• MESO: Nws Weather Prediction Center College Park Md

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 9 08:52:58 2025
    AWUS01 KWNH 090852
    FFGMPD
    WIZ000-MNZ000-IAZ000-091435-

    Mesoscale Precipitation Discussion 0884
    NWS Weather Prediction Center College Park MD
    452 AM EDT Sat Aug 09 2025

    Areas affected...northern IA into southeastern MN and western WI

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

    Valid 090851Z - 091435Z

    SUMMARY...The threat for flash flooding is expected to increase
    this morning from northern IA into southeastern MN and western WI.
    Areas of training with rainfall rates in the 1-3 in/hr range are
    expected with 2 to 4+ inch totals through 14Z.

    DISCUSSION...Regional radar imagery at 0830Z showed an expanding
    cluster of thunderstorms just west of Minneapolis with outflow
    oriented ENE to WSW moving into the downtown portion of the city.
    This cluster has produced rainfall rates of 0.5 to 1.5 inches in
    15-30 minutes from training over Wright County and a short term
    flash flood threat appears likely into the Twin Cities over the
    next hour or so.

    Elsewhere across MN and IA, thunderstorm activity was fairly
    limited in coverage but was beginning to trend upward ahead of a
    large closed low over the Saskatchewan/U.S. border, steadily
    advancing eastward with downstream ascent over the eastern Dakotas
    into MN. At the surface, a slow moving (nearly stationary) front
    was analyzed over west-central MN, from north to south, with a
    secondary cold frontal surge with notable dewpoint falls to its
    west across the Red River Valley. Ascent ahead of the large mid to
    upper-level low, including upper level divergence and diffluence
    tied to the right-entrance region of a 100 kt jet over ND, will
    act to further increase thunderstorm coverage over the next 3-6
    hours over the region.

    As the ongoing cluster of thunderstorms to the west of MSP
    continues to shift eastward into northwestern WI over the next
    couple of hours, expansion of a second thunderstorm cluster is
    expected from northwestern IA into southeastern MN ahead of the
    cold front within a zone of low level moisture transport fed by
    30-40 kt southerly 850 mb winds. This area of thunderstorms is
    expected to follow the deeper layer mean flow toward the
    northeast. As the secondary cold front reaches northwestern IA
    near/just after 12Z, another round of thunderstorms is expected to
    develop over northwestern IA with similar northeastward
    advancement.

    The pattern will favor repeating rounds of thunderstorms with
    embedded periods of training which are likely to generate some
    areas of flash flooding with rainfall rates of 1-2 in/hr, perhaps
    as high as 2-3 in/hr within the anomalously moist/unstable airmass.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6g9HpouFQjdOui-ds94a79wlXIembMAjSiYu1hcWO2YvhV7RdE11DohMr9C4_akR4YJo= oBn5VaZbPvyvcQBKjoEMdpQ$ for graphic product...

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

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 46119202 45699032 44538980 43709015 42849193=20
    42089495 42709620 43599584 45149406=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 9 14:32:00 2025
    AWUS01 KWNH 091431
    FFGMPD
    MIZ000-WIZ000-MNZ000-IAZ000-091900-

    Mesoscale Precipitation Discussion 0885
    NWS Weather Prediction Center College Park MD
    1031 AM EDT Sat Aug 09 2025

    Areas affected...Northern Iowa, Southeastern Minnesota, and
    Central Wisconsin

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

    Valid 091430Z - 091900Z

    SUMMARY...Local rain rates to 2.5 inches per hour are occurring
    within a very slow moving line of storms. Some of the hardest hit
    areas could see 6" of rain over the next 4-6 hours. Flash flooding
    likely.

    DISCUSSION...A very slow moving front draped from central Iowa
    into Wisconsin, with an attendant low along it, has become the
    forcing for numerous showers and thunderstorms across a portion of
    the upper Midwest this morning. The storms are very slow moving,
    and while aligned along the front, the storms aren't really
    training, but simply moving so slowly that they have time to drop
    multiple inches of rain. The front has nearly stalled because the
    upper level low and its cold front to the north have turned
    northeastward, and thus are moving parallel to the front,
    resulting in very little push for the front to continue eastward.
    As is typical, PWATs with the convection have been increasing
    according to SPC Mesoanalysis, with a stripe over 2 inches along
    and immediately ahead of the front. While there remains some CIN
    around, MUCAPE has been increasing, now over 2,500 J/kg. The
    instability this afternoon should increase to over 4,000 J/kg
    ahead of the front, supporting any storms easily maintaining the
    capability of 2+ inch per hour rainfall rates.

    Meanwhile, a weakening overnight LLJ is surging incredible amounts
    of instability and moisture northward ahead of the fronts. The LLJ
    is weakening due to typical daytime heating disrupting the
    otherwise laminar southerly flow through convection. This
    weakening of the inflow should allow convection to become more
    isolated and gradually weaken into the afternoon, but this may
    take a while. CAMS guidance has been poorly resolving the coverage
    and intensity of thunderstorms thus far, but the HRRR has been
    coming into line with subsequent resolving of the current
    conditions. The HRRR suggests the storms very slowly move east
    into the early afternoon, as the line weakens. The storm motion
    should increase later this afternoon as the storms try to leave
    the front and follow the increasing instability during peak
    heating.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7itMHL4WR7SAQBC9_juyOgOPwvUvV91N4FQxaCix6E7cnrOEArMHifflf2QCcX-1ewd7= EnXZduXiC1MNoiAh0kndJR4$ for graphic product...

    ATTN...WFO...ARX...DLH...DMX...DVN...GRB...MKX...MPX...MQT...

    ATTN...RFC...MSR...NWC...

    LAT...LON 46118880 45708843 44918804 44588800 43788939=20
    43169052 42339189 41649329 41799436 42449488=20
    43079463 43659418 44379297 44479274 44579223=20
    44989117 45349035=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 9 19:41:32 2025
    AWUS01 KWNH 091941
    FFGMPD
    SCZ000-FLZ000-GAZ000-100140-

    Mesoscale Precipitation Discussion 0886
    NWS Weather Prediction Center College Park MD
    340 PM EDT Sat Aug 09 2025

    Areas affected...SC Pee Dee/Lowcountry...Far Eastern
    GA...Northeast FL

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

    Valid 091940Z - 100140Z

    SUMMARY...Bands of heavy showers and thunderstorms should tend to
    increase in coverage over the next few hours. Very heavy rainfall
    rates will be likely, which will pose a threat for at least some
    urban flash flooding/inundation concerns.

    DISCUSSION...The latest GOES-E IR satellite imagery shows a
    general expansion of cooling convective tops just offshore of the
    Southeast coastline, with radar and surface data showing a general
    westward advance of the shower and thunderstorm activity.

    Very moist low-level cyclonic flow along the coast and extending
    offshore in vicinity of a front should help maintain at least
    disorganized convection over the next several hours which will
    further be aided by the pooling of moderate instability. MLCAPE
    values along the coast are near 1000 J/kg, and there is a fair
    amount of frictional convergence noted along the coast which is
    further supporting the potential for convective bands to at least
    focus near and just inland of the SC/GA coastline. Areas of
    northeast FL will tend to have a bit more of an inland diurnal heating/instability focused threat for slow-moving areas of
    convection within the cyclonic low-level flow regime.

    PWs of 2.2 to 2.4 inches are in place, and thus indicative of a
    very tropical environment. This moisture along with the
    instability should favor rainfall rates capable of reaching 2 to 3
    inches/hour with these bands of convection, and some localized
    cell-training concerns will be possible which could foster some
    spotty totals of 3 to 5 inches by this evening. This is generally
    supported by some of the recent HRRR guidance.

    Given the rainfall potential, some urban flooding concerns will be
    possible, and this threat may be locally exacerbated along the
    immediate coast by the elevated tides associated with the
    persistent onshore flow.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9fMEkmp4jfVjtWkbspGz2PMvdCGl6_1Mkh1PiDHh0rOBITh2-fNcfRMRdZ5KJJsrCvei= EcFrd3GwXrnj0ZuSLhMbk6w$ for graphic product...

    ATTN...WFO...CAE...CHS...ILM...JAX...MLB...TBW...

    ATTN...RFC...ALR...NWC...

    LAT...LON 33917908 33447888 32258039 31228107 30388122=20
    29228102 28968181 29578252 30388271 31308242=20
    32538143 33218065 33757982=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 9 23:30:05 2025
    AWUS01 KWNH 092330
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-COZ000-100525-

    Mesoscale Precipitation Discussion 0887
    NWS Weather Prediction Center College Park MD
    727 PM EDT Sat Aug 09 2025

    Areas affected...Eastern CO...Much of Northern KS...Southern NE

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

    Valid 092327Z - 100525Z

    SUMMARY...Increasing coverage of supercell thunderstorms with
    gradual consolidation into an MCS is generally expected this
    evening. Locally high rainfall rates and cell-merger activity will
    pose at least an isolated threat for flash flooding.

    DISCUSSION...The late-afternoon GOES-W visible satellite imagery
    along with radar shows multiple supercell thunderstorm clusters
    organizing and generally expanding in coverage across portions of
    eastern CO.

    This activity will be gradually advancing off to the east this
    evening into a strongly unstable airmass pooled along and north of
    a stationary front, with MLCAPE values currently on the order of
    2000 to 4000 J/kg. The environment is strongly sheared and
    conducive for additional supercell thunderstorm development which
    will gradually set the stage for cell-mergers and consolidation of
    activity into a larger scale MCS later this evening. Additional
    factors supporting convective expansion is arrival of stronger
    upper-level jet support/forcing from the central Rockies out ahead
    of a digging upper-level trough over the Intermountain West.

    A gradual increase in a southerly low-level jet is also forecast
    this evening across the central Plains which will further aid
    ascent across the High Plains in close proximity to the
    aforementioned frontal zone. In fact, the latest HRRR guidance
    supports a 40+ kt low-level jet nosing up across northern KS by
    late this evening and this will likely support a more organized
    level of convection advancing east from eastern CO and into areas
    of northern KS and southern NE, which may include downstream
    development ahead of the eastern CO MCS evolution.

    Rainfall rates with the stronger supercells and with any
    cell-merger activity may reach 2 inches/hour, and the increase in
    moisture transport later this evening will encourage these higher
    rates.

    Some localized storm total amounts going through midnight may
    reach 3 to 4+ inches. The antecedent conditions for most of the
    region is on the dry side, but the cell-merger activity and
    resultant rainfall totals may foster some isolated flash flooding
    concerns.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6nAZzP8RQyE2TSvJixwe3jsJaDy_qDZyIA-f4vq5EdyRvFF57gTKgae_Pli53uy9J03i= o3hqrJvTg2b3OwZPU8bhLcI$ for graphic product...

    ATTN...WFO...BOU...DDC...EAX...GID...GLD...ICT...LBF...OAX...
    PUB...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 41419772 41299637 40429550 39209582 38749823=20
    38469961 37980172 38120289 38740389 39960404=20
    40690258 40970116 41199961=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 10 00:47:05 2025
    AWUS01 KWNH 100047
    FFGMPD
    WIZ000-ILZ000-IAZ000-100645-

    Mesoscale Precipitation Discussion 0888
    NWS Weather Prediction Center College Park MD
    845 PM EDT Sat Aug 09 2025

    Areas affected...Southern WI...Northern IL...Eastern IA

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

    Valid 100045Z - 100645Z

    SUMMARY...Increasing coverage of very heavy shower and
    thunderstorm activity is expected by later this evening and going
    into the overnight period. Slow-moving and locally
    backbuilding/training convective cells are expected. This coupled
    with high rainfall rates will promote areas of flash flooding,
    some of which may be significant.

    DISCUSSION...The latest surface analysis shows a well-defined
    outflow boundary that is nearly stationary across portions of
    northeast IA and across southern WI, with a rather significant
    cold pool situated just to the north given the earlier convective
    activity today.

    A very moist and unstable airmass though has been pooling along
    and just south of the boundary across eastern IA through northern
    IL with MLCAPE values of 2500 to 3500+ J/kg. PWs are generally on
    the order of 1.8 to 2.0 inches and generally suggestive of a
    tropical environment. The latest CIRA-ALPW data shows rather
    concentrated levels of moisture in the 850/500 mb layer and this
    further supports the overall high PW environment.

    This extremely favorable thermodynamic environment coupled with a
    gradual increase in a south to southwest low-level jet along the
    outflow boundary should support an uptick in convective
    development by later this evening. Increasing coverage of showers
    and thunderstorms should be most notable over southern WI where
    isentropic ascent/cold pool interaction will be stronger, but
    there is a likelihood for convection to develop and focus
    eventually back into areas of northwest IL and eastern IA where
    the nose of the low-level jet will be a bit stronger and thus
    indicative of stronger speed convergence.

    The level of moisture and instability that is in place coupled
    with an increase in moisture transport overnight near this outflow
    boundary will support extremely high rainfall rate potential that
    could easily reach 2 to 3 inches/hour. The environment will
    gradually become conducive for some backbuilding convective cells
    as the low-level jet strengthens, and thus concerns for
    cell-training will exist in time.

    Recent HRRR and WoFS solutions have been supporting as much as 3
    to 6+ inches of rain at least locally, with the heaviest rainfall
    likely being over parts of southern to southeastern WI. Given the
    environmental setup, these rainfall totals certainly seem
    plausible, and locations such as Madison and Milwaukee may be
    impacted by these heavier totals. In time overnight, areas as far
    west as Dubuque, IA may see a similar threat.

    Given the high rainfall rate and storm total potential, areas of
    flash flooding are likely tonight, and some of this flash flooding
    may be notably significant. This will include a threat for strong
    urban flooding impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9x0FEnoA_6QZM949Wm4Gt2aeSVTKLbVjsdtM1Gbw9D4fr4lH68LS4UvkPV28mRSw-Ly2= kmxAVJAoDoXZc5zj1ZImeZc$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...LOT...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 43718920 43688789 43158714 42418740 41928839=20
    41349106 41629218 42519239 43219127=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 10 01:45:28 2025
    AWUS01 KWNH 100144
    FFGMPD
    SCZ000-GAZ000-100740-

    Mesoscale Precipitation Discussion 0889
    NWS Weather Prediction Center College Park MD
    943 PM EDT Sat Aug 09 2025

    Areas affected...Eastern GA...SC Lowcountry

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

    Valid 100140Z - 100740Z

    SUMMARY...Locally concentrated bands of showers with high rainfall
    rates will continue to be a threat going into the overnight hours
    across coastal areas of eastern GA and SC. Additional urban
    flooding impacts will be possible.

    DISCUSSION...The latest GOES-E Proxy Visible satellite imagery
    along with radar shows loosely focused bands of heavy shower and
    thunderstorm activity continuing to focus along and offshore of
    the GA/SC coastline.

    Very moist low-level cyclonic flow along the coast and extending
    offshore in vicinity of a front will remain in place going into
    the overnight hours, and this coupled with the persistent pooling
    of moderate instability and stronger convergence near the coast
    should help to facilitate additional bands of convection that will
    generally advance west or northwest into the coast.

    MLCAPE values along the coast are still generally near 1000 J/kg,
    with a very moist/tropical environment characterized by PWs of
    2.25 to 2.5 inches. This has been favoring very high rainfall
    rates of 2 to 3 inches/hour with some of the more recent activity
    seen just southwest of Charleston.

    Additional rainfall amounts of 3 to 5 inches cannot be ruled out
    overnight with these bands of additional convection and especially
    given concerns for localized cell-training. This has generally
    been consistent with recent output from the HRRR guidance.

    The additional rains along with wet antecedent conditions will
    promote a threat for additional flash flooding overnight.
    Generally this threat will tend to be localized, with the more
    urbanized locations at greatest risk including Charleston and
    Savannah.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ShEmZAGhhooKBYAPpl1DzFOQntucjCoFiUZANbvfO1T8aywLR2xrska8DgO_2fYCzeL= ig0TxrCnazd4eABQw3O85_o$ for graphic product...

    ATTN...WFO...CAE...CHS...ILM...JAX...

    ATTN...RFC...ALR...NWC...

    LAT...LON 33737940 33277908 32378013 31658088 31138149=20
    31598203 32428159 33218065 33697982=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 10 06:23:39 2025
    AWUS01 KWNH 100623
    FFGMPD
    WIZ000-ILZ000-MOZ000-IAZ000-KSZ000-NEZ000-101100-

    Mesoscale Precipitation Discussion 0890
    NWS Weather Prediction Center College Park MD
    222 AM EDT Sun Aug 10 2025

    Areas affected...southeastern NE into IA, southwestern WI and
    northwestern IL

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

    Valid 100622Z - 101100Z

    SUMMARY...Flash flooding will be likely over the next few hours,
    especially in southeastern NE, but eventually affecting portions
    of IA into southwestern WI and northwestern IL. Hourly rainfall of
    2 to 3+ in/hr on a localized basis can be expected along with
    storm total rainfall of 3 to 6+ inches through 12Z.

    DISCUSSION...Radar imagery at 06Z showed a well-defined MCV over
    southern NE, roughly 30 miles southeast of Hastings, tracking
    toward the ENE. A damaging straight line wind event has been
    occurring south of the NCV but warm advection to the north of a
    long lived and sharply defined trough axis (located from
    northeastern KS, across northern MO into western IL) was forming a
    west-east axis of thunderstorms over southeastern NE. Overrunning
    thunderstorms to the north of the surface trough (marked by a weak
    temperature gradient) were oriented parallel to the track of the
    MCV, setting up a favorable environment for training. SPC
    mesoanalysis data from 05Z showed a region of 3000 to 3500+ J/kg
    MLCAPE just ahead of the MCV over northeastern KS/southeastern NE
    and eastward to the western IA/MO border.

    Locally enhanced low level southerly flow just ahead of the MCV
    will boost an already moderately strong 25-40 kt southwesterly 850
    mb jet axis which was positioned from south-central KS into
    southern IA and the WI/IL border. An expanding coverage of
    thunderstorms, already blossoming from south-central IA into the
    WI/IL border, should continue to evolve ahead of the advancing MCV
    and broader overrunning southerly flow in place. Lift should be
    aided by divergence within the right-entrance region of a
    strengthening upper level jet (per RAP forecasts) from eastern SD
    into MN. Given the forcing in place and high moisture (1.8 to 2.1
    inch PWATs per SPC mesoanalysis), high rainfall rates are expected
    within areas of training, easily capable of 1 to 2 inches in an
    hour along with localized hourly totals of 2 to 3+ inches. While
    there will be relative minimums of rainfall within the MPD threat
    area, there is a broad threat with areas of flash flooding likely
    embedded within, extending from southeastern NE into IA and the
    WI/IL border.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!85PWg1_MzokC-iM-OYt6zKd_TqVuBxT0yf7-iwblAyyxGHRpmLL_cFAg3Ahwm4hdmGcj= sjNMYATtEa0Kn1k82Z6VaYQ$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...EAX...FSD...GID...LOT...MKX...
    OAX...TOP...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43479076 43328954 42788927 41958956 41359035=20
    40899245 40509436 40019614 39719768 40209823=20
    40939786 41839645 42919319=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 10 07:01:08 2025
    AWUS01 KWNH 100701
    FFGMPD
    WIZ000-100945-

    Mesoscale Precipitation Discussion 0891
    NWS Weather Prediction Center College Park MD
    300 AM EDT Sun Aug 10 2025

    Areas affected...southeastern Wisconsin, including Milwaukee metro

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

    Valid 100659Z - 100945Z

    SUMMARY...An ongoing flash flood event over the city of Milwaukee
    appears to be shifting to the north. However, areas of training
    with locally high rainfall rates of at least 2-3 in/hr will
    continue to impact portions of southeastern WI for another 1-2
    hours with the threat beyond 09Z-10Z uncertain.

    DISCUSSION...A focused heavy rainfall event has produced 7-9
    inches of rain over the past 6 hours over the southwestern side of
    Milwaukee (per area CWOP gauge reports) with areas of considerable
    flash flooding. 20-25 kt of southwesterly flow at 850 mb has been
    overrunning a nearly stationary outflow boundary located from Lake
    County IL into south-central WI with Corfidi vectors suggestive of back-building and training.

    SPC mesoanalysis data from 06Z indicated 1500+ J/kg MLCAPE
    remained along the outflow boundary but the northward shift
    appears to be related to the ongoing warm advection regime and
    northward displacement of the elevated portion of the surface
    outflow. This northward shift of the heaviest rainfall has been
    accompanied by scattered thunderstorm development to the north and
    west over portions of south-central WI. Expect areas of training
    to continue over south-central to southeastern WI with localized
    hourly rainfall of 1 to 3 inches along with continued areas of
    flash flooding through at least 09Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!60lEz1r__BMNFL2DCk-hoCZeEAstkiISJSh7CZZdD_0oY09HB5hkJlWUqOHEKqox-rCx= eTdpHCytBnUbMRO1nYPfWyc$ for graphic product...

    ATTN...WFO...ARX...GRB...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 43978812 43628722 42958700 42548745 42508828=20
    42868907 43418981 43938940=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 10 10:40:43 2025
    AWUS01 KWNH 101040
    FFGMPD
    WIZ000-ILZ000-MNZ000-IAZ000-101500-

    Mesoscale Precipitation Discussion 0892
    NWS Weather Prediction Center College Park MD
    639 AM EDT Sun Aug 10 2025

    Areas affected...IA into/across MS Valley and southern WI

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

    Valid 101039Z - 101500Z

    SUMMARY...Scattered areas of flash flooding will continue to be
    likely from central IA, east-northeastward into southern WI and
    far northern IL. Training of heavy rain will produce peak hourly
    rainfall of 2 to 3 inches along with additional totals of 2 to 4+
    inches through 15Z.

    DISCUSSION...Radar and infrared satellite imagery showed an MCV
    over west-central IA, just ahead of another area of cyclonic
    rotation along the NE/IA border...with movement toward the ENE.
    Out ahead of these features, radar imagery showed scattered
    thunderstorms extending eastward from the MCV into eastern IA,
    southern WI and northwestern IL, to the north of a remnant outflow boundary/trough axis that extended from southern IA into northern
    IL. Areas of embedded training contained MRMS-derived hourly
    rainfall of 1-2 inches but with localized hourly rainfall of 2 to
    3+ inches over the past 1-3 hours. Low level flow of 25-40 kt was
    overrunning the boundary along with ascent ahead of the upstream
    vortex and given a similar orientation of low level winds to the
    somewhat weaker deeper layer mean wind, Corfidi vectors were
    oriented into the inflow layer supporting areas of training and
    backbuilding.

    SPC mesoanalysis data from 10Z showed MLCAPE of 1000 to 2000+ J/kg
    was in place from central IA into southern WI, along with PWATs
    near 2 inches. Aloft, IA was within a favorable region for ascent
    within the right-entrance region of a 110 kt speed max aloft over
    northern MN. This environment is expected to sustain for at least
    another 2-4 hours which will continue areas of training downstream
    of the MCV/vorticity max's track toward the ENE. While the
    mesoscale pattern across the Upper Midwest is rather complex at
    the moment, there are indications that low level winds will begin
    to weaken at least somewhat with the diurnal cycle through 15Z,
    but some low level enhancement ahead of the MCV should remain.
    Areas of training are expected to maintain a likely flash flood
    threat through 14Z/15Z across the Upper Midwest with potential for
    an additional 2 to 4+ inches in a few locations, but some
    potential weakening of rainfall intensities will be possible near
    15Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!45upNSkFLCmx7YLR762l8qBIjUl1Gorhu4wKMpQZJa6H1Rm-uXMbobC97zOsQfl-S-cz= 9WJMlV3hwBw4Q1xP4BOZbHA$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...GRB...LOT...MKX...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 44648957 44288792 43398776 42698882 41209061=20
    41159441 42339497 44029263=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 10 13:23:43 2025
    AWUS01 KWNH 101323
    FFGMPD
    WIZ000-101730-

    Mesoscale Precipitation Discussion 0893
    NWS Weather Prediction Center College Park MD
    923 AM EDT Sun Aug 10 2025

    Areas affected...Southeast Wisconsin

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

    Valid 101321Z - 101730Z

    SUMMARY...Additional heavy rain with peak hourly rainfall of 1 to
    2 inches will worsen ongoing flooding conditions in the Milwaukee
    metro rest of this morning.

    DISCUSSION...The leading edge of a shortwave trough has seen an
    increase in heavy rainfall coverage over southeast Wisconsin.
    Ample moisture inflow continues with low level SWly flow around
    25kt at 850mb which will reinforce 2" PW. SBCAPE of 1500 J/kg will
    allow further development as this leading edge crosses the rest of
    southeast Wisconsin and the Milwaukee metro. Recent rainfall
    estimates from KMKX are up to 2"/hr. Given the multiple rounds of
    heavy rainfall over and north of the Milwaukee metro since last
    evening with 3-8" measured, this additional heavy rain will
    further exacerbate ongoing flooding conditions including
    considerable threats.

    Additional upstream activity currently along the eastern IA border
    will need to be monitored for further impacts over southeast
    Wisconsin later this afternoon. Recent HRRR guidance has that
    activity shifting in this afternoon, but not the RRFS. Both of
    these models do not have this current activity, so there remains
    uncertainty for this afternoon. This will continue to be monitored.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6HD6ktknlqv7GKdy6MQuwBnkL3ihU7pjip7oXAoHanaus31G7wKUn4fVA7yhULJKbsA3= CCcyfgCJc4CKHAXC61k0FjE$ for graphic product...

    ATTN...WFO...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 43398772 42818749 42498773 42628867 42928878=20
    43318845=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 10 18:04:47 2025
    AWUS01 KWNH 101804
    FFGMPD
    TXZ000-NMZ000-AZZ000-110003-

    Mesoscale Precipitation Discussion 0894
    NWS Weather Prediction Center College Park MD
    203 PM EDT Sun Aug 10 2025

    Areas affected...in and near portions of southeast AZ & NM

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

    Valid 101803Z - 110003Z

    Summary...Showers and thunderstorms have begun to form as CIN
    erodes across portions of southern AZ and southern NM. Hourly
    rain amounts to 2" with local totals to 4" are possible.

    Discussion...GOES-18 and GOES-19 Veggie Band imagery along with
    trends in SPC mesoanalyses indicate CIN erosion across the region,
    with isolated showers and thunderstorms developing. The region is
    diffluent aloft at the base of an upper level trough and not far
    to the northeast of an MCV approaching the central Mexico/AZ
    border. Precipitable water values of 0.5-1.2" lie across the
    region. ML CAPE has built quite a bit across southern AZ, with a
    few areas with 2000+ J/kg. ML CAPE has been starting to build as
    of late across NM, but isn't especially high at the present time
    with a couple pockets of 500-1000 J/kg. Flow at 850 and 700 hPa
    is west to northwest at 10-20 kts.

    The mesoscale guidance shows a broadening and intensifying of
    convection as time marches on this afternoon. ML CAPE could
    increase an additional 1000 J/kg or so in areas where convection
    holds off on visiting. The low-level flow should pin convection
    across southeast AZ, making it difficult for activity in the
    mountains to march into lower elevations. However, the incoming
    MCV could cause convection to break out in lower elevations close
    to the AZ/Mexico border. Convection should show a tendancy to
    move east to southeast today. Given the moisture and building
    instability, hourly amounts to 2" with local amounts to 4" where
    cells manage to train or merge are considered possible. This
    rainfall would be most problematic in urban areas, dry
    washes/arroyos, and areas with burn scars.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!94KYcaNLnjjMZeQMQt0BVyGpfIlBVp6Lqy4mKIFxxazv_1BwhZJ4T4MNiV-G1iDXv7ei= AZFhsZw7PxJrz-fKNnJU7To$ for graphic product...

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

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 34680667 34370564 32470519 31650610 31150884=20
    31131104 31881210 33561077 33990946=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 10 18:53:17 2025
    AWUS01 KWNH 101853
    FFGMPD
    ILZ000-MOZ000-ARZ000-OKZ000-KSZ000-110051-

    Mesoscale Precipitation Discussion 0895
    NWS Weather Prediction Center College Park MD
    252 PM EDT Sun Aug 10 2025

    Areas affected...in and near southern MO & southeast KS

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

    Valid 101851Z - 110051Z

    Summary...Showers and thunderstorms developing across southeast MO
    & northwest AR are expected to give way to new activity to the
    west and northwest with time as CIN erodes and the low-level
    inflow backs. Hourly amounts to 3" with local totals to 5"
    possible.

    Discussion...The combination of a surface trough and outflow
    boundary have generated new convection with heavy rain across
    portions of southeast MO. Precipitable water values are 1.75-2"
    per GPS data. An ML CAPE gradient exists across portions of
    southwest MO and southern KS, with 3000-4000 J/kg existing in the
    instability pool in northeast OK. An area of effective bulk shear
    of 25-40 kts is approaching from the west. CIN is eroding from
    east to west across the region.

    As CIN erodes, the primary foci for new convection are expected to
    be along or near the outflow boundary in southeast KS and
    southwest MO, from east to west as the 850 hPa inflow backs, as
    well as closer to the incoming front which is through the Kansas
    City MO/KS metro area. Given the ingredients in place, hourly
    amounts to 3" with local totals to 5" are possible. Most of the
    region has received minimal rainfall over the past week, so widely
    scattered impacts are expected primarily with urban areas and
    sections of the Ozarks.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_5H77Aq8zXpS8RmIiCDoopxKS8HuE6Av_pV5Rx5aVXm3tiRopfQ5ywJDPXDDiufxPNSd= AKNqX5R5iHaUtVofCMFBU14$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...LZK...SGF...TOP...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38919038 37439093 35729329 36419536 36789617=20
    37259680 37879624 38679446=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 10 19:25:49 2025
    AWUS01 KWNH 101925
    FFGMPD
    OKZ000-KSZ000-NEZ000-COZ000-NMZ000-WYZ000-110124-

    Mesoscale Precipitation Discussion 0896
    NWS Weather Prediction Center College Park MD
    324 PM EDT Sun Aug 10 2025

    Areas affected...portions of eastern CO

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

    Valid 101924Z - 110124Z

    Summary...Showers and thunderstorms in the mountains of central CO
    are about to emerge into the High Plains. Hourly amounts to 2.5"
    with local totals to 4" are possible, which could lead to
    scattered flash flood concerns.

    Discussion...Showers and thunderstorms have been forming within an
    environment with parallel low-level cloud bands across the
    mountains of central CO. The upper level pattern is diffluent
    ahead of a shortwave seen on water vapor imagery near the UT/CO/WY
    border junction. Several overshooting cloud tops have been seen
    on recent satellite imagery as the storms push towards the High
    Plains. Upslope flow is strongest across northeast CO behind a
    fine line/leading edge of expanding cumuliform clouds seen in
    satellite imagery. Precipitable water values in the High Plains
    are 1"+. ML CAPE is 1000-2500 J/kg, and increasing, while CIN
    erodes regionally. Effective bulk shear is 35-40 kts.

    Guidance indicates that thunderstorms should increase in coverage, organization, and intensity over the next several hours. While
    the mean 850-400 hPa flow favors east-northeast movement, ML CAPE
    gradients in the region would favor a more east to east-southeast
    movement, which is more reflective of what's advertised within
    mesoscale guidance. The concern is that a combination of
    mesocyclones and merging convective clusters over could lead to
    hourly rains as high as 2.5" and local totals to 4" as
    precipitable water values pass 1.25" locally, which is exceedingly
    high for any time of the year for the High Plains of CO. Pockets
    of eastern CO have seen much above average rainfall this past
    week, making the region sensitive, in spots. Urban areas would
    also see problems should the higher end rainfall intensities move
    through them. Scattered instances of flash flooding are possible.

    Roth=20

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8ntetD5Chl_C1sDKfnUESsQYfAMfKpP2eBYC17BuaFdL6ApM2rySjVw-UvHOizqefSut= P9pT6nsPg-CTfjELeI9roDc$ for graphic product...

    ATTN...WFO...ABQ...AMA...BOU...CYS...DDC...GLD...LBF...PUB...

    ATTN...RFC...FWR...KRF...STR...TUA...NWC...

    LAT...LON 41700553 41400346 40310142 37810172 36910265=20
    36990529 37340612 38280630 39250565 40630600=20
    41490619=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 10 20:52:23 2025
    AWUS01 KWNH 102051
    FFGMPD
    WIZ000-ILZ000-IAZ000-110159-

    Mesoscale Precipitation Discussion 0897
    NWS Weather Prediction Center College Park MD
    450 PM EDT Sun Aug 10 2025

    Areas affected...portions of northeast IA & southwest WI

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

    Valid 102049Z - 110159Z

    Summary...A small cluster of thunderstorms is trying to organize
    as it moves east-northeast. Hourly amounts to 2" with local
    totals to 4" are possible, which could lead to isolated to widely
    scattered instances of flash flooding.

    Discussion...A small convective cluster is trying to grow in
    coverage and intensity as it moves east-northeast near a frontal
    wave within a zone of 850 hPa wind confluence. Precipitable water
    values are ~1.8". ML CAPE in its vicinity is 500-2000 J/kg and
    CIN has been eroding from west-southwest to east-northeast.=20
    Effective bulk shear of ~30 kts exists near this cluster.

    The main concern would be that the cluster grows much further in
    size and organization, as it is tracking into an area that
    received 2-5" of rainfall during the past 24 hours. Hourly
    rainfall up to 2" with local amounts to 4" appear possible, given
    the ingredients available. Recent HRRR runs have had some concept
    of future expectations in respect to locations impacted, and shows
    the cluster evolving into a forward propagating line by 02z as
    instability begins to decline, which would lessen the heavy rain
    threat from that point forward.=20

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!59h50jJXWLg2iJFB7iHh5I8n89EYm-_79GRtp7SnrANmpVk4KgYAoPk5ejN_vK2pY826= bmbLc_uRbD121QYUoWAU1Aw$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 43469082 43338986 42668996 42359046 42059228=20
    42019248 42039296 42619254 43029200 43309145=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 Aug 10 23:29:50 2025
    AWUS01 KWNH 102329
    FFGMPD
    TXZ000-NMZ000-AZZ000-110328-

    Mesoscale Precipitation Discussion 0898
    NWS Weather Prediction Center College Park MD
    729 PM EDT Sun Aug 10 2025

    Areas affected...portions of the TX Big Bend, Southern NM, &
    Southern AZ

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

    Valid 102328Z - 110328Z

    Summary...Showers and thunderstorms continue to hold on across the
    region, and should do so for another several hours as they sink
    towards Mexico. Until they wane tonight, hourly amounts to 2"
    with local totals to 4" remain possible.

    Discussion...Overshooting convective tops continue with the
    convection across the TX Big Bend, southern NM, and southeast AZ.=20
    The region is at the base of an upper level trough which is
    providing difluence aloft. Precipitable water values are
    0.9-1.3", fairly moist for sites with elevation. ML CAPE of
    500-2000 J/kg remains across the region, and CIN is beginning to
    return to the area.

    The expectation is for thunderstorms with heavy rainfall to
    continue sagging south and eastward, either dissipating on their
    way to the US/Mexico border across AZ and NM weakening while
    entering northwest TX or the TX Panhandle over the next four
    hours. Guidance insists that thunderstorms with heavy rainfall
    will hold on the longest near the southeast AZ border with Mexico.
    Until they fade or cross into Mexico, hourly rain amounts to 2"
    with local totals to 4" remain possible.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8thnvrDqD6DjnWZfoG4rYQ2wFQp3not2GtqVWxxqcwqvZLh3hf9iDN_y7OH-CRmD9mxJ= u7lg9PHZWgUz51x_UW9M9Ss$ for graphic product...

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

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 34630190 31970233 29390382 30510587 31200706=20
    31070872 31101118 31531240 32281265 33651106=20
    34111005 34230857 33050638 32810420 34380358=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 Aug 11 00:16:02 2025
    AWUS01 KWNH 110014
    FFGMPD
    WIZ000-ILZ000-IAZ000-110412-

    Mesoscale Precipitation Discussion 0899
    NWS Weather Prediction Center College Park MD
    813 PM EDT Sun Aug 10 2025

    Areas affected...southern WI

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

    Valid 110012Z - 110412Z

    Summary...A convective cluster is moving briskly into southwest
    WI, and along with additional thunderstorms forming in its
    neighborhood, is threatening saturated areas of southeast WI.=20
    Hourly rain amounts to 2" with local totals to 4" remain possible.

    Discussion...A small thunderstorm cluster continues moving
    east-northeast at 30 kts into southwest WI. Overshooting cloud
    tops continue to be noted prior to sunset on Veggie Band imagery.=20 Precipitable water values are 1.75-2". An instability gradient
    exists across southern WI which continues to edge northward to
    sustain this cluster, with maximum values of 2000-2500 J/kg.=20
    Effective bulk shear of 25-35 kts exists in the area.

    As new cells are forming at its leading edge and to its east
    closer to Chicago, there is little sign of the cluster trying to
    arc out into a convective line yet. As soils were significantly
    saturated across southeast WI with 5-14" of rain last night, they
    would be sensitive to hourly amounts to 2" or local totals to 4"
    wherever cells merge, train, or a mesocyclone manages to form and
    track. The mesoscale guidance as a whole has been struggling
    here, so left the category as Possible, but wherever the cluster
    moves over saturated soils or urban areas, flash flooding would be
    possible.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_mAknFSP-2poDSznjFXOEwP5IXOD6S7vqEEu-HVJg-wlsfsplz0g4eoeqRo3zefBiWSS= zC7lOa-ft_DYMDi01rtYSF8$ for graphic product...

    ATTN...WFO...ARX...DVN...LOT...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 43758869 43538789 42538759 42278781 41989025=20
    42019156 42629138 43349035=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 11 00:54:20 2025
    AWUS01 KWNH 110054
    FFGMPD
    MOZ000-TXZ000-OKZ000-KSZ000-COZ000-NMZ000-110653-

    Mesoscale Precipitation Discussion 0900
    NWS Weather Prediction Center College Park MD
    853 PM EDT Sun Aug 10 2025

    Areas affected...eastern CO, western KS, near the KS/OK border, &
    southwest MO

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

    Valid 110053Z - 110653Z

    Summary...Thunderstorms are expected to bridge across from CO near
    the KS/OK border over the next six hours. Hourly rain amounts to
    3" with local totals to 5" over an increasingly broad scale should
    allow for scattered to numerous instances of flash flooding
    through 07z.

    Discussion...Over the past 2-3 hours, thunderstorms have been
    developing and congealing across portions of southwest MO and near
    the eastern KS/OK border within and in the gradient north of an ML
    CAPE pool of 3500 J/kg. CIN continues to erode here. A front
    bisects the OK/KS border from east-northeast to west-southwest.=20
    To the west, elevated thunderstorms continue their march across
    eastern CO and far northeast NM. Precipitable water values of
    1.25" in the High Plains to 2" farther east are seen near the
    boundary. Effective bulk shear of 25-35 kts exist across the area.

    As the low-level jet continues backing/edging to the west along
    the OK/KS border, there should be a tendency for convection to
    reform farther west from southwest MO and southeast KS. At the
    same time, convection from CO is expected to move across western
    KS. By 06z, either a merger of the two convective areas or
    outflow from the activity currently across CO should lead to a
    significant enhancement of heavy rainfall in or near southwest KS.
    The 18z HREF advertises a nearly 20% chance of 5" through 06z,
    and has similar odds of 8" in the 00z-12z time frame in far
    southern KS. Meanwhile, the WoFS maximum is mostly south of the
    eastern two-thirds of the OK/KS border, possibly due to ongoing
    convection eroding the northern portion of the instability pool in
    that area. Cell training, possible random mesocyclones, and cell
    mergers are expected to lead to locally higher rain totals. With
    a broadening scale of hourly rain amounts to 3" and local totals
    to 5", and despite dryness over much of these region during the
    past week, scattered to numerous instances of flash flooding are
    expected overnight, which is expected to be underway before 07z.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!47i8czHkhAkAkTnNQFH3PKpQcV5Eqb9_Wj957hAp3ylTFyR884A4903Tssi3CKigeuv1= sy9FqW_kYowunYcsH1wepIM$ for graphic product...

    ATTN...WFO...ABQ...AMA...BOU...DDC...EAX...GLD...ICT...LSX... OUN...PUB...SGF...TOP...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 40240316 39830139 38519954 38209793 38559547=20
    38969282 37259262 36369516 35819960 35760028=20
    35890207 36460351 38000446=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 11 04:24:41 2025
    AWUS01 KWNH 110424
    FFGMPD
    WIZ000-ILZ000-IAZ000-110900-

    Mesoscale Precipitation Discussion 0901
    NWS Weather Prediction Center College Park MD
    1223 AM EDT Mon Aug 11 2025

    Areas affected...northern Illinois through central Wisconsin

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

    Valid 110423Z - 110900Z

    Summary...Showers and thunderstorms expanding ahead of a shortwave
    will likely train across parts of Wisconsin tonight. Rainfall
    rates of 1-2"/hr at times will produce 1-3" of rainfall, and may
    result in renewed flash flooding.

    Discussion...The GOES-E IR imagery tonight shows expanding
    convection evident via cooling cloud tops across parts of northern
    Illinois and southern Wisconsin. These thunderstorms are generally
    developing in response to the overlap of a shortwave analyzed by
    the RAP and noted in the satellite imagery lifting across eastern
    IA, with the slow veer of an 850mb LLJ analyzed by regional VWPs
    to be 20-30 kts from the S/SW. This LLJ is drawing elevated PWs
    northward, which were measured via the 00Z U/A soundings at DVN
    and ILX to be above 1.9 inches, or well above the 90th percentile
    for the date. These PWs are aligned with a ribbon of high MUCAPE
    above 2000 J/kg, and as the LLJ continues around 30 kts the next
    several hours, these robust thermodynamics will resupply an
    environment favorable for heavy-rain producing convection.

    Recent radar-estimated rainfall rates from KMKX have been as high
    a 1.5"/hr, and the HREF neighborhood probabilities for 1"/hr
    remain as high as 40% through around 09Z, while the HRRR
    indicates an isolated potential for brief 3"/hr rain rates
    (0.75"/15min). The strongest convection is likely during the next
    few hours, primarily across southern WI, before the LLJ begins to
    veer. This is also when the greatest height falls/PVA will occur
    downstream of the shortwave as it lifts northeast, providing
    enhanced ascent into the favorable thermodynamics.

    There may be two areas of focused heavier rainfall, one across
    central WI and a secondary maximum in southeast WI. Across central
    WI, the LLJ nose will develop leading to enhanced convergence
    before it begins to veer after 07Z. This suggests regenerating
    cells in this region with enough support from thermodynamic
    advection to produce repeating 1"/hr rain rates. With cells likely strengthening right along this convergent axis, rainfall could
    reach 1-3" leading to isolated instances of flash flooding within
    a narrow corridor.

    Farther south in WI and into far northern IL, the greatest
    isentropic ascent is likely, which will act into a plume of the
    most intense MUCAPE. Here, propagation vectors collapse to around
    5 kts and become aligned obliquely right of the mean wind
    suggesting backbuilding cells and a higher training threat. Rain
    rate probabilities also peak in this vicinity, and the HREF 6-hr
    rainfall probabilities for 3" rise above 15%. Southern WI has also
    experienced tremendous rain the past 24-hrs of 2-5", and in some
    areas more than 9" of rain, leading to extremely vulnerable soils
    such that any heavy rain could quickly lead to runoff and
    instances of flash flooding.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_3v1zRJNRvp-j3FKUYPjRVhvGbxMCsh4UlA9MC-EWaAO33e92oTzGb6w6MjJBQ3xGOED= QYViyd1hxpt_9-5SRx_1Czs$ for graphic product...

    ATTN...WFO...ARX...DVN...GRB...LOT...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 45258843 45058781 44668756 44198757 43318773=20
    42818781 42348803 41878897 41819016 42209087=20
    42559100 43419084 44409024 45008936=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 11 05:17:59 2025
    AWUS01 KWNH 110517
    FFGMPD
    NCZ000-SCZ000-GAZ000-111115-

    Mesoscale Precipitation Discussion 0902
    NWS Weather Prediction Center College Park MD
    116 AM EDT Mon Aug 11 2025

    Areas affected...Coastal Georgia through Coastal Southeast North
    Carolina

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

    Valid 110515Z - 111115Z

    Summary...Heavy showers and isolated thunderstorms pivoting
    onshore will continue overnight. Rainfall rates of 2-3"/hr are
    likely, which through training could produce 2-3" of rain with
    locally higher amounts. Flash flooding is possible.

    Discussion...The regional radar mosaic this evening shows
    expanding convection lurking just offshore to the east of the SC
    and GA coasts. This convection is expanding in response to ascent
    driven via strung-out vorticity aligned along the coasts combined
    with increasing thickness diffluence noted in the mid-level
    thickness fields. At the same time, 850-500mb winds are generally
    from the E/SE around a mid-level trough axis, with recent 850mb
    winds measured at KJAX and KCLX VWPS of 20-30 kts, more than twice
    the mean wind, supporting additional ascent. This lift is
    occurring into impressive thermodynamics characterized by PWs
    measured by GPS of 2.3 to 2.4 inches, nearly the daily record for
    the region, overlapping MUCAPE of 1000-3000 J/kg as analzyed by
    the SPC RAP. Together, this is resulting in an expansion of heavy
    rainfall with embedded thunderstorms, with impressive reflectivity
    above 40dBZ identified near shore via the regional radar mosaic,
    but also additionally farther offshore utilizing the satellite
    GREMLIN product, with sufficient GLM lightning density to support
    its output.

    As onshore flow persists and forcing remains, convection should
    expand and intensify through the night. As is typical with
    nocturnal flare ups like as expected, the heaviest rainfall should
    be confined to offshore and the immediate coast due to a rapid
    dropoff in instability inland. The simulated reflectivity and
    rainfall footprint from the available CAMs supports this
    conceptual model, but with 850mb winds continuing to exceed the
    mean wind, some inland push of heavier rainfall is possible.
    However, the most intense rain rates, which have a 15-25% chance
    of exceeding 2"/hr from the HREF, and may locally exceed 3"/hr at
    times (15-min HRRR rainfall of 0.75") should remain along the
    immediate coast. Despite storm motions of 10-15kts to the NW,
    Corfidi vectors collapsed to 5 kts or less and aligned against the
    mean wind indicate backbuilding and repeating cells will rotate
    onshore to enhance the duration of rainfall. Where this occurs,
    total rainfall through morning will likely reach 2-3". with local
    amounts as much as 5" possible.

    3-hr FFG from the Georgia coast northeast into the Grand Strand is
    generally 2-3"/3hrs, although is locally compromised to as low as
    1.5"/3hrs due to 24-hr MRMS measured rainfall of 3-5". While the
    flash flood risk appears generally isolated, should any of these
    training bands occur atop these more vulnerable soils, or into any
    more urbanized areas, flash flooding would become more likely
    overnight.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7BGhqHsZ-MdeMYOjwksyB6wdTCG6tK8QRWAaO1NuzEL4UrP7pKXRdmJBBUplSxbdGUq6= ab1_mirvjP-0jKM5Wxfv-Z0$ for graphic product...

    ATTN...WFO...CHS...ILM...JAX...

    ATTN...RFC...ALR...NWC...

    LAT...LON 34347830 34227783 33877777 33527829 33177880=20
    32887920 32188020 30948101 30848140 30988167=20
    31328190 31658176 31968150 32188132 32488103=20
    32868069 33318020 33877959 34207906=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 11 06:46:39 2025
    AWUS01 KWNH 110646
    FFGMPD
    TXZ000-OKZ000-KSZ000-111200-

    Mesoscale Precipitation Discussion 0903
    NWS Weather Prediction Center College Park MD
    245 AM EDT Mon Aug 11 2025

    Areas affected...Southern Kansas and far Northern Oklahoma

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

    Valid 110644Z - 111200Z

    Summary...An MCS moving across southern Kansas will interact with
    an outflow boundary/stationary front to enhance convection through
    early morning. Rainfall rates of 2-3"/hr are expected, which
    through training could produce 3-4" of rain with locally more than
    6" possible. Flash flooding is likely.

    Discussion...The regional radar mosaic early this morning shows
    expanding thunderstorms with heavy rainfall stretching across much
    of southern Kansas and far northern Oklahoma. Within this
    convection, dual MCVs are noted moving eastward, with a potent MCS
    associated with the leading MCV pushing into central KS. This MCS
    will continue to track eastward through the morning, interacting
    with downstream convection, and leaving a residual outflow
    boundary, to persist and intensify rainfall.

    Thunderstorm activity is being driven by an impressive overlap of
    synoptic and mesoscale ascent. A large-scale mid-level trough axis
    is advecting eastward from the High Plains to produce broad height
    falls, while an upper jet streak intensifies downstream to place
    favorable RRQ diffluence atop the Central Plains. This deep layer
    ascent is being enhanced by a strengthening southerly 850mb LLJ
    measured via VWPs at KICT/KVNX to be 30-35 kts. This LLJ has
    exhibited rapid strengthening and broadening the past few hours,
    which is helping to intensify the thermodynamic environment by
    drawing PWs of 1.8-2.0 inches and MUCAPE of 2000 J/kg northward to
    support ongoing convection. Additionally, this LLJ is
    isentropically ascending the hybrid outflow boundary/stationary
    front analyzed by WPC to provide enhanced mesoscale lift.

    While the CAMs are struggling to resolve the exact evolution of
    the current radar, the recent HRRR and ARW have at least a better
    handle on the positioning/timing of the features leading to
    increased confidence in their output the next several hours. These
    suggest that the LLJ will remain primarily from the south
    overnight, with some local acceleration possible immediately
    downstream of the MCV. As this occurs during the MCS translation
    to the east, it will result in persistent and slow moving
    thunderstorms downstream (Corfidi vectors collapsed to just around
    5 kts) until the MCS sweeps through by morning. Additional
    convective development is likely along other outflow boundaries as
    well, further lengthening the duration of rainfall in some areas.
    With thermodynamics supporting rainfall rates of 2-4"/hr (30-40%
    chance of 3"/1hr from the WoFS, and HRRR 15-min rainfall as much
    as 1"), rapid runoff is likely even despite 0-10cm soil moisture
    from NASA SPoRT that is below the 20th percentile.

    Most concerning, however, is the threat for training or slowing of
    these intense rain rates. The HREF PMM and WoFS 90th percentile
    rainfall by 12Z are quite well aligned with a maxima across
    Kingman, Barber, and Harper counties, KS. Here, both these systems
    predict as much as 6-7 inches of rainfall, with a broad swath of
    2-5" (10-30% chance from the HREF) surrounding it and stretching
    as far east as the KS/MO border. This indicates that flash
    flooding is likely in many areas overnight, with an isolated
    significant impact possible if these higher amounts occur over a
    more vulnerable location.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_MmBJ-WCVuHop1IQ1whv3QTsPnmIqSts1uQ-MlIhGX88CgWhjhHzTEJH9OYuhoWTd7pS= Emu8Bqy3BEYE1pq4BZKOh5k$ for graphic product...

    ATTN...WFO...AMA...DDC...ICT...OUN...SGF...TOP...TSA...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 38759928 38669773 38549705 38339627 38089551=20
    37779511 37419496 36919484 36559505 36059620=20
    36169750 36389914 36440071 36530111 36850170=20
    37400139 38060091 38550011=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 11 12:04:25 2025
    AWUS01 KWNH 111203
    FFGMPD
    MOZ000-OKZ000-KSZ000-111600-

    Mesoscale Precipitation Discussion 0904
    NWS Weather Prediction Center College Park MD
    802 AM EDT Mon Aug 11 2025

    Areas affected...Eastern Kansas into Missouri

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

    Valid 111201Z - 111600Z

    Summary...Development ahead of an MCS allows a flash flood risk to
    persist this morning over southeast Kansas into western Missouri.

    Discussion...The MCS that crossed southern Kansas overnight has
    seen renewed growth over southeast KS with a left book end vortex
    turning into an MCV near Emporia. Currently activity that
    developed near Chanute is now having the MCS cross which raises a
    localized flash flood concern. An axis of high moisture with some
    instability extending east into Missouri poses a possible flash
    flood risk rest of this morning as the MCS progresses east.

    SWly 850mb flow of 25-30kt is forecast by the RAP to persist ahead
    of the MCS into western MO through 14Z. This will maintain PW
    around 2". MUCAPE is a bit lacking ahead of the MCS generally
    between 500-1000 J/kg, but given recent upward trends, there may
    be sufficient instability to allow further growth. Furthermore,
    areas ahead of the MCS along the KS/MO line have lowered FFG of
    1.5/hr given heavy rain yesterday. Flash flooding is considered
    possible over the rest of southeastern KS south of the KC metro
    into western MO and this activity will continue to be monitored.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_j3YL7eprleIk666mpilVuZdyd0pqGJZ8v8FHZo0u1spix3hbDb1FPkO78QUsOga6I3y= sEpZEzw5x0PgwdKZa0p-VLM$ for graphic product...

    ATTN...WFO...EAX...ICT...SGF...TOP...TSA...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 38869359 38179304 37429311 37069422 36949496=20
    37089599 37949590 38459614 38809523=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 11 12:40:26 2025
    AWUS01 KWNH 111239
    FFGMPD
    SCZ000-111600-

    Mesoscale Precipitation Discussion 0905
    NWS Weather Prediction Center College Park MD
    838 AM EDT Mon Aug 11 2025

    Areas affected...Greater Charleston SC Metro

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

    Valid 111237Z - 111600Z

    Summary...Heavy thunderstorms with hourly rainfall of 2 to 3
    inches should continue to lift up the SC coast this morning. At
    the current pace, the heavy rates would impact Charleston near
    morning high tide which would enhance localized flooding.

    Discussion...A band of heavy thunderstorms is currently pushing
    inland and up the coast between Hilton Head Island and Charleston.
    This is being fed by 25kt Sly flow with PW still around 2.25" with
    a high instability gradient with 3000 J/kg just offshore per the
    RAP. Max hourly rainfall is estimated from KCLX in Charleston
    County south of the Charleston metro.

    As onshore flow persists this activity should persist along and
    just inland from the coast with a northward trend. This would
    place torrential rain over the Charleston metro near the 10a high
    tide which would enhanced the localized flooding risk.
    Furthermore, the 1hr FFG is generally around 2.5", so localized
    flash flooding is possible over the areas impacted by this heavy
    band. As of now the offshore component of the activity is somewhat
    disorganized and the cloud tops have recently begun a warming
    trend. However, given the high instability, redevelopment is
    possible which makes for a possible flash flood risk rest of the
    morning around the greater Charleston metro.



    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-KPobCGAsTzzbsZSJNwkPUZdJJifdA_l6VqbIt_Yp9tP31h81BG8dwk-VHIkWxqpye0W= IAbEwaeyDDAXc9KB5vNXivg$ for graphic product...

    ATTN...WFO...CHS...

    ATTN...RFC...ALR...NWC...

    LAT...LON 33338015 33027946 32607964 32478033 32798053=20
    32988056=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 11 14:34:30 2025
    AWUS01 KWNH 111434
    FFGMPD
    FLZ000-111930-

    Mesoscale Precipitation Discussion 0906
    NWS Weather Prediction Center College Park MD
    1033 AM EDT Mon Aug 11 2025

    Areas affected...Florida Panhandle

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

    Valid 111432Z - 111930Z

    Summary...Heavy thunderstorms will continue to push west from
    Apalachee Bay rest of this morning. Extreme rainfall rates of 3"+
    per hour should continue with this activity. Flash flooding is
    considered possible through the early afternoon in this rather
    flash flood resistant area.

    Discussion...A trough extends up through Apalachee Bay with
    rotation apparent in regional radar. Scattered thunderstorms with
    torrential rain rates are focused west of this trough along the
    western Apalachee Bay shoreline. Westward expansion and shifting
    of this complex is expected to continue as directed by an upper
    ridge extending from the Atlantic along the FL/GA border. Extreme
    moisture is present along this trough axis with recent RAPs
    estimating 2.5" PW. High instability is also present with SBCAPE
    up to 3000 J/kg estimated by the RAP in Apalachee Bay with a tight
    gradient to 1500 J/kg near the Apalachicola National Forest SW of
    Tallahassee.

    Continued rainfall rates of 2-3"+/hr should be expected with
    potential for localized 5"+ in three hours. Given 3hr FFG around
    4", the flash flood threat would be for repeating activity which
    is not currently developed and recent HRRRs do not depict much
    additional development through early afternoon. However, renewed
    development certainly could occur given the high instability
    upstream over the Bay and peak diurnal heating. This area west of
    the FL Big Bend is rather flash flood resistant, but rainfall
    exceeding 4" through midday would cause at least localized
    flooding issues. Flash flooding is considered possible at this
    time.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6CGFOW9-0_-_CLE7SbAp2XL46xR5B2AYx3xgrqwlRLUJZo_M7vTtzwxewz_eguWWm7lm= U_pHUghRRE5QzpTpagfb4v8$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 30398483 30138428 30008414 29748430 29568470=20
    29508501 29648544 30158588 30378546=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 11 16:24:28 2025
    AWUS01 KWNH 111624
    FFGMPD
    NCZ000-SCZ000-112215-

    Mesoscale Precipitation Discussion 0907
    NWS Weather Prediction Center College Park MD
    1224 PM EDT Mon Aug 11 2025

    Areas affected...Carolinas

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

    Valid 111622Z - 112215Z

    Summary...Heavy showers and isolated thunderstorms will continue
    developing along an axis from the South Carolina Coast to the
    North Carolina Blue Ridge rest of this afternoon. Rainfall of
    2"/hr is likely to continue and expand in coverage with localized
    totals exceeding 4" possible rest of this afternoon. Localized
    flash flooding can be expected.

    Discussion...Broad scale southerly flow is present over the
    Southeast with a trough along the Carolina Coast. A somewhat
    focused corridor of activity has developed from the SC coast north
    of Charleston inland to the NC Blue Ridge which is ahead of a
    mid-level vort lobe drifting north over southern SC per recent RAP
    runs. Heavy thunderstorms moved through Charleston late morning
    with continued development lifting along the coast. A new cluster
    of thunderstorms have developed in the past hour over interior
    northern SC and heavy showers continue from this morning from
    around Charlotte west through the southern NC Blue Ridge (with
    further growth possible through the diurnal max). Robust,
    tropically sourced moisture is present over this corridor with
    2.3" PW along the coast and 2" butting up against the Blue Ridge
    which is around 2 sigma above normal across the region. SBCAPE of
    1500-2500 J/kg along this corridor is allowing this development
    and warm rain processes are maximizing rates with with recent
    hourly rainfall of 1.5-2" in the heaviest activity.

    Recent HRRR runs are a little subdued compared to reality, but
    generally focus afternoon development along this corridor. Flash
    flood guidance is 1.5-2"/hr in the Piedmont/foothills and
    generally 2.5"/hr in the Coastal Plains. The combination of
    extreme moisture and sufficient instability should allow for
    localized extreme rainfall rates of up to 3"/hr which would cause
    localized flash flooding rest of the afternoon.

    Given the broad scale of the elevated moisture across the
    Southeast, further consideration will be given to other areas
    outside this corridor (which is purposefully just north of
    vulnerable Columbia based on trends), but for now this appears to
    be the most likely area for flash flood concern this afternoon.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!77LrHy1BKj_4tDjjzsU5WhBxJE4Ckbp5p4kZZxM9J6FPdb3bTyIOg5lbRxyhTcjy5DZU= QMAAciAty_IQwNIQGgOoLvg$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 36148091 35548025 34977938 34157846 33837816=20
    33377879 32557976 33398034 34238083 34838193=20
    35248224 35698214 36108153=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 11 18:28:46 2025
    AWUS01 KWNH 111827
    FFGMPD
    VAZ000-NCZ000-112330-

    Mesoscale Precipitation Discussion 0908
    NWS Weather Prediction Center College Park MD
    227 PM EDT Mon Aug 11 2025

    Areas affected...Northeast North Carolina through Hampton Roads

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

    Valid 111825Z - 112330Z

    Summary...Heavy thunderstorms will continue developing and
    drifting north from northeast North Carolina through Hampton Roads
    this afternoon. Localized rainfall of 2.5"/hr is likely to
    continue with possible totals of 4" possible. Localized flash
    flooding can be expected to 23Z.

    Discussion...Southerly flow over eastern NC is pushing 2" PW up
    over Hampton Roads. Scattered thunderstorms have developed over
    northeast NC with newer activity in southern sections of Virginia
    Beach. Sufficient instability is present with SBCAPE of 1500-2500
    J/kg with a decreasing gradient north of Hampton Roads and warm
    rain processes are maximizing rates with with recent hourly
    rainfall of 2.5" in the heaviest activity.

    Recent HRRR runs are decent in coverage, but somewhat light on
    intensity and depict a bit of a northward drift in activity over
    southeast VA rest of the afternoon. Flash flood guidance is
    higher, generally 2.5"/hr, but lower as typical for the Hampton
    Roads metro around 1.5"/hr. The combination of high moisture and
    sufficient instability should allow for localized rainfall rates
    of up to 3"/hr which would cause localized flash flooding rest of
    the afternoon, especially in urban areas.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!84iEyxG36aIxsn_UaI8WR-zFv1D7DKjdtU4DWRFyckzMD1qb9skYB65hWAW1HNEXfdDN= -GIoES9MMpQwsa6LcprM4fo$ for graphic product...

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

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37217644 37007597 36567569 36077553 35727554=20
    35537676 36417780 36877783 37137736=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 11 19:04:55 2025
    AWUS01 KWNH 111904
    FFGMPD
    VAZ000-NCZ000-112333-

    Mesoscale Precipitation Discussion 0909
    NWS Weather Prediction Center College Park MD
    303 PM EDT Mon Aug 11 2025

    Areas affected...portions of central NC

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

    Valid 111903Z - 112333Z

    Summary...Pulse convection with heavy rain is moving towards a
    more hydrologically sensitive area over the next few hours.=20
    Hourly amounts to 3" with local totals to 5" are possible, which
    could lead to isolated to widely scattered flash flood concerns.

    Discussion...Thunderstorms across NC are moving inland near and
    ahead of a surface trough/convergence zone. Despite its forward
    progression, hourly amounts to 3" -- if not higher -- have been
    seen with this activity per WSR-88D radar estimates. While
    activity is generally moving northward, some cells are showing
    more chaotic motion, leading to occasional mergers which is aiding precipitation efficiency. Precipitable water values are 2-2.25"
    per GPS data. ML CAPE of 1500-2000 J/kg exists in the region.=20
    Effective bulk shear is shy of 25 kts, leading to its pulse
    character.

    Of concern is a swath of the Piedmont which has received 300-600%
    of their average weekly rainfall from Asheville northeast through
    Durham to just across the VA border. This wet week should have
    made the soils more sensitive, and shows up as a lower area of
    flash flood guidance values. Isolated to widely scattered flash
    flood concerns should be mostly within this wet area of the
    Piedmont or in urban areas.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-VKPMZClq23jekxG9GBgFYK-HQXrIez8PzfDMiyvSQE9EIEPI12bJdMFzIG0ZhJOno55= xsocLobH1wAdb1EB4XJMsnw$ for graphic product...

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

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37167743 36617798 36107755 35667712 35567698=20
    35017741 34627867 35417994 36268095 36918014=20
    37107883=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 11 19:48:04 2025
    AWUS01 KWNH 111947
    FFGMPD
    TXZ000-OKZ000-COZ000-NMZ000-120146-

    Mesoscale Precipitation Discussion 0910
    NWS Weather Prediction Center College Park MD
    347 PM EDT Mon Aug 11 2025

    Areas affected...circa northeast NM & the TX Panhandle

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

    Valid 111946Z - 120146Z

    Summary...Cumuli are showing growth near the NM/CO border and
    across portions of the TX Panhandle. Showers and thunderstorms
    which evolve from them have the potential for hourly rain amounts
    to 2" with local totals to 4".

    Discussion...Cumuli are getting feisty near the NM/CO border in
    area terrain not far to the east of an upper level low dropping
    into northwest NM, with some signal of cumulus growth also
    apparent in the northwest TX Panhandle where a surface convergence
    zone/weak baroclinic trough was noted in 19z surface observations.
    Precipitable water values of 0.5-1.5" lie across the region. An
    ML CAPE gradient is noted near the convergence zone on SPC
    mesoanalyses, with 500-2000 J/kg values in its vicinity.=20
    Effective bulk shear of 20-30 kts exists at the moment. CIN is
    reducing across the region.

    While there's some disparity amongst the mesoscale guidance, the
    most coherent signal shows that convection near the CO/NM border
    forms and drops southeast to south-southeast, roughly in line with
    the ML CAPE gradient and 850-400 hPa mean wind but somewhat into
    the instability field. Some of the activity that forms across
    portions of northern and central NM then turns east along the trough/instability gradient into the TX Panhandle while growing in
    scale as the low-level inflow from the Gulf begins to increase and
    moisture import increases further. Given the available
    parameters, hourly rain to 2" with local totals to 4" are
    possible. The region has been dry over the past week, so any
    flash flood issues are most likely to be isolated to widely
    scattered and near area burn scars, dry washes/arroyos, or across
    urban areas within this region.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6MVkTYOPbBiYoy0dlZKlJ0tTeBEDfkLTRi6TA19pauTbPQs3qA7fFm-iaZQ_g0jRffI5= 21zuMLyiCZPHemO7Ev7vb1g$ for graphic product...

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

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 37660514 37450462 36290277 36660047 36529988=20
    35769998 34490079 33810262 33750455 34780620=20
    36000569 36500540 37230523=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 11 20:18:34 2025
    AWUS01 KWNH 112018
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-120147-

    Mesoscale Precipitation Discussion 0911
    NWS Weather Prediction Center College Park MD
    417 PM EDT Mon Aug 11 2025

    Areas affected...KS/MO/OK border southwest across central OK

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

    Valid 112017Z - 120147Z

    Summary...Showers and thunderstorms have begun to develop from=20
    southwest MO into central OK. Hourly rain amounts to 2.5" with
    local totals to 4" are possible, which could lead to isolated to
    widely scattered flash flood concerns.

    Discussion...A surface convergence zone/baroclinic trough
    stretches from western MO past the MO/KS/OK border junction
    through north-central OK. Near this boundary is an ML CAPE
    gradient, with values of 2500-3000 J/kg lying to its south. An
    MCV from overnight convective activity is entering central OK from
    the west while another overnight MCV moves across portions of IA
    to the north. Precipitable water values are ~1.8". Effective
    bulk shear is just shy of 25 kts per SPC mesoanalyses. CIN has
    nearly eroded.

    The mesoscale guidance appears to be modeling the development of
    this convective activity well, thus far. It is showing the entire
    axis lighting up over the next several hours, which will help
    force the boundary southward late in the period. Northeastern
    areas near the KS/MO border have had a bit of rain lately, leaving
    them more sensitive. Otherwise, it's been dry across much of OK.=20
    Issues should primarily reside where soils have been partially
    compromised in northeastern areas, in urban areas, and any
    sections of the Ozarks or Boston Mountains that thunderstorms with
    heavy rainfall transect.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6JcSoLpPMAoIG3mXlrrw1ivQ9BbBREYoZEsirevNHU6ma63ijgnteiqi8nDHQiYPjB-1= 5CmcqpYM5NdycaZwmFt_94w$ for graphic product...

    ATTN...WFO...EAX...ICT...OUN...SGF...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 38169409 37899353 37259353 36639383 35409532=20
    35099798 35889815 36849682 37509557 38149468=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 Aug 12 00:45:34 2025
    AWUS01 KWNH 120045
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-NMZ000-120643-

    Mesoscale Precipitation Discussion 0912
    NWS Weather Prediction Center College Park MD
    844 PM EDT Mon Aug 11 2025

    Areas affected...portions of Eastern NM, the TX Panhandle, & OK

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

    Valid 120043Z - 120643Z

    Summary...Showers and thunderstorms across this region are
    expected to concentrate near southwest OK by 07z. Hourly amounts
    to 3" with local totals to 5" are expected, which would continue
    to lead to scattered flash flood concerns.

    Discussion...Thunderstorms continue to build and move across
    portions of eastern NM, the TX Panhandle, northwest TX, and
    portions of OK, focusing and being driven forward by outflow
    boundaries. They have a history of producing hourly amounts to 3"
    with local totals to 5" thus far this afternoon and evening. A ML
    CAPE gradient exists near the effective frontal zone, with pockets
    of 2000-3000 J/kg of instability in its warm sector. Effective
    bulk shear has spread eastward, with a magnitude of 25-35 kts
    regionally. Precipitable water values are 1-1.25" in the High
    Plains and 2"+ across portions of OK. So far, much of the
    thunderstorm activity has resembled pulse convection, with cell
    mergers and very short periods of training occurring and being
    important to heavy rain efficiency. In some areas, backbuilding
    has been noted. Central and southern OK convection has been
    backbuilding and pushing slowly westward, driven by outflow
    boundaries.=20

    Both the 12z REFS and 18z HREF probabilities suggest a set of
    outflow boundaries approaching Clovis NM helps drive a new
    convective cluster which joins forces with TX Panhandle activity
    in their combined quest to move eastward along an outflow boundary intersection. This cluster has the benefit of a stronger
    low-level inflow from the Gulf. Meanwhile, outflow boundaries in
    OK pushes convective clusters apart in central OK early on,
    driving some activity eastward to form one last merger not far
    from McAlester OK. Another, more significant merger between the
    TX Panhandle/northwest TX activity and the OK activity is
    advertised across far southwest OK by 07z with the TX activity
    appearing to grow in dominance/importance as it attempts to
    continue eastward thereafter, possibly aided to a growing cold
    pool. While there have been small pockets of heavy rainfall, much
    of the region has been dry during the past seven days. Scattered
    flash flood issues are expected to be mainly urban.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9aQARXSXRcfoWpzQbtTM7luyrGvNLApaUgxR8KwV5wRMFwP1DSY9Ui4XdT3JTmaavS0h= V0v3ZFu2_7UFnMKuHxWNg2Q$ for graphic product...

    ATTN...WFO...ABQ...AMA...FWD...LUB...MAF...OUN...SGF...SJT...
    TSA...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 36579481 36509413 35299454 34019570 33399700=20
    33269908 33740111 33350320 33420399 33580428=20
    33710506 34270438 35090434 35250306 35500190=20
    35790088 35599967 35459910 35379869 35349741=20
    35779619 36559495=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 12 01:13:06 2025
    AWUS01 KWNH 120113
    FFGMPD
    INZ000-ILZ000-120541-

    Mesoscale Precipitation Discussion 0913
    NWS Weather Prediction Center College Park MD
    912 PM EDT Mon Aug 11 2025

    Areas affected...northeast IL

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

    Valid 120111Z - 120541Z

    Summary...Showers and thunderstorms have begun to develop in
    north-central IL, trying to attain a training signature as they
    aim towards Chicagoland and grow in coverage. Hourly rain amounts
    to 2.5" with local totals to 4" are possible, which would be
    problematic in urban areas.

    Discussion...since 2330z, showers and thunderstorms have been
    developing, slowly growing in scale, and trying to align south and
    east of Peru IL within an area of low-level convergence. Hourly
    rain amounts in spots have exceeded 1.5" per radar estimates.=20
    Precipitable water values are ~1.9 per GPS data. ML CAPE is
    2500-3500 J/kg to their south. Effective bulk shear of 25-30 kts
    is trying to align the activity.

    The 12z & 18z HREF runs were insistent on this activity forming,
    whereas the 06z and 12z REFS had a much weaker signal, so used the
    HREF as a guide (outside of the IA contribution which is
    underperforming on the HREF). The convective packet is moving
    east-northeast at 15-20 kts, with individual cells moving quicker
    than the packet as a whole. Hourly rain amounts to 2.5" with
    local totals to 4" are possible over the next 3-4 hours. This
    could lead to problems in Chicagoland tonight.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8D0Dkr8qJgiiOsyFHMaTOAUmevGRDrB_k1_YukUqwjPYMd4mKpJvJOsTsDOnIOQO_dxT= KHM2l4AHhS_brtmO0U5dzfo$ for graphic product...

    ATTN...WFO...DVN...ILX...LOT...

    ATTN...RFC...MSR...NWC...

    LAT...LON 42208780 41668747 40738957 40698991 40858984=20
    41598892=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 12 03:31:05 2025
    AWUS01 KWNH 120331
    FFGMPD
    ILZ000-MOZ000-IAZ000-120900-

    Mesoscale Precipitation Discussion 0914
    NWS Weather Prediction Center College Park MD
    1130 PM EDT Mon Aug 11 2025

    Areas affected...Northeast Missouri, Southeast Iowa, Western
    Illinois

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

    Valid 120329Z - 120900Z

    Summary...Showers and thunderstorms expanding across northern
    Missouri will lift slowly northeast overnight. Rainfall rates
    within this convection will reach 1-2"/hr, locally higher at
    times, resulting in 1-2" of rainfall. This may cause flash
    flooding.

    Discussion...The regional radar mosaic tonight shows an expanding
    area of showers and thunderstorms developing from north-central
    Missouri into southeast Iowa. This convection is blossoming in
    response to ascent driven by an overlap of modest height falls
    downstream of a shortwave trough axis positioned over Nebraska,
    and an MCV from remnant convection moving into southern Iowa.
    Downstream of these features, a S/SW LLJ at 850mb has been
    recently measured via local VWPs to be 15 kts, which is
    originating from a region of elevated thermodynamics sufficient to
    fuel heavy rain in thunderstorms. As this LLJ locally backs and
    accelerates downstream of the MCV, it will draw PWs as high as 2
    inches, and MUCAPE above 2000 J/kg, northward, providing
    additional fuel for persistent convection within a WAA regime
    overnight.

    Rainfall rates as estimated via local radars have been generally
    modest so far at around 0.5-1"/hr. However, as the LLJ continues
    to strengthen it will not only resupply the more favorable
    thermodynamics northward, but also result in enhanced convergent
    ascent to drive stronger convection. During the next few hours,
    the CAMs, while mostly under-representing the current activity,
    suggest thunderstorms will become more widespread, and the HREF
    neighborhood probabilities indicate a 10-20% chance of 2"/hr rain
    rates developing, with brief rates to 3"/hr possible as shown by
    the 15-min HRRR rain accumulation. At the same time, while 0-6km
    mean winds will remain progressive to the northeast at 20-25 kts,
    sufficient bulk shear of 20-25 kts will help organize storms into
    clusters, coincident with Corfidi vectors collapsing to 5 kts or
    less and veering to the south. This indicates an increasing threat
    for backbuilding/training convection within the improving WAA.

    Although HREF 6-hr rainfall probabilities for 3" are modest at
    10-15%, indicating that generally 1-2" of rain is likely with
    locally higher amounts, this may still be sufficient to cause
    rapid runoff. Not only will the rates be intense, but FFG is as
    low as 1.5-2"/3hrs for which the HREF exceedance probabilities
    peak around 20%. This is further evidence for the increasing flash
    flood risk overnight, with at least isolated instances possible in
    urban areas, over the more vulnerable soils, or where the most
    significant training can occur.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6-Wg4J8PPfQV0EfImKwv_a2YKq5N6tCvRJ74PlVn6hiQp2b993WAitry3AS8TcYfvmL-= UtafYSWDJjsPlnjvfC8K56w$ for graphic product...

    ATTN...WFO...DMX...DVN...EAX...ILX...LSX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 42079071 41298973 40588957 39738995 39249075=20
    39199086 38789174 38629258 38949335 39559371=20
    40229386 40909354 41699259=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 12 04:23:52 2025
    AWUS01 KWNH 120423
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-121000-

    Mesoscale Precipitation Discussion 0915
    NWS Weather Prediction Center College Park MD
    1222 AM EDT Tue Aug 12 2025

    Areas affected...Eastern Oklahoma, Western Arkansas, far Northeast
    Texas

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

    Valid 120421Z - 121000Z

    Summary...Slow moving showers and thunderstorms will continue to
    pulse up along outflow boundaries and storm mergers overnight.
    Rainfall rates of 2-3"/hr are expected, which could produce 1-2"
    of rain in 30 minutes. Flash flooding is possible.

    Discussion...The regional radar mosaic tonight shows an expansion
    of convection across eastern Oklahoma into western Arkansas. This
    convection is associated with multiple remnant outflow boundaries
    that are clearly evident on radar, with convergence along these
    boundaries leading to rapid updraft intensification to produce
    dditional convective development. Estimated rainfall rates have
    been as high as 2"/hr from KSRX, supported by rich thermodynamics
    characterized by GPS measured PWs of 1.7 inches overlapping MUCAPE
    of 1000-2000 J/kg. Additional ascent is being provided via slow
    height falls downstream of a mid-level trough axis centered across
    KS/OK.

    The high-res CAMs are really struggling tonight with the current
    activity, so their solutions must be used cautiously. However, an
    ingredients based approach to the evolution combined with analysis
    of current radar trends suggests that there can be several more
    hours of slow moving storms before instability gets exhausted or
    overturned. With PWs and MUCAPE remaining robust within the
    pre-convective environment, any mergers/outflow collisions should
    additionally result in thunderstorm growth, and a slow trend E/SE
    in coverage is likely. 0-6km bulk shear across the region is
    minimal at less than 20 kts, so storms should remain primarily of
    the pulse variety. This suggests limited temporal duration of any
    individual cell, but with chaotic motions driven primarily by
    these small scale collisions thanks to weak 0-6km mean winds, some
    places could receive multiple rounds of convection.

    These thunderstorms will likely continue to produce rainfall rates
    of 2-3"/hr (HREF probabilities for 2"/hr 15-30%), so even though
    residence times will be limited, any storm may produce a quick
    1-2" of rain in well under an hour. This will be sufficient to
    cause rapid runoff despite elevated FFG, and a few instances of
    flash flooding are possible overnight, especially across any more
    sensitive or urban areas.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-s5q1JYBL5Es53Nme6TuhNiAPPNOU4PEWEWjW23lwSk5tBH8v8aZ9_SFS7_0m6LPLipU= 9KTQQ1-3tQOnpMSJUz4lh2g$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SGF...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 37169302 36809253 35989236 34889240 34079276=20
    33419371 33009481 32799566 32759667 33079736=20
    33579774 34119777 34389725 34659630 35069559=20
    35709530 36779400=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 12 06:47:47 2025
    AWUS01 KWNH 120647
    FFGMPD
    TXZ000-OKZ000-121200-

    Mesoscale Precipitation Discussion 0916
    NWS Weather Prediction Center College Park MD
    247 AM EDT Tue Aug 12 2025

    Areas affected...West/Central Oklahoma into far Northern Texas

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

    Valid 120646Z - 121200Z

    Summary...Slow moving showers and thunderstorms will move across
    parts of Oklahoma and Texas through morning. Rainfall rates of
    2-3"/hr are likely, which through this slow motion could produce
    2-4" of rainfall and instances of flash flooding.

    Discussion...The GOES-E IR imagery early this morning indicates a
    new swath of cooling cloud tops north of a large convective
    complex moving from the Texas Panhandle to along the Red River
    Valley of the South. This fresh convection is associated with
    increasing convergence along the nose of a S/SE oriented, but
    modest, 10-15kt 850mb LLJ measured via regional VWPs and analyzed
    by the SPC RAP. Despite the modest intensity, this LLJ is
    favorably transporting robust thermodynamics northward to support
    this new convection, with PWs above 1.75 inches and MUCAPE
    exceeding 1000 J/kg. Into these thermodynamics, forcing for ascent
    is being provided via convergence along the aforementioned nose of
    this LLJ, but also synoptically downstream of a trough axis
    kicking slowly eastward from the High Plains, and an embedded
    shortwave moving into the region through the base of the trough.
    Additionally, a small but well placed 300mb jet streak over KS is
    leaving favorable RRQ diffluence to increase deep layer lift.

    The CAMs are generally struggling with the current increase of
    convective coverage, so confidence in evolution through morning is
    somewhat limited. However, there is some evidence in the recent
    NAM3Km and RRFS of handling this new convection a bit better, so
    these are used to help gauge the flash flood risk. As the LLJ
    gradually veers (but with some acceleration immediately downstream
    of the shortwave) it should continue to resupply favorable
    thermodynamics to support thunderstorms with heavy rainfall. At
    the same time, forcing for ascent will persist for several more
    hours before the LLJ veers too far to the west by morning,
    suggesting thunderstorms will continue to expand. Rainfall rates
    within this development should exceed 2"/hr at times as reflected
    by both HREF and REFS neighborhood probabilities, and with mean
    0-6km winds of just 5-10 kts aligned with propagation vectors
    along the nose of this LLJ, regenerating and training cells with
    these intense rain rates are likely.

    Where the most pronounced training occurs, this could result in
    2-4" of rainfall as reflected by the HREF/REFS PMM. While there is
    considerable uncertainty into the placement of this heaviest
    rainfall due to the lack of model agreement and some interruption
    of the flow possible from other convective clusters in the
    vicinity, the EAS probabilities indicate the best threat will be
    along and just south of this LLJ nose. Regardless of the exact
    placement, slow moving/backbuilding of these intense rain rates
    will pose a flash flood risk during the next few hours.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-zBZKlRcWbXq2Q11z1MiHkmTXWqytgupKL_nDayQEDtE3iHItqR-6Xvncg_gWfN5ykiC= LY1VQaGXJEOrJgHBBWDIDJc$ for graphic product...

    ATTN...WFO...AMA...FWD...LUB...OUN...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 36629994 36309878 35869772 35169699 34549686=20
    34049707 33569747 33259812 33199891 33569973=20
    33990014 34780031 35420050 36020077 36500118=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 Aug 12 09:58:42 2025
    AWUS01 KWNH 120958
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-121430-

    Mesoscale Precipitation Discussion 0917
    NWS Weather Prediction Center College Park MD
    558 AM EDT Tue Aug 12 2025

    Areas affected...Central Gulf Coast through central Alabama

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

    Valid 120957Z - 121430Z

    Summary...Showers and thunderstorms streaming onshore will train
    north this morning. Rainfall rates of 2-3"/hr are likely, which
    could produce 2-4" of rain along the immediate coast. This may
    cause flash flooding.

    Discussion...The regional radar mosaic early this morning shows an
    expansion of showers with isolated thunderstorms across the
    northern Gulf. Although instability continues to be modest onshore
    (MUCAPE 500-1000 J/kg inland from the coast) a sharp instability
    gradient exists across the FL Panhandle westward to the coasts of
    AL and MS. Recent analysis of 850mb winds from the regional VWPs
    and the SPC RAP analysis indicate the inflow has increased to
    20-30 kts with some local backing to the SE, leading to increasing
    N-S oriented convergence which is helping to drive lines of
    convection pushing onshore. At the same time, weak MCVs noted in
    reflectivity and a surface trough analyzed by WPC are helping to
    enhance ascent locally as well.

    Ascent into the area will remain impressive through morning, and
    may actually intensify as the 850mb LLJ reaches 1.5x the mean wind
    (850mb winds to 30 kts, mean wind to 20 kts) forcing more broad
    lift. This ascent will act upon thermodynamics that will become
    increasingly robust through extreme PWs measured by GPS above 2.3
    inches and MUCAPE which will gradually expand inland both through
    the 850mb transport but also in response to daytime heating.
    Together, this suggests that convection will continue push
    onshore, while gradually spreading northward in response to the
    strengthening instability.

    The high-res CAMs have struggled this morning to resolve the
    ongoing activity, which is more widespread and intense than any
    available guidance. However, the recent HRRR runs have started to
    catch on and insist that convection will become widespread later
    this morning. This appears likely, and as the environment becomes
    more thermodynamically rich, rainfall rates will likely reach
    2-3"/hr as progged by both HREF neighborhood probabilities and the
    HRRR 15-min rainfall accumulation. More concerning to the flash
    flood risk will be that storms will likely train repeatedly south
    to north as mean 0-6km winds of 10-15 kts suggest progressive
    cells, but propagation vectors aligned anti-parallel and into the
    Gulf indicate backbuilding potential. Where this training is most
    prolonged, 2-4" of rainfall is possible through the morning.

    FFG across this area is quite high at 3-4"/3hrs, and HREF FFG
    exceedance probabilities are generally below 15%. However, where
    any of these narrow training bands persist, especially if they
    occur over urban areas, instances of flash flooding may result,
    with the greatest potential occurring along the immediate coast.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9mGE-pFkZny07w97O8ihRpXeXudfjyAWcejdl_7aYyLFwRq-vDMdHTt969QEt-t5BnRH= GQLDve1h_KI3zL_cashyD_0$ for graphic product...

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

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34128738 33708648 33128592 31628530 30388504=20
    30028536 30118611 30178665 30218707 30088793=20
    29498858 29138887 28928913 28978948 29128970=20
    29118999 29259022 29589018 29918978 30208937=20
    30458887 30738836 31338817 32178815 33098835=20
    33918831=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 12 12:09:51 2025
    AWUS01 KWNH 121209
    FFGMPD
    NCZ000-SCZ000-GAZ000-121808-

    Mesoscale Precipitation Discussion 0918
    NWS Weather Prediction Center College Park MD
    808 AM EDT Tue Aug 12 2025

    Areas affected...portions of central/Upstate South Carolina and
    central North Carolina

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

    Valid 121208Z - 121808Z

    Summary...Areas of heavier rainfall are materializing across the
    discussion area and 1 inch/hr rain rates are increasing in
    coverage. These rates are falling on sensitive ground conditions
    from prior rainfall. Flash flooding is possible this morning.

    Discussion...Over the past half hour, radar and satellite have
    indicated an uptick in convective intensity and coverage generally
    in areas from central South Carolina into southwestern North
    Carolina. This uptick in convective coverage appears to be tied
    to a weak mid-level shortwave trough/vorticity max over central
    South Carolina. The showers/storms are in a marginally unstable,
    but very moist environment (1.5-2 inch PW values, 1000 J/kg
    SBCAPE) with weak inhibition, fostering efficient rainfall rates
    with the ongoing activity. Latest MRMS data suggests that 1
    inch/hr rain rates were beginning to materialize in a few spots.=20 Furthermore, these rates were falling on sensitive local ground
    conditions due to prior rainfall, with FFG thresholds below 0.25
    inch/hr in a few spots across the discussion area.

    Models/observations are all suggestive of a gradual increase in
    both coverage and intensity of convection through the morning
    hours. With weak southwesterly steering flow in place, several
    areas of slow-moving convection and occasional cell mergers are
    expected to develop and boost rain rates into and above the 1
    inch/hr threshold at times. These rates will pose a flash flood
    risk, though the greatest risk of impacts may occur near sensitive
    urban areas and locales that have experienced the highest rainfall
    totals over the past 1-2 days. Areas just west of Columbia, SC
    could experience excessive runoff in the near term, with
    additional locales (including urban areas near Raleigh/Durham and
    Columbia) experiencing an increasing threat through 16Z/noon EDT
    or so.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4EKeuxKsk7-uujb1RTjzVj24QTN_HxsiRRw3en8OGRvX76ScVdRYaokfSDnyrYKlMvi9= Lvb1fb0043lWWUYt3lj3bWE$ for graphic product...

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

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 36297879 35577734 33738053 33548204 35158286=20
    35978159 36268043=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 12 21:16:50 2025
    AWUS01 KWNH 122115
    FFGMPD
    MIZ000-INZ000-ILZ000-130200-

    Mesoscale Precipitation Discussion 0919
    NWS Weather Prediction Center College Park MD
    514 PM EDT Tue Aug 12 2025

    Areas affected...Greater Chicagoland and surrounding portions of
    IL/OH/MI

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

    Valid 122110Z - 130200Z

    Summary...Hourly rainfall totals of 1-2" may locally train/repeat
    over sensitive urban areas. Locally significant/life threatening
    instances of flash flooding are possible.

    Discussion...Convection has proliferated in the vicinity of a
    surface trough of low pressure this afternoon, extending from
    western MI through northern IL. While deep layer moisture flux
    convergence has spiked synoptically along the trough axis, an
    enhanced meso to microscale area of near surface convergence
    exists along the southern shore of Lake Michigan (and most
    pronounced along the IL shore). This is occurring as upper-level shear/divergence is only increasing, as the base of a potent
    shortwave trough progresses eastward across northern MN/WI. The
    idealized right-entrance region of an associated jet streak (~110
    kts at 250 mb) may allow for this convection to persist for longer
    than anticipated, as CAMs have generally been much slower/weaker
    with convection than actual observational trends. With the
    mechanism for lift and convective longevity clearly established,
    plentiful instability (3000-3500 J/kg across northern IL) and
    anomalous tropopsheric moisture (~2.0" PWs above the 90th
    percentile, per ILX sounding climatology). MRMS estimates hourly
    rainfall amounts locally as high as 2", and even without
    training/repeating (thus far) the associated CREST unit streamflow
    values suggests minor to moderate flood impacts are already
    occurring (particularly where these 2" totals are co-located with
    more sensitive urbanized terrain).

    Going forward, CAMs suggest the potential for additional localized
    totals of 2-4" (HREF 40-km neighborhood exceedance probs for 3"
    threshold of 10-20% through 03z). Since most models were too slow
    to develop convection, much of this forecast rainfall may have
    simply occurred early. However, given the aforementioned favorable
    mesoscale environment (with little depletion of instability and
    increasingly favorable dynamics) it's quite possible that heavy
    rainfall will continue for several hours still, eventually coming
    to an end between 00-02z. Given the potential for
    training/repeating with little movement in the trough axis and
    baroclinic lake enhancement, a significant instance or two of
    flash flooding is possible (and may become life threatening in
    more sensitive, low-lying populated areas of Chicagoland).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-sAtEx_qMfvLfJ_Y_lQ-4btitGjJQjzNIHeugNXXgqFX5JYKzEWsIMiAeImX8FqLvam0= WiqkdDOBwKZk8uI-9NtV97I$ for graphic product...

    ATTN...WFO...ILX...IWX...LOT...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 42468708 42228647 41838622 41178670 40648751=20
    40468857 40608902 41598821 42218789=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Aug 13 06:49:24 2025
    AWUS01 KWNH 130649
    FFGMPD
    FLZ000-ALZ000-MSZ000-131200-

    Mesoscale Precipitation Discussion 0920
    NWS Weather Prediction Center College Park MD
    248 AM EDT Wed Aug 13 2025

    Areas affected...Portions of the Central Gulf Coast

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

    Valid 130647Z - 131200Z

    Summary...Showers and isolated thunderstorms will train onshore
    through morning from eastern MS through the western FL Panhandle.
    Rainfall rates within these tropical downpours will reach 3"/hr at
    times, which through training could produce stripes of 2-4" of
    rain. Flash flooding is possible.

    Discussion...The regional radar mosaic early this morning shows a
    rapid expansion of tropical showers with isolated thunderstorms
    aligned south to north in the vicinity of Mobile Bay, AL. This
    expanding convection is associated with a weak surface trough
    extending across the area, with upstream onshore flow from the
    Gulf drawing impressive moisture northward. The greatest
    instability (MUCAPE above 1000 J/kg) is confined to the immediate
    coast, and this has been the demarcation of the heaviest rainfall
    rates so far this morning, but PWs above 2 inches extend all the
    way into northern AL, with recent GPS measured PWs reaching 2.4
    inches near Mobile Bay. These extreme PWs and warm cloud depths
    over 15,000 ft have been supporting efficient warm-rain collision
    processes, with MRMS 15-min rainfall measured as high as 0.7
    inches (3"/hr) already in some of the cells training onshore.

    The high-res CAMs are actually in pretty good agreement both with
    the footprint and amount of the expected rainfall through around
    12Z, focusing from the AL/MS border eastward towards the Emerald
    Coast of the Florida Panhandle. Here, 850mb winds measured via
    current VWPs have already reached 15-25 kts, exceeding the mean
    wind of 10-15 kts to drive enhanced ascent through convergence. As
    this inflow continues to draw robust thermodynamics northward,
    regenerating cells are expected to develop across the Gulf and
    then repeatedly train northward and onshore.

    The HREF neighborhood rainfall rate probabilities for 2"/hr peak
    above 60% during the next few hours, suggesting the deeper cores
    will contain rates that may exceed 3"/hr at times. Although storms
    will move steadily northward, with several rounds of rainfall
    anticipated, this could result in 2-4" of rain with locally higher
    amounts possible as reflected by HREF/REFS 5"/6hr probabilities
    reaching 15-40%. The heaviest rainfall is expected to be along the
    immediate coast in the vicinity of Mobile Bay, but as the axis of
    elevated 850mb winds push northeast through morning, the
    environment could support more expansive heavy rainfall farther
    north into parts of southern AL as well. This suggests that while
    any impacts will be most likely along the immediate coast and over
    urban areas, any training of these intense rates, especially as
    instability pushes northward later this morning, could result in
    instances of flash flooding.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-L8Z3naUd_aU_PnOhf_tjoUlmUbMikEjE__X7VOIyUgudZcI23OlZBoO6tphKcpJ5aE9= 7vmbHKW50YIu6jCatQXU5Zo$ for graphic product...

    ATTN...WFO...BMX...LIX...MOB...TAE...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 32218747 32128689 31788655 31188610 30758593=20
    30308583 30118653 30068714 29998814 30068854=20
    30148882 30858909 31258859 31628832 32008791=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 Aug 13 08:42:55 2025
    AWUS01 KWNH 130842
    FFGMPD
    TNZ000-KYZ000-ALZ000-MSZ000-MOZ000-ARZ000-131330-

    Mesoscale Precipitation Discussion 0921
    NWS Weather Prediction Center College Park MD
    442 AM EDT Wed Aug 13 2025

    Areas affected...Northeast Arkansas through Central Tennessee

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

    Valid 130841Z - 131330Z

    Summary...Showers and thunderstorms will drift across the region
    through morning. Intense rainfall rates of 2-4"/hr will likely
    cause pockets of 2-3" of rainfall in less than 1 hour. This may
    cause instances of flash flooding, especially in urban areas.

    Discussion...Showers and thunderstorms noted on the regional radar
    mosaic early this morning have rapidly expanded across western and
    central Tennessee and back into northeast Arkansas. This
    convection is blossoming within a plume of elevated moisture
    evident on the GOES-E WV imagery on SW flow emerging from the Gulf
    Coast downstream of a mid-level trough axis that is still hung
    back across MO/AR. Cloud top cooling is continuing to occur across
    the area as well, indicating that convection is going to continue
    to develop and intensify in response to deep layer ascent provided
    through modest height falls, weak upper jet diffluence, and
    low-level convergence along a surface trough. Together these are
    driving sufficient lift for the rapid uptick in thunderstorm
    coverage, as this ascent is working upon robust thermodynamics
    characterized by PWs measured by GPS of more than 2 inches
    coincident with a ribbon of 1000-2000 J/kg MUCAPE.

    Storms that have developed already have produced MRMS measured
    1-hr rainfall of more than 2 inches in some areas, and the
    resulting FLASH unit streamflow response has reached 200-400
    cfs/smi. This has prompted already at least one FFW SW of
    Nashville, TN. The concern through the morning will be that these
    storms will continue to produce excessive rainfall rates of
    2-4"/hr, although the HREF and REFS neighborhood probabilities for
    2"/1hr are modest at just 10-15%. However, the CAMs are really
    struggling with the ongoing activity, so the ensemble
    probabilities are suffering and are likely too low. Additionally,
    with the primary 850mb inflow from the W/SW, propagation vectors
    have dropped to 5 kts or less and are aligned with the weak mean
    0-6km wind (around 10 kts) to the primary trough axis. This is
    resulting in cells that at times have net motion near zero,
    especially near mergers/outflow collisions driven by pulse storms
    in the weak shear environment, lengthening the duration of this
    heavy rainfall.

    Although confidence in the evolution the next few hours is lower
    than typical due to lack of model support, the recent HRRR has
    started to capture the ongoing scenario and has exhibited a rapid
    increase in coverage and amounts of QPF the next few hours. This
    indicates that the environment will remain favorable for heavy
    rainfall, and where storms train/stall, 2-3" of rainfall could
    occur in less than 1 hour, with locally 4" possible by later this
    morning. Despite elevated FFG from recent dryness, these rainfall
    rates falling atop any more vulnerable soils or less-permeable
    urban areas, could result in flash flooding.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6CTDGpysdS25mf6q1KvIInXWRn_m-k2LUW9IXXpzKQWXqhFp9f5QAxUfPAZIbAGIscEC= Nnoi-oKGS1ChFISn6RX9XMA$ for graphic product...

    ATTN...WFO...HUN...LMK...LZK...MEG...OHX...PAH...

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 37008724 36908570 36288544 35738569 35128660=20
    34838778 34848882 35069004 35549099 36289126=20
    36628992=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Aug 13 09:52:55 2025
    AWUS01 KWNH 130952
    FFGMPD
    VAZ000-NCZ000-SCZ000-GAZ000-TNZ000-KYZ000-ALZ000-131500-

    Mesoscale Precipitation Discussion 0922
    NWS Weather Prediction Center College Park MD
    552 AM EDT Wed Aug 13 2025

    Areas affected...northern Alabama through far northeast Tennessee

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

    Valid 130951Z - 131500Z

    Summary...Showers and thunderstorms will expand and intensify
    through the morning along a low-level convergence axis. Rainfall
    rates within the stronger storms will reach 1-2"/hr, which through
    training could produce 2-4" of rainfall. Flash flooding is
    possible.

    Discussion...The GOES-E IR imagery early this morning shows a slow
    uptick in coverage of rapidly cooling cloud tops along a linear
    boundary from northern AL through northeast TN. The colder and
    deeper clouds are associated with thunderstorms evident on the
    regional radar mosaic, with 1-hr rainfall measured via MRMS as
    much as 1.5" beneath the stronger cells.

    These thunderstorms are developing in response to intensifying
    ascent impinging across robust thermodynamics. A mid-level trough
    axis remains positioned well west of the region, which is leaving
    pronounced low-to-mid level SW flow emerging from the Gulf and
    advecting PWs above 2 inches northeastward, which is above the
    90th percentile according to the SPC sounding climatology. This is
    overlapped with a ribbon of MUCAPE 1000-2000 J/kg to provide an
    environment favorable for heavy rain. Acting upon this airmass is
    pronounced ascent driven by multiple ripples/weak shortwaves
    moving through the flow combined with weak RRQ diffluence in the
    tail of a jet streak positioned just NW of TN. Additionally, the
    850mb LLJ has been steady from the WSW at 15-25 kts on the
    regional VWPs, with the convergent nose providing an additional
    mechanism for lift.

    The result of this has been the growth and expansion of convection
    the past hour or so, which is likely to continue for the next
    several hours, potentially enhanced by an outflow boundary
    dropping southeast as well. The high-res CAMs are struggling to
    resolve the current activity, although the trends in the recent
    HRRR, as well as the ARW and HREF-PMM support the increasing flash
    flood risk. Rainfall rates will likely continue to surge to
    1-2"/hr, and storms should move slowly northeast on mean 0-6km
    winds of 5-10 kts. Concerning, however, is that propagation
    vectors are aligned to the mean wind and also just 5-10 kts,
    suggesting that cells will continue to regenerate along this
    convergent nose and track northeast, a clear training signature
    for the next several hours. While eventually the LLJ should veer
    more to the west to reduce the training threat, until this happens
    some areas could receive 2-4" of rainfall with locally higher
    amounts (HREF neighborhood probabilities for 5" up to 15%).

    Additionally, this rain could fall atop vulnerable soils where
    3-hr FFG is as low as 1.5-2 inches, and the HREF exceedance
    probabilities rise to 15-30%. Any training to produce locally
    heavier rainfall across these soils or in any urban areas/more
    sensitive terrain could produce impacts from flash flooding.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6FO-tex0-VR9730QWMzXkVuqEH1jhmntkVp9Buu4CWkRLPhxKB_RtcBPAICXYBmG8tFu= gq8yUGg2xBzt1sJcWcqYpyk$ for graphic product...

    ATTN...WFO...BMX...FFC...GSP...HUN...JKL...MRX...OHX...RLX...
    RNK...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 37148163 36968119 36488125 36048173 35678219=20
    34928316 34528412 34298496 34008606 33918704=20
    34098759 34878735 35708625 36238530 36618398=20
    37068243=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Aug 13 12:05:28 2025
    AWUS01 KWNH 131205
    FFGMPD
    FLZ000-ALZ000-131630-

    Mesoscale Precipitation Discussion 0923
    NWS Weather Prediction Center College Park MD
    804 AM EDT Wed Aug 13 2025

    Areas affected...Southern AL...Western FL Panhandle

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

    Valid 131204Z - 131630Z

    SUMMARY...Locally concentrated bands of showers and thunderstorms
    with high rainfall rates will continue this morning across
    portions of southern AL and the western FL Panhandle. Areas of
    flash flooding will be possible, and especially for the more
    urbanized locations.

    DISCUSSION...The early morning GOES_E IR satellite imagery along
    with surface observations shows a well-defined low-level vort
    center and a fairly sharp surface trough advancing
    east-northeastward to the east of Mobile Bay. This energy
    continues to foster some deep convection around its southern flank
    as very moist, convergent and unstable low-level flow advects
    inland off the nearby Gulf of America and into portions of
    southern AL and the western FL Panhandle.

    MLCAPE values of 1500+ J/kg are pooled up across the western FL
    Panhandle with PWs of 2.25+ inches, and this region in particular
    will tend to be the primary focus area for additional bands of
    convection over the next few hours. Rainfall rates up to 2
    inches/hour are expected to continue, and some additional storm
    totals amounts of up to 3 to 5 inches will be possible given
    localized cell-training concerns with these bands of convection
    that cross the Gulf Coast and advance inland.

    Some locations that will likely be impacted by heavy rainfall this
    morning include the Pensacola to Panama City corridor, and there
    may be some localized urban flooding concerns that materialize.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_invE_lQ121_TUQZYWLQcGoIH8TrLgKC8MsN5EYCKBkQBGPb911rfyn-cD2VFDrD7m4I= ZULtbITHY847L4EDYbJs5PA$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 31338613 30878515 30278497 29848528 30298638=20
    30208758 30368800 30988802 31288733=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Aug 13 12:36:30 2025
    AWUS01 KWNH 131236
    FFGMPD
    LAZ000-TXZ000-131800-

    Mesoscale Precipitation Discussion 0924
    NWS Weather Prediction Center College Park MD
    835 AM EDT Wed Aug 13 2025

    Areas affected...Portions of Central to Northeast TX

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

    Valid 131235Z - 131800Z

    SUMMARY...Slow-moving bands of heavy showers and thunderstorms
    over portions of central to northeast TX should foster at least an
    isolated threat for flash flooding going through midday.

    DISCUSSION...The early morning GOES-E IR/WV satellite imagery
    shows a well-defined mid-level vort center/shortwave gradually
    crossing central to northeast TX which coupled with a surface
    trough is helping to foster a broken axis of slow-moving shower
    and thunderstorm activity.

    Much of the convection is somewhat elevated, but is also focusing
    within a convergent low-level flow regime around the southern
    flank of the vort energy. MUCAPE value of 1000 to 2000 J/kg are
    noted, with PWs of 2.0 to 2.25 inches helping to support rainfall
    rates of up to 2.5 inches/hour with some of the stronger storms.

    Weak and somewhat variable upwind propagation vectors are noted
    around the southern flank of the vort energy, and this suggests an
    environment that is conducive for backbuilding and locally
    training showers and thunderstorms. Given this and the cooling
    cloud top trends, this activity is likely to persist for at least
    the next few hours across areas of northeast TX in particular.

    Recent HRRR guidance suggests locally an additional 3 to 5 inches
    of rain, and these additional rains are likely to result in
    scattered areas of flash flooding going through midday.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-qz1LvMSVK_QYA8dDdv1DtyEoP5H8DRZDG0c1mOOvH26k0xmaMnQfbtdnBy3XMYwOzhF= hk36v9g2pQPJj_cCZgRvEcg$ for graphic product...

    ATTN...WFO...FWD...SHV...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 33639463 32899395 31729491 31389691 31899810=20
    32479795 32759622=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Aug 13 14:27:21 2025
    AWUS01 KWNH 131426
    FFGMPD
    NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-DCZ000-WVZ000-132025-

    Mesoscale Precipitation Discussion 0925
    NWS Weather Prediction Center College Park MD
    1025 AM EDT Wed Aug 13 2025

    Areas affected...Portions of the Central Appalachians and
    Mid-Atlantic

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

    Valid 131425Z - 132025Z

    SUMMARY...Clusters of heavy showers and thunderstorms with locally
    extreme rainfall rates will tend to expand in coverage over the
    next several hours. Scattered areas of flash flooding will
    gradually become likely, and especially later this afternoon
    closer to the I-95 corridor of the Mid-Atlantic where an urban
    flash flood threat is expected to evolve.

    DISCUSSION...The latest satellite and radar imagery shows a band
    of heavy showers and thunderstorms moving into northern WV, and
    the latest trends show cooling cloud tops associated with this
    activity.

    This convection is associated with the southwest flank of
    mid-level vort energy going into the central Appalachians which is
    embedded within a very moist and moderately unstable environment.
    MLCAPE values across northern WV and western MD, and areas east of
    the Blue Ridge over the Mid-Atlantic, are locally on the order of
    1000+ J/kg. However, the PWs are quite high and locally over 2
    standard deviations above normal.

    In fact, the 12Z RAOB soundings from KPIT and KIAD showed PWs of
    1.86 and 2.22 inches respectively with tall skinny CAPE profiles
    and elevated WBZ/freezing levels. This is strongly suggestive of a
    very efficient and tropical environment that will promote highly
    efficient processes for locally extreme rainfall rates that may
    reach well into the 2 to 3+ inch/hour range.

    Convection should tend to generally build in coverage over the
    next several hours as this vort energy advances off to the east
    across the central Appalachians and northern Mid-Atlantic region.
    This will support heavy showers and thunderstorms advancing east
    through central and northern WV, western MD and southwest PA in
    the near-term.

    However, as instability and convergent low-level flow becomes
    better established this afternoon east of the Blue Ridge and into
    the Chesapeake Bay region, there will likely be the development
    and expansion of very heavy showers and thunderstorms across much
    of northern VA, central to northeast MD and southern PA, including
    areas along the I-95 corridor from Washington D.C. to Philadelphia.

    The latest hires model guidance may be underplaying the rainfall
    potential given the level of moisture that is in place, and there
    will the influence of diurnal heating and orographics that will
    also support an uptick in coverage of showers and thunderstorms.

    Slow cell-motions and localized cell-training concerns coupled
    with locally extreme rainfall rates may support some localized
    rainfall totals of 3 to 5 inches. Areas of scattered flash
    flooding will become likely in time, and this will include an
    increasing urban flash flood threat near the I-95 corridor by
    later this afternoon.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_BDgP8HIv5WDq8BcVl3dNGRRle70i2vNKdHEmFfl2ZsQtkVHeh08Ox-BZ5pMJwmlNwHH= O9WllFgWJyH_VkEemcudl3o$ for graphic product...

    ATTN...WFO...AKQ...BGM...CTP...LWX...PBZ...PHI...RLX...RNK...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 41027601 40757482 39907456 39127511 38337647=20
    37887805 37677977 37758073 38308145 39238129=20
    39828054 40087923 40477767=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Aug 13 15:01:30 2025
    AWUS01 KWNH 131501
    FFGMPD
    VAZ000-NCZ000-SCZ000-GAZ000-TNZ000-ALZ000-132100-

    Mesoscale Precipitation Discussion 0926
    NWS Weather Prediction Center College Park MD
    1100 AM EDT Wed Aug 13 2025

    Areas affected...Portions of the TN Valley...Southern Appalachians

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

    Valid 131500Z - 132100Z

    SUMMARY...Broken areas of heavy showers and thunderstorms will
    continue to impact areas of the TN Valley and the southern
    Appalachians going through the mid-afternoon hours. Additional
    scattered areas of flash flooding are likely.

    DISCUSSION...The latest GOES-E IR/WV satellite imagery along with
    radar shows an expansive axis of broken showers and thunderstorms
    extending from northern AL through eastern TN, northwest NC and
    southwest VA. This activity continues to be focused along an
    elongated axis of mid-level vort energy which is interacting with
    a combination of very moist/unstable air and favorable orographics
    near areas of higher terrain.

    3-hour MLCAPE differentials off the latest RAP shows a notable
    increase in instability across areas of eastern AL through
    northern GA and into the eastern slopes of the southern
    Appalachians. This instability along with moist southerly flow and
    influence from differential heating boundaries ahead of the vort
    energy should favor a general expansion of convection off to the
    east going through the early and mid-afternoon hours.

    PWs are locally over 2 standard deviations above normal and the
    environment is strongly conducive for highly efficient rainfall
    processes and potentially extreme rainfall rates. Areas of
    greatest short-term concern may tend to be across northeast AL
    through far southeast TN and northern GA where visible satellite
    imagery shows a well-defined differential heating boundary and an
    agitated CU field expanding in coverage.

    Additional areas of convection near and just east of the southern
    Appalachians from northwest SC and western NC into southwest VA
    will be expected as well with locally very high rainfall rates.
    Slow-moving cell-motions and the efficient tropical environment
    will support locally 2 to 3 inch/hour rainfall rates and some
    spotty storm totals of 3 to 5 inches by later this afternoon.

    These rains are likely to support additional scattered areas of
    flash flooding, and especially with locally wet/saturated
    antecedent conditions.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_fOPX_jkq-ATXh6gnquYJd8ItVsuzAAcrDAqm9NSjWPAJQXv4XeY47xX1cYITDPhyCBU= d8SBy8rAec8NJrPkWaAKdeU$ for graphic product...

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

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 37218083 36798037 35848104 34808215 34338299=20
    33508461 33308591 33408728 33978761 34758682=20
    35558556 36318387 36898240=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Aug 13 18:10:18 2025
    AWUS01 KWNH 131810
    FFGMPD
    MAZ000-NHZ000-VTZ000-CTZ000-NYZ000-NJZ000-PAZ000-140000-

    Mesoscale Precipitation Discussion 0927
    NWS Weather Prediction Center College Park MD
    208 PM EDT Wed Aug 13 2025

    Areas affected...Northeast PA...Northern NJ...Southeast
    NY...Southern New England

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

    Valid 131808Z - 140000Z

    SUMMARY...Increasing coverage of heavy showers and thunderstorms
    may produce isolated to scattered areas of flash flooding going
    through early this evening.

    DISCUSSION...The early afternoon GOES-E visible satellite imagery
    along with radar shows a gradual expansion of shower and
    thunderstorm activity occurring across areas of northeast PA and
    southeast NY. This convection is forming within an increasingly
    moist and unstable airmass that is currently characterized by
    MLCAPE values of 1000 to 2000 J/kg and PWs of generally near 1.75
    inches.

    Meanwhile, there is some upper-level support with the approach of
    an upstream vort center over northern PA which coupled with
    localized orographics and additional diurnal heating should favor
    additional expansion of heavy shower and thunderstorm activity
    over the next several hours which will include areas farther east
    eventually inclusive of northern NJ, the northwest suburbs of New
    York City, and adjacent areas of southern New England.

    Rainfall rates with the stronger storms will be capable of
    reaching 1.5 to 2.5 inches/hour, and with slow cell-motions and
    some concerns for localized backbuilding and training of
    convective cells, some rainfall totals by this evening may reach 3
    to 4+ inches. This is generally supported by the 12Z HREF guidance.

    The antecedent conditions across much of the region are on the dry
    side, and this will mitigate the flash flood threat to an extent.
    However, with such high rainfall rate potential and the localized
    storm totals that may occur, there may be some isolated to
    scattered flash flooding concerns. This will especially be the
    case near areas of more rugged terrain such as the Poconos and
    Catskills, along with any of the more urbanized locations to the
    northwest of New York City and across southern New England.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9fDd8jSDjRgfW5Fk6LwTG4L9XjIxiNXUHagBbH6WsG2upyGby22f4yc1wrSTRm2bKh8e= _ly2h57bo7DeSV2bqFftXYI$ for graphic product...

    ATTN...WFO...ALY...BGM...BOX...BTV...CTP...GYX...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 43657338 43497218 42507219 41807271 41257366=20
    40897475 41037599 41497634 41827601 42297536=20
    42907444=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Aug 13 20:19:11 2025
    AWUS01 KWNH 132019
    FFGMPD
    TNZ000-ALZ000-MSZ000-140215-

    Mesoscale Precipitation Discussion 0928
    NWS Weather Prediction Center College Park MD
    418 PM EDT Wed Aug 13 2025

    Areas affected...Mid-South

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

    Valid 132018Z - 140215Z

    SUMMARY...Broken areas of slow-moving showers and thunderstorms
    will continue to impact areas of the Mid-South going into the
    evening hours. Additional isolated to scattered areas of flash
    flooding will be possible.

    DISCUSSION...The latest GOES-E visible satellite imagery shows
    areas of slow-moving showers and thunderstorms with high rainfall
    rates impacting portions of middle TN down through northwest AL
    and northeast MS. This activity is embedded within a very noist
    and unstable airmass with relatively divergent flow aloft and some
    modest effective bulk shear facilitating some loose organization
    of the convective cells.

    MLCAPE values of 1500 to 2500 J/kg are in place with PWs of 2.0 to
    2.25 inches and this will continue to yield high rainfall rates
    capable of reaching 2 to 3 inches/hour with the more organized and
    stronger storms. The cell-motions are generally off to the
    south-southeast with the deeper layer flow, but the weak steering
    currents should maintain slow cell-motions through the evening
    hours.

    Some additional expansion of convection may occur over the next
    couple of hours as a combination of locally stronger instability
    and outflow boundary collisions favor swaths of more convective
    initiation. The latest hires guidance suggests areas of middle TN
    down through northwest AL should tend to be the primary corridor
    of heavier rainfall potential over the next few hours. This is
    also where the 12Z HREF has some of the higher probabilities for
    exceeding the 3-hour FFG values.

    Locally an additional 3 to 4+ inches will be possible through this
    evening, and these rains should continue to support concerns for
    isolated to scattered areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9d-nBPNtLrDdhYGfgu8Q-VHVfmydrNgs6mrBm7TISgI5CsL5g1i0EBGnDbvBpOyFa_VC= N0nECrQk1P3SenIXCMa91bE$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...MEG...OHX...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 36248717 36068624 35098609 33558685 32908804=20
    32928901 33908931 35388849=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Aug 13 20:59:17 2025
    AWUS01 KWNH 132059
    FFGMPD CTZ000-NYZ000-NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-DCZ000-WVZ000-OHZ000-14025=
    5-

    Mesoscale Precipitation Discussion 0929
    NWS Weather Prediction Center College Park MD
    455 PM EDT Wed Aug 13 2025

    Areas affected...Portions of the Central Appalachians and into the Central/Northern Mid-Atlantic and Southern New England

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

    Valid 132055Z - 140255Z

    SUMMARY...Clusters of heavy showers and thunderstorms with locally
    extreme rainfall rates will continue going into the evening hours
    across the interior of the central and northern Mid-Atlantic
    region. Scattered areas of flash flooding will be likely which
    will include strong concerns for urban flash flooding impacts near
    and along the I-95 corridor.

    DISCUSSION...The latest satellite and radar imagery shows clusters
    of heavy showers and thunderstorms impacting central to northern
    VA with some recent development noted across central MD. Meanwhile
    farther off to the northeast, there are locally more organized
    clusters of cold-topped convection seen impacting eastern PA.

    The convection continues to be associated with the leading edge of
    an elongated mid-level shear axis/vort center while interacting
    with a very moist and strongly unstable airmass that has pooled
    across much of the Mid-Atlantic region east of the Blue Ridge.
    MLCAPE values of 2000 to 2500 J/kg are noted across central VA up
    through southeast PA with some uptick in low-level moisture
    convergence noted across the region over the last hour including
    the middle and upper parts of the Chesapeake Bay area. The PWs are
    very high and locally over 2 standard deviations above normal,
    with values of 2.0 to 2.25 inches in place.

    Early morning RAOB soundings showed tall skinny CAPE profiles and
    elevated WBZ/freezing levels. This again strongly supports a very
    efficient and tropical environment that will promote highly
    efficient processes for extreme rainfall rate potential. Already
    some of the stronger storm clusters have been producing rainfall
    rates well into the 2 to 3 inch/hour range.

    Convection should tend to generally build off to the east through
    this evening into portions of the I-95 corridor from near
    Washington D.C up through Philadelphia and then on up to at least
    near the New York City metropolitan area. Meanwhile, the southwest
    flank of the MPD area involving central VA back westward into the
    central Appalachians will remain an area for convection as well
    given proximity of a well-defined outflow boundary. Radar shows
    locally concentrated areas of heavy thunderstorms across these
    areas.

    Localized/spotty additional rainfall totals of 3 to 4+ inches will
    still be possible going through the evening hours. This will
    likely promote scattered areas of flash flooding with concerns for
    potentially considerable urban flooding impacts if some of the
    heavier rainfall totals materialize over some of the larger
    metropolitan areas.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_tydoPRFcqIscxgWPKUD8vbbjFq-kOOhQuFnWq8Sae1XG1Jm9JdMcOxb_26om-e5wmLK= eI0OVTd9MQ24M4l2Pio-dU0$ for graphic product...

    ATTN...WFO...AKQ...ALY...BOX...CTP...LWX...OKX...PHI...RLX...
    RNK...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 41947338 41577241 39937358 38537549 37567763=20
    37528000 37888137 38608217 39168190 39228076=20
    38897995 38717888 39177744 40247621 41017485=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 Aug 14 00:46:45 2025
    AWUS01 KWNH 140046
    FFGMPD
    PAZ000-WVZ000-OHZ000-140415-

    Mesoscale Precipitation Discussion 0930
    NWS Weather Prediction Center College Park MD
    845 PM EDT Wed Aug 13 2025

    Areas affected...Far eastern OH...western PA...extreme northern WV

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

    Valid 140045Z - 140415Z

    Summary...Locally training thunderstorm segments will maintain the
    threat of isolated to scattered flash flooding through 4Z, with
    localized 2-3" possible.

    Discussion...Radar mosaic over the eastern OH Valley depicts two
    segments of thunderstorms exhibitng training characteristics ahead
    of a slow moving cold front approaching from the northwest. One
    segment of thunderstorms containing estimated 2-2.5"/hr rainfall
    rates over Youngstown, OH prompted a Flash Flood Warning as they
    trained over the city.

    These very efficient rainfall rates suggest the environment in the
    prefrontal airmass remains quite favorable for efficient warm
    rainfall production in any additional convection which develops.
    Recent mesoanalysis data corroborates this idea, and suggests
    1.75-1.8" PWATs (around the 97th percentile per the NAEFS),
    1000-1500 J/kg MLCAPE (with no CIN), and 20 kts of effective shear
    (oriented semi-parallel to the initiating boundary) are in the
    vicinity of the ongoing activity even with loss of diurnal
    heating. As such, the concern is for additional training segments
    to develop in the short term with additional 2-2.5"/hr rates
    possible. While the area has been dry as of late per NASA SPoRT,
    recent runs of the HRRR suggest localized amounts of 2-3" will be
    possible through 4Z, which could prompt additional instances of
    flash flooding as 1 HR FFGs are in the 1.5-2"/hr range.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8tK9BEc_yBGSTwd_WQUg7sobBt85XDGfZudaEYMCp3tjvmwXkPsw9TQprCCKAd_tiUla= jBx1epnCvRek3fRM759olW4$ for graphic product...

    ATTN...WFO...CLE...CTP...PBZ...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 41477986 41267878 40707858 40297896 40117970=20
    40228090 40618133 41228092=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Aug 14 04:24:19 2025
    AWUS01 KWNH 140421
    FFGMPD
    MNZ000-SDZ000-NDZ000-140857-

    Mesoscale Precipitation Discussion 0931
    NWS Weather Prediction Center College Park MD
    1220 AM EDT Thu Aug 14 2025

    Areas affected...Northeast SDak...Southeast NDak...Far
    West-central MN...

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

    Valid 140417Z - 140857Z

    SUMMARY...Regenerative warm-air advection thunderstorms will be
    slow to move initially resulting in spots of 2-3.5" and possible
    localized flash flooding, before shifting east-northeast toward
    early morning.

    DISCUSSION...GOES-E 10.3um and KABR RADAR show a few bands of
    thunderstorms across northeast South Dakota into far southeast
    North Dakota with downstream cirrus and lighter showers extending
    into western Minnesota. GOES-E WV and RAP analysis shows an
    exiting and flattening shortwave within synoptic scale ridging
    across south central MN into northeast IA, while a stronger
    shortwave and associated linear convective complex along the
    southern flank of the wave starting to reach central SDak and Sand
    Hills of NEB. The low-level jet has responded while recently
    strengthening to 45-50kts at 850mb with solid veered 925-700mb
    profile along/ahead of the approaching wave. This is obliquely
    intersecting the lingering boundary left in the wake of the prior
    wave. Recent strengthening and increasing deeper layer moisture
    with total PWat values up to 1.75" helps to differentiate the
    isentropic boundary across the southern portion of the Red River
    Valley; and given increasing core of the unstable air north-south
    axis generally along 98-99W with values of 2000-2500 J/kg MUCAPEs.
    The stronger moisture flux convergence is increasing rainfall
    efficiency for the thunderstorms. Rates of 1.5-2"/hr are starting
    to become more common with the recent cooling noted in the
    convective tops.=20

    Along with the strengthening flux convergence, the veered inflow
    is also supporting southwestward upwind propagation and given the
    sharpness of the ridging between the two mid-level waves, the
    deeper layer steering is also slackened to reduce eastward cell
    motions as well. This has resulted in back-building and localized
    training of downdrafts locally along the best isentropic upglide
    ascent plane to increase duration over an hour with repeating that
    may allow for localized 2-3.5" totals over the next few hours.=20
    Hourly rates are near the hourly FFG, but those locally higher
    totals have a good potential to exceed the 3hr FFG values which
    range from 1.5-2.5" across the area of concern. As such,
    localized flash flooding is considered possible for the next few
    hours. As the MCS/shortwave passes, winds will remain strong,
    but likely veer further and increase forward propagation into
    northwest and west-central MN...but with the decrease in local
    duration potential for exceedance will diminish.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4OdAPkGsM-ff6LYoFoLjaaDhOcApoe6CL-SGFGv2L4c2SAtoFdHry8aUUo1Gaz8cSaah= 1thAPr2Ybi-eIdpKsf40DnQ$ for graphic product...

    ATTN...WFO...ABR...FGF...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 46839674 46239622 45649600 45059601 44669643=20
    44739700 44939737 45409775 45799795 46059800=20
    46439794 46819753=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Aug 14 18:34:57 2025
    AWUS01 KWNH 141834
    FFGMPD
    VAZ000-NCZ000-SCZ000-150030-

    Mesoscale Precipitation Discussion 0932
    NWS Weather Prediction Center College Park MD
    233 PM EDT Thu Aug 14 2025

    Areas affected...SC Pee Dee...Southern and Eastern NC...Southeast
    VA

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

    Valid 141833Z - 150030Z

    SUMMARY...Clusters of heavy showers and thunderstorms will be
    developing and expanding in coverage going through the afternoon
    hours. High rainfall rates will pose a threat for scattered areas
    of flash flooding.

    DISCUSSION...A well-defined mid-level vort center with a weak
    surface low and associated trough is seen advancing northeast
    across central and eastern SC which will be lifting up across
    southern and eastern NC going through the afternoon hours. This
    energy will be interacting with increasing boundary layer
    instability and the pooling of tropical moisture for expanding
    clusters of heavy showers and thunderstorms.

    MLCAPE values have already increased to 2000 to 3000 J/kg across
    eastern NC with the aid of stronger solar insolation and some
    additional uptick and expansion of this instability is expected
    over the next couple of hours. PWs are very high from the SC Pee
    Dee region up through eastern NC with values of 2.25 to 2.5 inches
    noted.

    The strong instability and deep moisture parameters are expected
    to favor showers and thunderstorms with extremely high rainfall
    rate potential, with some of the stronger convective cells
    potentially yielding rainfall rates 2 to 4 inches/hour. Some
    uptick in low-level moisture convergence around the eastern flank
    of the aforementioned vort/low center will help to also facilitate
    some of these higher rainfall rates and a general uptick in
    convective organization by later this afternoon.

    By early this evening, there will also be some attention focused
    across southeast VA as a cold front settling southward toward the
    Hampton Roads/Tidewater region begins to interact with this low to
    mid-level energy lifting northeast across eastern NC. Stronger
    low-level convergence and an improvement in the instability
    profile by this evening will eventually drive an increasing threat
    of showers and thunderstorms with high rainfall rates.

    Expect some localized rainfall totals of 3 to 5 inches to be
    possible given the high rainfall rates, and potential for some
    spotty cell-training. Much of the hires model CAM guidance
    suggests southern and eastern NC will be the area of greatest
    concern through 21Z and 00Z, but portions of southeast VA in this
    time frame may begin to see the aforementioned uptick in
    convection that could drive a couple inches of rain, with more
    potential for heavy rainfall afterwards going well into the
    evening hours.

    Scattered areas of flash flooding will be possible which will
    include some localized urban flooding concerns as well.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-r3hLWvM7_EufC2TIGrholpHMsBWgelijqt1V4zV-j2XAu0MhWGq9L2PSfVfiJRmqGJ3= PvXwMw6lOZd6TQZVa90KqxM$ for graphic product...

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

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37017644 36827582 35817540 35187546 34677613=20
    34367732 33607810 33337891 33417949 34097982=20
    34527964 35467797 36667711=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Aug 14 18:40:54 2025
    AWUS01 KWNH 141840
    FFGMPD
    NMZ000-AZZ000-150039-

    Mesoscale Precipitation Discussion 0933
    NWS Weather Prediction Center College Park MD
    240 PM EDT Thu Aug 14 2025

    Areas affected...western New Mexico, eastern Arizona

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

    Valid 141839Z - 150039Z

    Summary...Isolated to scattered thunderstorm activity will expand
    in coverage and drift slowly through the afternoon hours.=20
    Isolated instances of flash flooding are expected with this
    activity.

    Discussion...Daytime heating and weak/modest ascent associated
    with nearby mid-level vorticity maxima were aiding on a gradual
    deepening of convection this afternoon. So far, the deeper cores
    have materialized on an isolated basis near terrain-favored
    peaks/ridges across southwestern New Mexico. Weak southerly flow
    aloft has contributed to slow, erratic storm motions so far, and
    PW values (ranging from 0.75 in NM to 1.4 in southern AZ) are just
    high enough to promote wetting rainfall and a quick burst of
    around 0.5 inch rainfall amounts beneath the more dominant
    activity.

    With continued daytime heating and surface-based destabilization,
    the ongoing scenario is expected to evolve slowly, with storms
    expected to expand in coverage. Some of the heavier rainfall
    could occur atop burn scars and/or low-lying terrain that could
    locally promote excessive runoff and flash flooding. Models
    suggest that the flash flood risk should primarily be diurnally
    driven, but should also persist beyond 00Z/6p MDT this evening.=20
    The heaviest rain rates should occur across portions of Arizona
    where higher moisture content is located, although local 1 inch/hr
    rain rates could materialize across the entire discussion area
    this afternoon.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-YGmfRGNxvHvUiX-DZREdW0C8PK7aACwabYmUjTRcVK6OR6c9jBmz82mwdp6gKo9m6i2= qotXpCHWP55b8lcmospacNM$ for graphic product...

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

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 36731249 36200907 34520743 32930680 32190705=20
    31510850 31461011 31811123 33481275 35261335=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 Aug 14 19:29:09 2025
    AWUS01 KWNH 141928
    FFGMPD
    MDZ000-VAZ000-DCZ000-142227-

    Mesoscale Precipitation Discussion 0934
    NWS Weather Prediction Center College Park MD
    328 PM EDT Thu Aug 14 2025

    Areas affected...portions of Maryland and vicinity

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

    Valid 141927Z - 142227Z

    Summary...Isolated instances of flash flooding cannot be ruled out
    as thunderstorms merge and produce heavy rainfall over the next
    couple hours.

    Discussion...Recent radar mosaic imagery depicts expanding
    convective coveage across Maryland from near Baltimore southward
    along western sides of the Chesapeake Bay to near Waldorf and
    Leonardtown. While initial development has been propagating at
    around 10-15 knots, the orientation of cells amid weak low-level
    shear should enable a greater frequency of cell mergers over the
    next couple hours. The airmass supporting thunderstorm
    development is abundantly moist (2+ inch PW values, 3000 J/kg
    SBCAPE), suggesting that local rain rates could reach 2 inches/hr
    in a few spots. This should promote flash flood potential -
    especially in urban areas across central/eastern Maryland that
    experience heavy rainfall.

    The evolving flash flood threat should be relatively brief. As
    storms migrate from north to south, rain cooled air/low-level
    stabilization should take hold and result in an eventual decrease
    in convective coverage after around 22Z or so.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6MBRT_ll1e9vlawqn4YbrK-IEUBJYQ-VYIrzPiiA8oo3jmi7lJdmtMp_iJCN7phgWfN7= 7m5ZqSm6qSl8Q82TIkaO05Y$ for graphic product...

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

    ATTN...RFC...RHA...NWC...

    LAT...LON 39697640 39307595 38487582 37957617 38067695=20
    39067718 39667707=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 15 00:28:57 2025
    AWUS01 KWNH 150028
    FFGMPD
    VAZ000-150327-

    Mesoscale Precipitation Discussion 0935
    NWS Weather Prediction Center College Park MD
    828 PM EDT Thu Aug 14 2025

    Areas affected...southeastern Virginia

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

    Valid 150027Z - 150327Z

    Summary...Flash flooding remains possible for a few more hours,
    though an overall downward trend in convective coverage is
    expected through 03Z/11p EDT.

    Discussion...Flash flood potential continues across southeastern
    Virginia. Scattered thunderstorms continue to migrate very slowly
    ahead of a front draped across the area (subjectively analyzed
    from near Danville, VA to Salisbury, MD). Widespread convective
    overturning has occurred across North Carolina that should serve
    to limit any renewed convective development here. Some
    overturning has occurred near Wakefield and Virginia Beach,
    although 80s F surface temps just north of that area (near
    Williamsburg and Richmond) was continuing to sustain scattered
    thunderstorm activity. Areas of 1 inch/hr rain rates were still
    being observed, which isn't surprising given the 2+ inch PW values
    within the pre-convective airmass. These rates still support
    localized flash flood potential - especially in low-lying and
    urbanized areas of southeastern VA.

    The ongoing flash flood threat should persist for another couple
    hours or so. Widespread convective overturning continues to
    exhaust surface-based instability across the region. Meanwhile,
    lack of surface heating and eventual progression of a front
    through the region should gradually limit the spatial extent of
    opportunity for renewed convection. Much of the flash flood
    threat should end after 04Z/midnight EDT or so.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7-C2NzmM7TLaKRAUgzLcqdmi842Rw-MCr_ucu5-IQbSHgysGXGev2qcXx7NqcTdyleZN= FXyAqHRQwHoZ0H8uCh3k4tU$ for graphic product...

    ATTN...WFO...AKQ...RNK...

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37657659 36967546 36557678 36577833 37097851=20
    37597787=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 15 05:01:31 2025
    AWUS01 KWNH 150501
    FFGMPD
    AZZ000-150930-

    Mesoscale Precipitation Discussion 0936
    NWS Weather Prediction Center College Park MD
    100 AM EDT Fri Aug 15 2025

    Areas affected...Central Arizona...

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

    Valid 150500Z - 150930Z

    SUMMARY...Slow moving thunderstorms with 1.5-1.75"/hr rates and
    localized totals to similar values may pose localized widely
    scattered incident or two of flash flooding overnight.

    DISCUSSION...Recent GOES-W 10.3um and KIWA RADAR depict an
    increase in convective activity over the last hour or so through S
    Yavapai into eastern Maricopa county. Evening outflow boundary
    coming off the San Francisco Plateau had lost much of the driving
    convective activity through the early overnight period and settled
    into the Sun Valley. Recent VWP and surface observations noted a
    slight uptick in southerly and southwesterly flow solidly
    increasing convergence along the boundary. GOES SWIR, suggests
    the leading edge may still be dropping south across SE Maricopa
    toward northern Pinal, but in the core of the return southerly
    flow strong ascent as seen tops cool to below -60C, tapping the a
    remaining small pool of unstable mid-level air with MUCAPEs
    analyzed around 1500-2000 J/kg per the RAP. VWP shows 10-15kts of
    flow at 850mb/cloud providing the solid moisture flux into the
    developing cells. CIRA LPW notes core of enhanced surface to
    850mb moisture is further west than the 850-700mb axis; which
    further tilts eastward across Pinal into central Gila county in
    the 700-500mb layer; so peak influx is about across central
    Maricopa into south-central Yavapai and with vertical totaling of
    about 1.5" on 15kts should support 1.5-1.75"/hr rates.=20

    Steering from 700 per VWP is weak and out of the west, but again
    backs more southerly through the core of the cells but still about
    5-10kts allowing for some tilting to keep the downdraft collapsing
    on the updrafts, but also support slow cell motions to allow for
    localized accumulation for a spot of 2" possible. Still,
    short-term rates in proximity to hard desert soils or urban
    centers will result in increased runoff and possibility for flash
    flooding through the overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7FvvK56e6K5TSG1JdEfE87sCaF2F7JrDjPP55FhikLxbpuNCDcnYxkxbfcUbMapzkdcQ= cAqL9qrjBPKcaFXlKqMHvt0$ for graphic product...

    ATTN...WFO...FGZ...PSR...

    ATTN...RFC...STR...NWC...

    LAT...LON 35051277 34891219 34581182 34161146 33661093=20
    33391088 33121126 33241210 33611265 34241306=20
    34751312=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 15 17:17:04 2025
    AWUS01 KWNH 151717
    FFGMPD
    TXZ000-152315-

    Mesoscale Precipitation Discussion 0937
    NWS Weather Prediction Center College Park MD
    115 PM EDT Fri Aug 15 2025

    Areas affected...Deep South Texas

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

    Valid 151715Z - 152315Z

    SUMMARY...Slow-moving and locally very heavy showers and
    thunderstorms this afternoon are expected to produce some concerns
    for mainly urban flash flooding across far southern TX.

    DISCUSSION...The latest GOES-E visible satellite imagery along
    with radar data shows some uptick in shower and thunderstorm
    activity across far south TX near the Rio Grande River and around
    the Brownsville metropolitan area. This is associated with the
    poorly organized tropical disturbance (98L) seen approaching far
    northeast MX and south TX.

    There is a fair amount of mid-level vort energy associated with
    this system, and this coupled with at least some locally focused
    low-level moisture convergence and moderate instability should
    yield an uptick and expansion of heavy shower and thunderstorm
    activity going through the afternoon hours.

    MLCAPE values of 1500 to 2500+ J/kg are in place and this coupled
    with very high PWs of 2.25 to 2.5 inches should yield at least
    some concentrated convective cells with rainfall rates capable of
    reaching 2 to 3 inches/hour.

    The hires model guidance overall is quite limited with the heavy
    rainfall potential across far southern TX, but there have been
    some increasingly wetter trends noted with the recent RRFS
    guidance, with some potential for locally slow-moving
    bands/clusters of convection impacting areas near and west of
    Brownsville over the next few hours.

    Given this and the recent radar and satellite trends, some spotty
    rainfall totals of 3 to 5+ inches will be possible where the more
    focused storms set up. While widespread flash flooding is not
    expected, there may be localized urban flash flooding impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4TRPF31fxLUTbLXNVZxHKpjf90EmIZkps6vWGVK8LLJLGTbpksIHZXsyxkH71kqD_v3S= zS4Xiniosd0osghOmBb3op4$ for graphic product...

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

    ATTN...RFC...FWR...NWC...

    LAT...LON 27009837 26929771 26799732 26409704 25939706=20
    25779745 25999837 26369892 26739885=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 15 17:33:49 2025
    AWUS01 KWNH 151733
    FFGMPD
    LAZ000-152230-

    Mesoscale Precipitation Discussion 0938
    NWS Weather Prediction Center College Park MD
    132 PM EDT Fri Aug 15 2025

    Areas affected...South-Central to Southeast LA

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

    Valid 151730Z - 152230Z

    SUMMARY...Heavy showers and thunderstorms over south-central to
    southeast LA may result in at least an isolated threat of flash
    flooding going through the afternoon hours. This will include some
    urban flash flooding concerns to the New Orleans metropolitan area.

    DISCUSSION...Slow-moving showers and thunderstorms with very high
    rainfall rates approaching 3 inches/hour will likely continue over
    the next few hours across portions of south-central to southeast
    LA.

    A localized band of stronger low-level convergence combined with
    strong instability characterized by MLCAPE values of near 3000
    J/kg will support convective sustenance in the near-term with aid
    also from localized outflow boundary collisions which will tend to
    facilitate new convective development.

    The latest hires model guidance, especially led by the RRFS
    solutions, suggests some potential for 3 to 5 inch rainfall totals
    by early this evening. These high rates and localized storm totals
    may impact areas near or into the New Orleans metropolitan area
    over the next few hours. Therefore, at least an isolated and
    mainly urban flash flood threat will exist as this axis of heavier
    showers and thunderstorms continues.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-bCYGL1cYWvcgZH6eSJjVzPr2MB5ysT6bxXQVeqmSTpGZfZRboQB1UoXrJYGkG_dzN1L= lQ0lGtc1R3Xe24_1eLSN31s$ for graphic product...

    ATTN...WFO...LCH...LIX...

    ATTN...RFC...ORN...NWC...

    LAT...LON 30709171 30489015 30088966 29568975 29349039=20
    29769181 30219226=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 15 19:06:39 2025
    AWUS01 KWNH 151906
    FFGMPD
    TXZ000-NMZ000-AZZ000-UTZ000-160100-

    Mesoscale Precipitation Discussion 0939
    NWS Weather Prediction Center College Park MD
    304 PM EDT Fri Aug 15 2025

    Areas affected...Southern UT...Much of AZ...Western and Central NM

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

    Valid 151904Z - 160100Z

    SUMMARY...Increasing coverage of locally heavy showers and
    thunderstorms can be expected going through the afternoon hours.
    Isolated to scattered areas of flash flooding will be possible,
    and especially given slow cell-motions and potential for impacts
    around the more sensitive dry wash, burn scar and slot canyon
    locations.

    DISCUSSION...The midday GOES-W visible satellite imagery shows
    three well-defined mid-level vort centers collectively embedded
    within deeper layer south-southwesterly mid-level flow over AZ and
    NM. The energy over the northern part AZ will be gradually
    approaching areas of southern UT over the next few hours which
    coupled with favorable orographics and an uptick in boundary layer
    instability should help drive the development and expansion of
    some shower and thunderstorm activity here.

    However, the more notable threats for stronger convection will
    likely be with the energy over southeast AZ and southwest NM where
    there is already locally strong diurnal heating and presence of an
    instability gradient/differential heating boundary that will help
    facilitate convective initiation.

    SBCAPE values over southeast AZ are locally over 1500 J/kg and
    close to 1000 J/kg along the northern AZ/southern UT border. The
    PWs are rather concentrated in the 500/700 mb layer based off the
    CIRA-ALPW data, and especially over southeast AZ and into
    west-central to southwest NM.

    On a regional basis, there should be the development and expansion
    of shower and thunderstorm activity that will be rather
    slow-moving and locally anchored near areas of higher terrain.
    More concentrated cells will be possible in close proximity to the
    vort centers as they lift off to the north and northeast. This
    convective evolution is supported by the latest hires WoFS
    guidance.

    Rainfall rates of up to 1 inch in as little as 20 to 30 minutes
    will be possible. However, some localized storm total amounts of 2
    to 3+ inches may occur given the slow cell-motions and
    terrain-focused activity. Some of the hires CAM guidance led by
    the NAM Conest, FV3 LAM and RRFS supports this.

    This will drive isolated to scattered areas of flash flooding
    potential which will mainly be focused on the dry wash, burn scar
    and slot canyon locations where there are greater sensitivities
    and concerns for enhanced runoff.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4Q1S0K-RnM736tvhuutPocJgepsOULovU9Yitc0OtHMiCN5iD6Di2e1FRQ_RNmE0xLoq= gSgGBqg6-erfvWHJE4uqyBw$ for graphic product...

    ATTN...WFO...ABQ...EPZ...FGZ...GJT...PSR...SLC...TWC...VEF...

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 38381223 38251075 37660985 37060924 36410774=20
    36040614 35350532 34380504 33280509 32460503=20
    31800532 31430580 31300655 31210772 31040956=20
    31221120 32011207 33351214 34561257 35731323=20
    37601317=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 15 19:11:09 2025
    AWUS01 KWNH 151910
    FFGMPD
    NCZ000-SCZ000-GAZ000-TNZ000-ALZ000-160000-

    Mesoscale Precipitation Discussion 0940
    NWS Weather Prediction Center College Park MD
    309 PM EDT Fri Aug 15 2025

    Areas affected...northern AL/GA into adjacent portions of TN/NC/SC

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

    Valid 151905Z - 160000Z

    Summary...Increasing thunderstorm coverage into the late afternoon
    with locally heavy rainfall (as high as 2-3"/hr rates) may result
    in isolated to scattered instances of flash flooding.

    Discussion...A distinct upper-level trough (most apparent above
    400 mb, associated with a PV anomaly apparently originating from
    cyclonic wave breaking) centered near the Midsouth is allowing for
    greater coverage of convection into downstream portions of TN/AL.
    The mesoscale environment is characterized by high tropospheric
    moisture (1.7-2.1" PWs, at or above the 90th percentile per FFC
    sounding climatology), effecitve bulk shear (25-30 kts, also at or
    above 90th percentile), and plentiful instability (SBCAPE
    2500-4500 J/kg). While the environment is lacking a surface
    boundary or focusing mechanism to efficiently organize convection,
    the increased coverage of cells alone will be sufficient to result
    in cell mergers and outflow boundary collisions to result in
    localized training/repeating of heavy rainfall rates (with as much
    as 2-3"/hr with the strongest updrafts, as deep layer mean flow of
    only 5-10 kts allows for longer residence times of assicated
    downdrafts).

    Hi-res CAMs are in relatively good agreement concerning both the
    precise spatial overlap of heavier convection (per HREF EAS 0.5"
    exceedance probs of 15-25% from east-central AL through northeast
    GA into adjacent portions NC/SC) and chances for localized heavy
    totals (40-km neighborhood 3" exceedance probs of 15-35%,
    generally along and north of the highest EAS probs). 3-hr FFGs
    across the region generally range from 2.0-3.0", suggesting
    relatively high chances for localized FFG exceedance (HREF 40-km
    probs for 3-hr FFG exceedance equating to 15-35% as well). Given
    the overall favorable environment and recent observational trends,
    isolated to scattered instances of flash flooding are possible
    through dusk. While some convection may linger into the evening
    hours, coverage and intensity should be diminishing overall with
    the dry air/subsidence associated with the backside of the upper
    trough ending heavy rainfall for northern/western portions (i.e.
    AL/TN) of the MPD first.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7LFF506LU6Y4ZM3Y29zYooJXw8vlpISsn8eYKNcHiiZ-FbtuEOKGzRZwI9XeJD2GPxcO= Pef0tkOtvzQleUUW5Wtzoag$ for graphic product...

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

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 36428474 36028423 35668359 35598242 35298191=20
    34648208 33928253 33518282 33208322 33088357=20
    32998420 33078483 33208536 33158588 33148642=20
    33608692 34498655 35468649 35828557 36338516=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 Aug 16 02:48:30 2025
    AWUS01 KWNH 160245
    FFGMPD
    AZZ000-160730-

    Mesoscale Precipitation Discussion 0941
    NWS Weather Prediction Center College Park MD
    1044 PM EDT Fri Aug 15 2025

    Areas affected...South-central to Southeast Arizona...

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

    Valid 160245Z - 160730Z

    SUMMARY...Slow moving thunderstorms to track slowly southwest
    perhaps with short-term training/repeating resulting in localized
    2"+ totals and possible localized flash flooding conditions.

    DISCUSSION...Fading GOES-W Visible imagery loop shows two NW to SE
    outflow boundary arcs across AZ, one up on the San Francisco
    Plateau, the other through the Sonoran Desert into southeast AZ
    and northeast Sonora, Mexico. GOES WV suite continues to depict a
    deep long wave trof with slight negative tilt orientation across
    Southern California with broadening diffluent region of
    southwesterly flow across much of the Colorado River Basin into AZ
    providing deep layer divergence across the region.=20

    As sunset was approaching, increasing southerly flow off the Sea
    of Cortez surged moisture through the surface to 850mb layer
    across Mexico into south-central AZ. This increased moisture flux
    convergence along the boundary providing solid isentropic ascent
    to break out clusters of thunderstorms. The dominant reaching -70C
    across southern Pima county. RADAR and EIR continues to show expansion/intensification within the cluster. RAP analysis
    denotes that MUCAPE values remain around 2000-2500 J/kg,
    especially further west to fuel these cells. LLJ of 25kts slowly
    reduces along the eastern edge of the jet and propagation vectors
    suggest slow southeastward evolution along the stalling outflow
    boundary (though the boundary will likely kick southward with time
    given cold pool generation). Surface Tds in the low to mid 60s
    and total PWats through the lower cloud support PWat values near
    1.5-1.75" and should support rates of 1.75"/hr, occasionally
    ticking up to 2" where cores can merge for short duration.=20=20
    Duration is likely to be 1-2 hours with similar rates, so
    localized 1.5-2.5" totals are possible across south-central
    Arizona and toward the Santa Cruz county border with Mexico. As
    such, localized incidents of flash flooding will remain possible
    through the early overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7S_MaR-y33KOHbIuy4c0dLYta8rZ8c4IVyIuO3A1_RE6ZyVrwS4ykbm1t46q908Jp_-J= EB9quBP7Ee5rPttqbs-aWGw$ for graphic product...

    ATTN...WFO...TWC...

    ATTN...RFC...STR...NWC...

    LAT...LON 32511194 32261127 31751065 31441001 31261001=20
    31251064 31301126 31451163 31671225 31931252=20
    32351247=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 16 03:11:59 2025
    AWUS01 KWNH 160311
    FFGMPD
    AZZ000-160830-

    Mesoscale Precipitation Discussion 0942
    NWS Weather Prediction Center College Park MD
    1110 PM EDT Fri Aug 15 2025

    Areas affected...Western to Central Arizona...

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

    Valid 160310Z - 160830Z

    SUMMARY...Expanding convective complex to slowly lift north,
    intersect with older outflow boundary. Cells with rates of
    1.5"/hr and slow motions may allow for localized 2"+ totals and
    possible localized incidents of flash flooding overnight.

    DISCUSSION...Fading GOES-W Visible and 3.9m SWIR shows a pair of
    outflow boundaries from earlier evening convective activity, both
    extending arched from NNW to SE. The northern one remains along
    or just off the Mogollon Rim across northern Arizona with a second
    extending from east of Blythe across the Sonoran Desert southwest
    of Phoenix toward Pima county. GOES-W WV suite along with GOES
    AMVs show deep layer upper-level trough over Southern California
    with a weak negative tilt as a subtle shortwave feature rolls
    eastward into the Cochella Valley toward the Colorado River
    Valley. This broad southwesterly flow is orthogonal to the
    orientation of the outflow boundaries, so all convection has been
    generally developing and back-shearing northeastward reducing
    forward overall propagation (at least in the short-term period).=20

    Recent stronger LLJ through out of the Sea of Cortez has surged north-northwestward across the Sonoran desert (using CIRA LPW and
    RAP analysis) with 15-20kts, responding to the advancing shortwave
    feature. Mid-level steeper lapse rates provide solid instability
    for stronger/deeper thunderstorm activity along the the southern
    boundary with MUCAPE values of 2500-3000 J/kg analyzed. The slug
    of moisture is estimated per CIRA LPW and RAP to be around 1.5"
    with most in the sub-700mb layer to allow for efficient warm cloud
    processes for stronger cells.=20

    Current 10.3um and RADAR mosaic show a few stronger clusters with
    the broadest up/downdraft along the Mohave/La Paz county line just
    east of the California border, as well as newer cells downstream
    along the Yavapai border. Given instability and moisture flux
    rates of 1.5-1.75"/hr are probable (along with some hail
    generation). As the shortwave lifts northeast, deeper layer mean
    southwesterly flow will allow for northeastward motions back
    toward the western Mogollon Rim, perhaps intersecting with areas
    affected earlier. Scattered incidents of 1.5" are probable, with
    an few more isolated totals of 2-2.5" with higher probability
    across Yavapai county per recent HRRR, WoFS and 00z Hi-Res CAM
    solutions.

    A few back-sheared convective columns can be seen north across E
    Mohave with the northern boundary, but most of those are generally
    weaker and widely scattered in coverage, but should still slowly
    propagate southwest eventually intersecting/integrating with the
    developing clusters moving northeast with the mean short-wave
    ejection. Similarly, these intersections/mergers will pose the
    greatest risk for flash flooding in the slopes of the Mogollon Rim
    throughout the overnight period, resulting in possible widely
    scattered incidents of flash flooding.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_SuwBf_PKHENhYETvwNv97alIgQuN-ADZKRki_oRwhmMzJ2-VMY8bvA0tr3f6pQPE9e2= a9M0x3cwbw8pt7T2mnLiork$ for graphic product...

    ATTN...WFO...FGZ...PSR...VEF...

    ATTN...RFC...STR...NWC...

    LAT...LON 36341314 35701240 35241150 34721133 34171142=20
    33751208 33561283 33591383 33761407 34291410=20
    35361417 35981373=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 16 06:52:08 2025
    AWUS01 KWNH 160650
    FFGMPD
    MNZ000-SDZ000-161200-

    Mesoscale Precipitation Discussion 0943
    NWS Weather Prediction Center College Park MD
    249 AM EDT Sat Aug 16 2025

    Areas affected...South-central & Eastern SD...Southwest MN...

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

    Valid 160650Z - 161200Z

    SUMMARY...Very progressive squall QLCS will have strong moisture
    flux for intense rainfall production with sub-hourly totals of
    1.5-2"; though best risk for flash flooding will be flanking line
    training for spots of 2-3" over hard/impermeable soils.

    DISCUSSION...GOES-E WV suite shows a compact 80kt 3H jet streak
    across the North/South Dakota border which continues to strengthen
    a compact shortwave within its broad right entrance region. 06z
    Surface analysis shows an inverted wave inflection along the
    strongest DPVA/divergent region within the southeast quadrant of
    the wave across central SDak. A surface stationary front extends
    east into west-central MN before angling north toward Duluth and
    is directing strong and very moist low level flow to enhance very
    strong moisture flux convergence. Additionally, steep lapse rates
    with the very rich moisture at the surface in the mid to upper
    70s, supports 4500-5000 J/kg and the combination is result in very
    broad and strong updrafts across south-central SDAK at this time.=20
    Numerous overshooting tops below -75 to -80C denotes the vigor of
    the updraft including their width.=20=20

    As noted, the surface Tds are well above normal and loading the
    low-level profile to support over 2-2.25" total PWat values and
    given the strength of the LLJ at 30-40kts, the lower cloud
    moisture loading is fairly high, even though some will be lost to
    hail production, there will be efficient rainfall production,
    further increasing with time/maturity of the squall. So while the
    limiting factor of forward speed/propagation for duration, the
    broad downdrafts will allow for some overall sub-hourly totals of
    1.5-2". Additionally, the strength of the bow is also supporting
    a veering low level profile and tight anticyclonic rotor along the southwesterly flanking line. VWP and RAP analysis suggest that
    flanking axis is likely to trail and has some solid angle toward
    the initial bow/squall line to add an additional duration of heavy
    rainfall. As such, an axis of enhanced totals of 2-3.5" in 2-3
    hours is becoming increasingly probable across south-central into
    eastern SDak and eventually into SW MN.

    Hydrologically, the area has been in a solid drought and ground
    conditions well below average running at about 10-25th percentiles
    with 0-40cm at 10-25%. This makes the soils hard and reduce
    infiltration particularly in the strength of the instantaneous
    rates sub-hourly totals...with 03z HRRR solutions suggesting 15min
    totals ranging from 1.5 to as high as 2", this suggests fairly
    quick totals with little/no infiltration, increasing run off. As
    such, localized flash flooding is considered possible, especially
    if the flanking line repeats behind the initial line.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Vh8PTkf1F0MIOfoehoFF2Lew4lcse0AoUz4MXvZw3BLK6bC0oHDF6U3CZ4_I-m3HXcd= trvGEa8u2TMdIZfYq6fPTAo$ for graphic product...

    ATTN...WFO...ABR...FSD...MPX...UNR...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45669531 45439422 44779398 44209493 43689625=20
    43229806 43040054 43190186 44050077 44769940=20
    45279730=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 16 12:07:20 2025
    AWUS01 KWNH 161207
    FFGMPD
    WIZ000-MNZ000-IAZ000-SDZ000-NDZ000-161805-

    Mesoscale Precipitation Discussion 0944
    NWS Weather Prediction Center College Park MD
    805 AM EDT Sat Aug 16 2025

    Areas affected...Northeast SD...Central/Southern
    MN...Western/Central WI

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

    Valid 161205Z - 161805Z

    SUMMARY...A strong MCS will continue to advance off to the east
    this morning across the Upper Midwest while fostering heavy
    rainfall and at least an isolated threat for mainly urban flash
    flooding going through midday.

    DISCUSSION...The early morning GOES-E IR satellite imagery shows a
    strong cold-topped MCS advancing across eastern SD and much of
    central and southern MN. A well-defined MCV is embedded within the
    convective mass, and this energy will be advancing east this
    morning through portions of eastern MN and into western WI.

    A very moist and unstable environment is in place which is being
    aided by a 40 kt southwest low-level jet aiming up across
    northwest IA and southwest MN. MUCAPE values are on the order of
    2000 to 3000 J/kg over southern MN currently, and this is also
    situated in close proximity to an area of low pressure and
    well-defined frontal zone.

    The low-level jet should tend to veer a bit more over the next
    several hours, but should maintain a rather strong warm air
    advection regime which coupled with the pool of instability should
    favor a sustainable and well-organized axis of convection.

    PWs are generally near or above 1.75 inches, and this coupled with
    the instability should favor rainfall rates capable of reaching 2
    inches/hour. The latest hires model guidance including the early
    morning WoFS and HRRR solutions suggest downstream rainfall totals
    along the path of the MCS reaching 2 to 4 inches. The 90th
    percentile of the WoFS suggest some spotty 5 inch totals will be
    possible.

    These additional rains will be capable of yielding at least an
    isolated threat for flash flooding over the next several hours
    with the more urbanized locations at greatest risk for impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-YkmdYBnF0dnXjaGbehXK8JPZ5LUh0QAPE2ig2Z_w4HKWciyUfU7OZKYIv_MYYGKF_rR= sjMlfZDHKGYTDBaT3cUPXWc$ for graphic product...

    ATTN...WFO...ABR...ARX...DLH...FGF...FSD...GRB...MKX...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 46579428 46419158 45738887 44488841 43568901=20
    43319043 43599255 43999448 44369655 45399735=20
    46379655=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 16 17:04:18 2025
    AWUS01 KWNH 161703
    FFGMPD
    SCZ000-FLZ000-GAZ000-162300-

    Mesoscale Precipitation Discussion 0945
    NWS Weather Prediction Center College Park MD
    102 PM EDT Sat Aug 16 2025

    Areas affected...Southern SC...Eastern GA...Northeast FL

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

    Valid 161702Z - 162300Z

    SUMMARY...A gradual increase in showers and thunderstorms can be
    expected through this afternoon. Slow cell-motions and high
    rainfall rates will pose a threat for isolated areas of flash
    flooding, with the more urbanized areas at greatest risk for
    impacts.

    DISCUSSION...The midday GOES-E visible satellite imagery shows a
    small band of showers and thunderstorms settling south across
    southern SC which is allowing for an outflow boundary to gradually
    approach the SC/GA border. This convection is generally being
    driven by nearby proximity of some weak vort energy. Meanwhile,
    some subtle sea breeze convergence along the coast from SC down
    through eastern GA is also helping to initiate a few areas of
    slow-moving convection.

    Over the next few hours, strong diurnal heating within a very
    moist environment should aid the development and expansion of
    clusters of heavy showers and thunderstorms. Already there are
    MLCAPE values of 2000 to 3000 J/kg from the SC Lowcountry down
    through northeast FL, and with multiple mesoscale boundary
    interactions expected this afternoon, there should be some locally
    concentrated areas of convection with high rainfall rates.

    Some rainfall rates of 2 to 3 inches/hour will be possible with
    the stronger storms. The activity should generally be pulse in
    nature given the lack of deeper layer shear, but there will be
    slow cell-motions and potential for cell-mergers that foster some
    rainfall totals of as much as 3 to 5 inches. This is consistent
    with a consensus of the recent HRRR solutions along with the
    latest HREF and REFS guidance.

    Some isolated areas of flash flooding will be possible through the
    afternoon hours, and especially with some of the more urbanized
    locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9bD8WYUrFX6s_kMlV8hKPqIC3b138GgMmM9j06oLNFFz-jmLR80Oe7VKjEubTq_vDFAM= mjCheKRII0QWKztz_nm8cmE$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 34068205 33658158 33278078 33247985 32727960=20
    32288026 31658086 30678124 29458148 29348207=20
    30028289 31618344 33378305=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 16 22:00:56 2025
    AWUS01 KWNH 162200
    FFGMPD
    INZ000-WIZ000-ILZ000-IAZ000-170300-

    Mesoscale Precipitation Discussion 0946
    NWS Weather Prediction Center College Park MD
    559 PM EDT Sat Aug 16 2025

    Areas affected...southern WI and north-central IL, as well as
    surrounding portions of IA/IN

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

    Valid 162155Z - 170300Z

    Summary...Very heavy downpours with 1-3" short-term rainfall
    totals likely to result in isolated to scattered flash flooding.

    Discussion...A compact and potent mid-level shortwave trough is
    translating rapidly east-southeast over the Upper Midwest this
    afternoon, driving a classic series of mesoscale convective
    systems (MCSs) along the northern periphery of a blocked synoptic
    scale ridge (centered due south over the Midsouth region).
    Persistent convection has favored the ML CAPE gradient (500-4000
    J/kg) over the past several hours, which has shifted southward
    coincident with prior MCS outflow and the associated tightening
    surface thetaE gradient. While some convection is still ongoing
    from the earlier morning MCS into northeast IL (rapidly
    approaching the Chicago metro with MRMS indicating very heavy
    downpours with 15-min rainfall totals nearing 1.0"), a trailing
    MCS (currently rapidly progressing through southern WI) is quickly
    becoming the more dominate expansive MCS. The mesoscale
    environment in the vicinity of theses MCSs is otherwise
    characterized by anomalously high tropospheric moisture content
    (PWs 1.6-2.0", at or above the 90th percentile per GRB/DVN
    sounding climatology), and effective bulk shear of 25-50 kts.

    While hi-res CAMs have certainly struggled with the precise
    convective evolution that has occured (rather typical in these
    highly dynamic, progressive MCS events), collectively analyzed
    through the HREF (and associated post-processing including
    time-lagged members) a valuable forward-looking signal for heavy
    rainfall still emerges. The 18z HREF local probability-match mean
    (LPMM) QPF suggests a period of localized 2-3"/3-hr associated
    with backbuilding along the west/southwest flank of the MCS (with
    new convective initiation occurring where low-level inflow and
    iscentropic lift coincide with the highest instability). While the
    HREF signal is likely too late/slow overall (as this is already
    beginning to occur into southwest WI), 40-km neighborhood
    exceedance probabilities for 2" exceedance range from 20-50%
    (confined to southern WI, though in reality lower-end
    probabilities for these amounts likely extend both upstream and
    downstream of the dominate MCS, due to underestimated forward
    propagation AND backbuilding by the CAMs overall). Although hourly
    runs of the HRRR have not proven as useful as the HREF signal
    (which also seems rather typical when the environment of the model initialization is mismatched with the observational assimilation),
    the experimental WoFS does suggest that similar 2"+ localized
    totals are possible (via an increasing trend in the 90th
    percentile QPF with a 27-km neighborhood 2" exceedance probs in
    the 20-40% range, notably displaced south and west of the HREF
    signal).

    While the greatest signal/risk for flash flooding is judged to be
    across southern WI and northern IL, the MPD also encompasses areas
    downstream (southeast into far northwest IN) and upstream (west
    into adjacent portions of IA) due to the aforementioned forward
    propagation and backbuilding threats. While these surrounding
    areas are less likely to realize localized 2"+ totals, the chances
    for 1"+ amounts (in as little as 15-30 min with very heavy
    downpours) are likely (per HREF/WoFS exceedance probs of 40%+)
    with associated 1-hr Flash Flood Guidance (FFGs) ranging from as
    low as 1.0-1.5" across a substantial portion of the region. As a
    result, isolated to scattered instances of flash flooding are
    considered likely (with conditional backbuilding of convection
    largely dictating the overall coverage and potential for an
    instance or two of more significant flash flooding).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!85RfJsxpSa7tuBurkDXC0aMjTJ4xX4BGbQjCHnUmnpeHIkFvJK0rzeISwXDJQFMobfZF= OoSfOBvy97Tpn6fDKz9qf-I$ for graphic product...

    ATTN...WFO...ARX...DVN...ILX...IND...IWX...LOT...MKX...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 43608890 43418789 42988769 42268726 41618674=20
    40868651 40208687 39998789 40058882 40418974=20
    40979028 41619055 42079078 42649143 42989143=20
    43249113 43369075 43408979=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 17 03:36:19 2025
    AWUS01 KWNH 170334
    FFGMPD
    WIZ000-ILZ000-MNZ000-IAZ000-170900-

    Mesoscale Precipitation Discussion 0947
    NWS Weather Prediction Center College Park MD
    1134 PM EDT Sat Aug 16 2025

    Areas affected...Southeast MN...Northeast IA...Southern
    WI...Northern IL...

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

    Valid 170335Z - 170900Z

    SUMMARY...Warm-advection thunderstorms with potential for training
    and spots of 2-4" across areas of recent heavy rainfall/saturated
    soils likely resulting in scattered incidents of flash flooding.

    DISCUSSION...GOES-E WV suite shows increased anticyclonic
    curvature in upper-level cirrus pattern indicative of shortwave
    ridging in the wake of the exiting shortwave across the Lower
    Peninsula of Michigan. The associated surface front extends
    through central Lake Michigan across southern WI into the northern
    row of counties in IA; though the effective boundary due to strong
    overturning from this evening's convection intersects the front
    near near KPDC and angles southeastward across NE IL into just
    north of KDNV. Deep layer moisture remains pooled along the
    frontal zone with 1.75-2" Total Pwats across N IA/S MN before
    broadening across S WI into northeast IL. LLJ response is a broad southwesterly 15-20kt flow along the entire front; so best
    moisture convergence/isentropic ascent is at the intersection
    remains along the intersection of the old outflow boundary and
    surface front in NE IA/SW WI/NW IL. Upper-level right entrance to
    the jet further enhances vertical ascent in proximity to the
    front, also helping to sharpen the isentropes vertically
    throughout the night. Efficient rainfall production given strong
    convergence and unstable air with favorable evacuation aloft,
    should support 1.5-2"/hr rates within the expanding cores.=20


    GOES-E 10.3um shows strong cooling tops below -65C along the
    orthogonal section of ascent, with upstream redevelopment and
    increasing TCu noted across SE MN. With flanking development and
    steering flow from NW to SE, a favorable training environment
    setup may allow for increased duration and localized 2-4" totals
    are likely especially from SE MN and SW WI, as potential for
    further upstream development is likely throughout the overnight
    period as well, and as such an isolated spot over 5" is not out of
    the realm of possibility.=20

    To compound issues, the area has seen recent heavy rainfall and
    the upper soil conditions remain relatively saturated with 0-40cm
    ratios well over 50 with spots near 70% across MN, WI (above 90th
    percentile) before reducing to below 40% over Chicagoland into NW
    IND per NASA SPoRT LIS product(though tonight's rain, likely
    improved those values. As such, infiltation may be a bit more
    difficult and increased runoff is likely to result in scattered
    incidents of flash flooding overnight tonight.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4XD5kfk4Uj5z4YB_V5dUsJJ-ohvachmPL8OrbNcd2VWkaq4KXlEBEZC03tNWaNyt83pI= qJgYtt6d7ZR79bcGiDWcutM$ for graphic product...

    ATTN...WFO...ARX...DVN...LOT...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 44199254 44149159 43789046 43278856 42758764=20
    41828746 41288783 41278892 41989046 42729175=20
    43359272 43649301 44039293=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 17 05:35:11 2025
    AWUS01 KWNH 170532
    FFGMPD
    SDZ000-NDZ000-171100-

    Mesoscale Precipitation Discussion 0948
    NWS Weather Prediction Center College Park MD
    132 AM EDT Sun Aug 17 2025

    Areas affected...Northwest South Dakota...South-central North
    Dakota...

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

    Valid 170530Z - 171100Z

    SUMMARY...Expanding convective clusters with potential
    repeating/merging elements. Rates of 1.75-2"/hr and localized
    2-3" totals pose localized possible incidents of flash flooding
    overnight.

    DISCUSSION...GOES-E WV suite shows an elongated north to south
    shortwave feature along the eastern edge of larger scale trough in
    the Northern Rockies, lifting northeastward out of northwest SD
    into southwest ND continuing to be enhanced by broad right
    entrance of 300mb 50kt jet entrance along its northwest quadrant.
    This is supporting a strong surface to low level wind response,
    further confluent/convergent along and north of the Black Hills
    across W SD. 05z surface analysis shows stationary front along
    the SD/NEB border with Tds in the low to upper 70s throughout the
    SD fluxed on solid, weakly confluent easterly flow. The bulk of
    the moisture resides north of the surface front, though 850-700mb
    moisture flux convergence is further increased deep layer flux
    given directional confluence from southerly to southeasterly along
    the southern flank of the elongated shortwave trough north of the
    Black Hills. As such, Total PWat values have increased from 1.75
    along the convergence axis. As such, strong clusters continue to
    expand and merge with pre-cursory convergence axes across
    northwest SD; noted in the RADAR mosaic and expanding/cooling
    10.3um IR canopy tops. Ample mid-level lapse rates and higher
    theta-E air support CAPEs over 2000 J/kg which further increase
    within the upstream inflow region north of the frontal zone. As
    such, cells are already becoming rather efficient in rainfall
    production with rates of 1.75-2"/hr noted throughout the expanding clusters.=20=20

    As the trough is lifting, differential shear within the steering
    profile (as the elongated trough lifts north) is helping to orient
    cell motions toward a repeating/short-term training profile, which
    is expected to become further convergent as the wave is reaching
    the apex of the synoptic ridging over south-central ND. As a
    result, an axis of 2-3"+ totals are likely to expand toward a
    larger cluster toward the central common border of the Dakotas
    over the next 3-5hrs. The rates alone are near/just above the
    1-1.75"/hr FFG values in all but a few scattered locations within
    the area of concern and localized areas are probable to exceed the
    2-2.5"/3hr values, suggesting flash flooding is possible through
    the overnight period. And while the top layers have been in
    prolonged drought with 0-40cm saturation ratio below 25%, the
    sheer rate on hard soils will further limit infiltration and
    result in increased runoff.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9A1tL6ALpcWkq0Q1jTWNfI1ulZQ3PVJDOTEd9YVG12RiO_Knvvl5ztfrimIZYxeLqCwP= DZ3lb1GNFPxlCSsBYCu2rCQ$ for graphic product...

    ATTN...WFO...ABR...BIS...UNR...

    ATTN...RFC...KRF...NWC...

    LAT...LON 46850021 46699900 46299858 45569891 45059981=20
    44620088 44070304 44470377 45150381 45670352=20
    46030294 46550185=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 17 06:06:12 2025
    AWUS01 KWNH 170603
    FFGMPD
    MNZ000-SDZ000-171200-

    Mesoscale Precipitation Discussion 0949
    NWS Weather Prediction Center College Park MD
    203 AM EDT Sun Aug 17 2025

    Areas affected...Southern Minnesota...East-central South Dakota...

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

    Valid 170600Z - 171200Z

    SUMMARY...Slow moving, potentially repeating cells pose 2-4"
    totals and possible localized incidents of flash flooding through
    the remainder of the overnight period.

    DISCUSSION...GOES-E 10.3um IR loop shows expanding cluster of
    thunderstorms across SW MN over the last few hours and starting to
    become better organized with broadening up/downdrafts;
    concurrently while newer development is developing between it and
    the downstream clusters in WI/MN/IA Tri-state area. Additionally,
    combined with 3.9um loop, low stratus north of the frontal
    boundary across central MN/N WI shows southward cold advection
    that is further steepening the isentropes across the frontal
    boundary that generally sits across the northern row of counties
    in Iowa. RAP analysis, confirmed by CIRA LPW shows pool of deep
    layer moisture with Total PWat values over 2" extending from
    northeast SD through SE MN, generally enhanced further west where
    flux has been greatest along the nose of the southerly low-level
    jet where winds are up to 20-25kt per KFSD VWP vs 15-20kts further
    east. The strong moisture convergence along the steepening
    isentropic surface, MLCAPEs of 3000-3500 J/kg, has resulted in a
    slightly southward development versus 00z Hi-Res CAMs and recent
    HRRR cycles, as such, proximity to stronger orthogonal moisture
    flux should support efficient rainfall production with rates of
    2"/hr.

    Stronger shortwave to the west and exiting one to the east has
    resulted in fairly unidirectional but also weaker steering flow
    just a bit south of due east and parallel to the frontal boundary.
    Mean winds of 10-15kts are expected and should allow for some
    potential training, but more likely slow overall cell motion
    allowing for a few hours of intense rainfall and pockets of 2-4"
    totals. Stronger LLJ due to the approaching wave over the western
    Dakotas suggest upstream convective development is probable later
    into the overnight periods far west as the Coteau des Prairies
    Plateau, but also intersect with back-building from upstream
    cluster/WAA cells in SE MN. As such, have included portions of SE
    MN that were incorporated in MPD 947 for longer valid time toward
    12z.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7STG0ZQBcR9jgl17njBbuRM45-xzCK3rQdwkyNG1TqkTolDpUFzKmxTd_1U_fV3ahuRZ= TOVzwQGN6EDSj8LTIAH8J7s$ for graphic product...

    ATTN...WFO...ABR...ARX...FSD...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45469700 45419560 45269458 44899338 44499251=20
    44019168 43729146 43539186 43579398 43759520=20
    44159650 44619756 44979777 45339764=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 17 08:30:33 2025
    AWUS01 KWNH 170830
    FFGMPD
    INZ000-ILZ000-171300-

    Mesoscale Precipitation Discussion 0950
    NWS Weather Prediction Center College Park MD
    429 AM EDT Sun Aug 17 2025

    Areas affected...Northeast Illinois...Northwest Indiana...

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

    Valid 170830Z - 171300Z

    SUMMARY...Isentropic ascent within remaining unstable/moist
    environment continues. Additional 1.5-3" totals training in
    proximity of Chicago and suburbs will keep risk of incidents of
    flash flooding possible through daybreak.

    DISCUSSION...GOES-E 10.3um IR loop shows much of northern IL has
    remained untapped through the overnight period. This is confirmed
    by recent RAP analysis fields with 2500-3000 J/kg of MUCAPE across
    N IL. Surface analysis continue to show affects of initial
    evening complex of return southeasterly flow with remnants of a
    boundary angled NW to SE from far NW IL toward DNV, which given
    recent elevated convective lines through Chicagoland; seems to be
    reinforced with steepened isentropes from north to south. This
    while VWP at DVN and LOT/ORD shows generally west and
    west-northwest 15-25kts orthogonal to the boundary. RADAR shows a
    few upstream cells redeveloping given the stronger moisture flux
    in the upglide through N IL. Moisture remains more than ample
    given Tds in the low to mid 70s from the source while mid-level
    moisture/RH remains solid for a core of 2"+ total PWats through
    the ascent plane. As such, thunderstorms will have solid vertical
    moisture loading to continue to support 2"/hr rates.

    Deep layer steering starts to curl anti-cylonically along the
    northeast edge of the deeper ridging, and convection has been
    bending right of mean flow becoming parallel to the IND/IL border.
    Though further southward, the inflow/upglide weakens and becomes
    displaced from the core of unstable air, so cells have been
    generally weakening further south or eastward, and this is likely
    to continue throughout the early morning, limiting the risk for
    additional heavy rainfall toward northeast IL/Northwest IND.=20

    Currently LLJ strength is strong and with heavy rainfall/cold pool
    generation closer to the Lakeshore, westward propagation and
    closer to surface rooting of cells may limit path of newer
    development to train over earlier tracks, but there will remain
    some intersection for an additional 1-3" with newer cells; combine
    that with proximity to urban environment near Chicago and
    increased run-off make it more probable that incidents of flash
    flooding/rapid inundation remain possible through the early
    morning hours.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5xAMj4-01uIHivdK-1pSE1hmvhDQfj2cxMRA2KrmTQ_coF3ArZdVaoWhH8TCLPPffO3V= ItuQiImU_QGYmK5y4pYxYFM$ for graphic product...

    ATTN...WFO...ILX...IND...IWX...LOT...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 42418859 42148785 41108660 40248662 40088755=20
    40518816 41288894 42248930=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 17 12:01:32 2025
    AWUS01 KWNH 171201
    FFGMPD
    MNZ000-IAZ000-SDZ000-NDZ000-171700-

    Mesoscale Precipitation Discussion 0951
    NWS Weather Prediction Center College Park MD
    800 AM EDT Sun Aug 17 2025

    Areas affected...Northeast SD...Southeast ND...West-Central to
    Southern MN...Far Northern IA

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

    Valid 171200Z - 171700Z

    SUMMARY...Additional heavy showers and thunderstorms this morning
    will continue to foster areas of flash flooding.

    DISCUSSION...The early-morning GOES-E IR satellite imagery along
    with radar shows a fairly organized axis of locally training
    showers and thunderstorms impacting southern MN. This convection
    is focused generally along and just north of a stationary front
    draped west to east across the Upper Midwest.

    MUCAPE values of 2000+ J/kg remain in place along this boundary
    which in conjunction with a relatively modest southwest 20 to 30
    kt low-level jet interacting with it should favor renewed rounds
    of heavy showers and thunderstorms. This activity will continue to
    be capable of training over the same area going through at least
    the mid to late-morning hours given alignment that is nearly
    parallel to the deeper layer steering flow. Some southward advance
    of this activity into far northern IA is also possible given the
    influence of the convectively enhanced cold pool close to the
    MN/IA border.

    Additional areas of heavy showers and thunderstorms will also be a
    concern upstream over parts of northeast SD and southeast ND as an
    upstream forward propagating MCS arrives and interacts with the
    aforementioned front while fostering somewhat stronger warm air
    advection out ahead of it. However, this activity at least by late
    this morning should begin to gradually weaken as it approaches
    west-central MN.

    Rainfall rates with all of the stronger and more organized cells
    in the short-term will still be capable of reaching 1.5 to 2.5
    inches/hour which is being supported by the instability and a
    corridor of 1.75+ inch PWs.

    Additional rainfall totals as high as 3 to 5 inches will be
    possible, and especially over southern MN where some of the most
    organized convective activity is occurring. The latest HRRR and
    WoFS guidance supports these totals at least locally as well.

    Given the ongoing areas of flash flooding locally, and with these
    additional rains, more areas of flash flooding are expected going
    through at least the mid to late morning hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!56TkRIQJK3ffzR8f1-r4_AVzE_ZpkgcinyTZePlWrZA1-epLQBqWltwsEUBJp8obdAXO= MBjDkXa8k1b8ajG3HF30ygE$ for graphic product...

    ATTN...WFO...ABR...ARX...BIS...DMX...FGF...FSD...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 47399736 47029653 45619526 44849413 44129220=20
    43509139 42869167 42889342 43409578 44189741=20
    45169862 46319889 47179848=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 18 01:47:11 2025
    AWUS01 KWNH 180145
    FFGMPD
    WIZ000-ILZ000-MNZ000-IAZ000-180600-

    Mesoscale Precipitation Discussion 0952
    NWS Weather Prediction Center College Park MD
    944 PM EDT Sun Aug 17 2025

    Areas affected...south-central/southeastern MN into
    north-central/northeastern IA and adjacent portions of WI/IL

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

    Valid 180140Z - 180600Z

    Summary...1-3"/hr rainfall rates to continue into the overnight,
    resulting in localized short-term rainfall totals as high as 4-8".
    Scattered to numerous instances of flash flooding likely, some
    significant/life threatening (particularly across south-central
    and southeastern MN).

    Discussion...Convection is proliferating this evening in the
    vicinity of a low-level frontal zone and associated
    instability/thetaE gradient, extending from southwestern MN
    through northeastern IA into northern IL. A weak shortwave/vort
    max immediately upstream (ND/SD/MN border region) seems to be
    resulting in the most intense/widespread convection across
    south-central MN into north-central IA (by way of DPVA and added
    divergence aloft from the right-entrance region of an associated
    jet streak), and this convective organization should continue into
    the early overnight hours as the low-level jet strengthens. The
    mesoscale environment is otherwise characterized by an MLCAPE
    gradient of 2500-4500 J/kg (with +400 J/kg in the past 3-hr over
    southern MN), precipitable water of 1.6-2.0" (well above the 90th
    percentile and approaching the max moving average, per MPX
    sounding climatology), and effective bulk shear of 25-30 kts.

    While observational trends favor portions of south-central and
    southeastern MN for the greatest coverage and intensity of heavy
    rainfall in the near term, the hi-res CAMs (18z HREF and 12z
    experimental REFS) strongest signal is displaced to the northwest
    (clustered over central MN, which is where the best dynamics are=20
    certainly located... but ultimately too far displaced from the
    best boundary layer thermodynamics which the deep convection has
    favored and anchored to). Despite this spatial displacement, the
    signal suggests relatively high chances for localized 3"
    exceedance (30-50% probs, per 40-km neighborhood of HREF/REFS).
    Farther to the southeast along the frontal zone (where dynamics
    are less impressive and training should be less of an issue, but
    storm motions tend to be slower with storms still capable of
    1-3"/hr rates) the CAMs still support the potential for 3"
    exceedance (10-30% probs) with the more recent experimental WoFS
    runs (23-01z) even suggesting the potential for localized totals
    of 4-8" from south-central/southeastern MN into
    northeastern/eastern IA (per 90th percentile QPF and associated 5"
    exceedance probabilities of 40%+).

    As much of the region remains fairly saturated from recent days
    heavy rains (with an axis of 2-4" of rain across a portion of the
    area over just the past 24-hr), Flash Flood Guidance (FFG) suggest
    impacts from as little as 1.0-2.0" over 1-3 hour period. As a
    result, scattered to numerous instances of flash flooding are
    considered likely. Given the particular hydrologic sensitivity
    across portions of southeastern MN (including the Twin Cities
    metro area), there is a higher than typical risk for localized
    instances of significant/life threatening flash flooding.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!76xaIs_f8fQ7BJ6EZvJ_qHK0uQiB3EF9kShSl3fQ7NBybjMyuGPDUNX5c-IH4NBJpSeE= R524hl5QYgDAH8jb2hGIVHw$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...FSD...ILX...LOT...MKX...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45599402 45539299 44939193 44209097 43499030=20
    42648973 40878869 40488968 41449141 41969241=20
    42659378 43249509 44269503 45059471=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 18 05:59:31 2025
    AWUS01 KWNH 180558
    FFGMPD
    WIZ000-MNZ000-IAZ000-NEZ000-SDZ000-181200-

    Mesoscale Precipitation Discussion 0953
    NWS Weather Prediction Center College Park MD
    157 AM EDT Mon Aug 18 2025

    Areas affected...Southeast SD...Northeast NEB...Northern
    IA...Southern MN...Western WI...

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

    Valid 180600Z - 181200Z

    SUMMARY...A muddled mess of shortwave, warm advection and
    small/storm scale forcing within a solidly unstable/deep moist
    environment should result in widely scattered thunderstorms with
    some weakly organized clusters capable of short-duration training
    elements. Widely scattered incidents of flash flooding remain
    possible through late overnight period

    DISCUSSION...Regional RADAR mosaic denotes two weakly organized
    shortwave features. The leading one having driven stronger
    thunderstorms and scattered flash flooding is progressing out of
    southeast MN into NW WI with the convergent banding noted from
    north-central IA through to the eastern quadrant of the shortwave
    into west-central WI. The second flatter west to east wave across
    southern SD is driving some smaller clusters with weakening bowing
    elements and trailing convergent thunderstorms in the eastern Sand
    Hills of NEB.

    Both reside in a broad southerly low level jet providing some
    moisture flux and isentropic ascent/convergence along stationary
    front that extends from east of KPIR to south of KFSD and through
    northern IA before angling southeastward from a weak surface
    inflection west of KALO southward into IL near KGBG. Surface Tds
    remain well above average ranging through the 70s with spots of
    75-77F pooled along it. This results in 1.9 to 2.1" total Pwats
    along its length; though stronger LLJ to 25-30kts west of the
    Missouri River is increasing moisture ahead of the western,
    upstream wave. Environment remains fairly unstable with ample
    well of 2000-3000 J/kg of MUCAPE for any areas of forcing focused
    enough to break through minimal capping with isentropic
    ascent/convergence along the front. Instability pool is a bit
    deeper and extends northward through the isentropic ascent further
    west with the stronger LLJ. Here rates are likely to be stronger
    up to 2"/hr but forward propagation may limit overall duration.=20
    Deep layer westerly flow aloft may also allow for some
    short-duration training/repeating across NE NEB/SE SD into NW IA;
    which will likely be necessary for localized totals over 3" in
    3-4hrs. These higher rates/totals will be more necessary across
    an area with higher FFG due to recent very dry conditions. Still
    widely scattered incidents remain possible.

    Further east across SE MN/NE IA/W WI...A wedge of
    enhanced/confluent flow due to exiting shortwave in MN will allow
    a narrow channel along its southern and eastern flank for
    additional elevated convection that has some potential for training/back-building. As the instability reduces quicker toward
    the northeast into central WI, the coverage and intensity will
    diminish quickly and likely not exceed the FFG into Northern and
    northeastern WI. However, continued upglide/back-building through
    lower FFG due to recent heavy rainfall across southern MN/SE MN
    and northern IA may see spots of 2-3" and similarly possible
    incidents of scattered flash flooding through 12z.

    Overall, confidence is below average for any given location for
    flash flooding given above average dispersion of Hi-Res CAM
    solutions to the evolution. Still, the environment remains
    solidly conducive that a few incidents of localized flash flooding
    are probable, especially over the recently saturated regions north
    and east of the surface front. Scattered 2-3" totals with
    isolated 4" totals remain possible through 12z.=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7P_gzk4TUTDVORWHTYeu_xM8uURX-V4bitHuGtd71LNKDGt8-zAnhoIhlIJ_tDcuTcUH= XgOPBCxy2q0rPI5XrEvetws$ for graphic product...

    ATTN...WFO...ARX...DMX...FSD...MPX...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45309238 44819084 43989037 43229057 42659215=20
    41989427 41269594 41299670 41929730 42359761=20
    42869792 43839826 44579601 45269474=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 18 18:39:39 2025
    AWUS01 KWNH 181838
    FFGMPD
    MDZ000-VAZ000-NCZ000-SCZ000-190000-

    Mesoscale Precipitation Discussion 0955
    NWS Weather Prediction Center College Park MD
    237 PM EDT Mon Aug 18 2025

    Areas affected...Coastal Plain from Southeast Virginia through
    Northeast South Carolina

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

    Valid 181836Z - 190000Z

    Summary...Showers and thunderstorms developing along a cold front
    will expand and intensify through the afternoon. These storms will
    be slow moving, and contain rainfall rates of 1-3"/hr. This could
    produce 2-3" of rainfall with locally higher amounts, and
    instances of flash flooding.

    Discussion...The GOES-E day-cloud phase microphysics RGB this
    afternoon is beginning to show rapid updraft growth from the
    Tidewater region of Virginia through eastern NC. These storms are
    developing along a slowly advancing cold front, with low-level
    convergence along the boundary the primary ascent mechanism. Lift
    along this front is occurring into robust thermodynamics to
    support heavy rainfall. PWs measured by GPS are as high as 1.6
    inches in southeast Virginia, and onshore northeast flow is
    funneling a narrow corridor of PWs above 1.9 inches into eastern
    NC. This elevated PW is overlapping MUCAPE of 2000-3000 J/kg
    centered along this front, and developing convection within this
    environment is producing radar-estimated rain rates that have
    already exceeded 1.5"/hr according to KMHX.

    The high-res CAMs are a little slow to capture the ongoing
    development, but are generally in agreement that a narrow corridor
    of thunderstorms will expand along this front through peak heating
    of the aftn. This is reflected by relatively high EAS
    probabilities for 1"/6hrs focused across eastern NC which reflect
    the good CAM agreement. These storms will be generally slow moving
    from N/NE to S/SW along the boundary, and cell motions progged by
    propagation vectors the next several hours will be just around 5
    kts. Additionally, these propagation vectors will remain aligned
    to the front, suggesting training and repeating cells through the
    aftn. With rain rates likely reaching 1-3"/hr (HREF neighborhood
    probabilities for 2"/hr peaking above 60% coincident with HRRR
    15-min rainfall above 0.75" suggesting brief 3"/hr rates), total
    rainfall could reach 2-3" with locally as much as 5" possible as
    shown by HREF neighborhood probabilities for 5"/6hrs as high as
    20%.

    This region has been quite wet recently as reflected by AHPS 7-day
    rainfall that is above 300% of normal in most of the discussion
    area. Although some of this rainfall has drained efficiently to
    lower 0-10cm RSM to less than 50% and elevate 3-hr FFG to above
    3", the forecast slow movement and training of these cells is
    still causing HREF 3-hr FFG exceedance probabilities above 40%.
    While this suggests the flash flood risk is generally confined to
    where the most significant training can occur, it is possible that
    any of these intense rain rates, especially if they occur atop an
    urban area, could cause instances of flash flooding through the
    aftn.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4I_e7VsRrKjX02qlF4k1XwL2QAT_xzlhXmOSA6OKnhEchwSbzt2AJDbrybOK6T94vTxU= NgzMyL-ZwtGJzDgtJFSu7So$ for graphic product...

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

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 38027567 37737546 37347537 36607542 36067548=20
    35467578 34927611 34637662 34427735 34257805=20
    34137857 33977928 33897995 33938042 34098063=20
    34338052 34637978 34897904 35457818 36247740=20
    36977686 37587637 37897615=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 18 21:51:58 2025
    AWUS01 KWNH 182150
    FFGMPD
    MIZ000-INZ000-WIZ000-ILZ000-MNZ000-IAZ000-190300-

    Mesoscale Precipitation Discussion 0956
    NWS Weather Prediction Center College Park MD
    548 PM EDT Mon Aug 18 2025

    Areas affected...eastern IA, southern WI, and northern IL into
    surrounding portions of MN/IN

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

    Valid 182145Z - 190300Z

    Summary...Thunderstorms with hourly totals of up to 1-2" are
    expected to train/repeat with short-term totals of 2-5". Scattered
    to numerous instances of flash flooding are likely (and locally significant/life threatening flash flood concerns are particularly
    elevated in the vicinity of the Chicago metro).

    Discussion...Convection is proliferating once again today across
    portions of the Upper Midwest, focused primarily in the vicinity
    of a weak surface low pressure and an associated warm front. The
    mesoscale environment very supportive of heavy rainfall with
    plentiful instability (1500-5500 J/kg of SBCAPE), highly anomalous
    tropospheric moisture (PWs 1.7-2.0", between the 90th percentile
    and max moving average, per DVN sounding climatology), and
    effective bulk shear of 20-40 kts (with the best shear farther
    north along the warm front, and generally below 20 kts farther
    south into the warm sector (southeast IA into north-central IL). A
    shortwave and associated vorticity maxima aloft (located nearly
    directly above the weak surface low @ 500 mb) will provide
    additional forcing for lift, along with a bit of additional
    divergence from an associated right-entrance region of a jet
    streak (though the best upper-level divergence is displaced to the
    northeast into northern WI/MI, where instability is much more
    limited). As the low-level jet strengthens into the evening hours,
    this should help to sustain updrafts and organize convection
    (despite only conditionally unstable mid-level lapse rates) with a
    series of linear segments of thunderstorms resulting in localized
    west-to-east training (despite relatively strong steering flow
    with 850-300 mb winds of 20 kts). With MRMS already indicating
    localized hourly totals as high as 1-2" with 3-hr Flash Flood
    Guidance (FFG) generally ranging from 1.0-2.0" across the MPD
    area.

    As the strongest convection (with hourly estimates as high as 2")
    approaches the greater Chicago metro area, the risk for instances
    of life threatening flash flooding are elevated late this
    afternoon and evening. Nearly all of the latest hi-res CAM data
    supports these significant flash flooding concerns, as the 18z
    NAM-nest and hourly runs of both the HRRR and experimental RRFS
    since then depict localized totals of 3-5" in the vicinity of the
    Chicago metro (with the NAM-nest and some RRFS runs indicating the
    potential for extreme localized totals of 5"+, which is also
    reflected in the 18z HREF neighborhood probabilities of 5"
    exceedance ranging from 10-20%). While southeast WI into northeast
    IL is certainly the greatest area of concern for prolong/repeated
    heavy rainfall, areas farther south and west are still likely to
    flood from expected 2-4" localized totals (given aforementioned
    FFGs of only 1.0-2.0" for much of the area). As a result,
    scattered to numerous instances of flash flooding are likely.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4MgnU1l7BBX0TE4tOcovvaLLc6qbPJbd9pwnHqFao_DUJt5zvmxmVPeuEKeRgbQfWojn= oiIAT6WbW2gP8WSBEDbbGS4$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...ILX...IWX...LOT...MKX...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 44239208 44019148 43569066 43198951 43098863=20
    43098782 42518752 42038714 41728636 41038677=20
    40638724 40488814 40548896 40839010 40749126=20
    40979179 41359214 42859191 43049262 43369245=20
    43619248 43779265 43999272 44149246=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 19 02:41:39 2025
    AWUS01 KWNH 190241
    FFGMPD
    MIZ000-INZ000-WIZ000-ILZ000-190845-

    Mesoscale Precipitation Discussion 0957
    NWS Weather Prediction Center College Park MD
    1040 PM EDT Mon Aug 18 2025

    Areas affected...Southern WI...Northern half of IL...Northwest
    IND...Far Southwest LP of MI...

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

    Valid 190245Z - 190845Z

    SUMMARY...Incidents of flash flooding likely to continue, yet
    overall coverage/totals will reduce with increasing forward speed.
    Best chance for flash flooding will be new 'repeated' cell tracks
    across S WI/NE IL

    DISCUSSION...GOES-E WV, RADAR and RAP analysis show southern
    stream, convectively enhanced shortwave/MCV feature is pressing
    eastward across Chicago into southern Lake Michigan at this time,
    continuing to drive strongest downstream low level convergence
    along the quasi-bowing feature from northwest IND southward across
    the Kankakee Valley. Storms remain in unstable environment with
    ample deep layer moisture (Tds in the mid 70s and total moisture
    over 2"), but the stationary front remains anchored across
    southwest LP of MI into north-central IND before Tds and unstable
    air rapidly srop off, so there is a narrow area of enhanced
    rainfall rates up to 2", but cells should quickly diminish into
    the more stable air. Additionally, area across LP of MI and
    Northeast IND has been much drier and FFGs reflect that, further
    reducing the risk to all but the most ideal training across
    urban/low infiltration ground conditions.

    However, the upstream flanking line across into central IL, does
    remain very unstable with MUCAPEs of 2000-3000 j/kg and solid
    moisture flux convergence along the confluent low level flow
    regime. Deep layer steering may allow for some southwest to
    northeast repeating, though height-falls from the passing
    shortwave/MCV should allow for southeast propagation to limit
    overall totals to 2-3", lower FFG values of less than 2"/hr and
    1.5-2.5"/3hrs in all but the further southwest portions of central
    IL remain at good risk of locally being exceeded through the next
    few hours.

    Further north...S WI/N IL...
    GOES-E WV depicts core of larger/synoptic to mesoscale shortwave
    feature across central to S WI, is exiting and downward mixing is
    starting to help advance the stationary front across SW WI through
    depth, sharpening convergence along and south of the boundary.=20
    While partially mixed, there remains ample remaining unstable air
    of 1500-2000 J/kg and ample deep layer moisture to support an
    additional round of stronger thunderstorms. These upstream
    thunderstorms will be narrower in nature but should have the
    opportunity to track across areas already affected by heavy
    rainfall with rates of 1.75-2"/hr; localized additional 1-3"
    totals would reaggravate any flooding conditions across S WI and
    few northern rows of N IL. As such, localized incidents of flash
    flooding are likely to persist through the overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8FSgKNGQdISKEqfYISW9rhW6hqzxvy4s9MUJ48_k8kXlVGsBMlIfs0Ib2wcDKqU5QdFX= pStbyaxUrQBwe3Rzztnfogs$ for graphic product...

    ATTN...WFO...DVN...GRR...ILX...IND...IWX...LOT...MKX...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 43398673 43118619 42518584 41708587 40518639=20
    39988741 39908888 40019006 40469037 40869000=20
    41278958 41708930 42168939 42489001 42988980=20
    43348839=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 19 13:25:12 2025
    AWUS01 KWNH 191321
    FFGMPD
    MDZ000-VAZ000-191918-

    Mesoscale Precipitation Discussion 0958
    NWS Weather Prediction Center College Park MD
    920 AM EDT Tue Aug 19 2025

    Areas affected...southeastern Virginia/far southern DelMarVa
    Peninsula

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

    Valid 191318Z - 191918Z

    Summary...A focused areas of nearly stationary convection has
    produced spots of 2.5-5 inch rainfall totals across the far
    southern DelMarVa Peninsula this morning. Additional totals of
    3-5 inches cannot be ruled out. Localized/isolated inundation is
    expected through at least 19Z.

    Discussion...Slow-moving convection has evolved across the
    southern DelMarVa this morning. The storms are embedded within a
    relatively focused area of low-level convergence just east of a
    weak surface low near PHF/Williamsburg, with low-level easterlies
    maintaining moisture/buoyancy against a more stable airmass across
    much of Virginia. Weak/modest kinematics were supporting slow
    cell movement, and spots of 1-3 inch/hr rain rates were being
    estimated per MRMS with the most dominant activity. A few flood
    impacts have also been observed near the Accomack, VA area this
    morning.

    Although the spatial extent of the flash flood threat is fairly
    localized, the slow evolution of meso-to-synoptic-scale features
    supporting heavy rainfall is a bit concerning. Heavy rainfall
    could persist in this regime through 19Z, with additional 3-5 inch
    rainfall totals possible. Models suggest that the convergence
    axis/low supporting heavy rainfall will gradually migrate westward
    through midday, which may temper the heavy rain threat eventually.
    Local impacts are expected to continue and may worsen while heavy
    rainfall persists.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7CDMLYKzxEq4_Nj_6X8tZAYHCj5Q4MritnzxdHRS-8x4Xwy8ZnclDBERWJuIEqpRzRTM= gHU0BKUZcEtDPLTOyGTbgg0$ for graphic product...

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

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 38167536 37587545 36727585 37217686 37937655=20
    38137597=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 19 13:26:02 2025
    AWUS01 KWNH 191321
    FFGMPD
    MDZ000-VAZ000-191918-

    Mesoscale Precipitation Discussion 0958
    NWS Weather Prediction Center College Park MD
    920 AM EDT Tue Aug 19 2025

    Areas affected...southeastern Virginia/far southern DelMarVa
    Peninsula

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

    Valid 191318Z - 191918Z

    Summary...A focused areas of nearly stationary convection has
    produced spots of 2.5-5 inch rainfall totals across the far
    southern DelMarVa Peninsula this morning. Additional totals of
    3-5 inches cannot be ruled out. Localized/isolated inundation is
    expected through at least 19Z.

    Discussion...Slow-moving convection has evolved across the
    southern DelMarVa this morning. The storms are embedded within a
    relatively focused area of low-level convergence just east of a
    weak surface low near PHF/Williamsburg, with low-level easterlies
    maintaining moisture/buoyancy against a more stable airmass across
    much of Virginia. Weak/modest kinematics were supporting slow
    cell movement, and spots of 1-3 inch/hr rain rates were being
    estimated per MRMS with the most dominant activity. A few flood
    impacts have also been observed near the Accomack, VA area this
    morning.

    Although the spatial extent of the flash flood threat is fairly
    localized, the slow evolution of meso-to-synoptic-scale features
    supporting heavy rainfall is a bit concerning. Heavy rainfall
    could persist in this regime through 19Z, with additional 3-5 inch
    rainfall totals possible. Models suggest that the convergence
    axis/low supporting heavy rainfall will gradually migrate westward
    through midday, which may temper the heavy rain threat eventually.
    Local impacts are expected to continue and may worsen while heavy
    rainfall persists.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7jxEu38haEH6mlmWZFGG1sQ5vn7L0IAWaB2c44_hdv1Zoayb99uNoq_IHQLf0WaArZpo= V0fwh_G8cmXkaXLR_8bR86g$ for graphic product...

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

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 38167536 37587545 36727585 37217686 37937655=20
    38137597=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 19 17:33:23 2025
    AWUS01 KWNH 191733
    FFGMPD
    TXZ000-NMZ000-AZZ000-192332-

    Mesoscale Precipitation Discussion 0959
    NWS Weather Prediction Center College Park MD
    132 PM EDT Tue Aug 19 2025

    Areas affected...eastern Arizona, portions of New Mexico

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

    Valid 191732Z - 192332Z

    Summary...Thunderstorms will increase in coverage and intensity
    through 00Z/6p MDT, with flash flooding possible especially in
    low-lying spots and near burn scars.

    Discussion...Latest satellite/radar imagery depicts abundant
    insolation leading to isolated convective development along
    favored ridgelines/terrain - especially in New Mexico. The storms
    are forming in an environment with just enough mid-level
    instability and moisture (0.75-1.3 inch PW values) for wetting
    thunderstorms to develop. Kinematic fields aloft suggest slow and
    at times erratic movement with any developing activity. Models
    and observations are also suggestive of continued expansion of
    convective coverage through peak heating hours and beyond.

    As cells continue to expand in coverage, areas of 0.5-1 inch/hr
    rain rates will become more common. Perhaps the highest
    concentration of higher rain rates will occur across southern New
    Mexico and southeastern Arizona where moisture content/PW values
    are highest. Areas of heavy rainfall may occur atop sensitive
    low-lying areas and burn scars that could enhance runoff locally.

    Models (particularly the HREF) depict that the peak convective
    threat will likely occur in the 21-00Z timeframe, with slow
    weakening expected beyond that timeframe. Flash flooding will be
    possible given the aforementioned scenario.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Het168qicskNAsHlcFvgNT6ffe7kkBl8tiXYh8DP59KVcR8OcKFoZT5BMkyoe9HslIv= i8XSwK8C79k4CxM4xhohGMs$ for graphic product...

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

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 36840536 35890489 33770473 32920503 31800612=20
    31710819 31370831 31371092 31641155 32631118=20
    33940991 34770860 35890735 36760636=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 19 18:25:54 2025
    AWUS01 KWNH 191825
    FFGMPD
    NCZ000-SCZ000-GAZ000-TNZ000-ALZ000-200000-

    Mesoscale Precipitation Discussion 0960
    NWS Weather Prediction Center College Park MD
    225 PM EDT Tue Aug 19 2025

    Areas affected...Southern Appalachians

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

    Valid 191823Z - 200000Z

    Summary...Thunderstorms with 2-3"/hr rain rates will expand across
    the Southern Appalachians this afternoon. These storms will be
    very slow moving, leading to 2-3" of rainfall with locally as much
    as 5" possible. Flash flooding may result.

    Discussion...The GOES-E day-cloud phase microphysics RGB this aftn
    shows a rapid intensification of updrafts now featuring cloud ice
    as Cbs develop along a line from west-central NC into far northern
    GA. This activity is blossoming in response to persistent upslope
    flow on E/NE winds behind a cold front that has sagged into the
    GA/SC coastal plain as analyzed by WPC. Despite being behind the
    front, this low level flow is pooling moisture across the Southern
    Appalachians as reflected by PWs measured by GPS as much as 1.5
    inches near Asheville, NC and 2.1 inches near Columbia, SC. At the
    same time, breaks in the clouds on the western periphery of the
    cold air damming (CAD) is allowing for a rapid increase of
    instability which is now analyzed via the SPC RAP to be 2000-3000
    J/kg. The fresh convection in northern GA has already resulted in
    MRMS hourly rainfall of nearly 1.5 inches and resultant FLASH
    response of 300+ cfs/smi unit streamflow.

    Although the CAMs differ in the coverage of convection through
    this aftn, the persistent upslope flow into this overlap of
    moisture and instability should support expansion and continuation
    well into the evening. Rainfall rates as progged by the HREF
    neighborhood probabilities have a 20-30% chance of exceeding 2"/hr
    within any of this convection, while the HRRR 15-min rainfall
    indicates up to 0.75" suggesting brief 3"/hr rain rates. Despite
    the uncertainty in coverage, the HREF EAS probabilities indicate
    the greatest potential for heavy rainfall will be across the Blue
    Ridge and southward into the northern GA Piedmont, and this is
    supported by the differential heating boundary caused by the cloud
    breaks within the CAD to the east. A ridge to the west will keep
    overall forcing generally light and flow weak, indicating that
    storms will move very slowly on 0-6km mean winds of just 5 kts.
    This could be problematic as the continued upslope flow will
    support regenerating cells, and at times storms may stall with
    zero net motion, especially during periods of boundary
    interactions within the otherwise pulse environment.

    The slow movement and regenerating behavior of these heavy rain
    rates could produce 2-3" of rain, with locally as much as 5"
    possible (10-15% chance from the HREF). This heavy rain will occur
    across soils that are vulnerable both due to the general
    sensitivity of the complex terrain, but also due to 0-10cm soil
    moisture that is above the 95th percentile according to NASA
    SPoRT. Any heavy slow moving heavy rainfall across this region
    could quickly result in runoff and instances of flash flooding.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7N3S-qjnsUCg83J-x0KRtNHFa29zN6Z9J63xmHkCyfCmVqURHlWm0kaxVrUsyedOUhlP= G6_aCnAIEG6CKFucLtd1qRM$ for graphic product...

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

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 36568158 36118170 35888189 35588221 34888283=20
    34168342 33818355 33658367 33518394 33568465=20
    33908534 34398560 34968542 35288499 35518446=20
    36268260 36438216=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 19 18:26:56 2025
    AWUS01 KWNH 191826
    FFGMPD
    MOZ000-KSZ000-192322-

    Mesoscale Precipitation Discussion 0961
    NWS Weather Prediction Center College Park MD
    223 PM EDT Tue Aug 19 2025

    Areas affected...portions of central and eastern Kansas

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

    Valid 191822Z - 192322Z

    Summary...Slow-moving thunderstorms will produce areas of 1-2
    inch/hr rain rates through 00Z/7p CDT tonight. Areas of flash
    flooding are possible.

    Discussion...A cluster of strong thunderstorms have developed in
    the Manhattan/Emporia region over the past half hour. The storms
    are embedded in a strongly unstable (2000-3000 J/kg MLCAPE)
    environment, with 1.8 inch PW values supporting heavier rainfall
    in water-loaded downdrafts. The cells are likely benefiting from
    weak mid-level vorticity maxima (over eastern Nebraska and western
    Kansas) providing ascent. Low-level convergence along a remnant
    outflow from morning convection was also likely providing a focus
    for updraft development in the area.

    Kinematics aloft are supportive of slow and at times erratic storm
    motions along with 1-2 inch/hr rain rates beneath dominant
    activity. The proximity of intense convective development and
    downdraft potential (from 7C/km lapse rates aloft) suggests that
    the storms will eventually form one or two small linear
    segments/clusters that propagate slowly southward toward US 50 and
    US 400 near/east of Wichita over the next 2-3 hours or so. Flash
    flood potential should accompany this activity - especially across
    east-central and northeastern Kansas where FFG thresholds are
    around 1 inch/hr and could readily become exceeded. Slightly
    higher rain rates may be needed with southward extent for any
    appreciable flash flood risk.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4xI791ETaJy8cmcFdaUDmb0gwdXp4gCPETA56apmkQ4Cv_nYZYGrI6wvXSgOh9cUgr6x= FwXuSbLophNmoRprCcbr6yY$ for graphic product...

    ATTN...WFO...DDC...EAX...GID...ICT...SGF...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39249529 37479456 37079656 37439953 39129912=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 Aug 19 19:03:23 2025
    AWUS01 KWNH 191903
    FFGMPD
    MOZ000-ARZ000-OKZ000-200100-

    Mesoscale Precipitation Discussion 0962
    NWS Weather Prediction Center College Park MD
    302 PM EDT Tue Aug 19 2025

    Areas affected...The Ozarks

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

    Valid 191902Z - 200100Z

    Summary...Showers and thunderstorms developing ahead of an MCV
    will expand in coverage through the aftn. Rainfall rates of
    1-2"/hr are expected, which could result in 2-3" of rainfall with
    locally higher amounts. Flash flooding is possible.

    Discussion...The regional radar mosaic this aftn depicts rapid
    expansion of increasing reflectivity associated with developing
    convection from southeast Missouri through far eastern Oklahoma.
    These thunderstorms are developing in response to ascent produced
    through weak upper level directional divergence atop subtle height
    falls as a convectively enhanced shortwave and remnant MCV tracks
    southward from Missouri. An outflow boundary (OFB) ahead of this
    MCV noted in satellite imagery is producing additional lift
    through convergence, while general N/NW flow is producing modest
    upslope ascent into the Ozarks as well. This ascent is acting upon
    favorable thermodynamics characterized by PWs measured by GPS of
    1.7 to 1.8 inches, around the 90th percentile for the date,
    collocated with MUCAPE around 3000 J/kg south of the OFB.

    Cells that have developed so far have been generally small with
    narrow updrafts, which within the pulse environment (limited bulk
    shear) is keeping rainfall intensity to around 0.5-1"/hr with
    short temporal lifespans. However, the CAMs suggest that
    thunderstorms will become more widespread and intense as the MCV
    and OFB drop southward into the evening, and as coverage
    increases, storm mergers and collisions will lead to regenerating
    cells with longer lifetimes. During this time, PWs are likely to
    increase to above 2", suggesting the thermodynamic environment
    will become even more favorable as the forcing intensifies, with
    the result being HREF neighborhood probabilities for 2"/hr rain
    rates peaking above 30%. Although cells should steadily move
    southward on mean 0-6km winds of 5-10 kts, propagation vectors may
    veer sufficiently to allow redevelopment upstream suggesting that
    in addition to storm mergers, some areas could receive repeating
    rounds of thunderstorms. Where this occurs, total rainfall of
    2-3", with locally 3-4", is possible as reflected by HREF
    exceedance probabilities for 3"/6hrs of 40%.

    Soils across this area are generally dry according to NASA SPoRT
    due to minimal recent rainfall noted via AHPS. This has allowed
    FFG to reach 3-4"/3hrs. While this should limit the magnitude and
    coverage of any flash flooding, isolated impacts are possible
    where any repeating cells can occur, especially within urban areas
    or any more sensitive terrain.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8tbCZYWYfdBJ1voqLUBZJKdolbsMBPy_63Dm0m98mkcIwOM2NyaWtnjkPczzYOj3z9EO= mIMEX0W2eonhkyqrqVDzHaI$ for graphic product...

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

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 37639064 37638986 37418952 36988951 36248997=20
    35739069 35389151 35249225 35029322 34849408=20
    34769465 34749508 35019555 35339540 35749483=20
    36279363 36969266 37259231 37569160=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Aug 20 19:48:45 2025
    AWUS01 KWNH 201948
    FFGMPD
    GAZ000-TNZ000-ALZ000-MSZ000-210100-

    Mesoscale Precipitation Discussion 0963
    NWS Weather Prediction Center College Park MD
    347 PM EDT Wed Aug 20 2025

    Areas affected...Portions of Tennessee, Alabama, and Mississippi

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

    Valid 201947Z - 210100Z

    Summary...Slow moving showers and thunderstorms will expand
    through the afternoon. Rainfall rates will likely exceed 2"/hr at
    times, leading to pockets of 2-4" of rainfall. This may lead to
    instances of flash flooding, especially over urban areas.

    Discussion...The regional radar mosaic this aftn indicates rapid
    development of showers and thunderstorms from south-central TN
    through central MS. This convection is developing ahead of an
    approaching cold front and along a low-level convergence boundary
    formed by the interaction of convective outflows and a surface
    trough. Ascent across this region is being additionally enhanced
    by a modest shortwave tracking E/SE near the MS/TN border.

    This broad ascent is acting upon a favorable thermodynamic
    environment to support heavy rainfall. PWs as measured by GPS are
    between 1.8 and 2.1 inches, around the 90th percentile for the
    date, overlapping MUCAPE that is between 3000-4000 J/kg south of
    the cold front. This is driving the rapid expansion of convection
    noted in the regional radar, with additional storms forming due to
    outflow collisions and storm mergers in the generally pulse-type
    environment.

    Rainfall rates have been estimated via local radars to be as high
    as 2-2.5"/hr from KHTX and KOHX, leading to MRMS hourly rainfall
    as much as 2.5 inches. As the aftn progresses, the continued
    ascent drifting southward into a ribbon of enhanced moisture
    confluence could support more frequent rainfall rates above 2"/hr
    as supported by HREF neighborhood probabilities, and the HRRR
    15-min precipitation accumulation suggests brief rates in excess
    of 3"/hr are possible. While storms should remain generally pulse
    due to minimal bulk shear, and mean winds support a slow southward
    advance of cells at 5-10 kts, frequent mergers and collisions will
    lead to slower and at times chaotic motion which could enhance the
    duration of rainfall. Where this occurs, total rainfall through
    this evening could reach 2-4" as reflected by HREF 6-hr rain
    probabilities exceeding 40% for 3 inches.

    7-day rainfall across the area has been scattered, but in some
    parts of the discussion area, especially in AL/TN, has been as
    much as 300% of normal, leading to 0-10cm soil moisture from NASA
    SPoRT that is above the 95th percentile. While FFG remains
    elevated, and FFG exceedance probabilities are modest in response,
    it is possible that any slow moving/lingering heavy rainfall could
    overwhelm soils to produce rapid runoff. However, this will be
    most likely across any urban areas which have the greatest
    potential for isolated flash flood impacts into this evening.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_AxvMuSPWL7KSY07MFdiDt52-GqDaTutEI9deFy5LT48LMqp2BpjHDnlaG_CRK7RvFt6= qGV86FtNSPGNVxC_uEp8Wpg$ for graphic product...

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

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 35948609 35908485 35648452 35018456 34358490=20
    33818568 33458724 33288747 32828818 32448880=20
    32188955 32178993 32489015 33079011 33699002=20
    34638895 35448751=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Aug 21 01:12:14 2025
    AWUS01 KWNH 210112
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-210600-

    Mesoscale Precipitation Discussion 0964
    NWS Weather Prediction Center College Park MD
    911 PM EDT Wed Aug 20 2025

    Areas affected...Southern Arkansas, western Mississippi, northern
    Louisiana

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

    Valid 210111Z - 210600Z

    Summary...Showers and thunderstorms will continue for several more
    hours ahead of a cold front before waning tonight. Rainfall rates
    of 2-3"/hr, while generally brief, will produce 2-3" of rain.
    Instances of flash flooding are possible.

    Discussion...A cold front analyzed by WPC dropping slowly across
    southern Arkansas will continue to drift into Louisiana tonight.
    The tail end of this front will continue to provide the impetus
    for ascent through low-level convergence, aided by a subtle
    shortwave dropping concurrently within the general weak northerly
    flow regime. Moisture across the region is being channeled ahead
    of the front and is analyzed by the SPC RAP to be above 2 inches
    even in the pre-convective airmass, with GPS measurements
    approaching 2.3 inches within convection. This extreme PW is
    overlapping MUCAPE that is still 2000-3000 J/kg despite SBCIN,
    supporting the regenerating convection seen over the past two
    hours. Rainfall rates have been estimated by local radars to be
    above 2.5"/hr, and MRMS 15-min rainfall has been as high as 0.8"
    in a few areas (above 3"/hr measured rainfall rates).

    The CAMs are struggling to resolve the current activity which is
    both much more intense and widespread than progs would suggest.
    With the front in place, aided by the weak shortwave energy aloft,
    and modest 700mb convergence, it has become more likely that
    thunderstorms will persist well after dark. This is despite a lack
    of bulk shear keeping storms of the pulse variety, but outflow
    boundary collisions and storm mergers in response to the
    widespread nature will support additional development. With storm
    motions generally slow and chaotic, and with some upstream
    development also possible as propagation vectors collapse to 5 kts
    and orient obliquely right of the mean wind, these intense
    rainfall rates (3"/hr at times continuing) could produce 2-3" of
    rain, with isolated higher amounts possible. This is in addition
    to rain that has already fallen.

    FFG across the area is quite elevated, generally 3-4"/3 hrs and
    even 2-3"/1hr. While HREF exceedance probabilities are modest,
    less than 10%, this is clearly under-forecasting the true risk.
    Additionally, with rainfall rates as intense as they have been,
    and with these likely to continue, 15-min rainfall of 0.75-1 inch
    in some areas could quickly overwhelm soils to become runoff
    despite the elevated FFG. For this reason, any storms that
    continue until full convective overturning later tonight could
    produce instances of flash flooding.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6ccWbhoL8ZCGKWfhd9EZLKyUzQYy083UtKffDFtqsrwbsW0psBep94vgit9t2bHPza9D= EATTPHIegGHhgAwO0GJwpHM$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...LZK...MEG...SHV...

    ATTN...RFC...ALR...FWR...ORN...TUA...NWC...

    LAT...LON 34798999 34728899 34478866 33938870 33398899=20
    33018941 32689000 32219065 31629093 31189131=20
    30879184 30749260 30759312 31209370 31869387=20
    32399385 33089345 33939271 34399201 34699105=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 Aug 21 18:10:57 2025
    AWUS01 KWNH 211810
    FFGMPD
    LAZ000-TXZ000-220009-

    Mesoscale Precipitation Discussion 0965
    NWS Weather Prediction Center College Park MD
    210 PM EDT Thu Aug 21 2025

    Areas affected...portions of central through southeast Texas and
    southwestern Louisiana

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

    Valid 211809Z - 220009Z

    Summary...Scattered to numerous thunderstorm activity will pose an
    isolated flash flood risk through 00Z/7p CDT this evening.

    Discussion...Strong insolation/destabilization and the presence of
    several meso-to-synoptic surface boundaries across the discussion
    area has resulted in an uptick in coverage of thunderstorms over
    the past half hour. The storms are in a very moist/buoyant
    airmass characterized by 2+ inch PW values and 1000-2000 J/kg
    MLCAPE values, favoring the eventual development of heavy rainfall
    rates as storms mature. Additionally, storms are in a very weakly
    sheared environment, with minimal steering flow aloft supporting
    slow/erratic cell movement. Areas of 2 inch/hr rain rates are
    expected at times through the afternoon hours, which poses an
    isolated flash flood threat.

    FFG thresholds are generally in the 2-3 inch/hr range (locally
    lower near urban areas near Austin/San Antonio and Houston. These
    thresholds and the pulse-type nature of the convection suggests
    that any flash flood threat will be relatively isolated and
    focused on urban and sensitive/low-lying areas. The bulk of the
    threat should be diurnally driven and exhibit a slow southward
    propagation toward coastal areas through 00Z/7p CDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9cFes5Y2kLXFfF92YCZhfr1qVsSj3Fm0dTE8P-1aYNI55Ix-E8MQbfOkMMLjP0fQdIOh= ZSn92Xz1I-85XNYNomPbsUA$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...LCH...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 31719608 31489428 31329243 30079263 29369463=20
    27699832 27719951 28070008 28930004 30049910=20
    30999761=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Aug 21 18:50:26 2025
    AWUS01 KWNH 211850
    FFGMPD
    UTZ000-220049-

    Mesoscale Precipitation Discussion 0967
    NWS Weather Prediction Center College Park MD
    249 PM EDT Thu Aug 21 2025

    Areas affected...southern/central Utah

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

    Valid 211849Z - 220049Z

    Summary...Scattered convection has the potential for brief heavy
    rain and an isolated flash flood threat through the afternoon
    hours.

    Discussion...Radar/satellite imagery indicates scattered
    thunderstorm developing along favored ridge lines in south-central
    Utah recently. These storms are in a relatively dry low-level
    environment (35-50F surface dewpoint depressions). Nevertheless,
    presentation on radar and mid-level moisture representations via
    satellite suggest that the environment may be a bit more
    moist/unstable aloft than suggested by mesoanalyses (depicting
    0.8-0.9 inch PW and minimal instability). The observational
    trends are also suggestive of brief heavy rainfall potential
    across the region, with a quick 0.5 inch of precipitation possible
    on an isolated basis with the strongest cells. These outflow
    driven storms will tend to propagate slowly northward over the
    course of the afternoon, but may produce heavy rain across
    terrain-favored low-lying areas/slot-canyons and burn scars.=20

    Isolated instances of flash flooding are possible given the
    aforementioned scenario. This diurnally driven threat should
    persist through 01Z/7p MDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9UGN-eqjpy1U1dwPJqazbEpL1FEoUe1P6IWfMajXr_oGVyw0RjSGKDlG56Dw17rMuTe7= jHPZMKEsfdYvPro56FV5t60$ for graphic product...

    ATTN...WFO...SLC...

    ATTN...RFC...STR...NWC...

    LAT...LON 39731183 39721085 38841034 37511091 37011238=20
    37421354 38421374 39191288=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Aug 21 18:44:28 2025
    AWUS01 KWNH 211844
    FFGMPD
    VAZ000-NCZ000-WVZ000-SCZ000-GAZ000-TNZ000-220045-

    Mesoscale Precipitation Discussion 0966
    NWS Weather Prediction Center College Park MD
    243 PM EDT Thu Aug 21 2025

    Areas affected...Southern Appalachians

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

    Valid 211845Z - 220045Z

    Summary...Slow moving showers and thunderstorms will expand across
    portions of the Southern Appalachians through this evening.
    Rainfall rates at times may reach 3"/hr which could overwhelm
    soils, especially in sensitive terrain. Flash flooding is possible.

    Discussion...The GOES-E experimental day-cloud phase micro-physics
    RGB this afternoon shows a rapid uptick in ice-bearing clouds
    suggestive of strengthening updrafts into Cbs from NW NC through
    central GA. These updrafts are associated with deepening
    convection, and there has been a recent uptick in lightning
    detection within these storms. This suggests that the environment
    is becoming increasingly favorable for thunderstorms containing
    heavy rain, as thermodynamics continues to intensify reflected by
    PWs measured by GPS between 1.6 and 1.9 inches, around the 90th
    percentile for the date, overlapped with MUCAPE as much as 3000
    J/kg. Despite the relatively recent growth across the area,
    radar-estimated rainfall rates have already exceeded 1.5"/hr
    according to KGSP.

    As the aftn progresses, the CAMs are in decently good agreement in
    both coverage and placement of activity. It appears likely that
    convection will become widespread as PWs surge to above 2" outside
    of the higher terrain. This will support rain rates within
    thunderstorms that will likely exceed 2"/hr (HREF neighborhood
    probabilities above 30%) and may reach 3"/hr at times as reflected
    by HRRR 15-min rainfall above 0.75" in a few locations. Storms
    that develop will be of the pulse variety in response to limited
    bulk shear, but will also move very slowly on 0-6km mean winds of
    just around 5 kts. This indicates that despite the relatively
    short lifetimes expected of any individual cell, total rainfall
    could reach 2-3" in some areas, and this will be most likely where
    any boundary collisions, storm mergers, or terrain influences can
    impact the relative strength and motion of these storms.

    Soil moisture across the Southern Appalachians is generally well
    above normal as reflected by NASA SPoRT 0-10cm percentiles that
    exceed 98% in many areas. This has reduced 1-hr FFG to as low as
    1-1.5" in some areas, for which the HREF exceedance probabilities
    peak above 25%. This is in addition to the general sensitivity
    across this area due to the terrain, as well as within any urban
    areas, so any slow moving thunderstorm could produce impacts due
    to flash flooding through this evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-dCixfr9qBzPF4SOXCZHuus7HaXsR8sNvbBCpD0ApBYcKAGJfz3FaQ8aSDyz1ZL8KsOc= uciRjDWptOg7sWA3OnlyZx0$ for graphic product...

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

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 37578044 37468009 36978015 35808076 34628216=20
    34088290 33708358 33558435 33578489 33868522=20
    34258544 34638551 35028530 35358470 35618366=20
    35958282 36388208 36828157 37268116 37508079=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 Aug 21 21:11:59 2025
    AWUS01 KWNH 212111
    FFGMPD
    SCZ000-FLZ000-GAZ000-220300-

    Mesoscale Precipitation Discussion 0968
    NWS Weather Prediction Center College Park MD
    511 PM EDT Thu Aug 21 2025

    Areas affected...Far northern FL hrough southwest SC including
    much of eastern GA

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

    Valid 212110Z - 220300Z

    Summary...Showers and thunderstorms will expand across eastern
    Georgia through this evening. Rainfall rates of 2-3"/hr are
    expected, which through slow storm motions could produce 2-4" of
    rain. This may result in instances of flash flooding.

    Discussion...The regional radar mosaic this afternoon shows
    widespread showers and thunderstorms across much of Georgia, with
    a slow expansion in coverage noted as far south as FL and east as
    SC. This activity is blossoming primarily in response to a weak
    low-level convergence axis noted in surface observations and 850mb
    analysis, with weak directional divergence at 300mb contributing
    ascent. Storms that have developed are generally pulse in nature
    due to weak bulk shear, and the resulting outflows/storm mergers
    are producing additional convective development.

    The thermodynamic environment in the Southeast remains extremely
    favorable for heavy rainfall, and is forecast to become even more
    impressive though the evening. PWs as measured by GPS are around
    2.1 inches, around the 90th percentile for the date, and
    corresponding MUCAPE is analyzed by the SPC RAP to be around 3000
    J/kg. These robust thermodynamics are supporting heavy rainfall
    rates in the ongoing convection, as reflected by radar-estimated
    rain rates as much as 1.5-2"/hr and MRMS measured 15-min rainfall
    locally above 0.75". As PWs continue to surge to as much as 2.25
    inches later this evening, these prolific rainfall rates will
    likely persist, and may even intensify, as HREF 2"/hr neighborhood probabilities peak above 35% by 01Z coincident with more
    widespread 0.75"/15min rainfall (3+"/hr rates) from the HRRR.

    Numerous thunderstorms are expected to develop as forecast by most
    available high-res CAMs, and these should move slowly in response
    to weak 0-6km mean layer winds of just 5-10 kts, with at times
    chaotic motion driven by collisions/mergers leading to repeating,
    training, or prolonged cells. Where this occurs, total rainfall of
    2-4" is possible as supported by both HREF and REFS 3"/6hr
    probabilities peaking at 40-60%.

    Although storms will move across soils that have some infiltration
    capacity and FFG that is generally 3"/3hrs, the slow motion of
    these intense rates could still overwhelm soils to produce rapid
    runoff. If this occurs across any urban areas, or even if less
    vulnerable regions experience multiple slow moving cells, this FFG
    could be exceeded leading to instances of flash flooding.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5xDxbUQ3NhfD7V1zd-2s5v9vdMglZkgqMj4VLzEnXDC95ktT5bfTM-LQZrf3sEjDhlHa= qU6P30gZyIHLM4tA6tm1hBw$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...JAX...TAE...

    ATTN...RFC...ALR...NWC...

    LAT...LON 33928339 33898281 33628184 32638125 32068103=20
    31618106 31188118 30748131 30358135 30038134=20
    29738155 29698181 29788218 29998256 30328281=20
    30778311 31438350 32268360 32408360 33378383=20
    33668375=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 22 00:39:47 2025
    AWUS01 KWNH 220038
    FFGMPD
    AZZ000-220600-

    Mesoscale Precipitation Discussion 0969
    NWS Weather Prediction Center College Park MD
    838 PM EDT Thu Aug 21 2025

    Areas affected...Southern Arizona

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

    Valid 220037Z - 220600Z

    Summary...Showers and thunderstorms along the Mogollon Rim will
    drop southwest through this evening while additional storms
    develop downstream. Rainfall rates of up to 1"/hr are expected,
    which could result in flash flooding.

    Discussion...The regional radar mosaic this aftn shows that
    convection has expanded along the Mogollon Rim, and storms are
    beginning to shift southwest off of the terrain. Although storm
    motions have been generally slow and tied to the terrain features
    thus far, anti-cyclonic flow around the large ridge of high
    pressure centered near the Four Corners will cause progression of
    these storms into the lower elevations. At the same time, a weak
    convergence axis noted in low-level wind fields is collocated with
    a plume of elevated MUCAPE above 1000 J/kg, which will support
    additional thunderstorm development. This instability is paired
    with PWs that were measured via the 00Z U/A sounding at KTUS to be
    around 1.3 inches, or the 75th percentile for the date. This will
    support at least brief heavy rain rates through the next several
    hours.

    So far, storms have been slow to move off the terrain, but this
    will change as the 0-6km mean winds increase to 10-15 kts from the
    E/NE. At the same time, a ribbon of modest but elevated bulk shear
    of 20-25 kts is progged to surge across southern Arizona, and this
    will support persistence of these storms as they track SW. At the
    same time, additional convection is likely to develop as more
    isolated storms in the lower elevations, and the interaction of
    these cells could briefly pulse rainfall rates up to above 1"/hr
    as progged by HREF neighborhood probabilities reaching 10-20%
    between 01Z-04Z. Additionally, the HRRR forced UA WRF depicts
    isolated 0.75"/1hr rain accumulations, further indicative of the
    potential rain intensities within the favorable thermodynamics.

    A notable inverted-V signature in the KTUS sounding combined with
    impressive DCAPE and the increasing forward motion of cells from
    the terrain indicates that wind, rather than rain, may be the
    primary threat this evening, and explains the modest HREF
    exceedance probabilities for 1"/6hrs that peak around 30%.
    However, the intensity of this rainfall could still overwhelm the
    soils, especially given the general vulnerability of this region
    due to currently dry soils (NASA SPoRT 0-10cm soil moisture below
    the 10th percentile). Although the risk appears generally
    isolated, any heavy rain moving atop sensitive terrain, burn
    scars, or urban areas could result in flash flood impacts through
    the evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5lroD-MT-SY_gkzlnVM0Wl-qYpTfub53RKfMo1c3-6Z3yX1mKQBrodnkgDDpm_dwH4N-= x-jB_GdEnTAo4GRUt-WPuVc$ for graphic product...

    ATTN...WFO...FGZ...PSR...TWC...

    ATTN...RFC...STR...NWC...

    LAT...LON 34581282 34371178 34011092 33530978 33050940=20
    32380960 32151004 31851054 31521101 31461138=20
    31461185 31581235 31801277 32111303 32621323=20
    33221332 33661324=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 22 01:26:32 2025
    AWUS01 KWNH 220126
    FFGMPD
    LAZ000-TXZ000-220630-

    Mesoscale Precipitation Discussion 0970
    NWS Weather Prediction Center College Park MD
    925 PM EDT Thu Aug 21 2025

    Areas affected...Coastal Plain from the Middle TX Coast through
    South-Central LA

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

    Valid 220125Z - 220630Z

    Summary...Showers and thunderstorms will continue to develop and
    move slowly along the TX/LA coasts this evening. Rainfall rates
    may at times reach 4"/hr, which could cause 2-3" of rain with
    locally higher amounts and instances of flash flooding.

    Discussion...The regional radar mosaic this evening shows an
    expansion of very slow moving thunderstorms aligned near the Gulf
    Coast from far SW LA through near San Antonio Bay, TX. This
    activity is blossoming in response to convergent ascent as
    low-level north winds over the land intersect east winds on the
    coast. This convergence is occurring beneath an elongated
    mid-level trough axis with subtly steeper lapse rates, providing
    additional ascent to the area. PWs measured on the KCRP and KLCH
    were around 2.1 inches, near the 90th percentile for the date,
    which is overlapping with MUCAPE of more than 2000 J/kg to produce
    an impressive thermodynamic environment. This environment is
    supporting radar-estimated rainfall rates from KHGX that have been
    2.5-3"/hr this evening.

    Although the CAMs feature a high variability in placement of heavy
    rain, there is good agreement that heavy rain amounts will occur
    during the next few hours. Moisture convergence along the coast
    may elevate PWs to 2.25 to 2.5 inches, supporting even more
    intense rain rates as forcing for ascent persists. This suggests
    that even with loss of daytime instability, the elevated MUCAPE
    will support intense rainfall, for which the HREF neighborhood
    probabilities forecast a 40-60% chance of exceeding 2"/hr, with
    brief rates reaching 4"/hr possible as suggested by the HRRR
    15-min rain accumulation product showing up to 1".

    While these rates themselves could be sufficient to overwhelm
    soils and lead to rapid runoff, the storms containing this intense
    rain will also be very slow moving to potentially prolong this
    prolific rainfall. 0-6km mean winds of just 5 kts will cause
    storms to drift generally to the east, but a lack of bulk shear
    indicating pulse-type convection will also result in chaotic
    motion during storm mergers and boundary collisions. This could
    lengthen the duration of heavy rain, or cause multiple rounds, in
    a few areas, leading to amounts that could reach 2-3" or locally
    higher (HREF and REFS probabilities for 3"/6hrs over 30%).

    FFG across the region is elevated at generally 3-4"/3hrs for which
    exceedance probabilities are modest. Despite this, at least
    isolated instances of flash flooding appear possible due to the
    intensity of this rain, with the most likely impacts occurring
    should any storm linger over more urban areas.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9UTroYqDAh338BSR9MARgzg82Li1kn0vvBfVdOG7v3-AcUL2t7Lg1G2Bvslq8TwZCTIV= wEluWXZW2nm921oZW_v4Vr0$ for graphic product...

    ATTN...WFO...CRP...EWX...HGX...LCH...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 31139339 30959251 30359179 29809173 29599191=20
    29529221 29499282 29319376 29049457 28719532=20
    28259625 27869679 27679716 27719746 27879754=20
    28379763 28789746 29379713 29819673 30589581=20
    30819514 30999448=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 22 04:32:04 2025
    AWUS01 KWNH 220431
    FFGMPD
    VAZ000-NCZ000-WVZ000-SCZ000-221000-

    Mesoscale Precipitation Discussion 0971
    NWS Weather Prediction Center College Park MD
    1231 AM EDT Fri Aug 22 2025

    Areas affected...west-central VA/NC into surrounding portions of
    WV/SC

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

    Valid 220430Z - 221000Z

    Summary...Slow moving, highly efficient heavy rainfall with rates
    up to 2-3"/hr will maintain a flash flood risk overnight.
    Localized totals of 5"+ may lead to isolated instances of
    significant, life threatening flash flooding.

    Discussion...As Hurricane Erin continues to move eastward over the
    open seas of the western North Atlantic, the storm seems to be
    indirectly contributing to a much more localized heavy rainfall
    event over portions of eastern VA into the eastern Carolinas. A
    massive anticyclonic wave break (AWB) is quite apparent over the
    western North Atlantic (characterized by low-PV air aloft injected
    from the tropics), contributing significantly to a blocked
    upper-level pattern/jet stream aloft. This blocking aloft has
    resulted in weak steering flow from the surface to the mid-upper
    levels with only a very weak/subtle trough apparent in the
    mid-levels (along with effective bulk shear of less than 20 kts).
    However, a PV (potential vorticity) streamer aloft (~250-300 mb)
    is associated with a narrow 40-50 kt jet streak (that is crucially quasi-stationary due the diabatically educed blocking from Erin)
    which has allowed for broad top-down driven ascent. Pockets of
    slow moving convection resulting from this upper-level feature
    (along with the other necessary components for heavy rainfall,
    including a pocket of deep tropospheric moisture with PWs of
    1.4-2.0" and MLCAPE of 500-1000 J/kg) are continuing to produce
    localized rainfall rates up to 2-3"/hr.

    Going forward, the slow southward propagation of convection is
    likely to continue (towards the pool of higher surface thetaE and
    associated MLCAPE 1000+ J/kg) with the 00z HREF mean storm motions appropriately indicating 10-15 kt S-SSW storm motions. While
    localized redevelopment further north cannot be ruled out in the
    neat term (as lingering instability still exists over portions of
    WV/VA that already received significantly locally heavy rainfall
    earlier), the threat going forward is certainly greatest for areas
    farther south (including Charlotte, NC and surrounding portions of
    NC/SC) where HREF probabilities for 3" and 5" exceedance are as
    high as 40-50% and 20-30%, respectively (which corresponds with
    25-35% probs for Flash Flood Guidance exceedance and up to 10%
    probs of 100-yr ARI exceedance). Isolated to scattered instances
    of flash flooding are possible, and localized totals of 5"+ may
    lead to isolated instances of significant, life threatening flash
    flooding (with particular concern for these totals occurring in
    more sensitive portions of the greater Charlotte metropolitan
    area).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Ujuz1WCLeHlyxv2eoo8DiIqpJnJhZ-9TkcGl4_e7EJw9seQhpze2XnOOdXcn2xIKbWX= 8tA1F4HGmZpz8gtA0oNF1S0$ for graphic product...

    ATTN...WFO...CAE...GSP...ILM...RAH...RLX...RNK...

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 38218001 37667980 37187977 36847988 36477974=20
    36077982 35008014 34677994 34018017 34238091=20
    34438157 34918201 35888214 36278153 36618097=20
    37368057 37988071=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 22 06:03:35 2025
    AWUS01 KWNH 220603
    FFGMPD
    MNZ000-SDZ000-221200-

    Mesoscale Precipitation Discussion 0972
    NWS Weather Prediction Center College Park MD
    202 AM EDT Fri Aug 22 2025

    Areas affected...central and eastern SD into some adjacent
    portions of MN

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

    Valid 220600Z - 221200Z

    Summary...Training and repeating of very heavy rainfall (up to
    2-4"/hr rates) may lead to isolated to scattered instances of
    flash flooding overnight.

    Discussion...Discrete convection is beginning to backbuild and
    proliferate this evening, in the vicinity of a sharp baroclinic
    zone with strong low-level frontogenesis. The mesoscale
    environment is otherwise characterized by MLCAPE of 1000-2500
    J/kg, PWs of 1.2-1.5" (near the 90th percentile, per ABR sounding
    climatology), and effective bulk shear of 35-45 kts. While
    steering flow is relatively strong at 20-30 kts towards the ESE
    with Corfidi vectors favoring southward propagation, current
    storms are anchored in the boundary layer near where low-level
    convergence is maximized with backbuilding towards the west
    favoring training/repeating of very heavy rainfall (with MRMS
    estimates indicating rates as high as 2-4"/hr).

    Latest hi-res guidance (00z HREF suite) is in remarkably good
    agreement with regard to the spatial axis of heavy rainfall,
    located in excellent proximity to where convection has
    proliferated. While the guidance is not in as good agreement with
    regard to the intensity of convection, the HREF does still
    indicate the extreme potential well with probabilities for 3" and
    5" exceedance of 40-50% and 5-10%, respectively (with the 00z ARW2
    and NAM-nest being the most aggressive in depicting 3-5" totals,
    along with some recent hourly runs of the experimental RRFS).
    Isolated to scattered instances of flash flooding are possible
    (with 3-hr FFGs generally ranging from 1.5-2.5" and associated
    HREF FFG exceedance probs of 30-40%), though impacts to life and
    property will likely be rather limited given how rural/sparsely
    populated the region is.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!62MjQZu1P30gFyRVFCIkljS7l3mHwOxLYzCOgJ7Dhz2d6bPgwec8ea20I81V77QKnax1= MBzyilZJvirpO1vs87e3uGc$ for graphic product...

    ATTN...WFO...ABR...FSD...MPX...UNR...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45309819 44869613 43889656 43699801 44049944=20
    44800116 45270021=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 22 15:53:44 2025
    AWUS01 KWNH 221553
    FFGMPD
    SCZ000-FLZ000-GAZ000-222152-

    Mesoscale Precipitation Discussion 0973
    NWS Weather Prediction Center College Park MD
    1153 AM EDT Fri Aug 22 2025

    Areas affected...portions of South Carolina, eastern Georgia, and
    far northeastern Florida

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

    Valid 221552Z - 222152Z

    Summary...Scattered, slow-moving storms will increase in coverage
    through the afternoon, with areas of 2-3 inch/hr rain rates
    becoming likely. Flash flooding is expected, especially in
    urban/low-lying areas.

    Discussion...Scattered, shallow convection has persisted across
    much of central South Carolina this morning downstream of a weak
    mid-level trough along the southern Appalachians. Over the past
    hour or so, deeper, more intense convection has materialized
    mainly along weak front extending from southern Georgia
    east-northeastward near the South Carolina coastline. The deeper
    convection has materialized in a very favorable environment for
    heavy rainfall (2-2.3 inch PW values, 1500+ J/kg MLCAPE, weak
    steering flow aloft). Areas of 2-3 inch/hr rain rates have
    materialized near the Charleston Metro area (including 0.9 inch in
    15 minutes at WFO Charleston and 2.25 inches in 30 minutes at KCHS
    recently).

    Over time, convection is expected to deepen and expand in coverage
    across the discussion area as surface heating promotes continued destabilization along with convergence along the aforementioned
    front. Heavy rain may also concentrate along any subtle
    sea-breeze boundaries that develop along the Georgia and Florida
    coastlines. Additional areas of 2-3 inch/hr rain rates are
    expected that should promote inundation especially in
    sensitive/urban locales. Convection should also be slow-moving
    given the relatively weak kinematics for steering flow aloft. FFG
    thresholds vary across the discussion area and peak at around 3
    inches/hr in less-sensitive spots, although these rates could
    still be exceeded occasionally given the moisture-rich environment
    in place supporting convective activity. Several instances of
    flash flooding are likely in this scenario.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_LxZGx6JC90Ce7XuKT6ir5Rk5UuRYcke3vtuIUfuTIvsZ_ip0pM9QlWoQ2w1Q3gwtA1s= 1pGz8GUa9wNbHm9Vr2OXYQA$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 33697952 33017912 32048012 30058119 29668148=20
    30268266 31078390 32068362 33078250 33658108=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 Aug 22 16:12:42 2025
    AWUS01 KWNH 221612
    FFGMPD
    LAZ000-TXZ000-222211-

    Mesoscale Precipitation Discussion 0974
    NWS Weather Prediction Center College Park MD
    1212 PM EDT Fri Aug 22 2025

    Areas affected...southeast Texas, southwestern Louisiana

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

    Valid 221611Z - 222211Z

    Summary...Slow-moving convection continues to expand in coverage
    this morning, with areas of 2-3 inch/hr rain rates becoming likely
    beneath the strongest storms. Flash flooding is expected.

    Discussion...Deep convection has been focused mainly along coastal
    areas of Texas and Louisiana for most of the morning. Over the
    past hour or so, storms has materialized just inland across the
    discussion area (nearer to I-10) due to 1) strong surface heating/destabilization, 2) abundant moisture (2.3 inch PW), and
    3) convergence along a weak front across the region (generally
    from Houston Metro east to Baton Rouge, LA). Kinematics/steering
    flow aloft are very weak (<5 knots), suggestive of slow-moving
    cells/clusters that are outflow dominant and propagate erratically
    through the afternoon. A few of these clusters were forming near
    Lake Charles and just north of Houston while already producing
    spots of 1-2 inch/hr rain rates.

    With continued surface heating, convective clusters are expected
    to expand in coverage. The orientation of storms relative to
    outflow from prior activity over the Gulf suggests potential for
    several cell mergers as well. 2-3 inch/hr rain rates will
    eventually materialize, and may impact populated/flashy urban
    centers such as Lake Charles, Beaumont, and Houston through 20Z.=20
    FFGs near those areas are as low as 1-1.5 inches/hr and should be
    readily exceeded. Surrounding areas have higher FFGs (in the 3
    inch/hr range) that should still be exceeded as stronger
    convection develops through the morning and early afternoon.=20
    Areas of flash flooding are expected given the developing scenario.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_wnU-7iT7MQkYAxXh3Al7S-FyxNAXNu1ZJgZgdIZDhdtW2AyLf32LS_uGSkr5tNcXItn= 2FSdcby0QR_ZutRo08dJZtc$ for graphic product...

