, KS to near Kirksville, MO has grown upscale into
    a linear complex oriented parallel to modest steering flow aloft.=20
    The presence of 25 knots of 850mb flow has also aided in
    organization while maintaining influx of a very moist/unstable
    airmass (2+ inch PW values and 1000 J/kg MLCAPE) into the complex.
    A series of weak midlevel shortwave troughs just upstream of the
    complex have also fostered continued convective development. The
    orientation of the cells has fostered training, with recent MRMS
    estimates of 2 inch/hr rain rates now noted about 30 miles
    southwest of CDJ/Chillicothe, MO.

    Despite modest boundary layer cooling, both observations and model
    guidance suggest that the ongoing complex should continue for at
    least another 2-4 hours tonight while continuing to maintain an
    orientation for training cells. 2 inch/hr rain rates should
    continue to threaten FFG thresholds across the region while
    translating very slowly southward and eastward in tandem with the
    complex. The orientation/propagation of the complex should spread
    the risk of heaviest rainfall toward the I-70 corridor in central
    Missouri through 09Z/4am CDT. Flash flooding will also remain
    possible through that time.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7DoO1EKEqme3-4D7dNd9oThczapU6sVC65R8Rxs7OBBlVoKxYJiaEMeMjzKAMtFQvZ2T= y7DVdGrOAFb8fN8U7gHGljc$ for graphic product...

    ATTN...WFO...EAX...LSX...SGF...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 39739370 39579222 39139136 38619153 38599392=20
    38989467 39429485=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 27 15:29:43 2025
    AWUS01 KWNH 271529
    FFGMPD
    GAZ000-TNZ000-KYZ000-ALZ000-MSZ000-272100-

    Mesoscale Precipitation Discussion 0526
    NWS Weather Prediction Center College Park MD
    1129 AM EDT Fri Jun 27 2025

    Areas affected...Middle TN...Northern AL...South-central KY...Adj
    Northeast MS & Northwest GA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 271530Z - 272100Z

    SUMMARY...Highly focused/efficient heavy rain bursts with
    localized 2-2.5" in less than 90 minutes may pose similarly
    focused incidents of flash flooding, particularly near urban
    areas.

    DISCUSSION...A very humid/unstable airmass exists across Middle TN
    extending into south-central KY and northern AL. GOES-E WV suite
    shows a very broad, well defined TUTT (Tropical upper-tropospheric
    trough) cell retrograding across the southeast with the core over
    central GA attm; resulting in an area of enhanced low to mid-level
    moisture (per CIRA LPW) and clearing across the area of concern.=20
    Thermal profiles denote solid saturation, weak capping and just
    small adjustments of the surface profiles result in large MLCAPE
    values over 3000-4000 J/kg. With solid morning insolation in the
    clearing east of the outer cirrus deck of the TUTT cells,
    temperatures are already reaching required values for convective
    initiation reaching mid-80s and Tds in the mid to upper 70s.=20
    Visible imagery and RADAR mosaic show the incipient boiling Tcu
    expanding across southern Middle TN into N AL. Combined with the
    best heating, there is some modest upper-level divergence at the
    western exit of the 40-50kt 3H jet on the northeast side of the
    TUTT before it arcs northward across central KY. As such,
    stronger updrafts will become scattered to numerous but given weak
    inflow in the low levels should remain narrow initially.

    Overall vertical loading of the available moisture given strength
    of the updraft should support wet-microburst/pulse downdrafts
    capable of 2-2.25" totals in sub-hourly to hourly duration.=20
    Outflows will trigger next updraft development and any colliding
    outflows will result in a larger slab ascent for the subsequent
    up/downdraft cycles; though similar results are likely to occur of
    up to 2" totals. Overall the pattern support a broad outward
    propagation from the initial centroid over southern TN/N AL more
    in line with the 12z ARW solutions.=20

    Any flash flooding is likely to be limited in areal coverage
    (though broadening slightly with each cycle/broader downdrafts,
    but still sub-county focused); with greatest potential across
    impermeable surfaces near urban centers. However, 1hr FFG values
    are in the 1.5-2" range across S TN/northern AL where 0-40cm
    relative making potential a bit greater in these areas.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!63GCCt2wWdVbrzxIQgMnreX_Gls426haxKUJ5YmUot8d5SR6BCXB7_oIlOoCQyrz95hR= 4L-_vWHRmxS38hSR6jrG_cU$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...JKL...LMK...MEG...MRX...OHX...
    PAH...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 37668597 37468452 36938414 36328424 35578470=20
    34578524 33828582 33498674 33878818 34658876=20
    35698870 36788797 37398707=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 27 16:52:18 2025
    AWUS01 KWNH 271652
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-272300-

    Mesoscale Precipitation Discussion 0527
    NWS Weather Prediction Center College Park MD
    1251 PM EDT Fri Jun 27 2025

    Areas affected...Eastern WV...Western and Northwestern
    VA...Western PA...Far Western MD...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 271700Z - 272300Z

    SUMMARY...Incidents of flash flooding, potentially significant,
    are likely to increase over the next few hours in complex/steep
    terrain.=20

    DISCUSSION...GOES-E Visible imagery shows well defined CAD due to
    back-door cold front dropping through the Mid-Atlantic this
    morning. The cold front has pressed to just south of the VA/NC
    boarder and has banked up through the Blue Ridge toward the
    Eastern Continental Divide Ridge in the wind field but the stratus
    deck leaves about 25-50 miles of gap of clearing with strong Td
    gradient even a few more miles further into the stratus deck. As
    such, surface Tds to low to mid-70s are pooled along the front
    from SW NY across W PA into the central Appalachian Range. As
    further insolation occurs temperatures are rising into the low to
    mid-80s and modified (deeply saturated) 12z RAOB profiles from PBZ
    and RAP suggest solid MLCAPEs of 2000 J/kg are probable toward
    peak in the next hour or two even with a narrow-skinny profile.=20
    Total moisture profiles remain above normal in the 1.75-2" range.=20


    Upstream, the tail end of enhanced moisture and low-level
    southwesterly speed max provided enough ascent to break out a
    cluster of thunderstorms which is starting to develop southward
    into SE OH; this is a timing of enhanced upslope flow from the
    west with increased moisture/higher theta-E air downstream of the
    main upper-level trof over the Great Lakes. This will combine
    with strengthening upslope flow from the moist post-frontal 'cold'
    air damming (CAD) further strengthening moisture flux convergence
    to break out scattered to numerous thunderstorms across W PA
    toward E WV/NW VA. This is likely to persist throughout the
    afternoon into evening given upstream trof strength and
    approaching height-falls. So while deep layer steering may lead
    to eastward propagation into the stable air across central PA into
    the Capital District region, favorable upstream
    redevelopment/flanking line support is probable for multiple
    up/downdraft cycles with main motions driven by cold pools/outflow
    likely southward into west-central VA/SE WV through the evening
    hours. Total deep layer moisture, strong updraft/unstable
    environment will support solid flux to support 2"/hr rates and
    given the aforementioned motions this may support localized totals
    of 2-4" in short-duration. Given complex cell motions and shear
    rainfall intensity expected, an incident or two of considerable to
    significant flash flooding is plausible as well.

    Given naturally lower FFG values due to complex terrain, flash
    flooding is considered likely; yet, recent heavy rainfall will
    further limit infiltration to the saturated deeper soil profiles,
    especially in SW PA where 0-40cm soil moisture remains well into
    the 90th percentile.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6tCpTMK-blfFSlmSnb5X2ivIL_Eei3kCEC7Y139eCbDnU8GpvmGbYuV65-PFrzjTKTEh= tk2ooJI7YemysqXdbLvCxzY$ for graphic product...

    ATTN...WFO...CTP...LWX...PBZ...RLX...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 41917883 41507851 40387890 39577797 39037791=20
    38607814 37817889 37098013 37348123 38178071=20
    39687991 40358027 41198027 41617949=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 27 17:31:44 2025
    AWUS01 KWNH 271731
    FFGMPD
    NYZ000-PAZ000-OHZ000-272230-

    Mesoscale Precipitation Discussion 0528
    NWS Weather Prediction Center College Park MD
    130 PM EDT Fri Jun 27 2025

    Areas affected...Northeast OH...Northwest PA...Western Upstate
    NY...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 271730Z - 272230Z

    SUMMARY...Narrow corridor of unstable air. Multiple rounds of efficient/intense thunderstorms may result in spots of 2-4" and
    possible localized flash flooding through the evening.

    DISCUSSION...GOES-E shows developing thunderstorms within a narrow
    unstable axis between the colder Lower Great Lakes and a strong
    differential heating boundary due to low level stratus across
    central NY and PA. Insolation has lead to temperatures reaching
    the mid-80s, but return southerly flow both along the western edge
    of the stratus and southwesterly upslope flow out of the Ohio
    Valley continues to transport fairly moist low level moisture into
    the mid-70s. Short-wave ridge aloft is starting to shift out of
    the region, though oblique right entrance ascent pattern remains
    across the area to help to aid updrafts starting to develop
    upstream of the mean height-falls across northern OH. As such a
    narrow axis of 1500-2000 J/kg of MLCAPEs exists along the Lakes
    and will act to corral upstream development helping increase the
    potential for cells to repeat/train as the main forcing presses
    through this evening.

    The downstream cells are likely to remain fairly stationary given
    upstream propagation vectors with south/southwesterly inflow and
    strong stability gradient to the east. Total deep layer moisture
    nearing 2", will support efficient rainfall and rates of
    1.75-2"/hr. Given the development environment/potential for
    repeating, there is potential for some localized totals of 2-4",
    which may result in possible incidents of flash flooding through
    the afternoon into evening hours especially in proximity to larger
    urban centers.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7vWCktZ-AWBMfgI_do6X0cG-RFDKQF_MdUkknzCl76oituZYuCEDMiNNv4aF71OPRUhp= WwR-NRwaolM2xGyPNBskE2Y$ for graphic product...

    ATTN...WFO...BGM...BUF...CLE...CTP...PBZ...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 43387739 42967668 42107748 41297919 40588163=20
    41368223 42048066 42677922 43327901=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 27 18:04:10 2025
    AWUS01 KWNH 271803
    FFGMPD
    ILZ000-MOZ000-ARZ000-OKZ000-KSZ000-280000-

    Mesoscale Precipitation Discussion 0529
    NWS Weather Prediction Center College Park MD
    203 PM EDT Fri Jun 27 2025

    Areas affected...The Ozarks

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 271801Z - 280000Z

    Summary...Showers and thunderstorms expanding across Missouri will
    intensify through the afternoon. Rainfall rates may peak above
    2"/hr at times within these slow moving storms, possibly leading
    to instances of flash flooding.

    Discussion...The regional radar mosaic this afternoon shows
    convection rapidly expanding along what appears to be an old
    outflow boundary downstream of a cold front draped NE to SW across
    southern Missouri. Ascent along this boundary is occurring due to
    convergence, but is being aided by synoptic lift through the RRQ
    of a jet streak arcing to the northeast and a shortwave moving
    eastward across KS. This lift is impinging into robust
    thermodynamics characterized by a ribbon of PWs of over 2 inches,
    near record for the date, combined with SBCAPE over 3000 J/kg
    fueled by steep lapse rates within the 850-600mb layer noted on
    the morning regional UA soundings. In this environment,
    thunderstorms have rapidly blossomed, with additional updrafts
    quickly expanding as noted on the GOES-E day-cloud phase RGB,
    suggesting the rain rates that are currently estimated to be above
    2"/hr from KSGF will only intensify the next few hours.

    Storms that have developed already are not moving quickly. The
    0-6km mean wind is only around 10 kts to the NE, but more
    concerning are Corfidi vectors aligned anti-parallel to the mean
    wind and collapsed to just 5 kts or less. This is dictating the
    slow storm motion already noted, and will support backbuilding of
    echoes into the greater instability to the SW as 850mb inflow
    remains from the W/SW at 10-20 kts. This will result in some areas
    receiving multiple rounds, or experiencing a long duration, of
    heavy rainfall. With the HREF (REFS) probabilities for 2"/hr
    reaching 20-30% (30-50%), this suggests brief rain rates of 3"/hr
    are also likely, which is additionally supported by HRRR 15-min
    rainfall peaking around 0.75" through this evening. Where these
    rates train or stall through backbuilding, 2-3" of rainfall is
    expected, with locally as much as 5" possible.

    The slow movement of these intense rates could quickly overwhelm
    soils leading to runoff, especially in urban areas. However, NASA
    SPoRT 0-40cm soil moisture also reflects recent wetness across the
    area, as soil moisture near the AR/MO border and into far eastern
    OK are in the 80th-90th percentile. Despite FFG that is quite high
    across the region (2.5-4"/3hrs), there is at least a 20-30% chance
    of exceedance due to the slow movement of these intense rain
    rates, further suggesting the increasing flash flood risk through
    this evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4Vh1-2_CCShQunh7CZpg9lXZ8zlwnD-xm7TXgSoFXQ0Snjn1HT9n5l4qJTVQO1-kDfOw= mpb4JEReYSI6G0ZNSE7B3oo$ for graphic product...

    ATTN...WFO...ICT...LSX...LZK...MEG...PAH...SGF...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38689096 38559036 38109002 37728990 37079024=20
    36249096 35739195 35489287 35449416 35609524=20
    35819583 36269632 36779633 37219599 37589502=20
    38039353=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 27 18:13:44 2025
    AWUS01 KWNH 271813
    FFGMPD
    TXZ000-NMZ000-280000-

    Mesoscale Precipitation Discussion 0530
    NWS Weather Prediction Center College Park MD
    212 PM EDT Fri Jun 27 2025

    Areas affected...Southeast New Mexico...Western Texas Panhandle...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 271815Z - 280000Z

    SUMMARY...Slow moving thunderstorm clusters (mainly near mountain
    ranges) capable of 1.5"/hr rates and localized totals to 2.5" may
    induce flash flooding conditions, especially

    DISCUSSION...GOES-E Visible imagery shows convective activity
    breaking through old convective debris in proximity to axis of
    deep layer enhanced moisture. CIRA LPW notes return surface
    moisture has pushed up through the Davis mountains toward the
    southern Sacramento Range with upper 50s to low 60F Tds; the
    850-500mb layers, show the core axis of moisture though the
    southwestern edge of the exiting northern stream trough and the
    western edge/influence of the Tropical Upper-Tropospheric Trough
    (TUTT) cell over S Nuevo Leon; bring overall moisture totals to
    1.25-1.5" around the 90-95th percentile. The old MCV appears to
    be providing solid deep layer confluence/convergence in proximity
    to the terrain for enhanced upslope for stronger thunderstorm
    activity and with ample buoyancy with 1000+ J/kg of CAPE, moisture
    flux will support rates of 1-1.5"/hr in the cores.

    With the shortwave/old MCV in close proximity and deep layer
    steering generally weak, drawing toward the northeast; cell
    motions will be slow to allow for further duration along the
    terrain and supporting localized totals up to 2-2.5", with highest probabilities within the Davis Mountains into the southern
    Sacramento Range. This places a few fresher burn scars at risk of
    being hit further enhancing the potential of rapid runoff and
    mud/debris slides. As such, flash flooding is considered possible
    through the late evening.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_v6QSyi7DecHMe43juVS_Xl6PN0XsbUbhKR7HuAyDdGYc7PA_Pi3pit4JJHjIpLokUtI= NmPgsEoAjxod_IbjZwxM3vc$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...NWC...

    LAT...LON 34350560 33910486 33660387 33620316 32880314=20
    32590358 32160375 31460333 30680299 30280307=20
    30000352 29950405 30340471 30830515 31170557=20
    31760592 32580611 33180646 33950626=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 27 18:41:45 2025
    AWUS01 KWNH 271841
    FFGMPD
    FLZ000-280045-

    Mesoscale Precipitation Discussion 0531
    NWS Weather Prediction Center College Park MD
    241 PM EDT Fri Jun 27 2025

    Areas affected...Florida Peninsula

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 271845Z - 280045Z

    Summary...Slow moving thunderstorms along the sea breeze boundary
    will drift slowly westward or stall through the evening. Rainfall
    rates of 2-3+"/hr are likely, which could result in isolated
    rainfall amounts approaching 5". Isolated flash flooding is
    possible.

    Discussion...The regional radar mosaic this afternoon shows
    widespread showers and thunderstorms ongoing along the east coast
    of the Florida Peninsula. These storms are blossoming within
    impressive thermodynamics characterized by SBCAPE of 3000-5000
    J/kg overlapped with PWs above 2 inches. Although deep layer
    ascent is modest beneath an upper ridge, convergence along this
    sea breeze will continue to force updrafts to drive convection,
    with additional storms developing along outflows and storm mergers
    within a region of weak 0-6km bulk shear.

    Radar-estimated rainfall rates from KMLB have been as high as
    2"/hr already this aftn, but storm lifetimes have been short in
    the pulse environment. This is likely to remain the evolution
    through tonight, but guidance indicates that a plume of enhanced
    bulk shear may spread into eastern FL this evening, helping to
    force at least modest storm organization as outflows and storm
    mergers occur. This could enhance the duration of heavy rainfall
    in a few areas as clusters move chaotically across the region due
    to the offsetting motion between the westward advancing sea breeze
    and mean S/SW 0-6km wind. With rainfall rates forecast by both the
    HREF and REFS to have a moderate chance (40-60%) of exceeding
    2"/hr, and the HRRR 15-min rainfall indicates up to 1" at times
    (short duration 4"/hr rainfall), these slow motions could produce
    2-4" of rain with higher amounts above 5" possible (10-20% chance)
    in isolated locations.

    There remains uncertainty into exactly where the heaviest rain
    will occur through this evening, but the pinned sea breeze and
    resultant clusters of storms should force the focus to be from the
    Space Coast southward as shown by HREF and REFS PMM, and supported
    by the synoptic flow. While FFG is high across the area, should
    any of these storms stall across the urban east coast, instances
    of flash flooding could result.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6OhYw0UuIKzzosHS_vuSFQyotQ3x8U_v3PGqXJG0XXBnjiv6SHB_7E0ME90OhGvOzZp1= jV55Kr030FeoCFfoZ1T4m3E$ for graphic product...

    ATTN...WFO...JAX...MFL...MLB...TBW...

    ATTN...RFC...ALR...NWC...

    LAT...LON 29348116 29138085 28498036 28018026 26847986=20
    26187995 25658018 25488036 25618048 25948073=20
    26408098 26958121 27648140 28348149 28998140=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 27 20:36:49 2025
    AWUS01 KWNH 272035
    FFGMPD
    VAZ000-NCZ000-WVZ000-SCZ000-OHZ000-GAZ000-TNZ000-KYZ000-280230-

    Mesoscale Precipitation Discussion 0532
    NWS Weather Prediction Center College Park MD
    434 PM EDT Fri Jun 27 2025

    Areas affected...Central to Southern Appalachians

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 272033Z - 280230Z

    Summary...Scattered pulse thunderstorms will develop through the
    evening across the Central and Southern Appalachians. Rainfall
    rates may briefly reach 3"/hr, producing short duration rainfall
    of 1-2". This could result in instances of flash flooding.

    Discussion...The GOES-E visible imagery this afternoon shows
    widespread convective development across the Appalachians. In
    general, these cells are discrete and scattered in a weakly forced
    environment, but local enhancement due to terrain features or
    storm mergers/outflow collisions have resulted in scattered
    clusters across the region as well. Thermodynamics today are
    favorable for heavy rainfall as PWs of 1.5 to 1.75 inches are
    collocated with SBCAPE of 2000-3000 J/kg. Forcing for ascent is
    generally provided via low-level upslope flow into the terrain and
    surface convergence along mergers/collisions, but weak diffluence
    aloft is also providing modest ascent in the area. Together, this
    ascent working into the favorable environment has produced
    radar-estimated rain rates of 1.5 to 2 inches per hour.

    The CAMs are in generally good agreement that scattered
    thunderstorms will continue to develop and move chaotically
    through loss of instability or convective overturning this
    evening. Mean 0-6km winds of just 5-10 kts combined with minimal
    bulk shear will provide a setup that supports primarily pulse
    convection with limited temporal duration. However, both the HREF
    and REFS ensembles indicate a moderate to high chance (50-70%) of
    at least 1"/hr rates leading to short-term rainfall as much as
    1-2", and 15-min rainfall from the HRRR as much as 0.75" (brief
    3"/hr rates). With storms expected to just drift across the area,
    any storm that occurs atop sensitive terrain or more urban areas
    could result in instances of flash flooding.

    While the threat is expected to be generally isolated, there is
    some potential in the next few hours of a more focused area of
    convection in KY and eastern TN. Here, pulse storms developing to
    the east will drift NW (along with outflows) and potentially merge
    with clusters coming out of the west. Some merging of these cells
    is shown, albeit with a lot of spatial spread, on the HRRR,
    NAM3km, and RRFS, which could briefly enhance the convection and
    accompanying heavy rainfall rate. Should this occur over some of
    the more sensitive soils (FFG as low as 1.5-2"/3hrs) it could
    cause a slightly higher risk for instances of flash flooding than
    the more isolated pulse type storms forecast across most of the
    area.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5i5gGy-GjUUQ_3mf5l7eCJCUSsq73Lp0t65-bkUqYqqbT4H_31ah0VArZtE9Ma0vKEPn= pTdpHPl5fO6pdtLYlmQDyg0$ for graphic product...

    ATTN...WFO...FFC...GSP...ILN...JKL...LMK...MRX...OHX...RLX...
    RNK...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 38768309 38568231 38268169 38058093 37368059=20
    36588093 35798137 35338181 34908248 34538358=20
    34528441 34818500 35458507 37038477 38368414=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 27 21:35:18 2025
    AWUS01 KWNH 272135
    FFGMPD
    GAZ000-TNZ000-KYZ000-INZ000-ALZ000-ILZ000-MOZ000-ARZ000-280200-

    Mesoscale Precipitation Discussion 0533
    NWS Weather Prediction Center College Park MD
    534 PM EDT Fri Jun 27 2025

    Areas affected...Western Kentucky, Central and Western Tennessee

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 272133Z - 280200Z

    Summary...Clusters of showers and thunderstorms will continue to
    lift slowly northward into the evening. Rainfall rates of 2"/hr or
    more will result in 1-3" of rain with locally higher amounts
    possible. This may result in instances of flash flooding.

    Discussion...The regional radar mosaic shows clusters of
    thunderstorms continuing to move slowly across central and western
    Tennessee this evening, with additional storms pushing into
    southern Kentucky. This convection has been ongoing for several
    hours, but is maintaining intensity due to 925-850mb winds drawing
    more robust thermodynamics (PWS 1.9 inches and SBCAPE above 3000
    J/kg) northward for support. Convection is continuing to deepen
    and regenerate as noted via the GOES-E day-cloud phase RGB which
    shows both fresh updrafts and overshooting tops in a region of
    increased Lightning Cast probabilities. Rainfall rates within this
    convection have been estimated via KOHX and KHPX WSR-88Ds to
    exceed 2, and even 3, inches per hour this aftn.

    During the next few hours, despite the modest 850mb inflow (15
    kts), convection should sustain as it lifts slowly northward in
    advance of a weak shortwave across south-central TN. Weak overall
    forcing and negligible bulk shear will maintain generally pulse
    type thunderstorms, but mergers and outflow collisions will help
    support at least periodic brief organization into clusters, and
    result in additional convective development. Rainfall rates should
    remain intense, reaching 2-3"/hr at times as reflected by HREF and
    REFS probabilities, with HRRR 15-min rainfall exceeding 0.75" in
    some places suggesting brief rates even above 3"/hr. With storm
    motions progged to remain slow on 0-6km mean winds of just 5-10
    kts, this could cause total rainfall of 1-3" with locally higher
    amounts in some areas.

    Soil moisture across TN and KY is generally above normal according
    to NASA SPoRT, reaching above the 90th percentile with respect to
    0-40cm depths in some areas. However, extrapolating out the
    current reflectivity for several hours, and combining this with
    the HREF/REFS probabilities for 3"/6hrs, suggests the greatest
    risk for heavy rain will actually occur atop the less sensitive
    antecedent soils of western KY and TN. This may somewhat limit the
    flash flood risk as the FFG is higher across those areas. However,
    the slow movement of these intense rainfall rates, at least
    through the onset of nocturnal stabilization, could still promote
    instances of flash flooding even as they become become more
    isolated the next few hours.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-TEmpHV95G-AZyzDNgB1RAWIIq1eQi8AKnFAmyuECQWjh0mqCfy4-T9YqJFvpeBgipjZ= tQ3tiVyj9nO7j0QNANEw_W0$ for graphic product...

    ATTN...WFO...FFC...HUN...JKL...LMK...MEG...MRX...OHX...PAH...

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 38028600 37458537 36728473 35968479 35088506=20
    34918541 34998572 35278638 35518702 35398809=20
    35168889 35078979 35449004 36408944 37318866=20
    37968720=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jun 27 22:52:54 2025
    AWUS01 KWNH 272252
    FFGMPD
    PAZ000-MDZ000-VAZ000-NCZ000-WVZ000-280400-

    Mesoscale Precipitation Discussion 0534
    NWS Weather Prediction Center College Park MD
    652 PM EDT Fri Jun 27 2025

    Areas affected...Central Appalachians and interior Mid-Atlantic
    states

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 272251Z - 280400Z

    Summary...Showers and thunderstorms are expected to increase in
    coverage along a stalled front through this evening. Rainfall
    rates within this convection will increase to 1-2"/hr, producing
    1-3" of rain in just a few hours, with locally higher amounts
    possible. This rain falling atop saturated soils and sensitive
    terrain may result in flash flooding.

    Discussion...The fading GOES-E visible imagery this evening
    combined with the GLM flash-extent lightning density product
    indicate that convection is continuing to expand and intensify
    across the Central Appalachians and Mid-Atlantic. These storms are
    developing most robustly within areas not worked over by aftn
    thunderstorms, especially across VA and eastern WV where SBCAPE
    above 3000 J/kg is sampled by the SPC RAP analysis. This
    instability is working in tandem with PWs of 1.7 to 1.9 inches,
    well above the 90th percentile according to the SPC sounding
    climatology, to support intense rain rates. Into these
    thermodynamics, ascent is being produced by broad height falls
    downstream of a longwave trough axis to the west, modestly
    diffluent 300mb flow, and most impressively by upslope/isentropic
    ascent of the low-level winds emerging out of the SW. This SW flow
    is impinging into a stalled back door type cold front, creating an
    impressive theta-e and instability gradient into which storms are
    expected to strengthen.

    During the next few hours, convection over PA/WV should wane in
    response to nocturnal overturning within a lack of significant
    bulk shear. However, areas to the south from the Laurel Highlands
    through the WV Panhandle and into central VA are likely to become
    the focus for additional development. This is supported by the
    simulated reflectivity of the CAMs, including recent HRRR and RRFS
    runs. These solutions are favored as the evolution matches the
    conceptual model for the next several hours, with storms
    developing along the front and any outflows/mergers, and then
    tracking slowly along the aforementioned gradients. With rain
    rates expected to peak above 2"/hr (15-25% chance) and 15-min
    rainfall peaking above 0.75" according to the HRRR, slow and
    chaotic storm motions of just around 5 kts could result in 1-3" of
    rainfall with locally higher totals.

    This region has experienced well above normal rainfall the past 10
    days, as evidenced by AHPS rainfall departures that are in some
    places 150-300% of normal. This has produced widespread 0-40cm
    soil moisture above the 95th percentile, further compromising FFG
    below the natural sensitivity of the region due to terrain. This
    further reflects the concern through early tonight as slow moving
    torrential rain rates result in rapid runoff and potential
    instances of flash flooding.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7o1o6Sm_X2AtsGzhseKab0cgQ5SlAV01Qg54KovfYKg9zmCIiRgVDzT9IatSxH--d9Bh= rj6Kj4Kg_GiOwka4BZIkcoc$ for graphic product...

    ATTN...WFO...AKQ...CTP...LWX...PBZ...RAH...RLX...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 41497931 41257868 40247835 39277838 38087830=20
    37487817 36857828 36537863 36617936 37008018=20
    37668078 38748089 39978071 41068002=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 28 00:17:47 2025
    AWUS01 KWNH 280017
    FFGMPD
    GAZ000-ALZ000-MSZ000-280430-

    Mesoscale Precipitation Discussion 0535
    NWS Weather Prediction Center College Park MD
    817 PM EDT Fri Jun 27 2025

    Areas affected...Northwest Georgia, Northern Alabama

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 280016Z - 280430Z

    Summary...Clusters of showers and thunderstorms will continue to
    drift across Georgia and Alabama through the next several hours.
    Rainfall rates may pulse up to 2-3"/hr at times during collisions,
    potentially leading to instances of flash flooding.

    Discussion...An impressive cluster of thunderstorms has developed
    over northern GA this evening, while a secondary cluster of
    slightly less intensity is drifting northward over central AL.
    These thunderstorms are blossoming despite a weakly forced
    environment in response to robust thermodynamics characterized by
    PWs of above 1.75 inches overlapping MLCAPE of 2500 J/kg. Despite
    modest ascent and negligible shear, leading to pulse type
    convection, the robust environment is supporting rapid updraft
    growth on outflow boundaries and during storm mergers, resulting
    in the clusters currently analyzed on the regional radar mosaic. Radar-estimated rainfall rates have been extreme in northern GA,
    more than 2.5"/hr, leading to rainfall of more than 2 inches in
    the past hour at some of the local mesonet stations, and multiple
    FFW issuances from WFO FFC.

    The CAMs are struggling to handle the coverage of convection this
    evening, leading to lower than typical confidence for the next few
    hours. Although it is likely that convective overturning and a
    loss of daytime heating/destabilization should result in a gradual
    downturn of thunderstorm activity (coverage and intensity), the
    environment for NW GA and northern AL appears favorable for a few
    more hours of thunderstorms with intense rainfall rates, despite
    minimal agreement in the CAMs about coverage or placement of
    convection. Multiple outflow boundaries noted on the national
    radar composite are all functioning as initiation points for
    additional cells, and these may merge over northern AL. Where this
    is progged to occur, MLCAPE is well over 2000 J/kg, and mean 0-6km
    winds are just 5 kts with chaotic and collapsed Corfidi vectors.
    This suggests that as storms develop along these boundaries, or
    due to storm mergers, they will continue to support impressive
    rainfall rates for which the HREF suggests have a 10-20% chance of
    exceeding 2"/hr, leading to 15-min rainfall that may reach 0.75"
    according to the HRRR (3"/hr rates). The slow and chaotic motion
    of these will cause some places to get repeating rounds or a
    longer duration of rain, causing as much as 3" of rain in a few
    areas.

    0-40cm soil moisture across much of AL and NW GA is saturated
    above the 95th percentile, leading to FFG that is as low as
    1.5-2"/3hrs, especially over northern AL. The intensity of the
    anticipated rainfall, combined with the slow motion of developing
    storms, could exceed these thresholds through around 04Z leading
    to instances of flash flooding.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-B7HvunQMIyxYTw1yPmMFjBTsLI2FbLkQcZphIBR-RFhmN_RdIglxW0hZnGnsxHD4KIY= pImIXxKoEYZiK73I7YSIEiQ$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...MEG...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34908671 34808519 34558399 34098355 33358340=20
    32758353 32538403 32528487 32878597 33288754=20
    33528795 34208832 34898810=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 28 01:35:16 2025
    AWUS01 KWNH 280134
    FFGMPD
    MNZ000-SDZ000-NDZ000-280700-

    Mesoscale Precipitation Discussion 0536
    NWS Weather Prediction Center College Park MD
    933 PM EDT Fri Jun 27 2025

    Areas affected...Eastern and Central North Dakota

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 280132Z - 280700Z

    Summary...Supercells blossoming over North Dakota will steadily
    intensify and grow upscale tonight. This convection will contain
    rainfall rates that could exceed 2"/hr at times, leading to
    stripes of 1-3" of rainfall. Flash flooding is possible.

    Discussion...The regional radar mosaic combined with the GLM flash
    extent density product this evening shows a rapid uptick of both
    coverage and intensity of thunderstorms across central North
    Dakota. This activity is strengthening in response to increasing
    ascent downstream of a shortwave moving out of western North
    Dakota with additional ascent provided via the LFQ of a modest
    upper jet streak and the slow increase in convergence along the
    nose of the 850mb LLJ. This LLJ is still modest, measured via VWPs
    across South Dakota at 20-25 kts from the south, but should
    steadily climb the next several hours to 30-40 kts. This will not
    only increase ascent, but also draw more impressive thermodynamics
    northward as PWs surge to 1.75 inches and coincident with MUCAPE
    surging to 3000 J/kg.

    This evolution downstream of the developing thunderstorms should
    promote an environment to support rapid growth and organization
    across central and eastern North Dakota. As the LLJ ramps up to
    improve the thermodynamics, it will additionally increase shear to
    40-50 kts to support both supercells and potentially an MCS.
    Although mean 0-6km winds are likely to remain progressive to the
    east at 25-35 kts, aligned Corfidi vectors suggest training is
    likely, especially along the typical SW flanks and outflows as
    convection shifts east and the LLJ veers subtly more to the SW.
    These intense thermodynamics will support rainfall rates for which
    the HREF indicates has a 10-20% chance of exceeding 2"/hr, from
    which the HRRR suggests 15-min rainfall could reach as high as 1"
    (brief 4"/hr rates) despite the progressive nature of convection.

    While the general fast motion of cells, at least in the next few
    hours, should offset some of the flash flood potential, these
    intense rainfall rates could still cause rapid runoff. This will
    be most likely along any short-term training boundaries where
    event total rainfall in the next several hours could be 1-3
    inches, and 3-hr FFG exceedance probabilities peak above 25%.
    Despite the uncertainty in the exact evolution reflected by
    variability in the CAMs, the environment will become increasingly
    supportive of these intense rates and short-term training, which
    atop the modest FFG could result in flash flooding instances
    overnight.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6imsz0UVU6e2GLkHqa_f8DPW8yE6g9adHf6pBTrrtoSASPWdTQsOThtIR5T6DEShzse3= xCmd6IW_KBPPyIq5bg-WwpY$ for graphic product...

    ATTN...WFO...ABR...BIS...FGF...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 48589836 48129668 47459642 46639687 45959777=20
    45859935 46530097 47210168 47530175 47970146=20
    48060133 48510027=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 28 02:35:32 2025
    AWUS01 KWNH 280233
    FFGMPD
    VAZ000-NCZ000-WVZ000-TNZ000-KYZ000-280600-

    Mesoscale Precipitation Discussion 0537
    NWS Weather Prediction Center College Park MD
    1032 PM EDT Fri Jun 27 2025

    Areas affected...far western Virginia, southern West Virginia, far
    eastern Kentucky, far northeastern Tennessee

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 280232Z - 280600Z

    Summary...Flash flood potential should continue for another 2-4
    hours.

    Discussion...Scattered convection continues to develop in earnest
    across southwestern Virginia and vicinity. This area has
    experienced a relative minimum in convective activity up until the
    past hour, enabling persistence of surface-based instability
    despite the time of day. SPC mesoanalyses indicate broad, weak
    confluence within the low-level flow field across this region,
    which was combining with weak terrain influences and a
    moist/unstable environment (1500 J/kg MLCAPE, 1.5-1.75 inch PW
    values) to promote strong updrafts. Peak rain rates are exceeding
    1.5 inches/hr in a few spots beneath the most persistent
    convection, which isn't surprising given the slow movement of
    cells and their outflow-dominant nature. These rates are
    exceeding local FFG and likely prompting localized impacts in a
    few areas.

    Despite the relative uptick in convective trends over the past 1-2
    hours, models/obs suggest that a weakening trend will eventually
    commence due to widespread convective overturning. This process
    may take another 2-4 hours to weaken convection, however, with
    deep convection continuing through at least 06Z or so. Isolated,
    locally significant flash flooding can be expected during this
    timeframe.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-OdgvMMP5GVBIXIwUtskSJjAUlYfjk2fo39oa7GUk6otzygd3tFR0kgRuHCAP_DJJ9oQ= dJpu-RVGq8sHSzb8-HnOrUQ$ for graphic product...

    ATTN...WFO...JKL...MRX...RLX...RNK...

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 38128208 37498071 36788066 36038304 36708397=20
    37338366=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 28 14:18:55 2025
    AWUS01 KWNH 281418
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-281915-

    Mesoscale Precipitation Discussion 0539
    NWS Weather Prediction Center College Park MD
    1018 AM EDT Sat Jun 28 2025

    Areas affected...Northeast OK...Southwest MO...Northwest AR...
    Exteme Southeast KS...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 281415Z - 281915Z

    SUMMARY...Small slowly decaying MCC giving way to new slow
    moving/efficient thunderstorms along unstable edges.

    DISCUSSION...GOES-E 10.3um IR and regional RADAR mosaic depict a
    smaller than average MCC with well defined MCV crossing out of SE
    KS with the outer banding feature continuing to maintain on
    stronger than forecast southwesterly warm air advection. AMV/RAP
    analysis suggests a 300mb 50+kt jet speed max crossing out of
    central KS northeastward, exposing favorable right entrance ascent
    and favorable outflow to maintain and due to internal convection,
    slightly enhance the MCV. This has also aided a solid south to
    southwest 30kt inflow which has been orthogonal to the trailing
    banding feature resulting in continued development. Initial
    clusters near Tulsa have kicked some outflow southwestward and
    visible imagery shows bubbling Tcu along the upwind instability
    axis where MUCAPE values remain about 1500-2000 J/kg but are only
    uncapped in the vicinity of the isentropic ascent.

    Downstream, weak low level stratus appears to be burning off and
    increased insolation is helping to bolster surface to boundary
    layer heating across the high low level moisture environment
    between the small MCC and the thunderstorm activity spurred by
    downstream confluence in the MS/OH River Valleys. CIRA LPW layers
    show area of concern remains the core of nearly all layers of
    moisture with overall totals exceeding 2" and with deep layer warm
    cloud processes (13-14Kft), will support efficient rainfall
    production (especially where WAA/isentropic ascent is greatest)
    with 2-2.5"/hr possible.

    Slow deep layer flow given the MCC ciruclation is slowly to the
    east and crossing into recently saturated (higher relative soil
    moisture ratios into the mid to upper 60%) across the Ozark
    Plateau. Combined with naturally lower FFG values due to the
    complex terrain and low water crossings, the potential for
    exceedance of FFG is higher and with spots of 3-4" totals suggest
    it possible for scattered incidents of flash flooding to occur.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6J2WxJ8tt-cY86Q1CuBywA1vklAnm8Bl-a7WMpf3MpQmPJfGs17VgI0e6BqVyOJs4ZLl= jEQqojbos3MiLepxMIWg_EA$ for graphic product...

    ATTN...WFO...ICT...LZK...SGF...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 37999355 37789289 37439209 36719204 35639212=20
    35109266 35119365 35299443 35429552 35789639=20
    36679662 37109592 37329565 37529532 37759484=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 28 13:19:35 2025
    AWUS01 KWNH 281317
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-281900-

    Mesoscale Precipitation Discussion 0538
    NWS Weather Prediction Center College Park MD
    917 AM EDT Sat Jun 28 2025

    Areas affected...Southeast MO...Northeast AR...Western
    TN...Western KY...Southern IL...Southern IND...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 281315Z - 281900Z

    SUMMARY...Highly efficient pulse convection with sub-hourly 2"
    totals and eventual broader downdrafts/cell mergers that pose an
    isolated total to 3" and localized possible flash flooding.

    DISCUSSION...Regional RADAR and GOES-E conventional imagery loops
    depict developing convective clusters across the central MS Valley
    into the Lower Ohio River Valley. WV loop and RAP analysis shows
    sharp upper-level ridge and rapid directional/divergent flow aloft
    to support weak but multi-directional outflow to support stronger ascent/updraft strength. At the lower levels, solid 15-20kt
    solidly confluent 850mb flow through the Lower Ohio Valley
    supports convergence of very deep moisture/narrow skinny profiles
    with modest but sufficient instability (1000 J/kg of CAPE). Total
    PWats over 2" and vertical flux convergence will allow for highly
    efficient warm cloud processes (12-13Kft depth); but with weak
    shearing/tilting of updrafts, downdrafts should collapse downward
    likely resulting in focused totals up to 2" in less than 30-60
    minutes. Further rounds of thunderstorms will be generated along
    outflow boundaries; so with each cycle the potential for broader
    updrafts increases with some potential for mergers or expansion
    over areas that were hit with prior rounds suggesting an isolated
    spot of 3" is possible.=20

    Hydrologically, the area has been above normal in rainfall and
    soil saturation in most locations in the MPD area. FFG values of
    2"/hr seem reasonable and may be exceeded, suggesting widely
    scattered incidents of localized flash flooding is possible.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6NP_yTzkQFRP7SOxPoEtN7yngkvuoAOMDAq4NXda1spifKU3-YLlBIYrabPyHH0bBPle= MlIfhUM9j24z_BPC5CpRBuc$ for graphic product...

    ATTN...WFO...ILX...IND...LMK...LSX...LZK...MEG...PAH...SGF...

    ATTN...RFC...KRF...MSR...ORN...TIR...NWC...

    LAT...LON 39358687 39208590 38388561 37658621 36748804=20
    35128929 35289193 37299188 38048995 38768825=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 28 17:41:59 2025
    AWUS01 KWNH 281741
    FFGMPD
    TNZ000-KYZ000-INZ000-282300-

    Mesoscale Precipitation Discussion 0540
    NWS Weather Prediction Center College Park MD
    141 PM EDT Sat Jun 28 2025

    Areas affected...Northern & Central Kentucky...Middle Tennessee...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 281745Z - 282300Z

    SUMMARY...Slow moving, highly efficient thunderstorms capable of
    quick sub-hourly totals up to 2". Given recent rainfall,
    saturated soils and urban locales; wide scattered localized
    incidents of flash flooding are possible this afternoon.=20

    DISCUSSION...Initial rounds of thunderstorms over the Middle MS
    and lower OH/TN valleys have started to generate solid outflow
    boundaries that are generally shifting eastward into central KY to
    NW Middle TN. Nearly full insolation is supporting temperatures
    into the upper 80s nearing 90, while deep layer moisture remains
    well above normal (mid 70s Tds) and total PWats in the 1.75 to
    1.9" range. As outflow boundary convergence is expected, this
    should result in broader, perhaps slab ascent updrafts. Deep warm
    cloud (12-14Kft) and vertical moisture flux convergence will
    support wet microbursts capable of 2" totals in 30 to 60 minutes
    with reinforcement of outflow boundaries to seek out remaining
    instability pockets through the evening and afternoon. Cells may
    have some increased duration of updraft given modest divergence
    aloft in the entrance region of the north to south jet streak on
    the northwest edge of the larger TUTT (Tropical Upper Tropospheric
    Trough) centered near Upstate SC/Western NC.

    Recent heavy rainfall/above average rain totals have resulted in
    well above average soil saturation ratios of 60 to near 70% across
    most of the area of concern. Generally 1hr FFG values of
    1.5-2.25" across the area are possible to be exceeded but in a
    very widely scattered 'buck-shot' pattern and result in possible
    localized flash flooding, with highest probability if cells align
    with impermeable urban ground conditions with very high runoff
    quickly.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8haWmxboKtfK-f7nRpP70KZ14xT7lVxnZ8HtE50TFRCmkG0nSSGXVCUfPc3n30lKpVG0= V4JYbgLB2eOUOuIneku9sKM$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...MEG...OHX...PAH...

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 38918487 38558400 37638396 36248520 35528645=20
    35168717 35228811 35848853 36838801 37698681=20
    38238606=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 28 18:22:28 2025
    AWUS01 KWNH 281821
    FFGMPD
    VAZ000-NCZ000-WVZ000-SCZ000-GAZ000-TNZ000-KYZ000-290030-

    Mesoscale Precipitation Discussion 0541
    NWS Weather Prediction Center College Park MD
    220 PM EDT Sat Jun 28 2025

    Areas affected...Central Appalachians

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 281830Z - 290030Z

    Summary...Slow moving showers and thunderstorms will rapidly
    increase in coverage across the Central Appalachians this
    afternoon. Rainfall rates of 1-3"/hr are likely within this
    convection, leading to pockets of 2-3" of rain with isolated
    higher amounts. Flash flooding is possible.

    Discussion...The GOES-E visible imagery this afternoon shows rapid
    growth of TCu from northern GA through central VA, primarily along
    the higher terrain of the Appalachians. These storms are pulsing
    up in an extremely favorable thermodynamic environment reflected
    by SPC RAP analyzed SBCAPE of 2500-3500 J/kg overlapping PWs above
    1.7 inches. Morning forecast soundings across the area indicate
    long-skinny CAPE profiles and generally moist-adiabatic lapse
    rates through much of the column, which when combined with warm
    cloud depths approaching 13,000 feet suggests the environment will
    support efficient warm-rain processes. Although synoptic ascent is
    weak outside of modest upslope flow, which is reflected by weak
    winds from the sfc through 300mb, there will likely be scattered
    to numerous thunderstorms which form across the area through this
    evening.

    Convection will generally form along terrain features today. As
    these storms pulse and decay, remnant outflow boundaries will
    serve as additional foci for updrafts, leading to more numerous
    cells later this aftn/eve. Storm motions will be quite weak and
    chaotic as reflected by 0-6km mean winds of just 5 kts and
    variable but weak Corfidi vectors, suggesting cells will move
    little during their lifespan, and may at time stall when they
    become terrain-tied. With rain rates progged by the HREF to have a
    20-25% chance of exceeding 2"/hr, and HRRR 15-min rainfall
    forecast to be as much as 1" (brief 4"/hr rates - supported by the
    efficient warm rain processes), these slow storms, especially
    during collisions/mergers or when storms become terrain tied,
    could lead to pockets of 2-3" of rain with locally higher amounts.

    The Central Appalachians have generally been dry the past 7-10
    days as noted in the AHPS rainfall departures, but scattered
    storms in the past week have created some pockets of more than
    200% of normal rainfall. This has led to areas of 3-hr FFG that is
    as low as 1-1.5"/3hrs, although FFG across much of the region is
    modest due to the general vulnerability of this terrain. The HREF
    3-hr exceedance probabilities are very scattered and peak at just
    10-20%, but the slow movement of these efficient rain rates atop
    generally sensitive terrain could result in at least isolated
    instances of flash flooding today.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_5I1_Zdh-v0uJ9uoyAiR1D_tmHe7sg0TUtvuLAMqBBnuTixMBo9ppn3IBlX0VD9trs3g= sRA8u4fsye79COmzrpKLfIM$ for graphic product...

    ATTN...WFO...AKQ...FFC...GSP...JKL...LWX...MRX...RAH...RLX...
    RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 38707847 38457811 37717845 36927961 36168046=20
    36138055 35468118 35028165 34608230 34558401=20
    35018444 35808384 36858294 37748159 38368034=20
    38677927=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 28 19:00:30 2025
    AWUS01 KWNH 281900
    FFGMPD
    TNZ000-KYZ000-ILZ000-MSZ000-MOZ000-ARZ000-282300-

    Mesoscale Precipitation Discussion 0542
    NWS Weather Prediction Center College Park MD
    300 PM EDT Sat Jun 28 2025

    Areas affected...Ozarks

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 281859Z - 282300Z

    Summary...Showers and thunderstorms will continue to expand in
    coverage and move slowly eastward across the Ozarks and into the
    Tennessee Valley. This convection will contain rain rates that at
    times may reach 3"/hr, leading to 2-3" of rain with locally higher
    amounts. Flash flooding is possible.

    Discussion...An area of showers and thunderstorms noted on the
    regional radar mosaic across MO/AR this afternoon is drifting
    slowly eastward while expanding. Rainfall rates within this
    convection has been estimated via local radars to be as much as
    2.5"/hr (from KSGF), leading to mesonet observed rainfall of 1-2+"
    so far today. This area of convection is expanding in response to
    a modest 850mb LLJ of 15-20 kts which is efficiently transporting
    PWs above 2 inches and MLCAPE as high as 3000 J/kg northward into
    the region. Additionally, despite modest synoptic lift due to weak
    flow around a ridge to the south, a weak shortwave approaching
    from the Central Plains and the convergence of this weak LLJ along
    its nose are helping to provide just enough ascent in the robust
    thermodynamics to fuel the widespread activity this aftn.

    The high-res CAMs are generally under-forecasting the current
    activity, although the 12Z NAMnest and ARWs appear to have the
    best handle on the breadth of the current activity. Despite that,
    the CAMs are likely eroding activity too quickly during the next
    few hours as the forcing/thermodynamics overlap will support a
    continuation of this activity well into the Tennessee Valley by
    this evening. As the favorable PWs and CAPE are continually drawn northeastward, this will support rainfall rates which have a high
    chance (>70%) of exceeding 1"/hr (from the HREF) with storms
    slowly moving eastward on 0-6km mean winds of just 5-10 kts.
    Additionally, weak bulk shear will result in storms manifesting
    primarily as pulse type, but some weak organization is possible
    along outflows or in the vicinity of the LLJ nose, leading to some
    short-term training or backbuilding to prolong these rain rates.
    Where this occurs, rainfall could be 2-3" or locally higher.

    FFG across the area is generally 2-3"/3hrs, for which the HREF
    indicates has a 20-30% chance of being exceeded. However, with the
    poor overall initiation of the HREF CAMs suite, the true
    probability is likely higher than this. Additionally, MRMS 24-hr
    rainfall has been 1 to as much as 3 inches, leading to pockets of
    fully saturated top-soils which will be more susceptible to
    runoff. While flash flooding is possible anywhere across the area
    this aftn, it will be most likely where any short term training
    can move across the more primed soils.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5SyBqEJ3mJ1qmMc5Eh7iEd-U0tFzehTvflgh6ZNNMxQbrvkAStGRN4H4YzKvJOipnNnR= Hq9HQjjzTG1qd1YOGblB2OY$ for graphic product...

    ATTN...WFO...EAX...LSX...LZK...MEG...PAH...SGF...TSA...

    ATTN...RFC...KRF...MSR...ORN...TIR...TUA...NWC...

    LAT...LON 38629272 38369174 37999067 37688938 37438845=20
    37068793 36248825 35628906 35108969 34819096=20
    35079227 35519309 36269353 36759361 37749371=20
    38509336=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 28 19:41:59 2025
    AWUS01 KWNH 281941
    FFGMPD
    PAZ000-MDZ000-WVZ000-OHZ000-KYZ000-INZ000-290130-

    Mesoscale Precipitation Discussion 0543
    NWS Weather Prediction Center College Park MD
    341 PM EDT Sat Jun 28 2025

    Areas affected...Ohio Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 281940Z - 290130Z

    Summary...Showers and thunderstorms blossoming ahead of a cold
    front will expand and train through the afternoon and into the
    evening. Rainfall rates of 1-2"/hr are expected, which through
    training could produce 2-3" of rain. Flash flooding is possible.

    Discussion...The regional radar mosaic this afternoon shows a
    rapid uptick of convective coverage aligned SW to NE from eastern
    Indiana through southwest Pennsylvania. These storms are
    continuing to expand and intensify as reflected by the GOES-E
    day-cloud phase RGB, suggesting more numerous storms will develop
    during the next few hours. This convection is blossoming in
    response to convergence along an approaching cold front, which is
    impinging into robust thermodynamics characterized by PWs around
    1.7 inches (above the 90th percentile at KILN according to the SPC
    sounding climatology) and SBCAPE over 3000 J/kg.

    Through the afternoon and into this evening, the cold front is
    likely to sag slowly south and east as modest 500mb height falls
    occur downstream of a shortwave moving into the Upper Midwest.
    This evolution combined with modest upper diffluence will help
    drive synoptic ascent atop the pronounced low-level convergence
    ahead of the front. This lift will move into an increasingly
    favorable environment as the 850mb inflow, while modest in speed
    (10-15 kts and veering) maintains a resupply of favorable
    thermodynamics as it originates from a pool of high PWs over 2
    inches. The HRRR is under-forecasting the current activity, but
    the ARWs, NAMnest, and even the RRFS have a better handle on the
    ongoing coverage and are favored through the evening. This
    suggests that storms will continue to expand and build into the
    greater instability to the SW, and then train steadily to the east
    as weak Corfidi vectors and 0-6km mean winds become aligned to
    each other and the sagging front.

    Rain rates will likely reach 1-2"/hr (50-60% chance from the REFS)
    leading to short duration rainfall as much as 0.5-1.5 inches in 30
    minutes, and this could quickly overwhelm soils leading to runoff.
    However, the greater concern is where training occurs, which
    should be prevalent along the front, as this could produce 2-3" of
    rain in some areas over a short period of time. If this training
    falls atop any urban areas, or across more sensitive soils due to
    terrain or FFG that is as low as 1.5"/3hrs from recent rainfall,
    instances of flash flooding would become more likely.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8nAQkQBFEPmn75sWybBmmLW7t2Es7pTBJnbpEXcrKt-EyjQ0gMBJVGVcKf4Cat3xwhEw= SClogB_jvOC_B__pauC6O_4$ for graphic product...

    ATTN...WFO...CLE...CTP...ILN...IND...JKL...LMK...LWX...PBZ...
    RLX...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 41017956 40737902 40127875 39187921 38577999=20
    38298060 38228211 38548386 38868527 39188601=20
    39458625 39778621 40138576 40198405 40418201=20
    40738094 40918023=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jun 28 22:01:02 2025
    AWUS01 KWNH 282200
    FFGMPD
    TXZ000-NMZ000-290300-

    Mesoscale Precipitation Discussion 0544
    NWS Weather Prediction Center College Park MD
    600 PM EDT Sat Jun 28 2025

    Areas affected...Southern New Mexico and West Texas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 282159Z - 290300Z

    Summary...Slow moving thunderstorms with 0.5"/hr rates or locally
    greater will continue across New Mexico and West Texas. This could
    produce as much as 0.75-1.25 inches of rain, leading to instances
    of flash flooding, especially across burn scars.

    Discussion...Scattered showers and thunderstorms have developed
    across southern New Mexico and West Texas this afternoon. This
    convection is expanding in response to favorable thermodynamics
    characterized by PWs of 1-1.4 inches, highest in West Texas,
    collocated with SBCAPE rising to 1000-2500 J/kg, highest in the
    High Plains of NM. In this environment, forcing is modest, but a
    shortwave is helping to enhance ascent that is otherwise primarily
    driven by upslope into terrain features and subsequent outflow
    boundaries in the pulse-convection environment. With PWs around
    the 90th percentile for the date, rainfall rates have been
    estimated via the local radars of around 0.5"/hr, and where these
    have occurred across recent burn scars, flash flood warnings are
    in effect.

    With a sharp gradient in moisture and instability in place across
    the area, convective coverage should remain generally isolated to
    scattered as reflected by available CAM simulated reflectivity.
    However, the presence of the shortwave could enhance ascent enough
    that storms become a bit more widespread than yesterday. In the
    pulse environment, this will result in outflows and storm mergers
    leading to additional development, with storm motions likely
    remaining chaotic and less than 10 kts using the Corfidi vectors
    as proxy. This will allow for heavy rain rates, which should
    exceed 0.5"/hr (>70% chance from the HREF) and may reach 1"/hr (UA
    WRF), especially during any mergers/collisions, to drift across
    the area through the aftn. Although general lifespans of these
    cells will be short, except during mergers, total rainfall could
    reach 1" or more in a few locations.

    This area is generally vulnerable to flash flooding. 1-hr FFG is
    only around 1", with even lower amounts likely needed to cause
    rapid runoff across sensitive terrain features and burn scars.
    Additionally, 7-day rainfall has been excessive at more than 600%
    of normal, further enhancing the vulnerability of the region as
    0-40cm soils are saturated above the 98th percentile in many
    areas. While the burn scars will have the most sensitivity and
    potential for flash flooding, any slow moving cell with the most
    intense rates could result in impacts through this evening.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4bkkhuMrVC7ZQQxNkLrq549efb7TuG7hfd8HwO28fsv4CmLpP8raU6A7bSZFpHzRgDZ-= HznrOl1N2OpS6Tex4-dSaqY$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 34730550 34690480 34370380 33280316 31870309=20
    30970314 30880322 30350336 30270388 30470469=20
    31030547 31720612 32010718 32150819 32380867=20
    32740875 33110875 33400893 33630876 33630827=20
    33850784 34060772 34390705 34610624=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 29 00:34:36 2025
    AWUS01 KWNH 290033
    FFGMPD
    WIZ000-MNZ000-SDZ000-NDZ000-290600-

    Mesoscale Precipitation Discussion 0545
    NWS Weather Prediction Center College Park MD
    832 PM EDT Sat Jun 28 2025

    Areas affected...Southeast North Dakota, Northeast South Dakota,
    Central Minnesota

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 290031Z - 290600Z

    Summary...Showers and thunderstorms will grow rapidly this evening
    and may congeal into an MCS during the next few hours. Rainfall
    rates of 2+"/hr are likely, which could produce 2-4" of rain with
    locally higher amounts through training. Flash flooding is
    possible.

    Discussion...The regional radar mosaic this evening shows two
    distinct areas of convection rapidly growing across the Dakotas.
    These storms are intensifying in response to an approaching cold
    front from the west, which is being pushed eastward by an
    accompanying shortwave embedded within weak troughing of otherwise
    zonal flow. Forcing for ascent is beginning to intensify
    downstream of this shortwave/front, aided by both the LFQ of a
    modest jet streak pivoting into SD, and through low-level
    convergence along the nose of an amplifying 850mb LLJ which has
    been measured recently at KFSD VWP at 30 kts. This LLJ is
    additionally transporting robust thermodynamics northward as
    reflected by the SPC RAP analysis, which suggests that MUCAPE has
    climbed above 4000 J/kg coincident with PWs of over 1.5 inches.
    Together, this lift and favorable environment will combine to
    cause an increase in convection through the evening.

    There remains considerable spread in the CAMs for the evolution
    this evening, causing somewhat lower than typical confidence in
    the flash flood potential. However, as the LLJ ramps up towards 40
    kts it will further replenish thermodynamics northward, while also
    enhancing ascent as it increases above the mean flow causing
    additional convergence into the warm sector ahead of the cold
    front. This combined with the cold front moving steadily eastward,
    and bulk shear rising to 30-35 kts, suggests hedging towards the
    CAMs with the most widespread and aggressive simulated
    reflectivity during the next few hours. This will support rainfall
    rates of 2+"/hr that are suggested by 20-25% probabilities from
    the HREF (which are likely too low due to model performance this
    evening), with brief rainfall rates of 3-4"/hr likely as shown by
    15-min HRRR rainfall of 0.75" to 1". Although individual cells,
    and the potential MCS produced via upscale growth, should be
    progressive, training will become increasingly likely as the MCS
    trails an outflow boundary to its south upon which additional
    storms will develop and then move east which is supported by
    veering Corfidi vectors. Where this training occurs, rainfall
    could be 2-4" with locally higher amounts.

    These intense rain rates will be sufficient to produce rapid
    runoff and isolated flash flooding. However, the antecedent
    conditions are also supportive due to 10-day rainfall that is more
    than 300% of normal causing 0-40cm soil moisture above the 98th
    percentile. This suggests minimal infiltration capacity of the
    soils, so that while the greatest risk for flash flooding will be
    through training, any of these intense rain rates, even if
    progressive, could quickly overwhelm the soils to produce impacts
    tonight.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!77aROJtk4PMF-eJ1Qsn6pNw9HR4KhZTmS0T7D6fVxaS7SxTPyVx2kz7rPGoVsGNQOb5n= 2mud6qjw8F3xhblxZWkA7H0$ for graphic product...

    ATTN...WFO...ABR...BIS...DLH...FGF...FSD...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 47379700 46979527 46629391 46259265 45879232=20
    45359251 44839287 44609354 44529363 44479505=20
    44709658 45299754 46059837 46499849 46999806=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 29 03:40:34 2025
    AWUS01 KWNH 290340
    FFGMPD
    MNZ000-SDZ000-290800-

    Mesoscale Precipitation Discussion 0546
    NWS Weather Prediction Center College Park MD
    1139 PM EDT Sat Jun 28 2025

    Areas affected...eastern South Dakota, southern/central Minnesota

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 290339Z - 290800Z

    Summary...Intense thunderstorms have taken on a favorable
    orientation for training, with spots of 2-3 inch/hr rates
    persisting for a couple hours just southeast of Watertown, SD.=20
    Heavy to extreme rain rates could pose locally significant flash
    flood potential through at least 07Z.

    Discussion...Recent mesoscale trends indicate a linear MCS
    extending from just southwest of Watertown, SD to near Willmar,
    MN. The linear MCS was backbuilding along the northern extent of
    a 25-30 kt southwesterly 850mb jet centered near Sioux Falls, SD.=20 Substantial backbuilding and training was occurring with this
    activity, and MRMS estimates of 5-7 inches of rainfall exist just
    southeast of Watertown with this activity. Steep lapse rates and
    abundant moisture will continue to fuel backbuilding activity in
    the short term, and heavy to extreme rain rates will likely
    accompany this activity.

    While the evolution of this band through the night is a bit
    uncertain, observations suggest that training convection will
    continue for at least the next 3-4 hours at least with
    synoptic-scale atmospheric features not expected to evolve much in
    that timeframe. The ongoing band will likely continue to
    backbuild while either remaining stationary or moving slowly
    southeastward in response to local cold pool development and other
    mesoscale processes. The band may also build eastward in to more
    of southern Minnesota. The degree of training in any one spot
    will be a primary factor modulating rainfall totals through 07Z.=20
    Additional 3-7 inch rainfall totals cannot be ruled out. Locally
    significant flash flooding may occur with this activity.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6grJJVDF1DuzAFEm1feLPyY8scMlD8SFbN4V5WFkQPCpdf-UKEXQNCH7uZ7cQBsIhEZG= RS1jbxJFfx4k3HhmVziLCS8$ for graphic product...

    ATTN...WFO...ABR...ARX...FSD...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45269446 45109341 44569281 43969300 43639568=20
    43859793 44659807 45099677=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 29 04:04:11 2025
    AWUS01 KWNH 290402
    FFGMPD
    MNZ000-SDZ000-290800-

    Mesoscale Precipitation Discussion 0546
    NWS Weather Prediction Center College Park MD
    1202 AM EDT Sun Jun 29 2025

    Areas affected...eastern South Dakota, southern/central Minnesota

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 290339Z - 290800Z

    Summary...Intense thunderstorms have taken on a favorable
    orientation for training, with spots of 2-3 inch/hr rates
    persisting for a couple hours just southeast of Watertown, SD.=20
    Heavy to extreme rain rates could pose locally significant flash
    flood potential through at least 07Z.

    Discussion...Recent mesoscale trends indicate a linear MCS
    extending from just southwest of Watertown, SD to near Willmar,
    MN. The linear MCS was backbuilding along the northern extent of
    a 25-30 kt southwesterly 850mb jet centered near Sioux Falls, SD.=20 Substantial training was also occurring with this activity, and
    MRMS estimates of 5-7 inches of rainfall exist just southeast of
    Watertown recently. Steep lapse rates and abundant moisture will
    continue to fuel backbuilding in the short term, and heavy to
    extreme rain rates will likely accompany the storms.

    While the evolution of this band through the night is a bit
    uncertain, observations suggest that training convection will
    continue for at least the next 3-4 hours at least with
    synoptic-scale atmospheric features not expected to evolve much in
    that timeframe. The ongoing band will likely continue to
    backbuild while either remaining stationary or moving slowly
    southeastward in response to local cold pool development and other
    mesoscale processes. The band may also build eastward in to more
    of southern Minnesota. The degree of training in any one spot
    will be a primary factor modulating rainfall totals through 07Z.=20
    Additional 3-7 inch rainfall totals cannot be ruled out. Locally
    significant flash flooding may occur with this activity.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4F2xc3ZVn4vMqrnT-GIo-xijucQyyMY8mnZYa4f2HAi98pKDVELsikniesse_DIUjHrv= DCZ0xIbT1icLe3NJJRU0Vko$ for graphic product...

    ATTN...WFO...ABR...ARX...FSD...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45269446 45109341 44569281 43969300 43639568=20
    43859793 44659807 45099677=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 29 08:03:23 2025
    AWUS01 KWNH 290802
    FFGMPD
    MOZ000-ARZ000-KSZ000-291400-

    Mesoscale Precipitation Discussion 0547
    NWS Weather Prediction Center College Park MD
    401 AM EDT Sun Jun 29 2025

    Areas affected...eastern Kansas into central and south-central
    Missouri

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 290800Z - 291400Z

    Summary...A few areas of slow-moving showers and thunderstorms are
    expected to expand in coverage across the discussion area. Areas
    of 1-2 inch/hr rain rates are expected through at least 14Z/9a CDT
    this morning, which could prompt flash flooding.

    Discussion...Scattered convection was developing along an axis
    from east-central Kansas (near Emporia eastward to near Sedalia
    and southeastward to the MO/AR border near Cherokee Village. The
    storms were being forced by ascent on the nose of stronger 850mb
    flow located across Kansas and the Missouri Ozarks, with speed
    convergence providing lift amid a marginally unstable (1000 J/kg
    MUCAPE) but plenty moist (1.5+ inch PW) environment. The storms
    are developing amid weak steering flow aloft, resulting in slow
    movement and redevelopment within the axis of best low-level
    convergence. The slow movement was already enabling spots of 1
    inch/hr rain rates to materialize in central Missouri, which may
    result in isolated excessive runoff in the near term despite
    values falling short of hourly FFG.

    Models/observations suggest that persistent low-level convergence
    across the discussion area will continue to promote redevelopment
    and expansion of convection through the early morning hours. An
    attendant increase in rainfall rates (into the 1.5 inch/hr range
    in spots) is also expected. These rain rates will threaten FFG
    thresholds and promote a risk of flash flooding especially in
    urban and sensitive locales through 14Z/9a CDT this morning.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6mFz9p25grdnoArPkxPNBzHQp-EV60no98FhHspYNDqAYVbYu_UAHSSz-_AMH6C0HRcC= lQupv2YJzShWD6xnupRlIH0$ for graphic product...

    ATTN...WFO...EAX...LSX...LZK...PAH...SGF...TOP...

    ATTN...RFC...KRF...MSR...ORN...NWC...

    LAT...LON 39749527 39699367 38599109 37209056 36509081=20
    36309167 36869256 38309426 38429556 39089600=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 29 09:43:37 2025
    AWUS01 KWNH 290943
    FFGMPD
    MOZ000-IAZ000-NEZ000-SDZ000-291400-

    Mesoscale Precipitation Discussion 0548
    NWS Weather Prediction Center College Park MD
    542 AM EDT Sun Jun 29 2025

    Areas affected...western Iowa, eastern Nebraska, far northwestern
    Missouri

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 290941Z - 291400Z

    Summary...A convective complex across northeastern
    Nebraska/northwestern Iowa will foster isolated flash flood
    potential as it migrates southeastward across the discussion area
    through 14Z/9a CDT.

    Discussion...Latest radar mosaic imagery indicates a mature
    convective complex extending from near Sheldon, IA southwestward
    to near Norfolk, NE this morning. Additional, isolated convection
    was beginning to develop across southeastern Nebraska. The storms
    are being supported by strong mid-level lapse rates (~8C/km) and a
    moist axis (1.4+ inch PW values) extending from northeastern
    Nebraska south-southeastward toward Kansas City Metro. Additional
    storms across far southeastern Nebraska were being supported by
    strong low-level convergence on the nose of 40-kt low-level flow
    focused over central Kansas. Most areas within this complex were
    experiencing modest rain rates except for far northwestern Iowa,
    where the orientation of cells were promoting 1.5 inch/hr rain
    rates that were approaching FFG thresholds.

    While the ongoing flash flood threat should remain fairly isolated
    in the short term, some concern exists that this potential could
    increase through 14Z/9a this morning. The ongoing, mature MCS
    should continue to migrate south-southeastward through abundant
    mid-level instability, resulting in continued potential for 1-1.5
    inch/hr rates at times. Additionally, low-level convergence (and
    resultant development) across southeastern Nebraska suggest that
    the mature convective complex will eventually begin to foster
    cellular mergers that locally prolong rain rates and boost
    rainfall totals in a few locales. FFG thresholds are in the 1.5-2
    inch/hr range areawide, and as mergers become more common, these
    thresholds should be breached on occasion.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6LylPw7-B2Mx1MTr6R90gwy5QWMUdHWA1F7Hq4ZsoJaZ44BVH-euHsQ7KTlgpjN4vmIX= 1Tk-Y63H2FWs8CUdCSZr3hU$ for graphic product...

    ATTN...WFO...DMX...EAX...FSD...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43219519 42799437 41679387 40549364 39909428=20
    40129604 40529694 42199718 43089634=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 29 13:43:11 2025
    AWUS01 KWNH 291343
    FFGMPD
    ILZ000-MOZ000-KSZ000-NEZ000-291930-

    Mesoscale Precipitation Discussion 0549
    NWS Weather Prediction Center College Park MD
    942 AM EDT Sun Jun 29 2025

    Areas affected...Northeast Kansas...Missouri...Far Southeast
    Nebraska...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 291345Z - 291930Z

    SUMMARY...Weakening convective complexes still have potential for
    additional 1-3" locally crossing areas already flooded this
    morning. Localized flash flooding still remains possible.

    DISCUSSION...GOES-E 10.3um loop shows scattered re-activation of
    scattered thunderstorms/cooling tops extending from dying
    MCS/Squall line across SE NEB/IA moving into NE KS/NW MO all the
    way south across central MO to southeast MO where remaining
    isentropic ascent continues with scattered clusters. Upwind
    areas across E KS and SW MO remain conditionally unstable with
    ample deep layer moisture up to 1.75-2" of total PWats and capped
    CAPEs up to 2500 J/kg which will further increase with clearing
    skies. The old MCV with the leading convective complex/WAA
    regime continues to decouple and slide eastward through the deep
    layer flow across E MO, but the resulting LLJ still is fairly
    strong for the diurnal minimum with TWX/EAX/SGF VWP suite
    continuing to show solid 30-40kt decelerating confluent flow
    toward the old outflow/isentropic gradient across west-central to
    southeast MO still able to overcome the weaker capping to support
    the remaining convective clusters particularly on the confluent
    upwind edge from Bates to Miller county. Given the moisture flux
    and buoyancy, scattered cells/clusters will move with favorable
    orientation for short-term training as well as intersecting areas
    affected last night/this morning across south-central MO; given
    broad scattered Tcu across the Ozark Plateau, additional
    development may occur hear as well, expanding the risk for flash
    flooding rainfall totals (1-3") south and west of the already
    flooded areas in SE MO.

    Upstream, the strong outflow/squall line is intersecting the
    northern apex of the instability axis across NE KS and strong
    convergence along the leading edge is sprouting stronger/broader
    updrafts with cores that are back-shearing over the colder
    under-cutting air, suggesting increased overall duration of
    intense rainfall can be expected over the next hour or so. In
    addition, the squall line is merging with older more scattered WAA
    cells lingering from the prior wave in combination over the Kansas
    City Metro area. Propagation will be more due south than
    southeast given the available instability westward to the old
    track of rain; but a balance may be stuck for intersection of this
    newer 1.5-3" totals over areas having 1-3" this morning.=20

    While overall coverage is likely to be more scattered in nature,
    the combination of rates over recently saturated grounds will
    continue the risk for a few more incidents of flash flooding
    through the next 3-5 hours as the LLJ further diminishes and
    capping further increases.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-mSwJJvnCo4nwUUGWVBMW7wbvzJSSu3EPvKTUpucSnhuvd1yVMTBIeM1Cz2iLFJIQTMa= vx2RZTzYXgucbjGzqeU5gmc$ for graphic product...

    ATTN...WFO...EAX...LSX...OAX...PAH...SGF...TOP...

    ATTN...RFC...KRF...MSR...ORN...NWC...

    LAT...LON 40559416 40209305 39449183 38279032 37498949=20
    36958946 36739007 36799152 37249318 38109480=20
    39259652 40109708 40509556=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 29 17:03:36 2025
    AWUS01 KWNH 291702
    FFGMPD
    GAZ000-TNZ000-ALZ000-MSZ000-292200-

    Mesoscale Precipitation Discussion 0550
    NWS Weather Prediction Center College Park MD
    102 PM EDT Sun Jun 29 2025

    Areas affected...Middle TN...Northern AL...Northwest
    GA...West-central MS...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 291700Z - 292200Z

    SUMMARY...Stronger than normal pulse thunderstorms within deep
    moisture, slow flow environment may support scattered to numerous
    cells with capability of 2" totals in 30-60 minutes. Incidents of
    localized flash flooding is considered possible.

    DISCUSSION...GOES-E WV suite once again shows closed TUTT cell
    over E GA just west of Augusta with northwest quadrant of enhanced
    moisture within/along NNE to SSW jet streak across Middle TN
    becoming more diffluent along and south of the TN River Valley.=20
    Clear skies and stagnant humid low level moisture have supported
    rapid increase in broad area of 2000-2500 J/kg of MLCAPE across
    much of northern and central AL, with extensions into west-central
    MS and western GA. Deep layer moisture is over 2". Differential
    heating along old cirrus canopy from the western portion of Middle
    TN into central MS has result in weak thermal circulation to
    support weak, yet sufficient convergence in this highly unstable
    environment for broader ascent with scattered to numerous coverage
    noted.=20

    Deep layer steering is very weak at 5-10kts and also a tad
    diffluent toward the south and southeast. So with stronger
    vertical moisture flux/loading to the updrafts, warm cloud depths
    over 13-14Kft will support up to 2" totals within 30-60 minutes.=20
    Limited dry air aloft will support moist outflow boundaries and
    convergence will support newer activity with each cycle
    potentially increasing the areal expanse of the updrafts resulting
    in a broader area of intense rainfall. Given the shear
    rate/magnitude...rapid inundation and runoff would be normally
    expected but lower FFG due to an above normal season may further
    limit infiltration and increase runoff. As such, highly
    focused/localized flash flooding may be possible in/near the cores
    and around urban centers such as Huntsville, Birmingham, Nashville
    or Atlanta.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4RwHvCg7IKrQNJWMGYkNGF_VkCOkgqv2zSamNuAnzjGYVnmFAicdWwsX1Q9MtKmeIzOY= OXPwMYbcIcylMjd7CzHKWYQ$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...JAN...MRX...OHX...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 36428678 36388549 35468504 34298461 33608397=20
    32808432 32558518 32618608 32498743 32398887=20
    33248920 33708820 34948777 35848747=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 29 18:47:46 2025
    AWUS01 KWNH 291847
    FFGMPD
    MIZ000-WIZ000-MNZ000-IAZ000-300030-

    Mesoscale Precipitation Discussion 0551
    NWS Weather Prediction Center College Park MD
    247 PM EDT Sun Jun 29 2025

    Areas affected...central Iowa through northeast Wisconsin

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 291846Z - 300030Z

    Summary...Storms developing ahead of a cold front will train
    through the afternoon. As rain rates intensify to 1-2"/hr, this
    training could result in axes of more than 3 inches of rain,
    potentially leading to flash flooding.

    Discussion...The regional radar mosaic this afternoon shows
    showers and thunderstorms expanding rapidly ahead of an
    approaching cold front. Although the front is still positioned
    well west of the axis of convection, storms are aligning SW to NE
    along the convergent nose of a modest LLJ and downstream of an MCV
    noted in the GOES-E visible satellite imagery to enhance ascent.
    This LLJ, while veering with latitudinal gain, is transporting
    robust thermodynamics northward as a ribbon of PWs above 1.5
    inches stretches northward into Wisconsin immediately downstream
    of the developing convection, collocated with a plume of SBCAPE
    above 4000 J/kg. Although ascent is generally modest, this lift
    acting into these favorable thermodynamics will continue to
    support intensifying cores, with an expansion of coverage also
    likely during the next few hours.

    Rainfall rates have been estimated above 1.5"/hr via KARX WSR-88D
    already this afternoon. These rates will likely continue to
    intensify, and both the HREF and REFS indicate a 10-20% chance of
    2"/hr rain rates during the next few hours. Short duration
    rainfall may be even more impressive as the 15-min HRRR indicates
    brief 3-4"/hr rates (0.75 to 1.0 inches in 15 minutes). As the MCV
    pushes northeast and the front approaches, shear may gradually
    increase to 20-25 kts, suggesting at least modest organization
    into multicell clusters is possible, with the CAMs identifying
    southern WI as the most likely location for this evolution.
    Regardless of any organization, training/repeating cells appear
    likely as Corfidi vectors collapse to around 5 kts and align to
    the mean wind, indicating that cells will continue to regenerate
    within the greater thermodynamics to the S/SW and then track
    northeast, impacting the same areas multiple times. With rain
    rates of 1-2"/hr or more expected, this could result in 1-3" of
    rain with locally higher amounts as forecast by HREF 6-hr rain
    probabilities.

    Soils across the area, especially in WI and southeast MN, are
    saturated above the 95th percentile within the 0-40cm layer
    according to NASA SPoRT due to recent heavy rain. This has lowered
    FFG to just 1.5-2"/3hrs which has a 20-30% chance of being
    exceeded according to the HREF. This further indicates the
    potential for these heavy rain rates to result in instances of
    flash flooding through the evening, especially during the most
    impressive training.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!92xgdl_3B6lBde2mbol7OGdC2T_JFEEcGUQlYpG2rasODkSnVgi6wIfZ7iLaRDTXCJ_9= syIf7qySfNrNN4vrOUyCYUk$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...GRB...MKX...MPX...MQT...

    ATTN...RFC...MSR...NWC...

    LAT...LON 45598869 45488782 44948768 44138806 43268913=20
    42669017 41979238 42549299 43369292 43969231=20
    44639129 45308957 45378935=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 29 19:49:17 2025
    AWUS01 KWNH 291949
    FFGMPD
    KYZ000-MOZ000-ARZ000-OKZ000-KSZ000-300100-

    Mesoscale Precipitation Discussion 0552
    NWS Weather Prediction Center College Park MD
    348 PM EDT Sun Jun 29 2025

    Areas affected...southeast Kansas through the Ozarks

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 291947Z - 300100Z

    Summary...Showers and thunderstorms developing along a surface
    trough and an accompanying outflow boundary will translate
    southeast through the afternoon. Rainfall rates in excess of 2"/hr
    are expected within this convection, leading to 2-3" of rain with
    locally higher amounts. Flash flooding is possible.

    Discussion...The GOES-E day-cloud phase RGB this afternoon
    indicates a rapid expansion of strengthening updrafts across much
    of southern Missouri. These updrafts are manifesting as
    strengthening thunderstorms, with two clusters noted via the
    regional radar mosaic. One of these is dropping out of southeast
    Kansas along an outflow boundary, while a second area is expanding
    across a surface trough in southeast Missouri. The low-level
    convergence driving this convection is moving into robust
    thermodynamics characterized by PWs nearing 2 inches overlapping
    MLCAPE of 3000 J/kg, leading to intense rain rates estimated via
    radar to be 2.5"/hr in some areas.

    Over the next few hours coverage should continue to expand across
    the area and track slowly to the southeast, although some more
    impressive organization through bulk shear of 20-30 kts may
    eventually result in a more progressive MCS as shown by the ARWs.
    Until then, the slow movement of cells combined with these intense
    rain rates may result in stripes of 2-3" of rain with locally
    higher amounts.

    The CAMs differ considerably in the evolution the next few hours,
    so confidence is reduced as to where the greatest potential for
    the heaviest rainfall will be. However, the slow southward advance
    of the strong CAPE gradient combined with the slow westward build
    of convection along the surface trough suggests south-central
    Missouri will become the focus of the heaviest and most prolonged
    rainfall this afternoon. This is potentially problematic as FFG in
    this area is most compromised to as low as 0.75-1.5"/3hrs, for
    which the HREF indicates has a 30-40% chance of exceedance. While
    the intense rain rates moving across any urban or more sensitive
    soils could cause flash flooding, the greatest risk will be across south-central Missouri where the the overlap of low FFG and
    highest rainfall may occur.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-sN7tAT_2ieEFTVd5YlPunizHwD1klzmMswP6gIQkPTna1iNCPlQcyUHq_sHx9MoaqWw= Dt6GuT-D4jov0wUyjiHzrSY$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...LZK...MEG...PAH...SGF...TOP...
    TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38749475 38709411 38419304 38119227 37699172=20
    37349091 37058988 36708936 36298969 36039087=20
    36089305 36499483 36829558 37179640 37429720=20
    38139668=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 29 19:59:03 2025
    AWUS01 KWNH 291957
    FFGMPD
    KYZ000-MOZ000-ARZ000-OKZ000-KSZ000-300100-

    Mesoscale Precipitation Discussion 0552
    NWS Weather Prediction Center College Park MD
    356 PM EDT Sun Jun 29 2025

    Areas affected...southeast Kansas through the Ozarks

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 291947Z - 300100Z

    Summary...Showers and thunderstorms developing along a surface
    trough and an accompanying outflow boundary will translate
    southeast through the afternoon. Rainfall rates in excess of 2"/hr
    are expected within this convection, leading to 2-3" of rain with
    locally higher amounts. Flash flooding is possible.

    Discussion...The GOES-E day-cloud phase RGB this afternoon
    indicates a rapid expansion of strengthening updrafts across much
    of southern Missouri. These updrafts are manifesting as
    strengthening thunderstorms, with two clusters noted via the
    regional radar mosaic. One of these is dropping out of southeast
    Kansas along an outflow boundary, while a second area is expanding
    across a surface trough in southeast Missouri. The low-level
    convergence driving this convection is moving into robust
    thermodynamics characterized by PWs nearing 2 inches overlapping
    MLCAPE of 3000 J/kg, leading to intense rain rates estimated via
    radar to be 2.5"/hr in some areas.

    Over the next few hours coverage should continue to expand across
    the area and track slowly to the southeast, although some more
    impressive organization through bulk shear of 20-30 kts may
    eventually result in a more progressive MCS as shown by the ARWs.
    Until then, the slow movement of cells combined with these intense
    rain rates may result in stripes of 2-3" of rain with locally
    higher amounts.

    The CAMs differ considerably in the evolution the next few hours,
    so confidence is reduced as to where the greatest potential for
    the heaviest rainfall will be. However, the slow southward advance
    of the strong CAPE gradient combined with the slow westward build
    of convection along the surface trough suggests south-central
    Missouri will become the focus of the heaviest and most prolonged
    rainfall this afternoon. This is potentially problematic as FFG in
    this area is most compromised to as low as 0.75-1.5"/3hrs, for
    which the HREF indicates has a 30-40% chance of exceedance. While
    the intense rain rates moving across any urban or more sensitive
    soils could cause flash flooding, the greatest risk will be across south-central Missouri where the the overlap of low FFG and
    highest rainfall may occur.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_2Sp5JUSjnAydKLCKsLwn6k8OmzbH1bnn4PT0tgcT0-lJOtnEPj2crL2pKWPDGZJKZlq= Ttd_14q3GlAmNjZLNgPcVcI$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...LZK...MEG...PAH...SGF...TOP...
    TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38749475 38709411 38419304 38119227 37699172=20
    37349091 37058988 36708936 36298969 36039087=20
    36089305 36499483 36829558 37179640 37429720=20
    38139668=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 30 01:42:48 2025
    AWUS01 KWNH 300142
    FFGMPD
    ARZ000-OKZ000-KSZ000-300700-

    Mesoscale Precipitation Discussion 0553
    NWS Weather Prediction Center College Park MD
    942 PM EDT Sun Jun 29 2025

    Areas affected...southeast Kansas, northeast Oklahoma

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 300141Z - 300700Z

    Summary...Showers and thunderstorms will expand along several
    outflow boundaries tonight. Rainfall rates in new convection may
    briefly pulse up above 3"/hr, leading to 1-2" of rain in less than
    1 hour. Flash flooding is possible.

    Discussion...The regional radar mosaic this evening shows clusters
    of thunderstorms dropping southward across parts of AR, OK, and KS
    along residual outflow boundaries from earlier convection. Radar
    estimated rainfall rates within the most intense cores have been
    above 2"/hr according to KVNX, which has resulted in MRMS measured
    rainfall of more than 3 inches in the past 6-hrs in a few
    locations, including a reported 3.9 inches near Piedmont, KS.

    These outflows will continue to drop steadily southward through
    the next several hours, serving as a focus for additional
    convective development. As the boundaries drop south, they will
    encounter more favorable thermodynamics reflected by the SPC RAP
    analysis indicating a pool of 2500-3500 J/kg of MLCAPE aligned
    with a ribbon of PWs approaching 2 inches. This will continue to
    support intense rainfall rates of more than 2"/hr, and the HRRR
    15-min rainfall accumulation product suggests rates will briefly
    exceed 3"/hr (0.75 to 1 inch in 15 minutes). Additionally, as
    these storms sag south and redevelop along the convergent outflow
    boundaries, the LLJ, currently analyzed via local VWPs to be from
    the SW at 20 kts, will provide additional ascent through
    isentropic upglide while concurrently resupplying the impressive
    thermodynamics into the clusters of storms.

    While the CAMs are exceptionally different with the evolution the
    next few hours, the recent HRRR appears to be catching on to the
    current activity, with some support from the ARW/ARW2 as well.
    Despite the lack of agreement, which is negatively impacting the
    HREF exceedance probabilities, the current radar combined with the
    expected continuation of the favorable thermodynamics suggests
    convection will persist, and may pulse up at times through the
    next few hours. Where this occurs, total rainfall could again be
    1-2" in less than an hour, with local maxima above 3" possible.
    This rain will occur atop soils that are saturated above the 90th
    percentile according to NASA SPoRT from 7-day rainfall that has
    been more than 200% of normal, highest in northeast OK. Any heavy
    rain falling atop these soils, especially if any training can
    occur along the boundary as it sags southward, could cause
    instances of flash flooding.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ry-0Q7fP_V0EQdGocVrPcaNGadbPKLFALlvxxBrHbcEJrFNC4VmT5qzSG1IPAFDpChz= bsV_QfYSy6YLpAjvKLx9AZk$ for graphic product...

    ATTN...WFO...ICT...OUN...TSA...

    ATTN...RFC...TUA...NWC...

    LAT...LON 37999698 37859578 37169522 36619478 36199445=20
    35569430 35199456 35129520 35299608 35679697=20
    36149750 36609785 37319784=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 30 06:34:57 2025
    AWUS01 KWNH 300633
    FFGMPD
    OHZ000-KYZ000-INZ000-ILZ000-301032-

    Mesoscale Precipitation Discussion 0554
    NWS Weather Prediction Center College Park MD
    232 AM EDT Mon Jun 30 2025

    Areas affected...central/southern indiana and vicinity

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 300632Z - 301032Z

    Summary...A loosely organized cluster of showers and thunderstorms
    were repeating over southern Indiana near Bloomington, where 1.75
    inch/hr rain rates and 5-7 inch rainfall totals have been observed
    since 00Z. Flash flooding is likely in this area through 10Z this
    morning.

    Discussion...Scattered showers and thunderstorms over southern
    Indiana are embedded in broad, modest west-southwesterly flow
    aloft currently. Recent radar mosaic imagery indicates that
    convection has begun to take on more of a training character,
    focusing on a subtle confluence axis evident at the surface and at
    850mb via SPC mesoanalyses and surface obs. The convection is
    embedded in 2 inch PW values and around 1000 J/kg MLCAPE.=20
    Meanwhile, upstream convection has deepened across far
    southeastern Illinois that should eventually repeat into areas of
    southern Indiana that have already received heavy rainfall. The
    current scenario suggests that additional 2-5 inch rainfall totals
    area possible in some parts of the discussion area near/south of
    Bloomington and vicinity.

    MRMS Flash responses are in moderate levels across the area that
    has received heavier rainfall over the past 3-6 hours or so.=20
    Additionally, and three-hourly FFG thresholds are in the 2 inch
    range and will likely be exceeded at times as convection moves
    across the region. Flash flooding is likely, and depending on the
    persistence of this band through/beyond 10Z, local significant
    impacts are possible.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_micK7amQXEsIaodOLfMMjMd8F9MhCDDtGLA4Dg_LrI-0dg5Kh4j-D1GiI871z1zpvcQ= yoQ3IdwKWm822Uq0L9d3-1M$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...LMK...PAH...

    ATTN...RFC...TIR...NWC...

    LAT...LON 39898503 39348482 38778508 38378621 38048846=20
    38858809 39258725=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 30 07:01:22 2025
    AWUS01 KWNH 300701
    FFGMPD
    KSZ000-NEZ000-301300-

    Mesoscale Precipitation Discussion 0555
    NWS Weather Prediction Center College Park MD
    300 AM EDT Mon Jun 30 2025

    Areas affected...portions of central Kansas into central Nebraska

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 300700Z - 301300Z

    Summary...A couple of thunderstorm complexes are expected to merge
    across the discussion area though 12Z this morning. Multiple cell
    mergers and localized training should enable development of areas
    of 1-2 inch/hr rain rates and at least isolated instances of flash
    flooding.

    Discussion...A complicated convective pattern is evolving across
    the central Plains currently. A fairly progressive MCS is
    leveraging modest steering flow aloft while forward propagating
    southeastward near LXN/Lexington, NE currently. The orientation
    of the convection and its speed has generally limited rain rates
    to around 1 inch/hr on an isolated basis, resulting in a very
    limited flash flood threat in the short term.

    Farther south, a mature MCS has evolved across southern
    Kansas/northern Oklahoma. This complex is leveraging both steep
    lapse rates aloft (around 7.5C/km) and convergence on the nose of
    a 30kt southwesterly low-level jet centered over northwestern
    Oklahoma and southwestern Kansas. The storms within this complex
    have substantially weaker mid/upper steering flow and are largely
    elevated atop an expanding cold pool. Slow movement has enabled
    several areas of 1-2 inch/hr rain rates to materialize, which has
    fostered isolated flash flood potential especially near Wichita
    where 2 inch/hr FFG thresholds were noted.

    Over the next 6 hours, the meso-to-synoptic setup favors the
    eventual merging of the southern Nebraska and southern Kansas MCSs
    along with intermediate convective development across
    western/central Kansas amid strong low-level convergence and 2500
    J/kg MLCAPE. The increase in convective coverage and relatively
    weak steering flow aloft suggest that areas of 1.5-2.5 inch/hr
    rain rates will become more common with time. These rates will
    exceed FFG thresholds at times - especially across southern NE and
    northern Kansas where 1.5-2 inch/hr thresholds were prevalent.=20
    FFGs are a bit higher with southern extent into Kansas,
    potentially pointing to a somewhat lesser flash flood threat in
    those areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6JQHJw6bFSfE1RGDj0ImMPJ9b_lyFd0k-sn84KNNkWdKaH90doxwtTnplhRUELr9TzOi= MJgXQ5r8roMwQjvVRbVi3lc$ for graphic product...

    ATTN...WFO...DDC...GID...GLD...ICT...LBF...OAX...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 41619840 40389698 38819640 37949679 37499729=20
    37459882 37990035 39040170 39890137 41260022=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 30 07:16:47 2025
    AWUS01 KWNH 300716
    FFGMPD
    OHZ000-KYZ000-INZ000-ILZ000-301032-

    Mesoscale Precipitation Discussion 0554...Corrected
    NWS Weather Prediction Center College Park MD
    315 AM EDT Mon Jun 30 2025

    Corrected for flash flooding "likely" tag

    Areas affected...central/southern indiana and vicinity

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 300632Z - 301032Z

    Summary...A loosely organized cluster of showers and thunderstorms
    were repeating over southern Indiana near Bloomington, where 1.75
    inch/hr rain rates and 5-7 inch rainfall totals have been observed
    since 00Z. Flash flooding is likely in this area through 10Z this
    morning.

    Discussion...Scattered showers and thunderstorms over southern
    Indiana are embedded in broad, modest west-southwesterly flow
    aloft currently. Recent radar mosaic imagery indicates that
    convection has begun to take on more of a training character,
    focusing on a subtle confluence axis evident at the surface and at
    850mb via SPC mesoanalyses and surface obs. The convection is
    embedded in 2 inch PW values and around 1000 J/kg MLCAPE.=20
    Meanwhile, upstream convection has deepened across far
    southeastern Illinois that should eventually repeat into areas of
    southern Indiana that have already received heavy rainfall. The
    current scenario suggests that additional 2-5 inch rainfall totals
    area possible in some parts of the discussion area near/south of
    Bloomington and vicinity.

    MRMS Flash responses are in moderate levels across the area that
    has received heavier rainfall over the past 3-6 hours or so.=20
    Additionally, and three-hourly FFG thresholds are in the 2 inch
    range and will likely be exceeded at times as convection moves
    across the region. Flash flooding is likely, and depending on the
    persistence of this band through/beyond 10Z, local significant
    impacts are possible.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_9rKskqQXgsdlX2UDgUjx6oUPToJiAuBtzc-eLGjGFZ7-WdhDMZL3y_4nJ63JakDmpAE= JmeRQbQJ8zEGiuz5EYfVh4E$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...LMK...PAH...

    ATTN...RFC...TIR...NWC...

    LAT...LON 39898503 39348482 38778508 38378621 38048846=20
    38858809 39258725=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 30 08:40:53 2025
    AWUS01 KWNH 300840
    FFGMPD
    OKZ000-KSZ000-301100-

    Mesoscale Precipitation Discussion 0556
    NWS Weather Prediction Center College Park MD
    440 AM EDT Mon Jun 30 2025

    Areas affected...far southern Kansas into northern Oklahoma

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 300839Z - 301100Z

    Summary...A band of elevated convection extending from near Pratt,
    KS to near Enid, OK has become nearly stationary over the past
    couple hours. Rain rates exceeding 2 inches/hr have been
    estimated in a few spots. These rates will pose an isolated flash
    flood threat for the next 2-3 hours or so.

    Discussion...A mature MCS over northern Oklahoma has experienced a
    complicated evolution this morning, with most of the vigorous
    convection now focused along a band from near Pratt, KS to near
    Enid, OK. This portion of the MCS features mainly elevated
    convection, although that convection has stalled atop expanding
    outflow/cold pool now over northwestern Oklahoma. Furthermore,
    25kt southwesterly 850mb flow was interacting favorably with the
    cold pool to help maintain the convective band while also likely
    helping to maintain elevated instability near the storms. The
    result is an axis of 1-2.5 inch/hr rain rates that has largely
    remained in a similar position over the past 3 hours, with
    MRMS-estimated rainfall totals of 3-5 inches also noted in that
    3-hour timeframe.

    The ongoing heavy rainfall pattern should persist for another 2-3
    hours or so. Later this morning, southwesterly 850mb flow should
    slacken some and result in reduced convergence and influx of
    instability into the convective band. This should result in
    weakening of the band along with lessening of rain rates, although
    specific timing on this anticipated weakening is uncertain. In
    the meantime, 1-2.5 inch/hr rain rates will likely continue. FFG
    thresholds are a bit high in the region (2.5+ inch/hr), but the
    multi-hour nature of the heavy rain threat suggests a continued
    (and at least isolated) flash flood risk through 11Z or so.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!--GcLw0JHkb-BmCswWSHvBLOTyerUqbsv4J5uH4qkmmGgYmCZg5f9Vd_q_gxWK5ky4nm= 5Ymdjh_rjvlMtC393j6NKog$ for graphic product...

    ATTN...WFO...DDC...ICT...OUN...TSA...

    ATTN...RFC...TUA...NWC...

    LAT...LON 37769973 37549783 36139674 35699732 35889924=20
    36649969=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 30 15:40:33 2025
    AWUS01 KWNH 301540
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-302000-

    Mesoscale Precipitation Discussion 0557
    NWS Weather Prediction Center College Park MD
    1139 AM EDT Mon Jun 30 2025

    Areas affected...Portions of the Central Appalachians in PA, MD,
    WV, and VA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 301538Z - 302000Z

    Summary...Thunderstorms should develop between Noon and 2 PM EDT
    in the Allegheny Mountains, Blue Ridge Mountains, southwest
    Pennsylvania, and surrounding areas. The storms may initially move
    slowly to the northeast, and the slow movement and heavy rain
    rates, with over 1 inch of rainfall in an hour, may lead to
    localized flash flooding in the early afternoon.

    Discussion...Thunderstorms will become more numerous over the next
    couple hours in the central Appalachians as most locations reach
    the convective temperature in the low 80s, as indicated in the 12Z
    PBZ and RNK soundings. Initiation will be favored first near the
    ridge lines, and this is already evident in visible satellite
    trends. LightningCast suggests that some lightning, and thus more
    vigorous convective rainfall, may begin by 1630Z in at least a few
    areas of the Allegheny and Blue Ridge Mountains. For the first
    couple hours, convection is likely to move slowly to the northeast
    based on hi-res model reflectivity and deep layer mean wind around
    10-15 knots. In some cases, this may lead to some training
    patterns where the terrain is closer to parallel with the mean
    wind vector. But slow storm motion could sustain heavy rain rates
    long enough over individual locations in general, and that could
    lead to some localized flash flooding.

    The probable increase in flash flood threat in the next few hours
    is supported by the latest 12Z HREF probabilities showing
    increasing chances of 1 inch per hour rain rates and 1hr and 3hr
    FFG exceedance in these areas between 17Z and 20Z. The environment
    is very supportive of intense instantaneous rain rates with
    precipitable water values generally above the 95th percentile for
    late June through the depth of the column (based on overall PW
    percentiles and CIRA layer PW products). Therefore, it would be
    plausible to even see some locations exceed an inch of rain in 30
    minutes in the strongest convection.

    Much of this area will be upgraded to a Slight Risk on the 16Z Day
    1 ERO, which will be issued shortly.

    Lamers

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5krKNLV5io90dzqiAS1bpHKqKXjWBI_GpbTGU8W_XEoQ7jYw6_1exHaUzcEs6JM0IALx= J0kaQFHuByq9cl9ZOVIAdD4$ for graphic product...

    ATTN...WFO...CTP...LWX...PBZ...RLX...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 41237901 40897858 40647797 39587776 38587806=20
    37987901 37237984 37578103 38398081 39497985=20
    39937999 40318031 40858008 41197955=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 30 16:15:37 2025
    AWUS01 KWNH 301540
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-302000-

    Mesoscale Precipitation Discussion 0557
    NWS Weather Prediction Center College Park MD
    1139 AM EDT Mon Jun 30 2025

    Areas affected...Portions of the Central Appalachians in PA, MD,
    WV, and VA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 301538Z - 302000Z

    Summary...Thunderstorms should develop between Noon and 2 PM EDT
    in the Allegheny Mountains, Blue Ridge Mountains, southwest
    Pennsylvania, and surrounding areas. The storms may initially move
    slowly to the northeast, and the slow movement and heavy rain
    rates, with over 1 inch of rainfall in an hour, may lead to
    localized flash flooding in the early afternoon.

    Discussion...Thunderstorms will become more numerous over the next
    couple hours in the central Appalachians as most locations reach
    the convective temperature in the low 80s, as indicated in the 12Z
    PBZ and RNK soundings. Initiation will be favored first near the
    ridge lines, and this is already evident in visible satellite
    trends. LightningCast suggests that some lightning, and thus more
    vigorous convective rainfall, may begin by 1630Z in at least a few
    areas of the Allegheny and Blue Ridge Mountains. For the first
    couple hours, convection is likely to move slowly to the northeast
    based on hi-res model reflectivity and deep layer mean wind around
    10-15 knots. In some cases, this may lead to some training
    patterns where the terrain is closer to parallel with the mean
    wind vector. But slow storm motion could sustain heavy rain rates
    long enough over individual locations in general, and that could
    lead to some localized flash flooding.

    The probable increase in flash flood threat in the next few hours
    is supported by the latest 12Z HREF probabilities showing
    increasing chances of 1 inch per hour rain rates and 1hr and 3hr
    FFG exceedance in these areas between 17Z and 20Z. The environment
    is very supportive of intense instantaneous rain rates with
    precipitable water values generally above the 95th percentile for
    late June through the depth of the column (based on overall PW
    percentiles and CIRA layer PW products). Therefore, it would be
    plausible to even see some locations exceed an inch of rain in 30
    minutes in the strongest convection.

    Much of this area will be upgraded to a Slight Risk on the 16Z Day
    1 ERO, which will be issued shortly.

    Lamers

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9oq2vSjndfvdfxUznyeXb1VL1zbnwv13wmBd_1FUNeE2Oej0ttB7IN5FDrKq5_oBxKWe= koeCY3F58mlm3P4_ZGgp3GY$ for graphic product...

    ATTN...WFO...CTP...LWX...PBZ...RLX...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 41237901 40897858 40647797 39587776 38587806=20
    37987901 37237984 37578103 38398081 39497985=20
    39937999 40318031 40858008 41197955=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 30 17:24:54 2025
    AWUS01 KWNH 301724
    FFGMPD
    COZ000-NMZ000-302200-

    Mesoscale Precipitation Discussion 0558
    NWS Weather Prediction Center College Park MD
    124 PM EDT Mon Jun 30 2025

    Areas affected...Central New Mexico and Far Southern Colorado

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 301718Z - 302200Z

    Summary...Thunderstorms are initiating over the mountains of far
    southern Colorado and central New Mexico in the late morning, and
    should continue to develop into the early afternoon. Any storms
    are likely to be very slow moving to nearly stationary, which will
    pose a threat for localized heavy rainfall and flash flooding
    wherever the storms develop. Burn scars in New Mexico would be
    particularly vulnerable if storms develop nearby, but a threat of
    flash flooding will exist across the region in general.

    Discussion...As of 11 AM MDT, thunderstorms were beginning to
    develop in the favored mountain locations from south-central
    Colorado through central New Mexico. This is expected to continue
    over the next several hours as convective temperature is achieved,
    and hi-res model guidance is consistent in showing a high
    probability of storms through at least 4 PM MDT (22Z), but
    possibly through the remainder of the afternoon. Available
    moisture and instability is not particularly anomalous in this
    case, so the threat of localized heavy rainfall and flash flooding
    should be driven more by extremely slow storm motions. Deep layer
    mean wind is generally around 5 knots or less, and simulated
    reflectivity on the hi-res guidance shows storms more-or-less
    anchored to near their development locations for at least a couple
    hours. So even though the instantaneous to 30-min rain rates may
    not be exceptional, heavy rain could be sustained long enough to
    produce localized rainfall maxima in excess of 2 inches,
    especially in New Mexico. This could be enough to lead to flash
    flooding based on flash flood guidance values. Burn scar locations
    or urban areas would be particularly vulnerable, but any impact
    would be dependent on storms developing close enough to those
    locations.

    Lamers

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_Pui8VAzLlFJfLM41QczHK4q_fnzpu01iBc6LEDgqj3nXeZO_LBX6r0ijlHxJGipTUdg= hGEue2RB7LwECyNxzNd3aCg$ for graphic product...

    ATTN...WFO...ABQ...EPZ...GJT...PUB...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 37730678 37410603 37500499 36850473 36080513=20
    35390520 34810557 34180552 33490550 32820574=20
    32830625 34060655 34900662 35610698 36200727=20
    36780689 37510728=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 30 17:54:54 2025
    AWUS01 KWNH 301754
    FFGMPD
    NJZ000-PAZ000-DEZ000-MDZ000-302200-

    Mesoscale Precipitation Discussion 0559
    NWS Weather Prediction Center College Park MD
    154 PM EDT Mon Jun 30 2025

    Areas affected...Southeast Pennsylvania, Southern and Central New
    Jersey, and Delaware

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 301752Z - 302200Z

    Summary...Isolated to scattered thunderstorms will continue early
    this afternoon in southeast Pennsylvania, southern and central New
    Jersey, and portions of Delaware. At times, these thunderstorms
    may move very slowly or become nearly stationary, which would lead
    to localized areas of very heavy rainfall and potentially flash
    flooding, especially if that occurs over urban areas. The threat
    of flash flooding should be highest through around 5-6 PM EDT, but
    could last longer.

    Discussion...Several well-organized thunderstorms have developed
    in an area of strong instability from SE PA into S NJ and DE.
    Hi-res model guidance has struggled with this, but the
    experimental RRFS may be doing the best as of 1730Z. It shows
    organized but isolated cells or small clusters persisting across
    the area through about 22Z (6 PM EDT), anchoring at times to sea
    breeze boundaries or a front draped across the region. There is
    some evidence of this already happening with a thunderstorm near
    coastal Sussex County, Delaware, and it could conceivably happen
    with other storms elsewhere in the region. The environment is very
    supportive of intense rain rates with PWs near or above 2 inches
    (above the 95th percentile for late June) and very strong
    instability. Therefore, hourly rainfall in excess of 2 inches is
    plausible and if storms stall in a given location for over an
    hour, rapid development of rainfall maxima over 3-4 inches would
    be possible. In these areas, flash flooding could develop,
    particularly if it intersects with urban areas.

    The outlook beyond 21-22Z (5-6 PM EDT) is less certain, as the
    hi-res model guidance doesn't look to be completely reliable. It
    seems doubtful that all the instability in the region would be
    completely exhausted by that time, so a continuation of the flash
    flood threat could continue into the early evening. However, the
    threat may shift to areas just outside where initial development
    is occurring.

    Lamers

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-ikzzo3BcEBkJ5Yx9c5lyDTmlbXGWCTsyOCFkQYjxBt_tCvvW41MUTQJOU15BIsiEHIh= n6TnJqEPgwu14Ii9wlPhU4M$ for graphic product...

    ATTN...WFO...AKQ...CTP...PHI...

    ATTN...RFC...RHA...NWC...

    LAT...LON 40897571 40737499 40397396 39817396 39407463=20
    38997486 38377496 38457537 38977564 39537578=20
    39827614 40147705 40807667=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 30 22:12:58 2025
    AWUS01 KWNH 302212
    FFGMPD
    NYZ000-NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-WVZ000-OHZ000-KYZ000-010330-

    Mesoscale Precipitation Discussion 0560
    NWS Weather Prediction Center College Park MD
    612 PM EDT Mon Jun 30 2025

    Areas affected...Eastern OH...West Virginia...Northern MD...Pennsylvania...Southern NY...Parts of NJ

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 302210Z - 010330Z

    SUMMARY...Unstable, very moist rich environment will likely
    continue to support hourly rates of 2"+. Storm interactions with
    possible repeating may generate spots of 2-3" resulting in widely
    scattered incidents of possible flash flooding past nightfall.

    DISCUSSION...GOES-E WV suite depicts a broad area of disturbed
    weather at the apex of large scale ridging over the southern
    Mid-Atlantic and points south. A digging large scale trough over
    the Upper Great Lakes is providing oblique right entrance ascent
    across the Lower Great Lakes, helping to drive deeper layer
    southwesterly flow and associated anomalous (1.5-2.5 standard
    anomalies) deep moisture through the Upper Ohio River Valley into
    the northern Mid-Atlantic and Northeast, ranging mainly above 2",
    with spots of 2.25" noted. A slow moving warm front leads the
    ushering of enhanced moisture and unstable air across the Hudson
    Valley into the Lower Mohawk Valley, though much of the area
    upstream remains quiet unstable with pockets of 2000-3000 J/kg
    still remaining toward the end of day (greater further east into
    the Mid-Atlantic).

    Visible and 10.3 EIR loops show numerous clusters of thunderstorms
    across the area; though as each has cycled and produced outflow to
    support newer downstream generations; the broad southwesterly
    steering upstream has brought some increased organization into
    some SW to NE linear features through E OH/W PA into WV. Flow is
    stronger having limited duration for initial
    development/downdrafts, but with the component of alignment to the
    mean wind, there are widely scattered incidents of short-term
    training increasing duration to support localized 1.5- 2" totals.
    Within the complex terrain that still remains fairly well
    saturated, these localized totals may induce flash flooding given
    hourly FFG over 1-1.5" and less than 2" in 3hrs; but may only
    affect one or two watersheds/narrow valleys in the Allegheny
    Plateau.

    Further east, cell motions are a bit weaker being closer to the
    apex of the larger scale ridge, though larger outflow boundaries
    are being generated and interacting with Bay/Ocean Breeze or other
    outflow boundaries to trigger newer/broader updrafts. Storm
    interaction may further slow forward motions resulting in
    increased duration that may last for slightly greater than 1hr. So
    spots of 2-3" are possible as 18z HREF suggests with 40-50%
    neighborhood probabilities for 2" and 20-30% exist over
    east-central PA into N MD. As such, incidents of widely scattered
    flash flooding remain possible through the late evening into early
    overnight as instability slowly diminishes with loss of solar
    heating.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7Br1aZ4UwNf_HXpYwde9yFHWOEa8DJkYYExKm30Ls9GFxAxtDEpI841UaHdntHyDkLO9= TZfEtVAsMIoFssLtHIR-ac8$ for graphic product...

    ATTN...WFO...BGM...BUF...CLE...CTP...ILN...LWX...PBZ...PHI...
    RLX...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 42897624 42387504 41017468 40357465 39577591=20
    39247672 39057733 38647910 38208089 37738173=20
    37948231 38848362 40588259 41718137 42357991=20
    42657818=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jun 30 22:39:43 2025
    AWUS01 KWNH 302238
    FFGMPD
    TXZ000-OKZ000-010340-

    Mesoscale Precipitation Discussion 0561
    NWS Weather Prediction Center College Park MD
    637 PM EDT Mon Jun 30 2025

    Areas affected...Southern Oklahoma...North and Northwest Texas...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 302240Z - 010340Z

    SUMMARY...Initially slow moving, but very efficient thunderstorms
    with 2-2.5"/hr rates will slowly propagate south and westward with
    storm mergers and localized spots of 3-4" resulting in scattered
    incidents of possible flash flooding

    DISCUSSION...GOES-E 10.3um EIR shows explosive convective
    development along the stalled outflow boundary from this morning's
    convective complex from Hughes to Comanche county. MLCAPEs to
    4000 J/kg and total PWats of 2" were trapped along the
    northwestern edge of the sub-tropical ridge over much of Texas
    into the northwest Gulf, the return flow axis remained nearly
    aloft and generally parallel to the surface outflow boundary
    though the dip (positive tilt) in the northern stream synoptic
    trough has helped with support a 50kt jet with broad right
    entrance ascent across much of the TX Panhandle into central OK.

    Southerly flow across TX but northern flow out of KS/N OK has
    helped to provide ample directional convergence but recent uptick
    to 20kts from th south/southwest provided the deep layer
    convergence to result in the entire line developing. CIRA LPW
    shows the convergence is further increasing flux and TPW values of
    2-2.25" that deep layer vertical moisture flux will support very
    efficient rates up to 2-2.5"/hr. That directional shear and
    proximity to the jet also support a bit of effective bulk shear
    toward 20-25kts for modest organization to keep the downdrafts
    fully collapsing into the updrafts and with weak dry air only a
    few hundred J/kg will be utilized for cold pool generation.=20
    Combine that with weak steering flow through depth toward the east
    at 5kts; propagation will likely be mostly south and west into the
    15-20kts of confluent boundary layer flow. So a hour or so should
    support localized totals up to 3-4" before dropping south and
    west.=20

    Interaction with cells developing along outflow boundaries from
    older complex over the Permian Basin will increase potential for
    mergers and storm scale interaction to help cells increase totals
    as the complex drops southward into northern TX as well. FFG
    values are reduced further north, so best potential will be early
    before moving into higher FFG values along/south of the Red River,
    but localized flash flooding is still possible .

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!894nxsMkMuuDXxCipbCVd18CuWJnYxbuetLGZlXB_WmMGDLjcTLYAxpg7GQQxdVizjEu= vbagok35x2XvtmbL2rlIN6w$ for graphic product...

    ATTN...WFO...FWD...LUB...OUN...SJT...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35319714 35099567 34389521 33349583 32929803=20
    32589952 32920040 33380108 33890099 34350044=20
    35069890=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 1 00:50:19 2025
    AWUS01 KWNH 010049
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-010630-

    Mesoscale Precipitation Discussion 0562
    NWS Weather Prediction Center College Park MD
    849 PM EDT Mon Jun 30 2025

    Areas affected...Southeast MO...Southern IL...Southwest IND...Far
    Western KY...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 010050Z - 010630Z

    SUMMARY...Slow moving, efficient thunderstorms to increase in
    coverage with cell mergers, potential repeat tracks resulting in
    localized 2-4" totals resulting in scattered possible flash
    flooding tonight.

    DISCUSSION...GOES-E WV suite shows a southern stream shortwave
    sliding out of SE MO into S IL south of the digging synoptic
    northern stream trough across WI to NE KS with an associated cold
    front. This front continues to dig south across the middle Great
    Lakes but due to the shortwave, a weak surface wave has developed
    in the buckling mid-level flow near Quincy, IL; before the cold
    front digs across central MO. The mid-level binary interaction
    between the shortwave and northern stream will further slow deep
    layer flow and help with boundary layer cyclogenesis
    near/southeast of the St.Louis Metro.=20

    Low level winds are already backing and deep layer moisture is
    increasing across S IL with solid convergence breaking out
    numerous updrafts. MLCAPEs of 2000+ J/kg and PWats over 2" will
    allow for strong moisture flux convergence into stronger updrafts
    and will support rates of of 2-2.25"/hr. These cells should
    remain along the southeast and eastern quadrants of the shortwave
    with perhaps a flanking line along the effective cold
    front/trailing convergence trof back into the Bootheel of MO.=20
    Cell motions will continue to be eastward to east-northeastward
    with some solid potential for mergers/training. Spots of 2-4"
    will become scattered acoss S IL into SW IND/W KY over the next
    4-6hrs with possible localized flash flooding.

    A bit more uncertainty with respect to flash flooding will occur
    with ongoing cells along the synoptic cold front. Most should
    remain progressive, but near the pivot; deeper confluence and
    chaotic cells motions as the cyclone tries to vertically
    stack/pivot may allow for some widely scattered cells that could
    pivot or potentially remain stationary as well. Cells may
    initially be close to Metro St. Louis to further make evolution of
    potential flash flooding more concerning, as broader impermeable
    surfaces would result in greater runoff IF cells do end up
    lingering in that vicinity further increasing potential for flash
    flooding.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!44AqSVeDllzwflwf0drMlrW1BejRylhHjVeRkBfuXLOCpkfj6FnkpP0-rqT5BzrPLrV_= xPvPaqHPxh4o5iUAMZxKWkM$ for graphic product...

    ATTN...WFO...ILX...IND...LSX...MEG...PAH...

    ATTN...RFC...KRF...MSR...ORN...TIR...NWC...

    LAT...LON 39938840 39818771 39178716 38418712 37948730=20
    37568743 36628879 36378987 36499049 37299055=20
    37889064 38559137 38949136 39299103 39528961=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 1 01:34:03 2025
    AWUS01 KWNH 010133
    FFGMPD
    TNZ000-MSZ000-MOZ000-ARZ000-OKZ000-010700-

    Mesoscale Precipitation Discussion 0563
    NWS Weather Prediction Center College Park MD
    933 PM EDT Mon Jun 30 2025

    Areas affected...Central AR...Southeast OK...Western TN...Northern
    MS...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 010135Z - 010700Z

    SUMMARY...Very moist/unstable axis with favorable deep layer flow
    for repeating/training cells. Spots of 2-4" totals in
    short-duration pose localized flash flooding through the early
    overnight period.

    DISCUSSION...RAP analysis shows deep layer convergence,
    particularly along the upwind convergence zone along northwest
    edge of 850mb ridge near mature convective complex in Southwest
    OK. A speed max of 20-25kts at 925-850mb is pressing eastward and
    expanding the convective line into western AR. The stronger
    convergence connects up to the old outflow boundary from last
    evening and intersects with the far southwest edge of trailing
    confluence of the exiting MCV/shortwave in SE MO. Total PWats are
    well above normal in the 2-2.25" range throughout the axis which
    further increases as westerly winds back to more southerly through
    the MS Valley into W TN/NW MS; resulting in enhanced instability
    pools of 2500-3000 J/kg across central AR and into the Delta
    Region.=20

    Northern stream trough is digging with warming in the GOES-E WV
    suite across NEB entering KS/NW MO. This will continue to
    maintain stronger deeper layer steering flow parallel to the
    boundary; though broaden the focus of convergence a bit more north
    to south. As such, 850mb winds will maintain and be more westerly
    to support back-building environment with deep layer westerly flow
    across AR. So with stronger updrafts and very deep moisture,
    vertical moisture flux could support 2-3"/hr rain rates; though
    there is some uncertainty cells will order to train ideally for
    sizable totals to exceed higher FFG values across SW to central
    AR.=20=20

    Convergence reduces across central to eastern AR before increasing
    again where LLJ has turned more southerly through the MS River
    Valley. This will reduce favorable training orientation, but
    stronger updrafts moving across reduced FFGs and recently
    saturated soils across N MS and W TN may allow for widely
    scattered 2-3" totals resulting in localized flash flooding
    through the early overnight period.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_uxYNr-16LVX457Am9wU5GKgi1SaupoaN1EJNERrys6QR_Y0wn5BHfZge4CxnRL_mHn_= mFaf8WVvz2pKdjMMvlXjBY4$ for graphic product...

    ATTN...WFO...JAN...LZK...MEG...SHV...TSA...

    ATTN...RFC...ALR...ORN...TUA...NWC...

    LAT...LON 36328880 35908822 34908833 34098899 33929084=20
    33839179 33759310 33809478 34469514 35089450=20
    35179264 35449106 36249019=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 1 03:29:32 2025
    AWUS01 KWNH 010329
    FFGMPD
    NJZ000-PAZ000-DEZ000-MDZ000-WVZ000-010727-

    Mesoscale Precipitation Discussion 0564
    NWS Weather Prediction Center College Park MD
    1128 PM EDT Mon Jun 30 2025

    Areas affected...southern/southeastern Pennsylvania and vicinity

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 010327Z - 010727Z

    Summary...Additional flash flood impacts are possible as deep,
    moist convection migrates from west-southwest to east-northeast
    across the region. Over time, nocturnal low-level stabilization
    should result in lesser coverage of storms through 07Z.

    Discussion...Flash flood potential continues across the discussion
    area, with significant impacts noted in/near Lancaster County, PA
    recently. The region remains under the influence of weak
    mid-level shortwave troughs passing over the region. These
    troughs were interacting with a very moist, unstable airmass (2+
    inch PW values and 1000+ J/kg MLCAPE) to promote scattered to
    widespread thunderstorm development. Some of these storms were
    training, with 1-2 inch/hr rain rates falling near Lancaster,
    Reading, and surrounding locales on top of saturated grounds that
    have already experienced 2-6 inches of rainfall today. Locally
    significant flash flood impacts are expected to continue in the
    short term (through 05-06Z).

    Over time, nocturnal boundary layer stabilization should result in
    a decrease in convective coverage across the discussion area.
    However, low-level flow into the discussion area remains strong
    (25-30 kts at 850mb) and a pool of 2000+ J/kg MLCAPE resides over
    Maryland just south of ongoing, strong convection. Mid/upper
    level fields also aren't necessarily prohibitive of any
    redevelopment of convection through the night. Although
    convective coverage is expected to decrease some over the next 2-4
    hours, sensitive areas of southeastern Pennsylvania (especially
    those that are already experiencing significant flash flood
    impacts) will need to be monitored carefully for additional heavy
    rainfall episodes through 07Z/3a EDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!45x22xs5QR6l0k90yrp21pYNuFEdySiVvMeNlHznflO_mkeliLby8B0bpm3USZ5HvWwl= BRfv0-xIB4gV6EOkoI6ua20$ for graphic product...