    ATTN...WFO...CRP...EWX...HGX...LCH...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 31019345 30519193 29869179 29589269 29619471=20
    28749616 29029737 29879728 30399670 30939521=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 Aug 22 17:01:14 2025
    AWUS01 KWNH 221701
    FFGMPD
    ALZ000-MSZ000-LAZ000-222259-

    Mesoscale Precipitation Discussion 0975
    NWS Weather Prediction Center College Park MD
    100 PM EDT Fri Aug 22 2025

    Areas affected...southeastern Louisiana, coastal areas of
    Mississippi, far southern Alabama

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

    Valid 221659Z - 222259Z

    Summary...Spotty/isolated flash flood potential exists with
    slow-moving thunderstorms across the discussion area through
    22Z/4p CDT.

    Discussion...Recent satellite imagery indicates deepening
    convection along a variety of subtle low-level confluence
    boundaries across the discussion area. Surface heating across the
    region has enabled development of 4000 J/kg SBCAPE in the
    pre-convective airmass amid 2.2 inch PW values. Deep, efficient
    convective process are already supporting spots of 1 inch/hr rain
    rates (estimated per MRMS). Additional areas of 1-2 inch/hr rain
    rates should develop through the afternoon as additional cells
    develop and mergers begin to occur.

    The rainfall will occur on locally sensitive areas due to
    urbanized/hydrophobic surfaces in/near New Orleans, Baton Rouge,
    and Northshore Lake Pontchartrain near Covington and Slidell.=20
    Isolated instances of flash flooding will become more probable
    during the afternoon hours.

    Much of the convective (and flash flood) threat will be diurnally
    driven today, although the degree of convective overturning will
    ultimately modulate the spatiotemporal threat of the flash flood
    risk through 22Z/4p CDT. Eventually, widespread low-level
    stabilization should result in a lower flash flood threat,
    although this scenario should take a few hours to play out.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4qmc1xLRNtT4GBhZO9kPhmytNW_ywPaqGJSGgUV5OvmQLj-QXoTwpVyk4C-FDmcBh5nS= 6pa-9XnEC6gwK6RtEZ0osA4$ for graphic product...

    ATTN...WFO...LCH...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 30989045 30788866 30468810 29618895 29148912=20
    28969035 29399160 29889234 30659225=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 22 21:02:16 2025
    AWUS01 KWNH 222102
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-230300-

    Mesoscale Precipitation Discussion 0976
    NWS Weather Prediction Center College Park MD
    500 PM EDT Fri Aug 22 2025

    Areas affected...Far Eastern CA...Southern NV...Central to
    Northwest AZ...Central and Southwest UT

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

    Valid 222100Z - 230300Z

    SUMMARY...Scattered monsoonal showers and thunderstorms are
    expected going through the afternoon and early evening hours
    across portions of the Southwest U.S. Some localized concerns for
    flash flooding will exist for the more sensitive slot canyon
    locations and burn scar areas.

    DISCUSSION...The early-afternoon GOES-W visible satellite imagery
    shows a substantial CU/TCU field over the Mogollon Rim of central
    to northwest AZ and also across much of southwest UT where a
    combination of orographics along with diurnally enhanced
    instability and the presence of monsoonal moisture are working to
    initiate additional areas of convection. Already there are
    scattered small-scale clusters of locally heavy showers and
    thunderstorms where differential boundaries and nearby
    terrain-induced circulations have been helping to initiate and
    locally concentrate pockets of convection.

    Early day cloud cover has locally helped to mitigate the level of
    surface-based instability, but satellite trends show substantial
    heating occurring over much of central to northwest AZ and into
    southwest UT which should help to facilitate additional scattered
    areas of showers and thunderstorms over the next several hours.
    There is also proximity of an MCV near the CA/AZ/NV border region,
    and differential heating along the eastern and northern flanks of
    this energy and associated cloud canopy may also help drive
    convective initiation this afternoon.

    The region is relatively moist today with PW anomalies coming in
    as high as 1.5 standard deviations above normal in close proximity
    to a 700 mb high center. CIRA-ALPW data generally shows some of
    the greater moisture concentrations in the 700/500 mb layer and
    this will help to support some relatively efficient convection for
    heavier rainfall rates.

    Some rainfall rates may reach as high as 1 inch in 20 to 30
    minutes with the stronger cells, with some spotty rainfall totals
    through this evening reaching as high as 1.5 to 2.5 inches where
    any cells tend to become anchored near areas of higher terrain.
    Some of the RRFS/REFS guidance supports this which seems plausible
    given the satellite and radar trends. This may result in there
    being localized areas of flash flooding. There are some sensitive
    burn scar concerns (especially over northern AZ) along with the
    normally sensitive slot canyon locations (southwest to
    south-central UT) that are vulnerable to any high rainfall rate
    activity, so these areas should be closely monitored.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6YDKnBG52iNQy2dp4u55cuA3H6DEvnr6GvljAi0db6MzWMTR4mtzjPNmMZaJFgSeFft9= I8oOgLEK3VFG52FX71C-Dhc$ for graphic product...

    ATTN...WFO...FGZ...LKN...PSR...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 39181115 39001068 37981065 36701168 35571155=20
    34731061 34291023 33791048 33641127 33651273=20
    33791397 34251523 35121602 36071625 36881610=20
    37781544 38421455 38751351 38861244=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 22 21:56:17 2025
    AWUS01 KWNH 222156
    FFGMPD
    COZ000-230355-

    Mesoscale Precipitation Discussion 0977
    NWS Weather Prediction Center College Park MD
    555 PM EDT Fri Aug 22 2025

    Areas affected...Eastern CO

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

    Valid 222155Z - 230355Z

    SUMMARY...Showers and thunderstorms should gradually expand in
    coverage this evening. Some cell-merger and cell-training concerns
    may cause some isolated areas of flash flooding.

    DISCUSSION...The latest GOES-E IR satellite imagery shows cooling
    convective tops near the Front Range and Palmer Divide which are
    expected to gradually grow upscale a bit this evening with some
    gradual consolidation into some loosely organized MCS activity
    over eastern CO this evening. The convection is forming in close
    proximity to a stationary front with the additional aid of
    orographic ascent/forcing within a moderately unstable environment.

    Much of the instability pool is along and just north of the front
    in this case with MLCAPE values across north-central to northeast
    CO as high as 1500 J/kg. This is mainly due to the fact that
    surface dew points (locally 55 to 60+) just north of the front are
    quite a bit higher than they are to the south out ahead of it.
    Weak shortwave energy rounding the top of a mid-level ridge near
    the Four Corners region will eject down across eastern CO this
    evening and interact with this instability axis and the
    aforementioned frontal zone to support the upscale growth of
    convection.

    A consensus of the latest 12Z HREF/REFS guidance suggests some
    spotty areas of 2 to 4 inch rainfall totals will be possible where
    some localized cell-merger and cell-training activity occurs. Both
    the HREF and REFS depict some low to moderate probabilities
    (generally 30 to 50 percent) of seeing the 3-hour FFG values
    exceeded this evening as this shower and thunderstorm activity
    continues to grow in coverage and intensity. As a result, some
    isolated areas of flash flooding will be possible.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!681kSBXyaO26XX5rMnmZmakGChP-LhLm_c90fIFh-sXfDp-iV-DoBI83gR2vw9ltl-a2= 6C4esbBRDCgavWH6nVFlFtU$ for graphic product...

    ATTN...WFO...BOU...GLD...PUB...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 40310271 39540211 38850248 38240349 37880472=20
    38070552 38580579 39360560 40030443=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 22 22:32:16 2025
    AWUS01 KWNH 222232
    FFGMPD
    SCZ000-FLZ000-GAZ000-230430-

    Mesoscale Precipitation Discussion 0978
    NWS Weather Prediction Center College Park MD
    630 PM EDT Fri Aug 22 2025

    Areas affected...Southern and Eastern GA...SC Lowcountry

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

    Valid 222230Z - 230430Z

    SUMMARY...Additional areas of very heavy shower and thunderstorm
    activity going through the evening hours will maintain a
    likelihood for more areas of flash flooding.

    DISCUSSION...The late-day GOES-E IR satellite imagery in
    conjunction with regional radar shows broken areas of very heavy
    shower and thunderstorm activity continuing to impact areas of the
    SC Lowcountry on down through eastern and southern GA. A
    combination of a stationary front along with multiple mesoscale
    outflow boundary collisions within a very moist and unstable
    airmass continues to facilitate the ongoing convection, and
    additional clusters of convection should continue into the evening
    hours.

    MLCAPE values are as high as 1500 to 2500 J/kg and this coupled
    with PWs of 2.2 to 2.4 inches will drive rainfall rates to locally
    still be well into the 2 to 3 inch/hour range with the stronger
    storms at least through early this evening.

    The additional rainfall footprint this evening will be dictated by
    the longevity of the instability pool along the front, but also
    mitigated by the proximity of convergent and moist low-level flow
    near the front, and with some weak right-entrance region upper jet
    forcing overhead.

    Recent runs of the experimental WoFS along with the HRRR and RRFS
    guidance suggest the convection may linger well into the evening
    hours, with some rather heavy additional totals. The steering flow
    over the region is also rather weak, and this is supporting slow
    cell-motions which with the high rainfall rates will favor some
    additional rainfall totals locally reaching 3 to 5 inches. In
    fact, the 90th percentile of the 6-hour QPF from the 21Z WoFS run
    suggests parts of south-central GA may see additional rainfall
    totals locally exceeding 6+ inches.

    Given the setup and additional rainfall potential, more areas of
    flash flooding are likely to occur going into the evening hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-98S0FHjnkcohEfm_nUkKVaiZlQrId7Kl_gFVyksAPYyKlrHPOkpHeJVtfjDnAFk0Lus= qEVHPwURi9hindXil4gpUDM$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 33668279 33588217 32958109 33387968 32897949=20
    32587992 32028077 30918166 30608323 30948457=20
    31638505 32268485 32918396=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 22 23:15:19 2025
    AWUS01 KWNH 222315
    FFGMPD
    NVZ000-CAZ000-230500-

    Mesoscale Precipitation Discussion 0979
    NWS Weather Prediction Center College Park MD
    713 PM EDT Fri Aug 22 2025

    Areas affected...Portions of the Sierra Nevada

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

    Valid 222313Z - 230500Z

    SUMMARY...Scattered slow-moving areas of showers and thunderstorms
    over the Sierra Nevada late this afternoon and early this evening
    may cause some localized concerns for flash flooding.

    DISCUSSION...The mid-afternoon GOES-W Day Cloud Phase RGB
    satellite imagery along with LightningCast data shows convection
    initiating and gradually increasing in coverage over portions of
    the Sierra Nevada. The convection that is initiating is in
    response to strong diurnal heating with increasing instability and terrain-driven circulations in a rather moist monsoonal regime.

    SBCAPE values have risen to over 1000 K/kg along the western
    flanks of the Sierra Nevada involving eastern CA with surface data
    showing modest upslope flow into the higher terrain. The latest
    RAP analysis generally suggests about 10 to 15 kts of southerly
    flow in the 850/700 mb layer from Lake Tahoe southward down
    Bishop.

    Coinciding with this is a rather moist mid-level column with
    CIRA-ALPW showing elevated moisture in the 700/500 mb layer and
    this is supporting PW anomalies across the region of 2.0 to 2.5
    standard deviations above normal. Deep layer southerly flow around
    the western periphery of the subtropical ridge over the Southwest
    U.S. is facilitating the poleward transport of monsoonal moisture
    up across these areas, and this is expected to help drive a threat
    for scattered heavy shower and thunderstorm activity going through
    the evening hours.

    Overall, the latest hires model guidance is rather ill-defined
    with the convective footprint. However, the satellite and radar
    trends suggest concerns for showers and thunderstorms to be
    locally anchored near the higher terrain this evening with some
    backbuilding characteristics which is further supported by weak
    propagation vectors and the orographic focus that is in place for
    development.

    Rainfall rates with the stronger storms may reach 0.75 to 1.0
    inch/hour, with potential for much of this to fall in as little as
    30 minutes. Spotty storm totals of 1.5 to 2.5 inches will be
    possible where any repeating cell-activity occurs. Given the
    setup, some localized areas of flash flooding will be possible
    going through this evening, and this will include potential for
    some burn scar impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_OhMyc7fizNcmV1Zhs2kWs62h4JevC1T6VoPZceqfq68OcDmk6RuxOXJXenwnfgBNS3a= 4WNIU4xmsTc3C9scPSrd_d8$ for graphic product...

    ATTN...WFO...HNX...REV...VEF...

    ATTN...RFC...RSA...NWC...

    LAT...LON 39371907 39131865 38311816 37671790 37091777=20
    36501775 36361800 36391833 36691869 37431910=20
    38031941 38741982 39181969=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 23 11:17:28 2025
    AWUS01 KWNH 231117
    FFGMPD
    SCZ000-231616-

    Mesoscale Precipitation Discussion 0980
    NWS Weather Prediction Center College Park MD
    716 AM EDT Sat Aug 23 2025

    Areas affected...coastal areas of South Carolina

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

    Valid 231116Z - 231616Z

    Summary...Localized areas of flooding are expected over the next
    4-6 hours (through 16Z/noon EDT) as convection over the Gulf
    Stream slowly migrates inland toward coastal areas of South
    Carolina.

    Discussion...Recent radar/satellite imagery indicates a fetch of
    deep convection along an axis from near Charleston to about 80-100
    miles east-southeast of Charleston. The convection was likely
    being maintained by several synoptic features, including 1) a
    mid-level vorticity maximum over Georgia that was providing ascent
    aloft over the region and 2) low-level easterly flow just north of
    a weak low near Savannah that was helping to maintain moderate
    instability (1000+ J/kg SBCAPE) right along coastal areas. An
    abundantly moist airmass (2.3 inch PW) remains in place,
    supporting efficient rainfall processes with stronger cells that
    develop. Additionally, parts of the region experienced 3-8 inches
    of rainfall over the past 24 hours, and onshore flow was
    persisting during this morning's high tide, which was likely
    resulting in inundation of low-lying coastal areas along with
    hindered runoff/drainage.

    The ongoing convective trends should continue for the next 4-6
    hours. Areas of 1 inch/hr rain rates have began near Charleston
    over the past 30 minutes, and these rates should continue
    periodically while the convective axis in maintained in the
    region. Areas of 2-3 inch rainfall totals are expected. Over
    time, the convective axis should drift northward and/or weaken (as
    depicted by CAMs), although this process should take several hours
    to unfold.

    Flooding is possible along coastal areas this morning and could be
    enhanced by the locally heavy rainfall that periodially moves
    onshore.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5WIE0gVjrnZ8e9Dfw0R5PBJGhSnKCAAZNTQaNH8c6g0ZibOBmamIJ7VmmBabubuODsTR= z-GQ0iQ1w7YJ2rxtgEZwLLA$ for graphic product...

    ATTN...WFO...CHS...ILM...

    ATTN...RFC...ALR...NWC...

    LAT...LON 33677915 33507868 32378027 32728065 33387996=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 Aug 23 13:34:29 2025
    AWUS01 KWNH 231334
    FFGMPD
    SCZ000-GAZ000-231933-

    Mesoscale Precipitation Discussion 0981
    NWS Weather Prediction Center College Park MD
    934 AM EDT Sat Aug 23 2025

    Areas affected...central/southern Georgia

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

    Valid 231333Z - 231933Z

    Summary...A few instances of flash flooding are expected today
    across Georgia. Heavy rainfall, with rain rates approaching 2
    inches/hr at times, are expected through 19Z/3p EDT.

    Discussion...An axis of shallow, slow-moving convection was
    located along subtle low-level confluence zone extending from near
    Peachtree City to Sandersville/east of Macon this morning.=20 Ascent/convergence along this axis and the presence of a mid-level
    wave aloft has aided in persistence of convection across the
    region despite modest amounts of surface-based instability (~500
    J/kg). The convection is in an abundantly moist environment (2+
    inch PW values), supporting efficient rainfall processes. Spots
    of 2 inch/hr rain rates are estimated per MRMS currently, which
    isn't surprising given the moist airmass and slow movement of
    convection along the convergence axis.

    The ongoing scenario for heavy rainfall should persist for a few
    hours - and perhaps through 19Z/3p EDT today. SPC mesoanalysis
    indicate an axis of deep moist convergence collocated with the
    axis of convection that should migrate very slowly or even stall.
    Areas of heavy rainfall are expected, and local rainfall totals
    exceeding 3-5 inches are possible depending on the persistence of
    convection at any one locale. Breaks in the cloud cover south of
    this confluence axis suggests that additional convection may
    develop and produce heavy rainfall (>1 inch/hr rain rates) that
    may also cause flash flood instances - especially in areas that
    received 2-5 inches yesterday in/near Macon. Flash flooding is
    likely given the aforementioned scenario.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!44rJHtEiQZGfgSQQTHfuh8tyvC4bKOVRlLnGaj0EwACrdxHIU2cyGTRRbwrZc7ZCNQjy= UNVISK16-GTon4POigRl_OY$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...JAX...TAE...

    ATTN...RFC...ALR...NWC...

    LAT...LON 33938451 33868302 33228107 32328070 31748183=20
    31608442 33198502=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 23 16:27:31 2025
    AWUS01 KWNH 231627
    FFGMPD
    SCZ000-GAZ000-232025-

    Mesoscale Precipitation Discussion 0982
    NWS Weather Prediction Center College Park MD
    1226 PM EDT Sat Aug 23 2025

    Areas affected...far southern South Carolina, coastal areas of
    Georgia

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

    Valid 231625Z - 232025Z

    Summary...Heavy rainfall will continue to impact coastal areas
    near Savannah, GA over the next 3 hours or so. Flash flooding
    remains possible, and could be locally enhanced by coastal
    flooding/inundation.

    Discussion...Although widespread convective overturning has
    stabilized much of the state of South Carolina, a small/focused
    area of instability resides across far southern portions of the
    state and in/near the Savannah, GA area. Weak low-level onshore
    flow just north of a low has maintained ~1500 J/kg SBCAPE in that
    area. PW values approaching 2.4 inches are also maximized there.
    The buoyancy/moisture combo is combining with weak steering flow
    aloft to foster deep convection with slow storm motions and
    1.5-2.5 inch/hr rain rates currently.

    The heavy rainfall continues to migrate inland toward areas that
    have experienced high tide earlier this morning and 3-9 inch
    rainfall totals over the past 24 hours. Wet soils and onshore
    flow should continue to hinder runoff/drainage and - when combined
    with heavy rainfall - may continue to pose flood/flash flood risk
    over the next 2-4 hours (through 20Z/4p EDT).

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_UC_6F2jmHZTTzSvk22UUH3dyf-73ZfElHqEmsdA96Xt6LGDaoxt7ZeHReqjyolQH_3n= ZWX8ZbuhPBFajMKMkGWMNFo$ for graphic product...

    ATTN...WFO...CHS...JAX...

    ATTN...RFC...ALR...NWC...

    LAT...LON 32728052 32358055 31258117 31258178 31708196=20
    32368162=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 23 18:39:01 2025
    AWUS01 KWNH 231838
    FFGMPD
    NVZ000-CAZ000-240037-

    Mesoscale Precipitation Discussion 0983
    NWS Weather Prediction Center College Park MD
    237 PM EDT Sat Aug 23 2025

    Areas affected...Southern and Eastern CA...Sierra Nevada

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

    Valid 231837Z - 240037Z

    SUMMARY...Deep layer monsoonal moisture advancing up across
    southern and eastern CA and into the higher terrain of the Sierra
    Nevada will foster scattered to broken areas of heavy showers and
    thunderstorms this afternoon. Scattered areas of flash flooding
    are likely, and especially over the Sierra Nevada.

    DISCUSSION...The deeper layer subtropical ridge over the Southwest
    is in a very favorable position to facilitate the northwestward
    transport of monsoonal moisture up across southern and eastern CA
    and well into the Sierra Nevada. The latest CIRA-ALPW data shows
    moisture near or above the 90th percentile of climatology in the
    700/500 mb and 500/300 mb layers respectively across the region,
    with PW anomalies overall running a solid 2 to 3 standard
    deviations above normal.

    This moisture coupled with placement of elongated mid-level vort
    energy and deeper layer upslope flow over the higher terrain will
    combine with increasing boundary layer instability for scattered
    to eventually broken areas of heavy shower and thunderstorm
    activity. Cloud cover over portions of the Transverse and
    Peninsular Ranges of southern CA have mitigated the build up of
    instability to a degree, but the proximity of vort energy and
    steeper mid-level lapse rates have already been focusing an axis
    of showers and thunderstorms. This activity should tend to expand
    a bit in coverage as differential heating boundaries and greater
    instability adjacent to the terrain help to drive additional
    mesoscale-enhanced circulations for new convective development.

    The Sierra Nevada overall is the area that will likely see the
    greatest concentration of heavier rainfall though given the level
    of anomalous moisture in place along with upslope flow. Even the
    hires CAM model guidance which can suffer with convective details
    over the Sierra Nevada has a footprint for impactful rainfall,
    including a signal for locally repeating cell-activity. The most
    recent visible satellite imagery along with LightningCast data
    shows convective initiation underway and suggestive of multiple
    rounds of convective potential in conjunction with the full
    diurnal heating cycle.

    Given the high moisture environment, rainfall rates up to 1.5
    inches/hour will be possible, with some localized storm total
    amounts by late this afternoon of 2 to 4 inches possible where any
    cells tend to become more terrain-anchored. Scattered areas of
    flash flooding are likely with today's convection, with the
    greatest threat over the Sierra Nevada where there will also be
    some burn scar sensitivities.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6jxbe72gLfvIl9oz_JQC2znK8LlCdDdfWl3Xj-JLfB9zPHkxSOiX7WrfOspbc1NhzrPw= ZSbUFG5s2dL5xWppXQEBwZU$ for graphic product...

    ATTN...WFO...HNX...LOX...PSR...REV...SGX...STO...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 39211974 39091885 38021760 36821708 35361691=20
    34501635 33481530 32731533 32551597 32621671=20
    33251717 33711785 34061855 34571913 35431918=20
    36151891 37041920 38001996 38692010=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 23 18:50:33 2025
    AWUS01 KWNH 231850
    FFGMPD
    SCZ000-FLZ000-GAZ000-240048-

    Mesoscale Precipitation Discussion 0984
    NWS Weather Prediction Center College Park MD
    250 PM EDT Sat Aug 23 2025

    Areas affected...southern/southeastern Georgia, southern/coastal
    South Carolina, northern Florida

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

    Valid 231848Z - 240048Z

    Summary...Scattered, slow-moving storms will continue to produce
    areas of 1-2.5 inch/hr rain rates at times. Flash flooding is
    possible - especially where heavy rain falls on
    sensitive/urbanized ground conditions.

    Discussion...Flash flood potential continues across much of
    southern Georgia and coastal areas of Georgia and South Carolina.
    Most of the deep convection was focused along and south of a weak
    differential heating and zone currently across central Georgia
    from just south of Atlanta through Macon to just north of
    Savannah. Along and south of this confluence zone, pockets of
    heating with an abundantly moist airmass (2+ inch PW values) has
    contributed to scattered development of deep convection. Weak
    steering flow aloft has allowed for slow and at times erratic
    storm motions along with several mergers, enabling rain rates to
    exceed 2 inches/hr at times in a few spots. Some of the heavy
    rain was falling on areas experiencing local inundation/poor
    drainage due to onshore flow along coastal areas, resulting in
    several instances of flooding impacts. In other areas, rainfall
    was occurring atop spots of 3-9 inch rainfall totals over the past
    24 hours, resulting in wet soils and increased potential for
    runoff.

    Ongoing convective trends will continue through at least 00Z/8p
    EDT tonight, with locally sensitive areas experiencing a continued
    threat of heavy rainfall. Several instances of flash flooding are
    possible, and local enhancement of flash flood risk from onshore
    flow near coastal areas should continue. Modest destabilization
    has also occurred along South Carolina coastal areas near
    Charleston, and although a lull in deep convective activity has
    been observed over the past 1-2 hours, redevelopment of rainfall
    (and 1 inch/hr rates) may occur through the evening, renewing the
    flash flood risk in that area.

    Cook=20

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5L-IkteKJH6e1ootPivcfjqIomPwV-vQ-l3ndi3zZ3msMBGXcVhgEgfOSrp73PGeFUD0= PnuOhvSz8UytAWnDiq-wlL0$ for graphic product...

    ATTN...WFO...CHS...FFC...JAX...TAE...

    ATTN...RFC...ALR...NWC...

    LAT...LON 33227991 33137938 31438111 30298167 30118367=20
    30148500 30808506 31298437 31998462 32748465=20
    32768322 32788091=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 23 19:32:34 2025
    AWUS01 KWNH 231932
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-240130-

    Mesoscale Precipitation Discussion 0985
    NWS Weather Prediction Center College Park MD
    331 PM EDT Sat Aug 23 2025

    Areas affected...Central to Southwest UT...Central to Northwest
    AZ...Southern NV...Far Eastern CA

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

    Valid 231930Z - 240130Z

    SUMMARY...Monsoonal moisture entrenched over the Southwest U.S.
    will support locally heavy showers and thunderstorms through this
    afternoon. Scattered areas of flash flooding will be likely today,
    and especially near and around the more sensitive slot canyon and
    burn scar locations.

    DISCUSSION...A deep layer subtropical ridge near the Four Corners
    region has allowed monsoonal moisture to become rather well
    entrenced around its western flank over the last couple of days,
    with PW anomalies this morning reaching as high as 2 to 3 standard
    deviations above normal across far eastern CA up through southern
    NV and into far northwest AZ and adjacent areas of central to
    southwest UT.

    The moisture is quite concentrated in the 700/300 mb layer based
    on the latest CIRA-ALPW data and this coupled with orographics and
    additional daytime heating/surface-based instability will favor
    expanding areas of showers and thunderstorms with elevated
    rainfall rates capable of reaching 1.5+ inches/hour. SBCAPE values
    of 1000+ J/kg are already noted over portions of central AZ and
    also over southern UT where there has also been recent convective
    development, and these values should continue to increase in the
    near-term.

    Given the influence of orographics/terrain-driven circulations and
    eventually convectively-driven outflow boundaries, there should be
    pockets of locally focused convection where some of the rainfall
    totals may reach as high as 2 to 4 inches. This will be supported
    by the anomalous moist monsoonal environment that is generally in
    place.

    These rainfall totals may result in there being enhanced
    runoff/debris flow concerns near any burn scar locations, and
    portions of northern AZ in particular are notably sensitive due to
    recent fire activity. Adjacent areas of southwest to central UT
    will also have concerns once again for slot canyon flash flooding
    which may be locally significant today. The flash flood threat is
    more conditional across southern NV and adjacent areas of far
    eastern CA, but in general across the MPD area, scattered areas of
    flash flooding are likely going through the afternoon hours as
    convection develops and expands in coverage.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!65ZV872x4R4Qvt_5TfR9p-kqddEwY-iXRwyh16S5PczJCf7cD-cJfgjOZNR9ot_2JdbC= eJf8ehBmU-TSd3v0mkXwugw$ for graphic product...

    ATTN...WFO...FGZ...PSR...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 39341208 38941097 37831070 35911120 34661037=20
    33741076 33661308 34531532 35851597 37191572=20
    37961485 38631382=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 23 19:57:01 2025
    AWUS01 KWNH 231956
    FFGMPD
    COZ000-NMZ000-240155-

    Mesoscale Precipitation Discussion 0986
    NWS Weather Prediction Center College Park MD
    356 PM EDT Sat Aug 23 2025

    Areas affected...Central and Southern CO...Northern NM

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

    Valid 231955Z - 240155Z

    SUMMARY...Heavy showers and thunderstorms will continue to expand
    in coverage over the next few hours. Scattered areas of flash
    flooding will be likely which may include some localized burn scar
    impacts.

    DISCUSSION...The early-afternoon GOES-W IR satellite imagery shows
    broken areas of heavy showers and thunderstorms impacting portions
    of central and southern CO on down into northern NM. Additional
    expansion of convection is expected over the next few hours as
    diurnal heating/instability coupled with very favorable orographic ascent/terrain-induced circulations continues to support vertical
    updrafts for convective initiation and sustenance.

    MLCAPE values over northern NM and southern CO are locally over
    1000+ J/kg and the region is quite moist with PW anomalies of 1.5+
    standard deviations above normal. Some mid to high-level monsoonal
    moisture wrapping around the northeast flank of the Four Corners
    subtropical ridge is contributing to this more anomalous moisture
    profile.

    The latest hires guidance strongly suggests that some of the
    heaviest rainfall this afternoon will tend to be over the Sangre
    De Cristo Range where some spotty 2 to 4 inch rainfall totals will
    be possible. Both the 12Z HREF and 06Z REFS guidance support these
    amounts. Locally heavy rainfall totals are expected though as far
    north as central CO by later this afternoon as diurnal heating,
    orographics and even some stronger shear profiles help to support
    stronger updrafts and locally heavy rainfall rates which may reach
    1.5+ inches/hour.

    Given the higher rainfall rates and localized storm potential near
    the more orographically favored terrain, there will likely be
    scattered areas of flash flooding including potential for burn
    scar impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7f21XVrSoxBvMaDDMJaSrE9OEHsvFlVtoddxZ7FFhHb20NIoniLTJZaFXBtcd0ZDQVAi= wannQMIr9rc4u3oWCR7OX2k$ for graphic product...

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

    ATTN...RFC...FWR...KRF...STR...TUA...NWC...

    LAT...LON 39920493 39550433 38830420 37840448 37350425=20
    36750370 35830381 35080455 34590558 34580648=20
    35160711 36220725 37170824 38130837 39220763=20
    39860642=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 23 21:03:02 2025
    AWUS01 KWNH 232102
    FFGMPD
    VAZ000-NCZ000-WVZ000-GAZ000-TNZ000-KYZ000-ALZ000-240300-

    Mesoscale Precipitation Discussion 0987
    NWS Weather Prediction Center College Park MD
    501 PM EDT Sat Aug 23 2025

    Areas affected...TN Valley...Southern Appalachians

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

    Valid 232100Z - 240300Z

    SUMMARY...Scattered slow-moving areas of showers and thunderstorms
    may pose an isolated threat for flash flooding going through this
    evening.

    DISCUSSION...The late-afternoon GOES-E GeoColor satellite imagery
    shows scattered areas of showers and thunderstorms impacting
    portions of the TN Valley and the southern Appalachians with an
    emphasis on the Cumberland Plateau.

    Moderate buoyancy with MLCAPE values of near 1500 J/kg coupled
    with modest moisture convergence near the terrain should help
    sustain the convective threat through early this evening. PWs are
    seasonably moist with values of 1.5 to 1.75 inches and this
    coupled with the available instability will support rainfall rates
    reaching as high as 1.5 to 2.5 inches/hour with the stronger
    storms.

    Overall, a lack of shear should keep the convection in pulse mode
    through the remainder of the afternoon and evening. However, with
    weak steering currents and the orographic focus of the activity
    near areas of higher terrain, there may be sufficient persistence
    of convection locally to yield some spotty rainfall totals of 2 to
    4 inches.

    The FFG values across portions of far southwest VA down through
    eastern TN are relatively low, and the 12Z HREF/06Z REFS suite of
    guidance shows some low to moderate probabilities (20 to 50
    percent) of seeing the 3-hour FFG values exceeded going through
    this evening. This suggests a threat for isolated areas of flash
    flooding with these pulse areas of convection.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_fDX79rI7xtOdKs1du2XA6IQ6eBLAMkKpP7Y6Bvjs91vWQLp5-aGgT2C6nkbskQp6VRs= ZzhsJ3Hn_Xs9PTNu2Q3ATGs$ for graphic product...

    ATTN...WFO...BMX...FFC...GSP...HUN...JKL...LMK...MRX...OHX...
    RLX...RNK...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 38328199 38218097 37628098 36628167 36028248=20
    35288382 35068463 34978543 34618589 33938660=20
    34108758 35018756 35738685 37138449=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 23 22:37:07 2025
    AWUS01 KWNH 232237
    FFGMPD
    NVZ000-CAZ000-240330-

    Mesoscale Precipitation Discussion 0988
    NWS Weather Prediction Center College Park MD
    635 PM EDT Sat Aug 23 2025

    Areas affected...Sierra Nevada

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

    Valid 232235Z - 240330Z

    SUMMARY...Locally heavy showers and thunderstorms will continue
    into the evening hours along the foothills and near the crest of
    the Sierra Nevada. Scattered areas of flash flooding are likely
    which will include localized burn scar impacts.

    DISCUSSION...GOES-W IR satellite imagery shows expanding and
    cooling convective tops across the Sierra Nevada along with some
    of the adjacent foothills. The convection is being strongly aided
    by orographic ascent/upslope flow into the terrain coupled with
    increasingly divergent flow aloft and an anomalously moist
    monsoonal moisture flow pattern.

    SBCAPE values of 500 to 1000 J/kg are noted along the western
    slopes of the Sierra Nevada with some modest effective bulk shear
    in place of 20 to 30 kts. The latest RAP analysis along with IR
    satellite imagery shows evidence of a weak upper-level jet streak
    lifting north up across the Central Valley of CA which is favoring
    some divergent and resulting diffluent flow structures aloft.

    This subtle uptick in deeper layer ascent along with the ongoing
    orographic and thermodynamic support should favor additional
    rounds of heavy showers and thunderstorms near the high terrain
    going into the evening hours. Rainfall rates will be capable of
    reaching 1 to 1.5 inches/hour given PWs running locally in the
    95th+ percentile of climatology and with the aid of upslope flow.

    Additional rainfall totals of 2 to 3 inches will be possible
    locally through this evening where any repeating cell-activity
    occurs, and this will continue to favor a likelihood for scattered
    areas of flash flooding. This will include localized burn scar
    impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4Ss8JmzyebEdu7vaw0Og0C1U3OsLnYIXxOKcMGCcFvSqz8Dn3Lw3KvJBnUbuRUa1EEzk= tOxO41DYm0PQsL9OYApTu4I$ for graphic product...

    ATTN...WFO...HNX...REV...STO...VEF...

    ATTN...RFC...RSA...NWC...

    LAT...LON 40931974 40431929 39481892 38041865 36691819=20
    36621906 37612001 39382058 40132048 40802021=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 Aug 24 01:21:38 2025
    AWUS01 KWNH 240121
    FFGMPD
    SCZ000-GAZ000-240720-

    Mesoscale Precipitation Discussion 0989
    NWS Weather Prediction Center College Park MD
    920 PM EDT Sat Aug 23 2025

    Areas affected...Coastal SC/GA

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

    Valid 240120Z - 240720Z

    SUMMARY...New bands of heavy showers and a few thunderstorms may
    focus along coastal areas of SC and GA overnight bringing a new
    threat of flash flooding.

    DISCUSSION...The early to mid-evening satellite imagery along with
    surface data shows an area of low pressure beginning to take shape
    along a frontal zone just off the SC/GA coast. This area of low
    pressure is forecast tonight to gradually lift off to the
    northeast, but be not far offshore of the SC Lowcountry. The
    latest suite of guidance including the evening runs of the
    experimental WoFS suggest the low center becoming better defined
    and strengthening a tad along the front which should facilitate an
    increase in low-level moisture convergence back into the coastal
    areas of SC and GA.

    An instability gradient along with an inverted surface trough is
    already noted along the coast, and radar imagery is showing a new
    band of warm-topped convection advancing westward back into some
    of the coastal areas of the SC Lowcountry, with some separate
    slow-moving cells over far eastern GA.

    The recent runs of the WoFS have been trending toward somewhat
    greater concentrations of warm-topped convection along the coast
    over the next several hours with a trend toward somewhat heavier
    rainfall totals. Some of the recent HRRR guidance has also
    exhibited a similar trend.

    Given the highly tropical environment with PWs of 2.2 to 2.4
    inches, the rainfall will be very efficient with some of these
    warm-topped convective bands capable of rates reaching 2+
    inches/hour. A localized concern for cell-training will exist as
    well, and thus some additional rainfall totals of as much as 3 to
    5 inches cannot be ruled out overnight right along the immediate
    coast.

    Additional areas of flash flooding for the coastal communities
    will be possible as a result, and especially with the already
    saturated soil conditions and concerns locally with tidal
    flooding/inundation.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9HzLpxUO0IxceXLcfcnt7amZjmOh1qKtuez0yQTIQNUQko5TWlf18JVHM8cOOXDcsunp= 2N3ZPXxhKPjI7c5qCDhQv_c$ for graphic product...

    ATTN...WFO...CHS...ILM...JAX...

    ATTN...RFC...ALR...NWC...

    LAT...LON 33677907 33457879 32867953 32278038 31478102=20
    30948124 30958159 31508155 32318107 33118012=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 Aug 24 18:42:59 2025
    AWUS01 KWNH 241842
    FFGMPD
    COZ000-UTZ000-250041-

    Mesoscale Precipitation Discussion 0990
    NWS Weather Prediction Center College Park MD
    242 PM EDT Sun Aug 24 2025

    Areas affected...eastern Utah, western Colorado

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

    Valid 241841Z - 250041Z

    Summary...Robust convective development is occurring ahead of a
    weak disturbance over northeastern Utah. Areas of rain rates
    reaching 1 inch/hr are possible. Flash flooding could occur -
    especially near burn scars and other low-lying, sensitive areas.

    Discussion...Recent radar/satellite imagery depicts a localized
    areas of robust thunderstorm development near/just south of
    Meeker, CO. The storms are being supporting by 1) a quickly
    destabilizing airmass (around 1000 J/kg SBCAPE), 2) anomalously
    moist PW values (near 1 inch), and ascent from a weak mid-level
    disturbance over northeastern UT/southwestern WY. Mean wind
    fields aloft are fairly weak, allowing ongoing convection to
    exhibit only slow eastward motions. Meanwhile, ground conditions
    are supporting runoff with only 0.5-1.0 inch/hr FFG thresholds
    and, with burn scars noted across the region representing enhanced
    runoff potential.

    Most of the convection across the discussion area should be
    diurnally driven today. Convective coverage will continue to
    increase through peak heating hours, and slow movement/cell
    mergers should all support local FFG exceedance/1 inch/hr rain
    rates at times beneath the deepest convection. The flash flood
    risk should be highest near burn scars and
    low-lying/terrain-favored areas. Flash flood potential should
    persist through at least 00Z/6p MDT this evening on an isolated
    basis.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-XgB761n-7HR79fQWmNLHDJ5Tt41fnz3IYepC3Bp4ZcpBm6IeBn7hq9Bh296IYQQiH2E= 1JfK9kXDWOLKE7BDM3Z9Sic$ for graphic product...

    ATTN...WFO...BOU...GJT...PUB...SLC...

    ATTN...RFC...FWR...KRF...STR...TUA...NWC...

    LAT...LON 40670853 40630674 39770585 38630573 37630593=20
    37090752 37291008 38661082 40160981=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 24 19:00:48 2025
    AWUS01 KWNH 241900
    FFGMPD
    NVZ000-CAZ000-250100-

    Mesoscale Precipitation Discussion 0991
    NWS Weather Prediction Center College Park MD
    300 PM EDT Sun Aug 24 2025

    Areas affected...Sierra Nevada...Western Nevada

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

    Valid 241900Z - 250100Z

    SUMMARY...Deep layer monsoonal moisture entrenched across large
    areas of the Southwest and into the Great Basin will favor showers
    and thunderstorms through this afternoon with locally high
    rainfall rates. Scattered areas of flash flooding will be likely
    which include potential impacts to burn scar locations.

    DISCUSSION...The deeper layer subtropical ridge near the Four
    Corners region remains in a conducive position to drive and
    sustain the transport of monsoonal moisture up across southern and
    eastern CA including the Sierra Nevada and adjacent areas of the
    Great Basin. The latest CIRA-ALPW data shows moisture near or
    above the 90th percentile of climatology in the 700/500 mb and
    500/300 mb layers respectively, with the 12Z RAOB sounding at KREV
    (Reno, NV) showing an impressive PW of 0.98 which is near a record
    for the date.

    This moisture coupled with placement of mid-level vort energy near
    the western foothills of the central Sierra Nevada and modest
    deeper upslope flow over the higher terrain will combine with
    increasing boundary layer instability for scattered to eventually
    broken areas of heavy shower and thunderstorm activity once again
    for this afternoon. The latest GOES-W Day Cloud Phase RGB
    satellite imagery along with LightningCast data suggests CI
    (convective initiation) is imminent along the terrain of the
    Sierra Nevada.

    Convection is also expected to develop farther east across the
    plateau areas of western NV to the east of the terrain where there
    will also be a combination of orographics and diurnal heating
    within this very moist monsoon pattern to support locally heavy
    showers and thunderstorms.

    Given the high moisture environment, rainfall rates up to 1.5
    inches/hour will be possible, with some localized storm total
    amounts by late this afternoon of 2 to 4 inches possible where any
    cells tend to become more terrain-focused. Scattered areas of
    flash flooding are likely going through this afternoon, and there
    will be localized concerns for burn scar impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-chfZMgdqkkHXqNCzQafAo4wMaeKktUOQSGJ94k_fUZxLvJ6v_f_0PN5-O35REqj2g3Z= 3K0HPjRbfnc9Teb1D9pZIP4$ for graphic product...

    ATTN...WFO...HNX...LKN...MFR...REV...STO...VEF...

    ATTN...RFC...RSA...NWC...

    LAT...LON 41782021 41451909 40421804 39771769 38961699=20
    37921676 37261712 36391738 35751751 35501782=20
    35421828 35891866 36621899 37781987 38842074=20
    40212148 41362128=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 24 19:04:49 2025
    AWUS01 KWNH 241904
    FFGMPD
    AZZ000-UTZ000-NVZ000-250103-

    Mesoscale Precipitation Discussion 0992
    NWS Weather Prediction Center College Park MD
    304 PM EDT Sun Aug 24 2025

    Areas affected...northwestern Arizona, southern Utah, and
    southeastern Nevada

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

    Valid 241903Z - 250103Z

    Summary...Scattered thunderstorms are quickly expanding in
    coverage across the Colorado River Valley and vicinity. The
    storms are in a favorable environment for localized rain rates
    exceeding 1 inch per hour. Flash flooding is likely - especially
    in terrain-favored areas and near burn scars.

    Discussion...Recent satellite/lightning data indicates a distinct
    increase in convective activity across terrain-favored ridgelines
    in northwestern Arizona and south-central Utah over the past hour.
    The storms are forming in response to 1) strong
    insolation/destabilization across the area, with MLCAPE values
    exceeding 1000 J/kg, 2) anomalously high moisture content (PW
    values as high as 1.4 inch), and 3) very subtle mid-level
    vorticity maxima rotating northward along the western periphery of
    a stout mid/upper ridge near the Four Corners region. Wind fields
    aloft were strong enough to favor slow northward storm motions
    (around 10-15 knots). Despite these storm motions, localized
    backbuilding (evident per radar/MRMS) and overall convective
    intensity has still supported local instances of rain rates
    reaching 1 inch/hr at times.

    These rain rates should occur across locally sensitive ground
    conditions resulting from several burn scars. Slot canyons in
    southern Utah and vicinity area also at risk of locally heavy rain
    rates. As convection continues to mature and expand in coverage,
    several instances of flash flooding are expected.

    Most of the convection should be diurnally driven, with model
    guidance suggestive of flash flood potential existing through at
    least 01Z/7p MDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4wTGC0DCHOW0D4pa35mAoBzjW8mKtcs0Th9B2gQwnpoNKsxWRuOw_12vfU808w1DB7Bn= yG5SPS2Y4ZHnRRycX2nSfXw$ for graphic product...

    ATTN...WFO...FGZ...GJT...LKN...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 39581229 39111117 37681086 37011072 35701114=20
    34911127 34151232 34631405 35071456 36321543=20
    37901527 39131400=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 24 19:45:50 2025
    AWUS01 KWNH 241945
    FFGMPD
    COZ000-NMZ000-AZZ000-250045-

    Mesoscale Precipitation Discussion 0993
    NWS Weather Prediction Center College Park MD
    345 PM EDT Sun Aug 24 2025

    Areas affected...Southern CO...Northern NM

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

    Valid 241945Z - 250045Z

    SUMMARY...Heavy showers and thunderstorms developing and expanding
    in coverage across southern CO and northern NM will pose a threat
    for isolated to scattered areas of flash flooding going into the
    early evening hours. The area burn scar locations and normally dry
    washes will be most susceptible to impacts.

    DISCUSSION...Convective initiation is well underway across the
    high country of southern CO and down into northern NM, with
    locally heavy shower and thunderstorm activity in particular
    beginning to focus over and near the Sangre De Cristo Range.

    MLCAPE values along the CO/NM border have locally increased to
    over 1000 J/kg and this coupled with deeper layer concentrations
    of monsoonal moisture and orographic ascent near the terrain
    should favor an additional expansion of convection over the next
    several hours.

    Facilitating some of the convective potential today will also be
    proximity of a well-defined mid-level vort center over northwest
    NM which should drift slowly off to the east over the next several
    hours. This energy coupled with the orographic nature of the
    convection may foster some smaller scale enhancement to the
    convection with locally enhanced rainfall totals.

    Rainfall rates of as much as 1 to 2 inches/hour are generally
    expected with the stronger convective cells, and with relatively
    slow cell-motions, there may be some totals by early this evening
    of 2 to 3+ inches. These rains will foster concerns for isolated
    to scattered areas of flash flooding, and primarily involving the
    more sensitive burn scar locations and normally dry washes.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9yF0FLyYFMlGe97an5m30LV4NHo2pw7X0zCWYuwPoVYlwxEIbZOU85ttYZTOBB_Jz9HO= d7bpl-XUAotofkyvlHriDSQ$ for graphic product...

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

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 38140516 37750444 36600454 35370516 34920608=20
    34830704 34960828 35360889 35850909 36620910=20
    36960875 37070724 37490622 37800571=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 24 22:56:21 2025
    AWUS01 KWNH 242256
    FFGMPD
    NYZ000-PAZ000-250345-

    Mesoscale Precipitation Discussion 0994
    NWS Weather Prediction Center College Park MD
    655 PM EDT Sun Aug 24 2025

    Areas affected...Northern PA...Southern and Central NY

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

    Valid 242255Z - 250345Z

    SUMMARY...A few bands of heavy showers and thunderstorms may be
    capable of locally training over the same area this evening. This
    coupled with high rainfall rates may yield at least an isolated
    threat of flash flooding.

    DISCUSSION...The latest surface analysis shows a cold front
    gradually making progress into the northern Mid-Atlantic and
    Northeast as an upper-level trough digs across the Great Lakes and
    OH Valley. The airmass ahead of this cold front is moderately
    unstable with MLCAPE values of 1000 to 1500 J/kg, and is
    seasonably moist with PWs of 1.3 to 1.5 inches.

    This coupled with some relatively strong moisture convergence
    along the front and favorable upper-level forcing/divergence
    should support multiple bands of rather heavy showers and
    thunderstorms across portions of northern PA through southern and
    central NY through this evening.

    Radar imagery already shows a couple of linearly oriented bands
    showing some organization and exhibiting some cell-training
    characteristics across portions of southern NY. There is some
    modest effective bulk shear in place that should tend to favor at
    least some broken multicell bands of convection through
    mid-evening until the cold front can advance more progressively
    through the area.

    Rainfall rates with the current activity are locally on the order
    of 1 to 2 inches/hour, and the 18Z HREF along with recent HRRR
    solutions suggest sufficient levels of cell-training to foster
    some 2 to 4 inch rainfall totals through mid-evening.

    These rains will foster concerns for some isolated areas of flash
    flooding as a result.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_W973_JMzr2W0xBo715b_hikk-hyKh6CcxGc2m1_OC5nL1xIT36LS76A2Q2lnV0tdW4B= rHoSgkGnels1PH3gjGQ9C4A$ for graphic product...

    ATTN...WFO...ALY...BGM...BTV...BUF...CTP...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 43927422 43557384 42897442 42077568 41567649=20
    41307740 41597771 42607664 43777503=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 24 23:51:23 2025
    AWUS01 KWNH 242351
    FFGMPD
    TXZ000-OKZ000-KSZ000-COZ000-NMZ000-250550-

    Mesoscale Precipitation Discussion 0995
    NWS Weather Prediction Center College Park MD
    750 PM EDT Sun Aug 24 2025

    Areas affected...Central to Southeast CO...Far Northeast
    NM...Southwest KS...OK/TX Panhandles

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

    Valid 242350Z - 250550Z

    SUMMARY...Clusters of heavy showers and thunderstorms will likely
    grow upscale with time this evening across portions of the central
    High Plains. Cell-merger activity and locally high rainfall rates
    will pose a threat for isolated to scattered areas of flash
    flooding.

    DISCUSSION...The late-day GOES-E IR satellite imagery shows
    clusters of cold-topped convection continuing to evolve over
    central to southeast CO and down through far northeast NM as
    moist/convergent and unstable low-level flow focuses along a
    quasi-stationary front draped from the OK/TX Panhandles
    northwestward into the eastern slopes of the central Rockies.

    MLCAPE values along the front are as high as 1500 to 2500 J/kg
    with locally 50+ kts of effective bulk shear in place helping to
    favor concentrations of multicell and supercell convection. The
    airmass is anomalously moist with at least some of the mid and
    high-level monsoonal moisture over the Southwest advancing east
    around the north side of the Four Corners subtropical ridge axis.
    This is helping to favor PW anomalies of 2+ standard deviations
    above normal.

    Weak embedded shortwave energy within the mid-level west-northwest
    flow over the central Rockies will eject east-southeast across
    eastern CO and eventually portions of southwest KS and the OK/TX
    Panhandles going into the overnight hours. This energy interacting
    with the favorable thermodynamic environment and the front should
    support an upscale grow of convection with time across the central
    High Plains.

    The experimental WoFS guidance along with the 18Z HREF suggest
    areas of southeast CO and eventually portions of the OK/TX
    Panhandles will tend to be the primary focus for more organized
    convection and heavier rainfall totals at least through the
    midnight time frame. This is also in close proximity to where
    stronger frontal convergence and greater instability will be.

    Rainfall rates of up to 2 inches/hour are expected with the
    stronger supercell mode convective cells and with any cell-mergers
    that occur over the next several hours. Going through midnight,
    the high rainfall rates and localized cell-mergers may foster some
    rainfall amounts of 3 to 4+ inches. This will drive a threat for
    isolated to scattered areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7OTY4HD50DL9C6HFPDpsl9dpddL-qCaVcc7ujN4BmCefqLcx4rQGMoFQJltemQhek4ti= vqeT2EsyxZpbqkmzCTFAfFk$ for graphic product...

    ATTN...WFO...ABQ...AMA...BOU...DDC...GLD...OUN...PUB...

    ATTN...RFC...FWR...KRF...TUA...NWC...

    LAT...LON 39690506 39580366 38720198 37800069 36409907=20
    35389969 35480177 36530430 37810555 39140571=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 Aug 25 00:32:53 2025
    AWUS01 KWNH 250032
    FFGMPD
    NVZ000-CAZ000-ORZ000-250600-

    Mesoscale Precipitation Discussion 0996
    NWS Weather Prediction Center College Park MD
    831 PM EDT Sun Aug 24 2025

    Areas affected...Sierra Nevada...Western and Central NV

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

    Valid 250030Z - 250600Z

    SUMMARY...Monsoonal showers and thunderstorms will continue
    through the evening hours across the Sierra Nevada and portions of
    the Great Basin. Additional areas of flash flooding will still be
    likely with localized burn scar impacts still a concern over the
    next few hours.

    DISCUSSION...The late-day visible satellite imagery shows an
    expansive area of monsoonal showers and thunderstorms impacting
    the Sierra Nevada and interior portions of the Great Basin
    including central and western NV.

    A fair amount of surface-based instability remains in place across
    central NV in particular, with an axis of instability extending
    westward back into the northern Sierra Nevada. SBCAPE values are
    on the order of 1000 to 2000+ J/kg, and there are some 3-hour
    SBCAPE differentials across central NV of +800 to +1000 J/kg which
    suggests that there are corridors of untapped instability that
    will help sustain the ongoing convective threat for at least a few
    more hours.

    Deep monsoonal moisture remains in place as evidenced by the
    latest CIRA-ALPW data which shows significant concentrations of
    moisture in the mid to upper levels of the vertical column. The
    00Z RAOB sounding from KREV depicted a PW of 0.96 which is again
    near a daily record.

    This moisture and instability coupled with upslope flow into the
    terrain along with localized outflow boundary collisions over the
    plateau areas of central and western NV favor clusters of
    monsoonal convection persisting through the evening hours.

    Given the high moisture environment, rainfall rates up to 1.5
    inches/hour will still be possible, with some additional isolated
    rainfall amounts of 2 to 3 inches possible which is supported by
    recent runs of the experimental WoFS guidance. Generally these
    additional rains are likely to foster some additional scattered
    areas of flash flooding over the next few hours, and there will
    continue to be concerns for localized burn scar impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6nixlvhIh_I9jdS5427KRxaRq7kuX1VCkuKYunDEDak_uiH_xxLUbjJCLFgMieSFnEYN= fADW2bw8vIMgwXfOvgvT0Sk$ for graphic product...

    ATTN...WFO...EKA...HNX...LKN...MFR...REV...STO...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 42022197 41862065 40971920 40761788 40971643=20
    40831473 40151416 39351460 38141624 37101747=20
    36721851 37021921 37641975 38442030 39622075=20
    39862096 40302126 40892193 41132253 41122298=20
    41502321 41922278=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 25 01:01:25 2025
    AWUS01 KWNH 250101
    FFGMPD
    AZZ000-UTZ000-NVZ000-250600-

    Mesoscale Precipitation Discussion 0997
    NWS Weather Prediction Center College Park MD
    900 PM EDT Sun Aug 24 2025

    Areas affected...Southern UT...Central and Northern AZ

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

    Valid 250100Z - 250600Z

    SUMMARY...Additional scattered areas of flash flooding will remain
    possible going through the evening hours from clusters of
    monsoonal showers and thunderstorms.

    DISCUSSION...The late-day GOES-W IR satellite imagery in
    conjunction with radar continues to show broken clusters of
    monsoonal showers and thunderstorms impacting portions of central
    and northern AZ and southern UT. The activity continues to be
    embedded within a moist and unstable airmass being facilitated by
    the synoptic scale monsoon pattern across the Southwest.

    There are still some pockets of untapped instability locally over
    northwest AZ and southern UT with some MLCAPE values of 1000+ J/kg
    noted. However, the region is gradually being convectively
    overturned, and this should support a gradual downward trend in
    the coverage and intensity of convection by later this evening.
    This is also being advertised by recent runs of the experimental
    WoFS and the broader hires model consensus.

    Regardless, the ongoing clusters of convection will still be
    capable of producing heavy rainfall rates of up to 1.5 inches/hour
    over the next few hours, with some additional spotty amounts of up
    to 2 inches going through late this evening.

    Some additional scattered areas of flash flooding will be
    possible, and this will include localized impacts potentially to
    the slot canyon areas of southern UT and some of the sensitive
    burn scar areas over central and especially northern AZ. Some of
    the normally dry washes may also be affected by suddenly rising
    flood waters.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9BwtiKiUnflZXZN7PlKn3_pBaT2_EzRGHlrgjSEDeoAwPsH80DYOET-_Z8I1TDLToz0I= _HrCA4MMvs-JcRd1ZFhLkf4$ for graphic product...

    ATTN...WFO...FGZ...GJT...PSR...SLC...VEF...

    ATTN...RFC...STR...NWC...

    LAT...LON 38371264 38371099 37450984 36150943 34330968=20
    33321093 33291241 33791347 34691396 35861411=20
    36771404 37991351=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 25 06:37:01 2025
    AWUS01 KWNH 250636
    FFGMPD
    TXZ000-OKZ000-KSZ000-NEZ000-COZ000-251200-

    Mesoscale Precipitation Discussion 0998
    NWS Weather Prediction Center College Park MD
    235 AM EDT Mon Aug 25 2025

    Areas affected...much of west-central KS into adjacent portions of
    CO/NE/OK

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

    Valid 250635Z - 251200Z

    Summary...Training showers and thunderstorms likely to result in
    localized 3"+ rainfall totals, isolated to scattered instances of
    flash flooding.

    Discussion...Convection has proliferated over the past couple of
    hours across portions of the western Central Plains, tapping into
    elevated instability with cloud bases in the vicinity of 850-700
    mb. While MUCAPE generally ranges from 250-750 J/kg (per SPC
    mesoanalysis), there is likely compensation from slantwise
    instability as isentropic upglide along the 305K surface has
    increased significantly with the veering low-level jet over the
    past several hours (with southwesterly flow of 15-20 kts becoming
    oriented perpendicular to isobars). The mesoscale environment is
    otherwise characterized highly anomalous tropospheric moisture
    content (PWs of 1.3-1.8 inches, between the 90th percentile and
    max moving average, per LBF and DDC sounding climatology) and deep
    layer (0-6 km) shear of 20-40 kts (on the periphery of the
    right-entrance region of a ~120 kt jet streak over the Mid-MS
    Valley within northwest flow and embedded shortwave/vorticity
    maxima in the mid-levels).

    While soils are relatively dry across the region (per NASA
    SPoRT-LIS soil moisture in the 0-1m layer generally at or below
    the 10th percentile), too much rainfall too quickly could lead to
    instances of flash flooding through the overnight. Localized
    training and repeating of cells are possible across all of the
    highlighted region, as northwest flow directs backbuilding
    convection from northwest to southeast over many of the same
    localities. Hi-res models (00z HREF suite) indicate the greatest
    odds for localized 3"+ totals (40-km neighborhood probs for 3"
    exceedance of 40-60%) in the vicinity of Dodge City, KS and points
    east and southeast, where instability is maximized (MUCAPE 500+
    J/kg) and the greatest coverage of convective cells are already
    occurring. As 6-hr FFGs (Flash Flood Guidance) are locally as low
    as 2.0" in this area (with the bulk of the region near or below
    3.0"), isolated to scattered instances of flash flooding are
    considered likely.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6WaEPkqWcssgTag046hZMqGzfOjbjyU1C1Ax20MiPM3m1rQNZ-pHqKdQG1Rn3OtPODel= kjcoDmvtb5ZAtcotb9dM9JM$ for graphic product...

    ATTN...WFO...AMA...BOU...DDC...GID...GLD...ICT...LBF...OUN...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 40640209 40520109 40000016 39239901 38059828=20
    37039741 36169756 35949847 36169951 36580016=20
    37260083 38480145 39160248 39660322 40110344=20
    40500323=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 25 17:25:34 2025
    AWUS01 KWNH 251725
    FFGMPD
    AZZ000-CAZ000-252330-

    Mesoscale Precipitation Discussion 0999
    NWS Weather Prediction Center College Park MD
    124 PM EDT Mon Aug 25 2025

    Areas affected...Southern Arizona...

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

    Valid 251730Z - 252330Z

    SUMMARY...Monsoon convection with rates up to 2"/hr. Localized
    1.5-2.5" pose possible widely-scattered localized flash flooding.

    DISCUSSION...A compact but atypically strong retrograding
    shortwave can be seen well in composite RADAR mosaic near Blythe
    starting to turn more northerly across the Lower Colorado Valley.
    The associated debris clouds will hamper insolation to build
    instability, however, the upwind areas over the Sonoran Desert has
    received solid insolation with anomalous moisture remaining across
    southern AZ. Surface Tds in the low to mid-60s combined with core
    of CIRA LPW up to 700mb, extends through much of southern AZ as
    well, with only mid-level drying at 700-500mb layer directly south
    of the boarder; providing enhanced buoyancy with CAPEs already
    building over 2000 J/kg, on their way to 2500-3000 J/kg with
    limited capping. Total PWats of 1.75" are above normal, about
    1.5-2 standard anomalies and being loaded mainly near cloud base
    (and below) should allow for solid efficiency.

    GOES Visible imagery shows, low level convergence along the upwind
    edge of outer band of the MCV is producing thunderstorms, that had
    been weaker, but with influx of increasingly unstable air from the
    desert, are starting to deepen and broaden. Low level flow is
    still responding to the exiting MCV and broader upglide into the
    strong divergence aloft from the expanding right entrance to the
    50+kt 3H jet streak across S NV/SE CA, as such, back-building
    (upwind propagation) may maintain for a few more hours allowing
    for effective slow cell motions increasing totals up to 2".

    Through the late morning/early afternoon, as the MCV exits, winds
    are expected to further strengthen with westerly upslope
    components across southeast AZ terrain across Cochise, SE Pima and
    S Graham counties. Vigor of low level upslope is likely to
    significantly increase toward/after 21z, with 15-20kts of westerly
    flow at 850mb. Peak heating/updraft strength and flux into the
    terrain, rates should increase to 1.5"/hr with some 2"/hr rates
    peaking toward 22-00z. Probabilities/Hi-Res CAM suite suggest
    best overall cells are likely to be along and just north of the
    US/Mexico border with a spot or two of 1.5-2.5" totals. With a
    bulk of the rain occurring in sub-hourly bursts and hard ground
    conditions, increased run-off suggest widely-scattered incidents
    of flash flooding are possible into the early evening.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8HObKstHlnYfdGf5gVZMB6GcnHye6stn_-6pmLbaY-nN5YWhtre8o-uGlFf4ohSB6T2g= -royNrvDuHby_XxCYQO3TgU$ for graphic product...

    ATTN...WFO...PSR...TWC...

    ATTN...RFC...STR...NWC...

    LAT...LON 33981380 33801324 33001185 33221030 32611001=20
    31641000 31251023 31231108 31591220 31871308=20
    32511428 32941465 33401478 33821434=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 25 19:41:36 2025
    AWUS01 KWNH 251941
    FFGMPD
    COZ000-NMZ000-WYZ000-AZZ000-UTZ000-260140-

    Mesoscale Precipitation Discussion 1000
    NWS Weather Prediction Center College Park MD
    340 PM EDT Mon Aug 25 2025

    Areas affected...Central and Southern CO...Northern and Central
    NM...Far Northeast AZ...Far Southeast UT

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

    Valid 251940Z - 260140Z

    SUMMARY...Showers and thunderstorms will develop and expand in
    coverage going through the afternoon hours over portions of the
    central Rockies and adjacent areas of the CO/NM High Plains.
    Scattered areas of flash flooding are likely.

    DISCUSSION...The midday GOES-E visible satellite imagery shows
    convective initiation well underway across portions of central and
    southern CO down through areas of northern and central NM. Strong
    diurnal heating continues to foster the build-up of surface-based
    instability which is resulting in the development of differential
    heating boundaries and terrain-focused circulations.

    MLCAPE values have already risen to 500 to 1000+ J/kg with a
    rather moist environment characterized by PWs of 1.5+ standard
    deviations above normal. This coupled with the aforementioned
    orographics and arrival of weak mid-level vort energy embedded
    within the deeper layer west-northwest flow aloft should favor a
    notable expansion of convection over the next several hours across
    the higher terrain and also into adjacent areas of the High Plains.

    Moist and increasingly unstable low-level upslope flow along with
    focused convergence along a stationary front near the Front Range
    on down to the eastern slopes of the Sangre De Cristo Range will
    be a key facilitator for convection across these areas to become
    locally focused by later this afternoon. In fact, surface dew
    points across eastern CO and northeast NM range from the mid 50s
    to the low 60s, and this moisture along with the deep layer
    environment should foster convection with efficiently high
    rainfall rates that may reach 2+ inches/hour. Localized upslope
    flow over the terrain will also support these high rainfall rates.

    Going through late this afternoon, expect sufficient convective
    organization for some rainfall totals to reach as high as 2 to 4
    inches. These rains will drive an elevated threat for at least
    scattered areas of flash flooding which will include concerns for
    localized burn scar impacts. Some areas of southern CO and
    northern NM have been rather wet recently, and these antecedent
    conditions may favor locally enhanced runoff concerns.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4imk3B1q2LkgxPhHbP_G6Lq9LdWhlXOgeAxE71DECaxWVS4BJp7kP9srfpHaRvQwoYo-= DK27J_cuucVLbj-t9mbSbb8$ for graphic product...

    ATTN...WFO...ABQ...BOU...CYS...FGZ...GJT...PUB...

    ATTN...RFC...FWR...KRF...STR...TUA...NWC...

    LAT...LON 41120512 40740404 39590339 37750353 35990400=20
    34980485 34550592 34440713 34700835 35410926=20
    36590984 37800959 38210835 38200663 39160585=20
    40750593=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 25 20:09:37 2025
    AWUS01 KWNH 252009
    FFGMPD
    NVZ000-CAZ000-260208-

    Mesoscale Precipitation Discussion 1001
    NWS Weather Prediction Center College Park MD
    408 PM EDT Mon Aug 25 2025

    Areas affected...Sierra Nevada...Southern CA

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

    Valid 252008Z - 260208Z

    SUMMARY...Scattered thunderstorms with heavy rainfall rates are
    likely through this afternoon across portions of the Peninsular
    Range of southern CA, and also into the central and southern
    Sierra Nevada. Scattered areas of flash flooding are likely, and
    this may include a threat for burn scar flash flooding and debris
    flow activity.

    DISCUSSION...The early afternoon GOES-W Day Cloud Phase RGB
    satellite imagery shows convective initiation underway across the
    higher terrain of the Peninsular Range of southern CA and also up
    across the central and southern Sierra Nevada. Daytime heating and
    the build of surface-based instability along and adjacent the
    terrain is fostering favorable differential heating boundary and terrain-enhanced circulations/ascent for convection which should
    generally expand in coverage over the next several hours.

    Monsoonal moisture remains quite prevalent and especially in the
    850/500 mb layer based on the latest CIRA-ALPW data. This is
    helping to drive PW anomalies again that are 1.5 to 2.5 standard
    deviations above normal. This moisture along with the increasing
    instability and orographic footprint of the convection should
    yield rainfall rates this afternoon reaching as high as 1.5 to 2
    inches/hour, with some of the heaviest rates probably focused over
    the Peninsular Range of southern CA where moisture here is a tad
    deeper (noting the 500/300 mb layer) relative to areas farther
    north. Also, there is some very moist low-level southeast flow off
    of the northern Gulf of California playing a role here in driving
    greater nearby instability.

    The convection today should again follow the diurnal heating
    cycle, and by late today, some spotty rainfall amounts of 2 to 4
    inches will be possible. This is supported locally by the latest
    experimental WoFS guidance, and especially over the Peninsular
    Range. Given the sensitivities with localized burn scar areas and
    the rugged terrain in general, scattered areas of flash flooding
    are likely. Some debris flow activity will be possible where any
    burn scar flash flooding occurs.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4ndsX6KA9fEXjpy0wdelhQQz5tqrzimNfEaoVjf97bEyQm3PQrit_tXPEeD8qz5kZXqZ= mrIcsIrA4pRFv1MUuipHEN0$ for graphic product...

    ATTN...WFO...HNX...LOX...PSR...REV...SGX...STO...VEF...

    ATTN...RFC...RSA...NWC...

    LAT...LON 39441960 38271829 36641772 35181763 34091633=20
    32511581 32361649 33041699 33451730 34271799=20
    34491839 34811881 34981884 35391887 36041883=20
    36871906 37631967 38742031 39392040=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Aug 25 20:37:37 2025
    AWUS01 KWNH 252037
    FFGMPD
    AZZ000-UTZ000-NVZ000-260235-

    Mesoscale Precipitation Discussion 1002
    NWS Weather Prediction Center College Park MD
    436 PM EDT Mon Aug 25 2025

    Areas affected...Southern NV...Southern UT...Central and Northern
    AZ

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

    Valid 252035Z - 260235Z

    SUMMARY...Monsoonal showers and thunderstorms will continue to
    develop and locally expand in coverage over the next several
    hours. Mainly isolated areas of flash flooding will be possible.

    DISCUSSION...The early afternoon GOES-W visible satellite imagery
    shows monsoonal shower and thunderstorm activity initiating and
    expanding in coverage across northern AZ into southern NV and
    southern UT. MLCAPE values have increased to as much as 1000+ J/kg
    and the PW environment remains quite moist with values running 1
    to 2 standard deviations above normal.

    An additional uptick in instability is expected over the next few
    hours which should work in tandem with orographics to drive an
    increase in the coverage of showers and thunderstorms. The
    convection will be capable of producing high rainfall rates of up
    to 1.5 inches/hour.

    The latest RAP guidance shows an increasing amount of mid-level
    southeast flow over central to northwest AZ and by later today
    around the western flank of the mid-level subtropical ridge/high
    centered along the AZ/NM border. Some effective bulk shear values
    may reach as high as 30 to 40+ kts which may support some
    organized convective structures in time that will further support
    high rainfall rates with enhanced updrafts, but also localized
    areas of convective sustenance/persistence near areas of higher
    terrain and including the Mogollon Rim.

    Some localized 2 to 3+ inch rainfall amounts will be possible, and
    this will favor a threat for at least isolated areas of flash
    flooding going through the afternoon and early evening hours. Slot
    canyon and burn scar flash flooding impacts will be associated
    with this threat.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_6UrYYzzMV4wXzh-OCvNO05LJPNUBUksnlOX0bw1zxCRsg4AfJSKHNEnulSQNpjlDCM5= EiiYIjgxBLjGSM_dBiDMrOw$ for graphic product...

    ATTN...WFO...FGZ...LKN...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 39131105 38541061 36681097 35611074 34901014=20
    34351027 34131095 34411197 35601347 36101538=20
    36681620 38001616 38711532 38911365 38781251=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 Aug 25 21:46:36 2025
    AWUS01 KWNH 252146
    FFGMPD
    AZZ000-CAZ000-260145-

    Mesoscale Precipitation Discussion 1003
    NWS Weather Prediction Center College Park MD
    545 PM EDT Mon Aug 25 2025

    Areas affected...Southern CA...Southwest to South-Central AZ

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

    Valid 252145Z - 260145Z

    SUMMARY...Locally very heavy monsoon-driven showers and
    thunderstorms are expected going through the remainder of the
    afternoon across southern CA into southwest and south-central AZ.
    Scattered areas of flash flooding are likely, some of which may be
    locally significant.

    DISCUSSION...The mid-afternoon GOES-W VIS/IR satellite imagery
    shows deepening and cooling convective tops across southeast CA
    and into adjacent areas of southern AZ where radar is confirming
    multiple concentrated bands of very heavy shower and thunderstorm
    activity.

    Mesoscale boundary forcings/interactions along with terrain
    influence and proximity of a very moist and unstable airmass is
    expected to drive corridors of additional convection with high
    rainfall rates going into the evening hours. MLCAPE values of 1500
    to 2500 J/kg are noted with recent CIN erosion helping to yield
    the recent uptick and organization of convection across southern
    CA and southern AZ. This includes the Peninsular Range and the
    adjacent deserts off to the east and south.

    Given the level of focused instability over the region with PWs
    reaching nearly 2.5 standard deviations above normal (with support
    from the very warm nearby Gulf of California), some rainfall rates
    may reach 2 to 2.5 inches/hour, with some spotty storm totals over
    the next few hours of 3 to 4+ inches. Recent WoFS guidance output
    suggests this potential, which will be aided by some localized
    cell-merger activity.

    Additional areas of flash flooding will be likely, some of which
    may be locally significant near areas of higher terrain and also
    for the dry wash/arroyo locations near and away from active areas
    of heavy shower and thunderstorm activity.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7vkAaj75rcrt-PIafMfdv1fVW3ZEAJXG763nWXhF9O2-b5Z22oJsCgvTPWRZV_AGO3EW= JGgmSXtpxO1OjwL-sJcN_vA$ for graphic product...

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

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 34681677 34481604 33611488 33431359 33201277=20
    33111094 32761015 31791014 31241072 31481240=20
    32001378 32321480 32411608 32861673 33841716=20
    34521716=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 26 01:11:09 2025
    AWUS01 KWNH 260111
    FFGMPD
    AZZ000-NVZ000-CAZ000-260600-

    Mesoscale Precipitation Discussion 1004
    NWS Weather Prediction Center College Park MD
    910 PM EDT Mon Aug 25 2025

    Areas affected...Southern and Eastern CA...Western and Southern AZ

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

    Valid 260110Z - 260600Z

    SUMMARY...Additional areas of flash flooding will be likely going
    through the evening hours across portions of southern and eastern
    CA through western and central AZ.

    DISCUSSION...The late-day GOES-W IR satellite imagery shows an
    extensive convective cloud canopy over areas of southern and
    eastern CA into western and central AZ. Very heavy showers and
    thunderstorms continue to locally percolate across the region in
    response to localized outflow boundary collisions and some
    orographically focused ascent.

    Diurnally driven instability continues to be gradually consumed
    via the process of convective overturning, but MLCAPE values
    remain locally over 1000 J/kg across some of the open desert areas
    of eastern CA and also through central AZ with much of this area
    so far escaping much of the convective activity.

    Recent runs of the experimental WoFS suggest some additional focus
    for mesoscale-driven shower and thunderstorm activity across
    central AZ in particular which may be aided by close proximity of
    some mid-level vort energy lifting northwestward out of the far
    northern Gulf of California.

    There is also a belt of relatively stronger effective bulk shear
    lifting up across southern and central AZ around the western side
    of the subtropical ridge off to the east. This shear and the
    lingering instability with generally moist deep layer southeast
    monsoonal flow will likely support convection lingering well into
    the evening.

    Rainfall rates will continue to be capable of reaching up to 1.5
    inches/hour with the stronger convective cores, with some
    additional spotty totals of 2 to 3 inches possible. The 90th
    percentile 6-hour QPF from 00Z WoFS supports this over parts of
    central and southwest AZ.

    This will continue to promote isolated to scattered areas of flash
    flooding through this evening before the convection gradually
    weakens. Any burn scar locations and the normally dry washes will
    continue to be most susceptible to impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9--6CKs_-_lYZCLU7KMZAHifHRWpc2GOFL6JGPBpgoiQTrScsha74K5421HW9LeKLvGB= wTnDG-GyDAvrDDq_Ybxelho$ for graphic product...

    ATTN...WFO...FGZ...HNX...LOX...PSR...SGX...TWC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 36671703 35421529 35601313 35541191 35241105=20
    34731033 33951015 33091063 32361180 32151283=20
    32281408 32571515 33061606 33641703 34921774=20
    36511781=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 26 01:59:12 2025
    AWUS01 KWNH 260159
    FFGMPD
    TXZ000-OKZ000-COZ000-NMZ000-260757-

    Mesoscale Precipitation Discussion 1005
    NWS Weather Prediction Center College Park MD
    957 PM EDT Mon Aug 25 2025

    Areas affected...Central and Southern CO...Central and Northern
    NM...TX Panhandle

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

    Valid 260157Z - 260757Z

    SUMMARY...Showers and thunderstorms will continue to develop and
    concentrate across portions of central and southern CO into
    northern and central NM. This will especially include the higher
    terrain of the Sangre De Cristo Range and adjacent areas of the
    High Plains. Scattered to numerous areas of flash flooding are
    expected tonight.

    DISCUSSION...The early evening GOES-E IR satellite imagery shows
    an expansive area of very cold-topped convection impacting areas
    of southern CO and especially central to northeast NM as heavy
    showers and thunderstorms interact with the higher terrain of the
    Sangre De Cristo Range along with favorable upslope flow.

    A corridor of MLCAPE values reaching 500 to 1000+ J/kg continue to
    be focused over north-central and northeast NM, with a separate
    axis of instability also still seen over parts of southeast CO.
    The environment remains very moist with PWs near 2 standard
    deviations above normal. This coupled with highly favorable
    orographic forcing/ascent and subtle mid-level vort energy
    dropping southeast across the central Rockies should favor
    additional concentrated areas of heavy showers and thunderstorms
    over the next several hours.

    The recent satellite and radar trends along with the last several
    runs of the experimental WoFS guidance would suggest northeast NM
    will be the primary focus for the heaviest rainfall amounts. This
    is where more favorable easterly low-level upslope flow into the
    terrain along with interaction with a stationary front will be
    noted. Greater instability in this area too should tend favor this
    area seeing the heaviest rainfall rates which is further supported
    by some of the very cold convective cloud tops currently over the
    region.

    Rainfall rates with the stronger storms may be capable of reaching
    2 inches/hour, and with the persistent upslope flow and frontal
    convergence, some additional rainfall totals of 3 to 5 inches will
    be possible. By later in the night, some of these heavier rains
    over northeast NM should begin to edge out into the TX Panhandle
    area which is strongly supported by the latest WoFS guidance.

    Scattered to numerous areas of flash flooding are generally
    expected, and especially over northeast NM where the heaviest
    totals should focus. Some locally significant impacts cannot be
    ruled out which may locally include sensitive burn scar locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!57uYAAIHBw_igN2z_cY9bvwL-kp0N83T1IorXzGeoUX7BSi49Mlolm9b_jQcNijREk9W= nSyuLqmd9TPFr_wfGMwHztk$ for graphic product...

    ATTN...WFO...ABQ...AMA...BOU...GJT...LUB...PUB...

    ATTN...RFC...FWR...KRF...STR...TUA...NWC...

    LAT...LON 39300478 38880387 38250352 36830313 36120235=20
    35730073 35120039 34490124 34360351 34060485=20
    34120636 34430722 35260750 36450676 37490671=20
    38540640 39150583=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 26 14:55:20 2025
    AWUS01 KWNH 261455
    FFGMPD
    CAZ000-261850-

    Mesoscale Precipitation Discussion 1006
    NWS Weather Prediction Center College Park MD
    1054 AM EDT Tue Aug 26 2025

    Areas affected...San Joaquin Valley into Sierra Nevada foothills

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

    Valid 261450Z - 261850Z

    SUMMARY...Slow moving thunderstorms will pose a threat for
    isolated flash flooding across portions of the San Joaquin Valley
    into the Sierra Nevada foothills over the next 2-4 hours. Rainfall
    rates of 1-2 in/hr will be possible.

    DISCUSSION...GOES West infrared satellite imagery and GLM data
    showed scattered thunderstorms expanding in coverage over the San
    Joaquin Valley and Sierra Nevada foothills as of 1430Z, within
    about 50 miles of Madera. Cells were located along a weak
    mid-level shear axis inferred on water vapor imagery, emanating
    from a vorticity maximum over west-central NV. The storms were
    likely elevated in nature, rooted just above 700 mb given RAP
    analysis point soundings, within a small region of weak
    instability ranging from 250 to just over 500 J/kg (via 14Z
    RAP/SPC mesoanalysis). Precipitable water values were very
    anomalous across central CA with standardized anomalies of 2 to 3+
    according to 12Z area soundings and short term GFS forecasts.

    With RAP-derived LFC-EL layer winds averaging near 5 kt, cell
    motions have been slow and MRMS-derived rainfall rates have been
    1-2 in/hr over portions of Fresno and Madera counties. Scattered
    thunderstorms are expected to continue over the next few hours but
    due to a lack of stronger winds aloft, storm organization should
    remain poor and new cell development will be aided by thunderstorm
    outflows. Localized flash flooding will remain possible over the
    next 2-4 hours. Trends will be monitored for updates as needed
    with the onset of better surface heating and turbulent mixing
    within the boundary layer potentially disrupting ongoing activity.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8sfJDnoD6T2oMTfFWM8mVKZEd0QpDHKC1kOgY7cujgR-4eFyevQO7XgMIUZFqEULC3Vx= CasgZXSdzkQ61BPG6-5h_Po$ for graphic product...

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

    ATTN...RFC...RSA...NWC...

    LAT...LON 38222076 37642001 37131943 36481908 36121922=20
    35971958 36071985 36692046 37222088 37862113=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 Aug 26 18:18:54 2025
    AWUS01 KWNH 261818
    FFGMPD
    NVZ000-CAZ000-270000-

    Mesoscale Precipitation Discussion 1007
    NWS Weather Prediction Center College Park MD
    218 PM EDT Tue Aug 26 2025

    Areas affected...eastern CA/western NV

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

    Valid 261816Z - 270000Z

    SUMMARY...Scattered thunderstorms are expected to develop along
    the Sierra Nevada through 21Z, some of which may produce flash
    flooding due to slow movement. Stronger cells will be capable of
    generating 1-2 in/hr rainfall rates.

    DISCUSSION...GOES West visible satellite imagery showed the
    development of cumulus and early stages of convective initiation
    along portions of the central and southern Sierra Nevada at 18Z.
    Despite some remnant cloud cover, the beginning of peak heating
    atop the elevated heat source was coinciding with anomalous
    tropospheric moisture (90th to 95th percentile for late August).
    The region of eastern CA/western NV was situated between a low to
    mid-level low offshore of the CA coast and low/trough extending
    from eastern OR into central NV. Between these two features was a
    section of relatively weak 0-6 km AGL layer winds of 5 to 10 kt
    which should contribute to slow storm motions.

    Continued heating should lead to the development of 500-1000 J/kg
    of instability across the region by mid-afternoon. Thunderstorm
    coverage will likely continue to expand over the next few hours
    with peak coverage in the 21-00Z time frame. Limited shear should
    keep storms disorganized in nature but slow movement and
    mesoscale/terrain interactions may allow for a few cells to
    exhibit little movement over the course of an hour or two before
    subsequent outflow initiates development downstream. Convection
    may move into valley locations later in the period. Due to the
    moist environment, rainfall rates of 1-2 in/hr (or less than an
    hour) will be possible. In addition to overlapping with locations
    that have received heavy rainfall over the past 3 days, these high
    rates will pose an increased flash flood threat along burn scars,
    urban locations or other areas of poor drainage, including the
    potential for debris flows in and around sensitive terrain.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!884UoJRx-SHbHd-iWAl7AZXOJzMYgmU3TEb-Ntl8fVjl7oR4HHAN4ovVHaZ-_dUkrmpl= eda8Wca-Of8dPpkj1yCR13o$ for graphic product...

    ATTN...WFO...HNX...REV...STO...VEF...

    ATTN...RFC...RSA...NWC...

    LAT...LON 39501976 39211916 38491843 37661772 36951705=20
    36151659 35671668 35441727 35421808 35571862=20
    36231878 36731900 37481984 38442031 39302048=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 Aug 26 18:39:22 2025
    AWUS01 KWNH 261839
    FFGMPD
    WYZ000-UTZ000-IDZ000-NVZ000-270030-

    Mesoscale Precipitation Discussion 1008
    NWS Weather Prediction Center College Park MD
    238 PM EDT Tue Aug 26 2025

    Areas affected...Southern ID...Northeast NV...Northern
    UT...Western WY...-

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

    Valid 261840Z - 270030Z

    SUMMARY...Highly anomalous moisture and strong dynamic forcing
    should allow for scattered to numerous thunderstorms capable of 1"
    rates & 1-2" localized totals. Favorable environment for
    redevelopment may allow for some repeating cells/tracks which will
    further enhance scattered incidents of flash flooding through
    evening.

    DISCUSSION...GOES WV mosaic suite depicts a very broad upper-level
    trough with some subtle WNW to SE negative tilting lifting
    northward across central NV with the core near central Nye county
    with broad downstream highly diffluent environment expanding
    across N NV, S ID into W WY/N UT providing areas of enhanced mid
    to upper-level cloudiness. This is greater near the core of the
    DPVA; allowing for better filtrated insolation further downstream
    across the ID/NV border, increasing heating. The bigger concern
    is seasonally near record moisture and flux streaming through the
    Great Basin, providing higher low level theta-E air with Tds in
    the mid to upper 50s in higher plateaus of NV and UT and even some
    low 60s near the southern portions of the Snake River Plain.=20
    While the filtered sunlight has some limitations for surface
    temperatures, the areas that have best clearing are already seeing
    convective development given limiting capping environments and
    strong DPVA and divergence aloft with large scale broad ascent
    pattern. MUCAPEs of 750-1250 J/kg have been increasing as the
    deep layer moisture reaches 1-1.25" total moisture (with a few 12z
    RAOBs breaking, or nearing daily record values). Surface to
    boundary layer moisture convergence is further enhanced near the
    clear skies of NE NV into SE ID and so convection is stronger
    there and downstream into S-central ID. Cores are likely to be
    narrow but increase in overall coverage allowing for some
    localized 1-1.5" totals in 30-90 minutes, as deep layer flow is
    generally weak support 5-10 kt cell motions and increased duration
    of moderate to heavy rainfall locally. As such scattered
    incidents of flash flooding are possible, particularly near burn
    scars.

    Through this evening, upper-level divergence further increases
    across NE NV into S ID, but along the eastern side of the
    circulation has increased convergence through depth with a smaller
    scale shortwave/vorticity center lifting northward along the
    central UT mountains. This shortwaves and interaction with
    outflow boundaries from initial cells will allow for secondary and
    perhaps tertiary development that may repeat. As such, the risk
    for heavy rainfall is likely to persist through much of the
    evening.


    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6NQydPb5XCTg83a4hfFgTuifh8rS1gvX42k7NT31o62I-SzZa5Me5zB78hdcQ5ZU-_B0= F1k--t3Mbad3rxec-6Kwcpo$ for graphic product...

    ATTN...WFO...BOI...LKN...PIH...RIW...SLC...

    ATTN...RFC...PTR...RSA...STR...NWC...

    LAT...LON 43931096 43581037 42781010 42071002 41241009=20
    40351032 38891133 38931209 39531217 40041231=20
    40811274 40961393 39961518 39871592 40361643=20
    42041699 43041689 43151684 43581620 43721511=20
    43591390 43541281 43701192=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 26 19:18:52 2025
    AWUS01 KWNH 261918
    FFGMPD
    NMZ000-AZZ000-UTZ000-NVZ000-270100-

    Mesoscale Precipitation Discussion 1009
    NWS Weather Prediction Center College Park MD
    318 PM EDT Tue Aug 26 2025

    Areas affected...Northern Arizona...Southern Utah...Extreme
    West-northwestern New Mexico...

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

    Valid 261920Z - 270100Z

    SUMMARY...Deep layer moist, confluent flow, and moderately
    unstable environment to support some repeating/training convective
    elements across dry/hard soils with localized 1-2" totals and
    possible flash flooding conditions through the evening hours.

    DISCUSSION...GOES WV mosaic depicts a well defined broad diffluent
    area across much of the northern Great Basin into the Rockies of
    WY/ID with core of weakly negatively tilted mid-level vorticity
    center in central NV angling into NW AZ. A convectively enhanced
    smaller scale shortwave is exiting southwest UT into central UT,
    lifting northward. The combination of the stronger height-falls
    has left the upstream areas within the southeast quadrant with
    above normal moisture flux out of the Sonoran Desert and across
    the San Francisco Plateau and across UT. Total PWat values of
    1-1.25" have expanded up through the valleys of Eastern and
    western UT and across N AZ mainly driven in the lowest layers with
    Tds as high as the low 60s at KPGA and CNY, similar to those more
    common along the Colorado River into SW UT (near KSGU) with all
    locations in the area of concern well above normal into the mid to
    upper 50s. In the wake of the height-falls and best divergence
    aloft, fairly clear skies have provided solid insolation to allow
    for increased surface heating and unstable environments support
    MUCAPEs of 1000 to 1500 J/kg (greater along the AZ/NM boarder)
    within the increasingly confluent streamwise flow. Convergence
    along the Mogollon Rim and Mountain/Valley circulations have seen
    numerous convective development areas across NW AZ, along the
    Mogollon Rim and into the enhanced unstable area along the AZ/NM
    border along and downstream of the San Francisco and Gallo Ranges.

    Given the flux convergence rates of 1-1.5"/hr are possible, though
    deep layer flow is stronger further south in the wake of the
    exiting waves, limiting duration. However, north-south confluence
    axes are likely to develop and will grant the best potential of
    1-2" totals due to short-term (1-2 hour) training or repeating
    through 3-5 hour periods. Hard/limited soil conditions with these
    rates suggest localized incidents of flash flooding are possible
    through the evening.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9hvKjIqfQ5nKLHMM2GpDRcLe5fNZJXYKSTRn-7OlVa4uX6aZ8D_bjfzdnRXR_C6F9poF= eAcnYrJLblRrXfkLhVKi3aY$ for graphic product...

    ATTN...WFO...ABQ...FGZ...GJT...SLC...VEF...

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 39080961 38600910 37050919 36420886 35990853=20
    35650797 34400788 33900843 33821029 34121183=20
    34271291 34901362 35671395 36881404 37931390=20
    38321304 38791089=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 26 20:17:25 2025
    AWUS01 KWNH 262017
    FFGMPD
    MTZ000-IDZ000-ORZ000-270200-

    Mesoscale Precipitation Discussion 1010
    NWS Weather Prediction Center College Park MD
    416 PM EDT Tue Aug 26 2025

    Areas affected...Central Idaho (Salmon River Range)

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

    Valid 262015Z - 270200Z

    SUMMARY...Increasing slow moving thunderstorms capable of 1"+/hr
    rates will eventually expand into a favorable collision/merger
    environment and support 1-2"+ totals resulting in scattered
    localized incidents of possible flash flooding.

    DISCUSSION...GOES WV suite depicts solid SE to NW short-wave
    ridging axis across central ID with very favorable divergence
    aloft as the northwestern edge of the jet streak expands westward
    across MT, further tightening the ridge axis as the core of the
    trough slides northeast into NE NV, south-central ID later
    tonight. While in the lowest levels, southerly moisture influx
    continues to filter through the Snake River Plain up into the
    terrain. RAP analysis suggests 850-700mb convergence axis is
    approaching, all the while, filtered sunlight has been increasing
    surface temperatures and with the increased moisture, greater
    instability. Currently MLCAPEs have reached 500 J/kg with limited
    capping; and a few of the highest peaks have seen convective
    development. As greater moisture and peak heating (1000 J/kg)
    increase toward 21-22z, expect convective vigor and coverage to
    expand throughout the range.

    At the apex of the ridge, mean steering flow will remain weak and persistent/increasing southerly upslope flow may allow for
    increased duration/redevelopment through the peaks before moving
    off. HRRR and WoFS rapid refresh suggest increasing coverage and
    slow motions with 15 and 5 minute rates suggestive of .5" and .2"
    rates, respectively, resulting in 1" exceedance probabilities to
    near 70-90% toward 23-00z. This is likely, as initial
    thunderstorms develop outflows, this will broaden moisture
    convergence for increased convective coverage and border updrafts
    with each up/down cycle. Mean cell motions of 5-10kts toward the
    north and northeast, countered by propagation toward the south due
    to inflow, suggests likelihood of cell mergers and localized
    instances of effectively stationary motions will allow for
    localized totals of 1-2". Naturally low FFG (.75-1"/hr &
    1-1.5"/3hrs) may be exceeded; while soils are dry per NASA SPoRT
    LIS generally below 25% compared to average, the harder top layers
    may be a bit more hydrophobic initially and if rates are intense
    enough should limit inflation and further increase run-off and
    potential for localized flash flooding.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!74pzFHqSJ8_XIdH-Y1UL7U9_mRLu7r4pLrEUZ-SpWKC10pCONMWsddZTtjyctxdMo63a= UGrO5MZgF2ZubsoZG5zGCSU$ for graphic product...

    ATTN...WFO...BOI...MSO...PIH...

    ATTN...RFC...PTR...NWC...

    LAT...LON 45661480 45531416 44711333 44051275 43521308=20
    43381397 43461543 43811675 44731706 45431601=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 Aug 26 21:00:55 2025
    AWUS01 KWNH 262100
    FFGMPD
    COZ000-NMZ000-WYZ000-270230-

    Mesoscale Precipitation Discussion 1011
    NWS Weather Prediction Center College Park MD
    500 PM EDT Tue Aug 26 2025

    Areas affected...South-central WY...Central
    Colorado...North-central New Mexico...

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

    Valid 262100Z - 270230Z

    SUMMARY...Initially slow moving thunderstorms along the Front
    Ranges of the Central Rockies will become increasingly efficient
    with rates of 1.5"/hr and localized 2-3" totals possible. In
    proximity to steeper terrain/urban settings localized flash
    flooding is possible.

    DISCUSSION...GOES-E Visible and Regional RADAR mosaic depict a
    compact shortwave/MCV feature moving through northwest CO nearing
    the apex of the larger scale ridge axis. The DPVA along the
    leading edge of the wave and across the southeast quadrant has
    been forcing scattered convection with intense rainfall production
    through the western Colorado Rockies. As the wave is approaching
    the Continental Divide, deeper layer moisture from the High Plains
    is starting to respond and increase upslope flow along the Front
    Ranges of CO and NM at this time. Sufficient morning/afternoon
    heating has resulted in the spine of the Rockies to become
    conditionally unstable with broad 1000-1500 J/kg of MLCAPE through
    the upslope region, given upper 50s Tds and modest mid-level lapse
    rates. The 850-700mb confluent flow is providing solid moisture
    flux even from the Four Corners region, but obviously greater
    depth up to 1.5" has been analyzed through the Front Range and
    with 10-15kts should support solid low level flux for efficient
    rainfall production as convection further organizes over the next
    few hours.

    Given core of height-falls remains far enough west, cell motions
    will be very slow/stationary given back-building influences; this
    is greater further south where mid to upper level flow is weaker
    in the anticyclonic rotor of the flow. So as the MCV and
    height-falls cross the higher terrain, cells further north will
    start propagating eastward a bit sooner than those across the
    Sangre de Cristo Ranges. As such, localized totals of 1-2.5" are
    probable across the central Rockies of S WY and northern CO; while
    spots of 2-3" are more likely (though still scattered in coverage)
    further south into Northern New Mexico. This generally aligns
    with the naturally low FFG within the upper-slopes of the Front
    Range that are .75-1.5"/hr and 1-2"/3hr; local exceedance is
    probable and scattered incidents of flash flooding are possible.=20
    The risk of flash flooding, of course, is slightly greater if the
    cells intersect with the larger urban centers along the Front
    Range.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!52xIQeOGHAzeEx7na_zT5Gve9InU0ZY3Pew0jWjFrEfn4qe8Vl9MmW7SVPuou2Tpp9k-= KsLRNteiAlvqnwdI1YBzz1k$ for graphic product...

    ATTN...WFO...ABQ...BOU...CYS...GJT...PUB...

    ATTN...RFC...FWR...KRF...STR...TUA...NWC...

    LAT...LON 41450661 41340566 41160490 40770438 40200410=20
    39600399 38660391 37240397 35890438 35350469=20
    35040539 35330637 35810689 36420671 36800620=20
    37550569 38190567 38910597 39550713 39960782=20
    40590811 41190762=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 26 22:01:25 2025
    AWUS01 KWNH 262201
    FFGMPD
    NVZ000-CAZ000-ORZ000-270300-

    Mesoscale Precipitation Discussion 1012
    NWS Weather Prediction Center College Park MD
    600 PM EDT Tue Aug 26 2025

    Areas affected...Northern Sierra Nevada Range & Far Northern
    California...

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

    Valid 262200Z - 270300Z

    SUMMARY...Strong convective thunderstorms capable of 1.5"/hr with
    potential for training across complex terrain of the Northern
    Sierra Nevada Range may result in localized flash flooding
    concerns through the late evening.

    DISCUSSION...GOES-W Visible and 10.3um trends show strong, cooling thunderstorms continue to expand and merge into a larger somewhat
    linear feature. RADAR and lightning animation, denote cells are strengthening/expanding but also propagating outward both west and
    east off the main ridge lines across northeast CA into far western
    NV. Total PWat analysis shows northern Central Valley and Great
    Basin are well above normal (at 1.2" ranges) with nearly localized
    maximum values over the last 30 years; while elevated, the
    northern Sierra Nevada range has similar, if slightly lower
    percentiles due to the lack of overall vertical depth to reach
    values near .7-.9" required. Still, the available moisture is
    highly anomalous to support highly efficient rainfall production
    given local surface Tds in the low 50s and with temperatures into
    the mid-70s, suggest CAPE values are slightly higher than analyzed
    at 1000-1500 J/kg. This supports rates of 1.5"/hr given weak but
    moist upslope convergent flow.

    Along the northwest periphery of the larger scale wave in the
    Great Basin has resulted in deeper layer steering/confluence
    across the northern Sierra to support a southwestward cell
    motions, this may allow for short-term training/repeating over the
    next few hours as the remaining inability is exhausted and cells
    further expand outward/downslope in each perpendicular to the mean
    flow. As such a spot or two of 2" totals remains possible in 30
    to 90 minutes, given complex terrain and low FFG values (1-1.5" in
    1 to 3hrs), localized flash flooding may be possible through the
    next few hours before instability/heating is fully exhausted.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-nr_auTAfUNqfK8xidrMCzmQkP4k__XItyVXXqq2AuFJ93DicLLDeIMBRiqJC2Mi5viQ= hia5OeDFB7a81VILZlhpcs0$ for graphic product...

    ATTN...WFO...MFR...REV...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 42032213 41802136 41352043 40932002 40501969=20
    40111941 39261907 38801945 38781994 39332050=20
    39972096 41032182 41432229 41682250 41962248=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 Aug 27 00:17:57 2025
    AWUS01 KWNH 270017
    FFGMPD
    NVZ000-CAZ000-270600-

    Mesoscale Precipitation Discussion 1013
    NWS Weather Prediction Center College Park MD
    817 PM EDT Tue Aug 26 2025

    Areas affected...Southern Nevada...Far Southeast California
    Deserts...

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

    Valid 270015Z - 270600Z

    SUMMARY...Converging clusters in vicinity of remaining unstable,
    moist air mass to continue widely scattered incidents of localized
    flash flooding through early overnight period.

    DISCUSSION...GOES-W WV suite continues to show main larger scale
    cyclone exiting the northern Great Basin toward the Snake River
    Plain with active clusters of activity along the far western
    peripheries across the terrain of the Sierra Nevada and in
    proximity to the San Bernandino Ranges. These clusters are
    expected to continue through northwesterly flow and generally
    merge across the southern Great Basin. Currently, there remain
    stronger thunderstorms across central San Bernandino county
    lifting northward feeding on the remaining limited unstable air at
    the northwestern edge of deeper lingering moisture (1-1.25" total
    PWats) through the higher deserts of southeast CA. Cells appear
    to have generated a cold pool resulting in northeasterly
    proapgation and are exepected to diminsh in the next few hours.=20
    Still, cells remain capable of a quick .5" of rain in less than
    30-60 minutes and given desert, hard rock conditions; flash
    flooding would remain possible though increasingly more scattered
    in nature with time.

    However, this cluster's outflow will remain important as it slides
    northeast into SW NV as it will intersect with outflow/convergent
    band at nose of northwesterly flow/downward mixing eminating from
    the central Sierra Nevada Range. Combine that with return
    moisture flow from south to southeasterly flow out of the Colorado
    River Valley, much of southern and central Nevada remain
    conditionally unstable with 1000-1500 J/kg of MLCAPE analyzed by
    the RAP. Total moisture also remains above normal with 1.25"+
    Total PWats. As the boundaries intersect toward sunset, an uptick
    in convective coverage and intensity is expected. Cell motions
    are likely to limit overall totals, but 1-1.5"/hr rates and
    localized totals of 1" over desert/rocky ground conditions (where
    FFG values are generally less than .75") suggests a few widely
    scattered, locally focused instances of flash flooding will remian
    possible through 06z.=20=20

    Of note, GOES-W Visible imagery shows a bit of mixed aerosols
    (mainly smoke over the central Great Basin (NW Nye county and
    northwest), cells that have been ingesting the aerosols have shown
    a slight increase in rainfall efficiency given increased
    nucliation resulting in small but more numerous rain droplets
    effectively acting like more tropical/warm cloud processes.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!74V1dPr2V1I7qJf3U3tYiCzCXFm_qRKibEVubKecco-jKljHyi40E6AStWz4aXw7Ht9p= V_ww2Bc9suShVQLNSbhwmIY$ for graphic product...

    ATTN...WFO...LKN...REV...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 40251764 40111691 39701583 39361516 38951453=20
    38251419 37241426 36291485 35281569 34911637=20
    34931728 35371759 35911762 36431763 37861786=20
    38501830 39141857 39681846 40111816=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Aug 27 00:47:56 2025
    AWUS01 KWNH 270047
    FFGMPD
    UTZ000-IDZ000-ORZ000-270630-

    Mesoscale Precipitation Discussion 1014
    NWS Weather Prediction Center College Park MD
    847 PM EDT Tue Aug 26 2025

    Areas affected...Southern Idaho...Far Northern Utah...Far Eastern
    Oregon...

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

    Valid 270045Z - 270630Z

    SUMMARY...Scattered incidents of localized flash flooding likely
    to continue through the early overnight period along the northern
    and eastern sides of larger scale mid-level cyclone. Additional
    totals of 2"+ possible, especially north and west.

    DISCUSSION...GOES-W WV suite shows core of large scale mid-level
    cyclone continues to lift northward and is currently centered in
    far NE NV with very impressive 150 degree highly diffluent
    upper-level jet pattern expanding across eastern OR into western
    MT before entering the core of the 80-90kt 250mb jet over the
    Northern High Plains. The sharpness of the ridging continues to
    provide very strong divergence pattern aloft across the Snake
    River Plain into the Salmon River Range and low level winds have
    responded, backed and accelerated through the Snake River Valley
    increasing convergence across southwest ID into the remaining core
    of greatest unstable air (1000-1250 J/kg of MLCAPE). Strong
    convective arc of overshooting tops can be seen across
    Boise/Elmore county extending north. Deep layer moisture to near
    1.3-1.4" and 850-700mb winds to 15-20kt per VWP suggest flux will
    support 1.5-1.75"/hr rates locally. Slow cell motions in the core
    of the ridge aloft should allow for some duration where localized
    1-3" totals are possible, which fits well toward the 90th
    percentile in recent WoFS run where qualitative assessment
    suggests maximum totals generally are just below that 90th
    percentile value and in some fairly close proximity. Given
    terrain and naturally low FFG values, this provides confidence
    that localized incidents of flash flooding are likely over the
    next few hours. Generally, convergence axis is expected to
    further lift northwest through the Snake Plain into eastern
    Oregon, though overall rates/totals should reduce out of the core
    of deepest overall moisture, but still remain a flash flooding
    risk.

    Further upstream, the warm conveyor belt and deep southerly
    moisture surge continues east of the deeper overall mid-level
    center through western UT into southeast ID, ongoing thunderstorms
    continue to burst through the cirrus canopy, through overall well
    of unstable air continues to reduce across UT into E ID/far W WY.=20
    Overall trends should be diminishing over the next few hours with
    that instability/heating loss, but overall moisture and strength
    of flux convergence will allow for ongoing activity to be
    efficient (though likely a bit less than the stronger deeper cores
    further west) spots of additional 1-2" are probable and may induce
    similar localized incidents of flash flooding through the early
    overnight period. New thunderstorm activity is possible near/just
    east of the mid to upper level center as DPVA may locally back
    winds and tap smaller areas of remaining unmixed unstable air, but
    should be very isolated across northern UT and just over the
    border.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_MHlBDhPOkyBWvFdzWaUzeAGghjP6LzZPq54HPJXp5jeifzOQjDTKfVP5h4QadF5xnnc= mCMoB37fK6q0fEY9eu6hgjs$ for graphic product...

    ATTN...WFO...BOI...MSO...PIH...SLC...

    ATTN...RFC...PTR...STR...NWC...

    LAT...LON 45081489 44181284 43351173 42671123 41941113=20
    41401174 41431359 42101407 42091623 42561769=20
    44071815 44801778 45041678=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Aug 27 19:33:40 2025
    AWUS01 KWNH 271933
    FFGMPD
    WYZ000-UTZ000-IDZ000-280030-

    Mesoscale Precipitation Discussion 1015
    NWS Weather Prediction Center College Park MD
    333 PM EDT Wed Aug 27 2025

    Areas affected...Southern Idaho...Northern Utah...Western
    Wyoming...

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

    Valid 271930Z - 280030Z

    SUMMARY...Above normal moisture and slow cell motions, with a few
    corridors of repeating cells may result in sub-hourly totals of
    .5-1" and isolated locations of up to 2". Complex, steep terrain,
    old burn scars are at greatest potential for localized flash
    flooding through evening.=20

    DISCUSSION...GOES-E WV suite and RAP analysis denotes a string of
    mid-level vorticity centers within a vortex roll-up pattern
    stretching from the strongest wave near the mouth of the Columbia
    River in WA/OR crossing the Bitter Roots, Centential and
    eventually across the Big Horns toward western Nebraska. Along
    and north of the line, scattered dense with very small breaks in
    the mid-level cloud canopy has resulted in limited infiltration of
    solar heating and therefore unstable environment. However, in
    their wake a broad area of fairly clear skies and lingering
    remaining moisture which is still well above normal ranging from 1
    to 1.3" for Total Pwat values, though most of the surface to
    boundary layer moisture remains at or above 60F for Tds across
    Snake River Plain, surrounding terrain/valleys into northern UT
    and far western WY. As such, near full insolation has brought
    SBCAPEs up across much of the area over 1000 J/kg with pockets of
    1500 J/kg typically in lower valleys (where vertical depth just
    adds to the overall totals).=20

    WV and other conventional satellite imagery also denotes a
    shortwave feature south of the main shear axis crossing SW ID at
    this time, the strength of the wave is maintained/enhanced aloft
    by sharp 250mb ridging along the main mid-level shear axis
    providing solid right entrance but also diffluent flow for solid
    outflow increasing broader vertical ascent/evacuation. As such,
    the westerly DPVA is helping to develop arched banding
    convergence downstream across SW ID and across the Range and Basin
    terrain south of the Snake River Plain across S-central to SE ID
    for increasing convective development. While initially narrow in up/downdrafts, vertical strength and low level moisture loading
    will increase rainfall rates toward .75-1"/hr. Cells will be
    fairly slow moving at 10-15kts and given the orientation of
    development across SE ID, some repeating is possible. As such, a
    spot or two of up to 2" is possible, though spots of .5-1" in
    sub-hourly totals may still result in localized enhanced run-off
    and possible flash flooding conditions.

    More north-south linear convective lines are developing southward
    across N UT, and should not train, but may repeat over areas
    affected earlier and may reaggravate any flooding
    conditions/higher run-off areas.=20

    Nearer the SW ID shortwave, cells should be stronger more
    progressive in nature given stronger deeper layer flow, but on the
    northern rotor, downshear of the vort center across the Southern Sawtooth/Salmon River Ranges, cells could hang up/slow allowing
    for isolated enhanced totals, so have included this area into the
    area of concern for overall lower end, isolated to
    widely-scattered potential for flash flooding conditions.=20

    At this time, have left much of central ID and along SW MT/ID
    border excluded given the lack of instability, though strength of
    dynamic forcing may continue to be main driver...but is a bit more
    uncertain for intense rates, even though Hi-Res CAMs and global
    guidance are more consistent with overall rainfall totals. So,
    will continue to watch observational trends if an MPD will be
    necessary across that area.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5IHZJqo_2o5Tpx5Na-mhAKJb3cmy6MgRIjUgJUNHKmOHUUeCU-YdzldClFYsDoVi57aO= LoU8Z8O0GmwxvWAUtA0dpN4$ for graphic product...

    ATTN...WFO...BOI...MSO...PIH...RIW...SLC...

    ATTN...RFC...KRF...PTR...STR...NWC...

    LAT...LON 44441173 44321079 43950984 43240903 42530921=20
    42131000 41501033 40631060 40071123 39911190=20
    40121247 41011295 41731355 42131416 42451492=20
    42841560 43541586 44101564 44311520 44371466=20
    44271390 44211303=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Aug 28 00:26:42 2025
    AWUS01 KWNH 280026
    FFGMPD
    KSZ000-COZ000-280530-

    Mesoscale Precipitation Discussion 1016
    NWS Weather Prediction Center College Park MD
    825 PM EDT Wed Aug 27 2025

    Areas affected...Eastern Colorado...Western Kansas...

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

    Valid 280030Z - 280530Z

    SUMMARY...Increasing convection at near strengthening surface low
    may result in slow moving clusters with eventual upstream mergers
    before main WAA/isentropic ascent/training event occurs
    downstream. Localized 2-4" totals through 04-05z may result in
    possible localized flash flooding incidents.=20

    DISCUSSION...Larger, synoptic scale trough over ID/MT Rockies
    continues to elongate into a string of vorticity centers along the
    northern edge of the synoptic ridging centered over the New Mexico
    and Colorado High Plains. The eastward edge of the vorticity
    strip has fostered strong convective cells, expanding into a
    forward propagating line of cells across W NEB into NE CO which
    will continue to march southward intersecting return low level
    moisture and upslope flow over E CO/NW KS over the next few hours.
    The DPVA along with strong right entrance of exiting
    northwesterly upper-level jet over central and eastern KS; as well
    as nose of approaching speed max out of the Four Corners is
    supporting solid divergent pattern over eastern CO to support the
    thunderstorm activity, but more importantly continue to deepen the
    surface cyclone south of Burlington, CO. A well defined surface
    front is bending under the deepening low's influence as well as
    increasing deep layer moisture convergence along/ahead of the
    advancing convective line with newer downstream cells starting to
    break out over W KS. These clusters will continue to
    strength/expand and with increasing deep layer moisture inflow
    will increase in rainfall efficiency over the next few hours over
    far E CO. Sub-hourly/instantaneous rates will be strong but
    forward propagation may only support localized 1.5-2" totals.

    However, pre-convective line cells developing in proximity to the
    surface low and southward trending pressure trof/convergence axis
    seen very well in late-day visible imagery have been developing
    slow moving thunderstorms with solid 20kt surface to boundary
    layer inflow of mid 60s Tds and are supporting 1.5-2"/hr rates.=20
    Slow motions, waiting for the upstream DPVA/height-falls have been
    allowing some localized totals nearing 2-3" and may continue to
    support other local totals up to 4" before the main line arrives.=20
    While much of SW KS has the locally higher FFG values, a few spots
    may be exceeded and result in a localized/focused incident or two
    of flash flooding.

    Eventually, as the boundary layer decouples after sunset and the
    LLJ starts to strengthen and broaden, isentropic ascent along the
    frontal zone ahead of the approaching convective line will develop
    and orient generally parallel to the mean steering flow allowing
    for training and eventual more likely flash flooding concerns
    later overnight into central KS (and downstream), but a subsequent
    MPD will be written close to that time frame, but until that
    time...scattered flash flooding remains locally possible.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9bE754lxoKw5PZsgItqw74IudG_FzFFHd9AjW4SzoVEeD2nJei7ET2paaCwiQHxiPcxx= SlgCy-euS1E0W2i9zW8vd1k$ for graphic product...

    ATTN...WFO...BOU...DDC...GLD...PUB...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 40140258 39810163 39209996 38769930 38379909=20
    37699933 37370015 37180122 37380175 37910231=20
    38210263 38560311 39030358 40090333=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Aug 28 05:01:16 2025
    AWUS01 KWNH 280501
    FFGMPD
    OKZ000-KSZ000-281000-

    Mesoscale Precipitation Discussion 1017
    NWS Weather Prediction Center College Park MD
    100 AM EDT Thu Aug 28 2025

    Areas affected...Western and Southern KS...Northern OK

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

    Valid 280500Z - 281000Z

    SUMMARY...Gradually organizing clusters of heavy showers and
    thunderstorms will eventually pose a threat for scattered areas of
    flash flooding going through the remainder of the overnight hours.

    DISCUSSION...The latest GOES-E IR satellite imagery shows cooling
    convective cloud tops across western KS as modest shortwave energy
    ejecting east-southeast across the region interacts with a
    stationary frontal zone and gradually strengthening warm air
    advection associated with an increasing south-southwest low-level
    jet.

    So far, area VWP show the low-level jet reaching only 20 to 30+
    kts across northern OK and southern KS, and the instability
    profiles are rather modest too with MUCAPE values along and
    northeast of the front of 500 to 1000 J/kg. This has been
    tempering the convective organization and coverage over the last
    couple of hours, but as the low-level jet strengthens further
    (especially after 0600Z), there should be a more substantial
    increase in elevated convection across western and southern KS,
    and perhaps across northern OK as well where the best instability
    gradient is currently situated.

    The latest hires CAMs show a fair amount of spread with the exact
    placement of the heaviest rainfall threat overnight along with the
    totals. Overall, the 00Z HREF suite appears to potentially be a
    bit overdone (especially considering the very aggressive 00Z
    NAM-Conest), and the consensus may be a bit too far off to the
    northeast into the more stable airmass that is currently locked in
    place across eastern KS.

    Radar and satellite trends along with some of the recent WoFS
    guidance suggests areas of western and southern KS will see the
    main concentration of heavier shower and thunderstorm activity
    over the next few hours. By later tonight, areas of northern OK
    should begin to also see more focus for convection as the nose of
    a gradually veering low-level jet impinges on this region.

    Rainfall rates of 1 to 2 inches/hour are expected with the
    stronger storms, and eventually sufficient organization is
    expected to foster some cell-training concerns. This will
    potentially support rainfall totals of 2 to 4 inches with isolated
    5+ inch amounts possible. These rains will eventually pose a
    threat for some scattered areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7k7bvNpDibNHpED4EjVF4mROf3qzlRcrXTOoyx5ugE0gUUo5iPs-DU0da-Vh8o6w0kgq= Y70vc59CQmQ-ZvM1x08FAZU$ for graphic product...

    ATTN...WFO...AMA...DDC...GID...GLD...ICT...OUN...TSA...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39410098 39179896 37919665 36589641 36089814=20
    36740033 37760163 38680190=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Aug 28 09:06:50 2025
    AWUS01 KWNH 280906
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-281505-

    Mesoscale Precipitation Discussion 1018
    NWS Weather Prediction Center College Park MD
    505 AM EDT Thu Aug 28 2025

    Areas affected...Southern KS...North-Central to Northeast OK...Far
    Southwest MO...Northwest to Central AR

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

    Valid 280905Z - 281505Z

    SUMMARY...Organized clusters and bands of showers and
    thunderstorms will continue through the morning hours. A
    combination of localized cell-training and heavy rainfall rates
    will likely result in areas of flash flooding. Locally significant
    urban flooding impacts will be possible.

    DISCUSSION...The latest GOES-E IR satellite imagery along with
    dual-pol radar shows organized clusters of elevated convection
    evolving across portions of central and southern KS on down into
    northern OK. Additional elevated bands of convection are also
    noted well off to the southeast down across northwest to central
    AR. The activity early this morning is being strongly supported by
    the east-southeast advance of weak mid-level shortwave energy
    interacting with a stationary frontal zone and the nose of 40+ kt
    southwest low-level jet overrunning it.

    A corridor of stronger speed convergence and with proximity of an
    elevated instability gradient over southern KS in particular has
    allowed for convection across these areas to gain substantial
    organization over the last couple of hours with heavy rainfall
    rates that are reaching upwards of 2 inches/hour with the stronger
    cells.

    Enhanced warm air advection/isentropic ascent across this region
    to the northeast of the aforementioned front should maintain
    convection over the next several hours, but with a gradual
    tendency for the convection to lose some latitude while also
    advancing off to the east. MUCAPE values are rather modest with
    values of 500 to 1000 K/kg, but the increase in low-level moisture
    transport and related speed convergence is expected to help
    compensate and continue to support locally high rainfall rates
    along with a generally organized axis of convection.

    The 00Z HREF/REFS suites of guidance are still likely too far to
    the north and east with their axis of heavier QPF this morning,
    and perhaps a tad too heavy. Recent runs of the HRRR, RRFS and
    WoFS all suggest more of a northwest to southeast axis of heavy
    rains that impacts southern KS into north-central and northeast OK
    going through the morning hours. Heavy rains will also be likely
    well off to the southeast across northwest to central AR and
    perhaps brushing somewhat into far southwest MO. Additional
    localized rainfall totals of as much as 3 to 5+ inches of rain
    will be possible, and especially with a favorable environment for cell-training.

    Given the elevated rainfall rates and storm totals that are
    expected this morning, areas of flash flooding are likely. This
    may include a locally significant urban flooding impact.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5m-I8xQQKVF8eKEDcLR_pMHmC76VOkazCCu9bo-T4wNOQpYhs4WIn2ZoV6VN2L4K3g1A= DB8QuI83r0GXOKsvZ9Lq2Sc$ for graphic product...

    ATTN...WFO...AMA...DDC...ICT...LZK...OUN...SGF...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 38069692 37859541 37269390 36169258 34639123=20
    33849142 33809223 34279317 34849419 35489588=20
    35739722 36019904 36329971 36750004 37429999=20
    37789949 38019828=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Aug 28 14:55:55 2025
    AWUS01 KWNH 281455
    FFGMPD
    ARZ000-OKZ000-281900-

    Mesoscale Precipitation Discussion 1019
    NWS Weather Prediction Center College Park MD
    1055 AM EDT Thu Aug 28 2025

    Areas affected...central/eastern OK into western/central/southern
    AR

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

    Valid 281454Z - 281900Z

    SUMMARY...Areas of training with rain rates ranging between 1 to 3
    in/hr are expected to produce areas of flash flooding from
    portions of eastern OK into western AR through 19Z. Additional
    rainfall over the next 4 hours should range between 2 to 4 inches,
    but localized higher totals cannot be ruled out.

    DISCUSSION...Radar imagery from 1420Z showed an elongated axis of
    elevated thunderstorms stretching from central OK into western AR,
    along with a secondary axis of NW to SE training from central AR
    into central MS. Since 12Z, embedded areas of training within this
    broad axis have shown hourly rainfall between 1-2 inches, but
    locally in excess of 2 inches as well. A convectively enhanced
    vorticity max was observed in water vapor imagery just southeast
    of Wichita, KS with movement toward the southeast. MUCAPE values
    to the northeast of a frontal boundary (extending from central OK
    into eastern TX) were a modest 500 to 1000+ via 14Z SPC
    mesoanalysis data but were likely "tall/skinny" with PWAT values
    compensating with estimated values near 2 inches within the
    ongoing convective axis. VAD wind data showed 925-850 mb winds
    overrunning the surface front with 25-35 kt of flow from the
    southwest.

    A recent southward push to thunderstorms over central OK were
    minimizing the flash flood threat across that portion of the state
    but new development downstream was showing signs of training with
    the coldest cloud tops on IR imagery from eastern OK into western
    AR. While forecasts from the RAP indicate a steady weakening of
    the 825-850 mb flow into the 15-20 kt range by 19Z, areas of flash
    flooding will be likely to sustain in the short term. Over the
    next 3-4 hours, forcing for ascent will continue to come from a
    combination of isentropic ascent atop the front, DPVA ahead of the
    advancing vorticity max positioned over southern KS and diffluent
    flow aloft within the anomalously moist environment. Hourly
    rainfall of 1-2 inches will be common within areas of training but
    isolated hourly totals of 2 to 3 inches may also occur. The
    greatest concern will be from eastern OK into western AR where an
    additional 2 to 4 inches of rain (locally higher) is expected
    through 19Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8avPSJ6cwdAZzHG7igoooXKdXQjxus8-hAHKmHcWhIzu7bO69r6n8DxVE5oSIzUXiQXz= uU-Pe5uQnoAr-uU58pKgA1U$ for graphic product...

    ATTN...WFO...JAN...LZK...OUN...SHV...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 36399520 35839394 35399297 34959201 34279136=20
    33579137 33339229 33709400 33999518 34399642=20
    34859707 35199730 35859696 36389581=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Aug 28 15:42:59 2025
    AWUS01 KWNH 281542
    FFGMPD
    ALZ000-MSZ000-LAZ000-ARZ000-282045-

    Mesoscale Precipitation Discussion 1020
    NWS Weather Prediction Center College Park MD
    1142 AM EDT Thu Aug 28 2025

    Areas affected...ArkLaMiss into central MS and far western AL

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

    Valid 281540Z - 282045Z

    SUMMARY...Heavy rainfall may result in localized areas of flash
    flooding across central MS in a northwest to southeast fashion,
    possibly impacting small portions of AR/LA and AL. Training of
    thunderstorms will be capable of 1-2 in/hr rainfall rates. Mostly
    dry antecedent conditions should limit the greatest flash flood
    risk to urban areas or other locations with poor drainage.

    DISCUSSION...Area radar imagery at 1530Z showed a NW to SE
    oriented axis of showers and embedded thunderstorms from central
    AR into central MS, with KDGX radar reflectivity/velocity data
    indicating an MCV to the northeast of Jackson over Leake County.
    Areas of heavy rainfall aligned with an elevated 925-850 mb
    convergence axis which was oriented northwestward from the MCV
    feature over central MS. Deeper layer steering flow oriented
    quasi-parallel to the convergence axis has supported periods of
    training over the past few hours with MRMS-derived hourly totals
    peaking in the 1-2 inch range over the past couple of hours
    (mostly in the vicinity of I-20).

    Short term RAP forecasts show the MCV tracking ESE toward western
    AL over the next 3-5 hours with the trailing convergence axis
    remaining from southeastern AR into central MS with a slow
    southward drift. While moisture is high (12Z JAN sounding with 2.0
    inches), elevated instability is a bit lacking within the ongoing
    precipitation axis at ~500 J/kg or less via 15Z SPC mesoanalysis
    data, but instability is higher to the south and increasing with
    daytime heating. Despite the weak instability, the potential will
    exist for localized flash flooding over the next 3-5 hours from
    training and 1-2 in/hr rain rates. Storm total rainfall of 2-3
    inches will be possible over a relatively short period of time.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9aNxwB2WRnJaftZCzmSC2XZzVpKIB7lnochofu74QBV-ALY80Igv6A7hLvqYSfvjpGBs= MXySrjwxZ5WvB_VNL529Nz4$ for graphic product...

    ATTN...WFO...BMX...JAN...LZK...MEG...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34379117 34049017 33608941 33298862 32918793=20
    32268786 31558812 31348924 31759065 33319185=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 Aug 28 19:03:57 2025
    AWUS01 KWNH 281903
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-290000-

    Mesoscale Precipitation Discussion 1021
    NWS Weather Prediction Center College Park MD
    303 PM EDT Thu Aug 28 2025

    Areas affected...in and around ArkLaTex

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

    Valid 281900Z - 290000Z

    SUMMARY...A few areas of isolated flash flooding will be possible
    from southeastern OK/northeastern TX into southern AR and northern
    LA through 00Z. Localized instances of training should support
    hourly rainfall of 1 to 2 inches with spotty hourly totals of 2 to
    3 inches.

    DISCUSSION...Radar imagery from 1830Z showed broken coverage of
    thunderstorms extending from east-central OK into central AR, with
    a reduction in rainfall intensity and training axes over the past
    couple of hours, partially tied to a weakened low level jet. There
    were embedded mesoscale circulations noted within the broader
    precipitation shield, located out ahead of a low to mid-level
    shortwave located near the MO/KS/AR/OK 4-state junction,
    translating downstream. This region of convection was located to
    the north of a well-defined stationary front, enhanced by
    differential heating, which extended WNW to ESE from the Red River
    Valley into southern MS. Low level flow of 10-20 kt was in place
    over northern TX into northwestern LA via VAD wind plots,
    supporting overrunning of the front with cells moving
    quasi-parallel to the boundary toward the ESE, allowing for
    localized training and repeating. Aloft, flow was diffluent,
    aiding in vertical ascent across the ArkLaTx region.

    Robust surface heating to the south of the front was aiding in a
    sharp instability gradient with 1500+ J/kg MLCAPE from far
    southeastern OK into eastern TX and central LA and PWATs were
    close to 2 inches in and around the ArkLaTex via 18Z SPC
    mesoanalysis data. Additional thunderstorms are expected to form
    near the frontal boundary over the next 2-4 hours with a general
    movement of cells off toward the ESE. While coverage of these
    additional cells remains uncertain, ongoing upstream convection
    over OK and AR should continue while advancing toward the
    SE/ESE...out ahead of the upstream shortwave. Alignment of
    boundaries and the mean steering flow will likely support a few
    areas of at least brief training and 1 to 2 inches of rain within
    an hour. However, higher hourly rainfall totals cannot be ruled
    out and may contribute to localized areas of flash flooding where
    training is able to persist for 1-2 hours.

    A negative to flash flood potential is that most of the outlooked
    area has received below average rainfall over the past 1-2 weeks
    leading to high flash flood guidance values of 3 to 5+ inches in 3
    hours. Therefore, the greatest flash flood risk will likely reside
    within urban areas or other locations with poor drainage.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5Oh1ytZJBqaRDC8CA5opGMb2tIZJ7XMq7SI7rROJplJToWFD761KOmyqxxCw5zhWk5Ms= aC4pMHHA0A7ha51JWCo09fI$ for graphic product...

    ATTN...WFO...FWD...JAN...LCH...LZK...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35159452 34899348 34149235 32749166 31129242=20
    31559426 32859630 34169663 34969591=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 29 07:01:34 2025
    AWUS01 KWNH 290701
    FFGMPD
    ALZ000-MSZ000-LAZ000-ARZ000-TXZ000-OKZ000-291300-

    Mesoscale Precipitation Discussion 1022
    NWS Weather Prediction Center College Park MD
    300 AM EDT Fri Aug 29 2025

    Areas affected...Northeast TX...Far Southern AR...Northern and
    Central LA...Central and Southern MS

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

    Valid 290700Z - 291300Z

    SUMMARY...Expanding bands of heavy showers and thunderstorms with
    cell-training concerns are expected going through mid-morning.
    This will gradually pose a concern for areas of flash flooding.

    DISCUSSION...The latest GOES-E IR satellite imagery is gradually
    showing an uptick in cooling convective tops near the Arklatex
    region, and with additional broken bands of elevated convection
    extending off to the southeast across northern LA and through
    central MS.

    A gradual increase in warm air advection/isentropic ascent is
    noted on the poleward side of a quasi-stationary front and within
    a very moist and moderately unstable airmass. MUCAPE values are as
    high as 1000 to 2000 J/kg along the front involving eastern TX
    through central LA, however, much of the elevated convection is
    rooted within the instability gradient farther north along the
    AR/LA border along with adjacent areas to the west and east. This
    is also where there is some modest frontogenesis and related
    forcing seen in the 925/850 mb layer. Meanwhile, the PWs are on
    the order of 2.0 to 2.25 inches and suggestive of a very tropical
    environment.

    The flow aloft is becoming increasingly divergent as an
    upper-level jet streak rounds into the base of the deeper layer
    trough over the Mid-South/OH Valley region, and this should drive
    a low-level response this morning with an additional increase and
    gradual veering of the low-level flow across eastern TX and
    central LA. This will interact with the aforementioned frontal
    zone and promote stronger isentropic ascent and frontogenetical
    forcing.

    This along with the pool of instability that is available will
    favor additional development and expansion of heavy showers and
    thunderstorms with at least some loose organization given
    proximity of 30 to 40 kts of effective bulk shear. Propagation
    vectors are relatively weak which suggests there may be some
    attempt at some backbuilding cells, and given the linear nature of
    some of these elevated bands of convection, there will be concerns
    for cell-training.

    Rainfall rates will be very high and capable of reaching 2.5
    inches/hour given the level of moisture and instability, and with
    the backbuilding/cell-training concerns, some rainfall totals
    going through mid-morning may reach 3 to 5+ inches.

    A gradual southward advance of the overall convective footprint is
    expected over the next several hours, but with these rains, there
    may be areas of flash flooding that materialize and especially for
    the more sensitive urban environments.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6JUvKl93dizNJOe4QATzDqiKcq_s5hv4AQ3X_iBV53O14dIFT2WG99iZSWvUZpUBM1kE= mLyb_aBCGGy6tH4E8qXVepA$ for graphic product...

    ATTN...WFO...FWD...JAN...LCH...LIX...LZK...MOB...OUN...SHV...
    TSA...

    ATTN...RFC...ALR...FWR...ORN...TUA...NWC...

    LAT...LON 33989551 33699411 33259262 32829060 32558959=20
    32318886 31518832 30338870 30189014 30679292=20
    31249453 32199614 33229668 33879630=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 29 13:01:09 2025
    AWUS01 KWNH 291301
    FFGMPD
    MSZ000-LAZ000-TXZ000-291730-

    Mesoscale Precipitation Discussion 1023
    NWS Weather Prediction Center College Park MD
    900 AM EDT Fri Aug 29 2025

    Areas affected...eastern TX into LA and southern MS

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

    Valid 291259Z - 291730Z

    SUMMARY...Localized to widely scattered areas of flash flooding
    will remain likely early this morning, possibly extending into the
    early afternoon from portions of eastern TX into LA and southern
    MS. While coverage of flash flooding may be limited, the potential
    for very high rates in excess of 3 in/hr will exist.

    DISCUSSION...1240Z radar imagery showed elevated thunderstorms
    from northeastern TX into central LA and southern MS with embedded
    areas of training and MRMS-derived hourly rainfall of 2 to 3+
    inches...mainly over the north-central TX/LA border and just north
    of Alexandria, LA. The environment was characterized by very high
    moisture (PWATs 2.2 to 2.5 inches) and 500-1000 J/kg MUCAPE via
    12Z SPC mesoanalysis data. Rainfall has been efficient given this
    environment with local 88D imagery showing cells containing low
    echo centroid signatures and 15 minute rates over 1 inch per MRMS
    and gauge data. An elevated convergence axis stretched
    southeastward from northeastern TX and was being overrun by
    925-850 mb winds of ~15 to 20 kt from the SW, favorably ascending
    the boundary with deeper layer mean winds translating cells toward
    the southeast.

    An MCV-like feature appeared to be located between JAN and PIB,
    with movement toward the east. The low level convergence axis has
    been advancing slowly but steadily toward the south over
    southwestern MS into central LA, limiting the coverage and
    magnitude of rainfall rates. The boundary was also advancing over
    TX, toward the southwest, but its orientation aligning more
    favorably with the mean wind was supporting a locally enhanced
    flash flood threat over northeastern TX as of 1240Z. This area
    will continue to be a locally higher concern in the short term
    with hourly rainfall of 2 to 3+ inches. Short term RAP forecasts
    show weakening and further veering of the low level flow through
    17Z which should tend to lessen the overrunning component from
    central LA into MS, but some isolated areas of training will
    remain along the elevated convergence axis.

    The flash flood threat should linger a bit longer over eastern TX
    into western LA where despite weakening low level winds into the
    rest of the morning, high moisture and areas of training should
    focus at least a localized flash flood concern over the next few
    hours. Additional development of thunderstorms with the onset of
    daytime heating across southwestern LA may also pose a flash flood
    threat after 15Z with an added component related to the advancing
    low level axis of convergence from the north.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9OirOFvdV-G9fEyWtv2r_Md_tzwHfgOGaGgx0Wv4dHtORV6jnS9XrcFvAEULfpGO-JS2= uFo0W2zCeDUCdl6ng-EkvOU$ for graphic product...

    ATTN...WFO...FWD...HGX...JAN...LCH...LIX...MOB...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 33179511 33179444 32529362 31919224 31789059=20
    31958945 31708869 31128847 30458876 29768996=20
    29429118 29439301 29719395 30539469 31489541=20
    32179566 32759557=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 29 18:14:15 2025
    AWUS01 KWNH 291814
    FFGMPD
    LAZ000-292111-

    Mesoscale Precipitation Discussion 1024
    NWS Weather Prediction Center College Park MD
    213 PM EDT Fri Aug 29 2025

    Areas affected...southern Louisiana

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

    Valid 291811Z - 292111Z

    Summary...Brief/isolated flash flooding is possible across
    southern Louisiana through 4p CDT/21Z.

    Discussion...Over the last hour or so, a mesoscale convective
    complex near Baton Rouge has increased in intensity while
    migrating slowly southward. Additional cells were developing from
    this complex southwestward toward Lake Charles, Lafayette, and
    along I-10. These cells were migrating toward an abundantly
    moist/unstable pre-convective airmass (2.3+ inch PW values, 3500
    J/kg SBCAPE), supporting strong updrafts and efficient rainfall
    rates within the most persistent activity. Despite southward
    motions, areas of 1-2 inch/hr rain rates have been estimated per
    MRMS near the Baton Rouge area. These rates may be enough to
    support an isolated flash flood risk especially near urban/flash
    flood prone areas across southern Louisiana.

    Models/observations are all suggestive of a continued, yet slow
    southward progression of the ongoing activity toward the Gulf
    Coast through 4p CDT/21Z. Some of the heavier rain rates may
    impact western portions of New Orleans Metro during that
    timeframe. Flash flooding could occur with ongoing activity, but
    should be isolated and focused on urban/sensitive areas. Areas of
    1-2 inch/hr rain rates should continue, with higher rates/rainfall
    totals possible near any localized areas of training/cell mergers.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_Zvkj-bUelgq3vwpm450SXtdlVxH7rveg9xI80KKeO097j4G-jNR2S31u7uSgiC3_RUe= ksU96Cba7uhXLuKarbBdUbE$ for graphic product...

    ATTN...WFO...LCH...LIX...

    ATTN...RFC...ORN...NWC...

    LAT...LON 30489171 30419035 29918921 29318911 29059006=20
    29149166 29609308 30209320=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 29 18:29:45 2025
    AWUS01 KWNH 291829
    FFGMPD
    TXZ000-NMZ000-AZZ000-300028-

    Mesoscale Precipitation Discussion 1025
    NWS Weather Prediction Center College Park MD
    228 PM EDT Fri Aug 29 2025

    Areas affected...New Mexico

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

    Valid 291828Z - 300028Z

    Summary...Isolated flash flood potential should expand/increase
    though 00Z/6p MDT this afternoon.

    Discussion...Satellite and radar depict isolated thunderstorm
    development primarily along favored ridgelines/high terrain from southern/southwestern through north-central New Mexico. The
    storms have formed due to abundant surface heating beneath a
    pronounced mid-level moisture plume across western and central
    parts of the state. Flow aloft (strongest over the western parts
    of the state) were supporting slow northeastward storm motions
    with developing activity, although localized backbuilding was
    already noted across south-central and southwestern New Mexico.=20
    Where the backbuilding has been most pronounced (east of
    Alamogordo), rain rates approaching 2 inches/hr have been
    estimated per MRMS.

    Given appreciable moisture values, weak mid-level disturbances,
    and continued surface heating, conditions favor an expansion of
    convective coverage through the afternoon and early evening hours
    across the discussion area. Any downpours near existing burn
    scars could promote a quickly evolving and locally significant
    flash flood threat. Areas of 1-2 inch/hr rain rates are likely to
    expand in tandem with increasing convective coverage, and the
    highest rain rates are likely across the southeastern 1/2 of the
    state where steering flow aloft is the weakest and tropospheric
    moisture content highest.

    Wind profiles across northeastern/east-central New Mexico favor
    eventual growth into slow-moving clusters of storms that may
    prompt a slightly higher concentration of flash flood instances
    over time.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_uJyp8RiiukATBXTgTjKeysUvouAANFSkFCZeONY0yCsSzC-eqw4XmMWyhlzKHLM50d_= Ur0SXdxLzu-Fl0M9yM_9x70$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...TWC...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 36700397 34410338 32000454 31840694 31790910=20
    33840879 36660668=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Aug 29 20:04:47 2025
    AWUS01 KWNH 292004
    FFGMPD
    FLZ000-300203-

    Mesoscale Precipitation Discussion 1026
    NWS Weather Prediction Center College Park MD
    403 PM EDT Fri Aug 29 2025

    Areas affected...portions of southeastern Florida

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

    Valid 292003Z - 300203Z

    Summary...Isolated/urban flash flooding is possible through the
    afternoon and early evening.

    Discussion...Recent satellite/lightning imagery depicts rapid
    development of deep convection along a sea breeze boundary just
    west of Miami (near Kendall), with additional, scattered activity
    located over the Everglades. The cells were forming in an
    environment characterized by strong instability (2000+ J/kg
    MLCAPE) and plenteous moisture content (1.8+ inch PW values).=20
    These environmental parameters - combined with weak/negligible
    tropospheric flow for steering) was promoting ongoing development.
    The cell near Kendall was already producing estimated 1-2 inch/hr
    rain rates, which isn't a surprise given its slow movement amid
    abundant moisture/instability.

    Models/CAMs suggest that ongoing development will continue to
    expand in coverage an intensity given continued
    heating/destabilization along the sea breeze, which was located
    just inland along populated areas of southeastern Florida.=20
    Additional areas of 1+ inch/hr rain rates are expected, which
    could result in flash flooding in urban and low-lying areas. Much
    of the flash flood risk should be diurnally driven, with weakening
    expected from both 1) loss of surface heating and 2) stabilization
    from scattered to widespread convective overturning across the
    discussion area.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4P9wSE9JUPm8UY_UWf3nZX8jBI-M5PpiYTrkvqv0xeYUGZUKYiGm0MsV_E2dHifisuAy= pOEoph6st-iCS1W817vzuOA$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 27628039 27268000 27177995 26617995 25958006=20
    25228030 24968060 25218080 25858069 27208048=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 Aug 29 22:48:21 2025
    AWUS01 KWNH 292248
    FFGMPD
    KSZ000-COZ000-300246-

    Mesoscale Precipitation Discussion 1027
    NWS Weather Prediction Center College Park MD
    647 PM EDT Fri Aug 29 2025

    Areas affected...central/eastern Colorado, far western Kansas

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

    Valid 292246Z - 300246Z

    Summary...Scattered thunderstorm activity was backbuilding along
    the I-25 corridor between Colorado Springs and Pueblo. A couple
    instances of flash flooding are possible through 02Z/8p MDT.

    Discussion...Recent radar mosaic imagery has depicted backbuilding
    convection along a relatively focused axis extending from I-25
    between Colorado Springs and Pueblo eastward to near State Highway
    71. The storms are forming in a weak low-level-shear environment,
    with 15-25F surface dewpoint depressions supporting mostly
    outflow-dominant storms. Despite the tendency for outflow
    dominance, upstream mid-level flow was aiding in maintaining
    7C/km mid-level lapse rates, and an upstream mid-level
    disturbance (evident via water vapor) was providing ascent aloft
    while moving toward the discussion area. PW values near 1 inch
    and the backbuilding character of convection was supporting
    occasional rain rates exceeding 1 inch/hr in spots that were
    beginning to exceed FFG thresholds on an isolated basis.

    The ongoing scenario should support a localized flash flood threat
    (tied to backbuilding convection) for a few hours this afternoon.=20 Models/CAMs suggest that ongoing activity will eventually pick up
    more of an eastward component of motion while moving toward
    eastern Colorado, supporting isolated flash flood potential
    downstream of ongoing storms especially where mergers/training can
    occur. The downstream airmass is slightly more favorable for
    heavy rainfall given higher PW values (1.5 inch near the KS/CO
    border). Isolated instances of flash flooding are possible in
    this regime.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-8aATgiuNWW-kCAHA4QdqTfVqAfCTbSPQpq_79RUQQx0luKXMfDDZrjx0rdfd58BSlqy= lAwOt8me5lHRWAz4PstURbM$ for graphic product...

    ATTN...WFO...BOU...DDC...GLD...PUB...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39740392 38690193 37090185 37740370 38140532=20
    39520558=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 30 00:29:48 2025
    AWUS01 KWNH 300029
    FFGMPD
    TXZ000-NMZ000-AZZ000-300328-

    Mesoscale Precipitation Discussion 1028
    NWS Weather Prediction Center College Park MD
    829 PM EDT Fri Aug 29 2025

    Areas affected...southern New Mexico, far southeastern Arizona

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

    Valid 300028Z - 300328Z

    Summary...Low-end/isolated flash flood potential continues for a
    few more hours.

    Discussion...Deep convection has materialized over the course of
    the afternoon and produced isolated spots of 1-1.5 inch/hr rain
    rates at times. Short-term trends indicate widespread convective
    overturning that has stabilized the low-level airmass in most
    areas. Despite stabilization, several areas of thunderstorms
    continue across south-central New Mexico (near the Sacramento
    Mountains) and along far northern Mexico (potentially drifting
    northward toward the AZ/NM international border area over the next
    1-2 hours). The pre-convective airmass supporting convection
    continues to be moist and unstable, with 1-1.4 inch PW values and
    500-1000 J/kg MLCAPE to support deep convection and isolated flash
    flood potential.

    With time, low-levels are expected to further stabilize with loss
    of surface heating. The flash flood threat (already isolated)
    should also progressively lower with time as well. Most of the
    threat should wane after 03Z or so.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8PncgyjeCZUkzyhRcMLqq7-naG5LnudJFl3sCWD6hhkJ_PVIguIUh5DdivP0NTdAwjaH= P58-HRYaMY-l4Xjzg_AVFlg$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...TWC...

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 34880638 34060439 32730448 31990655 31780811=20
    31400826 31281094 32101067 32940896 34200780=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 Aug 30 00:33:18 2025
    AWUS01 KWNH 300033
    FFGMPD
    TXZ000-NMZ000-AZZ000-300328-

    Mesoscale Precipitation Discussion 1028
    NWS Weather Prediction Center College Park MD
    832 PM EDT Fri Aug 29 2025

    Areas affected...southern New Mexico, far southeastern Arizona

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

    Valid 300028Z - 300328Z

    Summary...Low-end/isolated flash flood potential continues for a
    few more hours.

    Discussion...Deep convection has materialized over the course of
    the afternoon and produced isolated spots of 1-1.5 inch/hr rain
    rates at times. Short-term trends indicate widespread convective
    overturning that has stabilized the low-level airmass in most
    areas. Despite stabilization, several areas of thunderstorms
    continue across south-central New Mexico (near the Sacramento
    Mountains) and along far northern Mexico (potentially drifting
    northward toward the AZ/NM international border area over the next
    1-2 hours). The pre-convective airmass supporting convection
    continues to be moist and unstable, with 1-1.4 inch PW values and
    500-1000 J/kg MLCAPE to support deep convection and isolated flash
    flood potential. This potential may maximize in/near burn scar
    areas, where just a quick 0.5 inch of rainfall could cause
    excessive runoff.

    With time, low-levels are expected to further stabilize with loss
    of surface heating. The flash flood threat (already isolated)
    should also progressively lower with time as well. Most of the
    threat should wane after 03Z or so.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4_J6q96rSBzK4NCv0FiHpYdhTqeBOL71bsn0rWdiHe79Gmk8bi0IHU_DXLYFoudg5Y14= ZT86U9EPtmodkfozYDTzfGQ$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...TWC...

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 34880638 34060439 32730448 31990655 31780811=20
    31400826 31281094 32101067 32940896 34200780=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 Aug 30 00:47:19 2025
    AWUS01 KWNH 300047
    FFGMPD
    TXZ000-OKZ000-KSZ000-NMZ000-300545-

    Mesoscale Precipitation Discussion 1029
    NWS Weather Prediction Center College Park MD
    846 PM EDT Fri Aug 29 2025

    Areas affected...eastern New Mexico, west Texas, Texas South
    Plains/Panhandle, Oklahoma Panhandle

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

    Valid 300045Z - 300545Z

    Summary...Isolated instances of flash flooding are possible as
    convection emanates eastward from the southern High Plains this
    evening.

    Discussion...Maturing convection over New Mexico has gradually
    organized into clusters and linear segments while approaching the
    NM/TX border region and portions of the Oklahoma Panhandle. The
    storms were moving eastward toward a progressively more moist
    airmass (1.6 inch PW values) and sufficient instability (1500 J/kg
    SBCAPE) to sustain convection for at least 2-4 more hours.=20
    Kinematic fields feature relatively weak steering flow aloft,
    allowing for weak easterly/southeasterly cell movement driven
    partially by local convective organization/evolution. Areas of 1
    inch/hr rain rates are already estimated per MRMS, and the overall
    radar presentation seems to suggest that mergers will gradually
    become more frequent, increasing rain rates locally.

    As cells move eastward deeper into the Texas/Oklahoma Panhandles
    and Texas South Plains, they will migrate over regions of the
    country that have FFG thresholds in the 2-3 inch/hr range (locally
    lower). Furthermore, soil moisture profiles are a bit on the dry
    side, suggestive of soils that can handle some of the impending
    rainfall. The overall scenario suggests potential for isolated
    flash flooding to occur especially in any sensitive/low-lying
    spots. The risk may be locally maximized where mergers can
    prolong heavy rainfall and boost local rain rates.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4bJNTo6H477kWvtLG3ItNZHX_EQn63wiYDKLhK3x4p9w_WBNlKwn6RQ9qZmOj_AWswrF= YRZj9jwT2HlIQrqYwtEk2DY$ for graphic product...

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

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 37050121 36400081 34510129 31910124 31690224=20
    32120330 32890368 33940389 34670445 35820470=20
    36400386 36890223=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 30 05:02:24 2025
    AWUS01 KWNH 300502
    FFGMPD
    TXZ000-NMZ000-300930-

    Mesoscale Precipitation Discussion 1030
    NWS Weather Prediction Center College Park MD
    100 AM EDT Sat Aug 30 2025

    Areas affected...Southeast NM...Western TX

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

    Valid 300500Z - 300930Z

    SUMMARY...Heavy showers and thunderstorms will continue to pose a
    threat for some additional areas of flash flooding overnight.

    DISCUSSION...The latest GOES-W IR satellite imagery shows
    cold-topped convection continuing to evolve across portions of
    southeast NM and western TX. In fact, the trends have shown an
    uptick in convective organization with cooling cloud tops over
    especially southeast NM where radar confirms a couple of
    semi-linear bands of very heavy showers and thunderstorms.

    MLCAPE values of 500 to 1000 J/kg remain in place which coupled
    with subtle mid-level vort energy ejecting east out into the
    southern High Plains is helping to maintain the ongoing convective
    activity. However, cooling boundary layer temperatures and
    convective overturning continue to put pressure on the instability
    environment, and there should be a gradual weakening of the
    overall convective footprint by later in the night.

    PWs of 1.5 to 1.6+ inches are in place which is helping to yield
    heavy rainfall rates of 1 to 2 inches/hour with the stronger
    storms. These heavier rainfall rates coupled with locally slow
    cell-motions and pockets of cell-training may foster some
    additional isolated rainfall totals of 2 to 4+ inches. This is
    supported by the 00Z HREF guidance.

    These additional rains will support a threat for additional areas
    of flash flooding going through the overnight hours. However, by
    later tonight the convection should weaken sufficiently to allow
    for the flash flooding threat to diminish.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9KpuwMqdwZr74y4RUcRsZJXFAyv7EcZCQwACObI4GNhuQ_dKZaUgAh8lt2iam00TmyI9= GKCInVBnmdrLysOEpbb4zUs$ for graphic product...

    ATTN...WFO...ABQ...EPZ...LUB...MAF...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 34740141 34320066 33310052 32230157 31260328=20
    30810485 31110595 31830638 32590601 33330477=20
    33990379 34640259=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 30 13:05:27 2025
    AWUS01 KWNH 301305
    FFGMPD
    LAZ000-TXZ000-301715-

    Mesoscale Precipitation Discussion 1031
    NWS Weather Prediction Center College Park MD
    904 AM EDT Sat Aug 30 2025

    Areas affected...eastern TX into southwestern LA

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

    Valid 301303Z - 301715Z

    SUMMARY...Heavy to extreme rain rates over 3 in/hr are expected to
    occur within localized pockets over portions of eastern TX and
    southwestern LA over the next few hours. Areas of flash flooding
    are likely to continue through 17Z.

    DISCUSSION...1245Z radar imagery over the lower Sabine River
    Valley showed a small cluster of thunderstorms west and northwest
    of LCH with 3 Wunderground observation stations reporting 3+
    inches of rain in an hour two stations showing 5 inches in an hour
    through 12Z. Thunderstorm coverage was expanding NNW from
    southwestern LA into portions of eastern TX along an elevated
    (925-850 mb) convergence axis with low level flow intersecting the
    boundary from the west. Some of the "strongest" low level flow was
    located just south of the DFW Metroplex and over southwestern LA
    with about 10-15 kt oriented nearly perpendicular to the elevated
    convergence axis with mean layer winds directing cells slowly
    toward the southeast. SPC mesoanalysis data from 12Z showed MUCAPE
    values of 500-1500 J/kg coincident with PWATs of 2.1 to 2.3+
    inches.

    Short term forecasts from the RAP show the low level flow
    maintaining over the next few hours but with gradual weakening
    through 17Z which may act to disrupt organization late this
    morning. However, the environment will remain supportive of highly
    efficient rainfall production until then with pockets of extreme
    rain rates possible (3+ in/hr) and localized storm totals in
    excess of 5 inches through 17Z. Areas of flash flooding will be
    likely and trends will be monitored for additional MPDs as needed
    later this morning.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9LLqDy_VP4nvEvj6Oq1-i2fSu0y3E9K-Ehzuz9U53l86YISsyt50n__zjcrr8EX39JmT= SJbnJiW7TMNTNv_Y1ajrm7o$ for graphic product...

    ATTN...WFO...FWD...HGX...LCH...SHV...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 33749671 33139547 31009322 30339289 29939296=20
    29649337 29589393 29769442 30549520 31689627=20
    32679726 33539748=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 30 16:44:30 2025
    AWUS01 KWNH 301644
    FFGMPD
    KSZ000-NEZ000-SDZ000-302215-

    Mesoscale Precipitation Discussion 1032
    NWS Weather Prediction Center College Park MD
    1243 PM EDT Sat Aug 30 2025

    Areas affected...central SD into east-central NE

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

    Valid 301640Z - 302215Z

    SUMMARY...Slow moving cores of heavy rainfall are expected from
    central SD into east-central NE over the next 3-6 hours. Hourly
    rainfall of 1 to 2 inches can be expected at times, which may
    produce a couple of areas of flash flooding.

    DISCUSSION...Water vapor imagery from GOES East showed a complex
    pattern across the central U.S. with a number of mid-level
    vorticity maxima extending from the Dakotas into NE. Upstream, a
    longwave trough axis was noted across WY to the UT/CO border,
    advancing east with small scale vorticity maxima embedded within
    the southwest flow out ahead across the High Plains. Low to
    mid-level analyses showed a nearly stationary low over
    west-central SD, associated with a slow moving cyclonic swirl of
    heavy rain centered over Haakon County with MRMS-derived rainfall
    rates of 1 to 2+ in/hr ending 14 and 15Z, though recent rates have
    lowered to about 1 in/hr. A trough axis extended SSE from the low
    into central NE with widely scattered showers and thunderstorms
    over the NE Sandhills into portions of east-central NE.
    Satellite-derived precipitable water imagery indicated that a
    tongue of higher moisture extended northward through the central
    Plains into central SD, ahead of the quasi-stationary low. OSPO
    LPW imagery showed low level components of this moisture plume
    from the southern Plains and mid to upper level components from
    the Southwest, including remnant moisture from former T.S.
    Juliette in the eastern Pacific. The remnant tropical moisture
    could be a factor in enhancing rainfall efficiency this afternoon.

    As the longwave trough axis passes across the central Rockies this
    afternoon, downstream diffluence will increase over NE and
    southern SD, helping to increase ascent. While the low over SD is
    not expected to move through 22Z, the southern extension of the
    trough into NE should swing east and possibly develop with a
    secondary low center. Mesoscale circulations within this pattern
    are expected to support slow moving cores of heavy rain.

    One negating factor is the presence of weak instability with 16Z
    SPC mesoanalysis data showing only 500-1000 J/kg MLCAPE over parts
    of SD and western NE and less than 500 J/kg over eastern SD/NE.
    Widespread cloud cover may limit the development of higher
    instability over central to eastern SD/NE later this afternoon,
    capping rainfall intensity. However, the favorable moisture axis
    and slow movement of rainfall may still allow for localized
    pockets of 1-2 in/hr rates and possible flash flooding over the
    next 3-5 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9jwKvyGamGIGqHxeg9PdUqiMnAtKNUANn2FMc-ZvOXli28xbL41LCzb9IHB5l7eNkX6G= WVu_d_1Hp8nMZ03GtAqMSts$ for graphic product...

    ATTN...WFO...ABR...FSD...GID...LBF...OAX...UNR...

    ATTN...RFC...KRF...NWC...

    LAT...LON 45730200 45630108 44879969 43389808 41789709=20
    41009706 40149768 39939835 40019874 40279901=20
    40509918 40679930 41209947 41509951 41679949=20
    41799940 41799920 41739899 41679883 41579861=20
    41709841 41729829 41849810 42229811 42369826=20
    42559871 42699978 42950061 43430136 43590166=20
    44300289 45170313 45490274=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 30 17:29:01 2025
    AWUS01 KWNH 301728
    FFGMPD
    TXZ000-302100-

    Mesoscale Precipitation Discussion 1033
    NWS Weather Prediction Center College Park MD
    128 PM EDT Sat Aug 30 2025

    Areas affected...eastern TX into fa

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

    Valid 301726Z - 302100Z

    SUMMARY...Locally high rain rates will likely continue for at
    least another 1-2 hours, possibly extending through 21Z (4 PM CDT)
    for portions of eastern TX. Hourly rainfall of 1 to 2 inches will
    be most likely, though the potential for higher hourly totals in
    excess of 2 to 3 inches will remain a concern.

    DISCUSSION...Localized heavy rain continued over eastern TX as of
    17Z with one cluster over the Piney Woods region and a second a
    little east of Dallas. Convergence along an elevated boundary,
    located in the 925-850 mb layer, was focusing slow moving
    thunderstorms with MRMS-derived hourly rainfall of 2-3 inches
    (Piney Woods) and 1-2 inches (east of Dallas).

    Near Dallas, a 925-850 mb low has formed with slow forecast
    movement toward the east, along with localized low level
    convergence and thunderstorms likely to continue ahead of the low
    track. Meanwhile, RAP forecasts have been consistent with
    near-dissipation of the low level convergence axis that extended
    southeastward from near Dallas into far southwestern LA within the
    next 2-3 hours which should allow for a disruption to the ongoing
    areas of heavy rain over the Piney Woods region..

    However, visible satellite imagery showed growing cumulus along
    the upper TX coast into Montgomery and Liberty counties. Here,
    MLCAPE was estimated to be 1000-2000 J/kg along with 2.1 to 2.4
    inches of precipitable water. A few slow moving thunderstorms are
    likely to develop over the next couple of hours with slow movement
    given weak deeper layer mean flow over central TX to the upper TX
    coast.

    While flash flooding is considered likely in the short term for
    locations farther north, the flash flood threat related to
    expected thunderstorms over the TX Coastal Plain is less certain
    and may remain highly isolated. For these southern areas, the
    greatest flash flood threat will likely setup where overlap occurs
    with nearby urban areas, possibly including the Houston metro.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-H840MKsCSJsq8tXAMNnMy9Y2m50mafY4M9FLn4ANn9GM2yTsayuFXuNG-K0JBZY1XL9= ConEDibHgOKbm47-XpgRldg$ for graphic product...

    ATTN...WFO...FWD...HGX...LCH...OUN...SHV...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 33689635 33419524 32579447 31529388 30529376=20
    30109384 29459420 29129487 28789578 29109599=20
    29719611 30839614 31679632 32259668 32699715=20
    33439715=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 30 18:06:33 2025
    AWUS01 KWNH 301806
    FFGMPD
    TXZ000-NMZ000-310005-

    Mesoscale Precipitation Discussion 1034
    NWS Weather Prediction Center College Park MD
    205 PM EDT Sat Aug 30 2025

    Areas affected...southeastern MM into far western TX

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

    Valid 301805Z - 310005Z

    SUMMARY...Scattered thunderstorms are expected to develop over
    southeastern MM into far western TX over the next few hours. Slow
    movement and brief backbuilding/training will pose a flash flood
    threat from 1-2 in/hr rain rates through 00Z (7 PM CDT).

    DISCUSSION...Visible satellite imagery at 1745Z showed building
    cumulus over the Sacramento Mountains with mostly clear skies
    surrounding much of NM into western TX. Moisture profiles are a
    bit higher for southeastern NM into western TX compared to
    yesterday and the 12Z soundings from ELP and MAF showed PW values
    near the 95th percentile for the end of August. The region resided
    on the northern/northwestern edge of a mid to upper-level ridge
    centered over northern Mexico into TX, with 0-6 km AGL layer winds
    only about 5 kt (slightly weaker into the Big Bend region of TX),
    which will result in slow storm motions.

    Continued heating is expected to allow MLCAPE values to rise into
    the 500-1500 J/kg range by 21Z across southeastern NM and
    southward into western TX. Scattered thunderstorms are expected to
    develop within the areas of higher terrain first, and then advance
    eastward into southern portions of the southern High Plains where
    surface dewpoints ranged from the lower to upper 60s. At the
    surface, winds had an easterly component on the cool side of a
    stationary front which draped westward and then northward through
    far western TX which should add an upslope component to the setup.
    A few areas of flash flooding from 1-2 inches of rain in an hour
    or less will be possible from portions of southeastern NM into the
    Trans Pecos and Big Bend regions of TX through 00Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-yoEGOpjSGKau48O81mHtQRWZ16Pl82ytWBn1UT0fBvWVMhyQgvh1dGejdULdaxz59LF= UQG_Mldsm5Ni4YXuf1h05hg$ for graphic product...

    ATTN...WFO...ABQ...EPZ...LUB...MAF...

    ATTN...RFC...FWR...NWC...

    LAT...LON 34850481 34210342 33390287 31750284 30050267=20
    29100287 29010374 29480473 30520547 31210655=20
    32070690 34390642=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 31 00:49:37 2025
    AWUS01 KWNH 310049
    FFGMPD
    TXZ000-OKZ000-NMZ000-310643-

    Mesoscale Precipitation Discussion 1035
    NWS Weather Prediction Center College Park MD
    848 PM EDT Sat Aug 30 2025

    Areas affected...a large part of west Texas, portions of eastern
    New Mexico, and the Oklahoma Panhandle

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

    Valid 310043Z - 310643Z

    Summary...Isolated flash flood potential exists, although the
    extent of this threat will depend on convective coverage and
    evolution through 06Z/1a CDT.

    Discussion...Isolated to scattered convection continues across the
    discussion area this evening. The greatest concentration of
    storms exists over southwest Texas (near/southwest of Fort
    Stockton), where slow-moving storms have evolved into a linear
    structure/small complex. Additional storms were located near
    Roswell, north of Lubbock, and in the northeastern Texas Panhandle
    near Canadian and Perryton. The cells were in a favorable
    environment for flash flooding, with 1000+ J/kg MLCAPE persisting
    despite a loss of daytime heating. PW values of 1.5 inch (highest
    across eastern portions of the discussion) were also favoring
    heavy rain, while weak steering flow aloft (generally less than 10
    knots) was fostering slow storm motions and local rain rates
    exceeding 1 inch/hr at times. A few of these cells were
    persisting in sensitive terrain (across southwest Texas), while
    others were falling over areas of the Texas South Plains that
    received 2-5 inch rainfall totals last night and have current FFG
    thresholds in the 1-1.5 inch/hr range). Ground conditions are
    somewhat more susceptible to runoff compared to yesterday.

    The overall flash flood threat this evening will depend on the
    coverage of convection over the next 6 hours. Some uptick of
    coverage has been noted over the past hour areawide, although
    sources of forcing for ascent are not obvious per mesoanalyses and
    satellite imagery. Nevertheless, CAMs remain persistent on at
    least isolated coverage of storms, and an isolated flash flood
    risk seems apparent.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9sGj2Jymt3GSqw6dfBiYSgSss8COU6QxHw0xD4XYUToQInKa7_WrjnGGPFyzium1mZZ8= 1iDSHj2vbFGtoyGyi7lRvHg$ for graphic product...

    ATTN...WFO...ABQ...AMA...EPZ...EWX...LUB...MAF...OUN...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 36600140 36519997 34830014 31890104 30660056=20
    30010209 29140332 29590428 30090449 31090422=20
    31970503 32630568 35250531 36480441=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 31 08:03:10 2025
    AWUS01 KWNH 310803
    FFGMPD
    TXZ000-NMZ000-311230-

    Mesoscale Precipitation Discussion 1036
    NWS Weather Prediction Center College Park MD
    401 AM EDT Sun Aug 31 2025

    Areas affected...Eastern NM...Far Western TX

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

    Valid 310800Z - 311230Z

    SUMMARY...Additional broken clusters of heavy showers and
    thunderstorms going through the early morning hours may continue
    to pose an isolated threat for flash flooding.

    DISCUSSION...The latest GOES-W IR satellite imagery along with
    radar shows a few broken clusters of heavy showers and
    thunderstorms continuing to settle gradually down to the south
    across mainly the open plains of eastern NM and a small part of
    western TX.

    The convection is still be driven by a couple of smaller scale
    corridors of favorable moisture convergence along with some
    lingering instability. The latest MUCAPE values across eastern NM
    are still as high as 1000 J/kg in spots. This coupled with some
    modest right-entrance region upper-level jet support may tend to
    sustain these convective clusters at least going into the early
    morning hours.

    Rainfall rates may reach as high as 1.5 inches/hour with the
    stronger storms, and with relatively slow cell-motions, there may
    be a few localized rainfall amounts reaching upwards of 2 to 3
    inches. This may support an isolated threat for some additional
    flash flooding. However, this threat should diminish early this
    morning as the remaining instability continues to wane.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!84GGkr52-rZCCmaNbsroIxBdsH8yuGaSJHrzhwiF5I31zs1L1hUWUxbModLsTgLlukcW= fey-dFtudbowEU-qxIOG7UA$ for graphic product...

    ATTN...WFO...ABQ...EPZ...LUB...MAF...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35060355 34710303 34010270 33000265 32230307=20
    31980407 32250505 32880536 33990527 34630479=20
    34950428=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 31 09:42:13 2025
    AWUS01 KWNH 310942
    FFGMPD
    TXZ000-311540-

    Mesoscale Precipitation Discussion 1037
    NWS Weather Prediction Center College Park MD
    540 AM EDT Sun Aug 31 2025

    Areas affected...Portions of Central and Eastern TX

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

    Valid 310940Z - 311540Z

    SUMMARY...A gradual increase in shower and some thunderstorm
    activity is expected over the next few hours. High rainfall rates
    and concerns for areas of cell-training will pose a threat for
    isolated to scattered areas of flash flooding this morning.

    DISCUSSION...Radar and satellite imagery early this morning is
    showing a gradual increase in shower and thunderstorm activity
    across portions of central and eastern TX. The convection which is
    notably elevated in nature to the north of a stationary front is
    being facilitated by a gradual increase in warm air advection
    along with an uptick in low-level moisture convergence. MUCAPE
    values are on the order of about 500 to 1000 J/kg.

    Some additional expansion of convection is expected going through
    the morning hours as some weakly divergent flow aloft along with
    modestly convergent low-level flow in the 925/850 mb layer
    interacts with the available pool of instability. The environment
    is very moist with PWs of 2.0 to 2.2 inches and this should
    support convection with high rainfall rates capable of reaching
    1.5 to 2.5 inches/hour.

    Rather slow cell-motions given the weak mean layer steering flow
    coupled with the linear nature of some of the elevated convection
    will potentially result in some rather heavy rainfall totals at
    least locally this morning. Areas where any cell-training occurs
    may see as much as 3 to 5 inches of rain given the deep moist
    environment, and these rains will be enough to result in concerns
    for isolated to scattered areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8zTpTjFBN7L4mjThMsnoIdB_NIlWt1QuvRRgKUq6tlJYEOON3rhigTQvGyA1ke4t8Ef5= e4CRMaYrrbKkvYnb3YUHZeU$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...LCH...SHV...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32279631 32229530 31949430 31559393 31059404=20
    30759486 30679595 30709679 30779781 31099921=20
    31599929 31969851 32249729=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 31 16:47:49 2025
    AWUS01 KWNH 311647
    FFGMPD
    TXZ000-312100-

    Mesoscale Precipitation Discussion 1038
    NWS Weather Prediction Center College Park MD
    1246 PM EDT Sun Aug 31 2025

    Areas affected...southeastern TX

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

    Valid 311645Z - 312100Z

    SUMMARY...Isolated, mostly urban, flash flooding will be possible
    across portions of southeastern TX over the next 3-4 hours with
    hourly rainfall of 1 to 3 inches.

    DISCUSSION...Widely scattered showers and thunderstorms were
    beginning to form over the southeastern TX Coastal Plain as of
    1620Z, in advance of a small, forward propagating MCS located in
    the College Station/Huntsville vicinity of southeastern/eastern
    TX. An MCV was apparent near I-45, tracking toward the ESE into an
    instability minimum estimated over east TX. Therefore, there is no
    significant concern of flash flooding for locations near the
    Sabine River which has received heavy rain yesterday. However, the
    strongest convection was located along the southern flank of the
    MCS in the form of a forward propagating linear segment, advancing
    toward the south at roughly 20 kt, into a region containing
    1000-2000 J/kg MLCAPE and 2.3 to 2.5 inch PWATs via 16Z SPC
    mesoanalysis data.

    The unstable environment and mesoscale boundary interactions
    should contribute to at least isolated additional convective
    development between the Gulf Coast and southward advancing line of thunderstorms from the MCS over the next few hours. Deeper layer
    mean winds were quite weak from roughly I-10 and southward, at ~5
    kt, which will contribute to slow cell motions in advance of the
    propagating MCS. There will be an isolated flash flood concern
    where slow moving cells are overtaken by the gradually weakening,
    but still notable, propagating line of thunderstorms where 1 to 3
    inches of rain in an hour will be possible. Overlap of these
    higher rates with urban locations, including the Houston metro,
    may lead to isolated flash flooding through 21Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7PDV2hPP86BUOtrG4Iw8GzA-qLFND4vfN_37s-6oCiNocSyHEHA2oxoIJBTa09UX6zXw= _LGiOTRniZimIUzDsUDydUg$ for graphic product...

    ATTN...WFO...EWX...HGX...LCH...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30739468 29749411 29069466 28649568 28799648=20
    29519697 30129681 30649580=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 31 18:13:48 2025
    AWUS01 KWNH 311813
    FFGMPD
    TXZ000-010012-

    Mesoscale Precipitation Discussion 1039
    NWS Weather Prediction Center College Park MD
    212 PM EDT Sun Aug 31 2025

    Areas affected...portions of central and south Texas

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

    Valid 311812Z - 010012Z

    Summary...Areas of heavy downpours should become more numerous
    while developing southward toward the I-10 corridor and Rio Grande
    Valley through the afternoon. 1-3 inch/hr rain rates may cause a
    few instances of flash flooding through 00Z/7pm CDT.

    Discussion...Per 18Z radar mosaic imagery, scattered showers and
    thunderstorms were ongoing and focused along a couple of axes - 1)
    along a weak stationary surface front extending from near Fort
    Stockton eastward to near Llano that intersects with 2) an outflow
    boundary from Llano southeastward to near Houston. The cells
    along these boundaries were forming due to abundant surface
    heating and convergence. The cells were also in an abundantly
    moist (1.8+ PW) and unstable (1000+ J/kg) environment, supporting
    robust updrafts and efficient rainfall rates. Recent MRMS imagery
    estimated spots of 1-3 inch/hr rain rates near Brady and San Saba
    (east of San Angelo), and a couple spots of FFG exceedence have
    already been noted in that area. These trends aren't a particular
    surprise given the moisture profiles and weak steering flow aloft,
    favoring slow storm motions.

    Both models and observations depict a gradual increase in coverage
    of storms through the afternoon and early evening. The increase
    in convective coverage should promote eventual clusters of storms
    that slowly propagate southward - especially across central Texas
    and vicinity. Rain rates exceeding 1 inch/hr should become
    common, and localized spots of 2-3 inch/hr rain rates should
    materialize while locally exceeding areal FFG thresholds.

    Given the aforementioned scenario, a few instances of flash
    flooding are expected - especially as storms migrate through the
    Hill Country and urbanized areas near Austin and San Antonio.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_uSGoX9_KCWvAtbQO0ebifGTpb-DfUyJGf9YKQ53XGuoCDXKVahQfFMWT1R8tCgrnOek= gR9xUCgsjFp_FRuCRZKwpDk$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32319910 31699771 30499665 29409672 28869822=20
    28930060 29820170 29750330 30040379 30830342=20
    31510192=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Aug 31 18:17:18 2025
    AWUS01 KWNH 311817
    FFGMPD
    TXZ000-NMZ000-AZZ000-010015-

    Mesoscale Precipitation Discussion 1040
    NWS Weather Prediction Center College Park MD
    216 PM EDT Sun Aug 31 2025

    Areas affected...far western TX into central to southwestern NM
    and southeastern AZ

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

    Valid 311815Z - 010015Z

    SUMMARY...Thunderstorms will pose an isolated to scattered flash
    flood threat across portions of far western TX into central to
    southwestern NM and southeastern AZ through 00Z. Storms should be
    disorganized in nature, but some slow movement and brief training
    will carry a threat for 1-2 in/hr rain rates.

    DISCUSSION...Visible satellite and radar imagery at 18Z showed a
    gradual uptick in the coverage of thunderstorms, tied to the
    diurnal cycle, over the southwestern quadrant of NM. Mostly clear
    skies and anomalous moisture (12Z EPZ sounding with a PW of 1.3
    inches, just above the 90th percentile for the end of August) was
    contributing to a bubble of higher instability from near El Paso
    into southwestern NM with 500 to 1500+ J/kg MLCAPE shown on the
    18Z SPC mesoanalysis page. Moisture values were closer to average
    for northern NM and into western AZ.

    A 700-500 mb ridge was centered over the AZ/NM border with
    easterly low level flow located from far western TX into southern
    NM and this pattern will maintain through the late evening. A
    small region of weak deeper layer mean winds was located over
    south-central TX with (<10 kt 0-6 km) with 10-15 kt located
    elsewhere. Continued heating and moisture advection into
    southeastern AZ should allow for an expansion of instability with
    500-1500 J/kg becoming widespread across southwestern NM into
    southeastern AZ by 21-00Z. Low level easterly winds should cause
    an increase in low level moisture and instability into
    southeastern AZ by late this afternoon with thunderstorms either
    moving into or developing over southeastern AZ. Some thunderstorms
    will carry the potential for brief training along with slow
    movement, supportive of 1-2 in/hr rain rates. At least an isolated
    threat of flash flooding may continue beyond 00Z within lingering
    instability but the flash flood threat is expected to begin to
    wane after sunset.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4FB4A-G_uJXn_4vF618PbD-HzSbqiloOX0B5-1YanIYCJp0Vu6swWV2DPzPbuT7xm07v= EDpG6RBn0U2e2ROgtoOmr3g$ for graphic product...

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

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 34840748 34660549 33920502 32410525 31410603=20
    31320750 31030917 31341101 33500982 34340905=20
    34670834=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 1 00:07:23 2025
    AWUS01 KWNH 010007
    FFGMPD
    TXZ000-NMZ000-010430-

    Mesoscale Precipitation Discussion 1041
    NWS Weather Prediction Center College Park MD
    806 PM EDT Sun Aug 31 2025

    Areas affected...portions of south and west Texas

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

    Valid 010006Z - 010430Z

    Summary...Flash flood potential should linger for a few more hours
    - especially where instability continues to support new,
    slow-moving convection.

    Discussion...Earlier convection across central Texas and the Hill
    Country has evolved into a slow-moving complex currently near the
    San Antonio Metro area. Enough downstream instability exists for
    cells to continue to produce areas of 1-2 inch/hr rain rates.=20
    These cells will continue to move southward over the next couple
    hours while producing locally heavy rainfall over urbanized areas.
    Excessive runoff/flash flood potential remains a distinct
    possibility with this activity through 02Z/9p CDT.

    Upstream, a large area of relatively stable air as developed
    across the Hill Country due to prior convection. A few areas
    farther west (from near Midland southward to the Big Bend area)
    have still yet to stabilize, however, and deep, slow-moving
    convection continues to exhibit an uptick per radar mosaic and
    satellite imagery. Areas of 1-2 inch/hr rain rates remain likely
    beneath the stronger and more persistent convection, and these
    rates should threaten local FFG thresholds that are as low as
    1-1.5 inch/hr. Isolated flash flood potential continues -
    especially in low-lying/sensitive areas.

    Eventually, storms should exhibit a slow weakening trend with loss
    of surface heating, although weak/subtle mid-level waves should
    provide enough ascent for locally heavy rainfall to persist
    perhaps through 05Z/midnight CDT. where convective overturning has
    not led to low-level stabilization.

    Flash flooding remains possible across the area through 04-05Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_GLJXiunUX-ITyF353IcS69a7KavcWCvu-jriG0IDE6rllJBXybg_DSjV0ixnLnC9wRI= xSZOHmUvgdOQVuJaUm7HRFc$ for graphic product...

    ATTN...WFO...CRP...EWX...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32080276 31760178 30830060 30029904 29749730=20
    28869750 28439976 28820068 29670205 29590288=20
    29880397 30980453 31840402=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 1 02:28:25 2025
    AWUS01 KWNH 010228
    FFGMPD
    TXZ000-OKZ000-010630-

    Mesoscale Precipitation Discussion 1042
    NWS Weather Prediction Center College Park MD
    1027 PM EDT Sun Aug 31 2025

    Areas affected...Far Southern OK...North-Central TX

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

    Valid 010227Z - 010630Z

    SUMMARY...Additional slow-moving and locally training areas of
    heavy showers and thunderstorms are expected to continue through
    midnight across portions of southern OK and north-central TX,
    including portions of the Dallas-Fort Worth metropolitan area.
    Urban flash flooding in particular will continue to be a concern
    in the near-term.

    DISCUSSION...The latest radar imagery shows slow-moving clusters
    of heavy showers and thunderstorms across portions of far southern
    OK and north-central TX, including the Dallas-Fort Worth
    metropolitan area where more recently there has been some
    cell-training noted along with reports of flash flooding.

    The convection is largely being driven by proximity of a weak area
    of low pressure and a surface trough which is helping to focus
    small scale areas of favorable low-level moisture convergence
    within a moderately unstable airmass characterized by MLCAPE
    values of 1000 to 1500 J/kg. PWs are generally on the order of
    1.75 to 2 inches, which coupled with the instability is helping to
    drive rainfall rates of up to 2 to 3 inches/hour with the stronger
    storms.

    Some of the 18Z HREF and recent HRRR guidance suggests some
    localized persistence of the convective threat going through
    midnight, with locally an additional 3 to 4 inches of rain
    possible in close proximity to this weak area of low pressure
    which is nearly stationary.

    As a result, additional areas of flash flooding will be possible
    over the next few hours, and especially for the urban corridors
    around the Dallas-Fort Worth metropolitan area.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6ERzaNTAHLFG5BlVXLZDSF835s0mhsyLYw_r0JLHuGzhacm85Jt-ayEMJqOmPp8fXKqR= xpfumN8ed_QfgVnEXw2HyXc$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 34479577 34029533 33039544 32279617 32219710=20
    32629778 33609801 34259755 34339663=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 1 07:02:11 2025
    AWUS01 KWNH 010654
    FFGMPD
    IAZ000-NEZ000-011245-

    Mesoscale Precipitation Discussion 1043
    NWS Weather Prediction Center College Park MD
    252 AM EDT Mon Sep 01 2025

    Areas affected...Eastern NE

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

    Valid 010652Z - 011245Z

    SUMMARY...A couple of slow-moving and locally training bands of
    heavy showers are expected over eastern NE going through dawn.
    Some areas of flash flooding will be possible.

    DISCUSSION...The latest GOES-E WV suite shows a somewhat elongated
    mid-level trough axis over the central Plains, with a couple of
    embedded compact vort centers. One such vort center is nearly
    stationary over eastern NE and has been fostering an uptick in
    heavy shower activity over the last 1 to 2 hours.

    The cloud tops with this convection are relatively warm/shallow
    and suggestive of a warm rain environment that will be conducive
    for more efficient rainfall processes for elevated rainfall rates.

    On a small scale, there is a favorable corridor moisture
    convergence wrapping up around the eastern flank of the vort
    center, with an environment that is only modestly unstable. In
    fact, the MUCAPE values are only about 500 J/kg.

    Regardless, there is sufficient mid-level forcing/ascent working
    in tandem with the low-level south to southeast flow and
    instability for the convection to initiate and locally expand in
    coverage. Some additional nocturnal contraction/tightening of the
    low to mid-level circulation is expected over the next few hours
    and this may help to further concentrate these smaller scale bands
    of shallow-topped convection.

    The rainfall rates will be capable of reaching 1 to 2 inches/hour
    given the efficient environment, and with slow cell-motions and
    cell-training concerns, some rainfall totals going through dawn
    may reach as high as 3 to 4+ inches. The HRRR guidance is trending
    gradually wetter across eastern NE, and the radar and satellite
    trends would tend to favor these locally heavier totals
    materializing.

    Some areas of flash flooding will be possible across eastern NE
    given these rains. However, the antecedent conditions are quite
    dry, so the overall flash flooding threat should tend to be
    isolated and confined to where any cell-training occurs.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4V3pimRcGExDSSqfIuNmbuBbB6uIO1yFUN-onu0tuzdUWBJIv9PJHIO0YC7mOsGalnIt= HAY6XlJObvvBCBvKEixxMwE$ for graphic product...

    ATTN...WFO...FSD...GID...OAX...

    ATTN...RFC...KRF...NWC...

    LAT...LON 42519678 42329640 41989608 41059604 40219662=20
    40029759 40379782 40979744 41449734 41859727=20
    42349727=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 3 20:26:42 2025
    AWUS01 KWNH 032026
    FFGMPD
    AZZ000-UTZ000-NVZ000-040200-

    Mesoscale Precipitation Discussion 1044
    NWS Weather Prediction Center College Park MD
    426 PM EDT Wed Sep 03 2025

    Areas affected...much of northern AZ into southern NV and
    southwest UT

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

    Valid 032025Z - 040200Z

    Summary...Sub-hourly (15-30 min) rainfall of 1"+ with short-term
    totals of 1.5-2.5" may result in localized/isolated instances of
    flash flooding.

    Discussion...Complex upper-level pattern (slow moving
    trough/closed low to the west with poleward advancement of
    Hurricane Lorena to the south resulting in enhanced upper-level
    diffluence in left-exit region of sub-tropical jet streak)
    combined with anomalous tropospheric moisture content (at or near
    90th percetile) is resulting in a favorable environment for heavy
    rainfall across the greater AZ/NV/NM border region. Convection is
    initiating and proliferating in the vicinity of the higher terrain
    of the Mogollon Rim and Grand Canyon region (where the best low-
    to mid-level moisture is overlapping with upper-level moisture,
    per CIRA ALPW imagery). MRMS is indicating high instantaneous
    rainfall rates (2"+/hr) with initial downdrafts, resulting in
    sub-hourly (15-30 min) localized accumulations of 1"+.

    As convection continues to proliferate and move relatively slowly
    (~10 kts) towards the north-northwest with mean 850-300 mb flow,
    cells may locally train to result in localized short-term totals
    of 1.5-2.5" (supported by HREF and experimental RRFS neighborhood
    probabilities for 1" and 2" exceedance). While these higher
    localized totals are most likely in the vicinity of the higher
    terrain, the influence of upper-level dynamics may be enough to
    support updrafts beyond the typical pulse convection life cycle as
    they drift northward. Isolated/localized instances of flash
    flooding will be possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-CgLUwbUCk-Q701BInwzrz1V5k5eT7UICoZ_2V0MvKB4lSy7FZT4Ukf_zt27CarWQ71U= f5ipgi1gohLdkgNfoqtpJAE$ for graphic product...

    ATTN...WFO...FGZ...GJT...LKN...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 39121195 38381138 37911132 37491128 37211104=20
    37191067 37121031 36860999 36590964 36230947=20
    35730956 35590991 35591017 35411027 35161042=20
    34641028 34351048 34251099 34261152 34221195=20
    34251243 34481290 34871342 34901402 35371455=20
    35941515 36191566 36611588 37131599 37461630=20
    37221699 37851717 38411671 38341529 38781497=20
    38891414 38791283=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 4 08:39:52 2025
    AWUS01 KWNH 040839
    FFGMPD
    TNZ000-KYZ000-041338-

    Mesoscale Precipitation Discussion 1045
    NWS Weather Prediction Center College Park MD
    439 AM EDT Thu Sep 04 2025

    Areas affected...portions of Kentucky

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

    Valid 040838Z - 041338Z

    Summary...A few spots of 1-2 inch/hr rain rates have materialized
    near/east of Owensboro over the past hour. Isolated flash flood
    potential could materialize as the convection reaches
    central/eastern portions of the state.

    Discussion...Latest radar mosaic imagery depicts areas of training
    convection across northern Kentucky near/east of Owensboro.=20
    Localized training has led to rain rates exceeding 2 inches/per
    (estimated per MRMS). The training storms have materialized amid
    strong forcing aloft, with vigorous mid-level waves rotating
    through the base of a larger-scale trough over Indiana and
    Illinois. Furthermore, strong 850mb flow has maintained enough
    low-level flux of moisture/instability into the region to maintain
    around 500 J/kg MLCAPE amid low 60s F dewpoints. The orientation
    of convergence and cell development (with storms repeatedly
    deepening along a surface front near Owensboro and moving quickly
    eastward) is favoring areas of training.

    The axis of heaviest rainfall is occurring over relatively dry
    ground conditions from a lack of rain over the past couple weeks.
    Eventually, training convection will reach areas of eastern
    Kentucky that have been wetter and are more susceptible to flash
    flooding. Instability profiles are expected to gradually
    destabilize downstream (per RAP/SPC mesoanalyses), which should
    maintain convection downstream while providing opportunity for
    continued training and spots of 1-2 inch/hr rain rates. These
    rates may exceed FFG thresholds on a localized basis, providing a
    brief window for isolated flash flooding through 13Z/9a EDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4PfDzxgmbur0cI0aCVnOyKznsahmvM4kLSvgTRWwOAIyLcsaBg9jmazPZykY-l8cgBqo= 770ZI9eZbWvJmUmdWhnV7BA$ for graphic product...

    ATTN...WFO...JKL...LMK...MRX...

    ATTN...RFC...TIR...NWC...

    LAT...LON 38168424 37908306 37228262 36588439 37008639=20
    38138586=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 4 21:31:29 2025
    AWUS01 KWNH 042131
    FFGMPD
    AZZ000-NVZ000-CAZ000-050330-

    Mesoscale Precipitation Discussion 1046
    NWS Weather Prediction Center College Park MD
    529 PM EDT Thu Sep 04 2025

    Areas affected...much of AZ into adjacent portions southern CA/NV

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

    Valid 042130Z - 050330Z

    Summary...Isolated to scattered instances of flash flooding likely
    through the evening with the highest localized totals (2-4"
    amounts over 3-6 hour period) most likely from far southeastern CA
    into southwest and south-central AZ.

    Discussion...Monsoonally-driven diurnal convection is once again
    proliferating across much of the Southwest this afternoon, fueled
    by anomalously high tropospheric moisture content (PWs ranging
    from 0.8" in higher terrain to 1.9" in the low deserts, generally
    between the 90th percentile and max moving average per FGZ, TUS,
    VEF, PHX, and YUM sounding climatology) and ample instability
    (SBCAPE of 500-3500 J/kg with SBCIN nearly completely eroded).
    While convective initiation has largely focused on the higher
    elevations, widely scattered cells are also beginning to fire
    across the lower deserts of CA/AZ as well. Upper-level support for
    convective organization beyond pulse cells is mixed overall, as a
    weak upper-level trough axis (base near the AZ/NV border) is
    moderately supportive (via weak DPVA enhancing lift) while a
    modestly strengthening sub-tropical jet streak (to ~90 kts at 200
    mb by 00z) is unideally positioned with the left-entrance over AZ
    (supressing broad lift overall).

    Regardless of larger convective organization, locally heavy
    downpours (MRMS indicating instantaneous rainfall rates of 2"+
    with 15-min rainfall approaching 1" in association with pulse
    convection) will drive an isolated to widely scattered flash flood
    threat in the near term (and increasing shear could help
    prolong/intensify pulse cells). Increasing coverage of pulse
    convection will likely drive continued development of new cells
    via boundary collisions and mergers, potentially resulting in more
    substantial convective organization (i.e. training/repeating
    cells) across far southeastern CA into southwest and south-central
    AZ over the next 3-6 hours (where 12z hi-res CAMs suggest the
    potential for 2-4" localized totals). Isolated to scattered
    instances of flash flooding are likely.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4NRRKvkAeQSuldYTOgFwr9dC-kpUI1VoTeloEbDrBp9LIkJUF5bcBRA5EwwMywVoo_F4= fn7gJJAeHBWVnyH7-yqlg0Q$ for graphic product...

    ATTN...WFO...FGZ...PSR...SGX...TWC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 36891177 36821141 36521134 36201132 35821112=20
    35351093 35121057 34740999 34660949 34400926=20
    33780924 33300936 33000953 32800973 32331024=20
    31971044 31511076 31311113 31471192 32001353=20
    32541510 32501644 32871668 33401686 33971699=20
    34311681 34411586 34941577 35601584 36151596=20
    36531582 36671505 36281458 36101426 36031375=20
    36001336 36131296 36371253 36481233 36751201=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 5 08:31:40 2025
    AWUS01 KWNH 050831
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-051229-

    Mesoscale Precipitation Discussion 1047
    NWS Weather Prediction Center College Park MD
    430 AM EDT Fri Sep 05 2025

    Areas affected...southern Nevada, western Arizona

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

    Valid 050829Z - 051229Z

    Summary...A convective complex should move southward along the
    Lower Colorado River Valley for the next few hours. Spots of 1
    inch/hr rain rates were prompting flash flood concerns, and these
    trends may continue through 12Z/6a MDT/5a PDT.

    Discussion...A convective complex has gained organization across
    southeastern Nevada this morning. It is currently propagating
    southward along a moist/unstable axis (1.25+ PW, 500+ J/kg MLCAPE)
    that exists along the immediate Lower Colorado River Valley, which
    was likely supporting continued and robust updraft development
    along the leading edge of the complex. Ascent from stout
    mid-level waves over Utah was also supporting convection, and SPC
    mesoanalyses were also suggesting modest enhancement of
    low-level/850mb flow/flux into the complex, also supporting its
    organization. Spots of 1-1.25 inch/hr rain rates were being
    estimated per MRMS, which was readily exceeding FFG thresholds
    across the area. At least isolated flash flood concerns are
    likely between Las Vegas, Mesquite, and along the NV/AZ border in
    the near term.

    Each of the aforementioned atmospheric factors supporting
    organization will also likely support its persistent for a few
    hours this morning. Localized flash flooding is expected with the
    complex as it migrates southward from I-15 through Bullhead City
    and Kingman, AZ. Southward persistence beyond that area is
    possible, and portions of the CA/AZ border region near Lake Havasu
    City may also experience a flash flood threat later this morning
    (around 10-11Z). Lastly, westward backbuilding into the Las Vegas
    metro area (supporting urban flash flood potential) cannot be
    completely ruled out.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9M0eCtUf_hSQGiWe83-1wxMlDWeeHf8xqJbc-4i4gPwcj-av8cQt7S4SlyBHFkagpNiT= HoRq-TVWoxLzKgAxXrEVKnY$ for graphic product...

    ATTN...WFO...FGZ...PSR...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 37221598 37091383 36621272 34581256 33721353=20
    33721499 34721569 36301625=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 5 08:34:37 2025
    AWUS01 KWNH 050834
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-051229-

    Mesoscale Precipitation Discussion 1047
    NWS Weather Prediction Center College Park MD
    434 AM EDT Fri Sep 05 2025

    Areas affected...southern Nevada, western Arizona

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

    Valid 050829Z - 051229Z

    Summary...A convective complex should move southward along the
    Lower Colorado River Valley for the next few hours. Spots of 1
    inch/hr rain rates were prompting flash flood concerns, and these
    trends may continue through 12Z/6a MDT/5a PDT.

    Discussion...A convective complex has gained organization across
    southeastern Nevada this morning. It is currently propagating
    southward along a moist/unstable axis (1.25+ PW, 500+ J/kg MLCAPE)
    that exists along the immediate Lower Colorado River Valley, which
    was likely supporting continued and robust updraft development
    along the leading edge of the complex. Ascent from stout
    mid-level waves over Utah was also supporting convection, and SPC
    mesoanalyses were also suggesting modest enhancement of
    low-level/850mb flow/flux into the complex, also supporting its
    organization. Spots of 1-1.25 inch/hr rain rates were being
    estimated per MRMS, which was readily exceeding FFG thresholds
    across the area. At least isolated flash flood concerns are
    likely between Las Vegas, Mesquite, and along the NV/AZ border in
    the near term.

    Each of the aforementioned atmospheric factors supporting
    organization will also likely support its persistence for a few
    hours this morning. Localized flash flooding is expected with the
    complex as it migrates southward from I-15 through Bullhead City
    and Kingman, AZ. Southward persistence beyond that area is
    possible, and portions of the CA/AZ border region near Lake Havasu
    City may also experience a flash flood threat later this morning
    (around 10-11Z). Lastly, westward backbuilding into the Las Vegas
    metro area (supporting urban flash flood potential) cannot be
    completely ruled out.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-_tgIwc_uHeHqcr05UVfy1D_JonvcStOwvKTKr9Xd2OLfw-Jm4Rc6asiP7DnF--xDtmP= u1NgpcNzRuLqPyMBHcFFUxg$ for graphic product...

    ATTN...WFO...FGZ...PSR...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 37221598 37091383 36621272 34581256 33721353=20
    33721499 34721569 36301625=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 5 12:31:12 2025
    AWUS01 KWNH 051231
    FFGMPD
    AZZ000-NVZ000-CAZ000-051630-

    Mesoscale Precipitation Discussion 1048
    NWS Weather Prediction Center College Park MD
    830 AM EDT Fri Sep 05 2025

    Areas affected...Lower Colorado River Valley (Western Arizona, Adj California)...

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

    Valid 051230Z - 051630Z

    SUMMARY...Localized flash flooding threat continues downstream of
    slowly weakening MCS/convective clusters within the Lower Colorado
    River Valley.=20

    DISCUSSION...KESX and GOES-W 10.3um EIR show shrinking convective
    complex has had a resent uptick in convective vigor across central
    Mohave county. There was a typical weakening trend toward diurnal
    minimum, but the leading outflow boundary (combined with
    reinforcement from the northeastern dying convection) increased
    surface to boundary layer convergence as the cluster was reaching
    the nose of the Lower Colorado Valley where lingering unmixed,
    conditionally unstable air has been sitting through the overnight
    period. MUCIN has been below 25 J/kg and with some southerly weak
    flow intersecting the 30-45kt outflow has been sufficient to
    reactivate and break through the cap tapping some of the steeper
    profiles and 1500-2000 J/kg of ML/MUCAPE. Combine that with
    deeper available moisture in lowering elevation and inflow will
    continue to support intense sub-hourly rates and localized 1-1.25"
    totals.

    Most of the Hi-Res CAMs have been traditionally slow to the
    forward propagation of the cluster, reducing the moisture
    convergence but also delaying arrival to the reservoir of unstable
    air further south and have shown the erosion faster. However,
    recent RRFS solutions; though still too slow to reality of timing,
    do suggest continued southward propagation and longevity through
    the next few hours. Still, like any conditionally unstable air,
    the updraft strength will require the outflow's convergence to
    maintain, but current trends suggest this cluster may continue for
    a few more hours and the strength of rates will continue to pose
    sub-hourly FFG exceedance and localized flash flooding conditions
    along dry washes across the Lower Colorado Valley, mainly east of
    the River in Arizona.

    Of interest, but perhaps not reaching intensity required for
    inducing flash flooding; the rear-inflow jet continues to respond
    from NW to SE across south-central NV. Convergence along the
    western upstream edge has been similarly sufficient to tap the
    steeper mid-level lapse rates for scattered cells. These cells
    have favorable orientation for some weak training/repeating; but
    also are fairly elevated that evaporative loss may still keep
    overall rates/totals just below levels to produce flash flooding,
    except if they maintain/track through areas that received heavy
    rainfall overnight.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8aPH7a1SVnnQEXE9GCnjMwylxvLwnt0T0egP5wxPxB5Ft58ySvQIttC0BDGuTShqMw0b= v46Xr-E3SHgdw7QxcB1nyFY$ for graphic product...

    ATTN...WFO...FGZ...PSR...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 35521375 35161322 34481290 33541266 33011326=20
    33041421 33401453 34221475 34751481 35271456=20
    35501422=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 5 18:51:15 2025
    AWUS01 KWNH 051851
    FFGMPD
    COZ000-NMZ000-060045-

    Mesoscale Precipitation Discussion 1049
    NWS Weather Prediction Center College Park MD
    250 PM EDT Fri Sep 05 2025

    Areas affected...Northern NM & Southern CO

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

    Valid 051850Z - 060045Z

    SUMMARY...Scattered thunderstorms containing locally Excessive
    Rainfall rates may result in flash flooding, especially along
    sensitive and rugged terrain.

    DISCUSSION...A broad and weak positively-tilted 200-500mb trough
    axis is located over the Four Corners region and providing some
    minor upper-level ascent aloft. Meanwhile, a cold front is
    tracking south and east through the southern High Plains and into
    the Front Range of the Rockies. There is some modest ENE low-level
    flow in wake of the front that is advecting additional moisture
    into the region, evident in RTMA 6-hr dew point changes that are
    anywhere from 2-8F higher over eastern NM. In the mid-upper
    levels, guidance shows a moist 700-400mb column over southern CO
    and into northern NM that is helping to raise low-level RH values
    above 80%. This has led to PWATs that are ranging between
    0.75-1.0" which are encroaching upon the 90th climatological
    percentile. Visible satellite imagery also shows most areas west
    of the Continental Divide have witnessed modest surface-based
    heating that is supporting 500-1,000 J/kg of SBCAPE per RAP
    mesoanalysis. These ingredients are fostering a favorable
    environment for rounds of thunderstorms to develop within a moist
    and unstable environment that could result in flash flooding this
    afternoon.

    In terms of antecedent soil moisture conditions, NASA SPoRT-LIS
    shows 0-40cm soil moisture guidance has spotty areas of >90th soil
    moisture percentiles along the Sangre De Cristo Mountains on south
    to the Sacramento Mountains. Some areas are drier and the
    thunderstorms will generally provide beneficial rainfall, but
    between sensitive soils that are saturated in the higher terrain
    and nearby burn scars, there is a chance these thunderstorms that
    could generate >1"/hr rainfall rates may result in localized flash
    flooding through the early evening hours.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4C4Fe8D4q_beQF3kVNdF4_drAWRz6q3Y7D0rdDM9HAufUndX_S5UC7BxKRZIg2EhOVCX= X_oQM2OesLxu4Hxs3GuCONM$ for graphic product...

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

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 37790671 37710581 37130505 35890461 34720475=20
    33550522 33500588 33880628 34670638 35470629=20
    35570681 34990747 34920791 35170855 35820866=20
    37230873 37720843=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 5 21:52:48 2025
    AWUS01 KWNH 052152
    FFGMPD
    UTZ000-NVZ000-CAZ000-060345-

    Mesoscale Precipitation Discussion 1050
    NWS Weather Prediction Center College Park MD
    551 PM EDT Fri Sep 05 2025

    Areas affected...Great Basin & Southwest UT

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

    Valid 052150Z - 060345Z

    SUMMARY...Numerous thunderstorms capable of producing rainfall
    rates around 1"/hr in some cases may lead to additional areas of
    flash flooding.

    DISCUSSION...A negatively titled 250mb trough over central
    California is providing modest upper-level ascent over the
    southern Sierra Nevada and Great Basin this afternoon. GOES-19
    satellite imagery shows cooling cloud tops aloft as storms tap
    into as much as 500 J/kg of MLCAPE per RAP mesoanalysis. In
    addition, PWATs are unusually high across the region, topping
    0.75" for most areas and thus placing these PWAT values above the
    90th climatological percentile. PWATs are closer to 1" in southern
    NV and southwest UT. Given the initially strong surface based
    heating and synoptic-scale support from the approaching 250mb
    trough axis, look for storms to continue into this evening as
    emanating outflow boundaries kick-start new storms within the
    highlighted region. The available PWATs and MLCAPE should support
    maximum hourly rainfall rates around 1"/hr in the most intense
    storms. NASA SPoRT-LIS does show some parts of western Nevada and
    the eastern slopes of the Sierra Nevada featuring >90th percentile
    soil moisture values, so some soils may be rather sensitive to
    these heavier rainfall rates. Additional flash flooding is
    possible, especially in dry washes and areas with poor drainage.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5c7JB5z5XzZgrfBr-3Resna_Nd1fz-OY-bnCUpGC6iQjuQUM_OkWmeOqi3-KL2mXQ7ZO= FZneN8XdNPBQSSwIn3hpZos$ for graphic product...

    ATTN...WFO...LKN...REV...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 41241863 40851733 40321599 39231446 38931324=20
    38691228 38231182 37351191 37231318 37261432=20
    36851583 37051700 37151812 37891890 38531925=20
    39721955 40901951=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 6 03:38:23 2025
    AWUS01 KWNH 060338
    FFGMPD
    AZZ000-UTZ000-NVZ000-060936-

    Mesoscale Precipitation Discussion 1051
    NWS Weather Prediction Center College Park MD
    1137 PM EDT Fri Sep 05 2025

    Areas affected...southern/southeastern Nevada, far northwestern
    Arizona

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

    Valid 060336Z - 060936Z

    Summary...Flash flooding remains possible along a stalling
    boundary in the discussion area through 09Z/3a MDT.

    Discussion...Scattered thunderstorms were forming along a stalled
    low-level boundary extending from just north of Beatty to just
    north of Las Vegas to near Mesquite. The downstream,
    pre-convective airmass supporting storms is relatively moist and
    unstable, with 1+ inch PW values and 1500 J/kg MLCAPE noted amid
    8+ C/km mid-level lapse rates. 850mb flow fields (per SPC
    mesoanalysis) continue to depict a slight enhancement to southerly
    low-level flow (approaching 20 knots) perpendicular to the
    low-level boundary, sustaining updrafts and heavy rainfall. A few
    spots of 1 inch/hr rain rates are occurring. These rates exceed
    local FFG across the region and are potentially contributing to
    excessive runoff.

    The overall pattern will evolve slowly through the night, with
    sustained convergence expected to continue firing convection
    through 09Z. The slow movement and wetting nature of the storms
    should continue to promote flash flood potential on at least an
    isolated basis during that time. Mesoscale/convective evolution
    should result in small displacements in the boundary, and a drift
    toward the Las Vegas metro and adjacent areas of far northwestern
    Arizona cannot be ruled out. Flash flooding is possible in each
    of these areas, with local rainfall amounts of 2 inches expected.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4EoZjh7ViPJAN2skEFb2luhDp8pzSJ-rWKmvuxyaVK_V-dhvyDa-s7rTpiOzg3sn_c3e= yTOdMsgohMNgUMMjQ_YXmo8$ for graphic product...

    ATTN...WFO...FGZ...LKN...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 38561744 37751445 36271328 35091363 36261607=20
    37531759=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 6 03:58:52 2025
    AWUS01 KWNH 060358
    FFGMPD
    ARZ000-TXZ000-OKZ000-060657-

    Mesoscale Precipitation Discussion 1052
    NWS Weather Prediction Center College Park MD
    1158 PM EDT Fri Sep 05 2025

    Areas affected...southern/central Arkansas

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

    Valid 060357Z - 060657Z

    Summary...Isolated flash flooding is possible with thunderstorm
    activity moving eastward across the discussion area.

    Discussion...Recent radar mosaic imagery depicts a cluster of
    rapidly deepening convection over southwestern Arkansas near
    DeQueen forming just ahead of an eastward-propagating complex over
    McCurtain County, OK. The cluster of cells in southwestern
    Arkansas was moving slowly, with rain rates beginning to eclipse 1
    inch/hr in spots. Additionally, incoming rainfall from
    southeastern Oklahoma should result in another quick 0.5-1 inch of
    rainfall, resulting in local amounts of 2-3 inches in a short
    amount of time.

    These rain rates are falling on areas that have been relatively
    dry, with FFG thresholds hovering around 2-3 inches/hr. Flash
    flooding could occur on an isolated basis given the scenario, with low-lying/susceptible areas posing the greatest concern.

    The downstream airmass is supportive of continued convection, with
    steep lapse rates aloft (7C/km) supporting areas of 3000+ J/kg
    MLCAPE along and south of a surface boundary in southern Arkansas.
    PW values are also around 1.6+ inch. This airmass and
    convergence along/just north of the boundary should continue to
    support heavy rainfall as storms move/propagate eastward.

    Given the aforementioned scenario, isolated instances of flash
    flood potential are possible as spots of 1-2 inch/hr rain rates
    spread through central Arkansas. Local amounts of 3 inch totals
    are also possible through 08Z/3a CDT

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5brhvbclcIznn8ArH4epTp7q-VBoYUQqu52wAc_Ru7vMIshrLPksY1nfz_ULeuEboSDo= MHx5_3gil5ZEJ15g540eDEk$ for graphic product...

    ATTN...WFO...LZK...SHV...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 34869154 33599149 33399355 33719452 34689430=20
    34739325=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 6 09:32:27 2025
    AWUS01 KWNH 060932
    FFGMPD
    AZZ000-NVZ000-CAZ000-061330-

    Mesoscale Precipitation Discussion 1053
    NWS Weather Prediction Center College Park MD
    531 AM EDT Sat Sep 06 2025

    Areas affected...southeastern Nevada, western Arizona, far
    southeastern California

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

    Valid 060930Z - 061330Z

    Summary...A long-lived thunderstorm complex should persist for a
    few more hours and possibly prompt instances of flash flooding.

    Discussion...A long-lived MCS currently extends from near Las
    Vegas east to near the Grand Canyon. The complex remains
    organized and well positioned within a moist/unstable axis along
    the Colorado River Valley (1+ inch PW, 1000 J/kg SBCAPE). Weak
    southerly low-level flow was enhancing convergence along the
    leading edge of the complex, while mid-level vort maxima were
    likely aiding in ascent to help maintain the intensity of the
    complex. Areas of 1-2 inch/hr rain rates continue to be estimated
    per MRMS beneath the strongest, most persistent activity, which
    has likely led to excessive runoff in a few locales (based on MRMS
    Flash responses).

    Current trends suggest that the complex will continue to drift
    southward along the Colorado River into western Arizona along the aforementioned moist/unstable axis. Boundary layer cooling has
    been slow to take hold in this area, and point forecast soundings
    suggest continued potential for sustained updrafts. Weak
    southerly flow at 850mb should also help maintain the MCS for a
    few more hours. Gradually weaker mid-level lapse rates exist with
    southern extent though, suggesting that the complex may weaken
    eventually. The specific timing of the onset of this weakening
    trend is uncertain.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6Vxrhu5q0nQa3eQBDPUhUuJEMCj6hdoA8MKvEEVZtWX_9D_CP_NdVO5kcXjks7DjaZlX= wJWou7iVP2uuMVjlFUegws8$ for graphic product...

    ATTN...WFO...FGZ...PSR...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 36901451 36401339 35161254 33761289 33711463=20
    35891527=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 6 17:14:02 2025
    AWUS01 KWNH 061713
    FFGMPD
    MAZ000-NHZ000-VTZ000-CTZ000-NYZ000-NJZ000-PAZ000-DEZ000-MDZ000-062300-

    Mesoscale Precipitation Discussion 1054
    NWS Weather Prediction Center College Park MD
    113 PM EDT Sat Sep 06 2025

    Areas affected...northern Mid-Atlantic into southern New England

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

    Valid 061712Z - 062300Z

    Summary...A couple areas of flash flooding will be possible from
    the northern Mid-Atlantic region into southern New England through
    23Z. Areas of short term training will be capable of hourly
    rainfall from 1 to 2+ inches and spotty 3 inch totals. Given dry
    antecedent conditions, the flash flood threat appears to be mostly
    urban in nature.

    Discussion...17Z observations placed a cold front stretching from
    NH/VT into southern NY, eastern PA and central MD. Surface
    moisture ahead of this boundary has increased since 12Z with
    dewpoints in the low to mid-70s from southeastern PA into parts of
    NJ as layered PW imagery showed a swath of deep layered moisture
    advecting northeastward from the lower MS Valley. 17Z SPC
    mesoanalysis data showed estimated PWs of 1.5 to 1.7 inches and
    filtered sunshine has helped to increase MLCAPE into the 1000-2000
    J/kg range. Recent visible satellite and radar imagery showed the
    beginning stages of convective development along the front from
    northeastern MD into northwestern NJ.

    There is sufficient vertical shear for organized storms with both
    organized and ordinary cells likely containing forward speeds
    between 20-35 kt toward the northeast/east-northeast. Largely
    unidirectional flow from just above the surface to the tropopause
    was oriented parallel to the front which would normally be
    supportive of training. However, a steady 10-15 kt progression of
    the cold front is forecast which should limit training to
    mesoscale waves along the front and/or thunderstorm related
    outflow that cause convection to align with the mean wind. This
    situation could support 1 to 2+ inches of rain in an hour or less.
    Given much of the region has been dry over the past 1-2 weeks, the
    flash flood threat should remain mostly tied to overlap of heavy
    rain with the urban I-95 corridor and/or some of the surrounding
    more flash flood prone areas.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Qkd-zBGYYOiMWeSPgxat76eAuBOHHfvjx4z8EbgPUM1lrzCg9G-l9NdmffKtzi7DqYK= u1C2X4utZIE1WrYEr-Y0x4Y$ for graphic product...

    ATTN...WFO...ALY...BGM...BOX...CTP...GYX...LWX...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 43037179 42157189 40887301 39907419 39517521=20
    39337605 39437645 39877631 40777521 41777425=20
    42947297=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 6 18:27:34 2025
    AWUS01 KWNH 061827
    FFGMPD
    TXZ000-NMZ000-AZZ000-070030-

    Mesoscale Precipitation Discussion 1055
    NWS Weather Prediction Center College Park MD
    227 PM EDT Sat Sep 06 2025

    Areas affected...Southeast Arizona, Southwest New Mexico

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

    Valid 061830Z - 070030Z

    Summary...Showers and thunderstorms will expand across portions of
    New Mexico and Arizona this afternoon and evening. As convection
    intensifies, brief rainfall rates t0 3"/hr are possible resulting
    on 0.5-0.75 inches of rain in 15 minutes. This may cause flash
    flooding.

    Discussion...The GOES-E day-cloud phase micro-physics RGB this
    afternoon shows a slow expansion of ice-clouds associated with
    strengthening updrafts driving deepening Cb. At this time these
    are mostly positioned across southwest NM and focused in higher
    terrain, but should expand and move into lower elevations during
    the next few hours. Despite some drier air encroaching from the
    west noted in the LPW fields, PWs remain 1.25 to 1.5 inches as
    measured by GPS, above the 90th percentile for the date, which is
    overlapping SBCAPE that is climbing to 1500 J/kg within regions of
    clearing. These thermodynamics are supporting the increasing
    updrafts, with additional lift being provided by a weak surface
    trough analyzed by WPC and a shortwave that will slowly dig
    southeast into the evening.

    Despite the relatively fresh convection, these storms have already
    produced 15-min rainfall as measured by MRMS of 0.3 to 0.4 inches
    in the deeper cells. As the afternoon progresses to peak heating,
    surface instability may exceed 2000 J/kg, likely causing these
    rain rates to become even more intense. Additionally, the
    shortwave dropping southeast may help focus some organization
    later this afternoon, especially as storms begin to drop off the
    terrain and dive E/SE on 0-6km mean winds of around 10 kts. A lack
    of significant bulk shear will keep storms generally of the pulse
    variety, but in the presence of the increasing ascent and
    favorable thermodynamics, residual outflow boundaries will likely
    lead to additional development. This could reuslt in storm
    mergers/collisions causing rain rates to perk up to as much as
    0.75"/15 min as reflected by the HRRR-forced UA WRF precipitation
    rate and HRRR 15-min rainfall product.

    Although total rainfall in most areas will likely remain below 1
    inch, a few repeating rounds are possible which could cause
    locally more than 2 inches. While this will enhance the flash
    flood risk, it is possible that any of these intense rain rates,
    even if short lived, could cause rapid runoff as 3-hr FFG is
    generally only around 1 inch in many areas. The HREF exceedance
    probabilities for this 3-hr FFG peak as high as 50% in southern
    AZ, but any of this heavy rain falling atop vulnerable regions
    such as urban areas or burn scars, could experience impacts from
    flash flooding into this evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!99dzq7IUQKyvn3avb1hIDqbUdram2GDffIWqvWKCNKp6j-HbkSXA4qySCTl48fUZSWL-= -dyElsTl25kwMa3UEBNEa5Y$ for graphic product...

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

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 34830806 34680675 34470615 34080556 33270529=20
    32530539 32000602 31770667 31580729 31390809=20
    31270897 31281048 31271092 31441158 31791165=20
    32221127 32731077 34350905=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 7 00:43:37 2025
    AWUS01 KWNH 070043
    FFGMPD
    NMZ000-AZZ000-070630-

    Mesoscale Precipitation Discussion 1056
    NWS Weather Prediction Center College Park MD
    843 PM EDT Sat Sep 06 2025

    Areas affected...Southern Arizona

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

    Valid 070042Z - 070630Z

    Summary...Slow moving showers and thunderstorms will continue
    across southern Arizona for a few more hours. Heavy rainfall
    capable of producing 0.5-0.75 inches in 15 minutes may create
    instances of flash flooding.

    Discussion...The regional radar mosaic this evening shows
    continued development of showers and thunderstorms across much of
    Arizona and New Mexico. This convection is forming within
    favorable thermodynamics characterized by PWs measured on the TUS
    00Z U/A sounding of 1.39 inches (near the 90th percentile for the
    date) and 1500 J/kg of SBCAPE. A weak mid-level impulse embedded
    in generally westerly flow is helping to drive broad ascent across
    the region, while a weak surface convergence axis near the
    Mexico/Arizona border, as well as remnant outflow boundaries and
    collisions, are aiding to produce the activity this evening.
    Although storms moving off the terrain are generally moving
    progressively to the E/SE, clusters forming across southern AZ are
    slower moving and exhibiting some back building behavior.

    As the evening progresses, a local increase in coverage of
    convection is progged by many of the available high-res CAMs
    across southern Arizona, especially in the vicinity of Pima and
    Santa Cruz counties. This will be in response to subtle moisture
    convergence on weak 850mb flow along the gradient of some higher
    PWs, but also in response to subtle SW drift of convection as
    propagation vectors gradually veer into the higher moisture. With
    mean 0-6km winds expected to remain light, and propagation vectors
    additionally weak, these slow moving storms will linger across
    some areas despite being of the pulse variety. The 15-min HRRR and
    HRRR forced UA WRF both suggest intense rainfall could reach
    0.75"/15 mins, which is additionally supported by 5-10%
    neighborhood probabilities for 2"/hr from the HREF. Where these
    storms linger, or where multiple rounds can occur, locally as much
    as 2-3" of rainfall is possible.

    0-10cm soil moisture across southern Arizona is generally below
    normal according to NASA SPoRT, although there are some pockets of
    wetter soils across the area. Regardless, if these intense rain
    rates move atop the natural vulnerability of this region,
    especially across any burn scars, urban areas, or sensitive
    terrain, instances of flash flooding could result until convective
    overturning occurs around 06Z.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6XFuW3leIxN2zZrFWyQ7KZ3xRTLQsRnU5yiHnunDMFd-g48O60lLYYZLHGgAKmpRhJMO= TP2EIoC0i8_I9l1P8n1MiS8$ for graphic product...

    ATTN...WFO...EPZ...PSR...TWC...

    ATTN...RFC...STR...NWC...

    LAT...LON 32831100 32830976 32590916 32310900 31800895=20
    31390918 31080985 30971061 31141135 31381192=20
    31621251 31921300 32251350 32701352 32781264=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 7 06:15:12 2025
    AWUS01 KWNH 070615
    FFGMPD
    WAZ000-071000-

    Mesoscale Precipitation Discussion 1057
    NWS Weather Prediction Center College Park MD
    214 AM EDT Sun Sep 07 2025

    Areas affected...western/central Washington State

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

    Valid 070614Z - 071000Z

    Summary...An instance or two of flash flooding is possible across
    the Pacific Northwest as scattered thunderstorms move
    slowly/erratically over the next 2-4 hours. Areas of 1 inch/hr
    rain rates are expected.

    Discussion...Recent radar mosaic imagery depicts a gradual
    expansion in convective coverage across western and central
    Washington State currently. The storms are generally moving
    northwestward, though weak low-level shear was promoting areas of outflow-driven activity with erratic storm motions. Spots of 1
    inch/hr rain rates were being estimated per MRMS with the more
    dominant activity, suggesting that flash flooding might occur
    especially if that rainfall occurs atop sensitive ground
    conditions and/or burn scars. The storms are being supporting by
    1) ascent lifting northward around the base of a larger-scale
    mid/upper trough over the northeastern Pacific, 2) steep mid-level
    lapse rates (generally above 7C/km away from storms), and 3) a
    moisture plume across the area, with PW values generally in the
    1-1.3 inch range. Each of these factors suggest that an instance
    or two of flash flooding might occur as storms move through the
    region in the near term.

    Models/observations suggest the period of peak flash flood risk
    might only extend through 09Z/2a PDT or so. The mid-level
    vorticity max helping to force ongoing convection should lift
    northward into southwestern Canada, resulting in a minimum in
    forcing aloft amid stabilizing low-levels from widespread
    rainfall. A limited threat for thunderstorms may exist beyond the
    09Z/2a PDT timeframe, and flash flood potential will be reassessed
    around that time.

    Of note - some of the thunderstorms may also produce dry lightning
    and fire starts. Additional information on these threats can be
    found at your respective local forecast office (weather.gov) and
    SPC fire weather information (spc.noaa.gov).

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6-2GaFK6ln1qD0eK1_sxoe7WzmHRV_M3Au8Pv9bCEzSu2e0My9vEYfPd9g1SNhEkeD76= k6qOHzI6tSmoI5XNYTh_tiI$ for graphic product...

    ATTN...WFO...OTX...PDT...PQR...SEW...

    ATTN...RFC...PTR...NWC...

    LAT...LON 48712153 48411990 47381918 46222023 46612342=20
    47952347 48372269=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 7 12:32:44 2025
    AWUS01 KWNH 071232
    FFGMPD
    TXZ000-071800-

    Mesoscale Precipitation Discussion 1058
    NWS Weather Prediction Center College Park MD
    832 AM EDT Sun Sep 07 2025

    Areas affected...Western Hill Country & Lower Pecos River Valley
    of Texas...

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

    Valid 071230Z - 071800Z

    SUMMARY...Ongoing flash flooding likely to continue for the
    remainder of the morning with very slow moving and surprisingly
    efficient rainfall production producing highly focused 2"/hr rates
    over sensitive/low FFG terrain. Additional 3-5" totals resulting
    in likely focused flash flooding. A spot or two of considerable
    and/or significant flash flooding is possible.=20=20

    DISCUSSION...Regional RADAR mosaic over the last few hours has
    seen a slight uptick in convective activity in both strength and
    coverage with the scattered observations indicating surprisingly
    efficient rainfall production with 2"/hr rates and some localized
    2-5"/3hrs reported resulting in localized flash flooding. The
    overall environment is expected to change very little over the
    next few hours as cells continue to remain fairly stationary with
    small movement.

    The overall dynamics has been supportive of the scattered
    convective environment, as GOES-E WV shows a very concentric but
    broad upper-level ridge across northern Mexico, placing SW TX/Hill
    Country into a favorable upper-level divergent pattern at the
    entry of a speed max of a jet just east of the 30N100W benchmark.=20
    Small northeast quadrant diffluence, but also slightly digging
    northern stream influence across the Big Country in combination
    with approaching northern stream short-wave feature is combining
    to allow for solid evacuation of these thunderstorms. In
    addition, the shortwave to providing ascent, has strengthened
    surface easteries, though a shallow boundary layer/inversion is
    drawing moisture up through the Rio Grande Valley to the Lower
    Pecos (per Sfc-850mb LPW animation) and lifting in northward on
    850mb flow per VWP in the region. Total deep layer moisture is
    lower than expected for such an observed efficient cells; the flux
    is most likely loading the lower warm cloud portion with the low
    to mid-70s Tds for 2"+/hr rates for the highly focused updrafts
    that have developed.=20=20

    The vertical shear profile (along with the upstream height-falls)
    supports a westerly back-building environment counteracting the
    steering flow aloft to result in a fairly stationary nature in the
    short-term. As the height-falls/shortwave arrives, a slow
    southward motions are likely into the Rio Grande Valley toward
    Mexico. Flux up the Rio Grande is expected to continue to keep
    slow but efficient rainfall production likely over the next 4-6
    hours. As such, spotty 3-5" totals are probable and will result
    in focused (scattered in coverage) but potentially considerable
    flash flooding conditions (as FFG values are naturally low
    1-1.5"/hr & 1.5-2.5"/3hrs) in fairly rugged terrain.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ptKWcbjGgExB-8-QlbZCGkLXWgtuctLuGSmv2P_Qt21At6GM-JSOlf9z_KHR_FAq35s= YCqdFSmK26QpkhzxI_K7JOE$ for graphic product...

    ATTN...WFO...EWX...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31120201 31120100 30649929 29949871 29149935=20
    28850041 29180092 29640153 29870197 30260236=20
    30810241=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 7 18:57:20 2025
    AWUS01 KWNH 071857
    FFGMPD
    TXZ000-080100-

    Mesoscale Precipitation Discussion 1059
    NWS Weather Prediction Center College Park MD
    256 PM EDT Sun Sep 07 2025

    Areas affected...South-Central Texas through the Middle Texas
    Coast

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

    Valid 071900Z - 080100Z

    Summary...Showers and thunderstorms will continue to move slowly
    across the region through the evening. Rainfall rates of 2-3"/hr
    are likely at times, leading to 2-3" of rainfall with locally
    higher amounts. This may cause instances of flash flooding.

    Discussion...The regional radar mosaic this afternoon shows
    widespread showers with embedded thunderstorms from the southern
    Hill Country of Texas eastward through the Middle Texas Coast.
    This activity is blossoming/persisting in response to weak
    shortwave energy dropping SE around a ridge over northern Mexico,
    with some of this vorticity likely associated with the remnants of
    Lorena from several days ago. Additionally, a stationary front is
    draped across South Texas as analyzed by WPC, which is providing
    additional focus for ascent through convergence across the area.

    This lift is occurring within impressive thermodynamics
    characterized by PWs measured by GPS as high as 2.25 to 2.5
    inches, and measured via the KCRP special 18Z U/A sounding of
    2.26, approaching the daily record for the date, combined with
    MUCAPE of 2000-2500 J/kg. This is providing ample fuel for
    thunderstorm development, and moist-adiabatic lapse rates through
    500mb of the area sounding supports the efficient warm-rain
    processes which have somewhat surprised in intensity so far today
    in producing MRMS measured hourly rainfall of 1.5 to 2.5 inches,
    even in modest reflectivity signatures.

    As the aftn progresses, the CAMs are in good agreement that the
    focus should become along the stationary front where the enhanced
    convergence will drive deeper ascent. Modest bulk shear of 20-25
    kts will help organize some storms into clusters along this
    boundary, and as low-level easterly flow intensifies (as reflected
    by a surge in sfc-850mb LPW), storm motions will collapse to
    around 5 kts. These slow moving storms will contain rain rates for
    which the HREF neighborhood probabilities suggest will exceed
    2"/hr (as high as a 40% chance), producing locally as much as 0.5"
    to 0.75" in 15 min as reflected by the recent HRRR. Where storms
    train or repeat with these rain rates, 2-3" of rainfall with
    locally higher amounts is expected.

    Although rainfall south of the Hill Country has been modest
    recently as reflected by AHPS 7-day rainfall that is generally
    10-50% of normal, leading to a sharp gradient and increase in FFG,
    the region still appears vulnerable to at least isolated flash
    flood instances through this evening. This is due in part to the
    efficiency of the anticipated rainfall rates, but also due to
    expected repeating rounds near the stationary front leading to FFG
    exceedance as high as 30% from the HREF.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8BuOeNH8btnc9-4e-hEgXHzDm3HK-II08JrsbQzVW3PV4NnEhqWLDBt5_-ws5Xye9dKZ= cGbA6zbBii3y_gbdJF_Rjgs$ for graphic product...

    ATTN...WFO...BRO...CRP...EWX...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 29960018 29919816 29569601 29059580 28469603=20
    28149668 27879696 27539711 27289761 27309842=20
    27489923 27689976 28100028 29720128=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 7 21:55:24 2025
    AWUS01 KWNH 072155
    FFGMPD
    NCZ000-SCZ000-FLZ000-GAZ000-080330-

    Mesoscale Precipitation Discussion 1060
    NWS Weather Prediction Center College Park MD
    554 PM EDT Sun Sep 07 2025

    Areas affected...Coastal Plain from central Florida to eastern
    North Carolina

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

    Valid 072154Z - 080330Z

    Summary...Slow moving showers and thunderstorms will persist
    through evening along a stalled cold front. Rainfall rates of
    2-3"/hr are expected to be common, which through this slow storm
    motion could produce 2-4+" of rainfall. This may result in flash
    flooding, especially across urban areas.

    Discussion...The regional radar mosaic this evening indicates a
    continued expansion of showers and thunderstorms from the central
    Florida Peninsula northeast along the coastal plain through Cape
    Lookout, NC. This activity is blossoming along a cold front, which
    has merged in places with the sea breeze to stall near the coast.
    The combined ascent along this boundary is the primary focus for
    convective development, although a weak shortwave noted across the
    FL Panhandle is lifting northeast downstream of an anomalous
    trough axis to provide additional ascent.

    This lift is acting upon a rich thermodynamic environment
    characterized by PWs measured by GPS of 1.8 to 2.0 inches,
    overlapping pockets of SBCAPE analyzed by the SPC RAP that are
    above 2000 J/kg where convective overturning has yet to occur. The
    presence of this steady ascent into this robust airmass has
    produced scattered thunderstorms with rainfall rates estimated by
    the local radars of as much as 2.5"/hr, and measured via
    observations and MRMS to be as much as 3" in 1 hour. This has
    resulted in isolated flash flooding near the city of Charleston,
    SC already this aftn.

    The CAMs were slow to pick up on the uptick in activity, but have
    started to support a more widespread heavy rainfall event into
    this evening before loss of heating/instability occurs. HREF
    neighborhood probabilities for 2"/hr rates peak above 40% through
    01Z, coincident with loss of instability and finally a slow push
    east of the cold front. Until that occurs, however, widespread
    thunderstorms are likely, and although most should be of the pulse
    variety, some increased bulk shear to 20-25 kts in the vicinity of
    the mid-level shortwave could organize thunderstorms into clusters
    to enhance rainfall rates to locally as much as 1"/15 min (brief
    4"/hr rates). Weak storm motions as reflected by just 5 kts of
    0-6km mean winds and aligned Corfidi vectors suggest that storms
    could build SW along the front and into some more impressive
    thermodynamics, before training E/NE from northeast FL through
    eastern NC. This could result in local rainfall totals approaching
    4-5 inches.

    Although this area has been extremely dry (0% rainfall the past 7
    days according to AHPS outside of parts of the FL Peninusula),
    these intense rain rates could still overwhelm soils leading to
    rapid runoff. This will be most likely across urban areas, but
    some vulnerability exists even outside of the population centers
    should any of these intense rainfall rates train repeatedly across
    any given area. This suggests that flash flooding remains possible
    through the evening, but the risk should wane rapidly after dark.

    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4mnubCIcRvsRdUCL-ihIV7zyIPCX-Z6SDtRHEuOUyi8-nF6ocHiRzLkyJQgKJHg9H8dP= dHzsCRwWLzJawLbFN9JbNdc$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...ILM...JAX...MHX...MLB...RAH...
    TBW...

    ATTN...RFC...ALR...NWC...

    LAT...LON 35127693 35057628 34767613 34507629 34317677=20
    33967757 33637817 32927909 32397992 31758063=20
    30988099 29938085 29198046 28348046 28238099=20
    28338144 28758196 29468244 30138278 31128273=20
    32238221 33198104 34057989 34557865 34947770=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 8 13:18:16 2025
    AWUS01 KWNH 081305
    FFGMPD
    KSZ000-081700-

    Mesoscale Precipitation Discussion 1061
    NWS Weather Prediction Center College Park MD
    904 AM EDT Mon Sep 08 2025

    Areas affected...North-Central Kansas

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

    Valid 081303Z - 081700Z

    Summary...Heavy thunderstorms will continue to redevelop over a
    narrow corridor of north-central Kansas through the late morning.
    Rain rates up to 2.5"/hr should continue with additional rainfall
    of 2-5" possible. Localized flash flooding should persist.

    Discussion...A narrow north-south oriented axis of heavy rain
    persists over I-70 just west of Salina.
    Northwesterly upper level flow is over the central Plains
    downstream of a ridge axis over the central Rockies. Surface high
    pressure centered over the Great Lakes is aiding moist return flow
    up the Plains with a low level veering wind profile of southerly
    at the surface and 20-30kt 850 SWly flow. This is resulting in
    slow storm motions and upwind propagation allowing for repeating
    heavy rain.

    Despite the strong southerly low level flow, moisture is not that
    great with PW around 1.3" and sfc dewpoints in the mid-50s over
    central KS. Instability is sufficent with a gradient up to 1000
    J/kg upstream which quickly drops off to the east (before Topeka).
    Hi-res forecasts allow the southerly inflow to persist for at
    least a few hours this morning as opposed to the normal decrease
    of the LLJ after sunrise. Therefore, localized heavy rain should
    continue to occur. FFG is around 2.5"/3hr which has been met
    rather locally. The continued development should put areas well
    over FFG and cause perhaps locally considerable flash flooding
    rest of the morning.

    Recent HRRR runs have this activity shifting east, but as least
    for now the trend is to keep the line drifting south.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8OgRdrk97NKXsDtwXiMJBBm4VEhFv3bHGjqx2c7jNiSDsYj1D4shlFRPWVjksN3gIVmc= -f3qxZyEe8HgSURdtnlmrvQ$ for graphic product...

    ATTN...WFO...DDC...GID...ICT...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39549775 38999733 38159751 37999788 38209854=20
    38809837 39479817=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 8 16:57:06 2025
    AWUS01 KWNH 081656
    FFGMPD
    KSZ000-082100-

    Mesoscale Precipitation Discussion 1062
    NWS Weather Prediction Center College Park MD
    1255 PM EDT Mon Sep 08 2025

    Areas affected...Central Kansas

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

    Valid 081654Z - 082100Z

    Summary...Persistent heavy thunderstorms will continue to
    redevelop over a narrow north-to south corridor of central Kansas
    into this afternoon. Rain rates up to 2.5"/hr should continue with
    additional rainfall of 2-5" and storm total rainfall exceeding 12"
    possible. Flash flooding with localized considerable impacts
    should persist before finally easing later this afternoon.

    Discussion...The narrow north-south oriented axis of repeating
    heavy thunderstorms persists across I-70 west from Salina. The
    slow moving synoptic pattern of an upper ridge axis over the
    central Rockies and surface high pressure centered over the Great
    Lakes is maintaining northwesterly flow over southwesterly low
    level flow over the central Plain. Moist return flow up the Plains
    with a low level veering wind profile of southerly at the surface
    and 20-30kt 850 SWly flow has maintained slow storm motions and
    upwind propagation/redevelopment allowing for repeating heavy rain
    over the same axis. This axis has expanded south, into the low
    level flow, over the past few hours.

    Little change in this flow pattern is expected from the RAP until
    around 20Z with some mid-level veering which may dislodge this
    particularly persistent heavy rain axis.

    PW is now 1.5" (a little above normal) with this continued influx.
    The static nature of the pattern is also attributed to the
    instability gradient which has changed little over the past four
    hours with sufficent 1000 J/kg upstream quickly drops off to the
    east (west of Manhattan, KS).

    CAM guidance continues to struggle with this activity with the
    HRRR and RRFS still trying to shift it east. Once the mid levels
    veer more westerly then that should take place, making for mainly
    beneficial rain to areas east of this hard hit axis. Until then,
    considerable flash flooding will continue with localized totals
    reaching or exceeding 12".

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7fpxNVgyR9riDgyYdwqwgOs0MZV0Ks06Cp69irCDtSH8Vo_ulh79hLJPCz0eF17Xjcuq= CME5R8VeQFIEoGheglw3Ow8$ for graphic product...

    ATTN...WFO...DDC...GID...ICT...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39449828 39399778 39049732 38539738 38089759=20
    37719790 37869855 38389855 39049833=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 8 21:21:08 2025
    AWUS01 KWNH 082121
    FFGMPD
    OKZ000-KSZ000-090100-

    Mesoscale Precipitation Discussion 1063
    NWS Weather Prediction Center College Park MD
    520 PM EDT Mon Sep 08 2025

    Areas affected...south-central to southeastern KS and northern OK

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

    Valid 082119Z - 090100Z

    Summary...Areas of flash flooding will remain possible from
    portions of south-central to southeastern KS and northern OK over
    the next 3-4 hours. Hourly rainfall of 1-2 inches (locally higher)
    will be possible with potential near term impacts in the Wichita
    metro area within the next hour.

    Discussion...A long-lived MCS over east-central KS has been
    responsible for MRMS-derived rainfall totals up to 12 inches in a
    north-south axis to the west of Salina. As of 2045Z, this
    relatively compact system was moving south-southeastward, with an
    embedded MCV near Emporia, but with the heaviest rainfall rates
    were occurring on the west side of the complex along an
    instability gradient that was oriented NNE to SSW (MUCAPE up to
    1500 J/kg). Meanwhile, MUCAPE values over eastern KS were near
    zero, coinciding with stratiform rain and non-hazardous rainfall
    intensities. Thunderstorms were elevated in nature, rooted in the
    800-700 mb layer per RAP analysis soundings over the region with
    elevated convergence in this layer supporting continued pockets of
    hourly rainfall between 1 and 2 inches (locally higher).

    As the MCV continues to follow the northwesterly flow aloft toward
    southwestern MO, the axis of elevated convergence helping to
    support the continued high rainfall rates will translate
    southeastward, at the edge of the elevated instability axis. It is
    unclear if possible weakening of the convergence axis (per short
    term RAP forecasts) and/or movement of the convergence axis into
    weaker instability will occur, thereby weakening rainfall rates,
    but cloud tops continue to show bursts of cooling on infrared
    satellite imagery, suggestive of the flash flood threat continuing
    for at least another 1-2 hours. While a southeastward translation
    of forcing will shift the complex away from the stronger 850 mb
    jet axis (25-35 kt) over central KS, sufficient strength of the
    low level flow will likely maintain over the I-35 corridor to
    support some backbuilding and training of cells as heavy rain
    advances toward the S to SSE. Hourly rainfall of 1 to 2+ inches is
    expected to continue a flash flood threat, especially into the
    Wichita metro area in the next hour along with other locations
    along the I-35 corridor into northern OK through 01Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6XB2XUCGvLiDOsiHj5LEPgmBhvDo_PyyC21vialfBksdMEXpxT6HZ2jQN6LoCDGF2j19= ZXjhrXaD7kclMjrAuwPvivw$ for graphic product...

    ATTN...WFO...DDC...ICT...OUN...TOP...TSA...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 38929791 38889751 38499675 37979649 37239611=20
    36569606 36219624 36029720 36289853 37369896=20
    38189828 38779814=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 8 21:47:10 2025
    AWUS01 KWNH 082147
    FFGMPD
    FLZ000-090100-

    Mesoscale Precipitation Discussion 1064
    NWS Weather Prediction Center College Park MD
    546 PM EDT Mon Sep 08 2025

    Areas affected...southeastern FL

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

    Valid 082144Z - 090100Z

    Summary...Intense hourly rainfall of 2-4 inches will continue to
    be possible across the urban corridor of southeastern FL for
    another 2-3 hours. Flash flooding will be possible.

    Discussion...MRMS reflectivity from 2130Z continued to show areas
    of thunderstorms over southeastern FL where 21Z SPC mesoanalysis
    data showed MLCAPE of 1000 to 2000+ J/kg and PWATs of 2.0 to 2.2+
    inches. Cells were disorganized but very slow moving with MRMS and
    gauge data showing hourly rainfall in the 2-4 inch range and
    15-minute rainfall of 1 to 1.5 inches over eastern Palm Beach,
    Broward and Miami-Dade counties since 19Z.

    While the Miami-metro has already picked up 2-4 inches, and
    rain-cooled air has settled into the region, high surface
    dewpoints in the mid to upper 70s along the eastern Peninsula may
    be limiting low level convective inhibition, potentially allowing
    for additional convection later this evening. Another round of
    heavy rainfall may impact portions of the Miami/Fort Lauderdale
    metro over the next couple of hours as mean westerly flow may
    support translation and/or additional development near/ahead of an
    inland cluster of thunderstorms over southern Palm Beach into
    western Broward counties. Meanwhile, ongoing cells farther up the
    coast may lead to an isolated/urban flash flood threat within the
    next 2-3 hours, before cells likely weaken after sunset.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_dbVeJ5TgSHQvV2dtteXPk3NdAqS_RXdQhsfbtnUhwbPJLoliorIpMSyBIXs15XS7rzC= 2O1OPOGCscuW-he5BwVhe-A$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 26848034 26817996 26347984 25837998 25448024=20
    25428054 25618066 26138058=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 9 00:16:11 2025
    AWUS01 KWNH 090016
    FFGMPD
    CAZ000-ORZ000-090415-

    Mesoscale Precipitation Discussion 1065
    NWS Weather Prediction Center College Park MD
    815 PM EDT Mon Sep 08 2025

    Areas affected...southwestern/western OR

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

    Valid 090011Z - 090415Z

    SUMMARY...Scattered thunderstorms with repeating and brief
    training could result in an inch or two of rainfall with rainfall
    rates of 1 inch in an hour or less for portions of
    southwestern/western OR. Isolated flash flooding could result,
    with a particular focus across burn scars.

    DISCUSSION...Visible satellite imagery from GOES West at 00Z
    showed the low to mid-level reflection of a closed low west of the
    northern CA coast containing a number of smaller scale vorticity
    maxima rotating about the low center. In addition, another
    vorticity max was located inland, over northern Douglas County in
    southwestern OR, moving toward the north. Scattered thunderstorms
    were observed through radar/satellite imagery along and just west
    of the Cascades and across portions of the Klamath Mountains of
    southwestern OR. While PW values were anomalous for early
    September (+2 to +3 standardized anomalies), instability was
    somewhat limited with pockets of 500-1000 J/kg in place over the
    region via 00Z SPC mesoanalysis data.

    Deeper layer mean flow was from the south at 10-20 kt, similar to
    the low level inflow layer, which was favoring repeating and brief
    training of cells in a few locations. While the threat appears
    isolated, there will be the potential for cells to generate
    rainfall of an inch within 60 minutes or less time. These
    localized higher rainfall rates could overlap with sensitive
    terrain or burn scars to result in isolated flash flooding. The
    flash flood threat is likely to diminish with the loss of daytime
    heating and reduction in instability after 04Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7juXn12P2XvRjw5FO_GiHYeSjFptrhuUgWfLJv-2sRn91Z9VJotsm0KMG112qxLtbxTy= usJC8UcW58nvem7eaCrT9L0$ for graphic product...

    ATTN...WFO...EKA...MFR...PDT...PQR...

    ATTN...RFC...PTR...RSA...NWC...

    LAT...LON 44692233 44472206 43982189 43262205 42732214=20
    42252228 42022261 41922316 41982373 42242393=20
    43162394 44052370 44692285=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 9 01:10:50 2025
    AWUS01 KWNH 090110
    FFGMPD
    TXZ000-OKZ000-KSZ000-090600-

    Mesoscale Precipitation Discussion 1066
    NWS Weather Prediction Center College Park MD
    909 PM EDT Mon Sep 08 2025

    Areas affected...northwesten OK into the eastern TX Panhandle

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

    Valid 090106Z - 090600Z

    SUMMARY...Localized flash flood potential will exist from
    northwestern OK into the eastern TX Panhandle through 06Z. Hourly
    rainfall of 1-2 inches (locally higher) is expected with the
    threat potentially shifting slowly toward the south with time.

    DISCUSSION...Local radar imagery across northwestern OK into the
    northeastern TX Panhandle showed scattered thunderstorms with a
    couple of slow moving cells and cyclic supercells resulting in
    localized flash flooding. Surface observations from 01Z showed a
    few cells from northern OK into southwestern KS were along an
    outflow boundary related to earlier thunderstorms that moved
    through southern KS/northern OK. Meanwhile, an new cold pool was
    forming due to expanding convection from northwestern OK into the
    northeastern TX Panhandle.

    As the low level jet increases overnight, with RAP forecasts
    showing 850 mb wind speeds up to ~40 kt by 06Z, scattered
    thunderstorms or a small convective cluster may pose a flash flood
    threat with potential propagation toward the south into the low
    level inflow. With mean cell motions from the WNW to N, there will
    be the possibility for training along the western flank of the
    potential MCS if organization should develop and advance southward
    following Corfidi Vectors. While moisture is modest/average for
    early September, there is ample instability (2000 to 2500+ J/kg
    MLCAPE via AMA and DDC 00Z soundings) with steep mid-level lapse
    rates which should maintain sufficient CAPE well into the early
    part of the overnight. While increasing convective inhibition is a
    concern, ascent along the developing/advancing cold pool could be
    enough to overcome capping to allow at least a localized flash
    flood threat to maintain over the next few hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6b6m6rm8G1bCUqM_UiVW-xs5RBK6yLEsPJBz8VAFZbq5oz9WPRxWewI9ogNctO3Nyq5s= T5dYERj2wRRa2AwFZfwIS8I$ for graphic product...

    ATTN...WFO...AMA...DDC...LUB...OUN...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 37000045 36949921 35969934 35329947 34409961=20
    33950024 34110148 34680186 36280150=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 9 01:13:11 2025
    AWUS01 KWNH 090113
    FFGMPD
    TXZ000-OKZ000-KSZ000-090600-

    Mesoscale Precipitation Discussion 1066...Corrected
    NWS Weather Prediction Center College Park MD
    912 PM EDT Mon Sep 08 2025

    Corrected for typo in areas affected

    Areas affected...northwestern OK into the eastern TX Panhandle

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

    Valid 090106Z - 090600Z

    SUMMARY...Localized flash flood potential will exist from
    northwestern OK into the eastern TX Panhandle through 06Z. Hourly
    rainfall of 1-2 inches (locally higher) is expected with the
    threat potentially shifting slowly toward the south with time.

    DISCUSSION...Local radar imagery across northwestern OK into the
    northeastern TX Panhandle showed scattered thunderstorms with a
    couple of slow moving cells and cyclic supercells resulting in
    localized flash flooding. Surface observations from 01Z showed a
    few cells from northern OK into southwestern KS were along an
    outflow boundary related to earlier thunderstorms that moved
    through southern KS/northern OK. Meanwhile, an new cold pool was
    forming due to expanding convection from northwestern OK into the
    northeastern TX Panhandle.

    As the low level jet increases overnight, with RAP forecasts
    showing 850 mb wind speeds up to ~40 kt by 06Z, scattered
    thunderstorms or a small convective cluster may pose a flash flood
    threat with potential propagation toward the south into the low
    level inflow. With mean cell motions from the WNW to N, there will
    be the possibility for training along the western flank of the
    potential MCS if organization should develop and advance southward
    following Corfidi Vectors. While moisture is modest/average for
    early September, there is ample instability (2000 to 2500+ J/kg
    MLCAPE via AMA and DDC 00Z soundings) with steep mid-level lapse
    rates which should maintain sufficient CAPE well into the early
    part of the overnight. While increasing convective inhibition is a
    concern, ascent along the developing/advancing cold pool could be
    enough to overcome capping to allow at least a localized flash
    flood threat to maintain over the next few hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!81BbSdVex5g0vdcA-ex1_UxpGsamW46KqiZQW69Jep5OL_kp1VUNwTyT2q-FWbE0MYKA= ouNuuCztLjC35aHvkXvKRH8$ for graphic product...

    ATTN...WFO...AMA...DDC...LUB...OUN...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 37000045 36949921 35969934 35329947 34409961=20
    33950024 34110148 34680186 36280150=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 9 18:25:23 2025
    AWUS01 KWNH 091825
    FFGMPD
    FLZ000-100024-

    Mesoscale Precipitation Discussion 1067
    NWS Weather Prediction Center College Park MD
    224 PM EDT Tue Sep 09 2025

    Areas affected...Southeast Florida

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

    Valid 091824Z - 100024Z

    Summary...Thunderstorms are expanding along and ahead of a
    stationary front and associated surface low. Slow storm motions
    and periodic cell mergers could lead to 2-5" of rainfall within
    the highlighted area, which will drive an increasing risk of
    isolated to scattered urban flash flooding this afternoon.

    Discussion...Latest surface analysis depicts a stationary front
    and offshore wave of low pressure west of Tampa Bay, which extends
    eastward through Central Florida. Along and ahead of this front,
    showers and thunderstorms have expanded in coverage and intensity
    (MIA recently reported a 2.18"/hr rainfall rate) over South
    Florida amid persistent insolation and moistening, possibly
    coupled with right entrance ascent from a strengthening jet-streak
    to the north.

    Objective analysis estimates suggest very moist and unstable
    inflow characterized by 2500 J/kg of MLCAPE and 2.3-2.4" PWATS"
    (near the daily max for MFL and KEY) has materialized near this
    activity, which will support increasing probabilities of 3"/hr
    rainfall rates over the next 2-3 hours per the HREF and REFS.
    While weak vertical shear profiles on the order of 15-20 kts
    should support limit individual cell longevity, cell mergers along
    resulting outflows and the sea breeze could favor spots of 2-5"
    within the highlighted area. Accordingly, expect an increasing
    risk of isolated to scattered flash flooding in sensitive urban
    areas along the coastline this afternoon.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_G-kvjZ5XaswBZjZ-KraVtnVsg_eebenqujrrNFA5aoPU1sxGGhmjwcHKwkemFoxa66N= adL3WLbI7o0N9U4Zzejq2_s$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 27378021 27047991 26397992 25808001 25328023=20
    25398066 25808059 26498038 27088043 27338037=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 9 19:05:26 2025
    AWUS01 KWNH 091905
    FFGMPD
    FLZ000-100000-

    Mesoscale Precipitation Discussion 1068
    NWS Weather Prediction Center College Park MD
    304 PM EDT Tue Sep 09 2025

    Areas affected...Southwest Florida

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

    Valid 091902Z - 100000Z

    Summary...Heavy thunderstorms developing ahead of a low west of
    Fort Myers will continue to push over the southwestern FL
    Peninsula through the rest of the afternoon. The potential for
    repeating heavy rain raises isolated risk for urban flash flooding.

    Discussion...A trough extending from low pressure centered 150
    miles or so west of Ft. Myers is providing focus for heavy
    thunderstorms tracking from The Gulf into the SW FL coast. Recent
    hourly rainfall estimates from KTBW of up to 3" are a reasonable
    maximum that can be expected with this activity. A very moist and
    unstable atmosphere with 2.4" PW 3000 J/kg SBCAPE is present
    across the southern FL Peninsula. Weak vertical shear profiles on
    the order of 15-20 kts support limit individual cell longevity,
    but organization from forcing ahead of the low and convergence at
    the coast will continue to allow bands of heavy thunderstorms to
    develop and shift inland from Port Charlotte south through Naples
    rest of the afternoon. Rainfall of 2-6" is likely within the
    highlighted area which causes flash flooding concerns for
    sensitive urban areas.

    CAMs have struggled with this activity, but the diurnal
    enhancement of activity along a boundary in this extreme moisture
    environment warrants concern for excessive rainfall.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7mXjJfyzamDVio0V6eoXr9eelp2BlDw3UtM2T77RbpWgbE0NoczsBAQp5K-yLJX2zVnI= mad8bZ5AZzoO4Qa8xIGPgSE$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 27168221 27108163 26058128 25748138 25688166=20
    26098228 26968271=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 9 21:16:28 2025
    AWUS01 KWNH 092116
    FFGMPD
    FLZ000-100115-

    Mesoscale Precipitation Discussion 1069
    NWS Weather Prediction Center College Park MD
    515 PM EDT Tue Sep 09 2025

    Areas affected...Central Florida

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

    Valid 092115Z - 100115Z

    Summary...Scattered heavy thunderstorms are expanding along and
    south of a stationary front can be expected to continue to develop
    into the evening. Slow storm motions and periodic cell mergers
    could lead to 2-5" of rainfall and continued localized urban flash
    flooding.

    Discussion...A stationary front crossing the Florida Peninsula
    north of Cape Canaveral and Orlando is under an upper trough over
    the Southeast U.S. Scattered heavy thunderstorms continue to
    develop across central FL with isolated hourly rates of 3" and
    flash ponding/urban flash flooding concerns.

    High moisture (PW 2.3 to 2.4") and instability (2000-3000 J/kg
    SBCAPE) along with deep warmth is allowing for particularly
    efficient cells. Vertical shear profiles of 20-30kt are sufficient
    to retain development while keeping slow motion. Additional
    central FL locations receiving a quick 2-5" is possible through
    00Z before nocturnal processes begin to diminish the activity.
    This is in agreement with recent CAMs such as the HRRR and
    experimental RRFS.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9swSuAhP-ft50YLHZECCZhOO8KrtcLfo6cVrO4LoohkN43B_OwRJbDLWAxYXoV6N5hAh= rw0RHDqZ2x75rD83RC86xwQ$ for graphic product...

    ATTN...WFO...JAX...MFL...MLB...TBW...

    ATTN...RFC...ALR...NWC...

    LAT...LON 29088211 28898073 28298052 27468028 27248066=20
    27188136 27388181 27998191 28458247 28908274=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 10 21:05:13 2025
    AWUS01 KWNH 102105
    FFGMPD
    CAZ000-110300-

    Mesoscale Precipitation Discussion 1070
    NWS Weather Prediction Center College Park MD
    504 PM EDT Wed Sep 10 2025

    Areas affected...Northern California

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

    Valid 102100Z - 110300Z

    SUMMARY...Widely scattered slow-moving showers and thunderstorms
    across northern California are likely to contain maximum rainfall
    rates up to 1"/hr and may overlap with sensitive burn scar
    locations. Leading to the potential for isolated flash flooding
    through this evening.

    DISCUSSION...GOES-West ML-WV imagery depicts and vertically
    stacked mid-upper level low over northern California this
    afternoon, which has led to sufficient lapse rates up to 8C/km and
    blossoming thunderstorms coverage. Mean layer winds underneath
    this low are very weak or nonexistent, which has anchored most of
    the heavy rainfall to the Klamath and Siskiyou Mts of northern CA.
    These slow-moving storms and buoyant atmosphere may help rainfall
    rates peak up to 1"/hr, but with most cells likely exhibiting
    rates around 0.5"/hr.

    These rainfall rates are enough to cause concerns over recent burn
    scars that are most susceptible to rapid runoff. It is within
    these locations where isolated to scattered flash flooding is most
    possible through this evening until daytime heating diminishes and
    lapse rates lessen. However, isolated flash flooding is also
    possible elsewhere should thunderstorms containing 1"/hr rates
    maintain and remain stalled over an area for a few hours.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!47EWxXAU9ANuy96zr7gZZA9t8PU82v5iwhMSGIsRZw4F_IRmetrGPA1EWB5dGkqHIDNF= EU2YG37LswkWg2hJpPlSg4k$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 41872178 41652145 41112139 40482137 40042144=20
    40042187 40482215 40382246 40022256 39542248=20
    38812228 38652268 39062311 40032354 40902358=20
    41432323 41802251=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 10 23:42:45 2025
    AWUS01 KWNH 102342
    FFGMPD
    IDZ000-ORZ000-110540-

    Mesoscale Precipitation Discussion 1071
    NWS Weather Prediction Center College Park MD
    741 PM EDT Wed Sep 10 2025

    Areas affected...Parts of Central/Eastern Oregon and Western Idaho

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

    Valid 102340Z - 110540Z

    SUMMARY...Numerous showers and thunderstorms capable of 1"/hr
    rainfall rates across central/eastern Oregon and far western Idaho
    this evening may be slow-moving at times and could pose the threat
    for isolated flash flooding. This is primarily a concern over burn
    scars.

    DISCUSSION...A closed low over northern California evident on
    GOES-West satellite imagery this afternoon continues to usher
    southerly flow on the eastern periphery before upper flow becomes
    more easterly and convergent near eastern and central Oregon.
    Meanwhile, a southerly 300mb jet across the central Great Basin
    also places eastern OR/western ID in the favorable left-entrance
    region and provides additional upper lift for thunderstorm
    development and maintenance through early tonight. PW values range
    from 0.8-0.9" per SPC's mesoanalysis, which is +2.0 standard
    deviations above the climatological average for this part of the
    country. Additionally, SBCAPE values of 1,000-1,500 J/kg are
    sufficient for strong updrafts to tap into the available moisture.

    Current MRMS estimates for hourly rates are up to 1" near the John
    Day Highlands and 18Z HREF probabilities for over 1"/hr totals
    continue to exceed 20% until around 02Z. These rates when combined
    with coverage of thunderstorms could lead to flash flooding for at
    least a few additional hours should heavy rainfall overlap with
    the several sensitive burn scars across the region.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_TKX933nqAx5AVXQyGVp4FAgSLkLdplA3V82vAYsYEyFRelys96zZ2T72uBZ4EVamPre= x0Dg7QrLJHt3zeMfUzseUso$ for graphic product...

    ATTN...WFO...BOI...MFR...PDT...

    ATTN...RFC...PTR...RSA...NWC...

    LAT...LON 45151847 45111767 44851708 44161670 43271654=20
    42591663 42251706 42231760 42451794 43081834=20
    43241844 43561918 43392023 43392094 43642123=20
    44202091 44771975=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 10 23:46:15 2025
    AWUS01 KWNH 102346
    FFGMPD
    IDZ000-ORZ000-110540-

    Mesoscale Precipitation Discussion 1071...Corrected
    NWS Weather Prediction Center College Park MD
    745 PM EDT Wed Sep 10 2025

    Corrected for Typo in Discussion

    Areas affected...Parts of Central/Eastern Oregon and Western Idaho

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

    Valid 102340Z - 110540Z

    SUMMARY...Numerous showers and thunderstorms capable of 1"/hr
    rainfall rates across central/eastern Oregon and far western Idaho
    this evening may be slow-moving at times and could pose the threat
    for isolated flash flooding. This is primarily a concern over burn
    scars.

    DISCUSSION...A closed low over northern California evident on
    GOES-West satellite imagery this afternoon continues to usher
    southerly flow on the eastern periphery before upper flow becomes
    more easterly and convergent near eastern and central Oregon.
    Meanwhile, a southerly 300mb jet across the central Great Basin
    also places eastern OR/western ID in the favorable left-exit
    region and provides additional upper lift for thunderstorm
    development and maintenance through early tonight. PW values range
    from 0.8-0.9" per SPC's mesoanalysis, which is +2.0 standard
    deviations above the climatological average for this part of the
    country. Additionally, SBCAPE values of 1,000-1,500 J/kg are
    sufficient for strong updrafts to tap into the available moisture.

    Current MRMS estimates for hourly rates are up to 1" near the John
    Day Highlands and 18Z HREF probabilities for over 1"/hr totals
    continue to exceed 20% until around 02Z. These rates when combined
    with coverage of thunderstorms could lead to flash flooding for at
    least a few additional hours should heavy rainfall overlap with
    the several sensitive burn scars across the region.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7be0Pbm6fH-fgJpB4gspljXV0quXMyItl4hE2nBrRSgVXv2Er_CsfEOoDsoRPWQ8435l= FQSSF5FPoYJdDIa1XLbyNDs$ for graphic product...

    ATTN...WFO...BOI...MFR...PDT...

    ATTN...RFC...PTR...RSA...NWC...

    LAT...LON 45151847 45111767 44851708 44161670 43271654=20
    42591663 42251706 42231760 42451794 43081834=20
    43241844 43561918 43392023 43392094 43642123=20
    44202091 44771975=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 12 04:51:09 2025
    AWUS01 KWNH 120451
    FFGMPD
    NDZ000-120930-

    Mesoscale Precipitation Discussion 1072
    NWS Weather Prediction Center College Park MD
    1250 AM EDT Fri Sep 12 2025

    Areas affected...northern ND

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

    Valid 120449Z - 120930Z

    SUMMARY...Repeating and training of thunderstorms over northern ND
    may result in localized flash flooding over the next 3-5 hours.
    Hourly rainfall of 1-2 inches and localized totals of 2-4 inches
    are expected (locally higher possible). Some of the expected
    rainfall could overlap with an area of heavy rain which fell
    during the day on Thursday over northeastern ND.

    DISCUSSION...Radar imagery from KMBX through 0430Z showed a small
    cluster of thunderstorms, located roughly 20-40 miles ENE of
    Minot, with a history of backbuilding and training. The storms
    were elevated in nature, located north of a stationary front which
    draped southeastward from southern ND, with a 25-35 kt 850 mb jet
    supporting overrunning and robust low level moisture transport
    through the northern Plains. SPC mesoanalysis data from 04Z showed
    MUCAPE of 2000-3000 J/kg PWATs of 1.5 to 1.7 inches over
    north-central and northeastern ND. In the upper levels, there was
    a focused area of divergence and diffluence positioned under the
    left exit region of a 90 kt jet max centered over UT/AZ.

    The RAP supports eventual veering and weakening of the low level
    jet between 06-09Z over the northern Plains which should help to
    dislodge the ongoing activity over ND and shift it toward the
    east. An area of MRMS-estimated 2 to 5+ inches of rain impacted
    portions of northeastern ND over the past 24 hours which has left
    soils locally more sensitive to runoff from additional rainfall.
    This area is located east of the ongoing thunderstorms over
    north-central ND. Until the storms begin to shift downstream,
    there will be a short term flash flood concern from
    backbuilding/training cells over north-central ND with eventual
    translation toward the east. Additional rainfall of 2 to 4 inches
    is expected (locally higher possible) which may result in
    localized flash flooding through 09Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_pXY7uPRFq5WQC_aw0NImY3WdQunlflK3SIFAz2vQvLnkIArIua0BrfPMAb4nB7H7v-w= hONEfRZf0CyPf7oKUZozXo8$ for graphic product...

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

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 49119947 48929771 48189779 47849922 47720044=20
    47730123 47930188 48450205 48860187 49040134=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 12 07:00:13 2025
    AWUS01 KWNH 120700
    FFGMPD
    FLZ000-121100-

    Mesoscale Precipitation Discussion 1073
    NWS Weather Prediction Center College Park MD
    259 AM EDT Fri Sep 12 2025

    Areas affected...east coast of FL

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

    Valid 120658Z - 121100Z

    Summary...Localized flash flooding will be possible along the east
    coast of FL from nearly stationary cores of heavy rain through
    11Z. Hourly rainfall totals of 2 to 3+ inches and localized total
    rainfall of over 4 inches may occur.

    Discussion...Reflectivity from KMLB and KAMX showed an axis of
    heavy rain aligned along and just offshore of the FL Peninsula,
    from Saint Lucie to Palm Beach counties. A lack of lightning
    within this axis inferred warm rain processes ongoing with
    estimated PWs of 2.0 to 2.3 inches and 1000-2000 J/kg MLCAPE via
    06Z SPC mesoanalysis data. MRMS-derived hourly rainfall has been
    in the 1.0 to 2.5 inch range over the past 2 hours. The rainfall
    appears to have formed along the land breeze boundary and water
    vapor imagery helped identify a subtle vorticity max between Grand
    Bahama and Palm Beach County, helping with lift across the region.
    There may also be right-entrance region divergence aiding lift,
    tied to a jet max positioned just off of the Carolina coast. VAD
    wind plots showed that onshore flow in the 925-850 mb layer was
    from the northeast, with advection of unstable air from the warm
    offshore waters pushing slightly inland. Weak steering flow was
    supporting slow net movement of cells. In addition, a weak surface
    low may be forming along a stationary front draped east to west
    across the southern Peninsula with return flow focused into the
    coast, to the north of the low.

    West to southwest flow aloft implies the vorticity max should
    advance farther away from the coast over the next few hours but
    some degree of onshore flow will remain in the short term,
    supporting the potential for continued slow moving/nearly
    stationary cores of heavy rain along the coast from roughly Palm
    Beach County to southern Brevard County. The environment favors
    the continued potential for hourly rainfall from 2 to 3+ inches
    and storm totals possibly over 4 inches. However, this flash flood
    threat looks to be rather localized and short term, focusing the
    greatest impacts with overlap of the urban corridor.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!61ZNJoEs-0noFmVEDkY0TkfuRlJDFZHrDAuTCoLazWNx_98B_rJgQgggtvP-5HOxIQdi= Qb7ZAb-KCOaDzoXB2kmjI6E$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 28348050 28158019 27687992 27137982 26727975=20
    26177984 26258022 27068038 28178072=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 12 18:07:20 2025
    AWUS01 KWNH 121807
    FFGMPD
    COZ000-NMZ000-AZZ000-UTZ000-122330-

    Mesoscale Precipitation Discussion 1074
    NWS Weather Prediction Center College Park MD
    206 PM EDT Fri Sep 12 2025

    Areas affected...Western CO...Eastern UT...Northwest NM...Far
    Northeast AZ...

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

    Valid 121805Z - 122330Z

    SUMMARY...Quick bursts of sub-hourly .5-.75" totals and isolated
    repeating spots that may have localized maxima to 1.5" through the
    afternoon will push naturally low FFG values, especially near burn
    scars and steep gulleys. A few spots of flash flooding are
    possible through the evening hours.

    DISCUSSION...GOES-East WV suite depicts a global scale meridional
    trough between 117W and 114W slowly shifting eastward, with strong
    core of energy just west of the base of the overall trough across
    the Lower Colorado Valley providing a favorable downstream
    environment to draw remaining enhanced sub-tropical moisture out
    of the Sea of Cortez northward across the Four Corners region into
    western CO. CIRA LPW, denotes core of the best moisture remains
    along and just west of the NM/AZ line through the lowest levels
    though surface Tds across the Four Corners into Western CO still
    above normal with mid-50s in AZ/NM and upper 40s to low 50s in the
    higher altitudes of the San Juans and further north.=20
    Additionally, WV suite shows a kink in the upper level jet pattern
    with expanding right entrance region across S UT into CO as the
    upstrem jet core rounds the base over the Lower Colorado. This
    will further enhanced surface to 700mb southwesterly flow while
    also providing solid larger scale UVVs and outflow to maintain
    convective clusters.=20

    Currently best convergent clusters reside on the northwest nose of
    the deeper level moisture across East central UT starting to
    spread across west-central to NW CO. Total Pwats of .75-1" are at
    1.5 standard anomalies and with strength of deep layer flux
    convergence is supporting some above average efficiency
    thunderstorm activity (including some that induced flash flooding
    further west in E UT). This includes increasing agitation/TCU
    field across SE UT, though larger clusters capable of .5"/hr
    totals continue to expand over SW CO. Cells are fairly
    progressive, but also have a weak training/repeating orientation
    as the overall height-fall axis presses eastward very slowly over
    the next few hours. Scattered to numerous spots of .25-.5"
    totals are probable, though isolated sub-hourly totals up to .75"
    and a random potential for repeats may result in a spot or two of
    1-1.5". The sheer rate within complex terrain and natural low FFG
    values in that .5-1"/hr range, along with noted burn scars
    suggested widely scattered incidents of flash flooding remain
    possible this afternoon into evening.

    Further south, the speed max rounding the base of the trof and
    overall slow eastward motions further increased DPVA and favorable
    enhancement of weak shortwave feature lifting out of Northern Old
    Mexico into SE AZ. Stronger thunderstorms are developing at the
    intersection of the SSWly enhanced LLJ flow and the Mogollon
    Rim/San Francisco Mtns. Redevelopment along those ridges is
    likely to continue and support downstream repeating clusters
    across W and NW NM and far eastern AZ. Deeper layer moisture of
    1.25 to 1.4", especially loaded below 700mb suggest slightly
    higher efficiency than further north and spots of 1" are probable
    and possible to induce localized flash flooding in prone arroyos.=20
    =20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9T-OLZ3E2BSJf-K05TlOENTOtCk0lJGlk96RvKzpPjAOTrSvHu7bPX-8MlLw7Jm-GqJd= yv0rmGbwOBgdQRSwIi13sPQ$ for graphic product...

    ATTN...WFO...ABQ...BOU...FGZ...GJT...PUB...SLC...

    ATTN...RFC...FWR...KRF...STR...TUA...NWC...

    LAT...LON 40810709 40570572 39460533 36370664 35080728=20
    34280778 33850854 33900944 34340996 34831000=20
    35950987 36970970 37620997 38471034 39690972=20
    40650849=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 12 19:55:22 2025
    AWUS01 KWNH 121955
    FFGMPD
    NMZ000-AZZ000-130100-

    Mesoscale Precipitation Discussion 1075
    NWS Weather Prediction Center College Park MD
    354 PM EDT Fri Sep 12 2025

    Areas affected...Southeast Arizona...Southwest New Mexico...

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

    Valid 121955Z - 130100Z

    SUMMARY...Increasing convective coverage and eventually rainfall
    rates. Isolated rates of 1-1.5" and scattered spots of 2" may
    pose localized flash flooding conditions through evening.

    DISCUSSION...CIRA LPW shows subtropical moisture plume from
    850-500mb core along and just south of the US/Mexico border
    between Santa Cruz county, AZ and central Dona Ana county, NM
    extending northward along the AZ/NM within strong southerly
    confluent deep layer flow. Deep layer bulk shear, remains strong
    with 35-45kts mainly along the upwind edge in SE AZ as strong
    upper-level flow slowly approaches from the west. The base of the
    strong upper-level trough is also ejecting a upper-level jet
    streak to further support large scale ascent and divergence aloft
    for thunderstorms that do develop.

    Nearly full insolation being well south of mid to upper-level
    cloud coverge due to the exiting shortwave over N AZ/SE UT, has
    allowed temperatures to rise into the 90s across the lower valley
    and through the mid to upper 80s into the slightly higher
    topography along and south of the Mogollon Rim in SE AZ/SW NM.=20
    MLCAPEs of 1500-2500 J/kg will support strong updraft developing
    and isobaric influenced moisture flux to any even weakly rotating
    updrafts. Given Tds in the 60s and the overall Total PWat values
    of 1.25 to 1.5", should support some localized 1-1.25"/hr totals
    (as instantaneous rates would be well over 2"). Deep layer flow
    may reduce residency at a given location, but with the upstream
    forcing remaining strong and slowly ejecting, should support back-building/upstream flank development to support
    repeating/training locally. As such, spots of 1.5-2" in 1-3 hours
    are likely to scattered across the area of concern. Given
    rugged, hard-pan soil conditions across many locations, FFG values
    are naturally below these hourly rates and therefore localized
    flash flooding conditions are considered possible through the
    remainder of the evening across SE AZ/SW NM.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4bpg3qr9z-sedWc8YUNdyNgjj0lK_zgXTenA9xgAkR5W16azxrzxt97ITFhY1_y04uC6= udddRvUAfSFZZnuMDV0uBb8$ for graphic product...

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

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 33900782 33220739 31900720 31700762 31630808=20
    31210816 31170923 31231101 31851145 33381091=20
    33801000=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 12 21:03:53 2025
    AWUS01 KWNH 122103
    FFGMPD
    NEZ000-SDZ000-MTZ000-WYZ000-130230-

    Mesoscale Precipitation Discussion 1076
    NWS Weather Prediction Center College Park MD
    503 PM EDT Fri Sep 12 2025

    Areas affected...Northeastern WY...Far Western SD...Southeast
    MT...

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

    Valid 122100Z - 130230Z

    SUMMARY...Stationary to slowly repeating cells near Big Horns,
    likely to expand in coverage with approach of shortwave.=20
    Localized totals of 2"+ are possible but very isolated. Flash
    flooding is possible, particularly near burn scars and/or complex
    terrain.

    DISCUSSION...GOES-E WV suite shows an anti-cyclonically arched
    outflow band of cirrus along/ahead of embedded shortwave now
    entering southeast WY. Along an north of the outflow band,
    divergence has been driving deep layer ascent across the Big Horn
    mountain range, where a few cells developed over the last few
    hours. Deep layer steering generally resulted in northeasterly
    motion and initial downdrafts were generally drier or hail
    producing. However, low level response has strengthened
    northeasterly flow from deeper low level moisture across SE MT
    banking it up against the Big Horns while, mid-level moisture from
    the approaching shortwave, along with initial up/downdrafts having
    moistened the profile. While some instability was lost to this
    moistening, RAP profiles and instability fields still strongly
    suggest ample 750-1250 J/kg of instability along the left exit of
    the outflow jet. Recent Visible and EIR imagery from GOES-E
    suggest continued updraft vigor across the central Big Horns with
    increasing rainfall rates likely. Lightning from GLM/NLDN
    suggests a few stronger embedded rotating updrafts will likely
    keep the heavy rainfall footprint to be more isolated in nature.=20
    Total PWat values increase to 1" and given Tds in the low 50s, and
    solid moisture flux convergence, rates of .75"/hr are probable.=20=20
    This appears likely to continue for an additional hour or two.

    Upstream, the main shortwave is providing even further broader
    scale DPVA and therefore ascent. Banded Cu fields are starting to
    sprout stronger TCus and CBs across central WY. The increase in
    coverage and further deepening of mid-level moisture will
    eventually expand overall coverage of convection capable of
    localized .5-1" hour totals. Some flanking development may allow
    for some enhanced streaks of higher totals. As such, overall
    coverage is not likely to be high, but isolated totals of 1.5-2"+
    are probable and in proximity to terrain or steep river
    valleys/bluffs may result in localized flash flooding conditions.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5lEcyKsKzLRwa9Won-7uzYahcsgp61dz9-J-n0u2jcDVovsdeLRAeLVW2XBE0vCE_t3A= zUW8PovJ73NS8_Dp800syR4$ for graphic product...

    ATTN...WFO...BYZ...CYS...RIW...UNR...

    ATTN...RFC...KRF...NWC...

    LAT...LON 45970457 45710372 45280334 44650311 43710317=20
    42790416 42130578 42210690 42930746 44200744=20
    45370685 45930560=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 12 21:48:23 2025
    AWUS01 KWNH 122148
    FFGMPD
    MTZ000-130245-

    Mesoscale Precipitation Discussion 1077
    NWS Weather Prediction Center College Park MD
    547 PM EDT Fri Sep 12 2025

    Areas affected...North central Montana...

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

    Valid 122145Z - 130245Z

    SUMMARY...Stationary to very slow moving thunderstorms capable of
    1-"/hr and localized 1.5-2.5" totals pose localized flash flooding
    conditions through the evening.

    DISCUSSION...GOES-E WV suite depicts area of concern is located
    along the eastern edge of the northern portion of a large global
    scale meridional trough that extends from southern Alberta to the
    Lower Colorado River Valley in CA/AZ. Embedded within, are
    smaller shortwave centers, one lifting northwest to reinforce the
    apex of the larger trough and the center core over the W MT
    borders. This placement provides solid height-falls to support
    low level easterly flow out of the northern Plains where
    seasonally abnormal deep layer moisture resides, with nearly 2 to
    3 standard deviations from the Sept mean over the Dakotas. Though
    the anomalies are a bit less across the area of concern, the
    strength of the eastern flux over the last few hours along with
    solid insolation supported enhanced conditionally unstable air,
    generally centered through the Little Belt Mountains and Judith
    Basin of central MT. Total Pwats are nosing up from .75 toward 1"
    though heating and modest lapse rates support 500-1000 J/kg of
    MLCAPE.=20

    Convergence along the terrain supported convective initiation a
    few hours ago and rates of .75"/hr have been estimated with some
    higher values likely contaminated with hail, though that adds to
    moisture on the ground. The concern here, though resides in
    duration as mid-level steering flow is very weak at 15-30kts
    (increasing to the east), but in proximity to left exit of the
    larger scale anticyclonically curved jet over SE MT, providing
    divergence aloft. As such, effective cell motions are mainly
    driven on propagation/regeneration of updrafts along the outflow
    boundaries. This allows for some 1-2 hours of near stationary
    rates supporting some localized totals up to 2". Current trends
    in Visible/IR and GLM/NLDN lightning suggest further expansion
    northward across Chouteau and Blaine counties with trends that
    suggest mergers may result and increase rainfall efficiency toward
    1-1.25"/hr. Given FFG values of 1-1.25"/hr and generally less
    than 2"/3hrs, widely scattered incidence of exceedance and
    therefore potential localized flash flooding is considered
    possible through evening.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4IznCq-I-ZesXHtjHmIxjzpzKT_MyI23oO9G_ANceUTi01uwqPkeLetWxM-GGIkxLo-j= yPdXhIenD3lpvnq2ejmRVe0$ for graphic product...

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

    ATTN...RFC...KRF...NWC...

    LAT...LON 49031013 48990897 48930779 48390761 47370792=20
    46530846 46290904 46420964 46671004 47031069=20
    47311129 47811149 48831126=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 12 23:43:54 2025
    AWUS01 KWNH 122343
    FFGMPD
    SDZ000-NDZ000-MTZ000-WYZ000-130545-

    Mesoscale Precipitation Discussion 1078
    NWS Weather Prediction Center College Park MD
    743 PM EDT Fri Sep 12 2025

    Areas affected...Southwest ND...Northwest SD...Far Southeast
    MT...Far Northeast WY...

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

    Valid 122345Z - 130545Z

    SUMMARY...Slow moving, increasingly efficient thunderstorms
    capable of 1.75"/hr and localized totals of 2-3.5" across
    south-central ND with possible flash flooding, before expanding
    development from approaching wave increases convective coverage
    into the early overnight period.

    DISCUSSION...GOES-E Visible/10.3um EIR loops show an expanding
    cluster of strong updrafts and expanding anvil canopies across
    south-central ND with a few additional upstream cells developing
    ahead of the main approaching wave out of E WY. Surface analysis
    shows a narrow SW to ENE convergence axis from HEI and between
    KY19 and K7L2, which due to some enhanced low level moisture
    pooling and solid heating throughout the day, resulted in an axis
    of enhanced conditionally unstable air with 2500-3000 J/kg of
    MLCAPE available for the strong updrafts. A deep surface cyclone
    in the mid-Missouri River Valley across SD, further enhanced low
    level confluence/convergence while increasing though depth to
    support enhanced moisture with localized pockets noted in the
    lower 3 layers, surface to 850, 850-700 and 700-500mb in the CIRA
    LPW products; resulting in well above normal moisture (nearly 2-3
    std anomalies from Sept norms).

    The catalyst toward greater expansion is the slightly faster than
    progged, jet speed max enhanced by upstream convection along/ahead
    of main shortwave feature moving northward through the broad south-southwesterly flow. Broadening diffluence at the apex of
    the 500mb ridge is providing oblique divergence aloft to support
    broader scale ascent and reducing low level inhibition. Now with
    expanding thunderstorms, the deep layer flow in combination with
    the surface low in SD, is reducing forward propagation at the apex
    of the 500-1000mb thickness ridge, mid-level DPVA upstream further
    results in backed lower level flow to help with back-building
    environment for effective stationary to slow moving cell
    development, while continuing easterly inflow of unstable/moist
    air. As such, expanding downdrafts with ample moisture flux will
    support 1.75-2"/hr rates over the coming hours and with slow
    motions, localized totals of 2-3.5" are becoming more probable.=20
    West of the Missouri River in SW ND and NW SD, FFG values are
    naturally lower and 1hr FFG values of 1-1.5"/hr & 1.5-2"/3hrs are
    likely to be locally exceeded, suggesting a few incidents of flash
    flooding. Combine with an additional upstream round of strong,
    but progressive thunderstorms to further add to these scattered
    localized pockets of 2-3.5" and flash flooding is considered
    likely this evening into the early overnight period.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4b4jztBNOIchkIQzilcMlouvr6YDg8_GNva4C77sO6b5HQ2SwHtYAIViP3QuZZ3d1kpu= 6uJmAt4ej1TzAoVfVrxmb4k$ for graphic product...

    ATTN...WFO...ABR...BIS...BYZ...UNR...

    ATTN...RFC...KRF...NWC...

    LAT...LON 47240120 47079984 46449945 45669994 44970132=20
    44200330 44530447 45610459 46460358 47000241=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 13 00:27:26 2025
    AWUS01 KWNH 130027
    FFGMPD
    TXZ000-NMZ000-AZZ000-130600-

    Mesoscale Precipitation Discussion 1079
    NWS Weather Prediction Center College Park MD
    826 PM EDT Fri Sep 12 2025

    Areas affected...Southeast Arizona...Southern New Mexico...

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

    Valid 130030Z - 130600Z

    SUMMARY...Isolated totals of 1-2" in less than 3 hours continue to
    pose widely scattered incidents of flash flooding possible through
    early overnight period.=20

    DISCUSSION...Deep layer confluent southerly flow continues to
    slowly press eastward across central CO through central NM. While
    deep south-southwesterly flow is pooling moisture out of the Sea
    of Cortez through the Mexican Sierra Madre Occidental, it is
    starting to angle more southwesterly and with less direct flow.
    However, this may be compensated with some minor upslope flow
    through the Rio Grande Valley and Southern Plains (per CIRA LPW,
    Surface to 700mb layers). However, instability is reducing along
    the downstream edge into the Southern High Plains and activity
    will reduce in coverage and intensity through time, but some
    isolated .75"/hr and totals to near 1.5" are possible.

    Along the western edge of the deep layer moisture, fading visible
    imagery loops and limited surface observations suggest, westward
    propagation of the upwind edge remains across SE AZ. As the base
    of the larger scale trough exists, continued upslope moist flow
    will continue to support scattered to widely scattered
    thunderstorms, but with solid bulk shear; updraft rotation should
    concentrate moisture flux convergence to support efficient
    rainfall production given 1.25-1.5" total PWats. Rates of
    1-1.25"/hr remain possible. Deep layer steering may allow for
    some of the widely scattered cells to cross tracks with earlier
    rainfall tracks maintaining isolated incidents of flash flooding
    into the early overnight period across SE AZ into SW NM.=20=20


    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7oBswKL6qfz7lvcDYgPxzo1mk8cnZxDpQlg7Q1ae80qYVUQ7HJAaRmxHYQt90lYi95Vl= UsqHPJb_pu9Ho6LpNgJLEjI$ for graphic product...

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

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 35660628 35480520 34550473 32780510 31740637=20
    31690798 31230810 31170943 31151036 31281091=20
    32281059 33780957 35090788=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 13 06:24:29 2025
    AWUS01 KWNH 130624
    FFGMPD
    SDZ000-NDZ000-131200-

    Mesoscale Precipitation Discussion 1080
    NWS Weather Prediction Center College Park MD
    223 AM EDT Sat Sep 13 2025

    Areas affected...western ND into western/central SD

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

    Valid 130622Z - 131200Z

    SUMMARY...Scattered thunderstorms with periods of embedded training/backbuilding will pose a possible threat for flash
    flooding over the northern High Plains through 11Z. Hourly
    rainfall of 1.0 to 2.5 inches will be likely at times.

    DISCUSSION...Area radar imagery over the northern High Plains at
    06Z showed a NW to SE axis of thunderstorms advancing
    northeastward from southwestern ND into west-central SD, along
    with a few slower moving cells over northwestern ND. This activity
    was located out ahead of a mid-level vorticity max and
    southeastward extending shortwave trough axis located over WY.
    Numerous smaller scale vorticity maxima were embedded within the south-southwesterly flow aloft into the High Plains, out ahead of
    the shortwave trough, helping to focus areas of thunderstorms
    within areas of surface convergence beneath a diffluent and
    divergent flow pattern in the upper levels. SPC mesoanalysis data
    from 06Z showed CAPE of 1000 to 2000+ J/kg along with anomalous
    PWs of 1.3 to 1.5 inches over the western Dakotas, but with only=20
    a few small pockets of weak to negligible convective inhibition.
    Easterly low level upslope flow was in place over portions of the
    western Dakotas, aiding in convergence/ascent ahead of the
    advancing convective segment tracking through southwestern
    ND/west-central SD.

    Synoptic and mesoscale forcing aloft, out ahead of the main
    shortwave trough over the High Plains, combined with areas of
    surface convergence will likely maintain scattered thunderstorms
    over portions of the western Dakotas through the overnight, with
    potential for redevelopment and expansion of thunderstorms over
    western SD over the next 1-2 hours. While the evolution of
    convection over the next few hours looks a bit messy, flash flood
    guidance is relatively low over western SD and portions of western
    ND, with values between 1 and 2 inches in an hour. Some exceedance
    of these lower flash flood guidance values are expected with areas
    of flash flooding possibly resulting over the next 3 to 6 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6GKoZSud3hJ1MyCTViP7Xnu6BfC3lmjcoymGD8vGRCfo0fthLRciCtdkckxTq6Wv1xs8= JEjcDzs-5v7bI0U0z9Xbw5k$ for graphic product...

    ATTN...WFO...ABR...BIS...UNR...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 49110306 49010183 48430157 47280102 46420029=20
    45369974 44050027 43280161 43530294 44290358=20
    45710357 47520386 48960373=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 13 19:40:10 2025
    AWUS01 KWNH 131940
    FFGMPD
    TXZ000-NMZ000-AZZ000-140115-

    Mesoscale Precipitation Discussion 1081
    NWS Weather Prediction Center College Park MD
    339 PM EDT Sat Sep 13 2025

    Areas affected...New Mexico...Far Southeast Arizona...Portions of
    Western Texas Panhandle...

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

    Valid 131940Z - 140115Z

    SUMMARY...Deep layer available moisture and sufficiently unstable
    environment to support storms capable of up to 1"/hr. Some
    favorable development lines and deep layer flow may result in
    repeating tracks and localized spots of 2", resulting in possible
    widely scattered, but localized flash flooding throughout the afternoon/evening.

    DISCUSSION...Core of strong large scale trof continues to slowly
    lift northeastward across southern UT with solid downstream
    height-falls supporting broad scale ascent pattern allowing for
    increased overall convective coverage today. The deep layer
    sub-tropical moisture has further angled SW out of the northern
    Mexican Plateau into southern New Mexico, though the western
    gradient remains across far SE AZ into north-central NM. However,
    this is shifting eastward with strong, well defined dry slot
    (700-500mb CIRA LPW denotes this very well) off the San Francisco
    Plateau through the Four Corners. This is overall narrowing the
    moisture plume, but also increasing southeasterly upslope flow and
    surge of Gulf of America moisture through the Rio Grande/Pecos
    River Valley into the NM High Plains.=20=20

    Solid clear skies, particularly west of yesterday's leading height-fall/pressure trough currently seen through the TX
    Panhandle back southwest through the Davis Mountains and western
    TX panhandle. As such, surface temperatures have supported a
    solid increase in instability fields, slightly higher further
    southward given deeper overall moisture (Tds in the low 60s) and
    good lapse rates, though still with ample deep layer moisture to
    support efficient rainfall production.=20

    At this time, SW to NE linear features are expanding in convective
    anvils and embedded overshooting tops across far SE AZ and SW and
    west-central NM. Orientation is parallel to the mean flow so some
    repeating tracks are probable. However, cell motions are above
    normal limiting overall duration of any internal core, still quick
    burst of .5" totals and 1-1.25"/hr totals could be possible with
    said repeating. Hard ground conditions/naturally lower FFG values
    suggest localized exceedence is possible resulting in possible
    localized flash flooding.

    As the afternoon progresses, SSW to NNE 70 jet streak will
    continue to lift north across CO and increasing diffluence will
    further expand already sufficient divergence area, for further
    uptick in convective coverage with expanding clusters across
    central NM into the High Plains. The further acceleration of
    deeper moisture should also increase rainfall efficiency toward
    late evening (after 00z) with rates of 1-1.5"/hr becoming
    possible. An update to the MPD may be required as these clusters
    grow upscale later this evening.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7G_ir-FoXeVBA-9DkzF9snX7eZdnaBBt8lbX58RydRTFJF_8RvGni2LJH5Ii-J6_MBLD= kl_Jk2R6QhoX1JqhqyPtqM4$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...TWC...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 36870499 36840389 36320321 35130314 33120322=20
    32430404 31240490 31010565 31700679 31660792=20
    31230809 31180863 31220974 31311045 32371063=20
    33370940 34460826 35490738 36530617=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 13 20:20:39 2025
    AWUS01 KWNH 132020
    FFGMPD
    COZ000-UTZ000-140130-

    Mesoscale Precipitation Discussion 1082
    NWS Weather Prediction Center College Park MD
    420 PM EDT Sat Sep 13 2025

    Areas affected...Southeast Utah...Western Colorado...

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

    Valid 132020Z - 140130Z

    SUMMARY...Expanding slow moving, rotating cells capable of quick
    1"/hr rates and localized scattered incidents of flash flooding in
    arid, rugged terrain likely to continue through the evening.

    DISCUSSION...GOES-E WV suite shows core of strong base of larger
    scale trough is centered across south-central UT, slowly lifting
    ENEward. Strong DPVA and broad divergence along the UT/CO border,
    along and east of the 3H trof and west of the 50-80kt 3H jet is
    providing strong vertical ascent across much of the area of
    concern. Deep layer moisture has been pressed further east in the
    warm conveyor belt, but sufficient lingering westward wrapping of
    the western branch of the TROWAL has maintained a solid moisture
    gradient across SE UT into SW and south-central CO, all while the
    strong, well defined dry slot under-cuts the circulation across NE
    AZ/NW NM. CIRA LPW denotes this evolution very well, with still
    some lingering enhanced moisture to feed the strong vertical
    development noted in Visible and 10.3um EIR loops.=20

    Total moisture, mainly loaded from 850-700mb only totals about
    .75" but with north to northeast flow fluxing into the stronger
    cells along the northwest edge of the dry slot; sub-cloud
    evaporation is helping to moisten the full profile while
    intra-cloud processes slowly increase rainfall
    generation/efficiency. Effective bulk shear to 40kts, also helps
    to keep updrafts rotating, increasing moisture flux convergence
    through the lower profile and supporting rates up to 1"/hr.=20
    Additionally, being north of the stronger southwesterly steering
    flow also will slow northeastward cell motions up to 5-10kts and
    with Bunker's right moving propagation vectors near 15-20kts
    further aides residency of the stronger/broader up/downdrafts
    allowing for some localized 1-2" totals. Given the naturally
    arid, rugged geological formations, little infiltration is
    expected resulting in high run-off and localized flash flooding.=20
    Remaining pockets of 1000-1500 J/kg of MLCAPE and favorable slow
    northeastward drift across W CO, will likely maintain the risk for
    these local flash flooding incidents through the remainder of the
    evening.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_bPJikECOFoz7t_FqR15qvJnvKlZ_gNlH3pkWnDu-kfYcwOwDLomGTM72Qlc3cJUYaDz= wBX5SN7TiTql8DAoNowygyk$ for graphic product...

    ATTN...WFO...GJT...PUB...SLC...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 40340733 40070676 39140640 37990599 37110609=20
    37000708 37040849 37090964 37511045 38231041=20
    39000967 39880847=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 13 21:18:13 2025
    AWUS01 KWNH 132118
    FFGMPD
    NDZ000-MTZ000-140230-

    Mesoscale Precipitation Discussion 1083
    NWS Weather Prediction Center College Park MD
    517 PM EDT Sat Sep 13 2025

    Areas affected...Northwest NDak...East-central & Northeast MT...

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

    Valid 132115Z - 140230Z

    SUMMARY...Highly anomalous moisture, increasing instability and
    slow cell motions with some back-building training possible.=20
    Rates of 1.5"/hr and localized 2-3" totals may result in possible
    scattered incidents of flash flooding through early overnight
    period.

    DISCUSSION...GOES-E WV suite shows a conducive dynamic environment
    aloft to maintain and support new convective development within a
    seasonally, highly anomalous moisture regime. The northern,
    smaller closed low/short-wave to the parent large scale meridional
    trough is well defined and compact over central MT. It is
    connected via a boundary layer convergence/confluence axis that
    waves eastward before turning north along/just west of the MT/ND
    border where it eventually connects back up to the exiting
    vorticity center over southwest Canada. Along and east of the
    confluence boundary, deep layer moisture with highly anomalous
    (2-4 standard anomaly units) above average exists across the
    Northern Plains. Upper 60 to low 70s Tds with southeasterly flow
    strengthening to 20kts at 850 provide deep layer convergence to
    the boundary.=20

    GOES-E Visible imagery shows developing overshooting tops through
    the mid-level cloud deck along the boundary, some denoting some
    Wedge/'V' shaped signatures. This is indicative of the exiting
    upper level 70kt speed max and the cells moving into better right
    entrance ascent. Combine this with sharply arched cirrus canopy
    over central SD denoting the nose of the next speed max suggests
    this favorable divergence aloft will likely maintain for quite a
    few hours into the early overnight period. Limited motion of the
    convergence boundary is expected given the surface to low level
    flow, providing a solid opportunity for convective cells to
    train/repeat over NW ND through the evening. The limiting factor
    continues to be the lack of surface heating due to the mid-level
    canopy, so vertical vigor may limit overall rainfall
    production/intensity in the range of 1-1.5" (given total PWat
    values of 1.5-1.7") and CAPE 500-750 J/kg. As such spots of 2-4"
    are possible resulting in possible flash flooding.

    Further west,
    Clearer skies, has supported some low level heating near the
    stationary mid-level feature and eastward along the low to
    mid-level shear axis into eastern MT. A few stronger cells have
    developed, utilizing the enhanced surface heating and weak to
    moderate convergence. Limiting factor with these cells mainly in
    in the deeper moisture profile. While still above normal Tds in
    the low 50s and total Pwats range from 1-1.25". This should
    reduce overall efficiency and rates to around 1-1.25"/hr but slow
    cell motions perhaps even stationary near the vorticity center
    itself could result in localized 2-3" totals in 3-6hrs. Recent
    rainfall and FFG values in the 1-1.5"/hr & 1.5-2"/3hrs suggest
    these rates/totals may result in an incident or two of flash
    flooding through the evening.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-9oKTOZFx8OhC-Giohk7XbHE7S77PP1jzDox3MeYvKRp4E6NkOBkJ_UIGAPtfcy9q9Nf= 1nVl_4wd0IyWEGVeN8arw8c$ for graphic product...

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

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 49100372 49100195 48970143 47790197 47080269=20
    46510356 46050498 46160712 46190863 46330927=20
    46850995 47500964 47690877 47730798 47970679=20
    48390554 49050456=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 14 04:37:19 2025
    AWUS01 KWNH 140437
    FFGMPD
    TXZ000-NMZ000-141000-

    Mesoscale Precipitation Discussion 1084
    NWS Weather Prediction Center College Park MD
    1236 AM EDT Sun Sep 14 2025

    Areas affected...West TX into southeastern NM

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

    Valid 140435Z - 141000Z

    SUMMARY...Isolated to widely scattered areas of flash flooding
    will be possible across a fairly broad region of western TX into
    southeastern NM through 10Z. Cells containing periods of training
    and/or slow movement will be capable of 1-2 in/hr rain rates and
    isolated totals in excess of 2 to 3 inches.

    DISCUSSION...Radar imagery from 0415Z showed a broken line of
    thunderstorms extending from the TX Panhandle into southeastern NM
    across Roosevelt and Lea counties. Meanwhile, cell coverage was
    increasing across the Trans-Pecos region of far western TX with
    general movement toward the east. These thunderstorms were located
    ahead of the southern portion of a shortwave trough crossing
    central NM with broadly diffluent flow located aloft across the
    region. In the lower levels, 850 mb wind speeds have been
    increasing as noted via VAD wind data from KMAF and KLBB with
    30-35 kt at 04Z, a 15-20 kt increase since 01Z. These winds have
    been coincident with a surge of low level moisture advecting
    northward up the Rio Grande Valley as viewed on the sfc-850 mb
    layer of OSPO LPW imagery. PW anomalies were +1 to +2 standard
    deviations above the mean and MLCAPE was estimated via 04Z SPC
    mesoanalysis data to be 500-1000 J/kg with varying degrees of
    inhibition.

    Forcing ahead of the eastward advancing mid to upper-level trough
    and mesoscale axes of lift/convergence at the leading edge of
    ongoing convective outflow, the low level jet and terrain
    influences are likely to continue scattered thunderstorms over the
    next 3-6 hours. With the mean steering flow oriented generally
    from the west (SW to NW), any convective line orientation matching
    the steering flow will support training and potential for 1-2
    in/hr rain rates. This is most likely from the TX Panhandle
    southward to about I-10. Farther south across the Trans-Pecos,
    scattered cells are likely to continue as they track east into the strengthening low level jet (forecast to reach 40-45 kt by 08Z)
    with brief instances of repeating and training possible.

    Overall, the flash flood threat appears to be low, but a couple of
    areas could see a quick 2 to 3+ inches of rain which may lead to
    flash flooding depending on exactly where this occurs in relation
    to locally sensitive areas across western TX.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8YI7bZIpIko-K8nRck8Z-AdO4-FwXq3Op_CU5Z_QIwsB3bSpvU5341fUzJNF8P8yW9tO= hMqOcokc1ba4TKcR_gPKLE8$ for graphic product...

    ATTN...WFO...ABQ...AMA...EPZ...LUB...MAF...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35110122 34810029 34250013 33150050 31390146=20
    30330227 29450309 28970358 29080420 29460483=20
    30100501 30940575 31650608 32190566 32680446=20
    33720340 34300252 35010211=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 14 18:34:28 2025
    AWUS01 KWNH 141834
    FFGMPD
    SDZ000-NDZ000-150000-

    Mesoscale Precipitation Discussion 1085
    NWS Weather Prediction Center College Park MD
    233 PM EDT Sun Sep 14 2025

    Areas affected...central North Dakota

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

    Valid 141830Z - 150000Z

    Summary...Localized rainfall totals as high as 3-4" in 2-3 hours
    may result in isolated instances of flash flooding.

    Discussion...A mid-upper level shortwave trough lifting north
    across the Central High Plains is driving the organization of deep
    convection over north-central SD early this afternoon, as a
    strengthening area of low-level (concentrated at 850 mb) moisture
    flux transport becomes better aligned with the right-entrance
    region of a ~100 kt jet streak centered near eastern MT into
    Saskatchewan, Canada. While lapse rates are unimpressive overall
    (solidly moist adiabatic throughout the low to mid-level profile),
    MUCAPE of 250-500 J/kg has been sufficient with aforementioned
    strong dynamics to result in efficient 1-3"/hr rainfall
    accumulations (with PWs of 1.5-1.7" near record territory for
    mid-Sep, closer to the max moving average of the climatological
    peak during late July and early August).

    Localized south-to-north training of convection within the=20
    meridional flow regime will likely result in additional 2-3"
    totals, and may locally exceed 3" (per 12z HREF neighborhood
    probabilities of 20-40%). While USGS streamflows in the region are
    generally indicated to be above normal, tributaries of the
    Missouri River are well below flood stage. Therefore any isolated
    instances of flash flooding should be confined to particularly
    vulnerable low-lying areas (with urbanized surfaces quite limited
    in this rural area) that receive as much as 3-4" of rainfall in
    2-3 hours.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-fCmDq4-APeJaEJlYRovtuTiLtGng8VvbtMLV4QfcLUK6G5NtFU72e6wosk17mLahEtj= Lr2OIBWSgsKcEj5MdzhkIhg$ for graphic product...

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

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 49180048 49049938 47719957 46589979 45749999=20
    45440074 45750148 46950168 47760162 48730160=20
    49120120=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 14 21:27:01 2025
    AWUS01 KWNH 142126
    FFGMPD
    KSZ000-NEZ000-150200-

    Mesoscale Precipitation Discussion 1086
    NWS Weather Prediction Center College Park MD
    526 PM EDT Sun Sep 14 2025

    Areas affected...South-Central Nebraska...Adj Northwest Kansas...

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

    Valid 142130Z - 150200Z

    SUMMARY...Very slow moving thunderstorms capable of 1.5"/hr with
    possible short-term mergers up to 2"/hr locally may result in
    scattered 2-4" totals over the next few hours before eventual
    increased propagation eastward.

    DISCUSSION...GOES-E WV suite shows core of mid-level closed low
    over the southern Sand Hills of Nebraska, with a smaller scale
    vorticity center rotating around the northern into the northwest
    quadrant of the larger parent. This has sharpened the southern
    base of the larger scale center, allowing for early afternoon
    clearing to enhanced insolation and increase broader pool of
    unstable air with narrow pool of 2000 J/kg CAPE be maintained
    across south-central Nebraska, along and east of the slow moving
    frontal zone. With bulk of stronger mid-level forcing and solid
    eastern side meridional jet, the unstable air south of the Sand
    Hills still has sufficient moisture angled back toward a weak
    surface inflection near McCook. Tds in the mid 60s and total PWat
    values of 1.25 to 1.4" fluxed on slightly backed surface to
    boundary layer flow has maintained solid deep layer moisture flux
    convergence for isolated cells (southwest Custer county over the
    last few hours) to start increasing in coverage, expanding into
    far northwest KS. Hourly rates of 1.5"/hr are likely and with
    very slow cell motions nearly directly under the steering flow
    axis, shows only very slow eastward propagation over the next few
    hours. As such, localized totals of 2-4" are becoming more
    probable, given slow motions and remaining instability/moisture
    pool downstream.=20=20

    Limiting factor toward flash flooding is, typical of the region,
    soil conditions being near the Sand Hills. However, lower FFG
    south of the main Hills region through the Platte River Valley and
    across into N KS are 1.5"/hr and generally 2-2.5"/3hrs; given area
    is in prolonged drought with 0-40 cm soil saturation ratios below
    10%, the top portions may have become a bit more hydrophobic, and
    given intensity of rates, may result in increased runoff and
    possible incidents of localized flash flooding.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8_b5T0SXqTS89SLz4voo1SPwFglBjbJ3oDM0DNN0FtBhAwfsXU4v67guPn3hTcr_BhZo= b8LHzZCmWIdTm_6KCMzV5IY$ for graphic product...

    ATTN...WFO...GID...GLD...LBF...

    ATTN...RFC...KRF...NWC...

    LAT...LON 41859888 41659855 40579862 39569922 39420057=20
    40000109 40710098 41180063 41390032 41779966=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 15 03:48:08 2025
    AWUS01 KWNH 150348
    FFGMPD
    TXZ000-OKZ000-150715-

    Mesoscale Precipitation Discussion 1087
    NWS Weather Prediction Center College Park MD
    1147 PM EDT Sun Sep 14 2025

    Areas affected...TX Panhandle into western OK

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

    Valid 150345Z - 150715Z

    Summary...Brief training of thunderstorms may result in 2+ inches
    of rain in an hour or less along with isolated flash flooding
    across the TX Panhandle and possibly into western OK. The threat
    Is expected to persist for at least a couple more hours.

    Discussion...KAMA reflectivity at 0330Z showed a small area of
    thunderstorms over the northeastern TX Panhandle into far western
    OK, drifting south but also backbuilding toward the west. The
    storms formed along a weak, retreating dryline which has moved
    westward to near Cannon AFD as of 03Z. A southward sinking
    boundary was evident via surface observations and reflectivity
    data, a combination of outflow and a weak cold front which has
    pressed south of Dalhart and Dumas since 00Z. Meanwhile, southerly
    850 mb winds were increasing across West TX with RAP forecasts
    indicating speeds near 30 kt by 06Z.

    Given MLCAPE of roughly 1000-2000 J/kg over the Panhandle (00Z AMA
    sounding and SPC mesoanalysis) and relatively weak CIN which
    should continue to be overcome by overrunning of the southward
    sinking psuedo-cold front, thunderstorms are expected to persist
    for another couple of hours. Periods of backbuilding are likely to
    continue and with mean westerly flow aloft, some training could
    result. Earlier rainfall measurements over the northeastern TX
    Panhandle showed ~0.75 inches of rain in 15 minutes, which could
    result in 2+ inches of rain in an hour or less should training
    persist long enough over a given location. The flash flood threat
    should remain isolated in nature but also persist for an
    additional 2-4 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-7EI611l50GQRgfoignEVvvvS4WIk2IVD_VSEJ9nlW9qskEN8A8UNRQ8OWXeA1EjMwfm= rhNd9VpoGNlnXbdzr8gBrD4$ for graphic product...

    ATTN...WFO...AMA...OUN...

    ATTN...RFC...TUA...NWC...

    LAT...LON 36129985 35669969 35229988 35030039 34900123=20
    35140190 35670199 36080140 36100054=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 15 05:50:38 2025
    AWUS01 KWNH 150550
    FFGMPD
    SDZ000-NDZ000-151145-

    Mesoscale Precipitation Discussion 1088
    NWS Weather Prediction Center College Park MD
    149 AM EDT Mon Sep 15 2025

    Areas affected...central to western ND

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

    Valid 150547Z - 151145Z

    SUMMARY...Slow moving showers and thunderstorms will pose an
    isolated risk for flash flooding for central and western ND
    through 12Z. Hourly rainfall of 1 to 2 inches is expected along
    with 2 to 4 inch storm totals.

    DISCUSSION...GOES-E WV suite showed a NW to SE elongated mid-level
    low centered over western SD at 0530Z, slowly lifting north, with
    embedded smaller scale vorticity maxima. These vorticity maxima
    were contributing to widely scattered showers and thunderstorms
    from the ND/SD border into western ND. The environment across the
    western half of ND was characterized by a small pocket of 500-1000
    J/kg MLCAPE and 1.3 to 1.6 inch PWATs (90-95th percentile) via 05Z
    SPC mesoanalysis data. MUCAPE values were slightly higher with low
    LPL levels below 750m AGL.

    As the closed low moves north over the next 3-6 hours, a
    combination of slightly colder 500 mb temperatures (locally
    increased instability) and associated vorticity maxima are
    expected to lead to development of additional showers and
    thunderstorms over west-central ND. Deep layer mean winds beneath
    the closed low were fairly weak at 10 kt or less, which will
    support slow moving cores of heavy rain, with the expected
    coverage of slow moving cores peaking over the next 2-5 hours. The
    anomalously moist environment and slow moving cores of heavy rain
    should lead to hourly rainfall of 1 to 2 inches along with spotty
    2-4 inch storm totals. These localized heavy rainfall areas may
    lead to isolated flash flooding through 12Z considering 3-hr FFG
    values below 2 inches in many locations.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8JvCWaV2gr9UM0b8XuReM0k0df62_TYCVZ6XJmm9C7plvOYDRWV4LMy0VRNbnWpU7ICj= 7xUBtSSW-bRr-8LwXuO11Y0$ for graphic product...

    ATTN...WFO...ABR...BIS...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 49110183 49000131 48470118 47820084 46980035=20
    46380031 46000082 45870163 46100259 46740342=20
    47770369 48830356 49050295 49070234=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 15 20:32:36 2025
    AWUS01 KWNH 152032
    FFGMPD
    MOZ000-ARZ000-160100-

    Mesoscale Precipitation Discussion 1089
    NWS Weather Prediction Center College Park MD
    431 PM EDT Mon Sep 15 2025

    Areas affected...North to South Central Missouri...Far
    north-central Arkansas...

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

    Valid 152030Z - 160100Z

    SUMMARY...Band of slow moving pulse-like convection with
    1.5-1.75"/hr and widely scattered localized totals to 2"+ in 1-3
    hours. Localized flash flooding and low-water crossing issues are
    possible through evening.

    DISCUSSION...A narrow ribbon of enhanced moisture and low-level
    theta-E is being squeezed by oblique passing of very broad/strong
    upper-level trough over much of the Northwest CONUS and return
    flow under the closed ridge over the Great Lakes. This ribbon of
    1.5-1.75" extends along the Upper Mississippi River through MO
    into central Arkansas. Solid surface heating with temperatures
    into the low 90s over mid 60s Tds supported fairly unstable
    environment with 2000-2500 J/kg of MLCAPE along the eastern/upwind
    edge of the deeper moisture plume.=20

    The deeper layer confluence, along with weakened cap resulted in
    initial thunderstorms, though recent uptick has been noted over a
    much longer length of the instability/moisture axis. Strong
    updrafts with numerous overshooting tops dotting the length of the
    convective line, from Shelby to Osage to Texas and to Howell
    county in MO, becoming more scattered further south where
    mid-level convergence is slightly reduced (nose of return flow
    across south-central MO).

    Very oblique right entrance divergence and subtle 20kt effective
    bulk shear may allow for some vertical disconnect to the
    up/downdraft couplets to support a few updraft cycles, though
    overall organization is fairly weak and cell longevity is likely
    to be limited to 1-2 hours. However, vertical loading to the
    downdraft and very slow cell motions may allow for rates of
    1.5-1.75"/hr and may result in widely scattered 2"+ totals in less
    than 2hrs. Overall, the grounds are quite dry with 0-40cm
    relative soil moisture at or below 30%, so while FFG values are
    very high, they may be discounting the initial harder/impermeable
    nature before eventual infiltration occurs, and given the sheer
    rate, the initial runoff may be higher than expected, resulting in
    widely scattered flash flooding conditions, especially near
    low-water crossings that dot the area and therefore is considered
    possible over the next 3-4 hours.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5sLA42kk-nHBN0tFeRaAJbC4enJwgUEj0QCsqbVwwwsomzGDpA_wJQwe1ASN8uoMj4hn= BZpxv0YGVUH7RBYlY2rnthM$ for graphic product...

    ATTN...WFO...EAX...LSX...LZK...SGF...

    ATTN...RFC...KRF...MSR...ORN...NWC...

    LAT...LON 40379249 39809183 39149162 37979136 37299133=20
    36429134 36109214 36389272 36909316 38189353=20
    39829328 40369283=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 16 08:33:16 2025
    AWUS01 KWNH 160833
    FFGMPD
    VAZ000-NCZ000-161400-

    Mesoscale Precipitation Discussion 1090
    NWS Weather Prediction Center College Park MD
    432 AM EDT Tue Sep 16 2025

    Areas affected...coastal southeastern VA and northeastern NC

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

    Valid 160831Z - 161400Z

    Summary...At least a localized flash flood threat looks to be
    increasing across coastal sections of southeastern VA and
    northeastern NC this morning. Increasing rainfall rates with
    hourly totals potentially reaching 3 inches are expected to impact
    a few coastal locations through 14Z.

    Discussion...08Z surface observations and shortwave IR imagery
    from GOES East showed a surface low centered about 65 miles east
    of Cape Hatteras. Over the past 6 hours, the surface low has been
    gradually lifting north to northwest while occasional mesoscale
    lows have appeared in the broader low level cloud swirl in
    satellite imagery. It appears the main surface low has been
    associated with the most recent burst of convection to its
    northwest, with area radar imagery showing reflectivity echoes
    crossing over Hatteras Island. SPC mesoanalysis data from 08Z
    showed the convective burst along the western edge of a MLCAPE
    bubble offshore within 1000-2000 J/kg, just east of the northern
    Outer Banks. Meanwhile, moderate to occasionally heavy rain has
    been observed over VA, to the southwest of Norfolk, with 1-2
    inches reported since midnight. However, a lack of better
    instability has limited rainfall intensity for inland locations.

    Short term RAP guidance over the past 6-10 cycles has been in
    relatively good agreement with the current surface low position
    and supports the low tracking toward the northwest, closer to the
    Outer Banks, through 14Z. This movement makes sense given the
    low's placement relative to a closed mid-level low centered over
    the central NC/SC border. Even if the RAP is wrong, there is the
    potential for convectively induced mesovortices within convection
    that may reach the coast before dissipating. An expected
    northwestward movement of the surface low should support
    increasing MLCAPE from roughly Cape Hatteras to Virginia Beach
    with values of 500 J/kg to the north and up to ~1500 J/kg over
    Hatteras Island by 12-14Z. In addition, a primary axis of low
    level convergence to the northwest of the low center is expected
    to make it to the northeastern NC and southeastern VA coast with
    increasing rainfall intensities beneath favorably diffluent flow
    in the upper levels. Additional, weaker and more transient axes of
    low level convergence will be possible farther inland from the
    coast which could support increased rainfall intensities as
    instability increases later this morning.

    Earlier gauge observations had shown ~0.75 inches of rain in 15
    minutes which would support hourly rainfall up to 3 inches.
    Expected hourly rainfall of 1 to 3 inches will be possible from
    portions of northeastern NC into southeastern VA which may result
    in localized flash flooding, especially over any urban locations.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_qFJKYsDtL4cZcV9URN8n6DzfJPHVrjrdZ4SrWpKuYZJT3MpZOotEOBGA3Yh_Nh-nYXj= iy_iNscaFNoTEa2lzNuZGzE$ for graphic product...

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

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37197676 37137627 36787569 35957506 35177532=20
    35167600 35567677 36077735 36497755 37067729=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 16 14:01:49 2025
    AWUS01 KWNH 161401
    FFGMPD
    VAZ000-NCZ000-162000-

    Mesoscale Precipitation Discussion 1091
    NWS Weather Prediction Center College Park MD
    1001 AM EDT Tue Sep 16 2025

    Areas affected...Southeast VA and far Northeast NC Tidewater
    Region

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

    Valid 161400Z - 162000Z

    SUMMARY...Ongoing heavy rainfall across parts of southeast VA and
    far northeast NC associated with a potent nearby coastal low is
    expected to continue through at least this afternoon. Maximum
    rainfall rates are expected to remain in the 1-3"/hr range, with
    6-hr totals up to 4". This is anticipated to lead to scattered
    instances of flash flooding, which may be exacerbated due to
    coastal flooding impacts and urbanized ground conditions.

    DISCUSSION...Latest GOES-EAST visible satellite imagery highlights
    a compact surface low pressure system about 40 miles east of the
    NC Outer Banks, with regional radar imagery and surface
    observations depicting moderate to locally heavy rainfall across
    coastal sections of VA and far northeast NC. Rainfall amounts
    through 1330Z of 1.5-2.0" have been reported in the
    Norfolk/Virginia Beach region, mainly associated with a band of
    heavy rainfall that moved westward through the region this
    morning. The highest rainfall rates (up to 3"/hr per MRMS) are
    currently offshore and associated with the deepest convection
    (coldest cloud tops around -66C) near the low pressure center.
    However, an axis of low-level convergence extends to the northwest
    along the VA/NC coastline and enhanced by 30-40kt
    east-northeasterly 850mb winds and an associated warm front
    extending east-northeast from the low pressure system. This strong
    easterly flow, while enhancing convergence, is also maybe more
    importantly aiding to increase MUCAPE above 500 J/kg per the
    latest RAP into northeast NC. Elevated instability is expected to
    continue increasing gradually through this afternoon as the
    surface low slowly drifts north-northwestward, as well as PWs
    which should remain near or slightly below 2". This will help
    maintain rainfall rates in the 1-3"/hr range and eventually lead
    to greater coverage of these higher rates through around 20Z as
    additional rainbands move inland.

    Radar representations over the next 6-hrs will likely exhibit
    north-south bands of heavy rainfall moving inland along the coast
    where greatest convergence exists intersecting the coastline and
    influence from an associated warm front and easterly flow. These
    bands will likely weaken as they progress westward, before being
    replaced by new heavy rainfall bands oriented in a similar fashion
    as the coastal low drifts closer to southeast VA. Latest HRRR and
    experimental RRFS guidance depicts additional rainfall amounts up
    to 4" possible through 20Z and most likely along the immediate
    coast of southeast VA and the southern Delmarva Peninsula, but
    with even heavier amounts possible just after 20Z. These rainfall
    amounts when combined with coastal flooding and any urban
    influence (i.e. Norfolk/Virginia Beach) are likely to lead to
    scattered instances of flash flooding during this time period.
    Additional MPDs will likely be needed this evening as the event
    continues through tonight.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7gTRZCSpog-C5MyufQ3TDTH0pwcX6tkmHt6QpYZ-K42h1LT0wga_hPz_SMhsMBkuRAWo= YTDU5dTV9Z0iIvN7unyfh3M$ for graphic product...

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

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37727599 37647566 37447549 37257559 36887571=20
    36457573 36377601 36707647 37107668 37427662=20
    37647633=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 16 18:45:54 2025
    AWUS01 KWNH 161845
    FFGMPD
    TXZ000-NMZ000-AZZ000-170045-

    Mesoscale Precipitation Discussion 1092
    NWS Weather Prediction Center College Park MD
    245 PM EDT Tue Sep 16 2025

    Areas affected...Southeast Arizona into southwest/central New
    Mexico

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

    Valid 161845Z - 170045Z

    SUMMARY...Scattered slow moving convection initiating this
    afternoon will contain the potential for localized rainfall rates
    of 1.0-1.5"/hr between southeast Arizona and southwest/central New
    Mexico. This may lead to isolated flash flooding, especially near
    burn scars and dry washes.

    DISCUSSION...Satellite and regional radar imagery across
    east-central AZ into central NM highlight ongoing convection
    blossoming over the last hour within an unstable environment (RAP
    analysis of 1,000-1,500 J/kg SBCAPE). PWs are not anomalous and
    remain under 1" outside of southern AZ/NM. The greatest factor
    increasing the flash flood risk, when combined with the sufficient
    instability levels, are weak mean layer westerly winds around
    10-15kts. This may allow for convection tied to sensitive terrain
    to remain mostly stationary for enough time with rainfall rates up
    to 1.0-1.5" and lead to isolated flash flooding. Additionally,
    some west-east training of cells are possible across central NM
    through this evening should convection align in this orientation.

    This flash flood risk, while isolated, is greatest near recent
    burn scars and dry washes. Considerable flash flooding is possible
    should thunderstorms directly impact the most sensitive terrain in
    the region.

    Snell

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8PQg8iv6qvvbFsEnsBA24u0eBzMBhSYKFBVaX0HGZ2cmSNPz1PXQvzj9fT_shMhnhr2K= wMclO_hpKeRbLd_W0B3DkEk$ for graphic product...

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

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 35040588 34870514 34360493 33030512 32140560=20
    31790645 32140746 31960886 31271054 31271139=20
    31651184 32621074 33310997 34190975 34420855=20
    34860707=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 16 18:55:26 2025
    AWUS01 KWNH 161855
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-162253-

    Mesoscale Precipitation Discussion 1093
    NWS Weather Prediction Center College Park MD
    254 PM EDT Tue Sep 16 2025

    Areas affected...Iowa, northwestern Missouri, far northeastern
    Kansas

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

    Valid 161853Z - 162253Z

    Summary...Isolated to scattered thunderstorm activity was
    developing and moving slowly across the discussion area. Local
    rain rates reaching 2 inches/hr are possible in a few spots,
    potentially causing isolated flash flooding.

    Discussion...Radar/satellite imagery depicts developing
    thunderstorms across central Iowa generally along an axis from
    near Mason City south-southwestward to west of Des Moines. More
    isolated convective activity was attempting to deepen into far
    northeastern Kansas. Strong insolation/surface destabilization
    has enabled deeper convection to become sustained along a subtle
    surface confluence in that vicinity. Meanwhile, PW values
    exceeding 1.5 inch and minimal convective inhibition is
    contributing to efficient rainfall processes, with local 1-1.5
    inch/hr rain rates already noted west of Des Moines. Both forcing
    aloft and kinematics were weak, resulting in slow-moving activity
    that should persist for a few hours this afternoon.

    The longevity of ongoing activity (and extent of flash flood risk)
    should generally be tied to the persistence of subtle low-level
    confluence across the region today. Models suggest that storms
    should persist for at least another 3-5 hours or so. Ground
    conditions are a bit on the dry side (modest soil moistures per
    NASA SPoRT data) and relatively high FFG thresholds (around 2
    inches/hr). Each of these factors, plus questions about the
    spatial extent of convective coverage through 23Z/6p CDT) are all
    suggestive of an isolated flash flood threat at best.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6FCF-YyOcArnRO2MP5B6HBflcxen68JbVGfYG0zACTfGyMQyVm-vi6C6zxAMqS5Pvi1k= mKv5t1ZU4stxMH2UJcMCDpU$ for graphic product...

    ATTN...WFO...DMX...EAX...OAX...TOP...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43259428 43209326 41879333 40659384 39569404=20
    39419477 39829600 42129526=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 16 19:35:24 2025
    AWUS01 KWNH 161935
    FFGMPD
    DEZ000-MDZ000-VAZ000-170134-

    Mesoscale Precipitation Discussion 1094
    NWS Weather Prediction Center College Park MD
    334 PM EDT Tue Sep 16 2025

    Areas affected...southeastern Virginia, southeastern Maryland, far
    southern Delaware

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

    Valid 161934Z - 170134Z

    Summary...Flash flood potential continues across the discussion
    area. Heavy rainfall will continue around the center of a
    westward-moving low pressure area near the southeastern VA coast
    over the next 6 hours.

    Discussion...Flash flood potential continues across southeastern
    Virginia. Heavy rainfall continues near the center of a coastal
    low (centered just east of Virginia Beach). That low was moving
    slowly westward toward mainland Virginia while spreading areas of
    0.5-2 inch/hr rain rates into the discussion area. Some of these
    heavier rain rates will spread over areas that have already
    experienced 2-4 inch totals today. Flood/flash flood impacts have
    already been noted near Norfolk and Virginia Beach. Impending
    rainfall (perhaps reaching 2-3 inches in spots) should exacerbate
    any flooding conditions in the area and cause new instances of
    flash flooding through at least 23Z/7p EDT.

    An addition to the aforementioned scenario, a deep convective band
    has materialized over coastal waters southeast of
    Salisbury/Pocomoke City, MD on the northeastern periphery of the
    coastal low. The amount of lightning associated with this
    activity suggests that mesoanalyses may not be accurately
    depicting instability profiles in that region. Surface-based
    instability is expected to make it to shore and support
    persistence of this band across southeastern Maryland and adjacent
    parts of Virginia, with rain rates exceeding 1 inch/hr for a few
    hours. Excessive rainfall/flash flood potential will also
    accompany this activity through 02Z/10p EDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_3G9l2zeNRO6vY7onx6yFLgGMxhJrN7BmxQ61N_fOUf5-IqClfbv5nKCSANUXNygqHOn= 0VLHiSo1wZKqd3Hesg_XfZs$ for graphic product...

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

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 38597577 38527504 37657525 36597588 36727724=20
    37697698=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 16 21:18:54 2025
    AWUS01 KWNH 162118
    FFGMPD
    KSZ000-NEZ000-COZ000-170317-

    Mesoscale Precipitation Discussion 1095
    NWS Weather Prediction Center College Park MD
    518 PM EDT Tue Sep 16 2025

    Areas affected...southwestern Nebraska, northwestern Kansas

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

    Valid 162117Z - 170317Z

    Summary...Slow-moving convection continues to deepen across the
    discussion area, with areas of 1+ inch/hr rates noted beneath the
    strongest storms. Areas of flash flooding are possible through
    03Z/10p CDT.

    Discussion...Scattered thunderstorms were increasing in coverage
    across the discussion area over the past hour. The storms appear
    to be focused along low-level convergence near an apparent weak
    boundary (wind fields shifting from southerly to easterly along an
    axis from near Holyoke, CO to near Hebron, NE. Along this
    boundary, 1-1.2 inch PW values, 2000+ J/kg MLCAPE, and steep lapse
    rates aloft were allowing for intense updrafts and locally heavy
    rainfall. Most storms were drifting northward amid modest deep
    layer flow, although a cell near McCook, NE has anchored along
    this boundary and slowed substantially while exhibiting
    backbuilding character. Rain rates appear to be at a peak near
    this storm (exceeding 1.5 inch/hr), and it cannot be ruled out
    that other storms exhibit this same behavior in the short term.

    Storms appear to be aided by ascent aloft associated with a weak
    mid-levels shortwave trough evident in water vapor imagery over
    northeastern Colorado. This wave will take several hours to
    traverse the region, and ascent from this feature should continue
    interacting with the strong instability in place to keep fostering
    deep convective development. Southerly 850mb flow into the area
    should continue to maintain the pool of instability. Scattered,
    slow-moving storms are expected to continue through at least
    03Z/10p CDT this evening across the region. Local rain rates
    exceeding 1.5 inches/hr should readily exceed FFG thresholds.=20
    Flash flooding is probable on at least an isolated basis.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5FSQXGqhLMX1uVRBLlZ4oYfAXAnTmE3HW3X65HnkGI2ywM_kfZPqz0VBj79Hdk-0DDHd= HVOmXjRjrNaTme03JwTHu7I$ for graphic product...

    ATTN...WFO...BOU...DDC...GID...GLD...ICT...LBF...

    ATTN...RFC...KRF...NWC...

    LAT...LON 41370236 40999943 39999801 38879816 39580196=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 16 21:21:56 2025
    AWUS01 KWNH 162121
    FFGMPD
    KSZ000-NEZ000-COZ000-170317-

    Mesoscale Precipitation Discussion 1095
    NWS Weather Prediction Center College Park MD
    521 PM EDT Tue Sep 16 2025

    Areas affected...southwestern Nebraska, northwestern Kansas

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

    Valid 162117Z - 170317Z

    Summary...Slow-moving convection continues to deepen across the
    discussion area, with areas of 1+ inch/hr rates noted beneath the
    strongest storms. Areas of flash flooding are possible through
    03Z/10p CDT.

    Discussion...Scattered thunderstorms were increasing in coverage
    across the discussion area over the past hour. The storms appear
    to be focused along low-level convergence near an apparent weak
    boundary (wind fields shifting from southerly to easterly along an
    axis from near Holyoke, CO to near Hebron, NE. Along this
    boundary, 1-1.2 inch PW values, 2000+ J/kg MLCAPE, and steep lapse
    rates aloft were allowing for intense updrafts and locally heavy
    rainfall. Most storms were drifting northward amid modest deep
    layer flow, although a cell near McCook, NE has anchored along
    this boundary and slowed substantially. Rain rates appear to be
    at a peak near this storm (exceeding 1.5 inch/hr), and it cannot
    be ruled out that other storms exhibit this same behavior in the
    short term.

    Storms appear to be aided by ascent aloft associated with a weak
    mid-levels shortwave trough evident in water vapor imagery over
    northeastern Colorado. This wave will take several hours to
    traverse the region, and ascent from this feature should continue
    interacting with the strong instability in place to keep fostering
    deep convective development. Southerly 850mb flow into the area
    should continue to maintain the pool of instability. Scattered,
    slow-moving storms are expected to continue through at least
    03Z/10p CDT this evening across the region. Local rain rates
    exceeding 1.5 inches/hr should readily exceed FFG thresholds.=20
    Flash flooding is probable on at least an isolated basis.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4jmi6-Km_tH2OSDdTYFMa-kPDpy9lp1iuYSZIfeFlCsbinrPGu9HfxOBM43lS8NPCTsn= ZCIu9LpzWoZSH2_y_KkSZM0$ for graphic product...

    ATTN...WFO...BOU...DDC...GID...GLD...ICT...LBF...

    ATTN...RFC...KRF...NWC...

    LAT...LON 41370236 40999943 39999801 38879816 39580196=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 17 01:11:58 2025
    AWUS01 KWNH 170111
    FFGMPD
    NMZ000-AZZ000-170510-

    Mesoscale Precipitation Discussion 1096
    NWS Weather Prediction Center College Park MD
    911 PM EDT Tue Sep 16 2025

    Areas affected...southern New Mexico, southeastern Arizona

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

    Valid 170110Z - 170510Z

    Summary...Flash flood potential will exist on an isolated basis
    for a few more hours - perhaps through 05Z/11p MDT.

    Discussion...Scattered storms have developed in earnest and moved
    slowly across the discussion area this afternoon. As of 01Z,
    radar mosaic imagery indicates the heaviest thunderstorm activity
    located across southern New Mexico from near Silver City to near
    Alamogordo, with more isolated activity noted near Tuscon.=20
    Surface-based CAPE remains in place in the pre-convective
    environment (ranging from 500-1000 J/kg) and PW values remain
    around 1-1.2 inch. Additionally, steering flow/kinematics
    continue to favor slow- and erratically moving storms, with
    perhaps a very slow southward component of propagation noted
    across south-central New Mexico. Spots of 1 inch/hr rain rates
    will continue to threaten local FFG and pose a risk of flash
    flooding in localized areas.

    The extent of the flash flood threat should continue for another
    2-3 hours or so. The loss of daytime heating and continued
    overturning should allow for a lessening of both convective
    intensity and coverage through the early overnight hours.=20
    Isolated flash flooding remains possible through 05Z/11p MDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9VnATxD6wneBFkKlJbs0pC2m79OBrH2VN4o4ue6HJV89321kNuz5Z_yIV4Yo2s3FG98O= oTE0w2TVW52covsJO7I7Lsg$ for graphic product...

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

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 33950560 32630478 31970675 31360842 31651198=20
    32151226 33651008=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 17 03:26:01 2025
    AWUS01 KWNH 170325
    FFGMPD
    IAZ000-KSZ000-NEZ000-170810-

    Mesoscale Precipitation Discussion 1097
    NWS Weather Prediction Center College Park MD
    1125 PM EDT Tue Sep 16 2025

    Areas affected...northern KS into central/eastern NE

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

    Valid 170324Z - 170810Z

    Summary...A few areas of flash flooding will continue to be
    possible from northern KS into central/eastern NE through 08Z. 1-2
    in/hr rates within training are expected.

    Discussion...03Z radar imagery showed ongoing thunderstorms along
    the western KS/NE border into east-central NE, located southeast
    of a stationary front that extended NE to SW through central NE.
    An outflow boundary was analyzed ahead of the thunderstorms with
    overrunning of an estimated 30-40 kt 850 mb low level jet in
    west-central KS beneath a diffluent flow pattern aloft. The bigger
    picture showed a closed mid to upper level low over WY with a
    southward extending trough axis into western CO. This trough axis
    is expected to advance eastward over the next 6 hours with
    diffluent flow maintaining over much of NE into northern KS.

    Areas of strong ascent will continue over the next several hours
    across the central Plains with lingering instability of 1000-2000
    J/kg MLCAPE aiding in the maintenance of thunderstorms with high
    rainfall rates. As the outflow boundary continues to advance
    downstream toward the south and east, overrunning of the low level
    jet atop the boundary with deeper layer mean steering flow
    aligning with the boundary orientation will support areas of
    training at times from SW to NE. Rainfall rates of 1-2 in/hr are
    expected with additional storm totals of 2-4 inches through 08Z
    which may allow for a few areas of flash flooding from northern KS
    into central and eastern NE.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4vEcU5WwLldfJTdEHUbPwTFoIITQFfuXx8YiqwQ30tDiN3tcMrsg3xf-OOX5VuQ0VZio= -JA9pwNJq-LVVTtTh6ntgoo$ for graphic product...

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

    ATTN...RFC...KRF...NWC...

    LAT...LON 42569757 42419687 42159630 41819610 41499628=20
    40939691 40089751 39199818 39270019 39600094=20
    39890116 40890035 41489958 42089867=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 17 03:51:40 2025
    AWUS01 KWNH 170351
    FFGMPD
    IAZ000-NEZ000-170700-

    Mesoscale Precipitation Discussion 1098
    NWS Weather Prediction Center College Park MD
    1150 PM EDT Tue Sep 16 2025

    Areas affected...western/central IA

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

    Valid 170349Z - 170700Z

    SUMMARY...A few slow moving thunderstorms will continue at least a
    localized flash flood threat over western IA over the next few
    hours with hourly rainfall of 1 to 2+ inches.

    DISCUSSION...GOES East infrared imagery was continuing to show
    cooling cloud tops over the past 30-45 minutes over western IA
    where an outflow boundary was being overrun by a 10-20 kt low
    level jet. Aloft, deeper layer mean wind speeds were weak,
    supporting slow cell motions over IA with MRMS derived rainfall
    rates of 1 to 2+ inches in an hour since 00Z. While the stronger
    upper level forcing and low level jet magnitude were located to
    the west across NE, a weaker branch of the low level jet extended
    over eastern NE into western/central IA into the upper MS Valley,
    proving sufficient for overrunning and scattered low moving storms
    where MLCAPE ranged from 500-1500 J/kg via 03Z SPC mesoanalysis
    data. Continued areas of slow moving thunderstorms will continue
    at least a localized threat of flash flooding over the next 2-4
    hours with increasing convective inhibition possibly lowering the
    threat after 07Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_qaWfoF4k1_2qc5TOW7O4StwE49Ae9_97v_RYBCjEx16i3qswK5RMSCf9UWDli2oBd-n= 3HzGmDGx1rCE58mwutbqofc$ for graphic product...

    ATTN...WFO...DMX...FSD...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43439448 43189370 42369300 41269400 40999576=20
    41349626 42109652 42559627 43019587 43379520=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 18 00:26:15 2025
    AWUS01 KWNH 180026
    FFGMPD
    MNZ000-SDZ000-180524-

    Mesoscale Precipitation Discussion 1099
    NWS Weather Prediction Center College Park MD
    825 PM EDT Wed Sep 17 2025

    Areas affected...eastern South Dakota, far western Minnesota

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

    Valid 180024Z - 180524Z

    Summary...A fairly focused band of slow-moving convection is
    producing rain rates exceeding 1.5 inches/hr. Areas of excessive
    runoff and flash flooding are expected. This risk should persist
    through around 05Z/midnight CDT.

    Discussion...A fairly focused band of convection was pivoting
    slowly westward on the eastern periphery of a surface low center
    south of Pierre, SD. This band extended from just north of Huron,
    SD eastward to just west of Marshall, MN. This band was also
    collocated with focused low-level convergence and a stationary
    front in the area. South of the front, areas of 500-1000 J/kg
    SBCAPE and 1.5 inch PW values were promoting updrafts with
    efficient rainfall processes. With convection slowly moving and
    focused along the nearly stationary front, spots of 2 inch/hr rain
    rates were being estimated per MRMS. These rain rates were
    persisting in local areas for some time, likely causing at least
    isolated runoff concerns.

    Models generally depict that this scenario will not change much
    over the next 3-5 hours. Instability south of the boundary will
    only be slowly exhausted with boundary layer cooling. Spots of
    1-2 inch/hr rain rates are likely to continue, and isolated areas
    could experience total amounts of 3-5 inches over the next few
    hours. Convection should only gradually weaken after 05Z or so.=20
    Flash flooding is possible in a localized basis in this scenario.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_AlqbLxOJ3EYu3kmeAcfrfTm2Nb6SDNqDlb-bOUepbeMHIzPk6C-Xu_djkN0NFkB5aBL= PYfckMWEw00GGln7F4EhZUo$ for graphic product...

    ATTN...WFO...ABR...FSD...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45229781 45229552 44589504 44109618 43799983=20
    44939977=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 18 01:57:16 2025
    AWUS01 KWNH 180157
    FFGMPD
    TXZ000-OKZ000-KSZ000-COZ000-NMZ000-180745-

    Mesoscale Precipitation Discussion 1100
    NWS Weather Prediction Center College Park MD
    956 PM EDT Wed Sep 17 2025

    Areas affected...Southeast CO...Far Northeast NM...Southwest
    KS...OK Panhandle...Northern TX Panhandle...

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

    Valid 180155Z - 180745Z

    SUMMARY...WAA band with some short-term training across TX
    Panhandle to given way to upscale convective clusters out of SE
    CO/NE NM. Scattered repeating through the overnight period may
    present hourly rates/totals to 1.5" and localized 2-3 3-6 hour
    totals downstream. Isolated incident or two of flash flooding is
    considered possible.

    DISCUSSION...GEOS-E WV suite shows a broad closed low over the
    central High Plains though the inner core short wave/vorticity
    features are fairly consolidated but showing a generally flat
    elongated orientation across central CO toward the Sand Hills of
    Nebraska. The upstream shortwave is sliding eastward with an
    associated upper level speed max into a weakly diffluent region
    across SW KS attm. As speed max rounds the base, this will expand
    and overall divergence aloft will be favorable for upscale
    convective growth toward the later portion of the period.=20

    However, in the short-term term, scattered more severe-type
    convection with solid hail generation exists across much of SE CO,
    though organization suggests some random collision/mergers are
    possible over the next few hours. More concerning is VWP and RAP
    analysis suggests strengthening southerly to south-southwesterly
    low level jet across the Texas Panhandle is responding to the
    overall height-falls/ejection of the wave. A weak thermal
    boundary from NNW to SSE is acting as the isentropic ascent fact
    across far NE NM into the northern TX Panhandle. Here, WAA is
    solid and MUCAPEs are near 2000 J/kg to support the elevated
    convection. CIRA LPW also notes backed up moisture gradient from
    afternoon upslope, combined with an axis of enhanced 850-700 to
    .5" near this ascent plane, allowing for increasing moisture flux
    into the currently severe/hail producing cells. Given total
    moisture to 1.25" and increasing speed to 35kts, convergence
    should support 1.5"+/hr rates.=20=20

    Deep layer flow at the southern edge of the jet is support some
    weak south-easterly motions for some scattered potential for
    training/repeating elements. This may result in localized 2-3"
    totals and possible flash flooding conditions over the next few
    hours. With time, the strength and veering of the LLJ will
    expand ascent across SE CO into SW KS into the aforementioned
    expanding divergence field toward 06-07z. Forward propagation is
    likely to limit overall coverage, but repeat tracks and expanding
    clusters may also support localized 2-3" totals and isolated flash
    flooding conditions through middle of overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9MXfjDXLe0g4EuNA_kspVcIBGmDFRnIA_hjcQzRmgqAhNjIiRQD-utosqBglXLfDCAsS= a9FJQ3jEiP6VKvF01Emqufk$ for graphic product...

    ATTN...WFO...ABQ...AMA...DDC...GLD...OUN...PUB...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 38580228 38510076 38069976 36809946 35410016=20
    35220225 35830347 37200421 38270358=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 18 16:32:26 2025
    AWUS01 KWNH 181632
    FFGMPD
    AZZ000-NVZ000-CAZ000-182230-

    Mesoscale Precipitation Discussion 1101
    NWS Weather Prediction Center College Park MD
    1231 PM EDT Thu Sep 18 2025

    Areas affected...Southern and Eastern CA...West-Central to
    Southwest AZ...Far Southern NV

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

    Valid 181630Z - 182230Z

    SUMMARY...A gradual increase in the coverage and concentration of
    showers and thunderstorms will be expected over the next several
    hours. Increasingly heavy rainfall rates will pose a growing
    threat for isolated to scattered areas of flash flooding by
    mid-afternoon.

    DISCUSSION...The early-day GOES-W visible satellite imagery along
    with radar shows a broken axis of locally heavy showers and
    thunderstorms impacting portions of eastern CA as a deep layer
    fetch of tropical moisture/warm air advection and mid-level
    shortwave energy related to former Tropical Storm Mario advances
    up into the Southwest U.S.

    Despite the current regional coverage of cloud cover, there will
    be a gradual uptick in solar insolation across southeast CA and
    into southwest AZ over the next several hours which is where
    visible satellite imagery does show some thinning/clearing of the
    cloud deck. This will drive an uptick in surface-based instability
    over time, and with a well-defined instability gradient already in
    place (SBCAPE values of 1000 to 2000+ J/kg) from the Gulf of CA
    northward into the Lower CO River Valley, an increase in the
    coverage of heavy shower and thunderstorm activity will be
    expected.

    Differential heating boundaries near areas of higher terrain and
    also near the edge of the deeper layer cloud decks will be
    facilitators of additional convective initiation. Additionally,
    the flow aloft is rather divergent around the northeast flank of
    the mid-level shortwave energy offshore of southern CA, and this
    forcing interacting with the deeper layer southerly moisture/warm
    air advection regime will also promote an increase in convective
    coverage.

    PWs are well into the 95th+ percentile of climatology across
    southern and eastern CA in particular, with CIRA-ALPW showing substantial/highly anomalous concentrations of moisture in the
    700/300 mb layer. This moisture coupled with the uptick in
    surface-based instability should easily support convective cells
    capable of producing 1 to 2 inch/hour rainfall rates by early to
    mid-afternoon.

    The latest 12Z HREF guidance suggests some localized backbuilding
    and cell-training concerns, and the concentration of convection
    will support rainfall totals by mid-afternoon of as much as 2 to 4
    inches.

    Isolated to scattered areas of flash flooding will become
    increasingly likely with time given the high rainfall rates and
    storm totals over the next several hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-dfCmWJ6CY2uuqTzuU-eee670QKSLFTWh2ApJ8Q9ixofl5V4_XFU_aHWvTI_InYcdTXh= XIBqvSTzKN_xCpJPU805pRE$ for graphic product...

    ATTN...WFO...FGZ...HNX...LOX...PSR...SGX...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 36091632 36071540 35891429 35361298 34351203=20
    33571209 33171309 32741382 32331443 32241510=20
    32281583 32541653 33261700 34081727 35001829=20
    35781806 36041724=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 18 19:41:00 2025
    AWUS01 KWNH 181940
    FFGMPD
    TXZ000-NMZ000-AZZ000-190139-

    Mesoscale Precipitation Discussion 1102
    NWS Weather Prediction Center College Park MD
    340 PM EDT Thu Sep 18 2025

    Areas affected...southern New Mexico, southern/central Arizona,
    far west Texas

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

    Valid 181939Z - 190139Z

    Summary...Isolated thunderstorms are developing and moving
    slowly/erratically across the discussion area. Peak rain rates of
    around 1 inch/hr are likely with the most dominant storms.=20
    Isolated instances of flash flooding are expected through 02Z/8p
    MDT.

    Discussion...Abundant insolation across the discussion area has
    contributed to sufficient instability for convective development
    this afternoon. Currently, thunderstorm initiation has occurred
    mainly along terrain-favored ridgelines. Moisture profiles are
    marginally supportive of heavy rainfall (around 0.9-1.1 inch -
    highest in south-central Arizona), although recent radar
    mosaic/MRMS depicts several spots of 1 inch/hr rain rates across
    the discussion area. Kinematic profiles (containing weak steering
    flow aloft) was allowing for cells to move slowly and even
    erratically across the discussion area, further supporting very
    localized areas of heavy rainfall. Some of these areas of heavier
    rain were occurring over/near burn scars across southern New
    Mexico, which could prompt a relatively fast increase of local
    runoff in nearby flood-prone areas.

    The ongoing scenario supporting flash flood potential should
    continue for a few hours this afternoon as we're still early in
    the diurnal heating cycle. Models depict scattered, slow-moving
    convective activity to continue across the discussion area through
    at least 02Z/8p MDT - perhaps lingering a bit longer across far
    southern New Mexico and vicinity. Isolated instances of flash
    flooding are expected during that timeframe.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_1tSnOKkfIHjlCIhn9STXdSvsc9DB7gSDvh4AGoDvHeQmoVG0MUalkGozrGi4L3jXukb= Y8xg43Fo1VJg7gB9rVaPNK0$ for graphic product...

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

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 35311239 35171158 34540949 34400828 34460678=20
    33820522 31750449 30920424 30470440 30880520=20
    31920667 31730823 31340824 31520986 31881128=20
    33351258 34541279=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 18 22:38:00 2025
    AWUS01 KWNH 182237
    FFGMPD
    AZZ000-NVZ000-CAZ000-190436-

    Mesoscale Precipitation Discussion 1103
    NWS Weather Prediction Center College Park MD
    637 PM EDT Thu Sep 18 2025

    Areas affected...southeastern California, southern Nevada, western
    Arizona

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

    Valid 182236Z - 190436Z

    Summary...Scattered instances of flash flooding are ongoing.=20
    Locally significant impacts are possible. The ongoing threat
    should continue through at least 05Z/10p PDT.

    Discussion...Scattered to numerous thunderstorm activity continues
    to drift generally northward across the discussion area. A
    relatively focused cluster of storms has exhibited backbuilding
    tendencies across southwestern Arizona, where a mature cold pool
    has been established. The region remains under the influence of
    deep southerly flow on the eastern edge of a disturbance centered
    near the California coastline south of San Luis Obispo. The
    southerly flow is maintaining a fetch of extremely moist and
    unstable air from the Gulf of California, with pre-convective air (characterized by 1000-2000 J/kg MLCAPE and 1.5-2 inch PW)
    continuing to support deep moist convection. Furthermore,
    kinematics are modest enough to support slow storm motions and
    continued backbuilding - especially near mature cold pool(s) and
    near terrain-favored areas.

    The ongoing scenario should continue to support locally heavy
    rainfall in several areas. Local rain rates reaching 2 inches/hr
    should continue. These rates should readily exceed FFG thresholds
    across the region. Locally significant flash flood impacts remain
    possible. Over time, widespread overturning and boundary layer
    cooling should result in a lessening of convective coverage, but
    this process should take several hours to play out. Deep
    convection is likely to be ongoing through 05Z/10p PDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9LEkFD13iGcI__47ManaCAbp6z3eXQYxs2e_668ORkWFNJ49AOANlUT_TUNIppOw6S_W= Ny7YlvCbE6vWlrtXHe0L6rc$ for graphic product...

    ATTN...WFO...FGZ...HNX...LOX...MTR...PSR...SGX...TWC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 37331872 36591507 35901209 33411127 31371148=20
    32481495 32501662 33571704 34401845 34921967=20
    36382068 37292044=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 19 03:44:33 2025
    AWUS01 KWNH 190343
    FFGMPD
    NVZ000-CAZ000-190930-

    Mesoscale Precipitation Discussion 1104
    NWS Weather Prediction Center College Park MD
    1142 PM EDT Thu Sep 18 2025

    Areas affected...Southeastern California...Far Southwest Nevada...

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

    Valid 190345Z - 190930Z

    SUMMARY...A few more hours of slow moving, efficient heavy
    rainfall, rates of 1"+/hr and spots of additional 2-3" possible.
    Flash flooding remains likely. A few incidents of mud/rock slides
    and considerable flooding remain possible.=20

    DISCUSSION...GOES-W WV suite shows impressive deep layer cyclone
    continuing to advance through California into the Great Basin with
    broad area of anticyclonically curved outflow across the northern
    half of the overall, indicative of the favorable outflow
    environment. The core of the upper-low remains just southeast of
    Monterrey Bay with stronger southwest and west-southwesterly flow
    starting to sharpen the negative tilt trof through the lower San
    Joaquin Valley toward the Inland Empire. This 250mb jet is
    strengthening to 70-80kts, though eastern side jet streak with
    favorable right entrance ascent pattern is sliding away and
    divergence is reducing with time.=20

    A strong shortwave/MCV had developed in the negative tilt/high
    divergence region through the Antelope Valley and along the
    Tehachapi Range and this continues to provide solid DPVA and
    ascent while keeping easterly and southerly flow from 850 to 700mb
    directed through the northern Antelope Valley toward the Indian
    Wells, Rose Valley and perhaps into the Panamint Valley and
    through Death Valley later into the overnight period. The
    remaining unstable and increased moisture flux still is leaking
    through the Imperial Valley into Barstow and through the Antelope
    Valley...with some 500-1000+ J/kg of MLCAPE and Total PWats of
    1.5" available for the MCV to maintain solid convection near the
    MCV until crossing the higher terrain into Inyo county and toward
    SW Nevada. Confluence along the southeastern edge directly under
    the larger scale negative tilt trough will allow for more
    scattered cells along effective flanking lines that still could
    repeat but with slowly diminishing effectiveness toward 09z when
    instability should be exhausted and core of upper-level trof has
    swung northward. Still cells, particularly near the MCV will
    have capability of 1"+/hr, which will likely continue ongoing
    flash flooding conditions, but will slowly reduce in
    coverage/magnitude through Death Valley into SW Nevada by 09z.=20
    Additional 2-3" totals through the northern Antelope Valley toward
    China Lake remain possible; incidents of mud/rock slides are still
    possible in/near the stronger cores for a few more hours as well.

    Further southeast toward the Colorado River Valley. A cluster of
    thunderstorms has been gusting out being along just southeast of
    the base of negative tilt trof. Better access to deeper moisture
    and slightly enhanced instability may allow for a few of these
    cells to propagate along the developed outflow/cold pool lifting
    northward. Some weak divergence may support some scattered totals
    to 1" but more likely, forcing will continue to reduce and overall
    coverage is likely to become more widely scattered to isolated
    with time as well. Still, desert/hard ground conditions may still
    allow for an isolated incident of possible flash flooding.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-iDHdhX873ffv6ZOgtxsyJBKgHzq0gySuLRk_5vdJwnAuA5n2tHLHpZCAo6cQ-N0eIE7= wqvtEuumfkY2EwSYHW1eLhY$ for graphic product...

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

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 37841691 37621630 36861580 36111558 35391525=20
    34541505 33631499 33271545 33631631 34451700=20
    34941754 35431818 36101868 36791864 37521772=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 19 07:24:09 2025
    AWUS01 KWNH 190724
    FFGMPD
    AZZ000-191200-

    Mesoscale Precipitation Discussion 1105
    NWS Weather Prediction Center College Park MD
    323 AM EDT Fri Sep 19 2025

    Areas affected...Central Arizona...

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

    Valid 190720Z - 191200Z

    SUMMARY...Increasing convective development within some
    WAA/upslope out of weakly capped conditionally unstable airmass in
    the Sun Valley.

    DISCUSSION...GOES-E WV suite depicts a convectively enhanced
    shortwave feature along the SE Mohave/W Yavapai county line still
    with fairly symmetric outflow and shortwave trough extending
    southeastward within the left exit of the strengthening WSW
    upper-level jet that is cutting across the Lower Colorado River
    Valley and southern Arizona into SW NM. Lingering surface heating
    in proximity to the Phoenix Metro heat island and still enhanced
    deeper layer moisture through the valley with some steepening
    lapse rates aloft, has maintained a small pocket of 1500-2000 J/kg
    of MUCAPE. The combination of the left exit ascent and DPVA from
    the NNE advancing shortwave and trough axis has allowed for veered
    700mb flow to ascend isentropically to destabilize into steepening
    terrain.

    The 925-850mb 15-20kt of ESE to SE flow has maintained the ample
    moisture in the lower levels and contributed to the deeper layer
    moisture flux convergence to help support the expanding convective
    development noted with a few rapidly cooling CBs on 10.3um EIR and
    scattered updrafts in the KIWA RADAR domain. Nose of the deeper
    layer moisture in the sfc to 700mb layers on CIRA combined with
    the 20-30kts of flow support flux for moisture loading through the thunderstorms with limited sub-cloud evaporation expected.

    As such, localized rates of 1.25-1.5"/hr are possible, though
    steering flow is fairly strong even in the diffluent left exit of
    the jet, limiting individual cell's residency. Yet, the upstream
    environment and general upslope flow for the passing wave/upper
    level divergence should maintain a modest probability for upstream
    regeneration to allow for some localized repeating over the next
    few hours. As such spots of 1-2" totals may induce localized
    flash flooding concerns particularly near steeper terrain in the
    lower slopes of the Mogollon Rim or near any burn scars that dot
    the area of concern.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!--W3iV5M4FZouwYySjHKU6ZDNK82yAOMwPoClkgJR6gZafLjH21XCVYhU8ZuEVMGCbl2= jBmEhjNWUdH4hMTPGHWMXr8$ for graphic product...

    ATTN...WFO...FGZ...PSR...TWC...

    ATTN...RFC...STR...NWC...

    LAT...LON 35001160 34981079 34421008 33530971 32880979=20
    32641024 32631110 33001168 33591217 34371218=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 19 13:25:16 2025
    AWUS01 KWNH 191325
    FFGMPD
    AZZ000-191800-

    Mesoscale Precipitation Discussion 1106
    NWS Weather Prediction Center College Park MD
    923 AM EDT Fri Sep 19 2025

    Areas affected...Central AZ

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

    Valid 191323Z - 191800Z

    SUMMARY...Small bands of locally training showers and
    thunderstorms may continue for at least a few more hours.
    Additional concerns for some flash flooding will exist this
    morning.

    DISCUSSION...GOES-W IR satellite imagery is showing a couple of
    small southwest to northeast oriented bands of heavy showers and
    thunderstorms impacting portions of central AZ. The activity is
    mainly focused in between Phoenix and Winslow, with some impacts
    noted into the southwest-facing flank of the Mogollon Rim.

    The convection is embedded within a modestly unstable airmass with
    MUCAPE values generally around 500 J/kg, and is aligned with a
    corridor of somewhat focused moisture convergence associated with
    the low to mid-level southwest flow regime that remains in place.
    There is also proximity of left-exit region upper-jet dynamics
    associated with the subtropical jet crossing far southern CA and
    southern AZ which is generating at least some deeper layer ascent
    over the region.

    The ongoing convection may tend to linger this morning for at
    least a few more hours given the upper-jet support, and there will
    be continuing concerns for some smaller scale backbuilding and
    training of convective cells. Anomalous moisture remains in place
    early this morning, with PWs running near 2 standard deviations
    above normal, and this will still help support heavy rainfall
    rates that may reach 1 inch/hour with the stronger storms.

    Given the cell-training concerns, some additional short-term
    amounts of up to 2 inches cannot be ruled out for this morning.
    This may result in some additional localized concerns for flash
    flooding with impacts primarily to the normally dry washes and
    burn scar locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4Zfl9qYtjFV0qRQi9IKv8_XLv_Xkat1Con5l6j1oQ53KFSJ-eDn-KreeNEw-MzJdND1j= gdhXUgTuK_BlkTfe_AKIKqE$ for graphic product...

    ATTN...WFO...FGZ...PSR...

    ATTN...RFC...STR...NWC...

    LAT...LON 35551100 35191020 34431013 33911083 33571236=20
    34031303 34721302 35271219=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 19 16:46:47 2025
    AWUS01 KWNH 191646
    FFGMPD
    TNZ000-MSZ000-ARZ000-TXZ000-192245-

    Mesoscale Precipitation Discussion 1107
    NWS Weather Prediction Center College Park MD
    1245 PM EDT Fri Sep 19 2025

    Areas affected...Southern AR...Northern MS

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

    Valid 191645Z - 192245Z

    SUMMARY...A localized and mainly urban concern for flash flooding
    will exist through this afternoon from pockets of slow-moving
    thunderstorms.

    DISCUSSION...The latest satellite and radar imagery shows a couple
    of different broken areas of slow-moving thunderstorm activity
    that may tend to grow a bit upscale going through the late
    afternoon hours. One cluster is near the Arklatex region with
    convection becoming a bit better focused across southwest AR, and
    there is a second area over parts of far eastern AR and into
    northwest MS. All of this activity is generally focusing along
    outflow boundary activity that was generated from earlier
    convection this morning, but also with the aid of improving
    boundary layer instability.

    MLCAPE values along the wavy outflow boundary orientation across
    the region have risen to as much as 1000 to 1500 J/kg, with some
    of the better instability focused closer to the Arklatex in closer
    proximity to a wave of low pressure that is seen in surface
    observations.

    While the low-level flow is quite weak, there is some modest MCV
    energy ejecting east into southwest AR which coupled with the
    low-level boundary and improving thermodynamic environment via
    solar insolation may help allow for convection to expand in
    coverage off to the east across southern AR with eventually some
    connection potentially to the ongoing activity downstream over
    northwest MS.

    The latest hires model guidance has a very poor handle of the
    current activity, but the cell-motions are rather slow with some
    hints at some localized backbuilding cell character. Given the
    moist and unstable environment, some rainfall rates will be
    capable of reaching 2 inches/hour, and some localized storm totals
    by later this afternoon may be capable of reaching 3 to 4 inches.

    Generally, any flash flooding threat with these thunderstorms this
    afternoon is expected to be localized and primarily an urban
    concern.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6icwqmFIm70mG9zJH3xXG-KXhQWsnjF4AmrskKhcdfR4kOguDjh1Z6Bqd92Eb5Z_a-jm= Q3Y7oUwsUyQ7HMhk7taMsIw$ for graphic product...

    ATTN...WFO...JAN...LZK...MEG...SHV...

    ATTN...RFC...ALR...ORN...TUA...NWC...

    LAT...LON 35008867 34818821 34218826 33788896 33498986=20
    33299109 33219231 33309378 33619447 34079432=20
    34429386 34659272 34749169 34779084 34888978=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 19 18:02:46 2025
    AWUS01 KWNH 191802
    FFGMPD
    TXZ000-NMZ000-AZZ000-UTZ000-NVZ000-CAZ000-200000-

    Mesoscale Precipitation Discussion 1108
    NWS Weather Prediction Center College Park MD
    200 PM EDT Fri Sep 19 2025

    Areas affected...Far Eastern CA...Far Southeast NV...Northern and
    Eastern AZ...Western and Central NM

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

    Valid 191800Z - 200000Z

    SUMMARY...A gradual increase in heavy shower and thunderstorm
    activity is expected going through the afternoon hours which will
    bring a concern for mainly isolated areas of flash flooding. This
    will include potential impacts to dry washes and burn scar
    locations.

    DISCUSSION...The GOES-E WV suite shows mid-level shortwave energy
    gradually ejecting off to the east across northern and eastern AZ
    and into western NM which should interact with the diurnal heating
    cycle today to yield scattered areas of heavy showers and
    thunderstorms.

    SBCAPE values are locally already upwards of 1000 to 2000 J/kg
    across southeast AZ, with adjacent areas of western NM also
    destabilizing rather rapidly due to strong diurnal heating. In
    fact, the latest visible satellite images are showing an
    increasingly agitated CU field beginning to take shape across
    these areas, and convective initiation will likely be taking place
    within the next hour or two near areas of higher terrain which is
    also suggested by the latest AI-based LightningCast output.

    PWs across the region remain anomalously high with values 1.5 to
    2.5 standard deviations above normal across southern AZ into
    western NM, and this coupled with the increasing boundary layer
    instability will favor heavy showers and thunderstorms with rates
    as high as 1 to 2 inches/hour.

    The 12Z hires CAM consensus indicates that convection will
    initially be more terrain-focused, but will also be advancing off
    the terrain into the open desert locations where forward
    propagation off to the east and southeast will be expected. Some
    modest effective shear will be in place, and some loosely
    organized multicell convection is expected given the
    instability/shear environment.

    Some localized storm total rainfall amounts where convective cells
    become anchored near the terrain may reach as high as 2 to 3
    inches, otherwise some spotty 1 to 2 inch amounts will be
    expected. Isolated areas of flash flooding will be possible going
    through this afternoon, and this may include impacts to dry washes
    and burn scar locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5x7e-3EkWsj3wL4sfi9ksFTypKgHpL4DHNXOKUHR65PSmQzc_k40We2WIVEskwTFZqmX= cB6dBYWnE9Tp2F-qgJKFT-s$ for graphic product...

    ATTN...WFO...ABQ...EPZ...FGZ...MAF...PSR...SLC...TWC...VEF...

    ATTN...RFC...FWR...RSA...STR...NWC...

    LAT...LON 37071337 36871226 35851080 35610934 35620716=20
    35080572 34310476 33470443 32610444 31980492=20
    31750662 31440763 31060900 31171080 31871192=20
    32721243 33511316 34151458 35261542 36221527=20
    36981437=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 20 00:27:25 2025
    AWUS01 KWNH 200027
    FFGMPD
    TXZ000-NMZ000-AZZ000-UTZ000-NVZ000-CAZ000-200426-

    Mesoscale Precipitation Discussion 1109
    NWS Weather Prediction Center College Park MD
    826 PM EDT Fri Sep 19 2025

    Areas affected...central/southern New Mexico, southern through
    northwestern Arizona, far southern Nevada

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

    Valid 200026Z - 200426Z

    Summary...Isolated flash flood potential should continue for a few
    more hours (through 04Z/10p MDT).

    Discussion...Isolated, deep moist convection continues to drift
    slowly eastward across the discussion area. Spots of 1 inch/hr
    rain rates are noted with the most dominant and slowest-moving
    activity (as estimated per MRMS). These rain rates have
    occasionally fallen on locally sensitive areas (i.e., burn scars,
    low-lying areas), posing a risk of excessive runoff and flash
    flooding. Isolated flash flood potential continues in the near
    term.

    Models/observations suggest that most of the ongoing activity
    should be diurnally driven, with a downward trend in both
    intensity and coverage expected through the early overnight hours.
    Most of the convective threat should diminish through 04Z. Flash
    flood potential should also persist through that timeframe, while
    becoming even more isolated thereafter.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_KOjLdmu83W7PgRi4gei56feCI1UhDrD3AiVbUx3ZrDlcV7TmuLs6ZvdQQeGZewXro3t= Aano8mpyFA5NxYRJahdQhdg$ for graphic product...

    ATTN...WFO...ABQ...EPZ...FGZ...GJT...LUB...MAF...PSR...SLC...
    TWC...VEF...

    ATTN...RFC...FWR...RSA...STR...NWC...

    LAT...LON 37731346 36941045 35841103 34451128 33890776=20
    34720650 34660422 33790297 30800370 30600515=20
    31450757 31030849 31471143 32441369 34761537=20
    36691580 37671447=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 20 02:37:53 2025
    AWUS01 KWNH 200237
    FFGMPD
    OKZ000-KSZ000-200800-

    Mesoscale Precipitation Discussion 1110
    NWS Weather Prediction Center College Park MD
    1037 PM EDT Fri Sep 19 2025

    Areas affected...South-central Kansas & Adj. North-central
    Oklahoma...

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

    Valid 200240Z - 200800Z

    SUMMARY...Warm advection thunderstorms with some short-term
    training potential may result in a streak of 2-3" totals and
    possible localized flash flooding concerns overnight.

    DISCUSSION...02z Surface analysis shows a developing wave over
    west-central KS with a stationary front angling southeast across
    south-central KS into far northern Oklahoma. Surface to boundary
    layer winds are starting to strengthen from the south, with
    veering with depth. Enhanced moisture and slightly higher theta-E
    axis exists across southwest KS and into the OK and far northern
    TX panhandle and Northwest OK before reducing slightly. As such a
    pool of enhanced unstable air with MUCAPEs up to 2000 J/kg exist
    in warm sector. As surface flow veers near the front, flow is
    increasing moisture flux convergence to overcome the reduced
    capping in the vicinity of Lane/Gove and Ness counties. GOES-E
    10.3um shows cooled overshooting tops cooling to -65C and
    back-sheared anvil indicative of slow moving, rotating updrafts
    with tops.

    WV suite also denotes strong northwesterly flow aloft at the far
    upwind edge of the exiting closed low over the Midwest but ahead
    of the ejecting wave out of UT/CO, providing solid divergence
    aloft while also maintaining favorable upwind energy to support
    backbuilding of the convective complex. Deep layer steering is
    faster than a traditional WAA/training complex and may limit
    residency for extreme totals; the rotating updrafts' propagation
    is reduced by 5-10kts from the mean flow (per Bunker's right mover
    propagation vectors) and are aligned fairly close to the
    orientation of the surface front and orthogonal to the
    strengthening LLJ to support some repeating. Total moisture is
    also a bit shallow at 1.25-1.4" and while flux convergence is
    enhanced to the stronger updrafts, overall rainfall rates are
    likely to be between 1.5-1.75"/hr. As such, streaks of 2-3" are
    probable, especially if the back-building can be maintained and
    ordination does not deviate much from NW to SE.
    Combine that with FFG values of 1.5-2"/hr and 2-3"/3hrs (steadily
    increasing from NW to SE into OK), spots of flash flooding are
    considered possible through the overnight periods.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4vCgITYds8oV0CwYQFt-T5kWn4AID1PiVICOkc-oVfI0ZP99yNHbJjU_OSvPJC1bHurM= 5gqXbqMqamjCyFMuybrGcJM$ for graphic product...

    ATTN...WFO...DDC...GLD...ICT...OUN...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39000054 38829992 38559916 38289825 37919753=20
    37239688 36699710 36519810 37049927 37770015=20
    37930032 38440072 38770087=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 20 03:56:01 2025
    AWUS01 KWNH 200355
    FFGMPD
    NVZ000-200730-

    Mesoscale Precipitation Discussion 1111
    NWS Weather Prediction Center College Park MD
    1155 PM EDT Fri Sep 19 2025

    Areas affected...West-central Nevada...

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

    Valid 200355Z - 200730Z

    SUMMARY...Short-term training with rates up to 1"/hr and localized
    totals to 1.5" may pose localized flash flooding concern for the
    next few hours.

    DISCUSSION...GOES-W WV suite shows further elongation and
    degeneration of the larger scale western trough across northern
    California into the Great Basin. At the col between the two
    larger vorticity centers resides a weak confluence region from
    700-500mb near the intersection of Nye, Mineral and Esmeralda
    counties. Deep layer confluence at the tailing edge of the
    upper-level trough, still has some sufficient DPVA as the shear
    axis lifts across the ridge line of the California Sierra Nevada
    Range. In the lowest levels, surface Tds remain in the low 50s
    and depth of moisture still remains well above normal with Total
    Pwat values of 1-1.1", with the bulk below 700mb as Tds at 700mb
    remain around 5C. Additionally, RAP analysis suggests a weakly
    capped pool of 500 J/kg of MLCAPE remains. The confluence though
    850-700mb is supporting sufficient convergence to overcome the
    weak low level capping and shallow thunderstorms continue to burst
    along this axis with further shallower activity extending
    northwestward toward Pershing and northern Churchill counties.=20
    Rates up to 1"/hr are possible and given cooling tops to -50C
    maybe ongoing.=20

    Deep layer flow from the southwest will steer any activity
    northeastward for some short-term training potential...with
    maximum totals of 1-1.5" possible. Low level inflow remains weak
    but sufficient through the valleys parallel to the CA/NV border to
    maintain a few more hours of further shallow development and
    training capability. Given FFG values are less than .75"/hr and
    less than 1-1.5"/3hrs, flash flooding is considered possible along
    this training axis, though persistent moderate showers may allow
    for other atypical stream flows further into the 700-500mb
    confluence zone toward the north-northwest in west-central NV.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Cam6uYz8tjFg8DvDCyzYnU1nxbiJZMnp6wl7hf7Ggt8qZBA1dmro-kw-fXlzgqe4p2M= _OKlAb5k5P36GHDOPIjdPPs$ for graphic product...

    ATTN...WFO...LKN...REV...VEF...

    ATTN...RFC...RSA...NWC...

    LAT...LON 40401887 40331754 39711678 39101675 38411713=20
    37831799 38161842 39181838 39951897=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 21 02:13:53 2025
    AWUS01 KWNH 210210
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-210800-

    Mesoscale Precipitation Discussion 1112
    NWS Weather Prediction Center College Park MD
    1009 PM EDT Sat Sep 20 2025

    Areas affected...Northeast OK...Southwest MO...Northwest AR...Far
    Southeast KS...

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

    Valid 210210Z - 210800Z

    SUMMARY...Increasing WAA from strengthening low-level jet
    intersecting pool of moist/unstable air. Favorable mid-level flow
    may support training and isolated back-building/cell mergers to
    support

    DISCUSSION...GOES-E WV suite shows a subtle shortwave feature
    moving along the central OK/KS boarder providing some mid-level
    DPVA and positive ascent profiles downstream, coincident with
    early evening low-level jet acceleration up to 20kt and eventually
    veering more southwest to northeast and into the 30kt range. This
    ascent is interacting with an old linger outflow boundary from
    this morning's activity that connects from the surface front just
    east of AVK toward SWO, MKO, FSM and more east across central AR.=20
    Enhanced moisture of upper 60s to even mid 70s Tds with still some
    remaining higher surface temperatures maintains a pool of
    2000-2500 J/kg of MLCAPE across NE OK. The ascent pattern
    convection has been pressing eastward into Osage county and
    isolated pre-cursory cells north of Tulsa have been fairly
    stationary in a 500-1000mb thickness ridge, that supports some
    upstream redevelopment. Stronger updrafts and low level moisture
    has made the cells fairly prolific/intense with hourly rates up to
    2"/hr, with some localized observations over 3" near
    Collingsville. This activity is likely to become a bit more
    progressive with time, but localized totals may intersect areas
    saturated this morning and have lower FFG values of 1.5"/hr and
    less than 3"/3hrs, suggesting increased run-off is possible.

    Further northeast, the northeast edge of the LLJ combined with the
    northern edge of this morning's rain foot has concentrated
    flow/convergence to support a NW to SE oriented 925-850mb FGEN
    band. The convergence along which has sprouted some elevated
    convection along the northeast edge of the higher instability air.
    Deeper layer flow, here initially will support NW to SE cell
    motions allowing for some potential training across SW MO/NW AR.=20
    Spots of 2-3" may be possible, but eventual backing of the deeper
    layer flow will reduce orthogonal ascent convergence and cells
    from NE OK, will slide northeast and meld/merge. Rates may
    trickle up to 1.75-2"/hr for these short-term mergers, but given
    more rugged terrain with low water crossings, there is some
    potential for possible incident or two of localized flash flooding
    through the overnight period here as well.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_xp65VQ2MNcpbph3TQEkY66KmhWeulAAQwOxxAycrLMAfmHAZREsooxCtV72-ZYUMn6W= wuxj_HVMHjB-3iXlzKTKUro$ for graphic product...

    ATTN...WFO...ICT...LZK...SGF...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 37469484 37159307 36649217 36029197 35679252=20
    35869334 35979438 35819600 36279667 36859667=20
    37239626=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 21 07:08:59 2025
    AWUS01 KWNH 210708
    FFGMPD
    MOZ000-ARZ000-211130-

    Mesoscale Precipitation Discussion 1113
    NWS Weather Prediction Center College Park MD
    308 AM EDT Sun Sep 21 2025

    Areas affected...Northwest and north-central Arkansas...Far
    Southern Missouri...

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

    Valid 210715Z - 211130Z

    SUMMARY...Mature MCS continues to be fueled by upstream unstable, warm-advection for a few more hours. Additional 2-3" totals over
    saturated grounds will continue to pose localized flash flooding.

    DISCUSSION...Regional RADAR mosaic shows a mature MCS with forward
    propagating outflow boundary convection along the southern flank
    of the complex from Madison to Marion counties in N AR. Resultant
    Meso-high is reducing residency for the squally line, however, VWP
    continues to depict favorable 15-25kt inflow from the southwest
    (out of NE OK), where the remaining pool of moderately unstable
    air, higher low level theta-E air resides. RADAR denotes this
    with the upwind edge lifting northeast across far NW AR,
    potentially back across the most saturated zones of SW MO and NW
    AR. This while remaining in fairly diffluent flow aloft at the
    splitting of the upper-level jet and right entrance of a 50kt
    speed max across far SE KS into western MO; these features will
    help to maintain the upwind WAA for a few more hours, but
    divergence and remaining unstable air should slowly reduce the
    convective vigor of the overall complex in the next 2-3 hours.=20=20

    Still, ample deep layer moisture and 1000-1250 J/kg of unstable
    air with the strength of flux will maintain some rainfall
    efficiency toward 1.5"/hr. As deeper layer steering flow backs
    from westerly to southwesterly, current orientation of the outflow
    boundary may yield some short-term training as well, mainly across
    saturated areas from this round, but also earlier Saturday
    morning. An additional 2-3" locally (particulalry along the
    upwind edge of the complex) will continue to pose a localized
    flash flooding risk through the late overnight period (3-4 hrs).=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-8EvAbxrjlXTy_-lIO4sDca2_KC1sDBToAAu5h3GJYPj3pBIV-MYRMusvaMuUyNTiovg= UacmOnKFKUi2p27rH1SeGvU$ for graphic product...

    ATTN...WFO...LZK...SGF...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 36879333 36719223 36529136 36159109 35659117=20
    35429171 35309264 35389383 35629431 36389445=20
    36789396=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 21 08:58:21 2025
    AWUS01 KWNH 210858
    FFGMPD
    KSZ000-211330-

    Mesoscale Precipitation Discussion 1114
    NWS Weather Prediction Center College Park MD
    457 AM EDT Sun Sep 21 2025

    Areas affected...Central Kansas...

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

    Valid 210900Z - 211330Z

    SUMMARY...A few scattered incidents of flash flooding are possible
    as cells capable of 1.5"/hr may repeat/train over the next few
    hours. A spot or two of 2-3" totals will near FFG, suggesting
    isolated localized flash flooding is possible.

    DISCUSSION...GOES-E WV suite depicts a very broad area of large
    scale diffluence across much of Kansas, as a strong 90kt 250mb jet
    turns southeast out of CO into NW TX; while a digging northern
    stream trough and shortwave crossing west-central NEB provide
    large scale divergence ascent across KS. Toward the surface, a
    poorly defined surface boundary extends from the Kansas City Metro
    southwest toward a low near Wichita, then extends due west before
    turning north across eastern CO. Broad southerly flow across the
    southern Plains remains about 20-25kts providing moderate moisture
    flux, with the nose of the moisture axis centered along 98W. CIRA
    LPW shows the enhanced pockets of moisture from surface (Tds in
    the low to mid 60s throughout KS/OK), overlap with maxima across
    the 850-700mb layer along the KS/OK border and 700-500mb in
    central OK...resulting in a 1.5" total PWat corridor toward the
    area of concern fluxed on the LLJ.

    Steeper mid-level lapse rates has provided broad area of
    conditionally unstable air with 1000-1250 J/kg of MUCAPE across
    the area of concern. However, maximized convergence has resulted
    in two west to east moisture convergence axes; the first lower,
    just near the boundary layer has activated scattered, narrow
    updrafts with a few stronger isolated near surface rooted embedded
    cells across SW KS that have greater cloud depth an moisture
    availability. This, while speed convergence and weak FGEN ascent
    could tap elevated unstable air near 800mb in proximity to I-70
    corridor. As such, regional RADAR shows greater convective vigor
    over a broader area, further north. Rates up to 1.25-1.5"/hr are
    probable with the elevated cells. Both areas have favorable
    orientation to the deeper west to easterly flow and with solid
    outflow aloft, should maintain on the modest remaining instability
    for the next few hours. Given repeating/training potential,
    widely scattered totals of 3"+ are possible.

    Hydrologically, FFG values are 1.5"/hr and about 2.5"/3hrs.
    However, there are areas of recent heavier rainfall that have
    likely rebounded a bit too quickly as noted in NASA SPoRT 0-40cm
    soil ratios in the 50-60% range from Hodgeman to Stafford counties
    and further south across Pratt, Barber, Kingman and Harper
    counties from last night's complex. Given the rates and cell
    orientation, FFG exceedance and localized flash flooding is
    considered possible, until southerly moisture flux convergence
    becomes too weak to maintain convective vigor

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_ZkBD8gzxo8ijy8VPzOzBVt_tpjly5t5uMLSvjb012_CRZ9Ni9J3wsQDVJbrSZBf7nHI= m0F4kJOLSHAMUStTLGYuhh8$ for graphic product...

    ATTN...WFO...DDC...GID...ICT...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39289872 39279787 39249743 39039690 38709640=20
    38359624 37979643 37699706 37569743 37409810=20
    37279902 37379974 37770046 38240049 38640018=20
    39069969=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 22 07:32:06 2025
    AWUS01 KWNH 220732
    FFGMPD
    ARZ000-OKZ000-221300-

    Mesoscale Precipitation Discussion 1115
    NWS Weather Prediction Center College Park MD
    331 AM EDT Mon Sep 22 2025

    Areas affected...Eastern Oklahoma...Western to Central Arkansas...

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

    Valid 220730Z - 221300Z

    SUMMARY...Area of concern will remain in favorable region for
    upstream redevelopment and repeat track clusters of storms. Rates
    to 1.5"/hr and spots of 2-3.5" suggest an incident or two of
    localized flash flooding is possible through daybreak.

    DISCUSSION...GOES-E WV suite denotes compact shortwave at base of
    broader scale long wave trough is exiting south-central MO, with
    trailing confluence trough through the low to mid-levels lingering
    across west-central AR into far eastern OK. A few stronger
    clusters with rates of up to 1.5"/hr and similar localized totals
    have been noted along this axis for much of the overnight period,
    helping to saturate the upper soil profiles and locally reduce
    FFG. However, recent 3.9um/10.3um IR loops show increasing
    mid-level cloudiness and agitated shallow convective environment
    across the upstream edge of the ongoing clusters. RAP analysis
    denotes a weakening cap with CINH reducing below 15 J/kg across
    western AR into far Northeast TX, generally coincident with
    instability and low to mid-level confluence axis. While, lapse
    rates are limited, low level theta-E remains and supports
    1000-1250 J/kg of MLCAPE trough this area and points west. CIRA
    LPW and RAP analysis also note the deeper layer moisture axis
    further west within the broader southwesterly 25-30kt LLJ across
    central to eastern OK, though overall deep layer confluence also
    depicts a pool of moisture to 1.7" along the best convergence over
    western AR.

    Aloft, the speed max of the subtropical jet is reaching the apex
    of the ridge further upstream over CO, but the exit of the jet is
    digging southward across central OK/NE TX, resulting is broadening
    left exit divergence to support upstream redevelopment and slow
    veering of the LLJ further increasing low-level convergence. As
    such, expectation for further upstream development is expected for
    the next 3-6hrs. Deep layer steering mean flow is toward the
    northeast as the shortwave exits, however, the strength of the
    approaching jet has sharpened the 500-1000 thickness ridge to the
    west and propagation vectors are starting to turn upstream to the
    low-level inflow, bending the storm track vectors more west to
    east. This should allow for upstream thunderstorm clusters that
    do develop to once again track through areas recently saturated.=20
    Rates of 1.5"/hr and potential for additional 2-3" totals suggest
    scattered incidents of localized flash flooding are becoming
    increasingly possible through the remainder of the overnight
    period. There remains some uncertainty to the latitude of the
    redevelopment, but any activity further north will also intersect
    areas saturated over the last two nights as well into NW,
    north-central AR.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8BblS9xxEqPsw_KBtK_DrEPLT3ltN387XEmCj8W7t-snZuSyK92wcWmOEthTaSIkNEDq= WcUO_g9tzGv6ePFuxOJ77HY$ for graphic product...

    ATTN...WFO...LZK...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 36169515 36049332 35769228 35319175 34679197=20
    34509246 34509322 34699424 35039523 35669561=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 22 13:01:33 2025
    AWUS01 KWNH 221301
    FFGMPD
    ARZ000-TXZ000-OKZ000-221740-

    Mesoscale Precipitation Discussion 1116
    NWS Weather Prediction Center College Park MD
    900 AM EDT Mon Sep 22 2025

    Areas affected...eastern OK into central/northern AR

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

    Valid 221259Z - 221740Z

    SUMMARY...Continued training of showers and thunderstorms will
    maintain an increased potential for flash flooding from portions
    of eastern OK into central/northern AR over the next 3-5 hours.
    Hourly rainfall will range from 1 to 3 inches.

    DISCUSSION...Radar imagery from 1230Z showed an ongoing cluster of thunderstorms over north-central AR, in the vicinity of I-40 to
    the west of Little Rock. This area has been associated with
    MRMS-derived hourly rainfall of 1 to 3 inches since at least 10Z
    within areas of training. A second small cluster was located just
    north of Dallas/Fort Worth while additional shower/thunderstorm
    activity was developing over eastern OK. All of these areas were
    located just north of an effective quasi-stationary front draped
    from AR WSW into northern TX enforced by rain-cooled outflow. VAD
    wind plots across the region highlighted 850 mb wind speeds of
    20-30 kt from the SW across TX into AR but with veering toward the
    WSW over TX since 10Z. Meanwhile, SPC mesoanalysis data from 12Z
    indicated MLCAPE of 1000-1500 J/kg along and north and just north
    of the effective front with short term RAP forecasts showing
    weakening inhibition over eastern OK over the next few hours with
    the onset of daytime heating and continued low level moisture
    advection into the region.

    Short term RAP forecasts are in line with weakening of the low
    level jet through 18Z but the boundary will remain and some degree
    of overrunning should continue over the next few hours with a
    strongly favorable diffluent/divergent region aloft over AR ahead
    of a sub-tropical jet max over KS/OK. Some expansion of
    shower/thunderstorm activity is expected over eastern OK over the
    next 1-2 hours with potential for training within the mean
    westerly steering flow. Given the high precipitable water
    environment (1.5 to 2.0 inches) and sufficient instability,
    pockets of training are likely to continue at least localized
    areas of flash flooding over the next 1-2 hours with possible
    continuation of the flash flood threat through 17Z, though
    confidence beyond the next 1-2 hours is lower than average given
    poor model handling of the ongoing activity.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7mMb_MBCtX5vSFb7ebwCcUwmlv3mlFQoNNIOP_o31Z9Ie_pL5TBxwBb1D-0tU0iRsX73= N0maKVVqiLfDKtL_EyRyz58$ for graphic product...

    ATTN...WFO...FWD...LZK...MEG...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 36049368 35959248 35739092 35419054 34569097=20
    34409275 34289423 33669526 32999622 33179711=20
    33599726 34759684 35579603 35999493=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 22 23:05:48 2025
    AWUS01 KWNH 222305
    FFGMPD
    NMZ000-230200-

    Mesoscale Precipitation Discussion 1117
    NWS Weather Prediction Center College Park MD
    704 PM EDT Mon Sep 22 2025

    Areas affected...Portions of Central and Eastern NM

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

    Valid 222304Z - 230200Z

    SUMMARY...Bands of heavy showers and thunderstorms will be
    impacting central and eastern NM over the next couple of hours.
    Some flash flooding impacts may occur over especially portions of
    the Sacramento Mountains where there are sensitive burn scar
    locations.

    DISCUSSION...The latest GOES-E IR satellite imagery along with
    radar shows a couple of bands of heavy showers and thunderstorms
    moving rather progressively off to the east across central NM.
    This activity is advancing east in conjunction with shortwave
    energy traversing the southern Rockies and interacting with a
    relatively convergent, moist and unstable boundary layer pooled
    across central and eastern NM.

    SBCAPE values are locally near 1000 J/kg with PWs across the
    region running upwards of 1 to 2 standard deviations above normal.
    Some shear is noted overhead with the belt of stronger shortwave
    energy nearby, and this is favoring some loose organization of the
    convection with bands of multicell activity.

    Despite the progressive nature of the convection, this activity
    will be capable of bringing heavy rainfall rates which will soon
    impact the Sacramento Mountains and portions of the Lincoln
    National Forest where there are multiple sensitive burn scar
    locations. This includes the Blue 2, South Fork, Salt and McBride
    burn scar complex, and notably near and adjacent to Ruidoso.

    Rainfall amounts of as much as a 0.50 inch in 15 minutes will be
    possible, with some spotty storm totals of up to 1 inch where any
    repeating cell-activity occurs through early this evening. These
    rains may result in there being some burn scar flash flooding
    impacts as a result over the next 1 to 2 hours until the activity
    passes off to the east.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6QEWH4X4cJCACaXajCgebzBFdObj0PLsGvdgycDMbAYD4-eeJ0khZyQnuz-wzT0vx6x3= xUrZGPGwDNp3gi-dv2fzSmU$ for graphic product...

    ATTN...WFO...ABQ...EPZ...

    ATTN...RFC...FWR...NWC...

    LAT...LON 34480446 33940410 33560422 33140479 32850604=20
    32880675 33110718 33440732 33800714 34270620=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 22 23:14:48 2025
    AWUS01 KWNH 222314
    FFGMPD
    KSZ000-COZ000-230500-

    Mesoscale Precipitation Discussion 1118
    NWS Weather Prediction Center College Park MD
    713 PM EDT Mon Sep 22 2025

    Areas affected...Portions of Far Eastern CO and Western KS

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

    Valid 222313Z - 230500Z

    SUMMARY...Developing and expanding clusters of heavy showers and
    thunderstorms are expected going into the evening hours across
    portions of far eastern CO and western KS. Isolated areas of flash
    flooding will be possible.

    DISCUSSION...Late-day GOES-E visible satellite imagery along with
    regional radar data shows developing and gradually expanding
    clusters of heavy showers and thunderstorms across parts of far
    eastern CO and northwest KS, with the activity focusing along a
    developing frontal boundary. Increasing low-level moisture
    convergence is noted along this front, and the convection is
    developing within a moderate to strongly unstable airmass
    characterized by MLCAPE values of 1500 to 2500 J/kg.

    This instability along with 30 to 40+ kts of effective bulk shear
    is already favoring some supercell thunderstorm development, and
    over the next several hours as upstream shortwave energy/forcing
    arrives from central Rockies and crosses the High Plains, there
    will be a favorable environment for expanding and organizing
    clusters of multicell and supercell thunderstorms.

    By early to mid-evening, the main convective threat area should
    involve far eastern CO and western KS, but a combination of
    cell-merger activity and upscale MCS development is expected in
    time as DPVA/height falls provide stronger forcing in conjunction
    with a strengthening southerly low-level jet across the central
    Plains ahead of the aforementioned front. This will gradually
    allow for the convective mass to expand off to the east and
    southeast going through the overnight hours.

    While much of the convection this evening will primarily be of a
    severe nature, there will be sufficient levels of moisture
    transport and convective cell organization to promote high
    rainfall rates that may reach 1 to 2 inches/hour. Cell-merger
    activity and localized cell-training concerns may foster there
    being some rainfall totals of 3 to 4+ inches by mid-evening. This
    is consistent with the 18Z HREF/12Z REFS suites of guidance.

    As a result, there may be an isolated threat for some flash
    flooding over the next several hours as these stronger multicell
    and supercell thunderstorm clusters evolve.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9IJ6lg5u3UtcfLHVvR4vbV7rFLaQCb6tyJnIuXhtyRieIFnzk0e7ShbKimi-k8gEWlIH= KCoQQcTf82-USiTV5IvTXQc$ for graphic product...

    ATTN...WFO...BOU...DDC...GID...GLD...PUB...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39710138 39670031 39479958 38769927 38109956=20
    37950065 38300152 38400196 38680289 38800343=20
    39250362 39500322 39620231=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 23 01:06:50 2025
    AWUS01 KWNH 230106
    FFGMPD
    NEZ000-SDZ000-230630-

    Mesoscale Precipitation Discussion 1119
    NWS Weather Prediction Center College Park MD
    905 PM EDT Mon Sep 22 2025

    Areas affected...Southwest SD...Northwest NE

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

    Valid 230105Z - 230630Z

    SUMMARY...Slow-moving heavy showers and thunderstorms may result
    in a threat for isolated areas of flash flooding over the next
    several hours.

    DISCUSSION...The latest GOES-E IR satellite imagery shows cooling
    convective tops across southwest SD in response to a combination
    of amplifying mid-level shortwave energy and a nose of moderate
    instability focused near a front. MLCAPE values of 1000 to 2000
    J/kg are noted across the region along with an axis of moderately
    strong moisture convergence.

    Model guidance suggests a further amplification of mid-level
    energy/height falls with a rather tight 700 mb circulation
    forecast to evolve overnight along the SD/NE border with a slow
    southward drift in time. This will help support a relatively
    strong mid-level deformation zone around the western flank of the
    low center, with a favorable axis of moisture convergence and some frontogenetical forcing working in tandem with the available
    instability to support additional concentrated focus for heavy
    showers and thunderstorms.

    Rainfall rates with the convection over the next few hours will be
    capable of reaching 1 to 2 inches/hour, and with the slow
    cell-motions, some localized storm totals may reach 3 to 4 inches
    which is consistent with the latest hires model guidance. An
    isolated threat for flash flooding will exist where the heavier
    rainfall totals materialize over the next several hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!591XiKxBXRChhYw7AD4xj8WZr883DGw6HhZ1CVNV_VSG5T2v_5HTGwA_s-p0GB7br9AN= P0w_s-4BeL3b1zTMoEAHZlE$ for graphic product...

    ATTN...WFO...CYS...LBF...UNR...

    ATTN...RFC...KRF...NWC...

    LAT...LON 44570340 44480281 43950219 43330120 42820105=20
    42670149 42620181 42480227 42100279 42310354=20
    43080399 43570395 44140386=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 23 02:32:02 2025
    AWUS01 KWNH 230231
    FFGMPD
    IAZ000-NEZ000-230800-

    Mesoscale Precipitation Discussion 1120
    NWS Weather Prediction Center College Park MD
    1031 PM EDT Mon Sep 22 2025

    Areas affected...Southwest Iowa...Eastern Nebraska...

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

    Valid 230230Z - 230800Z

    SUMMARY...Slow moving/stationary cells to intersect back-building
    upwind edge of southward moving squall line in IA. Strong
    moisture flux convergence will support rates up to 2" and
    localized spots of 2-4" resulting in scattered localized flash
    flooding.

    DISCUSSION...02z surface analysis shows a sharpening frontal zone
    across northern IA, in particular in NW IA before front stalls
    northeast of developing surface wave near Ord, NEB. This northerly
    flow is opposed by strengthening south and southwesterly flow
    across SE NEB and within 850mb 25-30kt LLJ. RAP analysis fields
    show much of eastern NEB and SW IA remain fairly unstable, though
    capped with over 2000 J/kg of MLCAPE. As FGEN/moisture flux
    convergence continues to strengthen, the cap has already weakened
    in a few places in E NEB for stronger cells to develop, but will
    continue to expand with time. Combine this with outflow from
    ongoing convective squall line in central IA, likely to further
    build/expand convective coverage westward into the strengthening
    WAA.

    Aloft, the dominant closed low over the Great Lakes is breaking
    eastward while the replacing stronger cyclone is building through
    the Central Rockies. This has lead to a decoupling/de-phasing of
    the longer wave trough and resulted in a mid-level col in the
    flow. Stretching and overall DPVA remains to provide strong
    ascent, though the deformation zone from 700-500mb will allow for
    very slow cell motions with upstream back-building likely along
    the flanking outflow boundaries from the cells themselves. The
    strength of moisture flux convergence of 25-30kts and Tds in the
    50s to mid 60s through 700mb supports total Pwats toward 1.75" and
    convergence to allow for cells to be highly efficient with rates
    of 2"/hr probable. The limited motions should also support
    localized totals of 2-4" over 2-3hrs especially before the cold
    front starts surging (mainly from east to west-southwest) through
    the early overnight period.=20

    While the area has been stricken by drought conditions, as NASA
    SPoRT 0-40cm RSM values are at or below 10%, the steer magnitude
    of rates on hard grounds will have limited infiltration initially
    and support higher run-off potential. Combine this with hourly
    FFG values around 1.5-2"/hr & 2-3"/3hrs, these scattered slow
    moving cells initially will pose a possible localized flash
    flooding concern though the early overnight period. As the front
    presses cells south, shorter residency should limit totals but
    isolated flash flooding will still be a problem in the area of
    concern.=20


    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!81GcsSC-8A_pdUA78uSry6rllqC7eTr38gojJa-rTH5W9swqUOe8N6PS7T9sx2_ZiPLJ= aLjUo53Bar31VoghLkM4jQU$ for graphic product...

    ATTN...WFO...DMX...GID...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 42179617 42129450 41919369 41309318 40639362=20
    40649603 40259793 40699884 41469880 42039733=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 23 04:42:50 2025
    AWUS01 KWNH 230441
    FFGMPD
    KSZ000-231015-

    Mesoscale Precipitation Discussion 1121
    NWS Weather Prediction Center College Park MD
    1241 AM EDT Tue Sep 23 2025

    Areas affected...Much of Western & Southern Kansas...Northern
    Oklahoma...

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

    Valid 230445Z - 231015Z

    SUMMARY...A highly dynamic environment will support strong
    moisture flux into a deformation zone resulting in slow moving but
    efficient rainfall production (rates to 1.75"/hr) resulting in
    localized spots of 2-3"+ and possible scattered localized flash
    flooding.

    DISCUSSION...GOES-E WV shows core of developing larger scale
    closed low over the Central Rockies with strong undercutting polar
    jet energy across Colorado into the Central Plains.
    Simultaneously, the apex of the subtropical jet has reached KS and
    with broad anticyclonically curved baroclinic shield of cirrus
    over much of northern KS and southern NEB, with occasional
    overshooting tops breaking out through the canopy. An older
    smaller scale shortwave exists in the increasingly divergent
    portion of northern KS and will meld with southern stream
    shortwave surging out of the TX/OK panhandles.

    With all the moving parts in the mid-levels, the surface pattern
    is lagging a bit being a bit further north for the frontal zone,
    with a cold front surging down eastern CO, a surface wave in NW KS
    is slow to advance southeast and with further surge of WAA across
    south-central into E NEB; this results in a broad conditionally
    unstable warm sector across much of western and central KS. With
    the southwesterly surge of low to mid-level flow, the warm
    conveyor belt/LLJ is strengthening and becoming increasingly
    convergent across the KS/OK border though is starting to back from
    southerly to southeasterly as the southwesterly drier air lifts.=20
    This is sharpening a shear/stretching deformation zone across
    west-central KS through toward north-central KS from TQK to HYS to
    CNK. This will support strong deep layer moisture flux
    convergence and with ample 1500-2000 J/kg of CAPE will allow for
    stronger vertical development and potential for rates of
    1.5-1.75"/hr, given flux of 1.5" PWs mainly loaded below 700mb.=20

    As the 700-500mb low sets up along the lower-level deformation
    zone, cell motions will be slow and eastward with potential for
    some mergers/collisions so occasional embedded uptick toward 2"/hr
    rates. The higher residency of a few hours to exhaust the
    unstable air, should allow for localized totals of 2-3"+ perhaps
    an isolated 4" total. There is a fairly sharp gradient of soil
    saturation conditions across central KS being wetter further
    south. Still, FFG values of 1.5"/hr and less than 3"/3hrs seem
    approachable suggesting a few scattered incidents of flash
    flooding are considered possible through the remainder of the
    overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9XoGsiMKe81FpYQMuvFd2upn0BNKW47QqxUDv1AuhqGwSm4qZF2umCqEw5VkaoSVrytK= b6pFOrSRyeAC_hpDXcJ7GvU$ for graphic product...

    ATTN...WFO...DDC...GID...GLD...ICT...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39499740 39369669 38579653 37849834 37820024=20
    38210134 38620178 39130159 39350117 39340033=20
    39239918 39299818=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 23 04:52:43 2025
    AWUS01 KWNH 230451
    FFGMPD
    KSZ000-231015-

    Mesoscale Precipitation Discussion 1121...Corrected
    NWS Weather Prediction Center College Park MD
    1250 AM EDT Tue Sep 23 2025

    Corrected for Correction for Areas Affected

    Areas affected...Western to Central Kansas....

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

    Valid 230445Z - 231015Z

    SUMMARY...A highly dynamic environment will support strong
    moisture flux into a deformation zone resulting in slow moving but
    efficient rainfall production (rates to 1.75"/hr) resulting in
    localized spots of 2-3"+ and possible scattered localized flash
    flooding.

    DISCUSSION...GOES-E WV shows core of developing larger scale
    closed low over the Central Rockies with strong undercutting polar
    jet energy across Colorado into the Central Plains.
    Simultaneously, the apex of the subtropical jet has reached KS and
    with broad anticyclonically curved baroclinic shield of cirrus
    over much of northern KS and southern NEB, with occasional
    overshooting tops breaking out through the canopy. An older
    smaller scale shortwave exists in the increasingly divergent
    portion of northern KS and will meld with southern stream
    shortwave surging out of the TX/OK panhandles.

    With all the moving parts in the mid-levels, the surface pattern
    is lagging a bit being a bit further north for the frontal zone,
    with a cold front surging down eastern CO, a surface wave in NW KS
    is slow to advance southeast and with further surge of WAA across
    south-central into E NEB; this results in a broad conditionally
    unstable warm sector across much of western and central KS. With
    the southwesterly surge of low to mid-level flow, the warm
    conveyor belt/LLJ is strengthening and becoming increasingly
    convergent across the KS/OK border though is starting to back from
    southerly to southeasterly as the southwesterly drier air lifts.=20
    This is sharpening a shear/stretching deformation zone across
    west-central KS through toward north-central KS from TQK to HYS to
    CNK. This will support strong deep layer moisture flux
    convergence and with ample 1500-2000 J/kg of CAPE will allow for
    stronger vertical development and potential for rates of
    1.5-1.75"/hr, given flux of 1.5" PWs mainly loaded below 700mb.=20

    As the 700-500mb low sets up along the lower-level deformation
    zone, cell motions will be slow and eastward with potential for
    some mergers/collisions so occasional embedded uptick toward 2"/hr
    rates. The higher residency of a few hours to exhaust the
    unstable air, should allow for localized totals of 2-3"+ perhaps
    an isolated 4" total. There is a fairly sharp gradient of soil
    saturation conditions across central KS being wetter further
    south. Still, FFG values of 1.5"/hr and less than 3"/3hrs seem
    approachable suggesting a few scattered incidents of flash
    flooding are considered possible through the remainder of the
    overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8CmRk1etGdEO6-eWZwsb5ll8cjyE_b2n0s0slx-Z4dZQhZWEBj494Vlkqh0ni14PBPwx= SYrLk1g74k_Uxy9CsqWAOWg$ for graphic product...

    ATTN...WFO...DDC...GID...GLD...ICT...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39499740 39369669 38579653 37849834 37820024=20
    38210134 38620178 39130159 39350117 39340033=20
    39239918 39299818=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 23 05:19:43 2025
    AWUS01 KWNH 230519
    FFGMPD
    OKZ000-KSZ000-231030-

    Mesoscale Precipitation Discussion 1122
    NWS Weather Prediction Center College Park MD
    118 AM EDT Tue Sep 23 2025

    Areas affected...Southern Kansas...Northern Oklahoma...

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

    Valid 230515Z - 231030Z

    SUMMARY...Efficient, intense, quick-hitting thunderstorms capable
    of sub-hourly totals of 1-2" and totals to 3"+ pose localized
    flash flooding concerns through overnight period.

    DISCUSSION...GOES-E 10.3um IR loop shows fast moving clusters of
    thunderstorms with isolated overshooting tops cooling to -80C
    across SW KS into NW OK. RADAR mosaic denotes the broadening arch
    of these cells in advance of a fast moving southern stream
    shortwave features exiting the OK Panhandle. The arch is an
    alignment of mid-level DPVA ascent and strong confluent boundary
    layer convergence of southwesterly flow off the high terrain and
    broadening, but strengthening LLJ responding to the much larger
    scale height-falls and organization of the closed low across the
    Central Rockies. VWP and RAP analysis shows the strong deep
    layer WAA veering with strengthening 30 to 35kt flow through
    925-850mb convergent on this arch. Low 70s Tds at the surface,
    60s through 850mb and even low 40s at 700mb shows convergence
    though depth very well within animation of the CIRA LPW resulting
    in 1.75" total PWats, but very strong deep layer flux convergence.
    MLCAPEs over 3000 J/kg combined with strength of flux is
    resulting in high rainfall generation/efficiency for these
    expanding clusters.=20

    Limiting factors are the strength of the flow, is resulting in
    very quick cell motions of 30-40kts, limiting residency. However,
    regional RADAR mosaic denotes the updrafts are broadening along
    the length of the mean flow, increasing duration ever so slightly.
    Currently, KDDC/KVNX suggest hourly estimates of 1-1.5", though
    are steadily increasing given overall increase of deep layer
    moisture. 03z HRRR suggests peak of 1.5-2" in 15 minutes across
    south-central KS between 06-08z, which does not seem implausible
    and aligns with 00z HREF 2"/hr probability of 40%. As such,
    localized totals of 2-3" in 1-2 hours may result in localized
    flash flooding conditions, especially given most areas within the
    area of concern have 1hr FFG values at or below 2", with some
    areas of south-central KS into northeast OK, slightly reduced
    further to below 1.5", given recent rainfall. Still, the overall
    speed of cells may result in a highly variant rainfall pattern
    resulting in scattered incidents of flash flooding overnight.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_yMbKuqR-e7d7sKqPNw_G-AL1eLFqdnLf-d_vov8B6wRoUxvkp5L8n8GikXRHdVpSuvJ= Wn5O2RWDIQbt_MG4Xb8sd5E$ for graphic product...

    ATTN...WFO...DDC...ICT...OUN...TSA...

    ATTN...RFC...TUA...NWC...

    LAT...LON 38229763 37959602 37539537 36979526 36529543=20
    36229603 36149709 36199823 36349917 36979966=20
    37519987 38019910=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 23 10:00:58 2025
    AWUS01 KWNH 231000
    FFGMPD
    MOZ000-KSZ000-NEZ000-231500-

    Mesoscale Precipitation Discussion 1123
    NWS Weather Prediction Center College Park MD
    600 AM EDT Tue Sep 23 2025

    Areas affected...Northeast Kansas...Northwest Missouri...Far
    Southeast Nebraska...

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

    Valid 231000Z - 231500Z

    SUMMARY...Broad scale over-turning of remaining unstable air will
    have short-term rates of up to 2"/hr and localized totals to 2-3"
    in 1-3 hours, resulting in possible localized flash flooding.

    DISCUSSION...GOES-E WV suite depicts broad diffluent region
    downstream of strengthening deep layer cyclone over the central
    Rockies. An embedded shortwave is sharpening and vertically
    stretching within the divergent pattern aloft, providing solid
    DPVA across northeast KS into far southeast NEB and northwest MO.
    This area has remained conditionally unstable and capped through
    the early overnight period with broad 2000 J/kg MUCAPE reservoir
    along and southwest of the Missouri River Valley.

    Outflow boundary and southward sinking cold front out of IA and
    east-central NEB initially provided sufficient convergence along
    the northeast edge of the instability core and rapid expansion has
    occurred over the last hour or so as southwesterly WAA has further
    impinged on the area. Strong ascent and ample deep layer moisture
    has supported localized rates of 1.5-2"/hr and with very
    slow/stationary cell motions, generally only moving due to
    outflow/propagation, an hour or so of intense rainfall may again
    result in widely scattered 2-3" totals in 1-3 hours.=20

    Additionally, as the southern stream shortwave melds with the
    northern stream feature, effectively elongating the mid-level
    trough toward a longer negative tilt orientation, but also
    strengthened southwesterly flow and deep layer convergence with
    the core of the southerly LLJ and effective moisture flux.=20
    Leading edge convergence is also building a west to east oriented
    arc of thunderstorms along the southwestern edge of the unstable
    air, slow northward migration and intersection with the convective
    outflow from the northwest will see a larger slab ascent with
    broad overturning of the remaining 1.5-1.75" total Pwats in the
    column and likely result in similar hourly rates up to 2"/hr but
    likely to diminish quickly thereafter, likely resulting in widely
    scattered pockets of 2-3" totals further southwest across
    northeast KS toward the KC Metro. The sheer rates may result in
    localized flash flooding conditions, especially near urban
    centers.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4pdf2qDoqkSdexjFO5QAtESE9qpn9JhQgDznwHGojPUQ9CdjCkId2y0f3Gli7Z4kI3Fj= CNK4mAUJtxG9CDmo2NPoxhI$ for graphic product...

    ATTN...WFO...EAX...GID...OAX...TOP...

    ATTN...RFC...KRF...NWC...

    LAT...LON 40709689 40639608 40299516 39759444 39249384=20
    38599419 38469488 38769571 39159679 39429830=20
    40279804 40599744=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 23 12:10:57 2025
    AWUS01 KWNH 231210
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-231709-

    Mesoscale Precipitation Discussion 1124
    NWS Weather Prediction Center College Park MD
    810 AM EDT Tue Sep 23 2025

    Areas affected...southwestern Missouri, far northern Arkansas, far
    northeastern Oklahoma

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

    Valid 231209Z - 231709Z

    Summary...Isolated, spotty flash flood potential exists for a few
    hours this morning (through 17Z/noon CDT).

    Discussion...A loosely organized complex of storms was located
    near the MOKSAROK (Missouri/Kansas/Oklahoma/Arkansas state border
    region) this morning. The loosely organized nature of this
    complex was favoring limited amounts of convective training -
    particularly in southwestern Missouri where downstream
    thunderstorm cells were developing along a warm front near the
    region very close to the Springfield area. Spots of 1 inch/hr
    rain rates were being detected/estimated per MRMS within the
    region of training. Coincidentally, these rain rates were falling
    across areas of the Missouri Ozarks that can be flood prone in
    sensitive areas. With FFG thresholds in the 1.5 inch/hr range in
    spots, any modest uptick in rain rates could cause isolated flash
    flood issues in the short term.

    The longevity of this flash flood risk is a bit in question,
    however. As storms continue to move/propagate east, they will
    eventually depart the region of greatest combined instability and
    low-level convergence (currently focused along the OK/KS border).
    Furthermore, radar data doesn't suggest that ongoing activity has
    sufficient organization for persistence deeper into the
    Missouri/Arkansas Ozarks east of the U.S. Highway 65 and 63
    corridors - especially in the absence of any larger-scale ascent.=20
    Thus - an already isolated flash flood risk may gradually become
    more conditional with time and eastward extent across the
    discussion area.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4YHEa8QUip9B0zHTI9fAaeoGmUgMGi9cFygNsngIv5YUOVxu6DX4SS7VFSQjub_tLoK-= CUm_kqXQ0K6SBPpkh6J0QUU$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...LZK...MEG...PAH...SGF...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38359359 38089199 37389075 36539030 35999152=20
    35829445 36369597 37399511 38219470=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 23 17:44:00 2025
    AWUS01 KWNH 231743
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-232342-

    Mesoscale Precipitation Discussion 1125
    NWS Weather Prediction Center College Park MD
    143 PM EDT Tue Sep 23 2025

    Areas affected...southwestern Missouri, western Arkansas, eastern
    Oklahoma

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

    Valid 231742Z - 232342Z

    Summary...Convective redevelopment is expected over the course of
    the afternoon, with local areas of potentially significant flash
    flooding expected.

    Discussion...Strong convection continues in a relatively focused
    band extending from just northeast of Fayetteville through Branson
    currently. This band of convection is tied to a lead mid-level
    wave over Missouri that should continue to lift slowly
    northeastward and result in subtle subsidence across the
    discussion area for at least an hour or two. These trends, along
    with slackening low-level flow, suggest that a brief reprieve from
    widespread flash flooding (outside of the aforementioned band) in
    the short term.

    Upstream, mid-level convection was already being agitated in part
    due to an approaching mid-level wave evident in satellite imagery
    across central Kansas/northern Oklahoma. Additionally, earlier
    convection has left behind an outflow boundary across northeastern
    Oklahoma and vicinity that connects to a surface low over
    north-central Oklahoma. Each of these features (low-level
    convergence, mid-level ascent) should result in a redevelopment of
    deep convection over the course of the afternoon - though it may
    take some time for deeper convection to materialize. The airmass
    south of the outflow remains abundantly moist and unstable (2 inch
    PW values, 2000+ J/kg MLCAPE). As convection redevelops,
    localized training should result in 2+ inch/hr rain rates that
    could result in significant flash flooding - especially if the
    rainfall occurs in 1) areas that received 2-4 inch rain amounts
    earlier today (southwestern Missouri, far northwestern Arkansas),
    and 2) across portions of the Arkansas River Valley that have
    received 2-8 inches of rain over the past 48 hours.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7rI1I6QlvWvbXX1rE5i0akfkIrAZYFQzvaJwiAevoq_O2ATKzQ99ggbhtq1B15DBKfRB= 9ZYXNadGAfS70RMA7a_sIu4$ for graphic product...

    ATTN...WFO...ICT...LZK...OUN...SGF...SHV...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 37969309 37239185 35349188 34269259 34149522=20
    34919639 36099646 36809616 37599486=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 23 23:46:07 2025
    AWUS01 KWNH 232346
    FFGMPD
    TNZ000-MSZ000-MOZ000-ARZ000-OKZ000-240415-

    Mesoscale Precipitation Discussion 1126
    NWS Weather Prediction Center College Park MD
    745 PM EDT Tue Sep 23 2025

    Areas affected...eastern OK into AR and the MS Valley

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

    Valid 232343Z - 240415Z

    Summary...Training cells will continue areas of flash flooding
    from portions of eastern OK into and across AR to the MS Valley
    into the early overnight. Hourly rainfall of 1 to 3 inches and
    additional localized totals of 3 to 5 inches are expected.

    Discussion...2330Z area radar imagery across the Ozarks into
    southeastern OK showed a line of thunderstorms extending ahead of
    a cold front in eastern OK, and just north of an outflow-enhanced quasi-stationary front which extended west to east through
    north-central AR. Areas of training just south of the Boston
    Mountains have been associated with gauge reports of 0.75 to 1.00
    inches of rain in 15 minutes and 2+ inches in an hour with ongoing
    areas of flash flooding from eastern OK into northwestern AR.

    Water vapor imagery showed the leading edge of a shortwave trough
    moving east from MO into eastern OK with diffluent flow aloft just
    downstream across southern MO and AR. Additional cells, though
    isolated, were noted across the 4-state region (MOKSAROK) in
    conjunction with the shortwave, with portions of southwestern MO
    and northwestern AR having received 72 hour rainfall totals of 2
    to 8+ inches (per MRMS estimates). While these cells are moving
    into an environment largely worked over, relatively steep lapse
    rates could support an isolated core with 1+ inches of rain.
    Meanwhile, 850 mb winds ahead of the slow moving cold front were
    15-25 kt from the SW, overrunning the outflow/stationary front
    across AR with west to east storm motions supporting training. SPC
    mesoanalysis data from 23Z indicated plenty of instability with
    2000-3000 MLCAPE across eastern OK into western AR along with
    PWATs near 2 inches, supportive of high rain rates with this
    environment continuing through at least 04Z with minimal CIN.

    As the mid-level shortwave continues to advance east, the surface
    response will support a slow eastward push to the surface cold
    front with cell motions generally toward the east but with
    potential for upstream development and continued training
    potential. Hourly rainfall of 1 to 3 inches is expected in a few
    location along with isolated 3 to 5 inch additional rainfall
    maxima through 04Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7lVsWVr0RTiCk-IP4eBt-5wdkDiuGDLA77gMOcfChsNeuepdQzAt3nxeyy7Q2neW3Bil= EfrnvvHpJLxy-wxx2B60Pdg$ for graphic product...

    ATTN...WFO...LZK...MEG...SGF...SHV...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 36649429 36569361 35999249 35989145 35638979=20
    34868983 34629068 34299182 33959388 34049490=20
    34309522 34699543 35189541 35769518 36229468=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 24 01:50:20 2025
    AWUS01 KWNH 240147
    FFGMPD
    KSZ000-240730-

    Mesoscale Precipitation Discussion 1127
    NWS Weather Prediction Center College Park MD
    947 PM EDT Tue Sep 23 2025

    Areas affected...western KS

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

    Valid 240145Z - 240730Z

    SUMMARY...Brief training/repeating/backbuilding of showers and
    thunderstorms may result in a localized flash flood threat over
    portions of western KS over the next several hours. Hourly
    rainfall totals of 1 to 2 inches will be possible.

    DISCUSSION...GOES East water vapor showed a closed low over
    eastern CO/western KS embedded within the base of a sharply
    positively tilted longwave trough that extended into the Great
    Lakes and eastern Canada. Radar imagery and gauge reports showed
    moderate to locally heavy rainfall occurring to the north and east
    of a 700-500 mb low along the northern CO/KS border, including a
    north-south oriented tail of rain extending toward the south over
    western KS. This axis aligned within a low level confluent flow
    regime and weak instability (500-1000 J/kg) axis. Mean westerly
    winds were found in the deeper layer flow, supporting individual
    cell motions toward the east, but the pattern will favor
    regeneration of cells within the low level convergence axis over
    the next few hours. In addition, left-exit region divergence is
    present over the region, tied to a 70-90 kt jet max located from
    northern NM into the southern High Plains, which should aid in
    vertical ascent over western KS.

    The environment will be supportive of 1 to 2 inch hourly totals
    due to the potential for brief training/repeating/backbuilding of
    cells (slow net movement) but modest moisture (standardized PW
    anomalies of +1 to +2) and only weak instability should preclude
    higher rainfall rates. Portions of western KS have received well
    above average rainfall over the past week (400 to 600+ percent of
    normal) with above average soil moisture values leading to a
    potentially increased threat flash flood on a localized basis
    given low flash flood guidance values of less than 2 inches in 3
    hours for portions of the region. The flash flood threat is
    expected to slowly translate south as the mid-level trough axis
    and low level forcing shift south over the next 6 hours as
    forecast by the RAP.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6pIWIJ7BEUMvmUTl6T2nKXh1HPDRkRwTOgoD0ao4ZUMFltBgTntVzK7pQKyLQaJU0Iz0= DdzqJmYp7-_46ubc7euIQ94$ for graphic product...

    ATTN...WFO...DDC...GLD...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 39870121 39830088 39610053 38940006 37539979=20
    37140000 37080064 37130099 37320120 37680143=20
    38300170 39040181 39500179 39690173 39820159=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 24 03:08:05 2025
    AWUS01 KWNH 240306
    FFGMPD
    ARZ000-TXZ000-OKZ000-240900-

    Mesoscale Precipitation Discussion 1128
    NWS Weather Prediction Center College Park MD
    1105 PM EDT Tue Sep 23 2025

    Areas affected...Much of Arkansas...Southeast Oklahoma...Far
    Northeast Texas...

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

    Valid 240310Z - 240900Z

    SUMMARY...Developing thunderstorms capable of 1.5-1.75"/hr, likely
    to repeat through areas of saturated soils with scattered pockets
    of additional 2-4" totals, likely resulting in new incidents of or
    continue ongoing flash flooding through the overnight period.

    DISCUSSION...GOES-E WV suite depicts broad core of deep upper low
    well upstream over the Colorado High Plains dropping southeast;
    while a broad elongated mid-level dry slot across centered along
    the KS/OK border extending through MO into the Midwest. This has
    resulted in a regionally flat mid-level shear axis along and north
    of the area of concern. The warm conveyor belt of enhanced deep,
    overlapping moisture axis remains very active with large clusters
    of cold cirrus shield mainly over SW AR, with only a few
    overshooting tops dotting along the moisture axis into far SW
    TN/NW MS.

    As such, the surface to low level environment remains aligned with
    the warm conveyor. A weak surface to 850mb low is exiting NE OK
    into the Ozark Plateau, with upstream cold advection occurring
    across E OK. This sharpening has increased convergence along a
    remaining axis of 2000 J/kg of MLCAPE supporting a secondary
    increase in convective vigor and coverage upstream of the initial
    band that is slowly eroding and becoming more scattered in nature
    across central AR toward the TN/MS line. With additional
    development upstream of areas already flooded across NW AR and E
    OK, additional 2-3" totals due to 1.5"/hr rates is likely to
    maintain ongoing flooding situations.

    However, further southwest, the reservoir of remaining
    unstable/unmixed air across the Red River Valley has a bit broader
    instability axis to work with and thunderstorms are just that bit
    stronger with tops below -70C. 500-1000mb thickness depicts a
    broadening divergence suggesting weakening propagation vectors,
    slowly backing upstream to suggest some back-building may occur
    over the coming hours. This clustering/expansion will increase
    mergers, short-term training across far SE OK/SW AR into far
    northern TX. Slightly higher moisture flux convergence will also
    support rates of 1.75"/hr, occasionally and locally peaking over
    2"/hr. As such spots of 2-4" are becoming more likely. The area
    has not seen the heavier rain over the last week or so, as further
    north, so grounds are a bit more accepting of these higher totals;
    given FFG values of 2-3"/hr or 3-4"/3hrs, suggesting incidents of
    flash flooding will still be more scattered in nature/coverage
    than further north, but a few incidents are still likely (with the
    only exception near Montague to Grayson county, TX).

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!44jtdujgBJ1BR-OWzjRm12Isx_zZyOiDd0-tIodVhFT_r9EPUHV_w59ZlRPmW7XyDPW3= j0Q9impEEnprN8J13F1okbo$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 36099332 35609171 34979117 34089141 33419292=20
    33149393 33009526 33099734 33709764 34529643=20
    35339522 36079432=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 24 08:42:14 2025
    AWUS01 KWNH 240842
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-OKZ000-241415-

    Mesoscale Precipitation Discussion 1129
    NWS Weather Prediction Center College Park MD
    441 AM EDT Wed Sep 24 2025

    Areas affected...Southern AR...Northern LA...Far Western MS...Ext
    Southeast OK...Ext Northeast TX...

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

    Valid 240840Z - 241415Z

    SUMMARY...Strong moisture flux and rates over 2"/hr with
    short-term training poses streaks of 2-4" totals and possible
    incidents of flash flooding through early morning.

    DISCUSSION...Regional RADAR mosaic continues to show stronger
    clusters of thunderstorms extending west to east along older
    convectively reinforced boundaries across central to southern AR
    and into NW MS. Broad southwesterly LLJ continues to flux
    enhanced lower level anomalous moisture to intersect with the
    boundary to maintain isentropic ascent, to tap skinny but still
    unstable profiles with 2000-2500 J/kg of CAPE. The southwesterly
    flux combined with very slow southward drift of the boundary has
    allowed for overall moisture profile to reach 2-2.25" total PWat
    values and raise warm cloud layers a few extra thousand feet,
    increasingly efficient warm cloud rainfall generation, supporting
    rates of 2-2.5"/hr.=20

    GOES-E WV suite shows base of the main core, upper-low continuing
    to advance across the TX Panhandle, this has delayed the
    advancement of the cold front across eastern OK, further allowing
    the length of the isentropic ascent to be long enough to allow for repeating/training for those scattered clusters. LLJ winds are
    expected to increase to 25-30kts but also veer a bit more to
    reduce angle of intersection with the effective isentropic
    boundary toward daybreak and may further reduce overall coverage.
    Still, the deep layer steering flow will be just a bit south of
    due east allowing for short-term training/repeating to remain
    across southern Arkansas and far Northern Louisiana and perhaps
    into far western MS after 12z. Streaks of 2-4" are possible but
    this will also be crossing areas that have been dry for a
    prolonged period and higher FFG values in general.

    NASA SPoRT LIS 0-40cm relative soil moisture values are generally
    below 30% with some as low as 10% in main river valleys. Intense
    rates initially up to 2.5"/hr may not have much time to infiltrate
    and could have above normal run off, so any flash flooding
    incidents are likely to be more widely scattered in nature and
    therefore the risk is considered possible through 14z.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-fBZGZfQ8KmwaZf1e3ZpdkCGVGFkwPwh4oASsTypnjtvIng4Z5YvxODWCTZ66vXGtinp= -ltHPoal8_P6C_DTFXjT89I$ for graphic product...

    ATTN...WFO...JAN...LZK...SHV...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 34589183 34159116 33239042 32699067 32609141=20
    32609301 32999465 33659507 34059491 34409418=20
    34289297=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 24 13:48:47 2025
    AWUS01 KWNH 241348
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-241900-

    Mesoscale Precipitation Discussion 1130
    NWS Weather Prediction Center College Park MD
    948 AM EDT Wed Sep 24 2025

    Areas affected...Eastern Texas through far Western Mississippi

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

    Valid 241347Z - 241900Z

    Summary...Clusters of showers and thunderstorms will continue into
    the afternoon as a cold front approaches from the Northwest. This
    convection will likely have rain rates of 2-3"/hr, which through
    training or repeating could produce 2-4" of rain and instances of
    flash flooding.

    Discussion...The regional radar mosaic this morning shows clusters
    of thunderstorms advancing across portions of Louisiana, Arkansas,
    and eastern Texas. These thunderstorms are developing ahead of a
    cold front analyzed by WPC moving across Texas, with outflow
    boundaries from prior thunderstorms driving additional ascent.
    Synoptically, deep layer ascent is also intensifying across the
    region as a longwave trough digs slowly across Oklahoma driving
    height falls, while a jet streak arcs from the Southern Plains
    into the Appalachians, providing favorable diffluence within the
    RRQ. Additionally, a wave of low pressure moving along the cold
    front is resulting in locally accelerated 850mb winds measured to
    25-35 kts, providing not only enhanced convergence, but driving
    more impressive moisture northeast into the region.

    Thermodynamics remain impressive as well. PWs as measured by GPS
    and morning 12Z U/A soundings are around 2 inches, above the 90th
    percentile from the SPC sounding climatology, which is overlapped
    with MUCAPE as much as 3000 J/kg. The impressive ascent into these
    robust thermodynamics is producing rainfall rates that are
    estimated via local radars to be more than 2.5"/hr, resulting in
    MRMS 1-hr rainfall that has been as high as 2-3" across parts of
    AR.

    As the morning progresses, the slow translation east of the cold
    front and accompanying wave of low pressure into the favorable
    environment should result in an expansion and intensification of
    convection, especially from eastern TX into the ArkLaTex region.
    Although the CAMs differ highly in their evolution and rainfall
    footprint, recent convective development across eastern TX
    suggests that activity will ramp up again, and both the HREF
    neighborhood probabilities and the HRRR 15-min rainfall
    accumulations indicate rates will surge at times to 2-3"/hr,
    locally and briefly up to 4"/hr.

    With 0-6km mean winds aligned to the front, and Corfidi vectors
    becoming increasingly anti-parallel to this mean wind, at least
    short term training is likely the next several hours. Although
    recent rainfall has been modest which is reflected by anomalously
    dry soils according to NASA SPoRT, any significant training of
    these intense rates could result in instances of flash flooding
    the next several hours.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!572e6vx4cbw-JQokAdKt_aOfli4n5MxOU8P-IqRKdBxKoPTfdOp9zBRhBSWovxtJ4UBG= o3Vq8fOUoN2_HrwVI4pCkGo$ for graphic product...

    ATTN...WFO...FWD...HGX...JAN...LZK...MEG...SHV...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 34549143 33539057 32979068 32539137 32119234=20
    31769341 31209480 30829545 30719646 31179695=20
    31879662 32909532 34369316=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 24 17:40:49 2025
    AWUS01 KWNH 241740
    FFGMPD
    MSZ000-LAZ000-TXZ000-242300-

    Mesoscale Precipitation Discussion 1131
    NWS Weather Prediction Center College Park MD
    140 PM EDT Wed Sep 24 2025

    Areas affected...Middle Texas Coast through southern Mississippi

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

    Valid 241739Z - 242300Z

    Summary...Showers and thunderstorms will continue to expand across
    the Central Gulf Coast this aftn. Rainfall rates will likely reach
    2-3+"/hr at times, leading to stripes of 2-4" of rainfall. This
    may cause flash flooding.

    Discussion...The regional radar mosaic early this aftn shows
    rapidly expanding coverage of reflectivity associated with
    increasing showers and thunderstorms from the Middle Texas Coast
    through southern Mississippi. This activity is blossoming
    downstream of a cold front that is slowly dropping southeast,
    driven by an elongated longwave trough axis diving through the
    Southern Plains. This evolution is driving subsequent downstream
    jet streak formation, leading to favorable RRQ diffluence aloft.
    Additionally, spokes of shortwave energy rotating through the
    trough axis are providing additionally focused ascent.

    This widespread deep layer lift is impinging into a destabilizing
    environment reflected by recent SPC RAP analyzed SBCAPE of
    2500-3500 J/kg. This instability is combining with impressive
    moisture (PWs of 2-2.2 inches as measured by GPS) to produce an
    environment ripe for heavy rainfall production. This is being
    realized by the expansion of convection, and recent
    radar-estimated rain rates have peaked above 1.5"/hr, despite
    current cells featuring relatively small updrafts with short
    temporal lifespans (pulse variety convection).

    As the aftn progresses, the high-res guidance is in good agreement
    that thunderstorm coverage will expand across most of the area,
    and recent HRRR runs have shown an increasing trend in coverage.
    This is likely supported by the more favorable overlap of ascent
    into the rich thermodynamic airmass this aftn, as the trough and
    accompanying cold front continue to expand southward.
    Thunderstorms that develop will also be supported by increasing
    bulk shear to help organize into clusters. This should have the
    dual-pronged effect of creating heavier rain rates (HREF
    neighborhood probabilities peak around 40% for 2"/hr coincident
    with 15-min HRRR rainfall as much as 1", or brief 4"/hr rates)
    while also leading to longer duration of this rainfall.
    Additionally, with 850mb inflow remaining out of the Gulf to
    resupply favorable thermodynamics, propagation vectors collapse to
    around 5 kts and veer more to the north, indicating that storms
    will be slower moving and may build south along the TX coast.

    Where clusters of storms move slowest or backbuild/train, these
    intense rainfall rates could produce 2-4" of rain (HREF 6-hr
    rainfall probabilities for 3" above 40%). This will be sufficient
    to produce rapid runoff even atop the relatively dry antecedent
    soils. While the greatest threat for impacts will occur where
    heavy rain falls atop urban areas, any training or repeating of
    these rain rates across this area could result in instances of
    flash flooding into this evening.


    Weiss

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_zRYIjj0FnOKPOPdWsofhDiO5Tk0fu2rbnBSPvxZt-6moVXQLnEfhWe4TkXBjQZbacQj= VgeYiIcPKq64JIi0A94N8rg$ for graphic product...

    ATTN...WFO...HGX...JAN...LCH...LIX...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 33139065 33088902 32388871 31468919 30378971=20
    30008992 29769040 29679116 29749201 29869315=20
    29709382 29489434 29239489 29029541 28909600=20
    29089656 29699573 30179528 30739486 31499392=20
    32729179=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Sep 24 20:25:54 2025
    AWUS01 KWNH 242025
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-250130-

    Mesoscale Precipitation Discussion 1132
    NWS Weather Prediction Center College Park MD
    425 PM EDT Wed Sep 24 2025

    Areas affected...lower to mid-MS Valley into northwestern TN and
    KY

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

    Valid 242023Z - 250130Z

    Summary...At least an isolated flash flood threat will evolve
    through this evening from the lower/middle MS Valley into
    northwestern TN and KY. Hourly rainfall of 1 to 2 inches and
    localized totals of 2 to 4 inches are expected through 01Z.

    Discussion...Radar trends over the past hour have shown an
    increase in the coverage of showers and thunderstorms from
    northeastern AR into southeastern MO and western KY. These storms
    were forming along a quasi-stationary front and just ahead of a
    positively tilted mid to upper-level trough axis located over
    IL/MO into northeastern OK as observed on water vapor imagery.
    Filtered sunshine and anomalous PWAT values of 1.5 to 2.0 inches
    have contributed to MLCAPE of 500 to 1000+ J/kg via 20Z SPC
    mesoanalysis data.

    850 mb winds of 20 to 30 kt were observed across the lower MS
    Valley into northern MS/southwestern TN via VAD wind data, just
    ahead of the base of the mid-level trough. As the trough axis
    advances eastward through the evening, the region of locally
    stronger low level winds are forecast by the RAP to expand
    northeastward into TN/KY, aiding with axes of low level
    convergence (in addition to the surface front and resultant
    outflows). This will occur beneath a divergent pattern aloft
    within the right-entrance region of a 110-130 kt jet at 250 mb
    expanding northeastward from MO/IL. The result should be an
    increase in thunderstorm coverage, especially over the
    lower/middle MS Valley with areas of training from SW to NE.
    Within axes of training, hourly rainfall of 1-2 inches will be
    likely with potential areas of flash flooding from 2 to 4 inches
    of storm total rainfall through 01Z to 02Z. Given somewhat meager
    instability and low level winds into KY/TN, the response is not
    expected to be well organized or widespread with any instances of
    flash flooding most likely remaining isolated to widely scattered.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9P6K1YSV1g-oYcsPKuRKvFlzLvYcIb1lOcX1ZD2dHC2KZTFTB8T6nspZU7uxLQV6Q9Ts= fKocw4fFrIkTggaDdrCiav0$ for graphic product...

    ATTN...WFO...JKL...LMK...LZK...MEG...OHX...PAH...SGF...

    ATTN...RFC...MSR...ORN...TIR...NWC...

    LAT...LON 38178393 37948310 37498279 37148314 36848430=20
    36318687 35898854 35299000 35149152 35749202=20
    36899120 37788852 38108581=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 25 01:30:37 2025
    AWUS01 KWNH 250128
    FFGMPD
    WVZ000-OHZ000-TNZ000-KYZ000-INZ000-ILZ000-MOZ000-250700-

    Mesoscale Precipitation Discussion 1133
    NWS Weather Prediction Center College Park MD
    927 PM EDT Wed Sep 24 2025

    Areas affected...far northwestern TN into most of KY to the OH
    River

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

    Valid 250127Z - 250700Z

    Summary...Localized flash flooding may continue across far
    northwestern TN into most of KY to the OH River through 07Z.
    Periods of training/slow net movement of heavy rain cores will
    support hourly totals of 1 to 2+ inches and possible isolated
    totals of 2 to 4 inches.

    Discussion...Regional radar imagery at 01Z showed scattered
    showers and embedded thunderstorms extending from southeastern MO
    into northwestern TN and western/central KY, near a
    quasi-stationary front which was analyzed near the OH River. A
    number of smaller scale mesovortices were noted within this axis,
    one just west of I-65 in central KY and another over southern KY
    to the southwest of HVC. While overall instability was generally
    weak across the OH Valley, with 00Z soundings from ILN and BNA
    showing less than 250 J/kg MLCAPE, pockets of higher instability
    (though still weak) likely remained over portions of TN/KY. One of
    the bigger drivers in a lingering flash flood threat is the
    anomalous moisture in place with PWAT values between 1.6 and 2.0
    inches (00Z BNA sounding and SPC mesoanalysis), supportive of
    efficient rainfall production with MRMS-derived rates of 1 to 2
    in/hr (locally higher) since 22Z.

    Forcing ahead of a slow moving mid-level trough/low over MO and
    associated shortwave trough will continue to support showers and
    thunderstorms through a good portion of the overnight for the OH
    Valley. As the shortwave spoke over MO advances eastward into the
    OH Valley through 12Z areas of heavy rain will clear from west to
    east. Embedded pockets of heavy rain are expected within lingering
    elevated instability pools and/or near transient mesovortices,
    with lift being augmented through divergence and diffluence aloft
    within the right-entrance region of an upper jet max currently
    over IN/OH. Within axes of training, hourly rainfall will continue
    to peak in the 1 to 2 inch range (locally higher possible) along
    with additional storm totals of 2 to 4 inches through 07Z.
    Localized flash flooding may result, especially if there is
    overlap with urban areas.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7iG0BeSVrc8-e8U2NIiwia8yQ1ZpFR7PuWCUkyHAp5UPY2t8HzoFNl9e48hQO_6Qpx-T= YaSnQxf9400Q2L7JM9sTT8A$ for graphic product...

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

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 39038267 38678217 38078287 37148386 36618525=20
    36298684 36098851 36078929 36418952 37188883=20
    38048683 38848449=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 25 07:17:01 2025
    AWUS01 KWNH 250716
    FFGMPD
    PAZ000-MDZ000-WVZ000-OHZ000-KYZ000-251300-

    Mesoscale Precipitation Discussion 1134
    NWS Weather Prediction Center College Park MD
    316 AM EDT Thu Sep 25 2025

    Areas affected...portions of northern KY/WV...southern
    OH...southwestern PA

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

    Valid 250715Z - 251300Z

    Summary...Localized hourly 1-2" rainfall expected to result in
    additional 2-4" totals, in the vicinity of recent localized 1-3"
    rainfall over the past few hours. Isolated to scattered instances
    of flash flooding are likely.

    Discussion...Showers with embedded thunderstorms have continued in
    the vicinity of a quasi-stationary front draped from southwest to
    northeast across the OH Valley. A deepening (but weak) wave of low
    pressure along the front is approaching an area of recent
    localized training (1-2" estimated hourly totals per MRMS) near
    the far eastern OH/KY border, fueled by a trailing mid- to
    upper-level shortwave/PV anomaly (evident via GOES-East water
    vapor imagery and 500 mb RAP analysis). The leading edge of
    moisture transport situated between 300-305K isentropes (~850 mb
    isobaric surface) is only just moving into the OH/KY/WV border
    region, as the low-level jet nears peak strength at 30-40 kts.
    This suggests that embedded hourly 1-2" totals will likely
    continue for at least the next several hours, training near recent
    1-3" totals in already sensitive hilly to mountainous terrain
    (with 3-hr FFGs, Flash Flood Guidance, generally ranging from only
    1.0-2.0"). Recent hi-res guidance supports the idea of additional
    localized 2-4" totals, suggesting isolated to scattered instances
    of flash flooding are likely.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5Aw_vEfG7FFGaSxd4hr9Wq9tNCJL1Mwli-GymTVjIsxs7osraLU9emLxSXg275LTpFAb= QJ-LnTPJVZrT6mUY1I_cXeA$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...PBZ...RLX...

    ATTN...RFC...TIR...NWC...

    LAT...LON 40898023 39507946 38588062 38038300 38158379=20
    38498393 38778366 39178306 39788228=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 25 13:03:33 2025
    AWUS01 KWNH 251303
    FFGMPD
    PAZ000-WVZ000-OHZ000-251702-

    Mesoscale Precipitation Discussion 1135
    NWS Weather Prediction Center College Park MD
    903 AM EDT Thu Sep 25 2025

    Areas affected...western/central Pennsylvania, far southeastern
    Ohio

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

    Valid 251302Z - 251702Z

    Summary...Deep convection should migrate eastward across western
    and central Pennsylvania this morning, producing areas of 1-2
    inches of rainfall (locally higher). These amounts may cause
    flash flooding especially in populated and sensitive areas.

    Discussion...Deep convection was being maintained across
    southeastern Ohio this morning due to strong forcing for ascent
    aloft with mid-level waves traversing the region. Latest MRMS
    estimated of 1-2 inch/hr rain rates were noted particularly with a
    cluster of cells near Wheeling, WV. These cells were moving
    eastward at an appreciable clip, but were still embedded in just
    enough instability aloft (around 250 J/kg MUCAPE) and abundant
    moisture (1.8 inch PW) to support heavy rainfall. These cells
    should impact the Pittsburgh Metro area over the next couple
    hours, and if rain rates persist as they are currently, at least a
    few instances of flash flooding are possible.

    Over time, convection is expected to continue spreading eastward,
    with multiple rounds of rain rates of at least 0.25-0.5 inch/hr
    expected. Localized areas of hourly rates exceeding 1 inch/hr are
    also possible at times. FFG thresholds are in the 1-1.25 inch/hr
    range and exceedence is likely on at least an isolated basis.=20
    Flash flooding is possible in this regime - particularly in
    low-lying and urbanized areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4hE2zsVbw4s659OivZb8zifpnq8tFG3kLmqkaiCb0qaria4T--OhaUzjYU26t5vMcKW4= 9TCQhHGnBgeEdJsI3evHzAo$ for graphic product...

    ATTN...WFO...CLE...CTP...PBZ...RLX...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 41577859 40907814 39897891 39338143 40858150=20
    41258051=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 28 13:45:29 2025
    AWUS01 KWNH 281345
    FFGMPD
    NMZ000-281700-

    Mesoscale Precipitation Discussion 1149
    NWS Weather Prediction Center College Park MD
    944 AM EDT Sun Sep 28 2025

    Areas affected...southern/central New Mexico

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

    Valid 281344Z - 281700Z

    Summary...Isolated instances of flash flooding are possible this
    morning - especially in sensitive areas/downstream of burn scars.

    Discussion...Scattered convection has persisted across much of the
    discussion area this morning. Recent radar/satellite shows
    additional shower/thunderstorm activity developing across southern
    New Mexico and drifting northeastward. The storms are in a
    favorable pattern for development owing to difluence aloft and an
    upper trough upstream over Arizona. Additionally, a pool of
    moisture over the area (1+ inch PW) will continue to support
    heavier rainfall especially where localized backbuilding can
    materialize. Most of the convection this morning has exhibited <1
    inch/hr rain rates, though localized backbuilding and prolonging
    of heavy rain rates cannot be ruled out in this regime.=20
    Furthermore, the onset of insolation/surface warming should
    readily increase SBCAPE values beyond 1000 J/kg this morning,
    which may result in an uptick in convective coverage through
    17Z/11a MDT.

    Though ongoing convective activity is relatively isolated, storms
    were unfortunately moving toward sensitive ground conditions near
    Ruidoso, NM. These trends are expected to continue this morning,
    prompting an isolated flash flood risk in the most sensitive
    locales. Rain rates may peak at around 1 inch/hr - especially as
    convection increases in coverage and local mergers/backbuilding
    become more common.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-pLeEWgvdRXR3lvxrf_RZ1C0BAwtZAX1gwuGl5Eh7pOXEvaUQdX8J8ZKRrj4DBjNBgeJ= DfvW1H85xU3ooSrFdY9BViA$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...NWC...

    LAT...LON 34440492 33380431 32260459 31850764 32140802=20
    33180738 34220632=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 28 17:06:30 2025
    AWUS01 KWNH 281706
    FFGMPD
    NMZ000-AZZ000-UTZ000-NVZ000-CAZ000-282305-

    Mesoscale Precipitation Discussion 1150
    NWS Weather Prediction Center College Park MD
    105 PM EDT Sun Sep 28 2025

    Areas affected...Eastern CA...Southern NV...Far Southern
    UT...Northern and Western AZ

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

    Valid 281705Z - 282305Z

    SUMMARY...Locally heavy showers and thunderstorms will be
    developing and expanding in coverage going through the early to
    mid-afternoon hours. High rainfall rates and slow cell-motions may
    result in isolated to scattered areas of flash flooding by
    mid-afternoon.

    DISCUSSION...A mid to upper-level low is gradually beginning to
    lift off to the northeast across northwest AZ, and this energy
    coupled with daytime heating/increasing instability and
    orographics/upslope flow near areas of higher terrain will drive
    the development and expansion of locally heavy showers and
    thunderstorms going through the mid-afternoon hours.

    SBCAPE values are on the order of 1000 to 1500 J/kg southwest of
    the Mogollon Rim and to the south of the low center. However,
    visible satellite imagery shows strong diurnal heating taking
    place across these areas which will support a notable increase in
    instability over the next several hours. The strongest forcing
    associated with the low center and broader upper trough axis
    should be generally across areas of central and northern AZ going
    into the afternoon, and this is generally where the heaviest
    rainfall threat will tend to be from developing and expanding
    areas of convection. Proximity of the Mogollon Rim will further
    support a terrain-induced element to the convective threat.

    Scattered areas of convection will also be likely to develop up
    across far southern UT, southern NV and portions of eastern CA as
    differential heating boundaries become established and focus
    smaller scale forcing/focus for convective initiation. In fact,
    there is evidence of an MCV over southern NV which may foster a
    concern for locally more concentrated convection.

    PWs are anomalously high across northwest AZ and especially
    southern UT, southern NV and eastern CA where the anomalies are
    locally 2 to 2.5 standard deviations above normal. This will
    support convective cells with greater rainfall efficiency and thus
    elevated rainfall rates.

    Rainfall rates will should be capable of reaching up to 1.5
    inches/hour with the stronger cells. Locally slow cell-motions
    with some concerns for terrain-anchored cells will facilitate the
    potential for some spotty 2 to 3+ inch rainfall totals. This may
    cause isolated to scattered areas of flash flooding which will
    include potential impacts to the area burn scar locations, slot
    canyons and arroyos.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8ErEAtlv0HYY17FTtPmEISsl5Jo4iq-iw6i8YScdnenXkZpH9JDmY0ji3LsNfBD81MZ-= zRbv5Nyr07voACSXIzaulqM$ for graphic product...

    ATTN...WFO...ABQ...FGZ...GJT...PSR...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 37951141 37510970 36810894 35840904 35210969=20
    34501040 33041225 33031402 33661475 34261528=20
    34761586 35581634 36321635 36691611 37221524=20
    37861332=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 28 17:46:02 2025
    AWUS01 KWNH 281745
    FFGMPD
    TXZ000-NMZ000-AZZ000-282345-

    Mesoscale Precipitation Discussion 1151
    NWS Weather Prediction Center College Park MD
    145 PM EDT Sun Sep 28 2025

    Areas affected...Central and Southern NM...Southwest TX

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

    Valid 281745Z - 282345Z

    SUMMARY...Increasing coverage of showers and thunderstorms is
    expected going through the afternoon and evening hours. Heavy
    rainfall rates are likely to result in scattered areas of flash
    flooding which may impact sensitive burn scar and dry wash
    locations.

    DISCUSSION...Midday GOES-E Visible and Day Cloud Phase RGB
    satellite imagery shows an increasingly agitated CU/TCU field over
    southern NM and southwest TX as stronger diurnal heating and an
    increase in boundary layer instability ensues. MLCAPE values have
    risen to 500 to 1000 K/kg across these areas, and additional
    destabilization is expected over the next few hours which will
    help set the stage for renewed areas of convective initiation.

    Already there has been a corridor of showers and thunderstorms
    that progressed through areas of southern NM in response to a lead
    shortwave impulse which is advancing quickly off to the northeast.
    However, in its wake, the flow aloft remains quite diffluent given
    the upstream approach of the broader upper trough over the
    Southwest U.S. The approach of these height falls along with a
    belt of stronger mid-level southwest flow and resulting shear
    should favor the development and expansion of relatively organized
    convective cells going through the afternoon hours.

    Effective bulk shear values are on the order of 30 to 40 kts which
    combined with MLCAPE values eventually reaching 1500+ J/kg should
    yield scattered multicell convection. The PW anomalies across the
    region are somewhat moist with values of 1.5+ standard deviations
    above normal. This will tend top support heavier rainfall rates
    with these more organized convective cells that could reach 1 to 2
    inches/hour.

    The more orographically favored higher terrain, including the
    Sacramento Mountains in south-central NM and the Davis Mountains
    of southwest TX are expected to be the locations that generally
    see the heaviest rainfall potential going through this evening.
    Some spotty totals across these areas may reach 2 to 4+ inches
    which is supported by some of the 12Z hires model guidance.

    Adjacent areas farther west across central to southwest NM will
    also see at least locally heavy totals from potentially more
    discrete pockets of convection away the terrain.

    Scattered areas of flash flooding will become likely in time due
    to the development and expansion of convection with these higher
    rainfall rates. The more sensitive burn scar locations (including
    the Blue 2, South Fork, Salt and McBride burn scar complex) and
    normally dry washes will be at greatest risk for impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7xelRpfMJtMEPIBSB9JA6mk_6F9bBX5JDjogUrwu3R4eyi1r2sWxZMLiBMZtdlHlkc3a= NgD4vO8qDuLUrsdVn89zbr0$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...TWC...

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 35450645 35030492 34370407 33340346 31650325=20
    30600342 29960395 29980476 31020587 31480683=20
    31420774 31250838 31370885 32320907 34370859=20
    35260777=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 28 22:56:36 2025
    AWUS01 KWNH 282256
    FFGMPD
    TXZ000-NMZ000-290455-

    Mesoscale Precipitation Discussion 1152
    NWS Weather Prediction Center College Park MD
    655 PM EDT Sun Sep 28 2025

    Areas affected...Central and Southern NM...Southwest TX

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

    Valid 282255Z - 290455Z

    SUMMARY...Clusters of heavy showers and thunderstorms will persist
    through the evening, bringing a likelihood of additional scattered
    flash flooding, particularly impacting burn scar areas and arroyos.

    DISCUSSION...Late-afternoon GOES-E IR satellite imagery shows
    cold-topped convective clusters affecting many areas of central
    and southern New Mexico, with the most concentrated and coldest
    cloud top temperatures focused over southwest Texas in the last
    couple of hours.

    Strong upper-level divergence continues over the region as an
    upstream upper-level trough approaches from the west. This deeper
    layer forcing and ascent continue to interact favorably with a
    moderately unstable airmass, sustaining the convection. In fact,
    the latest RAP analysis indicates MLCAPE values of 1000 to 1500+
    J/kg extending from southwest Texas northward across central New
    Mexico. Concurrently, effective bulk shear values reaching 30 to
    40 knots are contributing to locally well-organized convective
    cells with strong updrafts and heavy rainfall rates.

    Sufficient dynamical forcing and diurnally enhanced instability
    will continue into the evening, maintaining convective clusters
    across the region with localized heavy rainfall. Supporting this
    will also be corridors of stronger low-level moisture convergence
    which over the last couple of hours have been rather notable
    across southwest Texas and into far southern New Mexico.

    PW values remain generally 1.5+ standard deviations above normal.
    Given these environmental conditions, rainfall rates with stronger
    convective cells are likely to continue reaching 1 to 2
    inches/hour. The latest high-resolution CAMs suggest additional
    localized rainfall totals of 2 to 4+ inches through late this
    evening where some cell-merger and terrain-anchored convection
    materializes.

    These additional rains are expected to cause further scattered
    flash flooding throughout the evening. Normally dry washes and
    arroyos, as well as burn scar locations, will remain particularly
    vulnerable to flash flooding impacts over the next several hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!80FISsy1HC6iJi4VgvFYaDVf84S-OPSaSiuL7dSbLws1D55ZljEYSRH6-dGYuZ7TsEEE= yJZ8FivTYyinzpi6-yYwDQg$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 36170513 35400449 33510435 32150431 31230400=20
    30360370 29960395 29900470 30540549 30820584=20
    31440642 32380699 33130776 34010801 35210770=20
    36050661=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Sep 29 04:12:41 2025
    AWUS01 KWNH 290412
    FFGMPD
    NMZ000-290800-

    Mesoscale Precipitation Discussion 1153
    NWS Weather Prediction Center College Park MD
    1211 AM EDT Mon Sep 29 2025

    Areas affected...west-central NM

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

    Valid 290400Z - 290800Z

    Summary...Localized heavy rainfall (1"+/hr rates with as much as
    1" in 15-min) will support an isolated flash flood risk through
    the early overnight.

    Discussion...Convection is persisting into the late evening across
    portions of west-central NM, just downstream of a strong PV
    (potential vorticity) maxima (400-250 mb). As the low-level jet
    strengthens modestly over the next several hours with the diurnal
    cycle, updrafts may persist as precipitable water values remain
    elevated (~1.0", near climatological max levels per ABQ sounding
    climatology) supporting localized rainfall rates of 1"+ (with as
    much as 1" in 15-min, per MRMS estimates).

    New hi-res guidance (00z HREF) supports continued localized heavy
    rainfall (1"+/hr) for at least a couple more hours, though latest
    observational trends may support at least isolated convection
    continuing through about 09z (with a pool of MLCAPE of 250-750
    J/kg over the MPD area likely taking some time still to diminish).
    40-km HREF 2" exceedance probabilities are as high as 20% through
    09z, suggesting localized/isolated instances of flash flooding
    will remain possible.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6Dz7dDKykBox-GVCYrMX2qoIu1TENmbUsOy_f7qnVZATA3lJwPEAFhbjzt5vUycP-3ZA= -hCxAKGB9sZlzJyPDKCfzTc$ for graphic product...

    ATTN...WFO...ABQ...EPZ...

    ATTN...RFC...FWR...NWC...

    LAT...LON 35910610 35320570 34630610 33980616 33440662=20
    33500746 34440754 34960773 35490777 35760752=20
    35900678=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 25 18:56:38 2025
    AWUS01 KWNH 251856
    FFGMPD
    MEZ000-MAZ000-NHZ000-RIZ000-VTZ000-CTZ000-NYZ000-NJZ000-PAZ000-260050-

    Mesoscale Precipitation Discussion 1136
    NWS Weather Prediction Center College Park MD
    255 PM EDT Thu Sep 25 2025

    Areas affected...northern Mid-Atlantic into southern New England

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

    Valid 251854Z - 260050Z

    Summary...Training axes of heavy rain are expected from the
    northern Mid-Atlantic region into southern New England through the
    late afternoon and evening. Hourly rainfall of 1 to 2+ inches may
    result in localized flash flooding with a focus on any urban
    centers.

    Discussion...Radar imagery at 1845Z helped identify a pair of MCVs
    over the Northeast, embedded within areas of largely stratiform
    rain from portions of PA into New England. One vortex over central
    PA and the other near Albany, NY, were tied to surges of higher
    rainfall rates, with MRMS-derived values between 1 and 2 inches in
    an hour at times. These two features were located along the
    northern edges of a region of elevated CAPE with 500-1500 MUCAPE
    identified on 18Z SPC mesoanalysis data. The environment was
    characterized by anomalous moisture with PW values of roughly 1.7
    to 2.0 inches (2 to 3 standardized anomalies above the mean for
    late September), supportive of hourly rainfall locally in excess
    of 2 inches.

    As a cold front over central NY/PA and the aforementioned
    mesoscale waves continue to advance downstream, interaction with
    500-1000 J/kg MLCAPE from southeastern PA into far southern New
    England will support an increase in rainfall coverage and rates
    from the northern Mid-Atlantic into southern New England. Some
    breaks in cloud cover noted on visible imagery over southeastern
    PA into NJ may help to locally increase instability through better
    surface heating, yielding greater potential for higher intensity
    rainfall. While individual cell motions should remain progressive
    toward the NE, alignment of convective axes with the southwesterly
    deep-layered steering flow will promote training and locally 1 to
    2+ inches of rain in an hour at times. These locally higher rates
    could result in a relatively quick accumulation of rainfall
    totaling 2 to 3+ inches through 01Z. Localized flash flooding may
    occur as a result, especially if overlap occurs with impervious
    urban areas.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7qyxmCwKpVstv3jN3fWwdyMQipUMRXzIhAqbmAEL2oR2LO2905s5-kjeFo6cNeEXp8M6= 6v4dkwIDL3tkbvHKIqKkVYQ$ for graphic product...

    ATTN...WFO...ALY...BGM...BOX...BTV...CTP...GYX...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 44247137 43667053 43137030 42647034 42237087=20
    41847183 41297270 40817343 40227422 39927557=20
    39917773 40897709 42027600 42747491 43117379=20
    43807248=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 25 19:42:09 2025
    AWUS01 KWNH 251942
    FFGMPD
    NMZ000-AZZ000-260130-

    Mesoscale Precipitation Discussion 1137
    NWS Weather Prediction Center College Park MD
    340 PM EDT Thu Sep 25 2025

    Areas affected...central to southeastern AZ into southwestern NM

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

    Valid 251939Z - 260130Z

    Summary...Scattered thunderstorms are expected to result in a few
    areas of flash flooding from central and southeastern AZ into
    southwestern NM through early evening. Rainfall rates of 1-2 in/hr
    will be likely within the stronger cores.

    Discussion...Visible satellite and area radar imagery showed the
    rapid development of thunderstorms over north-central to
    southeastern AZ over the past hour. The storms overlapped within
    an anomalous low to mid-level moisture axis seen on LPW imagery,
    located east of a dry tongue which existed over southern CA into
    southern NV. Favorable surface heating beneath mostly clear skies
    and the anomalous PW axis (+1 to +2 standardized anomalies) have
    led to 500-1500 J/kg MLCAPE via 19Z SPC mesoanalysis data (~1100
    J/kg via 18Z TUS sounding) over a large portion of the MPD area.

    Steering flow varied across the region but was oriented from the
    SSW to W and was stronger across northern regions compared to
    locations closer to the Mexican border. Mid-level height falls and
    upper level left-exit region jet max divergence, at the nose of a
    zonally oriented jet streak moving into northern Baja California,
    should aid in lift across the region later this afternoon. The
    environment will support scattered thunderstorms increasing
    through the evening with brief training and outflow interactions
    as storm coverage increases. 1 to 2 inches of rain in an hour (or
    less) should be found within the stronger thunderstorm cores that
    develop and is expected to result in at least isolated flash
    flooding into the early evening.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6oje_8QJMjjKuArnunfaQn1FApIpa7M3iTh5gDWrUxTJgXgoaqCgwwYgFIHmazke7Q4g= mTqL1XAh1CmatsvDW4Cto_Y$ for graphic product...

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

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 35441210 35141068 34260919 33150779 32580722=20
    31660702 31120790 31090952 31261079 31661115=20
    32671115 33991164 35131245=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Sep 25 20:25:38 2025
    AWUS01 KWNH 252025
    FFGMPD
    NVZ000-CAZ000-260215-

    Mesoscale Precipitation Discussion 1138
    NWS Weather Prediction Center College Park MD
    424 PM EDT Thu Sep 25 2025

    Areas affected...Sierra Nevada into portions of central NV

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

    Valid 252023Z - 260215Z

    SUMMARY...Intense heavy rain cores are expected to result in at
    least isolated flash flooding into the afternoon and early evening
    hours from the Sierra Nevada into portions of central NV. Hourly
    rainfall of 1 to 2 inches is expected but with sub-hourly totals
    of 0.5 to 1.0 inches in 15-30 minutes.

    DISCUSSION...GOES West visible satellite imagery and ENTLN
    lightning data showed a few widely scattered thunderstorms from
    the Sierra Nevada into portions of south-central NV. The storms
    were located to the north and east of the 700 mb reflection of a
    mid-level low over CA, with highly anomalous moisture (2 to 3+
    standardize PW anomalies) extending from the low center into much
    of NV. VAD wind data at 700 mb and RAP guidance showed 20-30 kt
    wind speeds at 700 mb over the lower CO River Valley into southern
    NV but weakening to ~10 kt over central and western NV (some
    degree of speed convergence).

    Deeper layer mean wind speeds were weak (<10 kt) under and north
    of the mid-level low which will result in slow cell motions.
    Placement of the mid-level low to the west of the Sierra Nevada
    and southerly flow to its east, aligned with the orientation of
    the Sierra Nevada range will likely result in some repeating
    rounds of thunderstorms across the higher terrain where 500-1000
    J/kg of instability is forecast to expand by later this afternoon.
    Farther to the east, from western to central NV, favorable
    unidirectional southerly flow will increase the potential for
    training and brief backbuilding of cells where locally stronger
    low level flow exists. Due to the anomalous moisture in place,
    both areas of CA and NV will have the potential for high rainfall
    rates, hourly totals of 1 to 2 inches and 0.5 to 1.0 inches in
    15-30 minutes, which should result in at least isolated areas of
    flash flooding into the evening hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_nZGtwH_GXyul5EIDi8z1LU22llk81oAmhDmVrjBphJ_-ppZR8Z6Gytx8F2BTSt-WyXv= EPAlC_RBSuEqhOHi3m7piPQ$ for graphic product...

    ATTN...WFO...HNX...LKN...REV...STO...VEF...

    ATTN...RFC...RSA...NWC...

    LAT...LON 39871830 39761745 39141638 37841613 37041697=20
    36121781 35801851 35881877 36341898 36751920=20
    37171968 37512003 37962031 38332050 38912031=20
    39431975 39761896=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 26 16:04:23 2025
    AWUS01 KWNH 261604
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-262130-

    Mesoscale Precipitation Discussion 1139
    NWS Weather Prediction Center College Park MD
    1203 PM EDT Fri Sep 26 2025

    Areas affected...Far Southeast NV...Northwest to Central AZ

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

    Valid 261603Z - 262130Z

    SUMMARY...Increasing coverage of heavy showers and thunderstorms
    can be expected over the next few hours. Slow cell-motions and
    localized backbuilding of convective cells will promote sufficient
    rainfall concerns for isolated to scattered areas of flash
    flooding to be possible going through mid-afternoon.

    DISCUSSION...The latest GOES-W IR/WV suite shows a compact and
    relatively strong mid to upper-level low center dropping
    east-southeastward down across southeast CA. Left-exit region jet
    dynamics pivoting up across central to northwest AZ around the
    eastern flank of this closed low is already interacting with a
    nose of moderate instability pooling around the southwest-facing
    slopes of the Mogollon Rim and adjacent areas of central AZ. The
    result over the last couple of hours has been a corridor of
    cooling convective tops, with radar data showing pockets of
    backbuilding convective cells near and over top of the higher
    terrain.

    SBCAPE values are locally on the order of 1000 to 2000 J/kg, and
    additional boundary layer destabilization via solar insolation
    over the next few hours will contribute to an additional uptick in
    convective coverage with showers and thunderstorms becoming a bit
    more focused over the Mogollon Rim and adjacent areas just to the
    south over central AZ. A well established corridor of strong
    850/700 mb moisture flux anomalies are aligned with the deeper
    layer south-southwest flow riding up across southern and central
    AZ to the east of the closed low center, with these anomalies
    reaching 2 to 3 standard deviations above normal. This will
    facilitate the expansion of convection along with a favorable
    regime for backbuilding cells.

    Farther off to the northwest across northwest AZ and adjacent
    areas of far southeast NV, convection will be developing here over
    the next few hours as a mid-level deformation zone north of the
    closed low becomes better established. A destabilizing boundary
    layer coupled with terrain-influenced circulations will help
    further support convective development.

    Rainfall rates with the convection across the region will be
    capable of reaching 1 to 1.5 inches/hour with the stronger cells,
    and with slow cell-motions and some backbuilding cells, there may
    be some storm totals through mid-afternoon that region 2 to 2.5
    inches. This is consistent with the latest 12Z HREF guidance.

    Given the setup, isolated to scattered areas of flash flooding
    will be possible, and this threat is expected to continue
    throughout much of the day. Additional MPDs will be issued
    accordingly.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-DbPkAA0-R7L4BdeFk7FxNiGA5fR2J9USSaEG5r6qM0kzQ9t5yJ7n9cbhrEPBD3-VyZ3= nKcv1yFZLaWba0vs0qqLKOs$ for graphic product...

    ATTN...WFO...FGZ...PSR...SLC...TWC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 37241454 37071344 36491210 35751003 34670911=20
    33730917 33100985 32991121 33431260 34501353=20
    34901453 35621545 36331577 36971536=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 26 18:47:26 2025
    AWUS01 KWNH 261847
    FFGMPD
    NMZ000-AZZ000-270045-

    Mesoscale Precipitation Discussion 1140
    NWS Weather Prediction Center College Park MD
    245 PM EDT Fri Sep 26 2025

    Areas affected...Central to Southeast AZ...Southwest NM

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

    Valid 261845Z - 270045Z

    SUMMARY...Expanding clusters of heavy showers and thunderstorms
    this afternoon will likely drive scattered to numerous areas of
    flash flooding. Locally significant and life-threatening impacts
    will be possible.

    DISCUSSION...The latest GOES-W visible satellite imagery along
    with radar data shows expanding clusters of heavy showers and
    thunderstorms across central AZ to the southwest of the Mogollon
    Rim and to the north of Phoenix, with additional areas of
    convection also seen developing off to the east and southeast
    across southeast AZ. All of this convection is developing and
    expanding in coverage in response to the arrival of a compact
    closed low over southeast CA which is allowing for notably
    divergent flow aloft downstream across central and southern AZ
    while also interacting with a strongly unstable and moist boundary
    layer.

    MLCAPE values are on the order of 1500 to 2500 J/kg with 850/700mb
    moisture flux anomalies of 2 to 3 standard deviations above normal
    across the region ahead of the approaching height falls. As
    additional boundary layer heating ensues across the region, there
    will likely be additional expansion of convection which is
    expected to become locally quite concentrated across portions of
    central to southeast AZ. In time this afternoon, convection is
    also expected to develop farther off to the east into areas of
    southwest NM, which will have the aid of orographic ascent and
    differential heating boundaries to support convective development.

    Rainfall rates will be capable of reaching 1 to 2 inches/hour with
    the stronger storms, and the environment is highly conducive for
    pockets of slow-moving cells and backbuilding convection. This may
    support some rainfall totals reaching 2 to 4 inches by late this
    afternoon. This is generally supported by the latest HREF/REFS
    guidance suites.

    Given the coverage and intensity of the convection that is
    expected to unfold this afternoon, scattered to numerous areas of
    flash flooding are expected. This will include concerns for
    enhanced dry wash/arroyo flash flooding along with potential for
    areal burn scar impacts. Urban flash flooding will also be a
    possibility including locations such as Phoenix, Tuscon and
    Safford. Thus, locally significant and life-threatening impacts
    will be possible where these heavier rains materialize over the
    next several hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6ZnUcNqjMcMtxd7B7uzBHV7R59cx426Q6EmeUoLpra_febM6hg8lxqJq-jhapBGmxJwk= H6m270gD4kLpom0IjSTkYpQ$ for graphic product...

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

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 35021202 34541068 34470938 34600731 33260674=20
    31730756 31150855 31020977 31131108 31611178=20
    32301208 33061239 34221308 34871279=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Sep 26 21:31:59 2025
    AWUS01 KWNH 262131
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-270330-

    Mesoscale Precipitation Discussion 1141
    NWS Weather Prediction Center College Park MD
    530 PM EDT Fri Sep 26 2025

    Areas affected...Eastern CA...Southeast NV...Southwest
    UT...Northwest AZ

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

    Valid 262130Z - 270330Z

    SUMMARY...Heavy showers and thunderstorms will be a threat going
    into the evening hours across portions of eastern CA, southeast
    NV, southwest UT and northwest AZ. Additional isolated to
    scattered areas of flash flooding will be possible.

    DISCUSSION...The latest GOES-W IR satellite imagery shows
    cold-topped convective clusters impacting northwest AZ along with
    southwest UT. Radar imagery shows this activity gradually
    beginning to cyclonically advance westward into portions of far
    southern NV and with some cells attempting to develop over far
    eastern CA. The convection across this region is largely focused
    within a well-defined mid-level deformation zone situated north of
    a closed mid to upper-level low center across eastern CA.

    A corridor of focused moisture convergence is seen wrapping up
    around the eastern and northern flanks of the closed low, and
    there is an axis of MLCAPE values reaching 500 to 1000 J/kg nosing
    up through northwest AZ and into far southeast NV. This coupled
    with deep layer ascent/forcing north of the closed low should help
    maintain a threat for convection going into the evening hours.
    Overall, far northwest AZ should tend to see the greatest threat
    over the next few hours, but areas of southern NV and eastern CA
    will likely see more development of showers and thunderstorms
    given close proximity of the closed low. This is consistent with
    the latest runs of the experimental WoFS guidance.

    The moisture environment is relatively moist with PW anomalies of
    1 to 2 standard deviations above normal. This coupled with the
    larger scale ascent and instability should maintain convective
    cells capable of producing rainfall rates of 1 to 1.5 inches/hour.
    Additional rainfall totals locally of up to 2 inches will be
    possible by late this evening where some of these cells tend to be
    slow-moving or anchored near terrain.

    Additional isolated to scattered areas of flash flooding will be
    possible as a result going through this evening. This will include
    potential impacts to any burn scar locations along with the
    normally sensitive slot canyons and dry washes.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6A3ai2NIo4VpwyFwvySxD1vFN7nCkXNx8SpimzhhlzabtE4BIOz_C1KTNaaP9Dhprq2i= tLqM40gfidN9QyRZN_GFx2Q$ for graphic product...

    ATTN...WFO...FGZ...PSR...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 37911254 37681175 36991175 36001260 35181288=20
    34451317 33511359 33171437 33251529 33811597=20
    34971616 35791604 36511573 37231505 37741396=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 26 23:48:29 2025
    AWUS01 KWNH 262348
    FFGMPD
    VAZ000-NCZ000-TNZ000-270545-

    Mesoscale Precipitation Discussion 1142
    NWS Weather Prediction Center College Park MD
    747 PM EDT Fri Sep 26 2025

    Areas affected...Western NC...Southwest to South-Central VA

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

    Valid 262347Z - 270545Z

    SUMMARY...Slow-moving showers and thunderstorms may become a bit
    more focused going into the overnight hours. High rainfall rates
    and slow cell-motions may result in isolated to scattered areas of
    flash flooding.

    DISCUSSION...An upper-level trough gradually advancing into the
    Southeast U.S. will be interacting with a moist and unstable
    airmass this evening pooling up along a quasi-stationary front
    situated across the eastern slopes of the southern Appalachians
    and southern portions of the Mid-Atlantic region. Surface
    observations show a wave of low pressure developing along this
    boundary over southwest NC which is gradually lifting off to the
    northeast.

    This surface wave is being facilitated by the gradual
    amplification of height falls across the region which is promoting
    a southwest to northeast axis of right-entrance region upper jet
    dynamics and related deep layer ascent. MLCAPE values of 500 to
    1000 J/kg are pooled ahead of this wave along the front across
    western NC and some uptick in low-level moisture convergence into
    the boundary is expected over the next several hours.

    An increase in the concentration of convection along the front is
    expected across western NC and eventually parts of southwest to
    south-central VA going into the overnight hours as stronger upper
    jet forcing and strengthening frontogenesis takes place. The
    pooling of moisture and at least modest instability will be
    maintained as well, and some of the convection will be capable of
    producing high rainfall rates of 1 to 2 inches/hour.

    The higher rates will be supported by a gradual increase in PWs
    which are already near 1.5 inches, and with increasing potential
    for warm rain processes to take place going into the overnight
    hours. Moderate effective bulk shear of 30 to 40 kts will also
    promote at least some loosely organized convective cells in close
    proximity to the front which will further support elevated
    rainfall rates.

    Hires model CAMs going through 06Z/2AM EDT suggest rainfall totals
    of as much as 2 to 4+ inches at least locally. This may support
    isolated to scattered areas of flash flooding, and especially
    across portions of northwest NC into southwest VA where antecedent
    conditions are relatively moist.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!90yAwvX8v-WxaAj_C9qZbPnkJLnBAfhujoJAb7j5KfiJ5UvQkRcyMaZ4cCycFfxsHg8N= Nda4MXSitxhU-0zc5cUhogs$ for graphic product...

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

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 37407935 37367865 36957807 36447834 35917948=20
    35538017 35308069 35298131 35588190 36138199=20
    36898105 37308008=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 27 00:32:30 2025
    AWUS01 KWNH 270032
    FFGMPD
    NMZ000-AZZ000-270630-

    Mesoscale Precipitation Discussion 1143
    NWS Weather Prediction Center College Park MD
    830 PM EDT Fri Sep 26 2025

    Areas affected...Central to Southeast AZ

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

    Valid 270030Z - 270630Z

    SUMMARY...Clusters of heavy showers and thunderstorms will persist
    into the evening hours across central to southeast AZ. Additional
    areas of flash flooding will be likely with locally considerable
    and life-threatening impacts still possible.

    DISCUSSION...The latest GOES-W IR satellite imagery shows clusters
    of cold-topped convection continuing to develop and locally
    persist across areas of central to southeast AZ. Some of the
    strongest convection and heaviest rainfall rates are currently
    over portions of Pinal and Gila Counties. This is also where some
    of the strongest low-level moisture convergence and pooling of
    instability remains in place.

    MLCAPE values of 1000 to 1500 J/kg are noted in general across
    south-central AZ, and this coupled with larger scale
    ascent/forcing associated with the slow approach of an upstream
    closed low over eastern CA should continue to favor convection
    with high rainfall rates at least for the next few hours.

    Gradually there will be an increase in boundary layer CIN as the
    evening progresses which will allow for the convective footprint
    to begin to wane, but with elevated effective bulk shear of 30 to
    40 kts across central to southeast AZ, there may be some
    persistence of loosely organized convection through much of the
    evening time frame.

    Rainfall rates will still be capable of reaching 1 to 2
    inches/hour based on the latest cloud top cooling trends over
    Pinal and Gila Counties, and the experimental WoFS guidance
    supports this for at least a couple more hours.

    Some additional spotty totals may reach 2 to 3 inches where any of
    the stronger cells continue to backbuild or train over the same
    area. This will likely foster some additional areas of flash
    flooding for the evening hours. Once again, there will be concerns
    for enhanced dry wash/arroyo flash flooding along with potential
    for localized burn scar impacts and urban flash flooding where
    these heavier rains evolve. Thus, locally considerable and
    life-threatening impacts will still be possible for at least a few
    more hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4m7wuMKk98wpo0VQFaL3CKxKu7EsAOZQy19fm31h8dXEqp9ERppsD0smd1BP5N1ZoMJx= wIiW4mM7n7aDKTloTVIR0_4$ for graphic product...

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

    ATTN...RFC...STR...NWC...

    LAT...LON 34561110 34441041 33840945 32840904 31770912=20
    31230956 31181081 31571162 32221201 32991225=20
    33671232 34401195=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 27 05:57:12 2025
    AWUS01 KWNH 270556
    FFGMPD
    VAZ000-NCZ000-WVZ000-271200-

    Mesoscale Precipitation Discussion 1144
    NWS Weather Prediction Center College Park MD
    156 AM EDT Sat Sep 27 2025

    Areas affected...much of southern and central VA...portions of
    northwestern NC and southeastern WV

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

    Valid 270600Z - 271200Z

    Summary...Training banded heavy rain with 1-2"/hr rates expected
    to result in additional rainfall totals of 3-5" through 8 AM.
    Isolated to scattered instances of flash flooding are likely.

    Discussion...Disorganized showers and thunderstorms across
    southern portions of the Mid-Atlantic have consolidated into a
    defined band of heavy rainfall over the past couple of hours. This
    band extends a couple hundred miles across southern VA into
    northwestern NC, paralleling a surface/low-level frontal boundary
    and associated moisture gradient (PWs ranging from 1.5-2.0" across
    the gradient, nearing the climatological max moving average at
    GSO/RNK). MUCAPE of 500-1000 J/kg is sufficient to sustain deep
    convection, and strong upper-level dynamics (right-entrance region
    of a jet streak with DPVA via shortwave trough/PV anomaly
    upstream) along with modest easterly low-level moisture transport
    could allow for localized training of 1-2"/hr rainfall rates.

    While hi-res models overall have poorly handled the convective
    organization since 00z, the latest HREF suite still indicates
    relatively high odds (20-40%) for localized 3" exceedance through
    12z (per 40-km neighborhood exceedance probabilities). Given that
    banded heavy rainfall has already reached a level of organization
    beyond model depictions, these probabilities could be underdone.
    Expect that training of banded heavy rainfall lead to additional
    rainfall totals of 3-5" with corresponding 3-6 hour Flash Flood
    Guidance (FFGs) generally ranging from 1.5-3.0" (with portions of
    northwestern NC having already received localized totals of 2-3"
    from prior rainfall over the past 3-6 hours). Isolated to
    scattered instances of flash flooding are likely.

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-NEApKCJ4uPZO6DNJvFdxLGh9mWJaAOPtC9jNS0cpZKIgR3AfLtk4rCXduNNT3xAGa0P= jlzh2eNDBfDORe_QvkbnLnY$ for graphic product...

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

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 38038048 37947951 37637883 37567808 37377714=20
    37147680 36607710 36637809 36697890 36297952=20
    35957992 35768021 35708054 35798087 35998103=20
    36448113 36898090 37378079=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 27 15:29:11 2025
    AWUS01 KWNH 271529
    FFGMPD
    VAZ000-NCZ000-272127-

    Mesoscale Precipitation Discussion 1145
    NWS Weather Prediction Center College Park MD
    1128 AM EDT Sat Sep 27 2025

    Areas affected...southeastern Virginia, far northern North
    Carolina

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

    Valid 271527Z - 272127Z

    Summary...Mesoscale evolution of convective cells with
    supercellular characteristics should continue to prompt areas of
    2-3 inch/hr rain rates. Any localized backbuilding or training
    could promote locally significant flash flooding - especially in
    urbanized and sensitive locales.

    Discussion...A couple of supercellular structures were noted near
    Emporia, VA and Roanoke Rapids, NC over the past hour. Because of
    the rotational and supercellular character of these cells, slower
    and rightward-moving storm motions have enabled spots of 2-3.5
    inch/hr rain rates to develop. These cells were migrating
    northeastward parallel to a subtle confluence/baroclinic zone
    extending from Emporia to KW75/Saluda, VA. Localized vorticity
    ingest processes were likely promoting the supercellular
    development and maximizing rain rates locally.

    Southwesterly steering flow aloft should allow for convection to
    continue drifting northeastward and interacting favorably with the aforementioned confluence zone. This, along with 2 inch PW and
    1000-1500 J/kg SBCAPE on the warm side of the confluence should
    continue to support local 2-3.5 inch/hr rain rates through the
    Wakefield and Williamsburg areas. Furthermore, any backbuilding
    along the confluence axis could prolong rain rates and lead to a
    locally significant flash flood threat - especially in any urban
    or flash flood-prone areas. The mesoscale details supporting this
    risk should persist for at least a few hours, and perhaps through
    21Z/5p EDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9XffrvnDjU2arCQ_v_74REcog2S76BiHViToFBlEApskYCUn4wypKkrBUgoFVDsbFqct= 8oZCu02aOdVxzTPoYV3TEDM$ for graphic product...

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

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37857609 37137581 36367669 36007826 36647829=20
    37227789 37807691=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 27 15:31:41 2025
    AWUS01 KWNH 271531
    FFGMPD
    VAZ000-NCZ000-272127-

    Mesoscale Precipitation Discussion 1145
    NWS Weather Prediction Center College Park MD
    1130 AM EDT Sat Sep 27 2025

    Areas affected...southeastern Virginia, far northern North
    Carolina

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

    Valid 271527Z - 272127Z

    Summary...Mesoscale evolution of convective cells with
    supercellular characteristics should continue to prompt areas of
    2-3 inch/hr rain rates. Any localized backbuilding or training
    could promote locally significant flash flooding - especially in
    urbanized and sensitive locales.

    Discussion...A couple of supercellular structures were noted near
    Emporia, VA and Roanoke Rapids, NC over the past hour. Because of
    the rotational and supercellular character of these cells, slower
    and rightward-moving storm motions have enabled spots of 2-3.5
    inch/hr rain rates to develop. These cells were migrating
    northeastward parallel to a subtle confluence/baroclinic zone
    extending from Emporia to KW75/Saluda, VA. Localized vorticity
    ingest processes were likely promoting the supercellular
    development and maximizing rain rates locally.

    Southwesterly steering flow aloft should allow for convection to
    continue drifting northeastward and interacting favorably with the aforementioned confluence zone. This, along with 2 inch PW and
    1000-1500 J/kg SBCAPE on the warm side of the confluence should
    continue to support local 2-3.5 inch/hr rain rates through the
    Wakefield and Williamsburg areas. Furthermore, any backbuilding
    along the confluence axis could prolong rain rates and lead to a
    locally significant flash flood threat - especially in any urban
    or flash flood-prone areas. The mesoscale details supporting this
    risk should persist for at least a few hours, and perhaps through
    21Z/5p EDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!521WCHswjMDHevOyXf0WKx2TisetPY-_KeehgTDAFe38B0R7LwXHzUy9sWwCHgKE-eSb= pfVMH82ycMoD74ObCFk0yJY$ for graphic product...

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

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37857609 37137581 36367669 36007826 36647829=20
    37227789 37807691=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 27 16:30:14 2025
    AWUS01 KWNH 271630
    FFGMPD
    VAZ000-NCZ000-SCZ000-GAZ000-TNZ000-KYZ000-272228-

    Mesoscale Precipitation Discussion 1146
    NWS Weather Prediction Center College Park MD
    1229 PM EDT Sat Sep 27 2025

    Areas affected...eastern Tennessee, far southwestern Virginia, far
    western North Carolina, far northern Georgia, far northwestern
    South Carolina

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

    Valid 271628Z - 272228Z

    Summary...Slow-moving thunderstorms should continue to develop
    through the afternoon hours. Flash flooding is possible on an
    isolated basis.

    Discussion...Scattered, slow-moving convection has been persistent
    this morning beneath a cold mid/upper low centered over far
    northern Georgia this morning. Over the past hour or so,
    satellite imagery suggests an imminent uptick in convective
    coverage due to insolation, surface-based destabilization, and
    deepening cumulus in the region. The storms are forming directly
    beneath the mid/upper low, where weak steering flow has led to
    slow and erratic storm motions. Meanwhile, 1.4 inch PW values and
    1000 J/kg MLCAPE was supporting localized areas of 1-1.5 inch/hr
    rain rates that were exceeding local FFG thresholds at times.

    Ongoing trends should continue until widespread convective
    overturning takes hold and leads to stabilization and decreasing
    convective coverage. This process should take a few hours to play
    out, though. Areas of isolated flash flooding are expected at
    times through the afternoon.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!76sqHZHDAADayExOj2dt3jZ5baS5jSAOGBG1OWsPLsnaWHL9l4K0enYnVYQWnByfzyWR= iX__diZ3IL5UnBXiBhHAECY$ for graphic product...

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

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 37068288 36738076 34728190 33858421 35118542=20
    36298470=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 27 18:21:14 2025
    AWUS01 KWNH 271821
    FFGMPD
    AZZ000-NVZ000-CAZ000-280019-

    Mesoscale Precipitation Discussion 1147
    NWS Weather Prediction Center College Park MD
    220 PM EDT Sat Sep 27 2025

    Areas affected...southeastern California, much of Arizona, far
    southern Nevada

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

    Valid 271819Z - 280019Z

    Summary...An increase in convective coverage is expected through
    peak heating hours today. A few instances of flash flooding are
    possible.

    Discussion...Recent satellite imagery depicts deepening cumulus
    across a broad part of Arizona and adjacent areas of southeastern
    California. Satellite/radar also depicts a persistent, yet small
    cluster of cells just north of Yuma that were producing spots of
    1-2 inch/hr rain rates. The ongoing evolution of convection is
    being supported by a distinct mid/upper low centered over far
    southeastern California, in addition to surface-based
    destabilization due to sunshine and surface warming. PW values
    are in the 1-1.5 inch range, and SBCAPE values are around 1000
    J/kg - both supporting deep convection with heavy rainfall as
    cells mature. Of note is the fact that cells closer to the
    mid/upper low have been very slow to move/propagate so far due to
    weak steering flow in that area.

    Through the afternoon, increases in convective coverage (along
    with increasing prevalence of cell mergers) are expected across
    the discussion area. A few more areas of 1-1.5 inch/hr rain rates
    are expected - especially across southwestern Arizona where the
    best forcing, instability, and moisture combo exists. Isolated to
    scattered instances of flash flooding are possible. Much of the
    threat should be diurnally driven and persist through 00Z/5p
    PDT/6p MDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!465LAeGZjIfzKRajtIB4bzB_LVQG6fPe3Wr9SHFrNOxUQnrmkE1LghNiw6JDewBiz0eo= Bzn3zglQknUhXj5Sm59_Hmo$ for graphic product...

    ATTN...WFO...FGZ...HNX...LOX...PSR...SGX...TWC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 36631405 36391160 35371041 32620945 31450974=20
    30991091 32341461 32411552 32481632 33891689=20
    34701793 36171693=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Sep 27 21:12:44 2025
    AWUS01 KWNH 272112
    FFGMPD
    VAZ000-NCZ000-280111-

    Mesoscale Precipitation Discussion 1148
    NWS Weather Prediction Center College Park MD
    512 PM EDT Sat Sep 27 2025

    Areas affected...southeastern Virginia, far northeastern North
    Carolina

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

    Valid 272111Z - 280111Z

    Summary...Potentially significant urban flood potential exists
    around Norfolk/Virginia Beach through 00Z/8p EDT.

    Discussion...Over the past hour or so, progressive convection has
    tended to stall and backbuild along an axis extending from near
    Norfolk southwestward to near Windsor, NC. The slowed eastward
    progression of this linear complex has enabled focused training
    and a peak of rain rates into the 1-1.75 inch/hr range. These
    rates aren't surprising given the training and pre-convective
    airmass characterized by 2.1 inch PW and ~2000 J/kg SBCAPE.

    Unfortunately, these rates will spread northeastward into
    populated areas of southeastern Virginia (notably Norfolk and
    Virginia Beach). A quick 2-4 inches of rainfall could cause
    significant issues with urban runoff in this scenario. Low-lying
    areas may also experiencing excessive runoff.

    The eastward progression of this band will ultimately rely on
    local convective influences (i.e., upscale growth, merging cold
    pools, and propagation). It should take at least 2-3 hours for
    ongoing convection to clear the region. Again, flash flooding
    (locally significant) is likely through 8p EDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-uGgh1CJzogzlplRWtrAMWyBFh9jreOdQGicBGA8Fd9puaOYT_Zjk1K3kGwZwAetb5Q6= cIDpGsi5FmcZ4egMQjWqyFs$ for graphic product...

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

    ATTN...RFC...ALR...RHA...NWC...

    LAT...LON 37527558 36777576 36397565 35947601 35887700=20
    36587680 37147645 37497609=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Sep 30 16:41:09 2025
    AWUS01 KWNH 301641
    FFGMPD
    UTZ000-NVZ000-302200-

    Mesoscale Precipitation Discussion 1154
    NWS Weather Prediction Center College Park MD
    1239 PM EDT Tue Sep 30 2025

    Areas affected...East-central Nevada...West-central Utah...

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

    Valid 301640Z - 302200Z

    SUMMARY...Scattered to numerous small-cored convection within a
    favorable repeating flow regime and possible back-building may
    result in a few streets of .75-1.25" in 1-3 hours resulting in an
    isolated incident or two of localized flash flooding is possible.

    DISCUSSION...GOES 7.3um WV suite depicts a subtle shortwave at the
    right entrance to a 50kt S-N jet along the northern NV/UT border
    lifting northeast with typical back-arched upper-level cirrus
    indicative of the very favorable divergent flow aloft. Upstream
    the well defined drying also denotes the elongated main trough
    axis extending from SE OR through central NV; with the core of the
    west to east jet starting to nose southward delineating the mean
    trough axis.=20

    Low level response has been for enhanced return flow out of the
    Lower Colorado River bending eastward along a surface to boundary
    layer trough between the Salt Lake surface low and the southern NV
    low. Pooled moisture mainly below 700mb has supported total Pwats
    to 1" across the Salt Flats into SLC vicinity just along/ahead of
    the leading shortwave; though enhanced values up to .8-.9" still
    remain along the upwind edge. Some mid-level drying and clearing
    over east-central NV has provided some insolation/heating to
    support SBCAPEs nearing 1000 J/kg. In response to the DPVA, and
    low level convergence at the nose of the low level moisture flux
    feed; numerous small cored convective cells have begun to cluster
    across S White Pine county, NV with hints of further Cu field
    development across NE Lincoln county, NV into Millard county, UT.=20
    While the cores are shallow (-45 to -50C tops) and narrow, there
    is increasing coverage to support better moisture flux convergence
    for enhancing rates to near .75"/hr over the next few hours.=20=20=20

    Deep layer flow is broadly southwest to southeast parallel to the
    surface trough and considering the overall longer wave trof is
    filling at the base and shifting northeast, the deeper layer flow
    should remain similar to allow for repeating environment. This
    concurrent for upstream instability pool and low level moisture flux/convergence to support some back-building potential... all of
    which will slowly shift eastward. Given all this, a few repeat
    streets may allow for localized .75-1.25" totals in 1-3 hours.=20
    Naturally low FFG values are about .75-1"/hr and 1-1.5"/3hrs
    suggesting an isolated incident or two of localized flash flooding
    may be possible through the afternoon/early evening while
    instability pool remains viable.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8bR5yKjzVKRs6jBuMiXqmLNMmDXlRQeTqjnooRlFBRj2gxTI8Rwgd4km1QXzyJHJAWLs= H6Ty6cXJZFvKBuGeCP0eO2E$ for graphic product...

    ATTN...WFO...LKN...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 40831256 40821165 40001141 39451159 38801201=20
    38191282 37701405 37931487 38881502 39621464=20
    40311387 40591326=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Oct 2 22:28:50 2025
    AWUS01 KWNH 022228
    FFGMPD
    FLZ000-030310-

    Mesoscale Precipitation Discussion 1155
    NWS Weather Prediction Center College Park MD
    627 PM EDT Thu Oct 02 2025

    Areas affected...eastern FL

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

    Valid 022222Z - 030310Z

    SUMMARY...Localized but high rainfall rates are expected across
    coastal sections of eastern/southeastern FL over the next 3-5
    hours. Hourly rainfall of 2 to 3 inches is expected, but locally
    higher values cannot be ruled out which may lead to localized
    flash flooding.

    DISCUSSION...22Z visible satellite and area radar imagery
    indicated a narrow axis of showers/thunderstorms over Martin and
    northern Palm Beach counties, extending offshore and oriented quasi-perpendicular to the coast. MRMS showed hourly rainfall
    peaking in the 1-2 inch range. This axis and additional storms
    were located just south of a low level gradient in moisture,
    aligned from east to west as seen in the surface to 700 mb layer
    on LPW imagery from OSPO. Higher values of low level moisture
    extended southward from roughly Melbourne, while drier and more
    stable air existed to the north. Total PW values were estimated to
    be near 2 inches along the Treasure Coast where low level moisture
    flux was maximized and MLCAPE ranged from 1000-1500 J/kg via the
    22Z SPC mesoanalysis across southeastern FL.

    Some subtle low level cyclonic rotation appeared in visible
    imagery and 7.3 micron water vapor imagery which may be enhancing
    lift across the eastern/southeastern Peninsula Relatively strong
    low level easterly flow of 20-25 kt was in place and is expected
    to maintain over the next few hours, oriented largely
    perpendicular to central to south-central portions of the FL
    coast, maximizing convergence. Transient axes of low level
    convergence within the anomalous low level moisture plume are
    expected to support the possibility of additional narrow bands of showers/thunderstorms which may be slow moving due in part to
    opposing low level and upper level winds and mean steering flow
    matching the orientation of convergence axes. Hourly rainfall of
    2-3 inches should be easily attainable within any slow moving
    heavy rain axes but the environment will have the potential to
    support 3+ inches of rain in an hour as well. These high rainfall
    intensities would support an isolated flash flood threat should
    they overlap with the urbanized I-95 corridor, where runoff would
    be more likely despite the otherwise high flash flood guidance
    values across the region. However, the potential for these very
    high rain rates should remain quite localized from northern
    Miami-Dade to Indian River counties through 03Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!__p112XPLqRR13rzSuD82BUNXbfgZHunFD9agprIMC6A_1z7u5mnb8TZSBBGnQG_7D8C= DqKHwqNbfJy_qIx3HCFQ4VE$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 27778055 27718017 27498006 26957984 26317981=20
    25588006 25648054 26138057 26568054 26998074=20
    27378075=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Oct 2 22:58:50 2025
    AWUS01 KWNH 022258
    FFGMPD
    NVZ000-CAZ000-030400-

    Mesoscale Precipitation Discussion 1156
    NWS Weather Prediction Center College Park MD
    658 PM EDT Thu Oct 02 2025

    Areas affected...San Joaquin Valley into central Sierra Nevada

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

    Valid 022257Z - 030400Z

    SUMMARY...Training and repeating of showers and thunderstorms may
    result in localized flash flooding from the northern San Joaquin
    Valley into the central Sierra Nevada later this evening. Hourly
    rainfall of 0.5 to 1.0+ inches is expected which could result in a
    rapid 1-2 inches through 04Z.

    DISCUSSION...GOES West visible and local radar imagery over
    central CA was fairly quiet as of 2230Z in terms of
    showers/thunderstorms but that may change over the next 3-6 hours.
    A few cells appeared to be developing near the I-5 corridor across
    the northern San Joaquin Valley as seen on KHNX radar and
    additional development appears likely. MLCAPE was rather weak at
    500 J/kg or less via 22Z SPC mesoanalysis data but PW values were
    high at 1.0 to 1.4 inches. These values would equate to a
    standardized PW anomaly of +3 to +4 for early October.

    This region of CA was positioned ahead of the base of an
    approaching mid to upper-level trough located just off of the
    northern CA coast with strengthening right-exit region divergence
    of a 90-100 kt jet just east of the trough base. While surface
    heating through solar insolation has maximized, some additional
    advection of low-level moisture may locally boost instability
    values slightly higher over the next few hours. Showers and
    possibly a thunderstorm aligning within the unidirectional SSW
    flow along with upslope low level flow into the Sierra Nevada may
    act to boost rain rates with potential for 0.5 to 1.0 inches in an
    hour. While the threat for flash flooding appears to be highly
    localized, these higher rainfall intensities falling on sensitive
    burn scars or urban areas would be at most risk for localized
    flash flooding through 04Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4z5_pliYw5pYczaQJ8yWjKZdFcMmbpTjjftCcR_BX1T9hKCiEQ7glaarEk3k-77ghhr-= u5UTiOkB6XuuJuhzqGtywBM$ for graphic product...

    ATTN...WFO...HNX...MTR...REV...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 39172033 39162009 38901971 38531945 37891909=20
    37041902 36321932 36022001 36402078 37172113=20
    37972082 38592068 39052052=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Oct 3 03:42:57 2025
    AWUS01 KWNH 030342
    FFGMPD
    FLZ000-030900-

    Mesoscale Precipitation Discussion 1157
    NWS Weather Prediction Center College Park MD
    1141 PM EDT Thu Oct 02 2025

    Areas affected...Southeast FL

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

    Valid 030341Z - 030900Z

    SUMMARY...Locally concentrated areas of very heavy showers and
    thunderstorms across southeast FL will continue in the near-term.
    Concerns for urban flash flooding will exist near and south of the
    Miami metropolitan area.

    DISCUSSION...GOES-E Proxy Visible satellite imagery along with
    radar data shows some concentrated areas of very heavy showers and thunderstorms continuing to impact portions of southeast FL. Much
    of the activity is currently situated near and south of Miami with
    some relatively organized banding of convection that is
    well-aligned with the very moist/unstable low-level easterly flow
    impacting the FL Peninsula.

    Satellite and surface data also show signs of a weak low-level
    vort center near Biscayne Bay which is helping to concentrate an
    axis of strong moisture convergence into the coastal areas in
    between Miami and Homestead. MLCAPE values of near 1000 J/kg are
    in place, with PWs of 1.8 to 2.0 inches.

    Some cell-training concerns will exist over the next few hours
    with the convective activity impacting southeast FL, and
    especially with a persistently convergent low-level Atlantic fetch
    into the region. Rainfall rates have already been reaching as high
    2 to 3 inches/hour, and with any persistence of these stronger
    convective cores, there may be some rainfall totals that locally
    approach or exceed 5 inches. This is supported by some of the 00Z
    HREF guidance.

    Expect there to be at least some concerns for urban flash flooding
    with these heavier rainfall rates and storm totals set up over the
    next few hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!98UZoF4G0XdnPVYl7qoTSxbX3It1YKYOKQF0Sq7PDroixNuu6-KMzdtq7meHc1Y5QShB= t2qwfcqXCksXXWswGOrhleU$ for graphic product...