    ATTN...WFO...BGM...CTP...LWX...PBZ...PHI...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 41417691 41187566 40497462 39847443 39317530=20
    39267695 39767837 40417905 41237832=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 1 04:17:07 2025
    AWUS01 KWNH 010415
    FFGMPD
    OHZ000-KYZ000-INZ000-ILZ000-010814-

    Mesoscale Precipitation Discussion 0565
    NWS Weather Prediction Center College Park MD
    1215 AM EDT Tue Jul 01 2025

    Areas affected...southern Indiana and vicinity

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 010414Z - 010814Z

    Summary...A cluster of thunderstorms was moving toward sensitive
    parts of Indiana that received 3-11 inches of rainfall over the
    past 24-36 hours. Flash flooding is likely with this activity.

    Discussion...Deep convection has persisted across much of
    southern/southeastern Illinois over the past couple hours despite
    nocturnal boundary layer cooling. Abundant low- and mid-level
    moisture across the area ahead of the convection was helping to
    maintain an axis of 1000-1500 J/kg MLCAPE ahead of the storms
    while also supporting efficient rain rates within the convection.=20
    Areas of 1-3 inch/hr rain rates have been estimated per MRMS,
    which has occasionally exceeded local FFG thresholds and prompted
    spots of low to moderate MRMS Flash responses.

    Unfortunately, this cluster of heavy-rain-producing convection was
    moving toward portions of southern/central Indiana (near
    Bloomington) that have received between 3-11 inches of rainfall
    over the past 24-36 hours. Ground conditions are saturated as a
    result, and it is likely that as the cluster of storms moves
    eastward, FFG thresholds will be exceeded and excessive runoff
    will occur. Locally significant flash flood impacts cannot be
    ruled out.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9d8SB6JBcr5mvmQK6Y3CshSOz-9cUZvGD00qlTjNBTdHCa8xM0rrhTH0QYpFlqphTuHu= tByvELhu7-7iks58FArI734$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...LMK...LSX...PAH...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 39848510 39498437 38818470 38088624 37888802=20
    38178930 39328825 39588738=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 1 12:13:06 2025
    AWUS01 KWNH 011213
    FFGMPD
    PAZ000-MDZ000-WVZ000-OHZ000-KYZ000-INZ000-011810-

    Mesoscale Precipitation Discussion 0566
    NWS Weather Prediction Center College Park MD
    812 AM EDT Tue Jul 01 2025

    Areas affected...Portions of the Upper Ohio Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 011210Z - 011810Z

    SUMMARY...Ongoing showers and embedded thunderstorms across the
    Ohio Valley are expected to increase in coverage this morning,
    while potentially repeating and containing rainfall rates briefly
    over 2"/hr. Low FFG and saturated soils in the region elevate the
    potential for isolated to scattered instances of flash flooding
    through at least midday.

    DISCUSSION...GOES-EAST WV-ML imagery this morning shows a
    pronounced upper trough sliding across the Great Lakes and Midwest
    while strong northeasterly flow aloft occurs downstream over the
    Upper Ohio Valley. Showers and embedded thunderstorms are already
    evident on radar this morning and mostly progressing
    east-northeast ahead of an approaching cold front. Model soundings
    in the Ohio Valley suggest convective temperatures around 80
    degrees, which should be realized after a few hours of mid-morning
    sunlight. This will allow for thunderstorm coverage to blossom
    quickly both ahead and along the approaching cold front, which
    will increase the scattered flash flooding threat. Precipitable
    water values remain high when compared to climatology with values
    ranging from 1.7-2.1" (highest over KY and southern IN) per SPC's
    mesoanalysis, allowing for thunderstorms to contain efficient
    rainfall and hourly rates potentially reaching 2-2.5".
    Additionally, westerly flow throughout the column will support any
    activity forming ahead of the cold front to potentially train in
    an east-west orientation.

    Both HRRR and experimental RRFS guidance this morning show the
    potential for isolated 2-3" totals by about 18z and the 06z HREF
    depicts low chances (20-25%) of exceeding 3". However, this part
    of the country contains saturated and sensitive terrain
    susceptible to flash flooding. NASA SPoRT highlights 0-40cm soil
    moisture percentiles above the 80th percentile across much of
    southern OH and southwest PA. Additionally, FFG remains low and is
    largely below 2" in 3 hours, something well within reach on a
    scattered basis per the latest available CAMs. Given the largely
    isolated to scattered nature of convection and the potential for a
    localized linear axis of repeating cells, flash flooding is
    considered possible. Should convection repeat over communities
    most prone to flooding and given the moist environment at hand,
    locally considerable flooding is also possible through at least
    midday.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8l7utONPybga3tzZmMyGp_tz5OEAKnklu_u0qVevo3_PA8tVL61IJM3Enkj6-gKYkYH0= 84Hy2buirMZhcb9rGnlz5Ds$ for graphic product...

    ATTN...WFO...CLE...CTP...ILN...IND...JKL...LMK...PBZ...RLX...

    ATTN...RFC...TIR...NWC...

    LAT...LON 40577916 40087886 39217957 38388090 37968258=20
    37778400 37728559 38098620 38828602 39658527=20
    40128429 40368288 40518098=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 1 16:34:42 2025
    AWUS01 KWNH 011633
    FFGMPD
    NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-DCZ000-WVZ000-012230-

    Mesoscale Precipitation Discussion 0567
    NWS Weather Prediction Center College Park MD
    1233 PM EDT Tue Jul 01 2025

    Areas affected...Parts of the Central Appalachians and
    Mid-Atlantic

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 011630Z - 012230Z

    SUMMARY...Widespread showers and thunderstorms are expected this
    afternoon across the central Appalachians into the Mid-Atlantic
    within a very moist and unstable environment. Maximum rainfall
    rates of 2-3"/hr are anticipated and may overlap with the highly
    urban corridor between Washington D.C. and Philadelphia, as well
    as compromised terrain in southeast PA due to heavy rainfall last
    night. Numerous instances of flash flooding are likely, with some
    significant imapacts possible.

    DISCUSSION...GOES-East visible satellite imagery depicts a growing
    cumulus field along the Blue Ridge Mts of northern/central VA
    through the Mid-Atlantic, with recent LightningCast values spiking
    along the Blue indicative of convective initiation imminent (seen
    now on radar after 1610Z). These storms are developing ahead of an
    upper trough swinging through the Midwest, prompting strengthening west-northwesterly mean layer flow. Additionally, GOES-EAST WV-ML
    highlights a disturbance off the Southeast coastline which is
    helping to squeeze mid-to-upper level moisture transport towards
    the central Appalachians and Mid-Atlantic. PWATs are well above
    climatology (above the 90th percentile per the 00z ECENS) and even
    over the daily record for IAD (12z sounding of 2.07").
    Additionally, clear skies most of the morning across much of the
    Mid-Atlantic has allowed for SBCAPE to increase over 4000 J/kg
    from the central Chesapeake Bay northward into central NJ per
    SPC's mesoanalysis. The greatest bulk shear remains to the north
    over PA, but local bay/sea breezes and terrain should help
    developing updrafts organize and maintain strength.

    Additionally, the mean layer west-northwesterly flow will allow
    for repeating cells in this direction as leading convection
    eventually merges with activity progressing over the central
    Appalachians. Rainfall rates are likely to be very intense within
    the available environment and produce hourly rates up to 3", with
    instantaneous rates even higher. The limiting factor remains if
    convection can remain progressive, which would reduce the
    potential rainfall totals but not limit the impacts from rainfall
    rates alone. Southeast PA in particular is extremely susceptible
    to these intense rainfall rates as 1-hr FFG in the area is below
    1". It is this region, and the highly urbanized locations, where
    significant impacts are most likely should convection overlap and
    rainfall amounts maximize the available environment. Elsewhere
    across the Mid-Atlantic, scattered to numerous instances of flash
    flooding are also likely, but progressive west-northwesterly storm
    motions should limit severity.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_tULk7ArSfYZoKFHpQZiGsb0fKAJSZ5cGT6wyCiRur84oXeUcLoOTtQK85VqMTkBX1En= KRQakoOpCamDAvpG9yXfC-g$ for graphic product...

    ATTN...WFO...AKQ...CTP...LWX...PBZ...PHI...RLX...RNK...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 40867651 40597506 40107395 39557406 39207530=20
    38927633 38337757 37837852 37817937 38277981=20
    39397947 40447886 40857783=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 1 17:49:37 2025
    AWUS01 KWNH 011749
    FFGMPD
    TXZ000-012250-

    Mesoscale Precipitation Discussion 0568
    NWS Weather Prediction Center College Park MD
    148 PM EDT Tue Jul 01 2025

    Areas affected...South Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 011750Z - 012250Z

    SUMMARY...Scattered showers and thunderstorms moving
    north-northwestward into South Texas are capable of producing
    isolated instances of flash flooding and 2-3"/hr rates through at
    least early this evening.

    DISCUSSION...Latest radar and satellite imagery depicts
    north-south bands of tropical downpours streaming north-northwest
    into South Texas from the northern Gulf Coast of Mexico. These
    thunderstorms are occurring on the northwest periphery of a
    mid-level low churning over north-central Barry (can be tracked to
    the remnants of former T.S. Barry). Maximum estimated hourly
    rainfall rates from MRMS are around 2-2.5" over the last hour or
    so, with 1.55" recorded at the Brownsville International Airport
    over the last 3 hours. While this initial band appears to hang up
    along the coast, a separate one approaching from far northeast
    Mexico may provide greater coverage of heavy rainfall this
    afternoon based on recent radar scans and strong southerly 850-700
    flow around 20-25 kts. This is allowing PWs to remain well above
    what's necessary for intense rainfall rates as values climb to
    near 2.5" (over the 95th climatological percentile per the 00z
    ECENS). Additionally MLCAPE values of 1000 J/kg remain just inland
    from the Gulf as 2000 J/kg linger in the inflow region over the
    far western Gulf. Even though storm motions may be fast and on a north-northwesterly direction, upwind propagation vectors are weak
    and may lead to backbuilding towards the higher instability over
    the western Gulf. This supports an environment for additional
    heavy rainfall that may compound to lead to isolated flash
    flooding concerns over a region with relatively high FFG.

    3-hr FFG in far South Texas remains around 3", locally lower along
    the Rio Grande Valley. Even though CAMs are highly uncertain
    regarding the northward extent of heaviest thunderstorms, 12z HREF
    probs of at least 3" in 6-hrs (ending 21z) are around 30% for the
    southern Rio Grande Valley region of South Texas. This again when
    combined with current radar/satellite supports the potential for
    localized instances of flash flooding.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!517jVvMtSJcexGf_MNgLKbNenlxCfNRbdBslmsMOBOK1eF02mpGkx0auV3T8X_6pJ7l2= Jx3Q7OOtI07xuAd0JywvaTs$ for graphic product...

    ATTN...WFO...BRO...CRP...

    ATTN...RFC...FWR...NWC...

    LAT...LON 27889929 27799841 27129731 26369696 25819719=20
    25769779 26179878 26749953 27449971=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 1 18:25:09 2025
    AWUS01 KWNH 011825
    FFGMPD
    MDZ000-VAZ000-NCZ000-WVZ000-OHZ000-TNZ000-KYZ000-020024-

    Mesoscale Precipitation Discussion 0569
    NWS Weather Prediction Center College Park MD
    224 PM EDT Tue Jul 01 2025

    Areas affected...Eastern Ohio Valley and Central Appalachians

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 011824Z - 020024Z

    SUMMARY...Slow moving thunderstorms are advancing ahead of a
    sweeping cold front and producing rainfall rates briefly over
    2"/hr. These storms are expected to continue through this
    afternoon and move over particularly flash flood-prone terrain.

    DISCUSSION...Current radar observations depict widely scattered
    thunderstorms pushing eastward across the eastern Ohio Valley and
    central Appalachians. Some storms over western NC and VA were
    initially tied to the terrain, but have begun to slowly progress east-northeast. Otherwise, thunderstorm activity spanning from
    eastern TN to WV is ahead of an advancing cold front and upper
    level trough clearly evident in GOES-East WV-ML imagery. This
    region also continues to fall within a favorable right entrance
    region of an upper jet racing northeastward from northern OH.

    PWATs remain high and above 2" for parts of eastern KY per SPC's
    mesoanalysis, with mean layer winds out of the west-southwest.
    This supports the ongoing and expected heavy rainfall rates as
    storms progress eastward. SBCAPE also continues to increase and is
    estimated above 3000 J/kg across southwest WV as of 18z. However,
    given the current coverage of thunderstorms in an east-west
    orientation, repeating rounds of storms are possible and likely to
    lead to scattered instances of flash flooding. 3-hr FFG in this
    region spans from 3" to as low as 1.5" along the Appalachian
    crest. The 12z HREF highlights a large region as having 40-60%
    chances for exceeding 2" per 3-hrs by 00z tonight across southern
    WV, eastern KY, and along the central Appalachians of southwest VA
    and northwest NC. The available environment combined with ongoing
    radar represations and CAM output leads to the expectation for
    additional scattered flash flooding, with the most likely impacts
    for the typically flood-prone terrain.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9zhBV9zbbCjX1ARKKk-QdIBpxyR548A71RlGCW2MVFggbWTKIbeNj3uXd2iemuAwmlp5= pGe7pzyXrBhtDSl80UdR1vU$ for graphic product...

    ATTN...WFO...GSP...ILN...JKL...LMK...LWX...MRX...PBZ...RLX...
    RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 39488018 39187933 38187932 37187970 36348062=20
    36018218 36098392 36558473 37328458 38468326=20
    39308130=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 1 22:46:51 2025
    AWUS01 KWNH 012245
    FFGMPD
    NJZ000-DEZ000-MDZ000-VAZ000-NCZ000-SCZ000-TNZ000-020444-

    Mesoscale Precipitation Discussion 0570
    NWS Weather Prediction Center College Park MD
    644 PM EDT Tue Jul 01 2025

    Areas affected...Portions of the Mid-Atlantic and Northeast

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 012244Z - 020444Z

    Summary...Flash flooding threat will continue through the evening
    hours as cells containing 2-3"/hr rainfall rates at times train
    and repeat.

    Discussion...Radar depicts widespread thunderstorm coverage across
    the Mid-Atlantic and Northeast ahead of an approaching shortwave
    trough and associated cold front. Throughout the afternoon,
    training and repeating of these storms along a northeast-southwest
    axis led to prolific heavy rainfall across the region, with
    numerous instances of flash flooding reported.

    Over the last several hours, the most intense cells have
    propagated southeastward into the instability axis, characterized
    by 2000-3000 J/kg of MLCAPE and 2-2.3" PWATs according to
    objective analysis output. This regime should continue through the
    evening hours, with periods of cell training expected as the
    steering flow remains quasi-parallel to the synoptic forcing and
    leading composite outflow. The approaching shortwave trough and
    strengthening right-entrance region ascent this evening should
    also favor expanding convective coverage over the next several
    hours. Recent runs of both the HRRR and RRFS consistently depict
    swaths of 2-4" through 4-5Z across the highlighted region where
    cells can train the longest. This should maintain the threat of
    flash flooding through the evening hours -- some of which could be
    significant if it can overlap with hard hit areas.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_Zd6WnU0LOfO_Sk4BN7th6XED3_DOUPWBDj2QEvmYfmUChjue6a4z9ejZND7kWC7ug4n= DL_CJ63GKZSZ0jpygCe8_pI$ for graphic product...

    ATTN...WFO...AKQ...GSP...LWX...MRX...PHI...RAH...RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 40087395 39467375 38147530 37367678 36857781=20
    36097948 35118126 35248209 36378183 37897973=20
    38707704 39807495=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jul 2 12:37:17 2025
    AWUS01 KWNH 021237
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-021800-

    Mesoscale Precipitation Discussion 0571
    NWS Weather Prediction Center College Park MD
    836 AM EDT Wed Jul 02 2025

    Areas affected...High Deserts of California and Nevada

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 021235Z - 021800Z

    Summary...Showers and thunderstorms blossoming across the High
    Deserts of the Southwest will continue through the morning.
    Despite fast motion, rainfall rates of 0.5"/hr could result in
    instances of flash flooding.

    Discussion...The regional radar mosaic this morning shows rapidly
    expanding showers and embedded thunderstorms blossoming across
    southeast CA and southern NV. These storms are developing despite
    modest instability (SPC RAP analysis 500 J/kg of MUCAPE) but with
    a steady increasing trend noted. This instability is overlapping
    with PWs that are as high as 0.8 to 1.2 inches, or above the 90th
    percentile for the date. Offsetting the modest thermodynamics,
    forcing for ascent is increasing downstream of a strengthening
    upper trough digging across CA leaving height falls and spokes of
    vorticity/PVA across the Southwest, collocated with a low-level
    convergence axis on the periphery of an 850mb moisture surge out
    of Arizona. This ascent is helping to cause the rapid increase in
    convective coverage this morning.

    Rainfall rates have been estimated via KESX to be as high as
    0.5"/hr at times, which despite rapid storm motions on 850-300mb
    mean winds of 20-25 kts from the south, has produced 3-hr rainfall
    according to MRMS of up to 0.75 inches. As the ascent continues to
    maximize through the morning downstream of the upper trough, the
    low-level flow surges higher moisture northeast, and instability
    climbs through the morning, activity should expand and intensify.
    Although the CAMs are struggling with the coverage and intensity
    of ongoing convection, the environment suggests that storms should
    continue for several more hours, and the HRRR-forced UA WRF
    indicates rain rates will continue at as much as 0.5"/hr through
    this aftn with a slow northward advance of heavy rainfall. At the
    same time, convection will likely build repeatedly into the
    greater thermodynamics over the High Deserts of CA, with lines of
    storms training south to north producing locally as much as 1.5"
    of rain.

    These impressive rain rates will move across soils that are
    saturated above the 90th percentile with respect to 0-40cm depths
    according to NASA SPoRT. While impacts due to this rainfall are
    likely to be isolated and focused across any sensitive terrain
    features or urban areas, where any longer-duration training can
    occur through the next several hours, instances of flash flooding
    are possible.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_yV5bA2r-YrpC5-cxWemp6wayyCv4X9W8JMxXw4iO7pjXjHkr3MEhMYnxZ7j3q9ytU7d= fFZ8h7lJR33hfaLKKeb1EDg$ for graphic product...

    ATTN...WFO...HNX...LKN...PSR...SGX...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 38391576 38031475 37381394 36081394 34941409=20
    34231431 33861470 33831530 33981583 34391647=20
    34911710 35691768 36621780 37941705=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jul 2 15:28:18 2025
    AWUS01 KWNH 021526
    FFGMPD
    VAZ000-NCZ000-SCZ000-022100-

    Mesoscale Precipitation Discussion 0572
    NWS Weather Prediction Center College Park MD
    1126 AM EDT Wed Jul 02 2025

    Areas affected...Pee Dee region of SC through the Tidewater region
    of VA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 021525Z - 022100Z

    Summary...Showers and thunderstorms will gradually expand in
    coverage and intensify through the afternoon ahead of a front
    sagging slowly across the area. Rainfall rates at times this
    afternoon will likely exceed 2"/hr, leading to 2-3" of rain with
    locally higher amounts approaching 5". Flash flooding is possible.

    Discussion...Showers and thunderstorms are expanding across
    eastern/central North Carolina and far southern Virginia this
    morning. This convection is blossoming rapidly downstream of a
    slow moving, almost stationary, front which will eventually kick
    east as a cold front later this afternoon. The evolution of this
    front will be driven by a mid-level trough axis that will
    gradually swing east, and the overlap of the accompanying height
    falls with low-level convergence along the front will drive ascent
    to produce numerous thunderstorms through the afternoon. The
    environment into which this ascent will impinge will become
    increasingly favorable for heavy rainfall as 850mb SW flow of 20
    kts resupplies PWs of 2-2.2 inches and MLCAPE of 1000-2000 J/kg
    northeastward. Additionally, this low-level inflow will equal or
    exceed the mean wind in the generally weakly forced environment,
    suggesting additional ascent through convergence.

    Rainfall rates so far this morning have been estimated to be above
    2"/hr in the strongest cores, and a flash flood warning was just
    issued near Emporia, VA. While general cell motions have been
    modest on 0-6km mean winds of 15 kts, effective storm motions are
    much slower thanks to Corfidi vectors aligned increasingly
    anti-parallel to the mean flow and collapsed to just 5kts or less.
    This suggests that as the afternoon progresses and storms become
    more numerous, backbuilding/training of cells will become more
    common, lengthening the duration of heavy rainfall across many
    areas. Both the HREF and REFS suggest a moderate/high chance
    (40-70%) of rainfall rates exceeding 2"/hr, and with warm cloud
    depths rising to 13,000-14,000 ft, efficient warm rain processes
    may produce brief 3+"/hr rates. Through training, this has the
    potential (40-60% chance) of producing 2-3" of rain, with locally
    as much as 5" possible.

    FFG across this region is elevated (generally 3-4"/3hrs) so
    exceedance probabilities arelow, peaking at just 10-20%. This
    should generally limit the coverage of flash flood impacts today.
    However, the intensity of these rain rates, especially where
    training occurs or if they repeat across urban areas, could result
    in instances of flash flooding through the afternoon.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!75qQqfzl-yuapZAnE9C8i93lZa6z7NJym1GEuz-7KLWFd3ROPX9QWTou-OeIvczrIf_5= 5RNe9aaNSo8PjNuSToj9wBU$ for graphic product...

    ATTN...WFO...AKQ...CAE...GSP...ILM...MHX...RAH...RNK...

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37367652 37087614 36777590 36237548 35677540=20
    35207583 34687690 34277766 34027809 33937846=20
    34097911 34318003 34538030 34868032 35487990=20
    36397902 37247742=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jul 2 18:52:17 2025
    AWUS01 KWNH 021850
    FFGMPD
    NMZ000-AZZ000-030050-

    Mesoscale Precipitation Discussion 0573
    NWS Weather Prediction Center College Park MD
    250 PM EDT Wed Jul 02 2025

    Areas affected...Southeast Arizona and southwest New Mexico

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 021850Z - 030050Z

    SUMMARY...Slow moving thunderstorms developing this afternoon may
    contain rainfall rates up to 1"/hr and overlap with sensitive burn
    scars, urban regions, and complex terrain of southeast Arizona and
    southwest New Mexico. Isolated to scattered instances of flash
    flooding are possible.

    DISCUSSION...Recent radar and GOES19 IR satellite imagery depict
    numerous small-scale thunderstorms developing this afternoon
    across the Southwest in response to diurnal heating and within an
    anomalously moist atmosphere. PWs are estimated to be within
    1.2-1.5" per SPC's mesoanalysis, which falls between the 75th and
    90th climatological percentile per the 00z ECENS. Additionally,
    SBCAPE values are largely above 1000 J/kg across this region,
    which is necessary for coverage of thunderstorms to produce
    scattered instances of flash flooding and rainfall rates up to
    1"/hr.

    Mean layer flow in this region remains weak and out of the southas
    an upper low churns well to the west over coastal CA, which should
    lead to eventually thunderstorms becoming outflow dependent and
    tending to progress southward towards greater instability. As
    storms do this, cell mergers could briefly increase rainfall rates
    and potential flash flooding impacts. The 12z HREF shows the
    greatest potential for rainfall amounts exceeding FFG near and
    south of Tucson, AZ and along the AZ-Mexico border. It is here
    where a mid-level convergence axis may focus thunderstorm activity
    late this afternoon once storms reach their peak maturity and
    updrafts collapse. Given the sensitive burn scars across parts of
    southwest NM and the urban center of Tucson, scattered instances
    of flash flooding are possible should these slow-moving
    thunderstorms overlap.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8uag6s8NOjDaFJQ7N8mqZuASUnwK3rPI-9CwoXgQapVQzht_yEaSwGbOnZe3eLrMj4Or= Zn7njssz5U1RruYZR_tJpsE$ for graphic product...

    ATTN...WFO...ABQ...EPZ...FGZ...PSR...TWC...

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 34891065 34130980 33930895 34040789 33670742=20
    32630749 31720781 31190846 31070976 31171122=20
    31481221 32061283 32731275 32941177 33371144=20
    34221151 34731124=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jul 2 20:59:24 2025
    AWUS01 KWNH 022059
    FFGMPD
    NCZ000-SCZ000-030057-

    Mesoscale Precipitation Discussion 0574
    NWS Weather Prediction Center College Park MD
    458 PM EDT Wed Jul 02 2025

    Areas affected...Pee Dee region of South Carolina into far
    southern North Carolina

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 022057Z - 030057Z

    SUMMARY...A localized threat of flash flooding is expected to
    continue through this evening across parts of the Pee Dee region
    of South Carolina and far southern North Carolina, including the
    Cape Fear region. Training thunderstorms with rates up to 3"/hr
    and rainfall totals up to 4" are possible, potentially leading to
    instances of flash flooding.

    DISCUSSION...Latest radar imagery and surface observations depict
    repeating thunderstorms over eastern SC and far southern NC
    associated with an area of surface convergence ahead of an
    approaching cold front. This area of convergence is also being
    aided by a sea breeze denoted by GOES19 visible imager over SC,
    which should continue to be oriented parallel to 850mb flow over
    the next few hours and add to the training thunderstorm potential.
    Hourly rainfall rates have been estimated by MRMS as high 3" and
    when combined with the repeating nature of cells could lead to
    isolated flash flooding concerns. Even though the region is known
    for its sandy soils and high FFG (1-hr FFG of 2.5-4.0"), some
    localized totals of 4" could lead to isolated instances of flash
    flood. This is of particular concern in low-lying or urban
    locations.

    PW values per SPC's mesoanalysis remain above 2" and as high at
    2.4" in eastern NC, with MLCAPE values in the inflow region of
    central SC greater than 2500 J/kg. This environment supports the
    19z HRRR depiction of 3-hrly rainfall amounts possibly exceeding
    3" and nearing local FFG.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6QxlGEsfocsB6wSOV6ULBqf_KP7-FpPEBN2WpsU1TTsl3rRIDwXicQOklBBCuEMYkp6f= Xe53wF3TwSc4JXCWbTS3cck$ for graphic product...

    ATTN...WFO...CAE...ILM...

    ATTN...RFC...ALR...NWC...

    LAT...LON 34657918 34527801 34327755 34017751 33817789=20
    33777842 33687892 33417937 33527977 33907997=20
    34417977=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 3 00:51:53 2025
    AWUS01 KWNH 030050
    FFGMPD
    AZZ000-030550-

    Mesoscale Precipitation Discussion 0575
    NWS Weather Prediction Center College Park MD
    850 PM EDT Wed Jul 02 2025

    Areas affected...Parts of west-central into southern Arizona

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 030050Z - 030550Z

    SUMMARY...Clusters of thunderstorms containing rainfall rates up
    to 1.5"/hr are expected to continue early tonight and may produce
    isolated instances of flash flooding, particularly should storms
    converge near the Phoenix metropolitan area.

    DISCUSSION...GOES19 IR imagery shows cooling cloudtops associated
    with strengthening thunderstorms this evening across parts of
    central AZ. This ongoing while an upper low over central CA
    continues to funnel a plentiful amount of moisture northward into
    the Desert Southwest. SPC's mesoanalysis depicts the region with
    widespread PWATs above 1.5"and MLCAPE generally between 1000-2000
    J/kg. This environment is sufficient for 1.5"/hr rates that could
    overcome the dry complex desert terrain to lead to rapid runoff
    and flash flooding. Additionally, mean layer winds remain
    relatively light (per the 23z RAP) and around 5-10 kts out of the south-southwest. This leads to thunderstorms dominantly outflow
    dependent, as seem in current radar visuals, but also tied to an
    instability gradient extending across southwest AZ in a
    northwest-southeast orientation. This is where the strongest
    storms are current located in west-central and south-central AZ.

    Recent 23z HRRR, while not perfect, has a decent handle on ongoing
    convection and depicts the potential for isolated to scattered
    1-hrly totals of 1-2" to continue through at least 05z, while also
    encroaching upon the Phoenix metro. This area is also highlighted
    by RAP guidance as an area of increasing low-level convergence and
    MLCAPE by about 02z or so. Given the relatively quick outflow
    dominated storm motions, flash flooding coverage is expected to be
    isolated.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7pgdIXQgcu6i7l4VV4vPfUwixECDXtd_BjM6xJ_h_lquMi0L8J8rqanL4ruVnxvDPLC0= 7EFLw5r1t1T7Q1nW2nv6-l8$ for graphic product...

    ATTN...WFO...FGZ...PSR...TWC...VEF...

    ATTN...RFC...STR...NWC...

    LAT...LON 34511202 34221105 33411059 32201100 31601168=20
    31531227 31761266 32571286 33151328 33641411=20
    34061405 34351343=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 3 06:21:54 2025
    AWUS01 KWNH 030620
    FFGMPD
    AZZ000-NVZ000-CAZ000-031130-

    Mesoscale Precipitation Discussion 0576
    NWS Weather Prediction Center College Park MD
    218 AM EDT Thu Jul 03 2025

    Areas affected...northwestern AZ, southern NV into eastern CA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 030617Z - 031130Z

    SUMMARY...Isolated to widely scattered instances of flash flooding
    will be possible across portions of northwestern AZ, southern NV
    into eastern CA through 11Z. High rainfall rates of 0.5 to 1.0
    inches in 15 minutes will be possible with storm totals near 2
    inches.

    DISCUSSION...Area radar and GOES West infrared satellite imagery
    showed an increasing trend in convection over northwestern AZ,
    centered over central and southern Mohave County through 06Z. Low
    level confluence and low level moisture increasing from a
    combination of remnant outflow from the east and low level winds
    advecting in moisture from the south to southeast have allowed for
    an increase in MLCAPE over western/northwestern AZ with 06Z SPC
    mesoanalysis data showing 1000 to 2000+ J/kg. The SSE to NNW
    oriented instability max was co-located with anomalous moisture
    with SPC mesoanalysis estimated PW values of 1.5 inches along the
    CA/AZ border to 1.8 inches near PHX.

    Continued development of convection is expected over northwestern
    AZ, southern NV and eastern CA as low level moisture increases
    instability to the west and slightly north over the tri-state
    region over the next few hours. Aloft, the region resides to the
    east of an upper level trough over south-central CA with a 50-60
    kt jet max measured by GOES West DMV over eastern NV, placing
    locations over the tri-state region within the favored
    right-entrance region for ascent. Mean steering flow from the
    south to southwest at 10-20 kt should keep individual cells moving
    but upstream development could allow for brief training with high
    rainfall rates of 0.5 to 1.0 inches in 15 minutes, with similar
    rates observed earlier in the night to the west of the Phoenix
    metro. Any instances of flash flooding over southern Nevada,
    northwestern AZ and eastern CA should be isolated to widely
    scattered in coverage and storm total rainfall is expected to max
    out near 2 inches.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8DzBAAUfqvX8vr9XWeQSdqI7A_OPmPrluBuIjX-NFmCF4rniF8zFDXw2-uaui8axegoZ= -rzsWxNXSz_cerKGN97gswE$ for graphic product...

    ATTN...WFO...FGZ...PSR...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 37331563 37161428 36151322 34351332 33701460=20
    34101540 35471630 36721641=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 3 11:35:33 2025
    AWUS01 KWNH 031135
    FFGMPD
    TXZ000-031700-

    Mesoscale Precipitation Discussion 0577
    NWS Weather Prediction Center College Park MD
    734 AM EDT Thu Jul 03 2025

    Areas affected...Portions of West Texas from the Big Bend through
    the Edwards Plateaui

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 031134Z - 031700Z

    Summary...Showers and thunderstorms are expected to increase in
    coverage this morning and move slowly across parts of West Texas.
    Rainfall rates at times may reach 1-2"/hr, leading to 1-3" of
    rain. Flash flooding is possible.

    Discussion...The GOES-E IR imagery this morning shows an expanding
    area of cooling cloud tops over the Mexican state of Coahuila in
    response to a potent shortwave lifting northward over the
    Serranias del Burro. These cooling cloud tops are associated with
    intensifying convection approaching the Big Bend of Texas, and
    although reflectivity over the area is sparse at this time, the
    GOES-E GREMLIN radar emulation appears to match the IR imagery
    quite nicely showing higher reflectivity lifting towards the
    international border. At the same time, showers have begun to
    develop across the Edwards Plateau in response to a plume of
    increasing MUCAPE of 1000-2000 J/kg collocated with PWs that are
    analyzed by the SPC RAP to be 1.8 to 2.2 inches, or above the 99th
    percentile, thanks in part to a connection to tropical moisture
    associated with Tropical Storm Flossie over the Eastern Pacific
    noted via the ALPW products.

    Although the CAMs are struggling to resolve the ongoing activity,
    and admittedly are not exceptionally aggressive with rainfall the
    next few hours, the environment and evolution support heavy
    rainfall through the morning. Low-level S/SE flow measured at
    850mb on the VWPs at both DFX and MAF are around 20 kts, which is
    helping to transport the elevated PWs northward, and this flow may
    be locally accelerated downstream of the approaching shortwave.
    This will help to further improve the local thermodynamic
    environment, while at the same time leading to locally enhanced
    convergence into the mean wind which is generally around 10 kts.
    This evolution suggests that storms will increase in coverage
    (with additional ascent provided via the shortwave itself) and
    then move slowly/chaotically as Corfidi vectors veer strongly to
    the right of the mean wind and bulk shear remains minimal.
    Although the CAMs are not initializing very well, the accompanying
    HREF and REFS ensemble solutions do indicate increasing coverage
    of 10-30% probabilities for 1"/hr rates, leading to 1-3" of rain
    with isolated higher amounts.

    FFG across the region is highly variable due a wide variation in
    7-day rainfall, but in some places the 3-hr FFG is as low as 1.5
    inches, and 0-40cm soil moisture just north of the international
    border is above the 95th percentile. This indicates that some
    areas are locally vulnerable to rapid runoff, so as storms spread
    northward and expand/intensify, instances of flash flooding could
    result.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_8n5E9jOMxbByLpSD-CCFumC0eNUM-l0q9alrTzlNzLJ8mBnWdDAmmwgGqfVwW7DYxhG= tHWW4ZDttHByCH2LPad7jGs$ for graphic product...

    ATTN...WFO...EWX...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32390144 32240056 31970032 31319998 30569973=20
    29989966 29399983 28950014 28870061 29200124=20
    29440185 29150266 28960313 28870351 29080407=20
    29500445 29710463 30180465 30640416 31200337=20
    31350324 32100231=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 3 11:39:39 2025
    AWUS01 KWNH 031138
    FFGMPD
    TXZ000-031700-

    Mesoscale Precipitation Discussion 0577...Corrected
    NWS Weather Prediction Center College Park MD
    738 AM EDT Thu Jul 03 2025

    Corrected for areas affected

    Areas affected...Portions of West Texas from the Big Bend through
    the Edwards Plateau

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 031134Z - 031700Z

    Summary...Showers and thunderstorms are expected to increase in
    coverage this morning and move slowly across parts of West Texas.
    Rainfall rates at times may reach 1-2"/hr, leading to 1-3" of
    rain. Flash flooding is possible.

    Discussion...The GOES-E IR imagery this morning shows an expanding
    area of cooling cloud tops over the Mexican state of Coahuila in
    response to a potent shortwave lifting northward over the
    Serranias del Burro. These cooling cloud tops are associated with
    intensifying convection approaching the Big Bend of Texas, and
    although reflectivity over the area is sparse at this time, the
    GOES-E GREMLIN radar emulation appears to match the IR imagery
    quite nicely showing higher reflectivity lifting towards the
    international border. At the same time, showers have begun to
    develop across the Edwards Plateau in response to a plume of
    increasing MUCAPE of 1000-2000 J/kg collocated with PWs that are
    analyzed by the SPC RAP to be 1.8 to 2.2 inches, or above the 99th
    percentile, thanks in part to a connection to tropical moisture
    associated with Tropical Storm Flossie over the Eastern Pacific
    noted via the ALPW products.

    Although the CAMs are struggling to resolve the ongoing activity,
    and admittedly are not exceptionally aggressive with rainfall the
    next few hours, the environment and evolution support heavy
    rainfall through the morning. Low-level S/SE flow measured at
    850mb on the VWPs at both DFX and MAF are around 20 kts, which is
    helping to transport the elevated PWs northward, and this flow may
    be locally accelerated downstream of the approaching shortwave.
    This will help to further improve the local thermodynamic
    environment, while at the same time leading to locally enhanced
    convergence into the mean wind which is generally around 10 kts.
    This evolution suggests that storms will increase in coverage
    (with additional ascent provided via the shortwave itself) and
    then move slowly/chaotically as Corfidi vectors veer strongly to
    the right of the mean wind and bulk shear remains minimal.
    Although the CAMs are not initializing very well, the accompanying
    HREF and REFS ensemble solutions do indicate increasing coverage
    of 10-30% probabilities for 1"/hr rates, leading to 1-3" of rain
    with isolated higher amounts.

    FFG across the region is highly variable due a wide variation in
    7-day rainfall, but in some places the 3-hr FFG is as low as 1.5
    inches, and 0-40cm soil moisture just north of the international
    border is above the 95th percentile. This indicates that some
    areas are locally vulnerable to rapid runoff, so as storms spread
    northward and expand/intensify, instances of flash flooding could
    result.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-_IYstZlWNU4c9cGWKyJb99spL_po8VVePxwqB5ixSNfBY6O936l-rqYjjr3WadEgDpu= sD4TYrmi5jEHtw_HnQopM34$ for graphic product...

    ATTN...WFO...EWX...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32390144 32240056 31970032 31319998 30569973=20
    29989966 29399983 28950014 28870061 29200124=20
    29440185 29150266 28960313 28870351 29080407=20
    29500445 29710463 30180465 30640416 31200337=20
    31350324 32100231=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 3 12:27:50 2025
    AWUS01 KWNH 031226
    FFGMPD
    ARZ000-TXZ000-OKZ000-031730-

    Mesoscale Precipitation Discussion 0578
    NWS Weather Prediction Center College Park MD
    826 AM EDT Thu Jul 03 2025

    Areas affected...Central and Eastern Oklahoma through Southern
    Arkansas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 031225Z - 031730Z

    Summary...An axis of showers and thunderstorms will continue to
    train across eastern Oklahoma this morning. Rain rates of 1-2"/hr
    are expected within this convection, leading to 2-3" of rain with
    locally higher amounts. Flash flooding is possible.

    Discussion...The regional radar mosaic this morning shows an axis
    of expanding convection oriented NW to SE across eastern Oklahoma.
    This convection is blossoming along an elevated 700mb front north
    of a surface boundary draped over eastern Texas, with persistent
    isentropic ascent and moisture confluence occurring into the
    boundary on 850-700mb winds of 15-25 kts measured via local VWPs.
    Moisture is impressive across the area with PWs around 2.1 inches
    (above the 90th percentile) and 700-500mb RH above 90%. With 700mb
    winds gradually veering and converging into this front, moisture
    confluence is maximized along this boundary, which in combination
    with the accompanying lift is driving the ongoing thunderstorm
    activity.

    The CAMs are struggling to initialize both the breadth and
    intensify of the morning thunderstorms, leading to a lower than
    typical confidence for the evolution the next few hours. However,
    the ARW and ARW2, as well as the recent RRFS, all at least hint at
    the activity and are used to help forecast the flash flood risk.
    The setup will remain favorable for continued convection as
    moisture confluence into the boundary combined with the
    convergence will focus development along this axis. Mean 0-6km
    winds will remain light at just 5-10 kts, and with Corfidi vectors
    aligned parallel to the boundary and anti-parallel to the mean
    wind, an enhanced risk for backbuilding and training of cells will
    continue at least until the 850-700mb inflow weakens in the next
    few hours. Although the axis of heavy rainfall is expected to be
    narrow and focused along this elevated boundary, near-record PWs
    and a slow rise in MUCAPE will support rain rates above 1"/hr,
    which through training will create stripes of 2-3" of rain with
    locally higher amounts.

    FFG across the region is generally elevated at 2.5-4"/3hrs due to
    a lack of recent rainfall across most of the discussion area, but
    0-10cm soil moisture from NASA SPoRT has not fully dried and is
    still above the 90th percentile in many areas. This suggests that
    infiltration capacity of the soil is somewhat limited. So, where
    training can occur (to saturate the soils and then overwhelm
    them), instances of flash flooding are possible, but will be most
    likely across urban areas or where the most pronounced training
    does occur.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8UruzX9FDABfU30rss79ilt4DJCPLL0VlXOgEr08rjgz4qYB1PfxM6m4x8RArj7Tdtan= eyqQW-P2t1NAfFhtDavuwvg$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 36129736 36029613 35629516 35019440 34119356=20
    33669337 33099367 33019447 33239507 33269527=20
    33859660 34339764 34879814 35689808=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 3 16:31:35 2025
    AWUS01 KWNH 031631
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-032230-

    Mesoscale Precipitation Discussion 0579
    NWS Weather Prediction Center College Park MD
    1231 PM EDT Thu Jul 03 2025

    Areas affected...Vicinity of the Red River Valley of the South

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 031630Z - 032230Z

    Summary...Showers and thunderstorms will develop along a decaying
    frontal boundary and train through the afternoon. Rainfall rates
    may pulse up above 2"/hr at times, leading to 1-2" of rainfall
    with locally higher amounts above 3". Flash flooding is possible.

    Discussion...The regional radar mosaic late this morning shows a
    rapid uptick in convection developing along a decaying stationary
    front aligned near the Red River Valley of the South. Recent radar
    estimated rain rates from KTLX and KFWS have been as high as
    1.5"/hr within fresh convection, with storm motions generally of
    to the north at 10 kts.

    The environment is becoming increasingly favorable for heavy rain
    containing convection, with a ribbon of MLCAPE exceeding 1000 J/kg
    overlapping PWs as high as 2 inches, which is well above the 90th
    percentile for the date, and a daily max at KOUN according to the
    SPC sounding climatology. Modest low-level S/SW winds measured via
    VWPs at 10-20 kts lifting into the decaying front are resulting in
    increasing isentropic ascent, which is acting together with a weak
    impulse moving into North Texas and broadly diffluent 300mb flow
    to provide deep layer ascent. This lift occurring into these
    favorable thermodynamics will continue to support increasing
    coverage and intensity of thunderstorms through the aftn.

    The high-res CAMs are again struggling to handle the ongoing
    activity, although the ensembles, both HREF and REFS, appear to be
    usable. These ensembles both suggest that coverage of 1"/hr (and
    2"/hr) neighborhood rain rate probabilities will rapidly rise
    during the next few hours in a NW to SE oriented axis in the
    vicinity of the decaying front. With ascent remaining in place and thermodynamics becoming increasingly robust later today (SBCAPE
    approaching 2000 J/kg), thunderstorms should remain supported and
    intensify. This is suggested by HREF and REFS probabilities for
    2"/hr rates reaching 25-35%, coincident with HRRR 15-min rainfall
    exceeding 0.75" at times (brief 3"/hr rates). Although the models
    disagree on where the heaviest rain will occur, the maximum
    convergence just north of the boundary should be favored, which is
    also where Corfidi vectors are aligned most obliquely right of the
    mean flow to suggest enhanced training from NW to SE as the line
    forms and advects slowly northward.

    0-10cm RSM from NASA SPoRT is generally around 50% south of the
    Red River, but as much as 80% to the north, suggesting that OK is
    more vulnerable than TX today. This is also where the, albeit
    modest, FFG exceedance probabilities exist. While that area may be
    most susceptible today, any place that receives training of these
    more intense rain rates could experience instances of flash
    flooding through the aftn.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5GFA3EAGPZhTpFR1EoH9QTxDjMZdOKy_UjflhKJgW57Q7WAUshYrX3xmnGCtn67JLU2a= VQdm_O_Js4MCmcNoAIIVpPw$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35959870 35539757 34169560 33269406 33179395=20
    32699348 32269335 31989358 31839419 32089574=20
    32769774 33449901 34419950 35509952=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 3 17:22:38 2025
    AWUS01 KWNH 031722
    FFGMPD
    TXZ000-NMZ000-032315-

    Mesoscale Precipitation Discussion 0580
    NWS Weather Prediction Center College Park MD
    121 PM EDT Thu Jul 03 2025

    Areas affected...West Texas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 031719Z - 032315Z

    Summary...Showers and thunderstorms will continue to expand
    downstream of twin shortwaves moving northward across West Texas.
    Rainfall rates in excess of 2"/hr are possible at times, leading
    to rainfall of 2-3" with locally as much as 5". Flash flooding is
    possible.

    Discussion...The GOES-E WV imagery this afternoon indicates dual
    shortwaves moving northward across West Texas. The first is
    associated with an MCV which is remnant from an impressive MCS
    that lifted out of Coahuila, Mexico earlier this morning, while a
    secondary shortwave is moving over the southern Permian Basin.
    Both of these impulses are contributing impressive ascent into
    robust thermodynamics to support heavy rainfall rates. These
    thermodynamics are characterized by PWs that are above the 95th
    percentile within the 700-500mb and 500-300mb layer according to
    CIRA, overlapped with MLCAPE that is slowly climbing towards 1000
    J/kg according to the SPC RAP analysis. Rainfall rates within
    ongoing convection have been estimated above 1.5"/hr according to
    KMAF WSR-88D, and morning rainfall today has already been measured
    at 2-4" in some areas via MRMS and local mesonet observations.

    Flash flooding is currently ongoing across the region, and the
    slow poleward advance of these shortwaves will maintain or
    increase flash flooding potential through the afternoon. These
    shortwaves are going to continue to move northward as the region
    remains pinched between a trough approaching from the west and a
    ridge positioned to the east. Not only will this push these
    shortwaves northward to continue lift, but will also draw more
    impressive thermodynamics northward to support heavy rainfall.
    Although CAMs are struggling to resolve current activity, both the
    REFS and HREF neighborhood probabilities for 2"/hr rates rise to
    20-40%, while the HRRR 15-min rainfall accumulations reach as much
    as 0.75", indicating at least brief 3"/hr rates. With mean 0-6km
    winds remaining light from the S/SW at 5-10 kts, and Corfidi
    vectors pointing back into the better moisture (anti-parallel to
    the mean wind), this will support short term training of these
    rates leading to rainfall of 2-3" with locally higher amounts
    approaching 5" possible.

    In addition to the rain which has already occurred this morning,
    0-10cm RSM from NASA SPoRT is above the 75th percentile across
    much of the area, suggesting the soils are vulnerable to rapid
    runoff. This is additionally reflected by 3-hr FFG that is as low
    as 1.5"/3hrs. This indicates that any of these more intense rain
    rates, especially during periods of training, could overwhelm the
    soils leading to instances of flash flooding.

    Weiss/Shieh

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9P4sEI54wAfK3VVdXuBp82UxQYwuVt-dA9PTn7hIBz0x_igfg8AGrq5SrmUE264E_13v= id1BRKd9X0JqEPx3Hy5EN8Q$ for graphic product...

    ATTN...WFO...ABQ...EWX...LUB...MAF...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 34630194 34490144 34310114 33930073 33680050=20
    33100026 32540024 32020039 31480056 31310063=20
    30890081 30350084 30020105 29630161 29710236=20
    29850336 29680384 30080420 30780433 31270424=20
    31440391 31440347 31680308 31860292 31970292=20
    31980291 32630323 33460317 34370301 34500256=20
    34580250=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 3 19:01:08 2025
    AWUS01 KWNH 031901
    FFGMPD
    TXZ000-NMZ000-040100-

    Mesoscale Precipitation Discussion 0581
    NWS Weather Prediction Center College Park MD
    259 PM EDT Thu Jul 03 2025

    Areas affected...New Mexico & West Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 031900Z - 040100Z

    SUMMARY...Broad upper-level troughing and an unstable air-mass
    coupled with anomalous moisture and saturated soils could result
    in additional areas of flash flooding today, especially near burn
    scars.

    DISCUSSION...An upper-level trough approaching from Arizona will
    place a more efficient diffluent flow over much of New Mexico and
    as far south as West Texas. GOES-19 visible satellite imagery and
    GLM show a growing field of thunderstorms along the Southern
    Rockies that continue to strengthen. Visible satellite shows this
    area has generally been free of thick low-mid level clouds,
    allowing for surface-based heating to occur relatively unimpeded.
    RAP mesoanalysis depicts as much as 1,000 J/kg of MLCAPE in place
    over eastern NM with 17Z RAP guidance showing anywhere from
    1,000-2,000 J/kg later this afternoon. The region continues to
    sport highly anomalous moisture aloft with PWATs over the Southern
    Rockies and Rio Grande Valley generally between 1.0-1.25", while
    the High Plains of eastern New Mexico are more commonly between
    1.5-1.75". Regardless of the exact numbers, all these PWATs are
    comfortably above the 90th climatological percentile per ECMWF ENS
    guidance and even topping the 99th climatological percentile in
    southeast New Mexico.

    The approaching upper-level trough, copious amounts of moisture,
    and modest instability should allow for the thunderstorm threat to
    linger into the early evening hours. As the upper trough
    approaches, SWrly 850-300mb mean winds should accelerate to >15
    kts, which while this does help to keep storms moving along, this
    can also further act as a trigger for additional storms or
    back-building storms along windward-facing slopes. Storms along
    the Sangre De Cristo and Sacramentos could also move northeast
    into eastern New Mexico where any outflows emanating off the
    terrain or from thunderstorms over western Texas could aid in the
    development of thunderstorms producing >1.5"/hr rainfall rates.
    NASA SPoRT-LIS 0-40cm soil moisture percentiles still suggest
    soils of that depth remains quite saturated, or to the tune of
    80-95%. Given the favorable atmospheric parameters and sensitive
    soils, there is the potential for widely scattered thunderstorms
    to pose a flash flood threat. Burn scars and rugged terrain, as
    well as low-lying areas that drain poorly are most at-risk through
    this evening.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4OOKcQ77BlZYaUHPHvvztLf78W-VuVtVucnNFgSL8wQ7Tlhaog1rloaRxVcWrJA6Rvy8= 6Ul2j77iCK4ZKDOrpeLnaDk$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 36850564 36730511 36410479 36070451 35400405=20
    34560351 33720326 32840317 32170336 31250425=20
    30980511 30970555 31270612 31680679 31800713=20
    31860746 31980787 32300823 32640823 33060812=20
    33650803 34140818 34800815 35140796 35540754=20
    35700743 36030666 36280640 36620594=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 3 23:03:45 2025
    AWUS01 KWNH 032302
    FFGMPD
    TXZ000-040500-

    Mesoscale Precipitation Discussion 0582
    NWS Weather Prediction Center College Park MD
    702 PM EDT Thu Jul 03 2025

    Areas affected...Texas Hill Country

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 032300Z - 040500Z

    SUMMARY...Concerning trends for back-building and training
    thunderstorms over the Texas Hill Country this evening that could
    produce >3"/hr max rainfall rates.

    DISCUSSION...The remnant mid-level circulation associated with
    Barry (also classified as an MCV on the graphic) is over western
    Texas and slowly approaching the Texas Hill Country this evening.
    Barry's remnant circulation has a dearth of atmospheric moisture
    at its disposal with PWs ranging anywhere from 2.2-2.5". ECMWF ENS
    percentiles show these PWs above the 99th climatological
    percentile, as are the mean specific humidity (g/kg) values at
    both the 850mb and 500mb height levels. The atmosphere is also
    quite unstable with MUCAPE generally between 2,000-3,000 J/kg. As
    night falls, the low-level jet (LLJ) will gradually accelerate out
    of South Texas and intersect the Hill Country in a manner that
    supports topographically-forced ascent. This low-level jet is also
    part of a fairly strong southerly IVT for early July as the ECMWF
    ENS percentiles depict >500 kg/m/s values (above the 97.5
    climatological percentile) over the Hill Country between 00-06Z.
    The impressive moisture advection is making for some remarkably
    saturated RAP soundings where low-mid level RH values are >90% and
    warm cloud layers are 15,000ft deep in many cases.

    The concern with the MCV and remnant 500-700mb trough is that it
    is paired with a persistent LLJ that looks to be steadfast over
    the region well into the overnight hours. While there is not a ton
    of vertical wind shear, noticeable veering in the sfc-3km layer
    ensues as the LLJ strengthens this evening (SErly sfc winds, SWrly
    3km winds). This could provide cells with the ability to be
    somewhat self-sustaining and organized this evening. The other
    concern is for outflows associated with a growing cold pool from
    northerly convection to propagate south and be oriented in a way
    where the southerly LLJ intersects the outflows in a perpendicular
    fashion. The atmospheric parameters are supportive of not just the
    potential for >3"/hr maximum rainfall rates, but for back-building
    and training thunderstorms over the Hill Country.

    The I-35 corridor on west is most at-risk for flash flooding
    tonight. 1-hr FFGs are generally between 1.5-2.0" in portions of
    the Hill Country, which given the prolific rainfall potential
    these storms may contain, would have little problem causing flash
    flooding. For areas where back-building and training storms do
    occur, locally considerable flash flooding this evening is
    possible.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4HTUq9oReOifkEErBvNsVGeCd3qm4klwIk9b93F5tGu1pPpgmBj3Iz97euj4PO3RdvLj= iVUhkXutStPUlgcLqTYvcEM$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 33049861 32029772 30809750 29669772 29079855=20
    29169957 29860011 30700023 31420008 32959969=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 3 23:11:12 2025
    AWUS01 KWNH 032311
    FFGMPD
    TXZ000-040500-

    Mesoscale Precipitation Discussion 0582
    NWS Weather Prediction Center College Park MD
    710 PM EDT Thu Jul 03 2025

    Areas affected...Texas Hill Country

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 032300Z - 040500Z

    SUMMARY...Concerning trends for back-building and training
    thunderstorms over the Texas Hill Country this evening that could
    produce >3"/hr max rainfall rates.

    DISCUSSION...The remnant mid-level circulation associated with
    Barry (also classified as an MCV on the graphic) is over western
    Texas and slowly approaching the Texas Hill Country this evening.
    Barry's remnant circulation has an abundance of atmospheric
    moisture at its disposal with PWs ranging anywhere from 2.2-2.5".
    ECMWF ENS percentiles show these PWs above the 99th climatological
    percentile, as are the mean specific humidity (g/kg) values at
    both the 850mb and 500mb height levels. The atmosphere is also
    quite unstable with MUCAPE generally between 2,000-3,000 J/kg. As
    night falls, the low-level jet (LLJ) will gradually accelerate out
    of South Texas and intersect the Hill Country in a manner that
    supports topographically-forced ascent. This low-level jet is also
    part of a fairly strong southerly IVT for early July as the ECMWF
    ENS percentiles depict >500 kg/m/s values (above the 97.5
    climatological percentile) over the Hill Country between 00-06Z.
    The impressive moisture advection is making for some remarkably
    saturated RAP soundings where low-mid level RH values are >90% and
    warm cloud layers are 15,000ft deep in many cases.

    The concern with the MCV and remnant 500-700mb trough is that it
    is paired with a persistent LLJ that looks to be steadfast over
    the region well into the overnight hours. While there is not a ton
    of vertical wind shear, noticeable veering in the sfc-3km layer
    ensues as the LLJ strengthens this evening (SErly sfc winds, SWrly
    3km winds). This could provide cells with the ability to be
    somewhat self-sustaining and organized this evening. The other
    concern is for outflows associated with a growing cold pool from
    northerly convection to propagate south and be oriented in a way
    where the southerly LLJ intersects the outflows in a perpendicular
    fashion. The atmospheric parameters are supportive of not just the
    potential for >3"/hr maximum rainfall rates, but for back-building
    and training thunderstorms over the Hill Country.

    The I-35 corridor on west is most at-risk for flash flooding
    tonight. 1-hr FFGs are generally between 1.5-2.0" in portions of
    the Hill Country, which given the prolific rainfall potential
    these storms may contain, would have little problem causing flash
    flooding. For areas where back-building and training storms do
    occur, locally considerable flash flooding this evening is
    possible.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_yHIZeDGIDTRNYMDiGDn4Dfx7JVS2EEPIVonaO5RBBfPlBWbRc41SBIl3K9cGxGu6DMy= Czqt1QNOaq1-y-rSobAu9s0$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 33049861 32029772 30809750 29669772 29079855=20
    29169957 29860011 30700023 31420008 32959969=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 4 04:05:47 2025
    AWUS01 KWNH 040405
    FFGMPD
    WIZ000-MNZ000-040900-

    Mesoscale Precipitation Discussion 0583
    NWS Weather Prediction Center College Park MD
    1205 AM EDT Fri Jul 04 2025

    Areas affected...western to southern WI

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 040404Z - 040900Z

    SUMMARY...Training of thunderstorms over western to southern WI
    will likely produce a few areas of flash flooding through 09Z with
    hourly rainfall of 1 to 2 inches, though localized hourly rates
    near 3 inches in an hour will be possible. Some 3 to 5 inch totals
    may result.

    DISCUSSION...Radar imagery from 0345Z showed a NW to SE axis of
    thunderstorms extending along/north of a slow moving warm front
    which extended from just north of MSP to just south of MKE at 03Z.
    The environment over the region contained 2000 to 3000 J/kg MLCAPE
    and PWs of 1.5 to 1.8 inches, sampled well by the 00Z MPX
    sounding. Southwesterly 850 mb winds of 20-25 kt were observed via
    VAD wind plots from KMPX and KARX, overrunning the frontal
    boundary with mean steering flow oriented parallel to the front, a
    favorable setup for training. In addition, a remnant MCV near the
    central MN/WI border appears to be contributing to lift across the
    region.

    Warm advection driven thunderstorms are likely to continue across
    WI over the next few hours with southwesterly winds at 850 mb
    remaining a similar magnitude overnight, but with some slow
    advancement of the front toward the northeast expected. Congealing
    of thunderstorms may promote some southward motions toward
    southern WI, but upstream redevelopment will remain possible with
    continued potential for training from NW to SE and hourly rainfall
    likely to be in the 1 to 2 inch range, although one cannot rule
    out locally higher rates of 2 to 3 inches in an hour. Flash flood
    guidance of largely 2 to 3 inches in 3 hours across the region
    should be exceeded in a few locations, resulting in a likely flash
    flood threat over the next 3-5 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9arsfwhKDLsedHSW03BQldKlP-9emyfcpOJrDAXgM2y7JlKP2fA3bZCTxixiW59y5JEc= WITwNCa8GMOgnK-NJUDQATY$ for graphic product...

    ATTN...WFO...ARX...DLH...GRB...MKX...MPX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 46279187 45479087 44979031 44188916 43388843=20
    42658862 42578930 43149036 43979162 44649253=20
    45269293 46139273=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 4 05:27:52 2025
    AWUS01 KWNH 040527
    FFGMPD
    TXZ000-041030-

    Mesoscale Precipitation Discussion 0584
    NWS Weather Prediction Center College Park MD
    126 AM EDT Fri Jul 04 2025

    Areas affected...central TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 040525Z - 041030Z

    Summary...Areas of flash flooding will be likely across central TX
    overnight with very heavy rainfall expected. Hourly rainfall in
    excess of 2 to 3 inches seems reasonable given the environment and
    localized 6-hr totals over 6 inches will be possible. Some flash
    flood impacts could be significant, especially considering
    sensitive terrain over portions of the region.

    Discussion...05Z regional radar mosaic over central TX showed an
    ongoing area of thunderstorms with a few areas of very efficient
    rainfall resulting from embedded training. As of 05Z, some of the
    heaviest hourly rainfall (2 to 3 inches per MRMS) was occurring
    over Bandera and San Saba counties. Another area of training was
    found just southeast of San Angelo along US 87, tied to a remnant
    MCV circulation (related to the remains of Barry's mid-level
    circulation), located between SJT and JCT and embedded within a
    broader mid-level trough that extended NNW into eastern CO. The
    region was located within an extremely moist environment
    containing 2.0 to 2.5 inches of PW with contributions from the
    Gulf of America and tropical east Pacific clearly evident on
    layered PW imagery.