    ATTN...WFO...KEY...MFL...

    ATTN...RFC...ALR...NWC...

    LAT...LON 26168015 26028007 25758007 25328022 25278039=20
    25478053 25968043 26158027=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 5 19:46:43 2025
    AWUS01 KWNH 051946
    FFGMPD
    FLZ000-ALZ000-052345-

    Mesoscale Precipitation Discussion 1158
    NWS Weather Prediction Center College Park MD
    346 PM EDT Sun Oct 05 2025

    Areas affected...southern/coastal Alabama, parts of the western
    Florida Panhandle

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

    Valid 051945Z - 052345Z

    Summary...A band of heavy rainfall will move slowly across the
    discussion area, with rainfall totals of 3-5 inches occurring in
    some areas through 2330Z/630p CDT. Isolated instances of flash
    flooding are possible with this activity.

    Discussion...Latest radar/satellite imagery depicts a band of
    thunderstorms that has exhibited upscale growth and slow forward
    propagation along an axis from near Foley, AL south-southeastward
    to around 85 miles SSW of AAF/Apalachicola, FL. This band was
    moving slowly eastward, while individual cells were streaming
    northward toward coastal areas near Foley and Pensacola, FL. The
    band of convection was also exhibiting very localized training
    near coastal areas that was resulting in an uptick in hourly
    rainfall rates (into the 3 inch/hr range). These rain rates are
    still falling shy of local FFG thresholds, suggesting that any
    runoff issues may be isolated in the short term.

    The band of ongoing convection should persist for at least another
    2-4 hours given favorable low-level easterlies for
    inflow/low-level shear, slight low-level warming (supporting
    1000-1500 J/kg SBCAPE in the pre-convective environment), and an
    abundantly moist airmass (2-2.2 inch PW values supporting
    efficient rainfall processes). Isolated flash flood potential
    should slowly spread eastward along the western Florida Panhandle,
    with areas near Pensacola, Eglin AFB, and potentially Panama City
    experiencing heavier rainfall through at least 2330Z/630p CDT. 3
    inch/hr rain rates will remain possible with this activity.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_L0h8AHIVf3mgL5bBPLCuReypkeugKzGNxZaZPk3XgpRN4TGgQ5uYihplk-TQbiY7fZS= Fs_hIJijViKdBjXFS1-p4bk$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 31018783 30978673 30658550 29928509 29608528=20
    30218793 30748818=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 6 07:41:24 2025
    AWUS01 KWNH 060741
    FFGMPD
    MSZ000-LAZ000-061340-

    Mesoscale Precipitation Discussion 1159
    NWS Weather Prediction Center College Park MD
    340 AM EDT Mon Oct 06 2025

    Areas affected...South-Central LA into Southwest MS

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

    Valid 060740Z - 061340Z

    SUMMARY...Localized backbuilding and training of warm-topped
    convective bands early this morning across south-central LA up
    into southwest MS may produce some isolated flash flooding
    concerns.

    DISCUSSION...The latest GOES-E IR satellite imagery in conjunction
    with radar shows multiple warm-topped bands of very heavy showers
    and a few thunderstorms impacting portions south-central LA up
    into far southwest MS. The convection is associated with
    increasingly convergent flow around the eastern flank of a low to
    mid-level vort center lifting gradually northward into the Lower
    MS Valley.

    Locally enhanced moisture convergence is especially noted across
    southwest MS right now, with a nose of MUCAPE values reaching 500
    to 1000 J/kg stretching northward from the central Gulf Coast up
    into southwest MS in close proximity to a surface trough. A
    southerly low-level jet reaching 30 to 40 kts is noted around the
    eastern flank of the vort energy, and with weaker deep layer mean
    flow across the region, the Corfidi vectors are strongly
    supportive of an environment for backbuilding convection. This is
    being evidenced right now with the latest radar trends and
    especially with the convective cells/banding occurring over parts
    of south-central LA.

    PWs are quite high and locally upwards of 2 to 2.25 inches, and
    with this deep tropical environment along with elevated WBZ
    heights, some of the rainfall rates may reach 2 to 3 inches/hour.
    Given the alignment of the convection with the deeper layer
    southerly flow regime, there will be cell-training concerns at
    least locally. Going through early this morning, there may be some
    localized 3 to 5+ inch rainfall totals that materialize. This may
    result in at least some isolated concerns for flash flooding and
    especially if any of the more urbanized areas are impacted.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4oRu_NwHnPpnEWMcW438fAYjV3yFpFQclLdJ0OOdPdGjo-3Wv2jUZ3ffNnOYin5X9pOl= Su7ksAZXIeS0p-ZIYbANpG8$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...

    ATTN...RFC...ORN...NWC...

    LAT...LON 32789084 32249005 30908996 29759052 29529126=20
    29819175 30439172 31349151 32309151=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 6 12:12:41 2025
    AWUS01 KWNH 061210
    FFGMPD
    FLZ000-061809-

    Mesoscale Precipitation Discussion 1160
    NWS Weather Prediction Center College Park MD
    810 AM EDT Mon Oct 06 2025

    Areas affected...portions of Palm Beach & Broward Counties in FL

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

    Valid 061209Z - 061809Z

    Summary...Occasional convective bands could continue to set up in
    and near the Gold Coast of FL, possibly into early this afternoon.
    Hourly amounts to 2" with local totals to 4" could lead to
    isolated occurences of flash flooding.

    Discussion...An upper level disturbance across North FL combined
    with precipitable water values ~2.25", 2000+ J/kg of ML CAPE, and
    effective bulk shear of 20kt or so has led to the development and
    fading of a couple convective bands across east-central Palm Beach
    and northeast Broward Counties, downwind of the northwest Bahamas
    and within an area of low-level convergence near a stationary
    front. A more active convective band lies offshore Broward County
    at the time of this discussion's writing. Hourly rain estimates
    have approached 2" with the Palm Beach county band and above 1"
    near Deerfield Beach.

    The expectation is for convective bands to occasionally shift
    south/reorganize in different locations with time, primarily
    across Broward County, though additional activity in southeast
    Palm Beach County can't be ruled out. The mesoscale guidance (via
    the HREF and REFS probabilities) indicate the threat of heavy
    rainfall in and near the Gold Coast perhaps as late as 18z with
    some possible southward shift/reorganization which seems to follow
    a slight southward nudge of the highest moisture in the region.=20
    Until the bands dissipate or become less organized at some point
    this afternoon, hourly amounts to 2" with local totals to 4" could
    lead to flash flooding in urban areas.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4SZmsLD6fVmAlGZcsn3_ADjbNKkRCq6LhLl8BVguG67mpQK2vSw4G6JD6Y3vf_czwosm= p2INOnsxNkSdgXHi41affrY$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 26758005 26498002 25958013 26038037 26588037=20
    26738031=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 6 13:38:26 2025
    AWUS01 KWNH 061338
    FFGMPD
    MSZ000-LAZ000-061637-

    Mesoscale Precipitation Discussion 1161
    NWS Weather Prediction Center College Park MD
    937 AM EDT Mon Oct 06 2025

    Areas affected...portions of southeast LA and southern MS

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

    Valid 061337Z - 061637Z

    Summary...Training thunderstorms are possible over the next few
    hours roughly between Baton Rouge LA and Prentiss MS. Hourly rain
    amounts to 2.5" and additional local totals are possible where
    cell training occurs, which would be most problematic in recently
    saturated and urban areas.

    Discussion...A training band of convection remains active across
    south-central MS at the present time, while another area of slowly
    developing scattered convection near Baton Rouge aligning.=20
    Precipitable water values are around 2.25" per GPS data. ML CAPE
    of 500-1000 J/kg persists to the southeast of a low- to mid-level
    disturbance near southeast AR. Effective bulk shear across the
    region is 20 kts or so, which has fostered convective organization
    at times.

    The concern is that the scattered aligned convection in LA
    continues to slowly build, consolidate, and train in the next few
    hours, potentially advecting downstream into areas that receieved
    5-10" of rain this morning per radar estimates. The remaining
    convective band is also a source of concern for another 2-3 hours.
    Where training occurs, hourly amounts to 2.5" with additional
    local amounts to 4" would be possible, which would be most
    problematic in urban areas and were soils have recently saturated.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-HlW0Z7_20mpjxmZ3pPVoB8ronlYjmCSXAac0erYyKyg3YLk3QST8fpprRAMQE2LJqJi= m34tWFprAZ8Qzr9Tr17YJjA$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...

    ATTN...RFC...ORN...NWC...

    LAT...LON 31938979 31228976 30489041 30149122 30169166=20
    30619135 31359058=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 6 16:22:59 2025
    AWUS01 KWNH 061622
    FFGMPD
    FLZ000-062100-

    Mesoscale Precipitation Discussion 1162
    NWS Weather Prediction Center College Park MD
    1222 PM EDT Mon Oct 06 2025

    Areas affected...Space Coast of Florida into Central Peninsula

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

    Valid 061625Z - 062100Z

    SUMMARY...Strong, directed onshore flow with strengthening
    upstream low level flow, to support back-building training across
    the Space Coast with highly efficient 2-3"/hr rates pose localized
    urban flooding

    DISCUSSION...GOES-E 10.3um and KMLB RADAR shows strong
    back-sheared thunderstorms crossing Cape Canaveral into N Brevard
    county with slow weakening/disruption into the central Peninsula
    as some dry air mixing is resulting in low level convergence
    outrunning the deeper layer steering. This reduces the vertical
    depth of moisture flux convergence and rainfall generation.=20
    However, nearer the coast; upstream increased deeper layer
    moisture (including increasing 700mb RH) is maintaining broader
    convective development within an East to West band north of Grand
    Bahama into the Cape. MLCAPE of 2000 J/kg are solid given the
    narrow skinny/moist profile with depth. Combining to the vertical
    ascent is entrance to the 30-40kt 3H jet streak along 30N east of
    79W, is providing solid divergence aloft to help maintain the
    depth of rainfall production.

    Deep layer moisture of 2.25" and flux convergence given upstream
    winds of 25-30kts decelerating into the coast will allow for
    continued 2-3"/hr rates with a favorable back-building
    regenerative environment. Eventually, the forecast is for the
    outflow/jet entrance is to slide further east and reduce the
    divergence aloft; however, there is some trends in satellite
    loop/imagery that suggest the convection may be adding
    to/strengthening the jet in a narrow axis. If this were to occur,
    longer duration will increase overall localized totals of 3-5".
    Small southward wavering of the onshore axis is expected to help
    spread the heavy rainfall footprint. Given proximity to urban
    locations and sheer rate, localized rapid inundation/flash
    flooding is considered possible.

    A bit more uncertain, is how far downstream into the Central
    Peninsula this will extend. Each bout/updraft cycle will further
    moisten the low level environment and allow further downstream
    extension of the narrow heavy rainfall (E-W) corridor. Hi-Res
    CAMs continue to suggest a westward translating convergence wave
    lengthwise through the Peninsula, but current trends of upstream
    development suggests coastal training remains more likely for the
    greatest overall totals.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_G_ivsMkCGAo5PcurhnL7tIjaOrAE5fAtUtL0T9LF25M4UDunV-Rv3NUQEeihD7bCFhL= QWOiAWx9KYghJ7ltvqgu7UQ$ for graphic product...

    ATTN...WFO...JAX...MLB...

    ATTN...RFC...ALR...NWC...

    LAT...LON 29148147 29078097 28798063 28398036 27788042=20
    27848101 28378168 28728191 29038184=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 6 18:31:21 2025
    AWUS01 KWNH 061828
    FFGMPD
    ALZ000-MSZ000-LAZ000-070000-

    Mesoscale Precipitation Discussion 1163
    NWS Weather Prediction Center College Park MD
    227 PM EDT Mon Oct 06 2025

    Areas affected...Southeast Louisiana...Mississippi...Coastal
    Alabama...

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

    Valid 061830Z - 070000Z

    SUMMARY...Reinvigoration of convective bands will have similar
    potential for back-building and short-term training resulting in
    2-4" totals given 2-2.5"/hr rates. Localized flash flooding
    remains possible through the evening.

    DISCUSSION...GOES-E GeoColor Visible imagery shows well defined
    surface to mid-level circulation along the LA/AR border with broad
    warm advective regime along the eastern hemisphere across much of
    MS into SE LA. Surface analysis shows some weak reflection in
    pressures further south than the wind circulation along the
    border, but a defined frontal zone extend along the MS River into
    the Atchafalaya Swamps of south-central LA...east of it higher
    theta-E air with increasing temperature spreads into the 80s over
    Tds in the mid to upper 70s. Early morning south to north
    convective line exists along the eastern side of the warm sector
    before low to mid-level clouds have been keeping temps in near the
    Tds north of the warm front from GLH to north of JAN to E of HBG
    and south to Mobile Bay. Surface to boundary layer moisture
    pooling along the warm front intersects with SSW LLJ across SE LA
    into central MS where Total PWat values are well above average in
    the 2.25"+ range. The confluence of the conveyor belts has
    resulted in strong moisture flux convergence generally coincident
    or just north of the expanding instability wedge. MLCAPEs are
    increasing from 1000 to 2000 J/kg from the warm front southward to
    the Gulf; providing the strength for vertical development.

    Recent GOES-E Vis/IR loops along with regional RADAR mosaic
    denoted leading edge of old outflow and intersection of the warm
    front has seen increased convective vigor and vertical depth in
    the last hour or so. While winds are generally 20-25kts through
    depth, it is the strong confluence with height that present the
    stronger convergence to tap the unstable air. Moisture flux of
    the high moisture will result in increasing rain-rates of
    2-2.5"/hr. Steering flow will allow for south to north training,
    though momentum and some weak cold pool generation should allow
    for some eastward propagation to limit overall duration. Spots of
    2-4" are probable and may result in localized flash flooding
    concerns.

    Additionally, GOES-E WV suite denotes a weak inflection along the
    cold front near the Gulf coast lifting northeastward within the
    larger shortwave lifting north through the MS Valley, this is
    indicative of some increased low-level jet streak to support
    upstream back-building. In addition, while not in the core of the
    warm conveyor belt, convergence along the cold front toward the
    triple-point could see even slower, but shallower thunderstorms
    capable of intense rainfall as well. The potential of upstream
    development in proximity to the front could expose areas of
    lowered FFG from this morning's thunderstorm activity and
    reaggravate flooding concerns there as well. As such, have
    expanded the MPD area of concern to the cold front to encompass
    this lower confidence, wider scattered activity and flash flood
    potential.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5kqEn9ABgoaBy83TKamWfey1bpNGDWezyGFebiIOwJen41FITHNy3dd_b7IFD7cu0YYL= wKg-hUtcEvZN9uQo-AnY7Vw$ for graphic product...

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

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34698960 34158873 32378849 31398795 30508763=20
    30178795 30268891 30088985 30109055 30369132=20
    31569090 32719080 33569100 34289043=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Oct 7 01:30:04 2025
    AWUS01 KWNH 070130
    FFGMPD
    TNZ000-KYZ000-MSZ000-MOZ000-ARZ000-070700-

    Mesoscale Precipitation Discussion 1164
    NWS Weather Prediction Center College Park MD
    929 PM EDT Mon Oct 06 2025

    Areas affected...Mid-South

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

    Valid 070129Z - 070700Z

    SUMMARY...Concentrated areas of heavy rainfall will impact
    portions of northeast AR and western TN over the next several
    hours. Scattered areas of flash flooding are likely, and
    especially around the more urbanized areas such as Memphis and
    Dyersburg.

    DISCUSSION...A well-defined surface low and associated mid-level
    vort center continues to lift gradually north-northeastward up
    across eastern AR this evening and will be advancing through
    adjacent portions of the Mid-South and toward the Lower OH Valley
    by later tonight.

    The energy is fostering a concentrated area of very heavy rainfall
    currently over portions of far northeast AR and along the MS River
    just to the west of Memphis, TN. Enhanced southerly warm air
    advection and moisture transport is surging northward around the
    eastern flank of the surface low and vort center with the aid of a
    southerly low-level jet reaching as high as 30 to 40 kts.

    This is allowing for a substantial amount of tropical moisture and
    at least modest instability to be focused in close proximity to
    the low center and also downstream of it nosing across far
    northwest MS and into northeast AR through western TN. The latest
    RAP analysis shows as much as 500 to 1000 J/kg of MLCAPE across
    these areas with PWs of 2 to 2.25 inches.

    Additionally, some very strong moisture convergence is noted
    around the immediate northeast flank of the surface low and vort
    center itself, and radar is showing a corridor of enhanced
    convection producing extremely high rainfall rates in association
    with this. Overall, the larger convective footprint shows
    relatively warm convective cloud tops, but over the last hour
    there has been a substantial cooling of tops just west of Memphis
    where some rainfall rates of 2 to 3 inches/hour are occurring.

    Over the next several hours, this concentrated areas of very heavy
    rainfall should still impact portions of northeast AR, but will be
    advancing increasingly into western TN.

    Expect there to be notable concerns for urban flash flooding in
    the near-term around the Memphis metropolitan area along with the
    adjacent suburbs as this concentrated axis of heavy convective
    rainfall near to the low center advances off to the
    north-northeast. Additional downstream areas such as Dyersburg may
    impacted as well. Expect in general there to be scattered areas of
    flash flooding becoming likely even outside of the urban areas
    given rainfall totals that may reach 3 to 5+ inches in a localized
    fashion going into the overnight hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8iD9eiigab60asRk0DqBfwLb5TOdbLAP1AJZWBdRnj2z9bVJOvV6JQGVdAL_2A0USz4y= mnNCF-5FCd9UJ4fPrNmXczQ$ for graphic product...

    ATTN...WFO...LZK...MEG...PAH...

    ATTN...RFC...ORN...NWC...

    LAT...LON 36548906 36168811 35378841 34758980 34599092=20
    34679124 35139143 35869089 36229023=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Oct 7 09:21:14 2025
    AWUS01 KWNH 070921
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-071520-

    Mesoscale Precipitation Discussion 1165
    NWS Weather Prediction Center College Park MD
    520 AM EDT Tue Oct 07 2025

    Areas affected...Portions of the Mid South and Lower Ohio Valley

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

    Valid 070920Z - 071520Z

    SUMMARY...Heavy rainfall still impacting portions of the Mid-South
    early this morning will become increasingly focused across the
    Lower OH Valley over the next several hours. Some isolated to
    scattered areas of flash flooding will be possible where any
    cell-training of showers and thunderstorms occur.

    DISCUSSION...A well-defined surface low and associated mid-level
    vort center is beginning to edge into the Lower OH Valley along
    with a pronounced surge of tropical moisture. A southerly
    low-level jet of 30 to 40 kts continues to focus rather strong
    warm air advection and moisture transport around the eastern flank
    of the low center, and this combined with modest instability and
    some upper-level jet divergence should support broken areas of
    heavy rainfall overspreading the Lower OH Valley this morning.

    MLCAPE values are only on the order of 500 to 750 J/kg, but the
    moisture convergence parameters are rather strong around the
    northeast flank of the vort energy and especially near the low
    center itself. This is favoring some stronger convective elements
    with highly efficient rainfall owing to warm rain/relatively
    shallow-topped convection. Some embedded colder convective tops
    are occurring in sporadic bursts, and these smaller scale clusters
    of convection have been capable of producing rainfall rates on the
    order of 1.5 to 2.5 inches/hour.

    As this energy begins lifting northeastward across the Lower OH
    Valley this morning, there is expected to be some gradual
    interaction with an upstream cold front approaching the OH Valley
    from the northwest. This will support a more frontogenetical
    component to the heavy rainfall threat and should support a more
    elongated southwest to northeast axis of heavy rain with embedded
    convection.

    The 00Z HREF/REFS suites of guidance support some localized swaths
    of 2 to 4+ inches of rain going through late this morning, with a
    spotty 5+ inch total not out of the question where any
    cell-training of convection occurs. The heavier and more
    concentrated areas of rainfall should be close to the OH River
    involving areas of far southeast IL, western and northwest KY and
    into far southern IN.

    Antecedent conditions across the region are generally on the dry
    side, but the rainfall potential this morning is expected to be
    enough to drive a threat for isolated to scattered areas of flash
    flooding. This will especially be the case in vicinity of the more
    urbanized areas.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6s984LwdmtyLfd2gxOGVFuAgG_GO4HI8oTRXsdnDZ6HV7Ny2Ua9ua4PoKj_JB5_fo7N6= O_aOSlDrcjOZRCS4qTLPxWM$ for graphic product...

    ATTN...WFO...ILN...IND...JKL...LMK...MEG...OHX...PAH...

    ATTN...RFC...MSR...ORN...TIR...NWC...

    LAT...LON 39008471 38588377 37748383 37098453 36388586=20
    36088694 36008780 35988834 36028894 36278967=20
    36758973 37398939 38028844 38508736 38958580=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 Oct 7 15:01:47 2025
    AWUS01 KWNH 071501
    FFGMPD
    WVZ000-OHZ000-KYZ000-INZ000-072000-

    Mesoscale Precipitation Discussion 1166
    NWS Weather Prediction Center College Park MD
    1101 AM EDT Tue Oct 07 2025

    Areas affected...Far Southern IND...Northern & Central
    KY...Southern OH...Far Western WV

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

    Valid 071500Z - 072000Z

    SUMMARY...Prolonged moderate rainfall with embedded weak
    convective elemented within a long training profile into confluent
    low to mid-level flow downstream of cyclone pose localized 2-3"
    totals over 3-6hrs suggesting scattered incidents of flash
    flooding remains through afternoon.

    DISCUSSION...14z surface analysis depicts an elongating SW to NE
    surface low across Southwest KY as the mid-level shortwave
    continues to advance into the lower Ohio Valley into increasingly
    confluent flow aloft. A new triple point-like feature near OWB
    appears to be helping to back the low to mid-level higher moisture
    flux flow enough to maintain some solid convergence to tap the
    remaining conditionally unstable air of 250-500 J/kg along and
    downstream in proximity to the stationary front which appears to
    have taken residence in the Ohio Valley, proper. Solid deep layer
    moisture through the confluence stream remains well above normal
    at 1.75-2.1" of total PWats though CIRA LPW denotes the
    elongation/shearing of the moisutre axis as the surface to 850
    remains upstream near the low and slow advancing cold front, but
    700-500mb slug has shifted toward Northern Kentucky and southern
    Ohio.

    Still the oblique ascent across the effective boundary is further
    elongating the isentropic ascent that has moderate shield precip
    and weak convective entrainment, increasing further to the west.=20
    The flux is enhancing showers to .25-.75"/hr and given the
    orientation into the confluence zone further strengthens training
    profile and axis of 2" may result prior to even the arrival of
    stronger flux/deeper convective cores capable of 1.25-1.5"/hr
    though average more close to 1" for an additional 1-2 hours. This
    should result in 2-3.5" totals with a low possibility of a
    localized 4" total across the area of concern through the
    afternoon.=20

    The flashy, rapid rise concerns are low and likely very isolated=20
    but prolonged moderate rainfall, FFG values in the 3-6hr range are
    still about 2-3" along the frontal zone/training axis. This still
    suggests exceedance remains possible with scattered incidents of
    flooding especially in very poor drainage areas, such as urban
    settings.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5zZYIDwQf5bA7j5eVlGmC3eBSDbPZDSRiwc1NMkbgb7XXALrWMDtbLRRSMTz9O2--0gn= N1-caWr24-YYI4nclUtk__4$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...PAH...RLX...

    ATTN...RFC...TIR...NWC...

    LAT...LON 39578261 39348191 38818177 38358197 37888263=20
    37568380 37178594 36918765 37568756 38218703=20
    38748564 39258429 39468337=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Oct 7 17:46:50 2025
    AWUS01 KWNH 071746
    FFGMPD
    NMZ000-072345-

    Mesoscale Precipitation Discussion 1167
    NWS Weather Prediction Center College Park MD
    146 PM EDT Tue Oct 07 2025

    Areas affected...Central to Eastern New Mexico...

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

    Valid 071745Z - 072345Z

    SUMMARY...Scattered slow moving cells capable of 1.5"+/hr rates
    and totals over 2", especially near Sacramento Mountains posing
    localized incident(s) of possible flash flooding through evening.

    DISCUSSION...GOES-E Visible imagery shows the surface to boundary
    layer increased moisture indicated by banked up stratus east of
    the Sacramento mountains and through the saddle and into the far
    southern Sangre de Cristo Range. CIRA LPW and RAP analysis
    confirmed by surface Tds in the mid to upper 50s of this enhanced
    low level moisture with nose angling out of the Pecos River
    Valley. Solid upslope is deep enough to have bled through to the
    westward adjacent Rio Grande Valley with an effective dry line
    noted as Tds drop into the 20s/30s through the Black Mtn Range.=20

    Water vapor suite denotes an elongated shortwave across central AZ
    with a weak mid-level baroclinic leaf downstream into west-central
    NM angling out from the higher cirro-stratus in the sub-tropical
    jet that is centered across southern NM. The strong directional
    shear across the area has resulted in effective bulk shear into
    the 30-35kt range in central NM, suggesting organized, broader
    updrafts once destabilization occurs. Currently, the cloudy
    nature east of the terrain is limiting insolation but temps
    upstream of the terrain in the Rio Grande Valley are reaching
    mid-70s and where the moisture stream overlaps, SBACAPEs are
    starting to increase over 1000 J/kg. While upslope flow has not
    begun in earnest, the limited capping and weak divergence aloft at
    the entrance of the subtropical jet streak has resulted in some
    mid-level activity increasing as Lightning-cast Probability are
    reaching 60-75% over the next hour with some of the TCu features.=20
    Still believe this is a bit too early for the strongest updrafts,
    but these seeds could sprout earlier than the 20z expected
    destabilization noted in most of the recent Hi-Res CAMs.=20

    Low level winds should further back and strengthen to 15-20kts and
    further enhance deep layer convergence in the Sacramento
    Mountains. Initially anchored updrafts, may result in localized
    1" totals, before expanding and slowly decoupling from the
    terrain. The bulk shear suggests some rotation which will
    further increase moisture flux convergence to support 1.5"/hr
    rates. RRFS is most aggressive, but does not seem unreasonable,
    especially representation of convective mode. These cells are in
    general proximity to burn scars near Ruidoso and any overlap is
    more likely to result in FF, but that precision is not capable at
    this time scale but locals should remain weather-aware.=20

    As the afternoon progresses to evening, as upstream shortwave
    slowly drifting northeast into NW NM toward the late evening,
    upslope flow is expected to continue and strengthen
    through/westward past the terrain and expand convective initiation
    further north and west with time. Spots of 1-2" in hard pan
    ground conditions may result in additional localized incidents of
    flash flooding.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-8qqmcRz_YfiCGHaDKUaSlSAfSvoqEJyqTtHFcf3bf208VUCzu6xdMIee9bniVr9P45V= lmtTCRM8hEW9kSwQ3KmbAwc$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35850583 35650481 34390379 33330365 32630441=20
    32330510 32350589 32900652 34020639 34720647=20
    35260626=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Oct 7 19:55:23 2025
    AWUS01 KWNH 071955
    FFGMPD
    WVZ000-OHZ000-KYZ000-080030-

    Mesoscale Precipitation Discussion 1168
    NWS Weather Prediction Center College Park MD
    354 PM EDT Tue Oct 07 2025

    Areas affected...Northeast KY...Southern OH...Western WV...

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

    Valid 072000Z - 080030Z

    SUMMARY...A few more hours of training moderate showers with
    ending burst of intense rain near surface low, pose longer term
    flooding concerns with isolated rapid rise/flash flooding possible.

    DISCUSSION...GOES-E WV suite shows core of elongating southern
    stream shortwave continues to advance much faster than the
    low-level/surface features into increasingly confluent flow in the
    Upper Ohio River Valley. This vertical tilting further displaces
    deep layer moisture structure as total PWat values continue to
    reduce from 2" toward 1.75". Additionally, much of the area has
    become stable with limited <250 J/kg of CAPE. However, the warm
    conveyor and moisture flux convergence remains solid and more
    importantly elongated along the ill-defined boundary across NE KY
    into the Ohio River. Oblique ascent from 25-35kts of 850mb
    southwesterly flow to the boundary more WSW to ENE and larger
    scale downstream divergence continues to broaden the moderate
    precipitation shield.=20

    Rates of .25-.5"/hr continue within the broad moderate shield
    expanding as far east as the middle slopes of the Allegheny
    Plateau. However, the western edge of the warm conveyor belt has
    an associated surface low intersecting the boundary near KLEX,
    providing stronger convergence overlapped with modest mid-level
    drying has allowed for some conditional instability to reach
    500-750 J/kg. As such, GOES-E 10.3um shows some solid convective
    cores still cooling below -60C, suggesting an ending punch to the
    training moderate showers with a cell or two capable of
    1.25-1.5"/hr. So with 1-1.5" capped off with an additional 1-1.5"
    in about an hour, may result in a streak of additional 2-3" across Northeast/Eastern KY into W WV before fully weakening in favor of
    stronger forcing/backing flow to the northern stream frontal zone
    dropping in across central IND/OH.

    While the area has been dry, natural lower FFG values of
    1-1.5"/1hr are less likely to be exceeded but 3-6hr values of
    1.5-3" have a slightly higher potential. So the rapid rise
    flooding may be a bit more tempered, but FLASH unit stream flow
    values across much of central KY have been between 400-650 cfs/smi
    and even a slightly reduced value across the rugged terrain across
    NE KY into far S OH/W WV, are likely to remain above 300 cfs and
    suggest some flooding conditions are possible through the
    remainder of the evening hours.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6PMFqgw0bUH_lhpOmA9qsmp426tNy_jwGDoF3r_-1Fns65Eoqa4JuJbqAO4RkZgJKSg0= dN5JEwA0k6F5cwuh0v0dsVo$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...RLX...

    ATTN...RFC...TIR...NWC...

    LAT...LON 39318159 38988102 38468101 38018128 37698206=20
    37628247 37608353 37798422 38308467 38798423=20
    39078336=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Oct 7 23:46:25 2025
    AWUS01 KWNH 072346
    FFGMPD
    TXZ000-NMZ000-080400-

    Mesoscale Precipitation Discussion 1169
    NWS Weather Prediction Center College Park MD
    745 PM EDT Tue Oct 07 2025

    Areas affected...Portions of Central and Eastern New Mexico

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

    Valid 072344Z - 080400Z

    SUMMARY...Scattered slow moving cells capable of 1.5"+/hr rates
    and isolated rainfall totals in excess of 2", especially near
    Sacramento Mountains, pose a localized threat of flash flooding
    through this evening.

    DISCUSSION...GOES-E Visible imagery showed a surface boundary
    across portions of western Texas into eastern New Mexico while
    RAP-based moisture flux convergence maxima were mainly along or
    near the boundary with late afternoon/early evening surface Tds in
    the mid to upper 50s. Upslope is deep enough to have bled through
    to the westward adjacent Rio Grande Valley with an effective dry
    line noted as Tds drop into the 20s/30s through the Black Mtn
    Range.=20

    The cloudy nature east of the terrain has limited insolation but a
    combination of late afternoon temperatures in the 80s and 90s
    south of the front and dewpoints in the 50s has resulted in some
    pockets of surface based CAPE values in the 750 to 1000 J per kg
    range by 07/23Z. While upslope flow has not begun in earnest, the
    limited capping and weak divergence aloft at the entrance of a
    subtropical jet streak could result in additional showers and
    thunderstorms capable of producing rainfall rates in excess of an
    inch per hour due to destabilization noted in most of the recent
    Hi-Res CAMs and recent mesoanalysis. The environmental bulk shear
    suggests some rotation which will further increase moisture flux
    convergence to support 1.5"/hr rates. Any cells in the general
    proximity to burn scars near Ruidoso and any overlap is more
    likely to result in FF, but that precision is not capable at this
    time scale but locals should remain weather-aware.=20

    As the evening progresses, upslope flow is expected to continue
    and strengthen through/westward past the terrain and expand
    convective initiation farther north and west with time. Spots of
    1-2" in hard pan ground conditions may result in additional
    localized incidents of flash flooding.

    Bann

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8SjtSo5E--B0tQtfF9Ws5zNfujQop4RC5bEE_xFeQDbqK7XfwUDJuPHs642xdVdVVqIh= vqu1x4_TeWGQeTWwh-nUO48$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...NWC...

    LAT...LON 35200531 34270390 33540329 32280341 31790406=20
    31440489 31360595 31750647 31900762 33070770=20
    34450722 35160634=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Oct 8 19:50:40 2025
    AWUS01 KWNH 081950
    FFGMPD
    NMZ000-AZZ000-090130-

    Mesoscale Precipitation Discussion 1170
    NWS Weather Prediction Center College Park MD
    349 PM EDT Wed Oct 08 2025

    Areas affected...West-Central to Central NM... Adjacent Northeast
    AZ...

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

    Valid 081950Z - 090130Z

    SUMMARY...Scattered slow moving thunderstorms may result in spots
    of 1-2" totals in less than 2 hours, posing isolated localized
    flash flash flooding conditions. Adjacent

    DISCUSSION...GOES-E Visible and KABQ RADAR shows a sizable cluster
    of convective development across portions of west-central NM
    terrain (west of the Rio Grande Valley). An ill-defined frontal
    zone seems to be a confluent/pooling agent for southerly to
    southeasterly upslope flow and moisture advection out of the Rio
    Grande Valley. Tds in the mid 50s in the upslope regime while
    upper-level flow provides favorable divergence aloft at the apex
    of the anticyclonically curved sub-tropical jet originating out of
    the Sea of Cortez and across S NM. The confluent flow at the
    curvature of the front along with the upslope component appears to
    be allowing for the greater overall coverage/clustering.=20

    Prior to development, solid insolation and the lower moisture
    profile and modest drying aloft has supported 1000+ J/kg of SBCAPE
    and with the southerly/southeasterly confluent flow along the
    gradient of overall deeper moisture (favorably loaded in the lower
    profile per CIRA LPW) suggests modest rainfall efficiency for
    these cells as they mature. With the upper-level jet and weak
    directional shear, effective bulk shear of 25-30kts suggests some
    weak organization and perhaps some weak cell rotation to further
    enhance moisture flux into the updraft column. Mean winds of
    20kts, slightly deflected due to any weak rotation along with
    favorable upslope initially to help lock the up/downdraft to the
    terrain for a few hours suggests some increased duration of modest
    rates. As such, rates of .75-1"/hr are possible resulting in
    localized 1-2" totals in 1-2 hour time frames suggest localized
    flash flooding could occur in an isolated to widely scattered
    nature, with obviously higher potential in/around burn scars in
    the vicinity through the afternoon into evening hours in the area
    of concern.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8fLzURgYh2hPEArJHx1LUn7qW2LDZUh_QthgNfmuM3Rvtw1xGUb70eODADTng5l5NHaI= 8nmpQ9XP3YLuBgb_HWuM2pY$ for graphic product...

    ATTN...WFO...ABQ...FGZ...

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 36340704 36130620 36050606 35300549 34430565=20
    33820564 33420563 33460608 33610627 34250646=20
    34490671 34450703 33610734 33510812 33530857=20
    33960902 34480944 35170954 35780915 36300790=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 Oct 9 17:31:28 2025
    AWUS01 KWNH 091731
    FFGMPD
    FLZ000-092300-

    Mesoscale Precipitation Discussion 1171
    NWS Weather Prediction Center College Park MD
    130 PM EDT Thu Oct 09 2025

    Areas affected...Southeast to Southern Peninsular Florida...

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

    Valid 091730Z - 092300Z

    SUMMARY...Slow moving thunderstorms within a deeply rich moisture
    environment along inverted trof/tropical wave, will focus for some
    2-3"/hr rates and localized totals of possible 5" may result in
    rapid inundation flooding conditions through the afternoon.

    DISCUSSION...GOES-E Visible loop and 17z surface analysis depicts
    a confluent SW to NE axis extending across the Everglades toward
    the southern Space Coast with increasing convective activity
    concentrating along it. Low level tropical moisture exists
    through solid depth with mid 70s in surface and sfc-850mb LPW
    values near 1". This continues through 700mb, but along that
    confluence line/inverted trof, mid-level dry air from the
    northeast in the 700-500mb layer demarcates the boundary even
    further, south of which, the TPW values are over 2.25" nearing
    2.4" locally. Solid early morning sun and limited capping on the
    skinny profiles has brought temperatures well in the mid to upper
    80s and support MLCAPEs of 2000-2500 J/kg even with fairly moist
    adiabatic profiles.=20

    The streamline flow noted in satellite, is generally 10-20kts per
    VWP providing strong moisture flux convergence through depth along
    the axis for scattered to numerous updrafts. Flow aloft is
    reverse to the low level flow providing some vertical shear but
    not ideal for prolonged organized structures but the tilt will
    allow for some upper-level divergence/outflow to maintain stronger
    updrafts. As such, the strength of flux convergence and depth of
    moisture in deep warm cloud (13-15Kft) will support efficient
    rainfall production with capability of 2-3"/hr rates. Cell
    motions suggest east to west transient 15kt cell motions, but
    linear confluence features would support some repeating/training
    to allow for some localized 5"+ totals, with the 16z HRRR even
    suggesting localized totals over 7", so it is not completely out
    of the realm of possibility if training is prolonged/ideal but
    given the nature of the flow is still less likely than more.=20=20 Irrespective, the intensity of the rates into the 3"/hr range
    would still result in localized rapid inundation flooding
    especially in the east coast urban corridor, but also could affect
    portions of Alligator Alley and other cross peninsular roadways.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_7-I_yw0hYy9DAMXPNVB--mZEs64xggjnymLIGIYY67zch5p4NfEQCKBrsaoUZk6JguX= pCX2gehTg30_eJZBXlUMxT4$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 28178090 28128055 27788035 27338016 26907999=20
    26047999 26048056 25998104 26028147 26378168=20
    26928149 27288137 27668127 27898117=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Oct 9 20:37:00 2025
    AWUS01 KWNH 092036
    FFGMPD
    AZZ000-UTZ000-100200-

    Mesoscale Precipitation Discussion 1172
    NWS Weather Prediction Center College Park MD
    436 PM EDT Thu Oct 09 2025

    Areas affected...Northern Arizona...Southern Utah...

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

    Valid 092035Z - 100200Z

    SUMMARY...Increasing coverage of small core thunderstorms embedded
    with moderate shower activity. Localized .5"-.75"/hr rates over
    very flashy basins and multiple south to north rain bands may
    allow for some cross tracks and totals of 1-1.5" resulting in
    localized flash flooding conditions.

    DISCUSSION...Environment is starting to show initial signs of
    waves/bands of convective activity expected through the afternoon.
    CIRA LPW and RAP analysis also denote leading edge of enhanced
    subtropical moisture has grown deep enough to over-top the
    Mogollon Rim and is lifting northward through the San Francisco
    Plateau, Tds in the upper 40s to mid-50s have been noted and
    pockets of total PWats over 1" have started to be
    observed/analyzed. Clear skies has provided ample insolation to
    support increased SBCAPEs 750-1000+ J/kg with rapidly reducing
    CINH capping across the Plateau.

    GOES-W WV shows bulge of ideally anticyclonically curved
    outflow/sub-tropical jet from Priscilla, as well as broadening
    diffluence to its northwest under influence of the approaching
    northern flow/polar jet streak. Current divergence is small but
    effective for the initial band of showers along the AZ/UT border
    with recent uptick in embedded convective showers. The enhanced
    moisture flux and weak convergence associated with the broad scale
    ascent appears to support some rates of .5"/hr so far.

    As the evening progresses, the divergence pattern is expected to
    increase with approach of embedded waves through the sub-tropical
    stream. This will increase overall coverage and the smaller cored
    convection is expected to broaden with upstream redevelopment
    along the Mongollon Rim and volcanic peaks within the broader
    Plateau. General north to north-northeast propagation will allow
    for the potential for multiple bands resulting in random
    intersection with prior rainfall footprints. Localized 1-1.5" are
    possible, though most of the area of concern has naturally very
    low FFG at .5-1"/hr (especially in south-central and SE Utah) and
    less than 1"/3hrs. While overall coverage/totals are not
    expected to be sizable, a random scatter shot of widely scattered
    incidents of flash flooding are clearly possible.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_Cg1SRRfM8bjwrGfmNTYyzPb8aJMeT4Dy58m8lKQlWopQJzdXfGxiJb7Yzd7IeTE32jo= 78vsqHqpbBetEj8iQU53vvI$ for graphic product...

    ATTN...WFO...FGZ...GJT...SLC...VEF...

    ATTN...RFC...STR...NWC...

    LAT...LON 39491037 38740955 37710952 36910977 35921049=20
    35061158 34641310 35111391 36261394 37071312=20
    37621245 38261202 39211140=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Oct 9 21:01:28 2025
    AWUS01 KWNH 092101
    FFGMPD
    AZZ000-NVZ000-CAZ000-100200-

    Mesoscale Precipitation Discussion 1173
    NWS Weather Prediction Center College Park MD
    501 PM EDT Thu Oct 09 2025

    Areas affected...Southern Nevada...Southeast California...

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

    Valid 092100Z - 100200Z

    SUMMARY...Training showers/thunderstorms capable of .5-.75"/hr and
    localized streaks of 1-2" may result in localized flash flooding
    over the next few hours.

    DISCUSSION...CIRA LPW, VWP obs and RAP analysis, shows surge of
    subtropical moisture through the Lower Colorado Valley on 15-20kst
    of south to southeasterly confluent flow. Total PWat values have
    increased to over 1.25". Strong convergence along the tight
    moisture gradient has providing a sufficient differential boundary
    for isentropic ascent. Deep layer profiles are not particularly
    unstable (100-250 J/kg of CAPE) given the mid-level warming, but
    the strength of deep layer moisture convergence generally
    coincident with a combined diffluent portion of the polar and
    subtropical jet noted in GOES-W WV suite was sufficient to allow
    for elevated convective cores to develop, maintain and even expand
    upstream toward the San Bernadino Range. Total Pwats of 1.25"
    and moistening of the sub-cloud is allowing for some increased
    rainfall rates of .5-.75"/hr.=20

    Upstream shortwave energy rounding th western edge of the
    sub-tropical ridge shows some additional cumuliform mid-level
    clouds indicative of upstream energy and potential for further
    upstream redevelopment/back-building environment. As such, with
    deep layer steering generally oriented parallel to the ascent
    boundary there is increasing potential for repeating cores and a
    streak or two of 1-2" totals. Limited soil conditions and low FFG
    values of .75-1.25"/3hrs suggests localized flash flooding is
    possible within this band for the next few hours.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-TjeaugyAH17AL9diwgM5BcLIY8OnJF-Axeu_Gq9oefrHLEt_4bexssdL27yk5C-UbTB= LLkVtwYYZibVHg6AJcdJ3sI$ for graphic product...

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

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 37971501 37571416 36171431 34711595 34491710=20
    35291750 37001667=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Oct 10 01:06:03 2025
    AWUS01 KWNH 100105
    FFGMPD
    FLZ000-100704-

    Mesoscale Precipitation Discussion 1174
    NWS Weather Prediction Center College Park MD
    905 PM EDT Thu Oct 09 2025

    Areas affected...eastern Florida

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

    Valid 100104Z - 100704Z

    Summary...A few hours of heavy rainfall are expected along the
    east coast of Florida tonight. Local rainfall totals of 2-5
    inches can be expected where convection is most persistent. Flash
    flooding is possible in both urban areas and where coastal
    flooding can hinder runoff processes through at least 07Z/3a EDT.

    Discussion...Scattered, deep convection is persistent within a
    strongly confluent low-level regime along the east coast of
    Florida. These storms have initially persisted over open Gulf
    Stream waters, but recent radar mosaic imagery depicts a slight
    uptick in isolated convection over land areas especially just
    north of Melbourne. The storms are in an environment
    characterized by 2+ inch PW values and around 1000 J/kg SBCAPE,
    supporting efficient rainfall processes. Additionally, low-level
    easterlies veering to westerly aloft was promoting slow storm
    motions that - when combined with favorable thermodynamic
    parameters - will ultimately support a few areas of 2 inch/hr rain
    rates at times.

    Both observations and models suggest that the ongoing pattern
    supporting rainfall should evolve very slowly over the next 6
    hours at least. Spots of heavy rainfall (2 inch/hr rain rates)
    should remain common on an isolated to scattered basis -
    especially along coastal areas where updrafts will have access to
    slightly greater instability located just offshore. Areas of 2-5
    inch rainfall totals are expected.

    These rain rates will occur over urbanized areas along the I-95
    corridor from near/north of Daytona southward to around Ft.
    Pierce. Isolated, urbanized flash flooding is possible through
    07Z/3a EDT. Additionally, with onshore flow promoting localized
    coastal flooding and hindering runoff in some areas, flooding
    could become exacerbated by heavier rainfall on a localized basis.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8XwLr0VmFqtMdKnadkE1jKfI_RSgw7DUVPW8r3c0R2Yn7aXQ7B_DWYDXrSHvpIgMitOs= 6x_EYw4DpCV2NdqsCZ-sJsY$ for graphic product...

    ATTN...WFO...JAX...MLB...

    ATTN...RFC...ALR...NWC...

    LAT...LON 29938160 29578066 27977976 27108007 28248124=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 Oct 10 01:43:31 2025
    AWUS01 KWNH 100143
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-100541-

    Mesoscale Precipitation Discussion 1175
    NWS Weather Prediction Center College Park MD
    942 PM EDT Thu Oct 09 2025

    Areas affected...portions of the southwestern U.S.

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

    Valid 100141Z - 100541Z

    Summary...Scattered convection continues to produce isolated backbuilding/training and a few spots of rain rates exceeding 0.5
    inch/hr. Flash flooding is possible on an isolated basis for the
    next few hours (through 06Z/11p PDT).

    Discussion...Scattered convection continues to drift northeastward
    across a broad part of the Great Basin currently.=20
    Stratiform/shallow convection has been noted in many areas,
    although deeper convection with more focused training has resulted
    in an extended period of 0.5 inch/hr rain rates near Pahrump, NV
    and adjacent areas of southeastern California. Convection in that
    area is likely experiencing influence both from increased
    mid-level moisture associated with Priscilla and weak mid-level
    shortwave troughs related to a larger mid/upper wave west of
    California.=20

    Sufficient surface-based instability exists for convection to
    continue occasionally backbuilding/training for a few more hours
    on an isolated basis. Areas of 0.5 inch/hr rain rates should
    continue at times, with training resulting in local 1+ inch
    rainfall totals. Training axes like the one near Pahrump may
    develop on an isolated basis across northwestern Arizona,
    southeastern Nevada, and far southern Utah. Farther south along
    the Lower Colorado River Valley, weaker forcing should continue to
    keep flash flood risk isolated along with somewhat weaker rain
    rates.

    The greatest risk of flash flooding over the next few hours should
    remain focused across southern Nevada, southern Utah, and
    northwestern Arizona through 06Z/11p.=20=20

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-QiGbK05Ojo2s8N5uZuNkYv2PeIMAIJHAhIZtRJ5FIuF-clUTSL0K7Zm8uWjRyTJ3Wzd= TVrZS-UEq--pVNn3fDrcfJQ$ for graphic product...

    ATTN...WFO...FGZ...LKN...PSR...SGX...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 38751243 37611100 35681166 33291308 33181548=20
    34651693 36601644 38201538=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Oct 10 06:55:06 2025
    AWUS01 KWNH 100655
    FFGMPD
    AZZ000-100854-

    Mesoscale Precipitation Discussion 1176
    NWS Weather Prediction Center College Park MD
    254 AM EDT Fri Oct 10 2025

    Areas affected...southern/central Arizona

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

    Valid 100654Z - 100854Z

    Summary...Isolated flash flood potential continues as convection
    drifts north-northeastward across the discussion area. Rain rates
    of around 0.5 inch/hr are possible at times through 11Z/3a PDT.

    Discussion...Scattered shower/isolated thunderstorm activity has
    been persistent for most of the evening, although steady
    north-northeastward movement has tended to keep rain rates in
    check (generally under 0.5 inch/hr). Recent radar/satellite
    indicate a subtle uptick in convection generally from the Phoenix
    area southward to the International Border region that may be tied
    to a weak mid-level wave approaching the area. Subtle confluence
    at both 700mb and 850mb may also be contributing to the modest
    increase in convective activity. Lightning data has also shown an
    uptick in vicinity of the storms. Deep layer flow in excess of 20
    knots will continue to support northward movement of cells,
    although if strengthening continues, areas of localized training
    could bump rain rates into the 0.5 inch/hr range. PW values
    exceeding 1.5 inch and marginal instability (around 500 J/kg
    MUCAPE) are supportive of heavier rainfall with the more dominant
    activity.

    As typical for the region, low-lying areas and burn scars that
    experience heavier rainfall could result in an instance or two of
    flash flooding for the next few hours. The longer-term
    persistence of this activity is in question, however, as
    convergence/confluence may weaken some later tonight (after 10Z).
    As such, a conditional threat for flash flooding could continue
    around southern/central Arizona for the next few hours while cells
    persist.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!47NERrKDkKLc8gVQ6RQtq3skyJR5OUsbbBxPiSBq5oiPm96XNk2Vr0UdUrUIgxn7rMfC= X8NNZNVcSX0F5pMH7umiIF4$ for graphic product...

    ATTN...WFO...FGZ...PSR...TWC...

    ATTN...RFC...STR...NWC...

    LAT...LON 35201135 34631040 32081113 31821276 32391397=20
    34051318=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Oct 10 17:48:52 2025
    AWUS01 KWNH 101748
    FFGMPD
    AZZ000-UTZ000-102230-

    Mesoscale Precipitation Discussion 1177
    NWS Weather Prediction Center College Park MD
    147 PM EDT Fri Oct 10 2025

    Areas affected...central/northern AZ into southern UT

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

    Valid 101745Z - 102230Z

    Summary...Isolated to scattered instances of flash flooding appear
    likely to develop from portions of central and northern AZ into
    southern UT through the afternoon. Hourly rainfall of 0.5 to 1.0
    inches is likely but within axes of training, hourly rainfall over
    1 inch will be possible.

    Discussion...Between 1530-1730Z, regional radar imagery has shown
    an increase in the coverage and intensity of showers and
    thunderstorms extending in a SW to NE axis from central to
    northern AZ. These storms were located within a highly anomalous
    moisture plume, extending downstream of T.S. Priscilla which was
    located west of the Baja Peninsula. OSPO ALPW imagery showed the
    mid to upper level reflection of Priscilla beginning to cross the
    central Baja Peninsula and standardized PWAT anomalies across the
    Desert Southwest were +4 to +5 above the mean with 12Z sounding
    values at VEF (0.92 inches) and FGZ (1.27 inches) well above the
    SPC climatological max for October 10.

    Despite overcast skies, weak solar insolation was helping to boost
    instability across the region with some pockets of 500+ J/kg
    MLCAPE and a broader coverage of 500-1000 J/kg MUCAPE shown on the
    17Z SPC mesoanalysis. Fairly unidirectional southwesterly winds in
    the low to mid-levels will promote area of training where
    confluent 700 mb winds are located from western to central to
    northeastern AZ. RAP forecasts indicate some strengthening of the
    700 mb flow through 00Z which may act to increase coverage of
    cells through the afternoon. Subtle vorticity maxima embedded
    within the southwesterly flow aloft across the lower CO Valley
    will also likely contribute to development of convection over the
    next few hours. A continued increase in instability is expected
    through peak surface heating which will help to support locally
    higher rates which, given the remnant tropical moisture, may
    support sub-hourly rainfall of 0.5 to 1.0 inches in ~30 minutes.
    In addition to heavy rain overlapping with urban areas or burn
    scars, areas of flash flooding will be most likely within slot
    canyons, small streams and normally dry washes.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_fhNyipkb54HKzFWYzeGgKOFZkUl8yibXkLxsmv7AzdcSUPhiVTEU6vbKNW_lNUqbCMW= aZ2pa8pxQgloNG1hzf1UA0A$ for graphic product...

    ATTN...WFO...FGZ...GJT...SLC...VEF...

    ATTN...RFC...STR...NWC...

    LAT...LON 38810953 37960957 35671017 34351135 34111300=20
    35111413 36811378 37651320 38451206 38781062=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 Oct 10 19:43:16 2025
    AWUS01 KWNH 101943
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-110140-

    Mesoscale Precipitation Discussion 1178
    NWS Weather Prediction Center College Park MD
    342 PM EDT Fri Oct 10 2025

    Areas affected...southern CA, southern NV into central UT

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

    Valid 101940Z - 110140Z

    SUMMARY...Thunderstorms are expected to develop and expand in
    coverage over portions of southern CA, southern NV into central UT
    over the next 3-6 hours. Hourly rainfall of 0.5 to 1.5 inches is
    expected along with isolated to widely scattered instances of
    flash flooding.

    DISCUSSION...GOES West visible imagery from 1930Z showed mostly
    clear skies over the desert regions of southern CA into southern
    NV and central UT, northwest of an extensive cloud shield to the
    southeast. This region was located along the northwestern edge of
    an anomalous moisture plume with standardized anomalies of PW
    between 3 and 5 above the mean via the 12Z GFS. SPC mesoanalysis
    data from 19Z showed 500-1000 J/kg MLCAPE across a majority of the
    MPD threat area, but areas of low level inhibition remained,
    especially across southern CA into NV.

    Based on continued heating of the surface and advection of
    moisture seen in OSPO ALPW imagery within the surface to 700 mb
    layer, streaming north of Priscilla in the eastern Pacific,
    further erosion of convective inhibition is expected through the
    remainder of the afternoon. Convective development appears likely
    within the next 1-2 hours, first over areas of higher terrain and
    then spreading into the lower elevations with time. Some
    augmentation of divergence aloft, within the right-entrance region
    of a developing upper level jet max over southern NV will be
    possible, aiding in the general forcing for ascent.

    Unidirectional flow, generally from the southwest, will promote
    areas of repeating and short term training within subtle low level
    confluent axes. Coverage of cells may only become widely scattered
    but the moisture-rich environment will promote efficient rainfall
    production with 0.5 to 1.5 inches of rain in an hour expected.
    These high rain rates are likely to result in at least isolated
    areas of flash flooding, with a particular focus across any
    population centers and burn scars, while otherwise impacting any
    low lying and normally dry stream beds.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8n0YZyRg_lRWv0PSZqz8psF9S-5A5bx8N5kI8ye1FG0rnFnmrsk281Y6QRNxwz1PmToJ= 1se-mmr7K4vc6iZuzvl_2ew$ for graphic product...

    ATTN...WFO...GJT...LKN...PSR...SGX...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 39891291 39781057 39280943 38760947 38571076=20
    38211182 37571281 36281369 34951444 34281507=20
    33701587 33911680 34441741 35521712 36691669=20
    39011531=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Oct 10 22:35:20 2025
    AWUS01 KWNH 102235
    FFGMPD
    NMZ000-AZZ000-CAZ000-110330-

    Mesoscale Precipitation Discussion 1179
    NWS Weather Prediction Center College Park MD
    634 PM EDT Fri Oct 10 2025

    Areas affected...lower CO Valley into central/northeastern AZ and
    northwestern NM

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

    Valid 102230Z - 110330Z

    Summary...Isolated to widely scattered areas of flash flooding
    will be possible from the lower CO River Valley across central AZ
    into northwestern NM through 04Z. Hourly rainfall of 0.5 to 1.0
    inches is likely within stronger cores and isolated hourly totals
    in excess of 1 inch will be possible.

    Discussion...GOES West water vapor and OSPO ALPW imagery at 22Z
    showed mid to upper level moisture from Post-T.C. Priscilla
    streaming northeastward across the northern Baja Peninsula/Gulf of
    California. Regional radar imagery showed a few stronger
    reflectivity cores moving northward from Mexico into southeastern
    CA and southwestern AZ, co-located with the upper level moisture
    plume advancing into the region. Farther north, a broken SW to NE
    axis of showers/thunderstorms extended from southwestern AZ into
    northeastern AZ, along a remnant differential heating boundary and
    along the White and San Francisco Mountains. Despite the highly
    anomalous moisture plume in place across the entire Southwest
    region, instability has been rather fragmented due to extensive
    cloud cover limiting the coverage of higher rainfall rates up
    until this point.

    However, given the pockets of relatively higher MLCAPE that exist,
    according to 22Z SPC mesoanalysis data, some locally higher
    rainfall rates can be expected over the next 3-5 hours. 22Z SPC
    mesoanalysis showed 500-1000 J/kg over portions of eastern AZ into
    northwestern NM and into southwestern AZ, albeit with varying
    degrees of inhibition. As the mid and upper level energy and
    moisture plume from Priscilla continues to advance downstream
    across the Southwest, the potential for increased rainfall
    efficiency will exist within low level axes of confluence. These
    axes of confluence will occasionally align with the deeper layer
    mean steering flow from the SW, supporting repeating and training
    of heavy rain cores. Isolated to widely scattered hourly rainfall
    of 0.5 to 1.5 inches will be possible, generating possible flash
    flooding, especially if overlap occurs with an axis of 1 to 3+
    inches which has fallen over the past 24 hours from near Phoenix, north-northeastward across I-40. In terms of coverage, if recent
    WoFS cycles are any indication, 6-hr probabilities of exceeding 1
    inch are less than 40 percent and quite isolated across AZ into
    northwestern NM.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4M6w_YQ7TUizrI6ojZcY1oE6sc2O0vb4mcFnty_hSt-Uwhh2PFR9h_3IfCbc_h14VgeB= 3S7PWx8ftXhr6vXBYW69jWQ$ for graphic product...

    ATTN...WFO...ABQ...FGZ...PSR...TWC...VEF...

    ATTN...RFC...FWR...RSA...STR...NWC...

    LAT...LON 36220988 36120807 35090798 34030943 32581118=20
    32061270 32181445 32741528 34131506 35341290=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 11 01:53:51 2025
    AWUS01 KWNH 110153
    FFGMPD
    AZZ000-UTZ000-NVZ000-CAZ000-110552-

    Mesoscale Precipitation Discussion 1180
    NWS Weather Prediction Center College Park MD
    953 PM EDT Fri Oct 10 2025

    Areas affected...southern Nevada, northwestern Arizona, southern
    Utah, and far southeastern California

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

    Valid 110152Z - 110552Z

    Summary...Flash flooding remains likely across the discussion
    area, with locally significant impacts noted near the Las Vegas
    area.

    Discussion...Scattered convection continues to migrate
    northeastward along an axis from near Las Vegas metro
    northeastward to near St. George, UT. The cells remain embedded
    in an environment characterized by abundant moisture 1-1.75 inch
    PW values and sufficient surface-based instability for robust
    updrafts (1000 J/kg SBCAPE). Despite appreciable cell motions
    (around 20-30 knots), these cells were producing areas of 0.5-0.75
    inch/hr rain rates - enough to prompt local flash flood
    occurrences near the Las Vegas metro area. Localized training is
    also aiding in promoting higher rain rates on a localized basis.

    The ongoing scenario for flash flooding should continue for at
    least a few more hours. Low-level southerly advection beneath an
    expansive rain shield across the CA/AZ border region (Lower
    Colorado River) has stabilized the airmass in that area, and some
    of this stable air may work into the discussion area from the
    south. This stabilization, combined with nocturnal boundary layer
    cooling, should result in a gradual weakening trend with most
    convection through 06Z/11p PDT. Despite the anticipated weakening
    trend, the overall synoptic environment (with forcing from
    Priscilla's remnants to the south and a larger-scale upper trough
    near northwestern California) may continue to favor isolated
    convection (and localized flash flooding) where surface-based
    instability remains.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7Jdk6OFcssdUL7VS0etkLp9eFcyqu60lBp3b6XIlLWIh9tEK6kdMQ5NReK5L-dQaWucF= YG37iFyInTAiKcPtjCcDujg$ for graphic product...

    ATTN...WFO...FGZ...LKN...SLC...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 39071213 38351111 36601219 34201531 35791688=20
    37251612 38791414=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 11 03:30:18 2025
    AWUS01 KWNH 110329
    FFGMPD
    AZZ000-CAZ000-110928-

    Mesoscale Precipitation Discussion 1181
    NWS Weather Prediction Center College Park MD
    1129 PM EDT Fri Oct 10 2025

    Areas affected...much of Arizona

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

    Valid 110328Z - 110928Z

    Summary...Flash flood potential continues as remnants of Priscilla
    approach Arizona. Heavy rainfall will become more widespread for
    a few hours tonight, causing instances of flash flooding.

    Discussion...Mid-level remnants of Priscilla are approaching
    Arizona from the southwest. Ascent associated with the remnant
    system has resulted in widespread shower and isolated thunderstorm
    activity across western and central sections of the state along
    with 0.5-2.5 inch rainfall totals. The downstream airmass across
    the discussion area remains abundantly moist (PWs ranging from 1
    inch in the north to 2.1 inches southwest). Surface-based
    instability is maximized across southwestern parts of the state
    (1000 J/kg SBCAPE) and becomes minimal with northeastward extent.
    The environment continues to support widespread light rain along
    with locally heavier rain rates. Per the latest MRMS data, a few
    spots along the CA/AZ border and in terrain-favored areas of
    central AZ have exhibited rain rates approaching 0.5 inch/hr.

    Ongoing trends are expected to continue through the overnight
    hours. Precipitation may increase in intensity in a few areas as
    ascent from Priscilla approaches from the southwest. The heaviest
    rain rates will materialize as convective cells interact favorably
    with moisture/instability across southern sections of the state
    and orographic ascent locally raises rain rates near the Mogollon
    Rim. Rain rates approaching 0.5-0.75 inch/hr remain a good bet on
    at least an isolated basis over the next 6 hours (through 09Z/2a
    PDT). Areas of excessive runoff and flash flooding are expected.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-s4mU2M4gKkfDKiII_txtBqRkRtjtGn3Pp4nG-GTR18GdfHaa_HQcp_3IdlOPjILY1yB= BmiaVG0D3r5YSkvOuuR8Wqc$ for graphic product...

    ATTN...WFO...FGZ...PSR...TWC...VEF...

    ATTN...RFC...STR...NWC...

    LAT...LON 36461134 35660954 33490958 31771059 31851301=20
    32741462 34551414 35311358=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 11 19:02:04 2025
    AWUS01 KWNH 111901
    FFGMPD
    NMZ000-AZZ000-120100-

    Mesoscale Precipitation Discussion 1182
    NWS Weather Prediction Center College Park MD
    301 PM EDT Sat Oct 11 2025

    Areas affected...southeastern AZ into western/central NM

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

    Valid 111900Z - 120100Z

    Summary...Isolated flash flooding will be possible through 01Z (7
    PM MDT/6 PM MST) across southeastern AZ into western and central
    NM. Hourly rainfall of 0.5 to 1.0 inches is expected where showers/thunderstorms align and train, and isolated spot storm
    totals near 2 inches will be possible.

    Discussion...GOES West water vapor imagery showed a lead shortwave
    trough extending from western CO into northern NM tracking toward
    the east, associated with light to occasionally moderate rainfall.
    Southeast of this feature, visible imagery showed a mixture of
    clouds and mostly clear skies from southeastern AZ into central
    NM. The environment across the region contained highly anomalous
    moisture, with contributions from the tropical east Pacific,
    represented by +3 to +4 standardized anomalies of PWAT. While
    there was drier air aloft, the 18Z sounding from TUS contained a
    PWAT of 1.66 inches (well above the climo max for mid-October) and
    250 J/kg MLCAPE with a stable warm layer centered near 800 mb.
    Where better heating is occurring across the region, instability
    is likely a bit higher with 18Z SPC mesoanalysis data showing 500+
    J/kg over much of southeastern AZ.

    Continued heating over the next few hours is expected to support
    MLCAPE of 500-1500 J/kg later this afternoon over southeastern AZ,
    with values closer to 500 J/kg into portions of NM. While a few
    thunderstorms have been noted within a few disorganized cells
    moving into western NM, additional development is anticipated with
    better heating and weak forcing ahead of the aforementioned
    shortwave and broader height falls ahead of a large upper trough
    moving into the western U.S. In addition, an organizing upper jet
    near 300 mb is expected to provide some added support in the form
    of divergence and diffluence within its right entrance region over
    the southern AZ/NM border.

    As cells increase in coverage, mean WSW flow could promote some
    repeating and brief training of cells into the early evening
    hours. Expected hourly rainfall of 0.5 to 1.0 inches is expected
    which may result in some isolated flash flood issues atop
    sensitive terrain, normally dry washes and/or remnant burn scars
    widely scattered across the region.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8vCZEOPLBt_AWvq-2nEyqh9zBSynSEPL7AVgbfrlDg9vDEXhDd7I6VQtGBAeZrEsTFKK= 6zVrJVaJlhNaoqRmjngsdDg$ for graphic product...

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

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 36230587 36050524 34620519 32930553 32410667=20
    31830775 31230822 31160914 31091108 31621185=20
    32611165 33581051 34680912 35800739=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 12 05:14:44 2025
    AWUS01 KWNH 120514
    FFGMPD
    TXZ000-NMZ000-120912-

    Mesoscale Precipitation Discussion 1183
    NWS Weather Prediction Center College Park MD
    113 AM EDT Sun Oct 12 2025

    Areas affected...far west Texas, extreme southern New Mexico

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

    Valid 120512Z - 120912Z

    Summary...Conditional flash flood potential exists around the El
    Paso, TX area for the next few hours.

    Discussion...Deep tropical convection associated with the remnants
    of Raymond continue to stream from northwestern Mexico into far
    west Texas currently. Recent radar/MRMS observations depict
    training/repeating with a recent uptick in convective intensity in
    a cluster about 35 miles southwest of El Paso. Rain rates remain
    modest, however (around 0.25 inch/hr), but an uptick in rates has
    been noted southwest of El Paso also. The cells are in an
    abundantly moist environment with 1.3-1.6 inch PW values.=20
    Additionally, 1000 J/kg MUCAPE was sustaining stronger updrafts
    and likely resulting in the convective uptick noted in recent
    radar trends.

    These cells are likely to persist northeastward into the El Paso
    area over the next 2-4 hours. Rain rates may be marginal for
    flash flooding, although urban impacts in/near El Paso appear to
    be possible. Rain rates may both 1) exceed 0.5 inch/hr and 2)
    persist for longer than an hour, both supportive of excessive
    rainfall potential.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4uTcT5x5bOUWNZ6xNC_M0PQQni-ylZF99KF4dcC-e-UpbGBmZ9ZnOAIgL_ENvhR_QDJb= HyBxkQsydWHXrkGj-D_bCgY$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 32780684 32610532 31840485 30350475 31490627=20
    31730817 31380832 31570901 32220855=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 12 05:38:41 2025
    AWUS01 KWNH 120538
    FFGMPD
    AZZ000-UTZ000-NVZ000-121037-

    Mesoscale Precipitation Discussion 1184
    NWS Weather Prediction Center College Park MD
    137 AM EDT Sun Oct 12 2025

    Areas affected...northwestern Arizona, southern Utah

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

    Valid 120537Z - 121037Z

    Summary...Scattered thunderstorms are quickly developing across
    the discussion area and producing 0.5-1.0 inch/hr rain rates. A
    few instances of flash flooding are possible.

    Discussion...Robust thunderstorm activity is being forced by the
    approach of a stout mid-level disturbance over Nevada currently.=20
    The storms are embedded within a warm/moist axis along the
    Colorado River, with 0.7-0.9 inch PW values and a narrow axis of
    1000 J/kg SBCAPE along the Nevada/Arizona border area.=20
    Convergence within this axis was also supporting ongoing updrafts.
    The storms were embedded in relatively fast deep layer flow
    (approaching 50 knots per objective analyses), resulting in quick
    storm motions. Localized backbuilding and training were the likely
    mechanisms for enhancing local rain rates.

    Unfortunately, these rates were falling in/near areas prone to
    flooding, with slot canyons and local burn scars noted in the
    area. Ongoing trends are expected to continue for at least a few
    hours. Fast eastward storm motions may tend to carry some of the
    convection eastward toward a slightly drier airmass with weaker
    buoyancy, resulting in weakening. Meanwhile, some backbuilding
    may occur within the remaining warm/moist axis in northwestern
    Arizona, contributing to a localized flash flood threat there.=20
    Models suggest that this convective threat should be relatively
    short-lived, ending by 09-10Z as cooler/drier air filters into the
    discussion area from the northwest.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_0SwQEhlfDReAPwWpzIzQjUrALF3GxWI77foRe-9F-okottKbSMgqIipQ7bHdyOkUkPX= -mHgrcbUliWrMtohKG6aF_A$ for graphic product...

    ATTN...WFO...FGZ...SLC...VEF...

    ATTN...RFC...STR...NWC...

    LAT...LON 38091207 37391099 35451202 34491323 34561438=20
    35911468 37381378=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 12 08:12:16 2025
    AWUS01 KWNH 120812
    FFGMPD
    AZZ000-121411-

    Mesoscale Precipitation Discussion 1185
    NWS Weather Prediction Center College Park MD
    411 AM EDT Sun Oct 12 2025

    Areas affected...southern/central Arizona

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

    Valid 120811Z - 121411Z

    Summary...Showers and isolated thunderstorms will continue to
    increase in coverage through at least 13Z/7a MST this morning.=20
    Areas of flash flooding are expected during that timeframe.

    Discussion...Larger-scale ascent was beginning to overspread much
    of the Southwest due to a stout mid-level wave centered over
    Nevada and northwestern Utah. Meanwhile, a pool of 1000 J/kg
    SBCAPE and weak inhibition has supported development of scattered
    thunderstorms from the Phoenix area east to near Globe. The
    storms are embedded in a moist airmass (1.1-1.5 inch PW values),
    supporting rain rates at or above 1 inch/hr in the strongest
    cells. Relatively quick movement has been noted owing to 40 knots
    of mean steering flow. However, as cells continue to expand in
    coverage and intensity, local mergers and backbuilding should also
    bump rain rates to above 1 inch/hr at times. The flash flood
    risk will increase as a result.

    Models/CAMs suggest that the greatest concentration of
    thunderstorm activity will reside along and just south of the
    Mogollon Rim through 13Z/7a MST this morning. This includes the
    Phoenix Metro area. Much of the discussion area remains well
    ahead of any low-level boundaries that could stabilize this
    airmass, and with continued ascent/height falls over the region,
    flash flood potential will likely extend beyond 13Z/7a MST. Both
    urban and sensitive/low-lying areas will have the greatest flash
    flood risk.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5KHFFKLCfKHP79HS4HKsVvL2N0a3s-xJb_9m1OwSChAQUXuANbCvsiVKZ0v7LtkRGvIq= u6ucjJEG3YhQQhL9CEz7PrU$ for graphic product...

    ATTN...WFO...FGZ...PSR...TWC...

    ATTN...RFC...STR...NWC...

    LAT...LON 34471072 34050941 32830932 31381045 31801316=20
    32601435 33471431 33951357 34201246=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 12 12:01:51 2025
    AWUS01 KWNH 121201
    FFGMPD
    SCZ000-121530-

    Mesoscale Precipitation Discussion 1186
    NWS Weather Prediction Center College Park MD
    801 AM EDT Sun Oct 12 2025

    Areas affected...central/northern SC coast

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

    Valid 121159Z - 121530Z

    Summary...Localized high rain rates will continue a localized
    flash flood threat for the central and northern coastline of SC
    for another few hours. Hourly rainfall of 2-3 inches can be
    expected at times.

    Discussion...Localized heavy rain in and southeast of Georgetown
    has resulted in MRMS estimates of 6 to 10 inches since midnight,
    with a few Wunderground.com observations showing 6-7 inches in the
    city and along the coast. A strong surface low (991 mb) has been
    slow moving and was analyzed 115 miles east of Georgetown at 11Z
    and a slow moving low level convergence axis has focused an area
    of heavy rain containing hourly rainfall between 2-3 inches over
    coastal Georgetown County over the past couple of hours. While
    some weakening has occurred, VAD wind data showed ~50 kt of
    925-850 mb winds oriented from the northeast, parallel to the
    coast at KTLX, veering to a weaker and more perpendicular
    orientation at KCLX. Aloft, a potent divergence maximum was
    located along the coast of the Carolinas within the left-exit
    region of a 90-100 kt jet streak, east of an upper low located
    over the FL/GA border.

    Short term RAP forecasts show the surface low finally begins to
    make some northward progress over the next 6 hours along with a
    disruption to the nearly stationary low level convergence axis due
    to further weakening of the low level flow over southern NC and
    veering of the low level winds along the central SC coast over the
    next few hours. This should allow hourly rainfall values to lessen
    while translating southward through 15Z. Until then however,
    continued slow movement of heavy rain will maintain a localized
    flash flood threat along the Grand Strand with additional rainfall
    of 3 to 6 inches possible before expected weakening of rainfall
    intensities.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9M6bl6rYLJauILWID5zfksfrEPk_qS1vLL9uhykKPT9FQF1fRT8Ctn6Vte8xF_bVNp0Y= 77fIcq5-CJ3JROmH5IY1qzk$ for graphic product...

    ATTN...WFO...CAE...CHS...ILM...

    ATTN...RFC...ALR...NWC...

    LAT...LON 33947966 33887900 33737869 33557848 33107858=20
    33007873 32907930 33058024 33238047 33468048=20
    33698029 33888006=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 12 14:02:49 2025
    AWUS01 KWNH 121402
    FFGMPD
    NMZ000-AZZ000-121830-

    Mesoscale Precipitation Discussion 1187
    NWS Weather Prediction Center College Park MD
    1001 AM EDT Sun Oct 12 2025

    Areas affected...central/southern AZ into western NM

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

    Valid 121400Z - 121830Z

    SUMMARY...Scattered Thunderstorms are likely to continue a few
    areas of flash flooding across central/southern AZ over the next
    3-5 hours, possibly extending into western NM. Hourly rainfall
    over 1 inch will be found within areas of training.

    DISCUSSION...1330Z radar imagery across south-central AZ showed
    scattered thunderstorms, with a history of backbuilding and
    training, despite individual cell motions off toward the ENE at
    20-30 kt. OSPO ALPW imagery showed that the cells were located
    just ahead of a slow moving, north-south oriented, 850-700 mb
    moisture gradient found over the lower CO River Valley with
    notable directional shear between the KYUX and KIWA 850 mb wind
    vectors. The moisture plume over AZ remained anomalously high with contributions from former T.C. Raymond in the eastern Pacific. SPC
    mesoanalysis data from 12Z estimated PWAT values between 1.0 and
    1.5 inches over the southern half of AZ along with 500-1000 J/kg
    MLCAPE over south-central to southwestern AZ. In addition, AZ was
    situated within the right-entrance region of a 130+ kt upper level
    jet max extending from southern NV into northwestern CO.

    RAP forecasts over the next 3-6 hours show weakening 850-700 mb
    moisture transport into southern AZ but some increase in
    instability is expected over southwestern AZ due to the onset of
    daytime heating and continued jet-induced divergence aloft will
    remain. So while there are some conflicting signals for continued
    thunderstorm generation, lingering forcing for ascent should
    maintain thunderstorm formation over southwestern to south-central
    AZ over at least the next 2-4 hours. Mean steering flow from the
    WSW will continue periods of training as some backbuilding
    continues to occur, resulting in hourly rainfall of at least 0.5
    to 1.0 inches, but idealized training could result in 1-2 inches
    in an hour. A few areas of flash flooding are likely to continue,
    especially within the near-saturated ground conditions across the
    I-8 and I-10 corridors to the SSW of Phoenix.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7CvMA4CCxnaj_imwspYmaKZ96HLsNeVMrki7GJBp4PWN5OG2h-rTDQx7H_mf8HNXVA86= 8E44IHoniiUZxA8NDcsDLso$ for graphic product...

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

    ATTN...RFC...STR...NWC...

    LAT...LON 34750934 34160876 33390883 32380957 31781075=20
    31521189 31641255 32091427 33051418 33751272=20
    34511103=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 12 16:31:52 2025
    AWUS01 KWNH 121631
    FFGMPD
    NCZ000-SCZ000-122200-

    Mesoscale Precipitation Discussion 1188
    NWS Weather Prediction Center College Park MD
    1230 PM EDT Sun Oct 12 2025

    Areas affected...northern SC coast into southern NC coast

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

    Valid 121629Z - 122200Z

    Summary...Localized flash flooding will remain a concern along the
    northern coast of SC into the southern coast of NC into the
    mid-afternoon hours. High rain rates of 2 to 3 in/hr are expected
    at times, which may overlap with wet soils across the Grand Stand
    region and/or the Wilmington metro.

    Discussion...Visible satellite imagery showed that a surface low
    offshore of the NC/SC coast has moved a little north since 12Z and
    was estimated to be 993 mb and ~90 miles east of North Myrtle
    Beach at 16Z. A strong axis of low level convergence southwest of
    the surface low continued to focus an area of heavy rain along the
    coast of Horry County, with local Wunderground observations
    showing hourly rainfall of 1-2 inches since 13Z and 2-5 inches of
    rain since midnight. Strong convergence also existed north of the
    low along and just offshore of the southern NC coast along an
    occluded frontal boundary as seen in visible satellite imagery.
    Despite the strong convergence along the NC coast and 500-1000
    J/kg MLCAPE, deep convection has been lacking. In addition to this
    area being beneath the dry slot of the cyclone as seen on water
    vapor imagery, the 12Z sounding from MHX is telling, indicating a
    warm nose at 675 mb, capping the otherwise weakly unstable
    sounding.

    Short term RAP forecasts show the surface low will continue a slow
    northward motion through 00Z with an elevated instability gradient
    hugging the NC coast, with 1000+ J/kg just offshore but quickly
    lowering to <500 J/kg for inland locations. Low level convergence
    to the southwest of the surface low will likely continue to focus
    heavy showers/thunderstorms with 1 to 2+ in/hr rainfall for
    another couple of hours, despite weak instability. This area may
    drift or refocus just north of its present position.

    Farther north toward Cape Lookout, it would only take cooling of
    ~2 C within the warm nose noted on the MHX sounding to support the
    production of deep convection which would be capable of hourly
    rainfall between 2 and 3 inches given the forecast of near
    stationary movement of the coastal convergence axis. While this
    development would be highly conditional, it is worth highlighting.

    Therefore, while localized, a flash flood threat will remain
    likely from the northern SC coast into the southern NC coast
    through 21 to 22Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-MGmYAWFLP-8h-N2F2SLpu7JCGZPpXWLFV4r3tDZoxOW7cV0nQYMFNcr8PGC8l-ePmiE= UAiROu1FlKZ5wG-PtqmGJDw$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 35057725 34887687 34707655 34447646 34227663=20
    33727769 33157852 33087933 33497983 33887982=20
    34417925 34737862 35047795=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 12 18:29:53 2025
    AWUS01 KWNH 121829
    FFGMPD
    NMZ000-AZZ000-130025-

    Mesoscale Precipitation Discussion 1189
    NWS Weather Prediction Center College Park MD
    229 PM EDT Sun Oct 12 2025

    Areas affected...southwestern to south-central to southeastern AZ

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

    Valid 121828Z - 130025Z

    SUMMARY...Isolated to scattered flash flooding appears likely to
    continue over portions of southwestern to south-central to
    southeastern AZ through 00Z. Rainfall of 1 to 2 inches in 1 hour
    or less time should be expected within training of stronger cells.

    DISCUSSION...GOES West water vapor and visible satellite imagery
    at 18Z showed thunderstorms forming just ahead of the southeastern
    leading edge of a longwave trough over the western U.S., and
    within the right-entrance region of an associated 130-150 kt upper
    level jet max over northern AZ into UT and western CO. A WSW to
    ENE axis of thunderstorms has been persistent over the past
    several hours from southwestern AZ to locations just south of the
    Mogollon Rim in eastern AZ. These storms were forming within
    500-1500 J/kg MLCAPE and PWATs of 1.0 to 1.5 inches per 18Z SPC
    mesoanalysis data. Also of note, visible imagery showed a surface
    low over the northern Gulf of California, with warm/moist air
    feeding northward to the east of the surface low into northwestern
    Sonora and southern Yuma County.

    Over the next few hours, thunderstorms are expected to continue
    regenerating over southwestern AZ, with low level moisture
    transport on the eastern side of the Gulf low, with individual
    cell movement toward the ENE. Farther to the east, visible imagery
    showed outflow propagating southward from Pinal and southern
    Maricopa counties into northwestern Pima County. Surface heating
    between breaks in cloud cover over south-central and portions of
    southeastern AZ should allow for increasing instability with peak
    heating this afternoon. Development of additional storms along
    outflow and diurnal development along areas of higher terrain,
    south of the ongoing WSW to ENE axis to the north, should increase
    thunderstorm coverage through 21Z-00Z.

    The combination of these several different forcing mechanisms
    should support scattered coverage of thunderstorms through the
    afternoon along with isolated to scattered coverage of flash
    flooding with hourly rainfall totals maxing out in the 1 to 2 inch
    range and potential for isolated totals near 3 inches.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7oN7bYhG37msCKXOgYR3jbNNsmojlcqoqFccUKN3uUyV6GLvhIHTFLF6BVQ2Y-Ux3gjy= rmnzjmZ1qqBXuMYwNMp7KRg$ for graphic product...

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

    ATTN...RFC...STR...NWC...

    LAT...LON 34011025 33890934 33000896 32010906 31380965=20
    31111064 31291187 31921376 32161455 32591460=20
    32891345 33711147=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 12 22:02:28 2025
    AWUS01 KWNH 122202
    FFGMPD
    NCZ000-SCZ000-130400-

    Mesoscale Precipitation Discussion 1190
    NWS Weather Prediction Center College Park MD
    600 PM EDT Sun Oct 12 2025

    Areas affected...Northeast SC...Southern NC

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

    Valid 122200Z - 130400Z

    SUMMARY...Highly concentrated areas of heavy rainfall will
    continue to foster flash flooding impacts, some potentially
    significant, across portions of northeast SC and southern NC going
    into the evening hours.

    DISCUSSION...A strong coastal low continues to positioned just
    offshore of southeast NC to the east of Wilmington. A combination
    of this and the relatively strong area of high pressure over
    southeast Canada continues to channel a strong and very moist
    low-level jet into the western flank of the low center where there
    is currently a strongly forced environment for heavy rainfall and
    embedded convection.

    The 850/925 mb flow across southeast NC and into adjacent areas of
    far northeast SC is on the order of 40 to 50 kts. This is yielding
    strong moisture convergence which coupled with a nose of modest
    instability with MUCAPE values of 250 to 500 J/kg and notable
    divergence aloft for deep layer ascent is continuing to foster
    highly concentrated areas of very heavy rainfall.

    In fact the last radar imagery shows an axis of extremely heavy
    rainfall with embedded thunderstorms impacting Columbus County in
    southeast NC, and wrapping westward into Horry and Dillon Counties
    of northeast SC. Rainfall rates are currently on the order of 1.5
    to 2.5 inches/hour across these areas, and some rainfall totals
    here of 3 to 6 inches have occurred in the last 6 hours alone.

    Fortunately, the heaviest rains have pulled away from areas of
    northeast SC (especially along the Grand Strand) that were hard
    hit this morning and midday from very heavy rainfall totals, but
    the slow movement and concentrated nature of the current activity
    near the SC/NC border will support notable concerns in the
    near-term for additional heavy to extreme rainfall amounts. An
    additional 3 to 6 inches of rain will be possible at least locally
    this evening, and this will favor additional areas of flash
    flooding, some of which may be locally significant.

    By later this evening, the surface low should begin to weaken as
    the low becomes more vertically stacked, and this will allow for
    the deeper layer ascent to subside along with the rainfall rates.
    Therefore, conditions are expected to gradually improve later
    tonight.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4L8ZzFVuIyGn9B93YrY6I7bclVPXxiM0vD4PqVPCOyRwbcANCiayCfYMOHLE0e-0QMqj= t96ZY9h5wCl_OqufwQHJsHE$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 34927906 34877804 34537752 33917775 33647859=20
    33087923 33298005 33948033 34537994=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 13 00:18:30 2025
    AWUS01 KWNH 130018
    FFGMPD
    NMZ000-AZZ000-130515-

    Mesoscale Precipitation Discussion 1191
    NWS Weather Prediction Center College Park MD
    815 PM EDT Sun Oct 12 2025

    Areas affected...Southern AZ

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

    Valid 130015Z - 130515Z

    SUMMARY...Scattered areas of heavy showers and thunderstorms are
    expected to continue through the evening hours. Additional areas
    of flash flooding will be possible.

    DISCUSSION...There continues to be the redevelopment of locally
    heavy showers and thunderstorms across much of southern AZ, with
    the late-day GOES-W IR satellite imagery showing scattered areas
    of moderately cold-topped convection. The activity continues to be
    fostered by an unstable and moist boundary layer characterized by
    MLCAPE values of 1000 to 2000 J/kg along with presence of
    favorable right-entrance region upper-level jet dynamics.

    Moisture remains well-entrenched across the region with PWs of
    1.25 to 1.5+ inches which for this time of the year are a solid 3
    to 4 standard deviations above normal. Some of the moisture at
    least in the low-levels across southern AZ is being aided by
    southerly flow off the very warm and moist northern Gulf of CA
    which has been facilitated by placement of a weak area of low
    pressure and an associated surface trough.

    This moisture coupled with the instability continues to support
    convection capable of producing high rainfall rates of 1 to 2
    inches/hour. Additionally, there is a fair amount of effective
    bulk shear overhead with magnitudes of 30 to 40+ kts. This coupled
    with the instability has been yielding some organized convective
    structures with enhanced updrafts and thus sustainment of heavier
    rainfall rates.

    The loss of daytime heating suggests at least a gradual weakening
    trend of convection by later this evening, but at least for the
    near-term, there should continue to be sufficient levels of at
    least modest deep layer jet-aided ascent and instability for
    scattered showers and thunderstorms to persist. Local orographics
    involving areas of terrain will also facilitate pockets of
    convective sustenance.

    Additional rainfall totals by late this evening may reach 2+
    inches where any convective cells persist or locally repeat over
    the same area. This may drive some additional pockets of flash
    flooding which will mainly be a concern for the normally dry
    washes, but could also involve some localized urban impacts around
    the Tucson metropolitan area.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-YEL2OR_R9nVQKu6jESrZY6TyJn6HIQPQyFv9I-sxKXKZtGhC_v6tKrAWMpvr3SV9Ayr= BlzC6WR-t86FsYtTyHMzgj0$ for graphic product...

    ATTN...WFO...EPZ...PSR...TWC...

    ATTN...RFC...STR...NWC...

    LAT...LON 32860959 32520906 31880894 31470910 31220981=20
    31221119 31341186 31741295 32181308 32541273=20
    32661217 32671099=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 13 19:09:12 2025
    AWUS01 KWNH 131909
    FFGMPD
    NMZ000-AZZ000-140100-

    Mesoscale Precipitation Discussion 1192
    NWS Weather Prediction Center College Park MD
    308 PM EDT Mon Oct 13 2025

    Areas affected...Central and Eastern AZ...Western NM

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

    Valid 131908Z - 140100Z

    SUMMARY...Showers and thunderstorms with locally heavy rainfall
    rates coupled with moist antecedent conditions and elevated
    streamflows will pose a threat for isolated to scattered areas of
    flash flooding going through the afternoon hours.

    DISCUSSION...GOES-W visible satellite imagery shows a substantial
    amount of cloud cover across southeast AZ and southwest NM in
    association with broken areas of showers and a few thunderstorms.
    Meanwhile, a bit more clearing and stronger diurnal heating as a
    result is seen across central AZ into some adjacent areas of
    west-central NM. This includes portions of the Mogollon Rim.

    The latest RAP analysis does show as much as 500 to 1000 J/kg of
    MLCAPE pooling near and just southwest of the Mogollon Rim, and
    this coupled with additional boundary layer heating should help
    support the development and expansion of showers and thunderstorms
    across the orographically favored higher terrain and especially
    the south-facing slopes.

    In general, much of the region is seeing at least some deeper
    layer ascent via favorable right-entrance region upper-jet
    dynamics. This is occurring downstream of an amplifying trough and
    associated closed low along the West Coast. This forcing will
    complement the uptick in instability and orographics for a more
    expansive convective footprint across central and eastern AZ and
    into western NM going through the afternoon hours.

    The convective activity over southeast AZ and southwest NM has at
    least some weak support from mid-level vort energy traversing the
    region, and while this will tend to mitigate the instability
    profiles in the short-term, it will favor there being some
    differential heating boundaries that could support convective
    initiation around the periphery of the deeper cloud canopy.

    Many of the 12Z HREF members and other experimental NSSL-driven
    MPAS solutions support there being an uptick in instability-driven
    convection across areas of south-central AZ including the Mogollon
    Rim in particular between 21Z and 00Z. Given the instability and
    moderate levels of effective bulk shear, the uptick in convection
    may include some organization with sustainably strong updrafts.
    Given the anomalously moist environment, some rainfall rates of up
    to 1.5+ inches/hour will be possible.

    Some 2 to 3 inch rainfall totals may occur locally where any
    repeating cell-activity materializes and also into the terrain
    with more favorable orographics. This coupled with moist
    antecedent conditions and locally elevated streamflows from recent
    rainfall may pose a threat for isolated to scattered areas of
    flash flooding this afternoon. This will include potential impacts
    to arroyos and burn scar locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ogxy5DCi9cWIQbhXhCaUHZOuco2FCVpE5gdOn5PZICmwxpn6_kH2mvyrJIjwda-6BFn= 8t4CMV3jHgCPm3smO2odUjs$ for graphic product...

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

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 35900735 35510682 34780671 33510733 31940754=20
    31230863 31211049 31611134 32761208 33341260=20
    34111268 34771208 34961080 34660940 34920852=20
    35740795=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 13 22:31:44 2025
    AWUS01 KWNH 132231
    FFGMPD
    COZ000-NMZ000-AZZ000-140430-

    Mesoscale Precipitation Discussion 1193
    NWS Weather Prediction Center College Park MD
    630 PM EDT Mon Oct 13 2025

    Areas affected...Central/Eastern AZ...Western/Central
    NM...Southwest CO

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

    Valid 132230Z - 140430Z

    SUMMARY...Showers and thunderstorms will continue to impact areas
    of central and eastern AZ through western and central NM along
    with southwest CO. Given elevated streamflows from recent rainfall
    along with locally high rainfall rates this evening, additional
    isolated to scattered areas of flash flooding will be possible.

    DISCUSSION...GOES-W visible satellite imagery along with regional
    radar data shows a broken axis of heavy showers and thunderstorms
    impacting areas of central and eastern AZ through western and
    central NM, with an emphasis on areas near and adjacent to the
    Mogollon Rim. The convection continues to be enhanced by the
    gradual northeastward advance of modest shortwave energy that is
    embedded within the deeper layer southwest flow ahead of a
    stronger upper-level trough and closed low dropping south along
    the West Coast.

    The latest RAP analysis does show as much as 1000 to 1500 J/kg of
    MUCAPE across areas of south-central AZ and separately across far
    northwest NM and far southwest CO near the Four Corners. The
    instability in particular over south-central AZ continues to
    combine with moist low to mid-level southerly flow to support
    convection with high rainfall rates that are occasionally reaching
    1.5+ inches/hour. Elevated effective bulk shear is also favoring
    some organized multicells and persistence of the activity that
    coupled with orographics into the Mogollon Rim is yielding heavier
    rainfall totals.

    More recently, satellite imagery has been showing some greater
    vertical depth of convection across western NM and also in a more
    cellular manner across parts of southwest CO where improving
    instability and moist upslope flow into the San Juan Mountains is
    fostering an uptick in stronger thunderstorm activity.

    Going through the evening hours, as moist flow and at least modest
    instability continue to interact with the aforementioned shortwave
    energy and favorable orographic environment, there should continue
    to be broken areas of heavy showers and thunderstorms. Additional
    rainfall amounts may reach as high as 2 to 3 inches where any
    cell-training occurs, and this is consistent with a consensus of
    18Z HREF/12Z REFS model suites.

    The antecedent conditions are quite wet, and especially over areas
    of the Mogollon Rim and the high country of southwest CO near and
    adjacent to the San Juan Mountains. Given the additional rainfall
    expected this evening, there will likely be more potential for
    isolated to scattered areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7doVrWLjkwQa72VYniJNk6xk1yGikKd6Rti1oorXg66cVvPKz9cZGGsOU9oSXa0LDLGE= 6mPmcEvU8gOdRrz06ahPmiI$ for graphic product...

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

    ATTN...RFC...FWR...STR...NWC...

    LAT...LON 38440769 38300643 37560577 35720564 34050625=20
    33160789 32890989 32981093 33441197 34381233=20
    35001172 35211039 35750938 36450879 37770835=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 Oct 13 23:17:46 2025
    AWUS01 KWNH 132317
    FFGMPD
    CAZ000-140515-

    Mesoscale Precipitation Discussion 1194
    NWS Weather Prediction Center College Park MD
    716 PM EDT Mon Oct 13 2025

    Areas affected...Central CA Coastal Ranges into the Central Valley

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

    Valid 132315Z - 140515Z

    SUMMARY...Heavy showers and potentially a few thunderstorms will
    impact areas around the Bay Area through early this evening. While
    spreading gradually farther south along the coastal ranges, some
    of these heavier rains should spread into portions of the Central
    Valley. An urban flooding threat will exist, and especially around
    the Bay Area, with an isolated burn scar flash flood threat as
    well over some of the adjacent higher terrain.

    DISCUSSION...The latest GOES-W WV suite shows a strong upper-level
    low continuing to deepen as it drops southward just offshore of
    the West Coast. A rather strong frontal structure associated with
    these height falls coupled with enhanced upper-level jet
    divergence/forcing overspreading the central CA coastal ranges,
    including the Bay Area, along with adjacent portions of the
    Central Valley will support areas of heavy showers and potentially
    a few stronger thunderstorms going through the evening hours.

    A nose of MUCAPE values reaching 250 to 500 J/kg is noted along
    and just ahead of a developing frontal occlusion near the Bay
    Area, and radar imagery has been showing an increase in linear
    bands of convection along and just ahead of the front as it pivots
    inland from the coast. Deep layer forcing is expected to
    strengthen this evening which coupled with moist Pacific flow
    should favor some linearly oriented bands of convection to
    potentially make it even into parts of the Central Valley.

    Lowering ELs associated with the upper low and modest instability
    will favor low/warm-topped convective elements in this dynamically
    forced environment that will be rather efficient and capable of
    producing rainfall rates of up to 1 inch/hour.

    The relatively high rainfall rates coupled with favorable upslope
    flow into the coastal ranges will support some spotty 2 to 3+ inch
    rainfall totals. Generally, the interior areas of the Central
    Valley will see lesser totals, but some of the stronger convective
    elements here that occur may foster some locally excessive totals
    of 1 to 2+ inches.

    Concerns will exist for some urban flooding, and especially around
    the Bay Area through early this evening. Some of the area burn
    scars will also need to be closely watched for at least an
    isolated concern for flash flooding and debris flow activity.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!81rbhW0x8wR3EO92eXMf25Y-xC4pJGG5MjnbkZfa-pUGIzV2eud_0tr7iX73qqqvfje-= GwodklBZKSVXr2hLPCfeBy4$ for graphic product...

    ATTN...WFO...EKA...HNX...LOX...MTR...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 40672288 40552224 39362123 38122061 36672049=20
    35892024 35372018 35252070 35542130 36122186=20
    36792231 37442256 38762273 40092333=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Oct 14 05:35:52 2025
    AWUS01 KWNH 140535
    FFGMPD
    CAZ000-141134-

    Mesoscale Precipitation Discussion 1195
    NWS Weather Prediction Center College Park MD
    135 AM EDT Tue Oct 14 2025

    Areas affected...portions of central and southern California

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

    Valid 140534Z - 141134Z

    Summary...Strong onshore flow will continue to promote areas of
    heavy rainfall, with rates of 0.5-1 inch/hr becoming possible
    along upslope terrain areas. Flash flooding is likely -
    especially where heavier rainfall can materialize across burn
    scars and other sensitive areas.

    Discussion...A strong mid-upper low centered just west of San
    Francisco continues to move very slowly while promoting strong
    onshore flow across coastal areas of central California. Cold
    upper levels has fostered areas of 500 J/kg MUCAPE, promoting
    heavier rainfall in occasional convective bands that have traveled
    toward land on the southern and eastern peripheries of low. A
    belt of strong low- to mid-level flow (around 30 knots at 850mb)
    is oriented parallel to coastal ranges between Monterey and San
    Luis Obispo and was also aiding in heavy rainfall via orographic
    lift. The heaviest rain was located along and just ahead of a
    cold front that was migrating southward along the coastline near
    Monterey.

    Over time, the strongest of onshore flow will shift southward
    along the coast toward the Transverse ranges. 1-1.2 inch PW
    values and minimal instability will continue to promote heavy
    rainfall and rain rates exceeding 0.5 inch/hr at times. Areas of
    southern California (including the Transverse Ranges and Los
    Padres National Forest) will likely experience the heaviest of
    activity through 12Z. Local burn scars will enhance rainfall
    potential, and typical low-lying, flood prone spots will also be
    susceptible to flash flooding.

    An additional area of lighter rain is likely to be maintained
    across portions of central California and the southern San Joaquin
    Valley. Rain rates should be a bit lighter in most of these areas
    (0.1-0.5 inch/hr), but should persist for several areas and cause
    at least minor runoff issues.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-dO1Xb2Ee8YLBuIuvDf85AIky-PetUOunsyiThjwn7Y8rlK121JgeIM0rNgFvnj-c9eT= go8jJRBI5P6kxqAQQc-DrW4$ for graphic product...

    ATTN...WFO...HNX...LOX...MTR...SGX...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 38842155 38022017 37111947 36371911 35691934=20
    35001888 34561784 33881774 33511810 33921923=20
    34602076 35982190 36902208 37802222 38582215=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 Oct 14 12:40:00 2025
    AWUS01 KWNH 141239
    FFGMPD
    CAZ000-141838-

    Mesoscale Precipitation Discussion 1196
    NWS Weather Prediction Center College Park MD
    839 AM EDT Tue Oct 14 2025

    Areas affected...Southern CA

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

    Valid 141238Z - 141838Z

    Summmary...A band of showers and thunderstorms should continue to
    move east with time. Hourly rain amounts up to 1" and local
    totals in the 2-4" range are possible, which would be most
    problematic in area burn scars.

    Discussion...A narrow plume of moisture and instability near an
    incoming front and ahead of a cold low to the west-northwest of
    San Luis Obispo is expected to continue moving eastward through
    southern CA this morning. Precipitable water values of 1-1.1" per
    GPS data and MU CAPE of 250+ J/kg exist in this region.

    HREF guidance shows a high chance of 0.5"+ in an hour, though very
    low chances of 1"+, which fits the available ingredients. As
    instability winnows with time, the potential for 1" amounts should
    decrease. The mesoscale guidance suggests local amounts in the
    2-4" during the next six hours. Locations with the most concern
    would be area burn scars, which would be more susceptible to
    runoff/debris flows.=20

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_ufGLYKOP3DvquOzB86le3R3uxQpJxz2mBWSXE2K_3KzVyoYR-B7DXWvA1xvNFvERdMP= Kj5w75GoM8zlDlV1JUBMTKc$ for graphic product...

    ATTN...WFO...HNX...LOX...SGX...

    ATTN...RFC...RSA...NWC...

    LAT...LON 34891939 34771818 34551743 34491729 34311662=20
    33891676 33151731 33591833 33631836 33941868=20
    34001916 34191957=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Oct 14 18:26:34 2025
    AWUS01 KWNH 141826
    FFGMPD
    CAZ000-150015-

    Mesoscale Precipitation Discussion 1197
    NWS Weather Prediction Center College Park MD
    224 PM EDT Tue Oct 14 2025

    Areas affected...Southern CA

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

    Valid 141824Z - 150015Z

    SUMMARY...Locally heavy showers and possibly a few thunderstorms
    will maintain a threat for areal flooding impacts including
    potential burn scar flash flooding going through early this
    evening.

    DISCUSSION...A strong upper-level low and an associated frontal
    occlusion continues to drop gradually down across southern CA. The
    latest GOES-W visible and infrared satellite imagery shows the
    leading edge of the cold front and heavy rainfall continuing to
    advance through the Los Angeles Basin, with a substantial amount
    of post-frontal shower activity maintaining pockets of locally
    heavy rainfall.

    Rainfall rates with some of the stronger convective elements along
    the front and also into the southwest-facing slopes of the San
    Gabriel and San Bernadino Mountains have been upwards of 0.50" to
    0.75"/hour, and these rates are likely to be maintained at least
    for a few more hours as the axis of stronger moisture transport
    and convergence with the front continues to advance southeastward
    down the coast with an approach on the Peninsular Range.

    However, post-frontal instability associated with steepening
    mid-level lapse rates closer to the upper low will combine with
    low-level cyclonic flow into the terrain to maintain plenty of
    shower activity and perhaps a few thunderstorms going through this
    afternoon and early this evening. Additionally, the stronger
    dynamics associated with the digging upper-level low and influx of
    Pacific moisture wrapping northward up into the upslope areas of
    the southern Sierra Nevada and also the southern parts of the San
    Joaquin Valley will continue to foster areas of heavy rainfall
    here which will include a threat for some intense low-top
    convective showers.

    The heaviest additional rainfall totals should generally be across
    parts of the San Gabriel Mountains and especially the San
    Bernadino Mountains where as much as an additional 2 to 3 inches
    of rain may fall (below snow line) by this evening.

    Lowering snow-levels in time will tend to mitigate some of the
    runoff potential for the highest terrain, but sufficient rainfall
    over especially the Pacific-facing slopes and into some of the
    urban areas is expected to maintain concerns through early this
    evening for areal flooding impacts and some burn scar flash
    flooding. Rockslides and some localized debris flow activity near
    and downstream from burn scar locations will continue to be
    possible.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!83FIFmAZaUM2GZvSWjpAzgDb6wd4huOGcng7Ub5DWl4vbFkk3gdakmRFYie4oeWgfNL2= gvwbxQkRB4_o43BTnrHX9WY$ for graphic product...

    ATTN...WFO...HNX...LOX...SGX...VEF...

    ATTN...RFC...RSA...NWC...

    LAT...LON 36621923 36061849 35241815 34811741 34361675=20
    33991649 33341652 32631664 32571701 32781734=20
    33401770 33651827 33791851 33911881 34061919=20
    34151938 34291957 34441994 35251986 35902019=20
    36312014=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Oct 15 05:25:40 2025
    AWUS01 KWNH 150525
    FFGMPD
    NMZ000-151123-

    Mesoscale Precipitation Discussion 1198
    NWS Weather Prediction Center College Park MD
    125 AM EDT Wed Oct 15 2025

    Areas affected...southern/central New Mexico

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

    Valid 150523Z - 151123Z

    Summary...Scattered thunderstorms are developing over
    south-central New Mexico near Truth or Consequences. Areas of 0.5
    inch/hr rates were already being observed. These rates could
    increase to around 1-1.5 inch/hr at times while moving northward
    across the state. Isolated flash flooding is possible.

    Discussion...Thunderstorms were developing in the southern Rio
    Grande Valley of New Mexico over the past hour. These cells were
    drifting northward at around 25 knots. They were also embedded in
    a relatively narrow axis of weak to moderate instability (1000
    J/kg SBCAPE) and moisture (1-1.2 inch PW values), supporting brief
    heavy rainfall. The orientation of this convection (with movement
    parallel to the moist/unstable axis) was promoting localized
    training/repeating cells, with rain rates peaking at around
    0.5-0.75 inch/hr per MRMS. Low-level convergence on the nose of
    southeasterly 850mb flow across the eastern Plains was also
    contributing to ascent along the moist axis in tandem with subtle
    height falls from a larger-scale system centered over California.

    Each of these factors all point to a gradual increase in
    convective coverage across the discussion area over the next few
    hours, with storms drifting northward toward the central part of
    the state. Areas of 1 inch/hr rain rates could occur on a spotty
    basis. FFG thresholds exhibit spots of thresholds as low as 1
    inch/hr in the discussion area, suggesting isolated potential for
    excessive runoff. Additionally, a few burn scars in the vicinity
    may support excessive runoff on a localized basis.

    Eventually, the combination of convective overturning and
    nocturnal boundary layer stabilization will lead to a decrease in
    convective coverage (and attendant flash flood potential).=20
    Low-level convergence may also slacken toward 10Z as 850mb flow
    veers to more southerly across the eastern Plains, decreasing
    convective potential as well. These processes will take a few
    hours to play out, with isolated flash flood potential persisting
    through at least 10Z/4a Mountain Time.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ReaygMsm86PXcG_rHp7rBfT2EdmFiuvKZ-K63YsskLunA1cM-ami3emW1Xk-CwkjbLI= Whsnzo8WpliTI3gaTv-DBmA$ for graphic product...

    ATTN...WFO...ABQ...EPZ...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 36710485 36150431 34220501 32500611 31880695=20
    32030839 33680809 35790721 36470604=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Oct 16 02:27:51 2025
    AWUS01 KWNH 160227
    FFGMPD
    COZ000-NMZ000-160815-

    Mesoscale Precipitation Discussion 1199
    NWS Weather Prediction Center College Park MD
    1027 PM EDT Wed Oct 15 2025

    Areas affected...northern NM into southern CO

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

    Valid 160225Z - 160815Z

    Summary...Isolated flash flooding will be possible through 08Z (2
    AM MDT) from northern NM into southern CO with peak hourly
    rainfall between 0.5 and 1.0 inches.

    Discussion...02Z GOES East infrared imagery, lightning data and
    MRMS reflectivity showed a broken line of thunderstorms stretching
    from Rio Arriba County in northern NM into southern portions of
    the CO Rockies. Additional convective development was beginning to
    strengthen to the southeast of this axis, near Los Alamos and
    Santa Fe. These thunderstorms were occurring out ahead of a potent
    closed mid-level low tracking east through the Great Basin and
    associated cold front at the surface. Instability via ABQ's 00Z
    sounding and 02Z SPC mesoanalysis data showed MLCAPE between
    500-1000 J/kg along with anomalous PWATs between 0.6 and 0.9
    inches. Aiding ascent was divergence within the right-entrance
    region of a 110+ kt upper level jet extending from eastern UT into
    central WY.

    Within the lingering instability over northern NM and southern CO,
    additional thunderstorm development is expected over the next few
    hours as the upper trough and cold front move east. Steering flow
    is unidirectional from the SSW which could support some repeating
    and brief training, containing hourly rainfall up to about 1 inch.
    This will promote a very localized flash flood threat, which will
    mostly stay focused across sensitive burn scars and any shallow
    creeks or low water crossings.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9I9xdFVxTL3vOwEpa1JcByNqp-50AWQAvmbPEt5XUN0EeMmSpBINvCQb-OKHv89mNLC1= DeXenphqlok7yBazRX1ljSM$ for graphic product...

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

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 37990562 37750483 36860430 35870490 35100584=20
    34920660 35160697 35490707 36270704 37340655=20
    37750613=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 18 13:05:59 2025
    AWUS01 KWNH 181305
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-181904-

    Mesoscale Precipitation Discussion 1200
    NWS Weather Prediction Center College Park MD
    905 AM EDT Sat Oct 18 2025

    Areas affected...MO/KS/AR/OK border area

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

    Valid 181304Z - 181904Z

    Summary...There is growing convective coverage near the
    MO/KS/AR/OK border region. Hourly amounts to 2" with local
    amounts to 4" are expected, which could lead to isolated to widely
    scattered flash flooding.

    Discussion...WSR-88D radar and SPC mesoanalyses reveal a
    noticeable decrease in CIN across the area, which is leading to
    increased shower and thunderstorm coverage near the MO/KS/AR/OK
    border region. A significant shortwave is approaching the region
    from the TX Panhandle, which is clearly seen in GOES-19 water
    vapor imagery. Precipitable water values are 1.42" at Springfield
    MO, per the 12z sounding. MU CAPE of 500-1500 J/kg lies in the
    region per SPC mesoanalyses. Effective bulk shear is 40 kts. The
    flow at 850 hPa in convergent into the region ahead of a frontal
    boundary.

    The guidance shows increasing moisture into the region, due to
    both convective coverage and a slight uptick in low-level inflow
    into the region. Both the 850 hPa convergence and incoming front
    are expected to remain foci for convective activity as we move
    through the late morning into the early afternoon, which should
    further increase in coverage and intensity with time. Convection
    could lay down a mesoscale boundary across southern MO and
    northwest AR with time. Both the 06z HREF and 00z REFS appear to
    be too far to the east initially with areas receiving heavy
    rainfall, but the RAP guidance shows boundary layer moisture
    convergence extending eastward across portions of southern MO, so
    the expectation is for a convective band to attempt to form with
    embedded mesocyclones, with each meoscyclone both capable of heavy
    rainfall on its own and holding up any convective band forward
    propagation temporarily. This should lead to hourly rain amounts
    to 2" with local totals to 4" which would be most problematic in
    urban areas and Ozarks. Isolated to widely scattered occurrences
    of flash flooding is expected. Recent dryness should keep other
    areas from seeing significant impacts, so long as the convective
    development isn't more efficient than forecast.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!40hfYk-1H3mqxauxt8LFL7ErVg-dzpIVbsmuIKyRedH_g40xaen4MIOLF1Nof91U35gm= jI6Yxkb353ch7ObsDOa3sIg$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...LZK...SGF...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38589292 37719078 36169372 35669512 36309577=20
    37949468=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 18 17:11:05 2025
    AWUS01 KWNH 181710
    FFGMPD
    ILZ000-MOZ000-182300-

    Mesoscale Precipitation Discussion 1201
    NWS Weather Prediction Center College Park MD
    110 PM EDT Sat Oct 18 2025

    Areas affected...Southeast Missouri...Southern Illinois...

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

    Valid 181710Z - 182300Z

    SUMMARY...Prolonged training of moderate rainfall with occasional
    heavy bursts up to 1.5"/hr and localized totals of 2-3" and
    perhaps an isolated 3.5"+. Rates and totals are on the edge of
    FFG exceedance in drought/hard ground conditions for a possible
    incident or two of low-end flash flooding conditions, manly near
    urban or prone locations.

    DISCUSSION...GOES-E Visible/10.3um EIR loops depict a steadily
    cooling and consolidating scattered line of convection across the
    Eastern Ozark Plateau toward S IL. The stronger southern stream
    shortwave over central OK continues to progress and amply along
    the southeast portion of the larger scale trough while strong
    upper-level jet streak is finally rounding the base and expanding
    toward 110kts across KS into north-central MO in the next hour or
    so. The combination of mid-level features and weak outflow from
    convection is starting to combine the confluence/ascent axis
    downstream of the orthogonal strong convergence along and
    downstream of the southern stream shortwave over southern MO. The
    confluence axis is also aligning with the deeper moisture (up to
    1.6" attm) and elevated instability axis (up to 1500 J/kg),
    resulting in the uptick in convective vigor across south-central
    MO into SW IL. The overall coverage of cells remains scattered
    though some embedded cores have be observed producing .25-.5"
    totals in 15-30 minutes with hourly totals nearing 1-1.25". As
    low level flow and moisture flux continue to strengthen with
    rapidly expanding divergence area aloft from the strong right
    entrance region to the 110kt jet, occasional hourly totals up to
    1.5" are not out of the possibility.

    The key for flash flooding will be duration and soil conditions
    along the training axis. As the shortwave further amplifies, the
    deep steering flow appears to favor a slight northward shift,
    which should counteract the southeastward propagation expected
    from cold pool generation. This will allow the cells to remain
    favorable for longer training of 1-3 hours, but the lack of
    extreme instability and oblique convergence may continue to result
    in scattered to widely scattered nature of the stronger cores,
    limiting totals to 2-3", though an isolated spot of 3.5"+ is not
    completely out of the realm of possibility, with best potential
    upstream across south-central MO toward SE MO.

    The good news is the core of the training cells appear to be
    aligned ideally with the axis of the highest FFG values (2-3"/hr
    and 3-4"/3hrs), though there are some urban and complex/hilly
    terrain through the area that would be more prone. Additionally,
    the area has been in prolonged drought with 0-40 cm soil moisture
    ratios below 30%, mainly less than 15%. This is also suggestive
    that soils are compacted and probably a bit hydrophobic, limiting
    initial infiltration. As such, if first rainfall is the intense
    burst of those stronger cores, greater runoff should be expected.
    As such, an isolated to widely scattered incident or two of
    low-end flash flooding remains possible though the afternoon.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7njN2zcMasRNWG6xZRNgFfwZq6fEN-ToDcdjwyTX0eJXZ26_9ru8q-Qslh1yYr6mA4cF= TZmd9siu458_So0TeuvC45Y$ for graphic product...

    ATTN...WFO...ILX...LSX...PAH...SGF...

    ATTN...RFC...KRF...MSR...ORN...TIR...NWC...

    LAT...LON 39418894 39418811 38998773 38388802 37688947=20
    37229051 36939204 37589260 38239302 38809176=20
    39219019=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 19 03:02:10 2025
    AWUS01 KWNH 190302
    FFGMPD
    ALZ000-MSZ000-LAZ000-ARZ000-190800-

    Mesoscale Precipitation Discussion 1202
    NWS Weather Prediction Center College Park MD
    1101 PM EDT Sat Oct 18 2025

    Areas affected...northern LA/MS border into north-central MS and
    western AL

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

    Valid 190259Z - 190800Z

    Summary...Training of heavy rain is expected to result in 1 to 2
    inches of rain in an hour and localized totals of 2 to 4 inches
    through 08Z from the LA/MS border into western AL. These higher
    rain rates may result in isolated flash flooding.

    Discussion...Radar mosaic imagery from 0230Z showed a NE to SW
    axis of thunderstorms extending from western TN into northern and
    western MS and far northeastern LA, co-located with an elongated
    outflow boundary. A few linear clusters of thunderstorms were also
    observed upstream, across southern AR into northwestern LA,
    located ahead of the base of an upper trough tracking east through
    OK and northern TX. The environment across the Lower Mississippi
    Valley was characterized by MLCAPE of 500-1000 J/kg and PWATs
    between 1.7 and 2.1 inches per 02Z SPC mesoanalysis data and the
    00Z sounding from JAN. Southerly to southwesterly 850 mb winds of
    30-40 kt were present from LA into MS, allowing low level moisture
    transport and lift atop rain-cooled air with mean storm motions
    oriented from the southwest in MS but veering toward the west
    across northwestern LA. Flow aloft was diffluent, out ahead of the
    base of the larger scale upper trough located over the central U.S.

    Given the available instability and source region emanating from
    the south, continued forcing via synoptic scale and mesoscale
    processes, some filling in of convection between the leading
    outflow in MS and trailing activity in northern LA is expected
    over the next couple of hours. The potential for training is high
    from the MS River eastward, but the duration of training is
    questionable. However, even a 30-60 minute window of SW to NE
    training should be able to produce 1 to 2 inches of rain with
    potential for 2-4 inches if training is able to set up for a bit
    longer duration. These rainfall values may result in flash
    flooding.

    Dry antecedent conditions should limit flash flood potential, but
    these locally higher rain rates could focus an isolated threat
    across urban locations or other locations of poor drainage. The
    flash flood threat is expected to move east out of the area after
    08Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6MfX7yQlfiyfp69R0kFRwFC3E8EHDjXyDpEXrvnWCgZOK-zFQ-gELrRZAMUrmhSEBGtP= 3elaqsqk3bTTxnZoW3dWFAk$ for graphic product...

    ATTN...WFO...BMX...JAN...MEG...SHV...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34128834 33358769 32428824 31579042 31779220=20
    32609218 33249096 34018968=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Oct 24 02:04:28 2025
    AWUS01 KWNH 240204
    FFGMPD
    TXZ000-OKZ000-240700-

    Mesoscale Precipitation Discussion 1203
    NWS Weather Prediction Center College Park MD
    1003 PM EDT Thu Oct 23 2025

    Areas affected...Texas Big Country...

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

    Valid 240200Z - 240700Z

    SUMMARY...Short window of very intense slow moving cells before
    forward propagation begins. Narrow axes of training/repeating are
    possible across small area of naturally lower FF values. Widely
    scattered flash flooding remains possible for the next few hours.

    DISCUSSION...A well defined surface to boundary layer
    convergence/frontal zone was noted extending east-northeast
    generally along I-20 from a surface low near Ft. Stockton up to
    about KRPH. Winds had an easterly component further strengthening
    moisture flux convergence as southerly flow off the Western Gulf
    has been in the mid to upper 50s for Tds with low to mid 60s
    further eastward where larger synoptic continental polar air
    remains locked the Middle Mississippi to Tennessee Valleys. The
    higher theta-E air pooled along the old boundary showed a solid
    axis of enhanced 1000-1500 J/kg of CAPE. Polar jet exit has been
    advancing out of the southern High Plains with favorable left exit
    ascent in the vicinity of the convergence as well as the trailing
    positive tilt mid-level trough axis remained over far NW Texas as
    the wave lifts through central OK.=20

    As a result, strong vertical ascent and scattered to numerous
    updrafts were noted along the old frontal zone with broadening
    cooling tops falling below -65C nearing -70C; denoting the initial
    vigor to the updrafts. The strong moisture flux as resulted in
    broadening up/downdraft cores and efficient rainfall and small
    hail resulting in localized 1.5-2"/hr rates. A few spots have
    already experienced these totals with an 1-2" more possible.=20=20
    Slow forward motions were a result of the lingering northeasterly
    flow and anchor to the old boundary; however, as the nocturnal low
    level jet is starting to develop, the easterly component areas
    have been over-run and broad/strengthening south to southeasterly
    flow has taken over. This will allow for eventual eastward
    propagation on the development of weak cold pools.

    Orientation of the boundary is fairly parallel to the deepening
    unidirectional steering flow out of the west-southwest. Initially
    about 10-15kt, steering flow will increase to 20-30+kts over the
    next few hours likely to reduce the potential for larger rainfall
    totals and limit risk of flash flooding due to the initial burst
    of up to 1-1.25" in 15-30 minutes overwhelming the drier grounds
    with limited infiltration. As such, localized flash flooding
    will shift toward widely scattered and more likely limited to
    prone or urban/low infiltration ground conditions across the Big
    Country through the early overnight period.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5OAoGKhG_HXUQiOPtZoP-Enoe_t6I8d_QAakdbGjfEGQpe91kFJYrEZiJaGEIwS3bqyS= Oa-iQIQrhMkiCzuw2bESxmc$ for graphic product...

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

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 34189748 33789695 33039732 32689782 32399844=20
    32169959 31840075 31610177 32030223 32750153=20
    33410038 33759932=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Oct 24 06:09:29 2025
    AWUS01 KWNH 240609
    FFGMPD
    OKZ000-KSZ000-241200-

    Mesoscale Precipitation Discussion 1204
    NWS Weather Prediction Center College Park MD
    209 AM EDT Fri Oct 24 2025

    Areas affected...Eastern Oklahoma...Adj South-central Kansas...

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

    Valid 240610Z - 241200Z

    SUMMARY...Deepening low level confluence and WAA will provide
    consistent ascent for slow forward propagating/back-building
    updrafts with 1.5"/hr rates resulting in localized 2-3" totals and
    possible widely scattered incidents of flash flooding through
    morning.

    DISCUSSION...CIRA surface to 700mb LPW layers depict south to
    north plume of enhanced low level moisture across northwest to
    north Texas. A well defined stationary front/theta-E gradient is
    denoted along and just east of I-35 across much of central OK
    before angling westward along the KS/OK border toward weak surface
    wave in SW KS. GOES-E WV suite shows strong closed low continuing
    to advance out of the Four Corners with broad southwesterly flow
    across much of the Southern Plains; yet the frontal zone remains
    anchored by equally strong downstream low level ridging over the
    Lower Mississippi Valley. As such, the deep layer moisture plume
    which totals to 1.5 increasing to 1.75" of Total PWat is corralled
    well and fluxed on 40kt 850mb flow.=20

    CIRA LPW 700-500mb shows slug of enhanced moisture in the
    southwesterly flow along the northern edge of the 300mb jet streak
    axis associated with mid-level shortwave and left exit divergence
    area across west-central OK into north-central OK. The strong
    veering through this 850-700mb layer is moist and conditionally
    unstable with MUCAPEs over 2000 J/kg. The strong WAA through the
    layer is providing some weak isentropic upglide before providing
    sufficient directional/speed convergence to tap the unstable air
    for vertical ascent. As such, scattered clusters of thunderstorms
    are breaking out across much of central to northeastern OK,
    including far southern KS at different vertical layers (lower
    further west). Downstream flow supports cell motions toward the
    east, but with the stronger convergence and unstable air upstream,
    backbuilding will result in slowing effective cell/cluster motions
    and increasing localized rainfall totals. Rates of 1.5"/hr are
    more likely, though very transient uptick toward 2"/hr remain
    possible and isolated within the larger WAA flow regime. As such,
    with slow eastward motion of the overall pattern due to the
    stronger low level ridge to the east; scattered streaks of 2-3"+
    totals are possible. 00z HREF empowered by the NAM-Nest and ARW
    solutions suggest even a spot of 4" is not out of the realm of
    possibility with 10-15% of 5"/6hr by 12z over east-central OK.=20

    In general, FFG values are high (2"+/hr, 3-4"/3hrs) and rates are
    not too extreme, that slow infiltration is more likely; however,
    an isolated incident of flash flooding remains possible over the
    next 4-6 hrs. With that stated, this is just the start of
    prolonged moderate WAA ascent and repeating rounds likely to set
    the stage for later flooding concerns into the late morning early
    afternoon.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-wkIzyKaAfPmthRUgThy1ZMrXL2dT5YVSM-Cq53KusUN977G3VSfzydedzuu99eLoTqK= N6geyQpaNKPn4IBeDm2kAVE$ for graphic product...

    ATTN...WFO...ICT...OUN...TSA...

    ATTN...RFC...TUA...NWC...

    LAT...LON 37709742 37649652 36819579 36029535 35239552=20
    34709607 34459724 34929812 35479839 36199802=20
    36659783 37159777=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Oct 24 06:41:32 2025
    AWUS01 KWNH 240641
    FFGMPD
    TXZ000-241100-

    Mesoscale Precipitation Discussion 1205
    NWS Weather Prediction Center College Park MD
    240 AM EDT Fri Oct 24 2025

    Areas affected...North Texas...

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

    Valid 240640Z - 241100Z

    SUMMARY...Short QLCS segment propagating into deeper
    moisture/instability axis. Low-end incident or two of flash
    flooding possible given rates of 1.75"/hr and totals to 3".

    DISCUSSION...Recent KFWS and GOES-E 10.3um have shown a recent
    uptick in convective intensity with overshooting tops cooling near
    -70C occasionally with mature weak QLCS from earlier thunderstorms
    over the Big Country. The complex has history of localized 2"+
    totals upstream but is moving into a more focused low-level
    moisture flux/instability axis along and west of strong/reinforced
    stationary front across eastern TX. Surface observations show
    outflow is starting to reach southeasterly flow at the nose of
    surface Tds in the 60s, that are sourced with even higher moisture
    into the low 70s upstream by a few hours. A weak surface
    inflection of the meso-low along the line is helping to locally
    strengthen the influx of the higher moisture and slightly higher
    unstable air with MUCAPE up to 1500 J/kg in that stream west of
    the front.=20=20

    Aloft, GOES-E WV suite shows the cluster is at the hard cyclonic
    turning toward the northeast providing solid diffluence in the
    upper-level jet coincident and downstream of the cluster helping
    to further evacuate outflow to maintain stronger updraft strength
    for a few more hours. Total PWats of 1.5" and expected isallobaric
    inflow should provide rates of 1.75", occasionally up to 2" and
    with still some upstream potential for short-term training of an
    hour or two, localized totals of 2-3" remain possible. Given the
    strength of the rates and surface rooted cells in proximity to
    urban locales of North Texas and incident of low-end flash
    flooding remains possible for the next few hours before the cells
    cross the frontal boundary and move into much drier (upper 40s Td)
    and stable environment.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5W5JkTQaTOrTf8IvO-2JIkZjZVzWlEFk61Ub57gKCKbEgy-jU_WGViICRHoRqqr-kI_E= xfB7Tqysg6YJeBUAMr32ZdM$ for graphic product...

    ATTN...WFO...FWD...

    ATTN...RFC...FWR...NWC...

    LAT...LON 33319721 33289635 32929591 32469584 31979628=20
    31959723 32249820 32649845 33029825 33229785=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 Oct 24 15:45:34 2025
    AWUS01 KWNH 241545
    FFGMPD
    OKZ000-242100-

    Mesoscale Precipitation Discussion 1206
    NWS Weather Prediction Center College Park MD
    1144 AM EDT Fri Oct 24 2025

    Areas affected...North-Central to Northeast OK

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

    Valid 241544Z - 242100Z

    SUMMARY...An axis of heavy showers and thunderstorms across
    portions of north-central to northeast OK will be capable of
    cell-training over the next few hours. High rainfall rates
    associated with this will drive a threat for isolated to scattered
    areas of flash flooding, and especially for the more urbanized
    locations.

    DISCUSSION...The morning GOES-E VIS/IR satellite imagery shows a
    well-organized convective cloud canopy over areas of north-central
    to northeast OK. Convective trends show the activity exhibiting
    cooling cloud tops, with some tops to near -70C, and this is
    suggestive of an environment of increasing deep layer ascent along
    with favorable moisture and instability transport.

    Mesoscale analyses show the convection elevated in nature
    northeast of a stationary front draped across western OK down into
    the Red River Valley. The nose of a south-southwest 30+ kt
    low-level jet is overrunning this boundary at a largely orthogonal
    angle and is favoring a corridor of relatively strong moisture
    convergence within a favorably divergent flow regime aloft given
    favorable left-exit region upper-jet dynamics riding across
    northern OK. Coinciding the with the moisture transport and
    forcing is the pooling of elevated instability with MUCAPE values
    of 1000+ J/kg.

    Positive 3-hour MUCAPE differentials across central OK juxtaposed
    against negative 3-hour MUCAPE differentials over northeast OK
    suggests a strengthening of the elevated instability gradient
    which also suggests an axis of strengthening frontogenesis aloft.
    This will favor stronger ascent via isentropic lift and enhanced frontogenetical forcing in the near-term with the convection and
    support a further uptick in rainfall rates.

    Rainfall rates may reach up to 1.5+ inches/hour given the
    environment, and with an environment conducive to some
    backbuilding and cell-training of the convection, some rainfall,
    totals over going through mid-afternoon may reach 2 to 4+ inches.
    Dry antecedent conditions overall will mitigate the runoff
    potential in the near-term, but as some of these heavier rainfall
    rates persist, or get into a more urbanized setting, there may be
    a concern eventually for isolated to potentially scattered areas
    of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_xhQKScTxndQPI2HafFNlIkNdaXy6-Xc6cRZjoyFnFNbgw7nCYQYLcImv2FYNJ2oE83k= boJUFy9RDf2188ssUgoUAgg$ for graphic product...

    ATTN...WFO...OUN...TSA...

    ATTN...RFC...TUA...NWC...

    LAT...LON 36789745 36719576 36429480 35569461 35119574=20
    35289738 35679858 36129884 36529849=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Oct 24 18:51:38 2025
    AWUS01 KWNH 241851
    FFGMPD
    TXZ000-250030-

    Mesoscale Precipitation Discussion 1207
    NWS Weather Prediction Center College Park MD
    250 PM EDT Fri Oct 24 2025

    Areas affected...Southwest to Northwest Texas

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

    Valid 241850Z - 250030Z

    SUMMARY...Organizing clusters of heavy showers and thunderstorms
    may produce an isolated to scattered threat for flash flooding.

    DISCUSSION...Satellite and radar imagery continues to show the
    development and expansion of heavy showers and thunderstorms
    across portions of the Trans-Pecos region of southwest TX through
    parts of the Edwards Plateau and into the TX Big Country.

    The environment continues to destabilize out ahead of an upstream
    cold front and associated deep layer trough crossing the southern
    Rockies. MLCAPE values have risen to as much as 1500+ J/kg, and
    with enhanced effective bulk shear of 40 to 50+ kts, convection is
    quickly attaining a substantial level of organization with
    multicell and supercell convective clusters noted.

    Additional boundary layer destabilization will yield localized
    areas of MLCAPE exceeding 2000 J/kg by late this afternoon, which
    will include a much greater level of instability pooling up across
    the TX Big Country. The environment is increasingly moist with PWs
    reaching 1.5 to 2 standard deviations above normal, and this is
    being driven by a moist southerly low-level jet of 30 to 40+ kts.
    This moisture transport out ahead of the front coupled with the
    instability and shear should help facilitate rainfall rates
    increasing to as much as 1 to 2 inches/hour with the more
    organized convective cells.

    Some cell-merger activity is expected over the next few hours as
    the overall convective footprint takes on a larger scale QLCS
    evolution by this evening. Upscale growth of convection will be
    strongly connected to the arrival of strong jet-aided divergence
    aloft and the already favorable kinematic and thermodynamic
    environments.

    Expect some localized 2 to 4 inch rainfall totals to possible
    where any cell-merger and cell-training activity occurs going
    through early this evening. This may drive some isolated to
    scattered areas of flash flooding, and especially in around the
    more urbanized areas.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!95nBizNJjDyo2Y3Pc-KiHFFrVIZzhMck0pHgbCuyqCFi7vo5CFNzCJFEwmlXN3ZsnG8J= 0x9lhqRVBimeNasSj3AHzlA$ for graphic product...

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

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 34259948 34039855 33179816 32159877 31250020=20
    30500214 30210368 30480421 31120423 31850307=20
    32740187 33950035=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Oct 24 21:15:09 2025
    AWUS01 KWNH 242115
    FFGMPD
    TXZ000-OKZ000-KSZ000-250300-

    Mesoscale Precipitation Discussion 1208
    NWS Weather Prediction Center College Park MD
    512 PM EDT Fri Oct 24 2025

    Areas affected...Eastern Portions of the TX Panhandle...Northwest TX...Southwest and Central OK

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

    Valid 242112Z - 250300Z

    SUMMARY...Pockets of heavy showers and thunderstorms may expand a
    bit more in coverage going into the evening hours. A localized
    threat of flash flooding will exist.

    DISCUSSION...The late-day GOES-E IR satellite imagery shows
    cooling convective tops across parts of the TX Big Country up into
    far southwest OK. The convection is becoming increasingly aligned
    with strengthening deep layer ascent associated with stronger
    upper-level jet dynamics downstream of the approaching upstream
    trough over the southern Rockies. This is coinciding with MLCAPE
    values of near 1000 J/kg focused up in close proximity also with a
    frontal zone draped across the region.

    Some additional uptick in the coverage of convection is expected
    going into the evening hours as larger scale forcing increases
    further and interacts with the modest pool of moisture and
    instability nosing up across the region. This will generally be
    near and east of an area of surface low pressure over the TX
    Panhandle, but more closely aligned with areas of strongest
    low-level convergence and frontogenetical forcing near the front.

    By later this evening, some of the uptick in the coverage of
    convection is expected to involve central OK as the southerly
    low-level jet here strengthens and yields stronger moisture
    transport.

    Expect rainfall rates in the near-term to be capable of reaching
    well into the 1 to 2 inches/hour range, but with some
    cell-training concerns in place, there may be some localized
    swaths of additional rainfall totals reaching 2 to 4+ inches by
    late this evening. This is consistent with a blend of the 18Z HREF
    and 12Z REFS guidance.

    This will drive a threat for mainly localized and urban flash
    flooding concerns.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9_--XblOWRWkEG_g9oOKe9cFAwm-lvcMKaDSoQhsau4EL6-WKzwW9aljUlEEZdxRLY2K= qb-W-gGasQ_nQuPfXA2rzEI$ for graphic product...

    ATTN...WFO...AMA...DDC...ICT...LUB...OUN...TSA...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 37119822 36819707 36109666 34929704 33889811=20
    33559921 33580013 34170070 34820090 35840067=20
    36829965=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Oct 24 23:26:41 2025
    AWUS01 KWNH 242326
    FFGMPD
    TXZ000-OKZ000-250525-

    Mesoscale Precipitation Discussion 1209
    NWS Weather Prediction Center College Park MD
    725 PM EDT Fri Oct 24 2025

    Areas affected...Edwards Plateau/TX Hill Country into Northern TX
    and Southern OK

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

    Valid 242325Z - 250525Z

    SUMMARY...Well-organized clusters and bands of heavy showers and
    thunderstorms will evolve going into the overnight hours.
    Scattered areas of flash flooding will be likely, which is
    expected to include some regional-scale urban flooding impacts,
    some of which may be significant.

    DISCUSSION...Early evening GOES-E IR satellite imagery shows an
    expansive axis of well-organized cold-topped convection impacting
    portions of the Edwards Plateau and TX Big Country, with generally
    cooling cloud top trends and the convection inclusive of multicell
    and supercell modes.

    The environment across much of the region is moderate to strongly
    unstable with MLCAPE values of 1500 to 2000+ J/kg pooled across
    the region well ahead of an upstream cold front and deeper layer
    trough ejecting out across the southern High Plains. This
    instability which is being aided by a moist southerly low-level
    jet of 30 to 40+ kts is working in tandem with a sheared and
    dynamically forced vertical column to support strong/organized
    convection capable of producing rainfall rates of 1 to 2
    inches/hour.

    Over the next several hours, the convection will tend to take on
    the character of a QLCS, but with embedded swaths of convection
    where cell-training and supercells will be a notable concern. This
    will include portions of the Edwards Plateau and TX Hill Country
    going through the late-evening hours. However, numerous runs of
    the HRRR guidance along with recent RRFS solutions support an area
    of more focused and potentially higher-end rainfall impacts/flash
    flooding concerns closer into the Dallas-Fort Worth metropolitan
    area along with potentially adjacent areas of the Red River Valley
    of the South. This is being supported by the latest RAP analysis
    which does showing the pooling of higher theta-e air/moisture and
    instability nosing up across north-central TX toward the Red River
    Valley. This is also in close proximity to a stationary front
    which in itself is expected to interact with the low-level jet for
    an area of stronger low-level forcing/convergence.

    On a regional level, the more organized swaths of convection are
    expected to yield locally 2 to 4+ inches of rain which will mainly
    be connected to short-term cell-training considerations. However,
    some of the aforementioned guidance, especially across
    north-central TX (DFW metroplex region and adjacent suburbia) may
    see 5+ inch totals given trends toward a more unstable/strongly
    forced regime setting up this evening.

    Scattered areas of flash flooding are likely going into the
    overnight hours and this will include notable urban flooding
    concerns. Some of these impacts may be significant, and areas near
    the Dallas-Fort Worth metropolitan area in particular should
    closely monitor this situation over the next several hours.

    Areas also in the more flashy/sensitive TX Hill Country area will
    be at risk for elevated rainfall totals and flash flooding
    concerns late this evening and overnight that may be locally
    significant. This area could be the subject of a more targeted MPD consideration later tonight as conditions warrant.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7QAfLaznb4TeNmx_mk11HHddrWT-_R5iS99HSoCFi3qZu5PV4N4CBI6A0IRoBE2rixw2= GUMG1Mzvm-LF5QP_92WXyOw$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...MAF...OUN...SHV...SJT...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35019724 34799567 33509523 32359546 31159624=20
    30269725 29509860 29180037 29370140 30180214=20
    30850194 31690068 32709927 33769832=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 25 04:32:16 2025
    AWUS01 KWNH 250432
    FFGMPD
    TXZ000-251000-

    Mesoscale Precipitation Discussion 1210
    NWS Weather Prediction Center College Park MD
    1231 AM EDT Sat Oct 25 2025

    Areas affected...Eastern & South-Central Texas...

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

    Valid 250430Z - 251000Z

    SUMMARY...Upstream QLCS have slightly favorable training
    environment to maintain longer rainfall duration for spots of 2-4"
    totals and scattered possible incidents of flash flooding through
    late overnight period.

    DISCUSSION...Regional RADAR mosaic shows a mature QLCS rapidly
    advancing across North Texas into the Heart of Texas increasing in
    forward speed, while strong inflow vector becomes parallel to the
    line reducing overall convergence. However, GOES-E WV suite
    denotes main southern stream shortwave lifting northeast through
    the Red River Valley with trailing mid-level trough axis back
    toward the Big Bend of the Rio Grande Valley. Strong
    diffluent/split flow from 80kt sub-tropical jet streak, generally
    aligned along South Texas and through the Upper Texas Coast
    combined with right entrance to 70kt south to north polar jet
    streak across the Big Country allows for increasing divergence in
    proximity to the trailing convective outflow (southern edge of
    strong 1015 Meso-high).=20

    Strong surface to 925 south-southeasterly flow at 10-20kts is
    pumping low 70s Tds and increasingly unstable air off the western
    Gulf generally orthogonal to the orientation of the
    trough/convergence axis. This is providing more than ample strong
    moisture flux convergence for a strengthening cluster along the
    upwind edge with overshooting tops to -70C. Pooled moisture is up
    to 1.5" through depth, though maximized in the lowest portion of
    the column allowing for efficient rainfall production with
    1.75-2"/hr rates. Downstream along the northeast edge, isentropic
    WAA is providing some scattered towers pre-wetting the soils as
    the peak cores rapidly advance. While forward speed will limit
    overall totals, the combination of prolonged moderate rainfall
    with peak rates up to 2" (with 03z HRRR suggesting 1.25"/15
    minutes) may be intense enough to overcome the regionally high FFG
    values. A few urban locations along the path would be more prone
    to these rates for scattered flash flooding concerns particularly
    San Antonio Metro.

    Of note, but a bit less certain, in the wake of the cluster there
    is a solid upstream remaining pocket of 1000-1500 J/kg of MUCAPE
    through the Big Bend/Lower Pecos Valley. While mid-level
    shortwave and ideal jet diffluence will be downstream, low level
    flow intersecting the flanking outflow has some solid potential
    for redevelopment. While not likely as strong as the initial
    cluster any totals of 1-2" additional would further expand those
    areas that were close to exceeding with the initial round and
    maintain a risk of localized flash flooding for a few additional
    hours.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_xzXZ80QIJTG7LPofMaIHf3Qh0QagUEjt7_3SPKnxEcuHmWDDY0XXEnkg2CfJPEAqnf8= RPaLTgyMVvzV2AgZsvoQijY$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30869829 30849640 29899569 28839627 28649903=20
    28880036 29250109 30000129 30189935=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 25 07:22:18 2025
    AWUS01 KWNH 250722
    FFGMPD
    TXZ000-251300-

    Mesoscale Precipitation Discussion 1211
    NWS Weather Prediction Center College Park MD
    321 AM EDT Sat Oct 25 2025

    Areas affected...East-Central to Southeast Texas...

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

    Valid 250720Z - 251300Z

    SUMMARY...Forward speed to slow slightly and allow for 2"+/hr
    rates locally. Widely scattered spots of 2-4" totals and
    localized flash flooding remain possible, especially near Houston
    Metroplex.

    DISCUSSION...Regional RADAR mosaic depicts older initial QLCS
    across eastern TX has started to slow with fractured, but still
    broad updrafts, particularly in the southern edges of the line
    from Leon to Henderson county, as the main forcing from shortwave
    DPVA continues to become more oblique as that wave exits across
    the Red River Valley into SE OK. The upstream trailing shortwave
    associated with the strong divergent pattern across the Heat of
    Texas combined with strong meso-high/cold pool is propagating the
    secondary squall line quickly eastward starting to align SSW to
    NNE with the initial line. Solid southeasterly surface inflow,
    veers with height to 850mb becoming increasingly confluent with
    strong 30kts and 30-45 degrees of directional convergence.=20
    Moisture is also much deeper though the Coastal Plain with Tds in
    the low to mid 70s and overall PWats over 1.75".=20

    As the main mid-level wave exits and core of the closed low slowly
    drops southward, the downstream ridging is likely to increase and
    forward speeds are to slow with steering flow shifting from SW
    toward SSW. This will increase overall rainfall duration in
    combination with the strength of moisture flux convergence.=20
    Surface temperatures off the Gulf are also into the lower to mid
    80s providing further buoyancy over the next few hours. Rates
    will increase to 2"/hr and developing streamers off the Gulf,
    localized maxima/transient mergers may further enhanced highly
    localized tropical/deeper warm cloud processes to support focused
    2.25-2.5"/hr totals. The line will still be forward propagating
    and should limit some of the duration but still support scattered
    incidents of 2-4" totals while an isolated 5" not completely out
    of the realm of possibility given 00z HREF probability of 20-25%
    across far SE TX through 15z; though 3" probability reach 70-90%
    along and downstream of the Houston Metro providing some
    confidence for localized possible flash flooding incidents through day-break.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8up3DJtTG51ajbcvYZByA5q3tpR4ley3ETFHi-w3FNGrkTh7yo9xAjXaOONmrwmu_WTB= Jl3OeIXS3oi0-5XiZf2F1Ps$ for graphic product...

    ATTN...WFO...FWD...HGX...LCH...SHV...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32269484 31969414 31429380 30819371 29789401=20
    29199489 28609569 28629623 29219645 29909640=20
    30369634 31479614 31899590 32159556=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Oct 25 19:25:55 2025
    AWUS01 KWNH 251925
    FFGMPD
    TXZ000-260115-

    Mesoscale Precipitation Discussion 1212
    NWS Weather Prediction Center College Park MD
    323 PM EDT Sat Oct 25 2025

    Areas affected...Central TX

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

    Valid 251923Z - 260115Z

    SUMMARY...Heavy showers and thunderstorms will be redeveloping and
    gradually expanding in coverage going through the early evening
    hours. Some cell-training concerns and locally high rainfall rates
    coupled with recent moistening of soil conditions may foster
    localized areas of flash flooding.

    DISCUSSION...The early-afternoon GOES-E visible satellite imagery
    in conjunction with surface data shows the boundary layer across
    central TX gradually destabilizing as a cold front approaches from
    the west. This is evidenced by an expanding CU/TCU field along
    with a southwest/northeast oriented axis of showers and
    thunderstorms that has developed from KBBD to just north of KMNZ.

    Solar insolation combined with fairly steep mid-level lapse rates
    have allowed MLCAPE values across the eastern portions of the TX
    Hill Country to increase to as much as 1000 to 1500 J/kg. This
    coupled with moderately strong effective bulk shear values (30 to
    40 kts) and arrival of deeper layer ascent associated with jet
    energy rounding the base of the southern Plains upper
    trough/closed low should favor an uptick the coverage of
    convection over the next few hours across central TX.

    Areas a bit farther off to the east involving eastern TX are much
    more stable in the wake of the early morning QLCS, and the latest
    RAP analysis shows this region struggling to destabilize, so much
    of the heavy rainfall threat in the near-term should be across
    portions of the TX Hill Country up into the TX Triangle region.
    This is where better low-level convergence ahead of the front and
    interaction with unstable southwest flow will be noted.

    Some cell-training concerns are going to be possible with the
    convection given the linear nature of the activity along with
    alignment close to the deeper layer steering flow. Rainfall rates
    will be capable of reaching 1.5 inches/hour with the stronger
    storms, with some localized 2 to 4 inch rainfall totals possible
    where the better cell-training occurs through early this evening.
    The latest HRRR and RRFS guidance supports this, but the RRFS is
    notably wetter and probably too wet given the modest PW
    environment (~1.25 inches) and moisture transport regime.

    Given the rainfall potential and locally moistened soil conditions
    from last night's rainfall, there may be a localized threat for
    some flash flooding heading through early this evening.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5abBr_tUvcIQ38IHIAQqo8ktwJT7BlAcXgbR9Vm24rUZLEPHbahC6jGXaDGXn3OYNIZ8= BGMPcugFs-TiQJJXnGwgWGI$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32749635 32559589 32159571 31509585 30719681=20
    30239838 30279977 30580014 30910011 31219959=20
    31499898 31799842 32629718=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 26 02:12:02 2025
    AWUS01 KWNH 260211
    FFGMPD
    MSZ000-LAZ000-TXZ000-260800-

    Mesoscale Precipitation Discussion 1213
    NWS Weather Prediction Center College Park MD
    1011 PM EDT Sat Oct 25 2025

    Areas affected...Southeast TX...Much of Western & Central LA...Far
    Southwest MS...

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

    Valid 260210Z - 260800Z

    SUMMARY...Expanding convective lines to merge/converge with some
    internal cell training/repeating expected. Uptick in moisture
    flux will increase rainfall efficiency and support up to 2"/hr
    rates. SW to NE swath of 2-4" totals may result in scattered
    incidents of flash flooding overnight.

    DISCUSSION...GOES-E WV suite shows broad, symmetric and well
    defined closed low dominating the Southern Plains encroaching on
    the Lower Mississippi River Valley as the lead height-falls has
    pressed through into MS toward W AL. The secondary/wrap around
    energy and core of the upper-low is currently tracking along the
    Red River with another internal jet streak and associated
    upper-level divergence and DPVA for broad scale ascent across the
    southeast quadrant of the circulation across E TX into LA. EIR
    loop shows scattered overshooting tops along a west to east axis
    of convergence along a pre-frontal trough dropping southeast
    becoming more orientated to the deeper layer southwesterly
    steering flow. However, the favorable ascent pattern has positive
    influence across much of SE TX into LA, where low level cu-field
    noted in 3.9um and regional RADAR mosaic are showing developing
    narrow cored thunderstorms broadly from the central TX coast into
    central LA ahead of the main line.

    RAP/CIRA LPW analysis denotes core of higher theta-E air and
    moisture values of .75-1" in the surface to 850mb layer across the
    TX Coastal Plain into SW LA and up the MS River to near the AR
    border. Highest buoyancy air also tends to reside closer to the
    coastal region with MLCAPE up to 1500 J/kg along and downstream of
    the main line. As such, additional downstream cells are
    expanding/developing in the next few hours with broad LLJ over the
    Western Gulf becoming increasingly confluent increasing overall
    convergence for expanding convective development. In addition,
    this flux of 1.5-1.8" total PWats (mainly below 700mb) and LLJ
    ramping up to 25-30kts over the next few hours will support
    broadening updrafts capable of 2"/hr. As the DPVA further drops
    southeast, orientation of broader SW to NE wedge of convective
    complex will support embedded northeast motions for short-term training/repeating as the overall propagation is steadily
    east-southeast. Prolonged moderate rainfall with these embedded
    strongest bursts should allow for a broader area of 2"+ rainfall
    with localized totals of 4"+ through 09z with best probabilities
    located from SW to central LA pushing toward SW MS toward the end
    of the period.=20

    Of note toward the end of the valid time (, the surface warm front
    along the MS is likely to be steepened through depth as the
    strength of the easterly flow across the Tennessee Valley and
    central AL undercuts and increases FGEN/ascent plane for
    isentropic development.

    Hydrologically, the area has been relatively dry though this
    morning's initial convective line has moistened up some of the
    upper soil columns for greater infiltration and naturally higher
    FFG due to sandier profiles ( 2-3"/hr and 3-4.5"/3hrs), should
    help to limit flooding potential. However, scattered to widely
    scattered flash flooding will remain possible, especially in/near
    prone urban centers.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5d1ibIQqoy2aXcOcc4_EYbSlKQJXhbqWQzWMesf7IxipAbB29iD-dZzFPhGt3NaKn0XU= cjT68MhRi8kzHLaER4cLPCk$ for graphic product...

    ATTN...WFO...EWX...HGX...JAN...LCH...LIX...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 32779209 32569099 31869082 30959140 30189242=20
    29479407 29069486 28529598 28809650 29909716=20
    30869599 31439529 32319423 32699347=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 26 06:45:33 2025
    AWUS01 KWNH 260645
    FFGMPD
    MSZ000-LAZ000-ARZ000-261230-

    Mesoscale Precipitation Discussion 1214
    NWS Weather Prediction Center College Park MD
    245 AM EDT Sun Oct 26 2025

    Areas affected...Lower Mississippi River Valley...

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

    Valid 260645Z - 261230Z

    SUMMARY...Large MCS cluster will continue to produce 1.5-2"/hr
    rates and streaks of 2-3.5" totals as it progresses across the
    Lower MS River Valley through early morning. Scattered incidents
    of localized flash flooding remain possible, especially near
    urban/poor drainage areas.

    DISCUSSION...GOES-E WV suite shows slightly unbalanced closed low
    has core of vorticity swinging with weak negative tilt from the
    center in SE OK across central LA. Further aloft, nearly ideal
    diffluent dual jet structure is providing about 30-45 degrees of
    split and strong divergence aloft to evacuate and maintain broad
    meso-scale ascent along and downstream of the shortwave trof.=20
    Regional RADAR mosaic denotes a weak MCV-like wave riding
    northeastward along the western side of the progressive
    squall-line located just west of ESF. Low to mid-level flow
    continues to respond with strong LLJ of 20-30kts extending from
    the upper TX coast through the Mouth of the MS all confluent
    downstream of this wave. Total PWats are nearing 2" given the
    overall piling of low to mid-level moisture and wedge of WAA
    remains fairly unstable with uncapped MLCAPE ranging from 500 J/kg
    up to the AR/MS/LA border and as high as 1500 J/kg south of Baton
    Rouge. As such, the strong moisture flux will maintain 1.75"/hr
    rates with occasional uptick toward 2"/hr where storm scale
    convergence is maximized.=20

    While the upper-low still is advancing at a solid eastward
    progression, the deep layer steering flow is starting to shift
    from SW-NE toward a more S to NNE angle. Downstream
    training/repeating will continue to allow for 2-3.5" streaks of
    rainfall in a 2-3 hour period generally between I-20 and I-10
    mainly as the instability reduces further north with time. More
    scattered but stronger cells may be capable of slightly higher
    rates, but duration is likely to be a bit more limited in/along
    the I-10 corridor.=20=20

    Hydrologically, FFG is 2-3"/hr (lower north of I-20) and
    3-4"/3hrs, so overall totals will be near those values suggesting
    scattered localized flash flooding remains possible with highest
    risk of flash flooding in urban locales due to impermeable
    surfaces and higher runoff. So all considered, flash flooding is
    considered possible through 12z.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!67Am17KXkXDdRIACj7ZxMsXJ217SGU2qQRBq71MGCB2Dw2JxLjp0OCR6bYw0QKEfeUOt= vQIX0lmai_G2QxP21xKO610$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...SHV...

    ATTN...RFC...ORN...NWC...

    LAT...LON 33469015 33158953 32578923 31398933 29848973=20
    28939002 29019097 29619317 30579278 31869218=20
    33109162 33419113=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 26 12:58:59 2025
    AWUS01 KWNH 261258
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-261856-

    Mesoscale Precipitation Discussion 1215
    NWS Weather Prediction Center College Park MD
    857 AM EDT Sun Oct 26 2025

    Areas affected...Central Gulf Coast

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

    Valid 261256Z - 261856Z

    SUMMARY...Isolated to scattered flash flooding will remain
    possible through the morning and into the early afternoon across
    portions of the central Gulf Coast as convection slowly moves
    eastward.

    DISCUSSION...Recent radar imagery shows areas of heavy rainfall
    continuing to move eastward across portions of southeast LA and
    southern MS this morning. IR imagery indicates colder cloud tops
    are being maintained, and GLM shows plenty of lightning activity.
    This convection is being supported by strong synoptic ascent ahead
    of a closed mid level low and within a strongly divergent region
    of the upper level flow. Meanwhile, 30 to 40 kts of low level
    south to south southeasterly flow is producing strong moisture
    transport and convergence. The better instability is confined
    closer to the coast, suggesting the highest rainfall rates should
    be across southeast LA into far southern MS. However some of the
    stronger low level convergence is farther north, which should help
    compensate for the lower instability and drive some localized
    higher rainfall rates here as well. The convection will continue
    to progress off to the east, limiting the duration of highest
    rates. However, some brief backbuilding/training of cells into the
    strong low level inflow will continue to support some areas of
    more persistent rainfall rates. Hourly rainfall should continue to
    locally get into the 2-3" range.

    Recent HRRR runs continue to indicate 1-3" of rain within the MPD
    area, with localized totals over 3". Recent RRFS runs are a bit
    higher, showing localized max values over 5" through 19z. Overall
    think a compromise of the two is most likely, with localized
    rainfall amounts getting into the 3-5" range through 19z where
    some brief backbuilding is able to locally extend the duration of
    higher rates. Will also note that the HRRR is probably a bit slow
    with the eastward progression of the convection, with the RRFS
    probably better with the idea of heavier rainfall totals getting
    into coastal AL by later this morning.

    FFG is quite high across this area, generally 3" in one hour and
    4" in 3 hours. It seems unlikely this will get exceeded on a
    widespread basis, however where some brief training can occur we
    should be able to continue to locally exceed these amounts. Thus
    an isolated to scattered flash flood risk is likely to continue,
    with an emphasis on urban areas where runoff is enhanced.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6-CVi1ln5byFJMQcIWGGY0CoTOnqyzzqDQAMZWm7T1h3sAbJKTef1dloAvCWRAzSZ0Bk= No94LJRzuGDbyWJknbDfBzo$ for graphic product...

    ATTN...WFO...JAN...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 31838994 31688862 31408795 30418726 29388857=20
    28908922 28918978 29279039 30039039 30549035=20
    30829040 31299048=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 26 21:03:12 2025
    AWUS01 KWNH 262103
    FFGMPD
    FLZ000-270300-

    Mesoscale Precipitation Discussion 1216
    NWS Weather Prediction Center College Park MD
    502 PM EDT Sun Oct 26 2025

    Areas affected...Space Coast region into central portions of FL
    Peninsula

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

    Valid 262100Z - 270300Z

    Summary...Rainfall rates as high as 3"+/hr with slow moving
    thunderstorms to result in short-term isolated totals of 5"+ with
    localized flash flooding likely.

    Discussion...Mid-level dry air has eroded sufficiently to allow
    for deep convection to take root across portions of the central FL
    Peninsula, becoming most robust along the eastern Space Coast
    region where low-level convergence has become maximized along the
    coast (with weaker, generally more progressive convection
    extending well to the west along a weak surface front/thetaE
    gradient). The mesoscale environment is characterized by PWs of
    1.5-1.8" (already near the 90th percentile, and may increase to
    beyond 2.0" locally with continued upscale growth of convection),
    plentiful instability (SB CAPE of 2000-3000 J/kg), and effective
    bulk shear of 30-40 kts (also near the 90th percentile, per XMR
    sounding climatology).

    Hi-res models trended quite wetter (and in surprisingly strong
    agreement) with the 12z cycle, as both the HREF and REFS indicate
    high odds of localized 5" exceedance through 03z (near 60% and 50% respectively, per 40-km neighborhood exceedance probabilities).
    This is near the corresponding 6-hr FFG threshold, though much of
    these totals could occur in a 3-hr period or less (as evidenced by
    estimated hourly rainfall near 3" from the first evident supercell
    near the Space Coast Regional Airport, which is nearly stationary
    in accordance with the bunkers right-mover vectors indicating
    motions of 5 kts or less). Given this strong hi-res guidance
    signal and recent observational trends, localized instances of
    flash flooding are likely (and may be locally significant in
    relatively low lying urbanized terrain with poor drainage).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_vIIAFNLjgdXNTMhbd1y_rT6ZamAyYMGqcKgE9sFIHRTR7ZttcM_Y6etTl8pQxx2NO3f= trw-SU5qKo1h0zpR--pjDLM$ for graphic product...

    ATTN...WFO...JAX...MLB...TBW...

    ATTN...RFC...ALR...NWC...

    LAT...LON 29488163 29258104 28618048 28218076 28288150=20
    28598201 28998214=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 26 23:51:14 2025
    AWUS01 KWNH 262351
    FFGMPD
    FLZ000-GAZ000-270549-

    Mesoscale Precipitation Discussion 1217
    NWS Weather Prediction Center College Park MD
    750 PM EDT Sun Oct 26 2025

    Areas affected...Eastern FL

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

    Valid 262349Z - 270549Z

    Summary...Thunderstorms are increasing in coverage from the Gulf
    Coast north towards the Space Coast. A threat for 3" an hour
    amounts and local totals to 7" exists/continues, which would be
    problematic in urban areas.

    Discussion...An upper level low near the MO Bootheel is moving
    east, along with the base of its attendant upper level trough
    across the central Gulf Coast. An additional shortwave is moving
    to the north of FL into the southernmost Appalachian Piedmont.=20
    Downstream across Florida, diffluent flow exists, which has helped
    to sponsor thunderstorms with heavy rainfall which are increasing
    in coverage from the Gold Coast northward. A weak baroclinic zone
    across the central FL peninsula was acting as a reasonable
    convective focus earlier, but recent radar trends suggest that the
    coastline is becoming a better focus as CIN develops inland and
    winds weaken inland after sunset due to frictional convergence.=20
    Precipitable water values are 1.5-2" across the state. Inflow at
    850 hPa is out of the east-southeast while the flow aloft is
    westerly. Effective bulk shear of 25-40 kts exists which is
    helping to organize some convection, but not all, which appears to
    about to lead to cell collisions.

    The thunderstorm activity as a broad group should shift north and
    possibly offshore northeast FL over the next several hours as 850
    hPa flow veers more to the southeast to south. The 18z HREF
    guidance appears to have a reasonable grasp on the current
    convective pattern. Thus far today, hourly amounts to 3" and
    local totals to 7" have occurred in east-central FL, which appear
    to be reasonable upper bounds on future potential. These amounts
    would be problematic along the East Coast of the state, which led
    to a recent broadening of the Marginal and Slight Risk areas in
    the evening Excessive Rainfall Outlook. Flash flooding is
    expected to be at least widely scattered in coverage.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6Nf-iyyNrwNGvgA3tnQptqT3PXkZXnS11TOp9xGoWMmY5pSKrz8khyqHg78FYEGCK5YC= mMtm-1Qnxn4U-2VdoBsZhRI$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 31118134 28818054 27308000 26207994 26038037=20
    27148064 28338126 29288163 30458190=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Oct 26 23:56:15 2025
    AWUS01 KWNH 262356
    FFGMPD
    FLZ000-GAZ000-270549-

    Mesoscale Precipitation Discussion 1217...Corrected
    NWS Weather Prediction Center College Park MD
    755 PM EDT Sun Oct 26 2025

    Corrected for amounts thus far in east-central FL

    Areas affected...Eastern FL

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

    Valid 262349Z - 270549Z

    Summary...Thunderstorms are increasing in coverage from the Gulf
    Coast north towards the Space Coast. A threat for 3" an hour
    amounts and additional local totals to 6" exists/continues, which
    would be problematic in urban areas.

    Discussion...An upper level low near the MO Bootheel is moving
    east, along with the base of its attendant upper level trough
    across the central Gulf Coast. An additional shortwave is moving
    to the north of FL into the southernmost Appalachian Piedmont.=20
    Downstream across Florida, diffluent flow exists, which has helped
    to sponsor thunderstorms with heavy rainfall which are increasing
    in coverage from the Gold Coast northward. A weak baroclinic zone
    across the central FL peninsula was acting as a reasonable
    convective focus earlier, but recent radar trends suggest that the
    coastline is becoming a better focus as CIN develops inland and
    winds weaken inland after sunset due to frictional convergence.=20
    Precipitable water values are 1.5-2" across the state. Inflow at
    850 hPa is out of the east-southeast while the flow aloft is
    westerly. Effective bulk shear of 25-40 kts exists which is
    helping to organize some convection, but not all, which appears to
    about to lead to cell collisions.

    The thunderstorm activity as a broad group should shift north and
    possibly offshore northeast FL over the next several hours as 850
    hPa flow veers more to the southeast to south. The 18z HREF
    guidance appears to have a reasonable grasp on the current
    convective pattern. Thus far today, hourly amounts to 3" and
    local totals to 10" have occurred in east-central FL. Believe
    hourly amounts to 3" and additional local amounts to 7" are
    possible. These amounts would be problematic along the East Coast
    of the state, which led to a recent broadening of the Marginal and
    Slight Risk areas in the evening Excessive Rainfall Outlook.=20
    Flash flooding is expected to be at least widely scattered in
    coverage.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9RRqNhRs5CLZzRZbOt3JS2A4damiKVzPADWhiDqYblGS-nEtnjHzg-jt43GBGOirN6bh= 55kGKxHuFiLsnqYkpmuYgQI$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 31118134 28818054 27308000 26207994 26038037=20
    27148064 28338126 29288163 30458190=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 27 02:14:18 2025
    AWUS01 KWNH 270214
    FFGMPD
    FLZ000-ALZ000-270800-

    Mesoscale Precipitation Discussion 1218
    NWS Weather Prediction Center College Park MD
    1013 PM EDT Sun Oct 26 2025

    Areas affected...Southern Alabama...Western Florida Panhandle...

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

    Valid 270215Z - 270800Z

    SUMMARY...Slow moving, efficient supercells in proximity to the
    front and ample deep layer moisture flux will support rates of
    2-2.5"/hr. Localized totals of 3-5" are possible in proximity to
    urban locations along I-10. Localized rapid inundation flooding
    is becoming increasingly possible.

    DISCUSSION...KMOB RADAR along with GOES-E 3.9/10.3um animation
    shows organizing thunderstorms across Mobile Bay. GOES-E WV shows
    the core of the upper-level jet is squarely atop of the developing
    cells but is shifting eastward bringing a more favorable larger
    scale ascent pattern over S AL into W FL over the next few hours.=20
    Combine this with strong shortwave digging across Arkansas,
    sliding a bit negative tilt across MS further adding larger scale
    ascent, while also strengthening low level confluent flow across
    the Northern Central Gulf. A persistent stationary front hugs the
    coastal zone from Mobile Bay toward Gulf county in the W FL
    Panhandle, south of which as solid theta-E, but also strong
    easterly flow is anchoring/steepening the front across the area
    too, increasing vertical isentropic ascent from south to
    southwesterly flow at and above the boundary layer with solid
    strong moisture convergence.=20

    The upper-level wave is helping to finally propagate the cold
    front across S MS and WAA is lifting the front off the Gulf. So
    cells and higher instability/theta-E air should lift into far S AL
    a bit more with 1000-1250 J/kg of MLCAPE. While deep layer
    moisture has been advected eastward, the surface to lower boundary
    layer remains very saturated with Tds in the low to mid 70s and
    total PWats at or above 1.75", mainly in the sfc to 850 layer with
    .75 to .9" per CIRA LPW. GOES-E 3.9um shows a SW to NE
    confluence axis from the Boothville, LA toward the MS/AL coast.
    This may be a solid trending axis for additional upstream
    development. Also, given the proximity to the front, the low
    level shear is fairly strong with over 35-40 kts of bulk shear,
    but also nearly 200 m2/s2 of low-level helicity supportive of
    super-cell structures. The combination of 45-60 degrees of
    southerly flow from SE to WSW through 800mb at 30kts+ will allow
    for high concentrated moisture flux convergence of these higher
    values and support rates of 2-2.5"/hr.

    Forward propagation near the warm front will be very slow as well,
    with Bunker's right mover propagation vectors about 5 kts to the
    east, further increasing duration and potential for localized 3-5"
    totals. Proximity to urban locations from Mobile Bay eastward
    along I-10 would support possible rapid inundation flooding
    potential as the cells continue to strengthen/broaden increasing
    rainfall coverage as well.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_bs5j5LJ0VqyhPFjGItx8AsYUVPG0vqpFBbeZ5_J27ViAmLa4NKJ2UfKLBgp6MVerhZs= HhRw-EPzAdQCBTaK_Of15OE$ for graphic product...

    ATTN...WFO...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 31288732 31198679 30868651 30528656 30318683=20
    30208728 30228820 30998826 31248785=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Oct 27 07:12:19 2025
    AWUS01 KWNH 270712
    FFGMPD
    FLZ000-271300-

    Mesoscale Precipitation Discussion 1219
    NWS Weather Prediction Center College Park MD
    311 AM EDT Mon Oct 27 2025

    Areas affected...Westerm Florida Panhandle...

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

    Valid 270715Z - 271300Z

    SUMMARY... Rates of 2"/hr and totals of 2-4" to continue risk of=20
    rapid inundation flooding along the urban locales of the immediate
    coast of western FL Panhandle=20

    DISCUSSION...GOES-E 3.9 SWIR and RADAR from EVX shows a pair of
    narrow N-S oriented bands within the warm sector over the near
    shore waters of the northern Gulf. Confluent flow has narrowed in
    direction but speed remains about 20-30kts through 700mb.=20
    Sufficient veering through depth shows WAA profile still
    supporting 50 kts of effective bulk shear and about 200 m2/s2 of
    helicity to maintain rotating updrafts. These rotating updrafts
    continue to slightly enhanced the localized flow providing further
    escalation of moisture flux convergence in the lowest 10-15Kft of
    storm. Given bulk of 1.75-2" total Pwats (~1-1.25" per CIRA LPW)
    will maintain solid rainfall efficiency with rates of 2"/hr likely
    to continue with these back to back lines of updrafts. Deep layer
    steering and Bunkers right mover propagation vectors suggest a
    slight increase in speed to 10-15kts but also a slight right
    deflection along the surface front and coastline, probably with
    some frictional speed convergence due to land as well.

    Aloft, the 80kt WSW to ENE speed max remains slightly upstream and
    to the southwest, leaving the developing cells within continued
    favorable divergence aloft in the left exit ascent region. The
    shear is strong, but mainly above 500mb and is not generally
    disrupting the depth of the rainfall generation region below
    700mb. Slow eastward propagation of the larger scale
    divergence/oblique height-falls across N MS/AL, duration of heavy
    rainfall could be 1-2+ hours given back to back updrafts. As a
    result a streak of 2-4" totals is plausible; however, greatest
    totals may start to fall just offshore or directly along the
    beaches. So while the area is sandy and has high FFG values, the
    area still remains fairly urban and more prone to rapid inundation
    flooding. As such, this style of flooding remains possible
    through the early morning hours along the western FL Panhandle.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-QqtMZV6dZlGOYQYuxmY2iKGSO0x53XygaABfgT6ZNCOMXwY3Ow0xU7zeNESQLbnDmf-= M77jWytZ_qNZgUuGxNeCG3U$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 30808683 30728600 30428520 30098505 29838513=20
    29668540 30128590 30318660 30348719 30638722=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 Oct 30 19:33:13 2025
    AWUS01 KWNH 301933
    FFGMPD
    MAZ000-CTZ000-NYZ000-NJZ000-PAZ000-310125-

    Mesoscale Precipitation Discussion 1220
    NWS Weather Prediction Center College Park MD
    332 PM EDT Thu Oct 30 2025

    Areas affected...northern NJ into southern NY/Long Island and CT

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

    Valid 301931Z - 310125Z

    Summary...Heavy rain across the Tri-State Area through this
    evening may result in localized flooding/flash flooding. Localized
    rainfall totals over 3 inches will be possible. Rainfall near 1
    inch in 15-30 minutes can be expected.

    Discussion...19Z radar imagery showed a low-topped squall-line,
    oriented from south to north, edging east from 40 miles east of
    ACY through NYC. This line was being aided by strong low level
    convergence with 45-50 kt from the SSE/SE in the 925-850 mb layer,
    located north of the triple point of an occluded cyclone over the
    northern Mid-Atlantic region. The line of showers has been
    accompanied by 0.50 to 1.00 inches of rain in 15 minutes across
    northern NJ into the Five Boroughs.

    Moisture from the Mid-Atlantic coast into southern New England was
    already anomalous as sampled by area 12Z RAOBs, with PWAT values
    of 1.2 to 1.5 inches. However, OSPO's ALPW has since shown an
    increase stemming from Melissa's circulation, especially near and
    below 700 mb, being drawn northward into NJ and southern NY. The
    continued addition of this remnant tropical moisture should allow
    for an increase in rainfall efficiency and locally higher rainfall
    rate potential into the early evening hours.

    While the line of showers has been progressive, there is some
    concern for very brief slowing/stalling given the LEWP-like
    appearance off the NJ coast, which could result in a quick 1-2
    inches as this line continues to advance east through the
    remainder of the afternoon. As a triple point low becomes better
    organized south of Long Island this evening, low level flow will
    maintain a southeasterly orientation, with possible backing.
    Therefore, some orographic component to lift will be added into
    the equation for the higher terrain north and west of I-95,
    combining with increasing right-entrance jet ascent associated
    with a forecast 130 kt jet streak on the east side of the parent
    upper low to the west.

    Farther south and west, instability is expected to remain weak
    (briefly peaking in the 500-1000 J/kg range) but perhaps
    sufficient to support a few additional heavy showers from eastern
    PA and southern NJ, rotating northward into the Tri-State region.

    Additional rainfall may result in isolated areas of rapid
    inundation of water. Given below average rainfall over the past
    few weeks and ongoing drought conditions across portions of the
    region, any flooding that occurs is likely to remain constrained
    to urban or other areas with poor drainage.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9FIRi1NKBOaCg4MfFWriOWtP0K6LX9dCRMYV3e6rRPxWaiMPuzVhGNzgIyu1jio3gLQk= znq132MoWRgl8CwwSNIVZGE$ for graphic product...

    ATTN...WFO...ALY...BGM...BOX...OKX...PHI...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 42367414 42157352 42087251 41907210 41397212=20
    40707286 40387404 40737491 41357535 42037519=20
    42327478=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Nov 13 09:59:44 2025
    AWUS01 KWNH 130959
    FFGMPD
    CAZ000-ORZ000-132158-

    Mesoscale Precipitation Discussion 1221
    NWS Weather Prediction Center College Park MD
    458 AM EST Thu Nov 13 2025

    Areas affected...much of central and northern California

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

    Valid 130958Z - 132158Z

    Summary...Heavier downpours should result in instances of urban
    flooding around San Francisco and vicinity during and after
    morning commute. Heavier rainfall will also spread into more of
    northern and central California from 13Z/6a PT through the
    evening. Flash flooding is expected especially near burn scars,
    urban areas, and other terrain-favored spots.

    Discussion...As of 0955Z, a band of convection was beginning to
    organize along a front extending from near 80 miles southwest of
    Eureka to 180 miles southwest of Monterrey. Individual convection
    along this band was streaming northward at a decent clip.=20
    However, the band was only moving slowly eastward and already
    favoring areas of repeating over open waters. 500 J/kg MUCAPE and
    areas of 1.3+ PW values were supporting the convective band, and
    MRMS data was already estimating 0.5-0.7 inch hourly rain rates
    over land just southwest of Eureka.

    The convective band and associated mid-level system are expected
    to make only slow eastward progress toward more land areas of
    California today. As the systems approach, low-level wind fields
    will strengthen, colliding with terrain and locally enhancing rain
    rates in many areas. Rates could reach 1 inch/hr on a localized
    basis. These rates will overspread portions of the San Francisco
    Metro beginning in the 12Z/5a PT hour and persist through the
    afternoon, impacting morning rush with wet roads and areas of
    excessive runoff. Portions of north-central through east-central
    California will also experience terrain-enhanced heavy rainfall,
    with some of the heavier rates (exceeding 0.75 inch/hr) falling on
    sensitive ground conditions and burn scars. Flash flooding is
    expected on at least an isolated basis. These areas could include
    terrain near/north of Redding (beginning around 13Z/6a PT) and
    upslope areas of the Sierra (near/east of Chico) beginning around
    14Z/7a PT. Heavy rainfall could last for 8-12 hours in many of
    the aforementioned areas, with totals of 3-5 inches likely through
    00Z Fri Nov 14.

    Again, at least a few instances of flash flooding are expected
    given the scenario.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5VKp-a7ebjiWmrdoxeWU409Xa9908ABb97wCJOe4OanaamOWmB6toVZM_1LbzpdVv3ry= Zvl45SPmtpirwxkshqXUjlM$ for graphic product...

    ATTN...WFO...EKA...HNX...LOX...MFR...MTR...REV...STO...

    ATTN...RFC...PTR...RSA...NWC...

    LAT...LON 42252315 42102191 41712116 41262098 40792092=20
    40142070 38461980 37801954 36581993 35282051=20
    35472124 37712319 40152469 41802483 42162420=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 13 21:36:24 2025
    AWUS01 KWNH 132136
    FFGMPD
    CAZ000-140900-

    Mesoscale Precipitation Discussion 1222
    NWS Weather Prediction Center College Park MD
    435 PM EST Thu Nov 13 2025

    Areas affected...western Transverse Ranges into central CA and
    northern Sierra Nevada

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

    Valid 132133Z - 140900Z

    Summary...Flash Flood potential will extend into the evening and
    overnight hours from portions of the northern Sierra Nevada into
    much of central CA and the western Transverse Ranges. Peak hourly
    rainfall of 0.5 to near 1.0 inches is expected along with peak 12
    hour rainfall values of 2 to 4 inches through 09Z.

    Discussion...21Z radar imagery and GOES West infrared satellite
    imagery showed a band of moderate to heavy rain extending from
    Monterey Bay and the northern Santa Lucia Range into the eastern
    Pacific, out ahead of a Pacific cold front. The cold front has
    been steadily advancing east since this morning and was preceded
    by an atmospheric river containing max PW values of 1.3 to 1.5
    inches along the coast and just offshore. Within this plume were S
    to SSW 850-700 mb winds of 40 to 50+ kt, supporting earlier hourly
    rainfall of 0.7 to near 1 inch across the Santa Cruz Mountains. A
    number of reports of flooding and debris flows have been observed
    since earlier this morning, in and around the San Francisco Bay
    region down to Monterey Bay.

    As a closed low centered near 41N 128W and southward extending
    trough/low, as seen on water vapor imagery, continues to advance
    closer to the coast, some weakening of the mid-level low is
    expected as the system continues to mature and evolve. The cold
    front will maintain a slow but steady movement toward the east but
    a ~10 kt weakening of the 850-700 mb winds is expected as the
    moisture axis advances downstream ahead of the cold front. This
    weakening will correspond to a lowering of IVT values over land,
    maxing out in the 600-800 kg/m/s range through 09Z Friday.

    Occasional peak hourly rainfall of 0.5 to ~1 inch is expected to
    be focused within locations where low level winds will focus into
    S to SW facing terrain. The most likely locations for these higher
    rates will be within the Coastal Ranges and Sierra Nevada but any slowing/stalling of a band of weak convection across the San
    Joaquin Valley will also have the potential to produce these
    higher rates given the moisture already present and weak MLCAPE up
    to 500 J/kg forecast by the RAP.

    Most instances of flooding/flash flooding are expected to be
    minor, but will be most probable across urban and other flood
    prone locations. However, localized occurrences of more impactful
    flash flooding will be possible where overlap of heavy rain occurs
    with any sensitive burn scars and terrain with potential for
    debris flows.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6vhVfx5PrvXg1YFxrXbaLnPzE8TiC_lEuN1IOc2Kw_1rXYSFvDpdUCX5jP9z4cFbAig2= v04FN10JYa31QCEWqszhT5M$ for graphic product...

    ATTN...WFO...HNX...LOX...MTR...REV...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 40682176 40442144 39982074 39642050 39382033=20
    39082023 38842014 38692005 38551994 38481986=20
    38361970 38241972 38131973 38081971 37921946=20
    37821936 37701937 37601929 37511915 37431904=20
    37151884 36991877 36861884 36661952 36832010=20
    36462052 35822041 35232021 34941972 34421932=20
    34271951 34302044 34462098 35252146 35842184=20
    36472222 37032175 38842141 40302192=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Nov 14 09:21:01 2025
    AWUS01 KWNH 140920
    FFGMPD
    CAZ000-141518-

    Mesoscale Precipitation Discussion 1223
    NWS Weather Prediction Center College Park MD
    420 AM EST Fri Nov 14 2025

    Areas affected...portions of southern California

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

    Valid 140918Z - 141518Z

    Summary...Flash flood potential continues across portions of
    southern California for at least another 4-6 hours. Areas of 2-3
    inch rainfall totals are expected that could cause excessive
    runoff and debris flows.

    Discussion...Flash flood potential will continue through at least
    15Z/7a Pacific Time this morning. A fetch of strong onshore flow
    continues just ahead of a cold front along the coast extending
    from near PRB near VBG. Just ahead of this front, mesoanalyses
    indicate a focused area of 35 knot 850mb flow oriented
    perpendicular to the western Transverse Ranges (Santa Barbara and
    Ventura Counties). This orientation, ~1.5 inch PW, and modest
    instability was supporting repeating heavy rainfall at times
    across the discussion area. The repeating nature of the rain was
    resulting in spots of 1 inch/hr rain rates in local areas from the
    Santa Ynez mountains through the Sierra Madre mountains and
    surrounding areas. Low spots were responding with runoff over
    area roadways over the past few hours, and reports of flooding
    have been received in the discussion area near Highway 101.

    The ongoing scenario will continue for another 4-6 hours or so.=20
    The mid-level system partially responsible for the ongoing heavy
    rainfall hazard has stalled, and the attendant cold front will
    also become stationary. Meanwhile, 35 knot 850mb flow will
    continue to impinge on the Transverse Ranges and prompt several
    hours of intermittent heavy rain. The very high PW values and
    local burn scars yield concern that locally significant flash
    flooding could occur. Rainfall totals of 2-3 inches are also
    possible in a few spots through 15Z.

    At some point around/after 15Z, 850mb wind fields should slacken
    some and result in a gradual lessening of heavy rainfall potential
    especially after 15Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-YSANlPNsKgyhhxUH_7CB_jGnyTop2DRWsmPl_jtGQwo0EXHDv54zvvlmZJGVIBF9zjD= uJIxqChoHOgAm-IC_6FrKYQ$ for graphic product...

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

    ATTN...RFC...RSA...NWC...

    LAT...LON 35782038 35561882 34761781 34121776 33911846=20
    34422009 34702073 35072071 35342098=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Nov 14 09:22:30 2025
    AWUS01 KWNH 140922
    FFGMPD
    CAZ000-141518-

    Mesoscale Precipitation Discussion 1223
    NWS Weather Prediction Center College Park MD
    421 AM EST Fri Nov 14 2025

    Areas affected...portions of southern California

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

    Valid 140918Z - 141518Z

    Summary...Flash flood potential continues across portions of
    southern California for at least another 4-6 hours. Areas of 2-3
    inch rainfall totals are expected that could cause excessive
    runoff and debris flows.

    Discussion...Flash flood potential will continue through at least
    15Z/7a Pacific Time this morning. A fetch of strong onshore flow
    continues just ahead of a cold front along the coast extending
    from near PRB near VBG. Just ahead of this front, mesoanalyses
    indicate a focused area of 35 knot 850mb flow oriented
    perpendicular to the western Transverse Ranges (Santa Barbara and
    Ventura Counties). This orientation, ~1.5 inch PW, and modest
    instability was supporting repeating heavy rainfall at times
    across the discussion area. The repeating nature of the rain was
    resulting in spots of 1 inch/hr rain rates in local areas from the
    Santa Ynez mountains through the Sierra Madre mountains and
    surrounding areas. Low spots were responding with runoff over
    area roadways over the past few hours, and reports of flooding
    have been received in the discussion area near Highway 101.

    The ongoing scenario will continue for another 4-6 hours or so.=20
    The mid-level system partially responsible for the ongoing heavy
    rainfall hazard has stalled, and the attendant cold front will
    also become stationary. Meanwhile, 35 knot 850mb flow will
    continue to impinge on the Transverse Ranges and prompt several
    hours of intermittent heavy rain. The very high PW values and
    local burn scars yield concern that locally significant flash
    flooding could occur. Rainfall totals of 2-3 inches are also
    possible in a few spots through 15Z.

    At some point around/after 15Z, 850mb wind fields should slacken
    some and result in a gradual lessening of heavy rainfall potential.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4kVz9ErDHVyIU0guZRGqc4RFSQxsXmSIXWegJ3Ytu8QbMk0sfY-OKaCW6SphBZsXzoCo= 9UcW436tz7Mjxjo7OEZcotY$ for graphic product...

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

    ATTN...RFC...RSA...NWC...

    LAT...LON 35782038 35561882 34761781 34121776 33911846=20
    34422009 34702073 35072071 35342098=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 15 10:10:50 2025
    AWUS01 KWNH 151010
    FFGMPD
    CAZ000-152209-

    Mesoscale Precipitation Discussion 1224
    NWS Weather Prediction Center College Park MD
    510 AM EST Sat Nov 15 2025

    Areas affected...portions of southern California

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

    Valid 151009Z - 152209Z

    Summary...Heavy rainfall will become more likely - especially
    beginning around the 14Z/6a Pacific timeframe. Rain rates
    reaching 1 inch/hr are possible with this activity. Flash flood
    potential will increase - especially across burn scars and other
    low-lying, urban, and sensitive areas.

    Discussion...Convection was beginning to deepen and move northward
    across open waters adjacent to the southern California coastline
    this morning. This convection was materializing in response to a
    deep cutoff low centered near 32N, 124.5W that was beginning a
    slow migration eastward toward the discussion area. On the
    eastern periphery of this low, a very moist airmass was in place,
    with PW values ranging from 1 inch near coastal areas to 1.6 inch
    just offshore. Weak instability and modest forcing for ascent
    over land areas are limiting factors for heavier rainfall
    potential in the short-term and toward 14Z or so.

    Later this morning, a belt of stronger southerly flow at 850mb
    will develop toward coastal areas extending from the LA Basin
    southward along the San Diego County coastline. Some of this flow
    will interact favorably with coastal ranges (particularly the
    Transverse) to promote an increasing risk of heavier rainfall.=20
    Quick moistening is also expected to accompany this flow over
    those areas. Rain rates should come up in tandem with approaching
    ascent and orographic lift, and areas of 1 inch/hr rain rates
    should occur on a more frequent basis. At least a few instances
    of flash flooding/excessive runoff are expected. Furthermore,
    these rain rates should occur over local burn scars, prompting
    dangerous debris flows in some areas. Locally significant impacts
    will become possible in this regime.

    Heavy rain potential will persist through at least 2200Z/1p
    Pacific Time today and beyond as the upstream mid-level wave makes
    only slow/gradual progress toward land areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7NmB96X_gKbvDQtUDkadiStzOtx5MFz8wPRwxfJkWWbtUL3__jOs9ytla2zeqyDQiJR4= -PFtCV8FgDw9DOF9htvwyZs$ for graphic product...

    ATTN...WFO...HNX...LOX...PSR...SGX...VEF...

    ATTN...RFC...RSA...NWC...

    LAT...LON 35351981 35191853 34841736 34211654 33441614=20
    32791601 32561639 32561714 33101753 33641831=20
    34191949 34552052 35082065=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 15 19:19:58 2025
    AWUS01 KWNH 151919
    FFGMPD
    AZZ000-NVZ000-CAZ000-160115-

    Mesoscale Precipitation Discussion 1225
    NWS Weather Prediction Center College Park MD
    219 PM EST Sat Nov 15 2025

    Areas affected...Desert regions of CA into southern NV and far
    western AZ

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

    Valid 151917Z - 160115Z

    Summary...Periods of heavy rain should become likely across the
    desert regions of eastern/southern CA into southern NV and far
    western AZ through 01Z. Peak hourly rainfall between 0.5 and 1.0
    inches (locally higher) is expected which may result in isolated
    to widely scattered instances of flash flooding.

    Discussion...Radar mosaic imagery across southern CA into southern
    NV at 19Z showed an arcing band of heavy showers continuing to
    move inland, from the Peninsular Ranges toward the far southern
    San Joaquin Valley. Observed hourly rainfall within this axis has
    been in the 0.5 to 0.9 inch range over the past 2-3 hours.
    Additional showers were noted from just west of the lower CO River
    into western Clark County in southern NV with MRMS-derived hourly
    rainfall in excess of 1 inch in eastern Imperial County. These
    showers were forced in response to lift ahead of a negatively
    tilted shortwave trough located ~100 miles off of the southern CA
    coast, swinging toward interior southern CA. In addition,
    divergence and diffluence were increasing across southern CA
    within the left-exit region of a 90-110 kt upper level jet max
    located just south of the shortwave trough axis. Moisture was
    highly anomalous for mid-November with regional PW standardized
    anomalies of 4 to 5+ throughout the area, with a source region
    stemming from the tropical eastern Pacific as seen on OSPO ALPW
    imagery.

    As the closed low and negatively tilted shortwave trough continues
    to advance east over the next 6 hours, low level moisture will
    continue to advect into the deserts with a transient swath of 6.0
    to 6.5 C/km 700-500 mb lapse rates (coincident with the shortwave)
    which should help to briefly boost instability, despite the lack
    of surface heating beneath clouds/rain. Also of note were the
    850-700 mb winds oriented from the southeast at 30-35 kt over
    south-central CA, forcing an upslope component along the eastern
    slopes of the southern Sierra Nevada. With little change to the
    low to mid-level wind fields anticipated over the next 3-6 hours,
    steady upslope forced heavy rain is expected into the terrain.
    Farther east, embedded higher rainfall rates are expected to
    develop through the afternoon within the scattered
    shower/stratiform rain regime. While CAPE values are generally
    forecast to stay below 500 J/kg (outside of the lower CO Valley),
    the anomalous moisture source should contribute to embedded higher
    rainfall values with periods of brief training, allowing for
    hourly rainfall in the 0.5 to 1.0 inch range (locally higher).
    Peak total rainfall of 1 to 2 inches is expected (locally higher
    near terrain) through 01Z which may result in areas of flash
    flooding.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9thXAR0MeAzY90w6Y5yt960fJNwMeBjCZqbAGy3VOG4ggdTCBbyCvWQaMI4GnO868aiI= 9KlPp1Z91dR8bBP6ueFEqGI$ for graphic product...

    ATTN...WFO...HNX...LKN...LOX...PSR...REV...SGX...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 38051725 37481583 36161447 35111412 33431409=20
    32231432 32471532 32481594 33171615 33501626=20
    33671637 33951653 34111664 34231678 34311702=20
    34391729 34501763 34651808 34781841 34911860=20
    35061867 35231863 35381859 35491856 35641849=20
    35721842 35801837 35891833 35961828 36081823=20
    36181815 36311810 36411813 36481817 36601822=20
    36661826 36751829 36851834 36931837 37031839=20
    37121843 37211847 37261852 37321860 37421865=20
    37621866 37861848 38041808=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 15 20:35:59 2025
    AWUS01 KWNH 152035
    FFGMPD
    CAZ000-160230-

    Mesoscale Precipitation Discussion 1226
    NWS Weather Prediction Center College Park MD
    335 PM EST Sat Nov 15 2025

    Areas affected...portions of southern CA

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

    Valid 152033Z - 160230Z

    SUMMARY...The flash flood threat will continue for coastal CA into
    the Transverse and Peninsular Ranges through 02Z. While the
    main/widespread threat of flash flooding is expected to wane over
    the next couple of hours, a lingering threat for more localized
    but potentially significant flash flooding will remain.

    DISCUSSION...Radar mosaic imagery at 20Z showed a band of moderate
    to heavy rain that extended from the southern San Joaquin Valley
    into some of the Valley/Desert regions east of the Peninsular
    Ranges. This axis of heavier rain has been following a plume of
    highly anomalous moisture translating eastward as seen on OSPO
    ALPW imagery, out ahead of a negatively tilted mid to upper level
    shortwave trough axis and vorticity max just west of the CA/MX
    border. Additional heavy rainfall appeared in the waters just east
    of Santa Catalina and San Clemente Islands, tied to the eastern
    lobe of the mid/upper level shortwave. Rainfall over the past 6
    hours has peaked near 1 inch for coastal locations into the
    Peninsular Ranges while 1 to 2+ inch values have been observed
    within portions of the Transverse Ranges, with hourly rainfall
    between 0.5 and ~1.0 inches.

    While relatively drier air was moving into southern CA as of 20Z,
    the moisture remains anomalous with PW values of ~1.0 to 1.3
    inches and despite continued drying of the layer, sufficient
    moisture will remain through the evening to support localized high
    rainfall rate potential. As the closed upper low center continues
    to slowly edge closer to the coast, 700-500 mb lapse rates will
    increase into the 6.5 to 7.0 C/km range and support localized
    MLCAPE values in excess of 500 J/kg near the coast. Lift will also
    be aided by left-exit region divergence/diffluence corresponding
    to a 100 kt upper level jet max positioned south of the upper low
    center. Hourly rainfall in the 0.5 to 1.0 inch range is expected,
    though localized spot training could exceed these values and/or
    support 0.5 to 1 inch of rain in about 30 minutes. The combination
    of continued forcing and increased ground sensitivity due to
    today's rainfall will likely support continued areas of flash
    flooding over the next few hours. This will especially be true
    where additional areas of heavy rain overlap with urban areas and
    burn scars where localized higher impacts could occur. Within
    sensitive burn scar regions, high rain rates are likely to result
    in mudslides and debris flows.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_j_67JJhFHvq_oLXeomayUqUVfoafWQU8SimSG6NwI_NxuB5p1MdyqdZT-jj6t1orl4x= bP4V2_PJ0kcdmAeJVjLQtOk$ for graphic product...

    ATTN...WFO...HNX...LOX...SGX...VEF...

    ATTN...RFC...RSA...NWC...

    LAT...LON 35541966 35531858 35111811 34381686 33961642=20
    33361612 32881611 32461613 32451668 32421710=20
    32521739 32741783 33201827 33431858 33891947=20
    34462098 35302118=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 17 10:04:23 2025
    AWUS01 KWNH 171004
    FFGMPD
    CAZ000-171600-

    Mesoscale Precipitation Discussion 1227
    NWS Weather Prediction Center College Park MD
    503 AM EST Mon Nov 17 2025

    Areas affected...portions of northern and central California

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

    Valid 171001Z - 171600Z

    Summary...A stout mid-level wave west of Eureka was prompting
    scattered shower and thunderstorm activity across a broad part of
    northern and central California. These trends will continue for
    the next few hours, and areas of 0.5-0.75 inch/hr rain rates are
    possible. A few instances of flash flooding could occur in
    sensitive areas and near burn scars.

    Discussion...A vigorous mid-level wave was providing ascent for
    several areas of convection 1) just west of Eureka over open
    Pacific waters and 2) along an axis from Redding south-southwest
    to near Monterrey. Over the past hour, more robust convective
    activity (with lightning) developed near/south of San Francisco
    and moved inland. Both of these regimes were responsible for
    areas of 0.5-0.75 inch/hr rain rates. The Redding/Monterrey
    convective band was being forced by a strong front moving
    southeastward across the region. PW values of 1 inch along and
    ahead of the front near the coast was aiding in the heavier rain
    rates.

    Over time, as the aforementioned front shifts southward across the
    state, strong upslope flow will aid in continued moderate to heavy
    rainfall and a few instances of flash flooding especially along
    upwind areas of the Sierra. The front will also aid in occasional
    bursts of heavier rainfall along coastal areas from Monterrey
    southward toward the Transverse Ranges/Santa Barbara County
    through 16Z/8a Pacific time. Sensitive areas/burn scars could
    experience another round of debris flows and excessive runoff.

    Another more conditional risk for heavier rainfall will occur near
    the center of the mid/upper trough near Eureka. Slow-moving
    convection was being supported by ascent from the trough and very
    cold temps aloft (-20 to -24C @ 500 mb). A conditional risk of
    heavier rainfall occurring over land areas between Eureka and
    Santa Rosa exists. Flash flooding is also possible with this
    activity.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!560lrQV056m3xGBG0stbT-bHIATx0Z9HQM1S20SgYEgnUXhKzyUrzp017a7UzT6gmk9-= EVim_853cWsvqz4dxWXL1b0$ for graphic product...

    ATTN...WFO...EKA...HNX...LOX...MFR...MTR...REV...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 41372415 41372308 41312155 40062055 37211977=20
    35161959 34441983 34832081 36762232 38532342=20
    39742426 40652451=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 17 10:14:53 2025
    AWUS01 KWNH 171014
    FFGMPD
    CAZ000-171600-

    Mesoscale Precipitation Discussion 1227
    NWS Weather Prediction Center College Park MD
    514 AM EST Mon Nov 17 2025

    Areas affected...portions of northern and central California

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

    Valid 171001Z - 171600Z

    Summary...A stout mid-level wave west of Eureka was prompting
    scattered shower and thunderstorm activity across a broad part of
    northern and central California. These trends will continue for
    the next few hours, and areas of 0.5-0.75 inch/hr rain rates are
    possible. A few instances of flash flooding could occur in
    sensitive areas and near burn scars.

    Discussion...A vigorous mid-level wave was providing ascent for
    several areas of convection 1) just west of Eureka over open
    Pacific waters and 2) along an axis from Redding south-southwest
    to near Monterrey. Over the past hour, more robust convective
    activity (with lightning) developed near/south of San Francisco
    and moved inland. Both of these regimes were responsible for
    areas of 0.5-0.75 inch/hr rain rates. The Redding/Monterrey
    convective band was being forced by a strong front moving
    southeastward across the region. PW values of 1 inch along and
    ahead of the front near the coast was aiding in the heavier rain
    rates.

    Over time, as the aforementioned front shifts southward across the
    state, strong upslope flow will aid in continued moderate to heavy
    rainfall and a few instances of flash flooding especially along
    upwind areas of the Sierra. The front will also aid in occasional
    bursts of heavier rainfall along coastal areas from Monterrey
    southward toward the Transverse Ranges/Santa Barbara County
    through 16Z/8a Pacific time. Sensitive areas/burn scars could
    experience another round of debris flows and excessive runoff.

    Another more conditional risk for heavier rainfall will occur near
    the center of the mid/upper trough near Eureka. Slow-moving
    convection was being supported by ascent from the trough and very
    cold temps aloft (-20 to -24C @ 500 mb). Heavier rainfall could
    occur between Eureka and Santa Rosa. Flash flooding is also
    possible with this activity.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8rzG_g6Z7dApF0i3lq4u5E6K6tP5BOaGy9fFex9v19JXKqseg8Owh9hveffNBlcDIn_G= wNucsI39g4QZODDfzDz9o8c$ for graphic product...

    ATTN...WFO...EKA...HNX...LOX...MFR...MTR...REV...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 41372415 41372308 41312155 40062055 37211977=20
    35161959 34441983 34832081 36762232 38532342=20
    39742426 40652451=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 17 21:45:46 2025
    AWUS01 KWNH 172145
    FFGMPD
    CAZ000-180345-

    Mesoscale Precipitation Discussion 1229
    NWS Weather Prediction Center College Park MD
    445 PM EST Mon Nov 17 2025

    Areas affected...Southern California...

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

    Valid 172145Z - 180345Z

    SUMMARY...Heavy rainfall conditions improving, but still an
    isolated potential for .5"/hr rates with max totals in the
    Transverse Ranges near 1.5" through evening. Saturated grounds and
    urban locations have possibility for isolated flooding concerns.

    DISCUSSION...GOES-W Visible and Regional RADAR mosaic denotes a
    broader shield of mid-level strato-cu across the western portions
    of the Transverse Ranges across E Santa Barbara county indicative
    of a subtle southwesterly shortwave lifting northeastward through
    in proximity to the cold front. This is in some response to the
    larger scale digging closed low orienting more NW to SE providing
    deeper layer divergence above 500mb and overall DPVA through the
    California Bight into Southern California this afternoon into
    evening. However, the lower level pressure gradient is
    broadening through the Bight and winds have diminished throughout
    the afternoon. Still, 20-25kts of southerly flow coincident with
    the vertically stacked moisture plume still advects .75 to 1"
    total PWats (IVT values of 250-300 kg/m/s) fairly orthogonal to
    the Transverse Ranges of Ventura and Los Angeles counties and will
    spill over to the San Bernardino Ranges through evening.=20
    Localized totals of 1-1.5" are possible in the highest elevations
    but overall rates and ascent will be diminishing with the
    weakening wind field.=20

    Off the terrain, the environmental conditions are very limited
    for flooding, but recent saturated grounds per NASA SPoRT suggest,
    above average run-off could be expected. With that stated, some
    modest surface to boundary layer heating has developed this
    afternoon providing some weak but sufficient instability; MLCAPEs
    of 150-250 J/kg are present and with 10-12 kg/m/s deep layer
    moisture convergence along the front, some vertical development
    and enhanced rainfall rates are possible through the evening
    likely topping out around .5"/hr perhaps inducing some isolated to
    widely scattered incident(s) of urban flooding concerns through
    03z.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9unAJHAWFEgaYz1VRg6fwIkbpTRW82pvEbKw7sViPYiDcu1XKujuA8lj8kRTgFAw-F2X= DADRCR0SzZl4uVJLQ4Km9H4$ for graphic product...

    ATTN...WFO...HNX...LOX...SGX...

    ATTN...RFC...RSA...NWC...

    LAT...LON 35061949 34961850 34191722 32761696 32611733=20
    33011763 33531807 33761859 33831901 34401968=20
    34741979=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Nov 18 03:54:22 2025
    AWUS01 KWNH 180354
    FFGMPD
    CAZ000-180753-

    Mesoscale Precipitation Discussion 1230
    NWS Weather Prediction Center College Park MD
    1053 PM EST Mon Nov 17 2025

    Areas affected...portions of southern California

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

    Valid 180353Z - 180753Z

    Summary...Flash flood potential continues for at least 2-4 more
    hours.

    Discussion...A warm conveyor continues to spread moderate to heavy
    rainfall into portions of southern California near the Los Angeles
    basin and adjacent areas of the Transverse Ranges. Recent
    observations suggest that 0.5 inch/hr rain rates were falling over
    or very near burn scars just north of Los Angeles, suggesting
    continued potential for excessive runoff and debris flows.=20
    Mesoanalyses indicate a continued fetch of southwesterly 850mb
    flow into the region oriented parallel to the coastal ranges,
    supporting continued orographic enhancement of rain rates at
    times. PW values near an inch and weak surface-based instability
    also continue to support the convective nature of the activity and
    locally heavy rain rates.=20

    Models suggest that these rates will continue to impact burn scar
    areas over the next 2-4 hours (through 07Z or so) while
    translating slowly eastward. Flash flooding will remain a
    possibility, though this risk should become more isolated with
    time as rain rates are expected to gradually weaken.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_Lg5brlhc3l8TD-QR5rcay76pvzFWwwYGIJQpPeKzNXG0xFgdiYBDr3pyuoXkzT3fOGP= k9Y_FcFrxoaKrLCXc2oRlZY$ for graphic product...

    ATTN...WFO...HNX...LOX...PSR...SGX...VEF...

    ATTN...RFC...RSA...NWC...

    LAT...LON 34971836 34901737 34381647 33161635 32611652=20
    32711701 33401774 34051865=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Nov 18 12:28:26 2025
    AWUS01 KWNH 181228
    FFGMPD
    AZZ000-CAZ000-181826-

    Mesoscale Precipitation Discussion 1231
    NWS Weather Prediction Center College Park MD
    727 AM EST Tue Nov 18 2025

    Areas affected...portions of western AZ

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

    Valid 181226Z - 181826Z

    Summary...An area of heavy rain with embedded thunderstorms should
    continue across portions of western AZ over the next several
    hours. Hourly rain amounts to 1.5" and local 3" totals are
    possible, which would continue isolated to widely scattered flash
    flood concerns.

    Discussion...An upper level low is sliding southeast down the CA
    coast past Lompoc. It has led to a broad area of divergence aloft
    across the Southwest. Precipitable water values of 1"+ are
    indicated in RAP forecasts, with some GPS values across Las Vegas
    and Phoenix in the 0.8-0.9" range. When combined with 1000-500
    hPa thickness values of 5550 meters, the atmosphere is saturated
    which has led to efficient heavy rainfall across portions of
    southwest AZ this morning, with radar indications of 1"+ in an
    hour at times. MU CAPE of 500-1000 J/kg exists downstream from
    the Gulf of CA northward across southwest AZ. Effective bulk
    shear of 25 kts is helping to organize the convective elements.

    A shortwave noted on water vapor imagery across southern CA could
    cause some backing of the low level flow in the short term,
    potentially shifting the heavy rain area somewhat westward with
    time. RAP guidance fields indicate expansion of the instability
    pool northeast with time, which could lead to some northeast
    shift. When taken together, the heavy rain footprint could
    broaden with time. Hourly rain amounts to 1.5" and local totals
    to 3" are possible where cells backbuild and train. Burn scar
    locations, arroyos/dry washes, box canyons, and urban areas should
    be most sensitive to this rainfall. Isolated to widely scattered
    flash flood concerns should continue into the day today.=20

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7OSVbJv1SfLB2tqivOYQ7yd1rXTyeoYa0kBIta9AhWA5J57n9H8MSQQSYN4wASMHjc2P= 4BFi9vPa5od_YLPyG_1EGIk$ for graphic product...

    ATTN...WFO...FGZ...PSR...VEF...

    ATTN...RFC...STR...NWC...

    LAT...LON 35721347 35591200 34471161 32961249 32731312=20
    32951388 33841422 35121412=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Nov 18 19:04:59 2025
    AWUS01 KWNH 181904
    FFGMPD
    AZZ000-NVZ000-CAZ000-190103-

    Mesoscale Precipitation Discussion 1232
    NWS Weather Prediction Center College Park MD
    203 PM EST Tue Nov 18 2025

    Areas affected...Western Arizona, Southeast California and
    Southern Nevada

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

    Valid 181903Z - 190103Z

    SUMMARY...Flash flood risk increasing this afternoon into the
    evening across the Colorado River basin between southeast
    California, southern Nevada, and western Arizona. Heavy rainfall
    potential existing through sunset leading to potential night time
    flash flooding concerns.

    DISCUSSION...Current radar/IR satellite composite indicates a
    brief lull initiating over portions of southwest AZ and
    southeastern CA. Meanwhile, a steady progression of a stronger
    convective pulse over far northeast Baja will make headway to the
    north as it migrates within the broad deep layer steering flow out
    of the south-southwest. This is due to the proximity of the=20
    persistent ULL presence off the southern CA coast with smaller
    shortwave perturbations emanating around the southern and eastern
    periphery of the upper-level circulation. Hi-res guidance,
    especially the last several HRRR iterations have been manifesting
    this very scenario of a brief lull, followed by the advection of
    the next stronger mid-level perturbation exiting out of Baja and
    shifting north along the adjacent Colorado River basin between
    AZ/CA/NV. This will coincide within a field of relatively buoyant
    air situated within the river basin, arcing back into southern NV
    along the warm/cold conveyor belt transition along the northern
    side of the surface low analyzed over the southern tip of NV.

    SBCAPE between 1000-1500 J/kg is analyzed across much of southwest
    AZ with an extension of 500-1000 J/kg located along the northern
    extent of the Colorado River basin between the three-state
    intersection. This setup is poised to advect further north with a
    greater SBCAPE alignment focused over the southern tip of NV down
    through far-southeast CA and much of western AZ. The combination
    of suitable vorticity advection and modest instability over an
    area of +2 to +3 sigma PWATs will assist in a re-invigoration of
    area convection with cells capable of 0.5-1.25"/hr at peak
    intensity, enough to favor some scattered flash flood prospects
    within the confines of northern Yuma, La Paz, Mojave counties in
    AZ, southern Clark county in NV, and far-eastern San Bernardino
    county in CA. Some training could occur with cells materializing
    on a north-south alignment for areas east of the Colorado River
    given the deep layer flow remaining fairly uni-directional. This
    could exacerbate flash flood concerns locally, leading to the
    threat running closer to the flash flooding likely prospect,
    especially within those western AZ counties.

    Kleebauer

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9qZwoR-eYoOBPiD_vew7g_oNGgxGIH2VQ3sBHQQpMbB4o_gJuygnmXAcdPidULM-OuUA= grZKvmqIF-vCYVPBbaCFAgc$ for graphic product...

    ATTN...WFO...FGZ...PSR...VEF...

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 35831459 35801375 35291312 34391280 33221314=20
    33161409 33711453 34251494 34881526 35531530=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 20 05:42:19 2025
    AWUS01 KWNH 200542
    FFGMPD
    TXZ000-201010-

    Mesoscale Precipitation Discussion 1233
    NWS Weather Prediction Center College Park MD
    1241 AM EST Thu Nov 20 2025

    Areas affected...portions of central TX

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

    Valid 200540Z - 201010Z

    Summary...Isolated to widely scattered instances of flash flooding
    will be possible over portions of central TX including the Hill
    Country through 10Z. Localized totals of 2 to 4+ inches may occur
    over a relatively short period of time.

    Discussion...Regional radar imagery through 0530Z showed widely
    scattered coverage of thunderstorms over central TX with an
    increasingly concerning cluster near/south of JCT with only small
    net-movement over the past hour. The environment over central TX
    contained anomalous precipitable water values of 1.3 to 1.7 inches
    and 500-1500 J/kg MLCAPE (SPC mesoanalysis and area soundings from
    00Z) with moisture contributions from the tropical eastern Pacific
    in the mid/upper levels and Gulf of America in the lower levels.
    0-6 km mean layer winds were a progressive 20-30 kt toward the
    northeast but sufficient speed shear was present for organized
    cells and slower storm motions right of the mean wind.

    While larger scale forcing ahead of a strong mid to upper level
    trough/closed low over the CA/AZ border was still well west of TX,
    the low level response out ahead of this feature was SSE 925-850
    mb winds of 20-30 kt with increasing low level moisture values
    into central TX since Wednesday evening as seen on OSPO LPW
    imagery in the surface-850 mb layer. Transient axes of low level
    convergence and upslope flow into the Edwards Plateau are expected
    to continue to support small clusters of thunderstorms with mean
    movement off toward the northeast. However, there will likely be
    areas of upstream convective redevelopment which will allow for
    training and repeating cells at times. Peak hourly rainfall of 1
    to 2 inches (locally higher) is expected within SW to NE axes of
    training with 3-hr totals of 2-4 inches, although idealized
    training over a particular location has the potential for rainfall
    totals over 4 inches in 3 hours. Current thinking is that the
    coverage of flash flooding through 10Z will remain low enough to
    keep the "flash flooding possible" wording on this message given
    dry antecedent conditions, but concerns for rapid rises of water
    will exist across portions of the sensitive Hill Country despite
    the dry antecedent grounds.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_LYpBNhMlhdGrOmNgOUQY3aTCioz2NPMkd1VVanuIvyaHF12_R4dS_2zri_aZ5-ZJWhe= ULn-yQhCMPB3_j4eFKk9eD4$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32119869 31429791 30329826 29749881 29269946=20
    28930081 29550147 30710103 31759995=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Nov 20 08:02:53 2025
    AWUS01 KWNH 200802
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-OKZ000-201400-

    Mesoscale Precipitation Discussion 1234
    NWS Weather Prediction Center College Park MD
    302 AM EST Thu Nov 20 2025

    Areas affected...northeastern TX, southeastern OK into
    south-central AR

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

    Valid 200800Z - 201400Z

    SUMMARY...Localized flash flooding will be possible across
    portions of northeastern TX, southeastern OK into south-central AR
    through the early morning hours. 2 to 4 inches of rain in 2-3
    hours is expected within idealized training, but the threat is
    expected to primarily exist across urban areas or other locations
    with poor drainage.

    DISCUSSION...Scattered thunderstorms were observed on 0730Z
    radar/infrared satellite imagery over portions of northern TX into
    southern OK. These storms were located beneath broad southwesterly
    flow aloft, with low level warm advection helping aid ascent over
    the region. While forcing for ascent was not strongly defined over
    any particular region of TX/OK/AR, leading to a somewhat
    disorganized pattern on radar imagery, trends have shown an
    increasing coverage in the number of cells over the past few
    hours, with movement off toward the northeast. MLCAPE was between
    500-1500 J/kg with varying degrees of CIN, though many of the
    ongoing cells were likely a bit elevated above the surface.
    Moisture values were anomalously high for mid-November with
    GPS-derived PW values between 1.5 to just over 1.7 inches as of
    06Z in and around the Dallas-Fort Worth region.

    Continued low level warm advection with transient axes of low
    level convergence are likely to maintain scattered thunderstorms
    with areas of short term training capable of producing 1 to 2
    inches of rain in an hour, and 3-hr totals of 2 to 4 inches. Mean
    movement of small thunderstorm clusters should continue off toward
    the northeast but upstream development and training will
    potentially result in flash flooding should these higher rainfall
    totals overlap with an urban or otherwise poorly draining
    location.

    The 06Z and 07Z WoFS seems to have locked onto a signal for higher
    rainfall potential with the 07Z cycle indicating a 40-50 percent
    chance of exceeding 3 inches through the 11-12Z time frame within
    an axis covering northeastern Dallas County into southern Collin
    County. However, given a lack of rainfall over at least the past
    2-3 weeks, flash flood guidance is relatively high which should
    limit the coverage of flash flooding over the next 3-6 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6D9fBgG0juDuoIIa30dzEkqdMbIIT5lBWjkA6bza_T8Tuc7n0CKIf3us7JMPxYLFw189= L9C8giu8UUC8lF9h_ZMtH68$ for graphic product...

    ATTN...WFO...FWD...LZK...MEG...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35659111 34999049 34359073 33769204 32719464=20
    32339727 32669814 33959781 35169407=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Nov 20 10:19:25 2025
    AWUS01 KWNH 201019
    FFGMPD
    TXZ000-201600-

    Mesoscale Precipitation Discussion 1235
    NWS Weather Prediction Center College Park MD
    518 AM EST Thu Nov 20 2025

    Areas affected...portions of central TX

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

    Valid 201015Z - 201600Z

    Summary...Another round of heavy rain with flash flood potential
    appears to be organizing across western portions of the Edwards
    Plateau. Areas of training are likely to produce hourly rainfall
    of 1 to 2 inches and 3-hr totals of 2-4 inches (locally higher)
    across portions of central TX. A few instances of flash flooding
    will be likely through 16Z.

    Discussion...Between 09-10Z, thunderstorm coverage has been
    increasing across western portions of the Edwards Plateau, from
    near SJT, south-southwest toward the Rio Grande. This recent
    increase could be related to increasing ascent ahead of an
    approaching mid-level trough over AZ and northwestern Mexico,
    which was beginning to acquire a negative tilt, but was still
    located a bit west of the region. In addition, 925-850 mb winds
    remained in the 20-30 kt range from the S to SSE, continuing to
    transport anomalous low level moisture northward from the western
    Gulf into central TX where 500-1500 J/kg MLCAPE was estimated by
    the 09Z SPC mesoanalysis page. Orographic lift across the Edwards
    Plateau and a recent increase of low level convergence are also
    contributing factors to the recent expansion of thunderstorms.

    Recent RAP guidance indicates an axis or axes of low level
    convergence aligning from Val Verde County toward the vicinity of
    San Angelo through 16Z, matching the orientation of the mean
    steering flow from the SSW. This signal, when combined with weak
    right-entrance region divergence tied to an upper level jet east
    of the upper level trough, is expected to result in areas of
    training with 1 to 2 inches of rain per hour, and 2 to 4 inches of
    rain in 3 hours or less time (locally higher possible). In
    addition, recent WoFS guidance has been increasing probabilities
    for 2+ inches of rain from near Val Verde County, north to
    northeastward to just southeast of San Angelo over the next few
    hours, with the 09Z cycle displaying a 40-70 percent probability
    of exceeding 2 inches through 15Z across this corridor. The
    anomalously moist environment will support locally high rainfall
    intensities which should overcome dry antecedent conditions,
    supporting at least a localized flash flood concern over the next
    3-6 hours, with locally considerable impacts possible across any urban/impervious surfaces.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8ctK3IvwUmNeuhMpezkSQKaDUREe_ipyjQqaaIn2NaAU7AYk0d1dAsqSQkMepj0XxAgP= CN2QcatTu6iZMWjZ_M4i8LQ$ for graphic product...

    ATTN...WFO...EWX...FWD...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32389946 32119884 31699846 30639852 29619945=20
    28910033 29010170 30760171 32090080=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Nov 20 16:53:30 2025
    AWUS01 KWNH 201653
    FFGMPD
    TXZ000-OKZ000-202230-

    Mesoscale Precipitation Discussion 1236
    NWS Weather Prediction Center College Park MD
    1152 AM EST Thu Nov 20 2025

    Areas affected...North TX into southwest OK

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

    Valid 201650Z - 202230Z

    Summary...Additional rainfall of 1.5-3.0" (and locally higher) is
    likely to result in scattered instances of flash flooding (and may
    be locally significant).

    Discussion...Low-level convergence upstream (southwest) of the DFW
    metro has gradually consolidated a SSE to NNW training segment of
    convection across portions of North TX with hourly totals now
    approaching 2"/hr (per MRMS estimates). This line of showers and
    thunderstorms is occurring along a ThetaE gradient well to the
    east of the primary front (near the Rolling Plains and Cap Rock
    south of the TX Panhandle) with precipitable water values of
    1.5-1.7" (near record values, and well above the FWD 90th
    percentile of ~1.2"), ML CAPE of 500-750 J/kg, and substantial
    deep layer shear of 45-55 kts. As southerly low-level moisture
    transport has recently ramped up, expect a period of several
    several more hours of off and on heavy rainfall (with an even more
    impressive train of showers is ongoing farther southwest over the
    TX Hill Country, likely to move into the region while still
    possibly maintaining 2-3"/hr rainfall rates).

    The bulk of the hi-res guidance suggests an addition 1.5-3.0" of
    rainfall over the next 3-6 hours (per 12z HREF probability matched
    mean QPF) with the potential for localized 3" exceedance (per
    40-km HREF >3" probs of 20-40%). With a narrow swath of 2-4" of
    rainfall already having fallen over the past 6-12 hours (per NSSL
    estimates), Flash Flood Guidance (FFG) are as low as 1.5-2.5" (and
    even lower to the northwest of the metro area where the maximum
    rainfall occured). Given these wet antecedent conditions and the
    potential for additional significant heavy rainfall, scattered
    instances of flash flooding are likely (and may locally be
    significant, particularly across more sensitive urbanized terrain
    and where streamflows are already elevated).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4irV483kYzdvk4QIYc2rRMeSYNgBQuyC8Mbjbl2gVhfVg5U5hcn2wKp_0KEqSN__j6v1= gifA8jUNzsMY1UilaXWyX64$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 34779506 34749469 34609448 34149451 33739464=20
    33489482 33219549 32879604 32429662 32159723=20
    32019790 32539822 32949780 33239739 33529712=20
    33869700 34159660 34509605 34679554=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Nov 20 18:08:02 2025
    AWUS01 KWNH 201807
    FFGMPD
    TXZ000-210000-

    Mesoscale Precipitation Discussion 1237
    NWS Weather Prediction Center College Park MD
    106 PM EST Thu Nov 20 2025

    Areas affected...South-Central TX into the Hill Country

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

    Valid 201800Z - 210000Z

    Summary...Additional rainfall of 1.5-3.0" (and locally higher)
    over portions of already saturated areas is likely to continue
    scattered to numerous instances of flash flooding (with
    expectations for locally significant flash flooding developing).

    Discussion...Sustained training convection has resulted in a
    narrow swath of heavy rainfall (2-5" over the past 3-6 hours, per
    MRMS estimates) through the morning hours. While numerous (but
    very geographically focused) flash floods are ongoing in portions
    of the TX Hill Country, concerns are growing for continued
    worsening of impacts as persistent low-level moisture transport
    and convergence have coincided with destabilization just upstream
    of the hardest hit areas (to the southwest into portions of
    South-Central TX near Del Rio). The mesoscale environment is
    otherwise characterized by precipitable water values of 1.4-1.7"
    (near daily records, as DRT sounding climatology indicates a 90th
    percentile of ~1.2"), most-unstable CAPE of 1000-2500 J/kg, and
    substantial deep layer shear of 55-65 kts. While a dry line is
    slowly approaching the region from the west, this is likely only
    increasing the low-level forcing over the next several hours with
    the expectation that the feature will stall west of Del Rio.

    Going forward, there is strong agreement among the hi-res CAMs for
    an additional 1.5-3.0" of rainfall (with at least one run of the
    HRRR indicating localized totals of up to 5", as well as HREF 3"
    exceedance probabilities of 15-25%). Given the wet antecedent
    conditions (and the already relatively sensitive terrain of
    portions of the Hill Country), continued scattered to numerous
    instances of flash flooding are likely (including some locally
    significant instances of flash flooding, as FFGs of 1.5" are lower
    are indicated across already hard hit areas).

    Churchill

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8gm6zExzPuqInA_FHv9lwYjvY6HraxezaB7ugrj84BH-qx3gctoRT7BOcYLMUDXdCSzx= G3klA6fn0bwz91ueqDS-uDc$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32459847 32329806 31959765 31639764 31299797=20
    30989823 30639859 30139902 29589955 29340009=20
    29340072 29590130 30100103 30600069 31080033=20
    31410010 31899969 32249924 32429888=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Nov 21 06:12:38 2025
    AWUS01 KWNH 210612
    FFGMPD
    CAZ000-211210-

    Mesoscale Precipitation Discussion 1238
    NWS Weather Prediction Center College Park MD
    112 AM EST Fri Nov 21 2025

    Areas affected...coastal southern CA

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

    Valid 210611Z - 211210Z

    Summary...Highly localized flash flooding will be possible from
    slow moving showers/thunderstorms capable of producing hourly
    rainfall up to ~1 inch. This threat will exist along portions of
    southern CA near the coast through at least 12Z.

    Discussion...GOES West water vapor imagery at 06Z showed
    a mid-level closed low centered over the central CA coast, slowly
    moving south. Several smaller scale vorticity maxima were observed
    within the cyclonic flow, with one of interest located over/near
    Santa Cruz Island. Cooling cloud tops were noted east of the
    vorticity center, northwest of a surface low within a mesoscale
    deformation zone. The 1009 mb low was located about 30 miles west
    of Santa Catalina at 06Z with an occluded/cold front extending
    southward. A weak plume of low level moisture transport was
    located ahead of the front, parallel to the southern CA coastline
    where a few showers have recently picked up in intensity with
    localized training along the Orange County coast.

    Weak instability up to a couple hundred J/kg was located along the
    southern CA coast from Santa Barbara to San Diego counties as
    noted in recent ACARS/model soundings. As the mid-level low
    continues to translate down the CA coast, the plume of low level
    moisture ahead of the front will push inland along with the
    initial round of stronger showers. Later in the night, some
    steepening of mid-level lapse rates should increase instability up
    to about 500 J/kg along the immediate coast and closer to 1000
    J/kg offshore. The surface low is forecast to edge closer to the
    Los Angeles/Orange County coasts through 12Z. With this movement,
    another round of slow moving showers and thunderstorms is expected
    to track toward the coast from the offshore waters, with potential
    for highly localized hourly (or sub-hourly) rainfall between 0.5
    and about 1 inch, due to slow movement.

    These spotty higher rainfall rates could result in flash flooding
    of urban areas or other sensitive terrain.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5hy1OjoPIczj9JA_LYobi4X_8NO48jWfR8lBVWDPe-RK1XsCwgWROEbmiMan9UUefKhF= UopZquPsB1jFEV3OzPJESk4$ for graphic product...

    ATTN...WFO...LOX...SGX...

    ATTN...RFC...RSA...NWC...

    LAT...LON 34581936 34531776 33821649 32841623 32541631=20
    32531634 32251753 32241756 32731790 33131881=20
    33501962 34001978=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Nov 21 12:45:47 2025
    AWUS01 KWNH 211245
    FFGMPD
    CAZ000-211830-

    Mesoscale Precipitation Discussion 1239
    NWS Weather Prediction Center College Park MD
    744 AM EST Fri Nov 21 2025

    Areas affected...Southern California

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

    Valid 211245Z - 211830Z

    SUMMARY...Risk of slow moving, narrow updrafts capable of
    .75"-1"/hr rates likely to continue to a few more hours. Isolated
    1-2" totals in/near urban locations in SoCal suggest localized
    flash flooding remains possible.

    DISCUSSION...A well-defined closed low is parked directly over
    southern California with an upstream highly anomalous
    shortwave/vorticity center descending southward along the western
    periphery of the low. This and favorable cyclonically curved
    geography of the coast and mountain ranges will help to keep
    surface to boundary layer cyclone relatively stationary for the
    next few hours just along/south of Long Beach, CA. The cold front
    and associated warm conveyor have pressed eastward into far NW
    Baja California (state) of Mexico before angling through Imperial
    Valley and lower Colorado River Valley. However, the western
    branch of the TROWAL and occluded front remain banked up against
    the Orange county and San Diego county beaches.=20

    GOES-W WV suite shows the core of the upper-level jet remains
    south near the San Diego country border with Mexico, allowing for
    solid cyclonically curved left exit ascent across much of SoCal
    providing solid ascent for updrafts that do develop with the solid
    surface/low level moisture convergence. The limiting factor will
    likely be unstable air/vertical ascent through convective
    processes. MUCAPEs have dropped to around 500 J/kg but are now
    mostly driven through cold advection aloft. The upstream
    shortwave will dull this advection for a few hours but may allow
    the lapse rates to maintain this weak 250-500 J/kg instability.=20=20
    As such, updrafts are likely to remain isolated and generally
    narrow, though with isallobaric response to the updraft, moisture
    convergence should allow for the .75-.9" total PWats (loaded
    mainly below 700mb) to support rates of .75-1"/hr.=20

    As such, a localized 1-2" total still remains possible for the
    next few hours. Naturally low FFG and/or urban hydrophobic
    conditions will result in solid run-off and maintain a risk of
    widely scattered incident or two of possible flash flooding
    through the morning.=20=20

    It is also possible (more likely toward 16-18z) that a few
    showers/cells may try to develop with some weak clearing through
    the Imperial Valley along the western branch of the TROWAL. These
    cells would be also similarly slow moving but likely translating
    NW rather than NE as with the coastal cells; but there is less
    certainty with that evolution and a secondary MPD may be required
    if trends continue to improve.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6defLsDhQO-ON-LqODLd4v4g66xlCixSbO2_VOxQBeCuFq2HkSlxnEp1Y3e9UPBfwxAh= InmHHKSqNelNU_uwQNCMueQ$ for graphic product...

    ATTN...WFO...LOX...SGX...

    ATTN...RFC...RSA...NWC...

    LAT...LON 34551850 34481788 34071704 33471650 32801624=20
    32581627 32531672 32561724 32981753 33301781=20
    33581827 33971908 34331893=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Nov 21 13:31:47 2025
    AWUS01 KWNH 211331
    FFGMPD
    AZZ000-NVZ000-CAZ000-211930-

    Mesoscale Precipitation Discussion 1240
    NWS Weather Prediction Center College Park MD
    831 AM EST Fri Nov 21 2025

    Areas affected...Inland Deserts of Southern California and Lower
    Colorado River Valley...

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

    Valid 211330Z - 211930Z

    SUMMARY...Prolonged moderate rain with embedded very weak showers
    capable of .3-.5"/hr rates. Scattered 1-1.5" totals pose longer
    duration flash flooding concerns (3-6hr exceedance).

    DISCUSSION...GOES-W WV suite shows core of deep upper-low has
    wobbled over the LA Basin, but a strong upstream shortwave along
    the western periphery of the upper-level closed low is digging
    sharply resulting an combined effect of tightening the overall
    flow across the deep cyclone while keeping the downstream older
    center stationary over the next 6-12hr. As a result, the core of
    the Atmospheric River will remain focused on NW Baja California
    before cyclonically turning (fairly sharply) through the Imperial
    Valley into the Mojave Deserts back toward the Tehachapi Range and
    southern San Joaquin Valley.=20

    CIRA LPW prior to the local outage showed a fairly strong sfc to
    850 and 850-700mb signal with 95th-99th percentile signals in each
    layer, combine that with some increase in the surface to 850mb
    layer from favorable southerly flow off the warm Sea of Cortez and
    total PWats remain at or slightly above 1" into the Imperial
    Valley and as high as .75" into the San Joaquin Valley. VWP and
    RAP analysis suggest strong cyclonic curvature but also 20-30kts
    of flux. So while there is sub-100 J/kg of instability, the
    vertical ascent through the strengthening western branch of the
    TROWAL suggests highly anomalous flux to maintain moderate showery
    activity through the deserts. Rates of .33"/hr are more probable,
    but an isolated rate of .5" is not impossible. Still, persistent
    weakly banded features will result in tracks of 1-1.5" totals in a
    3-6hr time period, so any isolated, enhanced vertical cell within
    the core may result in quicker stream/arroyo rises. FFG values
    being only .5"/hr and less than 1"/3hr and less than 1.5-2"/6hrs)
    suggest a few scattered incidents of 'flash' flooding are
    considered possible through early afternoon.

    While less certainty, there are CAMs suggesting some filtered
    insolation may be possible in the morning. Near zero inhibition
    through the profiles, suggest embedded widely scattered convective
    elements may evolve in the 16-19z time period, particularly closer
    to the warmer heat source of the Sea of Cortez across the Lower
    Colorado and southern Imperial Valley. Given the digging wave
    upstream off the SW CA coast, upstream winds may be favorable for
    some potential upstream redevelopment/back-building environment.=20
    Will continue to monitor those trends for any additional MPD later
    toward the afternoon.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_-WjtQ6vmZP70V-mcQSPBPEHSb5UPtn6MaaXF4h2x6fY00XJ7ZrT2AvFASaI-gjDsv3r= 8Ao-f3IcG6w7HoujVkdzYxE$ for graphic product...

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

    ATTN...RFC...RSA...STR...NWC...

    LAT...LON 36451689 36001550 35231468 34241409 33061394=20
    32331426 32491497 32691600 34241623 34841705=20
    34971779 35591825 36151792=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 22 23:00:08 2025
    AWUS01 KWNH 222300
    FFGMPD
    AZZ000-230458-

    Mesoscale Precipitation Discussion 1241
    NWS Weather Prediction Center College Park MD
    559 PM EST Sat Nov 22 2025

    Areas affected...portions of central and southeast AZ

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

    Valid 222258Z - 230458Z

    Summary...Convection continues to grow in coverage across portions
    of central and southeast AZ. Hourly rain amounts up to 1" with
    local amounts to 2" could lead to isolated to widely scattered
    issues in arroyos/dry washes, burn scars, and box canyons.

    Discussion...Infrared satellite imagery shows cooling cloud tops
    in association with showers and thunderstorms across central and
    southeast AZ within a region of 700 hPa confluence ahead of a
    progressive deep layer low, with some recent uptick in coverage.=20
    A first pixels of 0.5" an hour amounts were indicated recently
    from the Phoenix and Tucson AZ radars in association with their
    rainfall. Pockets of 500+ J/kg of MU CAPE exist across
    west-central and southeast AZ per SPC mesoanalyses, with
    instability increasing due to cooling aloft and some degree of
    daytime heating/sunshine, particularly across southeast AZ.=20
    Effective bulk shear of 30-50 kts exists here, which is leading to
    an environment with both organized and ordinary convective cells,
    with the organized activity edging east of due north while the
    less organized storms move just west of due north. Precipitable
    water values of 0.5-1" lie here. The atmosphere is cool, with
    1000-500 hPa thickness values of 5550-5600 meters. When combined
    with the available moisture, the column is approaching saturation.

    The mesoscale guidance implies increasing convective coverage and
    an increasing incidence of 0.5"+ an hour amounts over the next
    several hours, with the 12z REFS and 18z HREF guidance suggesting
    the heaviest rainfall in the 01-05z time frame. This could be due
    to cell training, occasional mesocyclone formation, or cell
    mergers between more and less organized convective activity. As
    the upper level system continues marching northeast, winds should
    veer somewhat which should allow convection to shift somewhat to
    the east with time, with activity shifting increasingly into
    mountainous areas. With hourly amounts to 1" and local totals to
    2" possible, the incidence of impactful heavy rain is expected to
    be isolated to widely scattered, mainly within arroyos/dry washes,
    box canyons, and any area burn scars.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_11Dt4vgOR_QWohFX9tvKqdE6LGVpOCutmRvWnF-mQw0JNZV4L9ax5MtPUIq6Oi9tax_= f7aVUm8MLuTaLbjJuyltsFM$ for graphic product...

    ATTN...WFO...FGZ...PSR...TWC...

    ATTN...RFC...STR...NWC...

    LAT...LON 34911210 34811085 33170939 31640956 31201086=20
    32061186 34001212=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 22 23:07:38 2025
    AWUS01 KWNH 222307
    FFGMPD
    AZZ000-230459-

    Mesoscale Precipitation Discussion 1241
    NWS Weather Prediction Center College Park MD
    607 PM EST Sat Nov 22 2025

    Areas affected...portions of central and southeast AZ

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

    Valid 222259Z - 230459Z

    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!7t0SwD1cDQnVIZMQFVCK0VNmTmtrm9FjFvl4QTMcv2akeLdM5pIq9MnzgXiYy9DDoUdR= 8TJcSa0aciWXjO4Mxbq4g9k$ for graphic product...

    ATTN...WFO...FGZ...PSR...TWC...

    ATTN...RFC...STR...NWC...

    LAT...LON 34911210 34811085 33170939 31640956 31201086=20
    32061186 34001212=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 22 23:10:09 2025
    AWUS01 KWNH 222310
    FFGMPD
    AZZ000-230458-

    Mesoscale Precipitation Discussion 1241
    NWS Weather Prediction Center College Park MD
    609 PM EST Sat Nov 22 2025

    Areas affected...portions of central and southeast AZ

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

    Valid 222258Z - 230458Z

    Summary...Convection continues to grow in coverage across portions
    of central and southeast AZ. Hourly rain amounts up to 1" with
    local amounts to 2" could lead to isolated to widely scattered
    issues in arroyos/dry washes, burn scars, and box canyons.

    Discussion...Infrared satellite imagery shows cooling cloud tops
    in association with showers and thunderstorms across central and
    southeast AZ within a region of 700 hPa confluence ahead of a
    progressive deep layer low, with some recent uptick in coverage.=20
    A first pixels of 0.5" an hour amounts were indicated recently
    from the Phoenix and Tucson AZ radars in association with their
    rainfall. Pockets of 500+ J/kg of MU CAPE exist across
    west-central and southeast AZ per SPC mesoanalyses, with
    instability increasing due to cooling aloft and some degree of
    daytime heating/sunshine, particularly across southeast AZ.=20
    Effective bulk shear of 30-50 kts exists here, which is leading to
    an environment with both organized and ordinary convective cells,
    with the organized activity edging east of due north while the
    less organized storms move just west of due north. Precipitable
    water values of 0.5-1" lie here. The atmosphere is cool, with
    1000-500 hPa thickness values of 5550-5600 meters. When combined
    with the available moisture, the column is approaching saturation.

    The mesoscale guidance implies increasing convective coverage and
    an increasing incidence of 0.5"+ an hour amounts over the next
    several hours, with the 12z REFS and 18z HREF guidance suggesting
    the heaviest rainfall in the 01-05z time frame. This could be due
    to cell training, occasional mesocyclone formation, or cell
    mergers between more and less organized convective activity. As
    the upper level system continues marching northeast, winds should
    veer somewhat which should allow convection to shift somewhat to
    the east with time, with activity shifting increasingly into
    mountainous areas. With hourly amounts to 1" and local totals to
    2" possible, the incidence of impactful heavy rain is expected to
    be isolated to widely scattered, mainly within arroyos/dry washes,
    box canyons, and any area burn scars.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-poSCiJYQEyoV4jMimyWuK08ybzHQY_GIPWcJWA0X1V9T6lRFwK8MhpkVkd7jpd8AvnV= Ow4HdefNJCTkabCRLzKUVSY$ for graphic product...

    ATTN...WFO...FGZ...PSR...TWC...

    ATTN...RFC...STR...NWC...

    LAT...LON 34911210 34811085 33170939 31640956 31201086=20
    32061186 34001212=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Nov 23 23:55:23 2025
    AWUS01 KWNH 232355
    FFGMPD
    TXZ000-240552-

    Mesoscale Precipitation Discussion 1242
    NWS Weather Prediction Center College Park MD
    653 PM EST Sun Nov 23 2025

    Areas affected...Edwards Plateau/Concho Valley in TX

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

    Valid 232352Z - 240552Z

    Summary...A band of thunderstorms is trying to consolidate and is
    expected to continue to slowly lengthen with time. Hourly rain
    amounts to 2" with local totals to 4" are possible through 06z.

    Discussion...A broken band of thunderstorms stretches from near
    Fort Stockton northeast towards Big Spring TX within the tail end
    of the warm conveyor belt of a deep layer low centered in the
    vicinity of southeast CO. Precipitable water values are up to
    0.9-1.2" per recent GPS data. MU/ML CAPE of 1500-2000 J/kg exists
    in the vicinity of the band's tail, with the 6C 700 hPa isotherm
    appearing to act as its southern limit. Effective bulk shear is
    significant, 50-70 kts, which has led to mesocyclone formation.=20
    Right-moving cells appear to be causing some eastward shift with
    time. Occasional backbuilding to near/slightly south of I-10 has
    been noted at times.

    RAP guidance shows an uptick in moisture and low-level inflow from
    the Gulf and existing convection over the next several hours,
    which should act to solidify and lengthen the band somewhat, aid
    precipitation efficiency, and causing the polar warm front to slow
    its northeast advance from the Pecos River valley. Mesocyclones
    along the existing, solidifying band are expected to cause cell
    training as they hold up portions of the convective band to the
    east-northeast, which could lead to hourly amounts to 2" and local
    totals to 4" as cells move just right of the mean 850-400 hPa flow
    in a general east-northeast direction. The combination of a
    broadening cold pool and slowly veering 850 hPa flow associated
    with an impinging front/pseudo dryline leads to increased forward
    progression of the band to the east to east-southeast. Portions
    of this region saw heavy rainfall Wednesday and Thursday, which
    has lowered 3 hourly flash flood guidance values to 2-3", which
    should be achievable in isolated to widely scattered spots. The
    12z REFS and 18z HREF were advised for the area outlined. Flash
    flooding is considered possible through 06z/midnight CST.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_zyP1sIM09MCIGlmT6X-1_ya4hUXy4M0OqKMFtaUfk4iqjVZGnYfxlcUIV9mjo_rBgr8= 7uVzWLSO13ttNTijlx2EvK4$ for graphic product...

    ATTN...WFO...EWX...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32390111 32270029 31450004 30250073 30050201=20
    30210274 30770303 31560210=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 24 05:52:55 2025
    AWUS01 KWNH 240552
    FFGMPD
    TXZ000-241015-

    Mesoscale Precipitation Discussion 1243
    NWS Weather Prediction Center College Park MD
    1251 AM EST Mon Nov 24 2025

    Areas affected...lower Pecos Valley into north-central TX

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

    Valid 240550Z - 241015Z

    Summary...An axis of SW to NE thunderstorms is expected to train,
    likely resulting in areas of flash flooding from the lower Pecos
    Valley into portions of north-central TX through 10Z. Hourly
    rainfall of 1-2 inches should be common, but isolated hourly
    totals in excess of 2 inches cannot be ruled out.

    Discussion...Regional radar imagery at 0530Z across TX showed the
    recent development of thunderstorms across the lower Pecos River
    Valley from SW to NE, crossing I-10 a couple of miles west of
    where US-190 meets I-10. Additional thunderstorms extended
    northeastward across I-20 between Abilene and Ranger. MLCAPE was
    500 to 1500+ J/kg via 05Z SPC mesoanalysis data though most of the
    region was capped. The eastward motion of a mid to upper level
    closed low/trough to the west has allowed sufficient lift to
    overcome a capping inversion noted on the 00Z DRT sounding,
    although the capping inversion is likely weaker to the north of
    DRT. The storms were located out ahead of a weak Pacific cold
    front analyzed over western TX at 05Z, along an axis of
    convergence represented the leading edge of low level moisture
    transport marked by 30-40 kt of flow per area VAD wind data in the
    925-850 mb layer. Some right-entrance region ascent is also likely
    present south of a 100 kt jet max located on the eastern side of
    the closed low/trough.

    Lift ahead of the eastward moving closed low/trough will continue
    to support the expansion of numerous thunderstorms over portions
    of west-central to north-central TX through 09Z. Thunderstorm
    alignment is expected from SW to NE, along the similarly oriented
    low level convergence axis, with mean steering flow paralleling
    the axis of convergence, supportive of training. Slow overall
    movement is especially likely where the leading edge of low level
    transport meets the approaching zone of lift from the west, closer
    to the Rio Grande, where eastward movement of the axis of forcing
    is expected to be slowest. However, coverage of thunderstorms with
    southward extent is a bit uncertain. The environment supports
    hourly rainfall of 1-2 inches but isolated hourly totals over 2
    inches should be attainable where thunderstorm axes are slower to
    translate east. Areas of flash flooding are likely to result,
    although coverage may be somewhat limited across the MPD threat
    area through 10Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!--J0Cgwx68s_3fUkCaer5oFLIJNr1rjgaRVVx80_87jephrSQ-YTTO7MFCqPzFly5cC0= qx9_h9ZLW7rl1Rkm4ORZB5U$ for graphic product...

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

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 33599849 33179739 32419736 31389870 30340081=20
    30000244 30570297 31730151=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 24 10:14:31 2025
    AWUS01 KWNH 241014
    FFGMPD
    ARZ000-TXZ000-OKZ000-241515-

    Mesoscale Precipitation Discussion 1244
    NWS Weather Prediction Center College Park MD
    513 AM EST Mon Nov 24 2025

    Areas affected...central TX into southeastern OK/southwestern AR

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

    Valid 241012Z - 241515Z

    Summary...Flash flooding is likely to continue for portions of
    central TX into southeastern OK/southwestern AR, at least on a
    localized basis, through the morning commute (through 15Z/9 AM
    CST). Hourly rainfall of 1 to 2+ inches will remain likely within
    areas of training and at least isolated/urban flash flooding will
    be likely in a couple of areas.

    Discussion...Radar imagery from 10Z showed a SW to NE axis of
    heavy rain that extended from near San Angelo to Graham,
    containing MRMS-derived hourly rainfall of 1 to 2 inches and has
    had a history of observed 15 minute rates between 0.5 and 1.0
    inches. The axis of thunderstorms was located along the leading
    edge of 30-40 kt of southerly 925-850 mb winds, which veered and
    weakened to the west, forming a SW to NE axis of convergence that
    has largely coincided with the line of thunderstorms over central
    to northern TX since 06Z. With the exception of the far southern
    edge of the line, the thunderstorms were mostly elevated above a
    stable layer north of a warm front that draped NW to SE across
    central TX to the Upper TX Coast. The environment contained ML/MU
    CAPE values of 500-1500 J/kg and precipitable water values of 1.3
    to 1.5 inches per 09Z SPC mesoanalysis data and these values are
    expected to continue to be in place as the system translates east
    to northeast.

    Short term forecasts from the RAP show the low level convergence
    axis translating eastward through 15Z, oriented parallel to
    southwesterly mean steering flow, which will continue to support
    areas of training over the next 3-5 hours. North of the Red River,
    instability is expected to be weaker (<1000 J/kg) which may limit
    rainfall intensities, but lift will be augmented by the
    right-entrance region of a 90-110 kt upper level jet max located
    on the eastern side of a upper level closed low/trough to the
    west.

    Therefore, while not everyone will see 1 to 2 inches of rain in an
    hour, SW to NE axes of heavy rain will continue to impact portions
    of central TX into southeastern OK/southwestern AR through 9 A.M.
    local time, which will could impact the morning rush, especially
    if overlap of high rain rates occurs with urban locations, such as
    the Dallas/Fort Worth Metroplex within the next 1 to 3 hours.
    Additional rainfall for many should be 1 to 2 inches but peak
    values through 15Z of 2 to 3 inches will likely occur.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4ZFTNzgVNwIfsPso7FHQYtRooV-OEmC5q63V7fbKprZpyFzny24Osy-GunOLEUcodKte= o_H4CPuu11FoxTF_I1Qa12E$ for graphic product...

    ATTN...WFO...EWX...FWD...LZK...OUN...SHV...SJT...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35019440 34799388 34309345 33309398 32169588=20
    31299741 30899864 30829950 31350015 32169926=20
    33519754 34869529=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 24 16:10:33 2025
    AWUS01 KWNH 241610
    FFGMPD
    LAZ000-ARZ000-TXZ000-242208-

    Mesoscale Precipitation Discussion 1245
    NWS Weather Prediction Center College Park MD
    1109 AM EST Mon Nov 24 2025

    Areas affected...portions of northeast Texas, northwestern
    Louisiana

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

    Valid 241608Z - 242208Z

    Summary...Areas of training/repeating thunderstorms should result
    in local 2-4 inch rainfall totals through 22Z/4p Central. Flash
    flooding is possible - especially where these heavy rainfall
    totals can occur in sensitive and/or urban areas.

    Discussion...A complex convective scenario is ongoing across
    portions of Texas and Louisiana this morning. A mature linear
    segment (extending from near Hot Springs, AR south-southwestward
    to near Longview, TX) was forward propagating eastward while
    producing areas of 0.5-1.0 inch/hr rain rates. An outflow
    boundary from this activity extends westward from Longview to near
    Waco, where another well-organized linear complex was moving
    eastward and also producing 0.5-1.5 inch/hr rain rates.

    Flash flood potential will reside between these two linear
    complexes over the next 4-6 hours. The east-west oriented outflow
    will interact favorably with enhanced low-level flow (30+ kt at
    850 oriented perpendicular to the boundary), resulting in
    repeating rounds of rainfall. Furthermore, heating along and
    south of a synoptic warm front across east Texas (from near Waco
    to near Lake Charles) will also aid in destabilizing to support
    strengthening convection throughout the discussion area. The
    overall scenario supports areas of 2-4 inch rainfall totals.

    Fortunately, hourly FFG thresholds across most of the discussion
    area are in the 3+ inch range where the heaviest rainfall is
    expected. These thresholds may not be exceeded on a widespread
    basis - although this depends somewhat on specific convective
    evolution also. Isolated to scattered instances of flash flooding
    are expected - particularly where the greatest rainfall can occur
    over low-lying and/or urban areas.=20=20

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9fUSUFL2ROiQxVrsYtVsEBgqdyxDf-bIOIvk-ma4iocAmW5lq1cRQobaTs_JYoM_o2p3= fcRDhqLMp_0tY5wFKqjPZb4$ for graphic product...

    ATTN...WFO...FWD...HGX...LCH...LZK...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 33439408 33429237 32409221 31929238 31359297=20
    31079432 30539631 30799728 31949726 32589596=20
    32979514=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 24 16:50:02 2025
    AWUS01 KWNH 241649
    FFGMPD
    TXZ000-242048-

    Mesoscale Precipitation Discussion 1246
    NWS Weather Prediction Center College Park MD
    1149 AM EST Mon Nov 24 2025

    Areas affected...portions of southeastern Texas, including Houston
    Metropolitan

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

    Valid 241648Z - 242048Z

    Summary...A cluster of thunderstorms has developed just west of
    Houston Metropolitan. Areas of 1 inch/hr rates have been
    estimated. These rates should spread/develop east-northeastward
    over the next 2-4 hours, possibly prompting excessive runoff
    especially in urban areas.

    Discussion...Scattered thunderstorms have developed along a
    pre-frontal confluence axis located west of Houston Metro over the
    past 1-2 hours. These cells are exhibiting rapid intensification
    as evidenced by robust lightning concentrations and cooling cloud
    tops via satellite. The storms are in an environment
    characterized by 3500 J/kg SBCAPE and 1.6 inch PW values, both
    supporting locally heavy rain. Furthermore, the cells are in a
    very weakly capped environment with subtle ascent aloft passing
    over the area from weak mid-level waves ahead of a larger-scale
    mid/upper trough over the Texas Panhandle. Each of these features
    along with strong vertical wind shear are supportive of convective
    longevity and modest increases in convective coverage over the
    next 2-4 hours.

    Rain rates of 1-1.5 inch/hr were estimated in a couple spots
    beneath the convection recently. Additional convective
    development and training should result in more areas of 1.5
    inch/hr rain rates over time, with some of this activity reaching
    perhaps northern sides of Houston Metro. Additionally, the
    presence of a warm front over the area may encourage instances of
    right-moving cells -and- mergers, further enhancing local flash
    flood potential. Direct impacts to Houston Metro are still in
    question currently, but cannot be ruled out as storms continue to
    mature. At least isolated instances of flash flooding are
    possible in this regime.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5x69WgDP4V7GXF8YIMVSa-qvfy3sErd_9r8Jumve8fsd8Pa8UfZ2q8vJhSAFDJ5I4IVu= rmSVFnLOGYYCFaicFHyltqc$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...LCH...SHV...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31379478 31199388 30469384 29729427 29079610=20
    28759708 30029731 30839687 31179619=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Nov 24 22:00:10 2025
    AWUS01 KWNH 242200
    FFGMPD
    LAZ000-ARZ000-TXZ000-250358-

    Mesoscale Precipitation Discussion 1247
    NWS Weather Prediction Center College Park MD
    459 PM EST Mon Nov 24 2025

    Areas affected...east-central/northeast Texas, western Louisiana,
    and southern Arkansas

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

    Valid 242158Z - 250358Z

    Summary...Areas of training thunderstorm continue to support 1-2.5
    inch/hr rainfall rates at times. These rain rates should support
    at least isolated instances of flash flooding through the evening.

    Discussion...Flash flood potential continues across the discussion
    area. This afternoon, several areas of scattered thunderstorms
    (organized into clusters and small linear segments) have migrated
    west to east across the discussion area. Over the past hour, and
    uptick in convective intensity has been noted across central Texas
    along and east of the I-45 corridor. An impressive 2.53 inch/hr
    rain rates was measured at Athens, TX during that time. Cells are
    being influenced by 1) a stout mid-level shortwave trough via
    water vapor that was advancing toward the region from west-central
    Texas and 2) confluent low-level flow, which was maintaining 1.7
    inch PW and 1000+ J/kg MUCAPE across the discussion area. THe
    storms were not congealed into a forward-propagating linear
    segment, with localized axes of training continuing to support
    heavier rainfall. FFG thresholds continue to range in the 2-3.5
    inch/hr range, suggesting that the bulk of the flash flood threat
    will likely remain tied to urban and/or sensitive areas in the
    short term.

    Over time, ongoing convective activity will shift eastward through
    the TX/LA border region (including Shreveport Metro), with spots
    of 1-3 inch/hr rain rates continuing. A cold front was making
    slow progress to the east across central Texas, reducing stability
    and ending the convective/flash flood threat from the west. This
    front will translate eastward, reaching the TX/LA border area near
    Shreveport in the 04-05Z timeframe. Flash flooding will be a
    distinct possibility through at least that timeframe.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6A_9Czlk4N8uJvMpEAy71KjENzSoGcbjTJuBlDeDK8nVn3CE6d2LzSn7W1JziWcAQYhd= dXd7ZpUi4kcGG5M4tApX0Mc$ for graphic product...

    ATTN...WFO...FWD...HGX...JAN...LCH...LZK...SHV...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 33739364 33529223 32669183 31189212 30469375=20
    30079619 30789702 32479634 33559493=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Nov 25 03:59:43 2025
    AWUS01 KWNH 250359
    FFGMPD
    TNZ000-ALZ000-MSZ000-LAZ000-ARZ000-TXZ000-250810-

    Mesoscale Precipitation Discussion 1248
    NWS Weather Prediction Center College Park MD
    1058 PM EST Mon Nov 24 2025

    Areas affected...northern LA into southeastern AR and
    central/northern MS

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

    Valid 250356Z - 250810Z

    Summary...Areas of flash flooding will remain possible from
    northern LA into southeastern AR and central/northern MS over the
    next few hours. Peak hourly rainfall values of 1 to 3 inches are
    expected within axes of training.

    Discussion...A broken squall line was observed through radar
    imagery at 0330Z from southeastern AR into northern/western LA and
    far eastern TX. This feature was located out ahead of an
    approaching shortwave and embedded vorticity max which extended
    from northeastern TX into southeastern OK, moving toward the ENE.
    Low level convergence, ahead of the associated surface cold front
    and along/north of the system's warm front, was helping to focus
    the SW to NE oriented axis of thunderstorms which has had a
    history of training and 1 to 3 inches of rain per hour since at
    least 01Z. The lower MS Valley also resided beneath the diffluent
    right entrance region of a 100 to 120+ kt jet max centered over
    the central MO/IL border which was aiding lift within the moist
    (1.5-1.7 inch PWs) and unstable (500-1500 J/kg MUCAPE) environment.

    As the shortwave and embedded vorticity max continue to advance
    downstream toward the ENE, The axis of thunderstorms will follow
    suit, with areas of embedded training within the SW to NE oriented
    mean steering flow. The environment will continue to support peak
    hourly rainfall of 1 to 3 inches at times, which is below FFG
    values for southern portions of this MPD, but at or above it for
    AR into northern MS. Therefore, the flash flood threat is
    considered possible and should be mainly confined to urban or
    otherwise sensitive locations where 2 to 4 inches of rain could
    fall in 3 hours or less time.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4a9nv8X4pl-iuXsYRf0vA3pX-uVyblhhJWRgGkOtkPsGQx8P7kA7L5qxKGPRBbJpJ4V2= q0MyJho1Nw54PYvtCxe_CGI$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LCH...LZK...MEG...OHX...SHV...

    ATTN...RFC...ALR...FWR...ORN...NWC...

    LAT...LON 35088927 35088829 34968780 34368761 33768814=20
    33018901 32329007 31849104 31289216 30859377=20
    31139431 31709418 32009364 32549301 33409201=20
    34709039=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Nov 25 08:25:16 2025
    AWUS01 KWNH 250825
    FFGMPD
    GAZ000-ALZ000-MSZ000-LAZ000-251400-

    Mesoscale Precipitation Discussion 1249
    NWS Weather Prediction Center College Park MD
    324 AM EST Tue Nov 25 2025

    Areas affected...northern LA/MS border into central MS/northern AL

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

    Valid 250823Z - 251400Z

    Summary...While the overall flash flood coverage looks to decrease
    later this morning across MS and AL, concerns remain for localized
    2 to 3+ inch totals from hourly rainfall of 1 to 2+ inches. A
    threat of flash flooding will linger through 14Z.

    Discussion...08Z radar imagery showed an axis of strong
    thunderstorms extending from western LA near DRI, northeastward
    into central/northern MS. The most powerful section of this axis
    was in western MS, between TVR and JAN, where some of the
    strongest low level winds were observed with near 50 kt at 850 mb
    from the south. A low level confluence axis from western LA into
    northern MS remained a focus for thunderstorms, out ahead of a
    potent vorticity max located over AR and within the
    diffluent/divergent right-entrance region of an associated upper
    level jet max which extended across the MS Valley into the Midwest.

    Cloud tops on infrared satellite imagery have shown trends toward
    warming overall over the past 2-3 hours, but bursts of colder
    cloud tops remained, such as what was occurring over western MS at
    08Z. A reservoir of 500-1500 J/kg MLCAPE remained from central MS
    into central/southern LA with up to ~1000 J/kg MUCAPE northward
    into western TN. Short term forecasts from the RAP show that as
    the vorticity max over AR continues to translate toward the ENE,
    925-850 mb winds will veer over southern MS/AL which will have the
    effect of weakening the existing axis of confluence across the
    region through 12Z. However, remnant low level
    convergence/confluence coincident with strong upper level ascent
    will continue a threat for heavy rain and periods of training. The
    environment will still be capable of localized rainfall rates over
    2 in/hr but 1 to 2 inches in an hour will be more common.
    Therefore, through 14Z, a localized flash flood threat will remain
    from the LA/MS border into central MS and central to northern AL
    where 2 to 3+ inches of rain could fall in a 2 to 3 hour window,
    with the greatest concern for flash flooding across urban or
    otherwise sensitive/low-lying areas.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-jACpZSiCr5zOCEqvi3Hw1pmfCDcwp6u1VTDCrhLJLJpXYVKShjKP0joJgzuyv8YHhtI= qpK0qVxJeQoKvKualHte1yI$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...JAN...LCH...LIX...MEG...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34998668 34728550 33428524 32468689 31268959=20
    30999128 31309200 31769195 32099144 32569074=20
    33528925 34128831=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Nov 25 15:10:48 2025
    AWUS01 KWNH 251510
    FFGMPD
    ALZ000-MSZ000-251909-

    Mesoscale Precipitation Discussion 1250
    NWS Weather Prediction Center College Park MD
    1010 AM EST Tue Nov 25 2025

    Areas affected...west-central into central Alabama

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

    Valid 251509Z - 251909Z

    Summary: The best chance of isolated flash flood potential exists
    across west-central into central Alabama over the next couple
    hours.

    Discussion...A complicated surface/low-level pattern exists across
    the discussion area currently. A remnant outflow boundary from
    earlier convection now over Georgia resides along an axis from
    just south of Tuscaloosa eastward to the AL/GA border just north
    of Auburn. This boundary was oriented perpendicular to strong
    southerly 850mb flow (around 40-45 knots), providing ascent for
    sustained, deep convective updrafts. Subtle mid-level waves
    across Louisiana/Mississippi were also providing ascent for
    updrafts. Convection has tended to focus along and just north of
    the aforementioned outflow, and with 1.4 inch PW values, moderate
    surface-based buoyancy south of the outflow, and deep layer flow
    generally parallel to the initiating outflow boundary, some
    opportunity exists for training of cells this morning from near
    Tuscaloosa into the southern sections of Birmingham Metro this
    morning. Some of this rainfall was occurring in areas that have
    already experienced 2-3 inches of rainfall over the past 6 hours,
    and with wet ground conditions and urban interfaces across the
    discussion area, potential exists for excessive runoff issues in
    the short term.

    Fast southerly low-level flow should allow for at least modest
    northward retreat of the outflow boundary along with a northward
    shift in the primary axis of training convection, though the
    northward retreat may not be as rapid as recent mesoanalyses
    indicate. Meanwhile, additional upstream convection over central
    Mississippi should gradually mature while moving toward the Tuscaloosa-to-Birmingham corridor this morning. This corridor
    could see a locally enhanced threat of isolated flash flooding
    over the next 2-4 hours or so (through 19Z/1p central).

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6oo1BSolf7M2qBcRNsBLpY_s_IwsR3N0WjlYfTIZJDSjo1V43q768zdRjEmPkHSL37-S= nj5LWzZgDLCEWCWE-B8J0X0$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...MEG...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34228682 33838585 33108582 32558693 32388875=20
    32808939 33598868 33928817=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Nov 26 04:17:58 2025
    AWUS01 KWNH 260417
    FFGMPD
    TXZ000-260920-

    Mesoscale Precipitation Discussion 1251
    NWS Weather Prediction Center College Park MD
    1117 PM EST Tue Nov 25 2025

    Areas affected...South Texas

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

    Valid 260415Z - 260920Z

    Summary...A localized flash flood risk will exist across portions
    of southern TX through at least 09Z. Slow moving and/or
    backbuilding of thunderstorms could result in isolated totals in
    excess of 3-5 inches, though some uncertainty in placement and
    timing remain.

    Discussion...04Z radar and infrared satellite imagery showed a
    lone thunderstorm over southern Webb County, about 15 miles east
    of the Rio Grande with a slow northward drift. Radar and satellite
    imagery also showed recent attempts at development over Live Oak
    County and portions of northern Mexico though low level CIN may be
    hindering further development. MRMS-derived hourly rainfall was
    over 2 inches with the cell although the likely presence of large
    hail may be over-inflating those values and no ground truth was
    available to confirm actual rain rates. The cell was located near
    a quasi-stationary front which has drifted north and west over the
    past couple of hours due to a weak low level easterly surge off of
    the warm Gulf waters with surface dewpoints in the lower 70s from
    CRP to BKS and southward to the Rio Grande. Low level convergence
    and lift augmented by a subtle shortwave impulse tracking east
    from north-central Mexico as seen in 6.2 micron imagery seem to be
    triggers for the storm(s).

    00Z soundings from CRP and BRO showed 1.3 to 1.6 inch PW values
    along with 1500-2000 J/kg MLCAPE, with this airmass likely in
    place near the cell over Webb County. The environment was
    supportive of a mixture of storm modes with sufficient shear for
    organized cells and straight-line hodographs which could support
    splitting storms. Bunkers right motion was toward the SSE near 20
    kt, Bunkers left from the SSW near 15 kt and deeper layer mean
    winds from the west between 5 and 20 kt.

    While recent hires model guidance shows a decent signal for
    localized heavy rain in the vicinity of southern TX, there is poor
    agreement in placement and timing. Current thinking is for the
    existing cell over Webb County to maintain for at least another
    1-2 hours with a continued drift toward the north or west with
    localized heavy rain. The future beyond that time is unclear as
    better low level confluence shifts westward into Mexico but
    additional convective development appears possible near the
    frontal boundary and south TX coast later in the night. Additional
    potential for high rates in excess of 2 in/hr and spotty totals in
    excess of 3 to 5 inches will remain possible.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-otaUnJHL9uHMhHKbJWde9LUbFGUwUeanvAO9Vad5_uIr0z-QeNKrL-6eTtn8HcWvIKY= zxOkhDsM0PZ1MCtcwAVzSW4$ for graphic product...

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

    ATTN...RFC...FWR...NWC...

    LAT...LON 28739716 28419661 27979657 27069704 25679698=20
    25829839 26089916 26689958 27359974 27970016=20
    28239969 28689774=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Nov 26 09:07:30 2025
    AWUS01 KWNH 260907
    FFGMPD
    TXZ000-261400-

    Mesoscale Precipitation Discussion 1252
    NWS Weather Prediction Center College Park MD
    406 AM EST Wed Nov 26 2025

    Areas affected...South TX

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

    Valid 260905Z - 261400Z

    Summary...A fairly localized flash flood threat will continue over
    portions of southern TX through sunrise. Slow moving thunderstorms
    will be capable of hourly rainfall in excess of 2 to 3 inches in
    an hour with potential for additional totals of 3 to 5+ inches.

    Discussion...Area radar imagery over southern TX at 0840Z showed a
    slow moving thunderstorm in the vicinity of Hebronville along with
    the recent (since 07Z) expansion of a broken line of thunderstorms
    extending west from Rockport. The line of storms to north of
    Hebronville appears to be elevated just above the surface given
    increasing northerly winds at the surface and lowering dewpoints
    just north of these storms, associated with a cold front which
    extended through the western Gulf into the lower Rio Grande
    Valley. While ground truth of observed rainfall at the surface has
    been limited, the ASOS from KHBV showed 0.88 inches of rain in 8
    minutes ending 0735Z. This is an example of what the environment
    over south TX can produce, represented by MLCAPE of 1000-2000 J/kg
    and precipitable water values near 1.5 inches (per 08Z SPC
    mesoanalysis data).

    The slow moving cold front will begin to move toward the south at
    a more rapid pace by 12Z and beyond, due to a strong ridge of high
    pressure to the north building in and a secondary cold front
    currently moving steadily through central TX. Until then however,
    the potential for slow moving thunderstorms will continue given a
    mixture of cell types and cell motions, some of which could be
    less than 10 kt toward the east. There is also some potential for
    cells to develop/stall near the coast as a corridor of relatively
    stronger low level flow near the front (15-20 kt 925-850 mb layer)
    acts to focus cells along a coastal convergence axis forced by the
    warmer Gulf waters relative to inland locations.

    While the potential for flash flooding looks to be isolated, the
    potential for high rain rates and localized totals in excess of
    3-5 inches will maintain concerns for rapid inundation of water
    until ~14Z, at which point, the cold front is forecast to be
    moving through Brownsville.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9MR70JC_4x4-U6ClozgFChiBGGoHQgRXY5C8hXC0VU8raHtYF-yjLC3JdDUp3Flb2bBw= quZZ_nlZZT1G0h3xDIRz-kE$ for graphic product...

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

    ATTN...RFC...FWR...NWC...

    LAT...LON 28419728 28369661 27979657 27069704 25679698=20
    25829839 26089916 26689958 27129972 27759937=20
    28169865=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Nov 26 14:15:35 2025
    AWUS01 KWNH 261415
    FFGMPD
    TXZ000-261710-

    Mesoscale Precipitation Discussion 1253
    NWS Weather Prediction Center College Park MD
    914 AM EST Wed Nov 26 2025

    Areas affected...south Texas

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

    Valid 261410Z - 261710Z

    Summary...Isolated flash flood potential will continue for another
    2-3 hours across south Texas.

    Discussion...Flash flood potential continues. Recent
    satellite/objective analyses depict a weak mid-level shortwave
    trough moving over south Texas, continuing to initiate and
    maintain deep moist convection along a synoptic frontal zone over
    the area (extending from Rio Grande City east to Padre Island and
    Gulf of American waters). 1.5+ inch PW values and 2000 J/kg
    SBCAPE continues to support efficient rainfall processes with
    storms. Meanwhile, kinematics (with weak flow below 500mb)
    continue to support slow cell movement and spots of 2-3 inch/hr
    rain rates. While there's still an appreciable chance for these
    rates to materialize along more populated/urbanized areas near the
    Rio Grande (i.e., Brownsville, Harlingen, etc.) and prompt flash
    flooding, overall convective trends suggest that eventual
    low-level stabilization (due to overturning and cooler air
    filtering into the region from the north) should result in flash
    flood potential decreasing especially after 16-17Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7niCFkluyJDIbuSuPYqL7SSm2hwkFMDS5usNSZMTspejBrOI4OseGZJF2Xlq8tLfJV8H= 26GLvedeOdEYdPP1KfKG9Ao$ for graphic product...

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

    ATTN...RFC...FWR...NWC...

    LAT...LON 27419817 26809699 25819722 26319917 26819957=20
    27299962=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Nov 29 21:53:25 2025
    AWUS01 KWNH 292153
    FFGMPD
    TXZ000-300351-

    Mesoscale Precipitation Discussion 1254
    NWS Weather Prediction Center College Park MD
    452 PM EST Sat Nov 29 2025

    Areas affected...Southeast Texas

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

    Valid 292151Z - 300351Z

    Summary...Thunderstorms near Houston TX are expected to grow
    upscale and potentially backbuild/train with time. Hourly amounts
    to 2.5" with local totals to 5" could lead to widely scattered
    instances of flash flooding.

    Discussion...Satellite and radar imagery indicate the formation of
    showers and thunderstorms near and east of a baroclinic zone
    oriented northwest-southeast across Southeast TX within a region
    of 850 hPa confluence near I-10. ML/MU CAPE to the west and
    southwest is 1000-2000 J/kg. Effective bulk shear is near 40 kts,
    which has led to right movers near IAH itself. The atmosphere is
    saturated, considering precipitable water values (1.25-1.5" per
    GPS data) within a region of 5630 meter 1000-500 hPa thickness
    values. Hourly rain amounts of are up to 0.5-1" in the past hour
    near Stagecoach TX, as of the time of this discussion's writing.

    The 18z HREF moreso than the 12z REFS indicates the continued
    building of thunderstorms in this area, with some further increase
    in convective coverage, which may show backbuilding, training
    character with time. Instability could erode/retreat westward
    with time depending upon the degree of convective coverage,
    essentially stalling the front west of Houston. Cell mergers are
    also possible as less organized convection moves more northeast
    while more organized convection moves more to the east. Given the
    parameters, hourly amounts to 2.5" with local amounts to 5" are
    possible over the next several hours, with the magnitude most in
    line with the 12z ARW and 20z HRRR guidance. There is a chance
    late in the MPD period of convection trying to form across
    northeast TX presently near and ahead of an advancing cold front
    approaching the southeast TX convective area, which could lead to
    more cell mergers at or beyond 04z. Since the 12z ARW and 18z
    HREF are closer to the convective evolution thus far, used their
    guidance for the defined MPD area. Widely scattered instances of
    flash flooding are considered possible, particularly in the
    Houston metropolitan area.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Vhatwq8jLS3mZorPAMnYdTnKTx4EfsxLABG-GVOUpKylJtFpPdI52knRINntAjzbM-p= HzQOyXL5ZWPQujCk3_4mvYw$ for graphic product...

    ATTN...WFO...EWX...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30579626 30439491 29959459 29489490 29339650=20
    29869717=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Nov 30 03:57:29 2025
    AWUS01 KWNH 300357
    FFGMPD
    LAZ000-TXZ000-301000-

    Mesoscale Precipitation Discussion 1255
    NWS Weather Prediction Center College Park MD
    1056 PM EST Sat Nov 29 2025

    Areas affected...Central and Upper Texas Coastal Plain...

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

    Valid 300400Z - 301000Z

    SUMMARY...Slow moving, pre-frontal cells with rates of 2"/hr
    eventually merge with south-southeastward pressing cold front
    convection resulting in localized 2-4" totals in 1-3 hours.=20
    Isolated flash flooding remains possible, especially near urban
    centers.

    DISCUSSION...GOES-E 3.9um SWIR highlights a few low level
    boundaries that will remain the focus of scattered thunderstorm
    activity through the overnight period. The main being the surging
    cold front being reinforced by favorable upper-level orientations
    to support steepening of theta-E gradient while increasing
    northerly surface wind flow to over 20-25kts nearly counter to the
    weaker but solid onshore flow. Currently active convection along
    the leading edge of the front is slow moving from Burleson to Polk
    county as the winds are not fully intersecting with the line, but
    will likely be propagating southward in the next hour or so. The
    other boundary is the return moisture plume off the western Gulf
    (which arches similar to the Lower TX Gulf coast before angling
    east- northeast just south of the aforementioned convection). Tds
    in the upper 60s to near 70 can be traced best in CIRA LPW sfc-850
    and 850-700mb layers covering much of the MPD area of concern
    across the Central and Upper Texas Coastal Plain.

    Onshore flow is also increasing to 15-20kts resulting in
    frictional convergence near coast. Conditionally unstable airmass
    with MLCAPEs of 1000-1250 J/kg remain weakly capped but there are
    some signs in satellite imagery of some weak cu field near
    Victoria, TX as well as an isolated weakening supercells
    northeast of Galveston Bay. The merging of the boundaries is also
    allowing a westward expansion of new development upstream into
    Bastrop/Caldwell county vicinity.=20

    Total deep moisture of 1.5" as noted in the CIRA LPW is loaded
    below 700mb, but there is solid deep saturation. These isolated
    cells driven by frictional convergence will be slow moving and
    eventually capable of 1-2"/hr rates. Spotty 2-3" totals will
    occur in 1-2hrs, but as they mature and expand the slower moving
    cells along the cold front will have started increased forward
    speed and with very high low level moisture flux convergence will
    have the capability of 1-1.25"/15min rainfall totals as they
    intersect/merge with the cells across the Plain.

    00z HREF probabilities continue to suggest 3"/3hr totals in the
    20-30% range (3"/6hr over 50%) which is fairly impressive given
    the strength of the updraft due to instability is fairly limited.=20
    While the overall coverage will continue to be limited, spots of
    3-4" totals are probable through 09z. This places sufficient
    overlap of FFG exceedance (as 1hr FFG is 2.5-3" and 3hr is 3-4")
    for possible localized incident or two of flash/rapid inundation
    flooding. This only further increases with intersection with
    urban centers, such as Victoria, Houston and Beaumont.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6eBqZJFeXYwfdfjOanroH9GQeQtbydrQfNUR442JL4eOoRDBCnP5-W_eKdR2izXE3AJE= Wxq3reM5uV59a3QArZIE_ho$ for graphic product...

    ATTN...WFO...CRP...EWX...HGX...LCH...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30999472 30719393 30099362 29749380 29519420=20
    29359466 28499607 27779725 27969777 28499795=20
    29529752 29879714 30199681 30729602=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Dec 2 00:36:34 2025
    AWUS01 KWNH 020035
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-020634-

    Mesoscale Precipitation Discussion 1256
    NWS Weather Prediction Center College Park MD
    734 PM EST Mon Dec 01 2025

    Areas affected...portions of the central Gulf Coast

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

    Valid 020034Z - 020634Z

    Summary...A combination of cell training and backbuilding should
    continue to lead to hourly rain amounts to 1.75" with local totals
    to 4", which could cause flash flooding in urban areas.

    Discussion...Instability across portions of the central Gulf Coast
    continues to rise ahead of a negatively-tilted shortwave across
    OK. Precipitable water values are ~1.6" per GPS data and MU CAPE
    values of 500+ J/kg lie across the southeast tip of LA and
    continue shifting north towards the MS/AL barrier islands. Radar
    estimates from LIX/Hammond LA indicate that hourly amounts peaked
    near 1.75" not far from the eastern suburbs of New Orleans
    recently, with local totals above 2.5" so far. Occasional hourly
    rain amounts to 1.5" have been seen in backbuilding convection in
    southernmost AL. Effective bulk shear of 25-45 kts lurks across
    the area which is helping to form a band within an area of 850 hPa
    confluence.

    The band is showing some signs of shifting northward across
    southern AL and slightly eastward in southeast LA. Additional
    activity south of the LA/MS coasts within a convergence zone which
    extends from northwest Cuba towards the central Gulf Coast could
    advect northward towards portions of this area in the next several
    hours and cause additional issues. The guidance has not been
    ideal in this region thus far -- too far north and too light --
    though the 18z hi-res NAM appears to have the best idea, so used
    it as a starting point for the MPD bounds, making some adjustments
    based on radar reflectivity trends. The region has been dry, so
    flash flood guidance values are high. Hourly amounts to 1.75" and
    local totals to 4" appear possible where cells train and/or
    backbuild, which would be most problematic in urban areas.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6SdogcIUxTtroqQTUwxSALeN9Fo_uMvC5I4pW6eAAjX9DWw67VnyMfB31nkTA5_xaSPt= yY_XxORQJb-wb9BRCh179PU$ for graphic product...

    ATTN...WFO...BMX...LIX...MOB...TAE...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 31928616 31298582 30558670 30248743 30078846=20
    29938870 29778905 29439024 29689078 30768934=20
    31778728=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Dec 8 00:44:12 2025
    AWUS01 KWNH 080044
    FFGMPD
    FLZ000-080300-

    Mesoscale Precipitation Discussion 1257
    NWS Weather Prediction Center College Park MD
    742 PM EST Sun Dec 07 2025

    Areas affected...Portions of the Central Florida Peninsula

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

    Valid 080041Z - 080300Z

    Summary...A combination of locally intense rainfall and cell
    training should continue this evening which could cause flash
    flooding in urban areas.

    Discussion...Thunderstorms with isolated maximum rainfall rates
    approaching 1.5 inches per hour have been moving on-shore and
    tracking northeastward from near Tampa to Cape Canaveral early
    this evening. These storms appear to be associated with a
    mid-level vorticity maximum approaching from the eastern Gulf of
    America along the axis of a 2+ inch precipitable water plume and
    axis of boundary layer moisture flux convergence. Radar estimates
    from TBW/Tampa Bay indicate that hourly amounts have peaked near
    1.75 inches in parts of Pinellas and Pasco counties and that the
    maximum rainfall totals were approaching 3.25 inches in the same
    area. These amounts were embedded within a broader 1.5 to 2,5
    inch stripe of rainfall extending towards the central portion of
    the peninsula.

    With additional showers and thunderstorms located off-shore...the
    potential for flooding due to multiple rounds of heavy rainfall
    exists. The 18Z HREF/RRFS showed the probability of 1 inch per
    hour rates diminishing to less than 5 percent along the west-coast
    by 08/03Z. Their placement has been a bit too far north with the
    intense rates. Even so...the HREF captured the evolution in the
    broadest sense and was used it as a starting point for the MPD.=20

    Maximum Hourly amounts 1" to 1.75" and local totals to 3.5" appear
    possible where cells train and/or back-build, which would be most
    problematic in urban areas and regions of poor drainage as well as
    along small streams.

    Bann

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6pVmRublY1OVsAJkJg8O46F9ZFJcJq11wZG7H7yfyyETA4AMO-6DQLkDZoaZVaqobmxQ= aeSyDnVcKLlM3SGwH4kZuK0$ for graphic product...

    ATTN...WFO...MLB...TBW...

    ATTN...RFC...ALR...NWC...

    LAT...LON 28538137 28538106 28328102 28008125 27678210=20
    27488265 27958282 28338219 28488162=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Dec 8 16:53:22 2025
    AWUS01 KWNH 081653
    FFGMPD
    ORZ000-WAZ000-090400-

    Mesoscale Precipitation Discussion 1258
    NWS Weather Prediction Center College Park MD
    1152 AM EST Mon Dec 08 2025

    Areas affected...Western Washington...Far Northwest Oregon...

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

    Valid 081700Z - 090400Z

    SUMMARY...Very strong atmospheric river with persistent .25-.5"/hr
    rates falling on increasingly saturated soils will result in high
    run-off, swelling rivers and poor drainage/urban flooding but at
    minimum further set the stage for expected additional rainfall
    into the mid-week.

    DISCUSSION...Regional RADAR mosaic is showing the leading
    warm/moisture advection surge from the atmospheric river is
    expanding across the Pacific Northwest and into the Washington
    Cascades at this time. CIRA LPW animation depicts a long fetch
    core to the atmospheric river with a long tap back to the tropics
    near the Dateline; though the strength of the polar stream with
    150-170kt fairly zonal upper-level jet has resulted in very strong
    deep layer flow which has resulted in a fairly long/gradual
    isentropic incline to deplete any potential of vertical
    instability, the strength of moisture flux anomalies are pushing
    the maximum climatological percentiles for this time of year. This
    is generally confirmed by CIRA LPW percentiles in the 95-99th
    range through all layers but most noted in the 700-500mb at this
    time.

    The total PWat values are at or above 1.25" and have come ashore
    with the subtle but fast moving warm front denoted with wind shift
    from south to southwest and increase to 40kts at surface, 50-60kts
    near boundary layer and over 70kts at 700mb, this has lead to IVT
    values very near 1000 kg/m/s analyzed just offshore while
    remaining above 700 kg/m/s into the Cascades currently, but is
    expected to rise as the effective warm sector moisture intersects
    the terrain fairly orthogonally as well. As a result, broad
    .25-.33"/hr rates have been seen near the coastal areas so far and
    will expand into W WA over the next few hours. The nose of the
    upper-jet remains north for a bit and height-falls on the western
    side of the core will not start to dip southward until well after
    00z as the cold front reaches the mouth of the Juan de Fuca Strait
    around 00-01z.

    The strong flux, upslope flow will allow for rates of .5"/hr
    regularly through the mid to upper slopes of the Cascade Range as
    the WAA has freezing heights above all but the highest peaks. As
    such upper slopes will see 3-5" totals by 03z with foothills
    likely to be 2-4" and lower valleys less than 2"...with isolated
    totals to 6-7"+ along the core of the AR in the southern WA
    Cascade Range. Coastal Ranges including the Olympics may see
    4-6". Overall, FFG values are high enough even to encompass all
    but those highest extreme values being greater than 3.5/3hrs and
    over 5"/6hrs. However, NASA SPoRT LIS 0-40cm soil saturation
    values are generally above 70-80% across which is generally a bit
    above normal for the Coastal Range, but near 75-85th percentiles
    for the Cascade Range; however, full saturation should occur
    through the late afternoon, and as the main surge occurs toward
    00z, much of the rainfall should convert to run-off. This should
    swell the rivers fairly quickly with compounding issues resulting
    in riverine flooding (please refer to discussion and graphical
    products from NW River Forecast Center and National Water Center
    for further details).

    Given this is the first surge of a prolonged AR event, the
    potential for flash flooding is likely limited to the highest
    slopes/reaches of the watersheds or some localized urban flooding
    due to poor drainage. With the saturation of the soils through
    depth, there will be a slowly increasing potential for mudslides
    especially near/downslope any recent burn scars.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!41Gpl_K0C4oZ8oksLbVkshXJ6rbtTPELhF_yqA-pb03G5RNZm1ZMxwDtMJ02CLLoM3h0= Gh03LT2xq3MSxojGryzr5JQ$ for graphic product...

    ATTN...WFO...OTX...PDT...PQR...SEW...

    ATTN...RFC...PTR...NWC...

    LAT...LON 49112107 48812060 48292030 47312040 46882082=20
    45752140 45492147 45512177 45902229 46102264=20
    46062298 45822333 45732387 46362422 47182433=20
    47832456 48222487 48462487 48292398 47902348=20
    47362331 46992302 46942246 47252212 47702194=20
    48252209 48572212 48962190 49092160=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Dec 9 21:12:11 2025
    AWUS01 KWNH 092112
    FFGMPD
    ORZ000-WAZ000-100910-

    Mesoscale Precipitation Discussion 1259
    NWS Weather Prediction Center College Park MD
    411 PM EST Tue Dec 09 2025

    Areas affected...Northern Oregon and Western Washington

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

    Valid 092110Z - 100910Z

    Summary...The ongoing atmospheric river event over the Pacific
    Northwest will continue into tonight over portions of western
    Oregon and Washington. The axis of heaviest rainfall is expected
    to shift back north into Washington and also increase in
    intensity, which will bring an increasing flood and landslide risk
    to these areas.

    Discussion...The expectation is that the atmospheric river
    impacting northern OR will shift northward back into western WA
    this evening. After a temporary drop in Integrated Water Vapor
    Transport (IVT) today, values are forecast to increase again
    towards 03z resulting in an uptick in rainfall coverage and
    intensity into the overnight hours. With no forecast instability,
    rainfall rates will be driven mostly by the magnitude of moisture
    transport into the terrain. This will put a cap on the upper bound
    of rainfall rates, although this will be compensated by IVT values
    above the climatological 99th percentile and layered precipitable
    water (PW) generally above the 95th percentile at all atmospheric
    levels. This deep moisture and strong moisture transport will
    support hourly rainfall in the 0.25"-0.40" range, potentially
    approaching 0.50" in the highest mountain peaks. These rates
    should increase in coverage after 03z (per the 12z HREF
    probabilities), moving from northern OR into western WA overnight.
    Additional rainfall through 09z Wednesday is generally expected to
    be in the 1-3" range.

    Under typical conditions, rainfall rates and totals of this
    magnitude would not pose a significant hazard to this region.
    However, the past 24 hours have already brought 4-10" of rain to
    these locations, leading to saturated ground and elevated streams
    and rivers. Although parts of WA saw a brief lull today allowing
    for some recovery, hydrologic conditions remain sensitive.
    Consequently, when heavier rain returns this evening into tonight,
    additional flood impacts are expected.

    The primary impacts are expected to be flooding of rivers and
    streams, other low-lying flood-prone areas, and poor drainage and
    urban areas. Given the saturated ground, the risk of landslides
    and debris flows in areas of steep terrain will also increase
    tonight as rainfall intensity ramps up.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!43p-OkfUop706I6cKLYBBIwzA6nB0hPZtCxkYgIrTsd-VTMoHaWWkfw9qP6uMmlQkjOt= HZdFGfUJBx9ZZGkLPPdfEFs$ for graphic product...

    ATTN...WFO...OTX...PDT...PQR...SEW...

    ATTN...RFC...PTR...NWC...

    LAT...LON 47942123 47642074 46792112 46432130 45912145=20
    45412151 45322145 44952164 44572184 44412215=20
    44522255 44712277 45042250 45422224 45882270=20
    45822308 45252331 44842354 44972399 45782413=20
    46532407 47232417 47682412 47842384 47782333=20
    47392322 47042294 46852251 47122208 47482197=20
    47762182=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Dec 10 16:28:53 2025
    AWUS01 KWNH 101628
    FFGMPD
    WAZ000-110300-

    Mesoscale Precipitation Discussion 1260
    NWS Weather Prediction Center College Park MD
    1128 AM EST Wed Dec 10 2025

    Areas affected...Olympic and Cascade Ranges of Western
    Washington...

    Concerning...Heavy rainfall

    Valid 101630Z - 110300Z

    SUMMARY...Core of next atmospheric river surge through evening.=20
    Rates of .33-.75"/hr based on elevation likely to further compound
    ongoing river flooding throughout the foothills of the Olympic and
    Cascade Ranges. Mud/Landslide potential continues to increase
    with amount of deep soil moisture.

    DISCUSSION...Recent regional RADAR mosaic shows core of solid
    stratiform rainfall is expanding across much of western
    Washington. CIRA LPW shows solid sub-tropical moisture connection
    tapping just northwest of Kaua'i only narrowing/concentrating
    along and south of the stationary front 42N/142W to the Olympic
    Range. RAP analysis and recent VWP network observations denote a
    surge of increased moisture/warm advection south of the front is
    directed orthogonally to the Olympic Range and further downstream
    to the western Washington Cascades with 30-40kts of boundary layer
    orographic ascent and Tds in the mid 50s. CIRA LPW also notes
    that core of enhanced 850-700mb remains well displaced (east over
    WA at this time) to the surface core indicative of the long,
    gentle upslope of the AR moisture plume; so with limited unstable
    air, orographic moisture flux convergence remains the primary
    driver of intense rates, so stark rainshadows and much lower
    rainfall totals/rates are expected in main, lower elevation
    valleys.=20=20

    CIRA LPW analysis, extrapolation shows core of enhanced moisture
    below 700mb will continue to be directed toward the Juan de Fuca Strait/Northern Olympics into the Northern Washington Cascades
    over the next 6-9hrs supporting rates of .25" in the valleys to up
    to .75" in the highest terrain of the Cascades; and with the
    strong warm sub-tropic air, all but the most extreme peaks will
    continue to remain below the freezing levels. RAP/HRRR along with
    LPW extrapolation suggest core of enhanced moisture and winds will
    slowly reduce from supporting over 800 kg/m/s IVT values below 600
    kg/m/s toward 00z with the front sagging south toward the mouth of
    the Columbia river by 06z.=20=20

    FFG values are static in the Pacific Northwest and are not likely
    to be exceeded; however, NASA SPoRT shows 0-40cm saturation is
    near 90%, so nearly all those rates will be fully run-off. Flash flooding/rapid inundation flooding is not expected except for the
    highest reaches of watersheds/upper slope creeks, etc. but the
    rainfall will definitely continue a steady rise/expansion of
    ongoing river flooding across the area. Please refer to Northwest
    River Forecast Center and National Water Center products for
    details of these ongoing dangerous, life threatening conditions.=20

    Additionally, deep layer saturation of the upper soils suggests
    mud/landslides may become increasingly possible through this
    evening, especially given affects of strong winds acting upon the
    trees and therefore their roots. Remain aware of this potential
    and refer to local emergency managers and USGS reports/products
    regarding landslide concerns.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8L2D4ky7YUPIc_XTauE7f5mOBTS_tFcGMz7lVQIdQ_QXNey033P0XO5k-9kianVdLxxG= MzntNDwJCMC7cWkTFvSaRJ0$ for graphic product...

    ATTN...WFO...OTX...PDT...SEW...

    ATTN...RFC...PTR...NWC...

    LAT...LON 49092147 48632099 48032072 47612090 46942137=20
    46942189 47532210 47892184 48252199 48662228=20
    49002260 48782323 47892312 47002346 47192395=20
    47762440 48222461 48152365 48122326 49042328=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 Dec 11 04:09:00 2025
    AWUS01 KWNH 110408
    FFGMPD
    WAZ000-111530-

    Mesoscale Precipitation Discussion 1261
    NWS Weather Prediction Center College Park MD
    1107 PM EST Wed Dec 10 2025

    Areas affected...Western WA (including the Olympic Peninsula and
    Cascades)

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

    Valid 110407Z - 111530Z

    SUMMARY...Strong atmospheric river activity to continue overnight
    across much of western WA with a focus for additional heavy rain
    and locally significant areal flooding, including potential for
    debris flows, landslides and localized flash flooding.

    DISCUSSION...The latest GOES-W WV suite along with OSPO/CIRA ALPW
    data sets show a well-defined and strong atmospheric river
    continuing to advance inland across western WA, with an upstream
    orthogonal orientation of the deep Pacific moisture axis/plume
    relative to the Olympic Peninsula and the Cascades. Satellite and
    radar data continue to show areas of heavy rain impacting these
    areas with recent rainfall rates in the 0.25" to 0.40"/hour range.

    Much of the deeper layer trans-Pacific moisture transport into the
    region continues to be aided by the positioning of a strong
    subtropical ridge near and offshore of CA, and an elongated axis
    of mid-level troughing from the Gulf of AK southwestward to
    30N/40N and 160W. Offshore experimental CIRA LVT data is showing
    some gradual slackening of the low and mid-level moisture
    transport around the top side of the ridge axis, and this may
    allow for some of the more widespread heavier rainfall rates to
    gradually subside a bit going through the overnight hours.

    However, there will be the arrival of a new Pacific cold front
    across the region as shortwave energy moves into British Columbia,
    and this boundary should slowly push inland and become more
    oriented west/east across southern WA Thursday morning. IVT
    magnitudes along the front should remain elevated for the next 6
    to 12 hours, but by early Thursday morning, these values are
    forecast to drop down into the 600 to 800 kg/m/s range with the
    overall slackening of the low to mid-level kinematic wind field
    environment.

    The 00Z HREF guidance does continue to support rainfall rates in
    the Olympic Peninsula of around a 0.25"/hour, but with heavier
    rates occasionally reaching a 0.50"+/hour in the central and
    northern WA Cascades. Going through 15Z (7AM PST) on Thursday, an
    additional 1 to 2 inches of rain is expected for the Olympic
    Peninsula, but with an additional 2 to 4 inches in the central and
    northern WA Cascades.

    These additional rains will exacerbate ongoing areal flooding and
    especially to the river basins which are locally seeing
    significant impacts. Given the amount of rainfall that has
    occurred over the last few days in the Cascades in particular
    (with 12 to 15+ inches locally), the terrain is particularly
    sensitive, with the additional rains favoring concerns for debris
    flows, landslides and potential flash flooding around areas of
    steep terrain.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!71Jepf9yev7hmkJDrRvmtLMcUq8j50D7FgYNO7kSskSH7SKK20EaAmLtVqgpFTJ6kFC0= SGJjw80lHp4zyyPnh7ywKDw$ for graphic product...

    ATTN...WFO...OTX...PDT...PQR...SEW...

    ATTN...RFC...PTR...NWC...

    LAT...LON 49202170 49192044 48662002 47232051 46482165=20
    46642366 47412470 48122487 48372444 48112360=20
    48162268 48802244=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Dec 11 14:52:35 2025
    AWUS01 KWNH 111452
    FFGMPD
    WAZ000-112048-

    Mesoscale Precipitation Discussion 1262
    NWS Weather Prediction Center College Park MD
    951 AM EST Thu Dec 11 2025

    Areas affected...portions of western Washington State

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

    Valid 111448Z - 112048Z

    Summary...Ongoing moderate to heavy rainfall will continue to
    foster excessive runoff and flood/flash flood issues through at
    least 20Z/noon Pacific time.

    Discussion...A persistent atmospheric river continues to spread
    areas of moderate to heavy rainfall across the discussion area.=20
    Recent rain rates ranging from 0.15-0.5 inch/hr have been noted -
    especially in terrain-favored upslope areas of the Cascades. The
    rainfall was tied to strong 700mb flow perpendicular to the
    Cascades and 1 inch PW values - supporting abundant orographic
    ascent and precipitation. Unfortunately, these rain rates were
    continuing to impact inundated areas that have experienced 6-10
    inches of rain over the past 72 hours, with widespread,
    significant riverine flooding being reported as a result.

    Rainfall could continue for another 4-6 hours across the region.=20
    Eventually, models depict a weakening of 700mb flow over the
    Cascades as mid/upper ridging builds northward into the region.=20
    This may reduce acute flash flood potential, though riverine
    issues will likely continue for some time.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-ImXPjaEKxXDP2MXZn5DlOqZ-jEGbNw9fZaPqxDHzK7LZF4ZyYLNeT4WwF3zvzlNd8sy= HiRwBZt23t60q5z8yF4V1K8$ for graphic product...

    ATTN...WFO...OTX...PDT...PQR...SEW...

    ATTN...RFC...PTR...NWC...

    LAT...LON 48592119 48222044 47562035 46522081 46302172=20
    46582328 47552397 48042403 48322289 48502243=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 Dec 15 09:36:32 2025
    AWUS01 KWNH 150936
    FFGMPD
    ORZ000-WAZ000-152135-

    Mesoscale Precipitation Discussion 1263
    NWS Weather Prediction Center College Park MD
    435 AM EST Mon Dec 15 2025

    Areas affected...Western WA and Northwest OR

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

    Valid 150935Z - 152135Z

    SUMMARY...A new atmospheric river will be arriving this morning
    across the Pacific Northwest. New rounds of heavy rain will be
    associated with this across especially western WA and northwest
    OR, and this will gradually pose a renewed threat of flooding.

    DISCUSSION...The latest GOES-W WV suite along with OSPO/CIRA ALPW
    data shows a new trans-Pacific atmospheric river approaching the
    Pacific Northwest. The source region of the long-fetch moisture
    transport is situated well southwest of Hawaii along 160W to 170W,
    with a northeast advection of it up along and ahead of a
    well-defined frontal zone that extends from Hawaii to offshore of
    the West Coast. Satellite imagery and surface data also shows
    additional northern stream energy and a reinforcing cold front
    approaching from areas near and south of the Gulf of AK.

    Over the next 6 to 12 hours, strong deep layer southwest flow with
    embedded shortwave energy will approach and begin crossing the
    Pacific Northwest which will drive the aforementioned offshore
    fronts gradually inland across the coastal ranges. Strong warm air
    advection and enhanced low to mid-level flow will drive increasing
    rainfall rates across the orographically favored coastal ranges
    from northwest OR up into the Olympic Peninsula and eastward into
    the foothills and higher terrain of the Cascades.

    Microwave-based CMORPH2 data shows heavy rainfall rates associated
    with the offshore shortwave energy focused along 130W, with some
    rates on the order of 0.75" to 1"/hour. This is associated with
    broken areas of convection as validated by GOES-W GLM data
    indicating intermittent lightning activity. Some of these heavier
    rates should arrive gradually throughout the morning, and the 00Z
    HREF guidance shows high probabilities (>60%) of rainfall rates
    exceeding a 0.50"/hour across the Olympic Peninsula and the
    foothills of the Cascades, with some low-end probabilities
    (approaching 30%) of seeing these rates max out near 1"/hour in
    the central and southern WA Cascades.

    These high rates will coincide with the arrival of high IVT
    magnitudes that will be on the order of 800 to 1000 kg/m/s into
    the coastal ranges, with an inland penetration of the core IVT
    plume into the Cascades. Some modest instability with MUCAPE
    values up around 250+ J/kg along and just ahead of the frontal
    boundaries will also be a contributor to these elevated rates.

    Expect as much as 3 to 5 inches of new rainfall over the next 12
    hours, with the heaviest totals over the Olympic Peninsula and the
    windward slopes of the WA Cascades. Lesser amounts will be noted
    over northwest OR with as much as 1 to 3 inches here involving the orographically favored terrain.

    The region is extremely sensitive given the residual impacts from
    the recent high-impact multi-day atmospheric river. Elevated/high
    streamflows and saturated ground will support the additional rains
    going into runoff that will be capable of driving renewed areas of
    areal flooding. Some localized burn scar flash flooding, debris
    flows and landslide activity also cannot be ruled out today.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8CSOBZPag-i-C1aXm6jQzW12n-4RBwiZpBMzlfmSn5drA27YKyMJLZE9060HaBqpt42K= 23iAiSQIlsvBBUL7myAJ6NQ$ for graphic product...

    ATTN...WFO...OTX...PDT...PQR...SEW...

    ATTN...RFC...PTR...NWC...

    LAT...LON 49262217 49252090 48782034 47882038 46802093=20
    45402127 44392175 44302231 44662313 44682399=20
    45742427 47102424 48002466 48222357 47692293=20
    47822252 48592230=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Dec 15 21:57:21 2025
    AWUS01 KWNH 152157
    FFGMPD
    WAZ000-160900-

    Mesoscale Precipitation Discussion 1264
    NWS Weather Prediction Center College Park MD
    456 PM EST Mon Dec 15 2025

    Areas affected...western Washington

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

    Valid 152153Z - 160900Z

    SUMMARY...A subtle increase in rainfall intensity is expected over
    western WA through about 03Z with hourly rainfall peaking near 0.5
    inches. 12 hour accumulations of 1 to 2 inches will be possible
    through 09Z. While these higher rainfall intensities should remain
    isolated in nature across the Olympics and Cascades, the region
    remains saturated and quite sensitive due to last week's heavy
    rainfall event.

    DISCUSSION...The latest GOES West water vapor imagery showed the
    approach of a mid to upper-level vorticity max about 250 miles
    west of the mouth of the Columbia River, tracking toward the ENE.
    Total precipitable water values have come down since 12Z this
    morning as seen in recent blended TPW imagery with 0.6 to 0.8
    inches observed from the Washington coast to the Cascades at 21Z.
    850-700 mb mean layer winds were observed to be 50-60 kt via KLGX
    VAD wind data, forecast to decrease into the 30-45 kt range by 03Z
    via recent RAP forecasts. Hourly rainfall within the upslope
    regions of the Olympics and Cascades has peaked in the 0.2 to 0.3
    inch range over the past 2 hours with 2-4 inches (locally higher)
    observed over the past 24 hours in the Olympics and Cascades.

    The arrival of the offshore vorticity max has been preceded by
    cooling clouds tops on infrared satellite imagery and rainfall
    rates are likely to increase again over the next few hours over
    the Olympics and Cascades, at least locally, despite continued
    lowering of IVT values. This will be due to increased lift ahead
    of the vorticity max and the left-exit region of a powerful jet
    centered near 250 mb, centered ~1000 miles west of the WA/OR
    coastline. Recent GOES West DMVs measured a few points with 170 kt
    (10-15 kt higher than RAP forecasts). This jet max is forecast to
    continue strengthening as it translates eastward with left-exit
    ascent moving across western Washington tonight.

    Strengthening forcing for ascent coupled with weak elevated
    instability and mean WSW flow could support a couple of isolated
    hourly rainfall values near 0.5 inches and brief training of
    stronger echoes. The greatest probabilities for higher rainfall
    rates will occur with higher elevations/orographic lift which will
    be experiencing a transition to snow as freezing levels fall in
    the wake of a cold front which will limit contributions to
    additional flooding for the higher elevations above 5000 ft.
    However, where p-type will remain liquid, limited potential for a
    few hours of hourly rainfall in the 0.25 to 0.50 inch range
    through 06Z (locally higher) and additional rainfall totals of 1
    to 2 inches through 09Z within the windward slopes could result in
    additional flood concerns for the region.

    Due to the highly sensitive ground conditions, due largely in part
    to last weeks atmospheric river event, any additional rainfall
    will have the potential to renew or exacerbate flood concerns. The
    potential will also exist for isolated landslides/debris flows
    across the more sensitive regions of the Olympics and Cascades.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_ihbPIbF-hZ7NCZRjxSSeMKqV1C7qq5CnKKiK7KlcTB2BViBGIpgmm-d77a52eEHi0Iv= TvKo-4Ujjt6a7458NaeaiW8$ for graphic product...

    ATTN...WFO...PDT...PQR...SEW...

    ATTN...RFC...PTR...NWC...

    LAT...LON 48992144 48882113 48732105 48482127 48352141=20
    48162144 47962132 47792125 47612136 47432143=20
    47192137 47092151 47042160 47032170 47012180=20
    46962186 46892188 46832185 46782179 46762164=20
    46732161 46542156 46422167 46342213 46392236=20
    46582254 46762263 46912265 47082312 47122349=20
    47292387 47592402 47922419 48092409 48102367=20
    47972318 48052273 48532226 48942185=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Dec 18 14:01:00 2025
    AWUS01 KWNH 181400
    FFGMPD
    ORZ000-WAZ000-190200-

    Mesoscale Precipitation Discussion 1265
    NWS Weather Prediction Center College Park MD
    859 AM EST Thu Dec 18 2025

    Areas affected...Northwest Oregon...Far Southwest Washington...

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

    Valid 181400Z - 190200Z

    SUMMARY...Extreme surge of moisture flux into terrain as warm
    front passes will result in mid to upper slopes of coastal and
    Cascade Ranges to receive up to 1"/hr rates. Localized 5-7"
    totals are possible and may result in rapid rises and possible
    flooding in/along streams/rivers.

    DISCUSSION...GOES-W WV suite depicts a strong well
    anti-cyclonically curved ridge continue to dominate the eastern
    north Pacific with strong core of 150-180kt westerly 250 jet
    crossing the Juan de Fuca Strait attm. At the trailing edge
    increased divergence and subtle sheared shortwave is streaking
    through just west of 130W. This will focus surface to boundary
    layer cyclogenesis with a low 990mb low expected to lift northward
    toward the Strait by 21z. The energy through the atmospheric
    column is highly dynamic along and behind a surging warm front.=20
    This warm front has yet to reach the Pacific Coast, but is
    expected around 16-17z from south to north along the Oregon coast.
    Weaker southerly flow will quickly shift with 925mb flow swinging
    WSW to align through nearly the entire column to 500mb. Winds
    will increase to over 60kts with occasional speeds up to 70kt.=20=20

    CIRA LPW denotes the WAA aloft as just recently reached the coast
    though the 850-700mb layer with core of 99th and Maximum record
    values in this an 700-500mb layers (displaced further east over
    central OR attm due to the gentle slope of the deeper AR as a
    whole). As the warm front passes the total PWats will be over
    1.25" and fluxed on that strength of wind (50-80kts from
    925-700mb) will result in IVT values over 1000 kg/m/s with higher
    resolution guidance suggesting localized peaks nearing 1200 kg/m/s
    placing the surge toward the extreme range. While orientation to
    the terrain is not fully orthogonal, the magnitude of flux
    convergence and orographic ascent will support .75"/hr rates in
    the mid to upper slopes of the central to northwest Oregon Coastal
    Range and perhaps an hour later into the upper slopes of the
    Cascades north of Lane county. These rates are expected to surge
    and ebb through 00z, with an isolated 1"/hr rate possible. As
    such, rainfall totals will quickly total toward 5"+ in the terrain
    with rain-shadowed areas perhaps not even reaching .5". Early
    arriving 12z Hi-Res CAMs suggest isolated totals over 7" by 03z
    are not out of the realm of possibility. These values are pushing
    24hr ARI (Average Return Intervals) definitely into the 25 year
    range, with some suggestions of exceedance of 50 to 100 year
    values, in the upper slopes of the central Oregon Cascades. So
    the rainfall is highly atypical and therefore flooding is
    possible.

    FFG values in the region are static and are not likely to be
    exceeded at 1 or 3hr periods but may push the 6hr+ time range.=20
    Yet, NASA SPoRT LIS 0-40cm soil saturation remain above 70% given
    the connection to last week's event that was focused further
    north, and may result in above average run-off as upper profiles
    will quickly saturate. As such, even the glancing blow across into
    W WA could exacerbate ongoing flooding there and has been included
    in the area of concern, though rates/totals would be reduced to
    the core in central to northern Oregon. So any flooding is not
    necessarily going to be flashy in nature but notable surge in
    river levels will be noted. As such, please continue to monitor
    River Forecasts from local forecast offices, Northwest River
    Forecast Center, and products/discussion from the National Water
    Center.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!66DWPwXIdIRzihZ8KNWR2kFs3hqm9EhGdO2Y4CVe9gNTFathDiknnp_0mkOk5RDuyJAM= -pULRKiW904eJ5HzsifTnVs$ for graphic product...

    ATTN...WFO...PDT...PQR...SEW...

    ATTN...RFC...PTR...NWC...

    LAT...LON 46812171 46592138 46062138 44512157 43922193=20
    43642242 43972308 44012371 44032419 44232423=20
    44802415 45412406 46042402 46202370 46122328=20
    45572281 45862238 46232230 46612213=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Dec 19 02:09:55 2025
    AWUS01 KWNH 190209
    FFGMPD
    ORZ000-WAZ000-190807-

    Mesoscale Precipitation Discussion 1266
    NWS Weather Prediction Center College Park MD
    907 PM EST Thu Dec 18 2025

    Areas affected...portions of western Oregon and southwestern
    Washington State

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

    Valid 190207Z - 190807Z

    Summary...Flood/flash flood potential continues as a strong
    atmospheric river traverses the area through 08Z/midnight Pacific
    Time.

    Discussion...Flood/flash flood potential continues across the
    discussion area. A strong, landfalling atmospheric river
    continues to produce areas of 0.25-0.5 inch/hr rain rates across
    the region - highest across upwind, terrain-favored areas. This
    heavy rainfall regime has persisted for some time, resulting in
    around 1-3 inches of rainfall over the past 12 hours. These rain
    rates have contributed to at least isolated instances of excessive
    runoff and impacts in some areas. Soils are wet and streamflows
    are high across the region - especially where the heaviest
    rainfall has occurred.

    Models/observations suggest that at least another 3-5 hours of
    rainfall is expected across the discussion area, with 0.25+
    inch/hr rain rates and 1-1.5 inch totals potentially occurring
    through 08Z/midnight Pacific Time. Over time, a front will
    migrate from northwest to southeast across the discussion area,
    resulting in a gradual southeastward shift in the heaviest
    rainfall rates as peak low-level flow shifts toward central and
    southwestern Oregon. Areas of flooding/flash flooding remain
    possible given the sensitive ground conditions that are readily
    supporting excessive runoff.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_X7D6LBwyUIHGeozsPitQ2wTaN1VLJ2UMr87Cg64CYGoqaeZGBU2fXqJmKxikY9qKDSi= aP51iJ_xHhCZfbG7AsZ1cSk$ for graphic product...

    ATTN...WFO...MFR...PDT...PQR...SEW...

    ATTN...RFC...PTR...NWC...

    LAT...LON 47402191 47322132 46512095 45332117 44172139=20
    43472199 43212283 43812402 43902436 46612426=20
    46422320 46132280 46082242 46922217=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Dec 21 06:16:08 2025
    AWUS01 KWNH 210616
    FFGMPD
    CAZ000-211812-

    Mesoscale Precipitation Discussion 1267
    NWS Weather Prediction Center College Park MD
    113 AM EST Sun Dec 21 2025

    Areas affected...portions of northern and central California

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

    Valid 210612Z - 211812Z

    Summary...Onset of a long-duration heavy rain hazard is underway
    as an atmospheric river makes landfall across central and northern
    California. Upwind regions of high terrain could experience
    periods of 0.5-1.0 inch/hr rain rates. Flash flooding is likely
    through the morning hours.

    Discussion...Recent radar/MRMS data depicts an uptick in heavy
    rainfall/rain rates across northern and central California
    currently. The greatest rates were occurring across coastal
    ranges north/northwest of San Francisco, where strengthening, west-southwesterly 850mb flow (around 40 knots) was oriented
    perpendicular to ridgelines/terrain in that area. The combination
    of orographic ascent and 1.5 inch PW values located just upstream
    of the area were supporting areas of 0.25-0.5 inch measured rain
    rates over the past hour or so.

    Models/observations suggest that the ongoing areas of heavy rain
    will only expand and increase in intensity with time. 850mb
    should increase into the 40-50 knot range over the next few hours
    while impinging upon upwind slopes of the Sierra and northern
    California coastal ranges. This will allow for areas of 0.5 to 1
    inch/hr rain rates to materialize in terrain-favored areas and
    persist for 6+ hours.=20

    USGS Streamflow and NASA SPoRT-LiS Soil Moistures suggest ground
    conditions can handle initial rainfall with somewhat dry initial
    soil conditions and modest flow in local streams. Multiple hours
    of heavier rainfall will likely make ground conditions more
    favorable for excessive runoff and flood/flash flood impacts over
    time. The greatest risk for flood/flash flood instances will
    occur from 09Z/1a Pacific Time, and multiple instances of
    excessive runoff are expected through 18Z/10a.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6UfaRemdCkGYpLIhlFPONIeYmwwruTOcraTfEqSSeTpLE3--jvLref83zgvivudYXlzW= v-lQ7zarJ1Nt1ckhghWBPRM$ for graphic product...

    ATTN...WFO...EKA...HNX...MFR...MTR...REV...STO...

    ATTN...RFC...PTR...RSA...NWC...

    LAT...LON 41962247 41542157 40852066 39602031 37971979=20
    38042048 38322109 38922152 38772195 38162219=20
    37902249 38402334 39852421 41912439 41932330=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 21 18:24:44 2025
    AWUS01 KWNH 211824
    FFGMPD
    NVZ000-CAZ000-ORZ000-220620-

    Mesoscale Precipitation Discussion 1268
    NWS Weather Prediction Center College Park MD
    123 PM EST Sun Dec 21 2025

    Areas affected...central to northern CA

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

    Valid 211820Z - 220620Z

    Summary...A long-duration heavy rain event will continue through
    tonight. 12 hour rainfall totals of 2 to 4 inches for the Coastal
    Ranges and 3 to 7 inches for the Sierra Nevada are expected
    through 06Z (locally higher possible). Peak hourly rainfall of
    0.50 to 0.75 inches is likely with isolated values up to 1 inch,
    likely translating into flood/flash flood impacts across the
    region.

    Discussion...Moderate to heavy rain was occurring as of 18Z from
    roughly Point Arena, CA to southern OR with peak hourly rainfall
    between 0.5 and 0.75 inches, but with values locally up to 1 inch.
    An atmospheric river containing PW values between 1.0 and 1.4
    inches along the northern CA coast and southwesterly 850-700 mb
    winds of 40-50 kt were present. 24 hour gauge reports of 3-6
    inches (King Range) and 4-7 inches (north-central Sierra Nevada)
    were observed through 18Z and the northern CA region has
    experienced 200 to 400 percent of normal over the past week. There
    have been several reports of flooding and landslides over the past
    few hours within the northern Coastal Ranges and a couple of
    landslides reported within the Sierra Nevada.

    The approach of a positively tilted shortwave trough axis off of
    the Pacific Northwest coast will continue to advance ESE over the
    next 12 hours, allowing for a slow southward movement to the axis
    of highest moisture transport down the CA coastline. As this
    occurs, PWs are forecast to lower slightly and 850-700 mb winds
    should weaken about 10 kt through 06Z with IVT values of 800
    kg/m/s lowering into the 600-700 kg/m/s range. Steady peak hourly
    rainfall values of 0.50 to 0.75 inches are likely to continue over
    the next 6-12 hours. 12Z HREF probabilities showed 40 to 80
    percent probabilities of exceeding 0.5 in/hr through 02Z for the
    central to northern CA Coastal Ranges north of San Francisco and
    40 to 90+ percent for the north-central to northern Sierra Nevada
    through at least 06Z. Meanwhile, hourly probabilities for 1+
    inches in an hour are near or less than 10 percent through the
    overnight.

    Given wet antecedent conditions over the past week, including 24
    hour rainfall, the addition of another 2 to 6+ inches is likely to
    result in additional flooding, landslides/mudslides and debris
    flows. Where overlap of high rain rates occurs with sensitive burn
    scars or urban areas, more rapid flooding/flash flooding can be
    expected.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-N3fonV1wnIiFTFf7U_Ok7Dt2UfKXjgzF4Wstna-jHDUM2PoHkO-k6Iapux8XqvGKO4P= j7M3a0cP32dAi1_XlY33J7s$ for graphic product...

    ATTN...WFO...EKA...MFR...MTR...REV...STO...

    ATTN...RFC...PTR...RSA...NWC...

    LAT...LON 42022284 41832164 41492099 40542042 39901995=20
    38651967 38301964 38142001 38202058 38022121=20
    37712152 37302170 36992188 36762237 37242297=20
    37532336 38612413 40252494 41812489=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Dec 22 07:30:21 2025
    AWUS01 KWNH 220730
    FFGMPD
    CAZ000-221529-

    Mesoscale Precipitation Discussion 1269
    NWS Weather Prediction Center College Park MD
    229 AM EST Mon Dec 22 2025

    Areas affected...portions of central and eastern California

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

    Valid 220729Z - 221529Z

    Summary...Areas of moderate to heavy rainfall will continue for
    several more hours across upslope/western sides of the Sierra,
    prompting flood/flash flood concerns.

    Discussion...Recent radar/observational data depict continued
    areas of moderate to heavy rainfall along upslope sides of the
    Sierra in central/northeastern California. The rainfall continues
    as part of a landfalling atmospheric river across the region, with
    40 knots of 850mb flow oriented perpendicular to the Sierra
    promoting abundant orographic ascent. Additionally, 1-1.3 inch PW
    values are continuing to enhance rainfall rates across the region.
    Furthermore, the persistence of the atmospheric river has
    resulted in a focused area of 3-6 inch rainfall totals over the
    past 12 hours especially in the Tahoe and Lassen National Forests
    (east of an axis from Chico to Sacramento). Some instances of
    flooding/flash flooding and landslides have occurred, which isn't
    surprising given moderate MRMS Flash outputs and elevated
    streamflows per the USGS Water Dashboard.

    Ongoing trends should continue for several more hours. 850mb flow
    should remain perpendicular to the Sierra through at least 15Z/7a
    Pacific Time, prompting continued rainfall and runoff. Models
    suggest that flow should gradually slacken into the 20-25 knot
    range during that time frame, which should decrease orographic
    ascent and rain rates with time. Nevertheless, ground conditions
    continue to be sensitive and additional 0.25+ inch/hr rates are
    likely to continue. Flooding/flash flooding, debris flows, and
    landslides continue to be possible.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5iyvhhDbMLgpO0wdYJ0o3ApbhFqsnmdhB0ihXtI6v_mJfBQI739WZFXdnVdpfWrLxa66= -c7qLMepHMB4TgFXu1YM5yk$ for graphic product...

    ATTN...WFO...HNX...REV...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 40692210 40622126 39852056 38821992 37971968=20
    37641982 37902072 39222187 40052233=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Dec 24 08:52:47 2025
    AWUS01 KWNH 240852
    FFGMPD
    CAZ000-242049-

    Mesoscale Precipitation Discussion 1270
    NWS Weather Prediction Center College Park MD
    351 AM EST Wed Dec 24 2025

    Areas affected...portions of southern California

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

    Valid 240849Z - 242049Z

    Summary...Heavy rainfall was beginning to develop across western
    portions of the Transverse Ranges. The rain will expand in
    coverage through 20Z/noon Pacific Time. Widespread 3-5 inch
    totals are expected, with isolated 8-inch amounts possible. A
    dangerous scenario is unfolding, with widespread and significant
    impacts from flash flooding and debris flows expected.

    Discussion...The onset of a landfalling atmospheric river was
    beginning to increase rain rates across the western Transverse
    Ranges over the past hour or so (per radar mosaic/MRMS). The
    rainfall was associated with an axis of very strong
    south-southwesterly low-level flow (50+ knots at 850mb) beginning
    to make eastward progress into the discussion area. This flow was
    oriented perpendicularly to the Transverse Ranges, promoting
    strong orographic lift/ascent of an abundantly moist airmass (PW
    values from 1-1.5 inch per SPC Mesonanalyses). Weak surface-based
    instability was evident near immediate coastal areas as well. The
    regime was already beginning to spread 0.5-0.8 inch/hr rain rates
    into Santa Barbara County over the past hour.

    The overall pattern will shift only slowly eastward across the
    discussion area as a strong low pressure area west of Eureka, CA
    migrates northeastward/inland toward the Pacific Northwest. Heavy
    rainfall will increase in coverage and intensity through the next
    6-12 hours as well. A few areas of 1 inch/hr rain rates can be
    expected, and 3-5 inch totals (with local amounts reaching 8
    inches) can be expected across the Transverse Ranges through
    20Z/noon Pacific time. This rain will fall on sensitive terrain
    (i.e., burn scars, low-lying areas) creating a potentially
    dangerous scenario for widespread rapid runoff, flash flooding,
    debris flows, and rock/land slides. Significant impacts are
    expected in this regime.

    Other areas displaced from the Transverse Ranges could experience
    heavy rain as well (1-3 inch amounts). Flash flooding could occur
    - especially in urban areas and over burn scars.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5v6fNz6JRQ5fk-0hyZxoJYFxEGoCCYMVkWJrrpQsthUeto2mTJiSOx38Ww8po5CA8mfd= Gm2Qv9XSl3e2HhlGEHt32pQ$ for graphic product...

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

    ATTN...RFC...RSA...NWC...

    LAT...LON 37651974 37051892 36301813 35571804 35061803=20
    34731784 34541734 34251686 34061670 33921714=20
    33301749 33911887 34442054 35222101 35852150=20
    36312170 36322135 35922080 35371996 35431941=20
    36031933 36931957 37371990=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Dec 24 10:16:20 2025
    AWUS01 KWNH 241016
    FFGMPD
    CAZ000-241614-

    Mesoscale Precipitation Discussion 1271
    NWS Weather Prediction Center College Park MD
    515 AM EST Wed Dec 24 2025

    Areas affected...portions of northern and central California

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

    Valid 241014Z - 241614Z

    Summary...Areas of moderate to heavy rainfall will continue across
    the discussion area through around 16Z/8a Pacific Time.
    Flood/flash flood concerns could exist near sensitive ground
    conditions (urban areas, burn scars, and near flooded water sheds).

    Discussion...A strong area of low pressure was moving slowly
    northeastward toward northwestern California near Eureka this
    morning. Ahead of this low, strong low-level flow (50-70 knots at
    850mb) has developed across the discussion area that was advecting
    a very moist airmass (1-1.2 inch PW values) through much of the
    region. Additionally, weak surface-based buoyancy near coastal
    areas was noted per mesoanalyses. The result of this pattern has
    been several areas of moderate to heavy rainfall that has
    exhibited an uptick in intensity over the past 1-2 hours.=20
    Low-level flow against upslope areas has promoted localized
    0.2-0.4 inch/hr rain rates, and these rates are expected to
    continue (or perhaps increase into the 0.5 inch/hr range) through
    the overnight and early morning hours. Additionally, heavier
    convective development was noted just offshore of central coastal
    areas.

    These conditions are expected to continue through around 16Z or so
    as a front sweeps eastward across the discussion area. Ahead of
    this front, areas of 0.25-0.5 inch/hr rain rates should continue
    especially in terrain-favored areas. Additionally, deeper
    convective development approaching the central coastal ranges
    should eventually impact urban areas in/near San Francisco over
    the next 1-3 hours (through 13Z/5a Pacific) that could result in
    urban flash flooding. The ongoing threat of flooding and flash
    flooding should gradually end from west to east, but should also
    be most pronounced near 1) burn scars, 2) urban areas, and 3)
    watersheds that have already experienced heavier rainfall over the
    past week (upslope Sierra areas) that have wet soils and
    anomalously strong streamflows. Flash flooding is possible in
    this scenario.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!90s1Les1NlfJHKgB8Pm6TKIGfAJycEhNlKEi1VyWTlT_l0v2PlSAcKXbKz2Mfl29lBSY= abJ58tD_UjcTZnBlv5-zHDE$ for graphic product...

    ATTN...WFO...EKA...HNX...LOX...MFR...MTR...REV...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 41562233 41042137 40172081 38281986 37841933=20
    37111911 37472000 37942098 37052106 35942083=20
    35332100 36042177 37872288 40112426 40732426=20
    41032393=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Dec 24 15:17:54 2025
    AWUS01 KWNH 241517
    FFGMPD
    CAZ000-242215-

    Mesoscale Precipitation Discussion 1272
    NWS Weather Prediction Center College Park MD
    1015 AM EST Wed Dec 24 2025

    Areas affected...Central Valley into the Sierra Nevada Foothills

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

    Valid 241515Z - 242215Z

    SUMMARY...Significant atmospheric river activity continues to ride
    up through the Central Valley and into the Sierra Nevada foothills
    with heavy rainfall rates. Areas of flooding and some flash
    flooding will continue to be likely.

    DISCUSSION...The latest GOES-W IR satellite imagery shows an
    impressive fanning out of cold cloud tops across the Central
    Valley and into the Sierra Nevada as a full-latitude trough
    offshore of the West Coast continues to channel a strong deep
    layer atmospheric river inland across the region.

    A surface cold front has been making steady progress eastward this
    morning and has pushed east of the Bay Area and into the Central
    Valley. Radar imagery shows a well-defined and dynamically forced
    convective line just ahead of the cold front making its way closer
    to the Sierra Nevada foothills with rainfall rates that are on the
    order of 0.75" to 1"/hour. These rainfall rates are being
    facilitated by MUCAPE values of as much as 100 to 250 J/kg ahead
    of the cold front, but even more so by the very strong low-level
    moisture convergence riding up through the Central Valley and with
    impressively divergent flow aloft downstream of the offshore upper
    trough.

    Enhanced rainfall rates of up to 1"/hour will continue with these
    convective elements ahead of the cold front as it advances
    gradually eastward over the next several hours. The additional aid
    of orographic ascent into the Sierra Nevada foothills will further
    support the enhancement of rainfall rates. Given the strongly
    anomalous degree of moisture through the column including some
    tropical origins of the atmospheric river, the rainfall will be
    quite efficient, with additional totals through mid-afternoon of
    as much as 2 to 4 inches.

    Additional areas of flooding and some flash flooding will be
    likely, including portions of the Central Valley and into the
    Sierra Nevada foothills. Localized urban flooding impacts will
    continue to be a concern, and for areas in the terrain, localized
    burn scar flash flooding will be a threat. Can't rule out some
    landslide activity as well near areas of steep terrain.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!53-BwiZrl9T80oxjrbDTjD5St9EgADRAizby-f106X4xaimzSLI6Rng1qTi5hYs__yXH= NMi1oDBw2dNyDiht0mBs2c4$ for graphic product...

    ATTN...WFO...HNX...LOX...MTR...REV...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 40072068 39912039 39302013 38461984 37561932=20
    36731859 36231827 35571843 35281882 35281945=20
    35572006 35812034 36392080 37342095 39002111=20
    39862104=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wed Dec 24 19:51:24 2025
    AWUS01 KWNH 241951
    FFGMPD
    NVZ000-CAZ000-250600-

    Mesoscale Precipitation Discussion 1273
    NWS Weather Prediction Center College Park MD
    250 PM EST Wed Dec 24 2025

    Areas affected...Southern and Eastern CA

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

    Valid 241950Z - 250600Z

    SUMMARY...Heavy rainfall with dangerous and locally
    life-threatening flash flooding impacts will continue to impact
    portions of southern and eastern CA going into the evening hours
    as strong atmospheric river activity continues.

    DISCUSSION...GOES-W visible satellite imagery shows a significant
    atmospheric river bringing heavy rain across large areas of
    southern CA including the Los Angeles Basin, the adjacent high
    terrain of the Transverse Range, the southern Sierra Nevada and
    also adjacent interior desert valley locations. A deep
    full-latitude trough offshore of the West Coast continues to shift
    gradually eastward and is allowing for a cold front to advance
    inland through southern CA.

    This continues to help focus deep and very moist south-southwest
    flow up out of the eastern tropical-Pacific and across the region
    with enhanced IVT magnitudes of near 1000 kg/m/s aimed into
    portions of Los Angeles, Orange and San Bernadino Counties. This
    also includes the southwest facing slopes of the San Gabriel and
    San Bernadino Mountains where enhanced orographic ascent coupled
    with deep layer forcing and frontal convergence is yielding high
    rainfall rates of locally over 1"/hour.

    Over the next several hours, the cold front will continue to
    settle south and east, which will allow for heavy rain to arrive
    over the Peninsular Range of southern CA while also overspreading
    interior areas of eastern CA including some of the desert
    locations adjacent to the high terrain of the southern Sierra
    Nevada.

    The greatest short-term rainfall impacts and flash flooding
    concerns will likely be over Kern, Ventura, Los Angeles, Orange,
    and San Bernadino Counties, with eventually areas of Riverside and
    San Diego Counties getting into heavy rainfall later this
    afternoon and evening. Some of the rates for the aforementioned
    southwest facing slopes of the high terrain will continue to be
    locally near or over 1"/hour which is supported by the
    experimental WoFS guidance which has a particular focus over the
    next 6 hours across eastern parts of Los Angeles County, southwest
    parts of San Bernadino County, and also Orange County.

    Additional rainfall totals of 3 to 5+ inches going through late
    this evening will be possible for the orographically favored high
    terrain of southern CA, with as much as 1 to 3 inches elsewhere
    including portions of eastern CA near the southern Sierra Nevada.
    Some interior valley locations away from the terrain may even see
    as much as 1 inch of rain.

    Dangerous and locally life-threatening flash flooding is expected
    going into the evening hours across southern CA which include
    concerns for not only urban flash flooding, but also mud and
    landslide activity, and debris flows near and adjacent to the more
    sensitive burn scar locations. Areas of flash flooding will also
    be a concern for eastern CA where heavy rains here also contribute
    to enhanced runoff. This will include some open dry wash areas.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7iaagVot710bq-Swn8BA3WE_eOkheyqa6GwSFP3zaElDXOGKFOhl3OT5u2VyvOUtC3bb= n5cnUe0YP-mJZyyxD3M1o1M$ for graphic product...

    ATTN...WFO...HNX...LOX...PSR...SGX...VEF...

    ATTN...RFC...RSA...NWC...

    LAT...LON 37091767 36531652 35781566 35011537 34351558=20
    33801566 33051589 32591620 32511726 33451806=20
    33651851 34151951 34821971 35921915 36921862=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 Dec 25 08:04:13 2025
    AWUS01 KWNH 250803
    FFGMPD
    CAZ000-251800-

    Mesoscale Precipitation Discussion 1274
    NWS Weather Prediction Center College Park MD
    302 AM EST Thu Dec 25 2025

    Areas affected...portions of northern, central and southern CA

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

    Valid 250759Z - 251800Z

    SUMMARY...Another round of heavy rain will approach central and
    southern CA tonight into Christmas morning. Peak hourly rainfall
    of 0.5 to 1.0 inches is expected, with isolated hourly totals over
    1 inch. Due to recent heavy rainfall and areas of ongoing
    flooding, renewed areas of flood/flash flooding are likely from an
    additional 1 to 3 inches of rainfall (locally higher) through ~18Z.

    DISCUSSION...GOES West water vapor/infrared satellite imagery from
    07Z showed a mid-level vorticity max near 39N 127W with a
    southward extending trough axis, advancing toward the northeast. A
    surface low was associated with the vorticity max containing an
    attached occluded/cold front extending to the south. Infrared
    imagery and lightning data showed a line of showers/thunderstorms
    just ahead of the front, advancing closer to the central CA coast.
    This feature was located ahead of a broader closed low aloft, with
    steepening lapse rates in the 850-500 mb layer edging eastward
    central to northern CA.

    While the primary moisture axis from Wednesday has moved into the
    lower CO River Valley, layered PW imagery from OSPO showed a
    secondary moisture axis just ahead of the offshore cold front with
    blended TPW values of 0.8 to 0.9 inches. Instability along the
    coast and within the Sacramento/San Joaquin Valley was less than
    500 J/kg and should stay that way over the next 6-12 hours with
    some fluctuations up/down over time via recent RAP forecasts. RAP
    guidance also showed 850-700 mb winds from the south to
    south-southwest increasing into the 60-65 kt range from near San
    Francisco Bay to the northern Sacramento Valley ahead of the front
    which will likely be accompanied by a band of
    showers/thunderstorms sweeping inland containing peak hourly
    rainfall of 0.5 to 1.0 inches. The band will impact central to
    northern coastal locations first, followed by inland locations
    across the Sacramental Valley into the Sierra Nevada foothills.
    The band of heavy rain will also begin to advance southward down
    the Santa Lucia Range into the western Transverse Ranges between
    12Z and 18Z. Post-frontal low level axes of convergence could
    support additional narrow bands of showers/thunderstorms with
    brief training across central to northern CA locations with peak
    hourly rainfall near 0.5 inches.

    Through ~18Z, peak additional rainfall of 1 to 3 inches is
    expected (locally higher) for the Coastal Ranges into the Sierra
    Nevada foothills (below snow levels of ~5000 ft). This additional
    rainfall, coupled with brief high rates, should allow for areas of
    renewed flooding/flash flooding across urban/terrain and low-lying
    locations through 18Z. Due to saturated soils, the potential for landslides/debris flows will exist, including any sensitive burn
    scar locations.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Fy7N2vCbkgdsoukSqdAcxFlbzgguN4-zro9adZVuZDI_-2AgrwuRP_VHaaYvYkSzowB= F8uDF9qksst-8nX1MlQ43cs$ for graphic product...

    ATTN...WFO...EKA...HNX...LOX...MFR...MTR...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 41222225 40912174 40102152 39872122 39182064=20
    38632033 37621963 36411861 36311931 36131974=20
    35721981 35191938 34581808 34011806 33771847=20
    33841954 34132068 34802148 35772178 37082281=20
    38992416 40242462 40682433 40842312=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Dec 25 18:13:09 2025
    AWUS01 KWNH 251813
    FFGMPD
    CAZ000-260600-

    Mesoscale Precipitation Discussion 1275
    NWS Weather Prediction Center College Park MD
    110 PM EST Thu Dec 25 2025

    Areas affected...Portions of Central and Southern CA

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

    Valid 251810Z - 260600Z

    SUMMARY...Additional atmospheric river surge to impact central and
    southern CA going into the evening hours. Locally heavy rainfall
    rates coupled with extremely sensitive conditions on the ground
    from previous rainfall will promote additional areas of flash
    flooding with locally dangerous and life-threatening impacts
    possible.

    DISCUSSION...GOES-W visible satellite imagery shows a secondary
    cold front and associated atmospheric river surge advancing down
    across areas of central and southern CA with a particular focus on
    the Transverse Range and nearby areas of the Los Angeles Basin.
    While this surge of moisture is certainly more modest compared to
    yesterday, the additional rainfall associated with this will be
    falling on areas that have seen as much as 6 to 12+ inches of rain
    over the last 36 hours, and especially in the San Gabriel and San
    Bernadino Mountains.

    The latest CW3E IVT analyses suggest as much as 500 kg/m/s of IVT
    will be moving through the Transverse Range and Los Angeles Basin
    region going through this afternoon and into at least the early
    part of this evening. Lesser magnitudes will continue to impact
    areas farther north extending into the southern Sierra Nevada.
    There is some meaningful instability with MUCAPE values near 500
    J/kg situated along the offshore portion of the front, and the
    latest GOES-W and CMORPH2 microwave-driven data does show some
    convective showers with heavier rainfall rates offshore. These
    showers are likely to move inland over the next several hours, and
    the orthogonal orientation of the low to mid-level flow in general
    relative to the terrain should further support locally enhanced
    rainfall rates.

    A look at the 12Z HREF guidance and experimental guidance
    including the latest NSSL/MPAS and WoFS solutions suggests a slow
    southeast advance of shower activity down into the Los Angeles
    Basin along with the adjacent terrain. Some rainfall rates going
    through early this evening are likely to exceed a 0.50"/hour with
    some spotty, but stronger convective showers near the terrain
    potentially fostering rates as high as 1"/hour. Additional
    rainfall totals going through early this evening may reach as high
    as 2 to 4 inches over the higher terrain, with 1 to 2 inches in
    the lower elevations.

    Given the new rounds of heavy rainfall, and extremely sensitive
    antecedent conditions, additional areas of flash flooding are
    likely with potential for dangerous and life-threatening impacts.
    This will include localized urban flash flooding concerns, a
    threat for new mud and rockslide activity, and also debris flows
    near and adjacent to any burn scar areas.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9tCd1fNUm3drPEqqNgsb-dyEzZuFTsPMoi3SvR4sV8id1rDF_qoI-bDx33w-rZvHuMCg= pTnQ6c56bFOr857iq0_-lF0$ for graphic product...

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

    ATTN...RFC...RSA...NWC...

    LAT...LON 37191917 36801870 36261839 35631845 35031837=20
    34701782 34331738 33891750 33751824 33851892=20
    34211976 34382045 34732060 35202058 35902039=20
    36871969=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Dec 25 21:08:07 2025
    AWUS01 KWNH 252108
    FFGMPD
    CAZ000-260900-

    Mesoscale Precipitation Discussion 1276
    NWS Weather Prediction Center College Park MD
    405 PM EST Thu Dec 25 2025

    Areas affected...Portions of Central and Northern CA

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

    Valid 252105Z - 260900Z

    SUMMARY...New rounds of heavy showers and thunderstorms are
    expected this afternoon through this evening for areas of central
    and northern CA, including the Bay Area. Given the saturated soil
    conditions and high streamflows, additional areas of flooding and
    flash flooding are likely.

    DISCUSSION...The latest GOES-W IR/WV suite shows a deep upper
    trough and associated closed low offshore of the West Coast.
    Shortwave impulses continue to round the base of the trough and
    take aim on central and northern CA, with each impulse effectively
    driving renewed atmospheric river activity into the state.

    Solar insolation has facilitated sufficient levels of boundary
    layer heating across the northern portions of the Central Valley
    to result in SBCAPE values as high as 500 to 750 J/kg. This
    heating coupled with relatively divergent flow aloft downstream of
    the deep offshore upper trough/closed 500 mb low center will
    facilitate an increase in convective showers in the near-term
    across sizable areas of the Central Valley. Some locally organized line-segments will be possible given the elevated bulk shear
    parameters (30 to 50 kts), and this actually may become aligned
    with the deep layer flow for some periodic instances of
    cell-training.

    However, of greater significance will be the approach of a
    well-organized shortwave impulse rounding the base of the upper
    trough heading into the early evening hours. This shortwave energy
    which is well-depicted by the axis of cold convective cloud tops
    in IR satellite imagery along 125W to 130W will be ejecting
    northeast toward the northern CA coastal ranges in the 00Z to 03Z
    time frame, including the Bay Area. Thereafter, this new surge of
    energy and related Pacific-moisture transport should eject into
    the Central Valley and Sierra Nevada foothills. The coastal ranges
    and Sacramento Valley in particular will see the greatest IVT
    magnitudes. The 12Z GFS/ECMWF solutions suggest IVT values
    reaching into the 500 to 600 kg/m/s range with the aid of stronger
    low to mid-level southwest flow.

    The combination of this along with large-scale forcing/shear and
    at least modest boundary layer instability should set the stage
    for more organized bands of convection to approach the coastal
    ranges and then advance inland going into the evening hours. Heavy
    rainfall rates of 0.50" to 1"+/hour will be likely with these new
    rounds of heavy shower and thunderstorm activity.

    Additional rainfall totals by late this evening of 2 to 3 inches
    will be possible locally for the coastal ranges and especially the
    upslope areas of the northern Sierra Nevada foothills. Lesser
    totals of as much as 1 to 2 inches cannot ruled out in at least
    parts of the Sacramento Valley. By late this evening, this latest
    surge of energy and moisture should settle farther south into
    coastal ranges south of the Bay Area and adjacent areas of the
    Central Valley.

    Given the saturated soil conditions and high streamflows, these
    additional rains are likely to result in more areas of areal
    flooding and flash flooding, which will include urban flooding
    impacts (San Francisco, Sacramento, Chico and Redding all at risk)
    along with localized mud and landslide activity near areas of
    higher terrain.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-ottk6EO9X3DhmXLkaq_LhrYqExDpVA8k2z7-Xyqo_Zc6oWbZCMKZU6FtSSO45tk8kVr= vCEtkGhTo7CKh2iK1cj_1jE$ for graphic product...

    ATTN...WFO...EKA...HNX...LOX...MFR...MTR...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 41192196 40352163 39952136 39572073 39012031=20
    38592000 37901945 37291920 36791979 35902040=20
    35112065 35182118 35912190 37202260 37972308=20
    39012405 39682433 40372428 40802375 40872295=20
    41122238=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Dec 26 06:14:43 2025
    AWUS01 KWNH 260614
    FFGMPD
    CAZ000-261000-

    Mesoscale Precipitation Discussion 1277
    NWS Weather Prediction Center College Park MD
    113 AM EST Fri Dec 26 2025

    Areas affected...western Transverse Ranges / southern CA

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

    Valid 260612Z - 261000Z

    SUMMARY...Localized flash flooding is likely to continue across
    the western Transverse Ranges through 10Z (2 AM PST). Peak hourly
    rainfall of 0.5 to 1.0 inches and additional rainfall over the
    next 4 hours of 1 to 2 inches is expected, mainly from eastern
    Santa Barbara into Ventura counties.

    DISCUSSION...MRMS reflectivity and local gauge reports showed
    moderate to heavy rain continued to track across the Channel
    Islands into the western Transverse Ranges. Hourly rainfall has
    varied between 0.5 and 1.0 inches since 00Z and 3-hr totals ranged
    from roughly 0.75 to 1.5 inches ending 06Z, mainly within central
    Ventura County. This region of the western Transverse Ranges has
    been situated within a relative max in precipitable water values
    between 1.0 and 1.2 inches with a localized max observed on OSPO
    Layered PW imagery from the surface to ~500 mb pointed into the
    western Transverse Ranges. 850-700 mb layer winds were from the S
    to SSW at 25-40 kt with little change over the past few hours. The
    00Z VBG sounding and more recent aircraft-derived soundings showed
    instability was weak (MLCAPE less than or equal to 250 J/kg) and
    shallow, limiting lightning potential.

    Nearly stationary to perhaps slow eastward translation is forecast
    for the moisture axis through 10Z, out ahead of a larger scale
    mid/upper level trough axis over the eastern Pacific. Therefore,
    similar ingredients should remain in place for the region with
    850-700 mb winds between 25-40 kt supporting IVT values between
    300-500 kg/m/s. Weak/shallow instability combined with orographic
    ascent into the terrain will continue to favor peak hourly
    rainfall of 0.5 to 1.0 inches. Additional rainfall through 10Z of
    1-2 inches is expected (mainly within eastern Santa Barbara into
    Ventura County) which is likely to maintain localized flash
    flooding due to saturated soils and the majority of additional
    rainfall becoming runoff.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7xdk377ew3-HfJXl6wWFOeZ5TCj1i389a59mUWjUuYeZNMCESE3gRtvArR_MIkdiH-sG= PqIOgdVI09d7-rdd3wKjnfM$ for graphic product...

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

    ATTN...RFC...RSA...NWC...

    LAT...LON 35222013 34881960 34961930 34941907 34771869=20
    34691858 34181855 33921903 34241965 34402042=20
    34842055=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Dec 26 08:59:15 2025
    AWUS01 KWNH 260859
    FFGMPD
    CAZ000-261800-

    Mesoscale Precipitation Discussion 1278
    NWS Weather Prediction Center College Park MD
    358 AM EST Fri Dec 26 2025

    Areas affected...eastern Sacramento and San Joaquin Valleys into
    Sierra Nevada Foothills

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

    Valid 260856Z - 261800Z

    SUMMARY...A localized concern for additional flooding/flash
    flooding will exist across portions of the Sacramento and San
    Joaquin Valleys into the Sierra Nevada foothills through roughly
    18Z. Peak hourly rainfall of 0.25 to 0.5 inches will be possible,
    along with isolated hourly rainfall in excess of 0.5 inches.

    DISCUSSION...Area radar imagery from 0845Z showed scattered
    showers extending from the southern Sacramento Valley into the
    northern San Joaquin Valley and eastward into the Sierra Nevada.
    RAP analysis data and GPS-derived PWs ranged from 0.5 to 0.9
    inches and 850-700 mb winds were 30-50 kt from the southwest. Low
    level convergence has helped to focus a couple of SW to NE
    oriented axes of showers with brief training and hourly rainfall
    locally in excess of 0.5 inches per MRMS data. However,
    surrounding gauge data and a vast majority of the region contained
    peak hourly rainfall in the 0.25 to 0.50 inch range.

    As a longwave upper level trough axis over the eastern Pacific
    continues to translate eastward over the next 12 hours, total PW
    values and 850-700 mb wind speeds are forecast to gradually lower
    through 18Z which should have the effect of reducing higher hourly
    rainfall potential. Snow levels varied from 5000 ft (northern
    locations) to 8000 ft (southern locations) across the Sierra
    Nevada and lowering of these values will occur as the upper trough
    and colder air moves inland today. Until then however, localized
    potential will remain for brief areas of heavy rain with an
    additional 1-2 inches expected for some locations through 18Z. Due
    to largely saturated soils in many locations from recent heavy
    rainfall, additional heavy rainfall may lead to isolated
    flood/flash flooding including the possibility of
    landslides/mudslides.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!45fiue6QPyLVEwXtDh44fVO0rFR_8ROvcippO1XrAHZq_0Qqenz0GymvvfOdP477gfGz= 6QOztOkgmfg_Ye0ShoHvXw8$ for graphic product...

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

    ATTN...RFC...RSA...NWC...

    LAT...LON 39552097 39132068 38832050 38532036 38082008=20
    37741980 37371944 36931893 36101864 35491856=20
    35401886 35721919 36281965 37002024 37722093=20
    38682127 39302143=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Dec 26 09:37:47 2025
    AWUS01 KWNH 260937
    FFGMPD
    CAZ000-261900-

    Mesoscale Precipitation Discussion 1279
    NWS Weather Prediction Center College Park MD
    437 AM EST Fri Dec 26 2025

    Areas affected...northern CA coast

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

    Valid 260935Z - 261900Z

    SUMMARY...Isolated pockets of showers containing hourly rainfall
    in the 0.25 to 0.5 inch range will continue a limited threat for
    flooding/flash flooding across portions of the northern CA coast
    through about 19Z.

    DISCUSSION...0930Z water vapor imagery from GOES West showed a
    mid-level low/vorticity max ~150 miles west of Cape Mendocino,
    slowly advancing easGPS PWstward toward the northern CA coast.
    GPS-derived PW values along the northern CA coast were 0.4 to 0.6
    inches with 850-700 mb mean layer winds peaking near 40 kt from
    the southwest. Increasing ascent ahead of the approaching low to
    mid-level low and a subtle increase in IVT values (up to ~350
    kg/m/s) are expected to bring yet another round of locally heavy
    rain to the region through the remainder of the night into the
    late morning.

    Peak hourly rainfall of 0.25 to 0.50 inches will be possible as
    the low approaches where weak and shallow MLCAPE up to ~500 J/kg
    will be present per recent RAP forecasts. While these rates are
    not typically a problem for the climatologically wet northern CA
    coast, 7-day rainfall values are well above average and saturated
    to nearly saturated soils could be sensitive to additional
    rainfall. There will be potential for an additional inch or so of
    rain through 19Z which may result in isolated landslides/mudslides
    and/or urban flooding through the rest of the morning hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Vw0XqGFU03csV-wfMBmpT0d0WXdFw0HrhGqWokZzyE-GZOTnBx0SSfHr-uFvB6MrfzX= sbgMD0ba3LMH2B4sF7Hvwd4$ for graphic product...

    ATTN...WFO...EKA...MTR...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 41252417 41232369 40852368 40352349 40052341=20
    39722325 39282297 38762261 38562324 38892388=20
    39392423 40222470 40722458 41112433=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Dec 26 09:43:49 2025
    AWUS01 KWNH 260943
    FFGMPD
    CAZ000-261900-

    Mesoscale Precipitation Discussion 1279...Corrected
    NWS Weather Prediction Center College Park MD
    443 AM EST Fri Dec 26 2025

    Corrected for typo and addition within first paragraph

    Areas affected...northern CA coast

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

    Valid 260935Z - 261900Z

    SUMMARY...Isolated pockets of showers containing hourly rainfall
    in the 0.25 to 0.5 inch range will continue a limited threat for
    flooding/flash flooding across portions of the northern CA coast
    through about 19Z.

    DISCUSSION...0930Z water vapor imagery from GOES West showed a
    mid-level low/vorticity max ~150 miles west of Cape Mendocino,
    slowly advancing eastward toward the northern CA coast.
    GPS-derived PW values along the northern CA coast were 0.4 to 0.6
    inches with 850-700 mb mean layer winds peaking near 40 kt from
    the southwest. While the corresponding surface low (992 mb) is
    expected to weaken over the next 6-12 hours, increasing ascent
    ahead of the approaching low to mid-level low and a subtle
    increase in IVT values (up to ~350 kg/m/s) are expected to bring
    yet another round of locally heavy rain to the region through the
    remainder of the night into the late morning.

    Peak hourly rainfall of 0.25 to 0.50 inches will be possible as
    the low approaches where weak and shallow MLCAPE up to ~500 J/kg
    will be present per recent RAP forecasts. While these rates are
    not typically a problem for the climatologically wet northern CA
    coast, 7-day rainfall values are well above average and saturated
    to nearly saturated soils could be sensitive to additional
    rainfall. There will be potential for an additional inch or so of
    rain through 19Z which may result in isolated landslides/mudslides
    and/or urban flooding through the rest of the morning hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7cUis92kCnAv1SYIX1BnkZfC8PO2z0muo6pS5fcSJJR-u8sv3L0rZAz7Zy5cTv2v7Azu= HfhxekhLcAPq-eldFmJi8x8$ for graphic product...

    ATTN...WFO...EKA...MTR...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 41252417 41232369 40852368 40352349 40052341=20
    39722325 39282297 38762261 38562324 38892388=20
    39392423 40222470 40722458 41112433=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Dec 26 10:35:47 2025
    AWUS01 KWNH 261035
    FFGMPD
    CAZ000-262000-

    Mesoscale Precipitation Discussion 1280
    NWS Weather Prediction Center College Park MD
    535 AM EST Fri Dec 26 2025

    Areas affected...Transverse Ranges to southern CA coast

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

    Valid 261034Z - 262000Z

    SUMMARY...Areas of flash flooding will continue to affect portions
    of the Transverse Ranges to the coast overnight into the late
    morning hours. Hourly rainfall values of 0.5 to 1.0 inches
    (locally higher) are likely which will maintain concerns for
    impacts including landslides/debris flows and urban flooding.

    DISCUSSION...1015Z radar imagery combined with local mesonet and
    personal weather observations out of southern CA continued to show
    areas of heavy rain within a narrow axis from the offshore waters
    into mainly Ventura County. Hourly rainfall over 1 inch has been
    observed in Ventura County with 3-hour totals of 1 to 2+ inches.
    Local Wunderground gauges showed a couple of 30 minute rainfall
    values over 0.5 inches within the past 2-3 hours near Ojai. These
    rains were associated with a slow moving low level convergence
    axis (remnant frontal boundary) that was oriented SSW to NNE
    across Ventura County with PW values of 1.0 to 1.2 inches along
    the coast and SSW 850-700 mb winds of 25-35 kt. Enhanced
    divergence aloft may also be contributing to increased rainfall
    intensity over the region, within the right-entrance region of a
    150 kt jet streak aloft located over the Sierra Nevada.

    Short term forecasts from the RAP show the low level convergence
    axis and localized max in IVT values (up to 500 kg/m/s) slowly
    advancing eastward over the next 6-9 hours. The result will be
    localized high rain rates into the terrain, slowly shifting east,
    given the favorable orthogonal orientation of the low level winds
    to the axis of terrain. Hourly rainfall of 0.5 to 1.0+ inches
    should advance eastward from Ventura County into Los Angeles
    County through 15Z, possibly clearing Los Angeles County after
    roughly 17Z. While the greatest potential for these higher rates
    will be in the upslope favored terrain, shallow/weak instability
    up to ~250 J/kg and short term training could support 0.5+ inch
    hourly rainfall into the lower elevation urban areas as well.
    Additional rainfall of 1 to 3 inches will be possible through 20Z
    with potential for higher impact localized flash flooding over
    sensitive burn scar locations in and around the Los Angeles metro.
    Given heavy rain over the past 2 days, many locations contain
    saturated soils with additional rainfall likely translating
    directly into runoff. With this rainfall, there will be the
    potential for dangerous travel and life-threatening impacts from
    flooding.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-LZMtVUrN3iB_BZn50erNlgWuVFx2Gz-S7kpwOFNwFuPHWglkqMScRyfzLUyJeQPHOuE= N6Uq6vXg3BsEMf321O9Vt3M$ for graphic product...

    ATTN...WFO...HNX...LOX...SGX...

    ATTN...RFC...RSA...NWC...

    LAT...LON 34811863 34471778 34201694 33671672 33361764=20
    33471824 33761916 34071955 34451952 34761922=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 28 10:03:15 2025
    AWUS01 KWNH 281003
    FFGMPD
    MIZ000-INZ000-ILZ000-MOZ000-IAZ000-281600-

    Mesoscale Precipitation Discussion 1281
    NWS Weather Prediction Center College Park MD
    502 AM EST Sun Dec 28 2025

    Areas affected...northern MO/southeastern IA/north-central
    IL/northwestern IN

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

    Valid 281000Z - 281600Z

    SUMMARY...Isolated flash flooding will be possible from portions
    of northern MO, southeastern IA into north-central IL and
    northwestern IN through 16Z (10 AM CST). Rainfall of 1 to 2 inches
    in an hour will be possible with isolated 3 to 6 hour totals of
    2-3 inches.

    DISCUSSION...0945Z radar imagery Midwest showed scattered showers
    and embedded thunderstorms from northern MO, southern IA and
    central IL, located north of a quasi-stationary front that
    extended eastward from a 998 mb low just west of Salina, KS. SW to
    WSW 850 mb winds of 30-50 kt were in place to the east of the
    surface low with overrunning occurring atop the frontal boundary.
    OSPO ALPW imagery showed low level moisture rapidly advecting
    northward into the central U.S. beneath a plume of mid to upper
    level moisture with origins in the tropical eastern Pacific. Total
    PW values were estimated to be between 1.1 and 1.4 inches (SPC
    mesoanalysis) from eastern KS into western IN, which equate to +4
    to +5 standardized anomalies. The low level moisture return was
    allowing for the northward advection of instability and erosion of
    low level CINH amid 700-500 mb lapse rates of 7.0 to 7.5 C/km,
    supporting MUCAPE of 500-1500 J/kg from eastern KS into
    western/central MO via 09Z SPC mesoanalysis data. This change in
    the thermodynamic environment has been reflected in recent
    infrared satellite imagery showing bursts of colder cloud tops
    over northern MO and far southern IA.

    As the surface low over central KS moves eastward early this
    morning, strengthening low level flow will translate into MO and
    IL with 850 mb speeds locally exceeding 50 kt. Convergence at the
    nose of 925-850 mb moisture transport will align WSW to ENE or
    parallel to the mean steering flow. This will set up narrow axes
    of heavy rainfall with training and potential for hourly rainfall
    between 1 and 2 inches. The best overlap of low level convergence
    with moisture/instability will be from northern MO into
    north-central IL and northwestern IN through 16Z. Isolated
    flash/urban flooding may result from 2-3 inches of rain in 2-3
    hours. However, a lack of precipitation for this region of the
    U.S. over the past couple of weeks (lower than average soil
    moisture) and warmer than average temperatures (no/negligible
    frost depth) should limit runoff. Therefore, any flash flood
    concerns will likely be minor and remain limited to urban or
    sensitive low lying areas.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_YG17WL1A4Ubdi67KFfO43e18ICjEG2HKhTFDp5vHXyUA4EeS62zo9t6AgrSOJoLIuD2= e1GJtSo6yTGe-RHU4VJf4oo$ for graphic product...

    ATTN...WFO...DMX...DVN...EAX...ILX...IND...IWX...LOT...LSX...

    ATTN...RFC...KRF...MSR...TIR...NWC...

    LAT...LON 42178726 41658634 40918612 40448688 40038825=20
    39629015 39199219 39289312 39699398 40409379=20
    41329161 42118904=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jan 1 09:58:17 2026
    AWUS01 KWNH 010958
    FFGMPD
    CAZ000-011800-

    Mesoscale Precipitation Discussion 0001
    NWS Weather Prediction Center College Park MD
    457 AM EST Thu Jan 01 2026

    Areas affected...Southern CA

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

    Valid 011000Z - 011800Z

    SUMMARY...Flash flooding is possible from the Coastal Range to the
    Transverse Ranges where soils remain sensitive and saturated.
    Localized urban flash flooding around the greater Los Angeles
    metro area is also possible this morning.

    DISCUSSION...GOES-19 satellite imagery shows a compact 500mb low
    embedded within an increasingly negative 200-500mb mean trough
    located west of CA. This upper trough is working in concert with a
    700mb ridge near Cabo San Lucas to direct a highly anomalous plume
    of moisture into not only CA but much of the western U.S.. PWATs
    along the CA coast this morning are topping 1.25" and are above
    the 99th climatological percentile. IVT is also topping 500 kg/m/s
    and winds are out of the SW, which is supportive of some upslope
    enhancement along orthogonally-oriented terrain from the Coastal
    Range on south and east through the Transverse Ranges. As the
    triple point of an occluded low approaches, so will the nose of a
    500mb jet streak and low-level winds will strengthen off the
    coast. Steepening mid-level lapse rates are expected as the
    upper-low approaches and 00Z HREF guidance does show as much as
    250 J/kg of MUCAPE potentially available as far north as Big Sur
    this morning as a result.

    06Z HREF guidance shows high chance probabilities (>70%) for 6-hr
    rainfall totals >2" between 12-18Z along the San Bernadino
    Mountains and low-to-moderate chances (30-50%) along the San
    Gabriel. These are the mountain ranges most susceptible to
    potential flash flooding in wake of last week's significant flood
    event and lingering burn scars. As the the dry slot quickly moves
    in by 18Z, the core of the heaviest rainfall should move north and
    east with only lingering upslope flow keeping periods of rain
    around the Transverse and Peninsular Ranges. Given the low FFG's
    and sensitive soils in the higher terrain, as well as locally
    heavy rainfall rates around the highly urbanized Los Angeles metro
    area, flash flooding is possible this New Year's Day morning. Note
    that rock slides and debris flows are also possible in the
    Transverse Ranges where soils and burn scars are highly sensitive.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-pdJyxrIMrPLOD6igfuFQaU8Rv3UjlFuGAZequATOa06undIguDAQQi2SQYpTIG3hqbn= eJxporhP2q85F16qxrDgius$ for graphic product...

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

    ATTN...RFC...RSA...NWC...

    LAT...LON 36632190 36542164 36222137 35922107 35642076=20
    35252039 35022004 34881962 34851903 34941860=20
    34781831 34491824 34481790 34491738 34371706=20
    34221696 34061748 33891770 33651837 33821908=20
    34241954 34332017 34392067 35062099 35792164=20
    36092200 36412207=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jan 1 15:21:51 2026
    AWUS01 KWNH 011521
    FFGMPD
    CAZ000-012120-

    Mesoscale Precipitation Discussion 0002
    NWS Weather Prediction Center College Park MD
    1020 AM EST Thu Jan 01 2026

    Areas affected...portions of southern California

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

    Valid 011520Z - 012120Z

    Summary...Deep convection along and ahead of a surface cold front
    located about 85 miles west of San Diego will continue to foster a
    flash flood risk across the discussion area through 21Z/1p Pacific
    Time.

    Discussion...Areas of deep convection persist especially in/near terrain-favored upslope regions of the discussion area currently.=20
    The convection was being supported by mid-level cooling (which has
    fostered a pool of ~250 J/kg SBCAPE over Pacific and near-coastal
    regions of the discussion area), orographic ascent (sponsored by
    25-30 knot 850mb flow against Transverse and Peninsular coastal
    ranges), and 1-1.3 inch PW values - supporting efficient rainfall
    processes in/near convective activity. Recent MRMS/observational
    data depicts an uptick of rain rates in both Los Angeles Metro
    (into the 0.4 inch/hr range) and across San Diego County (where
    0.5-0.8 inch/hr rates were estimated). These rain rates were
    occuring over urban areas and near sensitive terrain from prior
    flash flood impacts, burn scars, and terrain. Flash flooding
    remains possible in these areas in the short term.

    Models/observations suggest that the aforementioned Pacific cold
    front will traverse the region from west to east and bring a
    substantial decrease in flood/flash flood potential over time.=20
    For the Los Angeles area and Transverse Ranges, this risk will
    likely extend into the 18-20Z timeframe before decreasing some.=20
    The front will take a bit longer to cross San Diego and adjacent
    Peninsular Ranges (around 21Z or so). Flash flooding will remain
    possible through the aforementioned timeframes.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6E_IiCTFWyRPvFYk288JNEQ4usNjEugJcYFb_BEOQMvQUtQtZ-envxiDu0hzGaAhh2h-= leCiEekM3pcilfnc8-zSexU$ for graphic product...

    ATTN...WFO...HNX...LOX...PSR...SGX...VEF...

    ATTN...RFC...RSA...NWC...

    LAT...LON 35241857 35091802 34771717 34251662 33621619=20
    32831597 32531613 32461695 32551746 33081815=20
    33981872 34691879=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jan 3 09:01:14 2026
    AWUS01 KWNH 030901
    FFGMPD
    CAZ000-031800-

    Mesoscale Precipitation Discussion 0003
    NWS Weather Prediction Center College Park MD
    400 AM EST Sat Jan 03 2026

    Areas affected...The Western Transverse Ranges of Southern
    California

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

    Valid 030900Z - 031800Z

    SUMMARY...Flash flooding is likely across the Western Transverse
    Ranges this morning as rainfall rates to 1 inch/hour lead to flash
    flooding and landslides, especially around burn scars.

    DISCUSSION...A highly dynamic weather pattern has set up across
    portions of California. A deep upper level low and associated
    upper level shortwave are approaching the West Coast. The
    shortwave is tapping into a moisture plume set up off the coast of
    Mexico and advecting some deeper tropical moisture towards the
    coast. PWATs will be increasing to over 1 inch, which is 2.5 sigma
    above normal for this time of year. Thus, as a series of surface
    fronts (not shown) approach, the addition of upper level energy
    from the shortwave and abnormal moisture will allow for rainfall
    rates to increase to up to 1 inch per hour into the western
    Transverse Ranges this morning.

    850 mb southerly flow of 20-30 kts will support increasing upslope
    enhancement of the rainfall, which will support the heavier
    rainfall locally from Lompoc east through Oxnard, including Santa
    Barbara. NASA Sport imagery shows soils are above the 90th
    percentile compared to climatology across the area. Thus, a brief
    period of heavier rain rates, expected later this morning, should
    be all that is needed to fully saturate the soils. Additional
    rainfall from there will quickly convert to runoff. This runoff
    will fill small streams and creeks, as well as increase the
    potential for landslides. Downstream flash flooding, particularly
    below the numerous burn scars in the area, is likely through this
    morning. The area of heavy rainfall, while progressive, will still
    be slow to track eastward down the coast. Any one area should see
    anywhere from 3 to 6 hours of rain, heavy at times, before the
    plume moves off to the east.

    The latest CAMs guidance suggests that by the time the area of
    heavy rain arrives into the heart of the Los Angeles basin this
    afternoon, it should both be weakening and narrowing. Thus, while
    Los Angeles is expected to pick up some rain later this afternoon,
    rainfall rates are not expected to be quite as heavy, so impacts
    should be somewhat limited.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-sz0p95xYO4NyQz7eawzmC7FC3Xcj-GxL5rzwc8o3o2CAHu5PvVWlLlY6cl-vNBdB_cr= QJlP1sRs0SX0ITy5ulgmzI4$ for graphic product...

    ATTN...WFO...LOX...

    ATTN...RFC...RSA...NWC...

    LAT...LON 35572092 35572058 35572025 35462016 35311989=20
    35091962 34861946 34751915 34641845 34521835=20
    34121866 34001899 34161953 34392077 35432121=20
    35492116=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jan 3 17:52:48 2026
    AWUS01 KWNH 031752
    FFGMPD
    CAZ000-040200-

    Mesoscale Precipitation Discussion 0004
    NWS Weather Prediction Center College Park MD
    1251 PM EST Sat Jan 03 2026

    Areas affected...Southern CA

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

    Valid 031750Z - 040200Z

    SUMMARY...Excessive Rainfall rates around 1"/hr will likely lead
    to additional flash flooding along the Coastal Range and Topatopa
    Mountains today where soils are sensitive due to recent heavy
    rainfall. Burn scars in the area are also prone to flash flooding
    and debris flows. Localized urban-induced flash flooding may occur
    in the suburbs north and west of Los Angeles

    DISCUSSION...Doppler Radar shows a narrow band of
    moderate-to-heavy rain oriented SW-to-NE over the Santa Ynez and
    San Rafael Mountains. A narrow squall line ahead of the cold front
    is also analyzed just west of Santa Barbara where a couple rain
    gauges southeast of Solvang have reported ~1"/hr rainfall totals.
    Aside from the squall, most 1-hour rainfall observations show
    0.5" totals as the band of heavy rain marches east towards Santa
    Barbara. Some 3-hr totals have reached 1.75", which also coincides
    with 1-hr averaged rainfall rates just over 0.5". This ribbon of
    rainfall is embedded just ahead of an approaching cold front with
    the warm sector approaching the Santa Barbara Channel. As the warm
    front collides with the western Transverse Ranges, a sliver of
    100-250 J/kg of MUCAPE will become available within a highly
    saturated atmosphere. Latest RAP forecast soundings near Oxnard
    show PWATs approaching 1.25" (above the 97.5 climatological
    percentile) and a fully saturated warm-cloud layer that is 9,000ft
    deep. Latest 12Z HREF probabilistic guidance does show moderate
    chances (40-60%) for 6-hour rainfall totals >3" over the Topatopa
    Mountains in Ventura County with similar probabilities along the
    Santa Ynez just north of Santa Barbara.

    As the frontal system moves east, so will the shield of heavy
    rainfall as it heads for the L.A. metro area. However, PWATs
    approaching 1.25" will retreat over off the coast and 850mb winds
    south of L.A. will tend to be weaker than the >30kt winds farther
    west. Therefore, rainfall rates should struggle to get much higher
    than 0.5"/hr except for the mountain ranges to the north and west
    where upslope enhancement will play a big role. In terms of
    impacts, the Santa Ynez, San Rafael, and Topatopa are of greatest
    concern given their lingering high soil moisture content (>95th
    soil moisture percentile in sfc-100 cm layer) and burn scars in
    these ranges. Debris flows and rock slides cannot be ruled out,
    particularly within burn scars. As for the urbanized communities,
    recent heavy rainfall has made soils sensitive and the greater
    concentration in hydrophobic surfaces naturally provides some
    flash flood concerns. Given the decreasing rates this afternoon,
    however, any flash flooding would generally be ponding on roads
    that could pose a hydroplane threat for motorists. In summary, the
    mountains north and west of L.A. are likely to witness additional
    flash flooding today, although localized flash flooding in more
    urbanized settings north and west of L.A. cannot be fully ruled
    out.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-7HaO-2_1JAsI4qeaTRyryPz2LAxCyYFSoB0xzT6DK0BMumMO9tgiqjxmTRaGq3lfeD3= Kt9uO69SZ7BkF6l3r30Lzy4$ for graphic product...

    ATTN...WFO...LOX...

    ATTN...RFC...RSA...NWC...

    LAT...LON 35201980 34861950 34741920 34761878 34731841=20
    34471830 34191839 33971867 34151933 34281964=20
    34331992 34402043 34712047 35142022=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jan 4 20:35:33 2026
    AWUS01 KWNH 042035
    FFGMPD
    CAZ000-050400-

    Mesoscale Precipitation Discussion 0005
    NWS Weather Prediction Center College Park MD
    334 PM EST Sun Jan 04 2026

    Areas affected...Southern CA Coastal Mountains

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

    Valid 042030Z - 050400Z

    SUMMARY...Narrow squall of heavy rain and embedded thunderstorms
    may produce rainfall rates up to 1"/hr. Given the highly saturated
    and sensitive soils along the Coastal Range and Santa Ynez
    mountains, flash flooding and mudslides are possible again this
    afternoon.

    DISCUSSION...Doppler Radar showed a potent squall line approaching
    Vandenberg AFB at 20Z moving east ahead of a weakening cold front.
    Compared to yesterday, PWATs are generally topping out between
    0.9-1.0" within the squall, a little less than yesterday. However,
    these values are still above the 90th climatological percentile
    and RAP mesoanalysis also shows the southern CA coast has >250
    J/kg of MUCAPE at these storms disposal. In addition, these
    squalls have upper-level support as the are located beneath the
    right-entrance region of a 120kt 250mb jet streak located over the
    central Sierra Nevada. Lastly, 925-700mb winds remain out of the
    SW and generally between 20-30kts, which is just strong enough and
    oriented favorably enough to support some upslope enhancement into
    the Coastal Range and Santa Ynez. With anomalous moisture,
    sufficient instability, beneficial synoptic-scale ascent, and
    topographic enhancement, these storms are likely to produce
    locally heavy rainfall as they move east.

    The soil sensitivities in the region have only grown worse since
    yesterday. MRMS CREST soil saturation over southern Santa Barbara
    County is over 85% and most locations within the highlighted
    at-risk area are over 50%. A recent FFW near Ventura referenced an
    LSR that mentioned more issues along highway 101 with one vehicle
    stuck in mud. That band of rainfall produced roughly 1.3" in under
    3 hours near Red Mountain and prompted flash flooding/mudslide
    issues. This approaching squall is more potent, however it is also
    progressive, which should help limit the extent of the flash flood
    potential. That said, the recent FFW near Ventura captures the
    most notable concern-- soils and burn scars in the area are highly
    sensitive and even hourly rates of 0.50-0.75" in an hour could
    prompt flash flooding and mud slides in the Santa Ynez. Expect
    rainfall totals to surpass 1" in the mountains which could be
    enough to trigger more flash flooding in southern Santa Barbara
    county this afternoon. Given the lingering instability and forcing
    aloft, additional cells could flare up over the Santa Barbara
    channel this afternoon and pose a flash flood threat into this
    evening.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5Qm--u4W-pSVK6xYxIwpTyDdgOjKxMsGhyoJ2zRpUOLE5MDP6Vdh9MaSfyAvfcYSvvwp= xwMHw3UfdSvE1h9YTlIJdRg$ for graphic product...

    ATTN...WFO...LOX...

    ATTN...RFC...RSA...NWC...

    LAT...LON 35682058 35402035 35091995 34881962 34761913=20
    34721859 34521867 34291923 34271965 34241980=20
    34311997 34412060 34552073 34962083 35222099=20
    35542098=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Jan 5 18:56:45 2026
    AWUS01 KWNH 051856
    FFGMPD
    CAZ000-060400-

    Mesoscale Precipitation Discussion 0006
    NWS Weather Prediction Center College Park MD
    156 PM EST Mon Jan 05 2026

    Areas affected...north-central CA

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

    Valid 051854Z - 060400Z

    SUMMARY...Isolated flood/flash flood impacts will be possible
    across portions of central to northern CA through the late
    evening. Peak hourly rainfall of 0.50 to 0.75 inches and peak
    additional total rainfall of 2 to 3 inches (locally higher
    possible) can be expected through 06Z.

    DISCUSSION...GOES West 6.9 micron imagery showed a mid-level
    vorticity max/closed low centered near 36.6N 127.0W at 18Z,
    embedded within a larger scale trough axis off of the West Coast.
    At the surface, low pressure was located ~70 miles northwest of
    Point Arena, with a cold front extending south and southwest. Over
    the past few hours bands of moderate to heavy rain have been
    observed moving across the northern CA Coastal Ranges with current
    radar imagery showing an axis of locally heavy rain oriented SSW
    to NNE into the North Bay region of San Francisco. In addition,
    infrared imagery showed a band of colder cloud tops just ahead of
    the cold front where weak MLCAPE values up to ~250 J/kg were
    estimated by short term RAP forecasts and SPC mesoanalysis data.

    850-700 mb winds were from the southwest at 30 to 40 kt ahead of
    the offshore trough axis into north-central CA with PWAT values
    ranging from 0.6 inches within the northern Sacramento Valley to
    about 0.9 inches just west of San Francisco Bay. Short term
    guidance is in good agreement with the track of the mid-level
    vorticity max/closed low slowly advancing toward the CA coast
    between Point Arena and San Francisco through about 03Z at which
    point stalling and eventual southward translation are forecast.
    The effect of these larger scale features will translate at the
    surface to a SSW to NNE band of heavy rain advancing eastward
    toward the central CA coast with embedded peak hourly rainfall
    between 0.5 and 0.75 inches (locally higher possible) through the
    afternoon and evening. Hourly rainfall up to about 0.5 inches in
    an hour will be likely for the northern Sacramento Valley where
    weak MLCAPE values up to 250 J/kg area forecast by the RAP from
    about 00Z-04Z.

    Recent heavy rainfall has left this region of CA more susceptible
    to heavy rainfall compared to normal, and there will be the
    typical enhancement of heavy rain impacts in and around the San
    Francisco Bay region to contend with. Within areas of higher
    terrain, localized landslides/rockslides will be possible and
    flooding of creeks, streams, urban areas and other
    low-lying/flood-prone locations will remain possible through about
    04Z. Beyond 04Z, low level winds are likely to weaken and orient
    more parallel to the coastline, diminishing the potential for
    flooding impacts across the region.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5yfdRhNsr5-w98AcBLIkgKfg5dwl82xgBx00_2ai_nPnbtaLIKpLyJFPncQgplhC3Gld= GFEcRSBOU4e1ZIqU2XZx8Rg$ for graphic product...

    ATTN...WFO...EKA...MTR...STO...

    ATTN...RFC...RSA...NWC...

    LAT...LON 41122240 41062196 40692174 40362164 39812141=20
    39542172 38992204 38132212 37402214 36942223=20
    36952281 37572330 38122362 38962364 39842330=20
    40422311 40932275=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jan 9 09:13:41 2026
    AWUS01 KWNH 090913
    FFGMPD
    MSZ000-LAZ000-ARZ000-091501-

    Mesoscale Precipitation Discussion 0007
    NWS Weather Prediction Center College Park MD
    412 AM EST Fri Jan 09 2026

    Areas affected...Central Mississippi...Eastern and Northeastern
    Louisiana...

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

    Valid 090911Z - 091501Z

    SUMMARY...Flattening steering flow to support segmented training
    corridors across the Lower Mississippi River Valley.=20
    Strengthening convergence and modestly unstable and seasonably
    moist air should support rain rates to 1.75" and localized streaks
    of 2-4" in 1-3hrs. Suggesting localized flash flooding is
    possible this morning to start a longer day of repeat
    thunderstorms.

    DISCUSSION...GOES-E WV suite shows mature/decaying shortwave
    rapidly elongating and sliding northeast through the central Great
    Lakes with a well defined broadly anticyclonically curved
    subtropical jet streak across Texas through KY/TN with a stronger
    base of the northern stream synoptic trough well upstream emerging
    into the southern High Plains. The strong flow and upper-level
    dynamic support has resulted in well above normal moisture flux
    across the Mississippi River Valley into the Great Lakes; CIRA LPW
    denotes core of higher moisture/theta-E air over the West Gulf is
    advancing into the entrance of the eastern US atmospheric river
    stream. Surface to 850mb values are nearing 1" and is noted with
    surface Tds in the upper 60s to even spots of 70 across the Lower
    MS Valley.=20

    The overall orientation of the upper-level flow is supporting a
    pre-frontal confluence zone across E LA at this time, providing
    sufficient deep layer convergence to tap the weakly unstable air.
    MLCAPEs are analyzed from 500-1000 J/kg through the Sabine River
    Valley into the Delta Region of SE AR and W MS. Flux convergence
    of 30-35kts at about 30 degrees of convergence overlaps with the
    core of the moisture axis with TPW near 1.7". As such, RADAR
    denotes a few clusters of thunderstorms developing across NE LA as
    well as further north across NE LA into W MS, the latter deeper
    into the more ideal unidirectional flow and may support some
    training elements as the overall convective development expands
    and intensifies over the next few hours. The strong moisture flux
    convergence mainly below 700mb will support rates of 1.75"; and
    while the forward speeds will limit any specific core, the
    upstream divergence aloft and strength of low level flow
    convergence will support back-building and redevelopment upstream
    through central LA throughout the morning.

    Localized storm outflows may be the key to establishing the most
    ideal training profiles, but even 1-2 hours of these rates could
    support 2-3" totals and locally higher values to 4" would then
    begin to exceed the high (3"/3hrs) FFG values in the area.=20
    00z/06z HREF Probability of 3"/3hrs peak around 30% in SW to
    central MS. Still even with dormant ground conditions, these
    rates/totals will have the greatest potential for flash
    flooding/rapid inundation conditions where intersecting urban
    centers. In any case, these cells will saturate the upper soil
    profiles prior to further convective activity expected throughout
    the day and evening. As such, flash flooding is only considered
    possible and limited to widely scattered in coverage through the
    early morning period.=20=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9acKgA_eVUQUbWukkTDJ3cwSbuwKek4CYWoR60Ef7vNo7XSoV4CCLFqlziyioqp90ODj= KtIhNIYw04qxDKJ-RKVXHog$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MEG...SHV...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34138908 34058839 33498829 32868864 32288915=20
    31568980 30709050 30919161 30929254 31469279=20
    32169248 33289103 33719020=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jan 9 15:16:14 2026
    AWUS01 KWNH 091516
    FFGMPD
    ALZ000-MSZ000-LAZ000-092000-

    Mesoscale Precipitation Discussion 0008
    NWS Weather Prediction Center College Park MD
    1015 AM EST Fri Jan 09 2026

    Areas affected...southeastern LA, southern MS, western AL

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

    Valid 091514Z - 092000Z

    SUMMARY...Peak rain rates of 2 to 3 in/hr are expected to produce
    at least Isolated flash flooding from northern portions of
    southeastern LA into southern MS and parts of western AL through
    20Z. 6-hr rainfall of 3 to 5 inches will be possible, through
    these higher end totals should remain rather isolated should they
    materialize.

    DISCUSSION...Radar imagery from 15Z showed a axis of heavy rain
    oriented ENE from the LA/MS border across the I-55 corridor into
    south-central MS and portions of western AL. This axis was located
    within an area of pre-frontal low level convergence, augmented by
    rain-cooled outflow that extended from near Baton Rouge, LA to
    Hattiesburg, MS to Thomasville, AL. 925 mb winds of 25-35 kt were
    observed over southeastern LA into southern MS, converging along
    this axis which was oriented parallel to the mean steering flow,
    supporting training. Hourly rainfall near and just over 2 inches
    has been observed near the LA/MS border within the past 2 hours
    where MLCAPE of 500-1000 J/kg and PWATs of 1.7 to 1.8 inches were representative of the environment, reported on the 12Z soundings
    from LIX and JAN.

    Short term guidance from the RAP shows similar low level flow
    continuing over the next few hours with the establishing cold pool
    likely serving as a focus for renewed convective development
    through 18Z to 19Z from the LA/MS border into southern MS. ENE
    steering flow is likely to support cells moving downstream into
    western AL while some upstream development occurs back to the WSW.
    The environment is capable of supporting hourly rainfall in the
    2-3 inch range, although 1 to 2 inches per hour will be more
    common. Localized potential for 3 to 5 inches over the next 6
    hours will exist with at least localized flash flooding appearing
    likely, especially within any urban areas and as high rain rates
    overcome dry antecedent conditions.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_TyiPQgtr4G0Ii50gtuvjxeex8vVdO5evYOP54YZtWf02QDLtAIGPEdd-TkMEu8RjjIG= d01F8d6HGazeOuastO5EijM$ for graphic product...

    ATTN...WFO...BMX...JAN...LCH...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 32848772 32518711 31988718 31498776 30978897=20
    30569019 30009159 30399210 31319161 32108995=20
    32618877=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Jan 9 20:05:18 2026
    AWUS01 KWNH 092005
    FFGMPD
    ALZ000-MSZ000-LAZ000-100100-

    Mesoscale Precipitation Discussion 0009
    NWS Weather Prediction Center College Park MD
    304 PM EST Fri Jan 09 2026

    Areas affected...south-central LA into south-central MS and
    western/central AL

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

    Valid 092003Z - 100100Z

    SUMMARY...Relatively narrow axes (or a single axis) of heavy rain
    appear likely to maintain an increased flash flood potential into
    the early evening from south-central LA into south-central MS and western/central AL. 2 to 4 inches and areas of flash flooding will
    be likely within portions of this corridor with locally higher
    rain totals possible.

    DISCUSSION...Radar imagery from 1945Z showed a persistent axis of
    moderate to heavy rain from near the southeastern LA/MS border
    into south-central MS and western AL which has been in roughly the
    same location over the past 3-4 hours. Embedded hourly rainfall
    has been observed in the 1-2 inch range at times and roughly 2 to
    4 inches have fallen from near Baton Rouge into south-central MS
    as far east as Waynesboro, MS since early this morning. A
    combination of rain-cooled outflow and a slightly elevated axis of
    convergence located within 925-850 mb layer have helped to focus
    these areas of heavy rain over the past few hours where MLCAPE has
    increased into the 500-1500 J/kg range from the southern MS/AL
    border toward Lake Pontchartrain (via SPC mesoanalysis data).
    Additional rainfall was occurring farther north in AL along the
    elevated convergence axis where 2 to 3 inches was reported over
    the past 6 hours, but a lack of instability has tempered rainfall
    rates across northern locations. Radar imagery also showed
    additional thunderstorms building over the I-10 corridor of
    south-central LA, rooted near the surface within weaker/more
    subtle axes of near surface convergence.

    RAP forecast guidance suggests an inflection point along the
    convergence axis (currently over the south-central MS/AL border)
    will advance northeastward in the short term while the axis of
    convergence to its west lifts slightly north. Meanwhile, the WSW
    to ENE oriented outflow boundary in place over south-central MS is
    likely to continue to serve as a focus for additional thunderstorm
    development. Therefore, expectations are for continued
    thunderstorms over the region through early evening, initiating
    along and just north of the surface outflow and farther north on
    elevated convergence with training via mean movement off toward
    the ENE. Embedded short term training may also occur with the
    thunderstorms moving northward through south-central LA.

    Hourly rainfall of 1 to 2 inches, but localized hourly rainfall in
    excess of 2 inches is expected through early evening from southern
    portions of the Lower Mississippi Valley into western/central AL.
    The better instability is forecast to remain situated west of the
    MS/AL border but pockets of locally higher instability into
    portions of AL may also support flash flooding to the east as
    well. Given dry antecedent conditions leading up to this event,
    flash flooding potential will be greatest over urban areas and
    where heavy rain has fallen over the past 12 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9m4qxItj-dnwomeDGXhQp86jHguqhmSXSAAR6bEQjaMBomi8lsV-t-Am1_0oAWUcpSxH= eCihXcSKifpS29MX2Hrx8sk$ for graphic product...

    ATTN...WFO...BMX...JAN...LCH...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 33568684 33488628 33168594 32648596 32198649=20
    31858711 31258872 30868957 30379076 30359177=20
    30639220 31179203 31969105 32449012 32698924=20
    33208778=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jan 10 01:47:19 2026
    AWUS01 KWNH 100147
    FFGMPD
    ALZ000-MSZ000-LAZ000-100545-

    Mesoscale Precipitation Discussion 0010
    NWS Weather Prediction Center College Park MD
    846 PM EST Fri Jan 09 2026

    Areas affected...Parts of Southern MS into western-central AL

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

    Valid 100145Z - 100545Z

    SUMMARY...A relatively narrow corridor of cell training will
    maintain the potential for isolated areas of flash flooding
    through the remainder of the evening. Additional rainfall totals
    of 2 to 3 inches are expected across many locales within this
    corridor through midnight CST, though isolated amounts of 4-5
    inches areas are expected.

    DISCUSSION...Latest GOES-E longwave IR imagery showed a well
    developed, rather expansive west-to-east Warm Conveyor Belt (WCB)
    of higher/colder cloud tops from northern Mexico northeast through
    eastern TX and into the Mid-South and TN Valley. Robust upper
    trough over the southern Rockies-High Plains and attendant upper
    level jet streak on the eastern flank is helping to enhance the
    deep-layer forcing and low-level frontogenesis ahead of the
    approaching cold front, which will coincide with the boost in the
    low-level moisture transport from the Gulf as 850 mb winds
    increase to 30-40 kts later this evening.

    Meanwhile, a narrow axis of higher deep-layer CAPE (1000-1500+
    J/Kg) will also nudge northeastward from the Gulf Coast into
    southern MS and southern-central AL, coinciding with PWs climbing
    between 1.8 and 2.0" in the expanding pre-frontal convective
    environment. Multiple, quasi-linear convective segments will tend
    to train within this narrowing corridor of more optimal
    instability and available PW. The mesoscale (CAM) guidance has
    struggled a bit handling the current setup, compared to the radar
    mosaic over the past few hours. Recent HRRR and RRFS runs have
    caught up a bit however. High res ensembles (HREF and RRFS)
    probabilities of hourly rainfall rates exceeding 1-2" are a bit
    lower than reality (especially the 2"/hr probabilities),
    indicative that the event may only just now be getting better
    handled by the guidance. Much of the CAM guidance show the
    heaviest rainfall south of BHM through midnight CST, however with
    notably lower FFG over northeast MS and northern AL, it would not
    take as much rainfall to cause additional runoff issues,
    especially considering what has already fallen.

    Hurley

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6j7wsjsHr8ga0tgXnpJ4FOHJWysiSmMEDaIqyT_p8lovh63Ekd-FfvWNITKFWu9QqJ3u= x9ZuW_d7bZj_84atsYa08l0$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34198699 32868611 31658789 30709029 31699073=20
    33308893=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jan 10 04:44:22 2026
    AWUS01 KWNH 100444
    FFGMPD
    MSZ000-LAZ000-TXZ000-101000-

    Mesoscale Precipitation Discussion 0011
    NWS Weather Prediction Center College Park MD
    1142 PM EST Fri Jan 09 2026

    Areas affected...Southeast to East Texas...Western and Northern
    Louisiana...

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

    Valid 100445Z - 101000Z

    SUMMARY...Strengthening scattered to widely scattered
    thunderstorms capable of 1.5"/hr and localized 2-3" totals given
    some short-duration training potential for flanking cell
    development. Greater soil saturation/lower FFG, north and
    proximity to Houston metro/urban runoff to south pose localized
    possible incident or two for flash flooding through overnight
    period.

    DISCUSSION...Regional RADAR mosaic and 10.3um IR loop depict a few
    stronger thunderstorm clusters extending from near Victoria
    northeastward across Southeast TX toward a weak surface low near
    KOCH. East of the low, a west to east stationary front crosses
    near I-20 and recently saturated upper soil profiles given broad
    1-2" totals throughout the day. Surface to boundary layer
    southerly flow continues to advect upper 60s/low 70s Tds with
    modestly unstable air mass in the warm sector with MLCAPE values
    remaining at or above 1000 J/kg with spots of 2000 J/kg near the
    Upper TX coast. Upper level jet streak continues to expand and
    strengthen across the Ozark Plateau though broad right entrance
    ascent is providing strong divergence aloft and supporting the
    slightly backed and 20-25kts of low-level jet flow to obliquely
    intersect the slowly eastward advancing cold front.=20

    While mid to upper levels remain dry, the anomalous moisture
    remains though 700mb with over 1.5" and spots nearing 1.75" within
    the warm sector. This results in solid moisture flux convergence
    and solid instability to maintain/expand the convective coverage
    though likely still in a scattered nature over the next few hours.
    Flux convergence is supporting moderately efficient rainfall
    production with 1.5-1.75"/hr rates. Forward progression will
    continue to be a limiting factor toward 2-3" streaks of rainfall
    totals across the area of concern, especially as the core of the
    jet (and therefore the right entrance divergence) shift
    northeastward and direct circulation allows for faster progression
    of the cold front through the TX Coastal Plain.=20

    Overall totals are not a tremendous concern across the Coastal
    Plain, with a solid exception of the hydrophobic urban/suburban
    corridor of Houston. The sheer rates would be the greatest
    potential and even slight probability of localized 2"/hr rates may
    be sufficient to result in localized flooding concerns. Further
    north across the northern Piney Woods of E TX into Northern LA,
    the recent rainfall will locally result in above normal runoff,
    and compromised FFG values of less than 2"/hr and 3"/3hr remain
    capable of being exceeded again. As such, a few incidents of
    localized flash flooding will remain possible through the
    overnight period as the front presses through from west to east.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5e45rP2JunIuVcPEhh0jU35Epu8JkIn1Nkw9iyBplNfFJrna5KVV_1R27PiPw8ZbzmRa= 2_o7E4DnM3kcR0t4xyG5GNM$ for graphic product...

    ATTN...WFO...HGX...JAN...LCH...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 32959190 32879118 32299104 31379165 30549283=20
    29959426 29399553 29649617 30229584 30649558=20
    31419478 32189422 32789339 32919271=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jan 10 05:36:51 2026
    AWUS01 KWNH 100536
    FFGMPD
    GAZ000-ALZ000-MSZ000-101100-

    Mesoscale Precipitation Discussion 0012
    NWS Weather Prediction Center College Park MD
    1236 AM EST Sat Jan 10 2026

    Areas affected...Southeast MS...Central AL...Northwestern GA...

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

    Valid 100535Z - 101100Z

    SUMMARY...Rainfall intensity is reducing though there remains a
    continued favorable training environment and persistent warm air
    advection for additional upstream development to maintain training
    through the overnight period. Already wetted/saturated soils
    with additional 2-3" may result in localized possible flash
    flooding.

    DISCUSSION...04z Surface analysis depicts main synoptic front
    bisects Middle TN into eastern MS before it starts to bend back
    westward across central MS to near Vicksburg and along I-20 under
    the influence of the upstream DPVA from the shearing upper level
    trough and strong 130kt+ jet over the Ozark Plateau. Still, the
    influence of the initial shortwave and atmospheric river/stream
    out of the western Gulf yesterday continues to slide northeastward
    across central AL toward the Southern Appalachians later this
    morning. VWP shows broad 25-40kt LLJ from SE LA across AL into
    western GA; which aligns with the core of enhanced moisture per
    CIRA LPW sfc-850 and 850-700mb layers with .75-.9" and .4-.5" in
    each layer respectively. RAP analysis and GPS network confirm
    1.75" core in central AL sliding northward.

    The flow through this layer remains strong and nearly
    unidirectional from 850 upward to support a narrow training
    profile for ongoing/weakening convection and anything that would
    redevelop upstream. The surface to boundary layer does still have
    some additional southerly component and surface
    analysis/instability axis denotes an effective rain-cooled
    isentropic ascent plain/front extending from the main front near
    Vicksburg to Jackson to south of Meridian to near Montgomery. As
    such mildly unstable air with 500-1000 J/kg of MUCAPE south of the
    boundary will isentropically ascend to provide some scattered
    thunderstorm activity upstream. This should help to maintain some
    training profile across central AL with occasional 1.5-1.75"/hr
    rates and localized 2-3" streaks, eventually extending toward W GA
    with slowly diminishing rates and therefore totals.

    However, given the prolonged nature, short term FFG values may not
    be exceeded except for areas already compromised across Southeast
    MS and far SW AL and urban centers along the way. However, add
    this 1-3" totals to the 1-2" totals already fallen across AL into
    GA and longer term exceedance is possible, suggesting localized
    flash flooding conditions remain possible through the overnight
    period into early morning.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!435-j2SzxdSRBUw-cE0OMsONPir6gcMUx4lDPm-ZmspqOtZkTROIgK4FzQEfJoUP2Gal= mFisCP7jRcMnc0sYzE9_uBw$ for graphic product...

    ATTN...WFO...BMX...FFC...JAN...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34408506 34308429 33678411 33238444 32488549=20
    31648728 31158841 31198950 31919077 32649045=20
    33158827 33538722 34128572=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jan 10 08:30:24 2026
    AWUS01 KWNH 100830
    FFGMPD
    ALZ000-MSZ000-LAZ000-101330-

    Mesoscale Precipitation Discussion 0013
    NWS Weather Prediction Center College Park MD
    329 AM EST Sat Jan 10 2026

    Areas affected...Eastern Louisiana...Southern Mississippi

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

    Valid 100830Z - 101330Z

    SUMMARY...Pre-frontal confluence band activating within narrow
    remaining instability axis in proximity to moisture axis enough to
    support 1.75-2"/hr rates. Cell motions support some short-term
    repeating though already saturated/flooded areas. As such,
    localized flash flooding is likely to occur again through early
    morning.

    DISCUSSION...GOES-E 10.3um and Regional RADAR depict an area of
    increasing convective development along a low level confluence
    line extending from near Marsh Island across Baton Rouge, LA
    toward McComb MS before intersecting with a broader west to east
    rainfall reinforced outflow or effective isentropic boundary. RAP
    analysis depicts a narrow instability axis with 1500-1750 J/kg of
    MLCAPE and generally aligns with the western edge of slightly
    higher low level moisture where Tds climb above 70 a few degrees.=20
    VWP also note an increase in low level wind speeds toward 40+kts
    and remain fairly unidirectional through 500mb well ahead of the
    frontal zone. As such, there remains a favorable training
    orientation for the convection. SPC MCD 18 alludes to favorable
    shear environment for some rotating cells as well, further
    increasingly moisture flux convergence allowing for rates to reach
    1.75-2"/hr potentially. Upstream cold front is starting to press
    eastward, but there remains a few hours of potential training of
    these cells. This matches most closely to the 00z ARW solution as
    well as recent RAP runs though other rapid refresh guidance
    provides some increased confidence to this evolution.

    Unfortunately, the orientation appears to intersect locations that
    had received over 4" yesterday afternoon. This has resulted in
    compromised FFG values below 2"/hr for solid portion of the MPD
    area of concern and with 1-2 hours of training spots of additional
    2-3" are probable and would likely result in localized flash
    flooding to occur once again across far northern East Louisiana
    into Southern MS. Combine this with any remaining convective
    cells along the cold front passing through by 14-15z, consider the
    potential for flash flooding to once again be likely across this
    area into the early morning hours.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4aacJg2RqFJ5V8-2vwdZ2lKcSM8fYZxP72KCyyCnUC5vlx1yoCazj4zpzWsinq-zZNFh= viusEplqvv9jnVIymFAi_pU$ for graphic product...

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

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 33058867 32998809 32558766 31878777 31448828=20
    31178870 30878924 30549032 30359117 30689162=20
    31319135 31909091 32838963=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jan 10 08:34:58 2026
    AWUS01 KWNH 100834
    FFGMPD
    ALZ000-MSZ000-LAZ000-101330-

    Mesoscale Precipitation Discussion 0013...Corrected
    NWS Weather Prediction Center College Park MD
    334 AM EST Sat Jan 10 2026

    Corrected for Concerning line: Flash Flooding Likely

    Areas affected...Eastern Louisiana...Southern Mississippi

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

    Valid 100830Z - 101330Z

    SUMMARY...Pre-frontal confluence band activating within narrow
    remaining instability axis in proximity to moisture axis enough to
    support 1.75-2"/hr rates. Cell motions support some short-term
    repeating though already saturated/flooded areas. As such,
    localized flash flooding is likely to occur again through early
    morning.

    DISCUSSION...GOES-E 10.3um and Regional RADAR depict an area of
    increasing convective development along a low level confluence
    line extending from near Marsh Island across Baton Rouge, LA
    toward McComb MS before intersecting with a broader west to east
    rainfall reinforced outflow or effective isentropic boundary. RAP
    analysis depicts a narrow instability axis with 1500-1750 J/kg of
    MLCAPE and generally aligns with the western edge of slightly
    higher low level moisture where Tds climb above 70 a few degrees.=20
    VWP also note an increase in low level wind speeds toward 40+kts
    and remain fairly unidirectional through 500mb well ahead of the
    frontal zone. As such, there remains a favorable training
    orientation for the convection. SPC MCD 18 alludes to favorable
    shear environment for some rotating cells as well, further
    increasingly moisture flux convergence allowing for rates to reach
    1.75-2"/hr potentially. Upstream cold front is starting to press
    eastward, but there remains a few hours of potential training of
    these cells. This matches most closely to the 00z ARW solution as
    well as recent RAP runs though other rapid refresh guidance
    provides some increased confidence to this evolution.

    Unfortunately, the orientation appears to intersect locations that
    had received over 4" yesterday afternoon. This has resulted in
    compromised FFG values below 2"/hr for solid portion of the MPD
    area of concern and with 1-2 hours of training spots of additional
    2-3" are probable and would likely result in localized flash
    flooding to occur once again across far northern East Louisiana
    into Southern MS. Combine this with any remaining convective
    cells along the cold front passing through by 14-15z, consider the
    potential for flash flooding to once again be likely across this
    area into the early morning hours.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8A94cu_2EwIsReGlPc-3vX9yAGxP4uM-DkHqQ9QnUZE7dddVxb0_aR_v2XJ7MMiUV3RH= ZqruWZkdv7CYjxwdXzJPM8o$ for graphic product...

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

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 33058867 32998809 32558766 31878777 31448828=20
    31178870 30878924 30549032 30359117 30689162=20
    31319135 31909091 32838963=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jan 10 13:55:58 2026
    AWUS01 KWNH 101355
    FFGMPD
    FLZ000-GAZ000-ALZ000-MSZ000-LAZ000-101954-

    Mesoscale Precipitation Discussion 0014
    NWS Weather Prediction Center College Park MD
    855 AM EST Sat Jan 10 2026

    Areas affected...portions of southeastern Louisiana, southern
    Mississippi, and southern/central Alabama

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

    Valid 101354Z - 101954Z

    Summary...Flash flood potential continues across southern
    Mississippi this morning. This threat will shift eastward while
    gradually becoming more isolated through 19Z/1p Central.

    Discussion...Recent radar mosaic imagery depicts an extensive,
    linear convective complex extending from near Gadsden, AL through
    Birmingham, AL and southwestward to near Hammond, LA. Convection
    has trended toward more forward propagation over the past several
    hours, but remain capable of 1-2 inch/hr rain rates - especially
    across southern Mississippi and southeastern Louisiana where
    forward motions are slower (around 20-30 knots) and quality
    pre-convective moisture exists. The storms are in an environment
    characterized by moderate surface-based buoyancy (around 1000-1500
    J/kg - highest from central Alabama through the New Orleans area)
    and 1.4-1.6 inch PW values - both characteristic of typical
    profiles supporting deep moist convection and heavy rainfall
    rates. Additionally, some of the activity was falling on areas of
    southern Mississippi that have received 5-8 inches of rainfall
    over the past 24 hours (particularly near Hattiesburg, Waynesboro,
    MS and surrounding areas). FFGs are near zero in those areas,
    supporting an imminent and ongoing flash flood threat there.=20
    Farther northeast and southeast of the Hattiesburg area, FFGs are
    a bit higher (around 1 inch/hr in Alabama - closer to 2-3
    inches/hr in Louisiana), suggestive of more scattered flash flood
    potential in those area in the short term.

    The forward-propagating nature of this complex will result in
    storms gradually moving out of the most sensitive, water-logged
    areas of the discussion area through the morning and early
    afternoon. The downstream airmass is still supportive of
    occasional areas of 1-1.5 inch/hr rain rates, promoting flash
    flood potential especially in urban and sensitive areas of the
    discussion area. Flash flooding remains most likely in
    southeastern Mississippi this morning, with a lesser-concentrated
    risk throughout the remainder of the discussion area.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7OGoiGqj85_Vesa1ojoKLDKhAaPxWV1B9qkkhqgPTdSo7FDat7FsdJY3lqM0RO53_it5= 34zevUAZFeSLoq2RL78HvGc$ for graphic product...

    ATTN...WFO...BMX...FFC...JAN...LCH...LIX...MOB...TAE...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34318457 33968412 32578415 31058531 30358760=20
    29228947 29239063 29609114 31409039 32788822=20
    34228567=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Jan 10 14:11:54 2026
    AWUS01 KWNH 101410
    FFGMPD
    FLZ000-GAZ000-ALZ000-MSZ000-LAZ000-101954-

    Mesoscale Precipitation Discussion 0014
    NWS Weather Prediction Center College Park MD
    909 AM EST Sat Jan 10 2026

    Areas affected...portions of southeastern Louisiana, southern
    Mississippi, southern/central Alabama, and western/northern
    Georgia

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

    Valid 101354Z - 101954Z

    Summary...Flash flood potential continues across southern
    Mississippi this morning. This threat will shift eastward while
    gradually becoming more isolated through 19Z/1p Central.

    Discussion...Recent radar mosaic imagery depicts an extensive,
    linear convective complex extending from near Gadsden, AL through
    Birmingham, AL and southwestward to near Hammond, LA. Convection
    has trended toward more forward propagation over the past several
    hours, but remain capable of 1-2 inch/hr rain rates - especially
    across southern Mississippi and southeastern Louisiana where
    forward motions are slower (around 20-30 knots) and quality
    pre-convective moisture exists. The storms are in an environment
    characterized by moderate surface-based buoyancy (around 1000-1500
    J/kg - highest from central Alabama through the New Orleans area)
    and 1.4-1.6 inch PW values - both characteristic of typical
    profiles supporting deep moist convection and heavy rainfall
    rates. Additionally, some of the activity was falling on areas of
    southern Mississippi that have received 5-8 inches of rainfall
    over the past 24 hours (particularly near Hattiesburg, Waynesboro,
    MS and surrounding areas). FFGs are near zero in those areas,
    supporting an imminent and ongoing flash flood threat there.=20
    Farther northeast and southeast of the Hattiesburg area, FFGs are
    a bit higher (around 1 inch/hr in Alabama - closer to 2-3
    inches/hr in Louisiana), suggestive of more scattered flash flood
    potential in those area in the short term.

    The forward-propagating nature of this complex will result in
    storms gradually moving out of the most sensitive, water-logged
    areas of the discussion area through the morning and early
    afternoon. The downstream airmass is still supportive of
    occasional areas of 1-1.5 inch/hr rain rates, promoting flash
    flood potential especially in urban and sensitive areas of the
    discussion area. Flash flooding remains most likely in
    southeastern Mississippi this morning, with a lesser-concentrated
    risk throughout the remainder of the discussion area.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Hlcy_JkIVC_spif7StIjfVMqKja9sq8Gg9rt_MmTn0QKzEocsUt4og8AxJVfmfAPSGm= Rp1xHZW4-kpUSY8JUQ28y5o$ for graphic product...

    ATTN...WFO...BMX...FFC...JAN...LCH...LIX...MOB...TAE...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34318457 33968412 32578415 31058531 30358760=20
    29228947 29239063 29609114 31409039 32788822=20
    34228567=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Feb 14 03:51:24 2026
    AWUS01 KWNH 140351
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-KSZ000-NMZ000-140949-

    Mesoscale Precipitation Discussion 0017
    NWS Weather Prediction Center College Park MD
    1049 PM EST Fri Feb 13 2026

    Areas affected...Northwest TX northeast to the MO/KS/AR/OK border
    junction

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

    Valid 140349Z - 140949Z

    Summary...Widely scattered to scattered thunderstorms are
    developing from western TX into western OK at this time. Hourly
    rain amounts to 2", with local totals to 4", could lead to
    continued isolated to widely scattered flash flooding.

    Discussion...An upper level low is progressing east-northeast
    across NM, leading to regional difluence aloft. Precipitable
    water values have surged to 1-1.25", which considering the
    coolness of the atmosphere, has led to saturation. SPC
    mesoanalyses indicate 500-1500 J/kg of MU CAPE across the region,
    with the broadest instability pool across central OK. This is
    helping to explain the backbuilding convection near the southern
    border of KS/MO. Effective bulk shear of 40-60 kts exists
    regionally, which has manifested itself across portions of the
    Rolling Plains, Caprock, and Permian Basin of northwest TX.=20
    Fairly unidirectional flow from the southwest is leading to
    training attempts near the mesocyclones across Northwest TX.

    The guidance indicates a general broadening of the instability
    field (when using the 500+ J/kg MU CAPE region) with time, with
    the greatest persistence across the Trans-Pecos region of western
    TX. This should continue to lead to a general broadening of the
    convective pattern which could increase bouts of training and
    possibly cell mergers between more organized convection clusters
    and disorganized thunderstorms. However, the broad pattern should
    attempt to progress eastward as 850 hPa flow veers. The best
    mesoscale model signal for heavy rainfall over the next six hours
    in the vicinity of the stationary front across OK. Hourly amounts
    to 2" and local totals to 4" are possible over the next six hours.
    Flash flood guidance is variable across the MPD area, with some
    areas more sensitive than others. These sort of amounts would
    compromise the relatively lower flash flood guidance values across
    northwest TX and the irregular MO/KS/AR/OK border junction.=20
    Isolated to widely scattered flash flooding is possible.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_a6eAtseqa0om1E8gkgzPFR1_L6Sgdn7CoE2FmTbkzeqVO6GgexZW10lmq9rsvIVN0g2= HKxQMYGgt-Bc18Z1u42P2cA$ for graphic product...

    ATTN...WFO...AMA...DDC...EAX...FWD...ICT...LUB...LZK...MAF... OUN...SGF...SJT...TOP...TSA...

    ATTN...RFC...FWR...KRF...ORN...TUA...NWC...

    LAT...LON 38589714 38019342 36539264 35739489 35349581=20
    32060045 31030356 32290359 33740150 34740112=20
    36610057 37709955=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Feb 14 09:13:56 2026
    AWUS01 KWNH 140913
    FFGMPD
    TXZ000-OKZ000-141512-

    Mesoscale Precipitation Discussion 0018
    NWS Weather Prediction Center College Park MD
    412 AM EST Sat Feb 14 2026

    Areas affected...portions of northern TX & southern OK

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

    Valid 140912Z - 141512Z

    Summary...Showers and thunderstorms are expected to invigorate and
    solidify into a slowly progressive line this morning. Hourly rain
    amounts to 2" with local totals to 4" remain possible, which could
    lead to isolated to widely scattered flash flood concerns.

    Discussion...Water vapor satellite imagery shows an upper level
    trough from CO south-southwest into northwest Mexico with two
    centers -- a weakening center lifting across southern CO and a
    more potent center moving just south of the NM/AZ border junction
    with Mexico. Difluence aloft remains downstream across the
    Southern Plains/TX; new convection is forming southeast of Midland
    at this time. Precipitable water values are 1-1.3" per GPS data.=20
    Gulf inflow continues to be best channeled up the Lower Rio Grande
    Basin then upward across west-central TX towards southwest OK.=20
    After initially dropping off after the evening convection, MU CAPE
    is back on the rise across west-central TX, in the range of
    500-1500 J/kg. Effective bulk shear is 50-75 kts regionally. The
    flow remains fairly unidirectional with height out of the
    southwest.

    The expectation is for a broad convective uptick into the late
    morning across portions of west-central and northern TX into
    southern OK as the mid-level low across far northwest Mexico
    approaches, which could back the mean winds somewhat more out of
    the south-southwest initially, possibly holding up convection for
    a short time. Once the line solidifies, convection should show
    some progression. The main concern from a heavy rainfall
    perspective is the possibility of embedded mesocyclones holding up
    segments of the line for an hour or two, leading to locally heavy
    rain that would locally exceed the three hour flash flood guidance
    (~2.5"). Issues would also be possible in urban areas. Flash
    flood issues could be isolated to widely scattered in nature.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_jNl3xZkw7WJLJXqFtOzbQ20pOidvGgFDz9eSsEuouRQhfO8muctXC1-uFwKLrvrwlK2= pUIXVs6oTQ4iMBdU9Gi0tIs$ for graphic product...

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

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35269728 34219634 31949880 30340135 29700289=20
    30420352 31310324 32770109 34519946=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Feb 14 17:36:32 2026
    AWUS01 KWNH 141736
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-142335-

    Mesoscale Precipitation Discussion 0019
    NWS Weather Prediction Center College Park MD
    1235 PM EST Sat Feb 14 2026

    Areas affected...Northeast TX into the Arklatex

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

    Valid 141735Z - 142335Z

    SUMMARY...Increasingly organized areas of heavy showers and
    thunderstorms with some localized cell-training concerns may
    foster isolated to scattered areas of mainly urban flash flooding
    going through the afternoon hours.

    DISCUSSION...The latest GOES-E IR/WV suite shows a strong southern
    stream shortwave trough ejecting east across the southern Plains
    which is interacting with a moist and modestly unstable airmass
    downstream across much of eastern TX.

    Strong forcing aloft with DPVA and a gradually increasing
    south-southwest low-level jet of 30 to 40 kts ahead of a cold
    front is facilitating a fairly expansive area of heavy showers and thunderstorms across central and northern TX and into the Red Red
    Valley.

    Recent radar trends has been showing a gradual increase in
    convective organization with the activity near the DFW
    metropolitan area, but with a generally progressive movement off
    to the east and northeast as the shortwave dynamics interact with
    the modestly favorable thermodynamic environment.

    MUCAPE values are generally only on the order of 500 to 1000 J/kg
    with PWs upwards of 1.5 inches. However, some uptick in these
    parameters can be expected over the next few hours as the
    low-level jet reaches 40 to 50+ kts and PWs increase locally to
    near 1.75 inches. This should help favor rainfall rates well into
    the 1 to 2 inch/hour range with the stronger and more organized
    cells which are being aided by much as 30 to 50 kts of effective
    bulk shear.

    Upscale convective growth is expected with at least the early
    stages of a QLCS evolution likely going through the mid-afternoon
    hours. The northern end of this convective mass will tend to focus
    across northeast TX and into the Arklatex region where there will
    be some localized cell-training concerns. A more progressive
    convective line is expected farther south. The 12Z HREF guidance
    suggests potential for some localized 3 to 4+ inch totals by later
    this afternoon around the Arklatex.

    The antecedent conditions are notably dry, but given the
    increasing rates and cell-training concerns, some isolated to
    scattered areas of mainly urban flash flooding will be possible.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5OUdtSYdwrifFZh_oEhT4OdhjIrhD4SEk6mtJ91CiUWM6k2tdiTTWeHidzgbtHRVgux2= uP243a-rpWdt2NZVMiTqjwg$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 34549428 34299311 33509314 32719423 32119559=20
    32029649 32239723 32699745 33319705 34129585=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 16 13:04:03 2026
    AWUS01 KWNH 161303
    FFGMPD
    CAZ000-162100-

    Mesoscale Precipitation Discussion 0020
    NWS Weather Prediction Center College Park MD
    802 AM EST Mon Feb 16 2026

    Areas affected...Southern California...

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

    Valid 161300Z - 162100Z

    SUMMARY...Strong dynamics/ascent will support strengthening
    moisture flux across Southern California and the Transverse Ranges
    this morning with pivoting cold front allowing for slightly
    increased duration of moderate rainfall with hourly rates of
    .5-.75"/hr with isolated potential to 1" locally. Totals of 1-2"
    along the coast and 3-5" in the terrain may result in increased
    runoff for possible flash flooding and or mudslides, especially
    near recent burn scars.

    DISCUSSION...GOES-W depicts a compact inner core of the deep upper
    low/trof continuing to dig southward near 36N129.5W with a broad
    diffluent region in the northeast quadrant where the exit of a
    130kt 250mb jet speed max is providing solid diffluence/divergence
    aloft for expansive upper-level cirrus shield with enhancing
    perpendicular transverse banding. A subtle but important embedded
    shortwave along the left exit of the jet shows a the developing
    baroclinic leaf just northeast of the 35N125W benchmark. This
    approaching wave coupled with the digging upper-level core is
    supporting surface cyclogenesis along the cold front in the
    vicinity of the SLO/Monterey county offshore waters, allowing for
    backing and strengthening low level flow off the California Bight
    through Santa Barbara county. VWP has seen an increase of
    925-850mb winds over 35kts while veering from SSE to SSW to over
    50kts at 700mb. This solid WAA profile has a bit of low level
    lapse rates as well to support 500-650 J/kg of MUCAPE in proximity
    to the cold front toward Point Conception.=20

    The overall interplay of the upper-level low and shortwave will
    allow for solid negative tilting of the upper-trof providing
    strong 75-90 degrees of low level directional convergence along
    the front while the confluence of 850 and 700mb moisture streams
    will align for enhanced moisture flux convergence bringing the
    slightly below average moisture values up toward something more
    average or slightly above average around 1" in total PWAT, with
    CIRA LPW animations denoting this trend is on track mostly in the
    surface to 850mb layer.

    So with the combination of increasing flux convergence and minor
    instability, pre-frontal showered and possible weak/narrow shallow thunderstorms convective cores of .75" to possible 1"/hr rates may
    occur over the next few hours as the front rounds the Cape and
    gets that extra bump due to steepening orographic ascent as well,
    though coastal showers will still be intense capable of a quick
    .5"+ rainfall total too, making urban style flooding problematic.=20
    The cold front will begin to press eastward, but in the short-term
    as surface low deepens, the pivot/fulcrum of rotation may allow
    for overrunning showers to persist across SBA into the TROWAL
    across SLO and Monterey counties for the next few hours keeping
    localized totals of 2-4" possible, with some continued higher
    runoff and possible localized flooding risk.

    Flash flooding risk will increase, as IVT values steadily increase
    from the 400 range toward 600 kg/m/s, likely peaking as the cold
    front and warm conveyor belt moisture stream flow orthogonally
    intersects the Transverse Range of Ventura county with HREF
    probably of 1"/hr near 30% between 18-20z, with 3-5" totals
    expected through 00z. As such, flash flooding is considered
    possible through the remainder of the morning and into the
    afternoon as it reaches the Los Angles Metro proper after 18z.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!95dfXy5F6loNRbNt-tcBUWF77z-5_cLiTGcwDMX-mJQ-THiN2tqReSdy2vY1Q0yF6ruy= SwLb9Vo1twaJhU1n4a2w99Y$ for graphic product...

    ATTN...WFO...LOX...MTR...SGX...

    ATTN...RFC...RSA...NWC...

    LAT...LON 36482138 36142073 35402021 34891962 34551875=20
    34521780 34001755 33261777 33361890 33732006=20
    34142075 34802105 35642182 36142185=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Mon Feb 16 19:30:06 2026
    AWUS01 KWNH 161930
    FFGMPD
    CAZ000-170130-

    Mesoscale Precipitation Discussion 0021
    NWS Weather Prediction Center College Park MD
    228 PM EST Mon Feb 16 2026

    Areas affected...Southern California...

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

    Valid 161930Z - 170130Z

    SUMMARY...Progressive cold front with strong pre-frontal southerly
    moisture flux will continue to shift eastward into the eastern
    Transverse and Peninsular Ranges through this evening. Less
    orthogonal ascent along terrain will reduce rainfall totals but
    intense sub-hourly totals up to 1" that may cause urban flooding
    and issues in and downstream of recent burn scars.

    DISCUSSION...RADAR and GOES-W visible imagery show a narrow band
    of intense showers/weak convective cores exiting Ventura county
    into S Los Angeles county extending southward through the eastern
    Channel Islands and starting to approach the southward turn of the
    coast across Orange and San Diego counties. Very strong moisture
    flux of 40-50kts of 925-850mb flow and steadily increasing
    moisture per CIRA LPW nearing .75" in that layer. Veering post
    frontal flow continues to be stark, with directional convergence
    remains between 75-90 degrees. Given the strength over 30kts (up
    to 50kts), it will continue to result in strong moisture flux for
    the convective elements supporting hourly rates of .75-1". This
    will continue what has been have observed moving through
    southward facing terrain of the Transverse Range including the
    Santa Monica Range, where totals of 2-3+" have been observed
    resulting in localized flash flooding.

    The strength of flow even below 850mb will continue to intersect
    the San Gabriel and San Bernardino Ranges lower to mid slopes with
    similar rates near .75-1"/hr though highest peaks will start
    converting over to moderate/heavy snowfall. However, with
    reducing southerly fetch, the Peninsular Ranges will see a quick
    pick up, but with less orthogonal convergence/orographic ascent
    will also see diminishing rates and therefore totals between
    22-00z tonight. The lack of moisture flux off the California
    Bight will also reduce the effective ascent through the TROWAL
    further back west across the central Transverse Ranges where
    lighter rain will continue to slowly add to the totals through 00z
    as well. With the loss of orographic ascent/convergence and
    deeper moisture availability, rates will reduce but increased
    westerly flow and steepening lapse rates aloft before the main
    cold front will allow for a few rounds of scattered upslope
    showers with .1-.25"/hr rates/totals adding to the initial
    mainline. Still, the overall risk for flash flooding will be
    limited to urban and recent burn scars east and South of the LA
    Basin.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_T2sFFPP0svERanV2yHB5IoA9mN_NCu8DjDbOL9-ENK0iN6I0_prGm9oGnmsdshK2Oz6= ETz3Y0zf0H5_pg1kbUamKeY$ for graphic product...

    ATTN...WFO...LOX...SGX...

    ATTN...RFC...RSA...NWC...

    LAT...LON 34701850 34251725 33811664 32841626 32471628=20
    32451709 32971743 33471782 33621834 33831850=20
    33981871 34221933 34601910=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Mar 5 16:12:59 2026
    AWUS01 KWNH 051612
    FFGMPD
    ARZ000-OKZ000-051730-

    Mesoscale Precipitation Discussion 0033
    NWS Weather Prediction Center College Park MD
    800 AM EST Thu Mar 05 2026

    Areas affected...Southeast OK...Far Western AR

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

    Valid 051300Z - 051730Z

    SUMMARY...Heavy showers and thunderstorms across southeast OK are
    expected to persist through mid-morning. Given high rainfall rates
    of up to 2 inches/hour and the slow cell-motions, some areas of
    mainly urban flash flooding will be possible.

    DISCUSSION...The early morning GOES-E IR satellite imagery shows a
    rather compact, but slow-moving cold-topped MCS over southeast OK.
    Some cloud-top cooling has been noted over the last couple of
    hours which suggests some deepening/strengthening of the
    convective updrafts and this has been corresponding to an uptick
    in rainfall rates.

    In fact, the latest MRMS data shows rainfall rates near 2
    inches/hour with the stronger storms over portions of Pittsburg
    and Latimer Counties, and there have been some clear signs of
    back-building cell activity around the southwest flank of the
    convective mass. The early-morning satellite imagery is showing
    some increasingly agitated CU/TCU across southern OK to the
    southwest of the convection, and this is correlated with a
    convergent low-level jet of around 40 kts in close proximity to a
    stationary front.

    The thermodynamic is generally modest with PWs of around 1.3 to
    1.4 inches and MUCAPE values of only 500 to 1000 J/kg. However, a
    wave of low pressure is noted in surface observations along this
    front near the area of most organized convection. Given the
    focused area of moisture convergence around this low center and
    the low-level jet aiming into the southwest flank of the MCS,
    there appears to be an environment to at least sustain the
    convection in the near-term.

    Morning CAMs are not doing the greatest with this MCS, but the
    latest RRFS guidance is generally the best with overall placement.
    However, it does suggest some convective persistence through at
    least the mid-morning hours. Given the convective trends, an
    additional 2 to 4+ inches of rain may be possible locally across
    areas of southeast OK, and especially with a favorable environment
    for back-building and training convective cells. The RRFS and some
    06Z HREF guidance suggest some parts of far western AR may
    eventually see some of this activity as well.

    Expect a concern for mainly urban flash flooding as a result over
    the next few hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4R6iCeI4LmUCaA5NzmFE9j-z2RPshOwLEWmKlicx_OB1_aZJ1YiUdTOF3ArjrFdHW0hV= Ywwb_p2vB3ikXFsa4onSyOM$ for graphic product...

    ATTN...WFO...LZK...OUN...SHV...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 35279546 35269464 34999407 34489415 34329513=20
    34419639 34779679 35139644=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Mar 5 23:44:05 2026
    AWUS01 KWNH 052344
    FFGMPD
    TXZ000-OKZ000-KSZ000-060542-

    Mesoscale Precipitation Discussion 0034
    NWS Weather Prediction Center College Park MD
    642 PM EST Thu Mar 05 2026

    Areas affected...portions of northwest TX & western OK

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

    Valid 052342Z - 060542Z

    Summary...Showers and thunderstorms should become more numerous
    with time from Northwest TX across portions of western OK. Hourly
    amounts to 2.5" with local totals to 4" are possible, which could
    lead to isolated to widely scattered flash flooding.

    Discussion...A deep layer trough lies across the West, with a
    subtle preceding shortwave just ahead of the main feature across
    portions of West TX, southeast NM, and the TX Panhandle. The
    combination of these incoming features is attempting to break a
    weak mid-level cap across the region, which has led to isolated
    shower and thunderstorm development. Precipitable water values
    are ~1.25", ML CAPE is 1500-2500 J/kg, and effective bulk shear is
    35-45 kts.

    With time, the cap breaks which should lead to increased shower
    and thunderstorm development near and poleward of where an area of
    850 hPa confluence intersects a warm front, with the zone of
    low-level confluence slowly veering with time. The 12z ARW and
    18z hi-res NAM are amongst the wettest guidance, showing a 3-4"
    maximum somewhere near the border of northwest TX and southwest
    OK. Given the ingredients above, hourly amounts to 2.5" with
    local totals to 4" are possible, lending some credence to their
    solutions. Cell training, cell mergers between more and less
    organized convective activity, and mesocyclone formation are
    expected to be the drivers for heavy rainfall. These amounts
    would exceed flash flood guidance on an isolated to widely
    scattered basis, and be more problematic in urban areas within the
    region. Used the 12z REFS & 18z HREF heavy rain signal to help
    define the MPD outline.=20

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!67chU8hr6wglojF9XFQcZQZ5f9RgUFP6UaatT-G40IV2BLK7d0_fXfjDMO7OIFxTB6fM= CRPmLUTn0hyH2IY20_YBaEM$ for graphic product...

    ATTN...WFO...AMA...DDC...LUB...OUN...

    ATTN...RFC...TUA...NWC...

    LAT...LON 37019878 36389723 34339850 33749996 34510128=20
    35760070=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Mar 6 09:16:43 2026
    AWUS01 KWNH 060916
    FFGMPD
    WIZ000-ILZ000-IAZ000-061500-

    Mesoscale Precipitation Discussion 0035
    NWS Weather Prediction Center College Park MD
    415 AM EST Fri Mar 06 2026

    Areas affected...IA into northern IL and far southern WI

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

    Valid 060911Z - 061500Z

    Summary...Isolated to widely scattered coverage of mainly minor
    flash flooding will be possible across central/eastern portions of
    IA into northern IL and the IL/WI border through 15Z (9 AM CST).
    Hourly rainfall of 1 to 2 inches will be likely where training of
    heavy rain occurs with isolated rainfall totals of 2 to 3 inches
    possible.

    Discussion...Regional radar imagery at 0845Z showed elevated
    thunderstorms over central and southern IA, with a general motion
    toward the northeast. The storms were located at the nose of a
    50-60 kt 850 mb jet seen on area VAD wind plots over central to
    eastern KS, located north of a wavy warm front which extended from
    southeastern NE into north-central MO and south-central IL. The
    low level jet was rapidly transporting low level moisture into the
    region, along with MUCAPE values of 500-1500 J/kg toward the
    northeast. Brief training of cells has supported observed rainfall
    of 0.75 to 1.25 inches in 30 minutes near the central MO/IA border
    between 07-08Z, showing the potential for locally high rainfall
    totals if cell training is able to maintain over a location for 30
    to 60 minutes. A strengthening 90-100 kt upper level jet streak
    was also observed on GOES East DMVs centered over southern MN,
    placing IA within the favorable right-entrance region.

    While the magnitude of the low level jet is likely near peak and
    RAP forecasts show some weakening through 12Z across eastern KS,
    continued warm advection driven thunderstorms are likely to
    advance downstream into portions of southern WI and northern IL
    over the next 3-6 hours as low level moisture continues to advect
    downstream and upper level support increases. Low level
    convergence axes at the nose of the low level jet are not
    favorably aligned to support longer duration training of cells
    with the mean steering flow from SW to NE (roughly at right angles
    to larger convergence axes), but increasing cell coverage could
    allow for some brief training from SW to NE or WSW to ENE this
    morning. The potential for 1 to 2 inches of rain in an hour and 2
    to 3 inches in 2 to 3 hours would surpass area-wide flash flood
    guidance values which are relatively low.

    Therefore, a couple of instances of lower-end/minor flash flooding
    will be possible over the next few hours with impacts mostly
    likely where overlap of heavy rain occurs with urban locations or
    other poorly draining areas.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8D9mYBbu0Iq8zqihAoDjR-bFNkrufn_JFv79UQULt56TOnftIXCqBoWPO1IsavPTsjBc= DUeLvMO8mcRND-sJY_TvDLY$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...FSD...ILX...LOT...MKX...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43049341 42899151 42709019 42548867 41818832=20
    41308877 40739090 40779355 41449517 42199543=20
    42869482=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Mar 6 22:12:52 2026
    AWUS01 KWNH 062212
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-KSZ000-070410-

    Mesoscale Precipitation Discussion 0036
    NWS Weather Prediction Center College Park MD
    510 PM EST Fri Mar 06 2026

    Areas affected...northeast TX into eastern OK, western AR, &
    central MO

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

    Valid 062210Z - 070410Z

    Summary...Showers and thunderstorms are broadening in coverage
    across southeast OK. Hourly rain amounts to 2.5" with local
    totals to 4" are possible, which could lead to isolated to widely
    scattered flash flooding.

    Discussion...Showers and thunderstorms are increasing in number
    across southeast OK and southwest MO as mid-level capping erodes.=20
    The OK activity in particular is near the intersection of a
    surface trough and an effective warm front. ML CAPE is 1000-2000
    J/kg, effective bulk shear is 40-55 kts, and precipitable water
    values are ~1.4". Water vapor imagery implies a weak disturbance
    is over the convection at the present time, with other shortwaves
    aloft approaching from the west and southwest. Thunderstorms are
    occurring on both sides of a cool wedge of air across central to
    northeast OK left behind by morning stratus/rainfall. The
    mesoscale guidance is struggling with the breadth of the coverage
    and the location, with the 12z REFS a few hours too delayed and
    the 18z HREF 1-2 hours delayed in this area.

    The GFS-based Galvez-Davison Index implies a convective uptick in
    coverage and intensity most centered in northeast TX, eastern OK,
    and northwest AR through 00z before activity wanes at 03z or so,
    which also matches the timing of the HREF/REFS convective
    evolution. Considering the parameters above, mesocyclones are
    expected. Hourly rain amounts up to 2.5" should be possible near
    mesocyclones and where convection of different levels of
    organization haphazardly merges, with local totals up to 4"
    possible. Cell training is also possible as the deep layer flow
    is fairly unidirectional out of the south-southwest. This flow
    veers slightly with time which should allow for a slight eastward
    shift and would theoretically limit even higher totals. The 18z
    hi-res NAM and 12z ARW are on opposing sides of the guidance
    spread, but at the moment, the 18z NAM appears to be doing
    somewhat better. The guidance all appears too wet in northeast TX
    at the present time, but given the incoming shortwaves from the
    west and southwest, additional convection is possible in that area
    at some point. Isolated to widely scattered instances of flash
    flooding are possible, particularly in urban areas.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5hXn_qD-Chh8OyMtbaonMLdCxO41R6d7gNxlB2gNo1GmXoX83zp-vlXgwgPFLCDSp6aR= x6q6_iWDZP02x1MvXegThV0$ for graphic product...

    ATTN...WFO...EAX...FWD...ICT...LSX...LZK...OUN...SGF...SHV...
    SJT...TSA...

    ATTN...RFC...FWR...KRF...ORN...TUA...NWC...

    LAT...LON 39029383 38769202 36599238 33899435 32109697=20
    31739900 33089868 34639827 35959795 36139782=20
    37599547=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Mar 6 22:30:23 2026
    AWUS01 KWNH 062230
    FFGMPD
    MIZ000-INZ000-ILZ000-070128-

    Mesoscale Precipitation Discussion 0037
    NWS Weather Prediction Center College Park MD
    529 PM EST Fri Mar 06 2026

    Areas affected...northeast IL, northwest IN, and southwest Lower
    MI

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

    Valid 062228Z - 070128Z

    Summary...A mesoscale wave is attempting to hold up convection
    from in and near Chicagoland into southwest Lower Michigan.=20
    Hourly amounts to 2" and local totals to 4" are possible, which
    could lead to flash flooding in urban areas.

    Discussion...A mesoscale convective wave across central IL is
    beginning to hold up convection in northeast IL rather close to
    Chicago. Precipitable water values are near 1.3", ML CAPE is
    1000-1500 J/kg, and effective bulk shear is 35 kts.

    The concern is that heavy rainfall will occur over a portion of
    Chicago's urban area, which includes far northeast IN. Some of
    southwest MI may see cell training as well. This situation does
    not appear to be handled well by recent mesoscale guidance. The
    parameters suggest hourly amounts to 2" with local totals to 4"
    are possible, which would be a problem in urban areas from a flash
    flooding perspective over the next several hours.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5wtNSRhaJZ0b-AkHJXJPRJ-g52HW4bwZseH-lj-Q-xnH-Roh6js4fiYsVibky7S7LO4F= 2MsfA3vV46HJbvhEzA2vAMk$ for graphic product...

    ATTN...WFO...GRR...ILX...IWX...LOT...

    ATTN...RFC...MSR...NWC...

    LAT...LON 42598593 41578648 40758845 40648918 40878939=20
    41018930 41548830 42178709=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri Mar 6 22:56:21 2026
    AWUS01 KWNH 062256
    FFGMPD
    ILZ000-070152-

    Mesoscale Precipitation Discussion 0038
    NWS Weather Prediction Center College Park MD
    555 PM EST Fri Mar 06 2026

    Areas affected...portions of Central IL

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

    Valid 062252Z - 070152Z

    Summary...A weak wave across western IL is holding up convective
    progression across central IL. Hourly rain amounts to 2" with
    local totals to 4" are possible, which would be a problem in urban
    areas.

    Discussion...In the wake of a mesoscale convective wave moving
    into north-central IL, the system's convective tail is being held
    up by a weak wave seen in the thermal field across western IL.=20
    Hourly rain amounts are up to 1.5" per radar estimates. ML CAPE
    of 1000-1500 J/kg lies to its south, effective bulk shear is ~35
    kts, and precipitable water values are ~1.4".

    It appears cell training in this region could last for 2-3 hours.=20
    In this time, hourly amounts to 2" with local totals to 4" are
    possible, which would be most problematic in urban areas.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_cu3PDWDwuxUiKwxwzpex5n8GbOkxAy35vzo6ex4qu-gnai0fFMgebW8YOLYV_NLTWJN= BYzCADTNScwVUB8N0-NjP98$ for graphic product...

    ATTN...WFO...ILX...LOT...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 40828877 40488805 39888912 39629031 40388936=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 7 00:55:52 2026
    AWUS01 KWNH 070055
    FFGMPD
    WIZ000-ILZ000-MOZ000-MNZ000-IAZ000-NEZ000-070654-

    Mesoscale Precipitation Discussion 0039
    NWS Weather Prediction Center College Park MD
    754 PM EST Fri Mar 06 2026

    Areas affected...in and near Iowa

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

    Valid 070054Z - 070654Z

    Summary...Showers and thunderstorms are developing across portions
    of Iowa which have recently received heavy rainfall. Widely
    scattered occurrences of flash flooding are possible over
    partially saturated soils and in urban areas.

    Discussion...The leading edge of an upper low over the West is
    pushing across portions of Nebraska and southeast SD at this time.
    Elevated showers and thunderstorms have begun to blossom near a
    surface low due to the difluent flow aloft ahead of this feature.=20 Precipitable water values are just over 1". MU CAPE of 500-1500
    J/kg lies across IA along with effective bulk shear of 30-65 kts.

    Moisture should increase further across IA with time, with
    precipitable water values eclipsing 1.25" in some areas.=20
    Sufficient instability should be available to keep convection
    going well into the overnight period. Hourly rain amounts up to
    2" are possible where mesocyclones form, cell training occurs, and
    where lesser and greater organized convection merges. Local
    totals should stay at or below 3". The flow noticeably veers as a
    front progresses eastward, which should limit overall totals.=20
    However, given recent saturation, hourly rain amounts could be
    sufficient to exceed the low flash flood guidance values seen
    across a good portion of IA. Widely scattered flash flood
    occurrences are possible through 07z, both over partially
    saturated soils and within urban areas.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8t-DVljKG8AePntYFJXiFaWqOUul6m6NleTEz-6TA7k68JCDan_Ut9hsSHGs-VWS4Bj3= Z1QII3DY3X-BNzoIM31_5yM$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...EAX...FSD...MKX...MPX...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43709310 43369042 41699019 40319259 40109486=20
    40619596 42499611=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 7 04:30:24 2026
    AWUS01 KWNH 070430
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-071000-

    Mesoscale Precipitation Discussion 0040
    NWS Weather Prediction Center College Park MD
    1129 PM EST Fri Mar 06 2026

    Areas affected...northeastern OK, southeastern KS, northwestern AR
    into southwestern/central MO

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

    Valid 070428Z - 071000Z

    Summary...Training of thunderstorms from northeastern OK into
    central MO and adjacent portions of southeastern KS and
    northwestern AR is likely to result in at least isolated to widely
    scattered areas of flash flooding over the next 3 to 6 hours.
    Hourly rainfall of 1 to 2 inches is expected, but isolated 2+ inch
    per hour rainfall will be possible.

    Discussion...At 04Z, a line of thunderstorms was observed on area
    radar imagery from northeastern OK into southwestern and central
    MO, with a history of training and peak MRMS-derived hourly
    rainfall just over 2 inches between Tulsa and Pryor, OK, just
    south of I-44. This line has been established for a few hours now
    and has resulted in a region of rain-cooled air being overrun by a
    40-60 kt low level jet. The SW to NE orientation of the line,
    matching deeper layer steering flow has resulted in areas of
    training, but the line of storms has shown some eastward
    translation over the past hour or so. Farther south, additional
    convective development has increased over southeastern OK, within
    weakly confluent low level flow, and is advancing northward into
    the southern extent of the aforementioned line in northeastern OK.

    Areas of training are ongoing from northeastern OK into
    southwestern MO, and this is likely to continue in the short term.
    While overall eastward movement is expected, the most likely area
    for training storms will be along the southwestern flank where the
    low level jet intersects the line. Meanwhile, 1000 to 2000 J/kg
    MLCAPE extended from the MOKSAROK intersection into central OK,
    ahead of a cold front/dryline extending SSW from eastern KS into
    west-central OK. A line of thunderstorms is expected to become
    better established as the cold front continues to sweep
    southeastward through 09Z, eventually bringing another round of
    locally heavy rain to portions of northeastern OK. While this
    second round of storms is expected to remain progressive, up to an
    additional inch or so of rain will add onto locally heavy totals
    from the initial round of thunderstorms ongoing. At least isolated
    instances of flash flooding will be possible with locally
    scattered coverage possible.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9_C8PkJrA_Owm1xEsyOiWlev0uastmEwoOXMM7o6CzP4SIXhGqA7dVgZGWKsVHZsllej= U5my1FNm5afr5JQ-qT0xemg$ for graphic product...

    ATTN...WFO...ICT...LSX...LZK...SGF...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38429281 38409202 38259130 37739134 37089182=20
    36399277 35569413 35209490 35179550 35409584=20
    35779609 36279599 36849542 37479443 37879367=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 7 05:51:24 2026
    AWUS01 KWNH 070551
    FFGMPD
    WIZ000-ILZ000-IAZ000-070920-

    Mesoscale Precipitation Discussion 0041
    NWS Weather Prediction Center College Park MD
    1250 AM EST Sat Mar 07 2026

    Areas affected...IA/IL/WI junction into southern WI

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

    Valid 070547Z - 070920Z

    SUMMARY...Training of heavy rain with 1-2 inches per hour may
    produce localized flash flooding from the IA/IL/WI tri-state
    region into southern WI through 09Z.

    DISCUSSION...Local radar imagery over southern WI showed the
    presence of an MCV or at least a northern bookend vortex about 30
    miles NW of Madison, WI. The motion of this feature was toward the
    ENE at a rapid pace of 40-50 kt. A strong low level jet of 40 to
    70 kt (70 kt @ KDVN at 0504Z) was helping to rapidly transport
    rich low level moisture to the north where it intersected a
    southwestward extending line of storms from near the MCV center.

    Forecast motion of the MCV takes it into central Lake Michigan
    within the next 3-4 hours but there could be areas of training
    along the axis of thunderstorms flanking the southwestern quadrant
    of the circulation, with 1 to 2 inches per hour despite limited
    MUCAPE of ~500 J/kg. While recent hires models do not have a good
    handle on this feature, short term observational trends and
    extrapolation indicate the best potential for training from the
    IA/IL/WI tri-state region into southern WI with potential for 1 to
    2 inches of rain in about an hour through about 09Z. Given 3-hr
    flash flood guidance values below 2 inches across the region,
    minor flash flooding will be possible, especially if there is
    overlap with any urban locations.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_CbYSD-aj5mdLKSEPKlqZHichx8ffHHTjA6qAX6Jpx9_NZ16baOGfYA71z2Dj4NN2LoQ= znJ-AGHq9Ali2DPmnbzgfoY$ for graphic product...

    ATTN...WFO...ARX...DVN...LOT...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 43858844 43808755 42798771 42398875 42168975=20
    42249059 42509082 42869048 43508957=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 7 09:56:58 2026
    AWUS01 KWNH 070956
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-071530-

    Mesoscale Precipitation Discussion 0042
    NWS Weather Prediction Center College Park MD
    455 AM EST Sat Mar 07 2026

    Areas affected...northeastern TX/southeastern OK into AR and
    southeastern MO

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

    Valid 070955Z - 071530Z

    SUMMARY...Flash flooding will be possible across portions of
    northeastern TX, southeastern OK into AR and southeastern MO
    through 15Z. Hourly rainfall of 1 to 2 inches will be common
    within cell training, but isolated 2+ inch per hour rainfall
    cannot be ruled out.

    DISCUSSION...The coverage of showers and thunderstorms has been
    gradually increasing from northeastern TX into western/central AR
    over the past hour, ending 0940Z. The continued transport of low
    level moisture into the region and perhaps some weak low level
    confluence has contributed to the recent increase as low level CIN
    decreases. Meanwhile, a line of thunderstorms was located to the
    west, along a NE to SW oriented cold front, analyzed from a GMJ to
    ADH to DYS line at 09Z. The environment from southeastern OK into
    central AR consisted of 1000-2000 J/kg MLCAPE, 1.4 to 1.6 inch
    PWATs and sufficient effective bulk shear values for organized
    storms, per SPC mesoanalysis data.

    At least a modest increase in the coverage of cells is expected to
    continue from far northeastern TX into western/central AR over the
    next few hours with some degree of continued moisture advection
    beneath diffluent flow aloft. The environment will continue to
    support a line of thunderstorms along and ahead of the cold front
    as it continues to advance southeastward, reaching southeastern OK
    by 12Z and central AR by 15Z. As thunderstorm coverage fills in
    from southeastern OK into central AR, cell mergers and training
    potential will increase. Hourly rainfall of 1 to 2 inches will be
    common where cell training occurs and isolated 2+ in/hr rainfall
    values will also be possible. Peak storm total rainfall of 2 to 4
    inches should be expected through 15Z which could produce isolated
    to widely scattered instances of flash flooding. Below average
    precipitation experienced over much of the region over the past
    few weeks may act to mitigate flash flooding to urban overlap or
    otherwise poorly drainage locations.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!572Q3M5-9eW4h4Gdt6dqk8Vs-JAifHlJSFikncaokp8cFUECJNgx_bLRNBSaimpMRnR2= _ZLxbaqeT_K0mBGqvi_BF_A$ for graphic product...

    ATTN...WFO...FWD...LSX...LZK...MEG...OUN...PAH...SGF...SHV...
    TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 37099014 36168967 35189033 33709311 33439515=20
    33819637 34829581 36089355 37029134=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Mar 7 19:44:35 2026
    AWUS01 KWNH 071944
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-080100-

    Mesoscale Precipitation Discussion 0044
    NWS Weather Prediction Center College Park MD
    243 PM EST Sat Mar 07 2026

    Areas affected...Northern LA...Central MS...Adj. Portions of SE AR
    & E TX...

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

    Valid 071945Z - 080100Z

    SUMMARY...Progressive convective line likely to be limited in
    duration but will intersect/merge with precursory slower moving
    cells along the western Gulf return moisture axis. Widely
    scattered 2-3.5" in 2-3 hours pose low-end possible incident or
    two of localized flash flooding through evening.

    DISCUSSION...Regional RADAR mosaic and GOES-E imagery suite depict
    a forward propagating convective line with numerous cells
    developing along the forward flanks sliding east-northeastward
    through the deeper layer steering flow allowing for some stronger
    thunderstorms to linger for near an hour before pressing southeastward/redeveloping. Solid mid to upper 60s Tds and near
    .8-.9" of PW through the lowest layer and totaling near 1.7"
    across the Lower MS Valley; and solid lapse rates given 2000+ J/kg
    of MLCAPE support fairly efficient rainfall production given
    strength of flux (on 30kts of southerly inflow). This helps to
    support 1.5-1.75"/hr rates and similar totals, but again, also
    supports solid forward propagation vectors to limit duration.=20

    Overall FFG values (2-2.5"/hr 3"/3hrs), especially given dry
    recent conditions are not likely to be eclipsed by this alone;
    though intensity forecast by the HRRR of 1-1.25"/15 minutes would
    not likely infiltrate the harder upper soil column, greater
    rainfall totals still are needed to result in even localized flash
    flooding conditions.

    CIRA LPW along with VWP notes, strong low level moisture return
    off the western Gulf into along a sharp western edge of the 850
    ridge axis over the US Southeast. This has resulted in a fairly
    consistent pre-frontal convergence axis along this western Gulf
    moisture stream. RAP moisture convergence shows a weaker but
    sufficient moisture convergence axis in the vicinity of the
    Mississippi River. Remote sensing shows this convergence has been
    successful in developing scattered thunderstorms across E LA/W MS
    with a slower northeast cell motion likely to intersect with the
    approaching boundary. These will eventually merge, likely
    broadening the updraft, moisture flux and therefore rates in the
    short-term result in enhanced spots or streaks of 2-3.5" total
    rainfall in 1-2 hours as they pass. This still remains on the
    lower end of the FFG, so resultant flash flooding will be remain
    widely scattered and likely lower-end remaining possible across
    the area of concern through evening.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!49yzUqznTyi1UYmqoEk1AtTQlzvgALOEibaJmiq4eAEASUmVdZ-PmMN60cXl1m_Dr3Jv= 7T659iZnAQoypftrDRTPYng$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...SHV...

    ATTN...RFC...ALR...FWR...ORN...NWC...

    LAT...LON 33688954 33598878 33238852 32768843 32108876=20
    31408948 31059057 30979114 30999241 31259380=20
    31789434 32479385 32789329 33199171 33399093=20
    33579029=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Mar 7 14:20:33 2026
    AWUS01 KWNH 071420
    FFGMPD
    TNZ000-MSZ000-LAZ000-MOZ000-ARZ000-TXZ000-OKZ000-072000-

    Mesoscale Precipitation Discussion 0043
    NWS Weather Prediction Center College Park MD
    919 AM EST Sat Mar 07 2026

    Areas affected...Northeast TX...Northern LA...Southern & Eastern
    AR...Western TN...Northwest MS...

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

    Valid 071420Z - 072000Z

    SUMMARY...Scattered to widely scattered streaks of 2-3" totals in
    1-2 hours along favorable confluence and training convective lines
    suggest localized flash flooding is possible through late
    morning/early afternoon.

    DISCUSSION...GOES-E WV suite depicts a highly dynamic environment
    across the central U.S. with and exiting stronger northern stream
    wave across the Great Lakes providing a broad entrance region
    through the Mid-MS River Valley while a more subtle wave over the
    Big Country of TX has provided a subtle split jet feature
    providing solid downstream divergence aloft across the area of
    concern stretching from NE TX through the Delta Region. A stream
    of mid-level moisture is exiting from this shortwave along a
    surface to boundary layer WAA regime across the Red River Valley.=20
    GOES-E Visible imagery shows some breaks along/ahead of the
    shortwave and weak surface reflection with best backed low level
    flow providing strong moisture flux convergence and convective
    development near KTKI/KGVT moving south-southeastward slowly.

    Solid 1500-2000 J/kg of MLCAPE exist through eastern TX to
    maintain/feed these cells and with 35-40kts of southerly flow
    intersecting the outflow boundary, isentropic ascent may allow for
    downstream cells developing eastward. Deep layer flow should
    allow for some short-duration repeat/training. A slight reduction
    in overall moisture may limit overall rates, but over 1.5"/hr
    should support some localized spots/streaks of 2-3" in 1-2 hours
    before propagation southward limits overall totals. Slightly
    higher FFG across E TX/N LA may further limit overall coverage but
    localized flash flooding remaining possible.

    Further northeast, the window appears to be closing for longer
    duration, multiple rounds of thunderstorms as cold front is
    starting to make a push eastward through the MS Valley; one,
    cutting off the overall moisture totals along the 50+ LLJ streak
    but two, reducing duration of heavy rainfall. Still, regional
    RADAR mosaic and GOES-E Visible still shows a few southwest to
    northeast moving showers/thunderstorms pre-frontally across E AR
    with some TCU across north-central LA where the western edge of
    the western Gulf moisture stream is occurring.

    RAP/HRRR analysis shows deep layer convergence remains on this
    axis before becoming confluent with the surging convective line.=20
    The combination rapidly increases convective cooling as noted in
    central AR over the last hour or so, shows the merger/combination
    supports an hour or two of enhanced 1.5-2"/hr rates and localized
    streaks of 2-3" in less than 2 hours. These intersections are
    fleeting in duration but newer ones will be expected downstream
    into W TX/NW MS and N LA as the overall system slides eastward and
    convective line has positive southeasterly propagation vectors.

    Any intersection with urban centers will likely present the
    greatest flash flooding risk, but overall scattered to widely
    scattered flooding remains possible through the late morning/early
    afternoon across the area of concern.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!545MGXyZ_Ssl0BwFngKQPyaPOyUKXGCDNCyBov6WUEtoGs63xVol7-GKwX4uoJ6LGlZp= 3j5rXkygC2DvKdJg_MpFBI4$ for graphic product...

    ATTN...WFO...FWD...JAN...LZK...MEG...SHV...

    ATTN...RFC...ALR...FWR...ORN...TUA...NWC...

    LAT...LON 36219006 36128862 35228840 34138878 33228950=20
    32689032 32199196 31999355 31919515 31929641=20
    32209683 32869673 33259606 33399536 34529244=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Mar 7 20:49:07 2026
    AWUS01 KWNH 072049
    FFGMPD
    LAZ000-TXZ000-080247-

    Mesoscale Precipitation Discussion 0045
    NWS Weather Prediction Center College Park MD
    348 PM EST Sat Mar 07 2026

    Areas affected...portions of Southeast TX & Southwest LA

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

    Valid 072047Z - 080247Z

    Summary...Showers and thunderstorms are expected to become more
    numerous across southeast TX and southwest LA over the next
    several hours. Hourly amounts to 2.5" with local totals to 4" are
    possible, which would be most problematic in urban areas.

    Discussion...A frontal wave is becoming more pronounced in the pressure/wind/thermal pattern across southeast TX, which has been
    shifting southward as of late. It is tapping a corridor of higher
    dewpoints between the Middle TX Coast and Southeast LA, where
    there are in the lower 70s. Precipitable water values of 1.5-1.7"
    lie in and just south of this region. ML CAPE of 500-2500 exists
    in this area. Effective bulk shear is 25-40 kts, and increasing.

    The combination of higher dewpoints in the region and increasing
    effective bulk shear should result in convection with increasing
    coverage and increasing organization, which will ramp up hourly
    rain amounts. The frontal segment east of the frontal wave is
    likely to propagate slower than other segments of the boundary,
    which is expected to be the more likely focus for the heaviest
    rains. The main threats from a heavy rain standpoint are cell
    mergers between convection of various levels of organization,
    mesocyclone formation, and short periods of cell training as the
    flow is nearly unidirectional with height from the southwest.=20
    Hourly rain amounts up to 2.5" with local totals to 4" appear
    possible in this environment. The RRFS, which can bias high,
    shows a 10-20% chance of 5" amounts in the 21z-03z window. Due to
    ongoing drought, widely scattered instances of flash flooding are
    possible, more likely in urban areas.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8y-uNwIF0JZLmrqRcYDFGhiCq7zaQew6VfU_eEyPWTLoxZfoOHqdnVXpWd8_XUzItEVx= oKzK7k_hNNWECZysLs6MTHU$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...LCH...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 32059397 31349310 30019400 29609587 29889696=20
    31169596=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Mar 7 21:20:38 2026
    AWUS01 KWNH 072120
    FFGMPD
    TXZ000-080048-

    Mesoscale Precipitation Discussion 0046
    NWS Weather Prediction Center College Park MD
    419 PM EST Sat Mar 07 2026

    Areas affected...portions of South-Central TX

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

    Valid 072118Z - 080048Z

    Summary...An incoming mesocyclone and elevated thunderstorms out
    ahead of it with some backbuilding character could yield hourly
    amounts to 2.5" and local totals to 4" across South-Central TX
    over the next few hours. Flash flooding is more probable in urban
    areas.

    Discussion...A frontal boundary is edging southward across the
    region, with more southward sag east of San Antonio than from the
    city westward. Showers and thunderstorms with occasional
    backbuilding character are near and behind this front. To the
    west, northwest of Sabinal, a mesocyclone is progressing eastward
    elevated over the front. Precipitable water values of 1.4-1.7"
    lie here. ML CAPE is ~ 2000 J/kg, and effecitve bulk shear of
    30-50 kts is helping to sustain the mesocyclone.

    Radar reflectivity trends indicate the possibility of backbuilding
    and cell mergers with the incoming mesocyclone as the main causes
    for heavy rainfall over the next few hours. Hourly amounts to
    2.5" with local totals to 4" appear possible here given the
    available ingredients, which would be most problematic in urban
    areas due to ongoing drought conditions.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!95fFyTL52dXOxSaiUekZeNloeGDcLbzhxoPwcUc5rXUAcYdhD3gVJ53nK76zuXCBB5W6= QtPNf0JkpsockHL8hCfeISY$ for graphic product...

    ATTN...WFO...CRP...EWX...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30089917 29859665 28959664 28989790 29169900=20
    29469982 29849988=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Mar 7 23:50:10 2026
    AWUS01 KWNH 072350
    FFGMPD
    ALZ000-MSZ000-LAZ000-TXZ000-080600-

    Mesoscale Precipitation Discussion 0047
    NWS Weather Prediction Center College Park MD
    649 PM EST Sat Mar 07 2026

    Areas affected...northwest & north-central Gulf Coast

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

    Valid 080000Z - 080600Z

    Summary...Heavy rainfall concerns continue in the vicinity of a
    front sinking through the region. Hourly amounts to 2.5" with
    local totals to 4" could lead to flash flooding, primarily in
    urban areas.

    Discussion...A wavy front continues to settle southward towards
    the north-central and northwest Gulf Coast. Precipitable water
    values in the region are 1.3-1.7" per GPS data. Effective bulk
    shear is generally 25-50 kts, with the associated field sinking
    southward with the boundary. ML CAPE is 1000-3000 J/kg. The deep
    layer flow is generally out of the southwest. The above
    parameters support organized convection, and at times
    thunderstorms have organized into a linear or clustered
    appearance. Cell mergers have been common where 850 hPa inflow
    has shown some confluence in the Lower Mississippi Valley, while
    attempts at cell training have occurred north of Houston as of
    late. Mesocyclones have been present at times within the
    convective pattern. Backbuilding has also been seen at times.

    The mesoscale guidance suggests two main areas where heavy
    rainfall is preferred through 06z -- from far southeast TX through
    southern LA into southern MS, with a secondary maximum across the
    Brush Country of interior South TX. Based on the ingredients
    present, hourly rain amounts to 2.5" and local totals to 4" remain
    possible in these areas wherever cells merge, train, backbuilding
    occurs, or mesocyclones track. Much of the region is in long term
    drought so the three hour flash flood guidance values are rather
    high, in the 3-4" range. Urban areas appear most threatened by
    upcoming heavy rains. Flash flooding is considered possible.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6_31B0A2GaDp9yCuMrNtL1m7q3KSwVjiLETYDH5rg0VPMfyao5QAgd6DbBitCdCKZlUb= hTOn8LQy_SPD5O7JrtCkJ7Y$ for graphic product...

    ATTN...WFO...BMX...BRO...CRP...EWX...HGX...JAN...LCH...LIX...
    MOB...SHV...

    ATTN...RFC...ALR...FWR...ORN...NWC...

    LAT...LON 33128827 32318749 30788773 29878893 29439145=20
    29329399 28539567 26859715 26289912 27299997=20
    28349995 29679852 31229470 32299144 33048981=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Mar 8 06:02:43 2026
    AWUS01 KWNH 080602
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-TXZ000-081000-

    Mesoscale Precipitation Discussion 0048
    NWS Weather Prediction Center College Park MD
    101 AM EST Sun Mar 08 2026

    Areas affected...Gulf Coast from Galveston Bay to western FL and
    southwest AL

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

    Valid 080559Z - 081000Z

    Summary...The threat for flash flooding will linger across
    portions of the central Gulf Coast from near Galveston Bay to the
    western FL Panhandle and southwestern AL for at least another 3-4
    hours. Hourly rainfall of 1-2 inches will be most common within
    axes of training, but localized 2+ in/hr rates are also expected.

    Discussion...0530Z radar and surface observations showed a wavy,
    elongated outflow boundary that extended from Galveston Bay into
    southwestern AL. MRMS showed the highest hourly rainfall values
    from south-central LA into southwestern AL with a range between 1
    and 3 inches. 05Z SPC mesoanalysis showed MLCAPE along and south
    of the outflow boundary of 500-1500 J/kg and PW values of 1.5 to
    1.9 inches where cold tops continued to periodically cool on
    infrared satellite imagery. 850 mb winds varied across the Gulf
    Coast region but were generally between 15-25 kt from the S to SW,
    supporting overrunning. Aloft a low to mid-level shortwave trough
    axis was seen from central AL into south-central LA, tracking
    eastward beneath strongly diffluent and divergent flow aloft,
    within the right-entrance region of a 120+ kt upper level jet over
    the MS Valley to the north.

    The elongated outflow boundary is likely to continue slowly
    advancing south and southeast over the next few hours, eventually
    pushing south of a majority of the LA/MS coast while warm/moist
    air continues to overrun it from the south. Areas of training are
    likely to continue in the short term, but should become less
    widespread through time. This will be as the low-mid level
    shortwave and the upper level jet max advance toward the E/ENE,
    weakening and shifting large scale ascent away from the LA/MS
    coast. Diffluence will remain pronounced over the Gulf Coast
    however, so there is some potential for more isolated thunderstorm
    development back to the west, near the upper TX coast where the
    outflow boundary may continue to linger just inland of the Gulf
    Coast.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4nu5WEY2EOHy9lm9_7pVs8y7KZABMIuguyQaAk-lfeCccbqg5K9lhz5T_Xf26cuwoZUi= eeDl8XTGzGH9ED8YkRwGY9w$ for graphic product...

    ATTN...WFO...BMX...HGX...JAN...LCH...LIX...MOB...

    ATTN...RFC...ALR...FWR...ORN...NWC...

    LAT...LON 32618773 32518715 31938687 30888711 30108764=20
    29828838 29708944 29539053 29469202 29429360=20
    29109447 29279516 30029517 30359423 30739214=20
    31049025 31378932 31988841=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Mar 8 10:02:19 2026
    AWUS01 KWNH 081002
    FFGMPD
    LAZ000-TXZ000-081400-

    Mesoscale Precipitation Discussion 0049
    NWS Weather Prediction Center College Park MD
    501 AM EST Sun Mar 08 2026

    Areas affected...Upper TX Coast into Southwestern LA

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

    Valid 081000Z - 081400Z

    SUMMARY...Isolated flash flood potential will exist along the
    upper TX coast into southwestern LA through 14Z. Training of heavy
    rain could support 1 to 3 inches per hour

    DISCUSSION...Area radar imagery at 0945Z over TX/LA continued to
    show scattered thunderstorms from near Galveston Bay into portions
    of southwestern LA. 09Z surface observations showed these storms
    were located north of an outflow boundary that extended from
    Galveston Bay into the northern Gulf, south of the TX/LA border,
    and then eastward, hugging the LA coast into southeastern LA.
    Stronger, quasi-organized cells, were located along the northern
    extent of MLCAPE, estimated to be 500-1000 J/kg via 09Z SPC
    mesoanalysis data. The instability was present from the middle to
    upper TX coast to just south of I-10 in southwestern LA.

    850 mb winds were from the SSW to SW via area VAD wind plots at
    10-20 kt and are forecast by the RAP to maintain a similar
    intensity over the next few hours. Low level flow overrunning the
    outflow boundary with cell motions oriented roughly parallel to
    the boundary were allowing for a locally increased training
    potential. Flow aloft remain rather diffluent which will aid lift
    across the region. The environment is capable of supporting hourly
    rainfall of 1 to 3 inches per hour which could result in a
    isolated flash flooding, however, low coverage of these higher
    rainfall rates should limit the flash flood threat.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4IA2jrZhvNStomp_AhBZ8AQvQrtrc0aoxCuonFMDq7iY9EuCAfyQcm__EMm6XPiSUR1H= pDe3-TDmu6LMs3JBUF9qU1M$ for graphic product...

    ATTN...WFO...HGX...LCH...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 30729289 30489231 30129198 29509200 29329247=20
    29409357 29189442 29059518 29539561 30279496=20
    30649372=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Mar 8 12:37:49 2026
    AWUS01 KWNH 081237
    FFGMPD
    TXZ000-081700-

    Mesoscale Precipitation Discussion 0050
    NWS Weather Prediction Center College Park MD
    736 AM EST Sun Mar 08 2026

    Areas affected...South-central Texas...

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

    Valid 081235Z - 081700Z

    SUMMARY...Slow moving cells capable of 1.75"/hr rates near the
    Southern Balcones Escarpment/San Antonio Metro may pose localized
    flash flooding concerns through mid-morning.

    DISCUSSION...EWX RADAR and GOES-E 10.3um EIR continue to show
    increasing coverage and cooling top/intensifying thunderstorms
    across south-central Texas. Return weak southerly moisture flux
    over the shallow cold front across Deep South Texas combined with
    favorable divergence in the exit/diffluence of upper-level jet max
    has enhanced scattered early morning shower activity into
    deeper/broader updrafts capable of intense rainfall. VWP at EWX
    combined with RAP analysis suggests a recent uptick in 850-700mb
    flow to 15kts, but generally into the northern limit to the weak
    isentropic ascent providing this additional convergence to
    generate/expand convective activity. CIRA LPW shows sfc-850 and
    850-700mb tight moisture gradient indicative of the shallow front
    with values near .8-.9 and .5" respectively. The loading of this
    1.5 to 1.75" total PWat into the cells has increased rainfall
    efficiency to support 1.5-1.75"/hr rates, especially the broader
    cell in Bexar county, which also shows solid suggestion of upwind redevelopment.=20

    Deep layer steering driven mainly below 700mb has more of a slow
    northward shift within broadly westerly flow, which is also nearly
    parallel to the moisture/flux gradient. This may allow for short
    periods of repeating to allow for hour plus duration or random training/repeating from upstream cells too. Spots of 2-3" are
    possible in 1-2 hours though the mid-morning (through 15-17z)
    until favorable jet divergence slides further eastward/weakens as
    well.=20

    Proximity to San Antonio Metro/broad urban center and Balcones
    Escarpment will likely be the greatest driver of flash flooding
    potential. Naturally low FFG along/north of the city with hourly
    values between 1.5-2" are well within the potential of low-end
    exceedance and suggestive of localized possible incident or two of
    flash flooding, especially if combined with hydrophobic urban
    setting, further compounding run-off potential. Though south of
    the escarpment across the sandier Coastal Plain, FFG values
    increase rapidly and therefore flooding risk would be considerably
    lower, but still non-zero.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9tzj-zTZ90x2te8mwPXgbDHtrsqYx0S_4Cjxoj7kTw-4gQaI7vWu40Z0j9hJOpsjHCDG= UFRr_SquB34e9DYxpbqy-ek$ for graphic product...

    ATTN...WFO...CRP...EWX...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 29999741 29759663 29389614 28909595 28569640=20
    28349786 28389910 28619953 28919971 29259965=20
    29649922 29919843=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Mar 8 17:02:52 2026
    AWUS01 KWNH 081702
    FFGMPD
    TXZ000-082130-

    Mesoscale Precipitation Discussion 0051
    NWS Weather Prediction Center College Park MD
    1201 PM EST Sun Mar 08 2026

    Areas affected...South-Central Texas...

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

    Valid 081700Z - 082130Z

    SUMMARY...Risk of low-end, widely scattered incidents of possible
    flash flooding continue for a few more hours. Localized rates up
    to 2"/hr

    DISCUSSION...Surface to 850mb analysis shows the shallow cold air
    remains in place across the Coastal Plain of South Texas with
    surface north/north-easterlies across nearly all of the state.=20
    However, onshore flow has veered a bit toward southeast continues
    to isentropically ascend across the front which is banked up along
    the coast itself. Northeasterly flow through 925mb at EWX
    combined with recent CIRA LPW in the Surface to boundary layer
    level align to denote the moisture gradient aligns with
    directional convergence. MUCAPEs have modified slightly since
    this morning, but remain with pockets of values nearing 1500 J/kg
    to support the stronger vertical ascent for these scattered
    thunderstorms. Divergence aloft continues to be fairly solid in
    the weak split in the upper-level sub-tropical jet streak; but the
    upstream ridging is increasing and advecting eastward in WV
    showing the favorable environment will continue to shift and
    eventually diminishing through the evening as it reaching the
    central TX coast toward Victoria, TX

    Longer trend animation shows the 925 to 850mb just east of Rio
    Grande River near/centered around Cotulla; though WAA extends
    through 700mb before veering sufficiently for nearly west to east
    steering flow. This effective bulk shear nearing 50+kts along
    with RADAR animation shows updrafts have modest rotation to
    further isallobarically increase moisture flux convergence to
    broaden the updrafts increasing rainfall efficiency. Bunker's
    right mover propagation vectors allow for the more eastward
    deflection and slowing of forward motions to allow for increasing
    overall rainfall duration. Given total flux of the 1.75" at
    10-15kts through the low levels as increased rainfall efficiency
    in these cells toward 2"/hr with occasional localized upticks to
    2.5". As such localized streaks of 2-4" are starting to form and
    near the longer/higher FFG values (3-4"/3hrs). As such,
    localized flash flooding remains possible though likely remain
    widely scattered to scattered in overall coverage with overlap
    into urban centers resulting in the greatest flash flood
    potential.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!87kuqhY-PHOB8lpVdiEFATdF6AtIQzNEIP7IVPmpoLZjcG8lbRy0R0e63zzRLJHC7FVb= a5iY9d4hrVl9oZFkS6e-Snc$ for graphic product...

    ATTN...WFO...CRP...EWX...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 29749720 29629635 29379606 28989601 28599622=20
    28279687 28189739 28099840 28169892 28469928=20
    29019937 29509900 29739809=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Mar 9 17:13:40 2026
    AWUS01 KWNH 091713
    FFGMPD
    TNZ000-ALZ000-MSZ000-ARZ000-092230-

    Mesoscale Precipitation Discussion 0052
    NWS Weather Prediction Center College Park MD
    112 PM EDT Mon Mar 09 2026

    Areas affected...Central & Eastern AR...Southwest TN...Northern
    MS...Northwest AL...

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

    Valid 091715Z - 092230Z

    SUMMARY...Broadening upstream redevelopment of
    showers/thunderstorms with potential for increased
    training/repeating through afternoon. Rates increasing from 1 to
    1.5"+/hr with 2-3" totals over wet upper-soils posing localized
    possible flash flooding risk this afternoon.

    DISCUSSION...GOES-WV suite depicts a small and fairly compact
    roll-up vortex/shortwave over north-central OK shifting ENE along
    interface of strong zonal westerlies to the north and increasingly
    flattening sub-tropical stream across TX. This sub-tropical jet
    speed max at 70kts has left exit divergence favorably aligned over
    AR at this time helping to support/maintain initial convective
    activity into a broader complex. RADAR and EIR shows the leading
    edge of the convection has seen an uptick in activity/cooling as
    the cluster further expands into a weak bow like forward
    propagating MCS. The positive dPVA from the approaching shortwave
    is maintaining solid 40+ kts of west-southwesterly LLJ that slowly
    continues to veer with bulge of enhanced total PWats up to 1.7"
    interfacing with the upwind edge of the cluster. This will
    continue to support upwind flanking redevelopment on the
    isentropic moisture flux convergence (as noted with some weaker
    elevated development across Yell/Logan and Johnson counties at
    this time.

    RAP analysis along with GOES-E Visible imagery shows increasing
    clearing downstream east of the MS River and with slightly higher
    surface moisture; instability is starting to climb over 1000 J/kg
    perhaps reaching 1500 J/kg over the next few hours to further fuel
    the leading convective cells. Given the strength of moisture
    convergence, rain-rates will increasing from near 1"/hr currently
    toward 1.5"-1.75"/hr over the next few hours. As the inflow
    veers, and some weak divergence in the deeper layer steering flow
    across MS into AL, propagation should deflect southeastward a bit
    increasing the potential for the flanking development to
    repeat/train across east-central AR along and south of the TN/MS
    border (in proximity to an old eroding stationary front).

    As such, an axis of 2-3" totals are probable. Recent moderate to
    heavy rainfall has increased soil saturation over the last few
    days with current NASA SPoRT LIS 0-40cm ratios around 60-65% or
    slightly above normal. As such, increased run-off is possible and
    may result in possible localized flash flooding (as FFG values
    1.5-2"/hr; 2-3"/3hrs).=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7dAQwJKs4_u-8TvD6FLNcw5R__R8vOGlBxm4jPVMHErZbzOT0GBX90SS_B4FdjH9Z3XP= 52NByVPw9jnWkB0J219ny5k$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LZK...MEG...

    ATTN...RFC...ALR...ORN...TUA...NWC...

    LAT...LON 35629295 35619178 35439024 35058830 34578749=20
    33778780 33468887 33619089 34059281 34709372=20
    35369357=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Mar 9 21:31:14 2026
    AWUS01 KWNH 092131
    FFGMPD
    GAZ000-TNZ000-ALZ000-MSZ000-100329-

    Mesoscale Precipitation Discussion 0053
    NWS Weather Prediction Center College Park MD
    529 PM EDT Mon Mar 09 2026

    Areas affected...portions of northern MS and AL

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

    Valid 092129Z - 100329Z

    Summary...Backbuilding/training showers and thunderstorms are
    showing some increase in hourly rain amounts as of late. Hourly
    amounts to 2.5" with local totals to 4" are possible, which could
    lead to widely scattered flash flooding.

    Discussion...Showers and thunderstorms have been showing some
    backbuilding and training character across portions of northern MS
    and northern AL, as new activity forms near an instability/thermal gradient/pseudo front and then propagates east, downstream. This
    is occurring within an axis of some low-level confluence and ahead
    of a very positively tilted shortwave moving across southern MO
    and northwest AR, which is adding upper level diffluence.=20
    Precipitable water values are 1.4-1.8". ML CAPE to the south is
    1000-2000 J/kg.

    The 18z GFS-bases GDI implies further increase in cell coverage
    and intensity through at least 00z, which is seen at times within
    the 18z HREF and 12z REFS guidance. The area of low-level
    confluence is expected to shift east with time along with the
    parent upper level shortwave. Given the available ingredients,
    hourly amounts to 2.5" with local totals to 4" are possible.=20
    Given the somewhat lowered flash flood guidance from recent rains,
    flash flooding is expected to be widely scattered in coverage,
    with urban areas most sensitive.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7T4DzFEPuF-viri77kXj2gMO2pn24WoR5Kz3a6HYAWivFfTzypaIbnI3GhL9c0flkEnF= EZ2s8ND0UgNI7BCoUoSLLno$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...JAN...MEG...OHX...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 35138808 35058686 33908502 33328546 32348783=20
    33459038 34388969 35048869=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Mar 10 03:23:16 2026
    AWUS01 KWNH 100323
    FFGMPD
    GAZ000-ALZ000-100715-

    Mesoscale Precipitation Discussion 0054
    NWS Weather Prediction Center College Park MD
    1121 PM EDT Mon Mar 09 2026

    Areas affected...central AL into west-central GA

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

    Valid 100320Z - 100715Z

    Summary...A localized risk of flash flooding will persist across
    central AL into west-central GA through 06Z to 07Z. Training with
    peak rainfall rates of 0.5 to 1.0 inches in 15 minutes and up to
    2-3 inches total rainfall may occur.

    Discussion...03Z radar imagery from KFFC showed an MCV just
    northwest of Atlanta, associated with a weakening convective
    cluster over the AL/GA border. The MCV was tracking steadily
    toward the east and cloud tops have been warming on infrared
    imagery over the past 1-2 hours as instability weakens. However, a
    remnant outflow boundary was analyzed from western GA into central
    AL, and was aligned WNW to ESE or parallel to mean storm movement.
    MLCAPE has been lowering per SPC mesoanalysis trends between 00Z
    and 03Z but 500-1000 J/kg likely remained along and south of the
    outflow boundary.

    Some ascent will remain across the region ahead of a mid-level
    shortwave located over the MO Bootheel at 03Z, with 20-30 kt of
    southwesterly 925-850 mb flow overrunning the outflow boundary
    from MS into AL and GA. While the window for flash flooding is
    shrinking, there will remain some limited potential for an
    additional 1-3 inches of rain from portions of central AL into
    west-central GA.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8cb38SomtAxAHQ4y82lrqMJ0hKANJTS6kQvBRMpFHDlf8E51PDWUYt1xclqDrxVXj8sO= Hl2LrorvMmZK8mizs5DebHw$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...

    ATTN...RFC...ALR...NWC...

    LAT...LON 34078419 34008362 33598306 33148295 32628342=20
    32388406 32398492 32608646 33028760 33638818=20
    34038770 33848674 33768601 33738512=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Mar 10 21:05:00 2026
    AWUS01 KWNH 102104
    FFGMPD
    TXZ000-110300-

    Mesoscale Precipitation Discussion 0055
    NWS Weather Prediction Center College Park MD
    503 PM EDT Tue Mar 10 2026

    Areas affected...Hill Country into Central TX

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

    Valid 102103Z - 110300Z

    SUMMARY...Heavy showers and thunderstorms will be developing and
    expanding in coverage going through the evening hours. High
    rainfall rates capable of exceeding 2 inches/hour along with some
    periodic cell-training concerns will support a threat for some
    areas of flash flooding.

    DISCUSSION...The latest GOES-E WV suite shows a well-defined
    southern stream closed low and associated mid-level trough
    ejecting across northern Mexico. This energy will be gradually
    crossing the Rio Grande Valley going into the evening hours, but
    will be interacting with a very moist and unstable airmass pooled
    across large areas of central TX, including the Hill Country.

    MLCAPE values of 2000 to 3000 J/kg are already in place across the
    region with effective bulk shear values of as much as 40 to 50
    kts. Already CI appears to be underway based on the latest
    satellite and radar data west of a line from Del Rio to San
    Angelo. As the upstream shortwave energy gradually arrives, and
    what is left of the warm mid-level CAP erodes, convection should
    expand rather rapidly near and to the east of a dryline.

    A combination of multicells and supercells are expected within an
    anomalously moist environment characterized by PWs of 1.25+
    inches, with these values running about 1 to 2 standard deviations
    above normal for this time of the year.

    Rainfall rates will be capable of locally exceeding 2 inches/hour
    with the stronger and more organized convective cells, and some
    upscale growth into an elongated MCS is generally expected by
    later this evening. This will be supported by a convergent
    low-level jet reaching 30 to 40+ kts. Some cell-mergers and
    periodic cell-training can be expected, with some localized swaths
    of 2 to 4 inches of rain possible.

    These rains will pose a threat for isolated to scattered areas of
    flash flooding given the high rainfall rates and locally sensitive
    terrain.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-lC1A621pQswQp_M-xmUpnsH_VOPGMbO157Q0JLugxibBst1mQP3Sm5pQQiUFwjHJWHG= cimM2CDb3vHpCd6zyBWqsG8$ for graphic product...

    ATTN...WFO...EWX...FWD...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 33039909 32909793 31959754 30329885 29430014=20
    29290111 29920205 30890183 32310052=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Mar 10 21:31:31 2026
    AWUS01 KWNH 102131
    FFGMPD
    MIZ000-INZ000-WIZ000-ILZ000-IAZ000-110330-

    Mesoscale Precipitation Discussion 0056
    NWS Weather Prediction Center College Park MD
    530 PM EDT Tue Mar 10 2026

    Areas affected...Extreme Southeast WI...Northern IL...Northwest
    IN...Southwest Lower MI

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

    Valid 102130Z - 110330Z

    SUMMARY...Strong to severe thunderstorms will develop and increase
    in coverage this evening. High rainfall rates of 1 to 2
    inches/hour coupled with cell-training concerns will drive a
    threat for flash flooding, including for the Chicago metropolitan
    area, going into the evening hours.

    DISCUSSION...The latest RAP analysis along with surface
    observations shows a quasi-stationary front draped from southeast
    IA through northern IL and into southern Lower MI. Multiple waves
    of low pressure are transiting the front. Meanwhile, the boundary
    layer along and south of the front continues to rapidly
    destabilize with MLCAPE values of 2000 to 3000 J/kg seen nosing up
    across northeast MO through central IL. This is also occurring
    ahead of a wave of low pressure over southern IA.

    Upstream shortwave energy along with the eastward advance of this
    surface low will drive the development and expansion of strong to
    severe thunderstorms across sizable areas of the Midwest over the
    next several hours. This convection is then expected to gradually
    evolve into a couple of larger scale MCS clusters this evening.
    The 18Z HREF guidance and recent special RAOB soundings shows a
    strongly sheared kinematic environment, including along the
    aforementioned front, which coupled with the available instability
    should strongly support supercell thunderstorms at least
    initially. Cell-mergers and upscale growth of MCS activity will
    favor heavy rainfall totals in addition to the severe hazards.

    Rainfall rates of 1 to 2 inches/hour are expected which will be
    aided by a strong low-level jet of 40 to 50+ kts. This enhanced
    moisture and instability transport into the front should persist
    well into the evening ahead of the approaching low center which
    will favor convective sustenance. Cell-training concerns will
    exist in time given nearly parallel alignment of the deeper layer
    steering flow with the front. This will support concerns for as
    much as 2 to 4 inches of rain locally which will drive a threat
    for areas of flash flooding.

    This threat will extend across the more urbanized locations
    including the Chicago metropolitan area. The primary concern for
    excessive rainfall totals for this period will be across northern
    IL, but expect northwest IN and southwest Lower MI to also see
    this threat materialize late this evening and into the overnight
    period.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4tkbRv6AWfHvB_Pfak0CkgURwQLo4u8dMnTMDSaPAgHKgx0kTTqrTSpdB9DQhfin_EFR= f-PCtqkDF8E4XGzveS7td40$ for graphic product...

    ATTN...WFO...DVN...GRR...ILX...IWX...LOT...MKX...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 42718717 42588590 41908557 41268601 40648747=20
    40488904 40759037 41419074 42089016 42548857=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Mar 11 02:16:06 2026
    AWUS01 KWNH 110216
    FFGMPD
    ILZ000-MOZ000-IAZ000-OKZ000-KSZ000-110700-

    Mesoscale Precipitation Discussion 0057
    NWS Weather Prediction Center College Park MD
    1014 PM EDT Tue Mar 10 2026

    Areas affected...southeastern KS into central MO/western IL

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

    Valid 110212Z - 110700Z

    SUMMARY...Training of thunderstorms is likely to produce a SW to
    NE oriented stripe of heavy rain from southeastern KS into
    central/northern MO. Flash flooding will be possible in a few
    areas with 1 to 2 in/hr rates at times over the next 3-5 hours.

    DISCUSSION...Radar imagery from 0150Z showed thunderstorms
    expanding in coverage near Wichita, KS, which was the location of
    a surface low and attendant cold fronts. Another group of
    thunderstorms was located near a surface low in northern MO while
    additional thunderstorm development was expanding between the two
    surface lows along the frontal boundary from eastern KS into
    north-central MO. SPC mesoanalysis and area 00Z soundings within
    the warm sector showed PW values of 1.0 to 1.3 inches and MLCAPE
    of 1000 to 2000+ J/kg from southeastern KS into MO.

    The cold front is forecast to slowly by steadily advance toward
    the southeast over the next few hours but a strengthening low
    level jet with 850 mb wind speeds increasing in coverage and
    magnitude into the 50-60 kt range from southeastern KS into MO,
    will support increasing convergence of storms along the boundary.
    Mean storm movement parallel to the boundary will allow for
    training of cells and 1 to 2 in/hr rainfall rates as the
    cluster(s) of thunderstorms advance eastward with time. Storm
    total rainfall through 07Z of 1 to 3 inches is expected, but much
    of that could fall within 1 to 2 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7bKxiNe35-zdAn05yFCfxvJMNpMjns8sui7UVs8Igzc1H0RcQ9HeB3pmsvKrA6aQ_GWE= JyQD74mTWjIZ3B7e4U5yxeo$ for graphic product...

    ATTN...WFO...DMX...DVN...EAX...ICT...ILX...LSX...OUN...SGF...
    TOP...

    ATTN...RFC...KRF...MSR...TUA...NWC...

    LAT...LON 41239017 40708960 39628964 38639149 37709417=20
    37089624 36969803 37449813 38119730 39309487=20
    39849352 40659244 41159108=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Mar 11 03:27:06 2026
    AWUS01 KWNH 110327
    FFGMPD
    OHZ000-MIZ000-INZ000-ILZ000-110900-

    Mesoscale Precipitation Discussion 0058
    NWS Weather Prediction Center College Park MD
    1125 PM EDT Tue Mar 10 2026

    Areas affected...northeastern IL into northern IN, northwestern OH
    and southern MI

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

    Valid 110324Z - 110900Z

    SUMMARY...Training thunderstorms are likely to result in a few
    areas of flash flooding from northeastern IL into northern IN,
    northwestern OH and southern MI through 09Z. 1 to 2 in/hr rates
    and 2 to 4 inches of storm total rainfall can be expected.

    DISCUSSION...Scattered to numerous coverage of thunderstorms was
    ongoing over portions of the Midwest at 03Z with a training axis
    of cells from west to east through south-central Lower Michigan
    (locally 2+ in/hr), a forward propagating segment from southern
    Lake Michigan into northeastern IL and additional thunderstorms
    upstream. These storms were a combination of surface based and
    elevated with sufficient instability and moisture to produce 1 to
    2 in/hr rain rates where training was occurring.

    Ahead of the approaching upper trough, strengthening 850 mb winds
    of 40-50 kt will spread northward through the Midwest into Lower
    Michigan with overrunning of the front and rain-cooled boundaries
    within the warm sector. These storms will propagate overall in an
    eastward fashion, ahead of large scale ascent associated with an
    amplifying northern stream mid-level trough over the northern High
    Plains. However, areas of training are likely where cells orient
    with the mean steering flow from the west to southwest. A second
    round of convection is expected to approach northern IL from the
    southwest in the 07-10Z time frame tied to thunderstorms moving
    across the mid-MS Valley. 1 to 2 in/hr rain rates will be common
    within areas of training and storm total rainfall of 2-4 inches is
    expected where cell training maximizes through 09Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_YXQzp0WBLGmq37RbsyrVGLD9nd4E_oCY6E_eeiefE_GPYR8u8X96yci7Mb734hL8dC0= IIqkh2POK96yvvxoPpY5ee8$ for graphic product...

    ATTN...WFO...APX...CLE...DTX...DVN...GRR...ILX...IWX...LOT...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 44198346 44028268 43358224 42558233 41758268=20
    41128434 40858614 40758764 40878921 41898928=20
    42468705 43528596 43958454=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Mar 11 05:28:08 2026
    AWUS01 KWNH 110528
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-111000-

    Mesoscale Precipitation Discussion 0059
    NWS Weather Prediction Center College Park MD
    127 AM EDT Wed Mar 11 2026

    Areas affected...central to northeastern TX, southeastern OK and
    southwestern AR

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

    Valid 110526Z - 111000Z

    SUMMARY...Training of heavy rain from SW to NE is becoming
    increasingly likely from portions of central/northeastern TX into
    southwestern AR and possibly southeastern OK. Rainfall rates of
    1-2 in/hr and storm totals of 2-4 inches through 10Z along with
    isolated flash flooding will be possible.

    DISCUSSION...05Z infrared satellite imagery showed two regions of
    colder cloud tops over the Southern Plains, one over eastern OK
    and another over south-central TX. Radar imagery and surface
    observations showed an outflow boundary between these two regions=20
    of convection which extended from just west of Clarksville, TX to
    near Corsicana and southwestward to near Gatesville where the
    boundary intersected an eastward advancing line segment over
    central TX.

    A 50-60+ kt 850 mb low level jet (sampled via VAD wind data from
    KEWX and KGRK) will help to slow the southward advancement of the
    outflow over northeastern TX, and will likely support increasing
    thunderstorm development along and north of the boundary. Low
    level moisture transport will also act to reduce a relative dry
    layer between 850-700 mb as seen on OSPO LPW and RAP analysis
    point soundings across the northern Piney Woods section of
    northeastern TX. Mean steering flow oriented parallel to the low
    level axis of convergence will likely support areas of training as
    the advancing convection presently over central TX makes its way
    eastward. Additional, more discrete convective development will
    also be possible over portions of east-central and northeastern
    TX, out ahead of the advancing convective line, but this potential
    is a bit uncertain. With or without the development of discrete
    cells out ahead of the main cluster, it is appearing more likely
    that areas of training will occur through 10Z from northeastern TX
    into southwestern AR with 1 to 2 in/hr rain rates from training.
    Localized flash flooding will be possible with 2 to 4+ inches of
    peak storm total rainfall expected.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4fbnMO9VYH8iZH3LBiBz9oypgjNWu-931qlX_Mi7QkuuYxAras5dIugajCII3BK1K8LK= O87OCJH8M8shVaHD2v452IE$ for graphic product...

    ATTN...WFO...FWD...HGX...LZK...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 34779291 34469230 33709240 33309280 32509363=20
    31679442 30919577 30989736 31349792 31629802=20
    32099777 32729687 33229614 33829530 34609432=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Mar 11 08:53:12 2026
    AWUS01 KWNH 110853
    FFGMPD
    OHZ000-INZ000-ILZ000-111400-

    Mesoscale Precipitation Discussion 0060
    NWS Weather Prediction Center College Park MD
    452 AM EDT Wed Mar 11 2026

    Areas affected...eastern IL, central IN into northern OH

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

    Valid 110851Z - 111400Z

    SUMMARY...Areas of training will increase the potential for
    localized flash flooding from portions of eastern IL into central
    IN and northern OH through 14Z. Rainfall rates of 1-2 in/hr and
    storm total rainfall of 2 to 4+ inches can be expected.

    DISCUSSION...0830Z regional radar imagery showed a broken and
    elongated axis of thunderstorms from near St. Louis into central
    IL and western IN, followed by another linear segment over
    northeastern IN into northwestern OH. These convective axes were
    located within the warm sector of a WSW-ENE oriented frontal
    boundary, represented by 500 to 1500+ J/kg MLCAPE from
    south-central IL into northwestern OH along with PWs of about 1.0
    to 1.5 inches (08Z SPC mesoanalysis).

    Some minor strengthening of 925-850 mb southwesterly flow (up to
    ~60 kt) is expected to advance from southern IL into IN and
    eventually western OH over the next few hours, helping to focus
    one more more axes of convergence near convectively induced
    outflow boundaries which will at times be in general alignment
    with the mean steering flow from the WSW to SW. This setup will
    support training of heavy rain at times with 1 to 2 inches per
    hour likely within any axes of training.

    Forecasts of instability from the RAP are for a gradual reduction
    through 14Z across IL/IN/OH which will act to decrease rainfall
    intensity but strong divergence within the right-entrance region
    of a powerful 150+ kt upper jet max to the north may help to
    compensate for the forecasts of lessening instability. Therefore,
    a chance for localized flash flooding seems plausible across the
    Midwest over the next 3-6 hours with potential for storm totals of
    2 to 4+ inches.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_Z8cFphTvW_N8XFRMYwpQkbaXxErJGIprrWPEANPT9DQhVwQmEJMv9LGPheKZYpsmAo5= hBXdZ-oVJ1wK-8GuROINSvE$ for graphic product...

    ATTN...WFO...CLE...ILN...ILX...IND...IWX...LOT...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 42108112 41728081 41108194 40548310 39458592=20
    39148846 40248901 41158743 41688553 41668451=20
    41668360 41718284=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Mar 11 09:56:42 2026
    AWUS01 KWNH 110956
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-111500-

    Mesoscale Precipitation Discussion 0061
    NWS Weather Prediction Center College Park MD
    555 AM EDT Wed Mar 11 2026

    Areas affected...northeastern TX into central/southern AR and
    northwestern LA

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

    Valid 110954Z - 111500Z

    SUMMARY...A continued increase in thunderstorm intensity and
    potential training appears likely over the next few hours from
    northeastern TX into central/southern AR and northwestern LA.
    Training of thunderstorms will support hourly rainfall of 1 to 2+
    inches and possible flash flooding through 15Z.

    DISCUSSION...Trends in GOES East infrared satellite imagery over
    northeastern TX through 0930Z have shown an increase in colder
    cloud tops over the past hour, related to an increase in rainfall
    intensity along a narrow convective axis, out ahead of a forward
    propagating convective line extending from the southern OK/AR
    border into east-central TX. This activity was located to the
    north of a weakly defined outflow boundary which has made it all
    the way to the Houston metro and the recent uptick appears to be
    related, at least in part, to increased low level moisture seen
    advecting north on OSPO ALPW imagery in the surface to 700 mb
    layer over eastern TX/western LA. Confluent flow just above the
    surface located beneath modestly diffluent upper level winds was
    observed over the TX/AR border where 500-1500 J/kg MLCAPE was
    estimated on the 09Z SPC mesoanalysis with little to no inhibition.

    Low level moisture transport into the region and low level
    confluence appear to remain in the short term forecast across the
    ArkLaTex and eastward into southern AR and northwestern LA. Given
    sufficient instability looks to remain present across the region
    over the next 3-6 hours via recent RAP forecasts, an axis of heavy
    rain looks likely to setup from northeastern TX into AR/LA. While
    this expected SW to NE axis of heavy rain should generally move
    from west to east, there is the potential for the southwestern
    flank of the axis to stall, supporting the potential for increased
    training and rain rates that could exceed 2 in/hr. However, more
    likely rain rates within training should fall in the 1-2 in/hr
    range. Through 15Z, 2 to 4+ inches of rain will be possible, much
    of which could fall within 2-3 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9uI-asL2kWpYIuDXduHCMxNuxYzA8JgQ7Ajo5KuVy07eO8Qqht4G9OoHK1K5yMdEgfj6= 8Bl-L0RfqDeiXC9FeahlHVw$ for graphic product...

    ATTN...WFO...HGX...JAN...LZK...MEG...SHV...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35309103 34999037 33429120 31619338 31059480=20
    31729528 33069475 34859258=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Mar 11 16:52:15 2026
    AWUS01 KWNH 111652
    FFGMPD
    NYZ000-PAZ000-WVZ000-OHZ000-KYZ000-INZ000-ILZ000-112250-

    Mesoscale Precipitation Discussion 0062
    NWS Weather Prediction Center College Park MD
    1250 PM EDT Wed Mar 11 2026

    Areas affected...Portions of the OH Valley and Lower Great Lakes

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

    Valid 111650Z - 112250Z

    SUMMARY...Broken clusters of locally heavy showers and
    thunderstorms will continue through the afternoon hours. Locally
    high rainfall rates, moistening antecedent conditions and some
    cell-training concerns will maintain a threat for additional
    runoff problems including isolated to scattered areas of flash
    flooding.

    DISCUSSION...The latest GOES-E satellite imagery along with radar
    shows broken clusters of heavy showers and thunderstorms advancing
    across the OH Valley and Lower Great Lakes region. More broadly,
    this activity is associated with strong warm air advection and
    moisture transport continuing to lift northeastward ahead of a
    wave of low pressure over southern Lower MI by also with the
    advance of multiple shortwave impulses across the region.

    Warm-sector diurnal heating with increasing solar insolation is
    noted over central and southern OH and extending back to the
    southwest over northern KY, southern IN and southeast IL. This has
    allowed for these areas to increasingly destabilize, and MUCAPE
    values of 1000 to 1500 J/kg are noted here with 3-hour MUCAPE
    differentials of locally 250 to 500+ J/kg seen from far southern
    IN and northern KY through central WV. This is allowing for a
    well-defined differential heating/outflow boundary to establish
    itself which is expected to become an increasing focus for
    convection going through the afternoon hours. This will further be
    facilitated by arrival of a new shortwave impulse from the Midwest
    which should yield favorable 400 to 700 mb DPVA within the broader
    warm air advection regime to drive deeper layer ascent.

    Meanwhile, areas downstream over western PA and far western NY are
    under the influence of a lead shortwave impulse with focused warm
    air advection and DPVA yielding broken areas of convection. Some
    hints at mesocyclone activity is noted in radar over Lake Erie,
    and this may help to bring locally focused rains into far western
    NY in a couple of hours. The 12Z HREF/06Z REFS guidance does
    attempt to bring the upstream convection back over some areas of central/southern OH through northern WV and southwest PA later
    today.

    Expecting a gradual uptick in rainfall rates capable of reaching
    1.5"/hour with the stronger storms. Given the cell-training
    concerns near the aforementioned differential heating/outflow
    boundary, some additional rainfall totals of 2 to 3 inches will be
    possible. This will pose a threat for isolated to scattered areas
    of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4epEr0m_uTWVSbIfLr7vCQwmeFuPccCynI3AOkF4kTvyEbQ64setvRY_4fU5ij9gNgh0= Y3tb4NkGOR-qT7LFqWi1mCs$ for graphic product...