    Low level southerly winds sampled by area VAD wind plots at 850 mb
    were 20-30 kt and these winds are expected to maintain through the
    overnight with some subtle strengthening possible over the next
    couple of hours. The upper trough and remnant mid-level
    circulation over central TX is expected to slowly advance east
    while low level convergence continues to focus from the TX Hill
    Country, northward to the I-20 corridor. Terrain enhancement into
    the Hill Country and low level convergence at the leading edge of
    the stronger low level flow will set up favorably with the mean
    steering flow from the southwest to support areas of training. The
    tropical airmass will be capable of 2 to 3+ inches of rain in an
    hour and localized totals over 6 inches in a 6 hour period may
    also occur. These areas of heavy rainfall are expected to result
    in a few areas of flash flooding through the overnight, some of
    which may become locally significant.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9P_qb2_ryj1wccwMzPDr1Zq2h4Gb7zLZSphL8VSaWFJb8OVMPXMv-hHD3rBxSNm05SmV= JmrFmljjCq3Nn-HrP9p6hcU$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 33139936 32779820 31759771 30119833 29209929=20
    29330030 29950076 31250063 32340033=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 4 10:28:19 2025
    AWUS01 KWNH 041028
    FFGMPD
    TXZ000-041445-

    Mesoscale Precipitation Discussion 0585
    NWS Weather Prediction Center College Park MD
    627 AM EDT Fri Jul 04 2025

    Areas affected...central TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 041025Z - 041445Z

    Summary...Areas of high Impact flash flooding will continue for at
    least another 3-5 hour across portions of central TX. Slow to
    nearly stationary net movement of heavy rain cores will maintain a
    threat for hourly rainfall in excess of 3 inches in a couple of
    locations. Considerable to catastrophic flash flood impacts can
    continue to be expected.

    Discussion...10Z radar imagery over central TX showed a cluster of
    slow moving thunderstorms that extended from near San Angelo into
    southern portions of the Hill Country. Embedded cells within the
    cluster has exhibited near stationary movement with gauge reports
    of 13+ inches about 7 miles northwest of San Angelo and 11+ inches
    in Kerr County since 04Z. A long-lived embedded circulation
    remained just east of San Angelo but there has been some
    disruption over the past 30-60 minutes to the heavy rain cores
    near San Angelo and over Kerr County. The environment remained
    highly conducive to locally extreme rainfall with high freezing
    levels of 15-16 kft AGL, PWs of 2.0 to 2.5 inches and up to 1000
    J/kg MLCAPE via 10Z SPC mesoanalysis and RAP analysis data.

    Low level convergence in the vicinity of the slow moving
    circulation near San Angelo is expected to remain a focus for
    localized heavy rainfall rates over the next few hours with the
    axis of heaviest rainfall shifting a bit south and east in the
    short term. Farther south, newer/smaller cells feeding into the
    main complex over the Edwards Plateau are indicative of the
    continued convergence across the region with slow net movement of
    rainfall cores and MRMS-derived rainfall of 2 to 3+ inches in an
    hour for a few locations in central TX. The threat for continued
    higher end flash flooding is expected to remain relatively focused
    across central TX over the next 3-5 hours at which point movement
    of the mesoscale circulation and forecast weakening of the low
    level winds into the Edwards Plateau may begin to decrease or at
    least shift the heavy rain threat a bit toward the north and east.
    However, through the remainder of the morning, with area creeks
    and rivers rapidly rising, a very dangerous situation remains for
    anybody within the highlighted MPD area. Considerable to locally
    catastrophic impacts from flash flooding are likely to continue.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6mBkWL-35HTmwYhgglecFDGQvkRc86fThjGgHRAGza7qVHrIlCknqaFAckCEhFflLZp5= MyG_GzE0605UI22DQQC0eks$ for graphic product...

    ATTN...WFO...EWX...FWD...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32389983 32189901 31859845 31409817 30429813=20
    29799848 29239902 29159990 29490039 30230076=20
    31430114 31950102 32300071=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 4 14:34:06 2025
    AWUS01 KWNH 041433
    FFGMPD
    TXZ000-042000-

    Mesoscale Precipitation Discussion 0586
    NWS Weather Prediction Center College Park MD
    1033 AM EDT Fri Jul 04 2025

    Areas affected...Hill Country and Edwards Plateau of south-central
    Texas...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 041430Z - 042000Z

    SUMMARY...Slow moving MCC continues to compound significant flash
    flooding with some areal expansion expected over next few hours.=20
    WPC upgrade to Moderate Risk.

    DISCUSSION...GOES-E WV suite depicts the fairly symmetric MCC
    remains ideally within anticyclonic wedge; while not very strong
    outflow is sufficient with impressive transverse banding features
    along much of the northern hemisphere of the circulation and with
    the persistent strong updrafts/latent heat release the MCV
    continues to remain strong near the McCulloch/Saba/Mason county
    intersection. Regional RADAR mosaic denotes this with impressive
    arched convective band along the effective cold front within the
    western quadrant of the MCC from Mason to Sutton county and VWP
    shows solid warm advective profile off the Rio Grande confluent
    across central South Texas further expanding effective warm
    frontal banding like features along and downstream to the SE of
    the MCV. Upstream well of continued very moist and unstable air
    with TPW values over 2.25" and MLCAPE gradient of 1000-2000 J/kg
    along the southwest to southern side of the circulation. This
    will support cells capable of 2-3"/hr

    As the MCV wobbles and confluence increases into the WAA, the band
    will once again shift across the Guadalupe River Valley likely to
    induce another wave of flash flooding conditions. While Hi-Res
    CAMs continue to suggest a weakening phase over the next few
    hours, the upstream inflow and potential for upstream development
    along the WAA regime may result in relatively with south-southwest
    propagation equal/stronger than 10-15kt inflow resulting in
    stationary cells with spots of additional 4-6" possible. As such
    significant to catastrophic flash flooding is likely to continue
    with potential to expand along the southern periphery of the MCC.=20


    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-c199t51wM3K-1cTLCvw_4TQOsZo7kwZCvK34MKu9-9jlFG6cVXNwSV5NOlXaYxUawsz= 3r0rGDQAwPKKcjAE8bjYTx8$ for graphic product...

    ATTN...WFO...EWX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31449905 30979848 30689768 29959762 29429807=20
    29189869 29099927 29310003 29940063 30470084=20
    30860075 31040040 31299992 31429983=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 4 19:04:12 2025
    AWUS01 KWNH 041902
    FFGMPD
    TXZ000-050000-

    Mesoscale Precipitation Discussion 0587
    NWS Weather Prediction Center College Park MD
    302 PM EDT Fri Jul 04 2025

    Areas affected...Texas Triangle...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041900Z - 050000Z

    SUMMARY...Unstable air downstream of persistent MCC will have=20
    solid moisture flux allowing for intense localized 2-3"/hr rates
    and possible flash flooding.

    DISCUSSION...RADAR mosaic shows mature MCV has stalled in the
    vicinity of San Saba/Mills county but is also starting to stretch
    southwest to northeast. Dense central dense mid to upper-level
    cloud cover has resulted in a strong differential heating boundary
    along the NE to eastern side of the canopy with MLCAPEs building
    over 2000 J/kg (with greater values within the confluent boundary
    along the distant eastern side toward Houston/Galveston Bay.=20
    However, VWP shows solid 20-30kt weakly veered southerly flow
    across the Heart of Texas within the core of enhanced deep layer
    moisture with total PWats of 2.25" nearing 2.5". Currently, the
    DPVA from the inner core of the MCV shifting northeast though the
    mid-level elongation has started to break out stronger
    thunderstorms along that differential heating boundary.

    The flux convergence will support highly efficient rainfall
    production with 2-3"/hr rates. However, deep layer flow and
    southeastward inflow will support eastward propagation as cells
    move in the north to northeast steering flow. This steering flow
    is semi-confluent to suggest some merging/training but the
    propagation vectors of 15kts to the southeast, may reduce
    prolonged duration. Still spots of 2-4" are probable and given
    FFG values are higher/less compromised to the east; incidents of
    flash flooding are considered possible.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!84PmK_LEHNWLIjs_ofhsY-zXi7huL0gRdGGdYG-UBiu_ma1N5u4EpdgbtHyOZanSa7KU= A4r0HGTg1YcsgEQJJ4D8NsY$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32479764 32429670 32169626 31699591 31079582=20
    30519613 30059697 30029792 30509806 31379830=20
    31949849=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 4 19:11:20 2025
    AWUS01 KWNH 041911
    FFGMPD
    MNZ000-SDZ000-NDZ000-050110-

    Mesoscale Precipitation Discussion 0588
    NWS Weather Prediction Center College Park MD
    310 PM EDT Fri Jul 04 2025

    Areas affected...Eastern Dakotas & Northern Minnesota

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041910Z - 050110Z

    SUMMARY...Blossoming clusters of thunderstorms to produce >2"/hr
    rainfall rates poses a threat for potential flash flooding this
    afternoon.

    DISCUSSION...A potent 500mb trough approaching from the northern
    High Plains is working in tandem with the diffluent right-entrance
    region of a strengthening 250mb jet streak over the Red River of
    the North to provide a favorable synoptic-scale environment for
    upscale-growth of thunderstorms. A warm front has been lifting
    north through northern Minnesota today and has already triggered
    several intense thunderstorms close to the International Border.
    Meanwhile, thunderstorms have formed along a surface trough in the
    heart of the Dakotas that are tracking northeastward into a more
    unstable environment. Dew points are in the low 70s within the
    highlighted region with MLCAPE forecast by the RAP to surpass
    3,000 J/kg and PWATs above 2.0". The PWATs are likely to be above
    the 99.5 climatological percentile per ECMWF ENS guidance, and
    warm cloud layers are exceptionally deep for the region. The ECMWF
    ENS guidance also shows a >750 kg/m/s IVT over eastern South
    Dakota that is aimed at northern Minnesota this evening, favoring
    that area for the strongest moisture advection. By 00Z this
    evening, RAP soundings for International Falls, MN show a melting
    level near 15,000ft, which is nearly 6,000ft deeper than the 90th
    percentile (~9,000ft) in the SPC sounding climatology. Lastly,
    these storms will have modest vertical wind shear to keep these
    storms organized, with higher storm relative helicity values
    closer to the warm front over northern Minnesota.

    These factors all support the potential for organized clusters of
    storms that can produce exceptional rainfall rates that give
    credence to a flash flood threat through this evening. As the
    storms from the Dakotas approach into the more unstable and
    sheared environment, storms over the Dakotas could merge with
    developing storms along the surface trough. This should eventually
    spawn a larger cold pool and become a more organized MCS this
    evening. Rainfall totals ranging between 2-4" are anticipated from
    eastern North Dakota and northern South Dakota on east to northern
    Minnesota this afternoon. Areas long the Red River on east into
    northern Minnesota have the better odds for localized amounts
    topping 5" where they are more ideally placed closer to the warm
    front and where the more persistent area of 850mb theta-e
    advection is present. 1-hr FFGs are lowest along the Red River and
    along the Minnesota's International Border with FFGs as low as
    1.5" in some cases, although most areas along the Red River are as
    low as 1.5" for 3-hr FFGs as well. Given these factors, flash
    flooding is possible in impacted areas. Given it is the Fourth of
    July, those enjoying outdoor festivities should be sure to have a
    means of receiving any warnings issued this afternoon and evening.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_BIY8FshRA_V2vuu0erG8o4Dx_AbKPzT8M1CFxgflo9ogbmIoCMaq7CkfCdxLu-zxBJP= T2XosW9OgJeQpInVfCsFMpw$ for graphic product...

    ATTN...WFO...ABR...BIS...DLH...FGF...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 49099548 48989467 48739403 48759326 48469242=20
    47949270 47289413 46499574 45729688 45289728=20
    44869797 44599893 44519977 44650032 44910055=20
    45420052 46000022 47149905 47789833 48209769=20
    48719696 48949645=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 4 20:12:24 2025
    AWUS01 KWNH 042012
    FFGMPD
    TXZ000-050030-

    Mesoscale Precipitation Discussion 0589
    NWS Weather Prediction Center College Park MD
    411 PM EDT Fri Jul 04 2025

    Areas affected...Texas Hill Country

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 042010Z - 050030Z

    SUMMARY...Flash flooding looks to continue into the afternoon in
    parts of the Hill Country as the MCV slowly moves north and east.
    An additional 1-4" of rainfall is possible over the next few hours.

    DISCUSSION...The MCV responsible for the destructive and fatal
    flash flooding event in the Hill Country continues to inch its way
    north and east this afternoon. The region remains mired in a
    tropical air-mass that sports anywhere from 2.2-2.5" PWATs and
    modest southerly 850mb theta-e advection continues to be funneled
    out ahead of the MCV, wrapping around its western flank and into
    Mason and Llano counties. While instability has decreased, there
    remains a subtle 500-850mb mean troughing signal overhead. When
    combined with MUCAPE values of 250-500 J/kg (per RAP
    mesoanalysis), highly saturated soundings, deep warm cloud layers
    (RAP soundings suggest up to 16,000ft), and no capping present,
    the MCV will still be capable of triggering additional storms
    around the western and southern flank of the MCV. Doppler Radar
    shows thunderstorms over Mason County continue to produce
    torrential downpours with MRMS 15-minute estimates approaching
    0.5-1.0". While storms should gradually diminish this evening, the exceptionally sensitive soils will make any additional rainfall
    unwelcome and likely result in additional flash flooding through
    the remainder of the afternoon.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7sK1_Bo2P9MtB-01CKMiYg8FBtDUUG61a5Pc7B4uZqcWclScLuvXzXHeJ3J0ucal2KzG= Idx8BRjomY_yMo0MRjnIe1U$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31639869 31369834 31339832 31069821 30759809=20
    30479802 30229808 30119855 30059900 30149935=20
    30509966 30909997 31279995 31529963 31619916=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 4 22:35:57 2025
    AWUS01 KWNH 042235
    FFGMPD
    MNZ000-IAZ000-KSZ000-NEZ000-SDZ000-050400-

    Mesoscale Precipitation Discussion 0590
    NWS Weather Prediction Center College Park MD
    634 PM EDT Fri Jul 04 2025

    Areas affected...Eastern Nebraska...Southeast South Dakota

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 042233Z - 050400Z

    SUMMARY...Widespread thunderstorms containing 1.5-2.0"/hr rainfall
    rates may produce flash flooding this afternoon and evening,
    especially in low-lying poor drainage areas and in more urbanized
    communities.

    DISCUSSION...GOES-19 satellite imagery and Doppler Radar show no
    shortage of thunderstorms traversing central Nebraska this
    afternoon. Storms are developing as far south as central Kansas as
    an integrated vapor transport (IVT) topping 700 kg/m/s advects a
    plentiful source of moisture northward. Storms are gradually
    moving north and east into eastern Nebraska and southeast South
    Dakota where RAP forecasts depict PWs between 1.75-2.0" and MLCAPE
    between 1,000-2,000 J/kg with little to no capping present.
    Focusing on the PWs, these PWs are topping the 99.5th
    climatological percentile per NAEFS. Plus, RAP soundings within
    the highlighted region sport low-mid level RH values averaging 90%
    and warm cloud layers over 14,000ft deep, supporting warm rain
    processes within these storms. There is also sufficient vertical
    wind shear to sustain these segments of thunderstorms for several
    more hours as they continue their northeast heading.

    Much of the highlighted region is either in D0-D2 drought
    conditions, so for most areas, this rainfall will be largely
    beneficial. However, it is the concern for back-building
    thunderstorms as the southerly IVT remains healthy into the
    overnight hours to potentially allow for training, moisture-loaded thunderstorms in some cases. Flash flooding is possible this
    afternoon and evening, especially in low-lying spots that drain
    poorly and in communities with a greater concentration of
    hydrophobic surfaces.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-k4kdhtUlFFn39oxR8A-B7qKECOntLRvTsUe729osRk318BM1pT_c57saz4JqPjT77R3= QtGVWSrJjA5mq1k3IhLPucg$ for graphic product...

    ATTN...WFO...FSD...GID...GLD...LBF...OAX...

    ATTN...RFC...KRF...NWC...

    LAT...LON 44499787 44469729 44279681 43929640 43639635=20
    43079649 42399677 41669714 41069746 40639786=20
    40249833 39669905 39479942 39320020 39440054=20
    39900083 40540082 41120046 41749982 42299936=20
    42869901 43409876 43889852 44379810=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 5 01:15:25 2025
    AWUS01 KWNH 050114
    FFGMPD
    MNZ000-SDZ000-NDZ000-050630-

    Mesoscale Precipitation Discussion 0591
    NWS Weather Prediction Center College Park MD
    914 PM EDT Fri Jul 04 2025

    Areas affected...Northern Minnesota...Eastern South Dakota

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 050115Z - 050630Z

    SUMMARY...Thunderstorms containing up to 2"/hr rainfall rates
    could result in additional areas of flash flooding this evening.

    DISCUSSION...A congealing line of thunderstorms stretching from
    just west of the Minnesota Arrowhead to as far south and west as
    eastern South Dakota continues to track east. The heaviest
    rainfall is occurring along and just south of a warm front that is
    oriented parallel to the MN/Canada border. Meanwhile, outflow
    boundaries out ahead of the approaching line of storms is helping
    to force air parcels vertically while as much as 35-45kts of
    effective bulk shear helps to sustain these thunderstorms
    updrafts. The environment just west of the Arrowhead on south into
    central MN remains unstable with as much as 1,000-2,000 J/kg at
    these storms disposal. Most notably, the atmospheric moisture
    content remains highly anomalous with the RAP showing a plume of
    2" PWATs aloft thanks to a >750 kg/m/s IVT directing anomalous
    moisture into the region via the Southern Plains.

    Storms should generally remain transient on the southern periphery
    of the highlighted area, but training thunderstorms across
    northern MN are possible as storms from eastern SD head northeast
    over the next few hours. Expect another 1-2" of rainfall within
    the highlighted region tonight with localized amounts potentially
    approaching 4" where the heaviest set of training convection takes
    shape. The flash flooding persists this Fourth of July night in
    northern Minnesota with lower-lying, poor drainage areas most
    at-risk. Any instances of ponding or flash flooding will become
    increasingly harder to identify on roadways after sunset.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8_DUosAi7kIaw7tU7xtPOxrUoDOrE7_Be2RKQDSBjjBYATpsHEKJvv6Lw_ngIX7no-hK= zBDpBXPxqZ1qqHKbOyP8H_w$ for graphic product...

    ATTN...WFO...ABR...DLH...FGF...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 48559265 48399174 48119135 47649168 47159253=20
    47019271 46099393 45519449 44869550 44699674=20
    44699745 45099755 45459737 46219668 46739597=20
    47389505 48079399 48429331=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 5 05:40:12 2025
    AWUS01 KWNH 050538
    FFGMPD
    TXZ000-050935-

    Mesoscale Precipitation Discussion 0592
    NWS Weather Prediction Center College Park MD
    138 AM EDT Sat Jul 05 2025

    Areas affected...central TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 050537Z - 050935Z

    SUMMARY...Localized heavy rainfall will be likely across portions
    of central TX over the next 2-4 hours. Flash flooding will result
    from rainfall rates in excess of 3 in/hr at times, especially if
    heavy rain cores can edge eastward toward Austin/Round Rock and
    the I-35 corridor.

    DISCUSSION...0510Z radar imagery from KGRK showed a slow moving
    thunderstorm in western Travis County with MRMS-derived hourly
    rainfall of 4 to 5 inches and at least one gauge report from LCRA
    of 4.98 inches per 60 minutes ending 0510Z near Largo Vista. This
    cell appeared to be located just north of a remaining mesoscale
    circulation just on the cool side of a remnant rain-cooled
    boundary from Friday's rainfall combined with a trough/wind shift
    axis that extended southwest to the Rio Grande across Webb County.
    SPC mesoanalysis and 04Z RAP data valid at 05Z showed a stable
    airmass across the Hill Country and northern TX while MLCAPE of
    500-1000 J/kg resided along and southeast of I-35 from Austin
    southward. 00Z soundings from DRT, FWD and CRP showed PW values at
    or above the 90th percentile and tropical moisture was still in
    place in the vicinity of an elongated low-mid level low which was
    located over central TX.

    S to SSE 850 mb winds of 10-20 kt are expected to continue
    overnight with advection of weak instability back toward the
    northwest and focused convergence near the remnant mesoscale
    vortex. Weak deeper mean layer winds of 10 kt or less will favor
    slow to nearly stationary movement of heavy rainfall with hourly
    rainfall exceeding 3 inches at times. The duration of the core of
    heaviest rainfall is uncertain, and it may begin to drift to the
    northwest as the instability gradient pushes northwest over the
    next couple of hours. However, present trends indicate near
    stationary net movement with continued very high rainfall rates
    continuing in the vicinity of western Travis/Williamson and
    eastern Burnet counties.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!87mFxu6nHHQCCpP1tt7fYLNAnwSHTk2ekXwo0vui6NRuvm_8Sj-CylFvs40E7cMlMgBC= QBpXI4z5yijlSGBZdZW46j0$ for graphic product...

    ATTN...WFO...EWX...FWD...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31769776 31619741 31219713 30789731 30409750=20
    30069771 30039796 30249830 30689845 31489825=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 5 07:09:29 2025
    AWUS01 KWNH 050708
    FFGMPD
    MNZ000-IAZ000-NEZ000-SDZ000-051215-

    Mesoscale Precipitation Discussion 0593
    NWS Weather Prediction Center College Park MD
    308 AM EDT Sat Jul 05 2025

    Areas affected...eastern NE into western IA, southern MN

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 050707Z - 051215Z

    Summary...Training of thunderstorms will result in rainfall rates
    of 1-2 in/hr, with a localized threat for 2-4 inches of rain
    through 12Z from eastern NE into western IA and southern MN.
    Localized flash flooding may occur as a result of these heavy
    rainfall totals.

    Discussion...Area radar imagery through 0645Z showed an uptick in
    the coverage of thunderstorms over portions of eastern NE over the
    past 60-90 minutes. A subtle increase in 850 mb wind speeds toward
    40 kt has coincided with the increase on convection. The storms
    were located within an anomalous moisture axis (+2 to +3
    standardized PW anomaly) which extended NNE through eastern NE
    into western MN, just ahead of a mid-level shortwave trough axis
    and on the trailing edge of a mid-level vort max over southwestern
    MN. The storms were also located beneath the upper ridge axis
    (increased diffluence) and within 500 to 1000+ J/kg MLCAPE via 06Z
    SPC mesoanalysis data.

    Some further increase of thunderstorm coverage will be possible
    over eastern NE into western IA through 09Z, ahead of the
    advancing upper trough and to the east of a forward propagating
    linear convective segment advancing into south-central NE. Mean
    steering flow is from the SW at 20-30 kt, weaker than 850 mb winds
    of a similar direction. This setup will pose a threat for SW to NE
    training and brief backbuilding of cells as the entire convective
    axis shifts eastward over the next 3-6 hours. Hourly rainfall of
    1-2 inches and spotty 2-4 inch totals may result in localized
    flash flooding.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8GkHF3HeC9htsDHJbb70Md6xpOLw0iv21lmLzztE-HVSqf_xLYzWqWH5KwIv3s9xdfMh= 5owOcvFE3_gB8QkZ7gBo2aM$ for graphic product...

    ATTN...WFO...ARX...DMX...FSD...GID...LBF...MPX...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 44759520 44489353 43589285 42429333 41369463=20
    40879579 40749707 40809798 40989830 41389864=20
    41749862 42539720 43409635=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 5 07:43:44 2025
    AWUS01 KWNH 050743
    FFGMPD
    MIZ000-WIZ000-MNZ000-051300-

    Mesoscale Precipitation Discussion 0594
    NWS Weather Prediction Center College Park MD
    342 AM EDT Sat Jul 05 2025

    Areas affected...eastern MN into northwestern WI

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 050741Z - 051300Z

    Summary...Isolated flash flood potential will exist from eastern
    MN into northwestern WI through 13Z. Training of cells will
    potentially allow for 1-2 in/hr rates and spotty 2-3 inch totals.

    Discussion...Regional radar imagery at 0720Z showed a broken axis
    of showers and thunderstorms that extended from the southern
    Arrowhead region of MN into southwestern MN where a mid-level
    vorticity max was located. These storms were located ahead of a
    mid-level shortwave trough that extended from northern MN into
    eastern SD within a weak instability axis of 500-1000 J/kg but
    anomalously high PW values of 1.5 to 2.0 inches (via 07Z SPC
    mesoanalysis data). Aloft, the region resided beneath an upper
    level ridge axis which was allowing for locally enhanced
    diffluence aloft.

    The positively tilted mid-level trough axis will continue to
    advance east this morning, and the vorticity max located over
    southwestern MN should follow northeastward within the
    southwesterly flow aloft. Scattered showers and thunderstorms will
    advance eastward through eastern MN into northwestern WI over the
    next few hours with occasional bursts in convective activity.
    While no significant changes in the weak instability environment
    are forecast, the high PW environment may support brief but
    intense rainfall rates. Mean southwesterly winds will carry the
    potential for localized training which could support rainfall
    rates of 1-2 in/hr and perhaps an isolated spot or two of 2-3
    inches through 13Z. Isolated flash flooding may occur as a result,
    with better potential existing where overlap of low lying or urban
    environments occurs.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_k73ZV96RjxmfBBOX5xcJcwHuPmzf8008Na_iPzmxihn4zL1-fZxqFDxizwBBooOreZ3= pv-OhUIhvZMMcIFu-jzZ5LA$ for graphic product...

    ATTN...WFO...ARX...DLH...MPX...MQT...

    ATTN...RFC...MSR...NWC...

    LAT...LON 47519042 46848999 45519097 44419184 44009287=20
    44179443 45149490 46349423 47489197=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 5 09:38:30 2025
    AWUS01 KWNH 050937
    FFGMPD
    TXZ000-051305-

    Mesoscale Precipitation Discussion 0595
    NWS Weather Prediction Center College Park MD
    536 AM EDT Sat Jul 05 2025

    Areas affected...central TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 050935Z - 051305Z

    SUMMARY...The potential for locally catastrophic flash flooding is
    expected to continue over the next few hours over central TX,
    extending through sunrise. Extreme hourly rainfall near and in
    excess of 4 to 5 inches can be expected at times. Dangerous /
    life-threatening flash flooding is already occurring and will
    continue for at least another 2-4 hours.

    DISCUSSION...0915Z radar imagery showed that a small cluster of
    heavy rain continued to affect central TX, with the highest
    rainfall intensities over western Williamson and eastern Burnet
    counties. Gauge data from the Lower Colorado River Authority
    (LCRA) showed a 10.34 inch total in 3 hours ending 0910Z, 8 miles
    SSW of Betram as recent trends in radar imagery have shown the
    heaviest rainfall intensities shifting northward compared to a few
    hours ago. This northward shift appears to be tied to a northward
    translation of a west-east oriented instability gradient that
    bisected the small convective cluster. Latent heat release within
    the thunderstorm cluster has reinvigorated a mesoscale vortex
    which was located along the Burnet/Williamson county line and has
    been allowing for the development of new updrafts to its immediate
    north, following 20-30 kt of southerly 925-850 mb winds within the
    anomalous PW environment (2.0 to 2.2 inches per 09Z SPC
    mesoanalysis data).

    Some continued northward development is expected over the next 2-4
    hours, although the core of the heaviest rain near the MCV is
    likely to remain farther south. While there is some uncertainty in
    the duration of the heaviest rainfall with RAP forecasts of
    925-850 mb winds shifting east and weakening through 13Z,
    continued very high rainfall rates of 3 to 5+ inches in an hour
    are expected to persist for another 1-3 hours with additional
    rainfall of 5 to 10 inches possible on top of an already saturated
    and flooded region just west of I-35. These rains are likely to
    continue threats for locally catastrophic flooding across a small
    region of central TX through at least 12Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4bohymefUInPxbMZSK59nGfEIOWsFTzlJ2-ZX9rZtXkbig2gITXC98oeAONPbVu6htLw= pUK6oEsjhZNURO0QJlQ3AwQ$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32449795 32349756 31969740 31059754 30429784=20
    30359821 30599847 31019866 31549866 32099853=20
    32359819=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 5 13:18:05 2025
    AWUS01 KWNH 051317
    FFGMPD
    TXZ000-051900-

    Mesoscale Precipitation Discussion 0596
    NWS Weather Prediction Center College Park MD
    917 AM EDT Sat Jul 05 2025

    Areas affected...Western portion of Texas Triangle...Eastern Hill
    Country...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 051315Z - 051900Z

    SUMMARY...Scattered thunderstorms linger on periphery of dying
    MCS. Highly efficient with rates of 2-3"/hr possible and slow
    motions will likely continue to pose a flash flooding risk in
    vicinity. Localized spots of 3-5"

    DISCUSSION...The dying MCC remains in a mid to upper level col
    though shearing toward the north into northern TX has been noted,
    while further elongation appears to be occurring to the south as
    well. CIRA LPW shows core of deep layer moisture resides in the
    surface to 850mb layer across the southern and eastern sides of
    the cyclone, though 850 and aloft the deep layer moisture has
    shifted toward the central TX coast and due northward. As such,
    extreme total PWat values up to 2.5" exist in the southeast
    quadrant of the cyclone in proximity to I-10 in the northern
    coastal Plain east of Austin. VWP and RAP analysis shows this is
    the greatest moisture flux with 25-30kts of southerly 850-700mb
    flow skirting the eastern side and becoming increasingly
    convergent across the northern Triangle north of Waco toward
    Cleburne toward the Dallas/Fort Worth Metroplex. Due to the very
    high theta-E near the surface, even 6C/km lapse rates remain still
    left of the parcel; narrow skinny/unstable profiles support
    1500-2000 J/kg of MLCAPE for any cells to strengthen. As such,
    low level convergence along the eastern side of the dying MCS has
    two major clusters along the northeast quadrant and the southeast
    quadrant. Rates of 2-3"/hr should be common with updrafts, though
    peak intensity.=20

    Aloft, the diffluent portion of the upper-level jet is dropping
    southward slowly and is currently enhancing convection in the
    northern Coastal Plain in the southeast quadrant given the 30-40kt
    exiting jet streak heading south and southwest around the building
    ridge over W TX. However, weak divergence/diffluence aloft remain
    modest across northeast TX as well though winds are lighter.=20
    However, this slower flow will allow for greater duration as cell
    motions remain below 5/10kts in the col in the northeast. This
    may allow for a few hours of compounding totals with
    focused/localized totals of 3-5" possible, likely to induce
    additional flash flooding concerns.

    Hi-Res CAMs help to suggest that storms could move back northwest
    and west to affect areas most recently affected across the Middle
    Colorado River, but loss of instability/heating and weak steering
    flow make this seem more aggressive that observational trends
    show, however, this reduces confidence toward overall evolution
    and the area with significant ongoing flooding in the Colorado
    Basin may have some additional rainfall to further compound
    flooding concerns in the next 4-6hrs.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Z8ZOY13jdCMEA9w11XTz9fSoNEte1wK9-6FHVz6FeCspRL1vbnBmBnAqr4VwhtNH5lh= GA2HViFt6S8EpIsEV-h3XZM$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32909811 32669708 31899668 30929665 30129672=20
    29449704 29029732 28819795 28989854 30499839=20
    30969839 32279867=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 5 19:43:09 2025
    AWUS01 KWNH 051943
    FFGMPD
    TXZ000-060100-

    Mesoscale Precipitation Discussion 0597
    NWS Weather Prediction Center College Park MD
    342 PM EDT Sat Jul 05 2025

    Areas affected...Texas Hill Country

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 051940Z - 060100Z

    SUMMARY...Additional thunderstorms containing prolific rainfall
    rates up to 3"/hr are expected this afternoon in parts of the
    Texas Hill Country. Any additional rainfall will likely exacerbate
    ongoing flash flooding.

    DISCUSSION...GOES-19 visible imagery and Doppler Radar continues
    to paint a messy picture of lingering thunderstorms over Burnet
    county and points east to the I-35 corridor north of Austin.
    Visible imagery shows that the bulk of the cloud cover and
    residual showers are on the southern and eastern flank of the MCV.
    While this is helping to reduce instability on those flanks,
    visible satellite imagery also show modest surface-based heating
    on the western flank of the MCV, including in Mason and LLano
    counties. 3-hr RTMA shows theta-e increases and MLCAPE rising >800
    J/kg during this same time. There remains a healthy surge of
    low-level moisture out of the western Gulf with tropical PWATs
    ranging between 2-2.5".

    The 18Z HRRR is showing back-building convection into the western
    portion of the highlighted region over the next few hours. Area
    averaged soundings over Mason/Llano counties show veering winds at
    low-levels with >2,000 MLCAPE available, PWATs >2.0", and warm
    cloud layer wind speeds <10 kts. RAP soundings also show warm
    cloud layers remains over 14,000ft deep for much of the region and
    low-mid level relative humidity levels are averaging ~90%. These
    slow motions, particularly near MCV, will result in
    self-sustaining thunderstorms that continue to produce prolific
    rainfall rates this afternoon. This is evident in the storms in
    southern Burnet county where MRMS 15-minute estimated rainfall
    rates have approached 1.0" in some cases, implying hourly rates as
    high as 4" are still possible in the more robust cells. Soils in
    these areas will struggle to handle 1"/hr rainfall rates, let 15
    minute rainfall rates approaching 1". Note that eastern areas will
    still contend with storms, but the swath of heaviest rainfall
    should start to shift to the western flank of the MCV.

    These storms and their prolific rainfall rates within the more
    intense storms will continue to exacerbate ongoing flooding within
    the region, as well as any ongoing cleanup and search/rescue
    efforts. Additional significant to life-threatening flash flooding
    is anticipated this afternoon. Storms should diminish later this
    evening as storms eat away at the available instability and the
    MCV gradually weakens.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8hzCUL7MEoj4fl8QgQV-Zl1H12qToVUjHQE9ykvT3udeJzLajYjBj5cknoU9zGSpnyjC= dCJMSkGBh-zKVJpEAkGjzto$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31659890 31489768 31389735 30929702 30409702=20
    29729736 29379823 29549881 29929912 30409987=20
    31369983=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 5 22:36:11 2025
    AWUS01 KWNH 052236
    FFGMPD
    AZZ000-060300-

    Mesoscale Precipitation Discussion 0598
    NWS Weather Prediction Center College Park MD
    635 PM EDT Sat Jul 05 2025

    Areas affected...Southeast Arizona

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 052230Z - 060300Z

    SUMMARY...Scattered heavy thunderstorms producing up to 1.5"/hr
    rainfall rates may cause additional areas of flash flooding this
    afternoon.

    DISCUSSION...Thunderstorms have broken out across southeast
    Arizona thanks to a sheared off 500mb vorticity and remnant
    moisture associated with Flossie. 500mb winds are oriented out of
    the SW and are aiding in some upslope-enhancement along the ridge
    lines of southeast Arizona and northern Sonora. Modest instability
    is present with RAP mesoanalysis showing as much as 1,000-2,000
    J/kg of SBCAPE. There is also sufficient moisture in place for
    storms to be effective rainfall producers, thanks to the remnant
    moisture of Flossie boosting PWs to as high as 1.3-1.5". Storms
    will continue to produce locally excessive rainfall rates up to
    1.5"/hr in some cases. Even if rainfall rates are closer to 1"/hr,
    this is generally close to the 1-hr FFGs and any training along
    local mountain ranges could cause some rainfall amounts to range
    between 2-3". Storms should dissipate not too long after sunset,
    but until then, additional flash flooding is possible for the
    remainder of the afternoon. Areas most at risk are along
    rugged/steep terrain and in dry washes.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5C60p9w6pmITBiwXicoNFZNZZsXX_WUWFxzBURXT25_sWhIoXR9gg3bld4iyERoirXrq= weS87yKyECbQxZrnLtjQWQ0$ for graphic product...

    ATTN...WFO...TWC...

    ATTN...RFC...STR...NWC...

    LAT...LON 32860995 32570943 32040916 31380926 31160968=20
    31151028 31181109 31341183 31821198 32261169=20
    32751085=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 6 06:05:07 2025
    AWUS01 KWNH 060603
    FFGMPD
    NCZ000-SCZ000-061200-

    Mesoscale Precipitation Discussion 0599
    NWS Weather Prediction Center College Park MD
    203 AM EDT Sun Jul 06 2025

    Areas affected...coast of northern SC/southern NC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 060602Z - 061200Z

    SUMMARY...Heavy rain and localized flash flooding will be possible
    across coastal locations of the Carolinas as T.S. Chantal
    approaches the northern SC coast tonight. Rainfall rates from 1 to
    3 in/hr will be possible along with localized 2-4 inch totals
    through 12Z.

    DISCUSSION...T.S. Chantal was located about 35 miles SSE of Myrtle
    Beach, SC via the latest NHC advisory from 06Z and was moving
    toward the NNW at 7 kt. Recent GOES East infrared satellite
    imagery showed the bulk of convection located in its front-right
    quadrant due to a combination of southerly shear and dry air south
    of the surface circulation as noted on layered PW imagery. After a
    burst in colder cloud tops contained within the CDO from late
    Saturday evening into the early overnight, there has been some
    minor warming of cloud tops since 05Z from the center of the CDO
    but recent cooling to the northeast. Local radar imagery from KTLX
    showed outer bands moving across the northern SC and southern NC
    coast along with a core of slower moving heavy rain about 25 miles
    southeast of Myrtle Beach. A curved rain band was becoming better
    defined to the south of Cape Fear as Chantal's CDO edges closer to
    the coast, tied to the recent cloud top cooling northeast of the
    CDO.

    Increasing rounds of steady heavy rain associated with Chantal are
    expected to begin moving onshore near the SC/NC border over the
    next 1-3 hours with increasing potential for 1-2 inches of rain in
    30-60 minutes. Rain rates, perhaps as high as 2-3 in/hr, will be
    possible with slow movement of Chantal's inner core and/or with
    training from spiral banding to the northeast of the CDO as
    banding interacts with the coast.

    While only a small section of southern NC has received above
    average rainfall over the past week, the rest of the region has
    been relatively dry and therefore, much of the Coastal Plain of
    northern SC/southern NC has relatively high flash flood guidance
    values of 3+ inches in 3 hours. Given antecedent conditions, flash
    flood potential due to incoming rounds of heavy rainfall appears
    most likely across urban locations within the Coastal Plain from
    Myrtle Beach to Wilmington, where potential for 2 to 4 inches of
    rain will exist through ~12Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!95YdfjZTTcveJSr_lOnlVxzXNfMaMQIJIDZdH377H-Hdlv2_42yJ4Euod24yZOJ5P-nP= CuxxIhoVK3Yr9Z9geIYN3_4$ for graphic product...

    ATTN...WFO...ILM...MHX...RAH...

    ATTN...RFC...ALR...NWC...

    LAT...LON 34927824 34927783 34667737 34407730 34097742=20
    33727777 33317850 33097903 33177936 33757957=20
    34297935 34777874=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 6 07:22:11 2025
    AWUS01 KWNH 060720
    FFGMPD
    TXZ000-061115-

    Mesoscale Precipitation Discussion 0600
    NWS Weather Prediction Center College Park MD
    319 AM EDT Sun Jul 06 2025

    Areas affected...west-central to central TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 060717Z - 061115Z

    Summary...Localized to widely scattered, small scale regions of
    heavy rain are expected to generate localized flash flooding over
    the next 3-4 hours from west-central to central TX. Hourly
    rainfall of 2 to 4 inches will be possible, overlapping with
    portions of the region that have sensitive/saturated soils due to
    recent heavy rainfall. However, coverage and organization of this
    heavy rainfall threat remains uncertain through 11Z.

    Discussion...07Z GOES East 10.3 micron imagery showed a few widely
    scattered showers/thunderstorms from west-central TX across the
    Edwards Plateau to north-central TX, to the southwest of Fort
    Worth. The cyclonic swirl of a remnant low to mid level low was
    evident in satellite imagery, centered about 70 miles WSW of Fort
    Worth where a thunderstorm containing -40 to -50 C cloud tops was
    located. According to SPC mesoanalysis data from 07Z, this cell
    was located along a MLCAPE gradient oriented fron north to south
    with little to no instability over the eastern third of TX and 500
    to 2000 J/kG to the west with varying degrees of CIN present
    within. PW values remained high (2+ inches) in a SSW to NNE
    orientation, extending from the lower Rio Grande Valley into the
    DFW Metroplex, but PW values dropped off to the east and west of
    this axis.

    With mean southerly low level flow in place over west-central to
    east-central TX at 15-25 kt, some degree of overrunning of
    Saturday's rain-cooled air over central TX was occurring with
    showers forming near a weak elevated convergence axis located
    around 850 mb. While the degree of organization of heavy over the
    next 3-4 hours is uncertain, deeper layer mean winds are weak,
    with the weakest/slowest cell potential near I-35 with LFC-EL mean
    wind values of ~5 kt or less. An increase in the coverage of showers/thunderstorms will is expected over the next few hours
    with slow movement supporting very high rainfall rates that have
    the potential to reach 2 to 4 inches (locally higher cannot be
    ruled out). Given recent heavy rain that has impacted portions of
    this region of TX over the past couple of days, renewed areas of
    flash flooding are expected, although coverage is expected to
    remain limited at this time.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8lFML3QHCZa6rGUE6Bmlrzo-4GUFO72KlQabGUpoF0G4SwV8ovEVMmCIEuLkxO-BvicF= s2c7D9sSs_BL7UGr0wLJ3Xg$ for graphic product...

    ATTN...WFO...EWX...FWD...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32939795 32639735 32069725 30879753 30059857=20
    30000005 30180099 30560152 30900165 31210161=20
    31580142 31700085 31770041 31939984 32329915=20
    32739855=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 6 11:03:41 2025
    AWUS01 KWNH 061102
    FFGMPD
    TXZ000-061630-

    Mesoscale Precipitation Discussion 0601
    NWS Weather Prediction Center College Park MD
    701 AM EDT Sun Jul 06 2025

    Areas affected...central to north-central TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 061100Z - 061630Z

    SUMMARY...A likely but localized flash flood threat will focus
    across portions of central to north-central TX through 16Z. Hourly
    rainfall of 1 to 3+ in/hr and spotty 3 to 6 inch rainfall totals
    are expected. Overlap of additional heavy rain areas with
    sensitive/saturated soils due to recent heavy rainfall will
    increase potential for renewed flash flooding.

    DISCUSSION...Regional radar imagery through 1030Z showed that
    showers and thunderstorms continued to expand to the southwest of
    Fort Worth and into portions of the Edwards Plateau. MRMS-derived
    rain rates were locally over 2 in/hr between Granbury and Meridan
    and were increasing toward 2 in/hr over Mason County. A
    north-south elongated 700 mb low/trough was located between Fort
    Worth and Abilene, co-located with PW values between 2.0 and 2.2
    inches per 10Z SPC mesoanalysis data. SPC mesoanalysis data also
    showed the area of storms southwest of Fort Worth was along a
    north-south oriented instability gradient, with little to no CAPE
    over the eastern third of TX with 1000-2000 J/kg to the west.
    Meanwhile, 925-850 mb winds were parallel to I-35 between San
    Antonio and Dallas-Fort Worth, while these winds were veered to
    the west across the Edwards Plateau and Rolling Plains regions,
    allowing for confluent flow to the west of I-35. Weak deeper layer
    steering flow and the relatively stronger low level inflow layer
    will set the stage for potential training and back-building of
    cells.

    Given the environment in place, potential for slow moving cores of
    heavy rain, peak hourly rainfall of 2 to 3+ inches will be
    possible along with higher end totals in the 3 to 6 inch range
    over the next 6 hours. Overlap of these higher rainfall totals
    with portions of central TX that received heavy rainfall over the
    past 72 hours will increase the threat of flash flooding. However,
    these higher end totals should be fairly low in coverage. So
    therefore, while flash flooding is considered likely over the next
    several hours, coverage is expected to remain rather isolated.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4TOAoKRzMWOPk6h4MuQN2V5pSVXcXdreKE9R4bM75zL2kQz7mq7dady3ChruKI_gN5-Z= xskqUuLjIgkYhPGdG0nvSrQ$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 33169754 32579723 31499731 30399791 29749868=20
    29699954 30189988 30909965 31829927 32519877=20
    33169824=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 6 12:00:50 2025
    AWUS01 KWNH 061200
    FFGMPD
    NCZ000-SCZ000-061800-

    Mesoscale Precipitation Discussion 0602
    NWS Weather Prediction Center College Park MD
    800 AM EDT Sun Jul 06 2025

    Areas affected...E & SE North Carolina...Ext. E South Carolina...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 061200Z - 061800Z

    SUMMARY...T.S. Chantal

    DISCUSSION...GOES-E Vis/IR animation shows a small but still
    compact circulation to T.S. Chantal with a central dense overcast
    (CDO) cluster of thunderstorms straddling the eastern NC/SC border
    as it continues just north of northwest track. This CDO is
    expected to maintain given fairly solid vertical depth to the
    cyclone with at least 4-6 more hours before asymmetries evolve due
    to increased vertical shear profile. Deep layer moisture over
    2.5" and strong 30-40kt moisture convergence will continue to
    support very efficient rainfall processes with 2-2.5"/hr rates
    across much of the core. Given slow translation speeds, spots of
    3-5" are possible in/near the core.=20

    A solid banding feature continues to burst with similar cold
    overshooting tops to -65C though those cores are a bit more
    transient through the banding feature. Strong confluent inflow
    along the band in proximity to the Gulf Stream continues to
    support strong back-building environment in the near term, as such
    short-term training is possible through Onslow county. However,
    the dry slot rotating around the southern to southeastern quadrant
    is starting to impinge on the band, mix and aid northward
    propagation to reduce local duration of the band. So while
    intense, the duration should be much less than areas near the CDO
    and streaks of 1-3" are possible likely limiting flash flooding to
    urban/poor drainage areas overwhelmed by the shear short-term
    intensity of the banding features unless that back-building
    short-term training is ideal but that would be very widely
    scattered/isolated in nature.

    Toward 16-18z, the solid warm air advection (WAA) across the
    coastal plain of NC along with the wrapping dry slot will result
    into increased elongation of the deeper layer circulation and
    should result in a slowing of speed, but also a sharpening of a
    northward trending convergence boundary near the NC/SC 'corner' of Scotland/Marlboro counties. This convergence band will be slow to
    drift further west and the CDO should break down and expand
    northward along this axis, increasing rainfall totals and
    potential for 3-4" totals by 18z.

    Hydrologically, naturally sandy soils that have been fairly dry
    with relative soil moisture ratios below 40% and running in the
    20-40th percentile for dryness, should uptake much of the rain
    (with exception of impermeable urban settings) with hourly FFG
    values of 2-3" and 3-4"/3hrs; only the most persistent/intense
    rainfall areas are at risk of flash/rapid inundation flooding.=20
    Still, a few widely scattered incidents of flash flooding will
    remain possible through the morning hours most likely near the
    CDO.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6wO-pMq0tnoyDjNVt-HI5jczodIfk7nS5rOxkW_JCvgp62ix0zsuQIVEi-h8D1rzX8MT= JNExXIYuq_t2hZhK6XhMeTw$ for graphic product...

    ATTN...WFO...CAE...ILM...MHX...RAH...

    ATTN...RFC...ALR...NWC...

    LAT...LON 35977784 35667662 35067578 34577621 34447684=20
    34427787 34247845 34087893 33977935 34257978=20
    34798004 35397977 35897896=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 6 16:16:34 2025
    AWUS01 KWNH 061616
    FFGMPD
    TXZ000-062200-

    Mesoscale Precipitation Discussion 0603
    NWS Weather Prediction Center College Park MD
    1215 PM EDT Sun Jul 06 2025

    Areas affected...Northern & Central Texas...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 061615Z - 062200Z

    SUMMARY...Stubborn mid-level circulation and remaining tropical
    moisture plume.

    DISCUSSION...GOES-E WV suite shows favorable upper-level pattern
    is breaking down a bit as 40-50kt jet streak and entrance region
    shifts southward into central and southern TX with amplifying mid
    to upper-level ridge across the Permian Basin sliding southeast
    into the Big Country. As such, very favorable outflow regime is
    diminishing in influence and expected to slide. A highly
    stretched/sheared dryier axis exists across far E TX/LA;
    corralling the remaining (but reducing) overall deep layer
    moisture plume from the Red River Valley generally along I-35 and
    westward through the eastern Hill country with values of 2-2.25"
    remaining though mainly along the southeast quadrant of a
    persistent/stubborm mid-level circulation centered near Palo Pinto
    county. The core of the deep layer moisture has seen a recent
    rapid exhaustion of instability with the ongoing convective cores
    that are erroding from Tarrent to Bosque county.

    Surface, VWP and visible imagery analysis shows a convergence axis
    of the western gradient of the deeper layer mositure from a weak
    surface low near K6P9 back west across the Edwards Plateau from
    Callahan to Coke to Sterling county. Here, full insolation is
    providing surface heating for narrow, skinny unstalbe profiles up
    to 2000 J/kg; southwesterly to southerly flow along a pressure
    trof from the low to JCT is providing the convergence necessary
    for newer development. Rainfall efficiency will continue to be an
    issue with 2-2.5"/hr probable. However, given the shift of the
    favorable outflow aloft and stronger southerly inflow, propagation
    is likey to press cells south and westward toward the Hill
    Country, but given motion, more than likely limit duration at any
    given location to scattered 1-3" totals. Still, remaining
    sensitive soils and rapid run off still may result in possible
    localized flash flooding conditions.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7hmIdQpS6k6OVWvSMUAGE5uhIhI47NKh8G5l2yOiFSaQp6wJeXbBwzBHEP1rLwbljxut= JMESAa5Kmq7pnWwbaIPvw_Q$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 33329763 32969728 32109711 31259736 30519817=20
    30589966 31000023 31700038 32109983 32369933=20
    32629884 32879844 33179827=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 6 17:54:21 2025
    AWUS01 KWNH 061754
    FFGMPD
    VAZ000-NCZ000-070000-

    Mesoscale Precipitation Discussion 0604
    NWS Weather Prediction Center College Park MD
    153 PM EDT Sun Jul 06 2025

    Areas affected...Central North Carolina... Far South-central
    Virginia...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 061800Z - 070000Z

    SUMMARY...Tropical Depression Chantal. Prolonged moderate
    rainfall with training core of intense rainfall of 2-3"/hr
    possible. Localized 3-6" and flash flooding likely.

    DISCUSSION...GOES-E satellite suite shows classic vertical tilting
    of the deep circulation of Chantal with broad surface/boundary
    layer circulation becoming exposed along the southern and
    southeastern side of the remaining strong convective core of
    thunderstorms near Scotland/Richmond county expanding downshear (north-northeastward) into Moore/Lee counties. Upper-level speed
    max is starting to increase connect up with the northern stream
    main jet stream flow across the central Applachians; further
    expanding downstream outflow aloft. In doing so the mid to low
    level circulation will continue to expand and elongate through a
    deformation and low level convergence trough axis that can be seen
    starting to become active with scattered showers from Orange to
    Durham to Granville county area. Broad southeasterly to easterly
    confluent 850-700mb 30-35kt flow slows and veers more northward
    along this axis providing very strong moisture flux convergence
    along it.

    Cells will start with .5-1"/hr rates but increase as the
    convective core lifts north, effectively training/repeating
    through this same axis. Given deepest moisture of 2.5-2.75" of
    total PWats and strongest speed/directional convergence with the
    850-700mb cyclone center will support initially 3"/hr rates slowly
    reducing toward 2-2.5" toward 00z. So prolonged moderate rainfall
    amplifying to these higher rates will result in spotty 1-2" and
    saturating wet grounds in advance of the intense rainfall; likely
    limiting infiltration. Additional 2-4" totals along the
    convergence zone results in an axis of 3-6" through 00z. This
    will likely result in flash flooding/rapid inundation conditions
    along this narrow training corridor. Current trends suggest axis
    is likely across Moore to Chatham to Allamance and may split
    Greensboro and Raleigh metro areas, but small deviations of the
    axis (more probable eastaward) would result in a growing concern
    for considerable/significant flooding incidents due to urban
    impermeable surfaces near those metro areas (incl.
    Durham/Apex/Chapel Hill).=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6zTma3Rax4MNsSJ6rGKMHSxRTTT3ARAIkUD4LsGkKLmbOYJXAuvWOjrqUxrQh6mC33Xj= kGVBO8UknSTb2bMMSy-WcMc$ for graphic product...

    ATTN...WFO...AKQ...RAH...RNK...

    ATTN...RFC...ALR...NWC...

    LAT...LON 36837859 36797809 36397792 36137811 35767841=20
    35207884 34887937 34997990 35577996 36127964=20
    36437935 36707898=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 6 20:19:22 2025
    AWUS01 KWNH 062019
    FFGMPD
    TXZ000-070200-

    Mesoscale Precipitation Discussion 0605
    NWS Weather Prediction Center College Park MD
    418 PM EDT Sun Jul 06 2025

    Areas affected...South Central Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 062020Z - 070200Z

    SUMMARY...Scattered thunderstorms are likely to contain torrential
    downpours over sensitive soils across parts of the Texas Hill
    Country. Flash flooding is possible this afternoon.

    DISCUSSION...The air-mass across the Texas Hill Country continues
    to support tropical and pulse-like thunderstorms this afternoon.
    RAP mesoanalysis shows as much as 1,500-2,000 J/kg of MLCAPE and
    PWATs that range between 2.0-2.25". Unlike the past 48-hours,
    there is not as much upper-level support in south central Texas to
    organize most of these developing storms, making them shorter
    lived in duration. However, storms will likely produce outflows
    that can kick-start additional storms with little to no capping
    present throughout the region. 18Z RAP soundings near the San
    Antonio and Austin metro areas do support warm cloud layers nearly
    13,000ft deep and low-mid level averaged relative humidity values
    above 85%. These parameters continue to support efficient warm
    rain processes, evident by MRMS 15-minute radar estimated rainfall
    rates approaching 0.50" north of Fredericksburg and northwest of
    Liberty Hill. This suggests, should storms be sustained long
    enough to eclipse 1-hr in duration, there could be cases where
    2"/hr rainfall rates are met and 1-hr FFGs remain <2" along and
    west of I-35.

    0-40cm soil moisture percentiles according to NASA SPoRT-LIS show
    anywhere from San Antonio on north sports at least 80% soil
    saturation. These storms should be more pulse-like in nature, but
    given the soil sensitivities in the area, there is the potential
    for as much as 2-3" of rainfall (local amounts up to 4") in areas
    that do not need any more rainfall. Flash flooding is possible
    once again this afternoon. Thunderstorms should dissipate in
    coverage after sunset thanks to the loss of daytime heating.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7AA_xElWswOSkpeQP7Bpcmupj2ezhGoAkjibWu4pL1-usFLSnTt4HYKD5UgYc2qU8Hwv= 4_pcbsbXQmYFPs4LgFzQ2DU$ for graphic product...

    ATTN...WFO...EWX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30869817 30779768 30559729 29939706 29209787=20
    29079876 29089937 29230003 29430039 29700052=20
    30180033 30469988 30689896=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 6 21:25:49 2025
    AWUS01 KWNH 062125
    FFGMPD
    ILZ000-MOZ000-KSZ000-070300-

    Mesoscale Precipitation Discussion 0606
    NWS Weather Prediction Center College Park MD
    524 PM EDT Sun Jul 06 2025

    Areas affected...Southeast KS...Southern MO...Southern IL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 062120Z - 070300Z

    SUMMARY...Repeating thunderstorms training over select portions of
    the region could cause flash flooding through this evening.

    DISCUSSION...A cold front approaching from the north is helping to
    trigger storms just ahead of the front, while strong surface-based
    heating and emanating outflows from pre-frontal storms are likely
    to ignite more storms this afternoon. RAP mesoanalysis shows there
    is an abundance of moisture available from southeast Kansas to as
    far east as southern Illinois as PWATs are between 1.9-2.2", which
    are above the 90th climatological percentile for early July. The
    atmosphere, as depicted on GOES-19 satellite imagery and Doppler
    Radar, is quite unstable with MLCAPE values surpassing 2,000 J/kg
    for the vast majority of the highlighted region. The mean
    850-300mb wind flow is generally progressive with 10-15 knot winds
    averaged through the depth of the column, but there remains a
    steady fetch of southerly 850mb flow over the ArkLaTex that is
    feeding anomalous moisture into the region ahead of the cold
    front. With the added help of a passing 500mb vort max, there
    remains enough forcing at low-levels and upper-levels to support
    additional thunderstorms for the remainder of the afternoon and
    into this evening.

    MRMS 15-minute radar estimates suggests storms are producing up to
    0.50" of rainfall in that span, equating to near 2"/hr rainfall
    rates. Most of the region's soils are generally able to handle
    rates just below that, but anything over 2" (particuarly in
    southern Missouri where soil moisture anomalies are >80% in some
    areas), poses a flash flood threat. Given the numerous
    thunderstorms throughout the region, some places may receive 2-4"
    or rainfall from seeing multiple rounds of storms this afternoon.
    Flash flooding is possible, particularly in poor drainage spots
    and in urbanized communities sporting a greater concentration of
    hydrophobic surfaces.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-YHDbFiv9-o5mkq5KoZrZs0OdreC3xfLM1YkH4-VS0kROIbjehkAPsN2KkVGmMEoEfdX= 1PdOQguloregCDVPhWq49MI$ for graphic product...

    ATTN...WFO...EAX...ICT...ILX...LSX...PAH...SGF...TOP...

    ATTN...RFC...KRF...MSR...ORN...TIR...TUA...NWC...

    LAT...LON 39908866 39838792 39368766 38268816 37628893=20
    37089011 36799097 36679306 37019412 37119515=20
    37269687 37819725 38199688 38389608 38719391=20
    39079282 39549104 39679000 39818937=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 7 00:08:47 2025
    AWUS01 KWNH 070007
    FFGMPD
    VAZ000-NCZ000-070500-

    Mesoscale Precipitation Discussion 0607
    NWS Weather Prediction Center College Park MD
    807 PM EDT Sun Jul 06 2025

    Areas affected...Southern VA...Northern NC

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 070000Z - 070500Z

    SUMMARY...Chantal continues to produce Excessive Rainfall rates in
    excess of 2"/hr as it slowly tracks northeastward this evening.
    Additional flash flooding is likely with the potential for
    life-threatening impacts in affected areas.

    DISCUSSION...Thunderstorms associated with Chantal are more
    aligned with the storm's mid-level circulation as the surface
    circulation remains farther south, or just north of Fayetteville.
    Doppler Radar showed the core of heaviest rainfall occurring from
    Chapel Hill and the western suburbs of Durham on west along I-40
    and just east of Greensboro. Latest guidance shows Chantal slowly
    inching its way northeast this evening while still maintaining the
    heaviest rainfall north and west of Chantal's low-mid level
    circulation. Along its path, PWATs are over 2.0" and in some cases
    approaching 2.4" according to RAP mesoanalysis. RAP soundings
    within the core of heaviest rainfall depict classic warm rain
    processes that exist within the core of a tropical cyclone: skinny
    CAPE aloft (between 250-750 J/kg MUCAPE), > 90% sounding
    saturation nearly all the way to the tropopause, and warm cloud
    layers nearly 16,000ft deep. This is likely to remain the case as
    Chantal moves north and east this evening.

    Recent observations show as much as 2.6" in one hour have fallen
    just southwest of Durham with the storm only inching its way
    northeast at the moment. The storm should continue to gradually
    weaken along its track, but when taking area-averaged soundings
    around the Chantal using the HAFS-A model, steering flow within
    the 300-850mb layer at 06Z tonight was SW at ~10 kts. Meanwhile,
    the storm will still maintain a healthy SErly IVT that wraps
    around the storm and along its western flank. Latest 18Z HREF does
    show the gradually diminishing precipitation rates as the night
    progresses, but the highly saturated profiles combined with
    lingering MUCAPE and its slow progression makes flash flooding a
    big concern from north-central NC to south-central VA tonight.
    Over the past 6-hours, portions of central North Carolina have
    seen anywhere from 2-5" of rainfall with localized totals topping
    7". Expect similar totals once again over the next 6 hours from
    the western suburbs of the Raleigh-Durham metro area on north into
    far south-central VA. Significant to life-threatening flooding
    impacts within its narrow corridor of heaviest rainfall is likely
    this evening.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5drWCsuVAqPTmXDIy4JloDPZsxRv94piSGl5o6KI3nsYxoEyXt8A-MdMex1Us5yGplTC= DYv97gKNYKLesfZBUhuQeH0$ for graphic product...

    ATTN...WFO...AKQ...RAH...RNK...

    ATTN...RFC...ALR...NWC...

    LAT...LON 37017881 37007850 36847821 36547832 36137860=20
    35677888 35547920 35667951 35917964 36197962=20
    36657939 36897915=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 7 04:35:59 2025
    AWUS01 KWNH 070435
    FFGMPD
    TXZ000-070900-

    Mesoscale Precipitation Discussion 0608
    NWS Weather Prediction Center College Park MD
    1235 AM EDT Mon Jul 07 2025

    Areas affected...parts of central TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 070434Z - 070900Z

    SUMMARY...Thunderstorms are expected to increase across portions
    of central TX over the next few hours with areas of slow movement
    and locally heavy rainfall. Localized hourly rainfall in the 1 to
    3 inch range is expected, possibly leading to isolated flash flood
    concerns across the region.

    DISCUSSION...Local radar imagery across central TX appeared to be
    showing the beginning stages of renewed shower/thunderstorm
    development as of 04Z just east of I-35 from Austin to Jarrell.
    GOES East infrared imagery helped place a remnant MCV in the
    vicinity of Llano County, embedded within broader cyclonic flow
    tied to an elongated 700 mb low/trough that has been lingering
    over central TX, evident on 700 mb VAD wind plots. At the surface,
    a remnant rain-cooled outflow boundary was analyzed from just
    southeast of LHB to near BAZ and southwest to COT. Since 00Z,
    increased 925-850 mb wind speeds of 15-25 kt at KGRK and KEWX
    match RAP depictions of winds in this layer, which has helped to
    support an northward increase in MLCAPE past I-10 into portions of
    central TX. SPC mesoanalysis data from 04Z showed a plume of 1000
    to 2000+ J/kg MLCAPE nosing northward from the middle TX coast
    into the I-35 corridor between San Antonio and Dallas/Fort Worth
    containing little to no inhibition.

    RAP forecasts indicate 925-850 mb winds are near their peak in the
    short term, with slight weakening over the east and westward
    translation of relatively stronger wind speeds toward 09Z.
    However, the circulation around the remnant MCV and presence of
    the outflow boundary and overrunning potential within the high PW
    environment (2.0 to 2.3 inches via SPC mesoanalysis data) is
    expected to continue to support scattered shower and thunderstorm
    development over the next few hours. Weak steering flow and the
    relatively stronger low level flow will support the potential for
    training and back-building of cells. While the coverage of these
    cells remains a bit uncertain, the environment will be capable of
    generating 1-3 in/hr rainfall totals. Given the continuing
    sensitivity of soils across portions of the region, renewed flash
    flood concerns through 09Z appear possible.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Oax3ELJFf2URWGzPpp_XFZ3KFiak_ywVyZLeak6zYPvtTw9XK9CM6JsaeAcbhXccxdA= 4QpHPQrXjwNBgAaBh88XvIs$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31739711 31279664 30439657 29439708 28919834=20
    28899895 29159973 29749994 30319974 30649943=20
    31089860 31429816=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 7 05:39:59 2025
    AWUS01 KWNH 070538
    FFGMPD
    VAZ000-NCZ000-071000-

    Mesoscale Precipitation Discussion 0609
    NWS Weather Prediction Center College Park MD
    137 AM EDT Mon Jul 07 2025

    Areas affected...far northern NC into southern and central VA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 070536Z - 071000Z

    Summary...Heavy rain associated with T.D. Chantal will continue to
    spread northward into VA overnight. Hourly rainfall of 1-2 inches
    is expected with additional totals of 2-4 inches possible through
    11Z. Flash flooding remains likely, especially early on, although
    some decrease in the threat may occur by later this morning.

    Discussion...05Z radar imagery showed the core of Chantal's
    heaviest rainfall occurring south of Halifax, VA, along and just
    north of the NC/VA border. This area of heavy rain was displaced
    roughly 20-40 miles north of the surface low due to vertical
    tilting of the cyclone structure toward the north and west with
    height and heavy rain tied to the mid-level center. Observed
    hourly rainfall within the relatively compact cluster of heavy
    rain has been 1.0 to 2.5 inches between 04-05Z and movement has
    been toward the NNE over the past 3 hours. Trends in satellite
    imagery showed infrared cloud tops warming overall but with
    occasional bursts of colder cloud tops over southern VA.

    A continued translation of Chantal's mid-level center toward the
    northeast is expected over the next 3-5 hours, following steering
    between troughing to the west and a ridge over the western
    Atlantic. RAP forecasts indicate some weakening of low level
    convergence northwest of Chantal's surface low between 06Z-09Z,
    along with lowering instability which may act to decrease rainfall
    intensity and the threat for flash flooding. However, tropical
    moisture with PW values up to about 2.3 inches and favorable
    outflow within the northern semicircle of the system's circulation
    will continue to support bursts of heavier rain. The slow movement
    of Chantal will continue to favor areas of flash flooding over
    southern VA, especially in the short term, with the flash flood
    threat continuing into central VA later this morning.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!98f-bI9RCxZyYQssHzTws1URD__m8M1DAIfiJOYdxxW6MXZoL4KgOTCSen5tp9saGsjb= sxOqnfGFJVrbMAQmbqxJLF8$ for graphic product...

    ATTN...WFO...AKQ...LWX...RAH...RNK...

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37977773 37557751 36867780 36347848 36287912=20
    36567934 37257901 37877839=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 7 11:54:35 2025
    AWUS01 KWNH 071154
    FFGMPD
    TXZ000-071650-

    Mesoscale Precipitation Discussion 0610
    NWS Weather Prediction Center College Park MD
    753 AM EDT Mon Jul 07 2025

    Areas affected...portions of central TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 071150Z - 071650Z

    SUMMARY...Localized flash flooding remains possible this morning
    for portions of central TX. The potential for hourly rainfall of
    1-3 inches will exist, but mostly isolated in nature within widely
    scattered showers and thunderstorms.

    DISCUSSION...Recent radar and GOES19 IR satellite imagery shows
    developing showers and thunderstorms this morning across central
    TX within the vicinity of a sheared out remnant MCV. This MCV from
    Sunday afternoon has become rather difficult to find in satellite
    imagery as of 11Z. Extrapolating known placement from earlier, it
    is perhaps in the vicinity of Fredericksburg but it has lost the
    origination it contained earlier. In addition, a diffuse outflow
    boundary remained from near LHB to just west of SAT and then
    southwestward toward the middle Rio Grande Valley. Both of these
    features may not play a significant role in the future convective
    evolution over central TX but they are features to note
    nonetheless. The long-lived 700 mb low/trough over central TX has
    become more elongated and is forecast to slowly shift west during
    the morning hours. This is expected to encourage the minor
    expansion of weak low level southerly flow into the Edwards
    Plateau and remaining portions of central TX. With the onset of
    daytime heating through existing cloud cover, erosion of low level
    convective inhibition is expected to allow for the further
    development of shower and thunderstorms across portions of central
    TX.

    Weak deeper layer winds (weak steering flow) will support locally
    heavy rain with potential for back-building and brief training of
    cells. The high PW environment (near 2 inches), will be capable of
    producing 1 to 3 inch hourly rainfall totals in a widely scattered
    fashion across the region. Remaining sensitivity of near saturated
    grounds across the region could allow for a couple of areas of
    flash flooding through about 17Z. Recent 10Z HRRR seems to be
    under-forecasting current activity, so it is worth watching radar
    trends should convection become even more widespread given the
    weak steering flow currently in place this morning.

    Snell/Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9PRYUqY_aYEO19sV2Arpd43xH9exLcrfseYKHaTqOaTsoIdEKqQtqjxtdbjylKk01lbZ= fvXWC_SMCjMUYXiyZBpWrCw$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32189859 32059761 31499726 30689743 29779799=20
    29289875 29329954 29829994 30649987 31669939=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 7 13:56:26 2025
    AWUS01 KWNH 071355
    FFGMPD
    TXZ000-071955-

    Mesoscale Precipitation Discussion 0611
    NWS Weather Prediction Center College Park MD
    955 AM EDT Mon Jul 07 2025

    Areas affected...Parts of the Texas Hill Country

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 071355Z - 071955Z

    SUMMARY...Slow-moving thunderstorms producing local rainfall rates
    over 3"/hr are ongoing and expected to continue through early this
    afternoon. Some significant instances of flash flooding are
    possible, especially given the sensitive flood-prone terrain of
    central TX.

    DISCUSSION...Radar and satellite imagery highlight strengthening
    thunderstorms oriented along a strung-out 700 mb trough in a
    west-southwest to east-northeast direction. MRMS estimates hourly
    rainfall rates just west of Killeen over 3"/hr, with a HADS
    observation (supprted by surrounding obs) recording 4.2" in 3
    hours by 1330Z.

    The same highly moist and unstable environment remains over
    central TX, with mean layer flow generally less than 5 kts.
    However, upwind propagation vectors remain out of the
    north-northeast which supports back-building through this
    afternoon. MLCAPE remains elevated in the 1000-1500 J/kg range and
    will increase throughout the day due to the combination of
    southerly flow out of the western Gulf and diurnal heating. This
    setup supports the continuing threat of slow-moving thunderstorms
    producing 2-3"+ hourly rates, with scattered flash flooding
    likely. Significant flash flooding is also possible where any
    mesoscale circulations develop within thunderstorms and can stall
    these extreme rainfall rates over a region for a few hours (like
    what was seen west of Killeen). Locally, rainfall totals may
    exceed 5" within these intense thunderstorms.

    1-hr FFG across the sensitive soils of central TX are generally
    below 2" and as low as 1" locally. The 12z HRRR depicts convection
    eventually migrating westward, probably under the influence of the
    700 mb trough tilting west-east and lifting north. So, while the
    ongoing activity will likely move within a few hours it can be
    expected that scattered intense rainfall rates develop elsewhere
    and lead to flash flooding.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4rrZYKc0CcpfFuVS5Y3J5dGhwqLcWkNs1VrDduhkfHtElrO1yzHIvk_BZiZHuHISX8Fj= H0EYq0ZpCahoPYT0CuU6Nz8$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31739862 31509790 31039776 30649827 30309938=20
    30190046 30460087 31100046 31619958=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 7 15:50:05 2025
    AWUS01 KWNH 071550
    FFGMPD
    NJZ000-PAZ000-DEZ000-MDZ000-072150-

    Mesoscale Precipitation Discussion 0612
    NWS Weather Prediction Center College Park MD
    1149 AM EDT Mon Jul 07 2025

    Areas affected...Parts of the Mid-Atlantic between southern
    Maryland and northern New Jersey

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 071550Z - 072150Z

    SUMMARY...Slow-moving to stationary showers and thunderstorms
    associated with Post-T.C. Chantal are expected to increase in
    coverage and intensity this afternoon. Highly efficient tropical
    downpours (2-3"/hr rates) are expected within these thunderstorms
    and overlap with the urbanized corridor of eastern PA, NJ,
    northern DE, and central/eastern MD. Scattered instances of flash
    flooding are considered likely.

    DISCUSSION...Post-T.C. Chantal was analyzed across southeast VA at
    15z and continues to push northeast at around 30 mph. Meanwhile, a
    surface trough extends to the northeast across the northern
    Delmarva Peninsula and into northern NJ. This surface trough and
    area of convergence just to the north and west of Chantal's center
    will likely become the focus for developing slow-moving
    thunderstorms through this afternoon. The atmospheric environment
    in place supports efficient rain processes, with PWs of 2.0-2.4"
    and MLCAPE of 1000-1500 J/kg. In fact, although displaced just to
    the west of the heaviest rainfall threat IAD's 12z sounding
    depicted a PW of 2.13" and freezing level of 15,788 feet, both
    just below the daily max.

    There is anticipated to be two separate modes of heavy rainfall
    along the highlighted area from southern MD to northern NJ through
    about 21z. The first area of concern is near the center of
    Post-T.C. Chantal as it crosses over the Delmarva. Here,
    slow-moving thunderstorms will feed off enhanced tropical moisture
    (PWs over 2.3") and elevated levels of effective bulk shear (over
    25 kts). Additionally, as the center of Chantal opens into more of
    a mid-level trough by later this afternoon, weak steering flow
    will be evident directly under this trough across the Delmarva.
    This region is where the greatest potential exists for rainfall
    rates to reach or even briefly exceed 3"/hr, as well as rainfall
    totals exceed 5" potentially. The other area of concern will be
    across eastern PA and NJ where mean layer flow of 20 kts out of
    the south-southeast and out of an area of greater instability
    (greater than 3000 J/kg of SBCAPE) will promote back-building or
    stalled thunderstorms within a moist environment. Here, impacts
    are expected to remain mostly localized as storms remain generally
    small in size, but some impacts could be considerable given the
    urban and sensitive terrain.

    This region is most likely to experience impacts associated with
    urban flooding or rapid ponding of water on roadways, with an
    exception in southeast PA and central NJ where more rural and
    suburban flash flooding is possible near rivers and streams given
    the sensitive terrain and 1-hr FFG less than 1.5-2.0" in spots.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-R8bs3Hv-542-ryeM15lR8t5L_0AsV1rye2Spw5zS89eN4UuqYMJORmU1QVkIObEP5W0= 67OpKbeg69mUC_0uUUmw3g0$ for graphic product...

    ATTN...WFO...AKQ...CTP...LWX...PHI...

    ATTN...RFC...RHA...NWC...

    LAT...LON 40877524 40677446 39917465 38557534 38087589=20
    38227669 39197671 40287619=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 7 17:58:48 2025
    AWUS01 KWNH 071757
    FFGMPD
    NYZ000-PAZ000-WVZ000-OHZ000-072355-

    Mesoscale Precipitation Discussion 0613
    NWS Weather Prediction Center College Park MD
    156 PM EDT Mon Jul 07 2025

    Areas affected...Parts of the Upper Ohio Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 071755Z - 072355Z

    SUMMARY...A few instances of flash flooding are possible this
    afternoon and evening across parts of the Upper Ohio Valley as
    scattered thunderstorms contain the potential for 2"/hr rates and
    may repeat over similar areas.

    DISCUSSION...Radar and satelitte observations this afternoon
    highlight a cold front working its way slowly east-southeastward
    along with an embedded low pressure area off the southwest shores
    of Lake Erie as of 1730Z. Mean layer flow is quick (25-30kts) and
    out of the southwest, leading to progressive storms along and
    ahead of the frontal boundary. However, these storms are oriented
    parallel to this flow, which supports the potential for repeating
    rounds of storms that may lead to rainfall amounts exceeding local
    FFG. PWs are greatest near and just ahead of the frontal boundary
    where the best convergence is located, with values in the 1.7-2.0"
    range and near the 90th climatological percentile per the 00z
    ECENS. Daytime heating has also created an unstable environment
    with SBCAPE values of 2500-3500 J/kg and should allow for the
    coverage of thunderstorms to further increase this afternoon along
    with increasing rainfall rates up to 2"/hr.

    Local FFG in the usually sensitive terrain of the Upper Ohio
    Valley and particularly western PA are around 1-2.5" per 1-hr and
    2-3" per 3-hr. Recent 12z HREF guidance shows 40-50% chances for
    exceeding 2" in 3-hr across northeast OH and northwest PA through
    21z, which is where forecaster confidence is also highest for a
    few instances of flash flooding due to repeating storms.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7_a9HpX4O7DKXZWugtjXY2yMbBicobxGSdcFJ7ab4b3Lu9vOn7m2qR2mul5LR6x3C3PM= H0WDsjj1x0ZguhnSWKtDlG4$ for graphic product...

    ATTN...WFO...BGM...BUF...CLE...CTP...PBZ...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 42527802 42357722 41737712 40957819 40427988=20
    40268119 40468206 40968240 41368201 41638087=20
    42007958=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 7 19:30:09 2025
    AWUS01 KWNH 071930
    FFGMPD
    TXZ000-080030-

    Mesoscale Precipitation Discussion 0614
    NWS Weather Prediction Center College Park MD
    329 PM EDT Mon Jul 07 2025

    Areas affected...Southern Big Country & Edwards Plateau of
    west-central Texas...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 071930Z - 080030Z

    SUMMARY...Clusters seeking out remaining unstable environment.=20
    Still remains capable of 2"/hr rates and scattered incidents of
    flash flooding remain likely for the next few hours.

    DISCUSSION...RADAR mosaic shows clusters of thunderstorms starting
    to shift west and southward as modest cold pools are supporting
    forward propagation/outflow boundaries. GOES-E Visible also shows
    congested confluent inflow bands responding to the thunderstorm
    clusters especially across Schleicher and Sutton counties while
    more traditional cu streets show solid inflow from the south
    across Edwards and W Kerr county. This is a signal of competing
    environments for thunderstorm activity through the evening.=20
    Inflow and increased insolation enhancing unstable environment
    exist west toward the eastern Pecos River Valley and W Concho
    Valley; while better deep layer moisture axis and upper-level
    outflow support exists eastward toward the I-35 corridor. Some low
    level drying combined with 700-300mb drying aloft noted in the
    CIRA LPW shows gradient of total PWats decreasing from 2" to 1.4"
    near the Pecos River, though MLCAPE axis of 2000-2500 J/kg
    connects from the Rio Grande Valley into the Pecos Valley. Aloft,
    the sheared 700-500mb axis remains very moist from the Hill
    country northeastward with best vorticity center remaining north
    of the current complex, likely maintaining the 15-20kts of
    southerly confluent inflow along the southwest edge of the
    complex. Entrance region to eastern side of larger scale ridge
    over northern Old Mexico into the Permian basin combined with
    approach of the Tropical Upper-Tropospheric Trough (TUTT) cell
    over the Gulf supports solid divergence/outflow aloft but east of
    the best low level forcing.=20=20

    As such, convection is likely to continue to propagate along the
    outflow and into the southerly inflow and unstable environment.=20
    This will maintain some stronger cells but likely with drier air
    ingestion, will limit rainfall efficiency (espcially compared to
    prior days or even this morning) as well as still encouraging
    forward propagation limiting overall totals. Still rates up to
    2"/hr and localized spots of 2-4" remain possible especially given
    increased probability of colliding outflows and storm scale
    interactions including cell mergers. In these very isolated
    incidents, focused/localized flash flooding will still be likely,
    but those incidents should be reducing with time toward 00z given
    increasing disconnect between best forcing elements.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5dwlZjIU2ReKfU4dHqG4642MpY5LWm_7bfSPFDsWm0U-Xr0O7Ooi_vnS0ViZ62Si1n5X= KYWHF25VgrYssLegsB_sVfQ$ for graphic product...

    ATTN...WFO...EWX...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32599955 32289951 31039952 29680007 29640096=20
    29950156 30530178 31300165 31780128 32060093=20
    32500005=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 7 23:11:40 2025
    AWUS01 KWNH 072311
    FFGMPD
    PAZ000-MDZ000-WVZ000-OHZ000-KYZ000-080400-

    Mesoscale Precipitation Discussion 0615
    NWS Weather Prediction Center College Park MD
    710 PM EDT Mon Jul 07 2025

    Areas affected...Southeastern OH...Western & Northern
    WV...Southwest PA...Western MD...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 072310Z - 080400Z

    SUMMARY...Favorable orientation for some short-term training
    moving through rugged terrain/low FFG. Rates of 1.5-2"/hr and
    localized totals to 2-3" pose possible localized incidents of
    flash flooding through early overnight.

    DISCUSSION...Long-term Visible loop shows a corridor of agitated
    Cu field that narrowed into a linear feature that is shaped like
    an older outflow boundary and connects back up to the main frontal
    convection across western PA. As stronger moisture convergence
    near a weak surface wave in southwest OH has matured into a larger
    cluster of stronger cells with embedded rates of 1.5-2"/hr given
    ample available moisture. Surface Tds into the low 70s and
    enhanced low level confluent flow through the Ohio Valley noted in
    CIRA LPW, has resulted in total PWats in near or just below 2" and
    with solid 20kt inflow and modest but sufficient divergence aloft
    at the far periphery of the right entrance of 30-50kt upper level
    jet (solid ageostrophic response).

    Cells are likely to remain fairly organized with about 25kt of
    effective bulk shear. Fairly deep unidirectional flow through the
    steering level is parallel to the bow westward of this apparent
    older boundary like feature. As such, there is enough convective
    development to suggest a few hours of repeating/training potential
    even with some progressive nature to the convection (20-25kts of
    mean flow). Additionally, propagation vectors appear to be weak
    and along flow regime, but some outflow boundaries may still kick
    ideal training axis a bit south probably to some benefit to reduce
    higher overall totals.

    As such, the potential for a streak or two of 2-3" totals are
    probable. Given overall FFG values are naturally lower in fairly
    rugged/narrow valley orography of SE OH into WV/SW PA; exceedance
    is possible suggesting localized incidents of flash flooding.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7VDXJ1jvOYo8O751Ka04u0LxM3uxEAtCNrEi47doDqoWmrhAoVQBA8QTFqGDK5HTXDF_= IF2-WEFSqx0I85T48AQBlXg$ for graphic product...

    ATTN...WFO...CTP...ILN...LWX...PBZ...RLX...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 40847823 40477739 39687814 38608135 38378248=20
    38668314 39368302 39858189=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 7 23:43:11 2025
    AWUS01 KWNH 072343
    FFGMPD
    TNZ000-KYZ000-ILZ000-MOZ000-080500-

    Mesoscale Precipitation Discussion 0616
    NWS Weather Prediction Center College Park MD
    742 PM EDT Mon Jul 07 2025

    Areas affected...Western Kentucky...Northwest Tennessee...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 072345Z - 080500Z

    SUMMARY...Broader overturning along/southeast of outflow
    boundaries may support short-term repeating/training & possible
    mergers allowing for localized 2-4" totals and possible flash
    flooding into early overnight period.

    DISCUSSION...GOES-E Vis/EIR and RADAR animation depicts a mature
    convective complex with strong outflow boundary crossing southeast
    MO. Stronger deep layer convergence across a moderately unstable
    environment with 2000-2500 J/kg of MLCAPE has resulted in a few
    bands of stronger/broader convective overturning of the unstable
    air across Southwest KY and Northwest TN. Visible loops show
    cells have oriented along some older either confluence or outflow
    boundaries that extend eastward generally parallel to deeper layer
    steering flow. Aloft, there is a col in upper-level flow as the
    far northern periphery of the Tropical Upper-Tropospheric Trough
    (TUTT) cell that can be seen over the northwest Gulf south of LA
    with edge over N MS, while northern stream shortwave cross MO,
    with entrance to polar jet in the vicinity. This has maximized
    upper-level divergence in W KY/NW TN to further aid convective
    organization.=20

    Deep layer confluence into the northern stream through the Lower
    Ohio Valley has maximized total PWat values over 2", perhaps
    nearing 2.25". This will make cells very efficient with deep warm
    cloud processes supporting 2-2.5"/hr rates (with an isolated 3"/hr
    spot possible). Given deep layer flow into the northern stream is
    also fairly parallel to the aforementioned confluence boundary and
    slowly sagging cold front crossing the Ohio River; some repeating
    and training is possible over the next few hours. That increased
    duration may support some streaks of 2-4" totals in less than
    3hrs. Given FFG values of 2-3"/3hrs across the area, this
    suggests localized flash flooding is considered possible.=20=20
    Convection should wane with loss of daytime heating and
    overturning of the unstable air, but may still intersect remaining
    untapped unstable air eastward, but overall trends should slowly
    diminish after dark.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9iYO8hfpUaXS4snmiOwhNV-Z_sYnu2KoinrE6r-3d47E3mPyoRpJVKawnvngE4SEKV6K= 3IXWLH8j1oBjCKus0Y_YZ0A$ for graphic product...

    ATTN...WFO...LMK...MEG...OHX...PAH...

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 37538612 37148574 36718575 36408604 36148661=20
    35908809 35858892 36128940 36468938 36838891=20
    37108843 37498702=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 8 00:06:43 2025
    AWUS01 KWNH 080006
    FFGMPD
    IAZ000-NEZ000-SDZ000-080600-

    Mesoscale Precipitation Discussion 0617
    NWS Weather Prediction Center College Park MD
    806 PM EDT Mon Jul 07 2025

    Areas affected...Eastern NEB...Western IA...Far Southeast SD...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 080005Z - 080600Z

    SUMMARY...Merging clusters of severe weather and increasing
    mositure flux pose short-term intense bursts of heavy rainfall and
    localized totals of 2-3.5" and possible flash flooding.

    DISCUSSION...Regional RADAR mosaic and GOES-E Visible imagery show
    a large cluster of thunderstorms at the base of northern stream
    shortwave trough crossing the Red River of the North where surface
    warm front has lifted across the Missouri River Valley slowly
    today. Southerly low level winds of 850mb have been steadily
    increasing moisture return with Tds in the upper 60s and lower
    70s. While mid-level moisture is enahnced across the 700-500mb
    layer at this intersection of the northern stream trof and the
    returning moisture. As such, total Pwats are increasing to 1.75"
    and strong convective clusters with severe winds/hail are going to
    increase in rainfall efficiency over the next few hours.

    However, in the short-term some cells that have developed on the
    southerly WAA in northeast NEB continue to lift north and will
    start to merge with the southeastward cluster. This merger will
    rapidly enhanced rainfall rates to over 2"/hr and may slow the
    fairly progressive southeastward push of the overall system.=20
    Isolated spots of 3"/hr while uncommon, may result and may quickly
    overwhelm any soil condition; dry/wet or normal.

    However, deep layer steering and cold pool generation will quickly
    overcome that initial intersection and track/repeat southeastward
    likely limiting overall totals thereafter, especially further
    north and east within the overall complex. Though in the wake of
    the cluster, low level jet flow will remain out of the south an
    increase to 20-25kts and with some further veering may allow for
    further isentropic development along the flanking line. As such,
    upwind redevelopment will have the potential for training allowing
    for spots of 2-3.5" to occur, likely across northeat NEB just east
    of the Sand Hills over areas of FFG values of 1.5-2"/hr and
    2-2.5"/3hrs. As such, incidents of flash flooding may be possible
    along the flanking line through the early overnight period toward
    06z.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7DaC-9TeZrNxh5SYyWEbYO7L_7VfLJnKplVtaTbO7d7ymnYRmtTOUX7NjBT2X9liQ4P0= F_QMYTuBMAqF05MGFElxfRc$ for graphic product...

    ATTN...WFO...DMX...FSD...GID...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43519732 43299628 42679539 41899478 41229523=20
    40909629 40939748 41549807 42519825 43049815=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 8 09:36:47 2025
    AWUS01 KWNH 080936
    FFGMPD
    ARZ000-OKZ000-081500-

    Mesoscale Precipitation Discussion 0618
    NWS Weather Prediction Center College Park MD
    535 AM EDT Tue Jul 08 2025

    Areas affected...eastern OK into western AR

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 080933Z - 081500Z

    SUMMARY...Isolated flash flooding will be possible from parts of
    eastern OK into western AR through the morning hours. Hourly
    rainfall of 2 to 3+ inches and isolated totals in excess of 5
    inches will be possible through 16Z.

    DISCUSSION...GOES East infrared and area radar imagery showed the
    early stages of a few showers/thunderstorms forming over eastern
    OK as of 09Z. Water vapor imagery showed a mid-level shortwave
    advancing across northeastern OK, moving into an airmass that was
    partially capped but anomalously moist and weakly unstable (PWs
    near 2 inches and MLCAPE of 500 to just over 1000 J/kg via 08Z SPC
    mesoanalysis data). In addition, the flow aloft was diffluent
    between the sub-tropical jet to the north and a strong upper ridge
    centered over far northwestern Mexico.

    Over the past few hours, 925-850 mb VAD winds and RAP data showed
    a minor increase in low level moisture transport into the region
    from the SW, which should help to further reduce weak low level
    convective inhibition noted on RAP analysis soundings over eastern
    OK. A continued increase in the coverage and intensity of
    showers/thunderstorms is expected over the next 1-3 hours over
    eastern OK and portions of western AR as the shortwave trough
    continues to advance and low level CIN continues to erode.
    Steering flow for storm motions is fairly weak (~10 kt) and some
    brief training will be possible with cell motions generally moving
    from west to east. Due to the high moisture environment, rainfall
    rates of 2 to 3 inches (perhaps higher) will be possible along
    with 30 minute rainfall of 1-2 inches. While recent HRRR/RRFS runs
    have not been matching current radar trends, older HRRR and 00Z
    HREF members were doing better and indicate the potential for
    locally high rainfall totals (40 percent HREF probs for 3+ inches
    and 30 percent HREF probs for 5+ inches through 18Z).

    Given relatively low rainfall anomalies across the region over the
    past 2 weeks, FFG values are on the high side for the region with
    3 to 5 inches per 3 hours. Therefore, any instances of flash
    flooding are expected to remain isolated and more likely across
    any urban areas and/or typical flood prone regions of the Ouachita
    Mountains into the Ozark Plateau.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_vlLS1YZ29St9tPCQtjB0nrBrUaEl2KLMtN7W7AaI_ro8QQn8gN5s0Nr-MEcvAtYCseG= VxaDgM-wjPffcrGcvHGvT7Y$ for graphic product...

    ATTN...WFO...LZK...OUN...SHV...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 36499467 36279360 35819293 35199260 34419279=20
    34019385 34049540 34989657 35919588=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 8 14:23:21 2025
    AWUS01 KWNH 081423
    FFGMPD
    MOZ000-ARZ000-OKZ000-082015-

    Mesoscale Precipitation Discussion 0619
    NWS Weather Prediction Center College Park MD
    1022 AM EDT Tue Jul 08 2025

    Areas affected...Eastern OK...Western/Northern AR...Southern MO

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 081422Z - 082015Z

    SUMMARY...Locally slow-moving clusters of heavy showers and
    thunderstorms will tend to increase in coverage going into the
    afternoon hours. High rainfall rates and slow cell-motions will
    likely yield isolated to scattered areas of flash flooding, which
    will include a concern for localloy significant/dangerous flash
    flooding impacts near ares of rugged terrain.

    DISCUSSION...The morning GOES-E IR satellite imagery shows a
    small-scale vort center drifting gradually east along the OK/AR
    border in close proximity to the Ozark Plateau. This energy is
    embedded in a very moist and unstable environment as evidenced by
    the 12Z KLIT RAOB sounding along with RAP analyses, and is already
    producing slow-moving clusters of very heavy showers and
    thunderstorms.

    Much of the convection is somewhat elevated in nature, but is
    embedded within MUCAPE values ranging from 1000 to 2000 J/kg, and
    with PWs that are near 2 inches. The activity is also seen locally
    backbuilding along the OK/AR border in an environment with
    relatively notable low-level moisture convergence.

    Some expansion of heavy shower and thunderstorm activity is
    expected over the next several hours as the diurnal heating cycle
    evolves and promotes more surface-based convection. The
    aforementioned vort energy will continue to be slow-moving going
    into the afternoon hours, but will be interacting with greater
    surface-based instability along with differential heating
    boundaries that will favor small-scale convergence zones/forcing
    for additional convective development.

    Corfidi vectors depict a strongly favorable environment for
    backbuilding convection over the next several hours, and with such
    a strongly moist and increasingly unstable airmass pooled across
    the region, there will be notable concerns for slow-moving showers
    and thunderstorms with very high rainfall rates.

    The last couple of runs of the HRRR guidance shows potential for
    rainfall rates to reach 2 to 3+ inches/hour, with locally some
    rainfall totals by mid-afternoon of as much as 3 to 6+ inches
    given the slow cell-motions. Some of the 06Z HREF guidance also
    supports similar rates and totals.

    While the antecedent conditions are very dry, and reflective of
    high FFG values, the very high rainfall rate potential and
    localized storm potential suggests an elevated flash flood threat.
    Some of these rains will also potentially be occurring over rugged
    terrain which suggests an enhanced threat for runoff potential.
    Therefore, going into the afternoon hours, at least isolated to
    scattered areas of flash flooding will be likely. Some concern
    will exist for locally significant/dangerous flash flooding
    impacts nears areas of rugged terrain.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8PTQ_j0pbGkv1j-KgwZsyRENdS5azpYxIijJs-9rbHAlwfIJjkigAaTCjJ6ZIV3pCLsM= aZkQf2HtZ95tf0LMDfFV14M$ for graphic product...

    ATTN...WFO...LSX...LZK...MEG...OUN...PAH...SGF...SHV...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 37559266 37559084 36808969 35609021 34559200=20
    33839433 34419578 35669604 36669506=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 8 14:35:48 2025
    AWUS01 KWNH 081435
    FFGMPD
    MOZ000-ARZ000-OKZ000-082015-

    Mesoscale Precipitation Discussion 0619
    NWS Weather Prediction Center College Park MD
    1034 AM EDT Tue Jul 08 2025

    Areas affected...Eastern OK...Western/Northern AR...Southern MO

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 081422Z - 082015Z

    SUMMARY...Locally slow-moving clusters of heavy showers and
    thunderstorms will tend to increase in coverage going into the
    afternoon hours. High rainfall rates and slow cell-motions will
    likely yield isolated to scattered areas of flash flooding, which
    will include a concern for locally significant/dangerous flash
    flooding impacts near areas of rugged terrain.

    DISCUSSION...The morning GOES-E IR satellite imagery shows a
    small-scale vort center drifting gradually east along the OK/AR
    border in close proximity to the Ozark Plateau. This energy is
    embedded in a very moist and unstable environment as evidenced by
    the 12Z KLIT RAOB sounding along with RAP analyses, and is already
    producing slow-moving clusters of very heavy showers and
    thunderstorms.

    Much of the convection is somewhat elevated in nature, but is
    embedded within MUCAPE values ranging from 1000 to 2000 J/kg, and
    with PWs that are near 2 inches. The activity is also seen locally
    backbuilding along the OK/AR border in an environment with
    relatively notable low-level moisture convergence.

    Some expansion of heavy shower and thunderstorm activity is
    expected over the next several hours as the diurnal heating cycle
    evolves and promotes more surface-based convection. The
    aforementioned vort energy will continue to be slow-moving going
    into the afternoon hours, but will be interacting with greater
    surface-based instability along with differential heating
    boundaries that will favor small-scale convergence zones/forcing
    for additional convective development.

    Corfidi vectors depict a strongly favorable environment for
    backbuilding convection over the next several hours, and with such
    a strongly moist and increasingly unstable airmass pooled across
    the region, there will be notable concerns for slow-moving showers
    and thunderstorms with very high rainfall rates.

    The last couple of runs of the HRRR guidance shows potential for
    rainfall rates to reach 2 to 3+ inches/hour, with locally some
    rainfall totals by mid-afternoon of as much as 3 to 6+ inches
    given the slow cell-motions. Some of the 06Z HREF guidance also
    supports similar rates and totals.

    While the antecedent conditions are very dry, and reflective of
    high FFG values, the very high rainfall rate potential and
    localized storm potential suggests an elevated flash flood threat.
    Some of these rains will also potentially be occurring over rugged
    terrain which suggests an enhanced threat for runoff potential.
    Therefore, going into the afternoon hours, at least isolated to
    scattered areas of flash flooding will be likely. Some concern
    will exist for locally significant/dangerous flash flooding
    impacts nears areas of rugged terrain.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_5AuXO6HH-ES1Xw2_pq5cgjZeyqvS55YdWf5pzbsrjYKUHAJ7lKNpDCmTmPU2VIJkOaB= xAqQzyuLKT1zZhEyVK9DAa0$ for graphic product...

    ATTN...WFO...LSX...LZK...MEG...OUN...PAH...SGF...SHV...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 37559266 37559084 36808969 35609021 34559200=20
    33839433 34419578 35669604 36669506=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 8 18:24:52 2025
    AWUS01 KWNH 081824
    FFGMPD
    NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-DCZ000-WVZ000-090000-

    Mesoscale Precipitation Discussion 0620
    NWS Weather Prediction Center College Park MD
    224 PM EDT Tue Jul 08 2025

    Areas affected...Mid-Atlantic States

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 081823Z - 090000Z

    Summary...Showers and thunderstorms will expand across the
    Mid-Atlantic ahead of a cold front through this evening. Rainfall
    rates at times could reach 3"/hr, which through repeating rounds
    could produce 1-3" of rain. Flash flooding is possible.

    Discussion...The regional radar mosaic this afternoon shows a
    rapid expansion of higher reflectivity associated with an
    increasing coverage of thunderstorms from West Virginia into
    eastern Pennsylvania. These thunderstorms are blossoming ahead of
    a cold front which is approaching from the west, with a weak
    shortwave noted in GOES-E WV imagery moving across central
    Pennsylvania as well. This area is additionally in the favorable
    RRQ of a modest jet streak pivoting over the Northeast, enhancing
    deep layer ascent. This lift is impinging into impressive
    thermodynamics with a ribbon of MLCAPE exceeding 2500 J/kg being
    drawn northward into the DelMarva and 2000 J/kg reaching into much
    of PA on 850mb inflow of 15-20 kts. which is also pushing elevated
    PWs of 1.8-1.9 inches into the region. The 12Z U/A sounding out of
    IAD also measured a WBZ level of nearly 14,000 feet, well above
    the 90th percentile and approaching the daily record. This all
    suggests an environment which will support efficient warm-rain
    processes today, and recent radar-estimated rain rates from KCCX
    have been above 1.5"/hr.

    As the aftn progresses and the front and the accompanying ascent
    push into the destabilizing environment, thunderstorms should
    become more widespread. The mean 0-6km wind will remain
    progressive at around 20 kts to the E/NE, suggesting cells will
    continue to track steadily to the east, but the presence of the
    shortwave aloft and modest 20 kts of bulk shear could force subtle
    organization into clusters. More problematic will be the rainfall
    rates, for which both the REFS and HREF suggest have a 20-40%
    chance of exceeding 2"/hr, and HRRR 15-min rainfall is as high as
    0.75" indicating brief 3+"/hr rates. Even if storms remain
    progressive, this could be problematic as these intense rates
    would overwhelm soils leading to runoff, especially in urban
    areas. However, in some locations repeating rounds may occur as
    well, leading to total rainfall that has a 15-25% chance of
    reaching 3" in some areas this evening.

    Additionally, soils across the area (using NASA SPoRT 0-10cm soil
    percentile as proxy) have saturation that is generally normal to
    well above normal from 7-day rainfall that has been as much as
    150-300% of normal. This has locally compromised 3-hr FFG to as
    low as 1.5"/3hrs, especially between Washington, D.C. and
    Philadelphia, with a secondary minimum near the Shenandoah Valley.
    Although these heavy rain rates could be problematic anywhere
    across the area through the evening, it is these more sensitive
    soils or urban areas that have the greatest risk for impacts.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_iGWa40FIUaXyZ66c26fMfW9QUtYKRzHrdFaJkfYLa_S6ATUWh1pWXL-ZBz7GizTVXvG= 1VnWsXdEkYsxhj_0ZL6zjRE$ for graphic product...

    ATTN...WFO...AKQ...BGM...CTP...LWX...PBZ...PHI...RLX...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 41137619 40997535 40627494 40027499 39597540=20
    39107581 38597611 38127634 37727668 37377725=20
    37187831 37277990 37888073 38298112 38678096=20
    38998038 39387942 39857856 40547766 41007701=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 8 19:18:55 2025
    AWUS01 KWNH 081918
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-090100-

    Mesoscale Precipitation Discussion 0621
    NWS Weather Prediction Center College Park MD
    318 PM EDT Tue Jul 08 2025

    Areas affected...Eastern Oklahoma, Central Arkansas, and the
    ArkLaTex

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 081917Z - 090100Z

    Summary...Showers and thunderstorms rapidly expanding across
    Arkansas and eastern Oklahoma will continue. Rainfall rates of
    2"/hr or more are likely, which through slow motions and brief
    organization into clusters will produce 2-3" of rain with locally
    higher amounts. Flash flooding is possible.

    Discussion...The GOES-E experimental day-cloud microphysics RGB
    this afternoon depicts rapid updraft growth into Cb across much of
    AR and eastern OK. These updrafts are intensifying into
    thunderstorms across much of the area, with a rapid expansion of
    accompanying reflectivity noted in the regional radar mosaic. An
    MCV is clearly indicated across NW AR dropping southward, with an
    accompanying outflow boundary (OFB) draped back into OK serving as
    another focus for convective growth. Low-level convergence along
    this OFB, with more broad 850-700mb convergence across the area,
    is helping to drive this ascent, especially beneath extremely
    diffluent upper level flow. Thermodynamics within this region of
    impressive ascent are supportive of heavy rain rates, with PWs
    exceeding 2 inches, around 1.5 standard deviations above normal,
    overlapping MLCAPE of 1500 J/kg. The overlap of the strong ascent
    into these thermodynamics are supporting the expanding convection,
    with rain rates estimated via KLZK WSR-88D as high as 2"/hr even
    in fresh convection.

    As the aftn progresses, it is likely that convection will continue
    to expand from eastern OK through much of AR and into far
    northeast TX. Although 0-6km bulk shear will remain minimal,
    indicating generally pulse type storms, the widespread development
    will likely force outflow interactions and storm mergers to
    support occasional clusters. Additionally, some locally enhanced
    organization is likely along the OFB and MCV as they pivot
    southward. With rain rates expected to peak above 2"/hr (30%
    chance on the HREF, 40% chance on the REFS), with 15-min rainfall
    above 1" possible (brief 4"/hr rates). Despite the modest
    organization, repeating rounds or where storms merge to briefly
    intensify, total rainfall of 2-3" with locally higher amounts is
    possible (40-60%).

    FFG across the area is generally elevated to 3-4"/3hrs, and
    although there are some pockets of lower FFG, soil infiltration
    capacity appears elevated. This indicates that much of this rain
    should be able to be absorbed. However, the intensity of the
    forecast rainfall rates could still quickly become runoff,
    especially in urban areas, or where multiple rounds occur (such
    that the first round saturates the top soils). Where this occurs,
    instances of flash flooding could occur as progged by REFS and
    HREF 3-hr FFG exceedance probabilities rising to 15-30%.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8YANOh8smMsaH8MxfrNVGrQB0y298ICeIbmZO6yW9_Rr1pc7Q1RheFSeEePAWZtsUsyN= 2QZenyxZ6zz2C44LlFJwpDs$ for graphic product...

    ATTN...WFO...FWD...JAN...LZK...OUN...SHV...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 36029710 35879658 35679596 35539504 35179368=20
    34959248 34679156 34089117 33359136 32879205=20
    32829334 33209500 33569575 34219646 35149707=20
    35409720 35809734=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 8 20:10:41 2025
    AWUS01 KWNH 082010
    FFGMPD
    ILZ000-MOZ000-090200-

    Mesoscale Precipitation Discussion 0622
    NWS Weather Prediction Center College Park MD
    409 PM EDT Tue Jul 08 2025

    Areas affected...Southern Missouri through Central Illinois

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 082009Z - 090200Z

    Summary...Showers and thunderstorms will steadly expand across
    Missouri and Illinois into the evening. Rainfall rates of 1-2"/hr
    are likely, which through training could produce 2-4" of rain with
    locally higher amounts. This will likely cause flash flooding.

    Discussion...The GOES-E IR imagery this afternoon shows rapid
    cloud-top cooling associated with a line of deepening convection
    from central Illinois through southwest Missouri, including the
    St. Louis vicinity. These thunderstorms are rapidly intensifying
    within an impressive overlap of ascent and thermodynamics. A
    shortwave is noted in WV imagery moving over central MO, while a
    surface wave and accompanying trough continue to dig southeast.
    Additionally, a belt of enhanced westerlies is noted at 300mb
    tracking overhead, providing additional, and locally enhanced,
    lift. This deep layer ascent is acting upon favorable
    thermodynamics with PWs above 1.75 inches and MLCAPE over 2000
    J/kg. A pronounced CAPE gradient exists from NW to SE along this
    surface trough, providing the focus for thunderstorms, within
    which radar-estimated rain rates have already surpassed 2"/hr.

    Confidence is increasing that the flash flood risk will rapidly
    increase during the next few hours. As the surface trough drops
    slowly southeast and the accompanying wave of low pressure skirts
    into IL, it will interact with even more robust thermodynamics.
    This will be due to generally modest 850mb inflow from the SW at
    10-15 kts impinging and converging into the low-level convergent boundary/instability gradient. At the same time, the narrow
    corridor of enhanced westerlies will maintain generally westerly
    0-6km mean winds to align to the surface boundary, while
    concurrently enhancing bulk shear to force better, although still
    modest, storm organization. At the same time, Corfidi vectors will
    remain parallel to the mean flow and surface trough, indicating a
    high likelihood of training as storms back build into the greater
    instability and then track along the boundary.

    Rain rates in excess of 1"/hr are likely (>70% chance), with
    2+"/hr possible (40% chance) as warm rain processes dominate
    thanks to warm cloud depths approaching 13,000 ft. While the most
    pronounced training may occur across MO, there is an enhanced
    rainfall risk into central IL as well as the surface wave moves
    into the area and provides a focus for some slow
    moving/regenerating cells. With these intense rain rates expected
    to continue, this could produce 2-4" of rain, with locally higher
    amounts above 5" forecast by 10-20% chance of exceedance on the
    HREF.

    The CAMs are in very good agreement with this evolution the next
    few hours as reflected by significant (20-40%) 1"/6hrs HREF EAS
    probabilities that include St. Louis, MO and Springfield, IL. The
    limiting factor to flash flood instances may be antecedent dryness
    and FFG that is generally 2-3"/3hrs. However, both the HREF and
    REFS indicate a 30-40% chance of exceedance, and the urban areas
    are even more vulnerable, so instances of flash flooding are
    likely as cells train through the evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6uGQs6jPzlHWQaS4AjsZR_FaLzv5bChrINCfKAmwYKF0ZXvrNgmPbbWf2rsHWDpXk2yd= j89Bl1pK4i-U_e2ho4WPk_k$ for graphic product...

    ATTN...WFO...EAX...ILX...LOT...LSX...SGF...

    ATTN...RFC...KRF...MSR...ORN...TIR...TUA...NWC...

    LAT...LON 41148872 40728810 39968796 39208838 38448945=20
    37729087 37379241 37279334 37289406 37499450=20
    37849435 38229327 39119198 40009049 40898930=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 8 20:16:27 2025
    AWUS01 KWNH 082015
    FFGMPD
    ILZ000-MOZ000-090200-

    Mesoscale Precipitation Discussion 0622...Corrected
    NWS Weather Prediction Center College Park MD
    415 PM EDT Tue Jul 08 2025

    Corrected for Graphic

    Areas affected...Southern Missouri through Central Illinois

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 082009Z - 090200Z

    Summary...Showers and thunderstorms will steadly expand across
    Missouri and Illinois into the evening. Rainfall rates of 1-2"/hr
    are likely, which through training could produce 2-4" of rain with
    locally higher amounts. This will likely cause flash flooding.

    Discussion...The GOES-E IR imagery this afternoon shows rapid
    cloud-top cooling associated with a line of deepening convection
    from central Illinois through southwest Missouri, including the
    St. Louis vicinity. These thunderstorms are rapidly intensifying
    within an impressive overlap of ascent and thermodynamics. A
    shortwave is noted in WV imagery moving over central MO, while a
    surface wave and accompanying trough continue to dig southeast.
    Additionally, a belt of enhanced westerlies is noted at 300mb
    tracking overhead, providing additional, and locally enhanced,
    lift. This deep layer ascent is acting upon favorable
    thermodynamics with PWs above 1.75 inches and MLCAPE over 2000
    J/kg. A pronounced CAPE gradient exists from NW to SE along this
    surface trough, providing the focus for thunderstorms, within
    which radar-estimated rain rates have already surpassed 2"/hr.

    Confidence is increasing that the flash flood risk will rapidly
    increase during the next few hours. As the surface trough drops
    slowly southeast and the accompanying wave of low pressure skirts
    into IL, it will interact with even more robust thermodynamics.
    This will be due to generally modest 850mb inflow from the SW at
    10-15 kts impinging and converging into the low-level convergent boundary/instability gradient. At the same time, the narrow
    corridor of enhanced westerlies will maintain generally westerly
    0-6km mean winds to align to the surface boundary, while
    concurrently enhancing bulk shear to force better, although still
    modest, storm organization. At the same time, Corfidi vectors will
    remain parallel to the mean flow and surface trough, indicating a
    high likelihood of training as storms back build into the greater
    instability and then track along the boundary.

    Rain rates in excess of 1"/hr are likely (>70% chance), with
    2+"/hr possible (40% chance) as warm rain processes dominate
    thanks to warm cloud depths approaching 13,000 ft. While the most
    pronounced training may occur across MO, there is an enhanced
    rainfall risk into central IL as well as the surface wave moves
    into the area and provides a focus for some slow
    moving/regenerating cells. With these intense rain rates expected
    to continue, this could produce 2-4" of rain, with locally higher
    amounts above 5" forecast by 10-20% chance of exceedance on the
    HREF.

    The CAMs are in very good agreement with this evolution the next
    few hours as reflected by significant (20-40%) 1"/6hrs HREF EAS
    probabilities that include St. Louis, MO and Springfield, IL. The
    limiting factor to flash flood instances may be antecedent dryness
    and FFG that is generally 2-3"/3hrs. However, both the HREF and
    REFS indicate a 30-40% chance of exceedance, and the urban areas
    are even more vulnerable, so instances of flash flooding are
    likely as cells train through the evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6-c-V9g61S8pWuciJPkWcCV0uuHqMbUY8dyFBgJgY7LIldR_fdZUVUszydZ9DpOscenk= f2pOe2qgHJrsbyAI1uf48ks$ for graphic product...

    ATTN...WFO...EAX...ILX...LOT...LSX...SGF...

    ATTN...RFC...KRF...MSR...ORN...TIR...TUA...NWC...

    LAT...LON 41148872 40728810 39968796 39208838 38448945=20
    37729087 37379241 37279334 37289406 37499450=20
    37849435 38229327 39119198 40009049 40898930=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 8 21:21:34 2025
    AWUS01 KWNH 082120
    FFGMPD
    MAZ000-RIZ000-CTZ000-NYZ000-NJZ000-PAZ000-DEZ000-MDZ000-090300-

    Mesoscale Precipitation Discussion 0623
    NWS Weather Prediction Center College Park MD
    519 PM EDT Tue Jul 08 2025

    Areas affected...Eastern PA and DE northeast into Southern New
    England

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 082118Z - 090300Z

    Summary...Convection blossoming along a southward advancing cold
    front will exhibit short term training of 2-3"/hr rain rates. This
    could produce 1-3" of rainfall with locally higher amounts. Flash
    flooding is possible, especially within urban areas.

    Discussion...The regional radar mosaic this afternoon shows
    clusters of thunderstorms advancing eastward along and ahead of a
    cold front. This cold front is dropping slowly southward in
    response to height falls downstream of an approaching trough axis
    centered near the Great Lakes, with weak vorticity impulses
    embedded within the flow. As the front becomes strung out more
    west-east this evening, it will likely slow, continuing to be the
    impetus for thunderstorm development as it moves into a more
    robust thermodynamic airmass.

    PWs across the area are 2-2.2 inches according to the SPC RAP
    analysis, which is well above the 90th percentile and nearing
    daily records. The accompanying instability is equally impressive,
    with a narrow ribbon of 3000 J/kg SBCAPE emerging from the
    DelMarVa northward into southern CT and RI. This CAPE is
    characterized of the "tall skinny" variety as well as reflected by
    normalize dCAPE values of just 0.1 to 0.15, indicating moist
    adiabatic lapse rates through a deep column suggestive of an
    efficient rainfall environment. Thunderstorms that have already
    developed across the area have radar-estimated rain rates of more
    than 2"/hr according to KDIX, with FFWs already in effect across
    eastern PA.

    During the next few hours, the CAMs are in relatively good
    agreement that showers and thunderstorms will expand and spread
    eastward into the Tri-State area of NJ/NY/CT immediately
    downstream of the cold front. As the front aligns generally west
    to east, mean 0-6km winds of 15-20 kts parallel to the front
    combined with bulk shear increasing to 20-25 kts suggest storms
    will organize into clusters and repeatedly track/train along this
    front and the attendant instability gradient. With rainfall rates
    potentially ereaching 2-3"/hr at times (20-40% chance), leading to
    1-hr rainfall that could be up to 1.5-2.0 inches according to HREF
    and REFS PMM, any short term training or repeating could produce
    1-3" of rain with locally higher amounts possible.

    FFG across the area is generally 2-3"/3hrs, for which the HREF
    indicates has a low probability (10-15%) chance of exceedance.
    However, urban areas will likely need much lower rainfall to cause
    rapid runoff where 1-hr FFG is only around 1 inch. Additionally,
    the low-level SW flow could force some locally enhanced
    convergence/training, especially from northeast NJ, across Long
    Island, and into southern CT where FFG exceedances peak. This
    indicates that the greatest risk for flash flooding will be in
    this vicinity this evening, but anywhere short-term training of
    these intense rain rates can occur, impacts are possible.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9HbK1YMmEK91UQyWC_rUHETZhkv9EQKfcI7e72A-TkhKWu-WkxMiJqFbvLCU7NH5Ploz= aRUUcYpaGtMlgHMbc-QSUzI$ for graphic product...

    ATTN...WFO...AKQ...ALY...BGM...BOX...CTP...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 42257332 42257234 42217137 42037070 41797041=20
    41497061 40957191 40857222 40607284 40257346=20
    39857383 39537416 39027463 38527517 38447556=20
    38877591 40027610 40627639 41257647 41677621=20
    42087475=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 8 23:58:34 2025
    AWUS01 KWNH 082357
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-090530-

    Mesoscale Precipitation Discussion 0624
    NWS Weather Prediction Center College Park MD
    757 PM EDT Tue Jul 08 2025

    Areas affected...Southeast Oklahoma, The ArkLaTex, North Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 082356Z - 090530Z

    Summary...Showers and thunderstorms will expand across the
    ArkLaTex and North Texas through the evening. Rainfall rates of
    2-3"/hr are likely within deeper convection, leading to 2-3" of
    rain with locally higher amounts. Flash flooding is possible.

    Discussion...The regional radar mosaic this afternoon shows two
    outflow boundaries (OFB) draped in the vicinity of the ArkLaTex.
    One is moving south along the Red River Valley, while a second OFB
    lifts slowly northward across eastern Texas. Aloft, a shortwave is
    noted in WV imagery drifting south across Oklahoma, while
    impressive upper divergence pivots overhead to additionally
    enhance ascent. Across this region, PWs above 2.2 inches exist in
    a ribbon oriented SW to NE, collocated with a corridor of MLCAPE
    above 2500 J/kg. Convection forming along these OFBs is already
    producing radar-estimated rain rates of 1.5+"/hr according to KSHV.

    During the next few hours, it is likely that these OFBs will
    collide. The interaction of these boundaries will occur into the
    core of the most impressive thermodynamics, and beneath the most
    aggressive upper divergence, suggesting rapid convective growth
    along the convergence axis. The CAMs, while differing in exact
    timing and placement of this collision, all indicate an
    intensifying west-to-east oriented swath of convection during this
    collision, providing higher confidence in the evolution. With
    robust thermodynamics in place, this intense ascent will result in
    strong updrafts which could support rainfall rates of 2-3"/hr as
    forecast by HREF neighborhood probabilities for 2"/hr reaching
    40%. These thunderstorms will also likely move very slowly as
    0-6km mean winds are just 5-10 kts, with modest bulk shear of
    around 20 kts marginally supporting convective clusters. Where
    these develop, they may train from west to east along the
    boundary, at least briefly, lengthening the duration to produce an
    axis of 2-3" of rain with locally higher amounts approaching 5"
    possible.

    This area has been dry recently, which is reflected by FFG as much
    as 3-4"/3hrs, except SW of the Dallas metro and west of I-35 where
    FFG is considerably lower. The HREF exceedance probabilities for
    this FFG peak only around 20%, suggesting the flash flood risk
    will be generally isolated through the evening. However, with slow
    moving storms containing these intense rain rates, and the
    increasing potential for some upwind propagation along the
    colliding boundaries to slow the net motions, soils could be
    locally overwhelmed, especially in urban areas or atop the locally
    more saturated areas, leading to instances of flash flooding.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5bjdRDg3lqI9RtBnaIN5Dft3ch67ZuxT7Arhvrut15vjvz9OSiooc9u9zQMEtdtXv8Wj= q33Z3MI57U97nUQZAsZKMRQ$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...SJT...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 34419463 34339328 34039251 33339225 32749261=20
    32249344 31849481 31619622 31419741 31499874=20
    31849882 33239777 34369636=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jul 9 00:33:32 2025
    AWUS01 KWNH 090032
    FFGMPD
    DEZ000-MDZ000-VAZ000-WVZ000-090530-

    Mesoscale Precipitation Discussion 0625
    NWS Weather Prediction Center College Park MD
    831 PM EDT Tue Jul 08 2025

    Areas affected...Much of Virginia into the DelMarVa

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 090030Z - 090530Z

    Summary...Showers and thunderstorms will expand in coverage and
    gradually shift southeast through the evening. Rainfall rates of
    1-2"/hr are expected, which through training could produce 2-3" of
    rainfall. Flash flooding is possible.

    Discussion...The regional radar mosaic early this evening shows an
    uptick in convective development from SW Virginia through the
    Tidewater Region. Above this developing convection, IR satellite
    imagery indicates an expansion of cloud tops falling below -50C,
    indicatative of the continued strengthening thunderstorms. This
    convection is blossoming in response to ascent driven by low-level
    convergence along a surface trough, weak isentropic lift as the
    modest 850mb LLJ surges northeast, and modest upper diffluence
    within the tail of jet streak centered over New England. This
    pronounced lift is acting upon rich thermodynamics created via PWs
    measured by the SPC RAP analysis of 1.9 to 2.1 inches, well above
    the 90th percentile for the date, collocated with a plume of
    MLCAPE exceeding 2500 J/kg.

    During the next few hours, this trough should pivot slowly
    southeast, continuing to provide the needed ascent for
    thunderstorm development despite the wane of daytime instability
    combined with convective overturning. The continued convection
    will be additionally supported by a subtle increase in the LLJ
    (reaching as high as 20 kts) to provide persistent isentropic
    ascent and thermodynamic resupply thanks to MUCAPE remaining above
    1000 J/kg. This LLJ at 850mb is additionally progged to veer to be
    more aligned to the boundary, supporting enhanced training as
    storms develop in the next few hours. Although there continues to
    be some disagreement in the CAMs about the timing and spatial
    extent of convection through the evening, with rain rates forecast
    via HREF neighborhood probabilities to have a 60% (30%) chance of
    exceeding 1"/hr (2"/hr), any training could produce 2-3" of rain
    with locally higher amounts.