    ATTN...WFO...BUF...CLE...CTP...ILN...ILX...IND...IWX...JKL... LMK...LSX...PAH...PBZ...RLX...

    ATTN...RFC...MSR...RHA...TAR...TIR...NWC...

    LAT...LON 42827882 42437812 40997863 39528042 38428376=20
    37878744 38018892 38448943 38948890 40148540=20
    40948307 42168059=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Mar 15 18:42:13 2026
    AWUS01 KWNH 151842
    FFGMPD
    FLZ000-160000-

    Mesoscale Precipitation Discussion 0063
    NWS Weather Prediction Center College Park MD
    240 PM EDT Sun Mar 15 2026

    Areas affected...South FL

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

    Valid 151840Z - 160000Z

    SUMMARY...Slow-moving clusters of showers and thunderstorms with
    extreme rainfall rates may cause flash flooding going through
    early this evening. This could include some urban impacts.

    DISCUSSION...The latest GOES-E IR satellite imagery along with
    radar shows slow-moving clusters of very heavy showers and
    thunderstorms impacting portions of Miami-Dade and Collier
    Counties.

    This convection is focusing within a moist and unstable
    environment characterized by MLCAPE values of 1500 to 2500 J/kg
    and PWs of 1.5 to 1.7 inches. Some modest shear is in place with
    as much as 20 to 30 kts of effective bulk shear. Much of the
    activity recently though is tending to get its focus along the
    presence of multiple mesoscale boundaries including outflow and
    sea-breeze boundaries where there is small-scale convergence
    working with the favorable thermodynamic environment.

    Some modestly divergent flow aloft is noted also given proximity
    of a weak shortwave west of the FL Straits and Cuba. This modest
    deep layer ascent coupled with colliding surface boundaries should
    tend to keep the convective threat maintained going into the
    evening hours before sufficient levels of instability exhaustion
    occurs to promote a weakening trend of the convection.

    Already parts of the FL Everglades in Miami-Dade County have seen
    over 5 inches of rain, with much of the activity staying away from
    the urban areas. However, over the next few hours there will still
    be a threat locally for some of these stronger thunderstorms and
    heavier rainfall rates to impact the more populated areas of
    southern FL which in this case will extend to the the southwest
    coast including areas from Ft. Myers down through Naples. The
    southeast coast of FL meanwhile from Miami down to Homestead will
    still need to closely watch some of these slow-moving cells.

    Rainfall rates of 2 to 4 inches/hour and storm totals locally
    exceeding 5 inches are expected where any cells become anchored.
    Earlier runs of the HRRR and RRFS were suggesting this near parts
    of southwest FL in particular. As such, some areas of flash
    flooding will be possible given the very high rainfall rates and
    totals which may include some urban impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6VYKq4ZHl918Q3pvMYHNoqpOeYvAl-jH0wrrSGBnRCSi1o3jC2LsBNc7NHfFUTvg-7RE= -pJF1ZBRxkXB7uyLw6uPMHo$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 27018174 26468098 26118014 25657992 25178031=20
    25298104 26088186 26738218=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Mar 26 20:47:21 2026
    AWUS01 KWNH 262047
    FFGMPD
    NYZ000-PAZ000-WVZ000-OHZ000-270230-

    Mesoscale Precipitation Discussion 0064
    NWS Weather Prediction Center College Park MD
    446 PM EDT Thu Mar 26 2026

    Areas affected...Northern Ohio...Western & Central PA... Southwest
    NY...

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

    Valid 262045Z - 270230Z

    SUMMARY...Saturated upper-layer soils/low FFG may be locally
    exceeded given potential for quick burst thunderstorms capable of
    .5-.75"/hr rates and localized totals of 1.5-2", especially
    in/near corridor or two of repeating cells.

    DISCUSSION...A strong 150-180kt 250mb zonal jet is streaking
    across the northern Great Lakes into southern Quebec with a subtle
    but sufficiently diffluent right exit region across the Lower
    Great Lakes this afternoon. In response, strong southwesterly
    warm-air advection regime is drawing higher moisture and slightly
    above normal higher theta-E air across the northern Ohio Valley
    into the Allegheny Plateau. Low level flow is solid per VWP with
    35-45kts of 925-850mb flow from the southwest with sufficient
    veering through 700-500mb to allow for a fairly unidirectional
    steering flow, with allowable for upstream redeveloping cells to
    potentially repeat across the area of concern late this afternoon
    into evening.=20

    At the surface a well defined front extends from the main surface
    low in SE IA across the southern LP of Michigan where secondary
    weaker wave exists, likely responding to the mid-level
    shortwave/diffluence pattern aloft. Surface moisture convergence
    in proximity to the surface front is further enhanced by cooler
    Lake Breeze and sharper low level temperature gradient along the
    southern coasts. This isentropic boundary in the low level flow
    regime will support enhanced moisture convergence at the
    northwestern nose of the mid-level instability pool upstream over
    IL/IN/NW OH. Available moisture is slightly above average with
    total Pwat values AoA 1.25", though the bulk is below 700mb and
    any thunderstorm development will help to load in the lower
    profiles providing some increased rainfall potential. Forward
    propagation will be very fast limiting overall duration, but
    Hi-Res CAMs include recent WoFS runs suggest isolated but broader
    updrafts capable of the very quick bursts of .5-.75" in 15-30 minutes...particularly further west and deeper into the more
    unstable (1500+ J/kg MUCAPE), higher moisture.=20

    However, the hydrological ground conditions are very sensitive as
    green-up is just about to start. FFG values are below average
    with hourly values about 1" reducing to .5-.75" across northern PA
    into S central PA. NASA SPoRT LIS products show 0-40cm saturation
    values over 60% increasing to over 80% where the lowest FFG value
    are; so even less vertically intense showers/thunderstorms capable
    of .25-.5"/hr rates downstream into NY/Central PA are likely to
    shed nearly all rain toward runoff. The overall magnitudes and
    coverage are likely to be limited in scope and lower end, but
    still pose a possible incident or two of flash flooding. This is
    also a concern across the larger urban centers of NE OH toward
    Pittsburgh metro later this evening.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9JCEIU5YItr7GdI7YePu8DnzptH-WUp77K6dlDwxPSN7BGp-1c-UvyeeyqpzQ03SeznQ= 4fb5sFTjjRsN87RHTbZVBP8$ for graphic product...

    ATTN...WFO...BGM...BUF...CLE...CTP...ILN...IWX...PBZ...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 42667650 42057570 41177590 40477698 40127924=20
    40008191 39968419 40858437 41558200 42068053=20
    42287976 42627812=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Mar 31 08:26:12 2026
    AWUS01 KWNH 310826
    FFGMPD
    NYZ000-311425-

    Mesoscale Precipitation Discussion 0065
    NWS Weather Prediction Center College Park MD
    425 AM EDT Tue Mar 31 2026

    Areas affected...Western and Central New York

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

    Valid 310825Z - 311425Z

    SUMMARY...An broken and fairly organized band of heavy showers and thunderstorms will move into western and central New York going
    through the morning hours. Locally heavy rainfall rates and some
    potential cell-training concerns will couple with moist antecedent
    conditions and areas of melting snow to foster a threat for
    localized flash flooding.

    DISCUSSION...Recent regional radar mosaics and GOES-E infrared
    satellite imagery indicate that previously scattered convection
    over southern Ontario and Lower Michigan has congealed into a
    broken, linear band of semi-organized convection. Cloud tops have
    cooled significantly, denoting vigorous, sustained updrafts and
    thus a trend toward heavier rainfall rates.

    This activity is being driven by multiple upstream waves of low
    pressure over Lower Michigan that are transiting a stalled surface
    boundary draped across the Lower Great Lakes. Out ahead of these
    surface waves, the kinematic and thermodynamic environment is
    favorable for heavy, and locally training areas of convection
    which should enter western New York over the next couple of hours.
    A robust 50+ kt west-southwesterly low-level jet is nosing
    directly into the region, and this is generating intense speed
    convergence and enhanced warm air advection. The resultant
    isentropic ascent and forcing along the front coupled with the
    nose of modest instability with MUCAPE values of 500 to 1000 J/kg
    should allow for the upstream convective mass to advance east
    across western and eventually parts of central New York going
    through the morning hours.

    Rainfall rates are expected to climb into the 0.50" to 1.0"/hr
    range which is supported by the 00Z HREF guidance. Given the
    cell-training concerns, some rainfall totals this morning may
    reach 1.5 to 3.0 inches. The HREF guidance shows the highest
    probabilities of this generally near the Lake Ontario shoreline
    and the I-90 corridor.

    NASA SPoRT soil moisture and USGS streamflow data suggests an
    increasingly moist and sensitive environment that will be
    conducive for this morning's rainfall leading to an increase in
    runoff concerns. Some snowmelt over the Tug Hill Plateau region is
    ongoing and will further contribute to the risk. Thus, the threat
    for at least localized areas of flash flooding will exist which
    will include the highly urbanized I-90 corridor (Buffalo to
    Syracuse) and some of the adjacent steeper terrain.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8AHCzXz7s8TCfOg5ZP_VnIr4GREdIeEiVWfpL-qrMuZ5n0hODg8DcruXkoSt3K8v-wao= 1Z5e0VivG1oCnPGwt5-e5gw$ for graphic product...

    ATTN...WFO...ALY...BGM...BUF...

    ATTN...RFC...RHA...TAR...NWC...

    LAT...LON 44027576 43927446 43487388 42797394 42387468=20
    42307618 42467812 42797920 43377915 43497815=20
    43557751 43597685=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Mar 31 17:33:17 2026
    AWUS01 KWNH 311733
    FFGMPD
    NYZ000-PAZ000-312330-

    Mesoscale Precipitation Discussion 0066
    NWS Weather Prediction Center College Park MD
    132 PM EDT Tue Mar 31 2026

    Areas affected...West-Central New York...Northern Pennsylvania

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

    Valid 311730Z - 312330Z

    Summary...Training thunderstorms along a stationary front will
    support additional instances of flash flooding this afternoon as
    they overlap with moist antecedent soil conditions in west-central
    New York and northern Pennsylvania.

    Discussion...Airmass recovery is underway across portions of
    west-central New York and northern Pennsylvania as remnant heavy
    showers and thunderstorms from this morning depart the area ahead
    of a weak shortwave. Within the first round of storms, periodic
    cell-training led to an estimated 1-3" of rainfall near the Tug
    Hill Plateau per recent MRMS and NYS Mesonet data, which led to at
    least one report of flooding near Phelps, New York earlier this
    morning.

    While the first round exits, elevated thunderstorms are
    approaching upstream from the Midwest and Ontario as a 40 kt low
    level jet interacts with a shortwave and right entrance region
    ascent amid widespread 7-8 degree mid-level lapse rates. Over the
    next 3-4 hours, the RAP suggests this forcing will lift into the
    Northeast and support an environment characterized by 1000-1500
    J/kg of MLCAPE and 40-50 kts of effective bulk shear.

    Accordingly, CAMS are in good agreement for upstream storms to
    intensify and train with new development expected over western New
    York and northwest Pennsylvania this afternoon, even if they are
    too slow with the activity in the Ohio Valley. As these training
    storms eclipse 1-1.5"/hr rainfall rates at peak intensity this
    afternoon, additional instances of flash flooding are possible
    owing to the low FFG values over portions of west-central New York
    and northern Pennsylvania -- as low as 0.25-0.5"/hr in places.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5EJ-CgQX9tgN6nfLF0Fa6tiHXcmuxFoMcHFultO3zE69V3JEza4xWbKeQtuTn9gKjaR6= KwIuCGdxbVLgYyQfTr9zw60$ for graphic product...

    ATTN...WFO...ALY...BGM...BTV...BUF...CLE...CTP...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 44307567 44047418 43257383 42387405 41997487=20
    41857593 41787794 41977970 42797992 43527915=20
    43647722=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Mar 31 22:48:54 2026
    AWUS01 KWNH 312248
    FFGMPD
    OHZ000-INZ000-010300-

    Mesoscale Precipitation Discussion 0067
    NWS Weather Prediction Center College Park MD
    647 PM EDT Tue Mar 31 2026

    Areas affected...Northeastern Indiana and Northern Ohio

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

    Valid 312247Z - 010300Z

    SUMMARY...A line of training showers and thunderstorms could cause
    localized flash flooding across northeastern Indiana and northern
    Ohio.

    DISCUSSION...A line of storms, demarcated by a pair of segments of
    much more intense convection, has set up across northern Indiana
    and Ohio this afternoon. The initial segment of storms is
    weakening across far northeast Ohio and far western PA. The back
    segment of storms is closing in on Ft. Wayne, IN. In between, some
    weaker showers and storms have set up in an east-west line, with
    the storms also tracking east, resulting in training. The stronger
    storms in the back segment over Indiana have a history of
    producing rainfall rates to 1.5 inches per hour.

    Most high-resolution model guidance, while behind where the storms
    actually are by about 2 hours, still suggest that the back segment
    in Indiana will "fill-in" as it moves east, resulting in an
    east-west oriented cluster of more intense convection where
    individual cells embedded within the cluster train over the same
    areas. PWATs are over 1.25 inches into the Ohio Valley, and CAPE
    values are between 1,000 and 2,000 J/kg into central Illinois and
    Indiana. Combined with sufficient forcing along the front, the
    setup suggests that the storms will have no trouble keeping storms
    intense and capable of heavy rainfall through the late afternoon.
    Flash flood guidance of 1.5-2 inches in 3-hours over most of
    northern Ohio should be exceeded given the 1.5+ in/hr rates
    already seen with the storms over Indiana, especially as the area
    in between the segments of storms fills in over the next couple
    hours or so.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9katCsrILRBviETCD9baUTBW-entNocx3aUDfVX0zPtQ1-_gWeFWjQKpZxCjtuj3LBoR= n5aJas2ZuX-LnVZ95p0DOIY$ for graphic product...

    ATTN...WFO...CLE...ILN...IWX...PBZ...RLX...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 41428566 41388486 41388354 41338219 40998116=20
    40188133 39788205 39858257 40018339 40278406=20
    40528477 40908555=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Mar 31 23:34:54 2026
    AWUS01 KWNH 312334
    FFGMPD
    NYZ000-PAZ000-OHZ000-010500-

    Mesoscale Precipitation Discussion 0068
    NWS Weather Prediction Center College Park MD
    733 PM EDT Tue Mar 31 2026

    Areas affected...Western New York and Northwestern Pennsylvania

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

    Valid 312332Z - 010500Z

    SUMMARY...Additional convection moving into western Pennsylvania
    and New York will likely cause more flash flooding into the
    evening as additional line segments of storms move over previously
    hard-hit and low FFG areas.

    DISCUSSION... A series of line segments of showers and
    thunderstorms are quickly moving eastward out of Ohio and the
    Ontario Peninsula towards western New York and Pennsylvania. Very
    low FFGs are in place across much of western New York from ongoing
    or recently ended storms. As the next round of storms approaches,
    additional rainfall will be moving over areas with ongoing
    flooding, or in the case of portions of western Pennsylvania, over
    areas with low FFGs such that new flooding is likely as the storms
    continue to produce occasional rainfall rates exceeding 1" per
    hour. Diminishing daylight will help to gradually lower the
    instability and potential rainfall rates, however, even somewhat
    lighter rainfall under an inch per hour, with sufficient duration,
    will cause flash flooding.

    As the storms move across New York and Pennsylvania, they remain
    likely to align in a roughly west-to-east line, allowing training
    from multiple heavier rain cells to move over the same areas.
    Thus, while rainfall rates may decline with time, training over
    low FFG areas should still result in some flooding. This is in
    large part due to a 40-50 kt LLJ tracking WNW across the region,
    supplying moisture and instability to the warm environment ahead
    of the front, but at an angle sufficiently parallel to the front
    to support multiple rounds of training thunderstorms.

    Late this evening, all the activity is expected to sink south
    across Pennsylvania and weaken with time as nocturnal, more stable
    air builds, thus ending the rain threat.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5e9nYAagNkdaLmiARDmb5B-J7MLVifvbNFdGo3hkmYXuJtkjw9XZ1oWUyCPemCjLUfDu= WEZ4i5EVs1mqfDGjSL66QBI$ for graphic product...

    ATTN...WFO...ALY...BGM...BUF...CLE...CTP...PBZ...

    ATTN...RFC...RHA...TAR...TIR...NWC...

    LAT...LON 43427851 43347775 43287753 43307704 43307683=20
    43087627 42977548 42837468 42627382 41957389=20
    41857413 41547507 41197581 40797663 40507758=20
    40447868 40357938 40508016 41008064 41948069=20
    42547933 42847890 43047908 43307904=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Apr 1 02:56:58 2026
    AWUS01 KWNH 010256
    FFGMPD
    PAZ000-WVZ000-OHZ000-INZ000-010855-

    Mesoscale Precipitation Discussion 0069
    NWS Weather Prediction Center College Park MD
    1055 PM EDT Tue Mar 31 2026

    Areas affected...Central and Eastern Indiana...Ohio...Western
    Pennsylvania

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

    Valid 010255Z - 010855Z

    SUMMARY...Organized clusters of heavy showers and thunderstorms
    will continue to track across the Ohio Valley overnight. Training
    of convective cells will lead to additional localized rainfall
    amounts of 2 to 3 inches. Given wet antecedent conditions,
    isolated to scattered flash flooding is likely, particularly in
    urban areas and locations that have seen prior rainfall.

    DISCUSSION...Regional radar mosaics indicate a broad, active
    corridor of convection extending from central Indiana through Ohio
    and into western Pennsylvania. This activity is being driven by a
    persistent 40 to 50 kt west-southwesterly low-level jet that is
    maintaining strong moisture convergence and isentropic ascent over
    convectively induced outflow boundaries south of a slow-moving and
    largely stalled synoptic front.

    While absolute instability and moisture are modest, the highly
    favorable kinematics and the continuous convective regeneration
    along these boundaries are resulting in localized pockets of
    cell-training. Current MRMS instantaneous rainfall rates are
    generally 0.50 to 1.0 inch per hour, but are peaking as high as
    1.0 to 1.5 inches per hour occasionally with the strongest and
    most anchored cores.

    High-resolution guidance, including the 18Z HREF and latest HRRR
    runs, indicates this low-level jet will remain robust through much
    of the overnight hours before gradually weakening after 09Z. As a
    result, this regenerative convective threat will tend to be
    sustained at least over the next several hours. In time,
    additional slackening of the instability will tend to weaken the
    activity and lessen the rain rates. Nevertheless, additional
    localized rainfall totals of 2 to 3 inches are expected along the
    primary training axes overnight.

    Recent rainfall has left antecedent soil conditions wet to
    saturated across portions of the region, promoting significantly
    lower FFG thresholds. The combination of primed basins, fairly
    efficient rainfall rates, and rainfall duration will lead to areas
    of rapid runoff. As a result, isolated to scattered instances of
    flash flooding are considered likely, with an elevated threat for
    urban corridors and the sensitive terrain of western Pennsylvania.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5Cqq3Qkxda1cDhhl-m2210Q2IB8-1NPKXUSotooev16O4acN3ywmZbbQOEeHSEHgNphV= lpQWRHzZa9mdWjIbBM7F6J0$ for graphic product...

    ATTN...WFO...CLE...CTP...ILN...IND...IWX...PBZ...RLX...

    ATTN...RFC...MSR...RHA...TIR...NWC...

    LAT...LON 41917964 41667841 41117789 40387837 40058033=20
    39898267 39958431 40068543 40418605 40978622=20
    41488551 41678458 41628250 41868093=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Apr 2 00:01:44 2026
    AWUS01 KWNH 020001
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-020600-

    Mesoscale Precipitation Discussion 0070
    NWS Weather Prediction Center College Park MD
    800 PM EDT Wed Apr 01 2026

    Areas affected...Northeastern Oklahoma & Southeast Kansas into
    Central Missouri

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

    Valid 020000Z - 020600Z

    SUMMARY...Clusters of storms developing along a nearly stationary
    frontal boundary and developing area of low pressure are training
    and merging within the clusters as they track northeast. Despite
    very dry antecedent soil conditions, rainfall rates to 2 inches
    per hour with each strong cell will cause widely scattered
    instances of flash flooding.

    DISCUSSION...Cyclogenesis along a stationary frontal boundary is
    underway across southeast Kansas this evening. A cluster of storms
    have developed southwest of the low, and is quickly congealing
    with other storms that have developed roughly along the
    Kansas-Missouri border south of Kansas City. The storms across
    Oklahoma have a history of producing rainfall rates to 2 inches
    per hour. Any hail with the storms should diminish with time as
    the atmosphere more fully saturates in and around the cluster of
    storms. Thus, the heavy rainfall threat will increase into the
    night. The low center will likely merge with a second low and
    Pacific front which is back to the west (not shown). These two
    features approach to each other will stall the eastward
    progression of the storms over the next several hours, allowing
    additional time for training convection to produce heavy rain.

    Antecedent soil conditions are bone dry across all of the
    highlighted area, so it may take another couple hours of heavy
    rainfall across the warned area before flooding can occur. Locally
    however, any areas under an extended duration of heavy rain could
    see localized flash flooding occur sooner. PWATs to 1.6 inches are
    being advected into the low on 30-40 kt southerly winds at 850 mb,
    which will sustain the storms into the overnight as that same
    low-level-jet intensifies above 50 kts once the second Pacific
    front catches up to the storms.

    More substantive eastward progression of the complex is expected
    late tonight, after 06Z, as the Pacific front catches up to the
    stationary boundary of storms and pushes everything off to the
    east. This will substantially diminish the flash flooding threat
    for this portion of the Plains.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!67PWvjvzgF5U3nymtUVCkJZO5-yAqUJy5QknMaWNxx8umxVicCfAnM6P3mTvaFirmEm1= VPlHiKZWo96NK2E-cjjv8po$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...OUN...SGF...TOP...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 39889203 39669129 39089118 38339159 37269250=20
    36149391 35629503 35399613 35509702 35949717=20
    36489724 37049714 37489664 37869625 38649564=20
    39219497 39359466 39519416 39629374 39789302=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Apr 2 05:31:49 2026
    AWUS01 KWNH 020531
    FFGMPD
    MOZ000-OKZ000-KSZ000-021029-

    Mesoscale Precipitation Discussion 0071
    NWS Weather Prediction Center College Park MD
    129 AM EDT Thu Apr 02 2026

    Areas affected...far eastern Kansas, western/central/southern
    Missouri

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

    Valid 020529Z - 021029Z

    Summary...Locally significant flash flooding continues -
    particularly across west-central Missouri. Another 2-3 hours of
    moderate to heavy rainfall are expected, potentially exacerbating
    ongoing flash flooding.

    Discussion...An axis of training convection has persisted along a southwest-to-northeast oriented line from just west of Columbia to
    about 50 miles north of Joplin. Along this axis, persistent
    rainfall has resulted in around 2-6 inches of rainfall in the past
    6 hours. The rainfall is being supported by strong southerly
    low-level flow (~40 knots at 850mb) impinging on a remnant outflow
    boundary from earlier storms. Deep southwesterly steering flow
    aloft was enabling additional convective elements to develop
    initially from a slightly more buoyant airmass over southeastern
    Kansas and move northeastward along this axis. Heavy rain has
    resulted in numerous road closures tonight.

    Additional heavy rainfall is expected across the impacted region.=20
    Deep convection extends from near Joplin southwestward to the
    Oklahoma/Kansas border near Bartlesville that will migrate
    east-northeastward. The clearing line behind this activity is
    roughly along US 75 (near a propagating MCS) and will take another
    2-4 hours to clear the region. Flash flooding is expected to
    continue (and perhaps worsen) through 10Z/5a central.

    Farther south and east, dry antecedent conditions and the
    forward-propagating nature of the Oklahoma/Kansas linear
    segment/MCS should result in lower chances for flash flooding
    overall. Low-water crossing and sensitive spots will have the
    greatest risk of isolated flash flooding in this regime.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!96GsjcHescerhJ3lgQ1A_gnKd4VW2UJIOnsXQXRJG4FnT6XwEYGU8_Q5qKm5fK_XSf6x= XQ3WmURy7ynKUQ7yom-iMMo$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...SGF...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 39379336 39269155 37939119 36669237 36579402=20
    37059514 37569530 38519466=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Apr 2 19:06:29 2026
    AWUS01 KWNH 021906
    FFGMPD
    WIZ000-ILZ000-IAZ000-030030-

    Mesoscale Precipitation Discussion 0072
    NWS Weather Prediction Center College Park MD
    305 PM EDT Thu Apr 02 2026

    Areas affected...Southern WI...Eastern IA...Northern IL

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

    Valid 021900Z - 030030Z

    SUMMARY...Periods of heavy rainfall within approaching
    thunderstorms may result in localized flash flooding this
    afternoon, potentially impacting the afternoon commute.

    DISCUSSION...A narrow band of heavy rainfall north of I-80 is
    making its way through eastern IA, northwest IL, and southern WI.
    This focused area of mesoscale enhanced rainfall is due to strong
    50-60kt 850mb winds out of the SW that are intersecting the
    surface warm front as it lifts north. The Midwest is also feeling
    the effects or a negatively-tilted 500mb vorticity maximum that is
    crossing east of the MO River this afternoon, generating
    exceptional upper-level divergence atop the atmospheric column.
    The highlighted region features >1.25" PWs, values that are above
    the 99th climatological percentile. Meanwhile, strong
    thunderstorms have flared up along the surface cold front in
    southern IA and northern MO. MUCAPE is likely to range between
    500-1,000 J/kg this afternoon as the warm sector races in aloft.
    These storms are progressive, but are heading northeast towards
    the same section of southern WI, northern IL, and eastern IA that
    are seeing MRMS radar estimated rainfall rates over 0.5"/hr. HRRR
    sampled soundings show warm cloud layers as deep as 10,000ft, so
    while rates may not be overly impressive, the rainfall itself
    features some supportive warm-rain processes aloft.

    In most cases, these areas would handle 0.5"/hr rainfall rates
    fairly well. That said, 1-hr FFGs are generally between 1.0-1.5"
    and with MUCAPE values gradually increasing as the warm sector
    encroaches, the band of rainfall currently in progress and the
    approaching storms could generate hourly rainfall rates up to
    1"/hr over the next several hours. Showers and storms remain
    progressive, thus limiting the areal extent and capping the
    severity of the potential for flash flooding. However, any areas
    that contend with both the ongoing band of heavy rain in eastern
    IA, northwest IL, and southern WI that then see the more intense
    storms pass through this afternoon could encounter some localized
    flash flooding and ponding. Any ponding on roadways could cause
    some trouble for motorists during the afternoon commute. More
    heavily urbanized locations containing a larger concentration of
    hydrophobic surfaces are particuarly prone to flash flooding, as
    well as low-lying areas and typical spots that drain poorly.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4kI67TM1hzkNwiHmOSK6m1yN5LwLWpPS3lCNlXFC-Yg9N8M29zrJZ7LNa5kbZ4sXjl3B= DOoNLcqj2eA1r7UuMCigUkk$ for graphic product...

    ATTN...WFO...ARX...DVN...GRB...LOT...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 44098771 43658752 43058766 42608790 41848894=20
    41488991 41449125 41799184 42539174 42929097=20
    43488964 44088827=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 3 19:49:47 2026
    AWUS01 KWNH 031949
    FFGMPD
    PAZ000-WVZ000-OHZ000-INZ000-040150-

    Mesoscale Precipitation Discussion 0073
    NWS Weather Prediction Center College Park MD
    348 PM EDT Fri Apr 03 2026

    Areas affected...Lower Great Lakes & Western PA

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

    Valid 031950Z - 040150Z

    SUMMARY...Progressive but potentially training thunderstorms have
    the potential to generate rainfall rates over 1.5"/hr. Locally
    saturated soils could be particularly at-risk for flash flooding
    this afternoon and evening.

    DISCUSSION...Daytime heating and low-level theta-e advection has
    destabilized the atmosphere from central IN all the way to western
    PA with as much as 500-1,000 J/kg of MLCAPE having become
    available in the past 3 hours per RTMA. Mesoscale guidance is
    showing as much as 1.5" PWs will be available over the western
    half of the at-risk region while PWs range between 1.2-1.5" over
    eastern OH and western PA. All PWs referenced are comfortably
    above the 90th climatological percentile. Mean winds within the
    850-300mb layer are running nearly parallel to a quasi-stationary
    front located over northern OH and along the Chautauqua Ridge.

    As differential heating along the front strengthens and convective
    temperatures over the OH Valley are reached, widespread showers
    and storms will develop and track WSW to ENE this afternoon and
    evening. Storms tracking parallel to the front with no change in
    the mean storm motion will support the potential for training and
    even back-building storms this afternoon. Soils in the region have
    grown increasingly saturated, particularly eastern OH and western
    PA where MRMS soil moisture values are between 50-75% saturated.
    12Z HREF shows low chances (10-30%) for 3-hr QPF totals surpassing
    3-hr FFGs in northern OH between 21Z and 00Z this afternoon, with
    similar low chance probabilities in far western PA. Eastern IN is
    farther east of the better probabilistic guidance, but some recent
    CAMs runs have shown some potential for 1.5"/hr rainfall rates in
    developing cells.

    The progressive motion of these cells should limit storm residency
    times, but with redeveloping storms expected to the south and
    west, training of storms containing up to 1.5"/hr rainfall rates
    are possible. 1-hr FFGs for much of the area range between
    1.0-1.5" as well, making it possible for areas of flash flooding
    to occur this afternoon. Low-lying and poor drainage areas are
    at-risk, including more urbanized locations.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8l5tZCQ8U5jzSFpiqd3uD1sg9sw9HuwEmBUXx4_VUkwfn2SsR8DwDeLNy7zNTLlPDV96= lh7H6-9qcXBSYaN0UwToY5s$ for graphic product...

    ATTN...WFO...CLE...CTP...ILN...IND...IWX...PBZ...RLX...

    ATTN...RFC...TIR...NWC...

    LAT...LON 41877921 41557891 41047925 40688006 40088151=20
    39928202 39508341 39318469 39408562 40318614=20
    40828559 40998427 41158336 41368168 41728016=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 3 21:02:49 2026
    AWUS01 KWNH 032102
    FFGMPD
    TXZ000-OKZ000-040300-

    Mesoscale Precipitation Discussion 0074
    NWS Weather Prediction Center College Park MD
    501 PM EDT Fri Apr 03 2026

    Areas affected...Southern OK & Northern TX

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

    Valid 032100Z - 040300Z

    SUMMARY...Strong-to-severe thunderstorms flaring up along and
    ahead of the dryline and an approaching cold front will back-build
    this afternoon and produce rainfall rates up to 2"/hr. Instances
    of flash flooding are likely.

    DISCUSSION...Doppler Radar and GOES East satellite imagery show
    thunderstorms erupting along the cold front over southern KS and
    near the dryline from the Red River on south and west. There is no
    shortage of instability as RAP mesoanalysis shows anywhere from
    2,000-3,000 J/kg of MLCAPE present. PWs currently are less than
    1.5" where storms are initiating. That will soon change as
    southerly low-level flow sustains the ongoing 850mb theta-e
    advection. Meanwhile, the cold front diving south will slow down
    as southerly low-level winds intersect the boundary, allowing for
    a prolonged window of low-level forced ascent into a highly
    unstable environment. PWs will soon top 1.5" as the LLJ
    strengthens and warm cloud layers gradually deepen as the evening
    approaches.

    Excellent vertical wind shear aloft (40-50 kts effective bulk
    shear) and increasingly curved low-level hodographs containing as
    much as 100-200 m2/s2 of effective SRH will support supercells at
    the onset before congealing into a more organized linear cluster
    of storms this evening. Where mesocyclones develop, rainfall rates
    can be enhanced and exceed 2"/hr in some cases. The concern for
    locally significant flash flooding is due to the slowing of the
    cold front and the receding dry line as it backs up to the west.
    Several hours worth of southerly flow into these frontal
    boundaries combined with beneficial vertical wind profiles can
    give rise to back-building thunderstorms from north TX into
    central and northeast OK through this evening. 12Z HREF guidance
    does show low-to-moderate chances (20-50%) for storms that are
    capable of producing 6hr QPF > 6-hr FFGs through 06Z tonight. The
    20Z run of the WoFS (15km neighborhood probabailities) also showed
    some >50% probabilities for >2" of rainfall just north and south
    of the OKC metro area through 02Z.

    Soils in the Southern Plains welcome the rain given much of the
    region's D1-D3 drought status. However, these kind of excessive
    rainfall rates over very dry/hard soils can struggle to soak in
    rainfall right away and act more as like a hydrophobic surface.
    This can lead to rapid rises in water both in poor drainage areas
    and near by creek beds. Any metropolitan areas with a greater
    concentration of hydrophobic surfaces are also vulnerable. The
    combination of excessive rainfall rates up to 2"/hr and what is
    appearing to be multiple rounds of thunderstorms into this evening
    favors the likelihood for flash flooding. In cases where
    back-building and training occur, locally considerable instances
    of flash flooding are possible.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6AiuvJ3eOGnAlJe23itflsM8uEAPnBo3alG2JInTg3_-1idawiIBf7s1ydK8mL7Kuvt2= 5xfQLpIeifP-eGgyqd8U1u4$ for graphic product...

    ATTN...WFO...LUB...MAF...OUN...TSA...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 36929643 36649567 35409609 33489996 33020080=20
    32610173 32840212 33650126 34480022 35369909=20
    36499793 36859739=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 3 22:00:21 2026
    AWUS01 KWNH 032200
    FFGMPD
    INZ000-ILZ000-040400-

    Mesoscale Precipitation Discussion 0075
    NWS Weather Prediction Center College Park MD
    558 PM EDT Fri Apr 03 2026

    Areas affected...North Central IL...Western IN

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

    Valid 032200Z - 040400Z

    SUMMARY...Thunderstorms forming along and north of a warm front
    will be capable of producing up to 2"/hr rainfall rates. With
    prolonged, moist southwesterly flow expected to intersect the
    front for several hours, flash flooding is likely through early
    evening.

    DISCUSSION...Doppler Radar shows scattered thunderstorms having
    formed along a warm front that extends from the strengthening area
    of low pressure in northwest MO eastward into northern OH.
    Low-level southwesterly flow is providing healthy theta-e and
    moisture advection while MLCAPE along and just south of the warm
    front is >2,000 J/kg. PWs are forecast to surpass 1.5" this
    evening, which is above the 99th climatological percentile for
    early-mid April. Meanwhile, sheared shortwave energy racing north
    from the South Central U.S. will provide additional synoptic scale
    lift aloft later this evening. Vertical wind profiles will favor
    supercells with >40 kts of effective bulk shear and up to 200
    m2/s2 of SRH. As storm form along the front, persistent inflow
    into the warm front as it slowly moves north gives rise to
    back-building and training storms, increasing concerns for longer
    residency times for these storms.

    Latest 18Z HREF shows moderate chances (40-60%) for rainfall
    totals >2" in north-central IL. This is supported by the 21Z WoFS
    using cumulative >2" paint balls through 03Z. There are several
    CAMs members (RRFS, NSSL-MPAS, 20Z HRRR) that shows this cluster
    of storms having the potential to produce localized rainfall
    amounts >4" through this evening. 1-hr FFGs are generally below
    1.5" for the majority of the at-risk region, and even 3-hr FFGs
    are <2" (less than 1.5" on the southern periphery of the
    Chicagoland area). The southern tier of Chicagoland could contend
    with excessive rainfall this evening as elevated instability moves
    northward and the storms lift northward with the warm front.

    With concerns for training and back-building storms in an
    atmospheric environment suitable to generate up to 2"/hr rainfall
    rates, cases of flash flooding are likely in parts of central and
    northern IL, and potentially in western IN this evening. Should
    those >4" amounts on various CAMs come to fruition, locally
    significant flash flooding could unfold. Poor drainage areas and
    urbanized communities are most vulnerable to flash flooding this
    evening.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Zqm5EQ8QJ4eq_dcSvuMqxde5ctbOiPbRtt4oF45VVxHWWHl6sfIkyj0o4kWhAQPiZLT= Tld5yLbJaYh2F-PYKE5BD7o$ for graphic product...

    ATTN...WFO...DVN...ILX...IND...IWX...LOT...LSX...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 41768809 41418739 40948612 40618601 40098627=20
    40018747 39918909 39659073 39979130 40539086=20
    40919006 41388917=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 3 22:49:50 2026
    AWUS01 KWNH 032249
    FFGMPD
    MNZ000-IAZ000-040430-

    Mesoscale Precipitation Discussion 0076
    NWS Weather Prediction Center College Park MD
    647 PM EDT Fri Apr 03 2026

    Areas affected...Central IA...Southeast MN

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

    Valid 032245Z - 040430Z

    SUMMARY...Thunderstorms approaching from the southwest will
    produce additional heavy rainfall over northern IA and southeast
    MN that saw rainfall recently over the past 24 hours. With soils
    growing increasingly saturated, localized flash flooding is
    possible.

    DISCUSSION...Rounds of thunderstorms continue to develop just east
    of the MO River as moist southwesterly flow at low levels
    intersects the 850mb front oriented from western IA on north and
    east into far southeast MN. Strong low-level WAA north of the warm
    front is allowing for as much as 1,000 J/kg of MUCAPE over central
    IA. Another round of storms on the northern periphery of the
    surface low will continue to race north and east over the next few
    hours in an environment that sports >1.25" PWs, which are above
    the 99th climatological percentile into central IA.

    Soils within the highlighted region were already coming into today
    a little more saturated thanks to yesterday's rainfall. NASA
    SPoRT-LIS 0-40cm soil moisture percentiles in north-central IA
    were above 80% saturation coming into today. MRMS shows 3-hr QPE
    from just north of Des Moines on north and east have received an
    additional 0.5" of rainfall (locally higher totals too). Most
    hourly rainfall rates are less than 1"/hr, but as the low deepens
    and WAA increases, warm cloud layers will also deepen and warm
    rain processes will make for more efficient rainfall rates that
    could approach 1"/hr. Latest 1hr FFGs are as low as 1"/hr in
    central IA. Flash flooding is possible, particularly along and
    just north of the warm front and the track of the surface low
    where a better source of instability is present. Locations most
    at-risk to flash flooding are poor drainage areas and spots where
    soils are beginning to struggle soaking in recent rainfall.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_r_IuqUMUIjk7Ch6sdo2ZPzGX-yKrltvOs3UOyWDa5oCCDftKcQQGGNHMWCbK50e-3YC= iIzHNj7H21Uytp12tVR17xs$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43809169 43159133 42369175 41029340 40949450=20
    41969505 42589467 43089354 43729249=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Apr 4 01:31:52 2026
    AWUS01 KWNH 040131
    FFGMPD
    OHZ000-INZ000-040729-

    Mesoscale Precipitation Discussion 0077
    NWS Weather Prediction Center College Park MD
    930 PM EDT Fri Apr 03 2026

    Areas affected...Eastern IN...Northern OH

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

    Valid 040129Z - 040729Z

    SUMMARY...Additional training thunderstorms producing hourly
    rainfall rates up to 1.5"/hr remain possible through the overnight
    hours.

    DISCUSSION...Thunderstorms located along and just south of a warm
    front are also forming along a narrow outflow boundary to the
    south. Storms in northern OH have produced over 2" of rainfall in
    some spots per MRMS QPE and one LSR southwest of Canton reporting
    2 feet of water over a road. Rounds upon rounds of storms are
    likely to continue from eastern IN and northern OH to as far east
    as the WV Panhandle and southeast PA this evening. RAP
    mesoanalysis continues to show at least 1,000 J/kg of MUCAPE
    available, effective bulk shear up to 30 kts, and anomalous PWs
    between 1.25-1.5" at these storms disposal.

    1-hr FFGs have decreased to as low as 1" in parts of northern OH
    with all areas effectively below 1.5" thanks to this afternoon's
    thunderstorm activity. 00Z HRRR continues to suggest the
    persistent westerly 850-300mb mean layer winds aloft and low-level
    winds supplying rich theta-e into the front will create a steady
    diet of storms through the rest of the evening. 00Z HRRR 6-hr QPF
    shows an additional 1-2" of rainfall are possible with localized
    amounts over 3" possible between now and 08Z tonight. Given the
    current state of ongoing flash flooding in the area, and more
    excessive rainfall to come, additional flash flooding is likely.
    Locally significant flash flooding is possible where another 1-2"
    of rainfall occurs in areas that are already dealing with flash
    flooding. Note that flooded roadways will be more difficult for
    motorists to identify with the sun having now set. Motorists
    should exercise caution if they must be on the roads tonight.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-QCHH8OMPmGnSUAQ6cvwhTQNlISQOO_u7xsNTki7vtduQ6Yfb8xqYks-ICD21qvewlZx= D--TDlxavanM4ZMdv7ipPA4$ for graphic product...

    ATTN...WFO...CLE...ILN...IWX...PBZ...

    ATTN...RFC...TIR...NWC...

    LAT...LON 41218275 40998150 40778103 40268116 40118298=20
    40358467 40628531 40898531 41188402=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Apr 4 02:59:53 2026
    AWUS01 KWNH 040259
    FFGMPD
    TXZ000-OKZ000-040857-

    Mesoscale Precipitation Discussion 0078
    NWS Weather Prediction Center College Park MD
    1058 PM EDT Fri Apr 03 2026

    Areas affected...portions of Oklahoma and north Texas

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

    Valid 040257Z - 040857Z

    Summary...Flash flood potential will continue for the next few
    hours along the Red River Valley, north Texas, and central/eastern
    Oklahoma.

    Discussion...Recent radar depicts an expanding convective complex
    over central Oklahoma, with embedded supercellular structures near
    Shawnee, OK. This complex has recently produced 1-2 inch rainfall
    totals over Oklahoma City metro over the past hour, with moderate
    to high MRMS Flash responses suggesting likely urban flash
    flooding in the area. The complex was moving eastward at an
    appreciable pace (around 30 knots) toward
    less-sensitive/less-urban ground conditions, which may result in
    flash flood potential becoming more isolated with time. However,
    increasing low-level flow over eastern Oklahoma was contributing
    to an increase in deep convection ahead of this complex, with
    mergers likely to support continued 1-2 inch/hr rates at times for
    at least the next couple of hours along and south of the I-40
    corridor. Some training on the southwestern flank of this complex
    could also spread flash flood potential into the Ada, OK vicinity
    over the next 1-3 hours as well.

    Convection was also developing upstream along a southward-moving
    front through southwest Oklahoma and the Childress, TX area. The
    speed of the front should limit the degree of repeating/training
    convection here, and rainfall should occur over areas that have
    been relatively dry. Isolated flash flooding is possible in low
    spots where repeating can bump hourly totals above the 1-1.5 inch
    range.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8RR8Dwgx8Nc6M0A0rRRc7lEvTSp3Pc66kG1RjhwnissW-lHQcxBIxMjkCg_OVqBeydr1= NmrwFennnqw1AwUhDLDp2w8$ for graphic product...

    ATTN...WFO...AMA...FWD...LUB...OUN...SHV...SJT...TSA...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 36359490 35139451 33999530 32909765 33140060=20
    33670158 34770059 35119820 35499746 36219682=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Apr 4 04:17:20 2026
    AWUS01 KWNH 040417
    FFGMPD
    INZ000-ILZ000-040715-

    Mesoscale Precipitation Discussion 0079
    NWS Weather Prediction Center College Park MD
    1216 AM EDT Sat Apr 04 2026

    Areas affected...northeastern Illinois, northwestern Indiana

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

    Valid 040415Z - 040715Z

    Summary...Training convection could persist for another couple
    hours into southern suburbs of Chicago Metro.

    Discussion...A persistent, SW-NE oriented band of convection has
    trained along an axis very near I-55 between Joliet and Pontiac
    over the past couple hours. The convection is becoming
    progressively more elevated with time, but is persistent within a warm-advection regime located just above a stable boundary layer,
    with ~1000 J/kg MUCAPE (per SPC mesoanalyses) supporting strong
    updrafts. The orientation of the convection was supporting
    prolonged rainfall, leading to rates in the 1-2 inch/hr range
    (1-2X higher than estimated FFG in the region). Downstream
    instability profiles are supportive of this band of convection
    reaching southern sides of Chicago Metro and far northwestern
    Indiana over the next couple hours, resulting in at least isolated
    flash flood potential. Outside of this band, deepening showers
    were noted across a broader portion of northern and central
    Illinois that may repeat over some of the same areas in line for
    heavy rain from the aforementioned band, but degree of
    training/high-rain rates is uncertain.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5oGpcz_H95CrQ9P7DD1e772UzfPY8quem7gDqTHIPQBUNM21ddfJCYfx4tetiuCdKC1o= 5UVg3ubnlawvUTe_1gpyKOc$ for graphic product...

    ATTN...WFO...IWX...LOT...

    ATTN...RFC...MSR...NWC...

    LAT...LON 41888715 41528688 40948779 40988829 41278872=20
    41738828=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Apr 4 04:20:23 2026
    AWUS01 KWNH 040420
    FFGMPD
    INZ000-ILZ000-040715-

    Mesoscale Precipitation Discussion 0079
    NWS Weather Prediction Center College Park MD
    1219 AM EDT Sat Apr 04 2026

    Areas affected...northeastern Illinois, northwestern Indiana

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

    Valid 040415Z - 040715Z

    Summary...Training convection could persist for another couple
    hours into southern suburbs of Chicago Metro.

    Discussion...A persistent, SW-NE oriented band of convection has
    trained along an axis very near I-55 between Joliet and Pontiac
    over the past couple hours. The convection is becoming
    progressively more elevated with time, but is persistent within a warm-advection regime located just above a stable boundary layer,
    with ~1000 J/kg MUCAPE (per SPC mesoanalyses) supporting strong
    updrafts. The orientation of the convection was supporting
    prolonged rainfall, leading to rates in the 1-2 inch/hr range
    (1-2X higher than estimated FFG in the region). Downstream
    instability profiles are supportive of this band of convection
    reaching southern sides of Chicago Metro and far northwestern
    Indiana over the next couple hours, resulting in at least isolated
    flash flood potential. Outside of this band, deepening showers
    were noted across a broader portion of northern and central
    Illinois that may repeat over some of the same areas in line for
    heavy rain from the aforementioned band, but degree of
    training/high-rain rates is uncertain.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!95o1G44xhRAXek0_2DYk6pSIAZkkVhqDAI9oXcEzGf0JY7r_gN5CB_WeznGwL5J4COD_= ZWGH3d-nvcGE_myqltzA_K4$ for graphic product...

    ATTN...WFO...IWX...LOT...

    ATTN...RFC...MSR...NWC...

    LAT...LON 41888715 41528688 40948779 40988829 41278872=20
    41738828=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Apr 4 19:03:02 2026
    AWUS01 KWNH 041902
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-050101-

    Mesoscale Precipitation Discussion 0080
    NWS Weather Prediction Center College Park MD
    301 PM EDT Sat Apr 04 2026

    Areas affected...Eastern TX...North-Central LA...Southern
    AR...Western MS

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

    Valid 041901Z - 050101Z

    Summary...Heavy showers and thunderstorms will continue to
    increase in coverage across much of the ArkLaTex and ArkLaMiss
    regions through the remainder of the afternoon and into the
    evening hours. Areas with persistent training cells could get 1
    inch/30 minute rainfall rates, which could result in a few
    instances of flooding.

    Discussion...Regional Doppler radars and visible satellite imagery
    are indicating a steady increase in convection developing along
    and ahead of a strong cold front. Multiple broken line segments of
    pre-frontal storms have developed well ahead of the main line
    across much of central and northern Louisiana, and also across the
    northwestern half of Mississippi. These storms are starting to
    convectively train, leading to enhanced rainfall rates of 1-2
    inches per hour, and in some instances an inch in under 30 minutes
    where cell mergers happen. This will moisten the soils before the
    main line of convection approaches with the front later this
    afternoon and evening.

    Recent runs of the RRFS and HRRR are indicating the potential for
    scattered QPF maxima on the order of 2-4 inches through 00Z, with
    much of this likely occurring within a 2-3 hour time period for
    any given location. Although recent dry conditions across much of
    the region is a mitigating factor, the higher rainfall rates may
    be enough to result in a few instances of flooding, with a greater
    potential for this across urban locations.

    Hamrick

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6TJ5Yo_BSMsrzRQZKvYUNRSR_uJFpYLZ3vmsP37NhCSEIVqSUE_Ps1NeodLAbn1FmHOR= 1J2GOMXYqyotTJXZK116pzA$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...JAN...LCH...LIX...LZK...MEG...
    SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 34009043 33878966 33038933 31229040 30609073=20
    30419127 30769249 30769317 30659377 30399455=20
    30019552 29779623 29599690 29809730 30049737=20
    30439708 30819659 31309628 31709580 31949548=20
    32179511 32539463 32809414 33029372 33239315=20
    33349270 33429238 33569207 33669169 33859109=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Apr 5 01:27:07 2026
    AWUS01 KWNH 050127
    FFGMPD
    MSZ000-LAZ000-050500-

    Mesoscale Precipitation Discussion 0081
    NWS Weather Prediction Center College Park MD
    925 PM EDT Sat Apr 04 2026

    Areas affected...Southern LA and South-Central MS

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

    Valid 050125Z - 050500Z

    Summary...Numerous showers and thunderstorms will continue across
    much of southern Louisiana into southern Mississippi through the
    remainder of the evening hours, including extreme southeast Texas.
    Areas with persistent training cells could get 1 inch/30 minute
    rainfall rates, which could result in a few instances of flooding
    through midnight.

    Discussion...Regional Doppler radars and visible satellite imagery
    are indicating widespread convection along and ahead of an
    approaching cold front. There are several multi-cell clusters that
    have developed ahead of the main swath of convection associated
    with the cold front, and these are aligned in the general low
    level SSW winds and have been training over the past few hours.
    Many locations across central Louisiana and central Mississippi
    have already picked up 1-2 inches of rain over the past 6 hours,
    and locally higher, therefore making the soils more saturated and
    susceptible to potential flooding issues.

    Recent runs of the RRFS and HRRR are indicating the potential for
    scattered QPF maxima on the order of 1-3 inches through 5Z, with
    much of this likely occurring within a 2-3 hour time period for
    any given location. This activity should generally diminish in
    intensity going into the overnight hours as instability decreases.

    Hamrick

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4n9bWHs3DcmJI-CImz_pLZablPamVMzuhPYprk6cRUQCVqx1EJYLMgrvMwg8I9H8V1ET= 1swjHN2IRCxAozGJzLikTOE$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MOB...SHV...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 32978902 32908865 32708847 32308846 31608863=20
    30838893 30148940 29799008 29729157 29749267=20
    29929312 29999321 29999321 30389328 30679311=20
    31149258 31689172 32199099 32609030 32918956=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Apr 5 02:09:38 2026
    AWUS01 KWNH 050209
    FFGMPD
    TXZ000-050508-

    Mesoscale Precipitation Discussion 0082
    NWS Weather Prediction Center College Park MD
    1008 PM EDT Sat Apr 04 2026

    Areas affected...Deep South Texas

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

    Valid 050208Z - 050508Z

    Summary...A cluster of deep convection should eventually spread
    1-2.5 inch/hr rain rates into McAllen, TX and vicinity through
    04-05Z.

    Discussion...Deep convection has become increasingly organized
    across primary rural areas of Deep South Texas over the area. The
    storms are focused along an inverted surface trough extending into
    the area from northeastern Mexico, with light southeasterly
    low-level flow maintaining a surface airmass characterized by 80s
    F surface temps/70s F dewpoints into that axis. Storms were
    becoming more organized and developing cold pools/weak
    supercellular structures, which isn't surprising given directional
    shear through the troposphere. Southward propagation of this
    cluster should spread areas of 1-2.5 inch/hr rain rates into the
    McAllen, Texas area and vicinity, where urbanized surfaces may
    pose a risk of flash flooding as the cells move through.

    The overall synoptic scenario supporting heavy rainfall should
    change little through 05Z or so as the weak inverted trough
    persists and weak mid-level waves traverse the area. The
    longevity of convection along the Rio Grande is a bit uncertain
    and highly dependent on the local evolution of convection in that
    area, which should be relatively slow given weak wind fields aloft.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6-PGiJtHrnrSTk1OIvgeZk0r5sWUOI26gjZ65SduasNkLAfkKNnkwDeGtAD4f9eftZcj= WdMnKW9T-MaPgYhBOS0pi_Q$ for graphic product...

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

    ATTN...RFC...FWR...NWC...

    LAT...LON 26999850 26729741 25969739 26229887 26599905=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Apr 6 21:08:16 2026
    AWUS01 KWNH 062108
    FFGMPD
    FLZ000-070200-

    Mesoscale Precipitation Discussion 0083
    NWS Weather Prediction Center College Park MD
    506 PM EDT Mon Apr 06 2026

    Areas affected...Central Florida

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

    Valid 062105Z - 070200Z

    Summary...Slow moving thunderstorms are expected to increase in
    coverage through the early evening hours across central Florida
    near an approaching cold front. High rainfall rates up to 2
    inches/30 minutes may lead to some instances of flash flooding.

    Discussion...Regional Doppler radars and GOES-E satellite imagery
    are indicating a steady increase in slow moving thunderstorms
    across inland portions of the central Florida Peninsula late this
    afternoon. Several multi-cell clusters have been exhibiting signs
    of back-building over the past 1-2 hours, and these are producing
    outflow boundaries that will converge to generate additional slow
    moving convection that may be heavier that what is currently
    happening now. The environment is favorable for storms with high
    rainfall rates given mixed layer CAPE on the order of 1000-1500
    J/kg, PWs near 1.7 inches, and 20-30 knots of effective bulk shear
    per the latest SPC mesoanalysis.

    Recent CAM guidance through 2Z is portraying the potential for
    scattered QPF maxima on the order of 3-5 inches with the most
    persistent convection, and much of this is likely to fall within a
    two hour time period for any given location. HREF neighborhood
    exceedance probabilities of 3-hourly flash flood guidance are up
    to roughly 30% between Orlando and Fort Myers, and there are some
    low-end probabilities of 6-hour QPF reaching 100-year ARI for some
    of these areas. Although this area is in a drought, the high
    sub-hourly rainfall rates could be enough to overcome this
    limitation and result in some instances of flash flooding through
    10 pm local time.

    Hamrick

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_BCj-gL5y9Bht0KzO_qMa0emd3AmRjhExfsZOqRQ83_UtP26mbOpcV8kNYOWVCsm1DKi= ZcoPmWSl9HSE7FJnwRjG05M$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 28858171 28788116 28518087 28058066 27598059=20
    27328077 27158090 26968105 26688088 26268101=20
    26218148 26438174 27118228 27568238 28028244=20
    28358242 28568237 28788213=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Apr 8 18:26:51 2026
    AWUS01 KWNH 081826
    FFGMPD
    FLZ000-090025-

    Mesoscale Precipitation Discussion 0084
    NWS Weather Prediction Center College Park MD
    225 PM EDT Wed Apr 08 2026

    Areas affected...Treasure and Gold Coast of Florida

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

    Valid 081825Z - 090025Z

    SUMMARY...Scattered showers and thunderstorms with a history of
    rainfall rates over 2 inches/hour are impacting portions of the
    Treasure and Gold Coast of Florida, with increasing concerns for
    impacts over sensitive urban areas. Flash flooding is possible
    where the cells are the most persistent through the afternoon and
    early evening.

    DISCUSSION...Persistently moist and relatively unstable low-level
    easterly flow continues to focus areas of showers and some
    occasional thunderstorms into the Atlantic Coast of Florida. Much
    of the activity is aligned with the low-level steering flow and
    has been focusing near the offshore Gulf Stream with extensions
    westward into areas mainly south of Melbourne and especially areas
    just north of Stuart where convection is more concentrated. More
    scattered activity is situated farther south down the coast into
    the I-95 urban corridor of southeast Florida.

    Despite the relatively scattered nature of the coverage, with
    southwesterly flow aloft (as opposed to easterly flow in the lower
    levels), the extreme directional shear present across Florida is
    making an environment favorable for slow-moving and training
    storms. Daytime heating is also allowing for instability to
    increase, currently ranging from 2,000 J/kg near Miami to near
    1,500 J/kg near Melbourne based on SPC Mesoanalysis. Atmospheric
    moisture also ranges from 1.7" PWAT near Miami to 1.4" near
    Melbourne. Thus, the greatest threat for the heaviest rains are
    further south down I-95.

    Multiple days of rainfall across all of southern Florida this past
    week has sufficiently saturated the soils. Thus, expect much of
    any heavy rainfall today to favor increased runoff. Ultimately any
    impacts and the magnitudes thereof will be dependent on where any
    training cells develop relative to how urban the ground underneath
    the cells is. With rates in the strongest cells later this
    afternoon expected to potentially reach 3 inches/hour, localized
    totals to 6 inches can't be ruled out. This in turn would result
    in localized flooding. Regardless, expect that the storms that
    will be capable of flash flooding to remain isolated to widely
    scattered.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7reFGpJjrW38AH1Upf3utPD1RP59anTYXGOCvwwonvVJOkizU1tqghWCW4TM6SECp_jb= F2MXRT9fT1GHYMWwAo3DhII$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 28028067 27988037 26947997 25957994 25598022=20
    25498051 25708057 26008045 26288039 26648033=20
    26938037 27298050 27528056 27828068=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Apr 9 10:26:04 2026
    AWUS01 KWNH 091025
    FFGMPD
    FLZ000-091500-

    Mesoscale Precipitation Discussion 0085
    NWS Weather Prediction Center College Park MD
    624 AM EDT Thu Apr 09 2026

    Areas affected...east-central FL Peninsula

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

    Valid 091017Z - 091500Z

    Summary...Slow moving showers with possible embedded thunderstorms
    are expected to focus isolated areas of heavy rain along the Space
    and Treasure coasts through late morning. Localized hourly
    rainfall of 2+ inches will be possible with storm totals of 2 to
    4+ inches through 15Z, which may result in isolated flash flooding.

    Discussion...Regional radar imagery at 10Z showed scattered
    showers between southern Brevard County and southern St. Lucie
    County. 10.3 micron satellite imagery indicated cloud tops over
    land were relatively warm at -20 to -35 C, with an estimated cloud
    depth of 9 km AGL based on RAP analysis soundings over the region.
    Easterly winds of 20-30 kt in the 925-850 mb layer were oriented
    perpendicular to the coast while mid-upper level flow was from the
    west at a similar magnitude. This has set up favorable effective
    shear profiles for organized cells although 0-8 km AGL mean layer
    winds were about 5 kt or less, resulting in slow cell movement. In
    addition, the alignment of showers with the low level wind has
    also resulted in slow movement of heavy rain cores at times with
    recent development near Vero Beach showing signs of a weak MCV
    over eastern Indian River County. MRMS-derived and KVRB hourly
    rainfall of 2-2.5 inches has been observed with nearly 2 inches of
    rain in 32 minutes at KVRB ending 0940Z. Speed and weak
    directional convergence near the surface was allowing for the
    formation of quasi-transient bands of heavy rain within an
    expanding pocket of MLCAPE between 500-1000 J/kg (06Z-10Z SPC
    mesoanalyses) over the east coast of FL.

    While the future existence of the weak meso-vortex near Vero Beach
    is unknown, convergence in the surface to near-surface layer is
    expected to continue a threat for slow moving showers with
    embedded thunderstorms from Brevard County down to St. Lucie
    County over the next 3-5 hours. However, the concentration of
    heavy rain is expected to remain limited in spatial extent through
    the morning hours. Any areas of flash flooding that develop are
    likely to focus across urban and other areas of poor draining,
    remaining localized in coverage.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9mIL8BFa2gasaYWoyUi5qRG3Of1RRU_n9PRYp394FRPLoJ3dKXYY6S7SbSiGb2zS-sgD= TGJYn7ZaxolHVDjniKRixg4$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 28608054 27788010 27008004 26998066 27908111=20
    28528112=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 10 01:34:19 2026
    AWUS01 KWNH 100134
    FFGMPD
    MOZ000-KSZ000-NEZ000-100730-

    Mesoscale Precipitation Discussion 0086
    NWS Weather Prediction Center College Park MD
    932 PM EDT Thu Apr 09 2026

    Areas affected...Northeast KS...West-Central MO

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

    Valid 100133Z - 100730Z

    SUMMARY...Upscale growth of organizing supercellular convection
    into a multi-cell cluster/MCS will promote a localized and
    primarily urban flash flood threat going into the overnight hours.

    DISCUSSION...The latest radar and GOES-E IR satellite imagery
    depict a cluster of supercells along a slow-moving cold front near
    the KS/NE border. These storms are undergoing upscale growth, with
    supporting factors including fairly strong effective bulk shear of
    to 40 to 50 kts and MLCAPE of 1000 to 1500+ J/kg. Over the last
    hour, this has favored an expansion of deep, cold convective tops
    and intense updrafts.

    As the 850 mb low-level jet veers and intensifies to over 40 kts
    over the next several hours, low-level convergence will sharpen
    along the western and southern flanks of the convective mass. With
    storm motions of 15 to 25 kts generally parallel to the mean flow
    and the boundary, periods of cell-training and cell-mergers are
    expected. This will compensate for modest PWs of about 1.25 inches
    and drive potential for high rainfall rates that may reach 1.5 to
    2.5 inches/hour within the strongest cores and where any
    cell-mergers occur.

    While NASA SPoRT 0 to 10 cm soil moisture indicates significant
    infiltration capacity in rural northeast KS, the 18Z HREF PMM and
    neighborhood probabilities suggest localized 2 to 4 inch totals
    are likely. These totals will approach and may locally exceed FFG
    values and especially within the more sensitive urban corridors.
    Areas downstream including Topeka, Kansas City and St. Joseph may
    eventually see this activity later in the night. As such, the
    concern over the next several hours, aside from well-defined
    severe hazards with large hail, will be a localized and mainly
    urban flash flood threat.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_V7P-J8QajZr8lmjAAmMYppb9LFmhtmko5uyNfAQNigk4X-nlxLjoH4L5j2wU9TvIs0M= nU_APk1NO-Lbst4Tpg4ANoA$ for graphic product...

    ATTN...WFO...EAX...GID...ICT...OAX...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 40059625 39869477 39589418 38989419 38569493=20
    38389618 38599761 38989810 39639790=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 10 19:01:38 2026
    AWUS01 KWNH 101901
    FFGMPD
    OKZ000-110100-

    Mesoscale Precipitation Discussion 0087
    NWS Weather Prediction Center College Park MD
    300 PM EDT Fri Apr 10 2026

    Areas affected...North-Central to Northeast OK

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

    Valid 101900Z - 110100Z

    SUMMARY...Locally training areas of heavy showers and
    thunderstorms will pose a threat for some urban flash flooding
    going through early this evening.

    DISCUSSION...Cooling convective tops are seen in GOES-E IR
    satellite imagery becoming aligned in a general west to east
    fashion across portions of north-central to northeast OK in close
    proximity to a quasi-stationary front. Heavy showers and
    thunderstorms are becoming a bit more concentrated with this
    activity, and the latest radar trends suggest slow cell-motions
    and some increasing cell-training concerns.

    The activity is being facilitated by moist and unstable low-level
    southwest flow into the boundary with MLCAPE values of as much as
    1500 to 2000 J/kg and PWs of 1.2 to 1.4 inches across the region.
    Despite relatively modest kinematic wind fields, there is an axis
    of moderate moisture convergence in vicinity of the front, and
    this coupled with increasing differential heating/instability near
    the axis of convection should tend to sustain the convective
    threat over the next few hours.

    Generally the antecedent conditions are quite dry, with low soil
    moisture content, but the rainfall rates with some of the ongoing
    activity is already locally near 1.5 inches/hour. This coupled
    with the slow cell-motions may favor some short-term totals of 2
    to 4+ inches going through early this evening.

    An isolated and mainly urban threat of flash flooding will exist
    over the next few hours as a result, and this will include areas
    from near Stillwater to Tulsa and along with adjacent communities.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7OMNe7bjzHGDuwRqcrOJ2shcTqUhlC8m8hS1dASOvDqJHGktya8xtEnuVl08ZovWkQ9-= eoQLKiJCVgHcmzqf1PHbDHk$ for graphic product...

    ATTN...WFO...OUN...TSA...

    ATTN...RFC...TUA...NWC...

    LAT...LON 36599485 36349471 35939536 35829684 35999767=20
    36369765 36489701 36469622=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 10 21:42:55 2026
    AWUS01 KWNH 102142
    FFGMPD
    TXZ000-110200-

    Mesoscale Precipitation Discussion 0088
    NWS Weather Prediction Center College Park MD
    541 PM EDT Fri Apr 10 2026

    Areas affected...Southeast Texas including the Houston
    Metropolitan area

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

    Valid 102141Z - 110200Z

    SUMMARY...Slow-moving, outflow-driven thunderstorms interacting
    over highly urbanized areas will be capable of producing localized
    rainfall rates of 2+ inches/hour. Isolated totals of 3 to 4 inches
    may rapidly overwhelm municipal drainage, making localized flash
    flooding possible.

    DISCUSSION...Recent radar and satellite trends depict scattered,
    slow-moving clusters of thunderstorms developing across southeast
    Texas. The thermodynamic environment is characterized by a moist,
    weakly convergent low-level flow off the Gulf of America, with
    PWATs near 1.75 inches and MLCAPE values around 1500 J/kg. While
    deep-layer shear remains weak (effective bulk shear 20-30 kts),
    weak upper-level divergence is supplying modest deep-layer ascent,
    aiding in some maintenance of robust, high-efficiency updrafts.

    Given the weak steering flow, the convective mode is primarily
    pulse-type and outflow-dominant. The immediate flash flood threat
    will be driven by mesoscale boundary interactions. Regional radar
    currently shows multiple outflow boundaries in play?most notably
    one positioned southwest of the Houston metro and another near
    IAH. As these boundaries interact over the next few hours,
    mechanical lift may force rapid, near-stationary convective
    development and upscale growth directly over more sensitive urban
    locations.

    Rainfall rates have already approached 2 inches/hour with the
    strongest cells. High-resolution guidance, particularly the HRRR
    which has initialized the current convective evolution well,
    suggests these boundary collisions will support isolated
    additional rainfall totals of 3 to 4 inches through early this
    evening. Furthermore, the 12Z HREF highlights 10-30% probabilities
    for 3-hour FFG exceedance this over the next several hours. Given
    the high impervious surface coverage across the Houston metro,
    these rates and accumulations may overwhelm local drainage systems
    and bayous, leading to isolated areas of rapid-onset urban flash
    flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8UfP-FaEBTsYZq-U1BJISNdMdxS4kIjqF_7XutdEJFcVHfKrrsDx-b0npcVgfvZAwJZw= 5TdXzeXil7_qMLwkC4AGQLA$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31059623 30659519 30319469 29999457 29479462=20
    28919531 28909635 29599753 30359774 30939727=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Apr 11 05:15:43 2026
    AWUS01 KWNH 110515
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-111000-

    Mesoscale Precipitation Discussion 0089
    NWS Weather Prediction Center College Park MD
    114 AM EDT Sat Apr 11 2026

    Areas affected...northeastern KS into southern/southeastern NE and
    the MO Valley

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

    Valid 110507Z - 111000Z

    SUMMARY...Localized flash flooding will be possible from portions
    of northeastern KS into southern/southeastern NE and the MO Valley
    through 10Z. Brief training of thunderstorms will be capable of
    1-2 in/hr rain rates.

    DISCUSSION...Showers and thunderstorms were increasing in coverage
    across north-central KS into far southern NE as seen on area radar
    imagery through 05Z. The cells were elevated, displaced well north
    of a west-east oriented quasi-stationary front in OK, within an
    airmass containing 500-1000 J/kg MUCAPE per 05Z SPC mesoanalysis
    data. Since 00Z, Southerly 850 mb winds have been strengthening
    with 30-40 kt in place at 05Z per VAD wind data from northern OK
    into southern NE. PWAT values were estimated to be between 1.0 and
    1.3 inches across the central Plains with continued moisture
    advection likely to increase PWAT values into the MO River Valley
    through the night.

    Some additional strengthening of the 850 mb flow into the 40-45 kt
    range across KS is expected over the next 3-4 hours and the
    approach of a weak shortwave impulse over southwestern KS should
    continue an increasing trend in the coverage of elevated
    showers/thunderstorms from northeastern KS into
    southern/southeastern NE over the next few hours. As 850 mb winds
    increase overnight, some veering of the low level flow is also
    expected, bringing the low level wind orientation closer to the
    mean steering flow from the SW. Given the moisture, instability
    and forecast winds, some instances of training are likely to
    result in hourly rainfall of 1 to 2 inches. These higher rates
    should remain limited in coverage but flash flood guidance is at
    or below 2 inches in 3 hours for much of the region, due in part
    to locally heavy rainfall over the past 36 hours. Therefore,
    localized flash flooding may result overnight with 1 to 3+ inch
    total rainfall possible.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!48qr4XsdiFtClShi6w-ZrnC2lWuijYOSz66OvZpJ5YDM_U5fNmZMtF-REmLIPl0U20QT= 1Yeb5phRPebNuvpJ0GHXGlw$ for graphic product...

    ATTN...WFO...EAX...GID...ICT...OAX...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 41329712 41299612 41169573 40809531 40499501=20
    40259485 39909472 39469469 39099484 38789510=20
    38589566 38619653 39009760 39669878 40339891=20
    40899846=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Apr 11 09:55:43 2026
    AWUS01 KWNH 110955
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-111330-

    Mesoscale Precipitation Discussion 0090
    NWS Weather Prediction Center College Park MD
    554 AM EDT Sat Apr 11 2026

    Areas affected...northeastern KS/southeastern NE into southwestern IA/northwestern MO

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

    Valid 110953Z - 111330Z

    SUMMARY...A localized flash flood threat will linger for another
    few hours from northeastern KS/southeastern NE into southwestern IA/northwestern MO. The primary concern will be from
    repeating/training of thunderstorms which will be capable of 1 to
    2+ in/hr rain rates.

    DISCUSSION...A NW to SE axis of thunderstorms was observed on
    radar imagery at 0930Z from the KS/NE border near Superior, NE to
    near Westmoreland in northeastern KS. The slow moving axis has
    been associated with MRMS-derived hourly rainfall of 1 to 2+
    inches over the past couple of hours but the axis of thunderstorms
    appears to be slowly shifting northeast. 850 mb winds of 3o to 40+
    kt continued to overrun a warm front slowly lifting north from
    central OK with an axis of elevated convergence helping to focus
    the cluster of heavy rain beneath a ridge axis aloft locally
    aiding diffluent flow in the upper levels. A subtle shortwave was
    also observed on water vapor imagery earlier in the night and is
    likely approaching central KS with forecast movement toward the
    northeast, around the ridge, helping to support lift.

    850 mb wind speed magnitudes have likely peaked and recent RAP
    forecasts showed gradual weakening through 15Z following the
    diurnal cycle. However, ~25 to 35 kt of SSW 850 mb winds over
    eastern KS will continue to overrun the surface boundary to the
    south and the weak shortwave impulse approaching central KS from
    the southwest will continue to provide ascent from northeastern KS
    into the MO River Valley. Instability will be a limiting factor as
    current values of MUCAPE between 500-1000 J/kg are forecast to
    lower as moisture advection shifts the instability eastward across
    the MO River.

    The axis of heavy rain will likely translate eastward over the
    next few hours with continued periods of training/repeating cells
    with 1 to 2+ in/hr rainfall rates. This will continue to pose a
    localized threat for flash flooding from northeastern
    KS/southeastern NE into northwestern MO and possibly southwestern
    IA. Additional rainfall of 1 to 3 inches is expected through 14Z
    with locally higher flash flood potential where overlap occurs
    with wet antecedent conditions over northeastern KS due to locally
    heavy rain over the past 36 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8QQxASh5-vvLIyl0bOPmA5lpyQV8ph24pEYcquvTGWv9coFrhCZ5EnwIYxnrAS6KQ6_k= hg_4xliiOI76F61lkLRs1XE$ for graphic product...

    ATTN...WFO...DMX...EAX...GID...OAX...TOP...

    ATTN...RFC...KRF...NWC...

    LAT...LON 41019522 40889393 40389350 39719368 39169441=20
    39049551 39189654 39689754 40029835 40609801=20
    40819704=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Apr 11 13:38:02 2026
    AWUS01 KWNH 111337
    FFGMPD
    MOZ000-KSZ000-NEZ000-111636-

    Mesoscale Precipitation Discussion 0091
    NWS Weather Prediction Center College Park MD
    936 AM EDT Sat Apr 11 2026

    Areas affected...Northeastern Kansas...Northwest Missouri

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

    Valid 111336Z - 111636Z

    Summary...Training of thunderstorms containing 1-2"/hr rainfall
    rates will maintain the threat of localized flash flooding for
    another few hours, primarily over portions of northeastern Kansas.

    Discussion...Regional radar this morning continues to track a west
    to east axis of training thunderstorms within a slow moving MCS
    near the Kansas-Nebraska border. Recent MRMS estimated hourly
    rainfall rates have eclipsed 2"/hr at times in the heaviest cells
    at times. When combined with the slow net movement of the complex
    (Corfidi Vectors are around 10-15 kts), 4-5" of rainfall led to at
    least three reports of flash flood impacts in northern Kansas this
    morning.

    As highlighted earlier, the activity remains tied to a 35-40kt
    low-level jet which is bisecting a west-east oriented cold pool
    and synoptic front amid locally diffluent flow aloft. Radar
    imagery also suggests the presence of a weak MCV embedded in the
    complex which could locally enhance ascent in the area. Over the
    next few hours, the RAP suggests 30-35 kts of 850 mb inflow
    bisecting the west-east boundary could maintain the complex for a
    few more hours, even with modest instability in place (~500 J/kg
    MUCAPE). Much of the overnight CAM guidance has struggled with the
    placement and intensity of this complex. However, the ARW seems to
    have a better handle on the current activity and suggests the
    training axis could persist for the next few hours. As such, the
    threat of localized flash flooding will persist this morning, with
    an additional 1-2" of rain possible.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7JDOHnwHVyoR9jvHIv4Dnizxwzt84oyH6DeI-4eZAhUKsKh7HBFJN6Ci6MbF7c57gFaW= ya8_oxZmjL-r0Fiq-jZ10xE$ for graphic product...

    ATTN...WFO...EAX...OAX...TOP...

    ATTN...RFC...KRF...NWC...

    LAT...LON 40259601 40219520 40019439 39599433 39489490=20
    39379618 39389653 39449696 39759714 39979690=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Apr 11 20:28:47 2026
    AWUS01 KWNH 112028
    FFGMPD
    TXZ000-120226-

    Mesoscale Precipitation Discussion 0092
    NWS Weather Prediction Center College Park MD
    427 PM EDT Sat Apr 11 2026

    Areas affected...portions of western TX

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

    Valid 112026Z - 120226Z

    Summary...Showers and thunderstorms are increasing in coverage and
    intensity. Hourly rain amounts up to 2.5" with local totals to 4"
    are possible into this evening, which could lead to widely
    scattered flash flooding.

    Discussion...A region of 850 hPa confluence is slowly moving
    across western TX. Convection across the TX Big Bend is sending
    out an outflow boundary to the east. Precipitable water values
    are ~1.25". An incoming shortwave is moving across northwest
    Mexico, enhancing difluence aloft and increasing the effective
    bulk shear to 25-45 kts. ML CAPE is 500-2000 J/kg, and rising.

    With time, the area of 850 hPa confluence edges eastward across
    portions of the TX Big Bend, Trans Pecos, and northwest TX. The
    GFS-based Galvez-Davison Index implies that increasing convective
    coverage and intensity should maximize in the 00z-03z time frame.=20
    The shifting of the low-level confluence axis should keep amounts
    from becoming particularly extreme. The available ingredients
    suggest that hourly rain amounts up to 2.5" with local totals to
    4" would be possible in this environment. Since Flash Flood
    Guidance is modest, widely scattered flash flooding impacts are
    considered possible. Urban areas and locations with minimal top
    soil in western portions of South-Central TX would be most
    sensitive to these rainfall rates/amounts.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6S6CodPXk1xunr7JwSe-qfaJRSzvcJUN_gfh9rSEMdEsInWsF0bToaBGQrG4Q__GFerO= bHIbaYGzFZOD7tsUELiUuZM$ for graphic product...

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

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 34550074 34309932 33279892 32129929 31020003=20
    29800112 29510153 29590244 29080278 28910311=20
    29070379 29560431 31090307 33270244=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Apr 12 02:57:57 2026
    AWUS01 KWNH 120257
    FFGMPD
    TXZ000-120715-

    Mesoscale Precipitation Discussion 0093
    NWS Weather Prediction Center College Park MD
    1056 PM EDT Sat Apr 11 2026

    Areas affected...portions of the middle Rio Grande Valley into the
    Edwards Plateau

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

    Valid 120252Z - 120715Z

    Summary...Training of thunderstorms is likely to produce areas of
    flash flooding from portions of the middle Rio Grande Valley into
    the Edwards Plateau over the next 4-5 hours. Peak hourly rainfall
    could exceed 2 or 3 inches at times.

    Discussion...Regional radar imagery at 0230Z showed a broken line
    of strong convection extending from near SJT to the Rio Grande,
    roughly halfway between 6R6 and DRT. This line has been
    propagating slowly toward the east but northern portions of the
    line have been quicker to translate east compared to southern
    portions. MRMS-derived hourly rainfall briefly exceeded 2 inches
    along the Rio Grande in Val Verde County within the past hour due
    to training as the NNE to SSW line orientation aligns with the
    mean steering flow.

    Large scale ascent ahead of an upper trough axis tracking across
    AZ/NM and northwestern Mexico will continue over central TX
    overnight and 500-1500 J/kg MLCAPE is forecast to remain in place
    (higher values to the south) which should help to fuel intense
    cores of heavy rain. A strengthening low level jet with speeds of
    30-40 kt, oriented parallel to the Rio Grande, will act to
    transport moisture into the ongoing complex with the slowest
    movement of the convective line likely to remain near the Rio
    Grande, though brief hangups farther north will continue to remain
    possible, supportive of SSW to NNE training. The moisture rich
    environment with PWs of 1.5 to 1.7 inches and increasingly
    divergent/diffluent flow ahead of the upper trough will aid lift
    and allow hourly rainfall of 1 to 2 inches, but locally exceeding
    2 or perhaps 3 inches at times. While the best potential for the
    highest rain rates will remain toward the south, these higher
    rates may overlap with portions of the Edwards Plateau which
    contain greater sensitivity to flash flooding.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8TCPlAIuJOCoKdzncLt3D4dOp7-uC7Z02-DnORb5M7WF4hNu72dCxZYm4zIwjG3KZecP= Ar1IoDWt7NLkNFlA8tY8-OM$ for graphic product...

    ATTN...WFO...EWX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31779963 31379895 30349869 29649894 28929998=20
    28780081 29060090 29510140 29640177 30060169=20
    31190070=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Apr 12 04:21:06 2026
    AWUS01 KWNH 120421
    FFGMPD
    TXZ000-OKZ000-120920-

    Mesoscale Precipitation Discussion 0094
    NWS Weather Prediction Center College Park MD
    1220 AM EDT Sun Apr 12 2026

    Areas affected...north-central TX into south-central OK

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

    Valid 120419Z - 120920Z

    SUMMARY...Widely scattered to scattered instances of flash
    flooding will be possible from north-central TX into south-central
    OK through 09Z. Hourly rainfall of 1-2 inches (locally higher)
    will be possible with 2 to 4 inches in 2-3 hours.

    DISCUSSION...04Z radar imagery showed the northern portion of a
    convective line moving into the Edwards Plateau was getting
    slightly better organized over the past hour as it moved eastward
    across I-20. Instability was on the weak side with 500-1000 J/kg
    MLCAPE estimated via SPC mesoanalysis data and the 00Z FWD
    sounding, along with PWs near 1.5 inches near and south of the Red
    River. Water vapor imagery showed a couple of weaker vorticity
    maxima over western TX, ahead of the main upper level shortwave
    trough axis across northwestern Mexico which will continue to
    provide ascent into the weakly unstable airmass downstream across
    central TX into OK tonight.

    RAP forecast guidance showed favorably diffluent flow aloft
    maintaining over central TX into southern OK through 12Z Sunday.
    Expectations are for the current axis of thunderstorms to continue
    slowly advancing NNE and E ahead of the upper forcing to the west,
    with transient axes of training helping to support 1 to 2+ in/hr
    rain rates and possible flash flooding. While the main concern for
    higher rates will be with the leading edge of the convective line,
    there will be some potential for locally higher rates/training to
    refocus to the west of the line as it shifts downstream due to the
    diffluent flow aloft and an upstream impulse advancing
    northeastward toward the Trans Pecos region of western TX as seen
    on water vapor imagery.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-_-Q2hwEx7KarPBlHVSKjNr9BaEBTzQF2g4CKp3yUTtW7BuT45-6zIl9IGBqLsyjXz7B= olzEoDsYjDrWAyUfbyocJiQ$ for graphic product...

    ATTN...WFO...FWD...LUB...OUN...SJT...TSA...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35979748 35879671 35639634 35089609 34309618=20
    33629639 32879660 31959737 31309902 31389998=20
    32180015 33440001 34719940 35699834=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Apr 12 08:31:05 2026
    AWUS01 KWNH 120831
    FFGMPD
    TXZ000-121330-

    Mesoscale Precipitation Discussion 0095
    NWS Weather Prediction Center College Park MD
    429 AM EDT Sun Apr 12 2026

    Areas affected...Middle Rio Grande Valley into central TX

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

    Valid 120828Z - 121330Z

    SUMMARY...While the threat is not certain, the potential for at
    least localized flash flooding will continue across the middle Rio
    Grande Valley into portions of central TX this morning. The
    possibility of peak hourly rainfall of 1 to 3 inches will linger
    through 13Z.

    DISCUSSION...08Z radar imagery showed a weakening squall line over
    central TX, moving east toward I-35, north of Austin, where a
    relative lull in instability was estimated over central TX via 08Z
    SPC mesoanalysis data (peaking near 500 J/kg MLCAPE) while
    500-1500 J/kg MLCAPE remained west of I-35 and south of I-10
    within the middle Rio Grande Valley. The orientation of the
    remnant squall line or outflow boundary was from NE to SW across
    the Edwards Plateau to the Rio Grande near Del Rio, generally
    aligned with the mean steering flow, resulting in less forward
    motion for the southern portion of the outflow boundary. Isolated
    convective activity was observed north of the outflow boundary and
    south of the Rio Grande over northern Coahuila's Serranias del
    Burro.

    VAD wind plots showed that 35-40 kt of 850 mb southerly inflow
    remained over the lower Rio Grande Valley into the Edwards Plateau
    and atop the rain-cooled outflow boundary. Meanwhile, water vapor
    imagery showed an approaching lead shortwave trough over the Big
    Bend Country, advancing northeastward. Lift ahead of this feature
    was evidenced by the recent shower/thunderstorm development over
    northern Coahuila. It seems plausible that additional development
    may occur along the southwestern flank of outflow, tied to the
    eastward translating MCS over central TX with mean steering flow
    supporting training from SW to NE, within the lingering
    instability max. Aloft, a 90-110 kt upper level jet streak is
    forecast to cross the Rio Grande and advance into western OK
    through the morning hours, placing favorable right-entrance region
    ascent over the Edwards Plateau. In addition, RAP forecasts showed
    largely uninhibited MLCAPE returning northward back across eastern
    portions of the Edwards Plateau and the I-35 corridor this morning
    due to continued low level moisture transport. Therefore, while
    coverage of additional thunderstorms remains unclear, at least a
    localized flash flood threat will continue over the middle Rio
    Grande Valley into portions of central TX through at least 13Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_3FlNpW6BRCKRKImp4hH3qvBATr_8e3WL0zq0GV47pVlRjal9jyjHcjYCG8Ay8XtKy5l= 5F2VyGGL6b2WxpXiEWjjrEo$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31999652 31529594 30669610 30109658 29399760=20
    28769895 28629991 28650054 28770069 29250104=20
    29710163 30460033 31119904 31969747=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Apr 12 16:19:20 2026
    AWUS01 KWNH 121619
    FFGMPD
    TXZ000-122217-

    Mesoscale Precipitation Discussion 0096
    NWS Weather Prediction Center College Park MD
    1218 PM EDT Sun Apr 12 2026

    Areas affected...South-Central Texas

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

    Valid 121617Z - 122217Z

    Summary...Increasing potential for flash flooding this afternoon
    as thunderstorms containing 2-3"/hr rainfall rates develop in the
    next 2-3 hours and congeal into an MCS. Locally significant flash
    flooding is possible, especially atop sensitive urban areas in the
    region.

    Discussion...Showers and thunderstorms are showing increased
    development across South-Central Texas late this morning as a very
    moist airmass continues to destabilize. An intense, localized
    cluster of thunderstorms near Gonzales county recently exhibited
    2.5-3"/hr rainfall rates according to MRMS and KEWX. When combined
    with slow forward motions around 20 kts, a corridor of FFG
    exceedance was noted over the last 15 minutes.=20

    These early storms are tapping into a very favorable environment
    for efficient heavy rainfall production; 12Z RAOB from BRO and
    ACARS profiles from AUS and SAT depict a deep moist layer from the
    surface to 750 mb (PWAT of 1.7-1.8"), tall instability profiles
    characterized by 1000-2000 J/kg of MUCAPE, and WBZ heights over
    3500 m. An inversion above the moist layer has thus far suppressed
    more widespread development, although this is expected to weaken
    over time as large scale ascent strengthens over the next few
    hours while the column continues to moisten.

    As such, thunderstorms are expected to expand in coverage and
    intensity over the next few hours. By 17-18z, the 12z CAM suite is
    in good agreement for this activity to congeal into an MCS
    containing training thunderstorms along a NE-SW axis -- possibly
    along a remnant cold pool evident in surface obs. Forecast Corfidi
    vectors near 10 kts suggest this complex will be quite slow to
    move once it develops, in turn lengthening the residence time of
    2-3"/hr rainfall rates within the strongest individual cells.
    While the area has been dry according to NASA SPoRT soil moisture
    percentiles, the risk of flash flooding is expected to increase
    over the next 6 hours as 3-6" fall in the main axis of training.
    Significant flash flooding is possible should this fall over a
    sensitive urban area.

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6l5fxvgg0Ga24XrcAiL7fdIFH_5gslDM_qZveZxQ_cc0YwW17qlWHwCr4bDlkiesKVsA= EMVZR837bFWVyXMVWomDxKs$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31379590 30859516 29989564 29049725 28959831=20
    29579882 30369847 31079733=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Apr 12 20:18:47 2026
    AWUS01 KWNH 122018
    FFGMPD
    TXZ000-130216-

    Mesoscale Precipitation Discussion 0097
    NWS Weather Prediction Center College Park MD
    417 PM EDT Sun Apr 12 2026

    Areas affected...portions of central TX

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

    Valid 122016Z - 130216Z

    Summary...Showers and thunderstorms are developing across portions
    of central TX. Hourly rain amounts to 3" with local totals to 5"
    are possible, which could lead to scattered instances of flash
    flooding over partially saturated soils.

    Discussion...The combination of shortwaves aloft crossing the
    TX/OK border and northern Mexico have led to a difluent pattern
    aloft across the region. Precipitable water values are 1.5-1.8"
    per GPS data. Effective bulk shear of ~50 kts exists. ML CAPE is
    around 2000 J/kg (higher to the west and lower to the east).

    Inflow at 850 hPa slowly backs with time as the upper level
    shortwave in northern MX approaches, which along with no
    additional eastward progress in the instability gradient should
    hold up forward forward propagation to the northeast. The 12z
    GFS-based Galvez-Davison index implies that the current convective
    uptick maximizes in the 21-00z period before slowly fading
    thereafter in this area. Both the 12z HREF and 12z REFS have a
    heavy rainfall signal across the region, though of differing
    magnitudes. Given the above ingredients which favor mesocyclone
    formation and cell training, along with the possibility that
    storms of different levels of organization could merge, hourly
    amounts to 3" with local totals to 5" are possible. Given the
    recently compromised flash flood guidance values due to recent
    heavy rainfall, scattered instances of flash flooding are
    possible.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8j2UxM1SGtHNsq_QI1ob82WzX2FdtDrZMFk4nPqkt6h33-miTPan9qw8F2P0QPMkg4eY= Z1hEz4csPMkB4OnF9cs_Ej8$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32359813 32339732 31189682 29479732 29309826=20
    30019894 31669899=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Apr 12 21:01:51 2026
    AWUS01 KWNH 122101
    FFGMPD
    TXZ000-130259-

    Mesoscale Precipitation Discussion 0098
    NWS Weather Prediction Center College Park MD
    500 PM EDT Sun Apr 12 2026

    Areas affected...portions of southeast TX

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

    Valid 122059Z - 130259Z

    Summary...Thunderstorms with some level of organization will
    continue to attempt to train into this evening. Hourly amounts to
    3" with additional local totals to 5" are possible, which could
    lead to scattered instances of flash flooding.

    Discussion...Thunderstorms with heavy rainfall have been moving
    east-northeast inland of the Middle & Upper TX Coasts near the
    tail end of an MCV moving through portions of MO, which shows up
    as an eastward branch of the 850 hPa inflow/convergence. Earlier
    this afternoon, hourly rain amounts were quite high, though
    they've settled back towards 2.5-3" as of late. Precipitable
    water values are 1.8-2" per GPS data. ML CAPE is 1000-1500 J/kg.=20
    Effective bulk shear is 25-35 kts which is organizing convection.

    Both the 12z REFS and 18z HREF are at least a county too far
    inland with this convective activity. While their six hour
    probabilities show a tendency for the activity to approach the
    TX/LA border, the REFS hourly probabilities in particular are
    fairly far to the east/too quick when compared to recent radar
    reflectivity imagery. A combination of cell training and embedded
    mesocyclones appear to be the main cause for heavy rainfall in
    this region, though merging convection cannot be ruled out could
    any cells form south of the band and approach it. ML CAPE
    supports the idea of this activity making a run for the LA border,
    but with decreasing instability with time, there could be a
    tendency for increased forward propagation/decreased precipitation
    amounts with time. With somewhat higher instability to the north
    the farther east you go in this region, thunderstorm activity may
    try to correct towards the 18z HREF solution and edge a little
    more northward as well. Hourly rain amounts to 3" with additional
    local totals to 5" remain possible, which could lead to scattered
    instances of flash flooding.

    Roth

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5nMBgV5t9cCt79LlQETJWpm7K6GjQ240BRaV-E-svg4sWr9O9XPQSrTHrurNmmfxbRjA= aPMRiPqOIy0SlzDTLr2vtxk$ for graphic product...

    ATTN...WFO...HGX...LCH...SHV...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31319378 30159385 29649511 29629620 29979635=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Apr 13 03:24:54 2026
    AWUS01 KWNH 130324
    FFGMPD
    TXZ000-130700-

    Mesoscale Precipitation Discussion 0099
    NWS Weather Prediction Center College Park MD
    1123 PM EDT Sun Apr 12 2026

    Areas affected...central TX

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

    Valid 130322Z - 130700Z

    Summary...A small, slow moving cluster of thunderstorms is
    expected to maintain peak rainfall rates of 2 to 3+ in/hr and
    localized flash flooding across portions of central TX over the
    next 2-4 hours. Afterward, eastward translation and weakening is
    anticipated.

    Discussion...03Z radar imagery showed a small thunderstorm cluster
    over and just west of the Colorado River in San Saba and Llano
    counties. This cluster has had a history of backbuilding and
    training with observed hourly rainfall of 2.5 inches and
    MRMS-derived estimates locally over 3 inches over San Saba County.
    It was located just on the cool side of an elongated, remnant
    outflow boundary from earlier on Sunday that extended from near
    New Braunfels into the Hill Country and northward across I-20,
    just east of Abilene. Water vapor imagery showed a number of
    vorticity maxima embedded within the WSW flow aloft. At 03Z, a
    more notable vorticity max was located just northeast of San
    Antonio, with another more subtle feature over Concho and Menard
    counties, west of the ongoing thunderstorms.

    Expectations are for low level flow overrunning the outflow to
    continue to support thunderstorms over portions of central TX
    within a moderately unstable airmass characterized by 1500 to
    2000+ J/kg MLCAPE and PWs of 1.5 to 1.7 inches (SPC mesoanalysis).
    However, passage of the vorticity maxima/shortwave features aloft
    should cause the ongoing activity to shift east in another couple
    of hours while additional development occurs downstream toward the
    east, with eventual weakening as increasing CIN is encountered
    toward the east. There is some uncertainty with exactly how long
    the backbuilding signature will continue over San Saba and Llano
    counties, but current thinking is that the passage of the embedded
    impulses aloft should disrupt the ongoing activity within the next
    2-3 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8pcpmXpFhE2czLV347fybNztipkC3atoiLr2jFxkU4IQKY_67vA06heOHYA0UdhIf3n0= ErkfDhUi8YwEmk5Z5Ni57eA$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32069713 31929682 31659668 31359660 31129663=20
    30859695 30689738 30599828 30679895 30929919=20
    31089929 31379914 31579875 31879812 32039757=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Apr 13 21:42:38 2026
    AWUS01 KWNH 132142
    FFGMPD
    MIZ000-WIZ000-MNZ000-IAZ000-140330-

    Mesoscale Precipitation Discussion 0100
    NWS Weather Prediction Center College Park MD
    541 PM EDT Mon Apr 13 2026

    Areas affected...Much of Wisconsin, Southeastern Minnesota, and
    U.P. of Michigan

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

    Valid 132140Z - 140330Z

    SUMMARY...Thunderstorms forming along a warm frontal boundary will
    organize into training lines of storms, over an area of saturated
    soils through this evening. Flash flooding likely.

    DISCUSSION... Several areas of convection have begun to form along
    a warm frontal boundary across much of Wisconsin and southeast
    Minnesota this afternoon. These storms are being fed by moisture
    influx with PWATs around 1 inch along the front, but over 1.3
    inches along the Illinois/Wisconsin border, based on the latest
    SPC Mesoanalysis. CAMs guidance is in good agreement that the
    storms will continue to grow upscale into an MCS that will then
    support training storms propagating eastward across central and
    northern Wisconsin. A cold front shown across northern Minnesota
    will press southeastward and eventually help to push the MCS
    southward with time.

    Soils across Minnesota and Wisconsin are nearly saturated due to
    recent rainfall and around the U.P. of Michigan, recent snowmelt
    as shown on NASA SPoRT imagery. With above average river levels
    and nearly saturated soils across nearly all of Wisconsin, almost
    all of the rainfall expected from this forecast MCS will convert
    to runoff quickly. FFGs across this region on average are around
    1.5 inches/1 hour, 2 inches/3 hours, and 2.5 inches/6 hours. These
    values are likely to be exceeded with multiple rounds of training
    storms expected late this afternoon and this evening. The cells
    south of the Twin Cities have a history of rainfall rates
    exceeding 2 inches/hour at times, showing that the atmosphere is
    capable of rates exceeding these aforementioned FFG values.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7G1XSLTDBBKEgE6KnC6HjiSFk-T-6U4Bgr0ABoBXm8-JrDZHBYlj134353NlsdE9nf1H= lWiBku11TKmoojCTL9tJ1SM$ for graphic product...

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

    ATTN...RFC...MSR...NWC...

    LAT...LON 46828894 46588739 45458680 44468747 43548763=20
    43368904 43429003 43509140 43739228 44039312=20
    44719364 45179376 45829361 46349312 46619141=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Apr 13 23:31:52 2026
    AWUS01 KWNH 132331
    FFGMPD
    MNZ000-IAZ000-SDZ000-140330-

    Mesoscale Precipitation Discussion 0101
    NWS Weather Prediction Center College Park MD
    730 PM EDT Mon Apr 13 2026

    Areas affected...Southwest Minnesota and Northwest Iowa

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

    Valid 132330Z - 140330Z

    SUMMARY... Clusters of storms are forming across portions of
    southwest Minnesota and northwest Iowa this evening. Localized
    rain rates to 2" per hour could cause isolated to widely scattered
    instances of flash flooding.

    DISCUSSION... Convective coverage has rapidly increased across
    portions of southwest Minnesota and northwest Iowa this evening as
    part of a broader low pressure center and warm frontal system,
    tapping into Gulf moisture riding up to the south and east of
    these features. Rainfall rates of up to 2 inches per hour have
    been observed on radar, with somewhat moistened soils in the area
    from recent rainfall, based on NASA SPoRT imagery.

    CAMs guidance is in poor agreement in this area, with none of the
    guidance suggesting convective coverage would be as robust in this
    area than has already formed. For those that have a hint of the
    southern extent of this convection (NAMnest, ARW to a lesser
    extent, and HRRR to an even lesser extent), all suggest much
    faster and more eastward motions to these storms than have already
    been occurring. Thus, with slower and more northward storm
    motions, towards areas where storms have already formed across far
    southern Minnesota, expect more robust training and heavier
    rainfall rates than the guidance is suggesting, favoring more
    potential for flash flooding over the next few hours.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6X1tqeZU-LUfkuQOxQe1ZCk91388CwJGlSqrn-Xsd_p7IlWiLuBHXrVEhhbbR6vhNbAj= BNCnIg_odYgJqLuN6203qEk$ for graphic product...

    ATTN...WFO...ARX...DMX...FSD...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45369378 44999377 44649360 44179331 43929301=20
    43769257 43649215 43449216 43129229 42679296=20
    42619447 42549518 42579577 42809622 43209651=20
    43539693 44139664 44909551 45309470 45349421=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Apr 14 03:47:14 2026
    AWUS01 KWNH 140347
    FFGMPD
    MIZ000-WIZ000-IAZ000-140800-

    Mesoscale Precipitation Discussion 0102
    NWS Weather Prediction Center College Park MD
    1145 PM EDT Mon Apr 13 2026

    Areas affected...southern WI into central/northern Lower MI

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

    Valid 140344Z - 140800Z

    Summary...Areas of flash flooding will be likely from southern WI
    into central/northern Lower MI over the next 4-5 hours. Saturated
    to nearly saturated soils are expected to be a contributing factor
    to excess runoff from rainfall rates of 1-2 in/hr.

    Discussion...0320Z radar imagery across the Upper Midwest showed
    an MCS with an elongated convective line on its southern flank,
    oriented west-east from the MN/WI/IA tri-state region into
    northwestern Lower MI. The cluster of thunderstorms were located
    along a quasi-stationary front that extended west to east through
    central WI/MI with 500-2000 J/kg MLCAPE (highest over northeastern
    IA, lowest over Lower MI) estimated just south of the boundary per
    03Z SPC mesoanalysis data. Infrared imagery showed cloud tops
    continued to cool with divergence aloft aided within the
    right-entrance region of a 110-130 kt upper level jet streak
    positioned over Lake Superior into southern Quebec. 850 mb VAD
    wind data showed 50-60 kt of SSW flow from eastern IA into
    northern IL and southern WI, aiding rapid moisture transport
    across Lake Michigan into Lower MI with upstream moisture over the
    Midwest between 1.2 and 1.4 inches.

    As the main surface low along the front in northwestern IA
    advances ENE tonight, continued southerly flow ahead of the low
    into the ongoing complex of storms should sustain convection
    within the unstable airmass for several more hours. Mean cell
    motions from the W to SW will interact with the southerly low
    level inflow allowing for segments of the line to advance
    southeastward at times. Cell mergers and training within the
    linear segments of the MCS will attain rainfall rates of 1-2 in/hr
    at times with an overall movement toward the east through 08Z.
    Most soils across the region are saturated due to snowmelt and/or
    recent rainfall, with additional heavy rainfall more quickly
    translating into runoff compared to average. Therefore, areas of
    flash flooding are likely to occur across southern WI into Lower
    MI over the next 4-5 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7L1O-mnGFqvdnGQKawceVca5wKPKEE_53aZyZ3QByeXtRcHpH_iNlJdj0PPvcB--9qxe= 996tFkVy9okNckkMMmvxAfw$ for graphic product...

    ATTN...WFO...APX...ARX...DTX...GRB...GRR...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 45818459 45288327 44528305 43748367 42798585=20
    42498773 42528950 42719070 43409120 44019101=20
    44319034 44578902 45028737 45468637=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Apr 14 18:02:21 2026
    AWUS01 KWNH 141802
    FFGMPD
    INZ000-WIZ000-ILZ000-MNZ000-IAZ000-150000-

    Mesoscale Precipitation Discussion 0103
    NWS Weather Prediction Center College Park MD
    200 PM EDT Tue Apr 14 2026

    Areas affected...Eastern IA...Southern WI...Northern and Eastern
    IL...Western and Central IN

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

    Valid 141800Z - 150000Z

    SUMMARY...Developing and expanding clusters of heavy showers and
    thunderstorms coupled with locally wet/sensitive antecedent
    conditions will foster an isolated to scattered threat for flash
    flooding going through early this evening.

    DISCUSSION...Early afternoon GOES-E visible satellite imagery
    shows stronger diurnal heating promoting a steady destabilization
    of the boundary layer across eastern IA, western IL and nosing
    into southwest WI. This airmass is pooling south and east of a
    quasi-stationary front as multiple waves of low pressure advance
    along it.

    Some modest CINH remains in place across these areas, but MLCAPE
    values of 2000 to 3000 J/kg are already in place, and this is
    being supported by steep mid-level lapse rates transiting the
    Midwest. Meanwhile, satellite imagery shows a modest mid-level
    shortwave impulse ejecting northeastward across central and
    eastern IA down through northern MO and into western IL. This
    energy coupled with additional solar insolation should erode the
    remaining CAP across the region and set the stage for convective
    initiation. Much of this should be focused in close proximity to a leftover/diffuse outflow boundary from the early-day convection.

    As convection grows upscale, there will gradually be concerns for
    a few cell-mergers and some cell-training. A combination of
    multicells and supercells will be likely given the strong
    instability in conjunction with strong shear (effective bulk shear
    approaching 50 kts). The larger scale environment is also
    increasingly moist with aid from a southwest low-level jet of 30
    to 40+ kts. Deeper layer southwesterly moisture transport is noted
    aloft too with elevated CIRA-LVT magnitudes.

    Locally significant model disagreement is noted through this
    evening with the placement of the convection and its general
    evolution, but a multi-model consensus suggests eastern IA,
    northern IL and southern WI seeing one focus for convection, with
    areas of central/eastern IL and into western IN seeing a second
    focus.

    Rainfall rates will be capable of reaching 1 to 2 inches/hour,
    with some localized totals by early this evening of 2 to 4 inches.
    The antecedent conditions are locally quite sensitive, and
    especially from eastern IA through northern IL and southern WI.
    Isolated to scattered areas of flash flooding will be possible as
    a result.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6rVoRhS9MtZ95Sj6aCH05vO57EMIhqP-DU7yZfIuOyX3spDEUeEb69FAjBiqp3DRaLHv= v5fBXogv1SsUKymmwi2Cj7Y$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...ILX...IND...IWX...LOT...MKX...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 43969015 43808891 43378810 42458766 41648679=20
    41038574 40368523 39538567 39238682 39538845=20
    40048943 41199043 41619249 41909331 42369330=20
    42689297 43329238 43909121=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Apr 14 22:04:13 2026
    AWUS01 KWNH 142204
    FFGMPD
    TXZ000-OKZ000-150402-

    Mesoscale Precipitation Discussion 0104
    NWS Weather Prediction Center College Park MD
    603 PM EDT Tue Apr 14 2026

    Areas affected...portions of western North Texas and the
    southeastern Texas Plains into southern and central Oklahoma

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

    Valid 142202Z - 150402Z

    Summary...Ongoing convective evolution suggests an increasing
    flash flood threat for areas near Vernon, Lawton, and eventually
    toward the I-35 corridor in central Oklahoma through 04Z/11p
    Central.

    Discussion...Scattered, deep convection continues to increase in
    coverage across western north Texas and southwestern Oklahoma.=20
    Recent surface obs indicate subtle veering of flow west of a
    dryline across the Texas South Plains, and objective
    analyses/satellite suggest subtle vort maxima riding atop the
    dryline and over a warm, unstable airmass over the discussion
    area. These trends suggest continued expansion of convective
    coverage across the discussion area over the next few hours
    (especially as the low-level jet ramps up), with areas of training
    and mergers expected to foster spots of 1-2.5 inch/hr rain rates
    especially near the Red River.

    Antecedent conditions are a somewhat moist across the region from
    prior heavy-rain events over the past week. Sensitive terrain and
    urbanized areas (near Lawton in particular) could also experience
    a higher runoff risk. The overall focus for flash flooding should
    revolve around sensitive spots and locations of cell mergers -
    with background/mean flow fields (around 35-45 knots) suggestive
    that prolonged heavier rainfall (and >1.5 inch/hr rates/local FFG)
    may not occur on a widespread basis.

    Flash flooding is possible with this regime initially over
    southwestern OK and western north Texas, with the risk spreading
    northeastward toward I-35 in Oklahoma later tonight.

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6VoGB_M1a_9ytYeE6UWe8iLQ051eCBJO1BKLKOA725_8XkZLNT0flAJJgr3NBTOQttOi= 3Q_C8zlaihqgqTHhLhv-AsE$ for graphic product...

    ATTN...WFO...AMA...FWD...LUB...OUN...SJT...TSA...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35969737 35969640 34589601 33539662 33169844=20
    32870002 32960060 33570089 34530062 35180008=20
    35599891=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Apr 14 23:57:56 2026
    AWUS01 KWNH 142357
    FFGMPD
    MIZ000-WIZ000-ILZ000-150556-

    Mesoscale Precipitation Discussion 0105
    NWS Weather Prediction Center College Park MD
    756 PM EDT Tue Apr 14 2026

    Areas affected...portions of Wisconsin and Michigan

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

    Valid 142356Z - 150556Z

    Summary...Deep convection will continue to produce heavy rainfall
    while migrating eastward through Wisconsin, across Lake Michigan,
    and eventually into Lower Michigan. Flash flooding is likely
    given ongoing impacts and local sensitivities in the region.

    Discussion...Deep convection has evolved as expected from the
    Mississippi River eastward across much of Wisconsin and
    northeastern Iowa. Favorable interactions with a warm frontal
    zone and steep lapse rates aloft have enabled intense updrafts and
    embedded mesocyclones to occasionally merge and produce spots of 2
    inches/hr of rainfall at times. Areas of flash flooding are
    possible in the short term.

    Of particular concern is the potential for storms to expand
    northeastward and eastward in coverage. The position of warm
    frontal zone over central Wisconsin and cooler Lake Michigan
    waters may weaken convection as storms move atop slightly
    cooler/stable low-level air, although very steep lapse rates aloft
    downstream should maintain convection as it migrates toward areas
    that have experienced 3-5 inches of rainfall over the past 3 days,
    with ongoing impacts to local watersheds in the area. FFGs fall
    to below 1 inch/hr in a few downstream areas, highlighting the
    sensitivity of the ground conditions there. Approaching heavy
    rainfall may worsen ongoing recovery efforts and perhaps cause new
    instances of flash flooding to occur.

    Peak flash flood potential will spread into northeastern Wisconsin
    in the 00-04Z timeframe and eventually spread into Lower Michigan
    generally from 02Z onward.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7kgjJfhxvhUeO4YT74P3s8DQ6l_xpQ24IGlUfxoboD8Y2QG0QSY5486_Dp46h_RYXL9-= Huhx9HqLAuI5qFzRolT1pZE$ for graphic product...

    ATTN...WFO...APX...ARX...DTX...DVN...GRB...GRR...IWX...LOT...
    MKX...MQT...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 45408569 45298379 44028325 42218366 41788510=20
    41898733 42518836 42508976 43319091 44929033=20
    45348892=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Apr 15 00:25:03 2026
    AWUS01 KWNH 150024
    FFGMPD
    INZ000-WIZ000-ILZ000-IAZ000-150623-

    Mesoscale Precipitation Discussion 0106
    NWS Weather Prediction Center College Park MD
    824 PM EDT Tue Apr 14 2026

    Areas affected...eastern Iowa, northern Illinois, southern
    Wisconsin

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

    Valid 150023Z - 150623Z

    Summary...Thunderstorms are expected to not only persist, but
    train and repeat over areas very near the WI/IL border vicinity
    over the next several hours. Flash flooding is likely, and
    significant impacts cannot be ruled out.

    Discussion...Radar mosaic imagery depicts a mature convective
    complex with embedded linear structures and mesocyclones extending
    from south-central WI (near Madison) southwestward to near Dubuque
    and Cedar Rapids. Other convection was anchored/backbuilding near
    a warm front close to and just north of Milwaukee. Each of these
    convective clusters were producing expanding cold pools that were
    progressively orienting perpendicular to increasing southwesterly
    low-level flow, with 45kts now noted on mesoanalyses at 850mb
    across much of IA/IL. Latest indications are that these
    convective clusters will continue to backbuild and train owing to
    convergence along strengthening outflows and strong upstream
    buoyancy (~3000 J/kg MLCAPE).=20

    The scenario is beginning to favor multiple hours of repeating
    convection (1-2.5 inch/hr rain rates) very close to where ongoing
    convection exists currently. Localized 3-5 inch rainfall totals
    are possible over the next 6 hours. This could result in
    significant flash flood potential as FFG thresholds across the
    area are only at around 1 inch/hr and will be readily exceeded.=20
    This potential will likely exist through 06Z/1a central, with
    populated areas near Madison, Milwaukee, Rockford, and perhaps
    Chicago potentially experiencing impacts.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_RimPN4452Lz3CSs_IelT7ml5jPYxQHeJmRoaCJABg12dpxpwKNOMVjDMdImE2PL8K-g= NjzLo2BW4jUzEE5JhCUattE$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...LOT...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 43498958 43368824 42998765 41958741 41538758=20
    41248859 41319028 41369158 41559227 41839253=20
    42249259 43009239 43179125=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Apr 15 05:29:01 2026
    AWUS01 KWNH 150528
    FFGMPD
    OHZ000-MIZ000-INZ000-WIZ000-ILZ000-151020-

    Mesoscale Precipitation Discussion 0107
    NWS Weather Prediction Center College Park MD
    127 AM EDT Wed Apr 15 2026

    Areas affected...northeastern IL/southeastern WI to southern
    MI/northern IN

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

    Valid 150526Z - 151020Z

    SUMMARY...Scattered flash flooding will be possible in the
    vicinity of the eastern IL/WI border, eastward to southern Lower
    MI, northern IN and northwestern OH. Rainfall rates of 1-2 in/hr
    (locally higher) are expected along with peak additional rainfall
    totals of 2-3 inches through 10Z

    DISCUSSION...05Z radar imagery depicted a trailing stratiform MCS
    moving across Lower MI with the leading edge pressing
    southeastward across southern MI into northern IN. An outflow
    boundary was analyzed ahead of the convective line from
    southeastern MI into northern IN/IL with upstream thunderstorm
    development occurring north of the western portion of the boundary
    along the WI/IL border. 925-850 mb winds were from the SW at 45-55
    kt to the south of the boundary over north-central IL and
    1000-2000 J/kg MLCAPE extended from the MI/IN border back west to
    the MS River, per SPC mesoanalysis data.

    The leading edge of the MCS is expected to continue tracking
    toward the ESE across southeastern MI into northern IN and
    northwestern OH over the next 1 to 2 hours, but back to the west,
    continued convective development is likely as moist, low level
    flow overruns the slow moving western portion of the rain-cooled
    outflow. Mean cell motions are generally from the west which will
    setup a favorable pattern for training from west to east given
    alignment with the low level boundary. Rainfall rates of 1 to 2
    in/hr are likely (locally higher possible), and an additional 2 to
    3 inches of rain is expected through 10Z where cell training is
    maximized. Flash flood guidance is less than 2 inches in 3 hours
    for some locations, especially across northern IL/southern WI
    where heavy rain over the past 12-24 hours has contributed to
    reduced soil infiltration.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4gUZnv0Qxp7R8HWlZNMdEUOjnXzvwcsKhaQiAxAI-iAuF1r4A3I0uJ-ZiXaLC7iOJvba= 8vQFf0NVtX6daqnhMsw5PxE$ for graphic product...

    ATTN...WFO...CLE...DTX...GRR...IWX...LOT...MKX...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 43668276 43568226 43138209 42448225 41578312=20
    41298455 41268640 41468819 41788922 42428939=20
    42908878 42848652 42988484 43578350=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Apr 15 21:48:39 2026
    AWUS01 KWNH 152148
    FFGMPD
    WIZ000-ILZ000-IAZ000-160246-

    Mesoscale Precipitation Discussion 0108
    NWS Weather Prediction Center College Park MD
    547 PM EDT Wed Apr 15 2026

    Areas affected...southern Wisconsin, northern Illinois

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

    Valid 152146Z - 160246Z

    Summary...Thunderstorms will migrate eastward across wet/sensitive
    areas from yesterday's rainfall especially across Wisconsin.=20
    Flash flooding is likely.

    Discussion...Scattered thunderstorms have organized along a
    frontal boundary from just north of Dubuque to Des Moines. The
    storms are exhibiting linear organization so far in their
    evolution, with forward propagation and 40-50 kt speeds generally
    limiting their rainfall potential to around 1 inch/hr or less.=20
    Flash flooding is possible on an isolated basis in the short term.

    Over the next 1-4 hours, however, storms will migrate eastward
    along a remnant outflow/frontal boundary extending east-west
    across southern Wisconsin (generally from Sheboygan to Wisconsin
    Dells). As low-level flow increases over Illinois, convergence
    along this boundary could result in additional convection
    developing in southern/southeastern Wisconsin out ahead of the
    ongoing quasi-linear complex. This will increase potential for training/mergers and prolonged rainfall rates in areas that have
    already experienced 1-4 inches of rainfall yesterday near/north
    and west of Milwaukee and across far northern Illinois. FFGs are
    less than 1 inch/hr in some spots and could readily be exceeded
    where mergers take place. Flash flooding is likely - especially
    in sensitive areas that received rainfall/runoff issues late
    yesterday and early today.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5opxEbcOifoi00puOb7C5zg01c-pm_jWC9NSJEfq1mEfdNRUZ1jcte1ysb-WmCRTq14u= t29w5aSU3WiQJFXPtvtydIo$ for graphic product...

    ATTN...WFO...ARX...DVN...GRB...LOT...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 44558947 44408783 43208786 42008773 41548866=20
    41449051 42319153 43979095=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Apr 15 23:01:23 2026
    AWUS01 KWNH 152301
    FFGMPD
    ILZ000-MOZ000-OKZ000-KSZ000-160459-

    Mesoscale Precipitation Discussion 0109
    NWS Weather Prediction Center College Park MD
    700 PM EDT Wed Apr 15 2026

    Areas affected...much of Missouri, a small part of southeastern
    Kansas

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

    Valid 152259Z - 160459Z

    Summary...Deep convection is organizing into clusters/segments
    with localized training. Localized flash flooding is possible
    especially in low-spots and sensitive areas.

    Discussion...Convection continues to mature along and east of a
    dryline extending from near Kansas City south-southwestward to
    near Bartlesville and Oklahoma City, Oklahoma. The storms are in
    a very moist, unstable airmass (with 2000 J/kg SBCAPE and 1.5 inch
    PW values) supporting locally heavy rainfall at times despite
    appreciable storm motions of around 30-40 knots.

    The storms are in an environment with modest forcing for ascent
    due to the slow movement of the dryline, with an approaching
    vort-max over Nebraska and confluence ahead of the dryline helping
    to deepen and expand convective coverage. Because storms aren't
    strictly confined to the dryline, a few areas of training have
    been noted (especially across far southwestern Missouri near
    Joplin). These trends should continue for several more hours as
    evidence of any distinct upscale growth into forward-propagating
    linear segments (that would effectively reduce rain rates) is
    currently unclear.

    Localized training/repeating is likely to result in spots of 1-2
    inch/hr rain rates at times on a localized basis. These rain
    rates will threaten local FFG thresholds, with local sensitivities
    also contributing to a potential flash flood risk. This risk will
    persist for several hours this evening - perhaps through 03-04Z
    tonight.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4QBPUYiOvvcrSPYpuhtkEviwBvLAooHGfmdwrtbeqZBMskhBe_do-t8cvF3LxHUIUCMe= m9tMCSe9Cl1O5RzzcsdF2es$ for graphic product...

    ATTN...WFO...DVN...EAX...ICT...LSX...PAH...SGF...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 40509182 39399086 37999060 37039114 36699282=20
    36749448 37119532 38149503 39479452 40199364=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Apr 16 00:12:27 2026
    AWUS01 KWNH 160012
    FFGMPD
    ARZ000-TXZ000-OKZ000-160609-

    Mesoscale Precipitation Discussion 0110
    NWS Weather Prediction Center College Park MD
    810 PM EDT Wed Apr 15 2026

    Areas affected...southern/southeastern Oklahoma, far north Texas,
    far western Arkansas

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

    Valid 160009Z - 160609Z

    Summary...An axis of training convection has materialized from
    near Wichita Falls through Ardmore to near McAlister. This heavy
    rain axis should translate east-northeastward over the next few
    hours, with flash flooding possible especially across southern
    Oklahoma.

    Discussion...Initial scattered convection has recently aligned
    into a focused, training axis of cells along the Red River Valley
    this evening. The storms are in a weakly forced environment, with
    forcing for ascent resulting from the glancing influence of a
    mid-level wave over Nebraska and weakly confluent low-level flow
    across the region. The orientation of cells parallel to mean flow
    aloft - combined with their gradual maturity and establishment of
    cold pools - suggests that training convection will continue to be
    an issue for at least a few hours. This training band of
    convection will gradually translate east-northeastward into more
    of eastern Oklahoma and perhaps far western Arkansas through the
    overnight hours. A secondary training band of convection
    near/north of the Dallas/Fort Worth metroplex may also materialize
    over the next couple hours.

    Ground conditions are relatively dry in many areas, with hourly
    FFG thresholds exceeding 2-2.5 inches in spots. This suggests
    isolated flash flood potential across the region - mainly tied to
    low spots and/or urban areas. Persistence of training, however
    (as evidenced by 2-2.5 inch/hr rain rates near Ardmore) suggests
    that appreciable impacts may occur where rainfall is heaviest and
    most persistent. This isolated flash flood threat should persist
    for several hours - perhaps through 06Z/1a central.

    Cook=20

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!94K4h8YfYfUxaStsHe_mwQL2Cg4STxUAwOgtVe0vJgX8kBrY3h64uUeSF04aU6SgfTz9= sW5g0eOrXgiqZql0yM0HAKo$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35899509 35869426 34929421 33509505 33079635=20
    32859832 34239831 35069740=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Apr 16 02:34:44 2026
    AWUS01 KWNH 160234
    FFGMPD
    MIZ000-INZ000-WIZ000-ILZ000-160800-

    Mesoscale Precipitation Discussion 0111
    NWS Weather Prediction Center College Park MD
    1033 PM EDT Wed Apr 15 2026

    Areas affected...Northern IL...Far Southeast WI...Southern L.P. of
    MI...Far Northwest IND...

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

    Valid 160235Z - 160800Z

    SUMMARY...Potential for localized flash flooding continues through
    the early overnight period; though coverage should become more
    scattered with loss of heating/rainfall intensity. Rates of
    1.5-1.75"/hr and spots of 2-3" remain possible.

    DISCUSSION...Regional RADAR depicts a mature MCV across central
    Lake Michigan just east of Milwaukee progressing toward
    Holland/Muskegon, MI with a trailing QLCS convective line
    extending across SE WI into the NW Exurbs of Chicago along W I-88
    in N IL toward the Quad Cities. The cold pool appears to be
    maturing as well, increasing forward propagation of the line
    particularly through the middle, toward the WI/IL line, this is
    reducing overall residency time for extreme rainfall totals, but
    the short-term heavy bursts may still result in 1-1.5" in 30 to 60
    minutes. Given recent heavy rainfall and saturated upper soil
    profiles and proximity to hydrophobic urban conditions near
    Chicago will result in increased run-off and likely incidents of
    localized flash flooding/rapid rise flood, especially in the next
    few hours.

    GOES-WV shows expanding divergence region along the entrance of a
    100 kt 3H speed max across the LP of MI at this time, helping to
    maintain the MCV crossing the more stable air of Lake Michigan but
    solid southwesterly warm-air advection is allowing for downstream
    convergence with limited but sufficient MUCAPE of 500-750 J/kg.=20
    VWP shows solid 850-700 40-45kt flow at the western nose of the
    deep layer moisture axis where overall PW totals are increasing to
    over 1.25". This will likely continue to support 1.5-1.75"/hr
    rates and given the record wet spring across the SW LP; FFGs are
    compromised in spots and while typically sandy and able to absorb
    these rates and totals up to 2-3", saturation over 75% to 85% will
    still quickly be overwhelmed with above normal run off and
    potential for localized flash flooding conditions. However,
    proximity to the unstable air will be increasing (along with
    overall diurnal loss) and overall intensity of thunderstorms will
    be steadily increasing through the night reducing overall coverage
    and magnitude of flooding potential.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4LPc5RRJ7D_EWUR-GQyFYstxacfepZIrau-Gq7EetmrgliaA_S5VAKvEdlNZqw0hlovq= memycrUKXrRQJ4-THjJqulI$ for graphic product...

    ATTN...WFO...DTX...DVN...GRR...IWX...LOT...MKX...

    ATTN...RFC...MSR...NWC...

    LAT...LON 43868583 43758458 43508280 42468379 41648587=20
    41268769 41238976 41499024 42108976 42648902=20
    42968835 43578710=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Apr 16 03:11:57 2026
    AWUS01 KWNH 160311
    FFGMPD
    ILZ000-MOZ000-160800-

    Mesoscale Precipitation Discussion 0112
    NWS Weather Prediction Center College Park MD
    1110 PM EDT Wed Apr 15 2026

    Areas affected...Central Illinois...East-Central/Southeast
    Missouri...

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

    Valid 160310Z - 160800Z

    SUMMARY...Mature MCV continues to provide solid WAA ascent coupled
    with nose of enhanced deep layer moisture likely to support
    efficient rainfall production with rates of 1.5-1.75" and streaks
    of 2-3" totals resulting in possible incident(s) of localized
    flash flooding.

    DISCUSSION...Regional RADAR suite depicts a maturing MCV just
    southwest of metro St. Louis lifting northeastward at this time.=20
    GOES-E WV and RADAR show a broadening mid-level baroclinic
    leaf/shield indicative of continued favorable evacuation aloft to
    maintain the MCS for the next few hours. VWP and RAP analysis
    denote the broad divergence is supporting strengthening low level
    flow with solid confluence at the nose of the deeper layer
    moisture axis. CIRA LPW shows corridor of 850-500mb moisture is
    aligned ideally with the southwesterly flow but sfc to 850mb
    moisture is very broad and increasing to support TPW value in
    excess of 1.5". The 30-35kts of 850-700mb confluent flow in this
    moisture regime will support 1.5-1.75" rainfall production even
    with reducing/narrowing unstable axis (generally 500-750 J/kg of
    MUCAPEs). The MCV is also providing a corralling of downstream
    flow into a well defined deformation axis that is generally
    parallel to the deeper layer steering. This orientation will be
    the supportive requirement for increased duration to support
    localized steaks of 2-3" totals.

    Unlike further north, the ground conditions are much drier due to
    the prolonged drought. Yet, FFG values of 1.5-2"/hr and 2-3"/3hr
    are in the realm of exceedance and while not all locations will be
    exceeded there should be a few areas that may lead to localized
    flash flooding conditions through the early overnight period. As
    such, flash flooding is considered possible across central IL back
    through east-central MO; with slightly higher potential in the
    urban areas near Metro St. Louis, due to hydrophobic grounds and
    drainage.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_WoxM95G8ExX39lGSpA8s-H7qn-FUCdGbkYh4vn_8BhypuFWDWSIc__7RJp008JX_uhC= d3_AwawJzGwp-3qEB59Qe3Q$ for graphic product...

    ATTN...WFO...ILX...LSX...PAH...SGF...

    ATTN...RFC...KRF...MSR...ORN...TIR...NWC...

    LAT...LON 40338843 39928763 39148773 38638840 37699014=20
    37499135 37969181 38549157 38819130 39579024=20
    40138941=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Apr 16 04:44:56 2026
    AWUS01 KWNH 160444
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-160845-

    Mesoscale Precipitation Discussion 0113
    NWS Weather Prediction Center College Park MD
    1243 AM EDT Thu Apr 16 2026

    Areas affected...Northeast Oklahoma...Southwest Missouri...Adj.
    Northwest Arkansas...

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

    Valid 160445Z - 160845Z

    SUMMARY...A few more hours of potential localized flash flooding
    due to slow moving/training thunderstorms across the Ozark Plateau.

    DISCUSSION...GOES-E 10.3um IR and regional RADAR mosaic shows a
    solid warming/weakening trend to the convective line across much
    of the Ozark Plateau. RAP analysis shows warming low levels and
    increasing CINH trends across the remaining well of 1000-2000 J/kg
    of MLCAPE, the exception remaining along the upwind edge across NE
    OK; and this is where the healthiest updrafts remain. Still,
    KINX/KSGF show most are starting to have dominating outflow
    patterns. However, as the dry-line retreated and the mean
    upper-level shortwave trough across IA is kicking east; a weakness
    in the overall mid-level flow/steering is lying perpendicular to
    weakening but sufficient southerly surface to boundary layer/925mb
    flow providing solid moisture flux convergence in proximity to the
    remaining MLCAPE axis. Tds in the upper 60s to low 70s. With this
    convergence and steering flow parallel to the boundary (and
    slacking), training or increased downdraft residency may allow for
    a narrow axis of enhanced rainfall rates up to 1.75"/hr for a
    potential of localized 2-3" total. Beside naturally lower FFG
    due to complex terrain across the Ozark Plateau, even further west
    into NE OK, FFG values are locally lower with hourly values less
    than 1.5-2" and 3" values less than 3". So an isolated incident
    or two of flash flooding remains possible more likely over the
    next few hours (through 06z) than into late overnight hours.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-TvB5wH1yA2rEBw5_ycJhpkLeoKNTS-Ovu9k5jlIx-qJ2pkeb0t11tRXvyqCe5r2sRyr= ukq0ka5--mZ0V5dP_wCKRGU$ for graphic product...

    ATTN...WFO...SGF...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 37839174 37359132 36779169 36529332 36329416=20
    36139587 36179651 36579663 36769627 36979505=20
    37359379 37769264=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Apr 16 20:03:10 2026
    AWUS01 KWNH 162003
    FFGMPD
    ILZ000-MOZ000-170001-

    Mesoscale Precipitation Discussion 0114
    NWS Weather Prediction Center College Park MD
    401 PM EDT Thu Apr 16 2026

    Areas affected...a small part of Missouri

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

    Valid 162001Z - 170001Z

    Summary...Isolated, slow-moving thunderstorms could cause
    localized flash flooding for the next few hours (through 00Z/7p
    central).

    Discussion...A localized cluster of thunderstorms has become
    established across central Missouri. The storms have developed in
    response to strong insolation/surface destabilization beneath a
    very cold mid/upper wave (-18C at 500 hPa). The storms are also
    in a very localized area where mid-level flow drops off
    substantially, with right-moving storm motions falling to around
    5-10 knots per point forecast soundings. This explains recent
    behavior of the storm cluster very near Osage Beach, MO, where
    MRMS estimates of 1+ inch/hr in that area were already exceeding
    local FFG.

    Given the weak forcing for ascent, convective coverage is in
    question. Persistence of ongoing activity - or perhaps additional
    slow-moving cluster(s) of convection could produce 1 inch/hr rain
    rates at times. Again, these rates could exceed FFG, and given
    sensitive local terrain in the region, another instance or two of
    flash flooding cannot be completely ruled out. This risk will
    likely be diurnally driven and lessen some after sunset.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-ObucWhVuhSJtJ-DCrbSpVcGeYPrECRaPTiEJb1XmBzxTkejYnTMq5FUaz6gFsNiaqkA= M_oO_IyUC9okdjLdiTlDbSA$ for graphic product...

    ATTN...WFO...EAX...LSX...PAH...SGF...

    ATTN...RFC...KRF...MSR...ORN...NWC...

    LAT...LON 38919228 38839074 38279022 37459022 37119109=20
    37199248 37689329 38099339 38809317=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 17 18:11:42 2026
    AWUS01 KWNH 171811
    FFGMPD
    WIZ000-ILZ000-MOZ000-MNZ000-IAZ000-180010-

    Mesoscale Precipitation Discussion 0115
    NWS Weather Prediction Center College Park MD
    210 PM EDT Fri Apr 17 2026

    Areas affected...Northeast MO...Western and Northern IL..Eastern
    IA...Far Southeast MN...Central and Southern WI

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

    Valid 171810Z - 180010Z

    SUMMARY...Rapid convective development is expected over highly
    saturated soils this afternoon. Anomalous moisture and instability
    will support rainfall rates of 1 to 2 inches/hour. While
    individual cell motions will be fast, cell-training will lead to
    localized totals of 2 to 4 inches, making flash flooding likely
    given the sensitive antecedent conditions.

    DISCUSSION...GOES-E Day Cloud Phase RGB satellite imagery and
    surface observations indicate rapid destabilization across the
    Upper Midwest ahead of an ejecting upper-level trough and
    approaching strong cold front. A 40 to 50+ kt southwesterly
    low-level jet is fostering intense warm air advection and moisture
    transport into the region, resulting in an anomalously moist and
    unstable airmass for mid-April (PWATs climbing to ~1.25 inches and
    MLCAPE of 1500 to 3000 J/kg).

    Convective initiation is expected imminently as the cap erodes,
    particularly near surface waves analyzed over north-central IA and
    southeast MN which are locally enhancing convergence. Deep-layer
    ascent will continue to increase this afternoon and evening as a
    strong shortwave/jet streak rounds the base of the trough and
    approaches from the west. Convective mode is expected to feature a
    mix of supercells and organized multicell clusters.

    While strong deep-layer shear (40 to 50+ kts) will promote fast
    individual cell motions to the northeast, the southwesterly
    steering flow is largely parallel to the low-level jet axis and
    lifting warm front. This alignment will strongly favor corridors
    of cell-training and repeating rounds of heavy rainfall over the
    same areas. High-efficiency updrafts will be capable of producing
    1 to 2 inch/hour rainfall rates, with the 12Z HREF signaling
    localized swaths of 2 to 4 inches through 00Z.

    The primary driver for the flash flood threat is the highly
    sensitive antecedent conditions. Recent NASA SPoRT 0 to 10 cm soil
    moisture data indicates very moist if not saturated soils (80 to
    100%) across much of the region, and USGS streamflow networks show
    running waterways are already elevated. With minimal infiltration
    capacity, the intense 1 to 2 inch/hour rates will to convert to
    enhanced runoff concerns, and likely promoting scattered areas of
    flash flooding which will include some localized urban impacts as
    well.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9hjs2Z_oHmyo18eoaSQu7i3KoZD9Delq5_o_Aeyu83kiVMQIawM1h87TuD-4LEItpLhN= MhaDX-LNgGe5ulc54SN8dxk$ for graphic product...

    ATTN...WFO...ARX...DLH...DMX...DVN...EAX...GRB...ILX...LOT... LSX...MKX...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45659058 45318891 44168851 42578857 41148902=20
    40108946 39429028 39319154 39769277 40559338=20
    41339334 43079263 44399214 45129163=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 17 19:04:14 2026
    AWUS01 KWNH 171904
    FFGMPD
    MOZ000-OKZ000-KSZ000-NEZ000-180102-

    Mesoscale Precipitation Discussion 0116
    NWS Weather Prediction Center College Park MD
    303 PM EDT Fri Apr 17 2026

    Areas affected...portions of southern and eastern Kansas into
    northwestern Missouri

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

    Valid 171902Z - 180102Z

    Summary...Flash flooding is possible as storms expand in coverage
    and intensity across the discussion area through 00Z/7p central.

    Discussion...Convective initiation has occurred in earnest along a
    synoptic front extending from near St. Joseph, MO to near Wichita,
    KS over the past half hour. The storms are in an extremely
    unstable environment, with 2000-3000 J/kg MLCAPE and 1.2-1.5 inch
    PW values supporting heavy rainfall. The front and initial
    convection was also oriented parallel to deep southwesterly
    steering flow aloft, suggestive of areas of training as storms
    mature over the next 1-2 hours. The localized training (and
    perhaps cell mergers where individual cells can move right of mean
    flow) should result in a few spots of 1.5 inch/hr rain rates that
    could result FFG exceedance and flash flooding with time.

    Trends through the night will ultimately depend on the degree of
    convective coverage and any upscale growth into linear segments
    that could materialize. Even if the dominant storm mode becomes
    linear, local training axes are likely to materialize and enhance
    flash flood risk. These trends, along with any potential
    development out ahead of the main frontal band, will be monitored
    for any corridors of significant flash flood potential through the
    evening hours.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_6urUHJHWAXBLoWXgUTS01fJG-k_8qnlfcUOHJLu-Nf-cVPdz3_l-tPy6jQQo3CpjNI9= 066vCnaiDF9ytCYfuFMT224$ for graphic product...

    ATTN...WFO...DDC...EAX...ICT...OAX...OUN...SGF...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 40579404 40529265 39909261 37869402 37089542=20
    36999727 37289839 38509719 40219524=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 17 23:37:15 2026
    AWUS01 KWNH 172337
    FFGMPD
    MIZ000-INZ000-WIZ000-ILZ000-IAZ000-180434-

    Mesoscale Precipitation Discussion 0117
    NWS Weather Prediction Center College Park MD
    735 PM EDT Fri Apr 17 2026

    Areas affected...central/northern Illinois, much of Wisconsin,
    upper Peninsula of Michigan, western Indiana

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

    Valid 172334Z - 180434Z

    Summary...Flash flood potential continues especially across
    Wisconsin and northern Illinois. This threat will shift eastward
    through the evening hours.

    Discussion...A mix of linear and clustered convection continues to
    migrate east/northeastward across the discussion area. Areas of repeating/training were noted across far southern Wisconsin - and
    that area remains sensitive from prior heavy rainfall over the
    past several days. FFGs near/downstream of ongoing convection in
    southern Wisconsin are in the 1 inch/hr range (locally lower),
    with urban impacts from heavy rain expected in the Milwaukee area
    over the next 1-2 hours or so. Flash flooding remains likely
    there.

    Farther north, scattered convection has matured over central
    Wisconsin just ahead of a synoptic cold front despite widespread
    convective overturning. Instability profiles remain supportive of
    strong/deep convection in the short term (next couple hours),
    though the longevity of this convection is in question with
    eastward extent. Nevertheless, widespread impacts from recent
    heavy rain, swollen watersheds, and snow melt have left the region
    very sensitive (FFGs near 0 in the UP of Michigan, also <1 inch/hr
    elsewhere in parts of northeastern Wisconsin), and localized flash
    flooding remains possible.

    Cells in the southern part of this elongated conpmex (exiting
    southeastern Iowa) are more linear in nature, though a few cells
    have developed over west-central Illinois that should merge with
    this line over the next few hours. Ground conditions aren't as
    sensitive in central Illinois compared to farther north. Flash
    flooding may be more isolated/dependent on local rain rate
    enhancement from these mergers.

    Eventually, this elongated complex will shift eastward through
    northeastern Illinois and into western Indiana, with at least
    isolated flash flood potential continuing through 05Z/midnight
    central.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!75sQHgPWBmHMjZ1Iw9XEB_ZKL_6aH3-pygDpV2_kNNOuyft9zc_2YNqGB8JtW2UbmLfK= YzgLHaEoDJkopQwKKRSvHJA$ for graphic product...

    ATTN...WFO...ARX...DLH...DVN...GRB...ILX...IND...IWX...LOT... LSX...MKX...MQT...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 46768913 46698706 46338613 44718704 42648721=20
    41438661 40218642 39408761 39449008 40039107=20
    40969098 42259046 43959061 45999024=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 17 23:39:14 2026
    AWUS01 KWNH 172339
    FFGMPD
    MIZ000-INZ000-WIZ000-ILZ000-IAZ000-180434-

    Mesoscale Precipitation Discussion 0117
    NWS Weather Prediction Center College Park MD
    738 PM EDT Fri Apr 17 2026

    Areas affected...central/northern Illinois, much of Wisconsin,
    upper Peninsula of Michigan, western Indiana

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

    Valid 172334Z - 180434Z

    Summary...Flash flood potential continues especially across
    Wisconsin and northern Illinois. This threat will shift eastward
    through the evening hours.

    Discussion...A mix of linear and clustered convection continues to
    migrate east/northeastward across the discussion area. Areas of repeating/training were noted across far southern Wisconsin - and
    that area remains sensitive from prior heavy rainfall over the
    past several days. FFGs near/downstream of ongoing convection in
    southern Wisconsin are in the 1 inch/hr range (locally lower),
    with urban impacts from heavy rain expected in the Milwaukee area
    over the next 1-2 hours or so. Flash flooding remains likely
    there.

    Farther north, scattered convection has matured over central
    Wisconsin just ahead of a synoptic cold front despite widespread
    convective overturning. Instability profiles remain supportive of
    strong/deep convection in the short term (next couple hours),
    though the longevity of this convection is in question with
    eastward extent. Nevertheless, widespread impacts from recent
    heavy rain, swollen watersheds, and snow melt have left the region
    very sensitive (FFGs near 0 in the UP of Michigan, also <1 inch/hr
    elsewhere in parts of northeastern Wisconsin), and localized flash
    flooding remains possible.

    Cells in the southern part of this elongate complex (exiting
    southeastern Iowa) are more linear in nature, though a few cells
    have developed over west-central Illinois that should merge with
    this line over the next few hours. Ground conditions aren't as
    sensitive in central Illinois compared to farther north. Flash
    flooding may be more isolated/dependent on local rain rate
    enhancement from these mergers.

    Eventually, this elongated complex will shift eastward through
    northeastern Illinois and into western Indiana, with at least
    isolated flash flood potential continuing through 05Z/midnight
    central.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9U-h3PbHAPaEvnkDE8b8ojujiT2ikJcvFmDdocidQB9F7rW9CG0HfjZD7aSshrypXflm= 0uVx1ZhowZi6PlF2XOrL6hQ$ for graphic product...

    ATTN...WFO...ARX...DLH...DVN...GRB...ILX...IND...IWX...LOT... LSX...MKX...MQT...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 46768913 46698706 46338613 44718704 42648721=20
    41438661 40218642 39408761 39449008 40039107=20
    40969098 42259046 43959061 45999024=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Apr 18 00:43:51 2026
    AWUS01 KWNH 180043
    FFGMPD
    ILZ000-MOZ000-ARZ000-OKZ000-KSZ000-180641-

    Mesoscale Precipitation Discussion 0118
    NWS Weather Prediction Center College Park MD
    842 PM EDT Fri Apr 17 2026

    Areas affected...northern/central/eastern Oklahoma, southeastern
    Kansas, southern/central Missouri, northwestern Arkansas

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

    Valid 180041Z - 180641Z

    Summary...Isolated instances of flash flooding remain possible
    through 06Z/1a central.

    Discussion...Ongoing convection has largely organized into an
    extensive linear complex extending from near Osage Beach, MO
    west-southwestward through Ponca City and Gage, OK. The storms
    are mostly undercut by composite synoptic front/outflow, although
    a few elements in central Missouri and far north-central Oklahoma
    remain surface-based. The storms are migrating eastward between
    35-45 knots while exhibiting localized training and areas of 1-2
    inch/hr rain rates at times. These rates should be enough for
    isolated flash flooding as FFG thresholds are generally in the
    1-1.5 inch/hr range especially from north-central Oklahoma
    eastward.

    Storms will be maintained through the overnight hours by abundant
    instability (1000-2500 J/kg MLCAPE) and strengthening low-level
    flow oriented perpendicular to the aforementioned front/outflow,
    maintaining robust updrafts and occasional training. Cells may
    tend to weaken some in east-central Missouri, but re-development
    over western Oklahoma near a front/dryline intersection should
    maintain the heavy rain risk through at least 06Z/1a central
    tonight. Flash flooding is expected on at least an isolated basis
    where training is most pronounced, with terrain influences in
    southwestern Missouri also likely playing a role in enhancing
    flash flood risk. Lastly, models suggest that the ongoing
    convective band will gradually develop southeastward toward the
    I-40 corridor in Oklahoma through the night.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8uiQ__KyH0yp5gD3LVLtiqN8N1vgyEat01kFbc0VsJSyK8Qphlh3hQqt4IJgyiwUMQIe= xQ9i_b7j_xr2DclgdMvU51Y$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...LZK...OUN...PAH...SGF...TOP...
    TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 39309207 38969054 37709043 36569135 35499386=20
    34529681 34489883 35219970 36259956 36939828=20
    37899631 38929406=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Apr 18 19:45:23 2026
    AWUS01 KWNH 181945
    FFGMPD
    LAZ000-TXZ000-190145-

    Mesoscale Precipitation Discussion 0119
    NWS Weather Prediction Center College Park MD
    344 PM EDT Sat Apr 18 2026

    Areas affected...Southeast TX...Southwest LA

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

    Valid 181945Z - 190145Z

    SUMMARY...Potent thunderstorms capable of producing >2"/hr
    rainfall rates over the urbanized communities of southeast TX and
    southwest LA could cause localized urban flash flooding.

    DISCUSSION...Visible satellite and Doppler Radar show a bubbling
    field of convection over southeast TX and southwest LA in advance
    of an approaching strong cold front. Additional surface based
    heating this afternoon will yield over 1,500 J/kg of MLCAPE along
    the I-10 corridor. Winds in advance, and in wake, of the cold
    front are NErly while winds within the 700-200mb layer are firmly
    out of the WSW. This is supporting effective bulk vertical wind
    shear levels that the RAP suggests could surpass 40 kts. This
    would allow for thunderstorms to have more longevity than typical
    "pop-up" or "garden variety" storms. HRRR and RAP area averaged
    soundings show warm cloud layers up to 12,000ft deep and skinny
    CAPE profiles that found in typical warm rain processes. As 850mb
    and 700mb weaken over the region this evening, the concern is for
    additional thunderstorm development either along the cold front or
    induced by the growing cold pool.

    Given the favorable thermodynamic environment and increasing PWs
    that reach 2.0" east of Houston this evening, the concern is for
    2"/hr rainfall rates that manifest over urbanized environments.
    The 12Z HREF does show low-chance probabilities (10-30%) from the
    Houston suburbs on east into southwest LA this afternoon and
    evening. The vast majority of the expected rainfall over southeast
    TX and southwest LA this afternoon is welcomed (severe and extreme
    drought for many), which is also evident in the 1-hr FFGs that are
    no lower than 2" area wide. That said, the potential for
    slow-moving and repeating rounds of storms, combined with
    anomalous PWs and ample instability aloft, could cause localized
    flash flooding in urbanized settings that contain a greater
    concentration of hydrophobic surfaces. Low-lying areas with poor
    drainage are also susceptible to flash flooding this afternoon.

    Mullinax

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9x_hjSr_ftys34SFugzCvxjT-H0aqr-0ltdAUpbxeqrkiGilLjiBwS_-XpRE3GUtr1g_= A55YawAS8oeq-cWzDYFgzAg$ for graphic product...

    ATTN...WFO...HGX...LCH...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 30589389 30569330 30069327 29629387 29209491=20
    28939574 28839638 28939668 29259658 29709602=20
    30369451=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Apr 20 18:29:02 2026
    AWUS01 KWNH 201828
    FFGMPD
    FLZ000-210015-

    Mesoscale Precipitation Discussion 0120
    NWS Weather Prediction Center College Park MD
    227 PM EDT Mon Apr 20 2026

    Areas affected...southern FL

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

    Valid 201825Z - 210015Z

    SUMMARY...Slow moving thunderstorms capable of producing 2 to 3+
    in/hr are expected to impact southern FL over the next 4-6 hours.
    While a large portion of the area affected is covered by swamp,
    there could be impacts to urban areas along the southwest and
    southeastern coast.

    DISCUSSION...18Z surface observations and satellite imagery showed
    a cold front dropping south across Monroe and Miami-Dade counties
    along with sea breeze boundaries along the southwestern and
    southeastern FL coastlines. Visible satellite and radar imagery
    showed the early stages of thunderstorm development with at least
    one developed cell 10-15 miles southwest of Miami. SPC
    mesoanalysis data showed MLCAPE of 1000-1500 J/kg and PWs of 1.5
    to 1.7 inches. Low level flow was from the east to northeast and
    deeper layer mean winds were relatively weak from the WNW.

    Daytime heating and an apparent lack of CIN across southern FL
    will lead to additional rapid thunderstorm development within the
    next 1-2 hours along low level convergence boundaries forced by
    the cold and sea breeze fronts, and later, subsequent convectively
    driven outflow boundaries. Slow movement and brief training of
    these cores are likely to produce heavy rainfall rates of 2 to 3+
    in/hr with the possibility of storm total rainfall in excess of 5
    inches. While the 12Z HREF showed 40 km neighborhood probabilities
    of exceeding 3 to 5 inches of 20-40 percent, the likelihood of
    these higher rates falling over water or swampland is greater than
    that of impacting population centers along the coast. However,
    should these higher rates overlap with the Naples/Macro Island
    region or east-central Miami-Dade County to the upper Keys, urban
    flash flooding will be possible. The flash flood threat is
    expected to end from north to south and likely be over with after
    00Z as the front moves south of the Peninsula.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8AbXtSs2fP1pYZm6Urke5r5CjAgMjCRLCRbGztQ_qt2Cj4zKjJ7W_3kPEsfLCJ4xBv1L= QWbWIlP__ZXdYNaPHGCKEFU$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 26368187 26078093 25858011 25258007 24988041=20
    25138135 25888205=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Apr 20 19:32:33 2026
    AWUS01 KWNH 201932
    FFGMPD
    TXZ000-210009-

    Mesoscale Precipitation Discussion 0121
    NWS Weather Prediction Center College Park MD
    331 PM EDT Mon Apr 20 2026

    Areas affected...Central TX

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

    Valid 201929Z - 210009Z

    Summary...Additional development of efficient, shallow convection
    containing periodic 1.5-2"/hr rainfall rates will maintain the
    threat of scattered flash flooding this afternoon over portions of
    Central TX.

    Discussion...Recent radar mosaic over Central TX depicts an area
    of slow moving and efficient showers and thunderstorms which has
    persisted through the morning and afternoon hours. Over the last
    hour or so, a cell within the broader precipitation shield between
    San Antonio and San Marcos has exhibited an uptick in hourly
    precipitation rates to 1.5-2"/hr, or 0.50-0.63"/15 minutes per
    recent observations, MRMS, and KEWX data. When combined with slow
    cell storm motions estimated at 10 kts, this storm led to a quick
    uptick in CREST Unit Streamflows to 200-600 cfs/smi where a Flash
    Flood Warning was recently issued.

    This activity is occurring downstream of an approaching
    upper-trough and left exit region jet streak in Northern Mexico to
    support broad ascent across the region. At the low levels, an axis
    of modest 850-700 mb layer convergence and WAA is also noted just
    upwind of this activity. ACARS soundings near the heaviest showers
    and thunderstorms suggest a very moist and saturated column from
    the surface to 600 mb and 400-500 J/kg of MUCAPE to support
    efficient collision-coalescence processes in this activity. While
    the instability profile is very shallow, it is somewhat higher
    than what CAMS are initializing with (100-250 J/kg) in this area,
    which could partially explain why the observed rainfall is more
    robust than what is modeled. That said, the RAP does suggest the
    aforementioned low-level forcing will persist through the
    afternoon hours while the upper-trough approaches for the west.
    Thus, the threat of scattered flash flooding will continue through
    the afternoon as new cells with periodic 1.5-2"/hr rates could
    develop and overlap with the area of current heavy rainfall,
    leading to additional totals of 2-3".

    Asherman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6P27gS0htMUt6ruBzVjQGTOBciYb1I84fU-8LYNmHZqsrW2YvQ28M3ERE9FmwAUoPBGt= AyRfqbg7HBFjdj823bTghhI$ for graphic product...

    ATTN...WFO...CRP...EWX...HGX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30409962 30379879 30309766 30009691 29409657=20
    28979693 28989818 29339916 29929974=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Apr 21 00:26:36 2026
    AWUS01 KWNH 210026
    FFGMPD
    TXZ000-210504-

    Mesoscale Precipitation Discussion 0122
    NWS Weather Prediction Center College Park MD
    825 PM EDT Mon Apr 20 2026

    Areas affected...Central TX

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

    Valid 210024Z - 210504Z

    Summary...Additional thunderstorms are developing over portions of South-Central TX this evening. These cells will maintain the
    threat of flash flooding as they could train and overlap with
    areas of heavy rainfall earlier today.

    Discussion...Radar across South-Central TX depicts a rapid
    expansion in thunderstorm coverage and intensity along the leading
    edge of a shortwave near the Big-Bend of TX. At the same time, an
    axis of persistent shallow convection northeast of San Antonio was
    finally showing signs of weakening after producing 2-4" of
    rainfall this afternoon. This activity was quite impactful earlier
    today, and 1-2"/hr rainfall rates led to at least one report of a
    swift water rescue near Live Oak TX where CREST Unit Streamflows
    eclipsed 900 cfs/smi at times.

    With that in mind, the concern is for additional thunderstorms
    containing 1-1.5"/hr rainfall rates to expand southwest of San
    Antonio, in turn leading to periods of training/repeating near
    areas impacted earlier today. This scenario is supported by recent
    runs of the HRRR (which is an slow but overall has the best handle
    on the situation). Taking into account the timing of the HRRR,
    this suggests the threat of scattered flash flooding should
    persist through 4-5Z tonight. Localized rainfall amounts of 1-2"
    could support additional considerable flash flooding impacts,
    especially if they fall atop the areas of heaviest rainfall today
    (highlighted in red).

    Asherman=20

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-pgGySLa8E2fX8z1a-v1EJ-5dByc4dC3VwIx7_d_Lp_Oyn3qKBs_LqqdACbFnEkn5076= LY9CTpEWQN9KPvCUyWfLKis$ for graphic product...

    ATTN...WFO...EWX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30109900 30009752 29279747 28959854 29129944=20
    29649956=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Apr 21 10:00:38 2026
    AWUS01 KWNH 211000
    FFGMPD
    TXZ000-211530-

    Mesoscale Precipitation Discussion 0123
    NWS Weather Prediction Center College Park MD
    559 AM EDT Tue Apr 21 2026

    Areas affected...Triangle of Central Texas...

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

    Valid 211000Z - 211530Z

    SUMMARY...Flash flooding risk possible given slow
    moving/back-building warm-advective shallow but efficient showers/thunderstorms. Rates of 1-1.25"/hr are possible with
    localized 2-3" totals.

    DISCUSSION...A very effective dynamic environment is helping to
    draw above normal moisture into a favorable ascent pattern over
    the next few hours across the Triangle of central Texas. GOES-E
    WV suite depicts a decaying MCV across southeast TX along the
    southeast periphery of favorable mid to upper-level divergent
    pattern along the northeast quadrant of a 70kt 3H west to east jet
    along/north of 30N. Combined with NW to SE diffluent pattern from
    500-250mb providing strong divergence for effective convective
    outflow. However, it is also directing strong ageostrophic
    forcing by helping to accelerate the early morning western Gulf
    jet streak fluxing enhanced low level moisture northward into the
    isentropic ascent plane. CIRA LPW along with VWP vectors denote
    core of west Gulf jet is propagating 20-25kts in the core of .8 to
    1" moisture in the surface to 850mb layer. Combine this with the
    axis of 700-500 mid-level moist flow from the subtropical eastern
    Pacific results in combined PW values nearing 1.5" near the best
    isentropic ascent currently through the San Saba River Valley.

    As such, recent 10.3um EIR and RADAR show increasing shallow
    convective activity along the NW to SE oriented DPVA into the best diffluence/divergence region downstream. The only limiting factor
    is the lack of higher theta-E air resulting in a broader unstable
    layer. Currently, it is limited to 100-250 J/kg of MUCAPE but
    only expected to increase toward 500 J/kg toward mid-morning as
    the core of the western Gulf air reaches the area of concern.=20
    Deep layer flux and ascent should allow for solid convergence and
    low level precipitation development likely with smaller droplets
    in warm-cloud process generation. This should allow for increased
    rainfall rates, but without the greater vertical depth, is likely
    to be limited to the 1.25" range at max. Convective cells are
    likely to move toward the northeast, but with continued south to
    southwest low level inflow, propagation vectors should be
    supportive of upstream redevelopment/back-building of the shallow
    cores. This should allow for increased overall duration to
    potentially support highly focused/localized maximum totals of
    2-3" through to afternoon.=20

    Hydrologically, these maximum totals are at the minimum thresholds
    of 1 but more likely 3 hour FFG values in the area, particularly
    along the southwest edge of the area of concern. NASA SPoRT LIS
    0-40cm soil conditions suggest average saturation around 45-55%
    and as such, most rainfall will be beneficial, but an isolated
    incident or two of flash flooding is considered possible given the
    strong dynamics and setup's history.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_I219mon2hUaIT9iZgkore_06USnlzSqH8nUYqkck59CIiG6-YfaYH-y3ycu4YEpwlLD= 4FbM0lDcXhAwB3fCiFCScWs$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32539720 32209657 31769628 31419629 31169645=20
    30919666 30589712 30449755 30679836 31159887=20
    31779894 32509834=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Apr 21 15:35:41 2026
    AWUS01 KWNH 211535
    FFGMPD
    TXZ000-212100-

    Mesoscale Precipitation Discussion 0124
    NWS Weather Prediction Center College Park MD
    1133 AM EDT Tue Apr 21 2026

    Areas affected...East central Texas

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

    Valid 211533Z - 212100Z

    Summary...Slow moving heavy showers and thunderstorms continue to
    develop across eastern portions of central Texas late this
    morning, and are expected to persist going into the early to
    middle afternoon hours. Rainfall rates in excess of an inch per
    hour may lead to additional instances of flooding through 4 pm
    local time.

    Discussion...Regional Doppler radars and GOES-E satellite imagery
    continue to indicate a swath of heavy rainfall with embedded
    convection, centered mainly between San Saba and Columbus, Texas
    late this morning. This is primarily developing as a result of
    enhanced ascent from a 700 mb trough axis and mid-level shortwave
    intersecting moist 20-30 knot 850 mb southerly flow, and this band
    has been maintaining itself over the past few hours with only
    limited latitudinal displacement over the morning hours.

    The latest CAM guidance suggests the potential for scattered QPF
    maxima on the order of 1-3 inches through 21Z, with recent ARW
    runs most impressive with up to 4 inches possible during that
    time. The soils are becoming increasingly saturated and prone to
    additional flooding, with some regions getting 2 to 4 inches in
    just the past 12 hours as depicted in the graphic, and flash flood
    guidance is dropping in response to this. Even though the
    instability parameters are modest and most rainfall rates should
    be 1.5 inches per hour or less, some instances of flash flooding
    will be possible given the duration of the event.

    Hamrick

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6rZMdZryMnN1h6U47HcOTCMKMYBmebTgM_8KHuzizEgtqpQj8aSaafmjYcXXKRj4CWEH= y070S3biTHnSDXrWh992LpM$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31399745 31079654 30659580 30219534 29699511=20
    29059518 28879550 28899585 28989632 29229708=20
    29909767 30189812 30509848 30959864 31259830=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Apr 22 20:45:43 2026
    AWUS01 KWNH 222045
    FFGMPD
    TXZ000-230130-

    Mesoscale Precipitation Discussion 0125
    NWS Weather Prediction Center College Park MD
    444 PM EDT Wed Apr 22 2026

    Areas affected...central TX to middle/upper TX Coastal Plain

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

    Valid 222042Z - 230130Z

    Summary...Isolated flash flooding will be possible across portions
    of central TX into the middle and upper TX Coastal Plain through
    the early evening. Localized rainfall rates of 2-3 in/hr (locally
    higher) will be possible which could lead to runoff problems where
    overlap occurs with urban areas or other locations with poor
    drainage, especially given above average rainfall over the past
    few days.

    Discussion...Area radar imagery across southeastern TX at 2015Z
    showed scattered thunderstorms across the middle and upper TX
    Coastal Plain, mainly east of U.S. Hwy 77. SPC mesoanalysis data
    from 20Z showed uninhibited MLCAPE of 1000-2000 J/kg and PWs of
    1.3 to 1.6 inches across the region. The storms were located
    within northwest flow aloft between two vorticity maxima, one over
    the Gulf, south of western LA within a region of effective bulk
    shear between 30-35 kt, and a second vort max over northeastern
    TX. Bulk shear values dropped off significantly to the north and
    low level onshore flow between 925-850 mb of less than 15 kt
    appeared to be limiting organization over land. However, cell
    motions were fairly slow at 5-15 kt and portions of the region
    have picked up 2-4 inches of rain over the past 4 days, higher to
    the west near I-35.

    Therefore, while cells were not very organized, slow movement and
    outflow interactions/mergers could result in hourly rainfall of
    2-3 inches (perhaps locally higher) and localized totals of 2-4
    inches through 01Z. While congealing outflows could result in some
    westward migration of activity toward 00Z, the overall footprint
    of ongoing storms is not expected to change much over the next few
    hours. Isolated higher rainfall maxima could result in flash
    flooding should they overlap with more sensitive ground
    conditions, whether that be an urban location or locally
    hydrologically sensitive area due to recent rainfall.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_3LvrLfgRtViQVo-_a9F6P1Xv6F7kfWFSRPquiOqE_-jVWwsbw2FBSSnmKKdI1qasTBI= rsQcycUFdREyrZbFU_yPA64$ for graphic product...

    ATTN...WFO...CRP...EWX...HGX...LCH...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30799449 30649406 30429393 29889416 29389487=20
    28859565 28849669 29109711 29429747 29689764=20
    29999763 30269730 30379683 30509592 30759510=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Apr 23 20:00:37 2026
    AWUS01 KWNH 232000
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-240100-

    Mesoscale Precipitation Discussion 0126
    NWS Weather Prediction Center College Park MD
    359 PM EDT Thu Apr 23 2026

    Areas affected...northeastern KS, southeastern NE, southwestern
    IA, northwestern MO

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

    Valid 231956Z - 240100Z

    Summary...Isolated instances of flash flooding will be possible
    from northeastern KS into southeastern NE, western IA and
    northwestern MO. Training of thunderstorms will produce hourly
    rainfall of 1-2 in/hr with peak rainfall totals of 2-4 inches
    possible, through 01Z.

    Discussion...1945Z radar imagery showed a broken line of
    thunderstorms extending from south-central MN down to the NE/KS
    border, just ahead of a cold front. A cyclonic swirl was observed
    on visible imagery over northern KS, related to a low to mid-level
    vorticity max located just north of the surface triple point.
    Strong to severe thunderstorms were ongoing in the vicinity of
    Omaha, NE with rapid development noted south of Omaha to the NE/KS
    border. SPC mesoanalysis data from 19Z showed 2000-3000 J/kg
    MLCAPE from western IA into east-central KS ahead of the cold
    front with little to no CIN present.

    While thunderstorm activity to the north over western IA continues
    to grow and expand downstream toward central IA through 00Z, newer
    development to the south is also expected to expand within the
    unstable environment ahead of the front and favorably
    diffluent/divergent jet pattern aloft. A general eastward
    advancement of the line is expected but an inflection or two
    within the line of storms is anticipated, allowing for the
    increased potential for brief training from the NE/IA border down
    into northeastern KS as line orientation matches that of the mean
    steering from from the southwest. Elements of training will be
    capable of 1-2 in/hr rates and there will be isolated potential
    for 2-4 inches through 01Z as the line of thunderstorms advances
    off toward the east.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!77pisuZzS7nVKIjm86sEMRBSU92gf0hG8Jrg_GINe5iPA9dGpBPfqkUmC-wLry78e5nO= Fsv2NO7BvOXPtH-oP3LAvqs$ for graphic product...

    ATTN...WFO...DMX...EAX...ICT...OAX...TOP...

    ATTN...RFC...KRF...MSR...TUA...NWC...

    LAT...LON 41949521 41839435 41249367 39789434 37989595=20
    38109739 38699787 39899740 41119655=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 24 00:29:36 2026
    AWUS01 KWNH 240029
    FFGMPD
    MIZ000-WIZ000-ILZ000-MNZ000-IAZ000-240600-

    Mesoscale Precipitation Discussion 0127
    NWS Weather Prediction Center College Park MD
    828 PM EDT Thu Apr 23 2026

    Areas affected...Upper MS Valley into MN Arrowhead/western U.P. of
    MI

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

    Valid 240027Z - 240600Z

    Summary...Widely scattered instances of flash flooding will be
    possible across northeastern IA/southeastern and northeastern MN
    into WI and the western U.P. of MI over the next 6 hours. Training
    of heavy rain is expected to produce 1-2 in/hr rates with isolated
    totals in the 1 to 3 inch range.

    Discussion...Area radar imagery at 00Z showed an intense squall
    line which extended from north-central IA into northeastern KS,
    tracking slowly toward the east-northeast. Meanwhile, less
    organized convection was noted to the north near western Lake
    Superior into central WI along with additional scattered storms in
    eastern IA. Estimated MLCAPE from 00Z SPC mesoanalysis data showed
    500 to 1500+ J/kg from northeastern IA into the western half of WI
    (highest to the south, ahead of the SQLN). MUCAPE up to 1000 J/kg
    was estimated across the eastern MN Arrowhead, north of a surface
    warm front. Aloft, a 90-100 kt jet streak was captured via GOES
    East DMV over western MN, with diffluent and divergent winds
    within its right-entrance region, likely supporting the recent
    uptick in convective activity over eastern IA.

    Expectations are for the squall line to continue advancing toward
    the ENE, while coverage and intensity increases regarding the
    activity from eastern IA into WI, owing to strengthening jet
    support in the upper levels. However, one limiting factor for
    maintaining convective intensity through the first half of the
    night is the forecast for weakening instability with time and with
    northern extent. On the other hand, portions of the region have
    seen over 300 percent of normal rainfall over the past 2 weeks
    which will contribute to quicker runoff from heavy rain. Lingering
    snow cover in limited northern locations may also contribute to
    excess runoff from added heavy rainfall. Rainfall rates of 1 to 2
    in/hr within areas of training from northeastern IA into
    southeastern MN and portions of western/central WI can be expected
    at times, with storm total rainfall of 1 to 3 inches in a couple
    of locations. These widely scattered instances of heavier rainfall
    could lead to flash flooding within portions of the Upper MS
    Valley through ~06Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6kgfqTSwxWwKfzCXp6PG-UAyu1foOIh4ilYhnayi2dXgpRbpViVpumX8fci7fSoUunxJ= twj7iBcBPU6tjsc2DwGSc9s$ for graphic product...

    ATTN...WFO...ARX...DLH...DMX...DVN...GRB...MKX...MPX...MQT...

    ATTN...RFC...MSR...NWC...

    LAT...LON 48228962 47748933 45408862 43648935 42109078=20
    41619219 42109326 43829283 45429220 47259153=20
    48209035=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 24 01:11:41 2026
    AWUS01 KWNH 240111
    FFGMPD
    OKZ000-KSZ000-240630-

    Mesoscale Precipitation Discussion 0128
    NWS Weather Prediction Center College Park MD
    910 PM EDT Thu Apr 23 2026

    Areas affected...southeastern KS, northeastern OK

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

    Valid 240109Z - 240630Z

    Summary...A focused region of flash flooding is expected to set up
    over portions of southeastern KS into northeastern OK through 06Z.
    Slow movement/training of cells will lead to hourly rainfall of 1
    to 3 inches and storm total rainfall of 2 to 4+ inches over the
    next few hours.

    Discussion...Area radar imagery across the central Plains at 01Z
    showed two intense areas of slow moving convection. First over
    eastern KS, over and just northeast of Wichita and a second area
    over northern OK, bisecting I-35. The northern cluster of storms
    was near the triple point (near ICT) and was associated with an
    outflow boundary which intersected to the west, at the triple
    point. Both areas have been associated with training and resided
    within a very unstable environment with MLCAPE estimated in the
    2500-3500 J/kg range (00Z SPC mesoanalysis and 00Z OKC sounding).
    Fading visible imagery showed cloud streets oriented with the low
    level inflow, south to north, into the northern OK thunderstorms.
    The eastern KS/OK border lay beneath a diffluent upper level jet
    pattern, favorable for increased ascent over the region.

    As the low level jet continues to increase with the diurnal cycle,
    exceeding 50 kt over northeastern OK by 03-04Z (recent RAP
    forecasts), overrunning of the storm-generated cold pools should
    continue to support convective regeneration along the southwestern
    flank of the system with WSW to ENE training, while overall
    southward propagation occurs gradually with time. The low level
    flow is expected to veer by ~06Z which should allow the convective
    cluster to advance eastward away from its current initiation point
    along the dryline. However, up until that happens, locally heavy
    rainfall is expected to support areas of flash flooding with total
    rainfall totals of 2 to 4+ inches likely.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_4IhhlNU2-TD0lf6iOAtxNfWHMxiBhR6ZzQMqDoUwtb1AoqbV-UaP8nALEjLyD8ddVPY= CTr8DwZ8JwE5hBk8Xurdt5A$ for graphic product...

    ATTN...WFO...ICT...OUN...SGF...TOP...TSA...

    ATTN...RFC...TUA...NWC...

    LAT...LON 38339621 38269564 37749511 37399499 36559504=20
    35959602 35739762 35999840 36709810 37739759=20
    38179690=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Apr 24 05:40:39 2026
    AWUS01 KWNH 240540
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-241135-

    Mesoscale Precipitation Discussion 0129
    NWS Weather Prediction Center College Park MD
    138 AM EDT Fri Apr 24 2026

    Areas affected...Central to Northeast OK...Far Southeast
    KS...Southwest MO...Northwest AR

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

    Valid 240538Z - 241135Z

    SUMMARY...Backbuilding and training thunderstorms producing 1.5 to
    2.5 inch/hour rainfall rates will pose a significant urban flash
    flood threat across northern to northeast Oklahoma early this
    morning. Convection will eventually grow upscale into an MCS and
    track east-southeastward into the Ozark Plateau through dawn.
    Broad totals of 2 to 4 inches are expected, with localized amounts
    possibly exceeding 5 inches.

    DISCUSSION...Latest radar and satellite trends depict a highly
    active convective environment across northern Oklahoma.
    Thunderstorms are continuously backbuilding and training along a
    well-defined mesoscale outflow boundary, positioned east of a
    dryline and ahead of a surface wave transiting a cold front. The
    thermodynamic and kinematic environment is exceptionally
    supportive of extreme rainfall rates. A strong 40 to 50+ kt
    southwesterly low-level jet (LLJ) is impinging directly onto the
    outflow boundary, providing intense moisture convergence and
    tapping into a robust instability pool characterized by 2000-3000
    J/kg of MUCAPE. Furthermore, upper-level divergence associated
    with an ejecting trough is providing deep-layer ascent to sustain
    robust convective updrafts.

    Currently, this setup is fostering high-efficiency rainfall rates
    of 1.5 to 2.5 inches/hour. Given the quasi-stationary nature of
    the boundary and the parallel alignment of the convection to the
    deep-layer steering flow, persistent cell-training is occurring.
    This will pose a significant, localized flash flood threat over
    the highly sensitive urban footprints from Stillwater through the
    Tulsa metro over the next few hours.

    As the cold pool eventually strengthens and coalesces, convection
    is expected to grow upscale into an east-southeast propagating
    MCS. However, the strong southwesterly LLJ will continue to favor
    persistent backbuilding on the southwest flank of the convective
    mass, effectively slowing the forward translation of the heaviest
    rainfall cores. High-resolution guidance (including the HRRR and
    00Z HREF) supports widespread 2 to 4 inch totals, but given the
    prolonged training potential, localized storm totals up to 5+
    inches are highly probable.

    Towards sunrise and through the 12Z time frame, this complex will
    push into the Ozark Plateau across southwest Missouri and
    northwest Arkansas. As the low-level flow interacts with the
    complex topography of the Ozarks, mechanical lift will sustain
    high rainfall rates. The steep, flashy basins of this region will
    be highly susceptible to rapid runoff from these accumulations,
    carrying a localized flash flood threat right through the morning
    commute.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!87rVcEPmsU9ex1Yk0K8aWF2Pb8232nBhVf7ItOCXLPVZNzMyriOrFzStjEF4-wbQlPKD= d_jNmt4E0BBYixOlqowwVpI$ for graphic product...

    ATTN...WFO...ICT...LZK...OUN...SGF...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 37729347 37429237 36579207 35939265 35409427=20
    35209635 35369772 35869835 36199831 36419785=20
    36719636 37279469=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Apr 25 04:43:00 2026
    AWUS01 KWNH 250442
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-251000-

    Mesoscale Precipitation Discussion 0130
    NWS Weather Prediction Center College Park MD
    1240 AM EDT Sat Apr 25 2026

    Areas affected...Northeast TX...Far Southeast AR...Northern
    LA...Central MS

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

    Valid 250440Z - 251000Z

    SUMMARY...Locally heavy showers and thunderstorms with some
    cell-training concerns can be expected over the next few hours.
    Rainfall rates of up to 2 inches/hour may result in some isolated
    and mainly urban concerns for flash flooding.

    DISCUSSION...The latest radar and satellite imagery shows
    convection becoming a little more concentrated across portions of
    northeast TX as modest upstream shortwave/jet energy interacts
    with a well-defined outflow boundary and the pooling of rather
    strong instability along it. Meanwhile, farther east across far
    southeast AR and into central MS, an elevated axis of convection
    is seeing with cooling convective tops associated with warm air advection/isentropic ascent over the top of a well-established
    cold pool.

    MUCAPE values across northeast TX and through northern LA and
    southwest MS are on the order of 2000 to 3000 J/kg with modest
    low-level flow in the 850/925 mb layer of only 10 to 20 kts.
    However, there is some deeper layer ascent being facilitated by
    upstream shortwave energy that is embedded within the deeper layer
    westerly flow. This coupled with the low-level warm air advection
    and proximity of the outflow boundary should tend to favor some
    convective sustenance and perhaps further expansion of activity
    over the next few hours across northeast TX through northern LA
    and central MS.

    Given the level of instability and with PWs of near 1.5 inches,
    some of the rainfall rates may reach 2 inches/hour. Alignment with
    the deeper layer westerly steering flow in the 850/300 mb layer
    will suggest at least some concerns for localized cell-training,
    and this may yield some additional rainfall totals of 3 to 4+
    inches. This is also being advertised by some of the 00Z HREF
    guidance.

    Expect at least an isolated and mainly urban concern for flash
    flooding over the next few hours as a result.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ZkRTFNNWkfRCJJ2FBXzVe9MqwfN1u3t6urR953tBOnAQk-O2S2ZLVqfSPcLSDOHzWpy= KyTxBcxFRu0DUi3CEEDBNt0$ for graphic product...

    ATTN...WFO...FWD...JAN...LCH...LIX...LZK...MOB...SHV...

    ATTN...RFC...ALR...FWR...ORN...NWC...

    LAT...LON 33529134 33508963 32928865 32198847 31528903=20
    31269031 31369280 31829516 32229628 32869624=20
    32949521 33049332=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Apr 25 23:06:33 2026
    AWUS01 KWNH 252306
    FFGMPD
    TXZ000-OKZ000-260503-

    Mesoscale Precipitation Discussion 0131
    NWS Weather Prediction Center College Park MD
    704 PM EDT Sat Apr 25 2026

    Areas affected...Northeast TX into Southeast OK

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

    Valid 252303Z - 260503Z

    SUMMARY...A localized flash flood risk exists through the evening
    hours across portions of northeast TX into southwest OK.
    Supercells will be capable of producing heavy rainfall resulting
    in an urban flash flood risk. Additionally, localized cell mergers
    near the warm front may also result in isolated flash flooding.

    DISCUSSION...Supercell activity is expected through the evening,
    with development near a dryline and a warm front near the Red
    River. The environment is characterized by extreme instability
    (MLCAPE around 4000 j/kg) and strong shear (effective bulk shear
    around 50kts). This overlap of ingredients supports supercells
    with very large hail and heightened tornado potential (see SPC
    tornado watch 144). While these are likely the primary hazards
    associated with this convection, an isolated flash flood risk
    could also evolve.

    Limiting factors for heavy rainfall will be the very steep lapse
    rates and some dry air in the mid levels keeping PWs around
    1.4-1.6". However, strong mesocyclones within these supercells
    will enhance lift and help increase rainfall efficiency. This will
    result in heavy rainfall rates, though forecast supercell motions
    off to the east-southeast at 10-20 kts should limit duration.
    Consequently, the flash flood risk will primarily depend on
    supercell mergers or clusters extending duration. This is
    certainly a possibility, especially near the warm front where
    persistent convergence and storm tracks along the front could
    yield some training and local rainfall over 3". Even without cell
    training a localized urban flash flood risk exists as these cells
    can drop 2" of rain quickly.

    Recent HRRR runs seemingly have a decent handle on the expected
    convective evolution through the evening hours. The HRRR depicts
    an uptick in 850mb moisture transport later this evening into
    tonight, which will help sustain activity as convection
    increasingly forward propagates. However, with moisture transport
    persisting over northeast TX towards the Red River, we will need
    to monitor for additional development overnight depending on how
    this evenings supercells impact the instability field. If
    additional development occurs, the pattern would support some
    northwest to southeast training.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7Hyn8ePr9iIUeGEETHZyqRefzkhOuBk5OioV-2JVecsiaT7eE6mGIDCYy8_-xq3Td85K= BOvq6mqBoX6cyy3scyIbpeM$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 34809731 34729657 33959509 33499446 32589480=20
    32489608 32769762 33269827 33829861 34169838=20
    34509800=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Apr 26 00:43:40 2026
    AWUS01 KWNH 260043
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-260641-

    Mesoscale Precipitation Discussion 0132
    NWS Weather Prediction Center College Park MD
    842 PM EDT Sat Apr 25 2026

    Areas affected...Southeast KS, Eastern OK, Western AR

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

    Valid 260041Z - 260641Z

    SUMMARY...An isolated flash flood risk exists from far southeast
    KS into eastern OK and western AR as convection briefly trains
    and/or backbuilds across this corridor.

    DISCUSSION...Convection across southeast KS into eastern OK will
    pose an isolated flash flood risk tonight. This activity is well
    north of the warm front closer to the Red River, but is close to
    the 850mb front and moisture convergence axis. Despite a more
    stable boundary layer, steep lapse rates are resulting in MUCAPE
    over 2000 J/kg, with sufficient deep-layer shear to support
    organized convection and supercell development.

    While high resolution models have struggled with this activity,
    the 23z HRRR and WoFS are now indicating that convection may
    persist or grow upscale into eastern OK and west-central AR, and
    recent observational trends are beginning to show some signs of
    this. The 23z WoFS shows 90th percentile QPF exceeding 3" near the
    OK/AR border. With 850mb moisture transport/convergence forecast
    to maintain or increase a bit over the next several hours over
    this region, this persistence scenario seems plausible.

    There is some uncertainty regarding how convection further south
    (MPD 131) might impact the organization of this northern activity.
    If the activity further south grows upscale enough it could
    negatively impact the intensity and organization of this northern
    activity. However, given that current convection is over
    performing and the environment remains conducive to organized
    development, some flash flood risk exists over the next several
    hours. Recent rainfall has also lowered FFG enough to support
    isolated exceedances as cells move southeast or backbuild.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4B5qv05O2uHwvwtxBdoyY6_GbFqp-NjUbW7aDlr_fQ62iY_gtSdxKKbo5j-a-RZ1gG4U= iPXuhY1u19nB0NBayOk0Qpc$ for graphic product...

    ATTN...WFO...ICT...LZK...SGF...SHV...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 37389624 37029470 35619345 34709341 34329367=20
    34429455 34859503 35549550 36709632=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Apr 26 03:32:56 2026
    AWUS01 KWNH 260332
    FFGMPD
    ARZ000-TXZ000-OKZ000-260930-

    Mesoscale Precipitation Discussion 0133
    NWS Weather Prediction Center College Park MD
    1131 PM EDT Sat Apr 25 2026

    Areas affected...Northern Texas...South-Central to Southeast
    Oklahoma

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

    Valid 260331Z - 260930Z

    SUMMARY...Supercells and merging convective clusters will continue
    to organize and propagate southeastward overnight. An increasingly
    favorable nocturnal environment will support rainfall rates of 2+
    inches/hour. While antecedent conditions are relatively dry,
    intense localized rates and cell-mergers may yield totals of 2 to
    4+ inches, posing especially an urban flash flood threat.

    DISCUSSION...GOES-E IR/WV satellite imagery and recent
    mesoanalysis show a low-amplitude mid-level shortwave trough over
    the Plains interacting with a highly unstable airmass across the
    Red River Valley. A highly conducive thermodynamic environment is
    in place, characterized by PWs of ~1.5 inches, MLCAPE of 2500-3500
    J/kg, and very steep mid-level lapse rates (7.5-8 C/km). This is
    fueling robust supercellular convection, aided by deep-layer shear
    locally exceeding 50 kts. Convection over northern TX remains
    largely surface-based within the warm sector, while activity over
    southern OK is slightly elevated, supported by a stationary front
    and 925 mb frontogenesis.

    Through the overnight hours, the current 20 to 30 kt low-level jet
    is forecast to intensify, and this nocturnal enhancement will
    increase warm air advection and moisture transport directly into
    the Red River Valley, particularly toward south-central and
    southeast OK. Upwind propagation vectors are aligned to the
    southeast, strongly favoring the gradual upscale growth of merging
    supercells into a forward-propagating MCS.

    The 00Z HREF indicates a 20 to 30 percent probability of rainfall
    rates exceeding 2 inches/hour within the heaviest cores. Storm
    totals of 2 to 4 inches are expected, with locally higher amounts
    where cell-training or complex mergers occur. While Flash Flood
    Guidance (FFG) is higher across this corridor due to drier
    antecedent conditions, the sheer intensity of the 2+ inches/hour
    rates will easily outpace infiltration, resulting in isolated to
    scattered areas of flash flooding, especially over any urban
    footprints. This will include portions of the Dallas-Fort Worth
    metropolitan area over the next 1 to 2 hours in particular.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_WY6Q3jdw2wzm8UWjF8F_wtHXHhRQ1mYvg0Bix0Uq_GrsY_cSRLOHLMHc7GdIRqJ-Zu1= RPTZ2V72_NEnGTbwWKMPCMA$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 34429609 33999474 33359420 32639414 32009488=20
    32039649 32519751 32969786 33759788 34269736=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Apr 26 04:02:00 2026
    AWUS01 KWNH 260401
    FFGMPD
    LAZ000-ARZ000-OKZ000-261000-

    Mesoscale Precipitation Discussion 0134
    NWS Weather Prediction Center College Park MD
    1200 AM EDT Sun Apr 26 2026

    Areas affected...Far Eastern Oklahoma...Western and Southern
    Arkansas

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

    Valid 260400Z - 261000Z

    SUMMARY... Elevated thunderstorms will continue to organize and
    drop southeastward across western and southern Arkansas overnight.
    Locally sensitive antecedent conditions combined with rates
    approaching 2 inches/hour will support a likelihood for isolated
    to scattered areas of flash flooding which will include some urban
    impacts.

    DISCUSSION...A broken axis of slow-moving and locally training
    thunderstorms is ongoing across far eastern Oklahoma and western
    Arkansas. Unlike the surface-based activity further southwest,
    this convection is elevated and rooted near the 850 mb layer. It
    is being driven by strong 850 mb frontogenetic lift and the
    proximity of a sharp instability gradient, with the convection
    positioned well within an axis of 1500-2500 J/kg MUCAPE and PWs
    near 1.25 inches.

    Upwind propagation vectors point toward the southeast. Over the
    next several hours, this activity is expected to gradually grow
    upscale, but with multiple MCS clusters dropping southeastward as=20
    through west-central and eventually southern Arkansas. The 00Z
    HREF highlights a 20 to 30 percent probability of 2 inch/hour
    rainfall rates within the heaviest convective elements. Total
    rainfall amounts of 2 to 4 inches are anticipated where some of
    these convective clusters repeat over the same area.

    The primary driver for the flash flood threat in this corridor is
    the relatively sensitive antecedent conditions from recent
    rainfall. The latest NASA SPoRT 0 to 10 cm relative soil moisture
    data indicates highly moist antecedent conditions across eastern
    OK and western AR. With a fairly compromised infiltration
    capacity, the anticipated 2 inch/hour rates and any localized
    cell-training will readily convert to runoff, posing a continued
    flash flood threat through the predawn hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!49ecoj177dP5oakzAcDtYlovBERpppqbFIgfuctrNIPa3OSPO7idsMAYYXD9dWqzzI3D= MC7D4zb9BEuylvWALBqS6Zw$ for graphic product...

    ATTN...WFO...JAN...LZK...SHV...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 36149347 35579257 34639166 33889125 33219159=20
    32989235 33199342 34399461 35469508 36069459=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun Apr 26 21:01:17 2026
    AWUS01 KWNH 262101
    FFGMPD
    MOZ000-OKZ000-KSZ000-270258-

    Mesoscale Precipitation Discussion 0135
    NWS Weather Prediction Center College Park MD
    459 PM EDT Sun Apr 26 2026

    Areas affected...Eastern KS and Western MO

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

    Valid 262058Z - 270258Z

    SUMMARY...A generally progressive convective line crossing Kansas
    will produce locally heavy rainfall. An increase in backbuilding
    or training on the southern extent of the line could lead to
    isolated to scattered areas of flash flooding over the next
    several hours.

    DISCUSSION...Regional radar imagery shows a severe convective line
    progressing eastward across portions of Kansas. Thus far, the
    progressive forward motion of this activity has largely limited
    the flash flood threat. However, the mesoscale environment along
    the southern flank of this line is becoming increasingly
    supportive of additional convective development and possible
    training.

    Recent mesoanalysis indicates PWAT values are currently hovering
    around 1.4 inches. While not extreme overall, these values are
    above the 90th percentile for this time of year, providing
    sufficient moisture for efficient rainfall production. Instability
    is moderate, with MLCAPE currently analyzed around 1000-2000 J/kg.
    Higher instability values upstream are expected to advect into the
    region, driven by increasing southerly low-level moisture
    transport.

    As the primary convective line continues eastward, its progressive
    nature should keep the widespread flash flood threat low. However,
    the increasing moisture transport and instability feeding into the
    southern extent of the line should allow for some new updraft
    development, supporting backbuilding or training of cells. Should
    this mesoscale evolution materialize, localized training of
    intense rainfall rates could overwhelm local drainage capacity or
    sensitive basins, leading to an isolated to scattered flash flood
    threat across portions of eastern KS into adjacent areas of
    west-central MO. The northern extent of the line should remain
    progressive, keeping the threat confined to a localized urban risk.

    Confidence in the exact convective evolution over the next several
    hours remains somewhat below average, as the high-resolution model
    guidance have struggled to accurately handle the ongoing activity
    and placement. However, the 19z HRRR and 18z RRFS are starting to
    show an enhanced QPF signature over southeast KS into west-central
    MO. This supports the idea of an increasing training/backbuilding
    risk over this corridor with 3"+ rainfall possible, potentially
    focused around the southern extent of the outflow from the ongoing
    MCS.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4p2WqBT35d8F_3X-42PbXNVk_-lZoJ1pd66QqUzfhGDbuI7y2SW4U0YvLsxJN3CfoYhw= vDstoC_7o7Zp_Fk5oCgjbzM$ for graphic product...

    ATTN...WFO...EAX...ICT...SGF...TOP...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 39319460 39209427 38809342 38499314 37709302=20
    37129340 37039441 36989570 37009623 37009656=20
    37009692 37049731 37629699 38189612 38559589=20
    39199554 39299504=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Apr 27 02:03:18 2026
    AWUS01 KWNH 270203
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-270800-

    Mesoscale Precipitation Discussion 0136
    NWS Weather Prediction Center College Park MD
    1001 PM EDT Sun Apr 26 2026

    Areas affected...Southeast KS, Southwest MO, Northeast OK

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

    Valid 270200Z - 270800Z

    SUMMARY...Slow moving supercells and cell mergers will pose at
    least an isolated flash flood risk this evening across portions of
    Southeast KS, far northeast OK and southwest MO. The degree of
    upscale growth into a larger convective cluster remains uncertain,
    keeping confidence lower for a more widespread threat.

    DISCUSSION...Regional radar imagery currently depicts scattered
    supercellular convection ongoing across the region. Recent
    mesoanalysis indicates impressive MLCAPE ranging from 1500 to 3000
    J/kg collocated with strong deep layer shear. Moisture is
    moderate, with PW values analyzed around 1.3-1.5 inches, but
    rainfall efficiency will likely be enhanced within any stronger
    mesocyclones.

    Over the next several hours, large scale forcing for ascent is
    expected to gradually increase as a shortwave trough approaches
    from the west, accompanied by strengthening upper level
    divergence. Concurrently, low level moisture transport and
    convergence are forecast to intensify this evening. This evolution
    should promote at least some upscale growth of the ongoing
    convection into larger multi-cell clusters that slowly move off to
    the east-southeast. As convective coverage increases, the risk of
    cell mergers, backbuilding, and training will naturally rise,
    setting the stage for localized swaths of heavier rainfall.

    There remains some uncertainty regarding the exact degree of
    upscale growth this evening. At a minimum, the slow-moving nature
    of the ongoing supercells combined with a few cell mergers should
    result in at least an isolated flash flood risk. At a maximum, the
    increasing moisture convergence and large scale forcing will drive
    enough upscale convective growth to force a more focused area of
    flash flooding.

    Despite the uncertainty in the exact convective evolution, high
    resolution guidance highlights the heavy rainfall ceiling should
    consolidation occur. Notably, 00z WoFS depicts over an 90%
    probability of exceeding 3 inches of rainfall in a swath near the
    KS/OK/MO intersection, a 40-70% probability of localized totals
    exceeding 5 inches, and a 90th percentile rainfall of 7". The
    exact footprint of the WoFS may not perfectly verify, but it
    illustrates a realistic heavy rainfall potential given the
    ingredients currently in place.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9asc44z1Ie5HYee6Y51YDr4OzdBO8kbY-qpON2I9YMJvG8HCwnHWTsBRCpzNvuEj_5v4= bE2A5l3wPdn3uZpdrxV01Nw$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...LZK...SGF...TOP...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 38659279 38429233 37739183 36759218 36489325=20
    36449456 36559611 36999644 37759574 38059519=20
    38349420=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Apr 27 05:17:38 2026
    AWUS01 KWNH 270517
    FFGMPD
    MOZ000-KSZ000-NEZ000-271115-

    Mesoscale Precipitation Discussion 0137
    NWS Weather Prediction Center College Park MD
    115 AM EDT Mon Apr 27 2026

    Areas affected...Central and Eastern KS...West-Central and
    Northwest MO

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

    Valid 270515Z - 271115Z

    SUMMARY...An intensifying nocturnal low-level jet will foster a
    corridor of heavy, and locally training thunderstorms across
    portions of central and eastern Kansas through west-central and
    northwest Missouri overnight and into early Monday morning.
    High-efficiency rainfall rates of 1 to 2 inches/hour and localized
    storm totals of 2 to 4+ inches are expected. A concern for urban
    flash flooding will exist.

    DISCUSSION...Radar and satellite imagery is showing the
    development and expansion of cold-topped convection across central
    Kansas as upstream shortwave energy/troughing ejects east across
    the central High Plains and interacts with the nose of an
    increasingly strong southwesterly low-level jet. This is
    coinciding with the pooling of strong instability along and
    poleward of a warm front across southern Kansas.

    MUCAPE values are as high as 2000 to 3000 J/kg with PWs locally as
    high as about 1.25 inches. The increasing low-level jet overnight
    in conjunction with strengthening DPVA/jet-dynamics downstream of
    the approaching trough will facilitate upscale growth of
    convection over the next few hours across central and gradually
    eastern Kansas. Some of the latest guidance, and notably the HRRR
    solutions, suggests a well-defined surface low evolution from
    southwest to northeast Kansas by late tonight which would focus
    enhanced moisture transport and forcing up across areas of eastern
    Kansas and eventually northwest Missouri early Monday morning as
    the aforementioned warm front lifts northeastward.

    Given the level of low-level jet energy (reaching 40 to 50+ kts)
    and the high CAPE values nosing in aloft, the rainfall rates are
    likely to be rather high, and capable reaching well into the 1 to
    2 inch/hour range. This is generally supported by the 00Z HREF
    guidance, and especially recent HRRR runs. Alignment of the
    convection with the deeper layer westerly flow suggests a
    favorable environment for cell-training.

    The overall consensus of the CAM guidance would favor 2 to 4 inch
    rainfall totals with locally higher amounts possible going through
    the predawn hours. A concern will exist for urban flash flooding
    over the next several hours going through early Monday morning.
    Some areas that may see impacts will include the urban corridor
    from Manhattan through Topeka and the Kansas City metropolitan
    area.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-ASARoRq9Kw1WBYaLM81msO1W3Seni468uazA5s_h98oCspoXsKP1MqJ3uxOyuzvamTx= Ggq5WNHlCMehUFVCuCF3aro$ for graphic product...

    ATTN...WFO...EAX...GID...ICT...LSX...OAX...TOP...

    ATTN...RFC...KRF...MSR...TUA...NWC...

    LAT...LON 40249349 39989238 39429199 38939253 38399439=20
    38179626 38319799 38709869 39199870 39649764=20
    39979620 40169497=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Apr 27 09:40:10 2026
    AWUS01 KWNH 270940
    FFGMPD
    ILZ000-MOZ000-IAZ000-KSZ000-NEZ000-271535-

    Mesoscale Precipitation Discussion 0138
    NWS Weather Prediction Center College Park MD
    537 AM EDT Mon Apr 27 2026

    Areas affected...Northeast and East-Central KS...Central and
    Northern MO...West-Central IL

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

    Valid 270937Z - 271535Z

    SUMMARY...Flash flooding will be likely going through the morning
    hours from locally training thunderstorms that will be capable of
    producing 1 to 2 inch/hour rainfall rates. Additional rainfall
    totals of 2 to 4 inches with isolated heavier totals will be
    possible by midday, with a threat for locally significant urban
    flash flooding impacts as a result.

    DISCUSSION...Radar and satellite imagery shows a well-defined axis
    of heavy showers and thunderstorms impacting portions of northern
    and eastern KS, with activity very quickly advancing into
    northwest MO. This includes the Topeka and Kansas City
    metropolitan areas. Deep convection with cold convective tops as
    low as -70C are noted across the region, and the activity is
    exhibiting several overshooting tops which is indicative of
    particularly strong convective updrafts and enhanced rain rates.

    The activity continues to advance generally off to the east in
    association with an ejecting shortwave trough across western and
    central KS with excellent divergence aloft working in tandem with
    a southwest low-level jet of 50 to 60 kts around the southeast
    flank of multiple waves of surface low pressure. These ejecting
    waves of low pressure are helping to channel enhanced moisture and
    instability transport across eastern KS and into western and
    northern MO as a warm front gradually gains latitude downstream
    across central MO and southern IL.

    MUCAPE values are as high as 2000 to 3000 J/kg with PWs locally as
    high as about 1.5 inches across eastern KS and nosing through
    northern MO. This favorable thermodynamic environment coupled with
    enhanced kinematic wind fields/shear will strongly support a
    continuation of organized MCS activity traversing the Lower MO
    Valley this morning with convection likely becoming more
    concentrated by mid-morning across north-central MO and eventually
    into areas of west-central IL.

    Rainfall rates will easily be into the 1 to 2 inch/hour range, and
    with an excellent cell-training environment, some additional
    rainfall totals of 2 to 4 inches with isolated heavier amounts
    will be possible. Flash flooding is already occurring over parts
    of east-central and northeast KS through west-central MO including
    the Topeka and Kansas City metropolitan areas. Additional rounds
    of heavy rainfall over the next couple of hours here will support
    the potential for significant urban flash flooding impacts.

    Areas downstream across north-central MO and eventually
    west-central IL will likely see the threat for at least some flash
    flooding increase through the morning hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!66y8OBhaLeMgVBXpqi8DQMipRKbuYpDzNqw7oHVGloPDpxjTclEv-g8PmUDU_qnTar1B= XVoSaeMuRfh-HxGzh4KmGj0$ for graphic product...

    ATTN...WFO...DVN...EAX...ICT...ILX...LSX...SGF...TOP...

    ATTN...RFC...KRF...MSR...TUA...NWC...

    LAT...LON 40489182 40358991 39618884 38658930 38359141=20
    38249425 38349620 38679675 39239685 39759618=20
    40149478 40369334=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Apr 27 14:47:35 2026
    AWUS01 KWNH 271447
    FFGMPD
    INZ000-ILZ000-MOZ000-272045-

    Mesoscale Precipitation Discussion 0139
    NWS Weather Prediction Center College Park MD
    1046 AM EDT Mon Apr 27 2026

    Areas affected...Central Illinois through Greater St. Louis into
    Indiana

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

    Valid 271445Z - 272045Z

    SUMMARY...Flash flooding threat continues to progress east across
    Illinois through midday with a risk for training thunderstorms
    that produce 1 to 2 inch/hour rainfall rates. Rainfall totals of 2
    to 3 inches with isolated heavier totals are possible through the
    afternoon, with a threat for locally significant urban flash
    flooding impacts.

    DISCUSSION...A well-defined bowing line of thunderstorms with
    areas with rates up to 1.5"/hr is pushing into central Illinois
    with a tail extending to west-central Missouri. This is generally
    north of the St. Louis metropolitan area, but impacts will
    eventually reach there today. Scattered prefrontal activity from
    central to southern Illinois will also continue to develop and
    shift northeast.

    The activity is ahead of a shortwave trough over central KS with
    excellent divergence aloft working in tandem with a southwesterly
    low-level jet of 45 to 55 kts ahead of the surface low center near
    the KS/MO border. Enhanced moisture and instability continues to
    flow across southern MO and IL.

    MUCAPE values of 2000 to 3000 J/kg with PW around 1.5 inches
    across up the mid-Miss Valley. This favorable thermodynamic
    environment coupled with enhanced kinematic wind fields/shear will
    strongly support a continuation of organized MCS activity across
    central IL with the right tail laying down near I-70/St. Louis.

    Rainfall rates will remain in the 1 to 2 inch/hour range with
    localized additional rainfall totals of 2 to 3 inches. The
    progression of the system has recluded further flash flood
    warnings over eastern MO into IL, but given increasing coverage in
    central IL and the right flank laying down orthogonal to the
    inflow will be the focus for flash flooding in addition to urban
    areas.

    This activity will progress into Indiana this afternoon and
    further discussions are likely.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9SHhxJT_jN2-DO0zt70zh1rRab8y-4DUoh6jQXRFeyBSIikyzuH8Z0CGHa2s22PSm0gj= Jpfy_XDW1aSxsG6meub3gMQ$ for graphic product...

    ATTN...WFO...DVN...EAX...ILX...IND...IWX...LMK...LOT...LSX...
    PAH...SGF...

    ATTN...RFC...KRF...MSR...ORN...TIR...NWC...

    LAT...LON 41248926 41218700 40118643 38998649 38228721=20
    37888830 38178932 38189029 37849235 38059308=20
    38439333 38899204 39359064 40089034 40959066=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Apr 27 18:57:36 2026
    AWUS01 KWNH 271857
    FFGMPD
    OHZ000-TNZ000-KYZ000-INZ000-ILZ000-MOZ000-ARZ000-280030-

    Mesoscale Precipitation Discussion 0140
    NWS Weather Prediction Center College Park MD
    257 PM EDT Mon Apr 27 2026

    Areas affected...Southern IND...Southeast IL...Northwest KY...
    Bootheel of MO...Extreme Western OH...

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

    Valid 271900Z - 280030Z

    SUMMARY...Weakening of initial MCS and flanking WAA cells in the
    Lower Ohio River Valley. Rates up to 1.5"/hr and stripes of 2-3"
    still pose possible localized flash flooding concerns through
    evening hours.

    DISCUSSION...Regional RADAR and GOES-E Visible loop denote a
    decaying MCS continuing to advance eastward recently crossing the
    central IND/IL border. Though the MCV is shearing to the
    northeast in a degrading stratiform region, the southeast flank
    remains fairly active with a few scattered individual cells
    extending southward from the elevated warm front moving across the
    Ohio River proper. VWP still depicts strong low level southerly
    flow veering to southwest through S IL with 40-50kts through 700mb
    providing the advection of the higher theta-E air over the stable
    (reinforced by morning cloudy conditions) over south-central to
    southeast IND.

    Still,the higher moisture availability along with building sharp
    MUCAPE gradient to 500-2000 J/kg advecting northeast to help
    maintain these cells; through strengthening is probably a bit more
    limited. There remain strong flux convergence to support 1.5"/hr
    rates with occasional localized peaks to near 2". Combine these
    rates with a slightly flattening of the convective line to the
    deep mean steering flow should still support localized 2-3"
    streaks through the late afternoon into the evening hours. Strong
    upstream convergence would also support flanking
    cell/back-building environment to further increase overall
    coverage of thunderstorm activity...particularly across S IND and
    far the Ohio River counties of northwest KY.

    Relative soil moisture values are slightly below average and FFG
    values reflect this slightly higher requirement for exceedance and
    result in flash flooding to be considered possible and localized,
    though intersection with any urban center would increase this
    potential.

    Upstream shortwave will result in an additional line of strong convection/thunderstorm activity that will pose a higher potential
    for flash flooding into the overnight period; so even if this
    round doesn't result in flooding, it will saturate the upper soils
    likely to increase runoff problems. As such, please keep
    weather-wise to local WFO warnings and advisory and subsequent
    MPDs later this evening.

    ...MO Bootheel/S IL...
    Deeper in the warm sector across the Tri-River Confluence area,
    instability has built to over 3000 J/kg given temps nearing
    mid-80s and Tds into the low 70s. Capping will likely limit
    convective development, but Hi-Res CAMS still suggest isolated
    broader updraft cores. Departure from steering of exiting MCS
    influence and upstream height-falls over IA, leaves steering flow
    a bit reduced and muddled to allow for slower motions perhaps with
    some weak updraft rotation to further deflect forward propagation.
    Any cells that can form in this regime will have solid capability
    of 2"/hr rates give 1.5-1.75" total PWat and confluent low level
    flux convergence if they do develop. As such, quick compiling
    could be an issue given hourly FFG values of 1.5-2" and
    2-3.5"/3hrs and may also result in a possible incident or two
    localized flash flooding before cold frontal line later into the
    overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7BM7XiGh5nW6vF2CTMkPjRTSCsscWaLSbEvHhHDU4XFRRrOaiqSgEmaxEDU2zQBLglRP= CI3del5BhrzAEAXL7d0FoQA$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...IWX...LMK...MEG...PAH...

    ATTN...RFC...MSR...ORN...TIR...NWC...

    LAT...LON 40658478 39888425 38948457 38378532 37978609=20
    37288766 36808856 36288976 36629045 37328982=20
    38198890 38778835 40028703 40548594=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Apr 27 19:58:40 2026
    AWUS01 KWNH 271958
    FFGMPD
    ILZ000-MOZ000-KSZ000-280200-

    Mesoscale Precipitation Discussion 0141
    NWS Weather Prediction Center College Park MD
    358 PM EDT Mon Apr 27 2026

    Areas affected...Central to Southern Illinois and Missouri...

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

    Valid 272000Z - 280200Z

    SUMMARY...Repeating Thunderstorms capable of 3-6" totals across
    portions of Southern IL. More scattered, less efficient cells
    upstream may repeat across saturated grounds in the Ozark Plateau
    with more localized/scattered flash flooding likely too.

    DISCUSSION...The environmental setup looks conducive for repeating
    rounds of thunderstorm activity across portions of eastern
    Missouri into south-central IL through the evening into early
    overnight period, prolonging the potential for flash flooding
    condtions. A well-defined thermal boundary extends across central
    MO from near Fort Scott, KS to south of Jefferson City to near St.
    Louis, in response to this morning's MCS. Temperatures have
    returned to the low 80s with low 70s Tds in the lower elevations
    surrounding the Ozarks, with upper 60s Tds within the Plateau.=20
    However, CIRA LPW denotes, the core of the warm conveyor belt has
    translated across SE MO into S IL responding to the initial
    short-wave that sparked the MCS last night that has exited into
    the Great Lakes Region. The main upper-level trof and
    height-falls are starting to advance eastward over the
    Upper-Midwest and broader LLJ has backed to southerly in response;
    though a dry-slot can be seen nosing into from the SW over NE OK
    into SW OK. As such, a very unstable environment with MLCAPEs to
    3000 J/kg extends the length of the frontal zone with bimodal
    strong sfc to boundary layer moisture convergence maxima along the
    western end near the advancing northern stream cold
    front/height-falls in KS and along the warm conveyor belt from
    St.Louis to the old MCS squall line in SW IND.

    Reduced moisture into the upstream cells near the cold front will
    help reduce overall rates and while the updrafts will support more
    severe signatures of hail, winds and possible tornadoes (see SPC
    MCD 572), the compromised soils from the heavy rainfall last night
    2-5" have reduced FFG values to less than 1.5"/hr and broadly less
    than 2"/3hrs across much of the MO portion of the MPD. So
    accompanying the severe, will be solid moisture flux to support
    hourly rates of 1.5"/hr with much coming in sub-hourly
    time-frames. So flash flooding is likely along and south of the
    front especially between I-70 and I-44, though may be more
    localized and these isolated totals should be less than 3".

    Downstream, ongoing strong thunderstorms are intersecting the
    45-50kt SWly LLJ within the core of the warm conveyor belt/q-axis
    through the Mississippi River Valley. some post-MCS recovery has
    resulted in elevated MUCAPE back to 2500 J/kg and convection is
    once again expanding along the convergence line from the old MCS
    cold pool back along the remaining thermal boundary. Flux
    convergence will support rates up to 2"/hr though WoFS 5-min and
    HRRR 15-min totals suggest most will be sub-hourly in the cores of
    the broader downdrafts, with max values of .4-.5" and 1.25-1.4"
    respectively. Deep layer steering the wake of the inital
    shortwave and the relatively digging upstream shortwave support
    flow that is fairly parallel to the boundary with some
    south-southeast forward propagation with time. As such, a
    prolonged training/repeat environment is developing across the
    eastern portion of the MPD generally along and just south of I-70.
    Hi-Res CAMS including the HRRR and WoFS support areas of 3-5"
    with above average confidence particulalry further east, though
    the more rapidly refreshing solutions show a southward trend
    consistent with current Vis, RADAR loops. WoFS forecast mean
    around 4" and 90th percentile near 6" is a solid range though 00z;
    with a line of 2-3" back toward St. Louis ans the cold front fills
    in with another round. These totals are likely to result in flash
    flooding this evening into early overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_aWbu-ODH-Z-xIypGr_plPoXuzgvV27KplbdkmEpfRI3JIx56NWGYHNxRheEHzARg7wF= 6PDpCniPq67qjBNYitr3lsI$ for graphic product...

    ATTN...WFO...EAX...ILX...LSX...PAH...SGF...

    ATTN...RFC...KRF...MSR...ORN...TIR...TUA...NWC...

    LAT...LON 39718957 39718841 39448778 38758767 38188820=20
    37878902 37669009 37509105 37369209 37339298=20
    37429453 38239463 38619417 39499140=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Apr 27 21:37:49 2026
    AWUS01 KWNH 272137
    FFGMPD
    INZ000-ILZ000-MOZ000-280200-

    Mesoscale Precipitation Discussion 0142
    NWS Weather Prediction Center College Park MD
    537 PM EDT Mon Apr 27 2026

    Areas affected...Central and Northeast IL...Far Northeast MO...Far
    Northwest IND...

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

    Valid 272140Z - 280200Z

    SUMMARY...Elevated convection with capability of 1.5"/hr rates and
    totals up to 2.5" due to short-term repeating across recently
    saturated/low FFG soils pose possible localized flash flooding
    risk, especially near prone urban centers.

    DISCUSSION...GOES-WV shows shortwave at the base of mean longwave
    trough over the NEB/IA/MO/KS intersection lifting northeast
    providing solid DPVA along and downstream in northern MO. Low
    level jet response has been to lift the old outflow boundary/front
    northward over the last few hours with solid boundary layer WAA
    confluent along the upwind edge of a old surface pressure
    trough/convergence axis from Keokuk north through SW WI. As such,
    theta-E ascent along with some insolation recovery over central IL
    has seen a narrow wedge of increasing MLCAPE to 2000-2500 J/kg
    into far NE MO along the pressure trough but well ahead of the
    approaching cold front. Southeasterly surface flow with Tds in
    the the low 60s combined with the southerly 925-850mb proving
    sufficient moisture flux as well to feed developing thunderstorms
    along this axis.=20

    Hi-Res CAMs including the 18z Nam-Nest have shown a steady
    increasing trend to convective vigor and coverage into central IL
    toward the evening. Rates of 1-1.5"/hr are expected given the
    strengthening moisture flux convergence in the sharpening
    deformation zone/north of the main front ahead of the height-fall
    maximum. Cells will be faster moving along the nose of the 110kt
    jet streak but should be aligned for an hour or so, before
    eastward propagation stops the short-term training. Short-term
    totals should be 1-1.5" but in these streaks of short-term core
    training (especially over the next few hours), a spot or two of
    2.5" could be possible. Overall, the grounds had lower FFG due to
    higher seasonal rains, but this morning's MCS helped to saturate
    the upper soils, so capacity is slightly reduced. FFG values of
    1-1.5"/hr and less than 2"/3hr (especially further south across
    central IL) remain possible to be exceeded over the next few
    hours. Additionally, there is a lower possibility that cells may
    maintain or build far enough north before the height-falls/cold
    front wash over that sub-urban and southern Chicagoland may see
    these quick hitting sub-hourly 1"+ totals, which has typically
    been an issue for urban flooding as well.=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4ELlyUm2NjQ_I-_GsHCFMVuqWEqlwknvPVl0At1OkAjcVlkn4QobN80G9Bp10dA5l_1N= gVBeHe0ciysiWJHicAtw5zI$ for graphic product...

    ATTN...WFO...DVN...ILX...IND...IWX...LOT...LSX...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 42058784 41588676 40918642 40278668 39628790=20
    39538839 39449018 39319217 40639101 41588936=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Apr 28 00:30:20 2026
    AWUS01 KWNH 280030
    FFGMPD
    OHZ000-KYZ000-INZ000-ILZ000-MOZ000-280630-

    Mesoscale Precipitation Discussion 0143
    NWS Weather Prediction Center College Park MD
    829 PM EDT Mon Apr 27 2026

    Areas affected...Southeast Illinois...Central & Southern
    Indiana...Northwest Kentucky...Ext. Southwest Ohio...

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

    Valid 280030Z - 280630Z

    SUMMARY...Ongoing isentropic ascent over saturated areas for a few
    more hours before cold front convection rolls through with an an
    additional 1-2" in hour for localized pockets of additional 2-4"
    totals. Scattered localized incidents of flash flooding likely to
    continue overnight.

    DISCUSSION...00z surface analysis continues to show broad SSWly
    flow through the MS Valley intersecting a well defined and
    deepening cold pool from the prolonged MCS from last evening. The
    outflow boundary extends from south of CVG to SDF before
    intersecting the stationary front/effective warm front northeast
    of Evansville, IND. The warm front has slowly shifted eastward
    out of the MS Valley and generally in the vicinity of the
    Tennessee River. A 999mb surface just moved through the St. Louis
    Metro as the cold front is starting to surge eastward under the
    influence of the strong height-falls from the shortwave across
    northern MO at this time. As such, the LLJ has responded by
    broadening with VWP denoted 40-50kts of SSW intersecting the old
    outflow. East toward the outflow boundary, the instability is
    reduced just east and cells have fractured though still remain on
    a fairly favorable west to east repeating orientation across SW
    IND into NW KY near Louisville. Core of the warm conveyor
    belt/q-axis is aligned here with TPW values remaining above 1.5",
    with maximized values near 1.75" along the Wabash. As such, these
    cells remain fairly efficient occasionally reaching 2"/hr though
    1.5" seems to be average, though with some southward propagation
    of the cold pool, the overlap with areas flooded earlier this
    evening is decreasing resulting in a broader area of 2-4" totals,
    which is at or just above 1 to 3hr FFG values suggesting flooding
    is likely to continue locally, particularly in/near urban centers
    due to broad areas of hydrophobic surfaces.

    Upstream, the instability axis remains west of the moisture axis,
    due to slightly steeper mid-level lapse rates/intrusion of
    mid-level EML across SW to east-central MO. MLCAPEs of 2500 J/kg
    nose toward the surface low and frontal zone across S IL with 3500
    J/kg values upstream in SE MO to feed increased convective
    activity along the front. As such, convergence is maximized near
    the surface wave and stationary boundary and will likely maintain stronger/broader updrafts capable of highly efficient rainfall
    production. However, deep layer steering due to the height-falls,
    mid-level stronger jet has been and will reduce residency time and
    limit additional rainfall totals to 1-2", likely in 30 to 60
    minutes as the track through the saturated areas of south-central
    IL and eventually intersection with the ongoing west to east
    repeating cells and saturated areas of Southern IND. The
    quickness of rates/totals will more likely further expand any
    ongoing flooded areas, with some spots receiving up to an
    additional 4"+ through 06z.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8KNIAifvnIXx1Byaywpt-fsTJkLkuReKRQVvn4nVPGbAODsYBnBx59QQpmYyt-g-gXqN= KeEzzY-iithZeJgeeKbfjMo$ for graphic product...

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

    ATTN...RFC...MSR...ORN...TIR...NWC...

    LAT...LON 40258674 40238524 39498436 38508404 37858439=20
    37218647 36698861 37268959 38588882 39388815=20
    39918738=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Apr 28 01:38:18 2026
    AWUS01 KWNH 280138
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-280700-

    Mesoscale Precipitation Discussion 0144
    NWS Weather Prediction Center College Park MD
    937 PM EDT Mon Apr 27 2026

    Areas affected...Northeast Texas...Far Southwest Arkansas...Far
    Northwest Louisiana...

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

    Valid 280140Z - 280700Z

    SUMMARY...Slow right moving supercells with very high moisture
    flux and capability of 2-2.5"/hr rates pose highly localized 2-4"
    streaks capable of localized flash flooding in early overnight
    period.

    DISCUSSION...Surface and CIRA Sfc-850 LPW show a very moist
    boundary layer with a surge of Gulf moisture reaching the Red
    River though eastern TX with Tds in the middle 70s with a few
    upper 70s values dotted across. A dry line bulge exists across
    south-central OK with a surface wave near KSRE and the cold front
    slowly sagging southward across central to northeast OK. With
    loss of day-time heating/mixing, the dry line is already starting
    to retrograde as surface winds back to south and southeast in NE
    TX providing the convergence necessary to break the stronger cap
    near and northeast of the Dallas metro area in the last few hours.
    A few cells further north with reduced convergence, weakened, but
    now the the updrafts are established with ample rotation, the
    moisture flux is likely sufficient to maintain these cells.
    MLCAPEs of 4500 J/kg will keep updrafts strong to maintain
    increased isallobaric inflow.

    Additionally, given the stronger updraft rotation, cell motions
    are also going to decrease supporting increased residency of the
    cells. Currently, hail production has been dominant, but KDP
    signals have shown heavy rainfall production is starting to be
    more focused as well for the pair of right mover in Rockwall and
    Hopkins county.=20

    Given the strong inflow of those 70s Tds and overall TPW to 1.75",
    rates of 2-2.5"/hr are possible, especially as the updrafts
    broaden the overall profile moistens. As such, localized 3-4"
    totals are considered possible. While FFG values are naturally
    high and soils are dry, that means they are fairly hard as well,
    reducing uptake of the amount of water at that rate, suggesting
    localized flash flooding/rapid inundation ponding in urban areas
    is considered possible overnight.=20=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6uosHqGob-xjnGhbejXdEU3F7-7NlQfzF9s2CorLea9v0kO_jK6X2iAtxeYlLFGpo4Ki= v2gihXiT9rQgN1j4le0_Dvc$ for graphic product...

    ATTN...WFO...FWD...SHV...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 33759449 33559344 32999304 32419346 32289498=20
    32299563 32409658 32879705 33439661 33709572=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Apr 28 15:25:43 2026
    AWUS01 KWNH 281525
    FFGMPD
    ALZ000-MSZ000-282030-

    Mesoscale Precipitation Discussion 0145
    NWS Weather Prediction Center College Park MD
    1124 AM EDT Tue Apr 28 2026

    Areas affected...north-central MS into central AL

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

    Valid 281520Z - 282030Z

    SUMMARY...Training and repeating thunderstorms are expected for
    portions of north-central MS into central AL through the early
    afternoon. Peak hourly rainfall of 1-2 inches will occur (locally
    higher values possible) within areas of training with localized
    flash flooding possible.

    DISCUSSION...Radar imagery from 1510Z across northern MS and
    north-central AL showed scattered thunderstorms located north of
    an outflow boundary that stretched from near GWO to TCL to EUF.
    The western end of the ouflow boundary has been nearly stationary
    over the past few hours and 0-1 km AGL winds were from the SSW at
    15-20 kt, overrunning the outflow boundary and allowing for some
    very brief training and peak hourly rainfall up to ~1 inch at
    times. Aloft, flow was diffluent, helping to support broader scale
    ascent across the region. 12Z soundings from FFC to BMX to JAN
    showed that MUCAPE varied across the South, with MUCAPE values
    increasing toward the west with 1500-2000 J/kg at JAN.

    Recent forecasts from the RAP do not show any significant changes
    to elevated instability values from MS into AL through 21Z but do
    show the low level flow weakening and veering a bit. Therefore, it
    is unclear how much upstream development will continue but there
    will continue to be some degree of overrunning and likely upstream
    thunderstorm development for at least the next 2-4 hours, aided by
    subtle impulses aloft within the WSW mid-level flow. There will be
    the potential for repeating cells and training along and north of
    the outflow boundary with hourly rainfall of 1-2 inches and
    localized 3 to 4+ inch totals within 2 to 3 hours, possibly
    leading to localized flash flooding. Largely dry antecedent
    conditions may limit any flash flooding to urban or otherwise
    sensitive locations.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4vGPCOKiulQUd15Il53z5GxqSm1yeN7rH_TetrmvIGmf_YUMQdaF-iv9DWHNJB-L9jAs= RDtpHjlAvUBA874txxJ0VI0$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...MEG...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34488940 34228763 33688616 32828591 32308649=20
    32258763 32918901 33409048 34089045=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Apr 28 18:35:04 2026
    AWUS01 KWNH 281834
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-OKZ000-290015-

    Mesoscale Precipitation Discussion 0146
    NWS Weather Prediction Center College Park MD
    234 PM EDT Tue Apr 28 2026

    Areas affected...southeastern OK/northeastern TX into southern
    AR/northern LA

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

    Valid 281832Z - 290015Z

    SUMMARY...An increase in the coverage of thunderstorms is expected
    across portions of southeastern OK/northern-northeastern TX into
    southern AR/northern LA through the afternoon. Repeating and brief
    training of heavy rain could result in isolated 3 to 5 inch totals
    within a 2 to 3 hours window along with flash flooding, although
    any coverage of these higher rainfall values should remain limited.

    DISCUSSION...18Z surface observations helped place a
    quasi-stationary front from a low near the Red River, northwest of
    SPS, east-northeastward into central AR. The environment along and
    south of the front was very unstable with MLCAPE of 2500 to 4000+
    J/kg via 18Z SPC mesoanalysis data. Scattered thunderstorms were
    ongoing along and north of the front from south-central MO into
    western and southern AR, with motions averaging 30-40 kt toward
    the ENE. It was relatively quiet to the west but upstream, water
    vapor imagery showed a shortwave trough axis over the southern TX
    Panhandle with movement approaching the Red River. Visible imagery
    showed the early stages of convective development ahead of the
    dryline and near the stationary front ahead of the Red River
    surface low.

    Additional thunderstorm development within the unstable airmass is
    likely over the next few hours as upstream energy interacts with
    numerous boundaries (including an outflow boundary currently
    between the DFW Metroplex and the Red River) and the unstable
    environment where CIN is continuing to decrease with daytime
    heating. Sufficient shear exists for organized cells, with
    supercells and multicells containing movement from the W or WSW.
    While the general movement of most cells should be progressive
    toward the east, there is potential for some localized upstream
    redevelopment and brief training which could result in 1 to 2
    in/hr rates and 3 to 5 inch totals on an isolated basis.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_bGaOFFGjC6XB_HKwCI2eTopET_qfHn6SCXLfVcbDxgy9iAvjk0ir3l3fMI5jxzdH5H4= DSxNWgGytZKGc1DZrIrWe7s$ for graphic product...

    ATTN...WFO...FWD...JAN...LZK...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35449344 34919229 34009119 33359107 32789167=20
    32099310 31649567 31949757 32789856 33479896=20
    34219876 34709773 34929555=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Apr 28 20:31:48 2026
    AWUS01 KWNH 282031
    FFGMPD
    TNZ000-KYZ000-ALZ000-MSZ000-MOZ000-ARZ000-290200-

    Mesoscale Precipitation Discussion 0147
    NWS Weather Prediction Center College Park MD
    430 PM EDT Tue Apr 28 2026

    Areas affected...Western & Middle TN...Northern MS...Northwest
    AL...Eastern AR...Southwest KY...

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

    Valid 282030Z - 290200Z

    SUMMARY...Congealing clusters with rates of 2"/hr to have widely
    scattered to scattered 2-3.5" totals in 2-3hrs posing possible
    localized incident or two of flash flooding.

    DISCUSSION...GOES-E Vis and 10.3um EIR loops along with regional
    RADAR composite, denotes the scattered clusters of thunderstorms
    are starting to congeal across eastern AR with merging
    up/downdraft structures. Overshooting top/billowing anvils are
    denote the modest upper-level divergence in the area along the
    southern split in the polar (right exit)/subtropical jet. This is
    supporting accelerating low-level flow with confluence in boundary
    layer though the MS River Valley. Within this low level advection
    regime, surface Tds in the mid-70s and CIRA LPW core of sfc-850mb
    moisture near .75-1" value across southern AR should be advected
    well into the complex increasing efficiency with time. As such,
    the expansion coverage of ascent is increasing sufficiently to
    support broadening 1.75-2"/hr rates, with some overall residency
    time to likely support some localized 2-3.5" totals in 2-3hrs.=20
    Downstream instability pool of 2500-3000 J/kg of MLCAPE should
    help to maintain/expand the complex across western TN into middle
    TN with some possible southward building into N MS given the
    favorable moisture environment further south as well.=20

    Hydrologically, the grounds remain very hard and dry with RSM
    0-40cm values around or below 30%. This hardness given the
    magnitude of rates will be less absorptive at least initially,
    that runoff should be higher than would be expected in such
    drought conditions. Additionally, the FFG values across much of
    TN are 1.5-2"/hr and generally 2-3" so widely scattered to
    scattered incidents of flash flooding are considered possible
    given the expected 2"/hr rates and spots up to 3.5". Obviously,
    intersection with urban settings would further increase the
    probability of localized flash flooding.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7mxcq72tpRSbVi7H-XJMWjSBLC6IGrpesCWwJmoE1oRh0KDjI0fujRI8x9LPHEgnO0oo= x2yhA74l2HC9WH1KV5QFRo4$ for graphic product...

    ATTN...WFO...HUN...LMK...MEG...OHX...PAH...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 36948711 36878647 36488589 35678617 35148675=20
    34748778 34358945 34269016 34439090 35259095=20
    35849076 36268997 36698868=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Apr 28 20:55:17 2026
    AWUS01 KWNH 282055
    FFGMPD
    ALZ000-MSZ000-290200-

    Mesoscale Precipitation Discussion 0148
    NWS Weather Prediction Center College Park MD
    453 PM EDT Tue Apr 28 2026

    Areas affected...Central Mississippi...Central Alabama...

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

    Valid 282055Z - 290200Z

    SUMMARY...Expanding Complex of Thunderstorms with capability of
    2"/hr rates approaching areas saturated this morning, as well as,
    lingering scattered activity

    DISCUSSION...Regional RADAR and 20z surface observations show
    stabilized area and remnant outflow boundary across south-central
    AL from KEUF to KTOI to KPRN that is starting to angle more
    northwest to due north just west of the MS/AL line from KMEI to
    KLMS to KSTF. Broad southwesterly low-level flow has be weak but
    sufficient to maintain scattered thunderstorm activity along the
    edge of this meso-high/stabilized area, but recent uptick in wind
    along the upwind edge from the south and southwest to 30kts has
    increased convergence and isentropic ascent to break out further
    convection mainly on the SW edge toward Meridian, MS toward N
    Clarke/Wilcox county in AL. Deep layer steering will keep them in line/parallel to the boundary to support some possible
    training/repeating in proximity to areas affected by the initial
    thunderstorm line earlier today.=20=20

    However, further upstream; a strong divergence signal aloft in a
    split between the polar/sub-tropical upper-level jets has migrated
    eastward across the MS River and scattered thunderstorms have
    started to congeal/expand into a larger complex over west-central
    MS. Pooled moisture along the old outflow boundary as well as
    increased values from further west (noted in CIRA LPW) show above
    average moisture of sfc Tds in the low 70s, but overall TPWs
    reaching near 2". This along with sufficient moisture flux
    convergence should support rates of 2"/hr. The progressive nature
    to the east should limit overall totals to 2-3.5" which given
    recent drought and naturally higher FFG values are close but just
    below exceedance. However, this morning has reduced some values
    especially in proximity to Chickasaw to Noxubee counties in MS and
    into Pickens county in AL which reduced to below 3" in 6hrs and
    about 1.25-2"/hr; suggesting a slightly better chance of possible
    flash flooding across that portion of the MPD. Overall, isolated
    to widely scattered incidents of flash flooding will be possible
    where repeating or slightly longer residency can occur likely to
    storm-scale interactions.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7DYK6FGXdhXvSsgnqzGInQx2eAKE7jL1JNVI7BRx2y3bOBisQalNnQIFnSwAY9yu1Cbi= 743yq2pVYVFafXCMrWsac2E$ for graphic product...

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

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34328910 34058786 33248605 32498521 31818537=20
    31648627 31658732 31778863 31928947 32119028=20
    32449078 33049105 33799089 34259020=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Apr 29 00:33:43 2026
    AWUS01 KWNH 290033
    FFGMPD
    TNZ000-ALZ000-MSZ000-ARZ000-290600-

    Mesoscale Precipitation Discussion 0149
    NWS Weather Prediction Center College Park MD
    832 PM EDT Tue Apr 28 2026

    Areas affected...Eastern AR...Northern MS...Northwest
    AL...Southwest TN

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

    Valid 290030Z - 290600Z

    SUMMARY...Increasing convective coverage with strengthening of the
    low-level jet, ample moisture and occasional training/repeating
    elements support rates up to 2+"/hr locally and widely scattered
    spots of 2-4" inducing possible incident(s) of flash flooding
    through early overnight period.

    DISCUSSION...GOES-E WV suite shows broad diffluence between the
    split in the polar jet (which is deflecting northward through the
    Ohio Valley) and the sub-tropical jet that is diving south across
    E TX. This has supported some broad ascent and favorable
    vorticity development across E AR in the mid-levels to support a
    weak surface wave and northward warm-advective shift across
    northern AR. LLJ continues to increase in speed and is utilizing
    the western fridge of a shallow outflow that has been reinforced
    by multiple rounds of convection across N MS today. Deep layer
    moisture is pooled along that outflow boundary and is providing
    solid flux to developing storms. However, RAP analysis shows
    increasing capping across S AR with a remaining weakly capped or
    uncapped area of 2000-2500 J/kg of MLCAPE across north-central AR
    angling southwest into NW MS attm. As such, increasing activity
    is utilizing the buoyancy and divergence aloft to expand in
    coverage and rainfall efficiency.

    Overall deep layer moisture is at or around 2" and given the
    vertical ascent capability and overall low level moisture
    convergence/flux should support rates of similar values (2"/hr).=20
    The limiting factor is the residency of any given cell, will be
    limited due to east to east-southeast cell motions and forward
    propagation. Orientation of the convective cells may allow for
    some short-term training, but overall cells will be repeating
    through areas that may have seen one or two earlier rounds today
    with streaks of 1-3" locally. So an additional potential for 2-3"
    with a worst case 4" total, is in line with or slightly exceeds
    the FFG values in the area of concern. As such, a widely
    scattered incident or two of flash flooding remains possible
    through the overnight period as the wave/divergence maxima slides
    eastward into the Delta Region and eventually N MS/AL, though
    instability will be steadily reducing with time and therefore
    overall coverage and intensity should follow.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-CTkPKTremPgq0Snm9Zw_rkJMeDN_-_PBaLeBsmdx_ic-RaVtzMST6TGUxvL9an3ivjo= nCJuMme4tzbY_ob9ji78_LY$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LZK...MEG...

    ATTN...RFC...ALR...ORN...TUA...NWC...

    LAT...LON 35879144 35759006 35528911 35158827 34788758=20
    34248684 33328717 32928777 32868882 33469023=20
    34119139 34779289 35609302 35839249=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Apr 29 05:32:46 2026
    AWUS01 KWNH 290532
    FFGMPD
    GAZ000-ALZ000-MSZ000-ARZ000-291130-

    Mesoscale Precipitation Discussion 0150
    NWS Weather Prediction Center College Park MD
    130 AM EDT Wed Apr 29 2026

    Areas affected...Southeast AR...Central and Northern MS...Central
    and Northern AL

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

    Valid 290530Z - 291130Z

    SUMMARY...Broken clusters of heavy showers and thunderstorms will
    continue to advance east across large areas of the Mid-South
    overnight. Rainfall rates of 1 to 2 inches/hour are expected and
    some cell-training may result in additional localized swaths of 2
    to 4 inches of rain by dawn. This will foster additional concerns
    for isolated to scattered areas of flash flooding, and especially
    around the more sensitive urban corridors.

    DISCUSSION...The latest GOES-E IR satellite imagery shows a
    substantial cold-topped convective mass continuing to advance
    gradually east across large areas of the Mid-South, with an
    emphasis on southeast AR through central and northern MS, and also
    adjacent areas of central and northern AL. All of this is
    associated with the ejection of multiple waves of surface low
    pressure out of the Lower MS Valley and toward the OH Valley as a
    well-defined shortwave trough crosses the region.

    Favorable upper-jet dynamics along with the nose of a convergent
    30 to 40 kt low-level jet will continue to favor areas of locally
    organized convection through the predawn hours across especially
    northern MS and portions of central and northern AL. MUCAPE values
    are highest across southeast AR through northern MS with values of
    1500 to 2500 J/kg in place, and this coupled with PWs near 1.75
    inches will favor high rainfall rates capable of reaching well
    into the 1 to 2 inch/hour range. Effective bulk shear values of
    locally over 50 kts remain in place based on the latest RAP
    analysis and this should continue to favor multicells and some
    supercell thunderstorms in the near-term that will contain these
    enhanced rainfall rates.

    The nose of the low-level jet should increase the moisture and
    instability transport along with a corridor of well-defined
    isentropic ascent across central and northern AL, so some of the
    heavier rainfall may tend to focus across these areas over the
    next few hours. In fact, the cloud top temperatures currently over
    northwest AL are as cold as -70C, and thus indicative of strong
    vertical velocities with enhanced thermodynamic forcing.

    Additional rainfall totals of 2 to 4 inches can be expected where
    any cell-training occurs. Given that some areas of have already
    seen heavy rainfall, the additional rains will certainly continue
    to support a threat for isolated to scattered areas of flash
    flooding. The more sensitive urban corridors will also be at risk
    for seeing impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_5JHa6Gfbv3mZTTfrUFAUl9DFKc1XRjn5u6KgiYIiKuHziyi64waYSxe59MLWRtLFM-Z= F_yCGuPILJpfb6dRdQ20l2U$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...JAN...LZK...MEG...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34658825 34618704 34538615 34228559 33618527=20
    32888545 32388644 32588849 33159031 33639217=20
    34099237 34419113 34558971=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Apr 29 18:17:04 2026
    AWUS01 KWNH 291816
    FFGMPD
    ALZ000-MSZ000-LAZ000-ARZ000-300000-

    Mesoscale Precipitation Discussion 0151
    NWS Weather Prediction Center College Park MD
    216 PM EDT Wed Apr 29 2026

    Areas affected...Northern LA...Southern MS...Ext. Southwest AL...

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

    Valid 291815Z - 300000Z

    SUMMARY...Potential for training cells within deep moisture
    profile suggests locally higher rates and potential for 3" totals
    in 2-3 hours nearing FFG values suggests isolated incident(s) of
    flash flooding are possible.=20

    DISCUSSION...18z Surface analysis denotes last evening's outflow
    boundary remains angled ESE from SW AL across central MS
    intersecting the southward dropping cold front along I-20 between
    Jackson and Vicksburg, before being aligned to a weak surface wave
    in NW LA. Regional RADAR and visible imagery shows elevated
    convection in proximity to the best divergence along the right
    rotor of the upper-level jet crossing out of NE TX into LA;
    helping to support the weak surface low. Low level wind has
    responded with increasingly confluent surface to boundary layer
    flow from the southwest intersecting the boundary. Clear skies in
    the morning and surface temps to upper 70s over low to mid 70s Tds
    support ample buoyancy with core of MLCAPE of 2500 J/kg centered
    around and just north of the SW MS corner.=20

    CIRA LPW shows enhanced surface to mid-level moisture advecting
    toward this unstable area with values of .8-.9" in the sfc-850mb
    resulting in overall PW totals nearing or locally exceeding 2",
    suggesting efficient rainfall production in the relatively
    narrow/skinny CAPE profiles. The greater concern is the
    alignment of 800 to 400mb unidirectional steering flow mainly
    parallel to the old outflow boundary supportive of
    training/repeating potential. The strength of the low level
    inflow/flux is only about 15-20kts which may be weak relative for
    stronger updraft support but this weakness may counter-balance any southwestward propagation vectors to maintain the residency time
    to overcome the drier ground conditions, e.g. FFG values. Still,
    Hi-Res CAMs support short-term rates of 1-1.5" in 15-30 minutes
    and combination with training spots up to 3" which suggest
    localized FFG exceedance and therefore incident or two of
    scattered flash flooding is possible.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9qxNoxYIO3qyp5Bw6Cm_MoewymUBWUJxjunwmjj0ripARxJDK5XcrWplPvHSeReqBMbK= uaXHUSS6RlTHn9XsUnA-fYY$ for graphic product...

    ATTN...WFO...JAN...LIX...MOB...SHV...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 33089375 33029226 32789090 32458949 32028829=20
    31488807 30948836 30838922 30979021 31379156=20
    32019317 32509386=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Apr 29 23:41:11 2026
    AWUS01 KWNH 292341
    FFGMPD
    MSZ000-LAZ000-300530-

    Mesoscale Precipitation Discussion 0152
    NWS Weather Prediction Center College Park MD
    740 PM EDT Wed Apr 29 2026

    Areas affected...Central Louisiana...Southwest Mississippi...

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

    Valid 292340Z - 300530Z

    SUMMARY...Low end, isolated flash flooding risk continues as
    upstream redevelopment remains in favorable flow regime to repeat
    across areas affected with initial bout across central LA into S
    MS.

    DISCUSSION...Regional RADAR mosaic depicts MCV/precip shield
    continuing to slide ESE across S MS toward SW AL with well defined
    squall/bow of convective cores along the leading edge and along
    the western flank across SW MS entering LA, having laid out solid
    heavy rainfall swath of 1-2+" with isolated peaks of 3" totals
    helping to reduce the naturally higher FFG values in the area.=20
    GOES-E Visible and 10.3um EIR shows upstream new development
    across far E TX into West-central LA with scattered weaker
    isentropically forced cells over the outflow boundary betwixt the
    main cores near the MS corner. VWP and RAP analysis suggest some
    enhancing winds from LCH toward the northeast within the core of
    highest remaining overall moisture.

    Additionally, as the instability errodes or is utilized eastward,
    a ribbon of unstable 2000-2500 J/kg MLCAPE exists within this
    slightly strengthening SWly confluent low-level flow. As such,
    stronger convergence should help to maintain/redevelop cells in
    proximity to the outflow boundary and with deeper layer steering a
    bit south of due east may allow for continued repeating/training
    across central LA and perhaps into the affected areas of SW MS
    over the early overnight period. Rates of 2-2.5"/hr are possible
    given the the abundance of total moisture (over 2") and strength
    of ascent. While flux is not extreme, it will also not drive
    quicker southwestward propagation vectors further allowing the
    potential for repeating. And additional 2-3" over areas with the
    lowered FFG still suggest an isolated incident or two of localized
    flash flooding remain possible overnight.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!85JTAlwHYNsu4YkWn2jk6VH3XRaticcNFtQducnj3a8W-RpIhLFv9T_iN-8HrdiUZnuF= JvV7GoAeS3fHB5bMeaZ3fAA$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 32369104 32238984 31758937 30888938 30548951=20
    30389016 30489110 30709200 31039316 31359352=20
    31739359 32089314=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Apr 30 16:41:23 2026
    AWUS01 KWNH 301641
    FFGMPD
    MSZ000-LAZ000-TXZ000-302230-

    Mesoscale Precipitation Discussion 0153
    NWS Weather Prediction Center College Park MD
    1240 PM EDT Thu Apr 30 2026

    Areas affected...far southeastern TX into southern LA

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

    Valid 301638Z - 302230Z

    SUMMARY...Training and repeating thunderstorms are expected across
    portions of southern LA through at least the mid-afternoon. Peak
    hourly rainfall values over 2 inches will be possible with
    potential impacts to the I-10 corridor between Lake Charles and
    New Orleans.

    DISCUSSION...16Z visible satellite and area radar imagery showed
    developing showers/thunderstorms over southern LA, along and south
    of I-10, with a general movement off toward the ESE at 20 to 30+
    kt following the deeper layer mean flow. However, a few slower
    moving heavy rain cores were noted over Iberia and Assumption
    parishes. Surface observations from 16Z showed these cells were
    forming along a slow moving front which extended from the
    Chandeleur Sound, west-northwestward into southwestern LA and into
    a surface low northeast of Galveston Bay. 925-850 mb winds were
    marginally stronger at 10-15 kt from the SSW into the front
    (enhanced moisture flux) into the central Gulf Coast, between a
    weak ridge over the east-central Gulf and subtle cyclonic flow
    over TX.

    The environment as sampled by the 12Z LIX sounding and 16Z SPC
    mesoanalysis showed MLCAPE of 500 to 1500+ J/kg over southern LA
    and PWs of 1.7 to 1.9 inches with moisture contributions from the
    Gulf in the low levels and sub-tropical eastern Pacific in the
    mid-upper levels as seen on OSPO ALPW imagery. Sufficient bulk
    shear (40-55 kt via mesoanalysis) and instability was present for
    organized cells. Given the weakening of low level inhibition with
    continued daytime heating, thunderstorms are likely to continue
    expanding along the front with a mixture of modes and speeds.
    Given the mean steering flow oriented parallel to the initiating
    boundary, and continued low level inflow from the south, there are
    concerns for upstream redevelopment, repeating and training of
    cells which will contain hourly rainfall of 1 to 2 inches, but
    locally higher values in excess of 2 inches will also be possible.
    2 to 4 inch storm totals will be possible but the 12Z HREF and
    recent HRRR/RRFS cycles indicate the potential for 4+ inches
    through 23Z (although the RRFS appears overdone). Flash flooding
    will be possible, with the greatest concern within the
    metropolitan centers along I-10.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4b5N85STP0qax359_CZ0s9tF5YCu75GbpuU5Bikb13MRaxWusdEstSKpr6gG1O1NJmK6= ps7EUnab5xfAKe_W003Jx74$ for graphic product...

    ATTN...WFO...HGX...LCH...LIX...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 30729283 30659105 30298967 29808899 29268886=20
    29058934 29469049 29619162 29659296 29669378=20
    29729436 30409428=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 1 07:47:59 2026
    AWUS01 KWNH 010747
    FFGMPD
    TXZ000-011346-

    Mesoscale Precipitation Discussion 0154
    NWS Weather Prediction Center College Park MD
    346 AM EDT Fri May 01 2026

    Areas affected...South Central to Southeast TX

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

    Valid 010746Z - 011346Z

    SUMMARY...Elevated convection expanding north of a surface front
    will pose an isolated flash flood threat through 14Z. While
    individual storms will be fast-moving, multiple rounds of
    convection tracking over the same areas could result in localized
    totals of 2 to 3 inches, threatening urban areas and sensitive
    Hill Country basins.

    DISCUSSION...Regional radar imagery shows elevated convection
    continuing to expand across south-central to southeast Texas,
    situated north of a surface boundary. Convective coverage and
    intensity should be maintained into the morning hours as
    large-scale forcing for ascent strengthens, driven by an
    approaching mid-level shortwave and favorable upper-level jet
    divergence.

    The environment features a deep moisture profile, with
    precipitable water values currently around 1.8 to 2.0 inches. This
    is being supplied by a dual moisture feed, tapping into Pacific
    moisture in the mid to upper levels and Gulf moisture in the low
    levels. While this deep moisture generally supports efficient
    precipitation production, instability is a limiting factor. MUCAPE
    is currently analyzed between 500 and 1000 J/kg, but a slight
    downward trend has been noted recently.

    Spatially, the strongest instability remains confined to the
    southern periphery of the convective shield. Here, organized cells
    and embedded elevated supercells are maintained by strong
    deep-layer shear. However, much of the available CAPE is above the
    freezing level, supporting a notable hail threat that acts as a
    negative factor for overall rainfall efficiency. With northward
    extent, instability drops off, resulting in generally weaker storm
    intensities. Additionally, individual storm motions remain
    relatively quick across the board, which will limit the duration
    of heavy rainfall at any single location.

    Consequently, the flash flood threat will be contingent upon
    multiple rounds of convection affecting the same locations. While
    individual storms are capable of producing a quick 1 inch of rain,
    the fast storm motions and weaker instability will make it
    difficult to achieve significant totals from a single cell.
    However, where repeated rounds track over the same area, localized
    runoff issues could materialize as storm totals push toward 3
    inches. Urban areas and the naturally flashy, sensitive basins of
    the Hill Country will be most at risk, though at this time the
    overall flash flood coverage is generally expected to remain
    isolated through 14Z.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_oSL5XhjlOe7jYsYeXfqI8CSkANMdX9W0tVBf-MD6gcwQw-Fm8eGYNV2udRg8_hNjh56= lGpw3-mC32KRM5yqJ73hcxU$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...LCH...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30729653 30719530 30589433 29669486 28839726=20
    28369859 28070001 28060015 28490068 28860095=20
    29420057 30279841=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 1 14:17:40 2026
    AWUS01 KWNH 011417
    FFGMPD
    LAZ000-TXZ000-012010-

    Mesoscale Precipitation Discussion 0155
    NWS Weather Prediction Center College Park MD
    1016 AM EDT Fri May 01 2026

    Areas affected...south-central into southeastern TX into
    southwestern LA

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

    Valid 011415Z - 012010Z

    SUMMARY...Elevated thunderstorms will continue to affect
    south-central into southeastern TX, reaching southwestern LA later
    this morning. Peak hourly rainfall values near 1 inch are expected
    although hourly rainfall near 2 inches will be possible closer to
    the upper TX and LA coast. Repeating rounds of additional rainfall
    may result in additional rainfall totals near 3 inches through 20Z
    in one or two locations.

    DISCUSSION...Regional radar imagery from 14Z showed areas of
    moderate to heavy rain extending from near San Antonio into
    portions of southeastern TX. North of a stationary front, elevated
    instability with MUCAPE up to 1000 J/kg was estimated from
    south-central TX to the upper TX coast via 14Z SPC mesoanalysis
    data (though most locations were below 500 J/kg) and PWs were
    anomalous with 1.6 to 1.9 inches in place over the region. Low
    level convergence, centered near 850 mb, has aligned with the
    repeating rounds of convection which have been tracking between 40
    and 50 kt toward the ENE from roughly San Antonio, eastward along
    I-10 to just north of Houston. The quick-moving nature of
    convective segments has limited peak hourly rainfall values to 0.5
    to 1.0 inches but the repeating nature of the rainfall has
    generated an MRMS-derived 1 to 3 inches over the past 6 hours from
    the San Antonio metro to the northern side of Houston.