    Any location that receives training of these intense rain rates
    this evening could experience runoff capable of producing flash
    flooding. The greatest risk, however, appears to be generally from
    Richmond east to the coast where 0-10cm soil moisture from NASA
    SPoRT is above the 95th percentile and 1-hr FFG is locally as low
    as 1". Additionally the enhanced instability in the vicinity of
    the warm waters of the Chesapeake Bay could enhance any convection
    as well as the potential for regenerative and repeating cells.
    Although the risk should wane nocturnally, at least for the next
    few hours flash flooding will remain a threat across this area.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ZK0Y3jwGBWWbPYaO-agBK4kMalvJRkWti0MSZCVtGZwXrzZd_pyr2yHX2D9j_sf59UP= rCzoT0UsYPC5mICba8pW2kU$ for graphic product...

    ATTN...WFO...AKQ...LWX...PHI...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 38627659 38507513 37937503 37267543 36787678=20
    36577880 36588054 36918121 37478056 37977885=20
    38427742=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jul 9 05:48:57 2025
    AWUS01 KWNH 090548
    FFGMPD
    MDZ000-VAZ000-NCZ000-091015-

    Mesoscale Precipitation Discussion 0626
    NWS Weather Prediction Center College Park MD
    148 AM EDT Wed Jul 09 2025

    Areas affected...central to southeastern VA into southern DelMarVa
    Peninsula

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 090547Z - 091015Z

    Summary...A threat of flash flooding will continue across portions
    of central to southeastern VA and possibly into the southern
    DelMarVa Peninsula through 09-10Z. Rainfall rates of 1-2 in/hr
    (locally higher possible) and additional totals of 2-4 inches are
    expected.

    Discussion...Local radar imagery at 0520Z showed a region of
    thunderstorms extending west-east from central VA to just west of
    the Chesapeake Bay. MRMS has been matching local gauge reports
    fairly well over the past 2-3 hours in showing peak hourly
    rainfall totals in the 1-2 inch range. An outflow boundary was
    noted to be pushing south of the Richmond/Petersburg metro but
    additional storms to the west were likely being aided via a
    southwesterly axis of low level moisture feeding directly into the
    region at 20 kt/isentropic ascent, beneath weakly diffluent flow
    aloft. MLCAPE trends have come down significantly over the past 3
    hours with 05Z SPC mesoanalysis data showing less than 500 J/kg
    MLCAPE in place over most of VA. However, relatively steep lapse
    rates in the 850-700 mb layer (6.5-7.5 C/km) were contributing to
    elevated instability of up to 1000 J/kg across much of the region.

    Thunderstorms are expected to continue advancing east over the
    next few hours but with some southward translation due to cold
    pools and propagation into the inflow. While weakening of
    convective intensity is anticipated overall by 09/10Z, flash flood
    potential will continue to linger from 1-2 in/hr rainfall rates
    (locally higher possible) and the potential for an additional 2-4
    inches over the next 3-5 hours. If storms are able to survive,
    they will bring potential flash flood impacts to the
    Hampton/Norfolk/Virginia Beach regions of southeastern VA,
    although recent available hires models do not support storms
    maintaining significant intensity that far east.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!43rCDZxSRadQiVddtwu4KIstwZRB3IYROes-WevDbGzQChxIEay7gY-cgAuVITE-rQml= vHuuZGsPxL1mjB36sHezsT8$ for graphic product...

    ATTN...WFO...AKQ...RNK...

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 38137536 37817510 37257534 36547584 36507701=20
    36637865 37227873 37637750=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jul 9 15:22:18 2025
    AWUS01 KWNH 091521
    FFGMPD
    PAZ000-MDZ000-VAZ000-NCZ000-WVZ000-OHZ000-TNZ000-KYZ000-092120-

    Mesoscale Precipitation Discussion 0627
    NWS Weather Prediction Center College Park MD
    1120 AM EDT Wed Jul 09 2025

    Areas affected...Upper OH Valley...Central Appalachians/Blue Ridge

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 091520Z - 092120Z

    SUMMARY...Developing showers and thunderstorms will be expanding
    in coverage going through the afternoon hours. High rainfall rates
    are expected to drive a likelihood for at least scattered areas of
    flash flooding.

    DISCUSSION...The late-morning GOES-E satellite imagery shows an
    elongated shortwave trough gradually transiting the OH Valley
    which will be interacting with a moist and increasingly unstable
    airmass pooled across the region, and this will set the stage for
    developing and expanding clusters of heavy showers and
    thunderstorms going through the early to mid-afternoon hours.
    Already the latest radar imagery shows a few small-scale clusters
    of showers and thunderstorms developing over eastern KY, southeast
    OH and central WV.

    MLCAPE values have already increased to 1000 to 1500 J/kg with the
    aid of morning solar insolation, and PWs of 1.5 to 1.75+ are in
    place which are about 1.5 to 2 standard deviations above normal.
    Some gradually increasing mid-level west-southwesterly flow will
    promote some uptick in shear parameters over the next several
    hours with effective bulk shear rising to about 25 to 35+ kts.

    These environmental trends should be conducive for seeing bands of
    multi-cell convection which will tend to be expanding in coverage
    with the aid of differential heating boundaries and orographics,
    with cell-motions gradually off to the east that will include far
    eastern KY, southeast OH, and much of WV initially. By
    mid-afternoon, this activity should then advance or develop across
    adjacent areas of the MD/WV Panhandles, western VA and also
    northwest NC involving the Blue Ridge and portions of the
    Mid-Atlantic Piedmont.

    The anomalous PW environment alone will favor high rainfall rates
    that may reach as high as 1 to 2 inches/hour which is strongly
    favored by the 12Z HREF guidance, but there will potentially be
    some orographic/terrain-induced forcing that may elevate these
    rates a bit further. This will especially be the case by
    mid-afternoon for areas over the central Appalachians and adjacent
    areas of the Blue Ridge involving MD/WV/VA.

    The 12Z HREF and 06Z REFS guidance collectively suggest some
    rainfall total potential by late-afternoon of 2 to 4+ inches.
    These rainfall amounts are likely to result in at least scattered
    areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!99ZAMRbadncOExsCxUOv9BBPH2KEQfOO6_ZA2Tn1ofAU_Igklhc--o8wfW6u5pSeXe2p= Eb7BDcvzUmWhuEL6B9yK7-I$ for graphic product...

    ATTN...WFO...AKQ...CTP...GSP...ILN...JKL...LWX...MRX...PBZ... RAH...RLX...RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 39927742 39767683 38867716 37537862 36607948=20
    35728092 35488223 35658290 36288278 36728273=20
    37718283 38878310 39578238 39778093 39757863=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jul 9 18:22:47 2025
    AWUS01 KWNH 091822
    FFGMPD
    LAZ000-TXZ000-100000-

    Mesoscale Precipitation Discussion 0628
    NWS Weather Prediction Center College Park MD
    221 PM EDT Wed Jul 09 2025

    Areas affected...Middle and Upper Texas Coast into Southwest
    Louisiana

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 091819Z - 100000Z

    Summary...Showers and thunderstorms will increase in coverage
    along the Middle and Upper Texas Coasts through the afternoon.
    Rainfall rates will intensify to 2-4"/hr, resulting in pockets of
    2-3" of rain with locally higher amounts. Flash flooding is
    possible.

    Discussion...The regional radar mosaic this afternoon shows
    rapidly expanding coverage of showers and thunderstorms across the
    Middle and Upper Texas coasts, with activity lifting slowly
    northward across the coastal plain. This activity is responding to
    extreme thermodynamics, as PWs sampled via GPS are 2.0-2.1 inches,
    which is around the 90th percentile for the area according to the
    SPC sounding climatology, paired with MLCAPE that is over 2000
    J/kg. Into these robust thermodynamics, forcing for ascent
    continues to maximize in response to a shortwave and accompanying
    strung out vorticity maxima drifting southward from North Texas,
    and impressive upper level divergence as the region is sandwiched
    between mid-level synoptic high pressure ridges. Additionally,
    light onshore low level flow is allowing the gulf breeze to push
    inland, functioning as an axis for convergence and storm
    development. The overlap of this ascent and moisture is driving
    rain rates which have been estimated via KHGX WSR-88D to be
    1.5"/hr, leading to MRMS measured rainfall above 1.5" in a few
    spots the past hour.

    The high-res CAMs are in general under-representing the current
    activity, although the ARW/ARW2 seem to have the best handle on
    the current situation. Despite that, all CAMs indicate rapid
    expansion of coverage during the next few hours, which indicates
    that showers and thunderstorms should become numerous to
    widespread, which is additionally supported by the favorable
    overlap of instability, moisture, and ascent. As storms become
    more numerous, mergers and collisions will become more likely as
    bulk shear remains minimal, with resulting interactions leading to
    rapid updraft development. In the anomalous environment, rainfall
    rates of more than 2"/hr are expected as forecast by HREF (REFS)
    neighborhood probabilities reaching 30% (50%), with brief rainfall
    rates of 4"/hr possible as reflected by HRRR 15-min rainfall
    peaking around 1". Mean 0-6km winds will remain light at just 5
    kts, which when combined with the pulse type storms indicates slow
    and chaotic motions that could result in 2-3" of rain with local
    amounts as much as 5" into the evening.

    0-40cm soil moisture from NASA SPoRT is saturated above the 95th
    percentile in many areas, resulting in FFG that is compromised,
    especially for this region, to as low as 2.5"/3hrs, and both the
    HREF and REFS probabilities indicate a medium change (30-60%) of
    exceedance. This suggests that despite a lack of organization,
    these intense rainfall rates, especially during slow and chaotic
    motions or across more urban areas, could create rapid runoff
    leading to instances of flash flooding.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8yy2sDn2ran2vWR6TZzzlIezAchrqa8YRkbVAi7Wifad3oi7-EcpvwM-R9lCu8xVVoyD= POhcj_ZdT_yE9IMZz4_vdGI$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...LCH...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 31539407 31349344 31029288 30779260 30479259=20
    30109274 29649358 29209446 29029476 28759525=20
    28389597 27859698 27779765 27979806 28249830=20
    28859819 29649771 30219709 31149578 31449491=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jul 9 18:52:38 2025
    AWUS01 KWNH 091852
    FFGMPD
    NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-NCZ000-DCZ000-WVZ000-100050-

    Mesoscale Precipitation Discussion 0629
    NWS Weather Prediction Center College Park MD
    250 PM EDT Wed Jul 09 2025

    Areas affected...Mid-Atlantic States

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 091850Z - 100050Z

    SUMMARY...Heavy showers and thunderstorms will evolve across much
    of the Mid-Atlantic region going into the evening hours.
    Relatively wet antecedent conditions coupled with high rainfall
    rates and some cell-training concerns will drive an elevated flash
    flooding risk, with potential for locally significant and
    dangerous urban flash flooding.

    DISCUSSION...The latest GOES-E IR satellite imagery shows an
    expansive area of cooling convective tops associated with heavy
    showers and thunderstorms across the central Appalachians which
    are gradually advancing off to the east as an upstream shortwave
    trough over the OH Valley encroaches upon the region.

    The airmass downstream over a large portion of the Mid-Atlantic
    region is moderate to strongly unstable with MLCAPE values of 1500
    to 3000+ J/kg noted east of the Blue Ridge and extending toward
    the broader Chesapeake Bay region including portions of the
    Delmarva. A very moist environment is in place with PWs of 1.75 to
    2 inches, which includes a 1.82 inch PW in the 12Z IAD RAOB
    sounding. These PWs are on the order of 1.5 to 2 standard
    deviations above normal.

    This very favorable thermodynamic environment is going to combine
    with a gradually increasing level of deeper layer shear over the
    next several hours as stronger mid-level west-southwest flow
    arrives ahead of the upstream shortwave. In fact, at least for the
    central and and northern Mid-Atlantic, including northern VA and
    central MD east through the northern Delmarva, southeast PA and
    southern NJ, there will be as much as 30 to 40 kts of effective
    bulk shear.

    This will promote numerous areas of multi-cell and perhaps some
    localized supercell thunderstorm activity near and east of the
    Blue Ridge, and extending through the greater Chesapeake Bay
    region going through the remainder of the afternoon and early
    evening hours.

    High rainfall rates are expected given the organized nature of the
    convective threat along with the very moist and unstable
    environment. The latest hires CAM guidance supports rainfall rates
    of locally as high as 1.5 to 2.5 inches/hour with the stronger
    cells. The convective evolution in time should take on a more progressive/linear mode, but as this occurs there may be some
    localized corridors of cell-training. This will yield locally
    higher-end rainfall potential with some spotty storm totals of 3
    to 5 inches not out of the question. This is supported by the 12Z
    HREF and 06Z REFS guidance.

    This rainfall potential over the next several hours coupled with
    generally wet antecedent conditions and the highly sensitive urban
    areas of the Mid-Atlantic, including the I-81, I-64 and I-95
    corridors from southwest to northern VA, central MD and southeast
    PA, will favor an elevated risk of flash flooding. This will
    include concerns for locally significant and dangerous urban flash
    flooding for several major metropolitan areas.

    Orrison/Shieh

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_4kcZPVj-I0_f-v_rTRNV3b2DymOIUUkcbGXZZwkJGIBLmOWjQ868V4UFtFnlp7fzGxr= Vioz_qQk6BpKdHc3wFBhLnM$ for graphic product...

    ATTN...WFO...AKQ...CTP...GSP...LWX...PHI...RAH...RLX...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 40337512 40107433 39367429 38507518 37867607=20
    36847810 35447979 35428088 36288122 37998022=20
    39157876 40137665=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jul 9 19:10:52 2025
    AWUS01 KWNH 091909
    FFGMPD
    NCZ000-SCZ000-FLZ000-GAZ000-100050-

    Mesoscale Precipitation Discussion 0630
    NWS Weather Prediction Center College Park MD
    308 PM EDT Wed Jul 09 2025

    Areas affected...South-Central North Carolina through North
    Florida

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 091907Z - 100050Z

    Summary...Widespread showers and thunderstorms will continue to
    drift slowly across the area through this afternoon. Rainfall
    rates of 2-3"/hr are likely, which could produce 2-4" of rain with
    locally higher amounts. This may result in flash flooding.

    Discussion...The experimental GOES-E day-cloud microphysics RGB
    clearly indicates the breadth of convection across coastal GA and
    SC this afternoon. Widespread and rapid blossoming of updrafts
    into anvils are noted in the satellite imagery, which is
    collocated with expansive reflectivity above 40dbZ on the regional
    radar mosaic. The quickness with which updrafts surge into Cb is
    indicative of the extreme environment, characterized by SBCAPE
    eclipsing 4000 J/kg and PWs measured by GPS exceeding 2.25 inches
    which is above the 90th percentile and approaching daily records.
    Into these thermodynamics, forcing for ascent is being driven by a
    pair of vorticity maxima approaching the region beneath increasing
    upper diffluence from the distant tail of a jet streak positioned
    to the northeast. Additionally, the sea breeze boundary and
    resulting outflow boundaries from convection are providing
    low-level ascent to sustain and regenerate thunderstorms.

    The 12Z U/A sounding from both KCHS and KJAX measured freezing
    levels around 15,500 ft, with weak and chaotic winds of 10kts or
    less through most of the column. This indicates that efficient
    warm-rain processes will dominate today, with slow and chaotic
    cell motions also expected. This is clearly evident already, and
    recent radar-estimated rain rates have exceeded 2"/hr from KCLX,
    leading to MRMS measured 1-hr rainfall above 2.5" in isolated
    locations over southeast GA. As low-level flow converges across
    the area, with increasing PW advection surging onshore (as
    reflected by the sfc-850mb CIRA LPW percentiles), and ascent
    persists into the additional moistening, rainfall rates will
    continue to intensify, with widespread rates above 2"/hr likely,
    and brief 4"/hr rates possible as shown on the HRRR 15-min
    rainfall reaching 1" in spots. Although bulk shear will be minimal
    so storms will remain of the pulse variety, collisions and mergers
    of cells could cause additional development into clusters at
    times. With weak flow throughout the column, storm motions will be
    chaotic and slow as dictated by these collisions/outflows, and
    upwind propagation vectors into any clusters collapse to around 0
    kts suggesting net stationary motion at times. Where this occurs,
    total rainfall will likely (60%) exceed 3", with as much as 5"
    possible (15%) in a few locations.

    Although some parts of the coastal plain have received heavy rain
    the past 7 days, it has been very scattered, and NASA SPoRT 0-10cm
    soil moisture is generally normal to below normal. This has
    resulted in FFG that is generally 3-4"/3hrs, although likely lower
    across any urban areas. Despite that, 3-hr FFG exceedance
    probabilities reach as high as 20-30%, further indicating the
    potential for instances of flash flooding due to these slow moving
    storms into the evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_N50AuNE_ypbqvX5uXNzSJ9WLch0CK7gQjuOIkF0S1LbSiyv_ROhYmaFUdc9TSz92ds1= 4XVkl8ZIpECy9j-EYDiOGxI$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...ILM...JAX...RAH...TAE...
    TBW...

    ATTN...RFC...ALR...NWC...

    LAT...LON 35438047 35308008 35007979 34637962 34247968=20
    33747995 32908028 32258059 31628104 30928129=20
    30448135 30088131 29698134 29408239 30058303=20
    31088356 32158331 33028304 33718254 34378210=20
    34878173 35308127 35428093=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Jul 9 23:55:47 2025
    AWUS01 KWNH 092355
    FFGMPD
    VAZ000-NCZ000-SCZ000-GAZ000-TNZ000-100600-

    Mesoscale Precipitation Discussion 0631
    NWS Weather Prediction Center College Park MD
    755 PM EDT Wed Jul 09 2025

    Areas affected...Southern Appalachians into the Carolinas Piedmont

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 092354Z - 100600Z

    Summary...Showers and thunderstorms will increase in coverage
    through the next several hours. Rainfall rates within deeper
    convection will exceed 2"/hr leading to localized rainfall as much
    as 3-4". Flash flooding is possible.

    Discussion...The GOES-E IR imagery this evening shows a slow
    uptick of cooling cloud tops from northern AL through
    western/central NC. These cooling tops are associated with
    deepening convection within a belt of higher moisture clearly
    noted on the GOES-E WV imagery stretching from MS into New
    England. Embedded in this plume, a potent vorticity max is
    pinwheeling across central TN, accompanying the primary mid-level
    trough axis that is concurrently swinging eastward. This is
    driving mid-level height falls from eastern TN into the Carolinas
    and western VA, which is combining with S/SW 925-850mb flow and
    the resulting upslope/convergence into the terrain to produce
    significant ascent. Additionally, a pre-frontal trough and
    accompanying squall line are moving across central NC. This lift
    is acting upon a moist and unstable atmosphere characterized by
    PWs of 1.8-2.2 inches and MLCAPE that remains above 2000 J/kg,
    resulting in widespread thunderstorm development noted via the
    regional radar mosaic.

    Radar estimated rain rates have been as much as 2"/hr according to
    KGSP and KMRX, and these are likely to continue for several more
    hours as reflected by HREF 2"/hr neighborhood probabilities
    peaking above 30%. This is despite the slow wane of surface
    instability, as the residual elevated CAPE will be plentiful to
    support heavy rain. As the shortwave and mid-level trough axis
    over TN swing eastward, forcing for ascent should maximize over
    western NC and the surrounding mountains/foothills, leading to an
    increase in convective coverage. This is suggested by many
    high-res CAMs, and activity is expected to linger well beyond the
    typical diurnal maximum. As convection expands, bulk shear may
    approach 25 kts to help drive at least modest organization into
    clusters, but with mean 0-6km winds and accompanying Corfidi
    vectors remaining just 5-10 kts, storm motions will be slow and
    chaotic. This is concerning for the flash flood potential as the
    intense rain rates will continue, helping to drive the HREF
    neighborhood probabilities for 3"/6hr (5"/6hr) above 40% (10%).

    FFG across the region varies greatly since the mountains have been
    dry the last 7 days, but the Piedmont is vulnerable due to recent
    heavy rain. Despite the varying FFG, HREF 3-hr FFG exceedance
    probabilities peak at 15-30% across much of the region. This
    suggests a flash flood risk exists across the entirety of the
    area, with the vulnerable soils east, and sensitive terrain west,
    increasing the runoff risk through the evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7yst06KkSqxdriZn2l8VXmfCjEkwZvmiiIcIq84uP5AtJiEXoeoPAKydVNRpvksH9FSU= IAHKUnrExW804NMw9keUHQ4$ for graphic product...

    ATTN...WFO...CAE...FFC...GSP...JKL...MRX...RAH...RLX...RNK...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 37118106 36617969 35857935 35087952 34728008=20
    34508150 34438283 34558372 34678435 34898482=20
    35688476 36588357 36948259=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 10 00:48:42 2025
    AWUS01 KWNH 100048
    FFGMPD
    NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-NCZ000-DCZ000-100630-

    Mesoscale Precipitation Discussion 0632
    NWS Weather Prediction Center College Park MD
    848 PM EDT Wed Jul 09 2025

    Areas affected...Mid-Atlantic States

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 100047Z - 100630Z

    Summary...A line of thunderstorms along a pre-frontal trough will
    continue to move E/NE through the evening. Rainfall rates of
    1-3"/hr are likely within these storms, leaning to stripes of 2-4"
    of rain and additional instances of flash flooding.

    Discussion...The regional radar mosaic this evening shows an
    impressive squall line with continuous thunderstorms aligned from
    near Philadelphia, PA southwest to Charlotte, NC. This line has
    been slowly but steadily moving east, while cells along the line
    track northeast. As this line has moved east, it has left a swath
    of MRMS measured rainfall of 1-3" with locally as much as 4" in
    the past 6 hours, and radar-estimated rain rates from radars along
    the line continue to be 1.5-2.0"/hr.

    There is good agreement that the squall line will continue to
    pivot slowly eastward, although some faster progression has been
    noted recently across NC/VA. Thermodynamics downstream of the line
    remain impressive and favorable for the continuation of heavy
    rain. MLCAPE is above 2000 J/kg in a narrow corridor generally
    along and east of I-95, with collocated PWs of 1.9 to 2.2 inches,
    or +1.5 standard deviations according to the SREF. 850mb inflow is
    measured out of the S/SW at around 20 kts according to regional
    VWPs downstream of the line, which when combined with the highly
    anomalous PWs will continue to push anomalous 850-700mb moisture
    flux into the region. This will support the persistence of heavy
    rain rates above 2"/hr as progged by HREF 2"/hr neighborhood
    probabilities of 30-40%, with brief rain rates above 3"/hr
    possible as reflected by HRRR 15-min rainfall reaching 0.75" or
    more.

    Bulk shear along and ahead of the line will remain 20-30 kts
    through the evening, suggesting multi-cell clusters (and isolated
    supercells) will continue, and this organization may briefly
    intensify and temporally extend the heavy rain rates. This will be
    in addition to training of cells that is expected from SW to NE
    due to parallel 0-6km mean winds and Corfidi vectors from VA
    northeast. Farther south into NC, Corfidi vectors pivot to become
    aligned anti-paralle to the mean wind, indicating that
    regenerating and backbuilding cells into the greater instability
    is also expected. Either way, this suggests a high potential for
    training the next several hours, leading to rainfall that could
    reach 2-4", or locally higher, according to HREF 6-hr neighborhood probabilities.

    0-10cm soil moisture percentiles over this area are generally well
    above normal, and above the 98th percentile in parts of NC and
    from Washington, D.C northeast through coastal NJ. This is
    reflected by extremely compromised 1-hr FFG that is 1.5" or less,
    suggesting even outside of the urban areas the soils have limited
    infiltration capacity and are vulnerable to rapid runoff/flash
    flooding. With these intense rain rates expected to continue for
    several more hours as the line translates eastward, any training
    would likely overwhelm these soils quickly, leading to additional
    flash flooding across the region.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9r5T94Fa3iGEQvrUHdg6ZTRmV78a9FieTHz6yf2eHYvZnUTkGy_DAKcqVohbS6qCxLJ-= oOAT5kPkw13QSM4pIc-jC10$ for graphic product...

    ATTN...WFO...AKQ...CTP...GSP...LWX...MHX...PHI...RAH...RNK...

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 40527440 40277397 39617407 39097437 37317565=20
    36307665 35677769 35257893 35397955 35668005=20
    35948038 36388017 36757932 37297844 38157752=20
    39327662 40167588 40467534=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 10 06:11:14 2025
    AWUS01 KWNH 100611
    FFGMPD
    MAZ000-NHZ000-RIZ000-VTZ000-CTZ000-NYZ000-101200-

    Mesoscale Precipitation Discussion 0633
    NWS Weather Prediction Center College Park MD
    210 AM EDT Thu Jul 10 2025

    Areas affected...Southern New England...Eastern Long Island...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 100610Z - 101200Z

    SUMMARY...Strong MCS approaching Long Island & slow moving,
    isolated convection north of it across Southern New England.=20
    Rates of 1.5-2"/hr and totals of 2-3.54" may present localized
    possible flash flooding through early morning.

    DISCUSSION...GOES-E 10.3um EIR loop shows a mature symmetric MCC
    moving through the New York Bight toward eastern Long Island.
    RADAR shows impressive MCV and stronger thunderstorm activity
    extending eastward given stronger WAA along/ahead of the wave
    increasing appearance of a solid occlusion to the overall wave.=20
    This would suggest slowing northeastward propagation and
    increasing rainfall duration. Given ample deep layer moisture of
    1.75" and stronger flux noted by RAP analysis and upstream VWP out
    of NJ; would support up to 2"/hr and possible 2-3" totals along
    the MCV across LI and eventually into coastal SE CT/RI and SE MA.=20
    Given higher FFG naturally through the area, flash flooding
    potential is likely to be more urban in nature with this wave.

    Further north into southern New England; RAP analysis and surface
    observations support a remaining uncapped to slightly capped
    region of 1000+ J/kg SBCAPE along the slowly northward advancing
    warm front from the Upper-Hudson Valley across central CT toward
    the Gulf of Maine. GOES-E WV shows highly positive
    tilt/elongated trough axis across New England into the northern
    Mid-Atlantic supporting DPVA while strong exiting jet streak over
    90 kts at 3H across Interior New England providing strong right
    entrance ascent and evacuation to the environment. Proximity to
    the warm front also provides some weak low level shear to support
    helicity to 50 m2/s2. As such, RADAR shows a few cells
    developing across E NY, CT and MA that are narrow in nature but
    have a weak rotation. Given similar ample moisture, cells should
    have good efficiency and weak rotating updrafts will further
    enhance moisture flux. While overall deep layer flow is strong
    suggestive of progressive cell motions, the shear supports
    Bunker's right moving supercell propagation suggests reduced
    forward propagation allowing for increased rainfall duration.

    So cells will have capability of 1.5-2"/hr rates but the weaker
    instability will limit the overall width of the updraft and
    potentially counteract the overall rainfall footprint/streaks.=20
    Confidence is slightly increased given 00z Hi-Res CAM solutions
    and 00z HREF output suggesting 3"/3hr of 10-30% and totals of 2-4"
    remain possible through 12z. Given this is very close to areas
    affected by heavy rainfall last evening, soils may still be prone
    for decreased infiltration and higher run-off suggesting areas of
    possible flash flooding may occur again tonight.=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!48d8sN7E6k38Kb5_SDhVWAMtIOesHhqqkydFWTSievfhIHQNeLZTPUDSW0Q1doBDCULM= pdOIGVHaUJrAGi_5uiDlaeY$ for graphic product...

    ATTN...WFO...ALY...BOX...GYX...OKX...

    ATTN...RFC...TAR...NWC...

    LAT...LON 43217211 42727125 42097060 41717053 41317090=20
    41157146 40857219 40707286 41387305 41667377=20
    42257386 42837312=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 10 08:43:17 2025
    AWUS01 KWNH 100843
    FFGMPD
    NEZ000-101400-

    Mesoscale Precipitation Discussion 0634
    NWS Weather Prediction Center College Park MD
    442 AM EDT Thu Jul 10 2025

    Areas affected...Central Nebraska...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 100840Z - 101400Z

    SUMMARY...A few hours of oblique WAA training band, poses narrow
    axis of 2-3" totals and possible localized flash flooding.

    DISCUSSION...GOES-E WV and EIR loop depicts a progressive arc of
    thunderstorms driven by an slightly above average but compact
    shortwave over-topping the larger scale ridge ahead of the main
    northern stream wave back over the Wyoming Rockies. While the
    shortwave is sliding eastward, along with typical nocturnal
    cyclonic turning, the LLJ is responding with continued 40-45kts of
    southerly slowly veering southwesterly 850mb winds. This also
    aligns with the western gradient of an enhanced moisture from
    central KS through the Sandhills of NEB. Being on the western
    edge of the convective line, there has been lingering unstable air
    associated with the moisture axis remaining across a similar area
    with MUCAPE values of 2000+ J/kg extending into KS. The passage
    of the convective line also established a NNW to SSE boundary
    across central NEB that now aligns from Nuckolls to Brown county.=20
    VWP and surface observations show, LLJ remains more southerly not
    having fully veered to the southwest, but strength of winds and
    intersection with the boundary provide strong deep layer
    convergence and isentropic ascent maximizing further northwest
    along the boundary near Brown to Loup County. As such,
    thunderstorms have been greatest cross this area; but with
    700-500mb steering flow nearly parallel and opposite to the LLJ
    and boundary; cells have a favorable orientation to repeat. This
    orientation will shift slightly from NNW to SSE to more NW to SE
    with time as the 700-500mb flow shifts eastward with the exiting
    shortwave into central IA; but there will be sufficient overlap in
    time and space for favorable repeating.

    As this time, a limiting factor toward flash flooding is the
    overall available moisture. Surface Tds in the 60s are
    sufficient, CIRA LPW shows deepest moisture, particularly above
    700mb is shifting eastward with the shortwave and the upstream
    gradient is very tight allowing for greater overall dry air
    entrainment. Still, with 1-1.5"/hr rates and potential for 2-4
    hours of repeating, totals of 2-3" are possible. The other
    limiting factor is proximity to the Sandhills itself, where
    favorable infiltration of those lower rates are likely to mitigate
    much flooding potential north of Valley and Custer county.=20
    However, as LLJ veers more southwesterly, the expansion of
    stronger boundary layer moisture convergence southward along the
    training line, places counties southward where FFG values are less
    than 1.5/hr and 3hr values are 2-2.5".

    While Hi-Res CAMs are less aggressive with the overall totals and
    trend toward quick evaporation of the line; this is a known
    negative bias where WAA, particularly orthogonal isentropic ascent
    tends to 'over-perform' the forecast guidance. Each HRRR run is
    also a bit more aggressive toward increasing convection, as well,
    providing some increased confidence this bias is once again
    plausible. So, while not particularly high-end, nor over a great
    areal extent, there is sufficient observational trends that an
    incident or two of localized flash flooding due to 2-3" totals is
    possible through early morning.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-iWjdIqZQga1Vaa0bltm29zJcHfLLwGNX1UkreFTecMJC92-gNrw7o9_ARI8EKE_KbmI= boRkjSjE6P4AeKIUrWfQKG0$ for graphic product...

    ATTN...WFO...GID...LBF...OAX...

    ATTN...RFC...KRF...NWC...

    LAT...LON 42559933 42289852 41679780 41149742 40499787=20
    40529880 41529964 42299979=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 10 16:52:48 2025
    AWUS01 KWNH 101651
    FFGMPD
    MEZ000-NHZ000-VTZ000-NYZ000-102250-

    Mesoscale Precipitation Discussion 0635
    NWS Weather Prediction Center College Park MD
    1250 PM EDT Thu Jul 10 2025

    Areas affected...Vermont and New Hampshire...Far Western Maine

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 101650Z - 102250Z

    SUMMARY...Slow-moving showers and thunderstorms anchored near the
    higher terrain of the Green and White Mountains may result in
    isolated to scattered instances of flash flooding going through
    the afternoon hours.

    DISCUSSION...The latest GOES-E visible satellite imagery in
    conjunction with radar is showing the gradual development and
    expansion of slow-moving shower and thunderstorm activity along
    the higher terrain of the Green and White Mountains of Vermont and
    New Hampshire respectively.

    The activity is being strongly influenced by orographic ascent
    within an increasingly unstable environment characterized by
    MLCAPE values of about 1000 J/kg. PWs are relatively moist with
    values up to about 1.5 standard deviations above normal, and this
    will favor convective cells capable of producing heavy rainfall
    rates of up to 1 to 2 inches/hour.

    Going through the afternoon hours, the arrival of some shortwave
    troughing/DPVA from southeast Canada in conjunction with
    additional diurnal heating should promote some additional
    expansion of convection that will be embedded within rather weak
    steering flow. The cells will be aided by terrain-driven
    circulations that may tend to allow for some of the cells to be
    nearly stationary and anchored along the upslope areas of the
    higher terrain.

    The 12Z HREF and recent HRRR solutions suggest some localized 2 to
    4+ inch rainfall amounts will be possible, and this coupled with
    the rugged terrain of the Green and White Mountains may support
    there being some isolated to scattered instances of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!59SAmOqy9OARqABRqHyfq1fG_bofZd2lctxYyrPdAtl0esD9lzDNhHg-6eqTVqUKFg8e= gIKVyQ0DkQY7YL_V2-9KKFM$ for graphic product...

    ATTN...WFO...ALY...BTV...GYX...

    ATTN...RFC...TAR...NWC...

    LAT...LON 45267109 45067051 44587050 43567113 42957178=20
    42767239 42967331 43727347 44397329 44687296=20
    44857234=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 10 18:04:25 2025
    AWUS01 KWNH 101803
    FFGMPD
    VAZ000-NCZ000-WVZ000-SCZ000-TNZ000-110000-

    Mesoscale Precipitation Discussion 0636
    NWS Weather Prediction Center College Park MD
    201 PM EDT Thu Jul 10 2025

    Areas affected...Central Appalachians through the Carolina
    Piedmont

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 101800Z - 110000Z

    Summary...Scattered instances of flash flooding expected across
    the interior southern Mid Atlantic into the Carolina Piedmont.

    Discussion...Visible satellite this afternoon continues to depict
    a some hindrance of typical diurnal heating with scattered to
    widespread cloud cover extending south to north across the
    Carolinas into the Delmarva. Back into the interior southern Mid
    Atlantic, pockets of clearing can be seen over the western
    Carolinas with some enhanced cumulus development, mainly along and
    west of I-85. Better solar insulation materialized across far
    southern WV into southwest VA earlier today allowing for scattered
    convective development where destabilization was maximized. The
    expected convective cadence this afternoon is for slow clearing to
    eventually give way to regional destabilization allowing scattered shower/thunderstorm pulses to initiate within the outlined area.=20

    Sufficient buoyancy and reputable PWATs hovering between 1.8-2.1"
    will present a reasonable environment for scattered heavy
    convective cores later this afternoon, leading to rates between
    1-2 inches/hour, on average. A few stronger cells across the
    Carolina Piedmont could very well push closer to 2-3 inches/hour
    however, especially in proximity to a defined surface trough
    bisecting the region longitudinally based off the latest surface
    analysis. This will put areas across the central portions of NC/SC
    at the greatest threat for heavy rain and flash flooding and
    overlapping areas that has seen their FFG's lower as a result of
    previous convective impacts.=20

    Recent hi-res deterministic models have inferred on the threat of
    scattered convective activity materializing by mid-afternoon,
    carrying into the early evening before waning as the activity will
    be subject to mainly thermodynamic processes with a weak kinematic
    aid of a meager shortwave rippling eastward out of the Tennessee
    Valley. Shear will be negligible today which correlates to more
    pulse convective modes and slower storm motions once activity
    initiates. Any steering pattern is weak, but will offer a slow
    advancement eastward as we move through the afternoon. Once we
    reach sunset, expecting convection to slowly dissipate over the
    eastern Carolinas with the loss of diurnal heating considering the
    overall environmental evolution. This will leave a window of 6-8
    hrs for the greatest convective threat, enough for HREFbm output
    of 2-4+" scattered over the western Carolinas down through the
    Piedmont.

    The combination of slower mean storm motions and wet antecedent
    conditions over much of western and central NC down through the
    central SC Piedmont offers the risk of scattered flash flood
    instances with the greatest threat within more urbanized zones.
    Given lack of a true kinematic forcing and environmental bulk
    shear, organized multi-cell clusters will be less common, thus
    limiting the threat to flash flooding possible with more isolated
    to scattered signals across portions of the southern Mid Atlantic.

    Kleebauer

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5_KcLxHU90ogeDWr7pkPN2WBbovdm8FegwO1iHnEPRhZSjnD0Bd8qNEsJkYqoryaokfZ= 8-OwaKrvjT0G-P8PzOXpOG0$ for graphic product...

    ATTN...WFO...AKQ...CAE...GSP...ILM...LWX...MRX...RAH...RLX...
    RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 38527878 38117846 37187834 36647827 36427825=20
    36017830 35697834 35437843 35117863 34737900=20
    34527919 33987959 33787982 33648008 33588038=20
    33558059 33528087 33518109 33608137 33728156=20
    33908176 34068189 34238201 34398217 34548235=20
    34808247 35238278 35688285 36018270 36238247=20
    36418229 36628230 36808236 37028240 37248217=20
    37458188 37638162 37728133 37868113 37968096=20
    38058083 38218041 38267974 38427930=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 10 18:18:54 2025
    AWUS01 KWNH 101818
    FFGMPD
    NJZ000-DEZ000-MDZ000-102218-

    Mesoscale Precipitation Discussion 0637
    NWS Weather Prediction Center College Park MD
    218 PM EDT Thu Jul 10 2025

    Areas affected...Northern Delmarva...Southern NJ

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 101818Z - 102218Z

    SUMMARY...Slow-moving and locally training showers and
    thunderstorms are expected to continue over the next few hours.
    Additional areas of flash flooding are likely over the next few
    hours.

    DISCUSSION...The latest radar imagery shows an axis of slow-moving
    and locally training showers and thunderstorms impacting portions
    of the northern Delmarva and southern NJ. The convection has been
    showing some cooling cloud tops over the last hour and is
    generally focusing along a surface trough oriented in a
    west-southwest to east-northeast fashion across the region.

    Convergent low-level flow along this surface trough coupled with
    the pooling of a moderately buoyant airmass characterized by
    MLCAPE values of 1000 to 1500 J/kg should promote some additional
    expansion of convection at least over the next few hours. The
    airmass is quite moist too with PWs of 2.0 to 2.25 inches. This
    environment will favor high rainfall rates of 1.5 to 2.5
    inches/hour.

    The latest HRRR guidance and a couple of the 12Z HREF members are
    hinting at this axis of convection continuing to locally train
    over the same area, and suggest some additional rainfall potential
    of as much as 3 to 4+ inches.

    Additional areas of flash flooding are likely at least over the
    next few hours given the rainfall potential and locally sensitive
    antecendent conditions.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8a0z_jaGgQGWVLBK-4_PptS6K1jkMXw91Y0DnLXo0FHNgn6QkHcf5IRfRGgLeuJQlGzJ= Re_6qzHCHy0lW4EJm4OIAfE$ for graphic product...

    ATTN...WFO...PHI...

    ATTN...RFC...RHA...NWC...

    LAT...LON 39707471 39657428 39527418 39317440 39167471=20
    39037553 39257590 39527553=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 10 19:06:22 2025
    AWUS01 KWNH 101906
    FFGMPD
    VAZ000-NCZ000-110000-

    Mesoscale Precipitation Discussion 0638
    NWS Weather Prediction Center College Park MD
    305 PM EDT Thu Jul 10 2025

    Areas affected...Southeast VA...Northeast NC

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 101905Z - 110000Z

    SUMMARY...Slow-moving and locally training showers and
    thunderstorms are expected to continue over the next few hours.
    Additional areas of flash flooding are expected through the
    remainder of the afternoon, and this will include a notable urban
    flash flood threat to the Hampton Roads area.

    DISCUSSION...The latest GOES-E visible satellite imagery along
    with dual-pol radar shows a southwest to northeast oriented axis
    of heavy showers and thunderstorms impacting the greater Hampton
    Roads area of southeast VA, with a gradual increase in convection
    seen developing across northeast NC. The activity is developing
    and expanding coverage along a surface trough which is driving
    convergent low-level flow within a very moist and unstable
    environment.

    MLCAPE values of 2000 to 3000 J/kg are noted over eastern NC and
    into far southeast VA, with PWs of 2.25+ inches. This has already
    helped to contribute to rainfall rates of 2 to 3 inches/hour with
    the stronger storms, and these rates should be maintained at least
    through the remainder of the afternoon hours.

    The latest HRRR/RRFS guidance suggests some additional rainfall
    totals of 3 to 4+ inches where some of these cells locally train
    over the same area. Additional areas of flash flooding are likely
    given the setup this afternoon, and this will include some notable
    urban flash flooding concerns around Hampton Roads area in
    particular.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!96QMFKc2MkiTiqhK3lIVMpQ6RHwa4z6nkJH6nqELAXD7KHxIJrhk0v7hyj4VYFuBtJaE= mecEzg-95JxZHJAaa-Y55OU$ for graphic product...

    ATTN...WFO...AKQ...MHX...RAH...

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37317653 37257589 36517565 35507620 35127712=20
    35487773 36477742 36997700=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 10 22:30:58 2025
    AWUS01 KWNH 102230
    FFGMPD
    IAZ000-NEZ000-SDZ000-110430-

    Mesoscale Precipitation Discussion 0639
    NWS Weather Prediction Center College Park MD
    629 PM EDT Thu Jul 10 2025

    Areas affected...Eastern Nebraska and Western Iowa

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 102230Z - 110430Z

    SUMMARY...Showers and thunderstorms initiating along a surface
    trough across eastern Nebraska are growing upscale with some
    backbuilding, leading to an increasing flash flood threat.

    DISCUSSION...GOES-East satellite imagery indicates that the
    earlier line of elevated convection that moved through
    northeastern Nebraska left behind several hours of clearer skies,
    leading to enough daytime heating to initiate a new round of
    surface-based thunderstorms. A surface trough extending through
    eastern Nebraska from a surface low centered near northwest Kansas
    and southwest Nebraska is providing a zone of convergence that
    will serve as a focal point for continued convective initiation.
    MLCAPE values of 2000-3500 J/kg across the region, combined with
    30-40 knots of 0-6 km Bulk Shear, supports the development of
    severe convection. Convection should begin as scattered
    thunderstorms with some isolated supercells, then steadily growing
    upscale into an organized MCS later in the period as the
    upper-level shortwave energy rotates through and the existing
    convection across eastern Colorado and western Kansas eventually
    merges with the convection over eastern Nebraska as a larger MCS.

    Although the 850 mb low-level jet of 20-30 knots is relatively
    weak, there is significant moisture convergence occurring along
    the axis of the surface trough, with a 19Z sounding at LBF
    indicating a PW of 1.27" which is close to the 90th percentile
    relative to climatology. Combined with a deep-layer mean
    southwesterly flow of only 20-25 knots, relatively slow storm
    motions and propagation vectors into the weak low-level jet
    suggests that backbuilding and upscale growth over the next few
    hours will lead to an increased risk for flash flooding. CAMs
    guidance is in good agreement with this flash flood potential,
    with HREF probabilities at 50-70% of 3-hr QPF exceeding 2". Flash
    flood guidance values also drop off significantly from west to
    east across Nebraska, given the moist antecedent conditions across
    eastern Nebraska and western Iowa, so FFG is less than 2" across
    the area of concern.

    Shieh

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-UIYUdV548phRFqGcgYF6WTtP_p6Rt0cfwtD1dROZqkwxw0pd6rbLWD7oPxeUW-4mRgC= PIP4Mlo06IhfV0RRw26qNlc$ for graphic product...

    ATTN...WFO...DMX...FSD...GID...LBF...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 42909505 42259411 40979618 40269822 40269822=20
    40329939 41559969 42529753=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jul 10 23:23:56 2025
    AWUS01 KWNH 102323
    FFGMPD
    WIZ000-ILZ000-IAZ000-110522-

    Mesoscale Precipitation Discussion 0640
    NWS Weather Prediction Center College Park MD
    723 PM EDT Thu Jul 10 2025

    Areas affected...Northern IL and Southern WI

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 102322Z - 110522Z

    SUMMARY...Increasing risk of flash flooding as coverage of
    scattered thunderstorms expands along a warm front extending
    across northern IL.

    DISCUSSION...A warm front gradually lifting through northern
    Illinois is providing a zone of surface convergence with
    thunderstorms developing across eastern Iowa, northern Illinois,
    and southern Wisconsin. MLCAPE values of 1500-2500 J/kg together
    with a progressive, 500 mb trough swinging through will support
    the maintenance of deep convection. Higher values of 0-6 km Bulk
    Shear of 30-40 knots across eastern Iowa suggests that severe
    convection may begin as discrete cells before growing upscale into
    an MCS as the convection approaches the warm front. Meanwhile, a
    simultaneous cluster of convection ongoing across northern
    Illinois in a region of lower shear with slower storm motions is
    likely to remain anchored along the warm front, posing a greater
    flash flood risk.

    Ample moisture with PW values ranging from 1.5-1.75" is in place
    across the region, and CAMs guidance suggests an increasing risk
    for convection along the warm front to backbuild and remain
    quasi-stationary, particularly in extreme northern Illinois and
    along the border with Wisconsin. HREF 6-hr QPF flash flood
    guidance exceedance probabilities are 40-50% in that localized
    region. Latest radar imagery also suggests that the cluster of
    thunderstorms presently across north-central Illinois is beginning
    to backbuild toward the west along the warm front, leading to the
    likelihood of training convection for the next several hours. As
    the separate area of convection across eastern Iowa moves toward
    northern Illinois, the upscale growth of the resultant MCS will
    further increase the likelihood of flash flooding.

    Shieh

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6ibSnY1OEufY6Di4WkU0gDKdZT5RzN6G6RJ9FODcWJichy94ISaPHTb56Gw84rAS7P8z= wL27Jres2ideFrNzV0H3wnA$ for graphic product...

    ATTN...WFO...ARX...DVN...LOT...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 43649099 43058915 42198778 41548772 41758919=20
    42079013 42559077 43119117=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 11 01:45:55 2025
    AWUS01 KWNH 110144
    FFGMPD
    NCZ000-SCZ000-110542-

    Mesoscale Precipitation Discussion 0641
    NWS Weather Prediction Center College Park MD
    943 PM EDT Thu Jul 10 2025

    Areas affected...Eastern North Carolina

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 110142Z - 110542Z

    SUMMARY...Complex cell mergers associated with several clusters of
    ongoing convection are contributing to the possibility of isolated
    flash flooding.

    DISCUSSION...Several clusters of convection are ongoing across
    eastern North Carolina in an environment of weak deep-layer mean
    flow of 10-15 knots out of the west-southwest. As a result,
    erratic storm motions are being driven by the complex interactions
    of mesoscale cold pools. Although peak daytime heating has passed,
    MLCAPE is still in the 1500-2500 J/kg range. Furthermore, as the
    500 mb shortwave trough axis rotates through, the convection is
    likely to sustain itself for a few more hours.

    The atmosphere is still extremely moist with the 00Z MHX sounding
    indicating a PW value of 2.18", which exceeds the 90th percentile
    relative to climatology. This pool of moisture across eastern
    North Carolina and the Outer Banks is well represented by the CAMs
    guidance, and HREF 3-hr QPF probabilities of exceeding 2" is
    40-50% for the region, with probabilities of exceeding the 6-hour
    flash flood guidance at 25-40%. These values suggest that although
    the dynamics are not conducive for a sustained, widespread threat
    of flash flooding, the slow storm motions, erratic cell mergers,
    and high moisture content suggest that there is at least an
    isolated flash flood risk.

    Shieh

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Z0BeZzSWFrCgdpcPv7xO2xvhdO53_hgGW3BAKZeW5jmVFM3lM-fxsgA3OlDy16FNxo3= J6lI5bmt3cPiYIoibS40LlY$ for graphic product...

    ATTN...WFO...AKQ...ILM...MHX...RAH...

    ATTN...RFC...ALR...NWC...

    LAT...LON 36277616 35197542 34117702 33717882 34167944=20
    35187911 35967786=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 11 03:47:06 2025
    AWUS01 KWNH 110346
    FFGMPD
    INZ000-ILZ000-IAZ000-110930-

    Mesoscale Precipitation Discussion 0642
    NWS Weather Prediction Center College Park MD
    1146 PM EDT Thu Jul 10 2025

    Areas affected...Northern Illinois...Southeast Iowa...Ext
    Northwest IND...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 110345Z - 110930Z

    SUMMARY...Lead shortwave with flanking line development and
    potential for repeating across areas of Northern IL through the
    overnight hours. Hourly rates to 2"/hr suggest 3-5" totals are
    possible, resulting in likely incidents of flash flooding.

    DISCUSSION...Regional RADAR mosaic depicts a mature MCS with
    strengthening MCV over N IL with moderate shield precipitation
    straddling the IL/WI line. A surface wave can be analyzed
    southwest of RPJ with stationary front across NE IL into northern
    IND, while the trailing boundary extends across into central IA.
    GOES-E WV and RAP analysis shows the stronger parent shortwave is
    located much further north across central WI; though a stronger
    northern stream wave continues to organize upstream across the
    Missouri River Valley. As such, the combination is helping to
    retain strong broad southerly LLJ providing WAA and deep moisture
    convergence in proximity the surface boundary; winds are 20-25kts
    at 850mb and remain confluent to the shortwave across WI. As
    such, solid convergence remains along the upstream flanking line
    across NW IL with thunderstorms still cooling even as the
    instability has be diminishing relative to upstream as well.=20
    Downstream, even lower CAPE values toward NW IND shows the slow
    erosion of the convective cells and warming tops.=20

    CIRA LPW shows 850-700mb layer has been increasing (though recent
    uptick is likely due to a particular over-estimate of values since
    01-02z) but the pattern shows the flux to maintain near 2.0" total
    PWat values to maintain rainfall efficiency to the convection.=20
    Southwest to west-southwest instability flux will also support
    back-building potentially across into E IA, though capping is a
    tad stronger. Still, redevelopment in NW IL with slow east to
    east-southeast propagation will allow for tracks of repeating and
    potential for multiple hours of 1.5-2"/hr rates. Localized totals
    of 3-5" are not out of the realm of possibility especially in
    proximity to I-80. Given FFG values of 1.5-2"/hr and 3hr
    generally around 2-3"; a few incidents of flash flooding along the
    line are considered likely. Of particular concern, is upstream
    development across NEB into central IA, that may intersect with
    this area toward pre-dawn and will watch the evolution
    closely...an upstream MPD will also be issued within the next hour
    or so.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_y3-33BUqIaHK8xEJuHa3-D-W21F2gMVg6eOjrv7yE-1Jx8VGqxkXeHIhrsOtEpWICoD= M0HDfsaoTn8tHbT0_FDF_E0$ for graphic product...

    ATTN...WFO...DMX...DVN...ILX...LOT...

    ATTN...RFC...MSR...NWC...

    LAT...LON 42428874 42408787 41958730 41478709 40898745=20
    40618904 40629034 40789204 41069279 41609294=20
    41929244 41899131 41979045 42059000 42168949=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 11 04:31:59 2025
    AWUS01 KWNH 110431
    FFGMPD
    IAZ000-NEZ000-SDZ000-110930-

    Mesoscale Precipitation Discussion 0643
    NWS Weather Prediction Center College Park MD
    1231 AM EDT Fri Jul 11 2025

    Areas affected...Eastern NEB...Western & Central Iowa...Far
    Northeast SD...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 110430Z - 110930Z

    SUMMARY...Slow moving thunderstorms near mid-level low, with
    faster moving cluster crossing central IA. Additional 2-4" totals
    with repeating cells likely to continue localized incidents of
    flash flooding.

    DISCUSSION...Complex mid-level evolution continues to provide a
    favorable environment for strong thunderstorms with high rainfall
    efficiency; some locations where convection will be more
    progressive but stronger, while others may be weaker, but slower
    but both capable of 2-4" add'l totals, likely resulting in
    scattered incidents of flash flooding.

    GOES-E WV suite shows stronger main wave over southeast SDak,
    while a jet max is streaking out of central Rockies supporting an
    upstream shortwave crossing southern NEB. Binary interaction
    between the systems is leading to the main wave sharpening and
    stalling with strong LLJ response with 35-40kts of 850mb flow
    crossing out of the Central Plains, intersecting with a stationary
    front that extends from the central NEB/KS boarder north to a low
    along the Missouri River in far SW IA before extending nearly due
    east across southern IA. Remaining area of highly unstable air
    exists at this intersection across SE NEB into southwest/central
    IA with 3000-3500 J/kg of CAPE and strong moisture flux bringing
    surface Tds into the low 70s and overall total PWats to 2-2.2"
    values. Strong, fairly orthogonal isentropic ascent will continue
    to support stronger convection near the low and eastward.=20
    Clusters will have 2.5"/hr rates, but deep layer steering flow
    parallel to the boundary should be quick to limit overall totals
    with the initial burst to 1.5-2" though continued upstream
    convergence should support back-building and training across
    southwest to central IA. Totals of 2-4" are likely to induce
    incidents of flash flooding through to 09z.

    NE NEB/NW IA/SE SDAK...
    With the deep layer wave stationary, but deepening, the LLJ is
    responding by backing back from southerly to southeasterly along
    an inverted surface to mid-level trof/TROWAL-like feature along
    the Missouri River. As the undercutting jet streak and associated
    vort max moves across S NEB, convection near the main center will
    have reduced forward speeds and evolve with similar note to a
    SHaRS (Subtle Heavy Rainfall Signature), where cores of cells are
    very slow moving, but produce moderate rainfall in weaker
    1000-1500 J/kg of MUCAPE; but in exhausting that well have a few
    hours to increases those localized totals to 2-4" totals. Some
    weak cell motion further southeast along the trof/TROWAL may
    support some repeating as well, but overall more chaotic cell
    motions are also likely to induce localize incidents of flash
    flooding especially given lower FFG values (1-1.5"/hr & 1.5-2"/3hr
    across the Missouri River Valley).=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9vMQT2V05cNdM-4MctxovtSvRzOAZI-yXiFmAqbpXgzSNgnyZEIhKvXV19K9yLcY7Asz= 6hEvdUNd90t-0sMLmwV7coY$ for graphic product...

    ATTN...WFO...DMX...FSD...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43429810 43249704 42549493 41919312 41709258=20
    41269250 40929265 40949417 40999511 41179664=20
    42249754 42879825 43289847=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 11 16:46:39 2025
    AWUS01 KWNH 111646
    FFGMPD
    WIZ000-ILZ000-MOZ000-IAZ000-112245-

    Mesoscale Precipitation Discussion 0644
    NWS Weather Prediction Center College Park MD
    1245 PM EDT Fri Jul 11 2025

    Areas affected...Central and Eastern IA...Northern MO...Northwest IL...Southwest WI

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 111645Z - 112245Z

    SUMMARY...Expanding clusters of heavy showers and thunderstorms
    are expected going through the afternoon hours. Locally moist
    antecedent conditions along with high rainfall rates and some
    cell-training concerns will foster a likelihood for scattered
    areas of flash flooding.

    DISCUSSION...The latest GOES-E IR/WV suite shows a strong
    shortwave trough over the central Plains gradually advancing into
    areas of the Upper Midwest which is fostering the eastward advance
    of low pressure along a frontal boundary draped over the region.
    Already there are some cooling convective cloud tops noted over
    north-central IA as strengthening warm air advection and the
    pooling of strong instability occurs ahead of this low center.

    A well-defined west to east oriented instability gradient extends
    across central and eastern IA through western IL, with MUCAPE
    values across the region on the order of 1000 to 2000 J/kg.
    However, areas near and south of the front going down into
    northern MO show substantially stronger instability fields with
    MUCAPE values here of 3000 to 4000 J/kg. Over the next few hours,
    stronger shortwave-driven DPVA, along increasing moisture and
    instability transport along and north of the boundary should favor
    an increase in elevated convection for especially central and
    eastern IA, with convective clusters potentially becoming aligned
    in a west to east training fashion given their orientation to the
    deeper layer steering flow.

    However, by mid to late-afternoon, much more surface-based warm
    sector convection should initiate and expand in coverage across
    southern IA and northern MO ahead of the shortwave energy/low
    center, and especially as any remaining low-level CINH is eroded.
    Effective bulk shear parameters will be on the order of 30 to 40+
    kts, which coupled with strong instability will yield a
    substantial mixture of multi-cell and supercell convection.

    Modestly anomalous PWs of 1.6 to 1.8 inches are in place, which
    coupled with the expected organized nature of the convection
    should support rainfall rates reaching easily into the 1.5 to 2.5
    inch/hour range. High rainfall rates and some cell-training
    concerns along with cell-mergers may yield some localized rainfall
    totals of 3 to 5 inches.

    The antecedent conditions over portions of central and eastern IA,
    northwest IL and southwest WI are relatively moist from recent
    rainfall, and this coupled with the additional heavy rains will
    likely encourage somewhat more efficient runoff. Scattered areas
    of flash flooding are expected, and there will also be locally
    notable urban flash flooding concerns. There are drier conditions
    noted farther south over southern IA and northern MO which will
    temper the flash flood threat here a bit more, but even here, the
    high rainfall rates here will promote a well-defined concern for
    some flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7hBwOA0DfbmNPwr6YH1P9KcsiumAqIdXQYW7Omg9Ji34u1qecO7DuQsXJwCmt4LlCh0C= yJIqo-mAW_Xij6GRQ8BVwMg$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...EAX...ILX...LOT...LSX...MKX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43449143 43298957 42488904 41638942 40749061=20
    39609256 39459391 40009432 40559430 40939430=20
    41389436 42159470 42559456 43119352=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 11 18:29:37 2025
    AWUS01 KWNH 111829
    FFGMPD
    MSZ000-112228-

    Mesoscale Precipitation Discussion 0645
    NWS Weather Prediction Center College Park MD
    229 PM EDT Fri Jul 11 2025

    Areas affected...central MS

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 111828Z - 112228Z

    Summary...Convection is growing in scale and could align along a
    west-northwest to east-southeast axis shortly. Hourly rain
    amounts to 3" with local totals to 5" are possible, which could
    lead to flash flooding in urban areas.

    Discussion...Thunderstorms across MS over the past couple hours
    have been forming in a very moist and unstable environment, with
    precipitable water values of 2-2.25" and ML CAPE in western MS
    above 3500 J/kg. Westerly flow in the low-levels has been
    steering convection generally west to east, but radar imagery is
    implying the beginning of a cold pool forming across east-central
    MS. Effective bulk shear is 15-20 kts, which appears sufficient
    to lead to loose organization.

    The expectation is for an outflow boundary to shift south and
    somewhat westward with time, which should lead to a more northwest
    to southeast alignment with time downwind of the instability pool,
    which should retrograde somewhat farther in the next several
    hours. While hourly rain totals to 3" are possible, there's
    evidence that at least one location near Louisville MS managed 2"
    in 26 minutes, likely due to the strong instability present, which
    would bring instantaneous rain rates to 5"+. The 12z HREF
    probabilities of 0.5"+ appears to be doing a much better job than
    the 06z RRFS probs in this area. Hourly amounts to 3" with local
    amounts to 5" could cause flash flooding, particularly within
    urban areas.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-7UT_kAtlZUQ5Daf03T1A48rQA6yNsDwqrK3Jy36QvQbuIPOSGEqc0ltEx_egj1ZN8HL= tmU4eRCovDDSLU0CboudA3k$ for graphic product...

    ATTN...WFO...JAN...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 33298971 32788860 31748855 31488939 31799030=20
    32519079 33139051=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 11 19:03:05 2025
    AWUS01 KWNH 111902
    FFGMPD
    NCZ000-SCZ000-120100-

    Mesoscale Precipitation Discussion 0646
    NWS Weather Prediction Center College Park MD
    301 PM EDT Fri Jul 11 2025

    Areas affected...portions of the western Carolinas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 111900Z - 120100Z

    Summary...Showers and thunderstorms are beginning to cluster
    across southwest NC. As the move east-southeast, hourly rain
    amounts to 2.5" with local totals to 4" are possible.

    Discussion...Thunderstorms with heavy rain have formed across
    southwest NC. While individual storms are randomly showing storm
    tracks to the east to east-northeast, the whole group appears to
    be propagating east-southeast along a moisture and instability
    gradient within a region of 700 hPa thermal difluence where the
    18z observations show some cyclonic wind shear. Precipitable
    water values of 2"+ are evident, and the 12z sounding at
    Greensboro NC and Peachtree City GA showed effective bulk shear of
    15-20 kts, which tends to be enough for loose organization. ML
    CAPE of 1500-2500 J/kg inhabits the region.

    The expectation is for some additional upscale growth while the
    storms move east to east-southeast at 10 kts. Hourly rain amounts
    to 2.5" with local totals to 4" are possible in this area, which
    given the topography and flash flood guidance values could lead to
    isolated to widely scattered flash flood concerns.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6ZZ-I2gYvEGGLiFa490CphhLTvLyG1orFEks5D3aBVPZqIxV8PYkmGSHHoC40B_wGtkk= N28aXj7sgiTbtS4Lu7okRdM$ for graphic product...

    ATTN...WFO...CAE...GSP...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 36018216 35798122 34858060 34148113 34218215=20
    34708291 35578305=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 11 20:11:10 2025
    AWUS01 KWNH 112010
    FFGMPD
    FLZ000-GAZ000-120209-

    Mesoscale Precipitation Discussion 0647
    NWS Weather Prediction Center College Park MD
    410 PM EDT Fri Jul 11 2025

    Areas affected...portions southern GA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 112009Z - 120209Z

    Summary...Backbuilding thunderstorms with possible mergers with
    activity approaching from the south are expected to continue to
    lead to hourly amounts to 2.5" and local totals to 4".

    Discussion...Showers and thunderstorms have formed within a moist
    and unstable air mass with precipitable water values of 2"+ and ML
    CAPE of 2500-3000 J/kg. Effective bulk shear is roughly 20 kts
    per the Peachtree City GA and Jacksonville FL soundings, which
    appears to have been sufficient for some level of convective
    organization, as there have been backbuilding signatures as of
    late.=20

    Both the 12z HREF and 06z RRFS probabilities are stuggling in this
    area, with the HREF indicating western areas fairly well and the
    RRFS having some concept of issues in more eastern areas within
    the MPD area. Because of this, am having to rely upon conceptual
    models more than usual, which leads to confidence being no better
    than average. The existing thunderstorm activity should build a
    little further before ending from west to east as thunderstorm
    outflow from activity to the south tries to exhaust the available
    instability. As outflow from the two convective areas intersect,
    there could be a tendency for thunderstorms with heavy rain to
    "zipper" along the outflow boundary intersection from west to
    east. Hourly rain amounts to 2.5" and local totals to 4" could
    lead to isolated to widely scattered flash flood concerns into
    this evening due to backbuilding, cell mergers, or new convective
    development along the upcoming outflow boundary intersection.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!92xOtsS95HrhWgJk8E-6Kq3XUVNk-Fb-3SWPV_7tLnl-_c1CrHK701RShxvBL4MN3nHl= Pq2TUsN9NVDnwF6_NKmojWg$ for graphic product...

    ATTN...WFO...CHS...FFC...JAX...TAE...

    ATTN...RFC...ALR...NWC...

    LAT...LON 32908297 31548125 31028130 30558139 30718222=20
    31668346 31858410 32278424=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 11 20:50:13 2025
    AWUS01 KWNH 112049
    FFGMPD
    NEZ000-COZ000-WYZ000-120247-

    Mesoscale Precipitation Discussion 0648
    NWS Weather Prediction Center College Park MD
    448 PM EDT Fri Jul 11 2025

    Areas affected...portions of southeast WY, northeast CO, &
    southwest NE

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 112047Z - 120247Z

    Summary...Showers and thunderstorms are beginning to increase in
    number across the area, with a couple showing backbuilding
    character. Hourly rain amounts to 2" with local totals to 4" are
    possible.

    Discussion...Upslope flow behind a pair of fronts moving south,
    down the east side of the Rockies is leading to moistening in the
    central High Plains. Precipitable water values of 0.5-0.8" exist
    per VAD wind profiles. CIN is reducing at this time, and ML CAPE
    of 1000-2000 J/kg is approaching the region from the northeast,
    likely due to cooling at 700 hPa and moistening of the column from
    that direction. Effective bulk shear of 20-35 kts exists in this
    region, sufficient for convective organization.=20

    The guidance appears to develop a convective complex in the short
    term near the CO/WY border that moves through a region of 700 hPa
    temperature difluence east-southeast across northeast CO,
    potentially tracking across a small pocket of convection
    occasionally backbuilding near the NE/CO border. Given the
    environmental parameters, such as moisture and instability
    increasing over the next several hours, this evolution makes
    sense. However, the possible thunderstorm complex track could end
    up being steered more southerly across northeast CO, so extended
    the region a little south of the mesoscale guidance which is close
    to where recent RAP guidance has indicated 700 hPa convergence.=20
    Such a complex should be capable of hourly rain amounts to 2" and
    local amounts to 4", which given the flash flood guidance values
    in the region, could produce widely scattered to scattered flash
    flooding where cells train or mesocyclones manage to form.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9q68Y-tpGDBpPwpBbrsxeLz8sdq6iSYY2-e-Rk3Q2K9mJW5jHeqrWz4UVw2Ih5LE56Dm= 0GzI6gklGB-wy67omucQgjk$ for graphic product...

    ATTN...WFO...BOU...CYS...GLD...LBF...

    ATTN...RFC...KRF...NWC...

    LAT...LON 41570451 41430300 40850196 39810223 39840393=20
    40500546 41120617 41450587=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 11 21:55:43 2025
    AWUS01 KWNH 112155
    FFGMPD
    TXZ000-OKZ000-COZ000-NMZ000-120354-

    Mesoscale Precipitation Discussion 0649
    NWS Weather Prediction Center College Park MD
    554 PM EDT Fri Jul 11 2025

    Areas affected...NM/CO border into the TX/OK Panhandles

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 112154Z - 120354Z

    Summary...Thunderstorms near the CO/NM border are starting to
    increase in number. Hourly rain amounts to 2.5" and local totals
    to 4" are possible, which could lead to scattered flash flood
    concerns.

    Discussion...Showers and thunderstorms are beginning to increase
    in number near a front in the vicinity of the CO/NM border.=20
    Precipitable water values of 0.75-1", ML CAPE of 500 j/kg inhabits
    their neighborhood, with higher values lying to the east.=20
    Effective bulk shear of 30-40 kts also lies in the vicinity, which
    should organize the convective activity.

    Increasing low-level inflow, moisture, and instability should lead
    to a growing convective complex that moves into the TX Panhandle
    with time. The increasing moisture/instability may lead to a
    fairly broad convective profile as any outflow boundaries from the
    convective mass cause periods of new convective growth and
    reorganization. While the front itself appears to hang up, the
    700 hPa thermal difluence indicates that a propagation to the
    southeast or even south-southeast should be expected over time
    should occur near and south of a zone of wind convergence apparent
    in the 21z observations. Both the 18z HREF and 12z RRFS show this
    sort of propagation, which may be aided by new convection moving
    near the dryline south of the front. The moisture and instability
    support hourly rain amounts to 2.5" and local totals to 4". With
    flash flood guidance being modest in the region, this could lead
    to widely scattered to scattered flash flood concerns.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7qnBw3yoyyC4QCgVpkbzHHPT6htmr4um8N8yTi1d4TyI1YkKxtJft_hVGGsaQ3_9M2Q9= 8-ZxTnKSJso_YdazQHfo3Xs$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...PUB...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 37160373 36010157 34650197 34300354 35160498=20
    36170525 37020498=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 11 22:22:10 2025
    AWUS01 KWNH 112221
    FFGMPD
    WIZ000-ILZ000-MOZ000-IAZ000-KSZ000-120419-

    Mesoscale Precipitation Discussion 0650
    NWS Weather Prediction Center College Park MD
    620 PM EDT Fri Jul 11 2025

    Areas affected...portions of the Upper Midwest

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 112219Z - 120419Z

    Summary...An incoming convective line with preceding thunderstorms
    is expected to lead to cell mergers in the near term. Hourly rain
    amounts to 2.5" and local totals to 4" remain likely through 02z,
    and possible thereafter. Scattered to numerous areas of flash
    flooding are anticipated.

    Discussion...An MCV appears to be forming across northeast IA in
    association with a broadening and maturing convective complex over
    the Upper Midwest. Precipitable water values are near 2". ML
    CAPE up to 3500 J/kg lies within the warm sector. Effective bulk
    shear of 30-45 kts is helping to organize the convective area.

    In the near term, cell mergers between the incoming line and
    preceding convection along with random mesocyclones are expected
    to lead to hourly rain amounts to 2.5" with local amounts to 4"
    until at least 02z. Thereafter, a narrowing convective footprint
    is expected as it reduces the instability pool currently in the
    warm sector and the convective line winnows and picks up the pace.
    Still, random mesocyclones along the line after 02z could lead to
    a LWEP or QLCS structure for at least a couple more hours which
    would lead to locally heavy rainfall. Some portions of the region
    -- particularly northern IL & portions of Chicago -- have seen
    heavy rainfall recently, which has led to low flash flood
    guidance. Scattered to numerous flash flood events are expected
    through 02z, even outside urban areas, before becoming more
    scattered to widely scattered thereafter.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7Pgb-1FuaLDx04VaBZ-oBegYbYeEWKkWJYrgr88yWUqV8asucDTVdmYB1Bx8MdEMF6It= xmZ7l2X_4IHxq_uda6li5_w$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...EAX...ILX...LOT...LSX...MKX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43269062 43258926 42508784 41798763 40988958=20
    40029112 39239240 39059416 39729497 41109433=20
    41709295 42099149 42739114=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 11 22:37:12 2025
    AWUS01 KWNH 112237
    FFGMPD
    SCZ000-GAZ000-120135-

    Mesoscale Precipitation Discussion 0651
    NWS Weather Prediction Center College Park MD
    636 PM EDT Fri Jul 11 2025

    Areas affected...GA/SC border into central SC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 112235Z - 120135Z

    Summary...Thunderstorms are developing along a more linear
    structure and may be about to train near and ahead of an outflow
    boundary intersection. Hourly amounts to 3" with local amounts to
    5" are possible.

    Discussion...There has been a resurgence in convective activity
    from far northeast GA into central SC within a moist and unstable
    environment near an imminent outflow boundary collision.=20
    Precipitable water values remain 2". ML CAPE is 3000+ J/kg.=20
    Effective bulk shear is 20-25 kts.

    The guidance indicates that the activity with heavy rainfall could
    hold on for another few hours. Hourly amounts to 3" and local
    totals to 5" remain possible where convection is quasi-stationary
    and/or trains.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9iR5aGrRatW0XC2qFrAVhvmO5PVjIY5pCahXoxuTP6M-483ouw7M8nBZ0OAeBc4orBL5= kA2ZImBEC8BMqcXFYw3WoxQ$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...

    ATTN...RFC...ALR...NWC...

    LAT...LON 34688347 34558211 33287975 32468033 32218125=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 11 23:58:43 2025
    AWUS01 KWNH 112357
    FFGMPD
    OKZ000-KSZ000-COZ000-NMZ000-120256-

    Mesoscale Precipitation Discussion 0652
    NWS Weather Prediction Center College Park MD
    756 PM EDT Fri Jul 11 2025

    Areas affected...in and near portions of southeast CO

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 112356Z - 120256Z

    Summary...Thunderstorms with heavy rain are increasing in coverage
    north of MPD #649. Hourly rain amounts to 2.5" and local amounts
    to 4" are possible.

    Discussion...Thunderstorms with heavy rain have been developing
    west and south of Pueblo CO near a stalling front and moving
    little, sometimes chaotically, during their life cycle.=20
    Precipitable water values are 0.75-1". ML CAPE is 500-2000 J/kg
    in their vicinity. Effective bulk shear of ~35 kts lies in the
    vicinity which could organize the convection.

    Over the next few hours, these storms should have enough moisture
    and instability to work with to persist. Hourly rain amounts to
    2.5" with local totals to 4" are possible. The mesoscale guidance
    (HREF and RRFS) show that convection this far north could persist
    for another several hours. Chose a valid time that matches MPD
    #649 when the broader situation in this portion of the High Plains
    can be reevaluated.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!42TqqdZZZEBDr7JlmVIYQz46cem66hyKUozaUKeLEXAqclUlNujy6RPZzmv8MnHX3nv_= FXX8BCMM38BcoWZD_X5fiBg$ for graphic product...

    ATTN...WFO...ABQ...AMA...BOU...DDC...PUB...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 38730583 37840324 36940146 36500189 37140344=20
    37260457 36860530 37670571=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jul 11 23:59:10 2025
    AWUS01 KWNH 112359
    FFGMPD
    OKZ000-KSZ000-COZ000-NMZ000-120400-

    Mesoscale Precipitation Discussion 0652
    NWS Weather Prediction Center College Park MD
    758 PM EDT Fri Jul 11 2025

    Areas affected...in and near portions of southeast CO

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 112356Z - 120400Z

    Summary...Thunderstorms with heavy rain are increasing in coverage
    north of MPD #649. Hourly rain amounts to 2.5" and local amounts
    to 4" are possible.

    Discussion...Thunderstorms with heavy rain have been developing
    west and south of Pueblo CO near a stalling front and moving
    little, sometimes chaotically, during their life cycle.=20
    Precipitable water values are 0.75-1". ML CAPE is 500-2000 J/kg
    in their vicinity. Effective bulk shear of ~35 kts lies in the
    vicinity which could organize the convection.

    Over the next few hours, these storms should have enough moisture
    and instability to work with to persist. Hourly rain amounts to
    2.5" with local totals to 4" are possible. The mesoscale guidance
    (HREF and RRFS) show that convection this far north could persist
    for another several hours. Chose a valid time that matches MPD
    #649 when the broader situation in this portion of the High Plains
    can be reevaluated.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8oel01T7nDizAzE1hcjBpP4UIFtVgUXhiJWEnfxz3lOh4YEuNr4_0TDt14dqf4TywIvp= DeG4Jyqiek-jMDlZLbApTW0$ for graphic product...

    ATTN...WFO...ABQ...AMA...BOU...DDC...PUB...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 38730583 37840324 36940146 36500189 37140344=20
    37260457 36860530 37670571=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 12 02:22:47 2025
    AWUS01 KWNH 120221
    FFGMPD
    ILZ000-MOZ000-120700-

    Mesoscale Precipitation Discussion 0653
    NWS Weather Prediction Center College Park MD
    1020 PM EDT Fri Jul 11 2025

    Areas affected...Central Missouri to Central Illinois...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 120220Z - 120700Z

    SUMMARY...Diminishing flash flood threat as squall line begins to
    forward propagate. However, a few hours with ample moisture and
    remaining unstable air mass will support 2"+/hr rates and spots up
    to 3" and possible.

    DISCUSSION...GOES-E 10.3um IR and RADAR animations show the long
    mostly squall line is starting to show outflow boundary pressing
    southeastward, increasing perpendicular forward propagation
    reducing duration of heaviest rainfall and all but eliminating
    internal cells repeating along the squall axis. A small
    inflection in the line near Macon county, MO is has some increased intersection/mergers as northern edge is upstream developing or
    effectively back-building into the southern flank, generally near
    the highest remaining pool of unstable air which remains about
    3500-4000 J/kg. This also matches with increased ageostrophic
    outflow given a small kink in the upper-level jet streak
    maximizing right entrance ascent profiles as well. Deep layer
    moisture axis is nearly aligned with the squall line and low level
    inflow is nearly parallel from 850mb with surface to 925kt inflow
    still fairly oblique in ascent angle too.

    Given the strength and available moisture, sub-hourly rates/totals
    over 2" will remain for a few more hours before slowly diminish as
    the squall moves into lower moisture over the Ozark Plateau and
    into southern IL. Backsheared mid-level shield precipitation will
    likely allow for additional moderate rainfall with spots of 2-3"
    totals over the next few hours; and while the FFG values are also
    increasing further south and east, isolated incidents of flash
    flooding remain possible though reducing with time.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5wVXsVrvhPq4mwXE3jTr4tUj4nVYhfoNoDlnbggQJ6EUxB5InCnLOIOIQO2mhQm7LKB5= -YUPhIYmEyllTZoKsJXdres$ for graphic product...

    ATTN...WFO...DVN...EAX...ILX...LSX...SGF...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 40998995 40968933 40648880 40238855 39598871=20
    39058926 38688995 38429054 38049151 37929267=20
    38469375 38839396 39219365 39959195 40429086=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 12 03:21:47 2025
    AWUS01 KWNH 120320
    FFGMPD
    KSZ000-NEZ000-COZ000-120830-

    Mesoscale Precipitation Discussion 0654
    NWS Weather Prediction Center College Park MD
    1119 PM EDT Fri Jul 11 2025

    Areas affected...Eastern Colorado...Western Kansas...Far Southwest
    NEB...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 120320Z - 120830Z

    SUMMARY...Chaotic, slow cell motions support large mergers and
    repeating incidents within increasing moisture environment.=20
    Isolated to widely scattered incidents of flash flooding remain
    possible with 2-3" totals in 1-3 hours.

    DISCUSSION...Regional RADAR mosaic and Lightning detection
    networks show a broad area of active and locally intensifying
    thunderstorms across the High Plains of Colorado starting to
    advance into W Nebraska and NW Kansas. GOES-E WV shows a very strong/sharpening longwave trof digging over the northern High
    Plains with based of the trough providing deep layer DPVA along
    and ahead of it, particularly along the southward pressing cold
    front across central NEB into the NE corner of CO. Deep layer
    moisture had pooled along the boundary with Tds in the the mid-
    50s and low 60s, though some pockets of drier surface air do
    remain in the core of the area of concern. Still solid heating
    and return upslope easterly flow continue to maintain unstable air
    with solid moisture flux.

    A secondary cluster, shortwave over-topping the larger scale ridge
    in the Four Corners is also helped to initiate convection that has
    become a bit more linear south to north from Crowley to Washington
    county and with a bit less mid-level forcing/focus; cells are
    forward propagating into the remaining unstable air.

    As such, thunderstorms have been slow moving from west to
    southeast, but there are many outflow collisions and cell mergers.
    Given total moisture of 1.25-1.5" and confluent flux from
    20-25kts at 850mb; rates of 1.5"/hr are becoming more common and
    with mergers and broader slab ascent near these outflow
    boundaries, rates can locally reach 2". Duration is limited to
    30-60 minutes, but there are opportunities for some upstream cells (particularly along the cold front) to tap remaining weak
    instability and track through areas affected earlier. This may
    result in 2-3" localized totals and in proximity to FFG values of
    1-1.5"/hr and 1.5-2.5"/3hrs, random occuring widely scattered
    incident or two of flash flooding remain possible into the core of
    the overnight period.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_C59yA-ujaJqeC6tWbvZ99QWL1jreqVEIrTiC5_ltirVgNGk6c6pTn6uqDe-eWNdH3L_= f_pN29B3bJp1Yw3KWf1wi7o$ for graphic product...

    ATTN...WFO...BOU...DDC...GLD...LBF...PUB...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 40930287 40930133 40420071 39810035 39070016=20
    38290007 37070051 37210241 38070372 39550368=20
    40840442=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 12 09:42:19 2025
    AWUS01 KWNH 120942
    FFGMPD
    TXZ000-NMZ000-121500-

    Mesoscale Precipitation Discussion 0655
    NWS Weather Prediction Center College Park MD
    541 AM EDT Sat Jul 12 2025

    Areas affected...East-Central NM... Western Cap Rock/Northern
    Permian Basin of West Texas...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 120940Z - 121500Z

    SUMMARY...Elevated thunderstorms with training/repeating with
    hourly rates of 1.5-1.75" and spotty 2-3" totals may pose
    localized flash flooding through day break.

    DISCUSSION...In the wake of the initial bowing convective complex
    through the northern TX panhandle overnight, the southwestern
    untapped flank has remained a corridor a enhanced 850-800mb
    southeasterly moist return flow and providing a modest northwest
    to southeast theta-E gradient. As the MCS expanded, merged
    growing upscale into the larger shortwave trough currently
    centered over SW KS; return southerly 700mb flow intersected the
    boundary with enhanced 1500-2000 J/kg MUCAPE due to steepened
    mid-level lapse rates and ample remaining low level moisture. The
    15-20kts of fairly orthogonal isentropic ascent resulted in
    elongated activation and expansion of elevated thunderstorm
    clusters. Given deeper level moisture in the 850mb layer, based
    likely have lowered a bit and tapped greater moisture depth for
    increasingly efficient rainfall. Rates of 1.5-1.75" are becoming
    common within the broadening cores; combine this with favorable
    rear inflow jet orientation to the 700-400mb flow behind the dead
    bowing segments has allowed for favorable repeating axis over the
    next few hours. With strongly veered/WAA flow from 850-700mb,
    propagation vectors may deflect the overall clusters southward
    from ideal training, but there should be ample opportunity for a
    few locations to receive 2-3" in the next few hours.

    Hydrologically, east-central NM remains slightly above average in
    soil saturation especially from San Miguel/N Guadalupe,SW Quay,
    Roosevelt toward Bailey/Cochran in the western Cap Rock. Hourly
    FFG values of 1-1.5" in the west toward 1.5-2"/hr eastward and 3hr
    values generally from 1.5-3" are at some risk of localized
    exceedance. As such, an incident or two of flash flooding is
    considered possible through the early morning hours/day-break=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_HjyPzj1s6yKgFqXx10ApVpNnsATg6LvuMt2TnEyNH9lxRxKQ2O4USHBgnp8s-Z-0mXi= JYGAPknBvTWr1MklzRXggwM$ for graphic product...

    ATTN...WFO...ABQ...LUB...MAF...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35720476 34680306 33450151 32670235 33380359=20
    34380462 35160501=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 12 13:34:22 2025
    AWUS01 KWNH 121334
    FFGMPD
    ARZ000-OKZ000-121732-

    Mesoscale Precipitation Discussion 0656
    NWS Weather Prediction Center College Park MD
    933 AM EDT Sat Jul 12 2025

    Areas affected...Eastern OK

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 121332Z - 121732Z

    Summary...Localized heavy rainfall from slow moving thunderstorms
    will result in a continued isolated flash flood risk through mid
    morning across portions of eastern Oklahoma.

    Discussion...Recent radar and satellite imagery shows continued
    thunderstorm activity across eastern OK. This area is in between a
    few MCV features...with one over MO, one over the TX Panhandle and
    another over southwest KS. High res model guidance is not handling
    this activity well, although the 11z and 12z HRRR finally have
    some indication of this convection. HRRR forecast soundings
    suggest this activity is based around 750-800mb, with models
    struggling with the degree of saturation and convergence at this
    level. Convection has been initiating near a cloud line seen in
    satellite imagery trailing southwest from the MCV feature over MO.
    This was likely indicative of some lower to mid level convergence,
    which combined with a modest increase in elevated moisture and
    possible weak vort max over eastern OK, has likely resulted in the
    convective development.

    The lack of useful model guidance does lower confidence on
    convective evolution this morning. There is plenty of instability
    (around 2000 j/kg of MUCAPE) to sustain convection and PWs around
    1.8" supports heavy rainfall rates. Eventually the approach of the
    stronger MCV from the west will likely result in additional robust
    convective development by later today...however for the morning
    hours forcing is weaker. Thus any slight drying around 800mb or
    downtick in convergence would result in a weakening of convection.
    Thus it seems most likely that convection will gradually weaken by
    mid to late morning, before additional development occurs later
    today...but again confidence on this evolution is only average.

    In the meantime, the environment does favor slow cell motions...so
    even though the storm cores are quite small...localized heavy
    rainfall rates/totals will remain likely for the next couple
    hours. The activity is pretty high based, and the degree of
    lighting indicates sufficient ice in the cloud layer. Thus while
    the most efficient warm rain processes are probably not dominant
    in these cells...the high PWs and slow motions will still support
    hourly rainfall as high as 2", and total rainfall of 3-4" in
    spots. This will be enough to result in at least an isolated flash
    flood risk this morning...especially in any more sensitive urban
    areas.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_3dOh3QnOaKj3-PbEF5JGgoozJlGod5KVjXVznI4X6dUveXsV6RgA3asn5xAnVlh0gC6= D9Mg9GoDZoUwd4RGo_nkvhs$ for graphic product...

    ATTN...WFO...OUN...TSA...

    ATTN...RFC...TUA...NWC...

    LAT...LON 36449697 36399611 36239552 36169488 36009445=20
    35829428 35719440 35579476 35529538 35659611=20
    35709641 35849698 36149712=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 12 18:04:43 2025
    AWUS01 KWNH 121802
    FFGMPD
    MAZ000-NHZ000-VTZ000-CTZ000-NYZ000-NJZ000-PAZ000-130000-

    Mesoscale Precipitation Discussion 0657
    NWS Weather Prediction Center College Park MD
    201 PM EDT Sat Jul 12 2025

    Areas affected...Northeast PA...Central/Eastern
    NY...Central/Southern VT...Western MA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 121800Z - 130000Z

    SUMMARY...Scattered slow-moving showers and thunderstorms with
    heavy rainfall rates are expected going through the early evening
    hours. Isolated areas of flash flooding will be possible over the
    next several hours.

    DISCUSSION...The latest GOES-E visible satellite imagery shows a
    remnant MCV gradually drifting east across areas of central NY,
    and this energy will be interacting with a very moist and unstable
    airmass across the interior of the Northeast that will be
    conducive for scattered areas of slow-moving showers and
    thunderstorms going through the early evening hours.

    MLCAPE values of 1000 to 1500+ J/kg are in place from northeast PA
    through central/eastern NY and into areas of southern VT and
    western MA. PWs across the region are running on the order of 1.5
    to 2 standard deviations above normal, and the combination of
    these two parameters should favor convective cells being capable
    of producing rainfall rates of 1 to 2 inches/hour.

    A combination of the aforementioned vort energy along with
    localized orographic ascent near areas of higher terrain will
    favor some expansion of convective activity over the next several
    hours, but the convective cells will be embedded within rather
    weak steering flow, and any terrain-induced circulations may tend
    to favor some cells becoming orographically anchored.

    This will support some localized storm total rainfall amounts
    going through early this evening of 2 to 4 inches which is
    supported by the 12Z HREF guidance. This will support a concern
    for isolated areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_hgIg9nXt8F_M_65mwFypHax9xye74XIExxpLzPpRZHp0rlkuQHooLEZyUz7C2JZHhau= ky6Jqe8chb8eG2FxzgxOoyg$ for graphic product...

    ATTN...WFO...ALY...BGM...BOX...BTV...CTP...GYX...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 44337336 44137245 43337233 42707245 42077292=20
    41357439 40617568 40807693 41587714 42827640=20
    43357537 44097422=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 12 18:16:56 2025
    AWUS01 KWNH 121816
    FFGMPD
    OKZ000-KSZ000-130015-

    Mesoscale Precipitation Discussion 0658
    NWS Weather Prediction Center College Park MD
    215 PM EDT Sat Jul 12 2025

    Areas affected...OK and southern KS

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 121815Z - 130015Z

    Summary...Expanding convection ahead of an MCV will result in
    areas of heavy rainfall and an isolated to scattered flash flood
    risk over portions of central and eastern Oklahoma and far
    southern KS. A more concentrated area of flash flooding is
    possible near a lingering outflow boundary over central OK.

    Discussion...A well defined MCV moving across OK will likely
    trigger additional convective development as we head through the
    afternoon hours. A pretty messy convective pattern at the current
    time with several convective clusters ongoing ahead of the MCV.
    High res model guidance has been inconsistent in the handling of convection...but a combination of recent HRRR and RRFS runs, along
    with observational trends, has resulted in an increase in
    confidence on how things should evolve. Despite the ongoing
    convection and cloud cover, instability is on the uptick ahead of
    the MCV...with MLCAPE around 2000 J/KG. PWs average around 1.8",
    and should continue to tick up slightly, likely approaching 2" in
    spots by later this afternoon. Deep layer shear remains weak, but
    the combination of the MCV and decent upper level divergence
    centered over the state should help sustain convection. Deep layer
    mean flow is relatively weak (about 10-15 kts) out of the
    southwest. Given this is similar to the MCV track, would generally
    expect a slow northeast movement to convection. Upwind propagation
    vectors are divergent over the region...typically an indicator of
    potential backbuilding and/or stationary cluster motions. We have
    already seen some of this during the morning hours over portions
    of eastern OK.

    The overall expectation is that convection will expand in coverage
    over the next few hours ahead of the MCV as destabilization
    continues. The aforementioned slow deep layer mean flow and
    backbuilding potential alone would point to some flash flood risk.
    However this risk may be exacerbated by the presence of the long
    lived outflow boundary that resulted in the earlier flash flooding
    near Tulsa. This boundary has persisted longer than earlier
    guidance had expected...and now should play a role in the flash
    flood risk going forward as well. The general expectation is that
    convection will build into this boundary...with some continued
    south southwest propagation possible. This should allow for a
    pronounced training convective risk and the likelihood of at least
    some additional flash flooding, some of which could be locally
    significant.

    The 15z run of the experimental RRFS does indeed show an evolution
    such as this...resulting in additional rainfall of 3-5". Given
    that the RRFS seems to have a decent handle on the current
    outflow, its evolution seems plausible. The 16z HRRR is a bit less aggressive...but still shows 2-3" totals...despite not having a
    great handle on the aforementioned outflow boundary. Thus tend to
    think amounts will likely exceed the HRRR output, and would expect
    hourly rainfall locally exceeding 2", and additional rainfall
    totals approaching or even exceeding 5" on an isolated basis
    through 00z.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4FscZ5Sw7T6BhukzGeoovZf7l82HkjqgKu-0ck9UaZNCPv67PYfj5Zqi6Cq3eDt0raN6= -DLaviQulJHiX0DSQn87ghA$ for graphic product...

    ATTN...WFO...ICT...OUN...TSA...

    ATTN...RFC...TUA...NWC...

    LAT...LON 37609721 37469658 36719598 36399578 35829521=20
    35159477 34349554 34009674 34389765 35109806=20
    35899855 36909841 37389790=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 12 18:29:25 2025
    AWUS01 KWNH 121829
    FFGMPD
    VAZ000-NCZ000-130027-

    Mesoscale Precipitation Discussion 0659
    NWS Weather Prediction Center College Park MD
    227 PM EDT Sat Jul 12 2025

    Areas affected...Central to Southeast VA...Northeast NC

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 121827Z - 130027Z

    SUMMARY...Slow-moving showers and thunderstorms will continue to
    locally expand in coverage over the next few hours. Additional
    areas of flash flooding are expected which will include urban
    flooding concerns.

    DISCUSSION...Radar imagery shows multiple clusters of heavy
    showers and thunderstorms continuing to develop and evolve across
    areas of central to southeast VA along with northeast NC. This
    convection is focusing within a very moist and unstable
    environment with proximity of a weak area of low pressure and
    surface trough helping to provide moderately strong low-level forcing/convergence.

    MLCAPE values of 2000 to 3000 J/kg are in place with the aid of
    strong diurnal heating, and PWs are on the order of 1.75 inches.
    Much of the activity is pulse in nature with a lack of shear, but
    the rainfall rates are very high with rates of 1.5 to 2.5
    inches/hour given the moist/unstable environment.

    Some additional expansion of convection is expected over the next
    few hours given persistence of the low-level trough and also with
    potential for some outflow boundary collisions that may help
    induce additional regional scale convective development. The
    threat area should generally encompass central to southeast VA and
    northeast NC through this evening before eventually the
    instability is exhausted and the convective threat wanes.

    Until then, some additional rainfal totals of 2 to 4 inches will
    be possible. And this will favor some additional areas of isolated
    to scattered flash flooding, which will include the more urbanized
    locations. This will include the Richmond metropolitan area where
    flash flooding has already been occurring over the last 60 to 75
    minutes.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!79m58Q6EN_PPbkb1cbEslg0FCophDsJt3GhOlEzyVxqc_Jdas6lTiCU7VrS9tr0A0ZGO= g1AoW6EU2A1OEF9qhFHsY-k$ for graphic product...

    ATTN...WFO...AKQ...LWX...MHX...RAH...RNK...

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 38297777 37987708 37397660 36747639 35967600=20
    35537609 35587699 36527794 37257883 37937896=20
    38287846=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 12 19:06:24 2025
    AWUS01 KWNH 121906
    FFGMPD
    TXZ000-OKZ000-130104-

    Mesoscale Precipitation Discussion 0660
    NWS Weather Prediction Center College Park MD
    305 PM EDT Sat Jul 12 2025

    Areas affected...TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 121904Z - 130104Z

    Summary...Expanding convection ahead of an MCV will result in
    isolated to scattered flash flooding through the afternoon across
    much of central to northern Texas.

    Discussion...Two distinct MCVs are evident on visible satellite
    imagery...one across portions of western OK and another over the
    southern TX Panhandle. It is the latter one that will likely be
    the main player in an expanding thunderstorm threat over central
    and north TX this afternoon and evening. These are small scale
    features that can be difficult for models to resolve with much
    lead time, thus not too surprising that recent high res model runs
    are not doing a great job with the ongoing activity and evolution
    going forward. Given the downstream environment, the 17z HRRR in
    particular seems much too dry, oddly killing convection despite
    the MCV and downstream instability pool. Recent runs of the
    experimental RRFS are seemingly handling things better, albeit
    maybe progressing convection too quickly off to the east.

    The environment downstream of the MCV has a broad are of MLCAPE
    around 2000 J/KG and PWs over 1.6" (should continue to increase
    towards 1.75"). Deep layer wind shear is weak, but the flow at
    300mb is broadly diffluent, which combined with the MCV should
    help sustain convection long enough for locally heavy rain. The
    downstream environment is a bit messy, with subtle boundaries and
    some ongoing convection. It seems likely that we will see some
    cell merger activity in this environment as convection closer to
    the MCV runs into the more isolated downstream cells...which
    should locally increase the flash flood risk.

    While isolated flash flooding is probable, there remains
    uncertainty on the coverage of the threat through 01z. Most
    indications would suggest just this isolated coverage of flash
    flooding, as some eastward propagation and pulsing nature of
    convection preventing a more widespread risk through 01z. However
    still certainly the potential for localized higher end
    impacts...and upwind propagation vectors would support
    backbuilding/slowing of convection. Thus if activity is able to
    organize more than current models indicate, then a more organized
    flash flood risk could certainly evolve by 01z. In addition,
    guidance is trending towards the MCV being a focus for slow
    moving/backbuilding convection tonight (after the expiration of
    this MPD). So we will need to closely monitor observational and
    model trends through the afternoon and evening...as these
    nocturnal MCV driven events can produce a significant flash flood
    threat. Additional MPDs will be issued as needed as the risk
    evolves.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_RoTPIf3-R7iQq58cvtkXbS_cifgYX3zNSihCRHgD8MxkNWgo3fTf0YWj1-5A0kegXaY= -Hvd2KwaRq_Y4Finz_zvZOI$ for graphic product...

    ATTN...WFO...EWX...FWD...LUB...MAF...OUN...SJT...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 34259748 34089696 34039634 33579616 31859654=20
    31059756 30679910 30420051 30370084 30440152=20
    31440136 31670128 32570060 33359935 34189838=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 12 20:37:36 2025
    AWUS01 KWNH 122037
    FFGMPD
    VAZ000-NCZ000-WVZ000-SCZ000-GAZ000-TNZ000-KYZ000-130135-

    Mesoscale Precipitation Discussion 0661
    NWS Weather Prediction Center College Park MD
    435 PM EDT Sat Jul 12 2025

    Areas affected...Portions of the Southern Appalachians

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 122035Z - 130135Z

    SUMMARY...Locally slow-moving and anchored thunderstorms near
    areas of steep and rugged terrain may cause at least isolated
    areas of flash flooding going into the evening hours.

    DISCUSSION...The afternoon GOES-E IR satellite imagery shows
    cooling convective tops continuing across portions of the southern
    Appalachians including far eastern TN, southwest VA, western NC,
    upstate SC, and northern GA. This is in association with
    relatively slow-moving areas of heavy showers and thunderstorms
    which are being focused predominantly by orographic ascent/upslope
    flow near the higher terrain along with differential heating
    boundaries adjacent to it. However, there is also some very modest
    shortwave energy approaching from the TN Valley which is also
    acting as a catalyst for convective initiation and expansion of
    cells.

    MLCAPE values are as high as 1500 to 2500 J/kg, with PWs that are
    just slightly anomalous for this time of the year at about 1.5 to
    1.75 inches. Very little shear is in place, so the convective mode
    is mostly pulse, but the cell-motions are quite weak, and this has
    been allowing for some cells to produce hourly rainfall amounts of
    1.5 to 2.5 inches.

    These higher rainfall rates along with some recent trends for
    cells to become anchored near some of the higher terrain suggest
    the potential for some storm totals to reach 3 to 4+ inches over
    the next several hours, and this supported by some of the 12Z
    HREF/REFS guidance.

    These rains will be falling over areas of steep and rugged
    terrain, and as a result will be capable of producing a threat of
    at least isolated areas of flash flooding going into the evening
    hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4aZ64bTjjTloGwKLCWFpmpdNfGmYA2VgkYANaQQkPwn5IvO6ra8ymrhKv2aIv2TfNT1q= LOADLgbcFhoL7osl83Nr7I4$ for graphic product...

    ATTN...WFO...FFC...GSP...JKL...MRX...RAH...RLX...RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 37658120 37348028 36558018 35678060 34358206=20
    33938313 33938429 34218461 34678446 35288400=20
    36188337 37138284 37568209=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jul 12 21:17:14 2025
    AWUS01 KWNH 122116
    FFGMPD
    MDZ000-VAZ000-DCZ000-130115-

    Mesoscale Precipitation Discussion 0662
    NWS Weather Prediction Center College Park MD
    515 PM EDT Sat Jul 12 2025

    Areas affected...Northern VA...Central MD...Washington D.C.

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 122115Z - 130115Z

    SUMMARY...Slow-moving thunderstorms with very heavy rainfall rates
    of up to 2.5 inches/hour will result in concerns for urban flash
    flooding across portions of the Washington D.C. metropolitan area.

    DISCUSSION...Radar imagery and late-day GOES-E satellite imagery
    shows strong thunderstorms developing and expanding in coverage
    across areas of northern VA, central MD and notably the western
    suburbs of Washington D.C.

    MLCAPE values of 1500 to 2500+ J/kg are in place across the region
    and this coupled with PWs of 1.75 to 2 inches will yield rainfall
    rates of locally 1.5 to 2.5 inches/hour with the stronger
    convective cores.

    Small-scale mesoscale boundaries near the Potomac River and with
    outflow associated with the existing thunderstorm activity is
    promoting new convective development in a moist and unstable
    airmass. This airmass is characterized by MLCAPE values of 2000 to
    3000 J/kg with PWs of 1.75+ inches.

    Given the thermodynamically favorable environment along with a
    likelihood for additional small-scale mesoscale boundary
    collisions over the next few hours, additional shower and
    thunderstorm activity is expected to linger through the early to
    mid-evening hours. Thereafter, conditions should improve with the
    exhausting of daytime heating and related instability.

    Some localized storm totals of 3+ inches will be possible with
    this shower and thunderstorm activity given slow cell-motions.
    These rains will pose an urban flash flood threat to especially
    the western suburbs of the Washington D.C. metropolitan area
    including portions of northern VA and central MD.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6cMomLSEwQ-ro09gakndSdl3ZLbsjWTL7fghYTq6bWEBbDnRdbDiMZSmOBPQpsWfdc5L= XqvBI51I_k_GYuD4ZQ894nk$ for graphic product...

    ATTN...WFO...AKQ...LWX...

    ATTN...RFC...RHA...NWC...

    LAT...LON 39267732 39127685 38607695 38127732 37997764=20
    38177808 38627805 39067773=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 00:06:55 2025
    AWUS01 KWNH 130006
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-KSZ000-130605-

    Mesoscale Precipitation Discussion 0663
    NWS Weather Prediction Center College Park MD
    805 PM EDT Sat Jul 12 2025

    Areas affected...Northeast TX...Central and Eastern OK...Western
    AR...Far Southeast KS...Southwest MO

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 130005Z - 130605Z

    SUMMARY...Slow-moving areas of heavy showers and thunderstorms
    will maintain a likelihood for seeing at least scattered areas of
    additional flash flooding going into the overnight hours.

    DISCUSSION...The late-day GOES-E IR satellite imagery along with
    dual-pol radar continues to show a broken and elongated axis of
    heavy showers and thunderstorms across portions of northeast TX
    through central and eastern OK and into adjacent areas of
    southeast KS and southwest MO. The convection continues to focus
    out ahead of a slow-moving shortwave trough and embedded vort
    center stretching from southern KS down through western OK, with
    multiple surface lows and an attendant frontal boundary situated
    across the region as well.

    There remains a substantial amount of late-day instability across
    portions of the Red River Valley of the South and stretching
    northeastward up into portions of the Ozarks including much of
    eastern OK, western AR and far northeast TX. MLCAPE values of 2000
    to 3000 J/kg suggest strong instability, and the environment is
    quite moist with PWs of 1.75 to 2+ inches. CIRA-ALPW data suggests
    notably strong deep layer moisture content in close proximity to
    the vort center across far southern KS down through central OK
    where there has been very heavy rainfall noted over the last
    several hours.

    This mid-level shortwave energy and associated vort center will
    drift off to the east going into the overnight hours and this will
    foster very slow movement of the associated surface low along the
    front. Meanwhile, some gradual nocturnal strengthening of a
    southerly low-level jet is expected across northeast TX, eastern
    OK and western AR with the nose of this aiming into southwest MO.

    Low-level warm air advection and speed convergence coupled with
    modest shortwave-induced DPVA/forcing should promote a localized
    persistence and eventually a renewed expansion of convection
    across areas of eastern OK through western AR. Some back-building
    convective signals will be in place which may allow for northeast
    TX to get into a threat for more focused slow-moving thunderstorm
    activity which is suggested by the Corfidi vectors.

    Rainfall rates will be high and capable of reaching 2 to 3
    inches/hour with the stronger storms and especially as the
    low-level jet strengthens overnight. Some localized additional
    rainfall totals going through 06Z (1AM CDT) may reach 3 to 5
    inches given weak steering flow and slow cell-motions.

    Additional areas of flash flooding are likely overnight given the
    generally moist antecedent conditions and high rainfall rate
    potential.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_t_q8e7eykeSCeyn_aQzKX-pt9r6k9xnP4buVPY7fFjcdXLpUoD27iMKcokhua5aJEFI= vRdhPQJ9qXIwlkXO8HRt1pg$ for graphic product...

    ATTN...WFO...EAX...FWD...ICT...LZK...OUN...SGF...SHV...TSA...

    ATTN...RFC...FWR...KRF...ORN...TUA...NWC...

    LAT...LON 38079390 37839234 36819164 35829219 34579318=20
    33079401 32449517 32669675 33469736 34559714=20
    35799614 36619566 37759541=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 00:36:28 2025
    AWUS01 KWNH 130036
    FFGMPD
    TXZ000-COZ000-NMZ000-130635-

    Mesoscale Precipitation Discussion 0664
    NWS Weather Prediction Center College Park MD
    835 PM EDT Sat Jul 12 2025

    Areas affected...Southern CO...Central NM...Far Southwest TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 130035Z - 130635Z

    SUMMARY...Heavy showers and thunderstorms will continue to
    gradually settle south through this evening across southern CO
    down through much of central NM, and potentially into far
    southwest TX. Heavy rainfall rates near areas of high terrain and
    also locally into some of the normally dry washes and burn scar
    locations may cause flash flooding over the next several hours.

    DISCUSSION...The late-day GOES-W IR/WV suite shows shortwave
    energy digging gradually south down across southern CO and into
    central and northern NM. Cooling convective cloud tops are noted
    across the higher terrain and into the adjacent areas away from
    the mountains as a combination of relatively moist low-level
    upslope flow and instability work in tandem to initiate and expand
    convection.

    MUCAPE values of 1000 to 2000 J/kg are noted, and there is some
    modest effective bulk shear of 20 to 30+ kts arriving in
    association with stronger northwesterly mid-level flow and the
    aforementioned shortwave energy dropping down over the region.

    Some additional uptick in the coverage of convection is expected
    this evening given the rather favorable thermodynamic and
    kinematic environments, and there will be sufficient moisture and
    instability for some rainfall rates to reach 1 to 2 inches/hour.

    Given the influence of orographics/upslope flow and some localized cell-training concerns going through this evening, there may be
    some spotty storm rainfall amounts of 2 to 3+ inches. This may
    drive isolated to scattered areas of flash flooding, and this will
    include potential flooding impacts to the normally dry washes and
    burn scar locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5dLNxukzGXeftnpy9-73TOERo-ueW4Q4qR4aryxnYwDHJ_vAqmDhp8By2wAHwoQwwyzH= XheyJPBb4Q4xTjtJ50ZhHJM$ for graphic product...

    ATTN...WFO...ABQ...EPZ...PUB...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 38080492 37340408 35690440 34210476 31860495=20
    31210565 31590647 32410685 33480700 35160691=20
    36200669 37620600=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 02:30:41 2025
    AWUS01 KWNH 130226
    FFGMPD
    TXZ000-130825-

    Mesoscale Precipitation Discussion 0665
    NWS Weather Prediction Center College Park MD
    1025 PM EDT Sat Jul 12 2025

    Areas affected...Central Texas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 130225Z - 130825Z

    SUMMARY...A serious risk of high-impact flash flooding from
    slow-moving, and locally training showers and thunderstorms will
    exist later tonight across central TX, including portions of the
    Edwards Plateau/Hill Country.

    DISCUSSION...The GOES-E Proxy Visible satellite imagery shows a
    slow-moving vort center gradually drifting east across the Concho
    Valley which overnight will eventually advance into the broader
    Hill Country region. Based on the latest CIRA-ALPW data, this
    energy is embedded within a concentrated corridor of deeper
    moisture lifting up across central TX, with strong concentrations
    seen in the 850/500 mb layer with overall values of 1.5 to 1.75+
    inches.

    Meanwhile, the airmass more broadly pooled across the Hill Country
    region is quite unstable with MLCAPE values of 1500 to 2500 J/kg.
    This instability is seen pooling along a weak surface trough out
    ahead of a stationary front, and this coupled with the arrival of
    the aforementioned vort energy along with a gradually increasing
    southerly low-level jet should help drive developing areas of
    showers and thunderstorms with high rainfall rates.

    A nocturnal tightening of the mid-level vort energy along with
    increasingly convergent flow along its southern and eastern flanks
    near the surface trough will favor convection growing gradually
    upscale, but in a very concentrated manner in a southwest to
    northeast fashion across central TX. This region will also be in
    the right-entrance region of an upper-level jet to further support
    ascent for convection.

    Rainfall rates are expected to be on the order of 2 to 4
    inches/hour with the stronger storms, and the latest HRRR/RRFS
    guidance along with support from the 18Z HREF and 12Z REFS suites
    support these rates. An excellent environment will develop later
    tonight for back-building and training convection, with slow
    cell-motions. Favorable Corfidi vectors with weak steering flow
    are expected to align that will facilitate this convective
    evolution especially after midnight.

    Some rainfall totals by 08Z (3AM CDT) may reach as high as 4 to 6+
    inches, but with additional very heavy rainfall expected after
    this time frame going through dawn. A serious risk of high-impact
    flash flooding is expected overnight across the sensitive Hill
    Country region, with dangerous and life-threatening flash flooding
    likely by later tonight. Additional MPDs will be issued
    accordingly as this event unfolds.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-vsU0WVLz01ViCzvU0W8IADj050ikoiAprjycWpwjmETEh1R9-l6PiXjrT7CyA086VM9= uubePxfcPCkndJ4HcDlFNsg$ for graphic product...

    ATTN...WFO...EWX...FWD...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32939718 32759622 32189589 31489612 30639713=20
    29949852 29579995 29690106 30260173 30930152=20
    31320091 31669989 32209880=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 08:17:59 2025
    AWUS01 KWNH 130817
    FFGMPD
    TXZ000-131415-

    Mesoscale Precipitation Discussion 0666
    NWS Weather Prediction Center College Park MD
    417 AM EDT Sun Jul 13 2025

    Areas affected...Central Texas...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 130815Z - 131415Z

    SUMMARY...Potential for significant flash flooding likely to
    continue. Additional 3-6" totals may overlap with ongoing
    flooding areas but will result in overall areal expansion of
    additional flash flooding through day break.

    DISCUSSION...GOES-E WV suite shows a strong/compact center of base
    of long wave vorticity center over north-central to northeastern
    OK. A smaller scale shortwave that was noted earlier this evening
    has sheared/elongated and expanded the positive tilt trough all
    the through the Lower Pecos River Valley into northern Coahuila.=20
    This setup has maintained a surface low along the Rio Grande near
    KDRT with a surface trof that extends northeast through the
    southern Hill Country; while the main surface low along the front
    continues to sag south toward KBKD in Northwest TX, increasing
    surface to low level response. Additionally, this surface trough
    has a 5-7 degree Td gradient along it separating moist air, from
    very moist air with Tds into the mid-70s. Broad orthogonal surface
    to 700mb has been strongly convergent along the boundary for
    clusters of elevated storms to develop with increasing moisture
    flux supporting deep warm cloud processes and efficient rainfall
    production. Combine this with the elongation of the trof helping
    to expand the entrance to the northern stream jet across N TX into
    OK maximizing divergence aloft to help maintain the outflow.

    The slightly increased confluent flow through the Colorado River
    Valley nearer the frontal wave, has rapidly matured the convection
    into a smaller MCS with a solid bowing segment along the upstream
    edge. Total PWat values in this confluent region have remained
    elevated compared to further west with totals over 2" approaching
    2.25". Given strength of convergence, occasional rates of up to
    4" have be estimated with solid 2-3" totals observed across
    Lampasas county. 500-1000mb thickness and VWP suggest propagation
    vectors will shift from south to more west-southwest counter to
    the deeper layer steering flow, allowing for some
    training/repeating convective cores. Given high likelihood of
    broader 2-3"/hr rates (with smaller isolated 4" rates),=20
    additional 3-6" are probable but a localized maximum of 8" can not
    be fully ruled out.=20

    Further west, strengthening LLJ across the southern Hill Country
    into the Concho Valley has seen a maturing cluster centered near
    Schleicher county. Slightly reduced deeper layer moisture may
    support increased cold pool generation and orientation along the
    southeastern flank of the MCV/developing 500mb wave, cell motions
    toward the south and potentially eastward into the cluster is
    possible and similar 3-6" totals are growing more likely as well.
    Concern for this cluster to shift eastward and merge with more
    mature complex could present a worse case evolution, for increased
    duration to push those isolated additional 8" totals through 15z.=20 Regardless, areal coverage of intense rainfall to induce flash
    flooding is likely and given placement to the Hill Country, a few
    locations of significant flash flooding becoming increasing
    possible.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6KYpSylRVMYazhfYAF532G8iVtKSdoFwCAPE3hEqwxDhPFRaIWf-cZTbGiaFx3PQSO_b= 0SJmW3qVqAwNKhM7uYqfMso$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32639846 32519758 32189690 31659657 31069670=20
    30699714 30389772 29729936 29630074 30280123=20
    31120092 31850015 32279948=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 11:21:44 2025
    AWUS01 KWNH 131121
    FFGMPD
    ARZ000-TXZ000-OKZ000-131620-

    Mesoscale Precipitation Discussion 0667
    NWS Weather Prediction Center College Park MD
    720 AM EDT Sun Jul 13 2025

    Areas affected...Southeast OK into Southwest AR

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 131120Z - 131620Z

    SUMMARY...Scattered flash flooding remains possible this morning
    across portions of southeast Oklahoma and adjacent areas of
    southwest Arkansas.

    DISCUSSION...Expanding convection to the southeast of a well
    defined MCV has increased in coverage and intensity early this
    morning. The environmental ingredients in place seem supportive of
    this activity persisting into the morning hours. Instability is
    marginal (MUCAPE between 500-1000 J/KG), but we do have enough of
    an upstream instability pool off to the southwest to likely
    sustain this convection. PWs are over 2", and likely have a good
    amount of warm rain processes occurring increasing rainfall
    efficiency with this activity. Deep layer mean flow is off to the
    northeast at ~20 kts, however upwind propagation vectors are
    pretty weak and pointed south. This supports some of the southward
    backbuilding of convection we have been seeing this morning. The
    latest SPC mesoanalysis also depicts a corridor of deep moisture
    convergence over this area, with both the 925mb and 850mb moisture
    transport axis pointed into the region.

    While not necessarily the strongest signal, model guidance does
    have some signs of this convective cluster. Both the latest HREF
    and REFS have modest 3" neighborhood probabilities, and the 10z
    HRRR and 08z RRFS runs now show a better training signal. None of
    the guidance show too much more upscale development of the
    activity, and by mid to late morning these type of nocturnal
    events often tend to weaken. Thus generally expecting the scale of
    activity to remain similar over the next few hours, with
    backbuilding on the south and southwest flank of the northeast
    moving area of convection. Where this backbuilding persists an
    isolated to scattered flash flood risk will continue. Hourly
    rainfall locally over 2", and total amounts upwards of 3-5" seem
    probable in spots. By mid to late morning we should start to see a
    bit less organization as low to mid level moisture convergence
    should weaken. But we will continue to monitor convective trends.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!856zXrrEKuhQJUB20WNPQjXPh7BztrRWo3UhtvEr4DSRnqAlEyegE91fC0J8mlANAhtq= J4-otM4GEF1Y25jEcS8F99g$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 35329434 35209395 34689367 34179404 33799488=20
    33689571 33609593 33919623 34149642 34469664=20
    34599681 34819656 35189587 35259483=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 14:18:36 2025
    AWUS01 KWNH 131418
    FFGMPD
    TXZ000-131916-

    Mesoscale Precipitation Discussion 0668
    NWS Weather Prediction Center College Park MD
    1017 AM EDT Sun Jul 13 2025

    Areas affected...Texas Hill Country

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 131416Z - 131916Z

    SUMMARY...The flash flood risk continue this morning across
    portions of the Texas Hill Country. The extent and magnitude of
    the event has lowered from what occurred last night into the early
    morning hours, however some additional flash flood impacts are
    likely...and localized significant impacts remain possible.

    DISCUSSION...Latest radar imagery this morning continues to show
    an axis of heavy rainfall across portions of the TX Hill Country
    resulting in areas of flash flooding. The eastern edge of this
    activity has weakened over the past couple hours, likely due to
    the low level flow becoming more parallel to the outflow resulting
    in decreased convergence. However the western area of convection
    has been able to persist, with low level inflow more perpendicular
    to this portion of the outflow. This activity has continued to
    show signs of some forward propagation off the south, which is
    having the overall effect of slightly lowering hourly and total
    rainfall magnitudes.

    Going forward the expectation is that this gradual southward
    propagation should continue as low level inflow continues to
    undergo the typical diurnal weakening. This should result in a
    gradual downward trend in the overall magnitude of the event going
    through the rest of the morning. Probabilities of exceeding 2" in
    an hour rainfall in both the 06z HREF and REFS decrease this
    morning, and that aligns with the above thinking as well. However
    1" per hour rainfall probabilities remain in the 40-70% range into
    the early afternoon hours. Given the impressive pool of
    instability to the south (within the inflow region of the
    conevction), the divergent flow at 300mb, and continued influence
    from the MCV...it makes sense that convection will persist to some
    extent into the afternoon hours as the MCS gradually shifts
    south...and recent IR cloud top cooling supports convective
    persistence.

    As mentioned above, the organization and overall rainfall
    magnitude should continue to generally decline...however that does
    not mean that locally heavier rainfall amounts will not occur.
    With PWs around 2", convection will still be capable of dropping
    1-2" in an hour...enough to cause some additional flash flood
    issue in any more vulnerable locations. In addition, some discrete
    cell development south of the convective line is probable...and
    any discrete cells that do form will likely merge with the
    convective line/cluster causing it to temporarily slow and
    increase rainfall duration. Where this occurs we could still see a
    more localized event of 2-3" per hour rainfall. So while, on
    average, most places will pick up an additional 1-3" of rain,
    localized totals of 3-5" remain possible. On a broad scale the
    flash flood risk should be less severe than what we saw overnight
    in areas just to the north...however localized more significant
    impacts remain possible.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8gqByiYBcucs14Yh5aO_qYwxa-Ejlk2hJ_puSWPpPPav2WjnkKNvfUWWLmKzXdBLFyTs= CQZCxArfO5VJQXh7Rk-bNdg$ for graphic product...

    ATTN...WFO...EWX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31150012 30859938 30799885 30859825 30659795=20
    30329774 29999758 29649796 29359830 29259870=20
    29149987 29300036 29600047 29860054 30220092=20
    30670133 31000131 31090087 31130061=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 16:28:39 2025
    AWUS01 KWNH 131628
    FFGMPD
    INZ000-ILZ000-MOZ000-132227-

    Mesoscale Precipitation Discussion 0669
    NWS Weather Prediction Center College Park MD
    1228 PM EDT Sun Jul 13 2025

    Areas affected...Eastern MO into central and southern IL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 131627Z - 132227Z

    SUMMARY...Expanding convection will lead to an isolated to
    scattered flash flood risk over portions of eastern Missouri into
    central and southern Illinois this afternoon.

    DISCUSSION...Troughing with an elongated area of vorticity
    stretches from central OK into western IL, with some more
    mesoscale MCV features likely embedded within. Latest radar and
    satellite indicates one such feature currently moving across
    central MO and possibly another near the AR/MO border...and these
    will likely help drive an expansion of convection and at least
    some flash flood risk as we head into the afternoon hours. The
    initial focus will likely be near the MCV center over northeast
    MO, and then extending eastward near the stationary front into
    central IL. PWs are near 2", and the activity thus far is fairly
    low topped (per IR imagery), and thus we are likely getting some
    efficient warm rain processes. Given the slow cell motions near
    the MCV and along the front...these cells could locally produce
    upwards of 1-3" of rain per hour as convection intensifies over
    the next couple hours.

    Both the 12z HREF and 06z REFS show an uptick in the coverage of
    1" per hour probabilities after 18z from eastern MO into
    central/southern IL...with neighborhood probabilities over 60%
    covering much of the MPD area. Two inch per hour probabilities are
    lower, but still notable...around 40% in the HREF and as high as
    80% in the REFS. Continued destabilization ahead of the trough/MCV
    and broad upper level divergence will help drive this increase in
    convective coverage after 18z. Deep layer mean flow is out of the
    southwest around 20kts...so cells will be fairly quick moving.
    However guidance indicates an increase in the low level jet as we
    head through the afternoon...which acts to decrease upwind
    propagation speeds, and turn the vectors more south to even
    southwesterly. This suggests that as convection increases in
    coverage and attempts to grow upscale this afternoon we could see
    some backbuilding on the south to southwest flank of convection.
    This potential training of convection should locally increase
    rainfall magnitudes this afternoon...especially across central to
    southern IL...where some areas will likely exceed 3". The
    probability of exceeding 5" in both the HREF and REFS drops significantly...likely due to the overall progressive nature of
    the system. Thus generally expecting event total rain to peak in
    the 2-4" range...with any 5" amounts staying localized. This
    amount of rain should be enough to cause isolated to scattered
    instances of flash flooding.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!51BI0SB5L9_79E_F-QFPZqaZnOJVlXwNJ9hAlaEzj2a1hbkQLyR9hckdEbv1TJdF3Lz8= -xmejjGsmumixDQUEbXGrlo$ for graphic product...