    The axis of low level convergence is forecast by RAP guidance to
    persist over the next several hours, but translate downstream into
    southwestern LA by 18-20Z out ahead of a shortwave trough ejecting
    east from far western TX. A similar evolution of storm mode is
    expected into the early afternoon with bursts of intense rainfall
    forming upstream and tracking toward the ENE at a relatively quick
    pace. There could be brief alignment of heavier rainfall along the
    convergence axis supporting short-term training as well. The
    combination of repeating rounds and brief training of heavy
    rainfall is expected to lead to localized additional totals of 2
    to 3 inches through 20Z from southeastern TX into southwestern LA.
    Given instability increases with southward extent, there is some
    low-end potential for higher rates to impact coastal locations,
    anywhere from the middle/upper TX coast into southwestern LA, with
    hourly rainfall peaking near 2 inches. Localized flash flooding
    will continue to be possible for these regions of TX and LA into
    the afternoon, especially over urban areas or locations that have
    received heavy rainfall over the past 24-48 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_KlCGXYGAHEk0yT1cutM9x8HAQpRAB4E6FAJe1_3PuBixSIA93uGoWzSDzOOdX6QQCGf= GetRkYtrjt2g_jYsDcs93w8$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...JAN...LCH...LIX...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 31399315 30959148 29959142 29379210 29259392=20
    27939688 28939876 29559913 30339856 30699682=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 1 19:51:47 2026
    AWUS01 KWNH 011951
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-TXZ000-020200-

    Mesoscale Precipitation Discussion 0156
    NWS Weather Prediction Center College Park MD
    350 PM EDT Fri May 01 2026

    Areas affected...Southeast TX...Southern LA...Coastal MS/AL...

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

    Valid 012000Z - 020200Z

    SUMMARY...Multiple rounds of elevated convection capable of
    1.5"-1.75"/hr tracking through a few I-10 urban centers may result
    in localized spots up to 3" through early overnight. Flash
    flooding incidents remain possible.=20

    DISCUSSION...GOES-E WV suite depicts a potent shortwave emanating
    from northwest Mexico and the Southwest is starting to
    shear/elongate into a broader long-wave trof as it moves into
    confluent flow due to the broader northern stream digging trough
    seen in the Midwest. This is helping to support a strengthening
    right entrance region of downstream across the Lower Mississippi
    Valley into the 130kt jet over the Tennessee Valley. The
    combination of the broad DPVA and divergence aloft supports a
    broad southerly flow off the Western Gulf, but veering quickly
    through the low to mid-levels for west to east fairly
    unidirectional to support a repeating environment for activity.

    The surface front/boundary has shifted offshore for most location
    along the Upper Texas coast through the Central Gulf coast, with
    exception of possibly the Bird's Foot of SE Mississippi. Solid
    northeasterly flow north of the boundary is helping to steepen the
    isentropic slope and further enhanced moisture flux convergence.=20
    The higher theta-E and modest lapse rates allows for 500-1000 J/kg
    of MUCAPE that hugs the coast, so scattered elevated cells will
    continue to exist. Overall moisture availability of .75-.9" of
    sfc to 850mb PW is noted in CIRA LPW suite but mid-level moisture
    remains elevated as well to keep TPW between 1.75-2" throughout
    the next few hours to aid rainfall production/efficiency for these
    elevated cells. As such, intense cores followed by light to
    moderate rain, with additional rounds allow for spotty 1-3" totals
    mainly coming in those bursts. Given the number of larger urban
    centers along I-10, increases intersection with impermeable
    surfaces increasing run-off potential. So while most of the
    broader swamps and lower wetlands are not likely to be at risk of
    FFG exceedance resulting in flash flooding; rapid inundation in
    urban centers may result in localized flash flooding.=20=20

    It should be noted, as the core of the shortwave and divergence
    aloft shifts eastward toward sunset, the height-falls supports a
    weak surface wave and northward advection of the front perhaps
    back into far SE LA. This suggests some surface based convection
    potential will exist toward 00-02z, which would have higher
    rainfall rate potential up to 2"/hr. Confidence is not extremely
    high in this evolution, but there is ample loose agreement in CAM
    solution for some slightly higher concern in SE LA later this
    evening.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8vxmsO1STn8G8hwO6S6HaKxFBncSnAD0m4SaKAQqXlY8Or3E_Tq3WWIqEJDxeybaTRpt= 1w2MvvWwt4L5ij4etfU2He4$ for graphic product...

    ATTN...WFO...HGX...LCH...LIX...MOB...

    ATTN...RFC...ALR...FWR...ORN...NWC...

    LAT...LON 31108803 30898752 30298754 30128858 29708878=20
    29008895 28868973 28979092 29439247 29539380=20
    29359435 29079493 28489601 28899641 29539630=20
    30289651 30459554 30599338 30749165 30759049=20
    30858950 30918892=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 3 17:28:29 2026
    AWUS01 KWNH 031728
    FFGMPD
    FLZ000-032325-

    Mesoscale Precipitation Discussion 0157
    NWS Weather Prediction Center College Park MD
    127 PM EDT Sun May 03 2026

    Areas affected...southeastern FL

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

    Valid 031726Z - 032325Z

    SUMMARY...Thunderstorms are expected to expand in coverage through
    the afternoon across southern FL. Storm total rainfall of 2 to 4
    inches (locally higher) may occur across isolated sections of the
    urban southeastern corridor due to cell mergers and brief upstream
    development.

    DISCUSSION...17Z surface observations and visible satellite
    imagery showed a cold front from just south of FLL to ~20 miles
    south of MKY (marked by strengthening northerly winds and dewpoint
    falls) with a pre-frontal trough/outflow boundary extending from
    south of the Keys to just south of Great Abaco in the Bahamas. The
    southern boundary was acting as the effective front with northerly
    winds at the surface and cooler surface temperatures, but VAD wind
    data indicated that the rain-cooled boundary was only 1-2 kft
    deep. 17Z SPC mesoanalysis data indicated that the environment
    over southern FL consisted of 500-1500 J/kg MLCAPE (slightly
    higher MUCAPE) and PWs near 2 inches (near/above SPC sounding
    climatological daily max at MFL)

    In addition, effective bulk shear of 40-45 kt was sufficient for
    storm organization with the potential for supercells and
    multicells. Average cell motions should remain progressive,
    following the deeper layer mean wind from the WSW at 20-30 kt, but
    organized cells could deviate right of the mean wind. In the upper
    levels, the right-entrance region of a strong sub-tropical jet
    departing from off of the coast of the Southeast may continue to
    provided added support for ascent across southern FL into the
    evening hours.

    Given the shallow nature of the stable layer at the surface,
    breaks in clouds could allow some surface-based cells to form
    should sufficient heating through cloud cover occur. Regardless of
    where cells are rooted, eastward tracking thunderstorms are
    expected to develop and increase in coverage, perhaps quickly, in
    the 18-21Z time frame following peak diurnal heating and recent
    HRRR/RRFS forecasts. Upstream redevelopment will be possible given
    an unstable southerly component to the inflow, with potential for
    1-2 inch hourly rainfall and storm totals of 2 to 4 inches
    (isolated higher rates/totals possible). Given mostly dry
    antecedent conditions across southern FL (with a few exceptions),
    any flash flooding that occurs should be isolated and likely urban
    in nature.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4S5Kv2Jp5oiJPUJK2fgyCbkfmsNuQoYI3fmcIXrW81MJvcnLbXwl7KveBSQd4cyLQPXG= 4id5BSZKhC2GHYboy-PG204$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 27037996 26737974 25997978 25387999 25238015=20
    25258039 25528053 26458042 26988014=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 6 01:00:47 2026
    AWUS01 KWNH 060100
    FFGMPD
    TNZ000-KYZ000-ILZ000-MSZ000-MOZ000-ARZ000-060658-

    Mesoscale Precipitation Discussion 0158
    NWS Weather Prediction Center College Park MD
    859 PM EDT Tue May 05 2026

    Areas affected...Portions of the Lower to Mid-Mississippi Valley

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

    Valid 060058Z - 060658Z

    SUMMARY...Increased thunderstorm coverage along and ahead of a
    migrating cold front will intersect a modestly unstable
    environment capable of enhanced rates that could lead to localized
    flash flooding. Total rainfall between 2-4" will be plausible in
    the hardest hit areas with the greatest threat aligned within the
    Memphis metro into portions of northeast Arkansas.

    DISCUSSION...Current radar and satellite composite indicates the
    advancement of a cold front to the north and northwest of the
    Lower Mississippi Valley with a weak surface low progged near the
    OK/AR border. Increased 85H wind field ahead of the surface wave
    is indicative of a budding LLJ that will act to enhance regional
    shear profiles and low-level convergence along and ahead of the
    advancing cold front. Latest HRRR/RAP boundary layer convergence
    signal is quite robust across north-central AR, extending
    northeast into western TN with a general alignment right along the
    front as it slowly advances to the south-southeast. Prevalent
    moisture ahead of the front is well-documented as dew points
    nestle into the mid and upper-60s with areal PWAT anomalies
    settled between 1-2 deviations above normal according to the
    GEFS/NAEFS anomaly outputs. Modest MUCAPE on the order of 750-1500
    J/kg will be positioned ahead of the cold front which when coupled
    with the deep layer moisture will entice heavier precip cores
    capable of producing hourly rates between 1-2"/hr in the strongest
    cells.

    There is a general agreement on a crescendo of convective
    development between now and 06z this evening with the heaviest
    precip focused across east-central AR extending into southwestern
    TN. This would put the Memphis metro corridor and surrounding
    counties in the best convergent pattern capable of the higher
    rainfall totals which was expressed within the latest HREF
    neighborhood probabilities indicating the higher probs for >2"
    centered over southwest TN. This area has already experienced a
    period of heavier rainfall earlier today leading to some priming
    of the top soil layer which would make for a bit of an easier time
    to initiate run off capabilities. The urban center of Memphis also
    draws for an enhanced run off threat, so the coupling of the
    priming and impervious surfaces should give way to a greater flash
    flood threat in the metro, at least from a local perspective.

    Thunderstorms will continue to slowly migrate southeast with the
    cold front through the evening with a wave of convection likely to
    extend back over the I-30 corridor in AR. The approach of the weak
    surface low will also provide a localized convergence footprint
    capable of heavy rainfall and flash flood prominence as the low
    continues its progression east-northeastward. This signal will
    likely carry beyond the 6hr period with impacts likely to occur
    even beyond 06z for areas further south and east across AR/TN/MS.

    Kleebauer

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-63y0jxHNe6PbJnpBgj-GkcnJmfYgcEmX2C68TeyzKVV-JDRuhXr98FJWxalN34FMZwr= 4rzP7UPlJZRksYtYCIYSiy4$ for graphic product...

    ATTN...WFO...LZK...MEG...OHX...PAH...

    ATTN...RFC...ORN...TIR...TUA...NWC...

    LAT...LON 37038915 37008852 36948798 36938750 36708711=20
    36388709 36078757 35738819 35448852 35268871=20
    35068903 34848960 34659053 34579165 34639272=20
    34929319 35459315 35849270 36269156 36429094=20
    36619044 36768998 36878949=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 6 07:22:26 2026
    AWUS01 KWNH 060722
    FFGMPD
    TNZ000-ALZ000-MSZ000-ARZ000-061320-

    Mesoscale Precipitation Discussion 0159
    NWS Weather Prediction Center College Park MD
    321 AM EDT Wed May 06 2026

    Areas affected...Central AR, Southwest TN, Northern MS

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

    Valid 060720Z - 061320Z

    SUMMARY...Convection developing along and just north of a
    southward-moving surface front will pose an isolated flash flood
    threat through 13Z across portions of central AR into southwest TN
    and northern MS. Fast storm motions parallel to the boundary will
    allow for brief periods of training, with localized rainfall
    totals of 2 to 3 inches possible where upscale growth occurs.

    DISCUSSION...Regional radar imagery and surface observations
    indicate convection developing along and north of a surface
    frontal boundary draped across central Arkansas into southwest
    Tennessee and northern Mississippi. Ascent is being heavily driven
    by strong frontogenesis in the surface to 925 mb layer, which is
    fostering enhanced low-level convergence. Concurrently, strong 925
    mb moisture transport is being directed squarely into this frontal
    zone, providing ample fuel for precipitation production.

    The thermodynamic environment is becoming increasingly supportive
    of robust updrafts along the boundary. Recent mesoanalysis
    indicates a modest destabilization trend, with MUCAPE values
    increasing by roughly 400 J/kg over the past 3 hours. Absolute
    MUCAPE values now range from 1000 to 2000 J/kg. The warm sector
    ahead of the boundary remains strongly capped, effectively
    confining the convective development and heavy rainfall threat to
    the frontal zone itself or the immediate cool side to its north.

    Individual cell motions are relatively fast from west to east.
    Because these motions are largely aligned parallel to the
    orientation of the frontal boundary, there is an inherent risk for
    training convection. However, a key mitigating factor is the
    continuous southward progression of the front itself, which should
    serve to limit the duration of this training at any single
    location.

    Ultimately, the flash flood risk will depend heavily on the degree
    of upscale convective development along and just behind the
    advancing front. If sufficient consolidation occurs to maximize
    the brief training window, localized rainfall totals of 2 to 3
    inches are possible, which could overwhelm sensitive basins or
    poor drainage areas. There are some signs of this beginning to
    occur across central AR. Given the progressive nature of the
    boundary and the fast individual cell motions, the overall flash
    flood threat should generally remain isolated through 13Z.

    Chenard

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7IZMgGMW-dCFh9n9aLw6av-YCpHQiznnrA9h3YptSbuiqDg52PNhquLFeVGSJCB9Hr-G= Znd7P_G0Kv1FU2fo9q4033M$ for graphic product...

    ATTN...WFO...HUN...LZK...MEG...OHX...

    ATTN...RFC...ALR...ORN...TUA...NWC...

    LAT...LON 35868789 35698689 35168615 34728757 34448992=20
    34179209 34079284 34179331 34299379 34579379=20
    34989272 35239181 35688956 35768878=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 6 19:27:08 2026
    AWUS01 KWNH 061927
    FFGMPD
    ALZ000-MSZ000-LAZ000-TXZ000-070125-

    Mesoscale Precipitation Discussion 0160
    NWS Weather Prediction Center College Park MD
    325 PM EDT Wed May 06 2026

    Areas affected...Far East TX through much of LA, MS, and western
    AL

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

    Valid 061925Z - 070125Z

    SUMMARY...Increasing threat of heavy rainfall with scattered to
    widespread convective development initiating ahead of a
    slow-moving cold front to the north. Primed environmental
    conditions will allow for locally enhanced rainfall rates with
    totals approaching 2-4" in some of the heavier cells that develop.
    Isolated to widely scattered flash flooding will be possible.

    DISCUSSION...Radar and satellite composite indicate a rapidly
    growing convective initiation regime across areas of far eastern
    TX extending northeast through LA/MS/AL. A cold front situated
    over east TX through the Lower Mississippi Valley into the
    northern tier of AL/MS will continue to slowly sag southward with
    multiple areas of surface low pressure riding along the front in
    the process. First surface low is analyzed across east TX with an
    enhanced convergence pattern centered to the east of the low as
    flow remains backed within the area situated between the TX/LA
    border north of the Lower Sabine. Area MUCAPE is between 2000-3000
    J/kg in this location according to the latest mesoanalysis along
    with a moisture rich environment signaled by PWAT anomalies ~2
    standard deviations above normal, a testament to a deep moist
    convective environment suitable for locally enhanced rates and
    potential for areas to see a quick couple inches of rainfall
    during impact. 12z HREF was quite robust in the signal for
    neighborhood probs of >1"/hr at times with a swath of 50-80% probs
    located from the TX/LA line to points northeast through much of MS
    into western AL. This correlates well with the boundary layer
    convergence anticipated along and ahead of the approaching cold
    front as the front approaches the fairly buoyant environment
    further south.

    The other area of interest within this setup is across northeast
    MS into northern and western AL where the second surface wave will
    continue to migrate to the northeast leading to a general foci for
    convective development under the lows influence. Like areas
    further southwest with the low in TX, there will be an narrow
    corridor of enhanced convective potential within the locally
    backed flow centered just to the east and northeast of the surface
    wave's trajectory. The good news for this area is the front will
    migrate through the region and begin to provide a drier theta_E
    advection pattern on the backside of the low. However, the narrow
    corridor of elevated theta_E's analyzed over northeast MS into
    northern AL should still be sufficient for locally heavy rain
    cores, noted very well within the latest 18z WoFS iteration that
    is consistent with its signature of a band of heavier convection
    forming in the aforementioned area.

    The general setup for the entire area encompassed by the MPD will
    be suitable for heavy precip totals between 2-4" in the hardest
    hit areas with hourly rates between 1-2"/hr in the strongest
    cells. This is well-documented on the consistent signatures via
    the latest HRRR iterations, as well as the noted prob fields from
    the 12z HREF where CAMs were consistent in the potential between
    now and 01z in this corridor of the Southeastern CONUS.

    Kleebauer

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4xgFQaQWgnaGyzrHGv0cZaz6XRVw-aumE4Cx9XYIX3ZuO3zj74cHtpdiLAv0gi_yr_oi= M46WdOs1EpE3OyKaf3J3U8Q$ for graphic product...

    ATTN...WFO...BMX...HGX...HUN...JAN...LCH...LIX...MEG...MOB...
    SHV...

    ATTN...RFC...ALR...FWR...ORN...NWC...

    LAT...LON 34728734 34258671 33348667 32618703 32048788=20
    31728853 31468925 31229027 30869157 30589263=20
    30439371 30399448 30879466 31379435 31879363=20
    32109284 32399221 32619180 32909112 33249038=20
    33698949 34238869 34588778=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 7 01:01:15 2026
    AWUS01 KWNH 070101
    FFGMPD
    GAZ000-ALZ000-MSZ000-LAZ000-070658-

    Mesoscale Precipitation Discussion 0161
    NWS Weather Prediction Center College Park MD
    859 PM EDT Wed May 06 2026

    Areas affected...Central LA, Central and Southern MS/AL, and
    Western GA

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

    Valid 070058Z - 070658Z

    SUMMARY...Widespread thunderstorms will spread across the
    Southeastern U.S. with a heightened threat of training as the cold
    front continues to advance south through Louisiana, Mississippi,
    Alabama, and Georgia. Accumulations of 2-4 inches of rainfall,
    locally higher, are expected in areas of training leading to
    likely flash flooding as soils are primed from earlier rainfall.

    DISCUSSION...The 21z surface analysis continues to convey the
    methodical southern motion of a now wavy quasi-stationary front
    situated across the northern half of the Southeast CONUS. Multiple
    surface lows are embedded within the frontal structure with one
    still slowly ejecting eastward out of east TX, and the other
    analyzed over northern AL. The former area of low pressure will
    play a significant role in the convective evolution this evening
    as the low-level convergence regime amplifies into something more
    appreciable in regards to focusing convection over a more defined
    area. CAMs continue to be steadfast in their representation of the
    environment and synoptic scale evolution providing a solid
    consensus for where the heaviest rainfall will transpire as we
    move through the overnight period.

    Current environmental status remains very favorable with
    prevailing axis of elevated MLCAPE between 1000-2000 J/kg situated
    ahead of the stationary front from southwest LA through western
    GA. Deep layer moisture remains prevalent over much of the
    Southeast with PWAT anomalies solidly between 2-3 standard
    deviations above normal. Mean layer flow will run more parallel to
    the boundary as it slowly migrates southward through the evening
    leading to general convective forward propagation to overlap with
    each other as they progress through the evening. Upper level
    dynamics remain favorable, as well as a broad upper trough passing
    to the north will maintain reputable large scale ascent within the right-entrance region of a 140kt upper jet crossing through the
    Mississippi Valley. Nocturnal LLJ centered over southern MS
    extending into AL will only provide increasing low-level
    convergence and relevant bulk shear to maintain stronger
    mesocyclone cores that can provide heavier rainfall over extended
    periods of their life cycle(s).

    Considering the above factors, rainfall rates this evening will
    likely exceed 1"/hr in the stronger cells with 2-3"/hr well within
    reach despite the loss of diurnal destabilization. Even as cells
    begin the merger process and become a more cohesive, multi-cell
    structure, heavy rain with 1-2"/hr areal averages will certainly
    be plausible which will lead to widespread areas of 2-4" of
    rainfall with locally higher totals possible as inferred by
    low-end HREF probabilities for >5" centered over southeast MS into south-central AL to the AL/GA line. Secondary maxima could also
    occur further northeast into northwestern GA, including
    potentially close to the Atlanta metro where some CAMs are
    relatively bullish with heavy rain prospects in the urban
    corridor. The greatest threat is still likely further south and
    west, but the setup is still relevant for those areas downstream
    into the northwest quarter of GA. Areas of highest concern are
    likely within the confines of Laurel, MS over to Montgomery, AL to
    near Columbus, GA spreading 50-75 miles either side of that line.

    Kleebauer

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9juSkWDhsmkz1MRnOj1yQ-t0fCsAXwyH-PM2n0P0IkqgFYj8RZ7-4PRxOoWPXAvWT3TO= oY0eMYkM_EgNAjVfptgmZ0E$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...JAN...LCH...LIX...MEG...MOB...
    SHV...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34908514 34808461 34628420 34308401 33938385=20
    33418392 32848431 32378464 32068520 31748605=20
    31378698 31168791 31038901 30928992 30959150=20
    31079277 31769269 32429175 32879071 33218969=20
    34198708 34458635 34708575=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 7 06:50:19 2026
    AWUS01 KWNH 070650
    FFGMPD
    FLZ000-GAZ000-ALZ000-MSZ000-LAZ000-071247-

    Mesoscale Precipitation Discussion 0162
    NWS Weather Prediction Center College Park MD
    249 AM EDT Thu May 07 2026

    Areas affected...southern Alabama, far southwestern Georgia,
    southeastern Mississippi

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

    Valid 070647Z - 071247Z

    Summary...Areas of training thunderstorms are likely to continue
    for the next several hours, with isolated instances of flash
    flooding possible through 13Z/8a CDT.

    Discussion...Scattered thunderstorms continue to move eastward
    across the discussion area at around 40 knots while producing
    areas of 1-2 inch/hr rain rates. The heaviest of rain rates are
    currently displaced just south and east of where heavier rain fell
    earlier today near Montgomery/Selma and near Collins, MS --
    although deep convection continues to redevelop across
    southeastern Mississippi along and just ahead of a synoptic front
    extending from Baton Rouge through Meridian to near Birmingham.=20 Moist/unstable thermodynamic profiles and low-level/850mb
    confluence will continue to support new updraft development across
    southeastern Mississippi for several hours, with storms spreading
    eastward through southern Alabama and far southwestern Georgia
    through 13Z this morning.

    Any flash flood risk within this regime will exist 1) where
    convective training is most pronounced within the discussion area
    and 2) where scattered convection can repeat across the Montgomery/Selma/Collins areas where prior rainfall has lowered
    FFGs to near zero. Given the magnitude of prior rainfall in some
    of these areas, flood impacts may still be ongoing and could be
    exacerbated locally. New instances of flash flooding are also
    possible. Local rainfall totals of 2-3 inches are likely through
    13Z - particularly from Laurel/Hattiesburg eastward to Troy, AL
    and areas near/south of Columbus, GA.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!547HLYTGdFVIf4LHXnULs5IQlRg9YYGJNsX4HsCB5q50E3nC0aZU0ZbAVESd0Tm5JHpO= RpmZ09Ex7eF54TfgUkI7470$ for graphic product...

    ATTN...WFO...BMX...FFC...JAN...LIX...MOB...TAE...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 33548583 33178442 32328375 31438378 30878454=20
    30908730 30778950 31188994 31668978 32348879=20
    33178731=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 8 11:46:51 2026
    AWUS01 KWNH 081146
    FFGMPD
    MSZ000-LAZ000-TXZ000-081700-

    Mesoscale Precipitation Discussion 0163
    NWS Weather Prediction Center College Park MD
    745 AM EDT Fri May 08 2026

    Areas affected...Southeast Texas...Southern Louisiana...Southwest Mississippi...

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

    Valid 081145Z - 081700Z

    SUMMARY...Early morning elevated thunderstorms with potential to
    train this morning pose narrow axis of 2-4" totals and isolated
    flash flooding concerns near urban and areas of recent heavy
    rainfall.

    DISCUSSION...GOES-E WV suite depicts a broad positive tilt closed
    low across the southwest with a nicely shaped anti-cyclonic
    downstream shortwave ridge across central TX into confluent flow
    regime across the Lower Mississippi Valley into the Tennessee
    Valley. This places the surface front stalled along south and
    parallel of the Texas Gulf Coast before angling northward to a
    weak surface wave south of Houma, LA. CIRA LPW denotes the
    anomalously high sfc to 850mb moisture pooled along and north of
    the front generating a very tight gradient across southeast TX and
    across central LA. The 850-700 and 700-500mb layers are also
    complimentary to total PW values aligned across the area of
    concern that values of 1.75-2" exist between the surface front and
    the surface coastal pressure trof that goes from KNOG to KTME
    before crossing that tight PW gradient near KJAS to KAQV in
    western LA.

    Surface to boundary layer onshore flow is providing weak but
    sufficient WAA before veering to the southwest through the 850mb
    layer to provide sufficient convergence and isentropic ascent
    across the boundary to access the larger well of conditionally
    unstable air with MUCAPES of 1000-1500 J/kg...which extends
    eastward along and south of the PW gradient along and north of
    I-10 through E LA into S MS. As such, RADAR and GOES-E 10.3um
    depicts solid convective initiation along and south of the tight
    gradient which further helps to steepen vertical ascent plane.=20
    The overall depth of moisture is already supporting isolated to
    scattered .5-1"/hr rates but this will continue to increase with
    coverage and moistening of the mid-level profiles. Additionally,
    with some surface heating, a few nearer surface based cells with
    higher rate potentials to 1.75-2"/hr may develop over the next 3-4
    hours along or even south of the I-10 corridor.

    As mentioned, the deeper layer flow flattens west to east into the
    confluence downstream generally parallel to the boundary/ascent
    plane to support a favorable opportunity for repeating/training
    (especially further east into LA). This may allow for narrow
    streaks of 2-3+", with an isolated 4" total not out of the realm
    of possibility. Generally sandy soils and naturally high FFG in
    the region from overall drought should help to mitigate most of
    the heavy rainfall. However, there are is a axis of reduced FFG
    values especially from Vernon to Rapides to Concordia parish in LA
    and portions of SW MS that are recovering from heavy rainfall
    36-48rs ago as well as a number of prone urban centers along the
    area of concern that would be more susceptible to possible
    incident or two of localized flash flooding this morning.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!43JR2EjvKq_jQoiS8RC6iUhu4LPNsWcKcFQbrska-jrXiE-1twdbCM1a0Q4QEXPzapcP= RrLTQOglDchUGoLCPjpO9WE$ for graphic product...

    ATTN...WFO...FWD...HGX...JAN...LCH...LIX...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 31669219 31519034 31208953 30788938 30308968=20
    30129069 30159225 30159283 30059469 30149581=20
    30449631 30959639 31329594 31559489 31629321=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 8 16:25:15 2026
    AWUS01 KWNH 081625
    FFGMPD
    ALZ000-MSZ000-LAZ000-082230-

    Mesoscale Precipitation Discussion 0164
    NWS Weather Prediction Center College Park MD
    1224 PM EDT Fri May 08 2026

    Areas affected...Southern Louisiana...Southern
    Mississippi...Coastal Alabama...

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

    Valid 081630Z - 082230Z

    SUMMARY...Continued risk of possible urban and localized flash
    flooding with new axis of training development as initial band
    slowly weakens across S MS/S AL. Streak of 2-4" totals and
    occasional rate over 2"/hr along I-10 corridor.=20

    DISCUSSION...Very little has changed in the overall synoptic
    environment and placement of the surface stationary front parallel
    to the TX coast before angling toward the SE portions of LA before
    likewise angling eastward. The upper-level divergence has
    slightly up-ticked as well just downstream of the synoptic
    shortwave ridge in E TX, but the low-level flow has increased
    about 10-15 kts from the southwest particularly in the boundary
    layer to 850mb. This has resulted in increased convergence at a
    slightly lower elevation across far SE TX into SW LA and with
    greater boundary layer depth of moisture and its flux, intensity
    of rainfall rates will be increasing as well with occasional
    breaches of the 2"/hr rates given TPW nearing 2.0" (loaded mainly
    below 850mb) and MUCAPEs over 1000 J/kg. As this new has
    strengthend, the more elevated convection has been robbed and
    coverage is reducing along the upstream edge with only the leading
    edge convection maintaining across S MS, trending toward far S AL.


    The broader west to east ascent plane has also increased the
    overall coverage to allow for steering flow to support slightly
    better training/repeating profiles in proximity to the I-10
    corridor. Hi-Res CAMs have struggled a bit with the overall
    orientation and convective initiation, but the last few RRFS
    solutions appear to be most in line with the recent trends
    followed by the 12z ARW. This suggests further training potential
    along I-10 with an eventual weak cold pool to perhaps deviate cell
    motions a bit south of due east alluding the potential for
    intersecting even as far south as I-8 increasing intersection with
    the prone urban regions of the area.=20

    Unlike, further north in central LA/S MS, I-10 and south have been
    missed in prior events and FFG values are naturally at the highest
    values and may still be out of reach for broader flash
    flooding/rapid inundation potential, though isolated localized
    exceedance is possible. However, intersection with urban centers
    is more likely and therefore flash flooding remains more probable
    in those areas through the late afternoon/early evening.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_VWBFItyO23ZtJog41Nwsw-8rqH4Ayaz11KtYmqdGVjSQ3tQY3yh1uBdt87CZ58pMHBH= aIHNNHW_jxwhmKqGqplJUkg$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 31368957 31228831 31018769 30268757 29978891=20
    29578976 29789113 29879206 29969301 30209360=20
    30789342 31089261 31349100=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 9 09:14:05 2026
    AWUS01 KWNH 090914
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-091512-

    Mesoscale Precipitation Discussion 0165
    NWS Weather Prediction Center College Park MD
    512 AM EDT Sat May 09 2026

    Areas affected...central/southern Louisiana, southern Mississippi,
    southern Alabama, and far western Florida Panhandle

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

    Valid 090912Z - 091512Z

    Summary...Areas of convection (with scattered
    mergers/backbuilding) will pose a flash flood risk through 15Z/10a
    Central this morning.

    Discussion...Scattered convection has organized into a mix of
    clusters and linear segments along a couple axes -- one extending
    from near Natchitoches, LA to Jackson, MS to west-central AL and
    another, more scattered band from near Natchez, MS to near
    Slidell, LA. These cells were moving eastward at an appreciable
    clip (30-35 kt), but were being sustained by appreciable mid-level
    instability and 1.75 inch PW values. The loosely organized nature
    of the cells was supporting occasional training and mergers, with
    spots of 1-2.5 inch/hr rain rates focused primarily in northern
    Louisiana over the past half hour to hour. FFGs in this region
    were high (around 3-4 inch/hr), suggestive of only an isolated
    flash flood risk (at best) in the short term.

    With time, cells will migrate/evolve east-southeastward toward
    portions of southern Mississippi that have received 3-6 inches of
    rainfall over the past 72 hours. Soil moistures are wetter here,
    and FFGs are somewhat lower (near 2 inches/hr in spots). Portions
    of southern Louisiana have lower FFGs from prior rain (around 1
    inch/hr) as well. The slow northward drift of a remnant outflow
    from earlier convection (and attendant surface-based instabilty)
    will probably interact with ongoing convection favorably for more
    mergers and localized training as cells migrate
    east-southeastward, with rain rates over 2 inch/hr expected in a
    few spots (supported by abundant PW values). Areas of flash
    flooding are possible, and the overall risk will increase in the
    aforementioned areas (esp. southern LA/MS) between 10Z-15Z this
    morning.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9ZPHGrCo880vNxE2xZX0vXQcnQSi5Mda1AJTNWBlQcRSG2pf8LyinmjcgWhZy1nE0bVR= udUPzDc1cSTJMSyXyv-N29M$ for graphic product...

    ATTN...WFO...BMX...JAN...LCH...LIX...MOB...SHV...TAE...

    ATTN...RFC...ALR...FWR...ORN...NWC...

    LAT...LON 32938887 32498711 32278640 31948583 31048582=20
    30548756 30058985 30019105 30469219 30889319=20
    32419374 32689303 32649166 32769048=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 9 16:58:55 2026
    AWUS01 KWNH 091658
    FFGMPD
    LAZ000-TXZ000-092230-

    Mesoscale Precipitation Discussion 0166
    NWS Weather Prediction Center College Park MD
    1258 PM EDT Sat May 09 2026

    Areas affected...Southern LA...Far Southeast TX..

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

    Valid 091700Z - 092230Z

    SUMMARY...Continued flash flooding potential with over-running in
    southern LA. New convection across SE TX/W LA may be more
    pulse-like with cell mergers capable of a very quick 2" burst.

    DISCUSSION...Regional RADAR mosaic and surface observations depict
    orthogonal ascent from the core of the moisture axis (TPW at
    2-2.15") over cold pool centered over SE LA. Surface easterlies
    further help sharped the boundary with additionally rain-cooled
    air from the over-running convection, as such a few more hours of
    scattered isentropic convection will likely occur. The
    orientation of the ascent streamers will allow for narrow streaks
    of enhanced totals with values of 2-3.5" probable, falling over
    areas already affected with 2-3" so far this morning. However,
    the parent shortwave from the northern stream now, well displaced
    into the Southeast over AL/GA, is still sliding east-southeast and
    the moisture axis and remaining weak LLJ will continue to drift
    southeastward relative to the current activity further into the
    Bayous of S central and SE LA.

    However, upstream energy in the form of a strengthening right
    entrance region to a 100kt 3H jet streak can be seen by well
    defined anticyclonically curved upper cirrus pattern over far E TX
    into NW LA at this time. At the surface the old outflow boundary
    remains weakly defined across west-central to central LA and will
    likely remain the focus of some convective activity.=20
    Unfortunately, the influence of the downstream shortwave is
    pooling away the main warm-conveyor belt and there only remains a
    narrow pocket of enhanced surface to 850 and to 700mb per CIRA LPW
    with drier air mixing in aloft. This helps with some increased
    instability as 2000 J/kg of MLCAPE pool exists across E TX.=20
    Weaker flow into the complex, even with backing low level flow
    responding to the divergence aloft, suggests convective mode may
    be a bit more pulse-like with scattered clusters and propagation
    along collapsing outflow boundaries through the afternoon. The
    amount of moisture should allow for solid efficiency with spots of
    2-2.5"/hr (similar totals) possible across SE TX and West-central
    LA. Flash flooding will remain an isolated potential given
    recent heavy rainfall, wetter soils (especially east in LA) or
    over urban locales. As such, while the coverage and overall
    intensity is reducing; the risk of a few incidents of flash
    flooding remain across the MPD area of concern through late
    afternoon.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8hmqYYdh83CPtvPCxBRtf8ONeYLcxyfqprb9Oo4-kw5TbkHkHQgA3AsosaeCiCHlXOd7= cq_UfLiaWIRjSVTSSXeKPW8$ for graphic product...

    ATTN...WFO...LCH...LIX...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 31389302 31089232 30719144 30359070 30079019=20
    29668970 29168963 28929013 29089129 29709306=20
    30059433 30909437 31289399=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 10 20:50:51 2026
    AWUS01 KWNH 102050
    FFGMPD
    TNZ000-MSZ000-ARZ000-110100-

    Mesoscale Precipitation Discussion 0167
    NWS Weather Prediction Center College Park MD
    449 PM EDT Sun May 10 2026

    Areas affected...central/northern AR into southwestern TN/northern
    MS

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

    Valid 102048Z - 110100Z

    Summary...Scattered thunderstorms, some of which will be slow
    moving, are expected to continue to pose a widely scattered flash
    flood threat across portions of the Lower MS Valley over the next
    3-4 hours. Hourly rainfall of 2-3 inches could allow for a few
    isolated 3-5 inch totals within a 2-3 hour window.

    Discussion...2030Z radar imagery over AR showed an expanding
    coverage of thunderstorms with a few of the cells exhibiting
    backbuilding toward the west and slow overall movement, resulting
    in MRMS-derived hourly rainfall between 2-3 inches. A few of the
    cells were forming along a number of boundaries, including a
    diffuse stationary front that extended from south-central AR into
    north-central MS, marked by dewpoints in the mid-60s to lower 70s
    south of the boundary with dewpoints falling off into the 50s from
    TN into northern MS, north of the front. Meanwhile a stronger cold
    front to the north and rain-cooled air from eastern OK were
    marking the northern and western edge of the short term heavy rain
    threat. Lift across the region was being enhanced by placement
    within the right-entrance region of an upper jet max extending
    from MO into southern IL.

    SPC mesoanalysis data from 20Z showed MLCAPE of 500 to just over
    1500 J/kg along with PWs of 1.3 to 1.6 inches. Sufficient speed
    sheer was present for some organization to cells but their
    residence time over any given location appears to be limited to
    approximately 1-2 hours given undercutting of rain-cooled air at
    the surface. The threat should end from NW to SE with time, but
    this means locations near and just east of the MS River could see
    slow cell movement and possible flash flooding extending beyond
    00Z. Given the observed rates so far, high rain rates could lead
    to a couple of isolated to widely scattered locations picking up 3
    to 5 inches of rain over the next few hours, supporting a
    short-fused flash flood threat.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4XY2s_KzLP8N_fZaXXeM7LRui2aPxS8vQkKhPihvBv54c60VuieKyI4IYQ0bdeuJX0DW= 700y-61tvcIiATgOLgb4hZI$ for graphic product...

    ATTN...WFO...JAN...LZK...MEG...

    ATTN...RFC...ALR...ORN...TUA...NWC...

    LAT...LON 35919340 35899243 35659011 35178917 34378872=20
    33498890 32928924 32938999 33159121 33499225=20
    33849293 34189327 35119331=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 10 23:23:09 2026
    AWUS01 KWNH 102323
    FFGMPD
    TXZ000-110500-

    Mesoscale Precipitation Discussion 0168
    NWS Weather Prediction Center College Park MD
    722 PM EDT Sun May 10 2026

    Areas affected...Edwards Plateau into eastern TX

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

    Valid 102321Z - 110500Z

    SUMMARY...Isolated to scattered instances of flash flooding will
    be possible across portions of central to eastern TX through 05Z
    (12 AM CDT). Slow moving and/or merging of cells are expected to
    produce hourly rainfall of 2-3 inches and a few locations with
    storm total rainfall of 3 to 5+ inches.

    DISCUSSION...Radar imagery through 23Z over TX and LA showed
    thunderstorms becoming more numerous over southeastern TX into
    southwestern LA, along a sea breeze enhanced convergence axis
    (trough axis) at the surface, which extended westward from the
    southern TX/LA border toward I-35 just north of AUS. Farther north
    and west, scattered strong to severe thunderstorms were ongoing
    ahead of a southward sinking cold front which extended
    southwestward from northern TX into the Big Bend region and along
    an outflow boundary that preceded the cold front, extending
    west-east from near Coleman to Nacogdoches. SPC mesoanalysis data
    showed the environment across central TX was quite unstable with
    MLCAPE of 1500 to 3000+ J/kg and PWS that ranged from about 1.3 to
    1.6 inches.

    A general southeastward progression is expected regarding the
    ongoing thunderstorms ahead of the cold front and preceding
    outflow boundary as these boundaries continue to sink south, ahead
    of an approaching shortwave trough axis from KS to eastern NM.
    Meanwhile, thunderstorms are likely to increase in coverage from
    southeastern into central TX, along the trough axis as low level
    flow increases beyond 00Z. Some of these storms could be slow
    moving with backbuilding characteristics due to the weak 0-6 km
    mean layer wind over the region (<10 kt) and increasing 0-1 km
    winds from the southeast across the Coastal Plain of TX. These
    slow moving storms are expected to eventually merge with an
    approaching cluster of thunderstorms with the advancing cold
    front/outflow from the northwest. Peak hourly rainfall of 2-3
    inches (locally higher) is likely with slow moving and merging of
    cells, with potential for a few locations to pick up 3 to 5+
    inches of total rainfall through 05Z.

    Flash flood guidance varies across the region with high 3-hr
    values of 3 to 5+ inches in 3 hours to the east of I-35; lower FFG
    values for the Edwards Plateau. Therefore, despite the potential
    for high rainfall values, the flash flood threat will be most
    focused across urban locations and otherwise sensitive terrain
    west of I-35.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6bNzcVc7Z3vjDySNFQrektLOtDSC7LddZSpJrHTlW1yoFAg37i8IYCMmPVEDnjAXDu6G= 3ntMeWc8YPeONwcNu2VqSko$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...LCH...SHV...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32109793 31899619 31479428 30239416 29919577=20
    29539695 29049824 28349952 28700060 30930069=20
    31869979=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 11 05:15:15 2026
    AWUS01 KWNH 110515
    FFGMPD
    LAZ000-TXZ000-110813-

    Mesoscale Precipitation Discussion 0169
    NWS Weather Prediction Center College Park MD
    114 AM EDT Mon May 11 2026

    Areas affected...central/east Texas into far western Louisiana

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

    Valid 110513Z - 110813Z

    Summary...Flash flood potential will continue for at least 2-3
    more hours (through 08Z/3a central).

    Discussion...Flash flood potential continues especially in east
    Texas. A slow-moving mesoscale convective complex has matured,
    with individual cells exhibiting speeds of around 5-15 knots amid
    a strengthening mid-level circulation over central Texas.=20
    Meanwhile, remnant outflow boundaries/surface troughing downstream
    of the complex has fostered areas of scattered convective
    development especially near College Station eastward to near
    Leesville, LA/Fort Johnson. The slow movement of cells amid an
    abundantly moist environment (1.5 inch PW values) and lingering
    surface-based instability has supported several areas of 2+
    inch/hr rain rates at times. These rain rates have approached FFG
    thresholds on an isolated basis along with a few instances of
    flash flooding reported west of College Station.

    Ongoing trends suggest flash flood potential should continue for
    at least another 2-3 hours. The downstream airmass supporting
    convection remains moderately unstable (around 2000 J/kg MLCAPE),
    with convection continuing to refire both with the leading edge of
    the MCS and along the aforementioned east-west oriented boundaries
    across the region. FFG thresholds get generally higher with
    eastward extent however -- suggesting that any continued flash
    flood threat should remain concentrated near any low spots and/or
    urban areas that can experience 2+ inch/hr rain rates or have
    those rates extend for a period longer than 1 hour. The latter is
    possible on an isolated basis given the slow movement of cells.=20
    Over time, convection should approach the southeast Texas coast
    and move toward the northwestern Gulf, reducing flash flood
    potential thereafter.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-kcZPk_hmksR4wRcqDDmW0zeAK6VJNmkzYGSX7vtSCjh8LjH3KMlrdrC1wXjdsNBXz72= uoPGKIDYJLtTMfv1L_7W2fI$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...LCH...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 31559469 31309277 30249237 29639336 29349544=20
    29539691 31049679=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 11 20:43:58 2026
    AWUS01 KWNH 112043
    FFGMPD
    ALZ000-MSZ000-LAZ000-120215-

    Mesoscale Precipitation Discussion 0170
    NWS Weather Prediction Center College Park MD
    443 PM EDT Mon May 11 2026

    Areas affected...southern LA into southern MS/southwestern AL

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

    Valid 112041Z - 120215Z

    Summary...Scattered thunderstorms will pose a flash flood threat
    from southwestern LA into southern MS and far southwestern LA.
    Hourly rainfall of 2 to 3+ inches and localized totals of 3 to 5+
    inches are expected.

    Discussion...Radar imagery across southern LA at 2030Z showed slow
    moving thunderstorms stretching from near a surface low (southeast
    of LCH) into southern MS/AL (just south of a HZR to PIB line),
    near a slow moving cold front. Water vapor imagery showed a well
    defined shortwave advancing east from eastern TX, providing ascent
    across southern LA. 20Z SPC mesoanalysis data showed the region
    contained 500 to 1500 J/kg MLCAPE and anomalously high PWs at 1.6
    to 2.0 inches (1-2 standard deviations above the mean for
    mid-May).

    Thunderstorms are likely to continue expanding along the front and
    near the surface low with a general eastward translation to
    convection with time. In addition, thinning cloud cover in the
    vicinity and south of Lake Pontchartrain may allow for locally
    increased instability and potential for thunderstorms into the
    early evening. Effective bulk shear ranged from <20 to >40 kt
    across the region and coupled with the modest instability in
    place, cell organization should be mixed, but widespread
    organization is not expected.

    Two big factors for flash flooding through the remainder of the
    afternoon into the evening hours will be slow cell motions (0-6 km
    mean layer winds are <10 kt) and wet antecedent conditions. Given
    large portions of the central Gulf Coast to locations 100 miles
    inland have received 300 to 600 percent of their average rainfall
    over the past week, increased soil moisture will be more prone to
    runoff and flash flooding.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9e_GRW-GZUafZx1F4F7F4oKFue8kwmv3mEvMkrNnJN7cZEq0V88hNTtunm6eQdxjTJaR= -yySiDSE8VPsMQMKsZv0kfo$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 31648790 31258761 30838770 30338797 29668956=20
    29549070 29459270 29729335 30229355 30719323=20
    31029203 31309087 31528911=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 12 02:29:05 2026
    AWUS01 KWNH 120228
    FFGMPD
    FLZ000-GAZ000-ALZ000-MSZ000-LAZ000-120730-

    Mesoscale Precipitation Discussion 0171
    NWS Weather Prediction Center College Park MD
    1027 PM EDT Mon May 11 2026

    Areas affected...central/east-central Gulf Coast

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

    Valid 120226Z - 120730Z

    Summary...Heavy rain with embedded thunderstorms are expected
    along portions of the central to east-central Gulf Coast through
    07Z. Isolated flash flooding will remain possible due to hourly
    rainfall of 2 to 3+ inches and localized totals of 3 to 5+ inches.

    Discussion...Heavy rain remained in a few locations over
    southeastern LA as of 02Z with a small cluster of largely
    warm-topped showers/thunderstorms southwest of Lake Pontchartrain
    with MRMS-derived peak hourly rainfall between 2 and 3 inches. The
    00Z LIX sounding showed a moist environment with at PW of 1.9
    inches and only 5 kt of 0-6 km mean layer flow, supportive of slow
    cell movement. Instability was weak, however, with only 280 J/kg
    MLCAPE on the LIX sounding. Over the past hour, there has been
    some eastward development of localized heavy rain cores through
    southern MS/AL and the western FL Panhandle. These appear to be
    focused along a low level axis of convergence, just above the
    surface, represented in 925 mb VAD wind plots, extending from near
    Lake Pontchartrain into the FL Panhandle. Aloft, a potent mid to
    upper-level shortwave was noted on water vapor imagery just east
    of the Sabine River. Divergent flow aloft was focused just ahead
    of the shortwave and associated jet axis across southeastern LA
    into southern MS, aiding lift over the region.

    As the shortwave continues to move east tonight, ascent will
    translate downstream along the Gulf Coast, with embedded areas of
    heavy rain likely following suit. Given the moist environment (PWs
    of 1.6 to 1.9 inches), with warm-layer depths of 3500-4000 m,
    efficient rainfall will be likely with hourly rainfall of 2 to 3+
    inches at times and possibly 3 to 5 inches within a 2-3 hour
    period. While weak instability (less than 1000 J/kg) will limit
    the coverage of heavy rain, small pockets of flash flood potential
    will remain a possibility over at least the next 3-5 hours.
    Another consideration is the higher than average rainfall over the
    past 1-2 weeks across a good portion of the region which may leave
    locations more prone to runoff compared to average.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_tHGKIWrR5_z1HT4s_Ux8cvKXHhM1-bQm_cW0yKZ84gAO0sPlU85fQeEjNShPtHvgztW= T_aPohfp7eMG3kr7FRmYRu8$ for graphic product...

    ATTN...WFO...JAN...LIX...MOB...TAE...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 31538685 31348491 30798405 30038420 29538512=20
    29508610 29818860 29668986 29589045 29829090=20
    30359093 30979028 31238915=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 13 03:17:09 2026
    AWUS01 KWNH 130317
    FFGMPD
    FLZ000-GAZ000-130715-

    Mesoscale Precipitation Discussion 0172
    NWS Weather Prediction Center College Park MD
    1116 PM EDT Tue May 12 2026

    Areas affected...portions of southern Georgia

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

    Valid 130315Z - 130715Z

    Summary...A nearly stationary band of convection over
    south-central Georgia was producing 1-2.5 inch/hr rain rates just
    northwest of Valdosta. These rates could persist for another
    couple hours. Flash flooding is possible in the affected areas.

    Discussion...A nearly stationary band of convection has exhibited
    very slow and erratic movement over areas from near Thomasville to
    near Adel. The storms were situated directly beneath an upper low
    over the area, which was likely combining with weak, isentropic
    ascent to support persistent, shallow updrafts despite marginal
    instability (~500 J/kg MUCAPE per SPC Mesoanalyses). The overall
    scenario for flash flooding was not evolving quickly, and with
    peak rain rates exceeding local FFG and prompting modest MRMS
    Flash responses, it is likely that local impacts from excessive
    runoff are underway in at least a couple of spots.

    High-res guidance suggests that storms will weaken through 06Z,
    although their current handling of the scenario lends some
    uncertainty, and observations suggest that the ongoing threat will
    persist beyond 05Z/1a eastern. Additional local totals of 3
    inches cannot be ruled out. Conditions will be monitored for
    additional flash flood potential beyond 07Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_JLcn6ufdLbr1LKWHMaGV_GlcjUQjllUzR4txnx7YPCTIBOqgqz4DrpREUNqS1s9SB9i= AAZX3tszgbSnyYnhw1xaKOM$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 31508294 31318256 30888274 30568396 30898445=20
    31298384=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 13 03:23:11 2026
    AWUS01 KWNH 130323
    FFGMPD
    FLZ000-GAZ000-130715-

    Mesoscale Precipitation Discussion 0172
    NWS Weather Prediction Center College Park MD
    1122 PM EDT Tue May 12 2026

    Areas affected...portions of southern Georgia

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

    Valid 130315Z - 130715Z

    Summary...A nearly stationary band of convection over
    south-central Georgia was producing 1-2.5 inch/hr rain rates just
    northwest of Valdosta. These rates could persist for another
    couple hours. Flash flooding is possible in the affected areas.

    Discussion...A nearly stationary band of convection has exhibited
    very slow and erratic movement over areas from near Thomasville to
    near Adel. The storms were situated directly beneath an upper low
    over the area, which was likely combining with weak, isentropic
    ascent to support persistent, shallow updrafts despite marginal
    instability (~500 J/kg MUCAPE per SPC Mesoanalyses). The overall
    scenario for flash flooding was not evolving quickly, and with
    peak rain rates exceeding local FFG and prompting modest MRMS
    Flash responses, it is likely that local impacts from excessive
    runoff are underway in at least a couple of spots.

    High-res guidance suggests that storms will weaken eventually,
    although their current handling of the scenario lends some
    uncertainty, and observations suggest that the ongoing threat will
    persist beyond 05Z/1a eastern. Additional local totals of 3
    inches cannot be ruled out. Conditions will be monitored for
    additional flash flood potential beyond 07Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6OEC3aqxpJPnrs5VyIuUSgGYeHA44qztazW8scmJQfFPgwotsYc9lVlw8IW_qZ79RjBJ= mhdCFGRJ8j9zGJMO176dvOw$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 31508294 31318256 30888274 30568396 30898445=20
    31298384=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 16 19:51:56 2026
    AWUS01 KWNH 161951
    FFGMPD
    KYZ000-INZ000-ILZ000-170130-

    Mesoscale Precipitation Discussion 0173
    NWS Weather Prediction Center College Park MD
    350 PM EDT Sat May 16 2026

    Areas affected...Southern Illinois...Southern Indiana ...adjacent
    Northwest Kentucky...

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

    Valid 161950Z - 170130Z

    SUMMARY...Favorable environment for subtle heavy rainfall style
    event or two given proximity to mid-level shortwave center passing
    to southeast.

    DISCUSSION...19z surface analysis denotes a weak surface wave just
    southeast of St. Louis, MO sitting along a stationary thermal
    boundary, reinforced by early morning rainfall/outflow. CIRA LPW
    suite (oblique polar pass) shows a small pool of enhanced boundary
    level to 500mb moisture along combined with upper 60s and low 70s
    Tds through S IL/S IND, bringing a small pocket of overall totals
    over 1.75" within a favorable southwesterly to west-southwesterly
    WAA 925-850mb flow regime increasing moisture flux convergence
    along it. While cloud cover has been generally dense this morning
    into early afternoon, some clearing and broken insolation has seen
    temps into the low 80s, particularly downstream into NW KY/S IND,
    resulting in a narrow west to east axis of 2000 J/kg MLCAPE that
    is becoming increasingly uncapped.

    GOES-E WV suite along with visible loop, shows a small mid-level
    shortwave twist to the cloud pattern over NW KY that is expected
    to continue a east-northeast progression further providing larger
    scale ascent, especially downstream. However, aloft, RAP analysis
    denotes a strong divergence signal at the far right entrance to
    the jet streak over the Great Lakes across central IL, along the
    northwest periphery of the shortwave. The combination of all
    factors is supporting initial break out of deeper updrafts (rapid
    cooling and expansion of these clusters/cells shows potential
    instability of the broader area). So low level WAA/convergence
    should help feed the updrafts with slow eastward movement given
    15-20kts of deep mean steering flow, but overall inflow from the
    west-southwest results in favorable propagation vectors for
    back-building and or slowing of the forward progression of
    clusters that due develop mainly because of the proximity on the
    NW side of the mid-level shortwave. As a result there is good
    potential for increased residency of stronger/broader moist
    updrafts capable of 1.5-2"/hr rates. Localized totals of 2.5-3"
    are possible.

    Stronger cells with greater coverage are expected downstream/east
    of the shortwave but should be forward propagating quicker;
    however, these rates/quick totals of up to 1" could set the stage
    for the slower moving upstream allowing repeating. While the
    overall Midwest has been dry, NASA SPoRT 0-40cm soil moisture
    values of 50-65% across the area of concern, which is much higher
    than surrounding areas (not including this morning's rainfall
    tracks). So with FFG values of 1.5-2"/hr and 2-2.5"/3hrs, and
    proximity to flash flood prone cities like Evansville/Louisville
    there is sufficient potential for a localized incident or two of
    possible flash flooding through late afternoon/evening across the
    area of concern.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!497FomLp5UQm8ELrJMqWCK5KLr8wHwkWmjbAMOrKtiJSJGuJBZPcDRxdQwKFWbxiyYxg= P9lrIiE-5I43OJ3RgHbNsxE$ for graphic product...

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

    ATTN...RFC...MSR...ORN...TIR...NWC...

    LAT...LON 39598784 39508661 39328518 38868469 38278474=20
    37838551 37738654 37658748 37658849 37748931=20
    38118978 38618992 39198967 39518904=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 16 21:21:35 2026
    AWUS01 KWNH 162121
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-170315-

    Mesoscale Precipitation Discussion 0174
    NWS Weather Prediction Center College Park MD
    520 PM EDT Sat May 16 2026

    Areas affected...Northern MO...Southwest IA...Ext. Southeast
    NEB...

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

    Valid 162120Z - 170315Z

    SUMMARY...Slow moving, back-building thunderstorms with 1.75-2"/hr
    rates will support mergers and repeating through the evening
    hours. Localized 3-4" totals are probable with isolated 5"+
    possible. Flash flooding is considered possible, given recent dry
    conditions may help mitigate moderate rainfall totals.

    DISCUSSION...21z surface analysis depicts a weak surface wave near
    Nebraska City, generally at the western extent of the deeper
    moisture plume across the Central U.S. Deep southwesterly flow
    aloft is providing broad scale ascent and lowering surface
    pressures in the lee of the Rockies and driving a broad strong
    southerly LLJ across the Plains and Ozark Plateau. This
    moisture/higher theta-E air is generally mid-80s over upper
    60s/low 70s Tds, supporting total PWats near 1.5" and with
    southwesterly flow aloft, resulting in steepening lapse rates,
    supportive of 3000-3500 MLCAPE across E KS into NW MO.=20=20

    The surface low resides at the apex of a broader surface SW to NE
    trough with the frontal boundary extending along the KS/NEB
    boarder before angling northeast across south central IA into S
    WI. A more important outflow boundary from last night/this
    morning's convection has effectively become a deeper thermal
    boundary/warm front from near CSQ in IA dropping south across
    north-central MO toward KCOU before turning E across S IL. As
    such, the southerly surface to 700mb southerly flow is ascending
    isentropically across is boundary resulting in the first bands of
    deeper convection across north-central MO. Overall, vigor remains
    a bit limited but will further aid in steepening the
    boundary/isentropes over the next few hours, increasing deep layer
    moisture convergence. As the LLJ strengthens, flux convergence
    will help to broaden updrafts and rainfall efficiency as the
    overall moisture pool increases to 1.75" TPW toward 23z. Overall
    coverage and broadening updrafts will allow for cells to increase
    to 1.75"/hr rates with occasional 2-2.25" occurring and localized
    2.5" for eventual short-term mergers.=20=20

    The concern toward and after 00z, will be the broadening of the
    500-1000mb thickness lines, reducing forward propagation and
    bending steering flow a bit more south of due east further
    increasing convergence, though this will be concurrent with
    strengthening upstream inflow turning propagation vectors
    southwest with time, allowing for higher potential of an
    individual cell's residency and/or repeating tracks. Eventually,
    back-building toward southeast NEB. A broad swath of 2-5" is
    becoming more probable across this area with 18z HREF probability
    of 70-90% of 3"/6hrs along/near the intersection of the
    fronts/outflow along the IA/MO line. This is likely to shift
    (more likely south and west given trends); the 'good news' is the
    area has very high FFG values (2.5"/hr; 3-4"/3hrs) due to
    prolonged dry spring with 0-40cm Soil Moisture around 25-30%,
    though areas nearer the Missouri River and portions of SW IA are a
    bit more moist and have lower FFG values. Still, the overall
    rainfall and rates are still possible to induce widely scattered
    to scattered incidents of flash flooding through 03z. Please note:
    further upstream development over the Higher Central Plains is
    likely to roll through later into the overnight period (after
    03z), so at best, this round will only wet the upper soil column
    for those cells later too, a subsequent MPD may be required.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9VcXlr9_PjGyMcyHRwzaSKTnfhvLyeyW1M46Y6h_NlSaMkIhxNXPTJ7sbEeIN-kF0ZwC= aRfQxuA7aCSzyGbrlskHsqw$ for graphic product...

    ATTN...WFO...DMX...EAX...LSX...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 41479517 41439361 40519263 39679173 38959238=20
    39259379 40199563 40589631 41069611=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 17 00:35:29 2026
    AWUS01 KWNH 170035
    FFGMPD
    KSZ000-NEZ000-170600-

    Mesoscale Precipitation Discussion 0175
    NWS Weather Prediction Center College Park MD
    834 PM EDT Sat May 16 2026

    Areas affected...Southern Nebraska...Portions of Northwest
    Kansas...

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

    Valid 170035Z - 170600Z

    SUMMARY...Slow moving super-cells becoming localized heavy rain
    producers, before main upstream cluster/MCS puts final additional
    heavy burst to exceed very dry ground conditions for a widely
    scattered incident or two of localized possible flash flooding.

    DISCUSSION...00z surface and RAP boundary layer analysis depict a
    very tight moisture stream along and south of well defined
    stationary front that extends from active convection in SE IA and
    through southern NEB from south of Lincoln to Hastings to Holdrege
    before angling toward expanding progressive cluster, developing
    MCS coming out of NW KS. Strong surface pressure falls upstream
    has accelerated near boundary layer easterly flow increasing low
    level moisture profile as noted in CIRA LPW even through the
    700-500mb layer, with the 1.5" total PWat starting to nose as far
    west as south-central NEB. Surface southerly flow backing with
    height has provided solid low level moisture convergence given Tds
    rising into the low 60s, with some trapped moisture on the
    north-side of the boundary into the mid-60s as far east as Grande
    Island, NEB; reducing sub-cloud evaporation. As such, recent
    trends in KDP analysis show increasing degrees/KM suggesting
    additional higher rainfall rates with reducing near or sub-zero
    values for 'large hail' signatures strongly suggesting increasing
    rainfall efficiency over the last hour or so.=20

    Overall RADAR coverage of convective cores has increased as well
    given numerous left splitting super-cell structures; but with the
    updraft rotation, forward propagation has slowed mainly for the
    right movers to increase residency . While rain-rates are still
    likely inflated due to hail contamination, hourly rates of 1.5-2"
    are becoming more probable given the increasing moisture flux
    convergence due to isallabaric effects. Localized totals of
    1.5-2.5" are becoming increasingly possible but narrowly focused
    along and just north of the stationary front. However, the strong
    drought in the region is resulted in very dry conditions and
    allowing for a solid uptake of those totals, but the rates may
    still be a tad to great locally, resulting in some spots of
    localized flash flooding potential. This will only be exacerbated
    as the upstream MCS cluster sweeps up/merges with the remaining
    super-cells through the early overnight period across
    south-central NEB, with a sub-hourly burst of .75-1" in 15 minutes
    per recent HRRR output resulting in spot or two of 2-3" values
    which is in the range of 1 to 3hr FFG exceedance and localized
    flash flooding is therefore considered possible, more so eastward
    through the MPD area of concern.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4XlChmG_LE-3luG20gQb4qjwQH7bwTkdmvJOtRUNDq3vcXB-1_eD2fJKOb0yKc6dWZMA= vAczv6JUWFHWDSMDeuaQPHE$ for graphic product...

    ATTN...WFO...GID...GLD...LBF...OAX...

    ATTN...RFC...KRF...NWC...

    LAT...LON 41779746 41589658 41009601 40599586 40109621=20
    40059743 39919950 39590085 40280134 40880070=20
    41239990 41649855=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 17 03:31:14 2026
    AWUS01 KWNH 170331
    FFGMPD
    ILZ000-MOZ000-IAZ000-KSZ000-NEZ000-170720-

    Mesoscale Precipitation Discussion 0176
    NWS Weather Prediction Center College Park MD
    1129 PM EDT Sat May 16 2026

    Areas affected...middle MO RIver to middle MS River Valley

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

    Valid 170328Z - 170720Z

    Summary...Areas of flash flooding will remain likely across
    portions of southeastern NE, northeastern KS into southwestern IA
    and northwestern MO over the next couple of hours. Locations
    farther east may also experience flash flooding. Peak hourly
    rainfall of 2 to 3+ inches can be expected.

    Discussion...An axis of thunderstorms was oriented roughly west to
    east at 03Z, extending from southeastern NE into northwestern and
    northern MO, with a slow moving MCV in north-central MO along the
    eastern flank of the MCS. A Flash Flood Emergency was recently
    issued for Grundy County, including the city of Trenton where ~6
    to 8 inches of rain has fallen with embedded hourly rainfall over
    3 inches (and 2.5 inches in 30 minutes) at times. Back to the
    west, thunderstorm coverage was increasing over the southeastern
    quadrant of NE, in advance of a forward propagating line segment
    advancing along the central NE/KS border.

    The activity was largely elevated atop a remnant outflow boundary
    which extended ESE from southeastern NE, just south of STJ into
    north-central MO. MUCAPE values were 2000-3000 J/kg via 03Z SPC
    mesoanalysis data and 850 mb VAD wind data at KTWX showed
    strengthening flow between 00-03Z (30 to 55 kt) with further
    strengthening to near 60 kt possible by 06Z. Aloft, flow was
    fairly diffluent/divergent to the south of an 80-100 kt upper jet
    max north of the region. Sufficient shear and instability will
    sustain a mixture of supercells and multicells with a combination
    of slow cell motions, mergers and training leading to high hourly
    rainfall, locally in excess of 3 inches possible over the next 2-4
    hours.

    There are signs in the recent hires guidance that the pattern will
    be disrupted toward 06-07Z, in advance of the forward propagating
    line segment over the NE/KS border as increasing southerly flow
    and forcing shifts northward of the present axis. However, prior
    to that time, another 3-4 hours of locally heavy rain with areas
    of flash flooding will remain likely with an additional 3-5 inches
    of rain possible through 07Z, with a focus in and around the MO
    River Valley.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!760uQl1ohFv2KU1K6qPWh_0aJfvHwirl-l3LZ2hyyMw3Tv0DIsmmzLmmfVFlqTOOG4jb= 94fPrgL7u0SXf38ulDn2Wj4$ for graphic product...

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

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 41519233 41169114 39849151 39449302 39519515=20
    39959703 40439746 40809729 41219669 41429459=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 17 03:38:16 2026
    AWUS01 KWNH 170338
    FFGMPD
    ILZ000-MOZ000-IAZ000-KSZ000-NEZ000-170720-

    Mesoscale Precipitation Discussion 0176...Corrected
    NWS Weather Prediction Center College Park MD
    1137 PM EDT Sat May 16 2026

    Corrected for adjustment to capitalization in areas affected

    Areas affected...middle MO River to middle MS River Valley

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

    Valid 170328Z - 170720Z

    Summary...Areas of flash flooding will remain likely across
    portions of southeastern NE, northeastern KS into southwestern IA
    and northwestern MO over the next couple of hours. Locations
    farther east may also experience flash flooding. Peak hourly
    rainfall of 2 to 3+ inches can be expected.

    Discussion...An axis of thunderstorms was oriented roughly west to
    east at 03Z, extending from southeastern NE into northwestern and
    northern MO, with a slow moving MCV in north-central MO along the
    eastern flank of the MCS. A Flash Flood Emergency was recently
    issued for Grundy County, including the city of Trenton where ~6
    to 8 inches of rain has fallen with embedded hourly rainfall over
    3 inches (and 2.5 inches in 30 minutes) at times. Back to the
    west, thunderstorm coverage was increasing over the southeastern
    quadrant of NE, in advance of a forward propagating line segment
    advancing along the central NE/KS border.

    The activity was largely elevated atop a remnant outflow boundary
    which extended ESE from southeastern NE, just south of STJ into
    north-central MO. MUCAPE values were 2000-3000 J/kg via 03Z SPC
    mesoanalysis data and 850 mb VAD wind data at KTWX showed
    strengthening flow between 00-03Z (30 to 55 kt) with further
    strengthening to near 60 kt possible by 06Z. Aloft, flow was
    fairly diffluent/divergent to the south of an 80-100 kt upper jet
    max north of the region. Sufficient shear and instability will
    sustain a mixture of supercells and multicells with a combination
    of slow cell motions, mergers and training leading to high hourly
    rainfall, locally in excess of 3 inches possible over the next 2-4
    hours.

    There are signs in the recent hires guidance that the pattern will
    be disrupted toward 06-07Z, in advance of the forward propagating
    line segment over the NE/KS border as increasing southerly flow
    and forcing shifts northward of the present axis. However, prior
    to that time, another 3-4 hours of locally heavy rain with areas
    of flash flooding will remain likely with an additional 3-5 inches
    of rain possible through 07Z, with a focus in and around the MO
    River Valley.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6lp2bl8r2tBWDmKe5Xs-dZIdDzoRrojlanQquKmErPU2Z8lJDHRJW0g96IdmGe4yQwmJ= 1N4HSrlVSjiky8mbFPXahyE$ for graphic product...

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

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 41519233 41169114 39849151 39449302 39519515=20
    39959703 40439746 40809729 41219669 41429459=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 17 07:47:48 2026
    AWUS01 KWNH 170747
    FFGMPD
    WIZ000-ILZ000-MOZ000-IAZ000-NEZ000-171300-

    Mesoscale Precipitation Discussion 0177
    NWS Weather Prediction Center College Park MD
    346 AM EDT Sun May 17 2026

    Areas affected...western IA/MO border into IA and southwestern
    WI/northwestern IL

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

    Valid 170745Z - 171300Z

    SUMMARY...Localized flash flooding will remain a possibility
    through 13Z (8 AM CDT) from the western IA/MO border into IA and
    the MS River near the WI/IL border. Hourly rainfall of 1-2 inches
    and localized peak rainfall of 2-4 inches can be expected.

    DISCUSSION...Radar imagery across the middle MO River Valley
    showed a convectively induced vorticity max along the southern
    NE/IA border at 0715Z associated with an eastward bowing line
    segment crossing into southwestern IA and northwestern MO. Areas
    of stratiform rain preceded and followed the bowing segment (which
    has shown signs of weakening over the past 30 minutes), along with
    a few stronger cells near the MO/IA border. However, trends in
    MRMS-derived hourly rainfall showed a reduction in the coverage
    and intensity of high rain rates since 05Z as convective
    development just north of a remnant outflow boundary draped across
    northern MO has reduced.

    Short term forecasts from the RAP indicate the shortwave/vorticity
    max along the southern NE/IA border will track northeastward over
    the next 3-6 hours. Low level overrunning of the remnant
    outflow/effective front in northern MO will continue as the
    mid-level circulation advances toward the northeast beneath
    diffluent and divergent flow in the upper levels. Elevated
    instability of 500 to 1000+ J/kg was estimated over southern IA
    via the 07Z SPC mesoanalysis but these values fall off quickly to
    the north with only modest northward advancement of the elevated
    instability pool through 13Z forecast. Over the next 3-6 hours,
    there will continue to be the potential for short term training
    with 1 to 2 inches of rain in an hour and localized potential for
    2-4 inches through 13Z (8 AM CDT), located near the track of the
    shortwave. While the expected potential for heavy rain over the
    next few hours will be north of areas that experienced flooding
    earlier tonight in northern MO, portions of IA have received 1 to
    3 inches of rain over the past 48 hours which may contribute to
    isolated runoff where overlap of additional heavy rain occurs.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4GSUKMFNjbMh4tO-hoxs6y7pFNqyNKqPmwEgSMHZiECgN2PqEkh6QnZ4Xi3mrGDOUgHH= BdM-up4CIAjmW8DM5mtEfF0$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...EAX...LOT...MKX...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 43059094 42929044 42488989 41958968 41528997=20
    41139078 40659201 40059360 40149525 40569575=20
    41139579 42069401 42789210=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 17 20:00:06 2026
    AWUS01 KWNH 171959
    FFGMPD
    MNZ000-IAZ000-NEZ000-SDZ000-180200-

    Mesoscale Precipitation Discussion 0178
    NWS Weather Prediction Center College Park MD
    358 PM EDT Sun May 17 2026

    Areas affected...Southeast SD...Eastern NEB...Western IA...Far
    Southwest MN...

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

    Valid 172000Z - 180200Z

    SUMMARY...Increasing available moisture to support higher rainfall
    efficiency over the next few hours (up to 2"/hr). Progressive
    nature may be a limiting factor, but cells will move into a bit
    more prone to FF due to recent rains (esp. South).

    DISCUSSION...19z surface analysis depicts the very dynamic
    environment in place across the Plains this afternoon (given broad southwesterly flow aloft). The southern stream shortwave last
    evening that has progressed into the Great Lakes helped to
    reinforce a tight moisture gradient along the primary west to east
    from from a weak wave in E IA back across central IA to a surface
    wave near an strong cluster of thunderstorms with a history of
    hail and forward progression. CIRA LPW and RAP analysis shows a
    tight, enhanced moisture plume along and south of the boundary
    generally denoted by agitated Cu field (NE NEB, into central IA)
    opposed by north where transverse banding shows the greater
    stabilized area that is a bit drier as well across far NW IA into
    SW MN. Enhanced Tds in through 850mb along with slightly backed
    flow for solid moisture flux transport toward the surface low
    along/ahead of main cold front NE of O'Neil, Neb.

    Solid low level directional convergence has aided maintenance of
    the cluster with strong deep layer moisture convergence signals
    denoting the flux. As the cluster reaches the deeper moisture
    axis, expectation is both increased moisture loading to the
    updrafts helping to broaden downdrafts as well as increase
    rainfall efficiency. Rapid refresh guidance including the HRRR
    and WoFS solutions denote this uptick in the next hour or so with
    sub-hourly intense rates expected; with 15-minute HRRR totals over
    1-1.25" while 5-minute rates in the WoFS over .5", as high as .75"
    consistently across SE SDAK. Deep layer steering and cold frontal
    push are likely to limit residency time but some eastward
    development along the frontal/theta-E axis may break out
    additional downstream cells to help with some repeating to reach
    higher required totals to induce widely scattered incidents of
    flash flooding (2-3" in 1-3hrs).=20=20

    Further expansion of the convection toward the south along and
    north of the stronger 995mb surface low along the NEB/KS will come
    as embedded shortwave in the deeper southwesterly flow approaches
    and upper-level diffluence increases into a developing north-south
    jet streak placing much of the area of concern in favorable
    divergence/outflow environment aloft in the right entrance of said
    jet streak.

    Hydrologically, much of the area remains in solid drought with
    0-40cm ratios in the 20-30%, though scattered activity last night
    did wet a few areas, especially south and east across E NEB and
    through the Missouri River Valley. As noted, above the
    progressive nature will likely limit the overall coverage of flash
    flooding, but the shear intensity with some repeating and possible
    intersection with those wetter upper soils, suggest widely
    scattered flash flooding is possible this evening.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7dwM4qPIPaCm2epJ080lGFFhouAWdHzoYRclS2vg1hWL3BJR43tAvrJ_2Un0Mvx5YDMj= I4jqP5Dz8fofqhCJ4bf1SEg$ for graphic product...

    ATTN...WFO...FSD...GID...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 44499698 44179587 43629534 42319568 41069591=20
    40489702 40519934 40929935 41569836 42459794=20
    42909829 43449867 44209800=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 18 00:26:33 2026
    AWUS01 KWNH 180026
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-180600-

    Mesoscale Precipitation Discussion 0179
    NWS Weather Prediction Center College Park MD
    825 PM EDT Sun May 17 2026

    Areas affected...Southeast NEB...Southwest IA...Northwest
    MO...Central to Northeast KS...

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

    Valid 180025Z - 180600Z

    SUMMARY...Training/Back-building cells at apex of dry slot will be
    slow moving while higher moisture flux cells northward will track
    through areas of recently saturated grounds with rates of 1.5"/hr
    and spots of 2-3" totals, pose widely scattered incident or two of
    flash flooding into early overnight period.

    DISCUSSION...00z surface analysis depicts a very deep, but narrow
    surface trough extending from a surface low in SE SD, southward to
    a 993mb low just south of the central NEB/KS border at the nose of
    an equally narrow but very dry slot; simultaneously, a strong
    northern stream cold front is dropping southeastward from the low
    resulting is a very strong surface to boundary layer flow with a
    broad area of 20 to 30kts from the south slowly backing toward the
    frontal zone. This results is a long axis of strong moisture flux
    convergence, especially across SE NEB where Tds are in the high
    60s, tipping toward the low 70s across the Missouri River into
    IA/N MO. While the solid EML is well denoted in the CIRA LPW
    850-700mb layer across much of this areas, return moisture
    wrapped around the apex of the tight inverted trough, is pooled
    along the approaching cold front. So while the steep lapse rates
    are supporting MLCAPEs of 3000-4000 J/kd across E KS into SE NEB,
    there is some entrainment of higher moisture and stronger
    thunderstorms are starting to moisten the mid-layer profile and
    overall rainfall efficiency is starting to increase and will do so
    after sunset.

    Coincident with the inverted trough is a tight 500-1000mb
    thickness ridge the becomes a bit more divergent in isoheight
    lines along and east of the trough axis. This supports reduced
    forward propagation vectors, especially near the surface low and
    south across central KS and with deep layer fairly unidirectional
    flow from the SW, may allow for training/repeating across this
    area while cells/clusters further north will start propagating east-northeastward at a more reasonable rate across E NEB into IA.
    Evaporative loss will limit extreme rates, though the moisture
    flux on the 30+kt inflow should support 1.5"/hr with an
    occasionally uptick to 1.75"+, and may be slightly higher due to
    ingest of smoke particulates from the prairie fires in Clark and
    Meade counties.

    Northward in SE NEB and along the IA/MO border, the heavy rainfall
    last evening has brought FFG values into a range (1-1.5"/hr
    <2"/3hrs) that may be locally exceeded with the clusters moving
    east, suggesting a scattered incident or two of flash flooding
    will be possible through early overnight period. Southward across
    central KS, the unidirectional steering and upwind propagation may
    allow for increased residency; so while this area's soil
    conditions are very dry, the prolonged nature of rainfall with
    localized spots of 2-4" may also result in localized FF. (Note: a
    backyard observation near Dorrance, KS in E Russell county saw
    just below 2" in the last hour). So all considering, a few spots
    of flash flooding are considered possible across the MPD area of
    concern through the overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5IInHaJaZZMwD3wa0TaLpebr92Hz9Aevw48MwlnPPZbxy9I-twDjBNXJPhPeOPj8Va6D= _El-L9tZjN8AHI9Tq73wSfU$ for graphic product...

    ATTN...WFO...DDC...DMX...EAX...GID...ICT...OAX...TOP...

    ATTN...RFC...KRF...MSR...TUA...NWC...

    LAT...LON 42169490 42079412 41929340 41309302 40119334=20
    39529611 38429803 38269948 38889946 39559824=20
    40669796 41839753 42149622=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 18 00:59:07 2026
    AWUS01 KWNH 180059
    FFGMPD
    WIZ000-MNZ000-IAZ000-180600-

    Mesoscale Precipitation Discussion 0180
    NWS Weather Prediction Center College Park MD
    857 PM EDT Sun May 17 2026

    Areas affected...Northern Iowa...Southern Minnesota...Parts of
    Northwest Wisconsin...

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

    Valid 180100Z - 180600Z

    SUMMARY...Increasing convective coverage and increasing moisture
    flux into expanding convective clusters/small MCS features support
    potential for repeating and spots of 2-4". Localized flash
    flooding remains possible through the early overnight period.

    DISCUSSION...GOES-E WV suite depict broad long-wave trough across
    the Inter-mountain West with broad southwesterly flow downstream
    across the Plains. At the apex an expanding convective complex
    shows strong diffluent outflow pattern at the right entrance to
    strengthening jet streak aloft providing broad scale ascent as
    well as strengthening of a broad south-southwest LLJ. At the
    surface the northern surface low/apex of a tight and deep inverted
    surface trough is crossing out of SE SDAK into MN while drawing a
    well defined warm front northward. CIRA LPW and RAP analysis
    notes that core of western Gulf moisture is finally arriving
    northward along and east of the advancing cold front that extends
    from the surface low back across eastern NEB. The cluster in SW
    MN has a very long history of severe and strong isallobaric
    backing influence to maximize moisture flux pulled along and north
    of the surface front, supporting intense but short-term rainfall
    rates near 1.5-2"/hr mostly falling in 15-30 minutes. However,
    given the stronger LLJ and isentropic ascent, downstream
    convection is filling along and northeast where convergence is
    maximized. Deep layer steering flow will allow for some repeating
    of the cores to increase intense rainfall duration over 1-2 hours
    allowing for localized totals to reach 2-3" values.=20

    In addition, a second complex north of a secondary low across NE
    NEB has seen a similar rapid cooling of the cirrus canopy with
    numerous overshooting tops; deeper moisture pool has also
    broadened the downdrafts width as the line matures into a larger
    linear convective complex. While there is a general eastward
    propagation, RADAR and satellite trends suggest there is also a
    potential to repeat/track through similar areas of the northern
    cluster across portions of S MN/N IA. Recent WoFS runs helps to
    confirm this as mean and 90th percentile qpf suggest 2.5-5"
    maximum swath is possible. This provides some confidence that
    spots of 2-4" are becoming increasingly possible through the early
    overnight period.=20

    While NASA SPoRT 0-40cm soil moisture fields show drought is solid
    with ratios running from 25% in NW IA to near 40% in south-central
    MN toward the Twin Cities, the FFG values suggest 1hr rates of
    1.5"/hr and less than 2.5"/3hr could result in flash flooding. If
    that is the case, incidents of flash flooding are possible, but
    given the overall drought conditions would be looking to smaller
    localized incident or two where rates can reach closer to
    1.75-2"/hr, where infiltration would be reduced from the shear
    amount too fast. So given the overall pattern/trends, flash
    flooding continues to be considered possible across the MPD area
    of concern tonight.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6z3vCw4cBcd06sL2vpD6Yb8HccNxiHhZwedU4szunbouCqvjgG3v_xalByDNTvfqKBz2= SOYEEzqR1bhyP_Oz3PWcFVo$ for graphic product...

    ATTN...WFO...ARX...DMX...FSD...MPX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45259218 44609139 43359219 42549394 42299574=20
    42559638 43409586 44359487 45209331=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 18 06:14:12 2026
    AWUS01 KWNH 180614
    FFGMPD
    MOZ000-KSZ000-181016-

    Mesoscale Precipitation Discussion 0181
    NWS Weather Prediction Center College Park MD
    213 AM EDT Mon May 18 2026

    Areas affected...central/eastern KS into western MO

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

    Valid 180612Z - 181016Z

    Summary...Flash flooding is likely to focus in one or two
    locations from central to eastern KS into western MO through 10Z.
    Training will likely result in 1-2 in/hr rates (locally higher)
    with additional totals over 4 inches possible through 10Z on an
    isolated basis.

    Discussion...06Z radar imagery showed that an axis of elevated
    thunderstorms extended from near LYO, ENE into northwestern MO
    near MCI, just north and west of an outflow boundary. Training of
    thunderstorms in central KS has resulted in MRMS-derived rainfall
    of 3 to 9 inches over the past 6 hours from southern Rush County
    into northwestern Ottawa County, though some of that could be high
    due to hail contamination. However, there was at least one
    Wunderground PWS with 7.26" to the southwest of Lincoln ending
    0555Z.

    Current satellite trends in IR imagery showed the coldest cloud
    tops were slowly shifting east, coinciding with an area of strong
    upper level jet induced divergence and diffluence tied to a
    strengthening jet max extending from the west-central KS/NE border
    into the lower Northern Plains.

    A strong southerly low level jet of 50 to 65+ kt was seen in VAD
    wind plots at 850 mb from northern OK into southern KS, lifting
    atop the outflow boundary, with deeper layer wind vectors
    supporting SW to NE training at times. Steep mid-level lapse rates
    of 8-9 C/km were observed in 00Z soundings at OKC, TOP and SGF,
    supporting MUCAPE values between 3000 and 4000 J/kg. Veering of
    the low level jet through 10Z is forecast, as the outflow boundary
    likely continues to advance southeastward, supporting continued
    elevated thunderstorms with areas of training.

    While increased convective inhibition with southward extent may
    limit how far south convection will reach, inhibition for
    locations farther east is forecast to remain weak. Therefore,
    while flash flooding is not expected to be widespread, areas of
    training are likely to focus high rain rates and focused flash
    flooding from central to eastern KS into far western MO through
    10Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9_RvCK6VLD4SB8BJ7eXu9AFwKpyKQrJlac0mfDlhgLRBiWn6vCF-Guud2ENHWy1mM4cp= KrE-2EKhci4PgDhqBTBD8ak$ for graphic product...

    ATTN...WFO...DDC...EAX...ICT...SGF...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 40009416 39409365 38369394 37779489 37539666=20
    37369932 38089966 38849841 39509698 39779589=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 18 10:03:41 2026
    AWUS01 KWNH 181003
    FFGMPD
    MOZ000-KSZ000-181500-

    Mesoscale Precipitation Discussion 0182
    NWS Weather Prediction Center College Park MD
    602 AM EDT Mon May 18 2026

    Areas affected...eastern KS into western/southwestern MO

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

    Valid 181000Z - 181500Z

    Summary...While some uncertainty remains, concerns are increasing
    for possible flash flooding later this morning over
    western/southwestern MO into portions of eastern KS. Hourly
    rainfall of 1 to 2+ inches and 3 to 4 inches in 3 hours will be
    possible through 15Z (10 AM CDT).

    Discussion...0930Z radar imagery and surface observations showed
    that the southwestern end of an elongated outflow boundary has
    stalled over central KS, while it continued to steadily advance
    southeastward through MO. Showers and thunderstorms continued to
    develop on the cool side of the boundary over eastern KS and
    central MO as a strong southerly low level jet (LLJ) over KS/OK/MO
    overruns the well-defined boundary. While the LLJ has weakened and
    veered some over the central KS/OK border (less favorable angle to
    the outflow boundary), some recent strengthening was observed at
    the KINX VAD wind at 09Z to over 70 kt (but it as backed off a bit
    since then). Meanwhile, disorganized shower/thunderstorm activity
    has picked up over the past 45 minutes over southwestern MO,
    perhaps aided by lift ahead of a vort max observed lifting NNE
    from the southern OK/AR border on water vapor imagery. Steep
    mid-level lapse rates of 7 to 8+ C/km were contributing to sizable
    MUCAPE over 2000 J/kg from southeastern KS into central MO. Aloft,
    flow remained highly diffluent between the polar and sub-tropical
    jet streams aloft.

    While recent runs of the HRRR and RRFS have struggled to properly
    handle the outflow boundary's southward propagation, they have
    been consistent with an uptick in convective vigor over the next
    3-6 hours, favoring the southwestern flank of the outflow near the
    southern KS/MO border. It is here that the LLJ (though weakening)
    will focus from northeastern OK into southwestern MO into and atop
    the KS/MO outflow boundary. The environment will favor training
    with 1 to 2+ inches of rain in an hour and potential for 3 to 4
    inches of rain in 3 hours or less. While flash flood guidance is
    quite high over much of the region, some limited/isolated flash
    flood potential will exist through 15Z and perhaps continue into
    the early afternoon.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_UvjHrcgw5M0uUTr5HEaIVMm2x5FP0eHz_MxqwBVy80NNb9mokYis-w2AcVN15ETHQ0n= veVfgwkacB-bhK5SD-Y-Bp0$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...SGF...TOP...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 39039508 39009309 38669248 38179217 37279244=20
    36919354 37219542 37739683 37789774 38199784=20
    38789717 38949649=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 18 15:36:43 2026
    AWUS01 KWNH 181536
    FFGMPD
    ILZ000-MOZ000-KSZ000-182134-

    Mesoscale Precipitation Discussion 0183
    NWS Weather Prediction Center College Park MD
    1135 AM EDT Mon May 18 2026

    Areas affected...southern/central Missouri through southern
    Illinois

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

    Valid 181534Z - 182134Z

    Summary...Heavy rainfall will likely continue through 21Z along
    and north of the I-44 corridor, with areas of flash flooding
    possible.

    Discussion...A mature, elongated MCS continues to provide areas of
    training thunderstorms along an axis from near Fort Scott,
    KS/Nevada, MO east-northeastward through Saint Louis Metro and
    into south-central Illinois. The MCS has become a bit more
    perpendicular to southwesterly low-level flow (around 40-45 kts at
    850mb), supporting repeating/training convection. The elevated
    nature of the convection suggests seems to have limited rainfall
    rates to only around 1 inch/hr in a few spots. However, the
    persistence of convection (likely supported by an approaching
    shortwave from the Arkansas Ozarks) should likely continue
    reinforcing the mature cold pool and resulting in several more
    hours of occasionally heavy rainfall.

    While rain rates may not breach 1-hr FFG thresholds on a
    widespread basis, it appears possible that 2.5 inch/3-hr rates
    could be achieved at times along this axis. This should result in
    at least isolated flash flood potential - particularly in any
    low-lying and urban parts of the discussion area. Again, the
    rainfall/flash flood potential will likely continue through at
    least 21Z/4p CDT.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6d_3BeLUcvVriflbiqgnKPI48aIn6bliiJ9cBiWF2GKyCR4mpyal7mOikjM5djhbmbbh= Q07Cwkwiypv0XwgJRbycXQc$ for graphic product...

    ATTN...WFO...EAX...ILX...LSX...PAH...SGF...

    ATTN...RFC...KRF...MSR...ORN...TIR...TUA...NWC...

    LAT...LON 40018956 39938838 39348784 38518808 37868904=20
    37189093 37139355 37549452 38229469 38749458=20
    39069390 39649156=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 18 17:21:54 2026
    AWUS01 KWNH 181721
    FFGMPD
    OHZ000-KYZ000-INZ000-ILZ000-182320-

    Mesoscale Precipitation Discussion 0184
    NWS Weather Prediction Center College Park MD
    120 PM EDT Mon May 18 2026

    Areas affected...portions of Indiana, far southeast Illinois, and
    far southwest Ohio

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

    Valid 181720Z - 182320Z

    Summary...Flash flood potential is increasing especially across
    central and southern Indiana.

    Discussion...A mature convective complex was making steady
    eastward progress into western and central Indiana over the past
    hour per radar mosaic imagery. The southern flank of this MCS was
    oriented more of a WSW-ENE fashion over southern Illinois, leading
    to areas of training. Furthermore, a shortwave trough evident in satellite/objective analyses over northern Arkansas was helping to
    initiate convection along and south of the leading edge of the
    MCS, with several areas of mergers and 2-2.5 inch/hr rain rates
    (per MRMS) estimated southwest of Terra Haute (just south of
    Effingham).

    The overall scenario for flash flooding will translate eastward
    through the afternoon, with occasional spots of 1-2.5 inch/hr rain
    rates where training/merging is most pronounced. The rates will
    fall on areas of wet soils from prior rainfall, with FFG
    thresholds of 1.5 inch/hr at risk of being exceeded on at least an
    isolated basis. Low-level flow drops off considerably with
    eastward extent into Ohio, which lends some doubt/uncertainty on
    eastward persistence of convection. Should the convective complex
    remain organized, slightly lower FFGs over Ohio would suggest a
    continued, yet isolated flash flood threat there.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4L-CrEcpou9u14sn7VEarQ3qO4exrqegjdwzFRPD68CCfI-emlXJAst9ApVJY7-mAc9U= 9H4CbQL__YxCqgffEW0YHDc$ for graphic product...

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

    ATTN...RFC...TIR...NWC...

    LAT...LON 40438600 40438459 40228421 39648397 39128462=20
    38388651 38438819 39668793 40078728=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 18 18:47:05 2026
    AWUS01 KWNH 181846
    FFGMPD
    MOZ000-KSZ000-NEZ000-190000-

    Mesoscale Precipitation Discussion 0185
    NWS Weather Prediction Center College Park MD
    246 PM EDT Mon May 18 2026

    Areas affected...Central and Northeast Kansas...Far Southeast
    Nebraska...

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

    Valid 181845Z - 190000Z

    SUMMARY...Severe Super-cells will have significant moisture flux
    convergence to support localized rates over 2"/hr. Given
    compromised upper soil conditions, localized flash flooding
    conditions are considered possible in proximity to other severe
    weather hazards.

    DISCUSSION...SPC MCD 771 solidly describes the mesoscale setup to
    produce strong updrafts and super-cell structures through the
    afternoon period. Strong updrafts supported by MLCAPEs in excess
    of 3500 J/kg; while driven by steep/dry lapse rates are also being
    fed in the surface to boundary layer by well above average
    moisture values (CIRA LPW values are at period of record
    [2013-present] maximum values for most of the area). Values in
    the .75-1" range confirmed by surface Tds of upper 60s to low 70s
    are being advected at greater than 20-25kts into the front.=20
    Surface low west of KCNK has backed the flow slightly to increase
    surface moisture convergence/flux to very strong values. Combined
    through depth and IVT values are well over 1000 kg/m/s per CW3E
    plots.

    Convective initiation is occurring near the surface wave and
    southward through the cold front to around KGRD. Strong SRH will
    allow for convective mode for super-cell structures, likely with
    broad updrafts/downdrafts and given slight right turning, should
    reduce forward cell motions increasing residency time.=20
    Additionally, the isallobaric influences will further accelerate
    inflow and moisture flux convergence to overcome modest overall
    deep moisture (~1.5 TPW, currently), but will steadily increase to
    support 2"/hr rates...with HRRR 15-minute rainfall totals forecast
    in excess of 1.25", eventually reaching 1.5"/15 minutes by 22-23z
    time frame.

    As they mature along the front and toward the northeast, some left
    splitters and general northeast cell motions may allow for some overlap/repeating...so spots of 2-3" totals are becoming possible
    through 00z across NE KS into SE NEB. Given the recent heavy
    rainfall in the area, the 0-40cm soils have become much further
    saturated ranging from 50% to near 75% in far SE NEB. As such,
    FFG values are reduced with 1hr values less than 1.5" across much
    of NE KS, SE NEB, SW IA and N MO; with a narrow axis across
    Ottawa to Ness county that saw over 5" in spots. Given the
    scattered nature of the super-cells initially (before sunset)
    localized flash flooding is considered possible.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4TUv9HX-IwzVxgy5IzlGLffafe0fsF8LSmJKdfQYgZTH-_6tDr1N8t9_1LVyyQU3DHZt= p-2MXNurHa_EnIBsqJVgni8$ for graphic product...

    ATTN...WFO...DDC...EAX...ICT...OAX...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 40559578 40119531 39249571 38679693 38309783=20
    38009886 38419904 39229789 39689744 40549667=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 18 20:56:51 2026
    AWUS01 KWNH 182056
    FFGMPD
    KYZ000-INZ000-ILZ000-MOZ000-190245-

    Mesoscale Precipitation Discussion 0186
    NWS Weather Prediction Center College Park MD
    455 PM EDT Mon May 18 2026

    Areas affected...Southern MO...Southern IL...Southern IND...Adj.
    Northwestern KY...

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

    Valid 182100Z - 190245Z

    SUMMARY...Continued over-running redevelopment within favorable repeating/training flow regime will continue potential for
    1.5-2"/hr rates and additional 2-3" streaks in proximity to areas
    currently flooding or approaching. As such, localized incidents
    of new or renewed flash flooding are likely through evening.

    DISCUSSION...Regional RADAR mosaic and 21z surface analysis
    denotes the main push of the squall line and stronger
    thunderstorms from the Lower Peninsula of MI across NW OH into far
    SE IND before the boundary orients more parallel to the deeper
    steering flow aloft and acts more of an outflow boundary and
    isentropic ascent surface from around KBAK, IND across IL passing
    KLWV to KMVN before passing KFAM, TBN across S MO and fading to
    the mean environment just north of KFSK in E KS. South of which
    broad south to southwesterly flow with unseasonably high (ten-year
    climo maximum, per CIRA LPW) low level moisture with Tds in the
    upper 60s to low 70s along the length. CIRA LPW notes that the
    surface to 850mb layer is very broad back into the central Plains,
    but the keep to the higher moisture flux occurs with the core of
    the 850-700 and 700-500mb layers over eastern AR through southern
    IL resulting in total PWats at or just above 2" across S IL with
    1.75" extending back through the Ozark plateau.

    While GOES-E WV suite shows the main shortwave/vorticity center
    exiting across the central Great Lakes (aiding forward propagating
    squall line across OH), there does remain favorable divergence
    aloft within the right entrance of the jet across N MO into a 90
    kt speed max across WI; which continues to drive the broad and
    generally confluent LLJ to maximize convergence along the upwind
    edge of the outflow boundary. RAP analysis still shows a source
    of 1500-2000 J/kg across the Ozark Plateau into S IL; though with
    some capping remaining. The convergence along the isentropic
    surface still aids scattered convective initiation and maintenance
    from south-central MO. This will continue to develop in the
    favorable ascent regime and with ample deep layer moisture should
    remain fairly effective with 1.75"/hr rates occasionally
    increasing to 2" with strongest updrafts.=20

    As noted above, the deep layer steering flow remains parallel to
    the ascent plane and only subtly south of the earlier axis of
    convective activity. The overlap with the saturated/actively
    flooding areas of southern MO into S IL and SW IND, have a solid
    potential of renewing localized flash flooding through the evening
    as the core of the warm conveyor belt and mid to upper-level
    forcing shift eastward. Streaks of additional 2-3" totals
    (isolated locally 4" psbl) may further expand the risk of inducing
    new incidents of flash flooding further south of the initial axis
    as well. This may also affect some flash flood prone urban
    centers along the Ohio River as well, if cold pool/outflow
    generation is stronger than currently forecast...so have included
    portions of NW KY and extended the MPD, though the band is more
    likely to remain north.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6ziynu1zP-SbFbJeBhzuOm8b99ld3T41fgdEgBimPymBpylSD-WI_iRpWyhKys-tLEkL= Ec09Rw21XThQARnG1TaKJSU$ for graphic product...

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

    ATTN...RFC...KRF...MSR...ORN...TIR...NWC...

    LAT...LON 39918552 39138483 38298507 37758607 37238839=20
    37059076 37249252 37589377 38139360 39039122=20
    39388880 39748743=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 18 23:02:34 2026
    AWUS01 KWNH 182302
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-190500-

    Mesoscale Precipitation Discussion 0187
    NWS Weather Prediction Center College Park MD
    701 PM EDT Mon May 18 2026

    Areas affected...Southwest IA...Southeast NEB...Northwest
    MO...Central & Northeast KS...

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

    Valid 182300Z - 190500Z

    SUMMARY...Strong moisture flux convergence will help to spur
    upscale growth from individual supercells to larger clusters with
    increasing rainfall potential and coverage. Rates of 2"/hr+ and
    localized totals of 2-4" (isolated 5"), especially across areas
    recently saturated are likely to result in increasing incidents of
    flash flooding.

    DISCUSSION...22z surface analysis and RADAR mosaic have changed
    very little over the last few hours though the dryline has surged
    out of the OK/TX panhandles and helped concentrate southerly moist
    flux to expand convective initiation well into south-central KS.=20
    Main clusters of supercells have are at bit more progressive out
    of southeast NEB with some eastward turning and increasing
    coverage and has started to move out of MPD 185 area of concern
    into SW IA and far NW MO. Additionally, the remainder of the
    cold front from the northern inflection E of Lincoln, NEB and
    secondary low near Salina, KS has filled in with broadening
    up/downdrafts; as such total PWats have increased along the cold
    front as the total column moistens with this increasing coverage.=20
    Tds in the 70s and sub-boundary layer LPW values near 1" along
    with 20-30kts of southerly flow continue to provide strong
    moisture flux to encourage increasing rainfall efficiency over the
    next few hours.

    GOES-E WV shows the upper level jet streak is currently rounding
    the base of the negative tilt up-level trof over the Northern
    Plains and as a result, upper level divergence pattern will
    further increase over the next few hours within strengthening DPVA
    and right entrance ascent patterns across the frontal zone. This
    should support further upscale growth of the cells toward clusters
    as we near sunset. Cold pool generation, right-turning
    supercells, should support further storm-scale interaction for
    more eastward propagation allowing some increased short-term
    training/repeating (as noted with clusters in NW MO already). As
    such localized streaks of 2-4" totals will become more likely.

    Across the MPD area a broadening/divergent of the 500-1000
    thickness fields suggests east to southeast forward propagation
    with time as well; increasing orthogonal flanking line
    intersection to expand back-building potential. This
    slowing/turning could be the greatest further south along the
    upstream edge near the nose of the dryline/cold front where
    steering flow is just a tad weaker overall aloft and support
    longer residency times. Of course, south-central KS will require
    this longer residency given the area has missed out on the
    complexes/heavy rainfall over the weekend.=20

    While severe/tornadic hazards remain the primary concern
    currently, this will transition toward flash flooding and given
    the majority of the area (north of 38.5N latitude) has FFG values
    at or below the hourly expected rates (1-1.75"/hr) and generally
    less than 2.5"/3hrs. As such, incidents of flash flooding will
    become more likely and with greater overall coverage. Hi-Res CAMs
    including the WoFS/HRRR continue to suggest very intense
    sub-hourly totals (1.5"/15 minutes per HRRR) and isolated totals
    of 5".=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_k5xgZhLf7L-8NSAQvbjntdQ-T2kymdmVNQgK1iHUxefJgzd01xOQfhfC0sU7QRxPWKj= oQ_Km8qG3G4MUsdaJdSyab0$ for graphic product...

    ATTN...WFO...DMX...EAX...ICT...OAX...TOP...

    ATTN...RFC...KRF...MSR...TUA...NWC...

    LAT...LON 41899371 41709307 41259253 40579249 40039284=20
    39029379 38049551 37489790 37969841 38759779=20
    40729682 41509594 41829502=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 19 05:02:34 2026
    AWUS01 KWNH 190502
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-191000-

    Mesoscale Precipitation Discussion 0188
    NWS Weather Prediction Center College Park MD
    101 AM EDT Tue May 19 2026

    Areas affected...northeastern OK into southeastern KS,
    southwestern/central MO and northwestern AR

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

    Valid 190457Z - 191000Z

    Summary...Isolated to widely scattered instances of flash flooding
    will be possible through 10Z from northeastern OK into
    southeastern KS, southwestern to central MO, and perhaps far
    northwestern AR. Hourly rainfall of 1 to 2 inches is expected, but
    values may locally exceed 2 inches.

    Discussion...04Z surface observations showed a cold front
    extending from northeastern KS into northwestern OK and the
    northern TX Panhandle, preceded by a line of thunderstorms which
    arced from central MO into southeastern KS. An outflow boundary
    was located at the leading edge of the thunderstorms with a faster
    southeast motion over MO as compared to KS, allowing convective
    line orientation to match that of the mean steering flow from the
    WSW, supporting training and hourly rain of 1 to 2+ inches. 04Z
    SPC mesoanalysis data showed 1000 J/kg MLCAPE in central MO,
    increasing to as much as 3000 J/kg MLCAPE in north-central OK,
    west of I-35, out ahead of the outflow boundary.

    A strong southerly low level jet was observed over central OK (65
    kt at 850 mb VAD wind plots from KTLX and KINX), veering and
    weakening slightly into MO. This orientation will favor the best
    angle (closest to orthogonal) into the southward sagging boundary
    over OK where continued convective development is likely as the
    front/outflow move south over the next few hours. The convective
    line orientation will support WNW to ENE training at times with 1
    to 2+ in/hr rainfall and possible flash flooding from an
    additional 2 to 4+ inches through 09Z. Flash flood potential will
    be increased should training overlap with urban locations or
    lowered flash flood guidance due to heavy rain over the past 24
    hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8v38Pb97uNhb3tglFBsnMhOOeYQ3jUBEHeJ3oyqH4BhmH5-qkqPHeGpRotGvamrnTi-D= mRp7SwVKYmhaEwVc6tg8Lpo$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...OUN...SGF...TOP...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38989302 38819179 37939125 37089184 36359389=20
    35899567 35629673 35779761 36699814 37629629=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 19 13:19:00 2026
    AWUS01 KWNH 191318
    FFGMPD
    MOZ000-ARZ000-OKZ000-191830-

    Mesoscale Precipitation Discussion 0189
    NWS Weather Prediction Center College Park MD
    917 AM EDT Tue May 19 2026

    Areas affected...Ozarks

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

    Valid 191317Z - 191830Z

    Summary...Scattered instances of flash flooding likely, with
    possible localized considerable impact, over the Ozarks rest of
    the morning. Hourly rainfall of 1 to 2 inches is expected to
    continue with 3 to 4 inches possible in three hours.

    Discussion...A cold front continues to push southeast toward the
    ozarks with prefrontal organized activity still with two distinct
    areas currently over northern AR and over eastern OK. The junction
    of these two MCSs caused 2-5" rainfall near the OK/MO border early
    this morning with rainfall rates of 1-2"/hr still occurring over
    southwest MO and northern AR. An MCV is likely to develop in the
    left bookend from the OK MCS that generally works its way east
    along the MO/AR border rest of the morning. SWly low level flow is
    parallel to the outflow from eastern OK which should allow for an
    additional round of heavy rainfall. This area is quite dry with
    high flash flood guidance, but the Ozarks are a known flash flood
    prone area with the terrain and high runoff, so there are concerns
    for considerable impacts from 2-4" in a few hours.

    1500 J/kg MLCAPE and 1.8" PW with SWly flow of 20-25kt is
    sufficient to support repeating heavy thunderstorms along over
    much of the Ozarks rest of this morning. Recent HRRR and RRFS runs
    appear to be under analyzing the left bookend/MCV development
    risk. Those models place greater QPF focus over southeastern OK
    where activity is currently progressive.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9p7M17PwHANKTj4SqP95rmq8I3uH44ydydOuRRCmXMKTbHDF8N_9un3S5Eb-JGq8UVIP= DDi480Aqeu3o705JM5j-9E0$ for graphic product...

    ATTN...WFO...LZK...SGF...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 36919319 36699203 36449141 35449183 35079313=20
    35239454 35969486 36529458 36899422=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 19 14:09:04 2026
    AWUS01 KWNH 191409
    FFGMPD
    ARZ000-TXZ000-OKZ000-191930-

    Mesoscale Precipitation Discussion 0190
    NWS Weather Prediction Center College Park MD
    1008 AM EDT Tue May 19 2026

    Areas affected...Southeast Oklahoma and Northeast Texas into
    Arkansas

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

    Valid 191407Z - 191930Z

    Summary...Isolated flash flooding possible over southeast Oklahoma
    into northeast Texas and southwest Arkansas through the early
    afternoon. Slowing progression of organized thunderstorms should
    allow hourly rainfall of 1 to 3 inches with up to 4 inches
    possible in three hours over this previously parched area.

    Discussion...Prefrontal organized activity over southeast OK is
    oriented parallel to the southwesterly low level flow. This has
    caused a slowing to progression and longer duration of heavy rain
    over east-central OK. Continued new development merging in with
    this line will allow a flash flood threat to shift to northeast TX
    through midday. MLCAPE of 3000 J/kg and PW of 1.6 inches will
    maintain rapid development and heavy rainfall rates of 2 to
    possibly 3 inches per hour. This area has been dry for the past
    week, so flash flood guidance is quite high. Flash flooding should
    be restricted to the areas with the highest rainfall and in
    urbanized areas that get at least a few inches. Recent RRFS runs
    have been heavier than the HRRR which seem reasonble as the HRRRs
    have been underdoing current activity. Areas ahead of the cold
    front will continue to be monitored given the unstable and moist
    environment.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9xGuIJ2sMD90LaTgorzLktrKt6RVD1OvJZUQlQ2LZ3QMW6ZLHSY1HiM57fhH0FwvvcMQ= J3do1pGPsLfu2EoXT0jejaQ$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35429542 35409467 35079390 34609344 33679353=20
    32479558 32549776 33609832 34629744 35189636=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 19 17:50:32 2026
    AWUS01 KWNH 191750
    FFGMPD
    TXZ000-192330-

    Mesoscale Precipitation Discussion 0191
    NWS Weather Prediction Center College Park MD
    149 PM EDT Tue May 19 2026

    Areas affected...Central Texas and Concho Valley

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

    Valid 191748Z - 192330Z

    Summary...Additional instances of isolated flash flooding possible
    over northwest Texas/the Concho Valley into Central Texas through
    the afternoon. Thunderstorms developing along/just behind a cold
    front should continue to produce hourly rainfall of 1 to 2.5
    inches with up to 4 inches possible in three hours over this
    previously parched area.

    Discussion...Frontal activity has rapidly redeveloped along/behind
    a cold front near San Angelo. Earlier activity west of Abilene
    became stationary as low level flow fed it, allowing 3-4 inch
    maxima. The newer activity is more scattered in nature, but given
    the abundant instability (MLCAPE of 3500 J/kg) and moisture
    pooling along the front (1.4 to 1.6 inch PW from west to east in
    the drawn threat area) should continue to rapidly develop and
    could congeal into a more organized cluster in the lower shear
    environment (20-25kt effective shear).=20

    The HRRR continues to struggle with convection today with
    difficulty maintaining this central/NW Texas activity while the
    RRFS has a better handle on reality and seems reasonable with
    scattered output of 1.5 to 4 inches through 00Z across central and
    western portions of the drawn threat area.

    All of southern Plains have been dry for the past week which may
    allow increased runoff depending on the local soil type. Flash
    flood guidance is high, generally 2.5 inches per hour, so the
    flash flood risk should remain isolated through the afternoon.
    Activity should continue to shift south with the cold front, so
    followup discussions should be south of this area.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9PuE01FVqLsWcYrZKj-3Sno7EK4KS0V6esu-LmVasF3gtUITxSn883ddFDcg9iOhI5wo= FIJoNaGc1EdtBlFkLupiYf4$ for graphic product...

    ATTN...WFO...EWX...FWD...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32899797 32599726 31739728 31009795 30739923=20
    30600018 30800175 31470179 31830151 31910036=20
    32279940 32629863=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 19 19:43:43 2026
    AWUS01 KWNH 191943
    FFGMPD
    LAZ000-ARZ000-TXZ000-OKZ000-200141-

    Mesoscale Precipitation Discussion 0192
    NWS Weather Prediction Center College Park MD
    342 PM EDT Tue May 19 2026

    Areas affected...north/northeast Texas, southwestern Arkansas,
    northern Louisiana

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

    Valid 191941Z - 200141Z

    Summary...A slow-moving complex of thunderstorms will continue to
    produce local areas of 1-2 inch/hr rain rates. Isolated flash
    flood issues are possible -- especially in low-lying and urban
    areas -- through 0130Z/830p central.

    Discussion...A mature, linear convective complex was making slow
    southward movement across north/northeast Texas and the ArkLaTex
    region over the past hour. The slow movement was occurring due to
    weak steering flow aloft, slow propagation and expansion of a cold
    pool upstream of convection, and continued, renewed updrafts along
    the leading edge of the gust front. The airmass downstream of the
    complex was strongly unstable (2000-2500 J/kg MLCAPE) and weakly
    inhibited (negligible cap). These factors, along with the
    presence of a weak mid-level wave over east Texas, should continue
    to support scattered convection along and ahead of the complex for
    the next several hours.

    Slow movement and propagation has led to areas of 1-1.5 inch/hr
    rain rates at times, with isolated 2 inch/hr spots near the most
    persistent convection. This is generally lower that FFG
    thresholds areawide, suggesting that any flash flood threat should
    be tied to sensitive/urban terrain and mostly isolated in nature.=20
    Occasional cell mergers should result in brief local peaks in rain
    rates - especially with continued heating and ascent from the
    mid-level wave near the region. Convection should reach the I-20
    corridor in northeast Texas/north Louisiana over the next 2-4
    hours (2130-2330Z).

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6ZAPFXnApdZj3yMlqvhhFcxkPa9cb9xwebc8N5Na5H78oEIPaHL-l6yDCZshhF3Guwzh= gGVamI0QoX0NCvIdA6kdbqU$ for graphic product...

    ATTN...WFO...FWD...HGX...JAN...LCH...LZK...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35059191 33339167 32279193 31719240 30909412=20
    30699712 32089801 33139811 33669680 33679670=20
    34009564 34329428 34959291=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 19 23:32:12 2026
    AWUS01 KWNH 192332
    FFGMPD
    TXZ000-200530-

    Mesoscale Precipitation Discussion 0193
    NWS Weather Prediction Center College Park MD
    731 PM EDT Tue May 19 2026

    Areas affected...portions of west and central Texas

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

    Valid 192330Z - 200530Z

    Summary...Slow-moving thunderstorms continue to produce high rain
    rates - locally exceeding 2 inches/hr at times. Flash flooding is
    likely on at least a localized basis.

    Discussion...In the last half hour, an east-west oriented band of
    cellular convection has intensified rapidly along an axis from
    near Big Lake, TX east to near Llano, with other scattered
    convection northeast of that axis (west of Waco) and also just
    north of the Big Bend area. These storms were focusing along a
    very slow-moving cold front in that vicinity. Furthermore, very
    strong mid-level lapse rates (exceeding 8C/km) and near 70F
    dewpoints were contributing to 3000-4000 J/kg MLCAPE, further
    supporting strong updrafts. Weak steering flow was evident (only
    20 knots or so at 500mb), enabling convection to exhibit slow and
    at times erratic storm motions. Moisture/instability profiles
    were supporting local 2-2.5 inch/hr rain rates that were
    approaching FFG.

    Overall increasing convective trends are likely to continue amid a
    subtle increase in low-level flow into the aforementioned front
    through the evening hours. Slow/erratic storm motions are likely
    to continue with this activity, though upscale growth into a
    convective complex appears probable as cold pools mature and
    merge. Models hint at additional convection emanating from
    northern Mexican higher terrain that may also organize and merge
    with pre-existing convection across the discussion area and pose a
    flash flood risk. Areas of 2-3 inch/hr rain rates are likely to
    continue on at least a localized basis, posing a flash flood
    threat especially in sensitive locales. 5 inch totals are also
    possible. This threat is likely to continue through 05Z/midnight
    central time, and a gradual eastward and/or southeastward shift in
    flash flood potential should materialize, though this evolution is
    likely highly dependent on how quickly storms can grow upscale
    during the evening. Locally significant impacts are possible in sensitive/flood-prone areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5BnUTs18pNt79v1mrxFp1RI9sJob9cGID-yuhkGXdQhZExVWaWBLtEObLxJzhPJ7HSxo= 0ybwYKM-wB9jz9wB3vZCJJQ$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32169913 32029761 31589676 31199632 30409619=20
    29599647 28919807 28499958 28340015 29080082=20
    29660173 29460284 29830317 30790276 31910120=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 19 23:55:48 2026
    AWUS01 KWNH 192355
    FFGMPD
    OHZ000-KYZ000-INZ000-ILZ000-200353-

    Mesoscale Precipitation Discussion 0194
    NWS Weather Prediction Center College Park MD
    754 PM EDT Tue May 19 2026

    Areas affected...southern Indiana, southwestern Ohio, northern
    Kentucky

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

    Valid 192353Z - 200353Z

    Summary...Scattered thunderstorms were exhibiting localized
    training, with rates increasing to about 1 inch/hr on a localized
    basis. Isolated instances of flash flooding are possible.

    Discussion...Scattered thunderstorms were migrating eastward at a
    decent pace across the discussion area this afternoon (~30 knots).
    Storms in Ohio were organized into forward-propagating bands,
    though upstream areas over Indiana into southwestern Ohio were
    exhibiting slightly more favorable orientation for local training.
    The convective orientation was favoring areas 1 inch/hr rain
    rates on an isolated/spotty basis across the region, which was
    approaching rather low FFG thresholds across the region due to wet
    soils from prior rainfall the past few days.

    Current trends suggest that an isolated flash flood risk will
    exist for at least another couple hours. 1500-2000 J/kg MLCAPE
    values and 1.9 inch PW values should sustain thunderstorms with
    efficient rainfall rates at times through sunset. Thereafter, the
    combination of surface cooling, convective overturning, and an
    approaching front from the west should lead in a downtick in
    convective coverage and attendant flash flood potential. Peak
    risk will exist from now through around 03Z/11p eastern or so.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7Xq3kNuwUw8o0r4ib0YG7-HzIp87oQ6zkIH3E170SVZlDdZOcThaeQRxDGk7Pch8VxLH= c9LukOjbCkNkimrj4qU6JoQ$ for graphic product...

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

    ATTN...RFC...TIR...NWC...

    LAT...LON 40188453 40048307 39338280 38688362 38318491=20
    38128631 38118760 38638758 39088725 39628635=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 20 04:15:39 2026
    AWUS01 KWNH 200415
    FFGMPD
    MSZ000-LAZ000-200815-

    Mesoscale Precipitation Discussion 0195
    NWS Weather Prediction Center College Park MD
    1214 AM EDT Wed May 20 2026

    Areas affected...southwestern to central MS

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

    Valid 200413Z - 200815Z

    Summary...Brief training of heavy rain may allow for localized
    hourly rainfall of 2 to 3+ inches from southwestern to central MS
    over the next 2-4 hours. Localized flash flooding may result,
    especially if overlap occurs within urban centers along I-55 from
    Jackson to McComb.

    Discussion...04Z radar imagery and surface observations showed a
    NNE to SSW oriented line of thunderstorms moving east from western
    MS along an outflow boundary. The environment was quite moist and
    unstable with PWs between 1.8 and 2.1 inches along with 500-1500
    J/kg MLCAPE as seen in the 00Z JAN sounding and 03Z SPC
    mesoanalysis. The outflow boundary is expected to continue to
    slowly but steadily move east over the next couple of hours but
    recent development out ahead of the outflow in southwestern MS
    near the LA border may support localized higher hourly rainfall
    values aided by short term training. Where training sets up, the
    environment supports the potential for 2 to 3+ inches of rain in
    an hour and totals near 4 inches. Given the fairly high flash
    flood guidance, this threat should likely be more urban in nature
    or within other poorly draining locations.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-QXuIH5NQ7qC8QriiroSiKSFLqL9MVHxJJMa0lcAkNUWJ9_F09jgH9rSzliX55m3S2oQ= MQrZB7FhEs7A6R-qY8RGglg$ for graphic product...

    ATTN...WFO...JAN...LIX...

    ATTN...RFC...ORN...NWC...

    LAT...LON 33398994 33018939 31359022 30949071 31019132=20
    31449136 32039098 32769069=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 20 05:52:23 2026
    AWUS01 KWNH 200552
    FFGMPD
    TXZ000-201150-

    Mesoscale Precipitation Discussion 0196
    NWS Weather Prediction Center College Park MD
    151 AM EDT Wed May 20 2026

    Areas affected...south-central TX to middle TX coast

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

    Valid 200550Z - 201150Z

    SUMMARY...Over the next 3-6 hours, localized flash flooding will
    be possible over south-central TX to the middle TX coast due to
    high rainfall rates locally exceeding 2 to 3 in/hr at times and
    isolated storm total rainfall over 5 inches possible.

    DISCUSSION...0515Z radar imagery showed a roughly west-east
    oriented line of thunderstorms stretching from Kinney County to
    Brazoria County. These storms were located along a composite
    outflow boundary, sinking south, with an inflection point over
    Colorado County due to prior merging of two outflow boundaries. An
    northern bookend vortex/MCV feature, currently over Burleson
    County, has been associated with some of the highest rainfall
    rates with this complex. It is with this feature where
    MRMS-derived rates had been 2 to 3+ inches per hour for a few
    hours and local Wunderground sites near I-35 reported closer to 4
    inches in an hour between 00-02Z.

    High rain rates tied to the east-southeastward tracking MCV
    feature over Burleson County are expected to wane over time as it
    becomes further displaced from the better instability to the
    south. Going forward, the outflow boundary is forecast to continue
    dropping south with time into moderately strong MLCAPE of
    2000-4000 J/kg and PWs of 1.8 to 2.1 inches via 05Z SPC
    mesoanalysis data. While the outflow's exact motion remains
    uncertain, given the convective line's orientation is not a
    straight line, links/bends and short-term training will be
    possible as it advances generally southward. 850-300 mb and 0-6 km
    mean layer winds are less than or equal to 15 kt which will be
    supportive of slow cell motions at times just behind or perhaps
    just ahead of the outflow should pre-"frontal" cells form within
    the highly unstable environment. Localized flash flooding may
    result, including over a stripe of higher soil moisture due to 2
    to 4+ inches of rain which fell early Tuesday morning from Aransas
    to Corpus Christi Bay and westward.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6NX8hoVVmHJU-AZsF_YmMKPPVpyjpk0FfS99gLoSzn9YcYOidzlE--Jokl8NxLX16CqJ= ZRKEOMx7aZ60_kwXpULy9ik$ for graphic product...

    ATTN...WFO...BRO...CRP...EWX...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30409616 30379581 29519542 29159485 28759501=20
    28239599 27799670 27359740 27339875 27679991=20
    28730064 28990033 29019972 29039796 29519692=20
    30009652 30259646=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 20 17:49:06 2026
    AWUS01 KWNH 201749
    FFGMPD
    TNZ000-MSZ000-LAZ000-202345-

    Mesoscale Precipitation Discussion 0197
    NWS Weather Prediction Center College Park MD
    148 PM EDT Wed May 20 2026

    Areas affected...Louisiana and Mississippi

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

    Valid 201746Z - 202345Z

    Summary...Slow moving and possibly training thunderstorms bring a
    risk for localized hourly rainfall of 2 to 3+ inches to southern
    Louisiana and much of Mississippi this afternoon. Localized flash
    flooding may result, especially between Lake Charles and New
    Orleans and up the I-55 corridor through Mississippi.

    Discussion...Regional radar and surface observations depict a
    surface trough extending east of an MCV off the Upper Texas Coast
    to New Orleans and a north-south oriented trough spanning most of
    western Mississippi. Convective storms have broken out along both
    troughs where ample moisture (PW of 1.8 to 2") and instability
    (SBCAPE >2500 J/kg) are pooled. Continued rapid development of
    this activity is expected through the early afternoon. SSWly low
    level flow over MS will allow activity to repeat, raising the risk
    of flash flooding, particularly for urban areas and places west of
    I-55 that saw a couple inches of rain last night. Convergence on
    the southern LA trough should continue as onshore flow feeds
    development. Sensitive urban areas in LA such as NOLA and Baton
    Rouge are most vulnerable in this case of generally scattered
    convective activity. Areas with repeating activity could see
    2-3"/hr rates which are generally under flash flood guidance,
    limiting the flash flood risk to the more sensitive areas and in
    the isolated precip maxima.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ASTQtt1muyCN5k79iHIg4pMxJPCQUX95r12_Be92R_2InwbAv7FgZP4eHWYpOZzpbol= 4ofWmz3iEXzBGpH3o08nqTc$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MEG...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 35088908 34968841 34868819 33548849 31508942=20
    30198954 29449052 29279240 30039318 30829161=20
    32249119 33739068 34399026 34688989 34978955=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 20 18:03:09 2026
    AWUS01 KWNH 201803
    FFGMPD
    TXZ000-202100-

    Mesoscale Precipitation Discussion 0198
    NWS Weather Prediction Center College Park MD
    201 PM EDT Wed May 20 2026

    Areas affected...portions of west Texas

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

    Valid 201800Z - 202100Z

    Summary...Isolated flash flooding is possible across west Texas
    for the next 2-3 hours.

    Discussion...Scattered, deep convection has developed along an
    axis from Brownfield (southwest of Lubbock) southward to Odessa.=20
    Storms were drifting northward at a decent clip (around 20-25
    knots or so), though localized backbuilding and the orientation of
    the convection was supporting local rain rates over 1 inch/hr just
    northwest of Midland. These storms are being forced by a weak
    shortwave trough approaching the area from the TransPecos,
    leveraging mid-level moisture, strong cloud-bearing shear, and
    steep (8C/km) mid-level lapse rates for organized convection.=20
    This regime will continue to support isolated flash flood
    potential over at least the next 2-3 hours.

    Evolution beyond this time frame is in question. The lead wave
    encouraging ongoing convection will continue to eject
    northeastward and may result in a brief lull in convection for a
    time. However, upstream shortwave energy (per objective analyses
    over far southern New Mexico and vicinity could reinvigorate
    convection over areas currently experiencing heavy rainfall
    through the afternoon/evening. The overall flash flood threat
    should remain isolated and tied to local sensitivities -
    especially with high FFG thresholds across the region. The flash
    flood risk will exist through 20Z, with reevaluation of convective
    trends for another MPD issuance expected at around that time.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4C7NE9tIU-QUtUTW5i2YUMqO2rQhqWa-h3q0sffIQklw1_wzqENlnh-hv1MNpZKkL3Bk= RcJLOn7242cmQc4AcpUURnc$ for graphic product...

    ATTN...WFO...AMA...EWX...LUB...MAF...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35130100 33840007 31690032 30260160 30650264=20
    33850292 34840238=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 20 19:18:17 2026
    AWUS01 KWNH 201918
    FFGMPD
    NJZ000-PAZ000-DEZ000-MDZ000-VAZ000-DCZ000-WVZ000-210016-

    Mesoscale Precipitation Discussion 0199
    NWS Weather Prediction Center College Park MD
    316 PM EDT Wed May 20 2026

    Areas affected...portions of Maryland, Pennsylvania, northern
    Virginia, and the District of Columbia

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

    Valid 201916Z - 210016Z

    Summary...Thunderstorms increasing across the Appalachians may
    eventually pose an isolated flash flood risk as they move toward
    the I-95 corridor through 00Z/8p eastern.

    Discussion...Scattered thunderstorms have increased in coverage
    across the higher terrain of the central/northern Appalachians
    (from near Harrisonburg, VA north to near Harrisburg, PA). These
    storms are in an environment with moderate instability (around
    1500 J/kg MLCAPE) and sufficient deep-layer shear for
    organization. Spots of 2 inch/hr rain rates were noted in central
    Pennsylvania per MRMS data, with lower rates elsewhere across the
    discussion area.

    On their current track, storms are expected to reach the urban
    I-95 corridor from Washington, DC to Philadelphia in the 21-23Z
    (5p-7p eastern) timeframe. Isolated areas of 1 inch/hr rain rates
    cannot be ruled out as these storms move through. The heavier
    rainfall potentially occurring over urban/sensitive terrain could
    cause isolated flash flood instances through 00Z/8p eastern.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6RAm82rpGm3cxlM3mDIKWA6QYfoKwiUWj9jpSucli408F2YovmVfkNIPpVsWhmo2FT7v= 3DL3oBq84tlsYQRTYbSEorE$ for graphic product...

    ATTN...WFO...BGM...CTP...LWX...PBZ...PHI...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 40917596 40467476 39357615 38717707 38607885=20
    39687902 40717818=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 21 01:10:23 2026
    AWUS01 KWNH 210110
    FFGMPD
    TXZ000-210708-

    Mesoscale Precipitation Discussion 0200
    NWS Weather Prediction Center College Park MD
    909 PM EDT Wed May 20 2026

    Areas affected...portions of western through central Texas

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

    Valid 210108Z - 210708Z

    Summary...Scattered thunderstorms are beginning to expand in
    coverage south of San Angelo. These storms may ultimately form a
    complex that spreads areas of 2 inch/hr rain rates across portions
    of the Hill Country overnight. Flash flooding is expected on at
    least an isolated basis.

    Discussion...Scattered thunderstorms are expanding in coverage
    along an axis from near Ozona to near Menard - or along and just
    north of I-10. The storms are associated with 1) a bowing complex
    that originated from higher terrain over the TransPecos and 2)
    along a remnant boundary/front from prior convection yesterday.=20
    Storms were generally migrating eastward, but embedded in an
    environment with steep lapse rates (downstream of an EML over far
    west Texas) and supported by ~1500 J/kg MLCAPE along and south of
    the aforementioned boundary.

    As storms mature in this environment, they'll likely become prone
    to multiple mergers and limited training over time as modest
    low-level flow increases and results in convergence along the
    aforementioned boundary. This will likely aid in spreading 2
    inch/hr rain rates eastward over portions of the Hill Country that
    received 2-4 inches of rain last night. Flash flooding is likely
    in at least a few areas. Flash flood concerns may increase
    substantially if storms can persist eastward toward the general
    vicinity of Llano and Round Rock/Austin Metro. Those areas are
    likely sensitive from previous rainfall and impacts that occurred
    overnight last night.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6RysrWNZrAtRfRsVAq51_PTE14ve3ls0mbMRp3Fqo1j90__HWnMKIdTrbMrG5tOUZhrX= kC8us5KBUbkve15dJQ8TJlo$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32199832 31839692 30559672 29509806 29530081=20
    29860259 30770177 31250156 31660110 31810011=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 21 02:29:31 2026
    AWUS01 KWNH 210229
    FFGMPD
    TXZ000-210815-

    Mesoscale Precipitation Discussion 0201
    NWS Weather Prediction Center College Park MD
    1028 PM EDT Wed May 20 2026

    Areas affected...Lower Rio Grande Valley/Deep South Texas...

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

    Valid 210230Z - 210815Z

    SUMMARY...Initial slow moving cluster capable of 2"+/hr rates
    should pre-wet the upper-soils as main line/wave emerges out of
    Mexico in the middle of the overnight period. Localized 2-4"
    totals, isolated 5" may result in isolated to widely scattered
    flash flooding.

    DISCUSSION...A very moist, conditionally unstable environment
    exists in the lower Rio Grande Valley with a solid pocket of 2500
    J/kg of uncapped MLCAPE remaining, given mid-80s temps over low
    70s Tds. CIRA LPW along with RAP analysis/short-term forecasts
    show enhanced low level moisture moving up the river valley with
    winds recently backing in response to the approaching upstream
    shortwave over the Big Bend exiting to the northeast and favorable
    upper-level divergence pattern starting to emerge from the Sierra
    Madre in E Coahuila into N Nuevo Leon. As such, recent
    directional convergence in this response has seen fairly vigorous
    convective initiation across Starr county and points across the
    river in Mexico. Low level inflow has a few hours of
    southeasterly moist/unstable inflow to maintain the cluster.=20
    Given 2" total PWats and weak (less than 20kts of flow), moisture
    loading and updraft vigor should support 2"/hr rates with
    localized uptick to 2.5" possible. Deep layer sheared flow with
    easterly flow in the low levels and weak confluent 700-500
    steering flow from south to north, should allow for tilted
    updrafts but slow moving to allow for increased residency. Spots
    of 2-3" are possible.=20=20

    The greater concern, is this cluster will continue to expand but
    slowly weaken as the upstream inflow reduces (note veering profile
    recently at KBRO/KCRP), but upper-level forcing via DPVA and
    divergence aloft from the increasingly diffluent upper level flow
    (right entrance over the Edwards Plateau) to provide favorable
    environment for convective clusters to advance/merger out of the
    Mexican highlands into the RGV generally timed after 06-07z. As
    such, an additional 2-3" totals should occur and with overlap,
    broader area of 2-4" with isolated 5"+ totals are possible.=20=20

    While the area is in drought and have naturally higher FFG values,
    urban centers and intense rates would be the main driver for
    possible incident or two of localize flash flooding through the
    overnight period.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-sh4wMMi0kORMHE6gk5OMyl1GOh6y0rZBNZeISXBo8akF9v-3Zb0_irRrQTyH4uoXs6x= UYYPHCE85x5faDYsXQoE0Uk$ for graphic product...

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

    ATTN...RFC...FWR...NWC...

    LAT...LON 27889940 27549859 27139807 26509780 26139780=20
    25989807 26229873 26429914 26979946 27539960=20
    27749979=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 21 11:20:33 2026
    AWUS01 KWNH 211120
    FFGMPD
    TXZ000-211419-

    Mesoscale Precipitation Discussion 0202
    NWS Weather Prediction Center College Park MD
    719 AM EDT Thu May 21 2026

    Areas affected...portions of the middle Texas Coast

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

    Valid 211119Z - 211419Z

    Summary...Areas of slow-moving, banded thunderstorm activity may
    produce local rain rates of 2-3.5 inches per hour this morning.=20
    Flash flooding is possible if this activity occurs over sensitive
    locales.

    Discussion...A mature MCS is making slow, steady progress along
    portions of the lower Texas Coast and south Texas - generally
    extending from near Corpus Christi southward to Brownsville. Slow
    movement (around 20 knots - locally slower) and abundant
    moisture/instability downstream over adjacent Gulf waters was
    aiding efficient precipitation rates (around 3 inches/hr) in the slowest-moving, northern end of the complex.

    Meanwhile, a new band has developed downstream of this complex
    near Port Lavaca. This band is oriented more parallel to steering
    flow aloft and perpendicular to the approaching complex from the
    west. 2+ inch/hr rain rates are already being estimated with this
    activity.

    Over the next 1-3 hours, the forward propagation of the mature MCS
    and slow-movement of the downstream convective band will promote a
    prolonged period of heavy rainfall especially along/near the
    middle Texas Coast. FFG thresholds of 2.5 inch/hr should be
    eclipsed with this activity, and local totals of 5+ inches cannot
    be ruled out through 14Z/9a central this morning. Flash flooding
    is possible - especially if these rainfall totals occur over any
    sensitive or low-lying/flood prone areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-TaqzPOzCrKt7UDQr6CNoE1rVSLFPXlqvLdXrSAS3wLtOXHa6Fl8YR0MaGcLyWZLuy80= jtx0p06eTw8IJ5YN6m9vNkc$ for graphic product...

    ATTN...WFO...CRP...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 29209606 29159493 28569474 28449491 28289597=20
    27999679 27399667 27369726 27739758 28459782=20
    28959718=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 21 17:06:44 2026
    AWUS01 KWNH 211706
    FFGMPD
    TXZ000-212304-

    Mesoscale Precipitation Discussion 0203
    NWS Weather Prediction Center College Park MD
    105 PM EDT Thu May 21 2026

    Areas affected...portions of west Texas

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

    Valid 211704Z - 212304Z

    Summary...Areas of flash flooding will remain possible within an
    axis generally extending from near Midland to near San Angelo and
    San Saba.

    Discussion...Scattered convection continues to focus along a
    subtle surface boundary in the general vicinity of Midland to San
    Angelo to near San Saba. Heating south of this boundary has
    enabled 1500-2000 J/kg MLCAPE to develop with minimal inhibition,
    supporting continued convection. Additionally, cool easterly
    low-level trajectories and continued rainfall along and north of
    the boundary was likely acting as a reinforcing mechanism to
    continue maintenance of the boundary and continued updrafts.=20
    Modest storm motions and backbuilding was supporting occasional
    areas of 1 inch/hr rain rates to materialize with the most
    persistent activity. These rain rates were approaching FFG
    thresholds (around 1.5 inch/hr) on a localized basis.

    Rainfall was occurring on ground conditions that are likely
    sensitive from prior rainfall over the region in the last 72 hours
    or so. Isolated instances of flash flooding cannot be completely
    ruled out in this regime. While the persistence of this
    convection regime is uncertain (and likely modulated by the
    persistence and movement of the low-level boundary spawning the
    convection across the region), models are generally consistent in
    maintaining thunderstorm activity through the afternoon amid
    southwesterly flow aloft. It is also worth noting that slightly
    lower FFGs (around 1 inch/hr) exists generally from San Angelo to
    Junction (just south of ongoing activity), which may represent a
    slightly higher flash flood threat if heavier rain rates
    materialize there.

    Cook=20

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!94vsFyB58N6FlZzS3GXISzDBy84vGqb5ZhF1S8tquMYOC8itHL1ft6nW4mxkhDzjjcA3= XEYMxHG7vD5Rrz7CUAOpJVc$ for graphic product...

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

    ATTN...RFC...FWR...NWC...

    LAT...LON 33150160 32850033 31789879 31049845 30359895=20
    30119970 30330071 31260172 32020240 32490268=20
    32830244=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 21 20:17:09 2026
    AWUS01 KWNH 212017
    FFGMPD
    TXZ000-OKZ000-KSZ000-220215-

    Mesoscale Precipitation Discussion 0205
    NWS Weather Prediction Center College Park MD
    416 PM EDT Thu May 21 2026

    Areas affected...portions of Oklahoma and western north Texas

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

    Valid 212015Z - 220215Z

    Summary...Slow-moving thunderstorms are producing isolated spots
    of rainfall rates approaching 2-3 inches/hr at times. Flash
    flooding is possible on an isolated basis through 02Z/9p central.

    Discussion...A complicated surface pattern exists across much of
    Oklahoma currently. Prior moderate to heavy rainfall has resulted
    in an expansive cold pool anchored across central Oklahoma as of
    20Z. On the southern and eastern peripheries of this cold pool,
    surface heating and subtle confluence along differential heating
    zones has led to scattered thunderstorm development. The
    pre-convective airmass supporting heavy rainfall is characterized
    by 500-1000 J/kg MLCAPE and 1.5+ inch PW values, while weak
    mid/upper steering flow has caused slow and at times erratic cell
    motions, further promoting heavy rainfall. As of 20Z, the
    heaviest rainfall was located near from the Wichita Mountains of
    southwest Oklahoma southward through western north Texas and also
    near McAllister and Okmulgee. FFG thresholds vary widely across
    the region, but are lowest from north-central Texas through
    eastern Oklahoma (around 1.5.2 inch/hr) and near 2.5 inch/hr
    elsewhere across the discussion area. These FFG thresholds were
    being exceeded on an isolated basis.

    Overall trends will continue for at least a few hours, with very
    slow/erratic movement and perhaps isolated upscale growth at
    times. It appears that convection across southwestern Oklahoma
    and western north Texas may prompt enough overturning with time to
    stabilize the low level airmass and lessen the flash flood risk,
    though this process may take some time to play out. Convection
    over eastern Oklahoma may have greater longevity with a broader
    pool of instability across that part of the state east of the
    aforementioned central Oklahoma cold pool. Flash flooding will be
    possible through 02Z/9p central.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9eem0gqBZ1QQPXCa5QlbilGhP1dPvi8_YngFOhgFdyjk_j9M5f3K7H8Pgoem8aPNb755= -BW6RSihhls-cmsIBnMPoCg$ for graphic product...

    ATTN...WFO...FWD...ICT...LUB...OUN...SHV...SJT...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 37109630 36959488 35519453 34049465 33359645=20
    32549786 32679963 33770046 34320034 34929972=20
    35189882 35149795 35349757 36069754 36799728=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 21 21:41:17 2026
    AWUS01 KWNH 212141
    FFGMPD
    TXZ000-220338-

    Mesoscale Precipitation Discussion 0206
    NWS Weather Prediction Center College Park MD
    539 PM EDT Thu May 21 2026

    Areas affected...portions of western and central Texas

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

    Valid 212138Z - 220338Z

    Summary...Thunderstorms continue to increase in coverage over
    sensitive areas from prior rainfall and terrain. Eventually,
    urban areas near Austin, San Antonio, and Waco may be impacted.=20
    Flash flooding is likely.

    Discussion...Over the past hour or so, thunderstorms have
    increased in intensity and coverage primarily across the Texas
    Hill Country. These storms are likely responding to a couple of
    changes in the thermodynamic environment: 1) heating of a moist
    airmass southeast of ongoing convection, 2) recharge of mid-level
    lapse rates from the EML originating over the southern Rockies,
    and 3) subtle shortwave troughs aloft forcing ascent and aiding in
    deep convective development. Weak low-level shear profiles
    suggest that cells will continue to grow upscale into short linear
    segments, but lingering boundaries from prior convection across
    the region will also allow for convective mergers to occur as
    well. The end result of this pattern will be continued
    development of areas of 1-2.5 inch/hr rain rates over sensitive
    regions from prior rainfall/wet soils, terrain, and eventually
    urban surface in the Austin/San Antonio/I-35 vicinity. Given
    ongoing trends, a greater likelihood of flash flooding exists,
    with locally significant impacts possible.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7N3Zlz5LwXvP2OWRSWQUuLF_b-5pSjapIbqCSdDzSWjCC9xgy7gjbjJT2egs9tm716TJ= m5IobS1V_2a7P3881PHwdoA$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32449676 31559583 29859604 28969855 29340094=20
    30300207 31280174 31420055 31749905 32319814=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 22 05:46:43 2026
    AWUS01 KWNH 220546
    FFGMPD
    TNZ000-MSZ000-LAZ000-ARZ000-221100-

    Mesoscale Precipitation Discussion 0207
    NWS Weather Prediction Center College Park MD
    145 AM EDT Fri May 22 2026

    Areas affected...Lower Mississippi Valley...

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

    Valid 220545Z - 221100Z

    SUMMARY...Slow, efficient warm cloud rainfall with
    training/repeating profile suggest localized 2-4" totals, with a
    secondary maximum near deep layer cyclone pivot and downshear axis
    across S Arkansas into N Mississippi.

    DISCUSSION...GOES-E WV suite depicts a well defined mid-level
    shortwave vorticity center across NE TX sliding northeast within
    the broader southeast edge of the larger scale broad upper-level
    trough. This provides deep layer DPVA and broad scale ascent with
    the entrance to the upper level jet streak over the mid-MS River
    Valley into the Great Lakes. At the surface, a weak surface wave
    in central LA remains a bit south of a stronger 850-700mb low
    along the AR/LA border, with a confluent surface to boundary layer
    LLJ/warm conveyor belt surging moisture north through the MS river
    and then bending back westward to the mid-level cyclone in the
    TROWAL. This provides broad moisture flux convergence through the
    area of concern; concurrent with bringing higher theta-E air into
    the ascent region. Narrow-skinny profiles with solid surface heat
    remaining provide a wedge of 500-1000 J/kg of uncapped MLCAPE
    generally to the surface boundary with MUCAPE extending downstream
    along the eastern branch of the TROWAL with 750-1000 J/kg into NE
    MS.

    The solid moisture confluence/convergence has broken out slow
    moving scattered convection through portions of E LA/SW MS; with
    slow motions and deeply saturated low level warm cloud processes
    providing tropical shower efficiency supporting 2 to occasionally
    2.5"/hr localized totals. Deep south-southwest steering to the
    northeast will be slightly deflected eastward given surface backed
    wind flow but given density of convective ascent pattern remains
    solid will increase potential for repeating to support up to
    focused 4" totals over the next few hours. Secondary maximum will
    exist where 850mb flow rapidly backs from south/southwest to more southeast/east north of the boundary in the deformation zone that
    generally parallels the front (though distance reduces further
    east into S MS...steepening the isentropic ascent boundary). FFG
    values are a tad lower within the MS River Valley (with 1hr spots
    of 1-2"/hr and 3hr values of 2-3") suggesting a localize flash
    flooding incident or two remains possible.

    Additionally, downshear of the 850-700mb low, strong dynamic
    ascent of the moisture flux into the western branch of the TROWAL;
    has resulted in broad moderate rainfall, though there is very
    limited instability that had not been worked over earlier this
    evening. Still the dynamic strength combined with the high
    moisture flux convergence should allow for increased duration for
    some localized spots of 2-3"; this still may not reach higher FFG
    in the area and may be more beneficial than resulting in flooding;
    but the duration/efficiency could still pose localized concerns
    enough to be included in the MPD area of concern through the
    overnight period. All in all,

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6l8mB3m1mE34re-D5fPCgZzWvEit8IqqEwkaaV17iTCTz5h3r-pYqvgVLYQ0kZfErjPx= QmZ6MJgCbbIoHH5p70ZPYv0$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...LZK...MEG...SHV...

    ATTN...RFC...ALR...ORN...TUA...NWC...

    LAT...LON 35138857 34738816 33868836 31688996 30979054=20
    30359136 30359208 30819238 32139206 32759223=20
    32859272 33229319 33849303 34289215 34709105=20
    35018966=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 22 08:27:32 2026
    AWUS01 KWNH 220827
    FFGMPD
    FLZ000-ALZ000-MSZ000-221230-

    Mesoscale Precipitation Discussion 0208
    NWS Weather Prediction Center College Park MD
    426 AM EDT Fri May 22 2026

    Areas affected...Coastal Mississippi and Alabama...

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

    Valid 220830Z - 221230Z

    SUMMARY...Effectively stationary/back-building Gulf streamers may
    result in localized very high totals and rapid inundation flooding
    remains possible through early morning.

    DISCUSSION...08z surface analysis, RAP analysis and sea-surface
    state from satellite, denote a core enhanced pocket of higher
    theta-E near surface pool resulting in near surface Tds in the
    upper 70s east of 90E from the coasts of MS/AL southward for a few
    hundred miles, generally within a area of confluent surface to
    850mb flow as return south-easterlies around the N FL ridging
    turns northward to intersect the south to southwesterly veered
    flow influenced from the approaching deeper layer trough across
    the Plains. While the core of the warm conveyor belt appears to
    be shifted to the west responding from the approaching
    height-falls; the surface regime is coming together near the
    frictional convergence zone of the near shore/beaches. The core
    of the SBCAPE axis of 4000-4500 J/kg is nosed to the MS beaches as
    well. As such, confluent Gulf streamers have lead to early
    morning convection focused on Mobile Bay and lingering affects of
    the pre-frontal trof convection that dominated the Pearl River
    Region yesterday.=20

    While shallow, the deep layer flow is favorably oriented to
    maintain the frictional convergence to support back-building that
    will help to repeat in this localized focused axes. Total PWats
    of 2", mainly loaded below 850mb (as noted in CIRA LPW above) with
    values around 1" should allow for deep warm-cloud rainfall
    generation processes and rain rates of 2.5"/hr. Already spots
    have seen greater than 2.5" and an additional hour or so will
    quickly result in rapid inundation. Proximity to urban centers
    along the beach and I-10 would be at greatest potential for these
    localize rapid inundation flooding events.=20

    Hi-Res CAMs suggest, a slight disruption to the surface flow to
    veer and reduce convergence at the surface shifting back west, but
    with time, the core of the Warm Conveyor Belt will also shift,
    especially given the instability axis remains upstream. So
    additional thunderstorm activity is probable and may maintain risk
    for localized inundation flooding through dusk.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5jt0nmx25bssA4QeIByEpASVgzJN1n2i8u4j7b7aXmhq1PPgUp4GNKhfv772pqBiSVk0= PrXDR3J5Wa8uzv9PxXayAEE$ for graphic product...

    ATTN...WFO...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 31928789 31768733 31438714 31058717 30628740=20
    30248771 30158788 30168851 30228948 30918911=20
    31268888 31818829=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 22 09:29:37 2026
    AWUS01 KWNH 220929
    FFGMPD
    OKZ000-KSZ000-221400-

    Mesoscale Precipitation Discussion 0209
    NWS Weather Prediction Center College Park MD
    528 AM EDT Fri May 22 2026

    Areas affected...Eastern Oklahoma... Adj SE KS....

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

    Valid 220930Z - 221400Z

    SUMMARY...Mid-level convergence in TROWAL resulting in very slow moving/stationary elevated cells with 1.5"/hr rates. Localized
    totals of 2" already with additional 1-2" possible may continue in
    localized flash flooding.

    DISCUSSION...Interesting deep layer dynamics environment with
    moisture entrapment and weak instability to result in a narrow
    band of heavy rainfall across eastern Oklahoma. GOES-E WV suite
    depicts an elongated vorticity/shortwave center over Texarkana
    moving northeastward with solid broad entrance region divergence
    across E OK and AR and through the Ozark Plateau. RAP analysis
    and VWP shows the western branch of the TROWAL is snaking from the
    main LLJ over the MS river Valley, ascending over the front
    westward through central AR before reaching an 850-700 convergence
    boundary veering more north to south to enter the jet streak
    aloft. CIRA LPW shows the enhanced core along this path with
    total PWat values of 1.75" at in SE OK reducing to 1.5" toward SE
    KS. Modest mid-level lapse rates support 500-750 J/kg of MUCAPE
    through the 800-600mb layer and given moisture flux convergence
    maximized at the base of that layer, convection has been weak but
    sufficient for modest rainfall rates up to 1.5"/hr.=20

    The slow/reducing forward propagation/deep layer steering has
    further enhanced localized flash flooding potential given
    increased residency time. Combine this with an axis of reduced
    FFG values across the area of concern (especially in Tulsa Metro
    area but even as far south as Pittsburg county) being about
    1.5-2"/hr and generally less than 2.5"/3hrs; localized exceedance
    remains possible through the late overnight period.=20

    Eventually, winds further slacken as the DPVA from the shortwave
    lifts further northeast into central AR and helps to sever the
    remaining TROWAL; winds veer further to the west and should result
    in a more widely scattered ascent pattern before weakening into
    the early morning hours. Spots of 2"+ have already fallen across
    the Pittsburg to Nowata county line with more scattered isolated
    cells further south. MRMS Flash responses of greater than 400-600
    cfs/sqmi have been noted in a few spots, especially in the urban
    center near Tulsa. With an additional 1-2" totals, spots of
    2-3.5" are probable and localized flash flooding will continue to
    be possible through 13-14z.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4mlU_8DMbMaEU2XsJSjLePocjxD_pRnGR6SO06SQWe3eQhtO3n8hm22wTUZigLMwWVit= nxLT3KZVXZutqUwPIER0ZAc$ for graphic product...

    ATTN...WFO...ICT...OUN...TSA...

    ATTN...RFC...TUA...NWC...

    LAT...LON 37269558 37019512 36279519 35549510 35229492=20
    34869488 34639496 34479544 34769607 35559637=20
    36469634 36959606=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 22 15:20:12 2026
    AWUS01 KWNH 221520
    FFGMPD
    FLZ000-ALZ000-MSZ000-222115-

    Mesoscale Precipitation Discussion 0210
    NWS Weather Prediction Center College Park MD
    1118 AM EDT Fri May 22 2026

    Areas affected...Southeast MS...Southwest to Central AL

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

    Valid 221518Z - 222115Z

    SUMMARY...Locally backbuilding and training convection are
    expected to pose an increasing flash flood threat through the
    afternoon. Rainfall rates of 2 to 3 inches/hour are expected, with
    localized totals of 4 to 6 inches possible by mid-afternoon.

    DISCUSSION...The regional environment is becoming increasingly
    favorable for high-efficiency rainfall production. A 30 to 35 kt
    southwesterly low-level jet is providing robust moisture transport
    and low-level convergence along a quasi-stationary surface trough
    situated from southeast MS through west-central AL. Precipitable
    water values are currently pooling between 1.75 and 2.0 inches,
    which is generally near or above the 90th percentile of
    climatology for late May.

    The 12Z morning KBMX sounding and recent RAP analysis confirm a
    tropical-like thermodynamic profile with a deep warm cloud layer
    exceeding 12,000 ft. This environment will support efficient
    warm-rain physical processes, allowing convective cores to sustain
    potentially extreme rainfall rates even with moderate instability.

    MLCAPE values of 1500 to 2500 J/kg are nosing up along and just
    east of the surface trough axis, and will support not only the
    high rates, but also a general expansion of convection over the
    next few hours as shortwave energy arrives from the southwest.
    This will generally involve southeast MS through portions of
    central and southwest AL for the main threat area.

    Kinematically, the environment is primed for convective training.
    Corfidi propagation vectors are largely offsetting the mean
    steering flow, suggesting that cell development will tend to favor
    at some backbuilding along and just ahead of the low-level
    convergence axis. Hourly rainfall rates of 2 to 3 inches are
    expected within the most persistent cores.

    The antecedent conditions are generally rather moist based off the
    latest NASA SPoRT-LIS soil moisture analysis, and the latest USGS
    streamflow data shows somewhat elevated baseflows from recent
    precipitation. These antecedent conditions will lead to high
    runoff efficiency and potential rapid responses in small creeks
    and urban drainage systems.

    The latest hires CAM guidance suggests some localized rainfall
    totals reaching 4 to 6 inches by mid-afternoon, and this will
    likely result in some ares of flash flooding which may be locally
    enhanced over the more sensitive urban corridors.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Yb6DLWS_OSuo2U9mN0tNWik0R_qkLixek2AhTT-J5G6Vs2mToBqlpN6Sv2heFvQPl_x= JLpGBnTgAfBzmnm2cofKwWw$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 33978649 33148629 31888665 30638735 30208792=20
    30188888 30668911 32488827 33488790 33968734=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 22 18:40:42 2026
    AWUS01 KWNH 221840
    FFGMPD
    GAZ000-TNZ000-ALZ000-222300-

    Mesoscale Precipitation Discussion 0211
    NWS Weather Prediction Center College Park MD
    239 PM EDT Fri May 22 2026

    Areas affected...Portions of Northern AL and Middle TN

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

    Valid 221839Z - 222300Z

    SUMMARY...Northward-moving convection will pose a localized flash
    flood threat through the afternoon and early evening. Rainfall
    rates of 1.0 to 1.5 inch/hour are expected, with localized totals
    of 2 to 3 inches possible where training occurs.

    DISCUSSION...Convection currently over central Alabama is expected
    to continue lifting north-northeastward into an environment
    characterized by PWAT values of 1.6 to 1.8 inches and moderate
    instability with MLCAPE values of near 1500 J/kg. While the
    overall thermodynamic environment is less efficient than areas to
    the south, a 30 kt low-level jet will continue to provide
    sufficient moisture transport to support locally heavy rain rates.

    The primary concern is the potential for localized cell-training
    or backbuilding along the nose of the low-level jet. While
    individual cells will be somewhat progressive, Corfidi vectors
    suggest a component of the flow may allow for repeated rounds of
    heavy rain over the same basins. Recent model guidance, including
    the REFS ensemble, indicates a 20 to 30 percent probability of
    exceeding flash flood guidance in localized areas, with some 2 to
    3 inch rainfall totals possible by early this evening.

    Given that soils are fairly moist across at least portions of
    northern AL and middle TN, the rainfall over the next few hours
    should favor at least an isolated threat for flash flooding. This
    will tend to be mainly an urban threat, but with some of the
    elevated terrain across the region, there may be some locally
    enhanced and channeled runoff potential for some of the small
    stream basins where any cell-training occurs.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5YJ7loOgBZcnIQxZOAUAtqGMVNQChjqtRYJVgkUMaZ09tsj4WCWqxhw5pLeMgMvbxuid= XgFZ3QIlR8_RTBfGQq2AmO8$ for graphic product...

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

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 35608577 35518554 35228545 34698560 34228584=20
    34008621 33938653 34068678 34598678 35318646=20
    35528615=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 22 20:24:28 2026
    AWUS01 KWNH 222024
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-230222-

    Mesoscale Precipitation Discussion 0212
    NWS Weather Prediction Center College Park MD
    423 PM EDT Fri May 22 2026

    Areas affected...southeastern Louisiana, southeastern Mississippi,
    southern Alabama, and the western Florida Panhandle

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

    Valid 222022Z - 230222Z

    Summary...Areas of thunderstorms continue to expand in coverage
    and intensity across the discussion area. Rain rates are likely
    to cause flash flood issues on at least an isolated basis.

    Discussion...Deep convection has intensified and expanded in
    coverage over the past hour - especially across southeastern
    Louisiana and southeastern Mississippi. The storms are in a very
    unstable airmass (80s F surface temps/mid-70s F dewpoints
    supporting 2500 J/kg MLCAPE). Meanwhile, broadly confluent,
    southwesterly low-level flow and weak inhibition was supporting
    updrafts. Convection was oriented parallel to southwesterly
    steering flow aloft, supporting localized training. Areas of
    1-1.5 inch/hr rain rates were noted per MRMS imagery recently.

    The storms were migrating over areas of relatively low FFG from
    prior rainfall (approx 2 inch/hr thresholds in spots across SE
    LA/SE MS, locally lower in southern AL). As cells migrate over
    these regions of abundantly moist soils (and urban population
    centers like New Orleans and Mobile), some risk of flash flooding
    will likely arise. Convection (and flash flood risk) is likely to
    be diurnally driven and weaken some shortly after sunset. The
    eastern extent of flash flood risk from SE LA/SE MS convection is
    in question, with widespread convective overturning across
    portions of south-central Alabama has lessened instability values
    there, and convection may struggle to be maintained with
    northeastern extent. Portions of the Mobile, AL area may recover
    from prior convective overturning and experience a renewed
    thunderstorm/flash flood threat, however.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-eBMlkL1UBVI8zSV158CTwx2SMG9yBw5ckwsdbROPe7b0c9EUz-UaY1if5TtjMkdbrXm= 8fyw8xODLGeIAl_jXSvu_g4$ for graphic product...

    ATTN...WFO...BMX...JAN...LCH...LIX...MOB...TAE...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 32158672 32108561 30678610 30118715 29688992=20
    29369046 29679156 30029176 30619173 31339010=20
    31908888=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 22 22:49:29 2026
    AWUS01 KWNH 222249
    FFGMPD
    VAZ000-WVZ000-OHZ000-TNZ000-KYZ000-INZ000-230447-

    Mesoscale Precipitation Discussion 0213
    NWS Weather Prediction Center College Park MD
    648 PM EDT Fri May 22 2026

    Areas affected...portions of Kentucky into southern Ohio and
    western West Virginia

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

    Valid 222247Z - 230447Z

    Summary...Scattered convection with embedded heavier rainfall will
    continue to spread northward toward the middle/upper Ohio Valley
    this evening. Moist ground conditions from antecedent rainfall
    will raise the flash flood risk in a few areas.

    Discussion...Scattered, deep convection continues along a general
    axis extending from near Hopkinsville east-northeastward to near
    Covington. These cells also happened to be collocated with a weak
    warm front through that same aforementioned axis. Along and south
    of the boundary, 70s F dewpoints were maintaining 1000-1500 J/kg
    SBCAPE, fueling heavier convective elements and spots of 1 inch/hr
    rain rates. A broad, negative-tilt mid-level trough over the
    Mid-Mississippi Valley and stout low-level flow across
    Kentucky/Tennessee was also providing ascent to support ongoing
    convection.

    This overall regime will gradually translate east-northeastward
    over the next 3-6 hours. Areas of heavier rain will fall on
    moistening soils that are gradually becoming more sensitive by the
    hour due to abundant rainfall. FFG thresholds are around 1
    inch/hr in most of Kentucky, but fall to around 0.5 inch/hr in
    northeastern Kentucky into southern Ohio and western West
    Virginia. As embedded convective elements reach these
    water-logged areas, flash flood potential will increase. This
    threat will exist through at least 02Z, with little indication
    that rainfall rates will decrease after sunset.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!79d-Wj68ojWqCrsF2yZFQ9Wp4LOVbIFTpCrrFnY29cx7R9rwOHsyfzU0_zbHVPQjFPfS= RSRRU7RfQF_QvnaOf2138HI$ for graphic product...

    ATTN...WFO...ILN...IND...JKL...LMK...MRX...OHX...PAH...PBZ...
    RLX...

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 40148277 39948082 38988042 38008173 37148259=20
    36508336 36738469 36748661 36658801 37538804=20
    38218691 39378497=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 23 00:55:12 2026
    AWUS01 KWNH 230055
    FFGMPD
    MSZ000-LAZ000-ARZ000-TXZ000-230453-

    Mesoscale Precipitation Discussion 0214
    NWS Weather Prediction Center College Park MD
    854 PM EDT Fri May 22 2026

    Areas affected...northern Louisiana into central Mississippi and
    far northeast Texas

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

    Valid 230053Z - 230453Z

    Summary...Scattered thunderstorms were developing along a
    confluence zone over the Mississippi Delta and adjacent northern
    Louisiana. 1-2 inch/hr rain rates were estimated. These rates
    will pose a flash flood risk for a few hours this evening.

    Discussion...Persistent convergence along a confluence zone
    extending from near Shreveport to near Monroe to near Rolling Fork
    in southern portions of the Mississippi Delta. This confluence
    zone was oriented parallel to west-southwesterly flow aloft,
    supporting local cell training. In addition, abundant surface
    heating along and south of this zone has enabled MLCAPE values to
    exceed 2000 J/kg amid ~1.75 inch PW values. These thermodynamic
    fields were enabling rain rates to reach 1-2.5 inch/hr in a few
    spots. The highest rain rates were threatening FFG thresholds,
    which generally range from around 1 inch/hr in MS to 2.5 inch/hr
    in northern Louisiana.=20

    Current trends suggest that most of the ongoing flash flood
    potential will be diurnally driven, with a possible weakening
    trend beginning after a few hours with loss of
    heating/destabilization. Flash flooding will still remain
    possible through at least 04Z/11p central given the favorable
    thermodynamic environment supporting deep convection with
    efficient rain rates. Flash flooding is possible - with
    particular concern in low-lying spots and across central
    Mississippi where ground conditions remain moist from prior
    rainfall.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-bQo8_XKZHJ9aXvQz09CnEA9cf51h-P3yWBCIEcftfiA4QbNEtbDUbqQEfOtu9-YFbBi= 3WG0LA_iirluOe5cz512ON0$ for graphic product...

    ATTN...WFO...JAN...LZK...MEG...SHV...

    ATTN...RFC...ALR...FWR...ORN...NWC...

    LAT...LON 34179016 33888932 32858903 32028984 31669202=20
    31709464 32689489 33109381 33279199 33919108=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 23 13:37:02 2026
    AWUS01 KWNH 231336
    FFGMPD
    MSZ000-LAZ000-TXZ000-231935-

    Mesoscale Precipitation Discussion 0215
    NWS Weather Prediction Center College Park MD
    935 AM EDT Sat May 23 2026

    Areas affected...Far Eastern TX...Central and Southern LA...Far
    Southwest MS

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

    Valid 231335Z - 231935Z

    SUMMARY...Expanding areas of heavy showers and thunderstorms, with
    some localized cell-training will result in an increasing flash
    flood threat through the mid-afternoon hours. Rainfall rates of 2
    to 3 inches/hour are expected, with localized totals of 3 to 5
    inches possible.

    DISCUSSION...GOES-E satellite imagery and radar shows some small
    scale MCS activity over far eastern TX along with an embedded MCV
    that will be moving east into areas of western LA over the next
    few hours. The latest surface data suggests a surface
    trough/outflow boundary near the southern LA coast that extends
    west-southwest back toward the Upper TX coast.

    Meanwhile, the airmass is moderately buoyant with a nose of MLCAPE
    values reaching 1500 to 2000+ J/kg across far eastern TX and
    across much of western LA in association with modest, but
    persistent southerly flow off the Gulf ahead of the upstream
    convection. Moisture is heavily entrenched through the column
    based off the latest OSPO ALPW data, with PWs overall running up
    to near 1.75 inches.

    The approaching convection and associated MCV energy is expected
    to interact with this surface trough near the Gulf Coast, and
    favor a general increase in warm air advection/isentropic ascent
    that coupled with the nose of instability should favor an increase
    in the coverage of heavy showers and thunderstorms. The latest
    Corfidi vector analysis suggests at least some low-end threat for
    backbuilding and training convection over the next several hours
    as the convection increases across areas of central and southern
    LA, and perhaps areas as far northeast as southwest MS.

    High rainfall rates are expected that could reach 2 to 3
    inches/hour with the stronger convective cores, and with any
    cell-training, some localized storm totals going through early to
    mid-afternoon could reach 3 to 5 inches. FFG is rather high across
    the region overall, with moderate soil moisture (50 to 70 percent)
    in the 0-10cm layer according to NASA SPoRT. However, with the
    high rainfall rates and localized storm total potential, some
    areas of flash flooding will tend to become likely over the next
    several hours. This will especially be the case for the more
    sensitive urban corridors.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-KQi3ZJNBFp2ejl5zDgZ2Jg7lR7tsfOr4FlcsN_tTCGKaKRIQE-FwBdhxhX2E3MwlWqg= Q56Fw7SOnkxhKJuE7DStGmM$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 31979285 31679154 31059027 30288969 29688969=20
    29369007 29269094 29589253 29629308 29789379=20
    30719441 31249432 31819377=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 23 15:32:13 2026
    AWUS01 KWNH 231532
    FFGMPD
    TXZ000-232130-

    Mesoscale Precipitation Discussion 0216
    NWS Weather Prediction Center College Park MD
    1130 AM EDT Sat May 23 2026

    Areas affected...South-Central to Southeast TX

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

    Valid 231530Z - 232130Z

    SUMMARY...Expanding clusters of heavy showers and thunderstorms
    will result in a regional threat for scattered areas of mainly
    urban flash flooding going into the afternoon hours. Rainfall
    rates as high as 2.5 inches/hour are likely, with localized totals
    of 3 to 5 inches possible.

    DISCUSSION...An ejecting shortwave trough/MCV crossing the Lower
    Rio Grande Valley will be interacting with a moist and strongly
    unstable airmass pooled along a surface trough currently situated
    across areas of south-central to southeast TX and extending
    offshore across the western Gulf. The approaching energy is
    already driving multiple clusters of heavy showers and
    thunderstorms across south-central TX, with a generally
    progressive character off to the east.

    MLCAPE values across south-central TX are on the order of 2500 to
    3500 J/kg with PWs locally up around 1.75 inches. This coupled
    with the forcing associated with the approaching shortwave
    dynamics will facilitate rainfall rates as high as 2.5 inches/hour
    over the next several hours as convection becomes increasingly
    concentrated in close proximity to the aforementioned trough axis.

    A general increase in the coverage of convection is expected going
    into the afternoon hours across coastal areas of south-central to
    southeast TX, including multiple metropolitan areas such as
    Victoria and Houston. There will be some occasional instances
    where the convection may repeat or train over the same area which
    would drive heavier rainfall totals. The 12Z HREF/REFS suites
    suggest some localized 3 to 5 inch rainfall totals going through
    mid-afternoon.

    Given the overall antecedent environment and expectations of
    rainfall over the next few hours, there will be a threat for
    scattered areas of mainly urban flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!67tA2NnIsFCry5e7BmZ0XHM7XyUu3NYCaXM_7jr8-HPEQZiDiJ_vTrTxJBhO6VV1jkKR= 7nL6goKHbEJ3aW-k7ebGSFM$ for graphic product...

    ATTN...WFO...BRO...CRP...EWX...HGX...LCH...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30549440 29729390 28989499 28009653 27239714=20
    26939766 27219814 27969832 28829814 29599742=20
    30159643 30459547=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 23 17:01:51 2026
    AWUS01 KWNH 231701
    FFGMPD
    WVZ000-OHZ000-TNZ000-KYZ000-232300-

    Mesoscale Precipitation Discussion 0217
    NWS Weather Prediction Center College Park MD
    100 PM EDT Sat May 23 2026

    Areas affected...Portions of the OH Valley

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

    Valid 231700Z - 232300Z

    SUMMARY...Wet antecedent conditions and additional showers and
    thunderstorms this afternoon may produce a localized threat of
    flash flooding this afternoon.

    DISCUSSION...The latest GOES-E satellite imagery along with
    surface data shows an area of low pressure associated with an
    upper trough across northwest OH. A trailing cold extends well to
    the southwest of this with a warm front that is situated over
    northern OH and down the west side of the Appalachians. A moist
    and confluent low-level southwest flow pattern ahead of the cold
    front is nosing up across much of central and eastern KY through
    far western WV and eastern OH.

    Warm sector MUCAPE values of 500 to 1000 J/kg and PWs of 1.5 to
    1.75 inches are already in place generally from southern OH
    through eastern KY, and this instability axis will lift a bit
    farther north this afternoon as southwest flow ahead of the front
    persists. Additionally, the latest visible satellite images show a
    fair amount of solar insolation taking place across these areas,
    and this is expected to yield a destabilizing boundary layer that
    will couple with modest low-level forcing/convergence for
    scattered bands of showers and thunderstorms over the next several
    hours.

    The mean layer flow is strongly unidirectional as seen on the 12Z
    upper-air RAOB from KILN, and this will suggest a concern for some
    localized training of these bands of convection. Already there is
    one linear band of convection extending from southern OH into
    north-central KY that has had a history of producing 1 to 2
    inch/hour rainfall rates, and these high rates should be
    sustainable this afternoon with the addition of more surface heating/instability.

    The latest hires CAMS may be slightly underdone with the
    convective threat and the overall QPF footprint this afternoon
    considering the training potential. Given the rates and training considerations, some localized 2 to 3 inch rainfall totals will be
    possible. The antecedent conditions are rather wet, and this
    coupled with the additional rainfall potential may support some
    localized areas of flash flooding this afternoon.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!71-1H9gosDQS7QWA22Ig2vHwXXspPL-ipWp4cf75PDtajGxyot6U94zt82aqcLLd8RXr= wkBrTuw9zAOXHJHtejK6zkI$ for graphic product...

    ATTN...WFO...CLE...ILN...JKL...LMK...MRX...OHX...PBZ...RLX...

    ATTN...RFC...TIR...NWC...

    LAT...LON 41218183 41148115 40618058 39278102 38118192=20
    37028306 36428420 36508513 36968551 37598527=20
    38248439 38978374 39828308 40888251=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 23 17:53:56 2026
    AWUS01 KWNH 231753
    FFGMPD
    ALZ000-MSZ000-LAZ000-ARZ000-232345-

    Mesoscale Precipitation Discussion 0218
    NWS Weather Prediction Center College Park MD
    152 PM EDT Sat May 23 2026

    Areas affected...Southeast AR...Central and Southern
    MS...West-Central AL

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

    Valid 231752Z - 232345Z

    SUMMARY...Isolated to scattered areas of flash flooding will be
    possible this afternoon and early this evening from showers and
    thunderstorms with high rainfall rates capable of reaching 2 to 3
    inches/hour.

    DISCUSSION...The latest GOES-E IR/WV suite shows a cold-topped MCS
    and embedded MCV continuing to advance east across central LA with
    recent radar trends showing downstream convective development
    across areas of southeast AR through central and southern MS. This
    energy will be interacting over the next several hours with a
    strongly unstable and moist environment characterized by MLCAPE
    values of 2000 to 3000+ J/kg and PWs over 1.75 inches.

    There is evidence of a surface trough across south-central MS
    which recently seems to be facilitating some of the development
    and expansion of convection across this region. The latest HRRR
    and RRFS guidance suggests rainfall coverage increasing over the
    next few hours as the upstream energy with the MCV approaches, and
    there is likely to be areas of relatively concentrated convection
    by later this afternoon that will be capable of producing very
    high rainfall rates. Given the thermodynamic environment, there
    will be some rainfall rates likely reaching 2 to 3 inches/hour.

    The high rates and relatively concentrated nature of the
    convection may support some rainfall totals that reach 3 to 4+
    inches by early this evening. Recent rainfall across portions of
    the region have allowed for the antecedent environment to become
    more sensitive, with increasing soil moisture concentrations. As
    such, the additional rainfall this afternoon may favor a concern
    for isolated to scattered areas of flash flooding. This would also
    include concerns for some of the more sensitive urban areas.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-xFujvhWvvLzNFZ1UlbBP_b4zFp39b1trxk9DdKvh_l8QF6cBvQ4UvK2w3qdnzoWc3NP= WYce8OlhfKTX9TbjcWsXkmo$ for graphic product...

    ATTN...WFO...BMX...JAN...LZK...MOB...SHV...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34119119 33279025 33098908 32808816 32478781=20
    31938776 31568825 31398904 31459029 31749128=20
    32279185 32659211 33599235 34109210=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 23 18:53:02 2026
    AWUS01 KWNH 231852
    FFGMPD
    SCZ000-GAZ000-232345-

    Mesoscale Precipitation Discussion 0219
    NWS Weather Prediction Center College Park MD
    252 PM EDT Sat May 23 2026

    Areas affected...Northeast Georgia through North-Central South
    Carolina

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

    Valid 231849Z - 232345Z

    SUMMARY...Heavy thunderstorms, with some localized cell-training
    bring an increasing flash flood threat rest of the afternoon from
    northeastern Georgia through north-central South Carolina.
    Rainfall rates of 1 to 2 inches/hour are expected, with localized
    totals of 3 inches possible over already saturated ground.

    DISCUSSION...Moist/unstable air flowing into the cold air damming
    wedge front over northeastern Georgia. This front is providing a
    focus for thunderstorm development generally west from Augusta.
    Southerly low level flow with effective shear of 25 to 30kt is
    allowing redevelopment along/beyond this front with SBCAPE of 2500
    J/kg and PW of 1.9" allowing hourly rainfall of 1.5 inches/hour in
    spots. The cold wedge front has been receding north which brings
    the focus into the area that saw 2-5" rainfall last evening. FFG
    of 1 to 1.5 inches/hour is along the current frontal location from
    GA to the flash flood sensitive Columbia, SC.

    Continued heavy rain over this already saturated area should cause
    localized flash flooding into this evening. Instability decreases
    rapidly north of the front keeping areas such as Greenville, SC
    away from the heavy rain at least for the next several hours.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9RyitIh4Q531mORIBqfHAg4s-K5xQ0fAwBaQdryk86pCizdxhuOqrhyPtZa-Sj2OpHoi= mAnZCOHKxG2jkKUwsj1MzO8$ for graphic product...

    ATTN...WFO...CAE...FFC...GSP...

    ATTN...RFC...ALR...NWC...

    LAT...LON 34828348 34748305 34658266 34478215 34578138=20
    34508044 33988084 33758132 33478194 33418220=20
    33448252 33608292 33918330 34488351=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 23 20:32:12 2026
    AWUS01 KWNH 232032
    FFGMPD
    MOZ000-ARZ000-OKZ000-KSZ000-240130-

    Mesoscale Precipitation Discussion 0220
    NWS Weather Prediction Center College Park MD
    431 PM EDT Sat May 23 2026

    Areas affected...Southwest Missouri into Kansas and Arkansas

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

    Valid 232030Z - 240130Z

    SUMMARY...Heavy thunderstorms repeating near a frontal boundary,
    bring an increasing flash flood threat into this evening over
    southwest Missouri into Kansas and Arkansas. Rainfall rates up to
    2 inches/hour are expected, with localized totals of 3 inches.

    DISCUSSION...An MCV over northeast OK is riding along a stalling
    frontal boundary over far southeast KS into central MO. The warm
    sector activity extends from northwest AR up to west-central MO.
    Sufficient moisture with PW of 1.5" and instability with SBCAPE of
    1500 J/kg will continue to allow heavy thunderstorm development
    rest of the afternoon. Light shear over the area causes slow storm
    motion while southerly low level flow recharges the environment
    through the frontal convergence. FFG is generally around 1.5
    inches/hour which has been observed the past hour over southwest
    MO. SWly jet level flow will continue to push the MCV along the
    front and maintain heavy rain ahead of it into the evening.

    Recent HRRR and RRFS runs do not handle the MCV well and result in
    too dispersive QPF into the evening. Given radar trends and the
    moist/unstable environment, localized flash flooding can be
    expected into the evening hours in areas with lower FFG, urbanized
    areas, and in the highest precip totals. The activity should
    eventually progress east, so further discussions may be warranted
    into the overnight hours.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-TfOJddi27ltmW5likwsam9bAO2tNIfqIk9VWDQNuV_g7ndjfLDdWo1yvtj6xwMHSTaU= oOSfMd3JLA0U0O0XA3Kqats$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...LZK...SGF...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 39009285 38669251 36609311 36119357 36589439=20
    37069474 37219544 37469539 37829483 38579382=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 24 00:18:37 2026
    AWUS01 KWNH 240018
    FFGMPD
    PAZ000-WVZ000-OHZ000-KYZ000-240530-

    Mesoscale Precipitation Discussion 0221
    NWS Weather Prediction Center College Park MD
    817 PM EDT Sat May 23 2026

    Areas affected...Upper Ohio Valley

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

    Valid 240016Z - 240530Z

    SUMMARY...Saturated soils and additional prefrontal thunderstorms
    this evening should continue to produced localized flash flooding
    over the Upper Ohio Valley into the overnight.

    DISCUSSION...A plume of moisture extends north up the west side of
    the Appalachians and the Upper Ohio Valley west of the cold air
    damming west on the east side of the Appalachians and ahead of a
    cold front over northern Ohio. A moist and confluent southwesterly
    low-level flow through this plume is providing 1.6" PW which is 2
    standard deviations above normal over southeast OH, western WV,
    into far western PA.

    Warm sector MLCAPE values of 1000 J/kg and the abundant moisture
    will continue to support scattered bands of heavy thunderstorms
    through the evening. Deep layer unidirectional SWly flow persists
    over this region which should maintain localized training of these
    bands of convection. Hourly rainfall up to 1.5 to 2" is likely to
    continue in training activity which is in agreement with recent
    HRRR/RRFS runs. The antecedent conditions are rather wet with
    flash flood guidance generally 1" or less. Therefore localized
    flash flooding can be expected into the overnight. Late night
    nocturnal trends may preclude the need for further discussion in
    this area overnight, though that will continue to be monitored.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_qTo1ziUydoIoJLKNj985gDznN4aCtucEOni6CUIa39iu4qt7sOyXV8xjsIpWMs9OhT7= z1bgPrqXS64u2i5xlZniOj4$ for graphic product...

    ATTN...WFO...ILN...JKL...LMK...PBZ...RLX...

    ATTN...RFC...TIR...NWC...

    LAT...LON 40638122 40428064 39978035 38938106 38068215=20
    37668342 38328420 39048362 39898219=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 24 01:25:42 2026
    AWUS01 KWNH 240125
    FFGMPD
    MOZ000-ARZ000-240630-

    Mesoscale Precipitation Discussion 0222
    NWS Weather Prediction Center College Park MD
    924 PM EDT Sat May 23 2026

    Areas affected...Ozarks

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

    Valid 240123Z - 240630Z

    SUMMARY...Heavy prefrontal thunderstorms repeating into the
    overnight maintain a localized flash flood threat over southern
    and northern Arkansas. Rainfall rates up to 2 inches/hour are
    expected, with localized totals of 3 inches.

    DISCUSSION...Outflow from earlier activity is maintaining
    convergence from southerly flow and renewed growth over northwest
    AR into southeastern MO. Sufficient moisture with PW of 1.5" and
    instability with MUCAPE of 1000 J/kg will continue to allow heavy
    thunderstorm development into the overnight. Light shear over the
    area causes slow storm motion while southerly low level flow
    recharges the environment through the frontal convergence. FFG is
    generally higher, around 2.5 inches/hour despite this being the
    flood prone Ozarks.

    Recent HRRR runs have a decent handly on this ongoing activity
    while the RRFS is underdoing it. Given radar trends and the
    moist/unstable environment, localized flash flooding can be
    expected into or through the overnight hours where highest precip
    totals occur.


    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9gQcWATB0duFocmJ93-PRp-o5AafAvFLlEM13Zxlu3UW1dJ5hY5uYQkM3N6x6okcHSFZ= B1Y7DqnmBssIveydCnLEjmU$ for graphic product...

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

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 37989132 37569065 36309042 35409209 35339412=20
    35899423 36369341 36859254 37359213 37909200=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 24 06:51:46 2026
    AWUS01 KWNH 240651
    FFGMPD
    ALZ000-MSZ000-LAZ000-241200-

    Mesoscale Precipitation Discussion 0223
    NWS Weather Prediction Center College Park MD
    250 AM EDT Sun May 24 2026

    Areas affected...Southeast LA...Coastal MS & AL...

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

    Valid 240650Z - 241200Z

    SUMMARY...Strong MCV with WAA training profiles increasing
    residency and therefore overall totals to allow for rapid
    inundation flooding.

    DISCUSSION...KHDC shows a very mature MCV with a tight inner
    convective core as well as a leading forward propagating leading
    band moving through the mouth of the Mississippi River and through
    the Chandeluer Islands. The strong outflow and localized pressure
    falls continues to support rapidly backed low-level inflow over
    the area of the north central Gulf that has remained over 80
    degrees and therefore increasing downstream theta-E advection and
    moisture flux.=20

    The latent heat release and favorable outflow orientation to a
    great outflow channel into the right entrance of the 80-90kt speed
    max continues to maintain and actually recently strengthen the
    MCC/MCV. RAP analysis and local observations show the downshear
    WAA off the Central Gulf has increased deep layer moisture to near
    2"/hr but also has pulled the instability gradient across the
    Chandeleur to central MS Coast and into south-central AL with
    MLCAPEs over 1500 J/kg along and downstream. This all has
    sharpened the effective warm front/deformation zone increasing low
    level isentropic ascent/moisture convergence along and ahead of
    the dense central core. Rates of 2-2.5"/hr are likely given the
    strength of the flux convergence and upward vigor of updrafts over
    the next few hours. As the convection continues to expand along
    the warm front, training/repeating will increase to support
    increased residency for localized 2-4" totals, with and isolated
    5" total possible in the 2-3 hours as it the band/core passes.=20

    The limiting factors will be placement relative to the land, with
    the core likely to remain SE of NOLA proper, but given deep layer
    steering look to come along the MS coastal area into S Alabama,
    where recent very high rainfall totals over the last 2 days or so
    have saturated the upper soils. FFG values have recovered, but
    given 0-40cm soil ratios, across portions of the MPD and overall
    rates of warm cloud tropical rainfall could result in rapid
    inundation flooding through the late overnight period and early
    morning.=20=20

    There is some uncertainty for trailing redevelopment South of SE
    LA, where confluent rear-inflow streamers could reform. About
    half of Hi-Res CAM suite suggests this redevelopment may persist,
    though environment may take too long to recover to have higher
    confidence, but the risk does remain.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5WIMBt4M39pYQ2L9f9XMTzG-N_06pU65Cs6ECrcP_0u-YolHoT7wpFM9glweOGgrCsbs= -yb5i67558CstYHz17P4vkk$ for graphic product...

    ATTN...WFO...JAN...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 31998811 31638766 31038759 30148821 29078933=20
    29079008 29639038 30648984 31288947 31908895=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 24 17:09:42 2026
    AWUS01 KWNH 241709
    FFGMPD
    PAZ000-VAZ000-WVZ000-OHZ000-TNZ000-KYZ000-INZ000-242305-

    Mesoscale Precipitation Discussion 0225
    NWS Weather Prediction Center College Park MD
    108 PM EDT Sun May 24 2026

    Areas affected...Central and Eastern Kentucky...Southern and
    Eastern Ohio...Central and Western West Virginia

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

    Valid 241708Z - 242305Z

    SUMMARY...Convective coverage and intensity will gradually
    increase and expand eastward through late this afternoon ahead of
    an approaching MCV. Hourly rainfall rates of 1.0 to 1.5+ inches
    overlapping with highly sensitive soils will make scattered areas
    of flash flooding likely.

    DISCUSSION...Regional radar and visible satellite imagery early
    this afternoon depict an expanding area of efficient showers and
    deepening convective clouds advancing downstream from an MCV
    currently migrating out of western Kentucky. While morning
    activity was generally subdued, continued diurnal heating is
    actively destabilizing the boundary layer across a broader
    footprint. This increasing instability is fostering an expansion
    of convective coverage and updraft intensity that will track
    eastward across central/eastern Kentucky, southern/eastern Ohio,
    and into central/western West Virginia over the next several hours.

    The 12Z high-resolution guidance suite (including the HREF and
    REFS) shows neighborhood probabilities for 1 inch/hr rainfall
    rates increasing toward 30-50% across the region, with a notable
    uptick in signal pushing into central and western West Virginia by
    late afternoon. Furthermore, the deep-layer mean steering
    flow?oriented southwest to northeast?will parallel the initiating
    boundaries, strongly favoring cell training. The latest CAM
    consensus points toward localized rainfall totals of 2 to 4 inches.

    The primary driver for the flash flood threat remains the low land
    surface capacity across this entire region. Recent soil moisture
    data and RFC Flash Flood Guidance indicate that the basins across
    the Ohio Valley and into the Appalachian foothills of West
    Virginia are already sensitive. The 12Z HREF/REFS blend shows a
    robust and expanding 30-50% probability of exceeding these low
    3-hour FFG thresholds. Given the antecedent conditions and
    potential for training convection, any 1.0-1.5"+/hr rates will
    drive runoff concerns, and likely overwhelming some small streams,
    creeks, and low-lying infrastructure. Therefore, scattered areas
    of flash flooding are generally likely this afternoon.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8wmf-1b4SO41LV9d8--fOutJehNOzV4EU5Du1lyJ4ba5kDdijOKgld-gB06nRVHlNRXt= 8hN6eftIqVYMWyIFKZC_w90$ for graphic product...

    ATTN...WFO...CLE...ILN...JKL...LMK...MRX...OHX...PBZ...RLX...
    RNK...

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 41218178 41208087 40818047 40058038 39258035=20
    38288059 37358159 36998231 36558393 36558497=20
    36678542 37358529 37958574 38488562 39158465=20
    39708363 40608255=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 24 16:19:39 2026
    AWUS01 KWNH 241619
    FFGMPD
    GAZ000-TNZ000-ALZ000-242215-

    Mesoscale Precipitation Discussion 0224
    NWS Weather Prediction Center College Park MD
    1217 PM EDT Sun May 24 2026

    Areas affected...Central to Northeast Alabama...Northwest
    Georgia...Middle Tennessee

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

    Valid 241617Z - 242215Z

    SUMMARY...Convective coverage and intensity will continue to
    expand early this afternoon as an MCV lifts northeastward.
    Rainfall rates of 1-2+ inch/hr, with localized maximum totals of
    2-4 inches, will make scattered areas of flash flooding likely
    this afternoon given the moist antecedent conditions.

    DISCUSSION...Regional radar and satellite imagery depict an
    expanding area of convection across central and northern Alabama,
    driven by a well-defined MCV and associated mid-level shortwave
    lifting northeastward. A coupled pocket of 850mb convergence and
    250mb divergence is providing robust synoptic lift. Concurrently,
    diurnal heating has actively destabilized the boundary layer,
    allowing MUCAPE values to surge into the 1000-2000 J/kg range.
    Combined with PWATs pooling between 1.7 and 1.9 inches, the
    environment is primed to support highly efficient convection with
    high rainfall rates.

    High-resolution guidance is in strong agreement regarding the
    evolution and intensity of the afternoon convection. The 12Z HREF
    highlights 50-70+ percent neighborhood probabilities for 1 inch/hr
    rainfall rates across the region, with 20-30+ percent
    probabilities for rates exceeding 2 inch/hr. The latest HRRR
    guidance corroborates this intensity, suggesting localized total
    accumulations of 2 to 4 inches through the afternoon as the
    convective footprint expands from into northeast Alabama, middle
    Tennessee, and eventually farther east with areas of northwest
    Georgia seeing a threat.

    The combination of high-end rainfall rates and expanding coverage
    will pose a flash flood threat. The 12Z HREF shows 40-50 percent
    probabilities for exceeding 3-hour Flash Flood Guidance (FFG)
    across the targeted area. The intersection of 2+ in/hr rates with
    the sloped terrain of the Cumberland Plateau and the more
    sensitive urban corridors will lead to potentially more enhanced
    runoff concerns, and thus overwhelming local drainage systems and
    small streams. Overall, scattered areas of flash flooding are
    likely across the region over the next several hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6nkighx3wfEaDfsRHYQ0MhHTbyp29_-ejb0xkuaYufEx4KbxZpsH8vZ_hA8tHPdKgJQC= NcV3s8kz7dqvcNxHQg_s_JI$ for graphic product...

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

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 36468476 35738436 34498476 33188559 32538648=20
    32458709 32918767 33688768 34738719 35588649=20
    36328568=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 24 20:26:03 2026
    AWUS01 KWNH 242026
    FFGMPD
    FLZ000-GAZ000-ALZ000-250130-

    Mesoscale Precipitation Discussion 0226
    NWS Weather Prediction Center College Park MD
    424 PM EDT Sun May 24 2026

    Areas affected...Southern Georgia

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

    Valid 242024Z - 250130Z

    SUMMARY...Repeating thunderstorms bring isolated flash flood
    threat to southern/central Georgia into the evening. Rainfall
    rates of 2-3 inch/hr will continue with localized maximum totals
    of 3-5 inches for this area which is not flood prone.

    DISCUSSION...Regional radar and satellite imagery depict an
    east-west oriented line of scattered heavy thunderstorms
    developing on low level convergence over southern Georgia with
    further upstream development in far north Florida. Instability is
    robust with SBCAPE of 3000 J/kg and moisture is extreme with 2.2
    inch PW (2.5 sigma above normal) supporting highly efficient
    convection with high rainfall rates of up to 3 inches/hr.

    Recent hRRR and RRFS runs are on the lighter side for rainfall
    compared to radar estimates. Fair rates of northward movement will
    continue with SSWly deep layer mean flow generally around 20kt.
    However, the additional upstream development and cell interactions
    make a concern for localized maxima of a quick 3-5 inches of
    rainfall in the coming few hours which would exceed the general
    flash flood guidance near 3 inch/hr. This activity will continue
    moving north and could bring concerns this evening to more
    sensitive areas such as Atlanta and areas of northeast GA into SC
    which have seen more rain in recent days due to the persistent
    cool air damming.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!73FTkC8m3598p8gBqwfzYyI6uf2NojWFSmkB9fund5L1uUQr5HyXr55Be9nysJZEbyNF= f2-dFCqIYmHWYyMB6looUog$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 33088432 32998344 32688250 31878236 31108254=20
    30458283 30348394 30698518 31418572 31938558=20
    32568537 32848500=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 24 21:02:08 2026
    AWUS01 KWNH 242102
    FFGMPD
    TXZ000-OKZ000-250200-

    Mesoscale Precipitation Discussion 0227
    NWS Weather Prediction Center College Park MD
    500 PM EDT Sun May 24 2026

    Areas affected...Dallas-Forth Worth Metro

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

    Valid 242100Z - 250200Z

    SUMMARY...Localized flash flooding over the greater Dallas-Fort
    Worth metro into this evening from slow moving heavy thunderstorms
    producing up to 4" rainfall.

    DISCUSSION...As of 21Z...thunderstorm clusters north of Ft. Worth
    and southeast of Dallas have developed in a moist/unstable
    environment. Instability is typical for North Texas summertime
    convection with SBCAPE around 3000 J/kg as is moisture with PW
    around 1.5" and dew points in the upper 60s. Light flow will
    continue to allow slow movement and popcorn type convection
    developing off outflow boundaries. Rainfall rates up to 2"/hr
    estimated by KFWS in the past hour should generally hold true for
    subsequent convection through the evening. There is a risk for
    some repeating convection/cell mergers which could allow localized
    4" totals which would be a concern for flash flooding, especially
    in the broad urbanized areas of the metro.

    Recent HRRR runs are underestimating the ongoing activity and
    generally underplay the heavy rainfall threat for this metro area
    into this evening. Hail is a concern with this activity, but
    enough rainfall should occur to cause localized flash flood
    concerns into the evening. Further thunderstorm development to the
    south may warrant additional discussions in Texas through this
    evening.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8-WaSVXFsd4dfERNS-1ssz10PzDgVEXMLkl2Kf2TtZtIl6kWR1Sz5COVFouQlCK-FWk6= -RIq4BmaA1BeQgIfgvR3w9w$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 33869791 33819644 33449506 32469498 31939579=20
    32039707 32369854 33489887=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 24 22:22:20 2026
    AWUS01 KWNH 242222
    FFGMPD
    NCZ000-SCZ000-GAZ000-TNZ000-250330-

    Mesoscale Precipitation Discussion 0228
    NWS Weather Prediction Center College Park MD
    621 PM EDT Sun May 24 2026

    Areas affected...North Georgia into South Carolina and Southern
    Appalachians

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

    Valid 242218Z - 250330Z

    SUMMARY...Widespread convection with embedded high intensity
    rainfall lift over Georgia and South Carolina this evening.
    Additional convection over eastern Tennessee will also continue
    ahead of an MCV lifting past Chattanooga. Rain rates of 2"/hr with
    localized maximum totals of 2-4 inches will make scattered areas
    of flash flooding likely through this evening given the moist
    antecedent conditions.

    DISCUSSION...As of 22Z...an MCV is moving over Chattanooga while
    scattered heavy convection is over the Atlanta metro east into
    South Carolina with an organized line of convection lifting from
    southern Georgia. This area has upper support from increasing
    right entrance jet dynamics over the eastern TN Valley and low
    level support in the form of topographic lift in the southern
    Appalachians as well as a remnant cool air damming wedge over the
    upland area of SC into northeast GA. Ample instability is present
    with 2500 J/kg SBCAPE over the GA/SC border and generally 1500
    J/kg elsewhere. A pool of 2.2" PW air is lifting north from
    southern GA while the 2" PW contour currently reaches Atlanta per
    the 22Z RAP mesoanalysis. Ongoing activity in northern Atlanta
    combined with the progress of southern GA activity warrants
    including Atlanta in this discussion area. The environment in the
    discussion area supports highly efficient convection with high
    rainfall rates.

    As is the recent trend, HRRR runs this afternoon are underdoing
    current activity, while the RRFS has maxes that are too hot in GA,
    but also too low in eastern TN per recent radar trends. Taking an
    average of the two makes for a more reasonable solution with a
    threat for 2-4" maxima through 03Z with 4-5" possible along the
    GA/SC border area.

    The combination of high-end rainfall rates and threat for
    repeating activity in deep layer SSWly flow of 25kt poses a
    scattered flash flood threat through the evening. The cool air
    wedge has kept heavy rain from the southern Apps in recent days,
    so the antecedent conditions are worse on the Piedmont/Cumberland
    Plateau. There is a localized flash flood threat in the southern
    Apps tonight as the wedge continues to break down and subtropical
    moisture encounters orographic lift.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8ZF2ReEL8Eu1gp6GVaTtshS2yuMRLUMaC6puJGAg1QdVZlLK9QgzTw1AqNN0yn5MFfSf= XljB2RnmjcEz3SujlMB2dTo$ for graphic product...

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

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 36568240 36228190 35578277 34768280 34548221=20
    34608161 34768086 34528066 34028066 33118118=20
    32718227 33058392 33598457 34108483 34498480=20
    35498514 36548440=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 24 22:55:52 2026
    AWUS01 KWNH 242255
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-OHZ000-TNZ000-KYZ000-250430-

    Mesoscale Precipitation Discussion 0229
    NWS Weather Prediction Center College Park MD
    654 PM EDT Sun May 24 2026

    Areas affected...Upper Ohio Valley

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

    Valid 242253Z - 250430Z

    SUMMARY...Repeating warm sector convection will continue to
    develop and lift north-northeast through the Upper Ohio Valley and
    western slopes of the Allegheny Plateau into the overnight. Hourly
    rainfall rates of 1.5 to 2 inches over already saturated soils and
    terrain of the western slopes will continue to allow scattered
    flash flooding.

    DISCUSSION...As of 23Z...A cold front is over western Ohio with a
    persistent warm sector ahead over the upper half of the Ohio
    Valley through the western slopes of the Allegheny Plateau and
    expanding across western PA. Ample moisture with a gradient of
    1.7" to 1.5" PW from south to north through the outlook area and
    instability with 1500 J/kg SBCAPE along with deep layer SWly flow
    of 35kt is allowing heavy bands to develop oriented close to their
    direction of motion. Hourly rainfall estimates of 1.5 to 2" are in
    the heaviest bands which has caused localized flash flooding given
    low FFG from recent rains in these areas. This activity is
    shifting farther east than recent days as the cool air damming
    wedge breaks down, but slope/terrain increases, making the western
    slopes of the Allegheny Plateau perpetually flash flood prone.
    Furthermore, an MCV currently over eastern TN will lift up along
    the KY/WV border this evening and potentially through WV
    overnight.

    Both recent HRRR/RRFS guidance have a decent handle on ongoing
    activity and the threat this evening with generally 1-3" from the
    western tip of VA through WV and western PA through 04Z. Given the
    wet antecedent conditions and expectation for continued training
    convection, any 1.5"+/hr rates will drive runoff concerns.
    Therefore, scattered areas of flash flooding are likely to
    continue into the overnight.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Ee6HDoBOGzoITdAw2tENfQr1ELj1iyLRMcvdhVag7SS5goy0Al7_aDMhG0OgDuOlpKq= Y4Qkvys0FmS5bnVhVt20-hM$ for graphic product...

    ATTN...WFO...CLE...CTP...ILN...JKL...LWX...MRX...PBZ...RLX...
    RNK...

    ATTN...RFC...ORN...RHA...TIR...NWC...

    LAT...LON 41738049 41517924 40337887 39027941 37018106=20
    36628195 36568323 36708410 37978340 39018265=20
    40088245 40768222 41218174 41498134=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 25 01:23:06 2026
    AWUS01 KWNH 250123
    FFGMPD
    FLZ000-GAZ000-ALZ000-250630-

    Mesoscale Precipitation Discussion 0230
    NWS Weather Prediction Center College Park MD
    921 PM EDT Sun May 24 2026

    Areas affected...North Florida

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

    Valid 250120Z - 250630Z

    SUMMARY...Thunderstorms continue to develop along a trough over
    the Florida Panhandle into North Florida well into the overnight.
    Rain rates of 2 to locally 3"/hr will continue with the axis
    nearly stationary. Localized flash flooding is possible overnight.

    DISCUSSION...As of 03Z...Scattered thunderstorms continue to
    develop over the FL Panhandle with a cluster of heavy
    thunderstorms near Gainesville that continue to propagate
    northwest. Abundant Gulf moisture and instability streaming in on
    15kt southerly low level flow will continue to converge along the
    trough axis. The PW is 2.2" along this trough with SBCAPE in a
    tight gradient to low over southern GA (where there was earlier
    organized activity) to 2500 J/kg along the FL Panhandle shore and=20
    over North FL. This will continue to support activity. Earlier
    heavy rain has lowered the FFG some which will allow localized
    flash flooding.

    Recent HRRR runs are higher in QPF than the RRFS with signs that
    the Gainesville activity should work its way toward the Big Bend.

    Jackson

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Efh_Ls21fUlXmBXpher_Wht893F0JVwkO45lEwXnqPXgVUmQ01Z217okaioHo3IGhfU= ZVvnVQmhelHrCNVlqiDCP8A$ for graphic product...

    ATTN...WFO...JAX...MOB...TAE...TBW...

    ATTN...RFC...ALR...NWC...

    LAT...LON 31368501 31078366 30518230 29548194 29318252=20
    29748296 30138390 30158501 30318548 30638650=20
    31268651=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 25 03:04:26 2026
    AWUS01 KWNH 250301
    FFGMPD
    TXZ000-251300-

    Mesoscale Precipitation Discussion 0231
    NWS Weather Prediction Center College Park MD
    1100 PM EDT Sun May 24 2026

    Areas affected...Central Texas....

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

    Valid 250800Z - 251300Z

    SUMMARY...Numerous very intense but narrow downdrafts capable of
    2"/hr rates have limited cell motions to support focused areas of
    heavy rainfall that may result in localized flash flooding.

    DISCUSSION...GOES-E WV suite depicts a very mature closed low in
    the Heart of Texas toward the northeast Hill country. At 250mb,
    the low is tilted from the 500mb center to the northwest to
    provide solid down-shear divergence aloft and broad scale ascent.
    In the low levels, proximity to the low has cyclonic convergence
    but the winds are fairly light at 5-15kts at best. However,
    originating convection across the Dallas/Fort-Worth Metro,
    supported a cold pool and associated outflow boundary that has
    remained strong enough to support convergence to activate updrafts
    along the leading edge.

    RAP analysis notes that capping is starting to win out with loss
    of heating, yet a small pocket of conditionally unstable air with
    CAPE values in the 1500 J/kg range from Runnels to Bell/N Burnett
    county. Deep layer moisture (including through the typically
    drier 700-500mb layer, as noted in CIRA LPW) is aligned to support
    1.5" total PWats. As such, the favorable broad scale ascent and
    the outflow are supporting numerous narrow updrafts in the region,
    with solid longevity history as noted from older convection that
    had originated the boundary... so scattered updrafts of 1.5-2"/hr
    rates have lingered with near zero steering flow or limited enough
    to help for some small collisions allowing for these highly
    focused incidents of 2-3" totals in 1-2 hours.=20

    Instability should be waning through the overnight period and the
    outflow boundary should weaken as well, reducing coverage but the
    risk remains for a few more hours overnight to suggest a few
    incidents of flash flooding will remain possible especially as the
    development continues to drift into lower FFG, near the San Saba
    River Valley and the northeast Hill Country.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Y3YR0tiPwDJDIw6tLQAvXTnBSxF3Qbu5O-7weB15ga5P3ED2ARACzG3X3s98imAx0yU= KbualKBgssB2SpQgHlIeb7I$ for graphic product...

    ATTN...WFO...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32439886 32419838 32279789 31949754 31399750=20
    31049781 30909829 30919879 31059917 31369949=20
    31789957 32179934=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 25 09:35:55 2026
    AWUS01 KWNH 250935
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-251500-

    Mesoscale Precipitation Discussion 0232
    NWS Weather Prediction Center College Park MD
    534 AM EDT Mon May 25 2026

    Areas affected...Southeast Louisiana...Southern
    Mississippi...Southern Alabama...Western FL Panhandle...

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

    Valid 250935Z - 251500Z

    SUMMARY...Intense, slow moving thunderstorms capable of 2-3"/hr
    rates crossing saturated grounds may result in localized rapid
    inundation flooding through early morning.=20

    DISCUSSION...A very favorable mid to upper level dynamics pattern
    continues to reside across the Central Gulf Coast region this
    morning with ample warm/moist low-level moisture to support highly
    efficient deep warm cloud showers and thunderstorms. GOES-E WV
    suite shows a deep layer, nearly stacked closed low over central
    Texas with an impressive anticyclonically curved upper-level
    cirrus across the Lower Mississippi Valley indicative of right
    entrance but also diffluent right quadrant jet ascent pattern in
    advance of a potent shortwave feature lifting north along 90W.=20
    This provides multiple favorable upper-level features for broad
    scale ascent but also effective evacuation for shower/thunderstorm
    activity to develop organized convective clusters/bands through
    this morning.

    There will be a more than sufficient deep moisture pool supported
    by early morning Gulf 'exhalation' of surface latent heat to
    provide surface warming/low level profile saturation to enhance
    instability given mostly narrow, skinny profiles with lapse rates
    below 6C/km; still with 12-13Kft of warm profile and stacked
    moisture plumes per CIRA LPW layers supporting 2"+ Total PWat
    values. So, currently the MLCAPEs are sufficient for 1000-1500
    J/kg, efficient warm cloud, heavy rainfall production.

    Moisture flux convergence will be increasing with low level backed
    easterly to southeasterly flow off the warm north-central Gulf,
    while quickly veering to the south and southeast above the surface
    to 700mb. The deep layer convergence will further aid rainfall
    production with moderately wide updrafts being capable of
    2-2.5"/hr rates, though may occasionally uptick to 3", especially
    near coasts where frictional convergence can support
    back-building/regenerative flanking development. Further east
    across Mobile Bay to W FL, the activity may be a bit less in
    coverage given more easterly low level flow reducing that
    frictional support compared to SE LA into S MS.

    Residency is a bit more uncertain, but deep layer flow in
    proximity to the south to north passing shortwave should support
    some repeating/training elements, so spots of 3-5" are probable,
    with a solid suite of Hi-Res CAMS hinting at some isolated spot or
    two of greater than 7". While most of the area is sandy or swampy
    in nature, recent heavy rainfall has fairly saturated the upper
    soils with 0-40 cm ratios over 70% with some spots over 80%; so
    way over the 95-97th percentiles (spots at maximum). As such,
    infiltration even at 'normal' intensities (1.5-1.75"/hr) could
    result in rapid inundation flooding. While the entire area of
    concern is clearly not likely to experience flash flooding, there
    are many locations that will, with some isolated to widely
    scattered considerable flash flooding possible especially if
    aligned with the urban centers, like NOLA or the MS coastal towns.
    As such, flash flooding is considered likely for this MPD through
    15z.



    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8JZZzdAB8ExsIMjG_ep-LcRdmT_dBYdbZvCN3Oe8qD2n3ue02-Zp6TeMKA1qwpjoNZbb= 87co7tB1gSmQBJ1tsxdgBOo$ for graphic product...

    ATTN...WFO...JAN...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 31698881 31658796 31438735 30858679 30418662=20
    30278711 30148774 30068863 29258893 28868916=20
    29048984 28959102 29959086 30849031 31498974=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 25 12:46:44 2026
    AWUS01 KWNH 251246
    FFGMPD
    TXZ000-251645-

    Mesoscale Precipitation Discussion 0233
    NWS Weather Prediction Center College Park MD
    845 AM EDT Mon May 25 2026

    Areas affected...central TX

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

    Valid 251244Z - 251645Z

    SUMMARY...Isolated flash flooding will be possible across portions
    of central TX with slow moving showers/thunderstorms. Hourly
    rainfall of 1 to 2 inches (locally higher possible) and totals of
    2 to 4+ inches are expected through 16Z to 17Z.

    DISCUSSION...1220Z radar imagery showed a remnant MCV located
    between Comanche and Eastland, TX with convection that continued
    to regenerate over Coleman, Brown, Callahan and Eastland counties.
    Elevated instability of 500-1000 J/kg was estimated via RAP
    analysis data to exist within a narrow corridor just southwest of
    the MCV circulation with low level southerly flow allowing the
    advection of instability northward, into the western half of the
    MCV circulation, helping to feed the renewed development of
    thunderstorms. Flow aloft was modestly divergent and diffluent,
    helping to support lift over the region. A slow westward drift of
    the MCV is forecast by the RAP through 18Z which will likely
    continue to support localized slow moving cores of heavy rain
    (5-15 kt motions) capable of producing 1 to 2 inches of rain in an
    hour (locally higher). Additional rainfall totals of 2 to 4+
    inches are expected through 16 to 17Z at which point, daytime
    heating and deepening of the boundary layer may act to disrupt the
    ongoing activity.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5xztdNf3NdPkqFbN0Pv7JvqYj3HAy7zPrQTEqT6YjuEgj_VqSP5oyE5T_q-XqyGJgK7F= 9TB22crcmUC8MINV6C-SMPw$ for graphic product...

    ATTN...WFO...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32989917 32509854 31919827 31499839 31089874=20
    31069960 31949999 32759978=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 25 15:19:59 2026
    AWUS01 KWNH 251519
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-252100-

    Mesoscale Precipitation Discussion 0234
    NWS Weather Prediction Center College Park MD
    1118 AM EDT Mon May 25 2026

    Areas affected...central Gulf Coast into eastern MS/western AL

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

    Valid 251518Z - 252100Z

    SUMMARY...At least localized areas of flash flooding will be
    likely across portions of the central Gulf Coast into eastern MS
    and western AL through 21Z. Areas of training thunderstorms will
    be capable of 2 to 3 in/hr rainfall and given saturated soils,
    areas of flash flooding are expected through the remainder of the
    morning into the afternoon.

    DISCUSSION...Regional radar imagery at 15Z helped identify a
    couple of MCVs within an area of scattered thunderstorms extending
    from southeastern LA, southern MS and the western FL Panhandle,
    northward into eastern MS and western AL. The environment was
    represented by 12Z soundings from LIX and JAN (along with 14Z SPC
    mesoanalysis data) showed MLCAPE of ~500 to 1000 J/kg along with
    PWs near 2 inches. Ascent across the larger scale environment was
    favorable for heavy rain with low level flow sandwiched between a
    700-500 mb low over eastern TX and a ridge off of the southeastern
    U.S., located beneath the divergent right-entrance region of an
    upper level jet positioned over the lower MS and lower OH Valleys.

    There is currently a relative minimum in MLCAPE over central to
    northern MS which should limit rainfall intensities with northward
    extent but pockets of higher MLCAPE exist to the south and east
    (into western AL). In addition, areas of increasing instability
    will be possible through some degree of surface heating among
    areas of thick cloud cover, supportive of intense rainfall via
    dominant warm rain processes. N to NNE movement of the two MCVs
    will continue as well as additional thunderstorms approaching from
    the northern Gulf with potential for MCV development. Areas of
    training are expected with high hourly rainfall of 2 to 3 inches
    at times. These high rain rates along with mostly saturated soils
    due to rainfall over the past week will likely allow for at least
    isolated areas of flash flooding through 21Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_djEPrzdmxZ8H-zvzUY2jrIMdPGkkiyW6lA-eGZhyLu3YWMfAUYPJrvUE5YfYuRjF56c= d-CAYqgx8EeSYhhGntfA0Ac$ for graphic product...

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

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 33968788 33608737 32798698 31738695 30298720=20
    29428788 28768897 28839023 30079032 31798989=20
    32438966 33888885=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 25 17:48:15 2026
    AWUS01 KWNH 251748
    FFGMPD
    TXZ000-252315-

    Mesoscale Precipitation Discussion 0235
    NWS Weather Prediction Center College Park MD
    147 PM EDT Mon May 25 2026

    Areas affected...central to western TX

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

    Valid 251745Z - 252315Z

    SUMMARY...Isolated to widely scattered flash flooding will be
    possible through 23Z across parts of central to western TX. Slow
    moving thunderstorms will be capable of producing hourly rainfall
    of 1 to 2+ inches along with totals of 2 to 4+ inches.

    DISCUSSION...Visible satellite imagery from 1720Z showed a field
    of deepening cumulus clouds over portions of the Edwards Plateau,
    northwestward into the Rolling Plains region of west-central TX.
    Cloud streets identified confluent low level flow into the region,
    located west of a remnant MCV located roughly 40 miles east of
    Brownwood. A lack of cumulus inferred stability near the MCV
    center from prior rainfall, but estimated MLCAPE of 1000-2000 J/kg
    was shown via the 17Z SPC mesoanalysis amid weakly anomalous PW
    values over central to western TX.

    Thunderstorm coverage is expected to increase through the
    remainder of the afternoon to the southwest and west of the slow
    moving (nearly stationary) MCV with some component of left-exit
    region upper level divergence aiding with broader scale ascent
    across central TX. The greatest concern for isolated to widely
    scattered flash flood coverage through 23Z is with slow movement
    of cells (5-15 kt) coupled with portions of the state that have
    picked up 300 to 600 percent of normal rainfall over the past
    week. Slow cell motions will likely yield hourly rainfall of 1 to
    2 inches (locally higher) which may result in isolated totals of 2
    to 4+ inches. Local runoff sensitivities of the Hill Country and
    possibly as far east as I-35 near San Antonio are also
    considerations into the afternoon.=20

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6yWpBt9U5fD3K9mNbvCfvsFn4cJ4wr-N3sjqGqu6sRDlWZmItqaZgNzRvksxeraZstgl= 76yHsj8Hy6CvenkR4FwUeS4$ for graphic product...

    ATTN...WFO...EWX...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32890077 31909993 30899845 29999804 29359854=20
    29490010 30240156 31280221 32230221 32880173=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 25 18:59:22 2026
    AWUS01 KWNH 251859
    FFGMPD
    AZZ000-260045-

    Mesoscale Precipitation Discussion 0236
    NWS Weather Prediction Center College Park MD
    257 PM EDT Mon May 25 2026

    Areas affected...Central and Northern Arizona

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

    Valid 251857Z - 260045Z

    SUMMARY...Slow-moving, pulse-type convection driven by an
    upper-level low will produce localized but occasional intense
    rainfall rates. While regional soils are exceptionally dry, these
    intense rates over steep terrain, locally hydrophobic soils, and
    potential burn scars will make highly localized flash flooding
    possible through this evening.

    DISCUSSION...Regional radar and GOES-West WV imagery this
    afternoon depict a relatively moist and unstable environment
    across central and northern Arizona, driven by a slow-moving
    upper-level low. The cold core associated with this upper low has
    established steep mid-level lapse rates. Despite a dry sub-cloud
    layer, continued surface heating has yielded SBCAPE values in the
    1000-1500 J/kg range. Concurrently, a somewhat anomalous moisture
    plume has pushed PWATs to around 0.75 inches which is more than
    sufficient for locally heavy rainfall rates when combined with the
    instability across this high-elevation environment.

    Given the proximity of the upper low, the kinematic environment is characterized by very weak effective bulk shear (generally <20
    kts) and weak deep-layer mean steering flow. This is resulting in
    a pulse convective mode with nearly stationary or erratic,
    slow-moving cells. Recent MRMS data indicates these cells are
    somewhat efficient after initially moistening the column, and are
    dropping 0.25 to 0.50 inches of rain in 15-minute intervals
    (equivalent to 1-2 in/hr rates) before the updrafts collapse. The
    12Z HREF/REFS guidance highlights a 20-30 percent probability of
    exceeding local Flash Flood Guidance (FFG) and 1 in/hr rates, with
    a few HREF members suggesting localized totals could approach or
    exceed 2 inches where cells anchor or merge.

    While NASA SPoRT soil moisture and USGS streamflow data indicate
    the region is exceptionally dry, the desert environment in this
    region is highly sensitive to short-duration, high-intensity
    rainfall. The baked, rocky terrain will tend to promote enhanced
    runoff with these higher rainfall rates. The flash flood threat
    will be notably isolated, but rather acutely focused on normally
    dry arroyos, slot canyons, and steep terrain along or near the
    Mogollon Rim. Furthermore, any stationary cores that develop over
    recent burn scars will carry a risk for debris flows and channel
    runoff.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9Z0ytRndCSgoeOo8m_k2qFUhQ2f-yoYzHuLybsphvRaLsm3FOZjaEx4UpC_2xRQUvSp3= 59y3695oDF01uBWybj8A6Lo$ for graphic product...

    ATTN...WFO...FGZ...PSR...TWC...VEF...

    ATTN...RFC...STR...NWC...

    LAT...LON 36601203 35841076 34761005 33610997 33171079=20
    33821223 34191327 35001403 35871416 36531349=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 25 19:55:28 2026
    AWUS01 KWNH 251955
    FFGMPD
    NCZ000-SCZ000-GAZ000-TNZ000-ALZ000-260145-

    Mesoscale Precipitation Discussion 0237
    NWS Weather Prediction Center College Park MD
    353 PM EDT Mon May 25 2026

    Areas affected...Northeast Alabama...Central and Northern
    Georgia...Central and Upstate South Carolina

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

    Valid 251953Z - 260145Z

    SUMMARY...Deep convection will continue to expand in coverage and
    intensity this afternoon and evening, driven by a surface boundary
    across Georgia/South Carolina and a northward-lifting MCV over
    Alabama. Intense rainfall rates exceeding 2 in/hr, coupled with
    relatively slow storm motions and highly sensitive urban
    corridors, will make flash flooding likely.

    DISCUSSION...Regional radar and satellite imagery this afternoon
    highlights an expanding footprint of deep convection across the
    interior Southeast. Across west-central Georgia through central
    South Carolina, activity is focusing along a surface trough and
    pronounced instability gradient. Further west, a well-defined MCV
    is noted over central AL in visible satellite images steadily
    lifting northward.

    The mesoscale environment ahead of both of these forcing
    mechanisms is highly favorable for extreme rainfall efficiency.
    The airmass is characterized by pooling PWATs of 1.8 to 2.0 inches
    and MLCAPE values surging into the 1500-2500 J/kg range in the
    warm sector. Shear is rather modest with effective bulk shear
    generally 20 to 30 kts at best, so much of the convective threat
    will tend to remain rather disorganized. Regardless, the pulse and
    localized multicell convection will be capable of high rainfall
    rates approaching or exceeding 2 in/hr which has already been
    confirmed with recent MRMS data.

    Given the high rainfall rates and presence of weak steering flow,
    there will likely be additional areas of convective persistence
    that will support scattered areas of excessive rainfall. The
    latest HREF and REFS guidance suggests additional pockets of 2 to
    4+ inch rainfall totals going through this evening.

    NASA SPoRT soil moisture data and USGS streamflow analyses suggest
    areas of sensitivity from recent rainfall, and these additional
    rains this afternoon and this evening will promote concerns for
    runoff issues. Scattered areas of flash flooding will tend to be
    likely, and this will also include concerns by this evening around
    the Atlantic metropolitan area.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4EgtUFe52QEX3VP6WsJj9zairWX8Fws5uI6et4v-hMOWC6et8UFG-dcq0hLQ25MJF1t_= g4Rx2VhG9_k1aEn7tnShd3E$ for graphic product...

    ATTN...WFO...BMX...CAE...CHS...FFC...GSP...HUN...MRX...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 35118486 34998426 34778347 34778274 34618183=20
    34318120 33538120 32908155 32378229 32298323=20
    32438402 32738471 33308560 33518618 33808686=20
    34258708 34778689 35068602=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 25 20:49:35 2026
    AWUS01 KWNH 252049
    FFGMPD
    FLZ000-TNZ000-ALZ000-MSZ000-260245-

    Mesoscale Precipitation Discussion 0238
    NWS Weather Prediction Center College Park MD
    447 PM EDT Mon May 25 2026

    Areas affected...Mississippi...Alabama...Florida Panhandle

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

    Valid 252047Z - 260245Z

    SUMMARY...Multiple Mesoscale Convective Vortices (MCVs) embedded
    within a deep tropical airmass will continue to drive rounds of
    heavy showers and thunderstorms through this evening. Intense
    rainfall rates of 2 to 3 in/hr, combined with wet antecedent
    conditions and cell-training concerns, will result in localized
    additional totals of 3 to 5 inches. Flash flooding is likely.

    DISCUSSION...Regional radar and satellite imagery late this
    afternoon show widespread, deep convection persisting across
    sizable areas of Mississippi, Alabama, and the Florida Panhandle.
    The mesoscale environment remains exceptionally favorable for
    highly efficient, tropical-like rainfall production. Recent RAP
    mesoanalysis indicates PWAT values ranging from 1.8 to over 2.1
    inches pooling along and inland of the Gulf Coast, juxtaposed with
    a broad axis of 1000-2000 J/kg of MLCAPE. This is fostering a deep
    warm cloud layer capable of sustaining extreme rainfall rates,
    which recent MRMS data confirms are occasionally reaching 2 to 3
    in/hr.

    The kinematic forcing is being driven by multiple compact MCVs
    lifting northward through the deep-layer southerly flow. A
    persistent axis of moisture transport and convergence is
    continuously feeding these features. The presence of these
    boundaries, combined with relatively weak upwind propagation
    vectors, is heavily favoring periods of backbuilding and
    cell-training.

    Going through the evening hours, the latest high-resolution
    ensemble guidance (including the HREF and REFS), as well as recent
    HRRR and RRFS iterations, are in strong agreement that portions of
    this convective axis will be maintained. The CAM consensus
    suggests additional localized rainfall totals of 3 to 5+ inches
    are likely wherever training bands anchor. Given the wet
    antecedent conditions and lowering Flash Flood Guidance (FFG)
    across the region, this additional intense rainfall will likely
    favor additional regional concerns for flash flooding. A localized
    instance or two of significant flash flooding cannot be ruled out
    if some of these rains anchor over the more sensitive urban areas.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4jTEwZrlWt1QNdginnGSyxpxeA8gazGmcZIBu2sFIT7X1o6PYIpbyzs4qD3dkl_yfNyu= ifRl3i27V8J8qArZbiP-7YY$ for graphic product...

    ATTN...WFO...BMX...HUN...JAN...MEG...MOB...OHX...TAE...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 35198758 34788670 34078624 32478551 31188528=20
    30008551 29728635 30078754 30548794 31428834=20
    32058886 33318963 34008972 34678934 35168843=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 25 21:28:09 2026
    AWUS01 KWNH 252128
    FFGMPD
    VAZ000-NCZ000-TNZ000-260325-

    Mesoscale Precipitation Discussion 0239
    NWS Weather Prediction Center College Park MD
    526 PM EDT Mon May 25 2026

    Areas affected...Western North Carolina...South-Central to
    Southeast Virginia

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

    Valid 252126Z - 260325Z

    SUMMARY...Heavy showers and thunderstorms will continue to impact
    south-central and southeast Virginia, while new convection
    develops across western North Carolina this evening ahead of a
    slow-moving cold front. Intense rainfall rates of 2 to 3 in/hr,
    combined with some cell-training, will yield localized totals of 3
    to 5 inches. Extreme rainfall rates may overpower dry antecedent
    soils, making flash flooding likely which will include urban
    corridors.

    DISCUSSION...Late-day satellite and radar imagery depicts an axis
    of intense, and locally training convection currently impacting
    portions of south-central and southeast Virginia, including the
    sensitive I-64 corridor from Richmond down through Hampton Roads.
    This activity is tapping into a deeply anomalous, tropical-like
    airmass characterized by PWATs pooling between 1.8 and 2.0 inches
    and MLCAPE values of 1000-1500 J/kg. The immediate forcing over
    this Virginia corridor is being driven by a stacked, high-end
    couplet of strong 850mb convergence and 250mb divergence.

    Further southwest, an upstream cold front approaching slowly from
    the northwest will interact with this same unstable, moisture-rich
    airmass going through the evening hours. This will trigger a
    separate and potentially focused area of convection across the
    Piedmont region of western North Carolina.

    Kinematically, the environment across both target areas is primed
    for organized, repeating rounds of heavy rainfall. Effective bulk
    shear of 25 to 35 kts will maintain persistent multicell clusters,
    while upwind propagation vectors oriented parallel to the
    respective forcing boundaries will strongly favor cell-training.
    The deep warm cloud depths will support highly efficient rainfall
    rates of 2 to 3 in/hr. Consequently, the 18Z high-resolution
    ensemble suite (HREF and REFS) strongly supports localized
    rainfall totals of 3 to 5 inches through the evening.

    While recent soil moisture data indicates dry antecedent
    conditions across portions of the Mid-Atlantic, rainfall rates of
    2 to 3 in/hr will likely exceed the maximum infiltration capacity
    of the soils, resulting in potential for rapid runoff. The flash
    flood threat is currently highest across the low-lying, densely
    populated urban footprint of south-central and southeast Virginia,
    but will concurrently increase across some of the Piedmont areas
    of western North Carolina as the frontal boundary approaches
    tonight.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_KRj4u6Q8wMtfB_QElWVybn108hHZT4bvXUNkuCeg2dZFejvW_LK8PqdYhXCtP1XtIkp= 7D7J9nv5gRq3nkD9_tjVaG8$ for graphic product...

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

    ATTN...RFC...ALR...ORN...RHA...TIR...NWC...

    LAT...LON 38097699 37837609 37297578 36817594 36567658=20
    36367791 35947992 35328163 35208272 35558286=20
    35948237 36278181 36708069 37187958 37837819=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon May 25 22:12:47 2026
    AWUS01 KWNH 252212
    FFGMPD
    TXZ000-260230-

    Mesoscale Precipitation Discussion 0240
    NWS Weather Prediction Center College Park MD
    611 PM EDT Mon May 25 2026

    Areas affected...Central Texas

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

    Valid 252211Z - 260230Z

    SUMMARY...A compact, slow-moving Mesoscale Convective Vortex (MCV)
    will continue to trigger scattered thunderstorms into this
    evening. Weak steering flow will lead to slow storm motions and
    localized rainfall rates of 1 to 2 in/hr. While coverage remains
    limited, this activity will make highly localized, primarily urban
    flash flooding possible.

    DISCUSSION...Late-day GOES-E visible satellite imagery along with
    radar depicts scattered, slow-moving thunderstorms continuing to
    initiate across north-central into central Texas. This activity is
    being driven by a stubborn, compact 500mb MCV currently spinning
    over the region. The mesoscale environment is characterized by
    pooling deep-layer moisture (PWATs of 1.5 to 1.7 inches)
    juxtaposed with moderate to strong instability (MLCAPE values of
    1500-2500+ J/kg).

    While the thermodynamic environment is supportive of efficient
    rainfall, the primary driver of the flash flood threat is the
    kinematic profile. Effective bulk shear is exceptionally weak
    (generally under 20 kts), and upwind propagation vectors are
    nearly zero. Consequently, any initiated updrafts are exhibiting
    very slow, erratic motions. Recent MRMS data indicates these
    nearly stationary cores are successfully producing localized
    rainfall rates of 1 to 2 in/hr.

    Despite the favorable mesoscale setup for heavy rain, overall
    convective coverage remains relatively limited, and
    high-resolution guidance suggests some uncertainty regarding how
    far into the evening hours this activity will persist before
    diurnal stabilization takes over. However, given the trajectory of
    the MCV, the convective footprint encompasses the sensitive
    Dallas-Fort Worth metropolitan area on down through Waco and
    Austin. At least eastern portions of the rocky, runoff-prone
    terrain of the Hill Country are also included in the threat area.
    Therefore, while widespread issues are not anticipated, isolated
    instances of flash flooding remain possible through the
    mid-to-late evening hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6IaTPwDXvDK6JTj3RYxDje9CGvQ0WIt4k-mDctHEHhpGFndDR3ZRfnHabf3cPfaQQfV9= gkUhLFcnYDcYtoB_gQuvqno$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 33359722 32419631 31329612 30359669 29809787=20
    29789869 30269905 31069825 31809806 32569831=20
    33259815=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 26 01:05:01 2026
    AWUS01 KWNH 260104
    FFGMPD
    NCZ000-SCZ000-GAZ000-TNZ000-ALZ000-MSZ000-260700-

    Mesoscale Precipitation Discussion 0241
    NWS Weather Prediction Center College Park MD
    903 PM EDT Mon May 25 2026

    Areas affected...Northern Alabama...Middle and Southeast
    Tennessee...Northern Georgia...Far Upstate South
    Carolina...Western North Carolina

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

    Valid 260103Z - 260700Z

    SUMMARY...Efficient showers and thunderstorms will continue to
    track across northern Alabama and into the complex terrain of the
    southern Appalachians tonight. Forcing from a nearby synoptic
    front and a translating MCV, combined with deep moisture, will
    support rainfall rates of 1 to 2+ in/hr. Localized additional
    totals of 2 to 4+ inches will make flash flooding likely.

    DISCUSSION...Early-evening GOES-E IR satellite and regional radar
    data shows an axis of highly efficient convection moving across
    the southern Appalachians, intersecting portions of southeast
    Tennessee, northern Georgia, and the western Carolinas. Further
    west, a distinct Mesoscale Convective Vortex (MCV) positioned
    along the AL/MS border continues to drive heavy rainfall across
    northwest Alabama. Through the late evening hours, the forcing
    associated with this MCV is expected to translate northeastward
    across far northern Alabama and middle Tennessee, generally
    merging with the ongoing convective threat over the higher terrain
    of the Cumberland Plateau and southern Appalachians.

    The mesoscale environment remains highly supportive of heavy,
    sustained rainfall. A synoptic-scale front draped across the
    region is interacting with 500 to 1000 J/kg of lingering MLCAPE,
    providing continuous fuel to sustain the convective threat. This
    is occurring within a deep tropical airmass characterized by
    Precipitable Water (PWAT) values of 1.75 to 2.0 inches.
    Furthermore, strong large-scale ascent is being provided by a
    stacked couplet of 850mb convergence and 250mb divergence centered
    over the region.

    As the convection tracks generally northeastward, low-level flow
    vectors are oriented to provide modest but persistent upslope
    ascent into the higher terrain of the Cumberland Plateau and Blue
    Ridge Mountains. This orographic forcing, combined with the deep
    warm cloud layer and the synoptic/MCV lift, is yielding highly
    efficient rainfall rates of 1 to 2 in/hr.

    The latest high-resolution guidance (including recent HRRR
    iterations) suggests that these intense rates will persist over
    the next several hours, capable of depositing localized additional
    rainfall totals of 2 to 4+ inches. Given the steep topography,
    flashy nature of the local basins, and wet antecedent conditions,
    rapid runoff is expected. Areas of flash flooding are already
    ongoing, and additional flash flooding is expected over the next
    several hours which will include rapid rises on small creeks,
    streams, and low-water crossings.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5T5-tBUse90iIR8cAVDePjIh0Zu0ljH8pr00Wf99SAlbt0bovSxKulXsCvO9NuuEFdHx= wjsyULM0p6TK3s9fqZyFvR0$ for graphic product...

    ATTN...WFO...BMX...FFC...GSP...HUN...MEG...MRX...OHX...RNK...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 36328158 35768116 35158196 34768288 34408398=20
    34108582 33718729 33878791 34268819 34908797=20
    35248721 35538594 35648481 35938352 36208256=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 26 02:02:08 2026
    AWUS01 KWNH 260202
    FFGMPD
    SCZ000-FLZ000-GAZ000-260700-

    Mesoscale Precipitation Discussion 0242
    NWS Weather Prediction Center College Park MD
    1000 PM EDT Mon May 25 2026

    Areas affected...Northern Florida...Eastern Georgia...Central
    South Carolina...

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

    Valid 260200Z - 260700Z

    SUMMARY...Slow moving,back-building potential within very deep
    moisture environment pose spots of 2-4" and possible widely
    scattered incident or two of flash flooding.

    DISCUSSION...CIRA LPW suite especially in the sfc to 700mb layers
    shows a dual streams of confluence from the central Gulf into the
    Northeast Gulf melding across the northern neck of Florida into
    southeast GA, resulting in a plume of 2-2.25" total PWats with
    solid deep layer convergence. Also, lower profiles show
    sufficient heating for narrow skinny profiles and a wedge of
    remaining 1500 J/kg. Aloft, anticyclonic curved right entrance of
    upper level jet is also providing solid divergence aloft along the
    confluence axis to help maintain updrafts. The deep layer
    confluence does have some split above 700mb to allow for some weak
    DPVA ascent to compliment the divergence aloft but given the
    oblique nature at the far eastern influence of the closed
    upper-low over Texas. As such, thunderstorm activity with
    15-25kts of upstream speed max at 850mb, supports potential for
    back-building, especially further south and likely to support
    2-2.5"/hr rates.=20=20

    With weak inflow, cell motions will also be diminished allowing
    for greater residency time and highly focused but widely scattered
    incidents of 2-4" totals. Sandy conditions across N FL into GA
    have naturally higher FFG, but recent repeating days of convection
    has lead to an increase in 0-40cm soil moisture values per NASA
    SPoRT, as such; given these rates, a few incidents of
    focused/localized flash flooding are considered possible.

    While the moisture flux is reduced further north, the Piedmont of
    SC has seen Total PWats up to 2.25" as well, and with slightly
    deflected low level flow responding to the upper-level ridge aloft
    and jet entrance to the northeast; a similar convective
    environment/potential exists as well. The main difference is the
    naturally lower FFG and prone areas along the Fall-line in central
    SC, so even with less rainfall rates/potential than further south,
    the hydrology will be easier to exceed given the moisture
    availability.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8mQciNTb-G1-PUEUKuF1u8CSN3ePK5WYz5ABJeJy2W46RextCdQHU5rnAfQyUgMIgStx= KLx_dLBYWOj5kGNQFI30Vaw$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...JAX...

    ATTN...RFC...ALR...NWC...

    LAT...LON 34508120 34268053 33018137 31938176 31008181=20
    29928183 29918258 31708291 32478299 33288286=20
    33958197=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 26 02:48:41 2026
    AWUS01 KWNH 260248
    FFGMPD
    TXZ000-NMZ000-260830-

    Mesoscale Precipitation Discussion 0243
    NWS Weather Prediction Center College Park MD
    1047 PM EDT Mon May 25 2026

    Areas affected...Southeast New Mexico...Western Texas Cap Rock...

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

    Valid 260245Z - 260830Z

    SUMMARY...Strong moisture flux convergence will support up to
    1.5"/hr rates with slowly advancing convective complex. Localized
    totals of 2-3" may produce localized flash flooding conditions
    overnight.

    DISCUSSION...GOES-E WV shows the larger scale closed low over the
    San Francisco Plateau of northern Arizona with broad/strong
    southwesterly flow along the southern periphery. Embedded within
    the weakly negative tilt trough is a tight vorticity/shortwave
    center that is well depicted in both WV and regional RADAR suite
    in the Rio Grande Valley near KHMN. The speed shear and vorticity
    is providing a strong upslope component along the lee of the
    Sacramento Mtns with a pair of surface low near Roswell and
    Carlsbad, with both having very high directional convergence along
    it (with northerly winds from NE NM and strong SE winds across the
    Pecos River Valley). Surface to boundary layer moisture is
    limited to mid to upper 40s Tds, but the CIRA LPW shows pool of
    enhanced banked up moisture in two lowest layers (850-700,
    700-500mb layers) providing total PWats into the 1" range
    currently. However, the strength of low-level flux through the
    Pecos Valley will be increasing throughout the early overnight
    period.=20

    Given the strong dynamics aloft and very convergent low levels,
    moisture flux is starting to support 1.25-1.5"/hr rates, given
    10.3um EIR shows complex cooling to -65C to -70C. As such, a
    convective complex is maturing over eastern and southeastern NM;
    with initial convective cells upscaling and merging into larger
    clusters and eventually a complex over the next few hours. This
    should allow for increased residency time and an area of 2-3"
    totals can be expected.

    Very dry/hard grounds with naturally high FFG values may help to
    mitigate broader flash flooding conditions, but given the
    intensity with localized bursts during mergers, localized flash
    flooding conditions may arise though the evening. Eventually a
    cold pool should develop and the complex should start to advance
    eastward, likely quickly given very strong propagation vectors
    given increasing east-southeast surface to 850mb flow over 40kts,
    so potential will diminish with time.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4fgCMyy8vR0xzYHXBC1an4ca8CQbZrr1azdB1mxEaW-d3yoN7MDlvuwc6YyedyuSuo4H= P4yo_9ImXhMmtXY3E1UFUIc$ for graphic product...

    ATTN...WFO...ABQ...LUB...MAF...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35390454 35270374 34760308 33980244 32760234=20
    31960297 31980411 32440459 33070493 33400507=20
    34280521 35070504=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 26 03:32:18 2026
    AWUS01 KWNH 260332
    FFGMPD
    TXZ000-NMZ000-260900-

    Mesoscale Precipitation Discussion 0244
    NWS Weather Prediction Center College Park MD
    1131 PM EDT Mon May 25 2026

    Areas affected...Western Texas Panhandle...Pecos River Valley...

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

    Valid 260330Z - 260900Z

    SUMMARY...Fast moving, but increasing intense rainfall rates with
    Sub-hourly totals of 1", resulting in quick run-off and possible
    localized flash flooding incident or two overnight.

    DISCUSSION...GOES-E 10.3um EIR denotes a expanding line of
    scattered thunderstorms increasing/cooling across the central
    portion of the Western Texas Panhandle spurred on by rapid
    height-falls from an ejecting shortwave in south-central NM within
    a broader base of the large scale trough centered in N AZ. The
    broad southwesterly flow crossing terrain has resulted in a very
    strong lee-pressure trough across much of eastern NM to a surface
    low near ROW; however, behind the main S/W lifting out, the
    surface trough then angles southwest into Hudspeth county and
    northern Chihuahua denoted well by some low-level warmer topped
    agitated Cu/Tcu.=20

    Strong response in the low-levels with up-slope winds steadily
    increasing past 30kts on their way to 40kts is helping convective initiation/development two fold. The initial is the strong mass
    convergence that extends along the entire surface trough to break
    out these scattered cells, the second is increasing moisture
    transport, Tds has steadily increased into the low 50s, but low
    60s and sfc-850mb LPW (up to .75") is coming up the Rio Grande and
    Pecos River Valleys to intersect the initial convective round.=20
    Not surprisingly given proximity to the elevated desert plateau,
    steep lapse rates are supporting increasing instability values as
    the higher theta-E air pushes in to allow for strong vigor of
    updrafts and moistening the columns. Currently rates are minimal
    due to evaporative loss, but as the overall moisture arrives, flux
    convergence will support intense rainfall rates capable of
    .5-.75"/15 minutes (per HRRR). While forward propagation will be
    equally fast and reduce overall totals, localized spots of 1.5"
    are possible in about 1hr and the harder ground conditions will be
    difficult for infiltration at those rates suggesting localized
    flash flooding is possible tonight.

    While a bit less certain, there are suggestions, given strong
    southwesterly flow and embedded mid-level impulses and expected
    limited eastward movement of the surface trough, additional
    development may be possible to allow for a secondary round to
    occur later in the period, with best potential further north along
    the TX/NM east-west boarder. Will continue to monitor those
    trends for any subsequent MPD necessity.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9FNM9rT40AmTjVu5cmW52AF9sGiR5_3d2Of1w2kKCglVD0tRAxRvfMMl-jWI1Or9gwXh= RsRIcxYae3EMWh1O5hqfY6c$ for graphic product...

    ATTN...WFO...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32340317 32170238 31690186 30950168 29930199=20
    29640258 29250280 28960324 29300415 29730461=20
    30450487 30810489 31600479 32050416=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 26 04:20:18 2026
    AWUS01 KWNH 260420
    FFGMPD
    FLZ000-GAZ000-ALZ000-260900-

    Mesoscale Precipitation Discussion 0245
    NWS Weather Prediction Center College Park MD
    1219 AM EDT Tue May 26 2026

    Areas affected...Western GA...Central FL Panhandle...Far Eastern
    AL...

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

    Valid 260420Z - 260900Z

    SUMMARY...A few more hours of potential training, highly efficient
    convection capable of 2.5"/hr and a streak or two of 2-4" totals
    resulting in possible localized flash flooding.

    DISCUSSION...Regional RADAR and 10.3um EIR from GOES-E continue to
    show flare-ups of convection along the eastern edge of the warm
    conveyor belt which appears to be at the near eastern limit of
    influence from the parent larger-scale decaying closed low in
    Eastern Texas. The warm conveyor continues to pump enhanced
    moisture through a deep fairly unidirectional south to north
    stream from the east-central Gulf northward along the AL/GA line.=20
    An equally narrow axis of instability remains along the eastern
    edge of the q-axis with solid overlap. Surface easterly flow has
    recently intersected the north-south boundary and new convection
    has developed along it. Given upstream elongated vorticity
    strip/shortwave over the north-central Gulf lifting north,
    combined with weak to moderate divergence at the entrance to the
    northeastward angling upper-level jet streak across the southern
    Appalachians, will help to maintain any of these localized low
    level convergence maxima that spark another round of convection;
    this included southerly frictional convergence at the Gulf/Florida
    Panhandle interface, especially as the sfc convergence retrogrades
    west deeper into the q-axis.=20=20

    Total PWat values of 2-2.25" and narrow skinny CAPE profiles (up
    to 1500 J/kg) with 20-30kts of LLJ inflow/flux convergence has and
    will likely to aid 2-2.5"/hr rates and with stronger flow off the
    Gulf, flanking line redevelopment can support back-building edges
    parallel to the deep layer steering allowing for localized 2-4"
    localized streaks. This may result in an incident or two of
    localized rapid inundation/flash flooding for prone areas and
    intersected urban centers. All in all, flash flooding is
    considered possible in an isolated to widely scattered manner
    through the overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9ekI4s4N01qIcb5We4Ud44vJvUYrxfAOp9zKbFmiR7DjkOR4jEx9_2Xddijm-z7h5JET= VsFEEAUgwV3dIf5LkCaWdr0$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 33998513 33908435 33198409 32078397 31038404=20
    29738461 30228605 31658572 32568554 33148547=20
    33788539=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 26 08:27:16 2026
    AWUS01 KWNH 260827
    FFGMPD
    TXZ000-NMZ000-261400-

    Mesoscale Precipitation Discussion 0246
    NWS Weather Prediction Center College Park MD
    426 AM EDT Tue May 26 2026

    Areas affected...Southeast New Mexico...Portions of the Cap Rock,
    Permian Basin and Trans-Pecos Regions of Texas...

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

    Valid 260830Z - 261400Z

    SUMMARY...Main cluster to maintain/enhanced through early morning
    with hourly rates of 1-1.5"/hr and additional 2-3" totals, with
    continued incidents of localized flash flooding possible.

    DISCUSSION...GOES-E WV suite depicts closed low tightening a bit
    over NE AZ with broad southwesterly flow across its southeast
    quadrant starting to lift with veering 500mb winds enhancing
    larger scale DPVA across the Rio Grande into Pecos River Valleys
    over the next few hours. This will help to broaden diffluence and
    dual jet divergence pattern across SE NM into the eastern portions
    of the W Texas Panhandle. The combination will help to
    maintain/evacuate the expanding convective cluster across SE NM
    moving into the W Texas portion of the Permian Basin.=20=20

    Low-level jet response remains strong with 30-40kts of
    southeasterly flow generally orthogonally intersecting the
    rainfall reinforced surface trof/isentropic ascent boundary that
    extends from a surface low east of Hobbs back west northwest of
    the Davis Mtns through southern Hudspeth county though surface to
    850mb flow is further backing south across the Big Bend due to
    strengthening surface to 850mb near the National Park. Tds into
    the upper 50s/lower 60s are now intersecting the boundary and
    helping to maintain the main cluster but also help to develop more
    cells upstream across W TX Panhandle over the next few hours,
    likely to track northeast and trend toward later period possible
    mergers. Total PWats at or just above 1.25" are filling in and
    rainfall rates continue to increase in efficiency ranging from
    1-1.5"/hr.=20=20

    Given the placement of the expanding complex to the split in the
    upper-level jet pattern; deep layer steering remains back-sheared
    to the north and north-northwest and likely to continue to be slow
    given the col in 500-1000mb thickness over the area. Forward
    propagation will continue slowly eastward with combination of
    strong inflow from the east, but also cold pool generation. As
    such, residency of a few hours should allow for some localized
    2-3" totals to manifest. As such, localized flash flooding
    concerns will continue to remain through the early morning.=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5IuurpHag8RebIAYrUU8nV6Xfd1UM_XunzmHQmNAiEJWQH-ZVz3eKc0ZAA228OSGh7g4= bge6gwjtFwX1azMb6B8kjgI$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...MAF...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35300296 34420154 33460106 32500121 31620182=20
    31120236 29850354 29830467 30790482 31910477=20
    32610430 33200413 34500414 35220393=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 26 13:47:18 2026
    AWUS01 KWNH 261347
    FFGMPD
    TXZ000-261945-

    Mesoscale Precipitation Discussion 0247
    NWS Weather Prediction Center College Park MD
    946 AM EDT Tue May 26 2026

    Areas affected...West Texas

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

    Valid 261345Z - 261945Z

    SUMMARY...A line of training thunderstorms across portions of west
    Texas this morning contains cells capable of 2+ inches/hour
    rainfall rates. Flash flooding is occurring resulting from these
    storms.

    DISCUSSION... An area of convection at the base of a highly
    negatively tilted trough over New Mexico has been producing 2+
    inch per hour rainfall rates across a portion of west Texas this
    morning. These storms have been slow-moving, allowing for the
    heavy rain rates to persist over the same areas for an extended
    period. At the south end of the line, much faster moving storms
    are pressing east just north of the Rio Grande in the Big Bend
    region. CAMs guidance is suggesting that once the storms to the
    south "catch up" longitudinally with the line just east of
    Midland, the whole new line of storms will take on a faster
    forward speed towards the east. This will reduce the flash
    flooding threat a bit going forward, but rainfall rates with the
    strongest cells will still pose a localized flash flooding risk
    with 1-2 inches/hour still possible.