    ATTN...WFO...EAX...ILX...IND...LSX...PAH...SGF...

    ATTN...RFC...KRF...MSR...ORN...TIR...NWC...

    LAT...LON 40258848 40238782 39998747 38498762 37598865=20
    37408922 37319018 37699127 38429185 38929239=20
    39379263 39829223 40029154 40089071 40208958=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 17:06:39 2025
    AWUS01 KWNH 131706
    FFGMPD
    PAZ000-MDZ000-VAZ000-DCZ000-132205-

    Mesoscale Precipitation Discussion 0670
    NWS Weather Prediction Center College Park MD
    105 PM EDT Sun Jul 13 2025

    Areas affected...Mid Atlantic

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 131705Z - 132205Z

    SUMMARY...Scattered convection along a weak convergence axis will
    likely result in localized instances of flash flooding this
    afternoon.

    DISCUSSION...Recent IR imagery shows cooling cloud tops along a
    weak convergence axis from southeast VA into south central PA.
    MLCAPE ranges from 1500-2500 J/KG along this corridor, with PWs
    near or above 2". This environment is supportive of efficient warm
    rain processes and expect heavy rainfall rates from these cells.
    Not much large scale forcing or deep layer shear to organize
    convection, so activity will primarily be of pulse nature. This
    will likely limit the coverage of the flash flood risk...however
    seeing enough deep growth and coverage to indicate that some cell
    mergers will occur. Where these mergers occur we will likely see
    just enough persistence of these higher rainfall rates to drive a
    flash flood risk. Hourly rainfall could exceed 2" in this
    environment with any cold pool/merger driven persistence...and
    this will be enough to result in localized instances of flash
    flooding.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_QempPqepK1gD3dQKOxoDnQpyunXGUFQ7O0U_N9j6EOFOR2ZJFoAqNxK3lVR2SW2tjWH= qOMHApoiXj0ZQmKZPZPKp4I$ for graphic product...

    ATTN...WFO...AKQ...CTP...LWX...

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 40177711 40037665 39057642 37897651 37737642=20
    37367659 37207700 37227746 37527763 37997751=20
    39287714 39767735=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 17:57:44 2025
    AWUS01 KWNH 131756
    FFGMPD
    PAZ000-MDZ000-VAZ000-NCZ000-WVZ000-TNZ000-132355-

    Mesoscale Precipitation Discussion 0671
    NWS Weather Prediction Center College Park MD
    155 PM EDT Sun Jul 13 2025

    Areas affected...Central Appalachians and Mid-Atlantic Piedmont

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 131755Z - 132355Z

    SUMMARY...Scattered showers and thunderstorms with very heavy
    rainfall rates will continue to develop and expand in coverage.
    Isolated to scattered areas of flash flooding will be possible
    going through the afternoon and into the evening hours.

    DISCUSSION...The latest GOES-E GeoColor RGB satellite imagery
    shows convection continuing to initiate and expand in coverage
    across portions of central NC through southwest and western VA.
    There will be additional areas of heavy showers and thunderstorms
    that will gradually develop further back across the central
    Appalachians with an expansion generally north near and west of
    the Blue Ridge including areas of eastern WV through western VA,
    the MD/WV Panhandles and large areas of southwest and central PA.

    Given strong diurnal heating near and adjacent to the terrain,
    MLCAPE values have increased to 1000 to 2000+ J/kg. Meanwhile, the
    column is very moist with the 12Z IAD RAOB showing a 2.14" PW and
    and a tall skinny CAPE profile that is strongly suggestive of
    warm/tropical rain processes. This will support enhanced rainfall
    rates with any thunderstorm activity this afternoon and this
    evening.

    Terrain-driven circulations/orographics and differential heating
    boundaries will tend to support a substantial amount of terrain
    focused convection over the next several hours given the level of
    moisture and instability in the column, but areas farther east
    over the Piedmont may also see convection become locally more
    expansive by later this afternoon. This will includes areas of
    central NC around the Raleigh-Durham area where a cluster of
    storms is noted just east of the city.

    Rainfall rates will be capable of reaching 2 to 3 inches/hour with
    the stronger storms, and with slow cell-motions, some spotty storm
    totals of 3 to 4+ inches will be possible by this evening. This is
    consistent with some of the 12Z HREF guidance.

    Isolated to scattered areas of flash flooding will be possible,
    and this will include areas of locally rugged terrain near the
    central Appalachians/Blue Ridge and also around any urbanized
    corridor that sees convection.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8y_Bz5FPdkJtHBQI6SyGqza8Qrc3tLsvrmHvhwBr1ULJtCfbA6dCsWOm08OE3uUlYMmw= 0L20HlyC8s7U2AwVw2-F9h0$ for graphic product...

    ATTN...WFO...AKQ...BGM...CTP...GSP...LWX...MHX...MRX...PBZ... RAH...RLX...RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 41977730 41677671 39997736 39247725 38537739=20
    37677744 36937667 35517739 35517855 36037966=20
    36088062 36298229 37008256 38068089 39397954=20
    40887868 41767804=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 18:03:10 2025
    AWUS01 KWNH 131802
    FFGMPD
    NYZ000-PAZ000-140000-

    Mesoscale Precipitation Discussion 0672
    NWS Weather Prediction Center College Park MD
    200 PM EDT Sun Jul 13 2025

    Areas affected...Central and Western New York State

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 131800Z - 140000Z

    SUMMARY...Scattered to widespread thunderstorms will increase the
    likelihood of flash flooding across central and western New York
    state through the afternoon and early evening.

    DISCUSSION...General focus for heavy convection for the afternoon
    and evening will reside across New York state with increasing
    thunderstorm coverage from southwest to northeast, west of the
    Hudson/Mohawk Valley's. Strong theta_E advection ahead of an
    advancing cold front has led to broad environmental
    destabilization within a warm sector positioned ahead of the
    analyzed cold front migrating eastward over neighboring Canada.
    PWATs running between 1.75-2.1" across western NY state were
    verified this morning via 12z KBUF sounding of 1.95", implicating
    a daily max for the site location. MUCAPE between 1500-2500 J/kg
    will be centered across much of western NY, plentiful
    thermodynamics to generate heavy convective cores capable of
    1-2+"/hour rates with some intra-hour rates approaching 3-4"/hr in
    spots.

    A secondary area of focus may occur right along the southern and
    southeast shores off Lake Ontario where HRRR/RRFS CAMs are
    indicating a lake breeze convergence area where cells could
    materialize and become anchored to the boundary. This would allow
    for very slow-moving convection to enhance heavy rain threats just
    off the lake shore this afternoon. Anywhere across western and
    central NY could see totals eclipse 2" with the 12z HREF
    neighborhood probs depicting a 60-90% bullseye for at least 2"
    located from the Tug Hill back through the eastern Finger Lakes to
    the NY/PA state line. Considering lower FFG's from previous
    convective patterns, this signal is high enough to warrant a flash
    flooding likely tag for the convective threat.

    Cells will migrate eastward later this evening with more potential
    downstream pending cold pool progression and convergence, so the
    end of the period of impact will be something to monitor.

    Kleebauer

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-3VGF7Lr6gyWyadzAlz6ZmP7XvxGYIiAsIxQJEo0lmQ80XKRc9nnV5msQ3rtoZ3eF4ZE= SvrLTAXDCjfva91um0Khmtw$ for graphic product...

    ATTN...WFO...ALY...BGM...BTV...BUF...CTP...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 44807517 44697474 44377454 43807419 43437439=20
    43177458 42927483 42677516 42507532 42217563=20
    42027589 41927628 41997689 42097735 42317769=20
    42577781 42817793 42997790 43187772 43247760=20
    43267743 43277720 43307716 43277699 43317684=20
    43467652 43567629 43687620 43867626 44047631=20
    44157635 44377602 44447592 44577575 44707547=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 18:59:40 2025
    AWUS01 KWNH 131859
    FFGMPD
    TXZ000-COZ000-NMZ000-140058-

    Mesoscale Precipitation Discussion 0673
    NWS Weather Prediction Center College Park MD
    258 PM EDT Sun Jul 13 2025

    Areas affected...Far Southern CO...Much of Central and Eastern
    NM...Southwest TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 131858Z - 140058Z

    SUMMARY...Scattered showers and thunderstorms will develop and
    gradually expand in coverage across the higher terrain of far
    southern CO down through central NM and into southwest TX.
    Isolated to scattered areas of flash flooding will be possible
    which will include concerns to the normally dry washes and any
    burn scar locations.

    DISCUSSION...The midday GOES-W Day Cloud Phase RGB satellite
    imagery shows convective intiation taking place across far
    southern CO and north-central NM involving the Sangre De Cristo
    Mountains. The airmass continues to destabilize across the region
    with strong diurnal heating near the eastern slopes of the
    terrain, with MLCAPE values across eastern NM and southwest TX on
    the order of 1500 to 2500 J/kg. Moist low-level east to southeast
    flow will continue through the afternoon hours and this will
    contribute to a favorable upslope flow pattern for convection to
    develop and expand over the terrain going through the afternoon
    hours.

    ML-LightningCast data is showing a likelihood for convective
    initiation soon farther south across the broader Sangre De Cristo
    Range, and also across the Sacramento Mountains. The convective
    threat to the Sacramento Mountains in south-central NM and also
    the Davis Mountains of southwest TX for this afternoon will also
    have some support from a slow-moving shortwave impulse which is
    showing up in the GOES WV satellite imagery.

    PWs are near normal for this time of the year, but with strong
    instability pooling near the terrain and also orographically
    focused lift/upslope flow, heavy showers and thunderstorms will be
    developing and expanding in coverage over the next several hours.

    Rainfall rates of 1 to 2 inches/hour will be expected with the
    stronger storms. However, with some concerns for slow cell-motions
    and terrain-anchored convection, some 2 to 3+ inch rainfall
    amounts will be possible by late this afternoon.

    These rains will drive a threat for isolated to scattered areas of
    flash flooding, which will include potential impacts to the
    normally dry washes, and especially any burn scar locations. This
    will include the highly sensitive Sacramento Mountain burn scar
    complex made up of the Blue-2, South Fork, Salt and McBride burn
    areas. Also, the Hermits Peak/Calf Canyon and Cooks Peak burn scar
    areas in the Sangre De Cristo Mountains may be impacted.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7TYVzpMUj8qEwwABK5vFibCqFN3KeXSUi0chtdknG-no_Jg7-siQObpZDBpySAp96bwg= 7tl9dH4BxS2CXsmBZy9TBqc$ for graphic product...

    ATTN...WFO...ABQ...EPZ...GJT...MAF...PUB...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 37890573 37740467 36720390 34260364 31950395=20
    31170464 31220581 31860651 32990697 34930725=20
    36940681=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 21:18:39 2025
    AWUS01 KWNH 132118
    FFGMPD
    NMZ000-AZZ000-140230-

    Mesoscale Precipitation Discussion 0674
    NWS Weather Prediction Center College Park MD
    517 PM EDT Sun Jul 13 2025

    Areas affected...Southeast AZ...West-Central to Southwest NM

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 132116Z - 140230Z

    SUMMARY...Showers and thunderstorms will continue to expand in
    coverage going through the afternoon and early evening hours
    across west-central to southwest NM and southeast AZ. While
    isolated to scattered in coverage, flash flooding will be likely
    for the more sensitive dry washes and burn scar locations,
    including the Trout burn scar.

    DISCUSSION...Monsoonal moisture is gradually becoming better
    established across portions of the Southwest U.S., and this
    moisture along with favorable instability and some northeasterly
    shear will favor scattered thunderstorms going through the
    remainder of the afternoon and early evening hours.

    PWs overall are near normal with values of 0.75 to 1.25 inches
    across the region, but SBCAPE values are on the order of 1000 to
    1500+ J/kg which may tend to increase a bit further over the next
    few hours given strong diurnal heating.

    A belt of stronger northeasterly mid-level flow is flow is
    promoting some effective bulk shear values of 20 to 30 kts, and
    this coupled with the instability and localized areas of
    orographic ascent/terrain enhancement is already yielding some
    areas of showers and thunderstorms.

    Over the next few hours, there may be some additional upscale
    growth and organization of the cells as they evolve down to the
    southwest across southwest NM and through southeast AZ. Rainfall
    rates of 1 to 1.5 inches/hour will be possible with the stronger
    storms, and while they will be rather progressive, there may be
    some spotty 2+ inches totals where any cells tend to be more
    focused near areas of higher terrain.

    Flash flooding will be likely for the more senstive dry washes
    where these thunderstorms organize, and there will be notable
    concerns for the more recent burn scar locations as well for
    impacts including the Trout burn scar in southwest NM which is
    currently being impacted by heavy rainfall and is under a Flash
    Flood Emergency.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4uTOcF1wcKbQSWrzmbrYtwIwNQnVFasIyoXAJmGB5YYGR1gqmW-GGLLdBnPt2lqYHGa6= 4jCcDGI8FfTKHAruKL4uFp4$ for graphic product...

    ATTN...WFO...ABQ...EPZ...FGZ...TWC...

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 34380816 34190757 33520733 32520754 31840810=20
    31380877 31260996 31301119 31551153 31951147=20
    32421077 32991027 33420993 33860945 34210887=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 21:33:38 2025
    AWUS01 KWNH 132132
    FFGMPD
    NMZ000-AZZ000-140230-

    Mesoscale Precipitation Discussion 0675...Corrected
    NWS Weather Prediction Center College Park MD
    531 PM EDT Sun Jul 13 2025

    Corrected for Discussion Wording

    Areas affected...Southeast AZ...West-Central to Southwest NM

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 132116Z - 140230Z

    SUMMARY...Showers and thunderstorms will continue to expand in
    coverage going through the afternoon and early evening hours
    across west-central to southwest NM and southeast AZ. While
    isolated to scattered in coverage, flash flooding will be likely
    for the more sensitive dry washes and burn scar locations,
    including the Trout burn scar.

    DISCUSSION...Monsoonal moisture is gradually becoming better
    established across portions of the Southwest U.S., and this
    moisture along with favorable instability and some northeasterly
    shear will favor additional areas of scattered thunderstorms going
    through the remainder of the afternoon and early evening hours.

    PWs overall are near normal with values of 0.75 to 1.25 inches
    across the region, but SBCAPE values are on the order of 1000 to
    1500+ J/kg which may tend to increase a bit further over the next
    few hours given strong diurnal heating.

    A belt of stronger northeasterly mid-level flow is promoting some
    effective bulk shear values of 20 to 30 kts, and this coupled with
    the instability and localized areas of orographic ascent/terrain
    enhancement is already yielding areas of heavy showers and
    thunderstorms.

    Over the next few hours, there may be some additional upscale
    growth and organization of the cells as they evolve down to the
    southwest across southwest NM and through southeast AZ. Rainfall
    rates of 1 to 1.5 inches/hour will be possible with the stronger
    storms, and while they will be rather progressive, there may be
    some spotty 2+ inches totals where any cells tend to be more
    focused near areas of higher terrain.

    Flash flooding will be likely for the more sensitive dry washes
    where these thunderstorms organize, and there will be notable
    concerns for the more recent burn scar locations as well for
    impacts. Thus will include the Trout burn scar in southwest NM
    which is currently being impacted by heavy rainfall and was
    recently put under a Flash Flood Emergency.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4AqfKHwR8k-dJGctuHZU3MhWlbfxYg5rCKbBrVQ-rYgqw39yuBRZlOC2Uko-zWCwczBw= X6XJAr-ynjMiZ0iqBEXrtv0$ for graphic product...

    ATTN...WFO...ABQ...EPZ...FGZ...TWC...

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 34380816 34190757 33520733 32520754 31840810=20
    31380877 31260996 31301119 31551153 31951147=20
    32421077 32991027 33420993 33860945 34210887=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 21:34:39 2025
    AWUS01 KWNH 132134
    FFGMPD
    NMZ000-AZZ000-140230-

    Mesoscale Precipitation Discussion 0674...Corrected
    NWS Weather Prediction Center College Park MD
    533 PM EDT Sun Jul 13 2025

    Corrected for Discussion Wording

    Areas affected...Southeast AZ...West-Central to Southwest NM

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 132116Z - 140230Z

    SUMMARY...Showers and thunderstorms will continue to expand in
    coverage going through the afternoon and early evening hours
    across west-central to southwest NM and southeast AZ. While
    isolated to scattered in coverage, flash flooding will be likely
    for the more sensitive dry washes and burn scar locations,
    including the Trout burn scar.

    DISCUSSION...Monsoonal moisture is gradually becoming better
    established across portions of the Southwest U.S., and this
    moisture along with favorable instability and some northeasterly
    shear will favor additional areas of scattered thunderstorms going
    through the remainder of the afternoon and early evening hours.

    PWs overall are near normal with values of 0.75 to 1.25 inches
    across the region, but SBCAPE values are on the order of 1000 to
    1500+ J/kg which may tend to increase a bit further over the next
    few hours given strong diurnal heating.

    A belt of stronger northeasterly mid-level flow is promoting some
    effective bulk shear values of 20 to 30 kts, and this coupled with
    the instability and localized areas of orographic ascent/terrain
    enhancement is already yielding areas of heavy showers and
    thunderstorms.

    Over the next few hours, there may be some additional upscale
    growth and organization of the cells as they evolve down to the
    southwest across southwest NM and through southeast AZ. Rainfall
    rates of 1 to 1.5 inches/hour will be possible with the stronger
    storms, and while they will be rather progressive, there may be
    some spotty 2+ inches totals where any cells tend to be more
    focused near areas of higher terrain.

    Flash flooding will be likely for the more sensitive dry washes
    where these thunderstorms organize, and there will be notable
    concerns for the more recent burn scar locations as well for
    impacts. Thus will include the Trout burn scar in southwest NM
    which is currently being impacted by heavy rainfall and was
    recently put under a Flash Flood Emergency.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5BSXalywof6p7tAWkk8HIo1Lie-JyVANkNowwPE7tm5Wn15FBHLzH-42tJqXKMxEVZ3K= 2UGCWorheo2uDxx7MAw5ibM$ for graphic product...

    ATTN...WFO...ABQ...EPZ...FGZ...TWC...

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 34380816 34190757 33520733 32520754 31840810=20
    31380877 31260996 31301119 31551153 31951147=20
    32421077 32991027 33420993 33860945 34210887=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jul 13 22:11:40 2025
    AWUS01 KWNH 132211
    FFGMPD
    OHZ000-KYZ000-INZ000-ILZ000-140410-

    Mesoscale Precipitation Discussion 0675
    NWS Weather Prediction Center College Park MD
    610 PM EDT Sun Jul 13 2025

    Areas affected...Portions of the OH Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 132210Z - 140410Z

    SUMMARY...Heavy showers and thunderstorms will continue to impact
    portions of the OH Valley going through the evening hours.
    Isolated to scattered areas of flash flooding will continue to be
    possible, and especially around the more urbanized locations.

    DISCUSSION...GOES-E IR satellite imagery shows cold convective
    tops associated with heavy showers and thunderstorms across
    southeast IL and portions of central and southern IN. The activity
    remains focused ahead of a well-defined mid-level vort
    center/shortwave trough and an accompanying area of surface low
    pressure which is transiting a frontal zone.

    MLCAPE values over the Lower OH Valley are generally on the order
    of 1500 to 2500 J/kg, and this coupled with anomalous PWs of 2.0
    to 2.25 inches will continue to favor very high rainfall rates
    that will be capable of reaching 2 to 3 inches/hour.

    Generally the convection should continue to advance off to the
    east, but there will be some relatively slow cell-motions, and
    pockets of localized cell-training and cell-merger activity that
    may allow for some rainfall totals to reach as high as 3 to 4+
    inches by late this evening.

    This is supported by a consensus of the 18Z HREF and 12Z REFS
    guidance. However, the latest hires guidance does appear to be a
    bit slow with the overall downstream convective evolution. Based
    on the latest satellite and radar trends, convection should
    advance across southern IN and into western OH by late-evening.

    Given the high rainfall rates and localized concerns for
    cell-training, isolated to scattered areas of flash flooding will
    continue to be possible. This will include concerns for the more
    sensitive urbanized locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5_ri_5eVgeS_6htc7prUzwCPNhkQFuMjZP2SCTLEwVM6HyKwWangoP03GnMiaTHmhg7C= kDOZOqey_3Hd2rsZC-VhUX4$ for graphic product...

    ATTN...WFO...CLE...ILN...ILX...IND...IWX...LMK...LSX...PAH...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 40928345 40288258 39458270 38548417 37838724=20
    38068854 38868916 39688827 40588572=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 00:16:12 2025
    AWUS01 KWNH 140016
    FFGMPD
    VTZ000-NYZ000-NJZ000-PAZ000-MDZ000-VAZ000-DCZ000-WVZ000-140613-

    Mesoscale Precipitation Discussion 0676
    NWS Weather Prediction Center College Park MD
    813 PM EDT Sun Jul 13 2025

    Areas affected...Portions of the Central
    Appalachians...Mid-Atlantic into the Northeast

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 140013Z - 140613Z

    SUMMARY...Scattered areas of heavy showers and thunderstorms will
    continue through the remainder of the evening and parts of the
    overnight period. Isolated to scattered areas of flash flooding
    will remain possible with some of the stronger storms given high
    rainfall rates.

    DISCUSSION...The early evening GOES-E IR satellite imagery shows a
    few broken clusters of heavy shower and thunderstorm activity
    continuing to impact portions of eastern WV and western VA up
    through central PA and through central/eastern NY and northern VT.
    This elongated axis of lingering convection is being highly driven
    by a combination of orographics/terrain-forcing and lingering
    instability with MLCAPE values still of 1500 to 2000+ J/kg.
    Additionally, the activity up PA/NY and VT is being aided by some
    very modest shear associated with some weak shortwave energy
    arriving from the Upper OH Valley and Lower Great Lakes region.

    A corridor of favorable moisture convergence is seen lingering up
    across areas of western VA through central PA and into southern
    and eastern NY in particular, and this may allow for some of the
    ongoing convection to linger over the next several hours, and
    especially with localized upslope flow near the terrain and the
    aforementioned pool of instability.

    The last few runs of the HRRR/RRFS and the 18Z HREF guidance
    suggest additional areas of convection going through the remainder
    of the evening hours will be capable of producing rainfall rates
    of 1 to 2 inches/hour. This is highly supported by the latest
    CIRA-ALPW data which shows deep concentrations tropical
    moisture/high PWs across the central Appalachians, Mid-Atlantic
    and interior of the Northeast.

    Some additional spotty 2 to 4 inch rainfall amounts will be
    possible going through midnight. This coupled with locally wet
    antecedent conditions will support a threat for some additional
    isolated areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_vyV8KW6PlhQPaRxwqolFMjjCdvJN_n2O5HgMsSHK1W2zeCJKtrpMJW01hGWTL3GoWa6= 4DYItdZ_h6q_Z_6UiJq3p-4$ for graphic product...

    ATTN...WFO...AKQ...ALY...BGM...BTV...CTP...LWX...OKX...PBZ... PHI...RLX...RNK...

    ATTN...RFC...ALR...RHA...TAR...TIR...NWC...

    LAT...LON 45157252 44877185 43627260 42027431 40657530=20
    39117687 37527816 36927916 37157999 38377978=20
    40197851 41837751 42617651 43147559 44447414=20
    44927346=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 01:52:17 2025
    AWUS01 KWNH 140152
    FFGMPD
    TXZ000-140750-

    Mesoscale Precipitation Discussion 0677
    NWS Weather Prediction Center College Park MD
    950 PM EDT Sun Jul 13 2025

    Areas affected...Portions of the TX Hill Country and South-Central
    TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 140150Z - 140750Z

    SUMMARY...Showers and thunderstorms may expand in coverage over
    the next several hours. Very heavy rainfall rates and slow
    cell-motions will be possible, and this may result in some areas
    of flash flooding.

    DISCUSSION...Early evening GOES-E IR satellite imagery along with
    recent radar trends shows developing areas of showers and
    thunderstorms across portions of south-central TX close to the Rio
    Grande River. Some weak vort energy is appearing in satellite data
    across northern Mexico which is slowly drifting off to the
    northeast toward south-central TX.

    An unstable airmass is pooled up across much of the Lower Rio
    Grande Valley with moist southeast low-level flow in place, and a
    moderate to strongly unstable boundary layer. MLCAPE values of
    1500 to 2500+ J/kg are noted in the latest RAP analysis, and this
    vort energy encroaching on south-central TX and at least some
    portions of the TX Hill Country may support some expansion of
    heavy shower and thunderstorm activity over the next several hours.

    PWs across the region are very moist with values of 1.8 to 2.2
    inches. This coupled with the instability should favor high
    rainfall rates reaching as high as 2 to 3 inches/hour with any of
    the stronger and more organized convective cells that do
    materialize.

    The latest hires model guidance is rather inconsistent on the
    timing and placement of the heaviest rainfall potential going into
    the overnight hours, but the ingredients are in place for some
    expansion of the convective threat over the next several hours.

    Some spotty rainfall totals going through 06Z (1AM CDT) may reach
    3 to 5 inches. Some areas of flash flooding will be possible as a
    result.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8g0PQHQdbi42sQGIWkX8l_h0AujRdGSVhZQoq0Ui6M95LJyg6xrd_H7f9kUFN3JeHHB3= EgcRfzeE6AbNN_jsiCe-fYA$ for graphic product...

    ATTN...WFO...CRP...EWX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30230034 29969934 29199870 28039887 27669962=20
    28090028 28460050 29140085 29740150 30100135=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 04:11:10 2025
    AWUS01 KWNH 140409
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-140830-

    Mesoscale Precipitation Discussion 0678
    NWS Weather Prediction Center College Park MD
    1208 AM EDT Mon Jul 14 2025

    Areas affected...Southeast MO...Southern IL...Western KY...Far
    Southwest IND

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 140410Z - 140830Z

    SUMMARY...Slow moving, highly efficient cells pose localized
    totals of 2-3" in 1-2 hrs. Isolated potential for some repeating
    may result in isolated higher amount. Small areal flash flooding
    may be possible overnight.

    DISCUSSION...As the core of the broader long-wave trough shifts
    through the Middle Ohio River Valley, the remaining narrower
    positive tilt trough extends upstream through the Ozark Plateau
    into Texas. A stronger shortwave is approaching with a surge of
    deeper layer moisture and is forcing newer scattered convection
    along the northern nose of the surge across NE AR attm. A weaker,
    shallower shortave or shear axis can be seen in the 925-850mb
    layer across S IL with a pool of enhanced deep layer moisture
    between 2-2.25" of total PWats and weakly capped MLCAPE of
    1000-1500 J/kg. Speed convergence and weak WAA has sprouted a few
    shallow thunderstorms with 13-14Kft of warm cloud to support
    efficient collision and coalesence processes for efficient
    tropical showers with 2-3"/hr rates. Deep layer steering is a tad
    weak in the wake of the exiting stronger wave across OH, and is
    fairly parallel to the warm conveyor belt that is along SE MO into
    the Lower Ohio River valley. This may allow for a random
    intersection for repeating that may result in a localized 3"+
    maximum over a 2-3 hour period (as noted in N Cape Girardeau
    county), but the more likely concern is scattered to widely
    scatterd 2-3" in 30-60 minutes totals across S IL into SE IND.

    Expanding convective activity across NE AR, is likely to expand
    northeastward along the warm conveyor belt into SE MO and W KY,
    with similar lower end/focused FF concerns; but there is enough
    organization (given 20kts of effective bulk shear) for an isolated
    or widely scattered incident or two of localized flash flooding
    through 08z within the area of concern.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9zpE4-zpBzhjoCKBMpTL6MlaYvLi3lJ39Hl3pCuXyvi_e16wEv2lqj8nxS8VvDQyWPrA= ffGqf-8ZWGoDrMZQfURncTw$ for graphic product...

    ATTN...WFO...LSX...LZK...MEG...PAH...

    ATTN...RFC...MSR...ORN...TIR...NWC...

    LAT...LON 38379008 38378869 38348756 38178705 37758712=20
    36828825 36108924 35529012 35459061 35729104=20
    36209103 36709081 37099056 37459068 37589095=20
    38139079=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 05:17:02 2025
    AWUS01 KWNH 140515
    FFGMPD
    NYZ000-NJZ000-PAZ000-141000-

    Mesoscale Precipitation Discussion 0679
    NWS Weather Prediction Center College Park MD
    114 AM EDT Mon Jul 14 2025

    Areas affected...Eastern PA...Southern Upstate NY...Northwest
    NJ...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 140515Z - 141000Z

    SUMMARY...Slowly decaying MCS in proximity to complex terrain
    continues to pose flash flooding risk through overnight period.

    DISCUSSION...Regional RADAR mosaic depicts a SW to NE convective
    line across the Poconos Mtns continuing a slow eastward
    advancement, as MCV peels off northeastward into the lower Mohawk
    Valley. While the peak of heating/intensity is likely in the
    past, the downstream environment across E PA/Delaware Valley
    remains favorable to maintain convective activity with slow
    weakening still likely. RAP, VWP, CIRA LPW analysis notes solid
    return moisture channel across the Mid-Atlantic into the Delaware
    Valley becoming increasingly confluent with southwesterly warm
    conveyor belt out of the Ohio Valley and through the Allegheny
    Plateau. This has brought a very deep, rich moisture environment
    with total PWat values of 2-2.2" feeding on 10-15kts of confluent
    inflow. Fluxed air remains unstable and generally uncapped south
    of the NY and PA/NJ common border with MLCAPEs of 500-1000 J/kg,
    though fingers of elevated MUCAPE to 500 J/kg still remains across
    the Hudson River Valley but is more capped and is probable for the
    reasoning of the erosion of convective activity toward the north;
    while updrafts remain solid strong further south. IR tops still
    cooling through -60C and additional cells southward are likely to
    maintain through at least the next few hours even as inflow
    continues to weaken.=20=20

    Given total moisture and vigor to updrafts, moisture flux to the
    cells will continue to support rates of 1.5"/hr; occasionally
    upticking toward 1.75-2" where some inter-band repeating/training
    occurs given cell motion is northeast fairly parallel to the
    orientation of the line. Propagation to the south and southeast
    will limit those durations and localized totals of 2-3" remain
    possible. Complex/steep terrain of the Poconos, Catskills and
    rugged NW NJ will remain at enhanced risk of excessive runoff and
    likely incidents of flash flooding especially early (next 1-3
    hours), slowly reducing in magnitude/coverage by 08-10z across far
    Southern NY/NE NJ with a much lower probability of reaching the
    NYC Metro area by dawn.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-8TNeizDRaGNTuUN8OgUHx18i-ulK-8JOYVz9fTaaWmQ1mktISlsOm2tyhw4yW02dzkd= raXMjYG0lrDLBmYIDsZFQws$ for graphic product...

    ATTN...WFO...ALY...BGM...CTP...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 42447436 42217381 41747376 41297403 40967430=20
    40707458 40417495 40007573 40217652 40657675=20
    41157657 41887580 42407509=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 07:17:00 2025
    AWUS01 KWNH 140715
    FFGMPD
    TXZ000-141230-

    Mesoscale Precipitation Discussion 0680
    NWS Weather Prediction Center College Park MD
    315 AM EDT Mon Jul 14 2025

    Areas affected...Heart of Texas...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 140715Z - 141230Z

    SUMMARY...Slow moving, efficient shallow convection near compact
    mid-level circulation may result in localized 2-4" pockets over
    wet grounds, posing small localized incidents of possible flash
    flooding.

    DISCUSSION...KFWS and GOES-E 3.9um SWIR loop shows shallow but
    organized line of convection across Hamilton to Hill county, TX
    along the south and southwest quadrants of a 700-500mb vorticity
    center. VWP suite depicts this elongated wave well, including the
    increase of 925-850mb slightly veered profile with 20-30kts of
    increased flow. Speed convergence along remnant boundary is
    providing sufficient isentropic ascent along the northern MUCAPE
    gradient with values of 500-1000 J/kg and deep layer moisture
    (pooled below 700mb per CIRA LPW) at or above 2". Fairly deep
    warm cloud processes still have been producing 2-3"/hr rates and
    given steering from 850-500mb is generally parallel or along-track
    of the convergence boundary toward the center of the vorticity
    center near the Dallas/Fort Worth Metro (per satellite imagery);
    spots of quick 3-5" are possible over the next few hours. Given
    heavy rainfall/saturated grounds, FFG values from Ellis to San
    Saba county are less than 2"/hr. As such, localized flash
    flooding is considered possible over the next few hours.

    Uncertainty lies upstream across the Colorado River Valley;
    surface to 850mb low level jet is less orthogonal to the deeper
    layer shear axis aloft and almost parallel. However, the
    anticyclonic turning of the LLJ responding to the mid-level
    vorticity center may have some convergence along the eastern side
    of the LLJ and support back-building toward the southwest of the
    ongoing convective line. Coverage should be more scattered in
    nature IF cells do develop, but given even higher ground
    sensitivity due to last evening's convection, have included it in
    the area of concern though with a much lower probability and
    higher uncertainty factor. An upstream MPD should be forthcoming
    for the southern Edwards Plateau and Rio Grand Valley of
    South-Central Texas.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9FiLunkAP7cXHmrMlQw2X0ShssTBCppDAUZJgaWvIN9k2j9b9jWmY53DmDoI19pPv7l-= STqkBEJQuH_Xr7-CKh6I4LU$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32979705 32829619 32269581 31669621 31249670=20
    30789811 30849875 31219892 31779873 32519798=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 07:47:02 2025
    AWUS01 KWNH 140746
    FFGMPD
    TXZ000-141300-

    Mesoscale Precipitation Discussion 0681
    NWS Weather Prediction Center College Park MD
    346 AM EDT Mon Jul 14 2025

    Areas affected...South-Central Texas...Southern Edwards Plateau...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 140745Z - 141300Z

    SUMMARY...Continued flash flooding risk through dawn given strong
    moisture flux and slow moving/potentially training convection.

    DISCUSSION...GOES-E WV suite shows stubborn elongated mid-level
    trough axis across North Texas into the Hill Country and
    eventually into the South-central Texas Rio Grande Valley.=20
    Earlier convective complex developed an MCV currently located
    along the Rio Grande just west of NW Kinney county; the outflow
    boundary has kicked eastward and while generally parallel to
    strengthening LLJ (15-20kts), some weak backed flow is providing
    sufficient convergence along the upwind edge to develop
    north-south bands of convection within the remaining 1500-2000
    J/kg of MLCAPE well along the eastern hemishpere of the larger
    mid-level circulation just NW of the MCV over the NE Serrania del
    Burro Range. Northward expansion of the convection is expected
    given solid speed convergence into the deeper SW to NE shear axis.
    Total PWats of 2-2.25" will support efficient rainfall production
    with rates of 2-3" likely; while initially narrow, broadening of
    the updrafts should come with storm scale enhancement/interaction.
    The back-building, south to north training may even allow for
    some narrow areas of 3-5" totals, which may spread north into
    Real/Bandara counties with time and perhaps with low confidence
    even toward lower FFG values in the southern Edwards Plateau/Hill
    Country from Sutton to Kimble county.

    Strong latent heat release into the mid-levels should support
    strengthening of mid-level height-falls and tightening of the
    vorticity center westward. This should back low-level flow and
    increased convergence back westward away from the southern Hill
    country toward Kerr, Gillespie counties and sparing the more
    sensitive areas, reducing low level convergence in that area and
    therefore from potential of the strongest cells/highest rates.=20
    However, there is enough suggestion a few showers/cells could
    reach these areas and so are included at much lower confidence
    toward flash flooding incidents in those areas...however, at the
    cost of increased totals further west over higher FFG values/drier
    soil conditions.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9y8oeFJTDxyvF3-QJ4GzO9jAMLYn4-J0hoQ-qhUtwKbktdCa1AocSJVWUWEFqPSQsXeQ= IXsgPt-_fl4lwSsHpPgygvM$ for graphic product...

    ATTN...WFO...CRP...EWX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30969928 30929856 30419837 29509896 28569904=20
    28199922 28019969 28190017 28890071 29440114=20
    30120119 30680064 30949974=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 08:29:46 2025
    AWUS01 KWNH 140829
    FFGMPD
    NMZ000-141300-

    Mesoscale Precipitation Discussion 0682
    NWS Weather Prediction Center College Park MD
    429 AM EDT Mon Jul 14 2025

    Areas affected...Eastern New Mexico...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 140830Z - 141300Z

    SUMMARY...Scattered, slow moving thunderstorms capable of
    localized 2-3" totals and possible flash flooding

    DISCUSSION...RAP analysis shows a narrow corridor of conditionally
    unstable air along the eastern side of larger scale ridge over the
    desert Southwest. MUCAPEs of 2000-3000 J/kg was slightly capped,
    but generally confluent southerly and westerly low to mid-level
    flow provided sufficient deep layer convergence to break out
    scattered strong thunderstorms from Union to Eddy county. EIR
    shows tops rapidly cooling below -65C indicative of the solid
    higher theta-E air. CIRA LPW shows a strong low-level moisture
    gradient with pockets of enhanced 850-700mb moist in east-central
    NM. Total PW values of 1-1.25"; focused in the lowest portion of
    the profile and strong lower cloud vertical moisture flux will
    continue to support solid rain-rates up to 1.5"/hr.

    A strong shortwave rounding the southeast side of the larger scale
    ridge is helping to have 700-500mb south to south-southwest
    steering at about 5-10kts though sharp shift in upper-level flow
    from southwest to northeast across the Cap Rock, may further slow
    cell motions while having some oblique outflow for updraft
    maintenance. As such, a hour or two of slow moving cells may
    allow for 1.5-2.5" localized totals which may exceed localized FFG
    values of 1-1.5"/hr and 1.5-2.5"/3hrs, suggesting focused
    incidents of flash flooding will be possible while the well of
    unstable air is exhausted over the next few hours...however,
    timing of weakening/disipation is very uncertain as very few if
    any Hi-Res CAM guidance even suggested thunderstorms currently.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6dFnJgC-pn4-aXWA6Z2xj4uuyS1DvuQRu5WE-K6rpBrNhf7bK_5epOW4gUt8SEbXOqh2= nwG61_et9u72DJak0gY4RG8$ for graphic product...

    ATTN...WFO...ABQ...MAF...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 36330383 36200309 35370307 33760339 32720365=20
    32410426 32560483 32920504 33540506 35220461=20
    35850433=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 13:23:04 2025
    AWUS01 KWNH 141315
    FFGMPD
    TXZ000-141814-

    Mesoscale Precipitation Discussion 0683
    NWS Weather Prediction Center College Park MD
    914 AM EDT Mon Jul 14 2025

    Areas affected...South Central TX

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 141314Z - 141814Z

    SUMMARY...Flash flood threat continues across portions of south
    central TX into the southern Hill Country. Locally significant
    impacts remain possible.

    DISCUSSION...Recent radar and IR satellite imagery continue to
    depict deep convection over portions of south central TX from the
    Rio Grande into the southern Hill Country region. This activity is
    focused near a compact MCV, which has been nearly stationary, but
    should gradually shift north or northeast today. Around 20kts of
    southerly inflow into this MCV continues to result in areas of
    slow moving and/or backbuilding convection. The mid morning hours
    are a tricky time of day for MCV driven convection, as the
    tendency is for a weakening trend as diurnal heating results in a
    weakening of the low level jet and also convergence near the MCV.
    However there are some signs that convection this morning may try
    to persist, as modeled 850mb flow really does not weaken all that much...staying close to 20kts. Certainly will have plenty of
    instability to the south, and PWs between 2" and 2.25", so the
    thermodynamic ingredients will remain favorable for excessive
    rainfall. The MCV and convection is positioned within a favorably
    divergent region of upper level flow as well, which is likely
    aiding in sustaining deep convection. Thus the main question for
    maintenance going forward is whether we have enough low level
    convergence to keep activity organized.

    Some weakening of this convergence is expected over the next
    couple hours...as is typical for this time of day. However, given
    the aforementioned persistence of southerly low level inflow into
    the MCV, it does seem like some persistence or reinvigoration of
    convection is possible this morning. Confidence is low on exactly
    how widespread and organized convection will end up being...but
    would expect some of areas of flash flooding to continue. Recent
    HRRR runs do indeed show some persistence to this training
    convection.

    Deep layer mean flow is southerly around 15kt...but upwind
    propagation vectors are northerly around 10kts. This is a
    favorable orientation for backbuilding convection. Given the
    ingredients in place, continued areas of significant flash
    flooding remain possible this morning. The hope is we will see
    some diurnal weakening of activity...but as the HRRR
    indicates...even if that occurs we could still see some additional
    convective development feeding into the MCV as the morning
    progresses. With areas of flash flooding ongoing, confidence is
    high on the threat continuing a couple more hours. However,
    confidence is lower on whether we see continued development
    through the morning or a gradual dissipation of the stronger
    cores. But the potential for continued development leading to
    additional locally significant flash flooding is enough to warrant
    keeping a close eye on trends through the morning hours. The
    general trend should continue to favor any backbuilding on the
    southern edge of the convective complex...but as the MCV drifts
    north it is possible we also see some gradual northward expansion
    of heavier rainfall rates this morning.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8wWJp9mNBGNIpx2YjKWkcNpGgeAxn1XhAgAnFJRdtkbWGOs6Qkz7oXqOQqGUQkPoZQKy= v6Dgjb41j6miDAtmA7uHU2w$ for graphic product...

    ATTN...WFO...EWX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30179995 30049940 29489917 28869936 28599987=20
    28570045 28870088 29150098 29380109 29610120=20
    29960108 30060068 30110045=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 15:30:28 2025
    AWUS01 KWNH 141527
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-OHZ000-142126-

    Mesoscale Precipitation Discussion 0684
    NWS Weather Prediction Center College Park MD
    1126 AM EDT Mon Jul 14 2025

    Areas affected...Southeast OH, Southwest PA, WV

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 141526Z - 142126Z

    SUMMARY...Localized flash flooding will be possible into this
    afternoon across portions of southeast OH, southwest PA and WV.

    DISCUSSION...Convection near an eastward moving shortwave/MCV
    should continue over the next several hours across portions of
    southwest PA into WV. Convection is not all that deep at the
    moment, likely due to somewhat limited destabilization with the
    cloud cover. However the ongoing activity does have a warm rain
    look to it on reflectivity...and we are likely getting some
    efficient rainfall out of even these lower topped cores. There
    will be some continued destabilization over portions of WV as we
    see some breaks in the clouds ahead the MCV which is likely still
    over southeast OH as of 15z. It looks like portions of WV into far
    southeast OH and southwest PA could end up with multiple rounds of
    convection as this shortwave/MCV moves across the region into the
    early afternoon hours. The extent of the flash flood risk remains
    a bit unclear, as cells are generally showing an eastward movement
    and the degree of convective organization remains of lower
    confidence. However given the efficient nature of the ongoing
    activity, and the likelihood of some deeper convective growth as
    we head into the afternoon hours...at least some flash flood risk
    appears to exist.

    Current expectations are that the flood risk will stay localized
    over this area, with the cell motions and limited convective
    organization keeping the risk from being higher. With that said,
    some cell mergers appear likely, and given the efficient rainfall
    expected, hourly rainfall could quickly get into the 1-2" range
    where any mergers occur resulting in the potential for isolated
    instances of flash flooding.

    The flash flood risk is expected to be higher to the east of the
    current MPD area over the Mid-Atlantic, and a subsequent MPD or
    two will likely be issued to describe that risk.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8q0Q5vgBNJllhDy6GsxZTVXYNSRghToVB64DwAC2mM9vIhPYDYwkMTfkMOQE1C9-q9r3= O3xn9qjveIaX61RusqUSQ3w$ for graphic product...

    ATTN...WFO...CLE...CTP...ILN...LWX...PBZ...RLX...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 41147992 40947925 39917898 38947918 38567932=20
    38337995 38308037 38288122 38288135 38408195=20
    38488231 38738263 39458248 39918224 40278159=20
    40828072=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 17:04:13 2025
    AWUS01 KWNH 141703
    FFGMPD
    NYZ000-NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-DCZ000-WVZ000-142302-

    Mesoscale Precipitation Discussion 0685
    NWS Weather Prediction Center College Park MD
    102 PM EDT Mon Jul 14 2025

    Areas affected...Mid-Atlantic

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 141702Z - 142302Z

    SUMMARY...Convection will continue to expand across much of the
    Mid-Atlantic this afternoon, resulting in scattered to numerous
    instances of flash flooding. Very high rainfall rates are expected
    from these storms...and some instances of significant flash flood
    impacts are possible.

    DISCUSSION...Latest radar and satellite imagery depicts
    thunderstorms quickly developing along and near the terrain from
    northeast WV into central PA. We are also seeing activity increase
    in coverage farther east across PA into southeast NY. Pretty good
    large scale forcing for this convection today, with a mid level
    shortwave axis approaching from the west and the right entrance
    region of the upper level jet overhead. Impressive thermodynamics
    are also in place...with MLCAPE either currently or forecast to
    get into the 1500-2500 J/KG range and PWs ranging from closer to
    1.75" over central PA to near 2.1" over the eastern Mid-Atlantic.

    The more organized convection will likely be the activity that is
    developing on/near the terrain as of 16z. This convection should
    organize as it moves east off the terrain and anticipate one or
    more convective clusters to then move eastward from northern VA
    into PA. This linear convection should become more progressive
    with time...but will be running into an airmass with PWs
    approaching 2.25", and thus even a quicker moving line will be
    capable of producing very heavy rainfall amounts...possibly
    upwards of 2-3" of rain in an hour.

    We will also see smaller scale convective clusters develop out
    ahead of this more organized line this afternoon. These storms
    will likely be slower moving...generally moving off to the east
    northeast around 10-15kts. These cells could also briefly
    slow/backbuild into the low level flow...especially over PA into
    NJ and southern NY where the low level inflow is a bit stronger
    and more aligned with the deep layer mean wind. Also likely to
    have some cell mergers briefly increase rainfall duration...and
    around 20kts of effective shear could be just enough to briefly
    sustain some multi cell structure. All this to say that these
    convective clusters out ahead of the expected convective line will
    also pose an increasing flash flood risk as the afternoon
    progresses.

    Scattered to numerous instances of flash flooding are likely
    across most of the MPD area, stretching from northern VA into
    southern NY. Some of this could be higher end flash
    flooding...especially if/where these higher rates overlap any more
    sensitive urban areas. Hourly rainfall upwards of 2-3" will be
    possible in the stronger more persistent storms...with event total
    rainfall likely exceeding 3" in swaths over this region. Both the
    HREF and REFS also indicate a 20-40% chance of exceeding 5"
    through 00z...and seeing localized totals over 5" certainly seems
    plausible given the aforementioned ingredients in place.

    The highest rainfall magnitudes will likely end up where we see
    both merging/training convective clusters this afternoon, and the
    more organized convective line(s) later this afternoon into the
    evening hours. Based on HREF/REFS probabilities and current
    observational trends...portions of south central to eastern PA
    seem most at risk for this potential...possibly extending into
    northern NJ and southeast NY as well. Farther south over MD and VA
    things remain capped for now, so may have to wait until the
    convection moving east off the terrain gets closer before stronger
    activity initiates here.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7FoV46fW_iw805VwamZhpq6JDkFriJgCPKywoB9vuc6IHRcsciLmNInk8hUQBTdsdYLS= 1qANo9IdDW-K4zO_fTc810U$ for graphic product...

    ATTN...WFO...ALY...BGM...CTP...LWX...OKX...PBZ...PHI...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 42127654 42097538 41767404 41277363 40247424=20
    39927456 39137602 38667721 38427911 39197911=20
    39467909 40157873 40997807 41837752=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 18:51:12 2025
    AWUS01 KWNH 141850
    FFGMPD
    FLZ000-150048-

    Mesoscale Precipitation Discussion 0686
    NWS Weather Prediction Center College Park MD
    249 PM EDT Mon Jul 14 2025

    Areas affected...South Florida

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 141848Z - 150048Z

    SUMMARY...Increasing threat of flash flooding across South Florida
    with the greatest potential centered over the urban corridor from
    West Palm Beach down through Miami.

    DISCUSSION...Regional radar mosaic across the Florida peninsula
    continues to show an expansion of convection over the interior
    with the northern periphery centered near Lake Okeechobee. Off the
    coast, a low-level circulation with a more defined tropical
    character continues to provide persistent onshore flow across the
    eastern FL coast leading to prominent moisture advection and
    enhanced low-level convergence within the western flank of the
    circulation. Recent mesoanalysis indicates an areal average of
    2000-2500 J/kg MUCAPE situated across South Florida, a formidable
    instability depiction when coinciding with PWATs hovering between
    2.1-2.3" as noted via forecast soundings and 14z RAOB from KXMR
    (Cape Canaveral). Despite some areas within the immediate coast
    around KMIA observing south to southeast flow, deep layer mean
    flow is situated out of the northwest leading to steering pattern
    focusing inland convection moving back over the urban metro
    corridor between Port St. Lucie down into the Miami metro.

    Latest HRRR runs have been consistent in the presentation of the
    multi-cell cluster over the interior advancing southeastward
    towards the coastal plain with additional cell formations out
    ahead of the thunderstorm cluster. This evolution would likely pin
    a period of heavy rainfall across the metro corridor leading to
    increasing flash flood potential where run off capabilities are
    highest. Hourly rates between 2-3"/hr will be common considering
    the environment in place, but the bigger flash flood concerns will
    be correlated with intra-hour rates pushing between 3-5"/hr,
    especially if enacted over the urban zones aligning the southeast
    FL coastal plain. 12z HREF probabilities for >2"/hr were running
    between 70-90% for the period between 19-00z across the metro
    corridor, a signal high enough to warrant some localized flash
    flood prospects in areas hit the hardest. Totals between 2-4" will
    be common in the setup, but maxima between 5-7" are plausible when
    assessing some of the recent CAMs output, coincident with the
    current environment.

    Kleebauer

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4wjecQL_zXWscI0VUXGghylnIQ1WnA3YKWGO43sey-OKzu1EU8MjdZkQvQZ4hj1fefXO= EmBjRGaU9_HM_eXwWovfB50$ for graphic product...

    ATTN...WFO...KEY...MFL...MLB...TBW...

    ATTN...RFC...ALR...NWC...

    LAT...LON 27668082 27618058 27518020 27238004 27067997=20
    26807990 26557996 26327997 26267997 25888008=20
    25458022 25218044 25178063 25348078 25558081=20
    25908080 26008081 26138080 26368079 26508083=20
    26758090 26988103 27308105 27558095=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 20:11:31 2025
    AWUS01 KWNH 142010
    FFGMPD
    MEZ000-MAZ000-NHZ000-VTZ000-CTZ000-NYZ000-150209-

    Mesoscale Precipitation Discussion 0687
    NWS Weather Prediction Center College Park MD
    410 PM EDT Mon Jul 14 2025

    Areas affected...New England

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 142009Z - 150209Z

    SUMMARY...Scattered flash flood concerns across New England ahead
    of a slow-moving cold front to the northwest.

    DISCUSSION...Current radar and satellite composite note a
    generally scattered convective development across New England with
    a few stronger cores located over northern New England and over
    interior southern New England. A cold front to the northwest over
    eastern Canada continues to slowly migrate eastward with ample
    deep layer moisture and instability located downstream over the
    northeast CONUS as evident by an 18z KGYX sounding of 1.98" PWATs,
    a daily record for the site. Sufficient boundary layer buoyancy
    across New England will allow for a suitable thermodynamic posture
    leading to multiple pulse and multi-cell clusters to materialize
    over the rest of the afternoon and early evening.

    Relative storm motions are mostly progressive north of I-90,
    however as noted via the 18z sounding out of KGYX, Corfidi upshear
    vector notes a much slower mean motion between 10-15kts which can
    be exhibited when assessing the broad convective regime already in
    place. Pockets of locally heavy rainfall can be seen migrating at
    a slower pace with some anchoring along the terrain encompassing
    interior New England. This could lead to enhanced heavy rain
    prospects with rates between 1-2"/hr over the span of a few hours
    within complex terrain located over VT/NH into western ME.
    Historically, this is when flash flood concerns become more
    notable, especially within environments exhibiting deep layer
    moisture of this magnitude and an increasingly uni-directional
    deep layer wind.

    Recent HRRR output has areas across southwest ME into northern New
    England as the primary area of focus with some ongoing stronger
    cores across CT/MA likely to continue for at least a few more
    hours as they shuffle eastward.

    More scattered nature of cells and faster mean cell motions
    overall should limit more significant flash flood prospects, but
    current scenario is feasible for isolated to widely scattered
    flash flooding leading to more "possible" wording for this
    issuance.

    Kleebauer

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8IRLFKIjpf1sfcVXV_cu_EkQh0Mvf3HFCjDi4w8Y8ucjBxoXsrJaXJ_xYhOFVfYG1kbY= kBiQBAjfesaxlp5h-CVXAYk$ for graphic product...

    ATTN...WFO...ALY...BOX...BTV...CAR...GYX...

    ATTN...RFC...TAR...NWC...

    LAT...LON 45857039 45856995 45646954 45326941 44856968=20
    44386989 44056999 43717027 43407058 43007075=20
    42627100 42267149 42007184 41897202 41787229=20
    41857264 41997294 42307307 42897326 43327342=20
    43707348 44087341 44437322 44697288 45037216=20
    45237159 45417094 45617073=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 21:42:55 2025
    AWUS01 KWNH 142142
    FFGMPD
    NMZ000-150341-

    Mesoscale Precipitation Discussion 0688
    NWS Weather Prediction Center College Park MD
    541 PM EDT Mon Jul 14 2025

    Areas affected...New Mexico

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 142141Z - 150341Z

    SUMMARY...Slow moving thunderstorms capable of isolated flash
    flooding through sunset across the southern half of New Mexico.

    DISCUSSION...WV satellite notes a weak shear axis bisecting the
    southern half of NM this evening with widely scattered convection
    littered over the region. Locally stronger storms have produced
    some elevated totals within the Sacramento mountains this
    afternoon, but outflows stemming from convection and allowed for
    redevelopment to the west off the terrain. Across the eastern NM
    Caprock, scattered heavy convection has produced pockets of rates
    exceeding 1.5-2"/hr at times with a relatively slower cell motion
    overall. Radar estimates within areas most impacted by heavier
    precip have seen between 2-3" fall in a span of a few hrs. with
    the most prominent flash flood reports over the Sacramento's near
    the remnant burn scars around Ruidoso.

    Environmental conditions are at least modestly favorable for
    continued convective impacts over the next 3-5 hrs. before
    dissipating with the loss of diurnal heating. Outflow generation
    from any cell can help enhance any nearby convection and provide a
    mechanism for other cells to develop within the instability axis
    situated across the southern portion of the state. SBCAPE between
    1000-2000 J/kg has been analyzed across the area with PWATs
    hovering between 1-1.2", enough to put the area between the 75th
    and 90th percentile for the daily climo.

    Widely scattered nature of the convection will limit the overall
    coverage of flash flood prospects, but isolated flash flood
    concerns will persist through sunset with the best threat over the
    terrain in south-central NM.

    Kleebauer

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7HcsuN02jpxB5tOSNABPCQRpI2PZfIa4_kUDEzms0VJLJc7RgzgN99u2lRzHBBTxu6cr= kiq8D0F55QtNDBo-PyihA3Y$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 34970400 34890341 34490316 33850326 33450342=20
    33050382 32680486 32420559 32240600 32120638=20
    32150682 32200747 32340802 32770856 33310892=20
    33800871 34110752 34300675 34640575 34780486=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jul 14 23:04:18 2025
    AWUS01 KWNH 142302
    FFGMPD MAZ000-CTZ000-NYZ000-NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-DCZ000-WVZ000-15050=
    0-

    Mesoscale Precipitation Discussion 0689
    NWS Weather Prediction Center College Park MD
    701 PM EDT Mon Jul 14 2025

    Areas affected...Central and Northern Mid Atlantic

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 142300Z - 150500Z

    SUMMARY...Widespread flash flooding concerns will continue through
    much of the Mid Atlantic with a threat of significant flash
    flooding across the urban centers from Richmond to New York City.

    DISCUSSION...Current radar mosaic across the Northeast and Mid
    Atlantic U.S. indicates quite a robust convective footprint
    situated southwest to northeast ahead of a trough just east of
    Lake Erie. A strong line of thunderstorms currently extends from
    northern VA up through southern PA in the central Mid Atlantic
    with a relatively robust multi-cell cluster bisecting eastern PA
    up through northern NJ and the Lower Hudson Valley in NY. PWATs
    between 1.8-2.2" have plagued the Mid Atlantic and continue to be
    a focal point for the heavy convective pattern leading to
    widespread flash flood issuance's through the course of the
    afternoon. Hourly rates between 2-3"/hr have been the reason for
    such a broad scope of impact as the environment has amplified the
    convective regime throughout the course of the day with the threat
    now carrying through this evening.

    Despite the loss of a traditional diurnal heat flux, remnant cold
    pools scattered through a slowly weakening thermodynamic
    environment will still act as a focus mechanism for convection,
    especially within the well-defined multi-cell clusters in place
    over northeast PA, northern NJ, and Lower Hudson of NY. Further
    south, expect the current line of convection to continue
    progression to the east with the line holding together beyond the
    DC/Balt/Phi metro before fading as it encounters a bit more stable
    air closer to the Atlantic. Further south into VA, thunderstorms
    over the Shenandoah will eject eastward through the central
    portion of the state, but will likely hold together through cold
    pool maturation and encountering the most favorable thermodynamic
    corridor along the eastern seaboard (3000-4000 J/kg MUCAPE from
    the Potomac down through southern VA).

    Recent HRRR/RRFS trends have been favoring the triangle between DC/Lynchburg/Williamsburg and the area across northern NJ as the
    greatest threats for heavy nocturnal convection with totals
    between 2-4", locally higher anticipated in these respective
    zones. This is a strong correlation with 18z HREF neighborhood
    probs for >2"/6-hrs. hovering between 60-80% for southern zone
    with >80% depicted across all of northern NJ. These signals are
    coincident with some of the more significant flash flood
    potential, even some prospects for life-threatening flash
    flooding, especially in those more urbanized areas where run off
    capabilities are maximized.

    There is potential for some of the heavier rainfall to extend into
    New York City proper which could lead to an elevated flash flood
    risk with even potential for significant flash flooding in spots
    across the metro. Best chances will occur in the first few hrs. of
    the threat window, but totals exceeding 2" in a short span of time
    could easily occur in the window. This is a quickly evolving
    scenario across area.

    Kleebauer

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_ytj5B_bqP0RM2soUph3tCGXRoxBThlHknT6UsBSlkTB39hXldgaUBE1-pDGd5k-6fx5= EBLBcFxvUgt3SgG9bV2jtxY$ for graphic product...

    ATTN...WFO...AKQ...ALY...BGM...BOX...CTP...LWX...OKX...PHI...
    RLX...RNK...

    ATTN...RFC...ALR...RHA...TAR...TIR...NWC...

    LAT...LON 42267414 42227383 42097356 41977334 41857318=20
    41557287 41357292 40957330 40687353 40467371=20
    40097399 39897400 39687420 39577437 39437480=20
    39327503 39147527 38967553 38777563 38587566=20
    38457570 38227578 38027589 37817601 37697605=20
    37327631 37077654 36957683 36857726 36787752=20
    36727787 36737834 36747873 36867923 36927979=20
    37117995 37478008 37808010 38198000 38467966=20
    38717921 38987884 39037869 39097812 39187788=20
    39287757 39417735 39427726 39537691 39817648=20
    40217625 40507607 41017588 41497539 41837484=20
    42227434=20

    =3D =3D =3D
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