    As the line progresses eastward towards San Angelo this afternoon,
    with daytime heating, expect multiple individual slow-moving
    thunderstorm cells capable of heavy rainfall rates to merge with
    the line. Where these mergers occur, localized flash flooding will
    be possible due to the extended period of time any heavy rain will
    occur over those areas. Many of the river valleys tend to
    efficiently convert heavy rainfall to significant river rises in
    this area, worsening any potential flash flooding. Behind the line
    of storms, cold pools and much more stable air will end the heavy
    rain and flash flooding threat.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-FAKY9L2F2kFTpx9statJZTQMKWk-a_ZTHSTWz1lq79q5OD2t7FnxJAtssbWaccWawJw= BJ0KEBURtrIVXYSH9Ks0QTI$ for graphic product...

    ATTN...WFO...EWX...LUB...MAF...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 34230074 33800026 33060002 32639985 32019952=20
    31059940 29999978 29100049 29340108 29660143=20
    29760198 29740237 29720272 29870326 30170336=20
    30450321 30750296 31110275 31770249 32570201=20
    34180164=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 26 16:05:33 2026
    AWUS01 KWNH 261605
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-262100-

    Mesoscale Precipitation Discussion 0248
    NWS Weather Prediction Center College Park MD
    1204 PM EDT Tue May 26 2026

    Areas affected...Southern Alabama and the Western Florida
    Panhandle

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

    Valid 261604Z - 262100Z

    SUMMARY...Clusters of storms are developing along the Gulf Coast
    in a pocket of maximized instability and atmospheric moisture
    content. The convection could produce rainfall rates to 3 inches
    per hour where training occurs. Flash flooding possible.

    DISCUSSION...With diurnal heating now in full swing, scattered
    strong thunderstorms have developed over the western tip of the
    Florida Peninsula, now extending into far southern Alabama. These
    storms have formed in an area of increased instability due to
    lesser prior cloud cover, as well as in a corridor of maximized
    atmospheric moisture. SPC Mesoanalysis shows PWATs to 2.2 inches
    just off the coast of Pensacola, and over 2 inches where the
    storms have formed. SBCAPE values are around 3,000 J/kg, so the
    storms have more than enough moisture instability to continue
    growing upscale into the afternoon hours.

    CAMs guidance shows the storms are likely to increase in coverage,
    taking advantage of the plentiful moisture and instability.
    Despite recent heavy rains in the area, 1-hr FFGs remain over 2
    inches for all of the highlighted area, and in some cases near the
    coast, close to 3 inches. Given those still high thresholds, flash
    flooding will generally be possible, confined to where the storms
    line up in such a way as to maximize the duration of heavy
    rainfall. Several urban areas could see those storms, in which
    case the local thresholds required to realize flash flooding will
    be lower.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8AP8n9DQBcxSaphOD6Cm_94edGMSPkg73FfwEoXwDXkip_d7Ao2vXWJa_vyK3VdCEKAk= eSTt-XmkzryxcTSEGZMqqfA$ for graphic product...

    ATTN...WFO...BMX...LIX...MOB...TAE...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 32618641 32578606 31998571 31458548 30838535=20
    30278549 30058558 30288603 30378660 30348716=20
    30198750 30178832 30238868 30148918 30358927=20
    30398927 30648930 31098900 31678871 32068818=20
    32458755=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 26 20:38:35 2026
    AWUS01 KWNH 262038
    FFGMPD
    TXZ000-270200-

    Mesoscale Precipitation Discussion 0249
    NWS Weather Prediction Center College Park MD
    437 PM EDT Tue May 26 2026

    Areas affected...central to south-central TX

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

    Valid 262035Z - 270200Z

    SUMMARY...A few widely scattered areas of flash flooding will be
    possible across the Hill Country into south-central TX through
    02Z. Hourly rainfall of 1 to 2 inches will be common but isolated
    higher values of 2 to 3 inches will also be possible.

    DISCUSSION...Regional radar imagery over west-central TX showed a
    largely forward propagating broken axis of thunderstorms
    stretching from the southern TX Panhandle to near Del Rio and
    northern Coahuila. More discrete cellular development was located
    ahead of this axis from the I-10 corridor across the Hill Country
    and as far south as US-57, with a general movement toward the
    northeast. The environment across this region of TX contained
    1500-3000 J/kg MLCAPE with little to no inhibition, PWs of 1.5 to
    1.8 inches and sufficient shear along and south of I-10 for
    organized cells (via 20Z SPC mesoanalysis). Forcing in the mid to
    upper levels was coming from a negatively tilted trough axis over
    West TX and divergent and diffluent flow within the left-exit
    region of a 100-120 kt subtropical jet over northern Mexico.

    A mixture of supercell, multicell and ordinary cells are expected
    given the environment with a range of speeds from the south to
    west. Right-moving supercells should have the slowest movement
    toward the east at ~10 to 20 kt. Some additional convective
    development ahead of the forward propagating axis to the west is
    anticipated through the remainder of the afternoon into the
    evening within the unstable environment. Higher rainfall rates
    will occur with areas of short-term training where line segments
    within the western axis of thunderstorms matches the deeper layer
    mean wind from the southwest allowing for 1 to 2+ inches of rain
    in an hour. Additional potential for higher rates will come from
    cell mergers and brief upstream development/training along and
    ahead of this axis. The combination of factors above may result in
    a few widely scattered areas of flash flooding, especially where
    overlap of higher rates occurs with lower flash flood guidance of
    the TX Hill Country to the I-35 corridor.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8KWeFV38JD7C_rWzAfPhhg8at7ud3cSFX5U0CWA_WPJ6-Pk_wMsoM6jkr_AAVscdeZHN= NYwSkwlQF5yQ5LkGagoJWMw$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31499951 31349867 30849776 29989740 29199745=20
    28409828 28049924 28010024 29010090 29510126=20
    30170124 30710067 31390013=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue May 26 22:51:23 2026
    AWUS01 KWNH 262251
    FFGMPD
    NCZ000-SCZ000-GAZ000-270445-

    Mesoscale Precipitation Discussion 0250
    NWS Weather Prediction Center College Park MD
    650 PM EDT Tue May 26 2026

    Areas affected...east-central GA into central/northern SC

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

    Valid 262249Z - 270445Z

    SUMMARY...Training of heavy rain and flash flood potential will
    increase from east-central GA into central/northern SC through the
    early overnight hours. 1 to 2 inch per hour rates (or 1 to 2
    inches in less than 1 hour) and 2 to 4+ inch totals will be
    possible through 05Z.

    DISCUSSION...GOES East visible imagery through 2230Z showed the
    inland push of a sea breeze boundary extending from just south of
    Columbia, SC into portions of southeastern GA. A few thunderstorms
    were located along the boundary but there was generally a higher
    coverage in SC compared to GA. Meanwhile, scattered thunderstorms
    were located across the Piedmont of SC into GA with a general
    movement toward the NNE, except in SC, where southeastward
    advancing outflow was causing propagation toward the east. SPC
    mesoanalysis data from 22Z showed 1000-2000 J/kg MLCAPE remained
    along with high PW values of 1.8 to 2.2 inches from GA into SC,
    containing estimated wet bulb zero heights of 12-14 kft.

    Some degree of continued inland advancement is expected with the
    sea breeze boundary containing scattered thunderstorms over the
    next 1-3 hours. Meanwhile, RAP forecast guidance has been
    suggesting 0-1 km flow becoming increasingly confluent along the
    western edge of the sea breeze boundary as veered flow occurs over
    the western half of GA. The combination of low level
    convergence/confluence atop modest diffluece aloft is expected to
    yield an increase in convection over portions of southeastern GA
    over the next 1-3 hours with a general NNE movement of cells. The
    alignment of cells with the deeper layer mean wind could support
    some periods of short term training. Farther north into SC, The
    eastward advancement of ongoing thunderstorms over Upstate SC,
    meeting with advancing activity farther east, could allow for
    mergers and brief training/high rain rates.

    The environment is supportive of warm rain processes and efficient
    rainfall production with potential for 1 to 2 inches of rain in
    15-30 minutes. Due to 3 to 6+ inches of rain that has fallen over
    a good portion of the region over the past 3 days, flash flood
    guidance is lowered in a several locations with the potential for
    isolated to widely scattered flash flooding possible through 05Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9y3eVJRYyNYfDoUWD-8_sx_obLFJMjW9Hbkv0xidNsj26HrBi0cO4OF8ZZVCtTRNxzCP= ZwQws_EK2rtEjYislsp_zGk$ for graphic product...

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

    ATTN...RFC...ALR...NWC...

    LAT...LON 35188124 34938073 34538034 33938028 32918094=20
    31168207 30758244 30818281 31178305 32288316=20
    33558300 34518253 35168179=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 27 02:15:43 2026
    AWUS01 KWNH 270215
    FFGMPD
    TXZ000-270630-

    Mesoscale Precipitation Discussion 0251
    NWS Weather Prediction Center College Park MD
    1014 PM EDT Tue May 26 2026

    Areas affected...central to south-central TX

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

    Valid 270212Z - 270630Z

    SUMMARY...An ongoing flash flood threat will linger across
    portions of central TX over the next 3-4 hours. Meanwhile, a new
    flash flood threat will evolve farther south from near the Rio
    Grande into south-central TX after ~05Z. Peak hourly rainfall of 2
    to 3 inches (locally higher) is expected.

    DISCUSSION...Regional radar imagery at 0145Z showed a forward
    propagating linear convective cluster arcing eastward from SPS to
    ACT to SCI with a SW to NE orientation allowing for MRMS-derived
    hourly rainfall of 1 to 3 inches from eastern Kerr to western Bell
    counties. Farther south, a severe bowing linear segment was
    identified over I-35, southwest of San Antonio.

    As the southern end of a negatively tilted upper level trough axis
    continues to advance eastward into central/south-central TX over
    the next 6 hours, favorable ascent aided by the divergent and
    diffluent left-exit region of the subtropical jet across northern
    Mexico will maintain lift across central/southern TX.

    =46rom roughly San Antonio and points northward, an additional 2 to
    4 inches of rain will be possible as the NE to SW line of
    thunderstorms continues to advance east, with hourly rainfall of 1
    to 2+ inches. Locally higher hourly rainfall totals will be
    possible where the northern end of the bowing segment SSW of San
    Antonio meets with the line segment to the north, allowing for the
    potential for 2 to 3+ inches of rain in an hour. However, the
    flash flood threat is expected to gradually diminish through 06Z
    for the northern (central TX) locations.

    Farther south however, there is growing concern for flash flooding
    to evolve across the Rio Grande Valley into portions of
    south-central TX later in the night as upstream/developing
    convection intensifies and moves east across Coahuila, potentially
    merging with new convective development along the remnant outflow
    boundary related to the bowing segment. This may occur as low
    level southerly flow interacts with the boundary where sizable
    MLCAPE will remain (2000+ J/kg). Should this scenario unfold, with
    specific timing remaining uncertain, flash flooding will be
    possible from Maverick to Webb counties and points east.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4cFWqlYHF_-fASHLvqtlsWdrSANYog6IRnbG_KE6yNY96rAevF7INQ_x25VkvWH9pa-c= yv3gSvjyS-DuQbamtbrQW9Y$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31899650 31759613 31449609 31109617 29749641=20
    28819701 27719803 27279906 27609986 28100023=20
    28550043 28709994 28939942 29629920 30159879=20
    31119792 31689740 31819710=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 27 04:14:57 2026
    AWUS01 KWNH 270414
    FFGMPD
    SCZ000-GAZ000-270900-

    Mesoscale Precipitation Discussion 0252
    NWS Weather Prediction Center College Park MD
    1213 AM EDT Wed May 27 2026

    Areas affected...Eastern Georgia...Central South Carolina...

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

    Valid 270415Z - 270900Z

    SUMMARY...A few more hours of potential repeating high efficiency
    thunderstorms across same corridor/wetter upper-soil conditions.=20
    Localized flash flooding potential remains possible overnight.

    DISCUSSION...GOES-E WV suite denotes very little
    evolution/transition of the subtropical high location with just a
    slight flattening of the northeast side of the ridging across NC/E
    SC. As such, the next in a sequence of jet streak enhancements is
    sliding along this section through the Cumberland Plateau=20
    providing anticyclonic divergence along the western periphery of
    the area of concern. The MPD remains aligned with the confluent
    surface to mid-level warm conveyor belt, which continues to
    receive confluent upstream from the western Atlantic feeder
    through northern FL into southern GA resulting in flux convergence
    and total PWat values of 2-2.25" still fairly anchored across the
    same corridor from the Okefenokee Swamp to the Augusta, GA region
    before deflecting across the Piedmont/central Fall-line of SC.=20
    This slight cyclonic curvature further supports convergence and
    increased overlap of the remaining instability axis to the east
    across the I-95 corridor in GA and through S SC. While overall
    low-level flow is slightly weaker at 10-20kts, there remains
    sufficient deep layer convergence with 750-1000 J/kg of
    narrow-skinny CAPE for a few more hours of scattered thunderstorm
    activity.

    Given the deep layer moisture and warm cloud depths, rainfall
    efficiency should remain high at 2"/hr. Slow north to
    northeastward propagation along the same corridor as the last few
    days will allow for intense rainfall to fall upon increasingly
    deeply saturated grounds with relative soil moisture values over
    70% dotted along the axis. Given the rates and limited capacity
    in the upper-soils, there should be increased run-off perhaps
    resulting in similar widely scattered but focused incidents of
    flash flooding as seen over the past few hours.

    While the deep layer flow suggests areas along the Fall-line of
    central SC and northwest where FFG values are most compromised
    should remain far enough northwest given current trends. However,
    a small deviation due to storm scale interactions still may result
    in this area remaining at risk for the earlier portions of the
    overnight period and have been included in the MPD area of concern.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!43sc9HScZLRX0coppH4K0Jfsbc6vv3pU569B2q_PjLtiQLmw0MaaiJ-U_LOF-yNRM-4A= smfnE3Wg4zJMMdDnrgGYt18$ for graphic product...

    ATTN...WFO...CAE...CHS...FFC...GSP...

    ATTN...RFC...ALR...NWC...

    LAT...LON 34818165 34728081 34258026 33808018 33418034=20
    33108063 32438138 32168162 31928183 32138275=20
    32888262 33628256 34368236=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 27 05:30:31 2026
    AWUS01 KWNH 270530
    FFGMPD
    TXZ000-271100-

    Mesoscale Precipitation Discussion 0253
    NWS Weather Prediction Center College Park MD
    129 AM EDT Wed May 27 2026

    Areas affected...Eastern & Southeast Texas...

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

    Valid 270530Z - 271100Z

    SUMMARY...Urban flash flooding risk as squall line weakens and
    stalls along the central TX coast, with quick burst of sub-hourly
    totals of 1.25-1.75", resulting in localized 2-3" and possible
    flash flooding overnight.

    DISCUSSION...
    Regional RADAR and 05z surface analysis shows strong, mature,
    progressive squall line emerging from the I-35 corridor moving
    into the Central Texas Coastal Plain rapidly approaching the
    College Station to Houston urban areas and moving out of MPD 251=20
    A pool of conditionally unstable air awaits it along the upper to
    central TX Gulf coast with low to mid-70s Tds (with some upper
    70s directly on the coast) and MLCAPE of 2000-3000 J/kg from a
    preceding surface trof from KCLL to KJAS into central LA and
    southward. Strong inflow and latent heat release aloft should
    continue to maintain that forward progress, but the shear
    magnitude of moisture fluxed into the leading edge will support
    very intense instantaneous rain-rates with 15-30 minute 1.25-1.75"
    totals expected given current observational trends and recent HRRR
    forecast trends. For the most part, the totals will remain at the
    edge/just below all naturally higher FFG values (1-6hrs) but urban
    and traditionally prone, poorly draining locations are probable to
    be overwhelmed in short-term. The question will be the overall
    volume and given the breadth of the squall line, neighboring
    upper-reaches of small watersheds may compound quickly for
    localized rapid inundation flash flooding.

    North of the trough axis, deep layer steering shifts to support
    back-shearing from southeast to northwest into the deepening
    outflow channel, cold pool and surface meso-highs are much weaker
    and left-bookend/cyclonic eddy may allow for slightly reduced
    rates/downdraft intensity to linger/greater residency to approach
    similar localized 2-3" totals. This still may not reach the
    higher FFG values in the area, but there remains a low-end risk
    for flash flooding here as well, especially near urban locales.=20=20=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9XGS5W5EHcaDcVlgv6ljeUn_Y8gGB-rnq1ClTqqtUklx4OJ7UUCCgY9-0jXozHJ2yhzg= fqFyVeo39SXpn-qU1dG3cxQ$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...LCH...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 33189613 33159523 32549462 31249394 30679380=20
    29959380 29159478 28539581 27989692 28329757=20
    28909760 29819715 30449675 31349606 32099612=20
    32829644=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 27 06:11:36 2026
    AWUS01 KWNH 270611
    FFGMPD
    TXZ000-271200-

    Mesoscale Precipitation Discussion 0254
    NWS Weather Prediction Center College Park MD
    210 AM EDT Wed May 27 2026

    Areas affected...South Texas...

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

    Valid 270610Z - 271200Z

    SUMMARY...Flattening squall line with upstream deepening wave,
    likely to result in expanding convective environment with ample training/repeating opportunities and likely result in 3-5" totals

    DISCUSSION...Regional RADAR shows mature progressive squall line
    crossing along I-10 through the central Texas Coastal Plain with
    the anti-cyclonic rotor of the squall resulting in a flattening
    west to east outflow boundary across south-central to southern
    Texas. A strong, broad super-cell anchors the base of the line
    with overshooting tops colder than -80C. Surface and VWP show
    southeasterly veering to southerly at 15-20kts and 35-40kts,
    respectively intersecting this boundary, leading to strong
    isentropic ascent. The advected air remains very unstable with
    MLCAPEs of 3500-4000 J/kg with mid to upper 70s Tds; resulting in
    strong to extreme moisture flux convergence 20+ kg/m/s.

    GOES-E WV suite notes and upstream speed max in the sub-tropical
    jet is dipping the orientation ever so slightly to support
    diffluence aloft, which is also aiding development of an embedded
    shortwave feature near 27.5N102W, leading to a new convective
    cluster over the Sierra Madre, still fairly displaced from the
    deeper surface to 850mb moisture. However, CIRA LPW does note
    that downstream of the wave, cross Mexican 850-700 and 700-500
    moisture connection intersects over the Lower Rio Grande Valley to
    support 2-2.25" total PWats. The combination of the approaching
    upper-level forcing with the isentropical ascent/convergence is
    likely to fill in the line between the upstream cluster and the
    tail of the squall. Strength of updrafts and flux convergence
    will support very intense sub-hourly burst, but hourly
    rates/totals of 2-3" are probable along the axis due to deep layer
    steering supporting repeating/training environment. There remains
    some uncertainty to the vigor of the cold pool generation and
    therefore the propagation vectors are wavering between due east
    and southeast within the Hi-Res CAM guidance suite. No deviation
    may result in the most extreme totals from Webb to San Patricio
    county with localized spots in excess of 6-7" by 12z; while more
    deviation to the southeast will broaden the overall heavy rainfall
    coverage to 3-4" areal expectations.=20=20

    While FFG values are naturally high, the shear moisture flux and
    rates with any increased residency, which looks very likely, will
    result in flash flooding conditions; if duration would to align
    with urban locations, such as Corpus Christi; inundation flooding
    could be considerable.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8O3XZqK8S-30Y47xAsJel_YCB0ORWKjuTdXMYWfd5selvNjk3eIZe_hUkWhezQJ550KM= pa2ekzjYHR9GcOuMyDMn5Qw$ for graphic product...

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

    ATTN...RFC...FWR...NWC...

    LAT...LON 29029723 28579667 28179654 27659707 26889741=20
    26759840 26999955 28430046 28889905=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 27 06:57:40 2026
    AWUS01 KWNH 270657
    FFGMPD
    PAZ000-MDZ000-WVZ000-OHZ000-INZ000-271245-

    Mesoscale Precipitation Discussion 0255
    NWS Weather Prediction Center College Park MD
    256 AM EDT Wed May 27 2026

    Areas affected...Eastern IND...Central OH...Southeast PA...Western
    MD... Northern WV...

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

    Valid 270700Z - 271245Z

    SUMMARY...Scattered warm-advection showers will have high rainfall
    efficiency with rates up to 1-1.5"/hr will eventually stall and
    align favorably for repeating along the mid-level front. Streaks
    of 1-2" over recently saturated soils pose widely scatted
    incidents of possible flash flooding.

    DISCUSSION...GOES-E WV suite depict the elongating/shearing older
    closed low near St. Louis Missouri with a deep laminar elongated, deformation/shear axis across central IL/IND/OH and PA. South of
    which, broad south to south-southwesterly 15-20kt low-level jet is
    lifting the surface front more in line with the aforementioned
    axis. Deep layer moisture remains pooled along the steepening
    frontal zone with values of 1.5-1.75" (slightly higher further
    east). Further west, a bit of drier air aloft and therefore
    slightly steepened lapse rates is support some 500-1000 J/kg of
    MUCAPE, though this becomes 250-500 J/kg further east through the
    central Appalachians. As such, solid moisture flux convergence
    along the vertically steepening isentropic boundary is starting to
    break out a few narrow currently scattered showers from central IL
    through eastern OH. WV suite also denotes core of upper-level jet
    streak over central OH before turning eastward over PA/NY,
    providing some modest divergence aloft, again slightly east.

    All elements considered the updrafts will support efficient
    rainfall production given the moist environment but due to the
    likely narrow updrafts due to weak instability, rates of .75-1"/hr
    will be more common, though ideal storm-scale interactions may
    allow for up to 1.5" locally and for short time periods. Ascent
    will continue through the late overnight period/early morning with
    increasing convective cells along the boundary. Deep layer
    steering quickly veers along the shear axis to support west to
    east propagation and potential for these showers to repeat.

    As such, localized streaks of 1-2" are possible though the morning
    with increasing potential from central OH to the spine of the
    Appalachians. Recent prolonged moderate to heavy rainfall has
    soaked the upper-soil environment particularly over E OH into the
    central Appalachians, where hourly FFG value are barely over 1"
    and 3hr values are mostly less than 1.5". Further west into
    central IL/IND, FFG values rise and are likely to be just out of
    reach with only exception for a very isolated stationary cell or
    two. As such, localized incidents of flash flooding will be
    considered possible from Eastern IND into SE PA/W MD/E WV.=20

    Note: There are some hints of prolonged training events within the
    Hi-Res CAM suite with higher localized totals of 2.5"+. While
    confidence is not high, these unidirectional flow regimes with
    trapped deep layer moisture, vorticity and prolonged training
    potential can be particularly dangerous especially in the complex
    terrain of E OH, N WV and SE PA/W MD.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6z5JaBq1DiZS0Bi0r2lQJtOQQgR7npXAVFCKxVzfESqNvEuIl93hMzYYPQHF_f7DXHt7= O_Z33TWe2grjJU-ruADxGGo$ for graphic product...

    ATTN...WFO...CLE...CTP...ILN...IND...LWX...PBZ...RLX...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 40378148 40307964 40047857 39757831 39227854=20
    38667926 38808013 39188204 39308360 39238533=20
    39658569 39998566 40318460=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 27 12:00:42 2026
    AWUS01 KWNH 271200
    FFGMPD
    TXZ000-271459-

    Mesoscale Precipitation Discussion 0256
    NWS Weather Prediction Center College Park MD
    759 AM EDT Wed May 27 2026

    Areas affected...portions of Deep South Texas

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

    Valid 271159Z - 271459Z

    Summary...Flash flood potential continues as a convective complex
    spreads 1-2.5 inch/hr rain rates across the region this morning.

    Discussion...An intense convective complex continues to migrate
    across Deep South Texas this morning. The northern portion of the
    complex (extending from near Karnes City to near Corpus Christi)
    was fairly progressive, with only isolated mergers noted that were
    boosting local rain rates above 2 inches/hr. FFGs are low in
    these areas from prior rainfall, and FFG exceedences were noted.=20
    Flash flood potential will likely exist for the next couple hours
    as this part of the complex reaches the middle Texas coast through
    14Z.

    Of somewhat greater concern is focused, training convection on the
    southwestern side of this complex. Convection in that area was
    oriented more parallel to steering flow aloft while remaining
    closer to steep mid-level lapse rates aloft, supporting
    backbuilding. A mid-level wave was evident per objective analyses
    along the Rio Grande Valley near Cotulla. That wave should
    continue to make slow northeastward progress through south Texas
    this morning, prompting continued, upstream updraft development.=20
    The temporal extent of this backbuilding is a bit uncertain -
    though it appears that at least two more hours of backbuilding
    convection (and rates approaching 3 inches/hr) are possible.=20
    Flash flooding is expected - especially if these downpours can
    begin to affect more populated areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9H_mZt6YGd09u9KltefruWuPDwDOaiU6U6P2P_g9mMBVbabLsm2uLMThFmAbmcoRapd9= NeHIuskPe0ji6_1Ci_ZQPiY$ for graphic product...

    ATTN...WFO...BRO...CRP...EWX...HGX...

    ATTN...RFC...FWR...NWC...

    LAT...LON 30179711 29969549 28899531 27739645 26719708=20
    26109729 26199856 26939979 27940007 28519909=20
    28739834 29989832=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 27 12:55:17 2026
    AWUS01 KWNH 271255
    FFGMPD
    PAZ000-MDZ000-VAZ000-WVZ000-OHZ000-INZ000-271853-

    Mesoscale Precipitation Discussion 0257
    NWS Weather Prediction Center College Park MD
    854 AM EDT Wed May 27 2026

    Areas affected...portions of Indiana, Ohio, West Virginia, western
    Maryland, and southwestern Pennsylvania

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

    Valid 271253Z - 271853Z

    Summary...Flash flood potential will continue through at least
    18Z/2p eastern today.

    Discussion...Scattered convection continues to remain focused
    along and just north of a warm frontal zone located from central
    Indiana eastward though northern West Virginia. Along and south of
    this boundary, near 70F dewpoints were supporting areas of
    500-1000 J/kg MUCAPE along with 1.6 inch PW values. These
    thermodynamics were supporting briefly heavy rainfall due to
    localized training despite appreciable storm motions (around 30
    knots or so). Spots of 1 inch/hr rain rates were noted over West
    Virginia and in western Ohio, which were approaching or even
    exceeding FFG thresholds on a localized basis (<0.75/hr in spots).

    The overall regime should continue through at least 18Z/2p today
    and likely beyond. The warm frontal zone will move very little
    today while weak mid-level waves and subtle convergence along the
    front support redevelopment of convection. Occasional training
    bands will readily exceed FFG thresholds on an isolated to
    scattered basis, and an appreciable coverage/number of flash flood
    instances are expected given the regime and sensitivity of ground
    conditions across the region. Areas of rainfall totals reaching 3
    inches are possible through 18Z, especially with convective
    coverage expected to increase due to surface
    heating/destabilization expected through the morning.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!46EgCW9vjFnu1lOif4X0tTIBXtiE_fWIG8EzQXxCnmota-0dXNJ3tJwftZJP9AdqA6v_= -uHRqEV3Of_z5NtFySMJwmY$ for graphic product...

    ATTN...WFO...CLE...CTP...ILN...IND...IWX...LWX...PBZ...RLX...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 40998239 40828009 40377813 40137789 39497770=20
    39157782 38747857 38467979 38618174 39288398=20
    39508616 40178658 40838612 40978465=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 27 13:22:19 2026
    AWUS01 KWNH 271322
    FFGMPD
    DEZ000-MDZ000-VAZ000-DCZ000-271519-

    Mesoscale Precipitation Discussion 0258
    NWS Weather Prediction Center College Park MD
    920 AM EDT Wed May 27 2026

    Areas affected...Maryland, District of Columbia

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

    Valid 271319Z - 271519Z

    Summary...Isolated flash flood potential will exist as a cluster
    of storms over western Maryland moves through the region this
    morning.

    Discussion...A persistent cluster of thunderstorms was noted via
    radar mosaic imagery near Frederick. These cells have shown
    modest signs of intensification in the last few minutes. They are
    being supported by weak mid-level waves moving through zonal flow
    over northern VA and near 70F dewpoints that were fostering 1.75-2
    inch PW values and ~1000 J/kg MUCAPE. Despite current rain rates
    of 0.5-0.75 inch/hr, moisture values increase with downstream
    extent toward the Chesapeake Bay. Though appreciable steering
    flow was supporting fairly quick movement of individual cells
    (around 35-40 knots), increasing downstream moisture profiles and
    urban ground surfaces/lower FFGs nearer to I-95 (0.75 in/hr) may
    support isolated instances of flash flooding this morning. This
    potential should be brief (perhaps extending through 15Z/11a).=20
    More upstream convection is possible later today and will be
    monitored for any flash flood potential beyond 15Z.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5igO96g-vGZ-IIMMg39nVl5zsxBvbZHOry29pAv0nGBaIt3RunBWy5jNiTncz1mP9jIb= 49E2ugkjZCi8kpY0Hxv1RQo$ for graphic product...

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

    ATTN...RFC...RHA...NWC...

    LAT...LON 39727661 39527578 38907572 38667657 39187757=20
    39657737=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 27 14:44:28 2026
    AWUS01 KWNH 271444
    FFGMPD
    TXZ000-OKZ000-271842-

    Mesoscale Precipitation Discussion 0259
    NWS Weather Prediction Center College Park MD
    1043 AM EDT Wed May 27 2026

    Areas affected...portions of north Texas, including Dallas/Fort
    Worth Metro

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

    Valid 271442Z - 271842Z

    Summary...A very slow-moving band of convection has formed over
    eastern Dallas metro while producing rainfall rates approaching 3
    inches/hr. Flash flood is likely with this activity over the next
    2-4 hours.

    Discussion...A focused band of convection near eastern Dallas
    metro has materialized over the past hour or so. The convection
    was focused along enhanced low-level convergence on the western
    edge of 20-30 kt 850mb flow in northeast Texas. A weak surface
    low was also noted in the general vicinity of the convection as
    well. The low-level convergence was likely operating in tandem
    with weak forcing from a mid-level wave over the area to force
    deep ascent of an abundantly moist (1.8 inch PW) airmass with
    sufficient conditional instability (~1000 J/kg MUCAPE) for strong
    updrafts. Given the heavy rainfall rates and higher-end MRMS
    Flash responses near Rockwall, it is likely that flash flooding is
    imminent beneath this band if not already occurring.

    The overall duration of this flash flood scenario is in question
    and will likely be tied to the persistence of enhanced, easterly
    low-level flow into the axis of convection. RAP/mesoanalyses
    suggest that this axis will weaken eventually, but may take a few
    hours to do so. A slow westward/northward drift will likely occur
    as long as convection persists, and with intense local rainfall,
    areas of 5+ inch rainfall totals cannot be ruled out through
    18-19Z (approx 2p central). Flash flooding is likely, and with
    nearby urban population centers at risk, significant impacts
    cannot be ruled out.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_bBFtQ-mamIxqGAtMhmZvdPZ824oI-Sf1fyb_zB5mMiJurwKYj0voKYbA0bPEA3VzIyq= xjbAgihYQ9foyCc_TgunhQs$ for graphic product...

    ATTN...WFO...FWD...OUN...SHV...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 33839674 33729587 33129552 32229564 32109661=20
    32849731 33749723=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 27 16:59:41 2026
    AWUS01 KWNH 271659
    FFGMPD
    ARZ000-TXZ000-OKZ000-272258-

    Mesoscale Precipitation Discussion 0260
    NWS Weather Prediction Center College Park MD
    1258 PM EDT Wed May 27 2026

    Areas affected...portions of southern, central, eastern Oklahoma,
    far north Texas, and far western Arkansas

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

    Valid 271658Z - 272258Z

    Summary...A convective complex over north-central Texas is
    drifting northward and should spread areas of 1-2 inch/hr rain
    rates into the discussion area over the next 2-4 hours. Flash
    flooding is possible with this activity.

    Discussion...A focused band of convection near east Dallas metro
    has gained mesoscale organization over the past hour while
    drifting northward and producing 6-8 inches of rainfall (estimated
    per MRMS/radar). That convection continues to remain organized,
    but has exhibited some weakening/lessening of rain rates over the
    past 30 minutes. Easterly low-level inflow and strong confluence
    near the convection continues to pose a heavy rain risk in the
    near term - especially in/near Sherman, McKinney, and Rockwall.

    The downstream airmass feeding convection continues to be plenty
    moist (1.5+ inch PW) and unstable (2000 J/kg MUCAPE), with plenty
    of sunshine/destabilization noted across eastern Oklahoma and
    Arkansas. The north Texas complex was already beginning to prompt
    heavier rain rates in far southern Oklahoma near Durant, and
    additional convection is expected over time across the entire
    discussion area given the combination of destabilization/ascent
    and weak inhibition.

    FFG thresholds are higher with northward extent from the Red River
    into southern/central Oklahoma (around 2 inch/hr). Flash flooding
    will remain possible, but will likely be tied to areas of training
    and cell mergers that can boost local rainfall totals. This flash
    flood threat will persist through at least 22Z/5p central.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7sT6f42c4FNkoyxiNGcy0JWPUWfetRgT33hrOll18s3b1UMrfG--Y3rQu4CdMPRZoPty= YygrexNHvG-j56b1fWs_Kwk$ for graphic product...

    ATTN...WFO...FWD...LZK...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 36439509 35749396 34129398 33699460 33569555=20
    33349645 33819735 35599735 36349658=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 27 19:50:29 2026
    AWUS01 KWNH 271950
    FFGMPD
    MDZ000-VAZ000-WVZ000-OHZ000-KYZ000-INZ000-280130-

    Mesoscale Precipitation Discussion 0261
    NWS Weather Prediction Center College Park MD
    349 PM EDT Wed May 27 2026

    Areas affected...OH Valley into Central Appalachians.

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

    Valid 271947Z - 280130Z

    Summary...A few areas of flash flooding will be possible across
    the OH Valley into the central Appalachians over the next 3-5
    hours. Rainfall rates of 1-2 in/hr area expected and shorter fused
    rates of over 0.5 inches in 15 minutes will also be possible.

    Discussion...Visible satellite imagery and surface observations at
    1930Z showed a southward sinking outflow boundary that extended
    from the southwestern corner of southwestern PA into southern OH
    and into south-central IN, co-located with scattered showers and
    thunderstorms. Additional thunderstorm activity was noted south of
    the outflow boundary from eastern KY into central WV, out ahead of
    a pair of vorticity maxima observed on water vapor imagery. A
    larger scale vorticity max/shortwave was observed across IL/IN,
    with eastward motion, helping support lift across the region.
    MRMS-derived hourly rainfall was largely below 1 inch for a
    majority of the the region, with the exception of south-central IN
    where training was supporting hourly rainfall of 1 to 2 inches but
    also 15-minute rates of 0.5 to 1.0 inches.

    With ample moisture/instability remaining in place via 19Z SPC
    mesoanalysis data (500 to 1500+ J/kg MLCAPE and PWs of 1.5 to 1.7
    inches), and continued forcing from ascent along/ahead of the
    outflow and ahead of the upstream shortwave/vorticity maxima,
    scattered thunderstorms will continue across the OH Valley into
    the central Appalachians through the early evening. Expectations
    are for individual cell movement toward the east at an average
    speed of 10-25 kt but with system evolution toward the south with
    time. Brief training will briefly enhance rain rates with 1 to 2
    inches of rain in an hour or less, likely supporting a few areas
    of flash flooding across the OH Valley into the central
    Appalachians where flash flood guidance values are mostly ~1 inch
    per hour.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_b-um9cBG32hinS9h0nsHCX6JVXaJXHQKVf5ihAOeJa5-677MN_JCdIxF56NzjE9uG7E= Nbpr-rm5oitn8zxWkhxApvk$ for graphic product...

    ATTN...WFO...ILN...IND...JKL...LMK...LWX...PBZ...RLX...RNK...

    ATTN...RFC...RHA...TIR...NWC...

    LAT...LON 39738605 39598500 39108341 39298184 39688014=20
    39027906 38297916 37558034 37558172 37778368=20
    37838433 38368599 39158629=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed May 27 20:43:35 2026
    AWUS01 KWNH 272043
    FFGMPD
    VAZ000-NCZ000-280230-

    Mesoscale Precipitation Discussion 0262
    NWS Weather Prediction Center College Park MD
    442 PM EDT Wed May 27 2026

    Areas affected...south-central to southeastern VA into far
    northern NC

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

    Valid 272040Z - 280230Z

    SUMMARY...Flash flooding will be possible over south-central to
    southeastern VA into far northern NC through ~02Z. Rain rates of
    1-2 in/hr and total rainfall of 1 to 3 inches are expected, with
    possible overlap with locations that have picked up heavy rain
    over the past couple of days.

    DISCUSSION...GOES-E visible satellite imagery at 2030Z showed a
    southward sinking outflow boundary from the southern DelMarVa
    Peninsula into central VA and a second outflow boundary from
    south-central VA into northwestern NC. The environment south of
    the northern outflow was estimated to contain 1000-2000 J/kg
    MLCAPE and PWs near 2 inches per 20Z SPC mesoanalysis data. As the
    northern outflow boundary continues to advance toward the south
    into the evening, additional convective development is expected
    along/ahead of the boundary with cells containing a mean west to
    east motion at 20-30 kt. Due to the similarly oriented low to
    mid-level flow and the boundary orientation, some brief training
    of heavy rain will be possible over the next 3-6 hours, with
    clearing occurring from north to south over time.

    Portions of southern/southeastern VA have received 3 to 6+ inches
    of rain over the past 48 hours and have limited capacity for
    additional infiltration of water. Therefore, hourly rainfall of 1
    to 2 inches and the potential for isolated totals near 3 inches
    could support areas of flash flooding through 02Z to 03Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!64TL9NajwaPmIhCwxLrlTX0gRhZ9C9--NwtEw9gRsuGJf2vclY7WDfZHD47F1XLCAgTF= 1lTxXfMamkO_dzvK5qGIqIM$ for graphic product...

    ATTN...WFO...AKQ...LWX...RAH...RNK...

    ATTN...RFC...ALR...RHA...TIR...NWC...

    LAT...LON 37907655 37537567 37037545 36507571 36417673=20
    36437775 36437906 36528003 37148017 37757815=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 28 05:24:59 2026
    AWUS01 KWNH 280524
    FFGMPD
    TXZ000-OKZ000-KSZ000-COZ000-281123-

    Mesoscale Precipitation Discussion 0263
    NWS Weather Prediction Center College Park MD
    123 AM EDT Thu May 28 2026

    Areas affected...Portions of the Central and Southern High Plains

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

    Valid 280523Z - 281123Z

    Summary...An increasing threat for localized flash flooding will
    occur over portions of western Kansas into the adjacent Oklahoma
    and Texas Panhandles as rainfall rates approach 2 inches per hour
    at times.=20

    Discussion...Broad upper level troughing with multiple smaller
    mid-level perturbations pivoting around the general circulation
    are causing a period of unsettled weather over the Central and
    Southern Plains this evening. At the surface, a defined surface
    trough axis is positioned over the western High Plains of Kansas
    down through the Oklahoma and Texas Panhandles with an area low
    pressure centered near Amarillo, Texas. Within the bounds of the
    surface trough, deep moisture and prominent instability maximum is
    co-located within the surface trough axis' and under the main area
    of circulation positioned over the New Mexico/Colorado/Kansas
    border. The alignment of the surface trough and primary upper
    trough correlate to a more formidable area of forcing which is
    well-documented in the latest deep moisture convergence pattern
    from the latest mesoanalysis.

    KDDC this evening experienced PWAT anomalies approaching the
    95-99th percentile of climatological means for this time of year,
    a testament to the depth and magnitude of sufficient deep layer
    moisture availability. MUCAPE between 500-1000 J/kg will be
    positioned across the area of interest providing sufficient
    buoyancy for updraft development and initiating stronger
    convective cores capable of heavy rainfall production. A few cells
    are already occurring in the region with pockets of 1-2"/hr rates
    and some intra-hour pulses reaching near 3"/hr at times as cells
    mature. Deterministic outputs from the latest HRRR and RRFS
    indicate some localized amounts between 2-4" over the next 6 hours
    as the axis of convergence within the surface trough placement
    begins to levy a more enhanced convective footprint over the
    course of the early morning hours, perhaps lingering through most
    of the morning if some of the CAMs are correct.

    The likelihood of flash flooding remains in the modest category
    due to the antecedent soil moisture conditions over the area as a
    prolonged drier pattern has firmly driven FFG's to a less
    favorable scenario for flash flooding compared to normal. As a
    result, there is a flash flood risk possible over the western High
    Plains between Kansas, Oklahoma, far southeast Colorado, and the
    northern Texas Panhandle.

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_--zGD1Hhgh1tmk6NVsMcJGiV3nLu5WZawmCS6KtDhgO7-1Tpqc3QGny0D0JHgyBDDt-= ChkxUSSk1N4pVR3t6WAlYVU$ for graphic product...

    ATTN...WFO...AMA...DDC...GLD...OUN...PUB...

    ATTN...RFC...TUA...NWC...

    LAT...LON 38520115 38320041 37489993 36309960 35759966=20
    35400025 35590117 36120209 36580235 37100235=20
    37780237 38320211=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 28 10:48:05 2026
    AWUS01 KWNH 281047
    FFGMPD
    FLZ000-281446-

    Mesoscale Precipitation Discussion 0264
    NWS Weather Prediction Center College Park MD
    647 AM EDT Thu May 28 2026

    Areas affected...urban southeastern Florida

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

    Valid 281046Z - 281446Z

    Summary...Slow-moving downpours could cause urbanized flash flood
    concerns this morning.

    Discussion...A small cluster of thunderstorms was located near
    Homestead. These storms were located along a subtle confluence
    zone parallel to the southeastern Florida coast, which was
    supporting strong updrafts amid minimal convective inhibition,
    abundant moisture (1.8 inch PW values), and ~1000 J/kg MLCAPE.=20
    Weak southerly steering flow was noted per objective analyses,
    which should aid in slow northward migration of ongoing cells
    through Miami/Ft. Lauderdale Metropolitan. Additionally, spots of
    1-2 inch/hr rain rates were noted/estimated per MRMS, and should
    these cells persist in intensity while drifting northward through
    Miami, urban flash flood potential will increase. Models/CAMs
    suggest that this isolated potential will persist for at least a
    few hours this morning (through 14Z/10a eastern).

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8tsKz4nRfzLIgN7vvD_l55yLjrcwJ0HeTetn5-E3Aoyj53yUnaLrA56adgna9fI5GNnb= ITJDw9omCPb5QRG-HnoAV5M$ for graphic product...

    ATTN...WFO...KEY...MFL...

    ATTN...RFC...ALR...NWC...

    LAT...LON 26818034 26817986 25328020 25348062 26288055=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 28 16:17:11 2026
    AWUS01 KWNH 281616
    FFGMPD
    ALZ000-MSZ000-LAZ000-282214-

    Mesoscale Precipitation Discussion 0265
    NWS Weather Prediction Center College Park MD
    1215 PM EDT Thu May 28 2026

    Areas affected...southern Mississippi, southeastern Louisiana, far
    southwest Alabama

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

    Valid 281614Z - 282214Z

    Summary...A cluster of thunderstorms producing heavy rain rates is
    evolving slowly primarily across southern Mississippi. Flash
    flooding is likely on an isolated to scattered basis through at
    least 19Z.

    Discussion...Persistent warm advection has enabled scattered to
    numerous thunderstorm activity in the general vicinity of
    Hammond, Picayune, and Wiggins over the past 1-2 hours or so. The
    storms are focused on the northern edge of enhanced 850mb flow
    over the north-central Gulf (20-30 knots per RAP/SPC Mesoanalysis)
    while also experiencing the glancing influence of upstream
    mid-level waves providing ascent. Abundant moisture (2+ inch PW
    values) and surface-based instability (exceeding 2000 J/kg) will
    continue to support repeating thunderstorm activity within the
    warm advection regime in place.

    Models/CAMs support repeating thunderstorm activity from
    southeastern Louisiana into southern Mississippi for a few more
    hours, with hourly rain rates exceeding 2 inches per hour where repeating/training is most pronounced. These rates are likely to
    exceed FFG over time and prompt flash flooding. Through 19-20Z,
    models suggest that low-level flow/convergence will slacken some
    and cause thunderstorm activity to 1) eventually shift to the
    northeast of its current axis and 2) exhibit lesser coverage over
    all. Some models remove thunderstorm potential entirely, but this
    scenario is doubtful as persistent mid/upper troughing to the west
    will provide lift/ascent for at least isolated thunderstorm
    activity to persist after 20Z through peak heating. Despite high
    FFGs across parts of southern Mississippi, high rain rates will
    likely result in at least isolated instances of flash flooding
    especially if rain can occur over more urban/sensitive interfaces.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-fvkGdfh2avWXaazlAGXCuI23fP4DkqifkF5JwmjFWOkDzBk9DzZQerSzyPfHBbDRTTE= 8cIGTkf1E0LecWwhhPoF6uQ$ for graphic product...

    ATTN...WFO...JAN...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 32158946 32098858 31788813 30708810 30108843=20
    29328918 29259045 30099053 31319053 31739041=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 28 16:35:38 2026
    AWUS01 KWNH 281635
    FFGMPD
    MSZ000-MOZ000-ARZ000-OKZ000-KSZ000-282234-

    Mesoscale Precipitation Discussion 0266
    NWS Weather Prediction Center College Park MD
    1234 PM EDT Thu May 28 2026

    Areas affected...portions of Arkansas, southern Missouri, and far
    southeast Kansas

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

    Valid 281634Z - 282234Z

    Summary...Scattered thunderstorms were beginning to increase in
    coverage and intensity especially across north-central Arkansas.=20
    Slow movement and efficient rainfall activity will result in a few
    areas of flash flooding through 22Z/5p central.

    Discussion...Storms are increasing in coverage and intensity along
    a general axis extending from near Flippin/Harrison south to near
    Camden, AR over the last hour. The storms are being forced by 1)
    ascent associated with a mid-level trough centered over Oklahoma
    and 2) differential heating through that aforementioned axis
    across central/north-central Arkansas. Abundant surface heating
    east of the axis has allowed for 2000 J/kg MLCAPE to develop amid
    an uncapped airmass, supporting deep convection. 2.1 inch PW
    values are also supporting efficient rain rates within the
    convection, while weak south-southeasterly steering flow aloft has
    enabled slow storm motions and localized training. Rain rates
    approaching 2 inches/hr have already been estimated in parts of
    north-central Arkansas, which isn't surprising given the regime in
    place to support heavy rain.

    The ongoing scenario will evolve slowly today, with convection
    continuing to expand northward and westward across the discussion
    area today. Additional convective development across northeastern
    Arkansas also appears likely. Areas of 3-4 inch rainfall totals
    are expected, which will likely overwhelm low-lying/sensitive
    areas and prompt flash flooding on and isolated to scattered
    basis. This risk will likely persist through 22Z/5p central and
    beyond, with convective coverage driven/modulated by the degree of heating/instability in the upstream airmass across the eastern
    half of the discussion area.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8YIaDTTQNAXznO16YGvzw6lxt-8Y78isY3_puggJvnAgsTPd-2AUUKPZVym_p-XKJj8F= u_-t9EyCwgdR6bFTpUDOfro$ for graphic product...

    ATTN...WFO...EAX...ICT...JAN...LSX...LZK...MEG...PAH...SGF... SHV...TOP...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38759486 38329259 37449070 35879018 33759115=20
    33119204 33489375 35429434 36949479 38009547=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 28 17:05:40 2026
    AWUS01 KWNH 281705
    FFGMPD
    MSZ000-LAZ000-ARZ000-282104-

    Mesoscale Precipitation Discussion 0267
    NWS Weather Prediction Center College Park MD
    104 PM EDT Thu May 28 2026

    Areas affected...portions of eastern/northeastern Louisiana,
    western Mississippi, and far southeast Arkansas

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

    Valid 281704Z - 282104Z

    Summary...A band of convection was taking shape/increasing in
    coverage along an axis from Monroe to Natchez. Isolated instances
    of flash flooding are possible with this activity as it moves
    slowly northward this afternoon.

    Discussion...Areas of 1-2 inch/hr rain rates were beginning to be
    estimated per MRMS within a convective band extending from Monroe
    to Natchez. These storms were in a distinctive warm-advection
    environment, with southeasterly low-level flow maintaining both
    upper 70s F dewpoints and 2+ inch PW values - both supporting
    heavy rainfall. Destabilization east of the ongoing convective
    band was also aiding in its intensification, while ascent
    associated with a mid-level trough over Oklahoma was also
    providing ascent for deep updrafts. Slow northward storm motions
    and localized mergers/training will both contribute to areas of
    2-3 inch/hr rain rates in a few spots through 19-20Z.

    The rain rates were falling on areas of relatively high FFG, with
    thresholds of 2.5-3 inch/hr noted across the discussion area. Any
    flash flood potential in the discussion area should be isolated
    and primarily tied to precipitation over sensitive/low-lying or
    urbanized areas. Convection will likely be diurnally driven, and
    may eventually be impacted by maturing convection over far
    southern MS and expanding cold pool/stabilization processes -
    especially in southern parts of the discussion area.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4z9cZ38byOwjuerr0q4JER0Kel9y8sSOjAFJkAdlZ-Sr-iRlmTpTGKuaPyaWA0NGTWhj= XPp7DnpCQjL6Ew8hs8HtGi0$ for graphic product...

    ATTN...WFO...JAN...LIX...LZK...SHV...

    ATTN...RFC...ORN...NWC...

    LAT...LON 33669021 32308969 31009136 32669228 33459195=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 28 21:10:06 2026
    AWUS01 KWNH 282110
    FFGMPD
    ORZ000-290230-

    Mesoscale Precipitation Discussion 0268
    NWS Weather Prediction Center College Park MD
    508 PM EDT Thu May 28 2026

    Areas affected...central OR

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

    Valid 282107Z - 290230Z

    Summary...Increasing thunderstorms coverage through the remainder
    of the afternoon into the evening may lead to areas of flash
    flooding across portions of central OR. Hourly rainfall over 1
    inch is expected in a few locations along with 15-minutes rates of
    0.25 to 0.75 inches. Total rainfall in a few locations may reach 2
    inches.

    Discussion...GOES West visible imagery showed the early stages of
    convective development across southwestern ID into southeastern
    OR, located north of an anomalous closed low centered over CA/NV.
    Surface heating to the north of cloud cover over the southern
    third of OR was contributing to decreasing convective inhibition
    with MLCAPE of 500-1500 J/kg via 20Z SPC mesoanalysis data. Shear
    parameters were sufficient for storm organization with individual
    cell motions forecast from the E to NE, while clusters should have
    more of a SE to NW movement. Any supercell structures would have
    the slowest motions at ~15 kt (with other cell types faster), but
    the combination of potential mesocyclones and the anomalous
    moisture (PWs of 0.8 to 1.1 in the pre-convective environment)
    will support precipitation efficiency and locally higher rainfall
    rates.

    Water vapor imagery identified a northward advancing shortwave
    spoke over northeastern NV, on the eastern side of the closed low,
    advancing toward southeastern OR. As this feature approaches
    through 00Z, increasing DPVA and diffluence aloft should increase
    convective coverage over central OR with an organized region of showers/thunderstorms likely developing through 03Z. Embedded
    hourly rainfall prior to and within the forecast convective
    cluster are expected to surpass 1 inch but with 15-minute rates of
    stronger cells in the 0.25 to 0.75 inch range. Given FFG across
    much of OR, east of the Cascades, is only 1 to 1.5 inches in 1
    hour (slightly lower/higher in various locations), some areas of
    flash flooding will be possible as cell coverage and merger
    potential increases through the evening. Due to fairly dry
    antecedent conditions, flash flood potential will be most likely
    across any urban areas or sensitive burn scar locations.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!88BI5Xzob7MxRvS0a25idYdXqE-cOwuq7lB0LOgElIXBl2sGfABzBF71XNlxVXetnUyq= PXGl_Rj_QaMCghUnUOQiV5o$ for graphic product...

    ATTN...WFO...BOI...MFR...PDT...PQR...

    ATTN...RFC...PTR...RSA...NWC...

    LAT...LON 45561958 45491897 45301828 44891795 44201824=20
    43431888 42752000 42392114 42322202 42432242=20
    42682253 43092260 43512258 43962249 44472229=20
    45092188 45212141 45472053=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu May 28 23:00:20 2026
    AWUS01 KWNH 282300
    FFGMPD
    TNZ000-MSZ000-MOZ000-ARZ000-290455-

    Mesoscale Precipitation Discussion 0269
    NWS Weather Prediction Center College Park MD
    659 PM EDT Thu May 28 2026

    Areas affected...southern MO/northern AR to the Lower MS Valley

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 282258Z - 290455Z

    SUMMARY...A few areas of flash flooding will continue to be
    possible across portions of central to eastern AR, possibly
    extending into southern MO, far southwestern TN and northwestern
    MS. Hourly rainfall of 1 to 2+ inches and additional totals of 2
    to 4 inches are expected through 05Z.

    DISCUSSION...2230Z radar imagery across southeastern AR into
    south-central MO showed an axis of slow moving thunderstorms with
    an outflow boundary slowly edging eastward. Meanwhile,
    thunderstorm activity has picked up over the past few hours from
    northeastern AR, northward into southern MO. In addition to the
    surface outflow boundary, larger scale low level convergence has
    been contributing to a SSE to NNW axis of thunderstorms across AR,
    with mean steering flow oriented parallel to the convergence axis
    allowing for training of cells. Earlier hourly rainfall was 1 to
    2+ inches with 6-hr MRMS estimates of 3 to 5 inches over portions
    of northern AR. While the coverage of heavy rain has diminished
    compared to earlier in the afternoon, a flash flood threat
    remains.

    SPC mesoanalysis data from 22Z showed that 1000-2000 J/kg MLCAPE
    remained over the eastern half of AR into adjacent portions of
    TN/MS. Aloft, a slow moving mid-level trough axis over western KS
    into southeastern OK was favoring a divergent and diffluent flow
    regime from MO/AR to the MS River.

    While not as contiguous as earlier, low level convergence
    (possibly fragmented sections) will continue to support localized
    heavy rain across the region into the early overnight hours. The
    primary and nearest term threat will exist across the northeastern
    quadrant of AR where ongoing thunderstorm activity was in place.
    Secondly, there is potential for increased low level convergence
    to the north of a 925-850 mb low located over northeastern LA,
    inferred via loops of visible satellite imagery, VAD wind data and
    RAP analyses. This farther south flash flood threat is less
    certain in occurrence, placement and timing, but may impact
    eastern AR into the southeastern quadrant of the state and
    northwestern MS after 00Z. As with locations in northeastern AR,
    portions of southeastern AR have also received well above average
    rainfall over the past week (200 to 600 percent of normal),
    contributing to greater potential for runoff due to additional
    heavy rain.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6OkyWS4maAzPRRpDECelKxXgR0ZueCASmzfq5sFa1ifkC1UayacBZajSSejNDMixqn7q= KjZRvCS6bYw_-S8PoodmZD0$ for graphic product...

    ATTN...WFO...JAN...LZK...MEG...PAH...SGF...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 37389279 37369205 36689065 35638967 34928946=20
    34038979 33419017 33009106 33139162 33849201=20
    34669249 35379281 36049315 36899310=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 29 01:59:34 2026
    AWUS01 KWNH 290159
    FFGMPD
    MTZ000-IDZ000-ORZ000-WAZ000-290700-

    Mesoscale Precipitation Discussion 0270
    NWS Weather Prediction Center College Park MD
    958 PM EDT Thu May 28 2026

    Areas affected...northern OR into southern/southeastern WA and
    northern ID

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 290156Z - 290700Z

    Summary...An isolated to widely scattered flash flood threat will
    linger across northern OR into southern/southeastern WA and
    northern ID over the next 3-5 hours. Potential will exist for peak
    hourly rain of 1 to 1.5 inches and isolated totals up to 2 inches
    through 07Z.

    Discussion...GOES West infrared imagery and GLM data showed a SW
    to NE oriented axis of thunderstorms advancing northwestward
    across central to northern OR at 0145Z. Cells to the northeast of
    this region across northern ID and western MT were more discrete
    in nature but a few smaller clusters were beginning to form. While
    instability had decreased across much of central OR, there
    remained impressive MLCAPE from northern OR into eastern WA and
    northern ID of 1000 to 2000+ J/kg according to the 00Z OTX RAOB
    and recent SPC mesoanalysis (highest in the southern ID Panhandle,
    south of I-90). PW values were also anomalously high at 0.9 to 1.2
    inches over much of the region.

    With sunset, the onset of nocturnal cooling at the surface is
    expected to stabilize the low levels and reduce ongoing widely
    scattered convective activity over western MT into portions of the
    ID Panhandle. However, strong ascent ahead of a mid to upper-level
    shortwave spoke advancing into southeastern OR (related to a large
    closed low centered over CA/NV), will maintain areas of
    thunderstorms as they continue to advance toward the north and
    west within a broken axis. Embedded stronger cores within this
    convective axis will be capable of producing 1 to 1.5 inches of
    rain in an hour or two, resulting in isolated to widely scattered
    flash flooding. This threat will be greatest where heavy rain
    overlaps with urban locations, sensitive burn scars or otherwise
    locally sensitive terrain.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7wtmhWdR1qrm0Le6723KvtMvEqdLZ2gpzeoNRb5GleYP5qq5r1ENBHO-xHcBRxQAnk92= RkggVYsKppa9_VqPeus9l5s$ for graphic product...

    ATTN...WFO...BOI...MSO...OTX...PDT...PQR...SEW...

    ATTN...RFC...PTR...NWC...

    LAT...LON 48651699 48421627 47831569 47021552 46101625=20
    45171702 44861888 44682017 44032116 43992185=20
    44402206 45452197 46742136 47912036 48511839=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 29 10:55:03 2026
    AWUS01 KWNH 291053
    FFGMPD
    MOZ000-ARZ000-291452-

    Mesoscale Precipitation Discussion 0271
    NWS Weather Prediction Center College Park MD
    652 AM EDT Fri May 29 2026

    Areas affected...northern Arkansas, southern Missouri

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 291052Z - 291452Z

    Summary...Scattered showers and occasional thunderstorms were
    drifting slowly northward while producing locally heavy rainfall.=20
    The combination of wet grounds from yesterday's rainfall and
    locally sensitive terrain poses an isolated flash flood risk this
    morning.

    Discussion...Scattered convection was drifting north-northwestward
    across the discussion area within a distinct warm-advection
    regime. The convection was embedded in an environment
    characterized by 1.8 inch PW values, 500-1000 J/kg MUCAPE, and
    low-level confluence - supporting occasionally strong updrafts.=20
    Most cells exhibited enough forward speed to keep rain rates at
    around 1 inch/hr or lower, though a few spots where local
    training/backbuilding has increased rain rates to near FFG --
    particularly near Pope County/Russellville, AR over the past hour.
    Occasional, yet isolated, flash flood potential will exist in
    this regime in the near term.

    Models suggest that ongoing activity will probably experience a
    decreasing trend in convective coverage through the morning as
    low-level flow/confluence decreases. Flash flood potential will
    probably peak over the next couple hours, before decreasing
    gradually through 14Z/9a central.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!__nBIANuDzfKkZyT0i-iNXyOhKrlv6eY-yQC0EyjO2bBQO20_hGB-7ahnCHTf2RmnT2y= 05ztim2FXaNSILOVTvVMdlc$ for graphic product...

    ATTN...WFO...EAX...LSX...LZK...PAH...SGF...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38579243 37529122 36189091 34869145 34369263=20
    35729413 37539432 38489421=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 29 18:01:45 2026
    AWUS01 KWNH 291801
    FFGMPD
    TNZ000-KYZ000-MSZ000-MOZ000-ARZ000-300000-

    Mesoscale Precipitation Discussion 0272
    NWS Weather Prediction Center College Park MD
    200 PM EDT Fri May 29 2026

    Areas affected...southern Missouri, much of Arkansas, western
    Tennessee, northwestern Mississippi

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 291800Z - 300000Z

    Summary...Afternoon heating has resulted in a recent increase in
    convective coverage across the discussion area, with flash
    flooding possible on an isolated basis.

    Discussion...Surface heating across much of Arkansas and the
    presence of modest ascent aloft associated with an overhead
    mid-level trough has resulted in renewed development of
    thunderstorm activity across the discussion area. The environment
    supporting thunderstorm activity remains moist (1.7+ inch PW
    values), with surface heating now fostering 1000-1500 J/kg MLCAPE
    - highest across Arkansas. Shear/steering flow aloft is weak,
    resulting in slow-moving convection and locally heavy rain rates.=20
    MRMS has already estimated spots of 1-2 inch/hr rain rates near
    some storms. Additionally, rainfall was occurring in/near areas
    that experienced heavy rain and flash flood impacts yesterday
    between Little Rock and Harrison. FFG thresholds are low along
    this axis, and may be readily exceeded at times given the
    aforementioned regime.

    Convective coverage will continue to expand gradually with time,
    although eventually, widespread convective overturning should
    result in a gradual lessening of convective (and flash flood) risk
    toward evening/00Z. In the meantime, areas of flash flooding are
    possible on at least an isolated basis.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8LRCiP-9W9fURQ-J9ksDi5qmMelq9TNwp_fGy2sbVpEbaMLub6mZoiemghWOSGwM6Gry= qkdKDZwMwAP03n-fGCLoPwk$ for graphic product...

    ATTN...WFO...EAX...JAN...LSX...LZK...MEG...PAH...SGF...TSA...

    ATTN...RFC...KRF...MSR...ORN...TUA...NWC...

    LAT...LON 38739267 38449204 37769007 36708922 35488906=20
    33419095 33939255 34629341 36529399 38159422=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri May 29 18:16:45 2026
    AWUS01 KWNH 291816
    FFGMPD
    SCZ000-GAZ000-ALZ000-300015-

    Mesoscale Precipitation Discussion 0273
    NWS Weather Prediction Center College Park MD
    215 PM EDT Fri May 29 2026

    Areas affected...portions of Georgia

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 291815Z - 300015Z

    Summary...Strong convection has focused along a subtle confluence
    zone extending from Atlanta to Macon to Brunswick. Convection
    along this axis is slow-moving, with heavy rainfall potentially
    leading to a few instances of flash flooding.

    Discussion...Strong surface heating along a weak low-level
    confluence zone from Atlanta to Macon to Brunswick has allowed for
    strong thunderstorms to develop and intensify over the past couple
    hours. The storms are in a very weakly sheared environment, with
    2 inch PW values, 2000 J/kg MLCAPE, and slow movement encouraging
    local areas of 1.5+ inch/hr rain rates especially from Macon
    southeastward. These rates were falling on areas of 2-2.5 inch/hr
    FFG thresholds (locally lower near Atlanta and northwestern
    Georgia). The overall regime supports areas of isolated instances
    of flash flooding - especially in/near low-lying and sensitive
    locales.

    With time and as thunderstorms mature, convective coverage will
    expand, with spots of 2 inch/hr rain rates becoming more common.=20
    Flash flooding will also become more of a concern given the slow
    storm movement and tendency for local mergers.=20

    Much of this activity will be diurnally driven, with any weakening
    trend of convection dictated by any 1) loss of surface insolation
    and 2) degree of convective overturning/stabilization. Flash
    flood potential will exist through 00Z/8p eastern on an isolated
    to scattered basis.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8H_qwgSQlJffD4J_iFU1VooC1N3PcFsj1inwI--wTbOOaoxJbpPYzi3rXNB8wLKhiTU6= 9oFY5vSUWcwSXsH0whRxiow$ for graphic product...

    ATTN...WFO...BMX...CAE...CHS...FFC...JAX...TAE...

    ATTN...RFC...ALR...NWC...

    LAT...LON 34728483 34038364 33478230 32868147 31878111=20
    30948145 30808229 31508430 32678510 34538545=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 30 01:11:57 2026
    AWUS01 KWNH 300111
    FFGMPD
    TNZ000-ALZ000-MSZ000-ARZ000-300700-

    Mesoscale Precipitation Discussion 0274
    NWS Weather Prediction Center College Park MD
    910 PM EDT Fri May 29 2026

    Areas affected...northern MS into western TN and eastern AR

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 300107Z - 300700Z

    SUMMARY...Isolated flash flooding will be possible through 07Z
    from slow moving thunderstorms from western TN into northern MS
    and far eastern AR. Potential for hourly rainfall of 1 to 3 inches
    will exist.

    DISCUSSION...01Z radar imagery across the Lower MS Valley showed
    scattered thunderstorms in the vicinity of I-40 from eastern AR
    into western TN. Many of the cells were slow moving with peak
    hourly rainfall of 1 to 2 inches (locally higher) per MRMS
    estimates. Water vapor imagery showed the activity was focused
    near a smaller scale vorticity max over southwest TN, part of a
    larger upper-level trough axis/closed low over the region, slowly
    advancing east. The environment remained moist and unstable with
    MLCAPE of 1000 to 2000+ J/kg and PWs of 1.8 to 2.1 inches via 00Z
    SPC mesoanalysis data and neighboring sounding data.

    Over the next few hours, areas of slow moving thunderstorms are
    likely to continue given the remaining instability and upper level
    forcing in place. Mean steering flow is rather weak, ~10 kt over
    north-central MS and less than 10 kt along the AR/TN border, which
    will allow for slow moving cells. Some modest nocturnal
    strengthening of 850 mb winds is expected over northern MS through
    06Z (10-15 kt), which may act to support backbuilding/upstream
    development of any thunderstorms across the region. Hourly
    rainfall of 1 to 2 inches should be common with any thunderstorms,
    but isolated hourly rainfall totals near 3 inches cannot be ruled
    out, especially with any training.

    While the occurrence of these high rain rates should remain
    localized/isolated in coverage, there is enough of a concern to
    highlight this potential for flash flooding over the region, which
    is expected to continue through 07Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4ktb16KhUdN7stNy_wOCFChC9C3RYAJUp9XjJJ79bVtMg683Q5IJA-gdoeVqOl2wHnbm= 1cqQvt9dpVOZb67xtvABDco$ for graphic product...

    ATTN...WFO...HUN...JAN...LZK...MEG...OHX...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 36448926 36278813 35478802 34218833 33358874=20
    32908923 32858976 32929021 33149060 33369086=20
    34019101 35049086 36018969=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 30 01:51:32 2026
    AWUS01 KWNH 300151
    FFGMPD
    NCZ000-GAZ000-TNZ000-ALZ000-300730-

    Mesoscale Precipitation Discussion 0275
    NWS Weather Prediction Center College Park MD
    950 PM EDT Fri May 29 2026

    Areas affected...western GA into far eastern AL, eastern TN and
    far western NC

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 300149Z - 300730Z

    Summary...Flash flood potential will linger across portions of
    eastern AL/western GA into portions of the TN Valley and southern
    Appalachians through 0730Z. Slow movement of cells will support
    potential for localized hourly rainfall of 1 to 3+ inches.

    Discussion...0130Z radar imagery showed a few lingering showers
    and thunderstorms over west-central and northeastern GA with
    MRMS-estimated hourly rainfall of 2 to 3 inches on a very isolated
    basis. Much of central GA has been worked over by earlier
    convection, reducing available instability and increasing low
    level inhibition, limiting near term concerns for additional heavy
    rain. However, the western portion of GA into eastern AL remained
    unstable with ~1000 to 1500 J/kg MLCAPE via 01Z SPC mesoanalysis
    data with little to no inhibition. The approach of a mid to
    upper-level trough from the west may provide forcing for the
    development of additional showers/thunderstorms, possibly
    increasing in the 03-06Z time frame. The reflection of the ongoing
    ascent ahead of the upper trough was represented by a small
    cluster of weakening thunderstorms over south-central AL as of
    0130Z.

    Farther north, radar imagery over the past 30 minutes has shown an
    expansion in the coverage of showers/thunderstorms over eastern
    TN. A relative max in MLCAPE resided over the region with 500-1500
    J/kg via the 01Z SPC mesoanalysis. While shear was lacking for
    storm organization, deeper layer mean winds were weak at less than
    10 kt from the southwest which will allow for 1 to 2+ inch
    rainfall (in excess of area FFG), especially where upstream
    development occurs.

    Moisture across the region was high with PWs ranging from 2.2
    inches over south-central GA (near a stationary front) to 1.6
    inches in eastern TN. Earlier observed gauge reports in portions
    of GA showed 3 to 3.5 inches in an hour, a testament to the very
    moist and efficient airmass in place over the region. The weak
    steering flow over AL/GA/TN will be supportive of slow moving
    cells with the potential for backbuilding/upstream development,
    supportive of isolated 2+ in/hr rainfall.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_eq5lwqiNdKtOJDzPBGVgwcZ75ZIs_t_eMwu4KMYFIKmMus9vJkRqpejISF1SyKBDNjH= cNJ-gIZANzq3t31g5FCw2BE$ for graphic product...

    ATTN...WFO...BMX...FFC...GSP...HUN...MRX...OHX...TAE...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 36478321 36288234 35778243 35488300 35288326=20
    34938352 34408363 32978332 32228304 31658357=20
    31608460 31818527 32288553 33138580 34108578=20
    35028550 35798499 36398402=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 30 04:08:13 2026
    AWUS01 KWNH 300408
    FFGMPD
    MTZ000-300700-

    Mesoscale Precipitation Discussion 0276
    NWS Weather Prediction Center College Park MD
    1207 AM EDT Sat May 30 2026

    Areas affected...Eastern Montana

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 300406Z - 300700Z

    SUMMARY...A nearly stationary line of storms is producing 2.5
    in/hour rainfall rates. Flash flooding possible.

    DISCUSSION...A nearly stationary line of storms caught on a trough
    near a surface low over eastern Montana is producing rainfall
    rates to 2 inches per hour on the county line between Valley and
    Phillips Counties. The outflow boundary has pushed well east of
    the storms, and should eventually work to cut off the inflow,
    however due to the proximity of a low level jet, the storms have
    been maintaining themselves just west of Glasgow. 1-hourly flash
    flood guidance shows 1 hour amounts are between 1.25 and 1.5
    inches in the area of the storms, so ongoing rainfall is exceeding
    those amounts.

    High-resolution guidance suggests that as the storms use up the
    instability, which is over 1,500 J/kg in SBCAPE and near 2,000
    J/kg in MUCAPE, the storms should detach from the trough, weaken,
    and push north into Canada. It should be noted that the guidance
    generally struggles with these kinds of mesoscale features. In
    this case, given the evident outflow boundary outracing the storms
    now by tens of miles, it appears likely that the storms' inflow
    should soon be cut off, resulting in weakening.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8q5Gd4lJX1JfxFZFqrpIuy-gyj2i10k8eeGy3LYXI8ki01aW-9iHW7TIQefqIL2hyJCd= V9f2iECWUgzPU4WtMaS_q8E$ for graphic product...

    ATTN...WFO...GGW...

    ATTN...RFC...KRF...NWC...

    LAT...LON 49100644 49060599 48720571 48220575 47850617=20
    47760666 47480704 47320718 47360770 47590787=20
    47870780 48220782 48650781 49040772=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 30 09:24:18 2026
    AWUS01 KWNH 300924
    FFGMPD
    VAZ000-TNZ000-KYZ000-301500-

    Mesoscale Precipitation Discussion 0277
    NWS Weather Prediction Center College Park MD
    523 AM EDT Sat May 30 2026

    Areas affected...Southern Kentucky to Eastern Tennessee

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 300922Z - 301500Z

    SUMMARY...Stationary front forcing a line of storms with erratic
    cell motions but ample moisture. Localized flash flooding possible.

    DISCUSSION...A stationary front denoted by a substantial moisture
    gradient is providing the forcing for a line of storms to form
    from southern Kentucky through eastern Tennessee. Weak, but
    nonetheless sufficient southwesterly flow into the front is
    allowing the moisture (PWATs as high as 1.9 inches in western
    Kentucky) to lift into the developing line of storms. Since they
    are both slow-moving and being reinforced by the moisture
    advection, expect the storms to persist for the next several hours
    until daytime heating works to disrupt the flow into the front, as
    well as introduce competing forcing from diurnal heating, cold
    pools, and in some areas, topography. This will result in a
    gradual diminishing of the storms associated with the front itself
    by late morning. While the front is stationary, since the overall
    flow into the front is stronger from the moist southwest side of
    the front, expect some northeastward drifting of the line of
    storms through the morning.

    HREF 6-hr FFG exceedance probabilities show as high as a 40-45
    percent in portions of south-central Kentucky, and another local
    maximum in eastern Tennessee of 25-30 percent through 15Z. Cell
    mergers northwest of Knoxville are already causing flash flooding,
    and expect with chaotic flow along the front that additional cell
    mergers will occur into southern Kentucky through the morning.
    What few pieces of high-resolution guidance are resolving the line
    of storms suggest that there will be rather rapid weakening of the
    storms by late morning for the aforementioned reasons, which will
    diminish the flash flooding threat.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7BouVMkgsq46_v2WTmBJdvBssIRjr-o--KZT97NbklbeuD66C9VPViWmoU5GeWiqxAIN= 6xbFYMeR1AmgC56y8orme6A$ for graphic product...

    ATTN...WFO...JKL...LMK...MRX...OHX...PAH...

    ATTN...RFC...ORN...TIR...NWC...

    LAT...LON 37878610 37738537 37548494 37418409 37198318=20
    36948243 36678187 36368205 36088271 35758336=20
    35608382 35858436 36238504 36498571 36498579=20
    36538581 36868663 37008689 37418701=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 30 15:40:26 2026
    AWUS01 KWNH 301540
    FFGMPD
    MTZ000-302138-

    Mesoscale Precipitation Discussion 0278
    NWS Weather Prediction Center College Park MD
    1139 AM EDT Sat May 30 2026

    Areas affected...portions of Montana

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 301538Z - 302138Z

    Summary...Scattered thunderstorms are increasing in coverage while
    migrating toward central Montana. These trends will continue for
    several hours, posing a risk of flash flooding through 21Z/2p
    mountain time.

    Discussion...Areas of surface heating have led to sufficient
    destabilization (areas of 500-1000 J/kg MLCAPE) for scattered
    thunderstorm activity from west of Jordan to east of Billings and
    eastward along the MT/WY border region. The storms were migrating
    slowly westward at around 10-15 knots due to easterly steering
    flow on the norther periphery of a distinct mid/upper low near
    northeastern UT. Northeasterly low-level trajectories were aiding
    in upslope/subtle orographic ascent across the discussion area,
    while low 60s F dewpoints and 1+ inch PW values were supporting
    heavy rainfall beneath persistent and locally backbuilding
    convection. Rain rates were peaking at around 1 inch/hr per MRMS,
    which 1) isn't surprising given the regime and 2) approaching FFG
    thresholds especially closer to central Montana.

    With time, continued insolation/destabilization within the
    low-level upslope regime across eastern Montana will continue to
    support a gradual expansion of convective coverage. Storms could
    become numerous after 18Z/11a mountain time, with continued areas
    of 1 inch/hr rates exceeding FFG especially across central
    Montana. Lighter rain rates along I-90 west of Billings, along
    I-15 through Helena and Great Falls, and across northern Montana
    near Glasgow could also cause runoff issues given low FFG
    thresholds in those areas. Flash flooding is expected in several
    areas today.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7OW31X31s4WnAYzd8HPTbWxtzD6kqGAZA_JPLx9KvErdiNj4Ux8GgekJPeGr1w5wPOB2= 1Ajj29GfXVrFPFrHCpkAjoI$ for graphic product...

    ATTN...WFO...BYZ...GGW...MSO...TFX...

    ATTN...RFC...KRF...PTR...NWC...

    LAT...LON 48991242 48970930 48820679 48040625 46830571=20
    45710501 45040534 45000878 45041107 45531216=20
    46821309 48731333=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 30 20:32:29 2026
    AWUS01 KWNH 302032
    FFGMPD
    MOZ000-OKZ000-KSZ000-310030-

    Mesoscale Precipitation Discussion 0279
    NWS Weather Prediction Center College Park MD
    431 PM EDT Sat May 30 2026

    Areas affected...Southeast Kansas...Southwest Missouri

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 302030Z - 310030Z

    SUMMARY...Slow-moving thunderstorm clusters will continue to track east-southeast across southeast Kansas and southwest Missouri
    through early evening. Rainfall rates of 1 to 2 in/hr may yield
    localized totals of 2 to 4 inches, making isolated flash flooding
    possible.

    DISCUSSION...Animated satellite and regional radar imagery show an
    expanding axis of convective clusters stretching across southeast
    Kansas into southwest Missouri. These clusters have recently
    exhibited rapidly cooling cloud tops, signaling robust updraft
    strength and active vertical development. Supported by a pooling
    moisture environment (PWATs climbing toward 1.4?1.6 inches) and
    moderate diurnal destabilization, these storms are highly
    efficient rainfall producers, with recent MRMS data estimating
    localized rates of 1 to 2 in/hr.

    The kinematic environment is characterized by weak mid-level
    steering flow and small upwind propagation vectors, leading to
    slow, grinding storm motions toward the east-southeast. While
    high-resolution model guidance exhibits typical summer spatial
    discrepancies, with the RRFS aggressively favoring 2 to 4 inch
    localized pockets through 00Z and the HRRR taking a more
    conservative 1 to 2 inch approach, the current observational trend
    strongly supports the higher-end rainfall potential where cells
    manage to cluster or briefly train.

    Given the somewhat moist antecedent soil environment indicated by
    recent NASA SPoRT soil moisture data, infiltration capacities are
    moderately reduced. While a widespread event is not anticipated
    due to the lack of strong synoptic forcing, these slow-moving 1 to
    2 in/hr rates will be capable of producing isolated short-term
    flash flooding, primarily concentrated across localized low-lying
    areas, small creeks, and vulnerable urban intersections.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6fssWYIZLBkibj5b4UX5CVsTI0uo5AKNv1vlrjdUfAz9pK7ZKIwq_WrN4vsrUmOhG4e4= sEbK-j4fxEbRFdipxU57RGs$ for graphic product...

    ATTN...WFO...EAX...ICT...SGF...TOP...TSA...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 38109564 38099400 37739308 37159290 36769326=20
    36699437 37169581 37769603=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 30 21:56:43 2026
    AWUS01 KWNH 302156
    FFGMPD
    NEZ000-SDZ000-NDZ000-MTZ000-WYZ000-310355-

    Mesoscale Precipitation Discussion 0280
    NWS Weather Prediction Center College Park MD
    555 PM EDT Sat May 30 2026

    Areas affected...Far Northwest Nebraska...Northeast
    Wyoming...Western South Dakota...Central and Eastern Montana

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 302155Z - 310355Z

    SUMMARY...Broken clusters of heavy showers and thunderstorms will
    continue to expand and organize across portions of far northwest
    Nebraska, northeast Wyoming, western South Dakota, and into
    central/eastern Montana this evening. Fueled by highly anomalous
    moisture and enhanced surface convergence along an elongated axis
    of surface low pressure, rainfall rates of 1 to 2 in/hr will be
    capable of producing localized 2 to 3+ inch totals. Flash flooding
    is likely, particularly across sensitive high-terrain basins.

    DISCUSSION...Recent RAP mesoscale analysis and satellite imagery
    depict a robust upper-level low centered over Wyoming, embedded
    within an elongated trough stretching across the northern Rockies.
    This low is projected to slowly lift northward through the evening
    hours, providing widespread, deep-layer forcing and ascent.
    Concurrently, a potent low-to-mid-level fetch is continuously
    transporting a deeply anomalous moisture plume from the Central
    Plains northwestward. Precipitable Water (PW) values within this
    plume are exceptionally high for late May, running 2 to 3 standard
    deviations above the climatological mean.

    At the surface, the latest mesoscale guidance indicates the
    organization of an elongated surface low pressure center
    stretching from northeast Wyoming up through southeast and central
    Montana. This feature is significantly enhancing low-level
    convergence across the region. Along and east of this boundary, an
    axis of moderate instability has materialized, with MLCAPE values
    locally exceeding 1000 J/kg extending down into northeast Wyoming,
    the Black Hills of western South Dakota, and far northwest
    Nebraska.

    Driven by this combination of deep synoptic lift, enhanced surface
    convergence, and high moisture efficiency, broken to locally
    organized convective clusters are expected to produce intense
    hourly rainfall rates of 1 to 2 in/hr along this corridor. The
    consensus of the latest high-resolution guidance, including the
    18Z HREF, 18Z REFS, and recent RRFS runs, strongly favors
    localized additional accumulations of 2 to 3 inches through the
    late evening.

    The 18Z HREF indicates areas of 40 to 60+ percent probabilities of
    exceeding 3-hour Flash Flood Guidance (FFG), particularly across
    central Montana and the Black Hills. Given some of the flashy
    nature of the regional terrain and the high efficiency of these
    convective cores, areas of rapid runoff are expected which will
    tend to lead to at least some areas of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_7I_3W3cBH4sMFgh7FCFr6xlRXGPvPZy5pBUVynG0TWaOJz6oQA44_CoEtqXaSsqZUrI= 0uthYGrDFobxeObCh5ktqAo$ for graphic product...

    ATTN...WFO...BIS...BYZ...CYS...GGW...LBF...RIW...TFX...UNR...

    ATTN...RFC...KRF...NWC...

    LAT...LON 49360786 48810655 47960486 45980291 45230218=20
    43850163 42760206 42490315 42670366 43730460=20
    44370529 44880727 44750918 45050999 45951047=20
    47221004 48700989 49260913=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat May 30 23:00:47 2026
    AWUS01 KWNH 302300
    FFGMPD
    KSZ000-NEZ000-COZ000-WYZ000-310330-

    Mesoscale Precipitation Discussion 0281
    NWS Weather Prediction Center College Park MD
    659 PM EDT Sat May 30 2026

    Areas affected...Northeast Colorado...Southeast Wyoming...Western
    Nebraska Panhandle

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 302259Z - 310330Z

    SUMMARY...A north-south axis of locally training thunderstorms
    along the intersection of the WY/CO/NE borders will continue to
    produce rainfall rates of 1 to 1.5 in/hr this evening. Localized
    totals of 2 to 3+ inches are possible, which may lead to isolated
    flash flooding.

    DISCUSSION...Real-time satellite and radar observations depict a
    highly organized, north-south oriented axis of convection slowly
    advancing northeastward across the western High Plains. GOES-E IR
    imagery shows a steady expansion of cooling convective tops,
    indicative of robust, sustained updrafts. This activity is being
    poorly handled by nearly all numerical model guidance but is
    well-supported by observational trends. Water vapor imagery shows
    strong mid-level forcing and ascent associated with an upper-level
    low spinning over Wyoming and a southward extension of shortwave
    energy ejecting out near the base of it.

    At the surface, an enhanced leeside trough is interacting with a
    strong instability gradient. Low-level easterly flow is actively
    advecting moist and unstable air westward into an inverted trough
    situated just north of a surface low over far northeast Colorado.
    This focused low-level convergence is allowing cells to
    continuously regenerate and locally train along the boundary. With
    high moisture efficiency, these cells are producing
    radar-estimated rainfall rates of 1 to 1.5 in/hr.

    Antecedent conditions across this portion of the High Plains are
    notably dry, which will act as a significant mitigating factor
    against flash flooding. However, given the persistence of the
    convection and orientation relative to the steering flow,
    localized rainfall totals of 2 to 3+ inches are achievable through
    mid-evening. Where these high rates persist over complex terrain
    features or localized urban footprints, rapid runoff and isolated
    flash flooding will remain possible.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!53QY7tuZ5YJ_a9aarJ3Roz32X6mVEyXkgYHYL8Phm4v7E-eYZyA-1ZaHPG4JwHYL2Gs5= nWWm-lDCTVHbqqBzbc-plc4$ for graphic product...

    ATTN...WFO...BOU...CYS...GLD...LBF...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 42880372 42680296 41900206 41160164 40330156=20
    39740193 39320269 39160364 39350419 39750451=20
    40650488 41200505 42040513 42630478 42860425=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 31 03:44:16 2026
    AWUS01 KWNH 310344
    FFGMPD
    SDZ000-310800-

    Mesoscale Precipitation Discussion 0282
    NWS Weather Prediction Center College Park MD
    1142 PM EDT Sat May 30 2026

    Areas affected...Northwestern South Dakota

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 310342Z - 310800Z

    SUMMARY... A drifting line of storms with a history of up to 4
    inch/hour rain rates will continue to pose a diminishing flash
    flooding threat as eastward motion slowly increases. Flash
    flooding possible.

    DISCUSSION...A very slow moving nearly north-south aligned line of
    storms across western South Dakota has a history of 4 inch/hour
    rainfall rates. An impressive 40+ kt low level jet is advecting a
    moist air mass with PWATs to 1.4 inches towards the northwest
    ahead of the line, with instability values between 1,000 and 2,000
    J/kg. This line formed along a nearly stationary trough. An area
    of low pressure over Wyoming is causing westerly winds behind the
    line, resulting in an area of enhanced convergence near the line,
    allowing the storms to persist. MRMS data show that where the
    heaviest amounts of fallen southeast of Rapid City, rainfall
    amounts have doubled FFGs. Since the line is still moving slowly,
    and the outflow continues to produce lighter, but still
    significant rainfall west of the line back to the Wyoming/Montana
    border, the flash flooding threat will persist in these areas for
    the next several hours.

    Hi-res CAMs guidance and radar imagery shows a second line of
    storms moving northward at the southern end of the main line. This
    second line of storms should work to gradually disrupt the main
    line as it pushes north and cuts off the moisture inflow to the
    downstream main line. This will promote a faster eastward
    progression of the entire MCS, which should occur over the next 3
    hours or so. That faster movement should allow for the overall
    flash flooding threat to reduce much more rapidly, especially with
    a lack of diurnal heating leading to a natural diminishing of the
    instability east of the MCS, despite the impressive advection.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-wfWTOIlnUE-qcvcnZUI6xxozrQLwiED6ZRY9No1-Srqdg3K3aOfIsfrpNrvMZi5-T9T= DRyNleiOED3--X2SFZrrNp4$ for graphic product...

    ATTN...WFO...ABR...UNR...

    ATTN...RFC...KRF...NWC...

    LAT...LON 45710201 45680186 45660133 45550084 45200016=20
    44679998 44100002 43930024 43670089 43500180=20
    43450207 43560269 43750311 44080339 44470365=20
    44930371 45550369 45670281=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 31 05:29:29 2026
    AWUS01 KWNH 310529
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-311000-

    Mesoscale Precipitation Discussion 0283
    NWS Weather Prediction Center College Park MD
    127 AM EDT Sun May 31 2026

    Areas affected...Northeast Kansas through Southwest iowa

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 310527Z - 311000Z

    SUMMARY...Several areas of convection have developed from
    northeastern Kansas through Southwestern Iowa. Backbuilding in
    Kansas and nearly stationary movement in Iowa could lead to areas
    of flash flooding.

    DISCUSSION...Multiple lines of storms have formed from
    north-central Kansas through Southwestern Iowa this evening.
    Starting with Kansas, a nearly stationary line of storms has been
    backbuilding into abundant moisture advection from the south.
    These storms are producing rainfall rates over 2 inches per hour.
    Due to the efficient backbuilding, any cells that advect off to
    the northeast are quickly replaced with new ones, resulting in
    effectively stationary storms. SPC Mesoanalysis shows PWATs to
    around 1.5 inches with 850 mb winds advecting the moisture of
    25-35 kts, which should support the storms for several more hours.

    Meanwhile a separate line of storms has developed across the
    southwestern corner of Iowa, and is expanding northwestward to
    just north of Omaha. These storms are nearly stationary as well,
    so hourly rainfall rates with those cells are also exceeding 2
    inches. PWATs are higher here, around 1.7 inches.

    High-resolution guidance are struggling to resolve these mesoscale
    features, but there is decent agreement that the storms over
    Kansas should begin to move eastward with time. Additional storms
    are likely to form to the east of/in advance of these lines of
    storms, resulting in multiple clusters of storms generally
    following each other, resulting in an extended period of time of
    heavy rainfall from Topeka through into Kansas City/St Joseph in
    the next few hours. FFG values are generally around 1.5 inches/1
    hr as a ballpark average, and with multiple cells across the area
    now producing 2 inch/hour rainfall rates, the resulting flash
    flooding threat is likely to continue.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5H42mv9rumMQqQrM-thxegRcP73RcyfinRsYmKbHVlgliqoROz5vwCwmZr_K2_b6CuoN= P6MPpUSNugnk_Dtddmeu_9U$ for graphic product...

    ATTN...WFO...DMX...EAX...FSD...GID...ICT...OAX...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 42349576 41909502 41429477 40789441 40209410=20
    39769398 38679432 38289493 38179557 38339712=20
    38689831 39159894 39189906 39889915 41309820=20
    42269683=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 31 12:18:37 2026
    AWUS01 KWNH 311218
    FFGMPD
    SCZ000-GAZ000-ALZ000-311816-

    Mesoscale Precipitation Discussion 0284
    NWS Weather Prediction Center College Park MD
    817 AM EDT Sun May 31 2026

    Areas affected...portions of Georgia, extreme southern South
    Carolina, and far northeastern Alabama

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 311216Z - 311816Z

    Summary...Slow-moving thunderstorms are increasing in coverage
    while producing spots of 2-3 inch/hr rain rates - especially just
    south of Augusta. Flash flooding is likely on at least an
    isolated basis through midday.

    Discussion...Scattered thunderstorms were gradually increasing in
    coverage along a nearly-stationary front extending from near
    Charleston, SC to Atlanta and Rome, GA. Along and ahead of this
    front, areas of ~500 J/kg MLCAPE were evident via objective
    analyses amid 1.7 inch PW values, supportive of deep convective
    updrafts with efficient rain rates. Additionally, shear
    throughout the lower troposphere was negligible (5-15 knots),
    allowing for storms to focus along the aforementioned front
    without moving much. As a result, areas of 2-3 inch/hr rain rates
    were noted with convection in far eastern Georgia, with additional
    convection developing due to heating/destabilization along the
    front. Flash flooding is expected on at least a localized basis
    given the evolving regime.

    Flash flood potential should continue through at least 18Z/2p
    eastern today. The aforementioned front will move very little,
    with any shifts in axes of heavy rainfall likely driven by local
    convective influences and any mergers of cold pools that occur
    through the morning. FFG thresholds are 2-3 inch/hr range
    (locally lower in northern Georgia and in areas that received
    ample rainfall yesterday closer to Athens and Eatonton). These
    thresholds should be exceeded at times on at least an isolated
    basis this morning.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-0vak7R8vPZqf0dLA079QiilWDpf5KX_bGXWq9fhyg1VfEx0Y5IYQ0wwqT6DGwYRpakg= 6Xjt72FaRORF26zEfIoJ8Fo$ for graphic product...

    ATTN...WFO...BMX...CAE...CHS...FFC...HUN...JAX...TAE...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 34578539 34428421 33748263 33098080 32348027=20
    31388080 31508314 33378595 34328603=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 31 17:35:12 2026
    AWUS01 KWNH 311735
    FFGMPD
    MTZ000-312333-

    Mesoscale Precipitation Discussion 0285
    NWS Weather Prediction Center College Park MD
    133 PM EDT Sun May 31 2026

    Areas affected...portions of Montana

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 311733Z - 312333Z

    Summary...Flood/flash flood issues are expected on at least a
    localized basis as several hours of moderate to locally heavy
    rainfall continue across the region.

    Discussion...Widespread areas of moderate to locally heavy
    rainfall continue to migrate westward into central Montana on the
    northern side of a distinct mid/upper low over northeastern
    Wyoming. Precipitation is being supported by widespread ascent
    tied to a mid-level trough across the discussion area and a
    mid-level deformation zone extending from the mid-level low
    west-northwestward across higher terrain of Montana into southern
    Canada. Rain rates have been modest (generally around or less
    than 0.20 inch/hr), though locally heavier rates have recently
    developed (per MRMS) in/near Great Falls. More importantly,
    ground conditions are water logged, FFGs are low/near zero, and
    the local riverine situation seems to be more supportive of local
    flooding compared to prior days (per collab. with the National
    Water Center). Each of these factors support local flood/flash
    flood potential on at least an isolated basis through in the near
    term.

    Models suggest that at least light to moderate rainfall should
    continue areawide for the next several hours -- and perhaps into
    the overnight timeframe across the most sensitive areas of
    Montana. Flood/flash flood potential will also accommodate this
    rainfall.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-Gy0tlJ0z1XJOx44HXj-yFshiQ6syAjSDekIRqjlsQrBot4KXB2DsncG5Ne518rYcwMf= e6Qxev7rZjvZHKOJu6HD9fA$ for graphic product...

    ATTN...WFO...BYZ...MSO...TFX...

    ATTN...RFC...KRF...PTR...NWC...

    LAT...LON 49021167 48830993 47900935 46940987 46091102=20
    46901262 48091371 48881387=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 31 17:47:44 2026
    AWUS01 KWNH 311747
    FFGMPD
    MTZ000-312333-

    Mesoscale Precipitation Discussion 0285
    NWS Weather Prediction Center College Park MD
    146 PM EDT Sun May 31 2026

    Areas affected...portions of Montana

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 311733Z - 312333Z

    Summary...Flood/flash flood issues are expected on at least a
    localized basis as several hours of moderate to locally heavy
    rainfall continue across the region.

    Discussion...Widespread areas of moderate to locally heavy
    rainfall continue to migrate westward into central Montana on the
    northern side of a distinct mid/upper low over northeastern
    Wyoming. Precipitation is being supported by widespread ascent
    tied to a mid-level trough across the discussion area and a
    mid-level deformation zone extending from the mid-level low
    west-northwestward across higher terrain of Montana into southern
    Canada. Rain rates have been modest (generally around or less
    than 0.20 inch/hr), though locally heavier rates have recently
    developed (per MRMS) in/near Great Falls. More importantly, local
    observations indicate increasing soil saturation and streamflows,
    which will result in low to near-zero FFGs over the region and
    increasing flood potential (per collab. with the National Water
    Center). Each of these factors support local flood/flash flood
    potential on at least an isolated basis in the near term.

    Models suggest that at least light to moderate rainfall should
    continue areawide for the next several hours -- and perhaps into
    the overnight timeframe across the most sensitive areas of
    Montana. Flood/flash flood potential will also accommodate this
    rainfall.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!78Oeu6ZVGyJIqbExO0XVBIEjxLCTYX9-lwDsVuwybeJ3cgJsLeDrJDdu3bkfJo2YmLcg= a4PXtp7sIwLrvYqCALnSyoY$ for graphic product...

    ATTN...WFO...BYZ...MSO...TFX...

    ATTN...RFC...KRF...PTR...NWC...

    LAT...LON 49021167 48830993 47900935 46940987 46091102=20
    46901262 48091371 48881387=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 31 18:05:56 2026
    AWUS01 KWNH 311805
    FFGMPD
    SCZ000-FLZ000-GAZ000-ALZ000-010003-

    Mesoscale Precipitation Discussion 0286
    NWS Weather Prediction Center College Park MD
    204 PM EDT Sun May 31 2026

    Areas affected...southern Georgia, far north Florida, far southern
    South Carolina, and southeast Alabama

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 311803Z - 010003Z

    Summary...Several areas of local rain rates over 2 inch/hr are
    occurring. Flash flooding is possible - especially where these
    rain rates occur over low spots and/or sensitive ground conditions.

    Discussion...Scattered convection has developed in earnest along
    and south of a nearly stationary front over central Georgia (near
    Macon). South of the front, mid/upper 70s F dewpoints and prior
    sunshine was supporting nearly 2000 J/kg MLCAPE and areas of 2-2.1
    inch PW values -- both supporting heavy rainfall rates within the
    stronger and more persistent cells. Low to mid-tropospheric shear
    is weak, supporting slow cell movement. Meanwhile, appreciable
    upper flow (30 kt at 300 hPa) was supporting storm ventilation
    while locally enhancing updraft strength. Isolated flash flood
    potential is evident with these cells.

    This potential should continue over the next several hours.=20
    Pockets of strong insolation were still occurring away from deeper
    convection. Meanwhile, slow and at times erratic storm motions
    were noted with some cells, supporting occasional mergers. Spots
    of 2-3 inch/hr rain rates can be expected at times. These rates
    will occur over FFG thresholds that are generally in the 2.5-3.5
    inch/hr range. This suggests that flash flood potential might
    occur on a scattered basis, but may focus around
    sensitive/low-lying locales that experience the heavier rates.=20
    Flash flood potential should persist through at least 00Z/8p
    eastern -- potentially beyond. Convection may also begin to
    impact more of northern Florida through the afternoon as well (per
    the HREF).

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5GZF5O5EKkRdorad7xDEgKw91tcFg4NFQ3bWHKx04wgGq6UQ-M5-ruhckF5ronFBQ7CM= PQKnPokyg78fKCTrJyR1JBk$ for graphic product...

    ATTN...WFO...BMX...CAE...CHS...FFC...JAX...MOB...TAE...

    ATTN...RFC...ALR...NWC...

    LAT...LON 33618703 33458539 33198421 32828261 32948103=20
    32498020 31738092 30978121 30418137 30178350=20
    30358578 30688696 31138731 31888711 32578728=20
    33488741=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 31 19:05:23 2026
    AWUS01 KWNH 311905
    FFGMPD
    GAZ000-TNZ000-KYZ000-ALZ000-010100-

    Mesoscale Precipitation Discussion 0287
    NWS Weather Prediction Center College Park MD
    303 PM EDT Sun May 31 2026

    Areas affected...Northern Alabama...Middle Tennessee

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 311903Z - 010100Z

    SUMMARY...Convection is initiating and will expand in coverage
    across northern Alabama and middle Tennessee through early this
    evening. Efficient rainfall rates of 1 to 2 in/hr may yield
    localized totals of 2 to 4 inches. Isolated to widely scattered
    flash flooding is possible, particularly across the complex
    terrain of the Cumberland Plateau.

    DISCUSSION...Recent mesoscale analysis highlights a relatively
    focused environment for heavy rainfall developing north of a
    stationary boundary draped across the South and in close proximity
    to an inverted trough that extends from northern Alabama through
    middle Tennessee. A pronounced instability gradient features a
    nose of 1500+ J/kg of MLCAPE extending northward near and just
    west of the Cumberland Plateau. This instability is co-located
    with a sharp moisture gradient, where Precipitable Water (PW)
    values range from 1.5 to 1.75 inches over middle TN to near 2.0
    inches across northern AL.

    The lifting mechanisms to tap into this buoyant airmass are
    multifaceted. The aforementioned inverted trough is currently
    fostering localized low-level surface convergence. Concurrently, a
    weak upstream shortwave translating across western Tennessee is
    providing subtle but necessary mid-level ascent. As low-level flow
    interacts with these features and is directed into the higher
    terrain of the Cumberland Plateau, orographic ascent will further
    enhance updraft development and sustainment.

    The consensus of high-resolution guidance, including the recent
    HRRR and RRFS solutions, suggests these anchored or slowly
    propagating cells will be capable of depositing localized 2 to 4
    inch rainfall totals through the early evening. The 12Z HREF
    strongly supports this potential, highlighting 50 to 70 percent
    probabilities for 1 to 2 in/hr rainfall rates. Given the flashy
    nature of the local basins and a 20 to 40 percent probability of
    exceeding 3-hour Flash Flood Guidance, isolated instances of flash
    flooding are possible as coverage expands this afternoon.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7fkueH4IbLNrn62hzDnSDzxqlNW9Aa7RkqPmvWvsHZILPgr8sRnggEiNJNyd1ynlCTOo= theNzRV6L5U-CDBYRf-rAh4$ for graphic product...

    ATTN...WFO...BMX...FFC...HUN...JKL...LMK...MRX...OHX...

    ATTN...RFC...ALR...ORN...TIR...NWC...

    LAT...LON 36688511 36578455 36098419 35528462 34858543=20
    33898617 33748671 34018750 34798785 35648754=20
    36198699 36488649 36648579=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sun May 31 22:48:45 2026
    AWUS01 KWNH 312248
    FFGMPD
    TXZ000-NMZ000-010300-

    Mesoscale Precipitation Discussion 0288
    NWS Weather Prediction Center College Park MD
    647 PM EDT Sun May 31 2026

    Areas affected...Southwest and West Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 312247Z - 010300Z

    SUMMARY...Expanding coverage of thunderstorms along and just east
    of the dryline will continue through the evening. Some of the
    stronger convective cores will continue to produce rainfall rates
    of 1 to 2 in/hr, with some spotty 2 to 3+ inch totals possible
    through this evening. Additional areas of mainly localized flash
    flooding will continue to be possible, and particularly across
    arroyos and low-water crossings.

    DISCUSSION...GOES-W visible satellite imagery and recent radar
    data coupled surface observations shows a few broken clusters of
    convection already occurring over southwest Texas, with new
    development noted farther north to the east of the dryline across
    west Texas. MLCAPE values of 1000 to 1500 J/kg are noted across
    the region, and while the PW environment is rather modest with PWs
    generally near 1 inch, the cell-motions of the convection are very
    slow given weak steering currents.

    Some additional storms are expected over the next few hours
    heading into the evening hours given expectations of some outflow
    related boundary collisions which will likely foster new cells.
    Cell development farther north along the dryline is expected as
    well which is advertised by the 18Z HREF. The stronger convective
    cores are expected to continue to produce rainfall rates of 1 to 2
    inches, hour with some storm totals by later this evening of up to
    2 to 3 inches possible. This will be facilitated by the slow
    cell-motions, but also a few occasional cell-mergers.

    While the antecedent soils are dry, the regional topography
    features rocky soils, locally steep terrain, and low-water
    crossings that are highly sensitive to intense, short-duration
    rainfall rates. Where these 1 to 2 in/hr rates persist over
    vulnerable basins or urbanized areas, rapid runoff will occur,
    making additional localized flash flooding possible through the
    mid-to-late evening hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-pCKUs6n1qJLHQaZtlsykGyBjX_NW38rHcNHFwWjcq7FMxkTVF-eYrG6z0tyz_kbG8cf= CsOBGcGQzIVIAJEcsrDtCC8$ for graphic product...

    ATTN...WFO...LUB...MAF...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 34280100 34280035 33510021 31610195 29660229=20
    29030328 29270406 29840467 30350498 31080464=20
    32070369 32910286 33740197=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Jun 1 00:53:30 2026
    AWUS01 KWNH 010053
    FFGMPD
    MNZ000-IAZ000-SDZ000-NDZ000-010530-

    Mesoscale Precipitation Discussion 0289
    NWS Weather Prediction Center College Park MD
    852 PM EDT Sun May 31 2026

    Areas affected...Central and Southern North Dakota...Northern and
    Eastern South Dakota

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 010052Z - 010530Z

    SUMMARY...An axis of convection moving through northern and
    eastern SD up through southern and central ND will continue in a
    broken fashion through the evening. Rainfall rates of 1 to 2 in/hr
    will be capable of producing localized 2 to 4 inch totals,
    supporting a localized threat for flash flooding.

    DISCUSSION...Surface observations and recent satellite trends
    depict an expanding axis of broken convection stretching from
    eastern SD through central ND. This activity is pivoting northward
    around the eastern periphery of a deep, elongated upper-level
    trough centered over the northern High Plains. Deep-layer ascent
    is being augmented by shortwave energy slotting up through the
    Dakotas, placing the region under a corridor of favorable
    divergent flow aloft.

    At the surface, a frontal occlusion is slowly shifting eastward,
    with a triple-point surface low analyzed along the border of far
    northern SD and southern ND. Ahead of this boundary, a narrow
    tongue of unstable air featuring MLCAPE values near 1500 J/kg is
    actively pooling. Stronger low-level convergence associated with
    the triple-point low will act to concentrate convective
    development over the next several hours out ahead of it. Given the
    moisture availability and strong forcing, cells will be highly
    efficient, with 18Z HREF guidance supporting rainfall rates of 1
    to 2 in/hr.

    As this system slowly wraps northward, localized training and
    clustering of cells near the surface triple point could easily
    yield localized 2 to 4 inch totals through midnight. While
    antecedent soil conditions are generally capable of absorbing
    initial rainfall, the high hourly rates and cell-training
    potential may support at least localized flash flooding concerns.
    This will especially be the case around any of the more sensitive
    urban locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6LnPVaowbN3z3mBymNXP4qP9cW9IVj1J8epRQbgelo4JtTcPgXdtmn4tUo2dpxyCSbiw= XFXXu6lZ3YPK6MVQSDxD1Ac$ for graphic product...

    ATTN...WFO...ABR...BIS...FGF...FSD...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 47950098 47559959 46589809 45349709 44369661=20
    43829645 43289656 43089721 43429798 44419920=20
    45530035 46670166 47480234 47880194=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Jun 1 04:03:50 2026
    AWUS01 KWNH 010403
    FFGMPD
    MOZ000-KSZ000-010800-

    Mesoscale Precipitation Discussion 0290
    NWS Weather Prediction Center College Park MD
    1202 AM EDT Mon Jun 01 2026

    Areas affected...East Central Kansas to Western Missouri

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 010400Z - 010800Z

    SUMMARY...A cluster of thunderstorms has developed along a
    stationary boundary in east central Kansas. With weak steering
    flow and upscale growth, flash flooding is likely.

    DISCUSSION...A cluster of storms with additional isolated cells
    around it has formed along a stationary boundary across east
    central Kansas this evening. These storms are feeding off PWAT
    values above 1.5 inches, extreme instability over 4,000 J/kg, and
    a 10-20 kt flow at 850 providing moisture advection into the
    storms. The result of all of these favorable ingredients is the
    cluster of storms likely continuing to grow upscale, merging with
    the individual cells around it, especially those to the west, and
    gradual drifting east and southeast along the boundary as the
    storms follow the best advection and instability. Corfidi Vectors
    are 5-10 kts out of the west, which will support slow storm
    motions, with cold pools supporting backbuilding. Recent heavy
    rainfall in the area have lowered FFGs, with 1-hour values
    averaging around 1.5 inches/hour. The storms that have formed in
    the cluster have been producing 2-2.5 inch/hour rainfall rates,
    suggesting that the FFGs will be a low threshold, easily exceeded
    by many of the strongest storms. Flash flooding is likely.

    CAMs guidance is understandably having a difficult time resolving
    the storms. Many of them show clusters of storms forming, but how
    widespread they get and where they go is in poor agreement. As
    mentioned above, it seems likely that the storms will follow the
    stationary boundary they formed along, which will take them mostly
    south of Kansas City and likely north of Joplin, but right turns
    to the south could bring Joplin into the flash flooding threat
    later tonight. A second stationary boundary over central Missouri
    could also support additional storm development over the next few
    hours. Recent heavy rains east of Kansas City there as well will
    also support flash flooding development. Due to the highly
    favorable environment, significant flash flooding is possible,
    especially in any flood prone, urban, and poor drainage areas.

    The storms are likely to persist into Missouri through the
    overnight, so an updated MPD for further east later tonight
    appears probable.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4ZtkUMv2NEJPPo8VPT_yR9bBncYAaPQRxqeskDkue4zDV47vSOcINMHnqpD63O4HdPRY= rrI4DFt3VYb8I2ZCveLHAa8$ for graphic product...

    ATTN...WFO...EAX...ICT...SGF...TOP...

    ATTN...RFC...KRF...ORN...TUA...NWC...

    LAT...LON 39379410 39379351 39239322 38569303 37789296=20
    37349304 36879330 36859400 36919425 37009464=20
    37139560 37539623 37589630 37989678 38519695=20
    38799684 38969663 39209613 39229587 39279530=20
    39329484=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Jun 1 06:13:02 2026
    AWUS01 KWNH 010612
    FFGMPD
    IAZ000-NEZ000-010900-

    Mesoscale Precipitation Discussion 0291
    NWS Weather Prediction Center College Park MD
    211 AM EDT Mon Jun 01 2026

    Areas affected...Southwestern Iowa and Far Eastern Nebraska

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 010611Z - 010900Z

    SUMMARY...A cluster of slow-moving thunderstorms is approaching
    the Omaha/Council Bluffs area from the north. The strongest cells
    are producing rainfall rates approaching 3 inches/hour. Flash
    flooding possible.

    DISCUSSION...A cluster of storms has developed over extreme
    eastern Nebraska into western Iowa this morning. The storms
    consist of slow-moving cells, some of which are training. The
    storms are moving east-southeast, and could threaten portions of
    the Council Bluffs area over the next hour, increasing the flash
    flooding threat. FFGs are around 1.5 to 2 inches per hour, so
    rainfall rates have been exceeding FFGs.

    CAMs guidance has been struggling with this cluster of storms,
    primarily that it's significantly north of the storms further
    south towards Kansas City, and so should be cut off from the best
    moisture advection. However, SPC Mesoanalysis shows MUCAPE values
    ahead of these storms over 2,000 J/kg, and PWATs around 1.3
    inches. Inflow into the storms is a paltry 5-10 kts out of the
    south. While this will support the storms remaining slow-moving,
    it's possible that the inflow will simply not be able to support
    the storms remaining as strong and heavy-rain capable over the
    next couple hours. This would follow with most of the CAMs,
    suggesting this cluster of storms will weaken with time.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9J4REKnPneJM3qN2gFgQ7o3aJAJfj2rquLMf6mKlb_Rus5gsMEPGmwZlsyZsiJBDEfBq= qsWqyA1bAJimu7s84oUdnGc$ for graphic product...

    ATTN...WFO...DMX...OAX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 42139570 41879523 41569476 41149408 40689375=20
    40649413 40679547 41699647 42089623=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Jun 1 08:02:12 2026
    AWUS01 KWNH 010802
    FFGMPD
    ILZ000-MOZ000-KSZ000-011400-

    Mesoscale Precipitation Discussion 0292
    NWS Weather Prediction Center College Park MD
    400 AM EDT Mon Jun 01 2026

    Areas affected...Much of Missouri into Southwestern Illinois

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 010800Z - 011400Z

    SUMMARY...Multiple clusters of storms over Missouri continue to
    pose a flash flooding threat as they increase their eastward
    motions across the state. Flash flooding possible.

    DISCUSSION...Impressive instability persists across much of
    Missouri with over 3,000 J/kg of MLCape across western Missouri. A
    sharp instability gradient roughly follows the Missouri/Illinois
    border near St. Louis. SPC Mesoanalysis shows PWATs roughly around
    1.5 inches over much of Missouri, albeit a bit less in the
    southwestern corner of the state south of Joplin. This should be
    sufficient moisture to allow the storms to persist, especially
    given the ample instability the storms still have to work with.

    The cluster of storms that stretches from Kansas City east between
    I-70 to the south and US-36 to the north consists of multiple sets
    of training cells. Fortunately, other than the Kansas City metro,
    much of this area is rural, which should preclude much impactful
    flash flooding. 1-hourly FFGs also increase to the east to up to
    2.5 in/hr. Further, while the coverage of storms still supports a
    flash flooding risk in that corridor of northern Missouri, the
    individual cells are increasing their eastward forward speed. This
    too should limit the flash flooding risk going forward. Meanwhile,
    a new cluster of storms appears to be forming along the
    Mississippi River, and appears likely to congeal into a line over
    or near St. Louis. This will reintroduce an urban flash flooding
    threat.

    The CAMs continue to struggle with resolving all of the various
    clusters of storms, but those that are showing some depiction of
    the developing line of storms along the Mississippi River suggest
    the storms will struggle to move east of the Mississippi River
    into southern Illinois. While the instability will advect into
    southern Illinois gradually with a southwesterly low-level jet,
    that should mark the rough eastern edge of any flash flooding
    threat, as any storms that progress too far into Illinois should
    weaken with time as the instability rapidly drops to near zero

    For southern Missouri, the flash flooding threat will be much more
    conditional. The cluster of storms in the southeast corner of
    Kansas has generally developed into a line oriented orthogonal to
    the storms' motions. This should greatly reduce the flash flooding
    threat they will pose as they move into southern Missouri.
    Nevertheless, with a few urban centers such as Joplin and
    Springfield ahead of this line, an isolated flash flooding threat
    can't be ruled out.=20

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8S-LjbL-EkJoGRNEtrm9_mhMn_11r8SA6HN25XUH3CkTUBsSvo91sElKB-nRIgQFUp6E= MGmnXyRTxjTkLN4UeSMVNzo$ for graphic product...

    ATTN...WFO...EAX...ICT...LSX...PAH...SGF...

    ATTN...RFC...KRF...MSR...ORN...TIR...TUA...NWC...

    LAT...LON 39739270 39689193 39729127 39489052 39108954=20
    38598918 38108878 37598897 37208941 36949095=20
    36749283 36819372 37009460 37039490 37069538=20
    37119602 37859546 38019498 38329468 39019476=20
    39659424=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Jun 1 11:45:34 2026
    AWUS01 KWNH 011145
    FFGMPD
    TNZ000-KYZ000-INZ000-ILZ000-MOZ000-011700-

    Mesoscale Precipitation Discussion 0293
    NWS Weather Prediction Center College Park MD
    744 AM EDT Mon Jun 01 2026

    Areas affected...Southern IL...Western KY...Western & Middle TN...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 011145Z - 011700Z

    SUMMARY...Repeat/Training thunderstorms expanding downstream of
    matured MCS. Hourly rates up to 2" and totals of 2-3"=20
    approaching FFG values, suggesting localized flash flooding is
    possible this morning.

    DISCUSSION...GOES-E EIR, early visible imagery and regional RADAR
    mosaic denote rapid cooling, convective initiation across western
    KYy expanding into northwest TN downstream of the mature MS across
    the central MS River Valley. GOES-E WV shows compact driving
    shortwave behind the MCS over NW MO with complex moving into
    broadening diffluent flow aloft. This remains supportive of broad
    larger scale ascent, though cold pool generation is supporting
    quicker southeast propagation.=20=20=20

    VWP and RAP analysis still show veering WAA low level flow of
    20-25kts across the MS Valley with slightly increasing downstream
    convergence to support the convective initiation. MUCAPE values
    of 2500-3000 J/kg remain slightly uncapped that this convergence
    was sufficient and the instability corridor extends further
    downstream into Western and Middle TN to suggest potential for
    further expansion/maintenance of the new cells and approaching MCS
    line. In addition to the confluence, the area downstream remains
    a pool of enhanced low to mid-level moisture supporting 1.75" of
    Total PWats, with CIRA LPW denoting even a narrow 700-500 mb axis
    through W KY into Middle TN to help reduce some mid-cloud
    evaporation. As such, common rates of 1.5-1.75" with occasional
    2"/hr values with strongest updrafts will align favorably to
    500-1000mb thickness pattern to support training/repeating
    environment. The limiting factor is likely to be the increasing
    forward propagation due to the cool pool/meso-high driving the MCS
    convective line (as the MCS weakens...noting warming already
    occurring in the main canopy).

    Hydrologically, southern IL remains very dry, with 0-40cm soil
    moisture at or below 25%, but soil conditions steadily moisten
    toward the southeast into Middle TN reaching the 40s and 50+%
    which is average to slightly above average per NASA SPoRT. As
    such, FFG values of 1.5-2"/hr and 2-2.5"/3hrs exist across W KY
    into Western and Middle TN; so there remains a low-end potential
    for exceedance with the best repeating and totals of 2-3" through
    mid-morning, suggesting a localized incident of flash flooding
    remains possible.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9ISqixdOeoJFRMptFgfoxx6dlD77eyKov1zHvLR3EvLUS6LGyJ8VP7IgUjhQoPL_fGeM= tYuJ8Ew5UrWpaCvsQFTuh3g$ for graphic product...

    ATTN...WFO...MEG...OHX...PAH...

    ATTN...RFC...MSR...ORN...TIR...NWC...

    LAT...LON 38178881 37928803 36648708 36028667 35358687=20
    35098735 35298814 35868864 36648928 37418964=20
    37888955=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Jun 1 20:48:59 2026
    AWUS01 KWNH 012048
    FFGMPD
    TXZ000-NMZ000-020245-

    Mesoscale Precipitation Discussion 0294
    NWS Weather Prediction Center College Park MD
    447 PM EDT Mon Jun 01 2026

    Areas affected...Southeast New Mexico... Southwest to West Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 012047Z - 020245Z

    SUMMARY...Slow-moving pulse convection developing over the complex
    terrain of the region will produce heavy rainfall rates of 1 to
    1.5 in/hr through the early to mid-evening hours. Localized
    rainfall totals of 2 to 3 inches may lead to isolated flash
    flooding, particularly across southwest Texas.

    DISCUSSION...Recent radar imagery and visible satellite trends
    show an uptick in convective initiation across portions of
    southeast New Mexico and southwest to west Texas. While the
    primary dryline remains positioned well to the west, intense
    surface heating has allowed for the development of localized
    differential heating boundaries near the terrain. These
    boundaries, working in tandem with orographic ascent along the
    higher terrain, are providing sufficient lift to tap into pockets
    of moderate instability with MLCAPE values ranging from 500 to
    1500 J/kg.

    The resulting convective mode is predominantly disorganized,
    pulse-type thunderstorms given lackluster shear. However, the
    prevailing kinematic environment features weak steering flow,
    resulting in nearly stationary to very slow-moving cells. As a
    result, these storms are capable on an isolated basis of producing
    excessive rainfall totals. Real-time radar estimates indicate
    these cells are locally producing rainfall rates of 1 to 1.5 in/hr.

    Recent high-resolution guidance, including the HREF and REFS,
    supports the potential for localized rainfall totals of 2 to 3
    inches, with the highest concentration expected over the steeper
    terrain of southwest Texas (totals will be slightly lower across
    southeast NM and adjacent areas of west TX). Given the flashy
    nature of the rocky soils, arroyos, and low-water crossings in
    this region, the high-resolution ensembles show a 15 to 30 percent
    probability of exceeding 3-hour Flash Flood Guidance.
    Consequently, isolated instances of flash flooding will be
    possible through the early-to-mid evening hours before the
    boundary layer begins to stabilize.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7Uih-T7g48vRmuvYL5KPaeXPj4T42fvMB0DOEKmhbznEp4xsu1GSW0aaO-2eJ9pikaFi= 23LB9Hx1CY0QEupTTuWuDfA$ for graphic product...

    ATTN...WFO...ABQ...EPZ...EWX...LUB...MAF...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 34450221 34060151 32630167 31450144 30350153=20
    29730221 29390293 29560391 30230449 30620483=20
    31210571 31930616 32700599 33510559 33750500=20
    33510418 33700320=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Jun 1 22:35:44 2026
    AWUS01 KWNH 012235
    FFGMPD
    FLZ000-TNZ000-ALZ000-MSZ000-LAZ000-ARZ000-020430-

    Mesoscale Precipitation Discussion 0295
    NWS Weather Prediction Center College Park MD
    634 PM EDT Mon Jun 01 2026

    Areas affected...Northern/Eastern Arkansas...Northeast Louisiana...Western/Central Mississippi...West-Central to
    Southwest Alabama

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 012234Z - 020430Z

    SUMMARY...Heavy thunderstorms will continue to expand in coverage
    along and ahead of a southward-advancing outflow boundary complex
    this evening. Training convection and localized cell mergers will
    support torrential rainfall rates of 1.5 to 2.5 in/hr. Localized
    totals of 2 to 4 inches may lead to isolated to widely scattered
    flash flooding.

    DISCUSSION...Recent GOES-E visible satellite imagery and regional
    radar mosaics depict a broad, complex corridor of active
    convection spanning portions of the Mid-South. A sprawling outflow
    boundary, originating from ongoing MCS activity over central
    Alabama, extends westward across central Mississippi and arcs back northwestward into northern/eastern Arkansas. This boundary is
    progressively sagging south and southwestward into a highly
    unstable and moisture-rich airmass.

    Latest SPC mesoscale analysis reveals a deeply primed warm sector
    situated ahead (or in this case southwest) of this advancing
    boundary, characterized by pooling MLCAPE of 3000 to 4000 J/kg and
    deep tropical moisture with PWATs approaching 2.0 inches. Lift
    along the primary outflow boundary will continue to sustain areas
    of intense, back-building, and locally training convection.
    Additionally, regional radars show new, discrete convective
    development firing within the warm sector out ahead of the main
    MCS clusters. As the primary boundary and associated line of
    storms advance southward, they will overtake this pre-frontal
    convection, leading to some cell mergers. These localized mergers
    will act to enhance rainfall efficiency.

    The 18Z high-resolution ensemble guidance (including the HREF and
    REFS) supports this regional threat, indicating 10 to 30 percent
    probabilities for 1-hour rainfall totals exceeding 2 inches and
    exceeding localized Flash Flood Guidance across this broader
    domain. Given the extreme instability, rainfall rates will
    frequently reach 1.5 to 2.5 in/hr. Where cell mergers occur or
    training convection anchors along the boundary, localized swaths
    of 2 to 4 inches of rain are expected. This may overwhelm local
    drainage and small streams, resulting in isolated to widely
    scattered flash flooding through the evening. The more sensitive
    urban locations may also see these impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_IbpUvgb5jIfxikqPFfBZdZJAlnSUoTINSDkQn_aVafGWK8EY-FLm3rMpEXFPShCUjSq= QTlM8VUB_HaIiHek34L11g0$ for graphic product...

    ATTN...WFO...BMX...JAN...LIX...LZK...MEG...MOB...SHV...TSA...

    ATTN...RFC...ALR...ORN...TUA...NWC...

    LAT...LON 36429298 36319185 35939108 35249035 34518974=20
    33238876 32408733 31808667 30998705 30838856=20
    31409075 32499209 34299323 35499367 36129357=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Mon Jun 1 23:26:21 2026
    AWUS01 KWNH 012326
    FFGMPD
    KSZ000-NEZ000-COZ000-WYZ000-020515-

    Mesoscale Precipitation Discussion 0296
    NWS Weather Prediction Center College Park MD
    724 PM EDT Mon Jun 01 2026

    Areas affected...Eastern Colorado...Western Kansas...Southeast Wyoming...Southwest Nebraska Panhandle

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 012324Z - 020515Z

    SUMMARY...Ongoing discrete supercells are expected to undergo
    upscale growth into a couple of Mesoscale Convective System (MCS)
    clusters this evening. Rainfall rates will increase as storms
    consolidate, leading to localized 2 to 4+ inch totals. Isolated
    flash flooding is possible.

    DISCUSSION...Real-time radar GOES-W IR satellite imagery across
    the central High Plains reveals scattered, discrete supercells
    ongoing from southeast Wyoming and the Nebraska Panhandle
    southward into eastern Colorado and western Kansas. This initial
    convection is being driven by low-amplitude shortwave energy
    ejecting eastward out of the Rockies, interacting with a
    moderately unstable (MLCAPE 1000-2000 J/kg) and highly sheared
    environment.

    Regional mesoanalysis indicates a south-to-southeast low-level jet
    (LLJ) currently ramping up across the Plains. As this LLJ
    strengthens to 30-40+ knots through the evening, it will maximize
    low-level moisture convergence along a quasi-stationary front
    draped across the region. This coupled with the available
    instability pool should sustain the convective threat well into
    the night with a gradual process of seeing merging/consolidating
    supercells grow into a couple of evolving MCS clusters. This MCS
    activity will then advance east out into the Plains with portions
    of Nebraska and Kansas seeing the impacts deeper into the night.

    Some localized backbuilding and cell-training concerns will exist
    with the thunderstorms which will be capable of producing 1 to 2
    inch/hour rainfall rates given the moistening low-level
    environment and available instability. As the upscale MCS growth
    takes place, some 2 to 4+ inch rainfall totals may materialize and
    this is supported by an overall consensus of the latest hires
    model guidance.

    While the soils across the High Plains can generally absorb this
    initial rainfall, the expected intense hourly rates and some
    persistence of it with the cell-mergers and any cell-training may
    locally overwhelm the infiltration capacities. Where the heavier
    rainfall totals focus, there will be a concern for isolated areas
    of flash flooding which will include some urban impact potential.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4R0Vo7-6acPP4UkvJ1n4DsfKLgy3koNRAqr_GkCEsTpC1QTtRvNT7SVi-HIXRp1QfrRs= JSbNzKMiVzRuLLF3RT4tqco$ for graphic product...

    ATTN...WFO...BOU...CYS...DDC...GID...GLD...ICT...LBF...PUB...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 42110415 42090320 41320212 40330081 39599946=20
    38729824 37559827 37099907 37040017 37240135=20
    37720238 38280298 38670378 38980430 39500456=20
    40260456 41140487 41750481=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Jun 2 04:33:46 2026
    AWUS01 KWNH 020433
    FFGMPD
    MSZ000-LAZ000-ARZ000-020800-

    Mesoscale Precipitation Discussion 0297
    NWS Weather Prediction Center College Park MD
    1232 AM EDT Tue Jun 02 2026

    Areas affected...Western Mississippi into Northern Louisiana

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 020432Z - 020800Z

    SUMMARY...Clusters of storms developing in an unstable and highly
    moist environment with weak steering flow may cause isolated
    instances of flash flooding into western Mississippi and Northern
    Louisiana.

    DISCUSSION...Clusters of storms have developed across portions of
    western Mississippi and far southern Arkansas this morning. The
    storms are in an environment characterized by PWATs around 1.75
    inches, 2,000 to 4,000 J/kg of MUCAPE, and flow in the lowest 400
    mb of atmosphere that is light and variable, as evidenced in the
    00Z Shreveport sounding. The storms in Mississippi have a hsitory
    of producing rainfall rates to 2 inches per hour. While that alone
    does not exceed the hourly FFGs in the area around 2.5 inches per
    hour, the very slow movement of the associated heavy rains could
    find some areas seeing 1-2 hours of heavy rain, so the 3-hr FFGs
    in the 3-4 inch range could be exceeded in places where the heavy
    rain is most persistent.



    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8UW7UTALyjFj6DrocfaVek0FD-UmfQVLDew5y6zoMT4DyUfho-htuVtAHWAvOdZ0PMjd= xG_x_10VayzTpCMA6uCP3Eo$ for graphic product...

    ATTN...WFO...JAN...LZK...SHV...

    ATTN...RFC...ORN...NWC...

    LAT...LON 33569003 33298984 32898981 32248976 31649021=20
    31529091 31599176 31789239 32319291 32899322=20
    33169322 33399283 33499187 33549138=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Jun 2 04:35:16 2026
    AWUS01 KWNH 020435
    FFGMPD
    MSZ000-LAZ000-ARZ000-020800-

    Mesoscale Precipitation Discussion 0297
    NWS Weather Prediction Center College Park MD
    1234 AM EDT Tue Jun 02 2026

    Areas affected...Western Mississippi into Northern Louisiana

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 020432Z - 020800Z

    SUMMARY...Clusters of storms developing in an unstable and highly
    moist environment with weak steering flow may cause isolated
    instances of flash flooding into western Mississippi and Northern
    Louisiana.

    DISCUSSION...Clusters of storms have developed across portions of
    western Mississippi and far southern Arkansas this morning. The
    storms are in an environment characterized by PWATs around 1.75
    inches, 2,000 to 4,000 J/kg of MUCAPE, and flow in the lowest 400
    mb of atmosphere that is light and variable, as evidenced in the
    00Z Shreveport sounding. The storms in Mississippi have a history
    of producing rainfall rates to 2 inches per hour. While that alone
    does not exceed the hourly FFGs in the area around 2.5 inches per
    hour, the very slow movement of the associated heavy rains could
    find some areas seeing 1-2 hours of heavy rain, so the 3-hr FFGs
    in the 3-4 inch range could be exceeded in places where the heavy
    rain is most persistent.

    CAMs guidance has been struggling with the developing convection
    in the area, particularly the HRRR. The RRFS depiction shows a
    cluster of storms that appears most similar to the current radar
    presentation. It suggests the storms will gradually drift south of
    west with time, likely following the pocket of highest instability
    in far northern Louisiana. This appears plausible as cold pools
    and storm-created forcings will likely drive additional
    development going forward. Moisture levels gradually increase with
    decreasing latitude, so there will be no shortage of moisture for
    the storms to work with, suggesting they will likely persist, as
    instability too remains plenty high enough for the storms to be
    sustained.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-l3jic8lPcqv8G7B7M2U5CpgfbvsL9pXuhKpM07DQgKnYw6mBOX-llI_47w2CEREyVNv= L__ozOafg18tkDv-9tLSYvI$ for graphic product...

    ATTN...WFO...JAN...LZK...SHV...

    ATTN...RFC...ORN...NWC...

    LAT...LON 33569003 33298984 32898981 32248976 31649021=20
    31529091 31599176 31789239 32319291 32899322=20
    33169322 33399283 33499187 33549138=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Jun 2 16:55:28 2026
    AWUS01 KWNH 021655
    FFGMPD
    TXZ000-NMZ000-022245-

    Mesoscale Precipitation Discussion 0298
    NWS Weather Prediction Center College Park MD
    1253 PM EDT Tue Jun 02 2026

    Areas affected...southeastern NM into western TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 021652Z - 022245Z

    SUMMARY...Scattered slow-moving thunderstorms are expected to form
    through the afternoon across southeastern NM into western TX. Rain
    rates of 1 to 2 inches in 30 to 60 minutes can be expected with a
    few cells which may result in widely scattered areas of flash
    flooding.

    DISCUSSION...1630Z visible imagery from GOES East showed mostly
    clear skies beneath some high clouds across southeastern NM into
    western TX. The exception was across the Sacramento Mountains with
    early convective initiation ongoing over northern Otero County.
    Moisture values have increased a few tenths of an inch compared to
    24 hours ago as seen in blended TPW imagery with 1.0 to 1.1 inches
    nosing in across southeastern NM as of 15Z.

    Low level flow is forecast to back and increase in magnitude
    slowly but steadily through the afternoon and early evening beyond
    18Z across the southern High Plains with 850 mb winds forecast by
    the RAP to reach 15-20 kt by 21Z. This will occur out ahead of an
    eastward advancing mid to upper-level shortwave over southeastern
    NM and as 850 mb ridging builds southward into OK and TX through
    00Z. In addition, left-exit region divergence and diffluence from
    an upper level jet max extending eastward across northwestern
    Mexico is likely to boost larger scale ascent across the region.

    Continued daytime heating is expected to lead to the
    development/expansion of 500-1500 J/kg MLCAPE with decreasing
    inhibition (via RAP guidance) into the afternoon. Typical
    development along the higher terrain is expected first, followed
    by subsequent development on outflows and within the unstable
    airmass. Standardized PW anomalies of +1 to +2 combined with slow
    cell motions (deeper layer mean layer flow of 5 to 15 kt on
    average) is expected to allow for some stronger/slower moving
    cells to produce 1 to 2 inches of rain in 30-60 minutes. Total
    rainfall of 1 to 2 inches will be most common from thunderstorms
    but localized totals of 2 to 3+ inches cannot be ruled out on an
    isolated basis into early evening.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!-i6Nnj5hC2iwpTSuBN1jkprDbFtX8OZEmyZa3o6pWF0LfMN0E-MkB8GsUd6CE_vTF35e= 5Q-ZOJShOyG7ryLbax4y74Q$ for graphic product...

    ATTN...WFO...ABQ...EPZ...MAF...

    ATTN...RFC...FWR...NWC...

    LAT...LON 34320522 34160462 33760399 33110345 31350321=20
    30270270 29710269 29230292 29050325 29060351=20
    29270381 29490421 29700446 30200473 30650503=20
    31140550 31480584 31840609 32700593 33530606=20
    34260575=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Jun 2 18:17:08 2026
    AWUS01 KWNH 021817
    FFGMPD
    TXZ000-OKZ000-COZ000-NMZ000-030000-

    Mesoscale Precipitation Discussion 0299
    NWS Weather Prediction Center College Park MD
    216 PM EDT Tue Jun 02 2026

    Areas affected...southern High Plains

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 021814Z - 030000Z

    SUMMARY...Slow moving thunderstorms may produce a few areas of
    flash flooding across northeastern NM into southeastern CO and the
    adjacent TX/OK Panhandles through 00Z. Hourly rainfall of 1 to 2
    inches but with 15-30 minute rates of 0.5 to 1.0 inches are likely.

    DISCUSSION...18Z radar and infrared satellite imagery showed a few
    slow moving cells over northeastern NM with a pair of supercells
    over southern San Miguel and northern Guadalupe counties, near a quasi-stationary frontal boundary. While shear for organized cells
    was on the lower end of the spectrum, MLCAPE was estimated at
    1000-2000 J/kg from northeastern NM into the southern TX Panhandle
    (latest SPC mesoanalysis) with easterly low level flow aiding
    convection via upslope lift. ~15 kt of flow was noted via VAD 850
    mb wind plots at KAMA, KFDX and KLBB and these winds are expected
    to continue through the remainder of the afternoon with local
    enhancement due to outflow.

    850-300 mb mean winds were ~10 to 15 kt from the south across the
    southern High Plains with slower and "right" of the mean wind
    motions forecast for right moving supercells. Aloft, there should
    be some modest contribution from weak right-entrance region upper
    jet forcing, focusing upper level divergence and diffluence across
    the eastern CO/NM border into eastern NM.

    Scattered thunderstorms will continue over the next several hours
    with potential for outflow boundaries and storm mergers to result
    in locally higher rates. Hourly rainfall of 1 to 2 inches is
    expected but sub-hourly rainfall of 0.5 to 1.0 inches in 15-30
    minutes may contribute to flash flooding in a few locations as the
    afternoon progresses.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4hotqj1fgLF0gcz7YHAuxQrxzHw94h5KotRqMXTxrMv3v-NFeZF7NbtoicErOU7oK68l= PY87NkLFKplgOK2GkxlaNcs$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...PUB...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 37730414 37490241 36020229 34560284 34280444=20
    34340568 34310639 34700643 35230633 35730597=20
    36360565 36590555 37100545 37430505=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Jun 2 19:47:47 2026
    AWUS01 KWNH 021947
    FFGMPD
    SDZ000-NDZ000-030130-

    Mesoscale Precipitation Discussion 0300
    NWS Weather Prediction Center College Park MD
    346 PM EDT Tue Jun 02 2026

    Areas affected...Central ND...Western SD...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 021945Z - 030130Z

    SUMMARY...Short-term repeating of 1.25-1.5"/hr rate cells may
    result in streaks of 2-3" totals in a highly dynamic environment.=20
    Dry soil conditions likely to limit coverage to those most intense
    downdrafts; though a spot or two of localized flash flooding
    remains possible.

    DISCUSSION...GOES-WV suite depicts a broad closed low along the Saskatchewan/Montana border with vigorous internal vorticity
    centers embedded within it; with a strong jet streak/internal wave
    starting to distort the wave more toward the southeast providing
    solid downstream dPVA. Along the outer influence of the low is an
    elongated 500mb wave rapidly moving northeast but along a tight
    shear axis and nose of 70kt 300mb jet streak lifting north
    centered at the MT/SD/ND corner. This helps to sharpen a
    stationary frontal zone from far southeast Saskatchewan to KDIK
    toward a developing surface wave northeast of KGCC, NW of W43 in
    far NE WY. The strength and depth of moisture return east of the
    boundary has brought mid to upper 50s and isolated low 60s Tds
    through much of the area of concern, enough so to delineate an
    effective dry line across far NE WY as well.

    Strengthening moisture flux convergence along the boundary and the
    broad scale ascent aloft has resulted in the initial convection at
    the front in W ND back to northeast SD, which has kicked out an
    initial outflow boundary. Though accelerated backed low level
    flow around the Black Hills has helped in further moisture flux
    convergence along/down-shear of the developing surface wave,
    resulting in the strongest, most persistent convection so far this
    afternoon. Backed low level moisture flux is helping to bring
    total PWats into the 1.25-1.5" range and with 15-25kts of inflow
    with further isallobaric influence is likely to increase rainfall efficiency/potential with time. Shortwave ridging as the jet
    streak slides by (with right entrance ascent help) will further
    back to support short-term deep layer fairly unidirectional
    steering flow to allow for repeating/training along the front
    before cold pools and height-falls help to forward propagate the front/convective line toward mid to late evening. Rates of
    1.25-1.5"/hr and repeating may allow for streaks of 1.5-2.5"
    totals to accumulate in NW SD into south-central ND.

    Further south, the effective dryline accompanied by the exiting
    jet streak as well as ideal southeasterly flow into the Black
    Hills has supported mass convergence and similar shape/orientation
    of the inflection denoted further northwest. As such, similar
    cluster growth with repeating potential could exist across SW SD
    into the Badlands through evening, spots of 1.5-2.5" may result as
    well in the shortest term period.

    As heating peaks and low-level jet increase, expansion of the
    clusters into complexes may result further supporting increasing
    rainfall efficiency toward 1.5"/hr with an occasional localized
    uptick to 2" locally possible. By this time, forward propagation
    may limit residency but spots of 1.5-3" will be possible,
    particularly across north-central ND into northeast ND where
    instability and moisture flux will be greatest after 00z.

    The uncertainty toward incidents of flash flooding is the mixed
    signals of naturally low FFG values across much of the area of
    concern with 1-1.5"/hr and generally below 2.5"/3hr (though some
    spots are as low as 1.5"/3hrs), juxtaposed by soil moisture values
    generally ranging below 30% (though spots of 40+ exist along the northern/eastern ring of the Black Hills). The longer drought
    should allow for uptake but the most intense (1.25-1.5"/hr) rates
    likely limiting the overall coverage and an incident or two of
    localized flash flooding through 01z.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8tjltLOMJ4r2lZ8tWim7F16OyOh5GMnZyzjwzHEfbGEHESp-EZ75imAg-wfEhV6c9Qx7= 4v4DZwbOyL-Nt5IIO-5cWZE$ for graphic product...

    ATTN...WFO...ABR...BIS...FGF...UNR...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 49049986 48939810 47499923 44170090 43190145=20
    43030209 43030386 43360395 44010333 44690353=20
    45200357 46230273 48320165 48980124=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Jun 2 22:21:07 2026
    AWUS01 KWNH 022221
    FFGMPD
    TXZ000-NMZ000-030400-

    Mesoscale Precipitation Discussion 0301
    NWS Weather Prediction Center College Park MD
    619 PM EDT Tue Jun 02 2026

    Areas affected...Western TX Panhandle...Southeastern NM &
    Adj.Portions of TX N Panhandle...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 022220Z - 030400Z

    SUMMARY... Widely scattered incidents of flash flooding remaining
    possible with cell mergers and/or repeating capable of quick
    1-1.5" and localized additional 2"+ totals as clusters organized
    into forward propagating complex.

    DISCUSSION...Terrain focused initial convective development has
    matured into a few clusters across the Southwest High Plains and
    West TX Panhandle and is starting to organize while seeking out
    remaining conditionally unstable air across southeast NM and along
    the slowly sagging cold front from the Big Country of NW TX into
    central Cap Rock. MLCAPE values of 2000-2500 J/kg are denoted
    with a minimum running between across the core of the Permian
    Basin, though values remain generally above 1000 J/kg. Though
    moisture flux continues to increase in overall depth out of the
    Pecos River Valley and along the front toward the maturing/growing
    clusters. The northern complex remains a bit more linear but is
    slowly sagging south to south-southeast along the
    instability/moisture flux stream ahead of the front while the
    southern instability stream rings the Dell Valley emerging from
    the Sacramento and Hueco Ranges. Moisture has deepened
    sufficiently to surge through the gap into the Rio Grande Valley
    and points west in S NM allowing other lower ranges to increase in
    convective activity over the last few hours as well.

    Aloft, broad diffluence between a weak shortwave in northeast NM
    and the main Southwest closed low in S AZ is providing increasing
    divergence aloft in proximity of SE NM further aiding upscale
    growth environment as the clusters seek out these instability
    pockets. Strengthening low level flow toward sunset will further
    help forward propagation to the east/southeast and promote cluster
    mergers. Deep layer moisture of 1.25" (mainly driven below
    700mb...noted by surface Tds in the low 60s) will allow for quick
    efficient rainfall production with limited evaporative loss as the
    clusters march east. These mergers will likely be the greatest
    potential for sub-hourly 1.5" totals and may result in isolated to
    scattered incidents of 2" totals and result in widely scattered
    incident or two of rapid run-off and flash flooding conditions
    through the early overnight period.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!67KdieroNj6QVQ3LO7avwxKOocXQzWFYkRd2uNzMvDIx9TAi4XELcVX2kYo7ZVvUAlI0= wsuBz4EDJYfchBHPwJsJv4o$ for graphic product...

    ATTN...WFO...ABQ...AMA...EPZ...LUB...MAF...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 36430215 36170140 35360151 34790197 34160237=20
    33180280 32120294 31330275 30820262 30230287=20
    29870352 29940446 30410500 30750540 31480614=20
    32700648 33190705 33600730 34140708 34910561=20
    35320475 35730388 36130308=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tue Jun 2 23:48:13 2026
    AWUS01 KWNH 022348
    FFGMPD
    MNZ000-SDZ000-NDZ000-030530-

    Mesoscale Precipitation Discussion 0302
    NWS Weather Prediction Center College Park MD
    746 PM EDT Tue Jun 02 2026

    Areas affected...Central and Eastern ND...North-central SD...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 022345Z - 030530Z

    SUMMARY...Favorable repeating/training along pre-frontal
    convergence trough poses risk of localized 2-3" totals and
    localized flash flooding through early overnight period.

    DISCUSSION...GOES-E Visible loop shows a deep layer confluence
    axis, generally aligned with the deeper moisture/q-axis has
    recently destabilized with numerous narrower updrafts expanding
    along it. The elongated mid-level trough and associated dPVA
    rapidly moved northeast across NW ND into southern Canada which as
    resulted in the deep layer confluence from 925 to 700 to maximize
    moisture flux convergence to overcome the weakening capping in the
    region. This is generally in advance of the larger scale
    height-falls and expanding right entrance region to strengthening
    jet expected over the next 2-4 hours arriving from the west.=20

    CIRA LPW and VWP shows shows enhanced 25-30kts of 850-700mb flow
    with .5-.75" through both lower layers helping to reach near 1.5"
    of Total PWat. The clearer skies east of the initial development
    further helped with insolation and increase of MLCAPEs over 2000
    to 2500 J/kg. As such, the strength/coverage of the updrafts
    should continue to blossom over the next few hours and support
    1.25-1.5"/hr rain rates, toward the base of the best deep layer
    convergence in north central SD. The key toward flash flooding
    will be the increased residency given the increase in overall
    convective coverage, vertical moisture loading with stronger
    updraft strength but most importantly the expected longer south to
    north deep layer steering. 850-400mb mean flow is a bit east of
    due north, but fairly parallel to the instability and low level
    convergence axis. Combine this with expanding area of divergence
    aloft into strengthening jet to the northwest and there are
    increasing probabilities of localized residency of a few hours due
    to repeating/training. This is greatest further north along the
    ND/Canadian border where a few rounds of supercells have already
    occurred and pre-wet the upper soil profiles.=20

    Localize streets of 2-3" are possible which would locally exceed
    the lower FFG values in the area. As such, the potential for
    localized flash flooding remains possible through the remainder of
    the evening into the early overnight period.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!62gv9KTMOBZUcBoohXmYVhiemsjf1BxkiSrXYbni1-n0Fv4MFutlyCsnw3ynnx1XDMr_= SU4Mzm3t3WXYEfrV86YfLYw$ for graphic product...

    ATTN...WFO...ABR...BIS...FGF...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 49049732 48919655 47789703 46749766 45579860=20
    45190008 45670118 46560121 47730072 48909999=20
    49039926=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Jun 3 01:07:25 2026
    AWUS01 KWNH 030107
    FFGMPD
    SDZ000-WYZ000-030700-

    Mesoscale Precipitation Discussion 0303
    NWS Weather Prediction Center College Park MD
    906 PM EDT Tue Jun 02 2026

    Areas affected...Southwest & Central SD...Far Northeast WY...

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 030110Z - 030700Z

    SUMMARY...Favorable environment for multiple rounds of intense
    heavy rainfall, likely to cross already saturated/flooding ground
    conditions. Localized flash flooding likely to continue through
    early overnight period.

    DISCUSSION...GOES-E shows small/compact shortwave in NE WY along
    the southeast periphery of the deep large scale closed low
    centered over S Saskatchewan continuing to provide strong dPVA
    ascent along/downstream across southwest SD helping to maintain a
    few small clusters/developing convective complexes, while also
    maintain isallobaric backed southeasterly flow to the developing
    surface wave near KW43 west of the Black Hills. An effective
    dryline bulge is starting to spread through the Black Hills with
    Tds dropping into the 40s and so surface FGEN forcing has be able
    to maintain/focus the upstream convective cluster across SW SD
    while additional new development has been filling in along the
    wedge from the surface low and north of the Hills but southeast of
    the stationary front. As such, streamlines continue to suggest
    effective moisture flux and base loading of moisture to support
    1.5"/hr rates.

    As the shortwave passes, the upper-level flow becomes increasingly
    diffluent especially as the right entrance to the strengthening
    jet over W ND expands toward 90-100kts by 04-06z later tonight.=20
    As such, upscale maintenance of the developing convection into a
    larger cluster with favorable orientation to WSW to SW steering
    flow should allow for some short-term training as well as
    repeating from the initial convective cluster that is starting to
    bow across the Missouri River Valley. Mesoscale features suggest
    some WAA, storm/meso-scale interaction between clusters that
    should orient parallel to the mean flow across southwest to
    south-central SDak tonight. However, proximity to mid-level
    drying should help to generate some cold pools and mitigate
    prolonged residency. Still, spots of 2-4" are probable and given
    already lowered FFG (3hr values of 1-2.5"; west to east), it is
    likely to exceed to maintain ongoing flash flooding, as well as
    potentially expanding to other nearby locations downstream toward
    central SD through the early overnight period.=20


    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9P4gsfHOulWX2hlChE2W6zqHbCqU6W9OYsIbVOB53JU-MEMOaEh9qQzJa-4O1660VAKk= XCbCwnjLEyRCoUzlvLGFBhw$ for graphic product...

    ATTN...WFO...ABR...FSD...UNR...

    ATTN...RFC...KRF...NWC...

    LAT...LON 45520161 45369920 45009819 43869808 43129887=20
    43030022 43020158 43060302 43230349 43780356=20
    44270373 44560470 44960402 45370320=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Jun 3 04:08:37 2026
    AWUS01 KWNH 030408
    FFGMPD
    TXZ000-NMZ000-030900-

    Mesoscale Precipitation Discussion 0304
    NWS Weather Prediction Center College Park MD
    1207 AM EDT Wed Jun 03 2026

    Areas affected...West Texas and the Texas Panhandle

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 030406Z - 030900Z

    SUMMARY...A slow-moving line of storms combined with cell-mergers
    will continue producing widely scattered instances of flash
    flooding through much of the overnight.

    DISCUSSION...A line of convection consisting of several clusters
    of very slow moving storms is drifting east towards the
    north-south extension of the Texas border. In addition to slow and
    chaotic cell motions of storms embedded within the line,
    additional clusters of storms are forming east of the line. These
    clusters have been both growing upscale and tracking northwestward
    towards the line. Thus, cell-mergers, interactions between storms,
    and continued slow movement will continue supporting extended
    durations of heavy rainfall to 2 inches per hour for the next
    several hours. PWATs ahead of the line range from 1.1 to 1.4
    inches in SPC Mesoanalysis. Instability values range from between
    2,000 and 3,000 J/kg across West Texas, which should also allow
    the storms to persist as they move into that environment.
    Near-term model guidance shows that instability will wane through
    the overnight hours, which is typical, that waning will be slow,
    with instability likely still around 1,000 J/kg by the wee hours
    of the morning. FFGs are generally between 2 and 2.5 inches per
    hour, and between 2.5 and 3 inches per 3 hours over the affected
    area. While storms may struggle to reach those 1-hourly
    thresholds, the slow movement suggests that the 3-hourly values
    will be more attainable. Urban areas such as Amarillo and Lubbock
    will each have a higher flash flooding threat, especially due to
    the increasing probability that cell mergers will occur near or
    over those cities over the next few hours.

    CAMs guidance are in remarkably similar agreement that the line
    will continue to drift east into West Texas and the Texas
    Panhandle, driven by a 20-25 kt southeasterly flow of moisture and
    instability from out of central Texas. Since instability only
    slowly diminishes, and there is a consistent feed of additional
    moisture for the storms to feed on, it's likely overall storm
    motions will be driven by the much smaller mesoscale or microscale
    features such as cold pools.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7IwD0hCyBTrJ9oPtMwtnjMPweAseoLPXoJ13fiRoWQGGPABrW39Uq4mhif7sP_ytPL4o= A78oBUldJ89R876H2mEkhPY$ for graphic product...

    ATTN...WFO...ABQ...AMA...LUB...MAF...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 36470257 36280141 35890100 35160101 33530101=20
    32570105 32130137 32070209 32320240 32500307=20
    32520364 32630380 32960412 33620410 34440393=20
    35260361 36060343 36350314=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Jun 3 05:31:48 2026
    AWUS01 KWNH 030531
    FFGMPD
    MNZ000-NDZ000-031000-

    Mesoscale Precipitation Discussion 0305
    NWS Weather Prediction Center College Park MD
    130 AM EDT Wed Jun 03 2026

    Areas affected...Northeastern North Dakota

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 030530Z - 031000Z

    SUMMARY...Training showers and thunderstorms continue across
    northeastern North Dakota. Rates to 2 inches/hour could continue
    with the strongest storms for another few hours, causing
    additional instances of flash flooding.

    DISCUSSION...A line of training thunderstorms has set up across
    northeastern North Dakota this morning. The storms are the result
    of a significant 25-35 kt low level jet at 850, advecting moisture
    up to 1.4 inch PWATs into the line of storms. Instability remains
    around 1,000 J/kg, which should allow the line of storms to at
    least persist with similar intensity for the next few hours. The
    entire complex of storms have been gradually translating
    northeastward, but with significant backbuilding across central
    North Dakota.

    At the surface, an area of low pressure over north-central North
    Dakota has a cold front draped to its south, with a trough to the
    east. These features are helping anchor the storms over the area,
    supporting the very slow movement of the entire complex, even
    though individual cells are advecting northeastward. FFGs are
    around 1.5-2 inches in central ND, lowering to between 1 and 1.5
    inches per hour near the Minnesota border. This lowering near
    Minnesota is the result of a widespread 2.5 inches of rain that
    has fallen thus far into the northeast corner of ND. With
    additional storms actively forming and advecting in that same
    direction, it appears the area along I-29 from Grand Forks north
    to the Canadian border appears at greatest risk for developing
    additional flash flooding.

    CAMs guidance is struggling with this feature. This is especially
    true of all the guidance outside of the HRRR and RRFS. Thus,
    focusing on those two models, they both suggest the storms will
    hang on across this region through much of the rest of the
    overnight hours, likely significantly weakening in intensity
    towards morning. For this reason, the flash flooding threat should
    remain elevated for the next few hours, then diminish with the
    weakening rainfall rates.

    Wegman

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4mvQmcXzGFe0iZTk7FR1pIWNf81fFreyQAiR7hxGMAcVsC-wG414Td3f7LVOH1GyasJx= k25Nwk8JtHO3zuqlziRKI-o$ for graphic product...

    ATTN...WFO...BIS...FGF...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 49069869 49039628 47929679 47789739 47459900=20
    47129960 46910007 46980076 47320117 48100099=20
    48410013 48609956=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Jun 3 15:27:51 2026
    AWUS01 KWNH 031527
    FFGMPD
    FLZ000-032125-

    Mesoscale Precipitation Discussion 0306
    NWS Weather Prediction Center College Park MD
    1126 AM EDT Wed Jun 03 2026

    Areas affected...southeastern FL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 031525Z - 032125Z

    SUMMARY...Scattered thunderstorms are expected to produce mainly
    an urban flash flood threat for portions of southern FL through
    the late afternoon. Peak hourly rainfall of 2 to 3+ inches will be
    likely with stronger cores but with high sub-hourly rates which
    will allow for efficient runoff atop paved surfaces.

    DISCUSSION...1515Z radar imagery across southern FL and the
    offshore waters showed widely scattered showers and thunderstorms
    with recent development south of FLL. These cells were occurring
    near and south of a cold front which was gradually advancing south
    across the south-central FL Peninsula. Surface dewpoints to the
    south of the cold front were in the middle to upper 70s,
    supporting high precipitable water values near 2 inches. OSPO ALPW
    imagery showed that contributions to moisture were high at all
    levels of the atmosphere and wet bulb zero heights were estimated
    to be 13 to 14+ kft via the 12Z KEY and RAP analysis soundings,
    supportive of efficient rainfall generation. MLCAPE was estimated
    at 500-1500 J/kg over the southeastern and southern Peninsula with
    weakening inhibition via surface heating through cloud cover (via
    SPC mesoanalysis data).

    As the base of a mid-level trough off of the southeastern U.S.
    coast continues to dig southward, the cold front will maintain a
    steady southward movement, possibly reaching Alligator Alley by
    00Z. While low to mid-level winds are weak, and should not support
    much in the way of organized cells, steering flow over southern FL
    to the south of the cold front is also weak. Currently, deeper
    layer mean winds are from the west at ~10 kt and are forecast to
    weaken to closer to 5 kt while veering toward the north through
    00Z.

    Continued weakening inhibition with surface heating should lead to
    the increased coverage of scattered showers and thunderstorms over
    the next 3 hours. Cells should follow a general movement toward
    the east to south with mergers and collisions supporting rain
    rates of 1 to 1.5 inches in 15 minutes and 2 to 4+ inches in 1 to
    2 hours. While coverage is expected to remain widely scattered,
    these high rates will pose a risk of flash flooding should they
    overlap with the urban southeastern FL corridor.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7FB3G6Ceb_1ALPOKJwothyXO4wZna0h-6TFEYKKLbTsLHW6pDaPrNDUGOIs3obx7llDm= E7kwgF6anR1Ia_a-yZdhE-w$ for graphic product...

    ATTN...WFO...KEY...MFL...MLB...

    ATTN...RFC...ALR...NWC...

    LAT...LON 27107997 26447980 25717986 25328013 25198059=20
    25628070 26188056 27058045=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Jun 3 17:33:04 2026
    AWUS01 KWNH 031732
    FFGMPD
    TXZ000-NMZ000-AZZ000-032330-

    Mesoscale Precipitation Discussion 0307
    NWS Weather Prediction Center College Park MD
    131 PM EDT Wed Jun 03 2026

    Areas affected...NM/west TX into southeastern AZ

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 031730Z - 032330Z

    SUMMARY...Isolated to scattered areas of flash flooding will be
    possible across a sizable portion of NM into far western TX and
    southeastern AZ. Slow moving cells will have the potential to
    produce 1 to 2 inches of rainfall in 30-60 minutes, with the flash
    flood threat continuing into the evening hours.

    DISCUSSION...GOES-E visible imagery at 17Z showed the early stages
    of cumulus development across the higher terrain of the Colorado
    Plateau into the Black Range and Sacramento Mountains. Skies were
    mostly clear over the Southwest (except eastern NM) allowing for
    surface heating and the expansion of instability. 17Z SPC
    mesoanalysis data showed 500-1500 J/kg MLCAPE (highest over
    southwestern NM) but with varying degrees of convective inhibition
    remaining. Blended TPW satellite imagery showed moisture was
    similar to this time yesterday over the eastern third of NM but
    higher for central NM into eastern AZ with standardized PW values
    presently at +1 to +2 throughout the region.

    Large scale forcing in the mid-levels showed NM was between a
    northward departing shortwave along the northern NM/TX border and
    a closed low west of the Baja Peninsula with weak shortwave
    ridging in between the two disturbances. With a lack of larger
    scale forcing in place, steering flow aloft was weak at less than
    10 kt for most of NM into eastern AZ. Thunderstorms are expected
    to form over the higher terrain over the next 1 to 2 hours with
    subsequent development on storm induced outflows and within the
    increasingly unstable airmass through the mid-afternoon.
    Increasing coverage of cells and mergers will enhance rain rates
    in a few locations with 1 to 2 inches in 30-60 minutes likely.
    These rates will be especially problematic should they overlap
    with sensitive burn scars or other locations with poor
    infiltration, possibly leading to flash flooding on an isolated to
    scattered basis.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4w7n4MR3qcvHGlcDItbro2FtLCAkH85NCfOeKdKU0xy2AzhpsTHQEZx37hVYfLxZMJ4e= ZEXkM1GVmzVnsShMzJbMT14$ for graphic product...

    ATTN...WFO...ABQ...EPZ...FGZ...MAF...PSR...TWC...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 36930421 36700325 36300339 35220432 34230472=20
    32790422 31030390 30170416 30040539 30530603=20
    31110681 31260822 31220966 31551015 32501030=20
    33421017 34000970 34480850 35610756 35990680=20
    36800539=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Jun 3 19:48:46 2026
    AWUS01 KWNH 031948
    FFGMPD
    TXZ000-OKZ000-KSZ000-040130-

    Mesoscale Precipitation Discussion 0308
    NWS Weather Prediction Center College Park MD
    347 PM EDT Wed Jun 03 2026

    Areas affected...Southwest KS...Eastern Panhandle and Northwest
    OK...Northeast TX Panhandle...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 031950Z - 040130Z

    SUMMARY...Favorable environment for repeating/training of
    thunderstorms; however, soil conditions will require this
    prolonged duration, moderate to high intensity to result in
    localized flash flooding, yet a spot or two remains possible.

    DISCUSSION...Convective initiation is starting to expand across
    the eastern quadrant of the older MCV from last night's convective
    complex. That MCV is currently at the corner of CO/NM and OK
    borders with a secondary smaller MCV near the Palo Duro Canyon
    lifting northward along the weakly defined mid-level shear axis
    that extends southeast across central TX. Further aloft, the
    core of the upper-level ridge is over central OK allowing for
    right entrance ascent and favorable outflow environment exiting to
    the 60-70kt jet streak over E CO.=20=20

    Surface to boundary level response shows strong directional
    convergence with backed, moist flow with Tds in the low to mid 60s
    across central OK, intersecting with southwesterly flow from a
    fairly strong 2021mb meso-high along the NM/TX border north of
    Clovis. Clear skies between the MCV features also has allow for
    solid insolation with temps rising into the low to upper 80s from
    SW KS into NW OK; supporting MLCAPEs to 2000 J/kg, increasing
    further north into KS. So the combination of surface convergence,
    solid vertical ascent capability and outflow aloft will maintain
    convective activity along the northwest edge of the moisture axis
    which will increases from just below 1.5: toward 1.7" into late
    evening. This will encourage rates of 1.5-1.75"/hr.=20

    Given placement of the MCVs, deep layer steering is also generally
    weak and fairly unidirectional/confluent into the right entrance
    of the jet streak in E CO. Given confluence/convergence axis is
    fairly parallel to the mean flow, and strengthening upstream
    inflow supportive of back-building should allow for some
    repeating/training through the afternoon into evening period.=20
    Propagation toward the east and northeast may disrupt ideal
    repeating but at 5-10kts, it should deviate that much.

    However, hydrologically, the area has naturally higher FFG but has
    also been in a prolonged drought. NASA SPoRT 0-40cm soil moisture
    values are in the single digits in many places, though portions of
    SW KS have seen some relief with values back to near or just below
    normal in the 40s; as such FFG values are high across TX/OK near
    3-4"/hr; but are 1-2"/hr and 1.5-2.5"/3hrs in KS). Expected
    rates are not so extreme to overwhelm infiltration, but localized
    2-3" totals may become an issue more so in SW KS, though a few
    towns in TX/OK may be intersected enough for an isolated instance
    of flash flooding through evening, there as well.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_srI1y9f5mrwiNMPoOg9zFA7qW35X69uZEqh_l6vnDxbJRKQxuJvYQTvtSvY3-g4xFhR= R92wfYEN4Q0h_tB9rIpTVnI$ for graphic product...

    ATTN...WFO...AMA...DDC...OUN...

    ATTN...RFC...TUA...NWC...

    LAT...LON 38300019 38099912 37489860 36019897 35289977=20
    35570066 37150188 38000165=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Jun 3 20:29:52 2026
    AWUS01 KWNH 032029
    FFGMPD
    KSZ000-NEZ000-040200-

    Mesoscale Precipitation Discussion 0309
    NWS Weather Prediction Center College Park MD
    428 PM EDT Wed Jun 03 2026

    Areas affected...South-central NEB...North-central KS...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 032030Z - 040200Z

    SUMMARY...Efficient convective clusters becoming oriented to mean
    flow to support some repeating/training with slow east/southeast
    propagation. Rates of 1.75-2"/hr and spots of 2-3.5" may result
    in localized possible flash flooding.

    DISCUSSION...Regional RADAR and GOES-E Visible imagery depict an
    expanding cluster of thunderstorms across south-central NEB,
    generally orthogonal to the deep layer moisture axis and southerly
    low-level jet. Total PWats of 1.5-1.7" mainly loaded below 700mb
    per CIRA LPW advected on 15-20kts southerly flow is providing
    solid moisture flux convergence. Additionally, initial
    convection was placed favorably within broad cyclonic entrance
    region to upper-level jet speed max (enhanced by early morning
    convective complex in NM/OK/TX) continues to allow for upscale
    enhancement with favorable divergence aloft. As such, individual
    cells have cycled toward an increasingly west to east line (with
    smaller faster moving cells on the north side of the initial cold
    pool racing away). This has favorably oriented the expanding line
    due to orthogonal moisture flux convergence. Full insolation
    through the morning/afternoon provided ample unstable environment
    with MLCAPEs to 2500 J/kg. As such, moisture loading is supporting
    rates of 1.75-2"/hr rates.

    Deep layer flow is generally weak with 15-20kts mean flow to the
    northeast while propagation is similarly about 5kts
    east/southeast. Visible imagery denotes further congestion of the
    cu field along the southern edge that suggests a further southern
    propagation is probable. Additional upstream development across N
    central KS may further allow for mergers/intersection later this
    evening near/along the border. Given slow motions, localized
    2-3.5" totals are possible. The evolution and placement matches
    the RRFS and Canadian GEM solutions (4"+) which are typically too
    hot/intense overall, but the other solutions from the HRRR/ARWs
    remained too capped compared to reality.=20

    Hydrologically, the rates of up to 2"/hr and spots to 3.5"/3hrs
    are in the vicinity of the FFG values in the region, but suggest
    localized exceedance is sufficient for localized possible
    incidents of flash flooding to occur through this evening as the
    complex continues to evolve and slowly drift east and south with
    time.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8j2BIsz0zhDMn88Y5pTaICNgrf3DKVNoImZX6Q19qwgdPj6NEyTHxSc8Lld64E0GKWTa= O4eph6d_bVBm6qzb6Lv5bXA$ for graphic product...

    ATTN...WFO...GID...GLD...OAX...TOP...

    ATTN...RFC...KRF...NWC...

    LAT...LON 41509767 41289702 40729672 40029682 39529713=20
    39299767 39259857 39289957 39700009 40230014=20
    40519986 40949940 41229860=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Wed Jun 3 23:17:10 2026
    AWUS01 KWNH 032317
    FFGMPD
    TXZ000-NMZ000-AZZ000-040500-

    Mesoscale Precipitation Discussion 0310
    NWS Weather Prediction Center College Park MD
    715 PM EDT Wed Jun 03 2026

    Areas affected...Southern & Eastern NM...Southeast AZ... Western
    TX Panhandle...NW Northern TX Panhandle...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 032315Z - 040500Z

    SUMMARY...Potential for widely scattered, highly localized
    incidents of flash flooding continue through early overnight
    period. Localized 1-1.5" sub-hourly to hourly rates.

    DISCUSSION...GOES-E WV suite depicts the core of the main
    upper-low is lifting out of the Southwest into Eastern Colorado
    with a great anti-cyclonically curved outflow jet aiding some
    convection within northeast NM. In the wake, a broad baggy trough
    still remains with a subtle shortwave features in proximity to El
    Paso, Texas. As a result, moisture continues to remain/weakly
    stream through the Middle Rio Grande Valley and across SW NM into
    far southeast AZ. Enhanced low to mid-level moisture is about
    1-1.2" across the area but given the modest lapse rates aloft,
    still continue to provide ample conditionally unstable environment
    for ongoing convection to seek out and help maintain subsequent
    updrafts developing on the outflow/cold pools. Given the terrain,
    a corral of convection across the portions of the Gila, Mogollan,
    and Black Ranges are likely to intersect and merge with cells
    lifting north out of SE AZ and northern Chihuahua. Tds in the
    upper 40s, low 50s and total Pwats given remaining 1500-2000 J/kg
    of CAPE, should provide vigor to support lower cloud moisture
    loading to support quick burst rates of 1"; with any
    intersections/mergers of updrafts potentially nearing 1.5" in 30
    to 60 minutes. The widely scattered to isolated nature falling
    over hard, limited soil types should result in localized high run
    off and an isolated incident of flash flooding or two.

    Further northeast...a secondary channel of enhanced low level
    moisture flux across the Pecos River Valley/Permian Basin into the
    High Plains of NM will increase to 20kts and bring total Pwats
    back toward 1-1.25". However, greater heating and steeper lapse
    rates, have supported slightly more unstable environment over E NM
    with CAPE of 2000-3000 J/kg available. Initial convection off the
    southern Rockies is already starting to emerge along with outflow
    off the Sacramento Range. This is likely to increase in
    convective coverage and vigor capable of 1-1.5"/hr rates, but
    forward propagation is likely going to limit localized totals to
    similar values. This area has been recently hit with heavy
    rainfall (including last evening) and while the environment is not
    as conducive as last evening, repeating through similar areas
    still has a solid possibility of widely scattered incident(s) of
    flash flooding.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4H9WpYwPNBdy5hV37loTHPBhN6DZl_e2XyrLPyCo9uTLttNTFHkZMGeg_YCbQrhe0eSl= oEuF0eN0UUdPjsjiQnxSZKw$ for graphic product...

    ATTN...WFO...ABQ...AMA...EPZ...LUB...MAF...TWC...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 36590316 35450217 34780298 33540394 32690454=20
    31200429 30410434 30370506 31170598 31300612=20
    31590685 31600811 31530900 32160996 32970984=20
    33170818 33550740 33950699 34660643 35060609=20
    36060515 36530445=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Jun 4 00:35:21 2026
    AWUS01 KWNH 040035
    FFGMPD
    MNZ000-IAZ000-SDZ000-040600-

    Mesoscale Precipitation Discussion 0311
    NWS Weather Prediction Center College Park MD
    834 PM EDT Wed Jun 03 2026

    Areas affected...Eastern South Dakota...Southwest Minnesota...Ext.
    Northwest Iowa...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 040035Z - 040600Z

    SUMMARY...Increasing convective coverage and orientation to the
    flow suggest increasing potential for repeating cell tracks and
    increasing rainfall efficiency to support 1.75"/hr and localized
    streaks of 2-3" totals. Widely scattered incident or two of
    localized flash flooding is possible through early overnight
    period.

    DISCUSSION...00z surface analysis continues to depict a surface
    low along the Missouri River between KPIR and K9V9 with a region
    of backed surface flow and enhanced moisture from northeast NE
    into SE SD, including a stark 2-4 degree increase near/north of
    HON/K6E5; additionally the cold front is starting to advance in
    the last few hours. This localized maximum of low level moisture
    was also between a convective cluster from the south and
    approaching supercell canopy providing the last few hours of
    insolation to maintain a pocket of enhanced conditionally unstable
    air. VWP and low level observational trends denote an increase in
    surface to boundary layer southerly flow through much of the area
    of concern up to 15-25kts from sfc to 850mb, providing enhanced
    flux and some WAA. MLCAPEs of 2000-2250 J/kg and Total PWats of
    1.5-1.7" with the strength of flux suggests 1.5-1.75"/hr rates are
    likely to become more common with broadening up/downdrafts cores.

    Aloft, GOES-WV shows strong cirrus streaks indicative of the jet
    streak across northeast SD into SW ND/NW MN. This is expected to
    further strengthen to 100kts after sunset placing much of the MPD
    area of concern into favorable right entrance ascent region
    allowing for upscale growth into a broader complex. Regional
    RADAR denotes this increase in activity east/downstream of the
    supercell in Tripp county; as well as the increasing dewpoint line
    from Spink to Deuel counties. Overall, deep layer steering is
    also increasing with the aforementioned jet strengthening, likely
    to limit any particular cell's residency except right-mover
    supercells. The concern is that the expansion of development is
    generally parallel to the deep mean flow, suggestive of increasing
    potential for repeating/training. As such, streaks of 2-3" totals
    across these two west to east axes will have the greatest
    potential of exceeding the 1-3hr FFG values in the region and
    present a localized flash flooding incident or two possibly
    through the early overnight period.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9RP-snRGpfAFL3bnOLJi7ecZo8VbbK3G_XLyPKLnn9tV7f64pD6js45zlOGfj_ynUfSw= EA_Q_mVI3lQV8wjqv0X2T_8$ for graphic product...

    ATTN...WFO...ABR...FSD...MPX...UNR...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45739710 45729615 45509504 45009436 44059454=20
    43369536 43059684 43019877 43319989 44409979=20
    45409795=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Jun 4 01:08:25 2026
    AWUS01 KWNH 040108
    FFGMPD
    KSZ000-NEZ000-040555-

    Mesoscale Precipitation Discussion 0312
    NWS Weather Prediction Center College Park MD
    907 PM EDT Wed Jun 03 2026

    Areas affected...North Central Kansas...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 040110Z - 040555Z

    SUMMARY...Colliding outflow boundaries to continue potential for
    localized flash flooding risk through early overnight period.

    DISCUSSION...Regional RADAR mosaic and surface analysis depict a
    pair of active outflow boundaries likely to intersect over the
    next hour or two across portions of central KS. The north to
    south oriented line from Rush county south into Barber and
    northern Oklahoma appears to be rapidly weakening as the leading
    convergence is starting to weaken as cells continue to back shear
    though with some south to north slow training. The northern one
    is arched from near Beatrice, Neb across north-central KS from
    Washington to Ottawa before flattening to the west into northern
    Graham county. Deep southeasterly surface to 850 flow still
    intersects this line fairly orthogonally but also appears to be
    balancing out as the core of the meso-high remains north toward Kearney/Hastings region in NEB.=20

    At this time, strong convergence is starting to occur as the
    outflows zipper from NW to ESE north of I-70. DPVA from the
    parent shortwave in SW KS is starting to slack and right entrance
    influence to the jet over E CO is starting to slip north and east,
    this will continue to veer the LLJ over the coming hours further
    reducing convergence with the north-south boundary in favor of the
    west-east. Effective warm sector still has upper 60s and even a
    few low 70s Tds and solid enough remaining 1500-2000 J/kg of
    MLCAPE to advect to maintain/support the ongoing convection.=20
    Eventually, the western cold pool should sever the connection but
    in the mean time, with rates of 1.5-1.75"/hr and near 5kts of
    forward propagation, nearly stationary elements of the
    over-running convection will have the potential for spots of 2-4"
    totals that may result in possible localized flash flooding
    incident or two.

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5uW_4gKfazqzv20GWUKhOowNnWjtLPkHAS724hM3qSKeXTBLMnwk9msdDraEhIB-QRnP= 1Q5MS4zRh49y9-zNd2AT_WU$ for graphic product...

    ATTN...WFO...DDC...GID...GLD...ICT...TOP...

    ATTN...RFC...KRF...TUA...NWC...

    LAT...LON 40339924 39939731 39379678 38749712 38509785=20
    38459891 38499989 39170042 40080074=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Jun 4 02:28:32 2026
    AWUS01 KWNH 040228
    FFGMPD
    FLZ000-040725-

    Mesoscale Precipitation Discussion 0313
    NWS Weather Prediction Center College Park MD
    1026 PM EDT Wed Jun 03 2026

    Areas affected...Southeast FL

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 040226Z - 040725Z

    SUMMARY...Heavy rainfall and urban flash flooding will be a
    concern over the next several hours across southeast FL, including
    the Miami metropolitan area, as concerns for training showers and
    thunderstorms persist.

    DISCUSSION...The latest radar imagery and surface observations
    show an axis of training showers and thunderstorms impacting
    northern portions of Miami-Dade County. This convection is aligned
    with the low-level flow and a small-scale axis of focused moisture
    convergence in close proximity to a stationary front draped over
    far southern FL.

    MLCAPE values are generally near 500 J/kg, but the PWs are very
    high with the 00Z RAOB from KMFL indicating a PW of 2.13 inches
    and a deep moist vertical column that is highly tropical with WBZ
    heights of over 14,000 feet. As it is, much of the ongoing
    convection is rather shallow and extremely efficient with a
    sizable component of the forcing seen in the warm cloud region of
    the low and mid-levels of the column.

    Warm rain processes are dominating the ongoing rainfall, with
    extreme rainfall rates of 2 to 3+ inches/hour ongoing. A consensus
    of the latest HRRR and RRFS solutions support an area of focused
    convergence tending to maintain itself in the near-term across
    southeast FL near this front, and they support additional rainfall
    totals of 3 to 5 inches locally.

    Already the northern suburbs of the Miami metropolitan area are
    seeing flash flooding due to the extreme rainfall rates, and with
    the overall band of convection gradually losing latitude and
    settling down through the highly urbanized Miami-Dade County
    corridor near I-95, additional urban flash flooding concerns are a
    significant concern.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8L7odpWvV7VpMLVDTsPESSqgKBNJ45IcJA4IJ16mUzVdT2yYnwovUfcJWlWfYmIoeoyA= aAg93UlIEtwRRXM8rRZrpy8$ for graphic product...

    ATTN...WFO...MFL...

    ATTN...RFC...ALR...NWC...

    LAT...LON 26138033 26098012 25978006 25718009 25488019=20
    25328035 25338059 25518074 25828068 26008058=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Jun 4 05:31:05 2026
    AWUS01 KWNH 040530
    FFGMPD
    TXZ000-OKZ000-KSZ000-NMZ000-041125-

    Mesoscale Precipitation Discussion 0314
    NWS Weather Prediction Center College Park MD
    129 AM EDT Thu Jun 04 2026

    Areas affected...Southeast New Mexico...West
    Texas...Texas/Oklahoma Panhandles...Southwest Kansas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 040529Z - 041125Z

    SUMMARY...A broken band of thunderstorms gradually advancing east
    across the southern High Plains will continue to produce localized
    heavy rainfall overnight. A generally isolated threat for flash
    flooding will continue given rainfall rates locally as high as 1.0
    to 1.5 inches/hour.

    DISCUSSION...Recent radar and satellite imagery shows a broken
    axis of thunderstorms still impacting areas of southern and
    eastern New Mexico and extending northeastward up toward the Texas
    and Oklahoma Panhandles and southwest Kansas. Pockets of ascent
    continue to be maintained by the presence of multiple embedded
    mesoscale convective vortices (MCVs) rotating through the base of
    a broad upper trough over the southern Rockies and adjacent High
    Plains.

    Ahead of the broken areas of convection are pockets of MUCAPE
    reaching as high as 1000 to 2000 J/kg, with the latest RAP
    analysis showing the greatest instability generally over southeast
    New Mexico with somewhat lesser values noted elsewhere over the
    southern High Plains. Meanwhile, the PWs are locally as high as
    1.0 to 1.25 inches, and with the instability, there are some areas
    of thunderstorms producing rainfall rates of up to 1.0 to 1.5
    inches/hour.

    The latest hires guidance continues to support a broken axis of
    convection gradually advancing east or northeastward overnight
    through portions of the southern High Plains, with some additional
    rainfall totals reaching 2 to 3 inches locally. The latest HREF
    and REFS guidance still supports some 20 to 30 percent
    probabilities of exceeding the 3-hour FFG.

    Therefore, given the current convective trends and level of
    instability that is still in place along with the MCV activity, an
    isolated threat for areas of flash flooding should continue
    overnight.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Cmi_CWn-FsNX7x6QcJt8Lx-SGKHureEmvd9NG7gjN0wUG5m9jVhcaw3SjcSi_RlKsEv= 0pwVkY8YNvXqzk1m4vBlYt4$ for graphic product...

    ATTN...WFO...ABQ...AMA...DDC...EPZ...LUB...MAF...OUN...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 37700102 37669994 36589968 34710054 33100181=20
    32000271 30740332 30390452 30830572 31320633=20
    31960661 32440648 32880602 33300533 34120430=20
    34760344 35570262 36480199=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Jun 4 15:21:45 2026
    AWUS01 KWNH 041521
    FFGMPD
    FLZ000-042115-

    Mesoscale Precipitation Discussion 0315
    NWS Weather Prediction Center College Park MD
    1120 AM EDT Thu Jun 04 2026

    Areas affected...southeastern FL

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041519Z - 042115Z

    SUMMARY...There will be the potential for flash flooding across
    mainly the urban corridor of southeastern FL through 21Z.
    Localized slow moving showers and thunderstorms will be capable of
    producing 2 to 3+ inches of rain in an hour but with 1+ inches in
    15 minutes.

    DISCUSSION...Visible satellite imagery at 15Z showed a few narrow
    streamers of low level convergence into southeastern FL with two
    located over Biscayne Bay becoming more active with shower
    development over the past hour. While a cold/stationary front was
    analyzed south of the Keys at 15Z, it was shallow, with deep
    moisture of ~2.0 to 2.2 inches as far north as Broward County.
    MLCAPE was estimated via 15Z SPC mesoanalysis data to range from
    500-1500 J/kg over Miami-Dade and Broward counties with little to
    no CIN. ENE winds of 10-15 kt in the surface to 0-1 km layer. as
    seen in VAD wind data from KAMX and RAP analysis soundings over
    southeastern FL, shifted to largely light and variable from about
    1 km AGL to 8 km AGL, resulting in a mean steering flow of ~5 kt
    or less over the region.

    Expectations are for additional shower/thunderstorm development
    into the afternoon, but with model forecasts showing some
    semblance of low level drying in the 18-00Z time frame from the
    north, the threat for heavy rain is likely to wane toward 00Z.
    While any additional cells that form through the afternoon should
    remain disorganized due to a lack of shear, they should also be
    slow moving, contingent upon the south/north shifting of the low
    level axes of convergence.

    Recognizing the environment in place, slow movement will allow for
    efficient rainfall production and heavy rain of 1+ inches in 15
    minutes along with 2 to 3+ inches per hour. These higher rates are
    likely to remain isolated in nature but should they overlap with
    the urban corridor of Broward and Miami-Dade counties, rapid
    runoff is expected to lead to flash flooding.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Xt2NKH67_6KNH9bxvJdOaETurBbM2d2qIr7VASjZdM0VphI65uGPghvQzhALxAgdd4l= NmOBMHaWa1uFYsAPW8yjXBI$ for graphic product...

    ATTN...WFO...KEY...MFL...

    ATTN...RFC...ALR...NWC...

    LAT...LON 26377999 25557990 25228027 25208060 25388076=20
    26278060=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Jun 4 18:12:10 2026
    AWUS01 KWNH 041812
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-050000-

    Mesoscale Precipitation Discussion 0316
    NWS Weather Prediction Center College Park MD
    211 PM EDT Thu Jun 04 2026

    Areas affected...northeastern KS/southeastern NE into northwestern
    MO and central IA

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 041810Z - 050000Z

    SUMMARY...Thunderstorm coverage is expected to increase across
    northeastern KS/southeastern NE into northwestern MO and central
    IA through 00Z. Areas of training thunderstorms are expected to
    result in hourly rainfall of 1 to 2+ inches with potential for a
    few 3 to 4+ inch totals through 00Z.

    DISCUSSION...Water vapor satellite imagery at 1745Z showed a
    mid-level vorticity max centered near the central KS/NE border,
    moving toward the northeast. Visible and area radar imagery helped
    identify a pair of MCVs, one over central KS near HYS and a second
    in eastern NE near JYR. A remnant outflow boundary from early
    morning convection was analyzed from west-central KS into
    southeastern NE and west-central IA with recent thunderstorm
    development along the boundary in southeastern NE. Additional
    storms were noted within a zone of low level confluence over
    east-central KS, aligning from south to north. Daytime heating
    near and south of the outflow has helped contribute to MLCAPE of
    500 to 1500+ J/kg (highest over northeastern KS) among PWs of 1.5
    to 1.8 inches (via SPC mesoanalysis). Aloft, the right entrance
    region of a jet max centered over MN was focused across the middle
    to lower MO Valley, which should aid in overall ascent given only
    a slow northeastward departure of the entire jet max.

    Over the next 3-6 hours, as the main vorticity max and embedded
    MCVs advance downstream, thunderstorm coverage should expand over
    northeastern KS/southeastern NE initially...eventually extending
    into far northwestern MO and west-central IA. SW to NE steering
    flow aligned with the remnant outflow boundary and expected axis
    of thunderstorms will support areas of training as a local
    southerly max of 20-30 kt at 850 mb supports a relative max in
    moisture transport from eastern KS into southeastern NE. Hourly
    rainfall of 1 to 2+ inches should be expected within areas of
    training with the potential for a couple of locations to pick up 2
    to 4+ inches through 00Z. Flash flood guidance is near or less
    than 2 inches in 3 hours for a majority of the region outlooked
    from northeastern KS into southeastern NE/western IA. Therefore,
    localized to scattered areas of flash flooding are anticipated
    into the early evening.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5ywpulN7hf51ZrHsg6_YV_oEnYmR3Ts-BB51_yY8HF8hrmOK5ZcaODZajt20LbU4EBtg= -sTmI_85WX1st1BVdu5qlRo$ for graphic product...

    ATTN...WFO...DMX...EAX...GID...ICT...OAX...TOP...

    ATTN...RFC...KRF...MSR...TUA...NWC...

    LAT...LON 42599348 41899300 40499412 39349542 38619631=20
    38079688 38109742 38729807 38989865 39549875=20
    40529737 41599596 42459457=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Jun 4 18:40:46 2026
    AWUS01 KWNH 041840
    FFGMPD
    TXZ000-NMZ000-050035-

    Mesoscale Precipitation Discussion 0317
    NWS Weather Prediction Center College Park MD
    239 PM EDT Thu Jun 04 2026

    Areas affected... NM into portions of west TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 041837Z - 050035Z

    SUMMARY...Slow moving thunderstorms may produce a couple of
    isolated areas of flash flooding through the late afternoon from
    southwestern NM into portions of west TX. Hourly rainfall of 1 to
    2 inches is expected.

    DISCUSSION...1830Z visible imagery showed a number of mesoscale
    circulations embedded within a broader scale mid-level shear axis
    which extended from the TX Panhandle into southwestern NM. While
    some remnant mid and high level clouds remained over the region,
    strong solar insolation was occurring elsewhere with MLCAPE
    increasing. 18Z SPC mesoanalysis data showed 500 to 1500+ J/kg
    MLCAPE from southwestern to southeastern NM into parts of west TX
    to the west of the Pecos River.

    Continued heating should allow for some increase and expansion of
    the existing instability over the region through the remainder of
    the afternoon. Similar to previous days, steering currents aloft
    are weak which should result in disorganized but slow moving
    cells. One difference compared to previous days this week is the
    added component of an upper jet max located to the ESE of a closed
    low over northwestern Mexico, with its left-exit ascent region
    located over western TX into southeastern NM. Coverage of
    thunderstorms into the afternoon is expected to remain widely
    scattered but slow movement and anomalous moisture (+1 to +2
    standardized anomalies for PW) may allow for areas of isolated
    flash flooding through 01Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8Dudq0lFBwkYSybzewnKiPAkNMaS7vszRj_IVjoUUCvvpQ5t_rXiYqiPcM7Bd74ZFkMg= oFwQXzvOXohI2fpoz_ADwEg$ for graphic product...

    ATTN...WFO...ABQ...EPZ...LUB...MAF...

    ATTN...RFC...FWR...STR...TUA...NWC...

    LAT...LON 34640320 34620266 34310214 33860195 33140207=20
    32020295 30400289 29630362 29690448 30200530=20
    30820593 31210659 31240746 31050861 31260885=20
    31930889 32750856 33350752 33830609 34310449=20
    34470360=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thu Jun 4 23:19:46 2026
    AWUS01 KWNH 042319
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-050500-

    Mesoscale Precipitation Discussion 0318
    NWS Weather Prediction Center College Park MD
    718 PM EDT Thu Jun 04 2026

    Areas affected...Northeast KS...Far Southeast NEB...Northwest
    MO...Southern to East-Central IA...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 042320Z - 050500Z

    SUMMARY...Southwest to northeast repeating thunderstorms result in
    streaks of 2-4" totals and continue risk of localized flash
    flooding through early overnight period.

    DISCUSSION...CIRA LPW suite depicts core of warm conveyor belt
    returning along northwest edge of deep layer ridge in the
    southeast, resulting in core of 1.75-2" Total PWat stretching from
    E KS across IA into W WI; with each layer in the 95th-99th
    percentile with higher percentiles in the lower layers (Tds in the
    upper 60s and lower 70s). Current complex along the axis is
    being forced by an old shortwave from the southwest that is
    starting to open back up in a broader wave in the 925-850mb layer;
    though mid to upper level dPVA and right entrance ascent patterns
    continue to maintain a weak linear convective complex.

    This is mostly given the limitations of the vertical heating and
    lack of general instability, with values across IA dipping below
    1000 J/kg which is sufficient to maintain moderate convection in
    the overall dynamic ascent; especially given deep layer flow is
    unidirectional through steering and quite favorable for
    repeating/training profiles. Upstream, however, clearer skies over
    E KS has MLCAPE pool of 2000 J/kg advecting into the confluent
    upstream edge of the exiting shortwave. As such, favorable
    back-building is starting to become more evident in the congested
    low level cu/TCu filed in NE KS (before stronger CBs are seen
    nearer the NEB border counties attm. Stronger northern stream
    influences (digging approaching trough) will further help
    strengthen the LLJ toward diurnal maximum to further enhance
    moisture flux convergence and rainfall efficiency.

    As such, the upwind edge will continue to see scattered
    1.75-2"+/hr rates, with some training capability into NE MO and
    southern IA through the early evening. Streaks of 2-4" are
    possible (greater upstream), but longer duration of training due
    to weaker cold pool and reduced height-falls/influence from the
    northern stream will allow for slower eastward propagation further
    northeast into central and eastern IA where the instability is
    less. As such, the risk for localized flash flooding will remain
    possible through early overnight period.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5UeQ4so_ouJR-rY5IMYfacQZgFt9FIGNm8Lg0klbnzmw6Kji1Qj8M8lmgkEYVrGlWSzv= 0aCHqZwqaUkAgrPlWGENZcw$ for graphic product...

    ATTN...WFO...DMX...DVN...EAX...ICT...OAX...TOP...

    ATTN...RFC...KRF...MSR...TUA...NWC...

    LAT...LON 42619225 42329136 41669151 40659230 39489380=20
    38679527 38119687 38229791 38869799 39759742=20
    40359683 41299580 42039454 42449337=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Jun 5 00:56:22 2026
    AWUS01 KWNH 050056
    FFGMPD
    SDZ000-050600-

    Mesoscale Precipitation Discussion 0319
    NWS Weather Prediction Center College Park MD
    855 PM EDT Thu Jun 04 2026

    Areas affected...Central to Eastern South Dakota...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 050055Z - 050600Z

    SUMMARY...Expanding cluster over areas saturated last evening,
    before approach of main shortwave/convective line after dark.=20
    Spots of 2-3" over wet grounds pose localized flash flooding
    issue.

    DISCUSSION...00z surface analysis denotes a surface wave southeast
    of Pierre with stationary front extending northeast generally connected/influence by a fast moving mid-level shortwave crossing
    into NW MN; while the upstream portion of the front angles more
    westward into SW SD before the approach of the main
    height-falls/shortwave that is directing fast moving
    stronger/severe thunderstorms out of the Black Hills. As such,
    surface to boundary layer flow has backed and increased with a
    pocket of enhanced low level moisture with Tds in the mid to upper
    60s and pool of 1.25-1.5" total PWats continue to flux/converge to
    increase rainfall efficiency. RAP analysis shows pool of
    conditionally unstable (but weakly capped) MLCAPE of 2000-2500
    J/kg along the front into central SD. The overall convergence
    with initial weakening convection/outflow impinging on the front
    resulted in rapid convective development with 10.3um EIR tops
    cooling past -65C across Hand into Beadle county. Given this
    rates of 1.5"/hr will steadily increase to 2"/hr with time.

    RADAR and EIR show further downstream convective development
    expanding the overall width of the downdrafts increasing residency
    time in the generally west to east flow; with an additional round
    still upstream. Combine this will traversing areas hit overnight
    yesterday and lighter/moderate activity this afternoon. A line of
    additional 2-3" total (in areas of 2-4") should be harder to
    infiltrate and result in increased run-off and potential for
    inducing localized flash flooding.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8QUJ94XzyfmDue1lfud9wRJ54MDoa67Xo20LhYONKbXzbEYtgiVZ1ima0qS-5UsgAAmS= UauIRtD0yPitDWHmx3I22Vo$ for graphic product...

    ATTN...WFO...ABR...FSD...UNR...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 45099748 44949668 44569647 44079679 43669791=20
    43479872 43419914 43310029 43330103 43560137=20
    44020126 44550013 44719964 45019894=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Jun 5 01:24:26 2026
    AWUS01 KWNH 050124
    FFGMPD
    TXZ000-050700-

    Mesoscale Precipitation Discussion 0320
    NWS Weather Prediction Center College Park MD
    923 PM EDT Thu Jun 04 2026

    Areas affected...Western Texas Panhandle...

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 050125Z - 050700Z

    SUMMARY...Strong slow moving thunderstorms capable of quick 1.5"
    in hour or less pose highly focused/localized incident or two of
    flash flooding.

    DISCUSSION...GOES-E WV suite shows a strong closed low over
    southern Sonora/N Sinaloa state in Mexico with broad diffluent
    pattern across Chihuahua and Western Texas Panhandle. The speed
    max is streaking westward with right entrance ascent, while the
    right branch and left exit of 70kt+ streak is bending
    anticyclonically across Coahuila into the Edwards Plateau of W
    Texas. Moisture has remained pooled along the Rio Grande Valley
    for the last few days with mid to upper 50s Tds analyzed (though
    upper 60s and 70s reside in the lower RGV, southeast of the
    Pecos); this and direct heating and modest lapse rates continue t
    to support 1500 J/kg of MLCAPE as the day fades. Outflow from
    initial convection in Mexico as well as peaks in far W Tx along
    the Hueco Range has helped to support some additional convergence
    for newer convective cells to sprout quickly, with a slow
    southeast propagation through the next few hours. The strong
    outflow aloft and sufficient low level moisture should allow for
    quick cloud base moisture loading to support quick bursts of
    1-1.5" in 30 to 60 minutes, kick an outflow to help trigger later
    convection down the line.

    A shortwave/vorticity center is lifting northward through the
    divergent flow and is likely to initiate further convection over
    the higher terrain of Chihuahua that has potential to reach the
    Big Bend later into the overnight and may also intersect with some
    of these initial scattered cells propagating southeastward. Given
    hard, rocky ground conditions, localized flash flooding will
    remain possible across the area through the early overnight
    period.=20

    Gallina

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4vYK6l8RNVKgSdrqhYFiGcvuzAIAiG62ogiud6gzjkbJBR3FRj9VTRVbODBik-SPw3gJ= vTS88KYabJrdK7JIEb-PkD4$ for graphic product...

    ATTN...WFO...EPZ...MAF...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31910548 31850492 31460421 30730286 29930191=20
    29410270 28960300 29070362 29580451 30360494=20
    30780548 31180596 31580592=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Jun 5 04:32:14 2026
    AWUS01 KWNH 050432
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-051030-

    Mesoscale Precipitation Discussion 0321
    NWS Weather Prediction Center College Park MD
    1230 AM EDT Fri Jun 05 2026

    Areas affected...Northeast Kansas...Far Southeast
    Nebraska...Northwest Missouri...Southern Iowa

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 050430Z - 051030Z

    SUMMARY...Heavy showers and thunderstorms with significant
    concerns for backbuilding and training of convective cells are
    expected overnight across northeast KS, far southeast NE,
    northwest MO, and southern IA. Already pockets of flash flooding
    are ongoing, and with 1.5 to 2.5 inch/hour rainfall rates expected
    with the convection, some additional rainfall totals of 3 to 6+
    inches will be possible overnight. Locally significant and
    life-threatening flash flooding will be possible as a result.

    DISCUSSION...The latest GOES-E IR satellite imagery shows a
    well-organized axis of heavy showers and thunderstorms across
    portions of northeast KS, northwest MO and southern IA. The
    convection is in a highly efficient environment for extreme
    rainfall rates as an ejecting compact vort center/shortwave
    interacts with a nocturnally enhanced 30 to 40+ kt southwesterly
    low-level jet.

    Deep moisture convergence is strong, with precipitable water
    values of 1.7 to 1.9 inches contributing to highly efficient
    warm-rain physical processes and deep warm cloud layers.
    Instability remains sufficient to support robust convection, with
    MLCAPE values of 1000 to 1500 J/kg, while 30 to 40 kts of
    effective bulk shear sustains storm organization.

    Of significant concern are the favorable Corfidi vectors promoting
    slow storm motions, backbuilding, and cell-training over areas
    with ongoing flash flood warnings. Instantaneous rainfall rates
    are peaking at 1.5 to 2.5 inches per hour. The 00Z HREF and REFS
    suite strongly supports 50 to 80 percent probabilities of
    exceeding 3-hour flash flood guidance through the overnight hours,
    with a consensus of hires CAMs supporting additional rainfall
    amounts of 3 to 6+ inches.

    The combination of intense rainfall rates, significant moisture
    anomalies, and a sustained training storm mode supports a likely
    flash flood threat with considerable runoff potential. Some urban
    locations may locally experience significant and life-threatening
    flash flooding over the next several hours. This may include the
    St. Joseph, MO vicinity along with adjacent communities back into
    northeast KS and also off to the northeast across northwest MO.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!71nTGmCRbx0FI_LKv03i3MeE1FlMuHrO6L1b3wneDcPgoUoGlRClZTfssgGodl9DAUAd= 4Jm8n_9p6n4cTODuWbhCCy8$ for graphic product...

    ATTN...WFO...DMX...DVN...EAX...OAX...TOP...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 41569216 41189184 40529216 39959294 39299426=20
    38989520 38919615 39159666 39679668 40229610=20
    40819493 41359357=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Jun 5 09:46:45 2026
    AWUS01 KWNH 050946
    FFGMPD
    WIZ000-ILZ000-MOZ000-IAZ000-KSZ000-051400-

    Mesoscale Precipitation Discussion 0322
    NWS Weather Prediction Center College Park MD
    545 AM EDT Fri Jun 05 2026

    Areas affected...Northern Missouri...Southern and Eastern Iowa

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 050945Z - 051400Z

    SUMMARY...Additional areas of locally backbuilding and training
    convection will continue to track across portions of northern
    Missouri and to a lesser extent southern and eastern Iowa through
    the mid-morning hours. Localized rainfall rates as high as 1.5+
    inches per hour falling on locally moist/sensitive grounds will
    maintain a threat for some additional flash flooding, but
    conditions should gradually improve by later this morning.

    DISCUSSION...A wave of low pressure and associated mid-level vort
    centered over southwest Iowa continues to track gradually off to
    the northeast along a well-defined surface trough that has some
    weak frontal characteristics. This continues to facilitate a
    mature cold-topped convective complex across northern Missouri,
    with a more elongated and broken axis of convection seen
    downstream across southern and eastern Iowa.

    The thermodynamic profile has stabilized a bit relative to earlier
    in the night, but there continues to be a nose of MUCAPE values on
    the order of 500 to 1000 J/kg across northern Missouri and
    southern Iowa which is being driven by a persistent southwest
    low-level jet of 30 to 40+ kt. This coupled with the high PW
    environment with values near 1.75 inches continues to favor
    rainfall rates reaching as high as 1.5+ inches/hour.

    The 06Z consensus of hires CAMs suggest a gradual decline in
    convective organization and intensity going toward and after 12Z
    this morning which will be largely driven by decreasing CAPE and
    eventually a decrease in the low-level jet, but there will still
    be at least a few more hours of locally heavy rainfall. This will
    include some concerns for additional backbuilding and
    cell-training across portions of northern Missouri in particular.
    Additional rainfall amounts of 2 to 3+ inches will be possible.

    As a result, some additional areas of flash flooding may occur
    across northern Missouri, with the threat overall a bit lower over
    southern and especially eastern Iowa where the antecedent
    conditions are not as sensitive.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6o2jvNMC_LDlzj9UdbKdHs9Xcs_PkrRyrJ_9zrDpwQpI7iAJoUuCZsQ33RpcNM1BuDt_= 5I1Uok06zP7AbqwvkwPZSTg$ for graphic product...

    ATTN...WFO...ARX...DMX...DVN...EAX...LSX...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 42689099 42399012 40999061 40129143 39619229=20
    39389360 39619490 39919526 40249513 40569434=20
    40999333 41809226=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Jun 5 12:25:36 2026
    AWUS01 KWNH 051225
    FFGMPD
    TXZ000-051700-

    Mesoscale Precipitation Discussion 0323
    NWS Weather Prediction Center College Park MD
    824 AM EDT Fri Jun 05 2026

    Areas affected...southeastern TX

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 051223Z - 051700Z

    SUMMARY...Widely scattered narrow axes of training showers and
    thunderstorms across southeastern TX may result in isolated
    pockets of flash flooding over the next 4-5 hours. Hourly rainfall
    locally in excess of 2 inches will be possible.

    DISCUSSION...12Z regional radar imagery over the TX Coastal Plain
    depicted scattered showers with embedded thunderstorms, moving
    from SSE to NNW. Low level flow of about 10 to 20 kt (slightly
    stronger over the upper TX coast into the Piney Woods region) was
    oriented perpendicular to the coast, resulting in the widely
    scattered shower activity. Surface observations at 12Z showed the
    reflection of a remnant surface frontal boundary, represented by
    lower dewpoints to its north and east, extending from the northern
    Gulf Coast into southeastern TX. MLCAPE was also reflective of
    this boundary with a gradient shown on the 12Z SPC mesoanalysis
    with 500 to 1500 J/kg located on the warm side of the remnant
    frontal boundary across the TX Coastal Plain, with little to no
    instability to its north. Near this gradient was weakly convergent
    flow in the 0-2 km AGL layer, partially aligned with the mean
    steering flow from the SSE.

    Due to the similar orientation of the low level and steering flow,
    with low level flow slightly stronger than 10-15 kt steering flow,
    some training and brief backbuilding of cells will be possible
    over the next few hours. Southeastern TX was also beneath the
    ridge axis of a broader upper ridge over the Gulf, aiding in weak
    upper diffluence. With GPS PWs of 2.0 to 2.1 inches over
    southeastern TX, the environment will be supportive of efficient
    rainfall with potential for 1 to 2 inches of rain in an hour
    (locally higher possible), and 2 to 4+ inch storm totals.

    While the coverage of these higher rates remains quite uncertain
    and could end up highly localized, portions of southeastern TX
    have picked up 3 to 6+ inches of rain over the past 2-3 days,
    resulting in pockets of higher soil moisture and reduced
    infiltration capacity. Therefore, in addition to urban overlap,
    additional heavy rain of 2 to 4+ inches falling atop any
    hyrdologically sensitive locations could result in isolated flash
    flooding over the next 4-5 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_G9RKQkhmDQZ3sXLVF50qCyFjJgUKqNUASWXfuJjPf8zWGS58lfJ4YmuNn-6vM27qSuS= wMCRa55wp2W-ZTONvKVrPSA$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...LCH...

    ATTN...RFC...FWR...NWC...

    LAT...LON 31459581 31229519 30809482 30519443 30209395=20
    29539397 28609538 27929674 29139734 30869710=20
    31369652=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Jun 5 17:04:28 2026
    AWUS01 KWNH 051704
    FFGMPD
    LAZ000-TXZ000-OKZ000-052130-

    Mesoscale Precipitation Discussion 0324
    NWS Weather Prediction Center College Park MD
    103 PM EDT Fri Jun 05 2026

    Areas affected...eastern TX into far southeastern OK

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 051700Z - 052130Z

    SUMMARY...An isolated flash flood threat will continue through the
    afternoon hours for eastern TX into far southeastern OK. Narrow
    axes of training showers and thunderstorms will support 1 to 2
    in/hr rainfall but also have the potential to produce hourly
    rainfall locally in excess of 2 inches.

    DISCUSSION...1640Z radar and visible satellite imagery showed
    scattered showers and thunderstorms over southeastern TX with some
    recent expansion northward toward the I-20 corridor between FTW
    and TYR. Breaks in cloud cover over eastern TX were helping with
    slightly better surface heating compared to the thicker cloud
    cover over central TX at the moment. The airmass over eastern TX
    remained very moist with PWs of 2.0 to 2.2 inches and unstable
    with 500 to 1500+ J/kg MLCAPE (via 16Z SPC mesoanalysis data). Low
    level directional convergence/confluence remained better focused
    across southeastern TX where low level southeasterly winds near
    the lower Sabine River met with a more southerly flow to the west
    over east-central TX.

    While confluent axes were weak and somewhat transient, there
    should remain a better focus for low level forcing over eastern
    TX, aligned with the mean steering flow, allowing for training and
    brief backbuilding of cells. The low level confluence axis is
    forecast by the RAP to slowly shift north this afternoon but lose
    some definition and become offset in orientation from the mean
    steering flow. Despite the less favorable setup into northeastern
    TX later this afternoon, this area will maintain a limited threat
    for training and brief backbuilding. Due to the moist and unstable
    environment, areas of training will carry the likelihood for 1 to
    2+ in/hr rainfall rates along with a few totals of 2 to 4 inches
    (locally higher). A few locations could see isolated flash
    flooding over the next 4-5 hours.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!8m2TkxfusEqUxVBKB4D3KTaodBbyWSqtE8qveOe-vuUkz_K84xlq-M-pgdtL0He9TiXf= 5zf_-1YNSDqNY7TvXdR_Avw$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...LCH...OUN...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 34599546 33419511 32329464 30299374 29509497=20
    29119590 29509662 31079726 32839746 34389654=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Jun 5 18:17:41 2026
    AWUS01 KWNH 051817
    FFGMPD
    TXZ000-NMZ000-060000-

    Mesoscale Precipitation Discussion 0325
    NWS Weather Prediction Center College Park MD
    216 PM EDT Fri Jun 05 2026

    Areas affected...western TX into southeastern NM

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 051816Z - 060000Z

    SUMMARY...Widely scattered thunderstorms, some with slow movement,
    will pose an isolated flash flood threat across portions of
    western TX into southeastern NM. Rainfall of 1 to 2 inches in 30
    to 60 minutes will be possible.

    DISCUSSION...GOES East water vapor imagery showed a closed upper
    level low over Chihuahua with a visually inferred and RAP analysis
    supported jet streak located to its southeast (80 kt) over
    Coahuila with left-exit region ascent over portions of western TX,
    west of the Pecos River. With a portion of the mid-level trough
    extending northeastward from Mexico into southeastern NM and the
    TX Panhandle, weak steering flow was in place for a notable
    portion of far western TX into southeastern NM and parts of the TX
    Panhandle.

    Visible satellite and radar imagery have already confirmed
    convective initiation across portions of the region where more
    favorable solar insolation has allowed for an expanding region of
    500-1500+ J/kg MLCAPE where PW values remained anomalous (+1 to +2
    standardized anomalies) as they have for the past several days.

    Thunderstorm coverage is expected to increase across portions of
    southeastern NM into portions of western TX with continued daytime
    heating and reduction of CIN. Another contributing factor will be
    the expected northeastward movement of the closed low over Mexico,
    which will provide increased ascent and diffluence aloft across
    western TX.

    While thunderstorm coverage is not expected to be numerous
    throughout the afternoon/early evening, there will likely be a few
    slower moving cells and smaller clusters with the potential to
    produce 1 to 2 inches of rain in 30 to 60 minutes. Portions of the
    region have seen well above average rainfall over the past week
    and areas of lowered flash flood guidance exist as a result.
    Therefore, isolated flash flooding will be possible over western
    TX into southeastern NM through ~00Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6-6lE0ArMIjd0K6itLZx_tsOkbpLP6amD24TmDO4rfD20t2H7oDsacoE7vERDc-H_1Hj= UQ1cG3cBypOrFr6G3L2pyVU$ for graphic product...

    ATTN...WFO...ABQ...AMA...EPZ...LUB...MAF...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 34760140 34280063 33460037 32560073 30980132=20
    30220193 29700315 29870364 30240402 30730433=20
    31130503 31510559 32240608 33490572 33560441=20
    33870320 34460224=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Jun 5 19:25:49 2026
    AWUS01 KWNH 051925
    FFGMPD
    TXZ000-OKZ000-060124-

    Mesoscale Precipitation Discussion 0326
    NWS Weather Prediction Center College Park MD
    324 PM EDT Fri Jun 05 2026

    Areas affected...western Oklahoma through western north Texas, the
    eastern Texas Panhandle, and surrounding areas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 051924Z - 060124Z

    Summary...Scattered, slow-moving thunderstorms are producing heavy
    rainfall, with rain rates of 2 inch/hr noted beneath stronger
    storms. Flash flooding is possible on an isolated basis.

    Discussion...Strong insolation has support sufficient instability
    for robust thunderstorm development generally along an axis from
    just west of Abilene (Snyder), TX north-northeast to near Enid,
    OK. The storms are in an environment with very weak shear (mean
    flow generally less than 15 knots across the discussion area), but
    strong instability (2500 J/kg MLCAPE) and abundant moisture (1.7
    inch PW) supporting deep updrafts and locally heavy rain. Forcing
    for ascent is weak, although objective analyses depict a very weak
    mid-level shortwave trough and vorticity max over western Oklahoma
    that was likely providing ascent to support the deeper convection
    currently developing. Peak rain rates of 2 inches were occurring
    in spots, which is generally falling below FFG thresholds of 2-2.5
    inch/hr (locally lower in west-central Oklahoma though).

    The ongoing scenario supporting isolated instances of flash
    flooding should continue for several more hours. Strong
    insolation will continue to maintain large instability across the
    discussion area, while localized/expanding cold pools support
    newer updrafts across the discussion area with time. Cell motions
    should be slow and at times erratic. Flash flood potential will
    be locally enhanced in areas of favorable cell mergers that can
    prolong rain rates in any given locale. The isolated flash flood
    risk should wane some after sunset/02Z or so.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9XED3-dcm_lleCcQTC_u36QEMdLqdAojJOIGbagyQ7KRAtnzHXTllhwgNnqfW7_RlzFG= q2RRvZsBRJyjtu3_SU24q48$ for graphic product...

    ATTN...WFO...AMA...FWD...LUB...MAF...OUN...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 36759724 35159732 33379860 32040037 32870097=20
    34870118 35730050 36089980 36659891=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Jun 5 22:06:36 2026
    AWUS01 KWNH 052206
    FFGMPD
    TXZ000-060204-

    Mesoscale Precipitation Discussion 0327
    NWS Weather Prediction Center College Park MD
    605 PM EDT Fri Jun 05 2026

    Areas affected...Deep South Texas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 052204Z - 060204Z

    Summary...Recent development of convection near the Brownsville,
    TX Metro area and along the Lower Rio Grande Valley poses a flash
    flood risk.

    Discussion...Radar trends depict several slow-moving cells over
    Deep South Texas that have persisted for several hours and
    produced occasional 3 inch/hr rain rates - primarily over rural
    areas where FFG thresholds are quite high (3-4 inches/hr, locally
    higher). Flash flood potential has been relatively
    isolated/sparse.

    Recent radar/satellite depicts convection forming nearer to the
    populated areas of the Lower Rio Grande Valley (near/just
    northeast of Brownsville and just south of McAllen). These cells
    are in a similar environment as the aforementioned cells farther
    north across Deep South Texas, and have potential for 3 inch/hr
    rain rates over more sensitive, urbanized locales. The risk for
    impacts from flash flooding have increased over the past 30
    minutes and will continue to do so while slow-moving cells
    continue over more sensitive/urban areas.

    This risk will likely continue for at least a couple hours.=20
    Models suggest that convection will be primarily diurnally driven
    and should lessen in intensity/coverage after sunset.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4f6FQdvSGYHEvXplVdvfV08ZlrF6WvfxhW6bIHF0Y-8bSzuvu3a6UO4ouaFOllSJhhip= uYMvo9DaGvBZac3XuatD1Lk$ for graphic product...

    ATTN...WFO...BRO...CRP...

    ATTN...RFC...FWR...NWC...

    LAT...LON 27789791 27469736 26429714 25769721 25819818=20
    26359895 27569892=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Jun 5 23:40:14 2026
    AWUS01 KWNH 052340
    FFGMPD
    TXZ000-060400-

    Mesoscale Precipitation Discussion 0328
    NWS Weather Prediction Center College Park MD
    739 PM EDT Fri Jun 05 2026

    Areas affected...portions of central Texas

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 052338Z - 060400Z

    Summary...A band of convection was organizing along a north-south
    axis from near Killeen to near Luling. This will spread heavy
    rainfall across portions of Austin Metro and surrounding areas for
    at least the next 2-4 hours. Flash flooding is possible in
    sensitive locales.

    Discussion...Recent radar mosaic imagery depicted a band of
    convection from near Killeen south-southeastward to Luling (east
    of San Antonio) that was increasing in organization and intensity
    over the past hour or so. The forcing mechanisms for this band
    are currently unclear, bur are likely tied to subtle influences
    from a mid/upper wave centered over far west Texas and subtle
    confluence along a weak boundary separating rain-cooled air from
    east Texas to slightly warmer conditions to the west.=20
    Unfortunately, these cells were organizing generally parallel to
    weak southerly steering flow aloft, allowing for individual cells
    to move slowly north while enabling the developing convective axis
    to stay nearly stationary. This has already resulted in spots of
    2-3 inch/hr rain rates (and local FFG exceedence) between Killeen
    and Georgetown along US 183, along with a gradual increase in
    rates farther south near Austin.

    With still a few hours of surface heating left, a window of
    opportunity exists for convection to pose a flash flood risk for
    the areas beneath this band. Additional, forward-propagating
    convection southeast of this axis (north of Victoria) may also
    exhibit similar behavior (spots of 1-3 inch/hr rates at times).=20
    Flash flooding is possible in this regime.=20

    Models suggest that a downward trend in convective coverage should
    materialize after sunset, though this will be modulated heavily by
    convective organization -- any upscale growth of convection will
    likely prolong activity and associated heavy rainfall risk. The
    current MPD will run through 04Z when flash flooding is most
    likely to occur, and trends will be reevaluated for continued risk
    around that time.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6NC9GR1vRRyJJIYIV94SagEFFy4QPCBsu1EyJ0huwFdyexWW9KW6WNuyKlD4M9M1Fr3j= FO-MKQguHnMPAwFJrF_Ev9A$ for graphic product...

    ATTN...WFO...CRP...EWX...FWD...HGX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32109796 31199670 29929652 29169676 28679833=20
    30009869 31579894=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Fri Jun 5 23:59:16 2026
    AWUS01 KWNH 052359
    FFGMPD
    TXZ000-OKZ000-NMZ000-060557-

    Mesoscale Precipitation Discussion 0329
    NWS Weather Prediction Center College Park MD
    758 PM EDT Fri Jun 05 2026

    Areas affected...portions of western through central Texas and the
    southeastern Texas Panhandle, far southwest Oklahoma, and
    southeastern New Mexico

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 052357Z - 060557Z

    Summary...Scattered, slow-moving thunderstorms persist, resulting
    in a continued flash flood risk across the discussion area through
    much of the early evening.

    Discussion...Deep convection continues beneath a mid/upper low
    centered over the Transpecos region of far west Texas. Abundant heating/instability beneath this mid/upper low and abundant
    moisture (1.2-1.75 inch PW values - highest with eastward extent)
    was continuing to support locally heavy rainfall, with rates
    exceeding 2-3 inches/hr in spots - especially across the
    southeastern Texas Panhandle, just north of Lubbock, near
    Sweetwater, and near Iraan. Flash flood potential remains likely
    with this activity for at least another 2-4 hours (through sunset).

    Models/observations depict that convection will remain
    slow-moving, with slow propagation expected near any linear
    segments or clusters that begin to propagate. Storms may
    eventually undergo a weakening trend with time after sunset, but
    it is likely that this process will take several hours to play out
    with lingering instability and the tendency for small upscale
    growth with some of the activity. There is some risk that
    additional convection forms over the Hill Country between Junction
    and US 281 given satellite presentation of local towering cumulus
    in that area, though forcing overall is weak and this risk is
    somewhat conditional. Moisture/buoyancy profiles support heavy
    rainfall/flash flood risk with any convection that develops in
    that region through the early evening.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5yt9EhQDxkF4vHAl-ky3zxUlUYd4HIx3N-f0GKD8Ov8ywlHLoRaBAuLqqlmOjmvZ4g-_= MD9xiQ7hCBKFhIpUGVlfZWY$ for graphic product...

    ATTN...WFO...ABQ...AMA...EPZ...EWX...FWD...LUB...MAF...OUN...
    SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35280126 35160010 34579916 32699862 30559871=20
    28949910 28690007 29570148 29760248 29050317=20
    29230398 29810474 31940610 33680594 34310433=20
    34600252=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 01:18:50 2026
    AWUS01 KWNH 060118
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-060717-

    Mesoscale Precipitation Discussion 0330
    NWS Weather Prediction Center College Park MD
    917 PM EDT Fri Jun 05 2026

    Areas affected...southeastern Nebraska into southern Iowa,
    northern Missouri, and a small part of northeastern Kansas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 060117Z - 060717Z

    Summary...Strong thunderstorms will continue to gradually develop
    across the discussion area. Slow movement and favorable
    orientation for backbuilding and training will pose a threat for
    flash flooding, with locally significant impacts possible.

    Discussion...Scattered thunderstorms are forming in earnest across
    southeastern Nebraska currently. The storms are likely responding
    to increasing low-level convergence related to increasing 850mb
    flow/low-level jet axis over western and central Kansas currently.
    The storms are in a strongly unstable and moist environment
    (MLCAPE nearing 4000 J/kg, 1.4-1.7 inch PW), with modest steering
    flow supporting slow storm motions and local backbuilding. Given
    the strong instability and favorable storm orientation, areas of
    1-2 inch/hr rates were already being estimated per MRMS in a few
    spots, approaching FFG thresholds (relatively low in southeastern
    Nebraska and points southeastward).

    Given the environment and downstream ground sensitivities (~1
    inch/hr rain rates immediately downstream from NE into northwest
    MO), flash flooding appears likely as convection slowly migrates
    eastward. Current evolution appears to support expanding
    convective clusters that eventually form a mix of cells and small
    linear segments as storm modes. Flash flooding could become
    significant in areas that experience prolonged rainfall and higher
    rain rates. Current trends suggest that FFG thresholds could
    easily be doubled (rain rates exceeding 2.5 inch/hr) in a few
    instances. This risk will persist through the overnight hours,
    again with backbuilding potential likely given the favorable,
    orthogonal positioning of the KS low-level jet to the surface
    boundary over southeastern Nebraska.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!6Qiq0jjMUE9VLTRdpRbWa1s9Oa3-2V2RssV8scpp6gnxOpke5hEdhcmIljax2IUiumAj= tS3M5jI6eJiAerBNdpYLKV0$ for graphic product...

    ATTN...WFO...DMX...EAX...GID...OAX...TOP...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 41689696 41629397 41429279 40429258 39559367=20
    39419704 40429907 41529907=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 02:56:30 2026
    AWUS01 KWNH 060256
    FFGMPD
    TXZ000-OKZ000-060700-

    Mesoscale Precipitation Discussion 0331
    NWS Weather Prediction Center College Park MD
    1054 PM EDT Fri Jun 05 2026

    Areas affected...Northwest Texas...Southwest to Central Oklahoma

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 060254Z - 060700Z

    SUMMARY...Thunderstorms will continue to anchor, back-build, and
    train across the region overnight. Torrential rainfall rates of 2
    to 3 in/hr will be capable of producing localized totals of 3 to 5
    inches. Flash flooding is likely.

    DISCUSSION...Recent GOES-E IR satellite imagery and regional radar
    mosaics show an organized area of slow-moving convection across
    central to southwest Oklahoma and adjacent northwest Texas. This
    activity is blossoming directly along and north of a
    quasi-stationary surface trough. Convective trends over the past
    hour show highly efficient, discrete cells tending to consolidate,
    with pronounced back-building occurring along the southern flank
    of the convective mass.

    The mesoscale environment is supportive of a localized, high-end
    flash flood threat. Recent RAP mesoanalysis indicates a nocturnal
    low-level jet (LLJ) slowly veering and strengthening to 30-35
    knots out of the south. This LLJ is slamming directly into the
    aforementioned surface trough and is yielding focused low-level
    moisture convergence and mesoscale ascent. The thermodynamic
    profile fueling this ascent is rich for early June, featuring an
    influx of 1.75 to 2.00 inch PWATs and 1000 to 2000 J/kg of
    elevated MUCAPE.

    The primary catalyst for flash flooding tonight will be the
    kinematic profile. As the LLJ continues to strengthen and veer, it
    is effectively shrinking the Corfidi upwind propagation vectors to
    less than 10 knots. Furthermore, these shortened vectors are
    orienting nearly parallel to the stalled surface boundary and
    opposite to the mean mid-level steering flow. This dynamic ensures
    that cell regeneration on the inflow (upwind) flank of the cluster
    will perfectly balance the downwind cell motion, leading to a
    nearly stationary convective footprint.

    Given the available moisture and instability, warm-rain processes
    will dominate, easily yielding torrential rainfall rates of 2 to 3
    in/hr. With relentless back-building and training expected to
    persist over the next few hours, localized rainfall totals of 3 to
    5 inches are likely. This will rapidly overwhelm local soils and
    drainage basins, leading to instances of flash flooding.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5gamVIMaaUI4_Zynu4uiT_jN3o65fM_lRkfuX_AfuL9i9JT6LLA-X5LDtQ81MTPG_Lt9= mfFoFJnUnhsnWE2g6ftfXSA$ for graphic product...

    ATTN...WFO...LUB...OUN...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35669767 35499713 34629748 33949813 33649903=20
    33609977 33870009 34269997 34729908 35499817=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 04:11:06 2026
    AWUS01 KWNH 060411
    FFGMPD
    TXZ000-061000-

    Mesoscale Precipitation Discussion 0332
    NWS Weather Prediction Center College Park MD
    1209 AM EDT Sat Jun 06 2026

    Areas affected...Central Texas/Hill Country

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 060409Z - 061000Z

    SUMMARY...Very efficient showers and thunderstorms will persist
    and regenerate across central Texas into the overnight hours.
    Extreme rainfall rates of 2 to 3 in/hr are possible which may
    result in localized additional rainfall amounts of 3 to 4+ inches.
    Flash flooding is possible.

    DISCUSSION...Recent regional radar imagery and GOES-E Proxy
    Visible satellite trends show an active, but broken area of
    slow-moving showers and thunderstorms impacting portions of
    central Texas and the Hill Country. This activity is being
    sustained by a highly anomalous and deep tropical moisture axis
    and subtle deep layer ascent. Recent 00Z RAOBs and OSPO/CIRA ALPW
    data indicate a dual-feed moisture tap with modest low-level
    moisture transport originating from the Gulf which is being
    superimposed by a deep mid to upper-level moisture contribution
    from the eastern Pacific given deeper layer southerly flow.

    The synoptic and mesoscale forcing mechanisms, while subtle in the
    lower levels, are highly supportive of sustained ascent. A subtle
    surface trough is currently draped across the region, providing
    the necessary low-level convergence. Aloft, the upper-level flow
    is becoming increasingly divergent ahead of a deep-layer trough
    over the southern High Plains. When combined with a moderately
    unstable thermodynamic profile characterized by 1000 to 2000 J/kg
    of MUCAPE, robust and persistent updrafts will continue to blossom.

    The primary hazard tonight is the extreme rainfall efficiency of
    these updrafts. With PWATs analyzed between 2.0 and 2.25 inches
    and a very deep warm cloud layer in place, warm-rain
    collision-coalescence processes will dominate. This will easily
    support torrential rainfall rates of 2 to 3 in/hr.

    While the 00Z REFS guidance appears considerably underdone and out
    of touch with ongoing observational trends, the latest
    high-resolution HRRR and the 00Z HREF suite are in much better
    agreement with the current radar presentation. Relying on the
    HREF/HRRR consensus, the expectation is for these highly efficient
    storms to produce localized additional rainfall totals of 3 to 4+
    inches overnight. Given the intensity of the hourly rates,
    isolated to scattered instances of flash flooding will remain a
    threat through the early morning hours.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9fCGYu72D8EYN-gPgXJujfSxOZSSURdZSnueuAauYChQZb2JwXZLEK7eY5Ygw-rWo63m= BFUXOcvmzMsn58vIVy29R14$ for graphic product...

    ATTN...WFO...EWX...FWD...HGX...SJT...

    ATTN...RFC...FWR...NWC...

    LAT...LON 32279745 32189668 31659620 30879615 30149649=20
    29599735 29539817 29999867 30789860 31619820=20 =20=20=20=20=20=20=20=20=20=20=20=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 06:00:17 2026
    AWUS01 KWNH 060600
    FFGMPD
    TXZ000-OKZ000-061030-

    Mesoscale Precipitation Discussion 0333
    NWS Weather Prediction Center College Park MD
    158 AM EDT Sat Jun 06 2026

    Areas affected...West-Central to Northwest Texas...Southwest to
    Central Oklahoma

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 060558Z - 061030Z

    SUMMARY...An elongated axis of slow-moving, locally backbuilding,
    and training thunderstorms will continue to impact portions of west-central/northwest Texas and southwest/central Oklahoma. High
    rainfall rates reaching up to 2 inches/hour will support locally
    an additional 3 to 4+ inches of rain going through the early
    morning hours. Regional areas of flash flooding are likely to
    continue with locally significant impacts possible.

    DISCUSSION...Recent regional radar imagery and satellite data show
    an expansive, elongated corridor of deep convection continuing to
    impact west-central into northwest Texas, extending northeastward
    into southwest and central Oklahoma. This convection is exhibiting
    classic nocturnal heavy rainfall characteristics, including
    persistent training and discrete backbuilding cells along the
    upwind flank of the axis.

    The atmospheric profile remains primed for extreme warm-rain
    efficiency. Precipitable water (PW) values across the region are
    highly anomalous, exceeding the 90th percentile of local
    climatology and running greater than 2.5 standard deviations above
    normal. This deeply tropical moisture plume is overlapping with a
    moderately unstable airmass, with recent mesoanalysis indicating
    elevated MUCAPE values pooling between 1000 and 2000 J/kg.

    Forcing for continuous convective regeneration is being provided
    by strong, divergent upper-level flow ahead of the southern High
    Plains trough/closed low which is interacting with a well-defined
    low-level surface trough. A strengthening 30 to 35 knot low-level
    jet is maximizing speed and directional moisture convergence along
    this low-level trough axis, continuously replenishing the
    instability.

    Furthermore, the local kinematic profile features highly favorable
    Corfidi upwind propagation vectors. As the low-level jet veers and
    reinforces the inflows, the resultant upwind vectors are shrinking significantly and orienting nearly parallel to the low-level
    convergent axis. This setup guarantees that new cells will
    repeatedly regenerate on the southwestern flank of the cluster and
    mature over the same downstream locations, resulting in a
    persistent train-echo effect.

    Given the deep warm-cloud layers and notable thermodynamic
    support, rainfall rates up to 2 inches/hour will still be
    achievable within the core of this activity. Where training
    becomes anchored for multiple hours, localized additional totals
    of 3 to 4+ inches are likely, which will continue to support a
    regional threat for flash flooding and potentially significant
    impacts.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4kuGlKSKhHWQ54WULKDNLnjlZWWtUsLqeu3JuPay9nFrnMwkb71RBOp0aFagi0lZRipf= 5epemFP_i8Ahrb7lOaCSPxE$ for graphic product...

    ATTN...WFO...FWD...LUB...MAF...OUN...SJT...

    ATTN...RFC...FWR...TUA...NWC...

    LAT...LON 35529794 35389750 34759749 34219772 33179821=20
    31779926 31500006 31680069 32000110 32470135=20
    33000107 33660021 34579936 35249872=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 07:12:25 2026
    AWUS01 KWNH 060712
    FFGMPD
    NEZ000-061015-

    Mesoscale Precipitation Discussion 0334
    NWS Weather Prediction Center College Park MD
    310 AM EDT Sat Jun 06 2026

    Areas affected...South-Central to Southeast Nebraska

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 060710Z - 061015Z

    SUMMARY...Locally backbuilding and training supercell
    thunderstorms will continue to foster concerns for flash flooding
    for a few more hours across south-central to southeast Nebraska
    before the activity weakens this morning.

    DISCUSSION...GOES-E IR satellite imagery shows deep cold-topped
    convection associated with a cluster of locally backbuilding and
    training supecell thunderstorms continuing across portions of
    south-central to southeast Nebraska.

    The activity remains somewhat anchored in close proximity to a
    front with notable moisture convergence. A southwest low-level jet
    of 30 to 35 kts interacting with the front coupled with a pool of
    elevated instability with MUCAPE values near 2000 J/kg has been
    helping top sustain the activity. Favorable Corfidi vector
    orientations have favored much of the slow overall advance of the
    convective mass over the last couple of hours with an excellent
    setup for backbuilding and training convective cells.

    Over the next few hours as boundary layer CIN increases further
    and the low-level jet weakens, the ongoing convection should begin
    to weaken and lose organization. For the next few hours, some
    additional rainfall rates of 1.5 to 2 inches/hour will be
    possible, and this may drive sufficient totals for some additional
    areas of flash flooding. However, the consensus of the latest
    hires CAMs suggest convection weakening toward dawn.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_5KxVtwV4FeDtqlA5z79jqWtbT9PN6DD2es5Pt7a5s1ZCcOvcA1dCMS89uySIU3_2VN8= cxImjpbkAu9_0OWcfrXjvoU$ for graphic product...

    ATTN...WFO...GID...OAX...TOP...

    ATTN...RFC...KRF...NWC...

    LAT...LON 41579848 41319709 40929630 40439610 39999656=20
    40019767 40439875 40969921 41399909=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 09:02:36 2026
    AWUS01 KWNH 060902
    FFGMPD
    TXZ000-OKZ000-061500-

    Mesoscale Precipitation Discussion 0335
    NWS Weather Prediction Center College Park MD
    500 AM EDT Sat Jun 06 2026

    Areas affected...Portions of Central and Northern Texas...The Red
    River Valley...Central and Eastern Oklahoma

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 060900Z - 061500Z

    SUMMARY...Expanding areas of highly efficient, locally training
    thunderstorms will spread northward across the region this
    morning. Pockets of extreme rainfall rates reaching 2 to 3
    inches/hour will be capable of producing localized totals of 3 to
    5+ inches. Scattered areas of flash flooding are likely, with
    sensitive urban locations being particularly vulnerable.

    DISCUSSION...An increasingly divergent flow regime is spreading
    aloft across the southern Plains as an upper-level trough and an
    associated closed low over west Texas gradually shift
    northeastward. Deep-layer southerly flow, positioned between this
    western trough and a subtropical ridge over the Southeast U.S.,
    has established a highly anomalous moisture conveyor belt. Recent
    OSPO/CIRA ALPW data highlights a dual-feed tropical moisture tap
    with Gulf moisture actively streaming northward in the low levels,
    while an eastern Pacific moisture feed is being drawn through the
    mid and upper-levels of the atmospheric column.

    This rich moisture profile features a substantial warm cloud
    layer. When coupled with moderate instability characterized by
    MLCAPE values locally up to 1500 J/kg, the environment is
    exceptionally primed for highly efficient, extreme rainfall rates.
    Furthermore, embedded vort maxima within the mid-level southerly
    flow are providing focused localized forcing for ascent. Over the
    past couple of hours, this energy has already supported focused
    convection with very high rainfall rates generally east of Waco
    (between the I-35 and I-45 corridors), where a band of storms is
    lifting north-northeastward and locally training over the same
    areas.

    Through the mid to late morning hours, the primary concern will
    shift northward as deep-layer moisture convergence and forced
    ascent increase across portions of the Red River Valley of the
    South. Convection is expected to increasingly impact northern
    Texas, including the highly vulnerable and densely populated
    Dallas-Fort Worth metropolitan area, as well as adjacent areas of
    southern, central, and eastern Oklahoma.

    The environment strongly supports the development of additional
    locally training and backbuilding thunderstorms. These high
    rainfall rates, which may reach 2 to 3 inches/hour with the
    stronger convective cores, and subsequent localized rainfall
    totals of 3 to 5+ inches this morning are strongly supported by a
    consensus of the 06Z HREF alongside recent runs of the HRRR and
    RRFS. This will likely result in at least scattered areas of flash
    flooding, posing an elevated threat to more sensitive urban
    locations.

    Orrison

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9dadn9aPspIktHaC7LfFauZ5-ampJcP2FRWywPfOdaOdU0mrmY6bgfdhDUOHRhMFNJIW= -nlmaiZOUzOLd2JwmgUaTw0$ for graphic product...

    ATTN...WFO...EWX...FWD...OUN...SHV...SJT...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 36599665 36509567 36049500 35319474 33919489=20
    32339546 30959646 30649748 30689837 31069893=20
    31669890 32269867 33479828 34479828 35709809=20
    36359748=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 14:45:40 2026
    AWUS01 KWNH 061445
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-KSZ000-062030-

    Mesoscale Precipitation Discussion 0336
    NWS Weather Prediction Center College Park MD
    1044 AM EDT Sat Jun 06 2026

    Areas affected...northeastern TX into eastern OK/western AR and
    adjacent portions of KS/MO

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 061443Z - 062030Z

    SUMMARY...At least localized patches of flash flooding appear
    likely from portions of northeastern TX into eastern OK and
    adjacent portions of western AR into southwestern MO and
    southeastern KS. Backbuilding and training of thunderstorms will
    produce 2 to 3+ in/hr rainfall.

    DISCUSSION...Regional radar imagery at 14Z across the Southern
    Plains showed scattered showers/thunderstorms extending from parts
    of northeastern TX into eastern OK as well as portions of
    northwestern AR. This activity was located within a region of
    pronounced upper level diffluence and divergence, to the east of a
    closed mid to upper-level low over northwestern TX. A very moist
    airmass existed from the west-central Gulf Coast into eastern
    OK/western AR with precipitable water values 0f 1.9 to 2.2 inches
    (12Z soundings/GPS ground-based stations). Wet bulb zero heights
    were 13-14 kft and MLCAPE was in the 500 to 1500 J/kg range with
    little to no inhibition. There were a number of embedded mesoscale
    vortices within the precipitation axis, helping to locally enhance
    rather efficient rainfall rates.

    With only a slow NNE motion forecast for the closed low, scattered thunderstorms will persist across northeastern TX into eastern OK
    and the MOKSAROK 4-state junction. Individual thunderstorm cells
    will advance north at 15-25 kt but with a southerly low level
    inflow of a similar direction and magnitude (highest over
    east-central OK with 850 mb winds of 25+ kt), the potential for
    backbuilding and training will be high.

    The placement of the upper low and corresponding zone of upper
    level divergence/diffluence combined along with the region of
    stronger low level flow over eastern OK seems to favor locations
    north of the Red River for the greatest threat for training and
    locally high rainfall over the next 3-5 hours. However, subtle
    regions of low level convergence over northeastern TX may also
    favor localized zones of training and high rainfall rates.

    The environment will support hourly rainfall of 2 to 3+ inches at
    times over isolated to widely scattered sections of TX/OK/AR with
    potential for 3 to 5+ inches on a localized basis through 20Z.
    These high rates are likely to lead to at least localized areas of
    flash flooding into the afternoon.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5f5tchBWXS0sgK9qmY-lPEBOjffZ8SVaJ-P77hdfWoZtU9u6kKRdcFw0piB3pbt-jQVJ= S36aJEA-rVZXllIzYCYU3KY$ for graphic product...

    ATTN...WFO...FWD...HGX...ICT...LZK...OUN...SGF...SHV...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 37199500 36889371 36529311 36159290 35389286=20
    34879325 33829422 32509443 31479474 31259515=20
    31329585 31609628 32469678 34139711 35699730=20
    36529719 36929674 37159584=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 15:39:12 2026
    AWUS01 KWNH 061539
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-062120-

    Mesoscale Precipitation Discussion 0337
    NWS Weather Prediction Center College Park MD
    1138 AM EDT Sat Jun 06 2026

    Areas affected...southeastern LA, southern MS/AL

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 061537Z - 062120Z

    SUMMARY...Very efficient showers and thunderstorms are expected
    over portions of the central Gulf Coast from southeastern LA into
    southern AL over the next several hours. Efficient rain rates of 1
    to 2 inches in 15-30 minutes are expected.

    DISCUSSION...1515Z radar imagery over the central Gulf Coast
    showed an axis of showers and thunderstorms stretching from just
    south of the MS/AL border into southern MS. A second but less
    pronounced axis was present to the east over eastern Baldwin
    County, AL into the northern Gulf. Visible satellite imagery
    showed hints of cyclonic turning over southeastern LA into
    southwestern MS with a low level convergence axis identified east
    of this feature over the Chandeleur Islands into the Gulf Coast of
    MS, before curving back toward the northwest into south-central
    MS. The 12Z LIX sounding sampled a very moist environment with a
    2.26 inch PW and a tall/skinny MLCAPE of 1150 J/kg. A SE to NW
    moisture gradient was evident in blended TPW imagery over the
    central Gulf Coast, a remnant of an old/dissipated frontal
    boundary.

    The RAP has been consistent with the forecast low level axis of
    convergence, remaining nearly stationary through 21Z, with only a
    gradual eastward translation. Given steering flow oriented
    similarly to the axis of convergence near the Gulf Coast, areas of
    training are expected along it with locally high rain rates due to
    the moist airmass. While areas of training will be somewhat
    transient due to a slight offset with the low level convergence
    axis and mean flow, warm rain processes should allow for 1 to 2
    inches of rain in 15-30 minutes and hourly rainfall of 2 to 3+
    inches. Back to the west, daytime heating and filtered sunshine
    over southeastern LA should lead to scattered thunderstorm
    development over the next 1-3 hours. High rain rates are likely to
    lead to isolated flash flooding along the Gulf Coast, with a
    particular focus across any urban areas. The flash flood threat is
    forecast to continue through 21Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!5twxHxeIkL_RNAFCinrwaHGOXf28hDJdvT_5WHjKh7mhxpBBZsUTUVg3C8R7U55tIrVg= RipWFvEHjeBzwfP45mCLzvk$ for graphic product...

    ATTN...WFO...JAN...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 31908959 31838890 31608812 31348769 30738739=20
    29898742 29218814 28858895 29308932 29508991=20
    29729084 30339099 30899076 31499024=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 16:18:46 2026
    AWUS01 KWNH 061618
    FFGMPD
    LAZ000-TXZ000-062200-

    Mesoscale Precipitation Discussion 0338
    NWS Weather Prediction Center College Park MD
    1217 PM EDT Sat Jun 06 2026

    Areas affected...southeastern TX into far western LA

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 061616Z - 062200Z

    SUMMARY...Isolated flash flooding will be possible across portions
    of southeastern TX into far western LA through the afternoon.
    While the coverage of any flash flood issues should stay limited,
    there will be the potential for very high rain rates in excess of
    2 to 3 inches per hour.

    DISCUSSION...GOES-E visible satellite imagery at 16Z showed the
    early stages of scattered showers/thunderstorms over the upper TX
    Coastal Plain, along with a southward sinking outflow boundary to
    the north which extended from Williamson to Walker counties. The
    cells were moving with the mean layer flow at 10 to 15+ kt toward
    the northeast, of a similar orientation to the low level flow,
    supportive of at least short term training. The environment was
    very moist with PWs of 2.0 to 2.2 inches along with MLCAPE of 1000
    to 2000 J/kg (SPC mesoanalysis, satellite blended TPW and GPS
    ground-based sensors).

    While no obvious axes of SW to NE low level convergence (oriented
    with the mean wind) are seen in the short term high res guidance
    through the afternoon, the potential for brief backbuilding and
    training will still exist over the next several hours. Diurnally
    driven convection with the added component of convergence with the
    southward sagging outflow boundary will maintain scattered showers
    and thunderstorms well into the afternoon. While much of this
    region of TX is usually able to handle high rain rates without
    problems, recent days of localized heavy rainfall have lowered
    flash flood guidance values into the 2 to 3 in/hr range across
    several locations. The lowered FFG combined with potential for
    urban overlap and high rain rates is enough to warrant a
    limited/isolated concern for flash flooding due to 2 to 3+ inches
    of rain in an hour.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4yBFIvGDNzg-XrVEW3ux6rnkjjuTyuu0b8BmPuVDlfFM3I8HDObHBoygWbEtJVqbg1cU= IU2rBIVAeE6xoa3j-CdarOE$ for graphic product...

    ATTN...WFO...CRP...EWX...HGX...LCH...SHV...

    ATTN...RFC...FWR...ORN...NWC...

    LAT...LON 31399362 31259304 30389299 29599338 29309457=20
    28679557 28459627 28609650 29419658 30309639=20
    30619602 30849523 31339427=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 18:30:04 2026
    AWUS01 KWNH 061829
    FFGMPD
    OHZ000-KYZ000-INZ000-ILZ000-070015-

    Mesoscale Precipitation Discussion 0339
    NWS Weather Prediction Center College Park MD
    228 PM EDT Sat Jun 06 2026

    Areas affected...eastern IL into central IN and western OH

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 061827Z - 070015Z

    SUMMARY...Thunderstorm coverage is expected to increase across
    portions of IL into IN and OH through the early evening. Widely
    scattered to scattered instances of flash flooding will be
    possible with training of cells expected to generate hourly
    rainfall of 1 to 2+ inches.

    DISCUSSION...18Z surface observations and visible satellite
    imagery showed the western fringes of an outflow boundary across
    eastern IL into IN and southern OH, related to a forward
    propagating cluster of storms that tracked through the Midwest
    this morning, and which was currently moving into northern
    WV/southwestern PA. Also observed on visible imagery was the early
    stages of likely thunderstorm development near the western end of
    the outflow from near/south of IKK to LAF and along a lake breeze
    boundary to the southwest of Lake Michigan. SPC 18Z mesoanalysis
    showed moderate to strong instability in the vicinity of the
    outflow boundary (MLCAPE of 1000-3000 J/kg) along with PWs of 1.5
    to 1.7 inches. Surface to 850 mb layer winds of 10-20 kt were
    acting upon the outflow boundary with continued convergence likely
    to result in the development of a few thunderstorms over the next
    1 to 3 hours from IL into OH.

    The WNW to ESE orientation of the outflow boundary is similar to
    that of the expected mean cell motion toward the ESE at 20-30 kt.
    Despite this progressive motion, a flash flood concern comes into
    the picture given the potential for upstream redevelopment of
    thunderstorms along the remnant or newly generated outflow
    boundary/boundaries. The unstable/moist airmass will be capable of
    1 to 2+ in/hr rainfall where cells train. Resulting rainfall
    totals of 2 to 3 inches (locally higher possible) could produce
    widely scattered to scattered occurrences of flash flooding
    through 00Z.

    Otto

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!7_JNhk-JkcJCjA45kLTAOliwj_jtDvMVgOSc7EidEX7sRl1I02a5IUVTauAfhCsAto10= yFDbL2Qh8azP1jGKpJGVg5M$ for graphic product...

    ATTN...WFO...ILN...ILX...IND...IWX...LOT...RLX...

    ATTN...RFC...MSR...TIR...NWC...

    LAT...LON 41578761 41008514 40408321 39678244 39058304=20
    39048463 39618647 40118863 40798889=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 20:13:43 2026
    AWUS01 KWNH 062013
    FFGMPD
    MOZ000-IAZ000-KSZ000-NEZ000-070212-

    Mesoscale Precipitation Discussion 0340
    NWS Weather Prediction Center College Park MD
    412 PM EDT Sat Jun 06 2026

    Areas affected...northern Missouri, southern Iowa, southeastern
    Nebraska, and northeastern Kansas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 062012Z - 070212Z

    Summary...Scattered thunderstorms are developing along an axis
    from Maryville, KS to Kirksville, MO. Sensitive ground conditions
    exist in these areas. Flash flooding is expected on at least an
    isolated basis through 02Z/9p this evening.

    Discussion...Scattered thunderstorms have developed in earnest
    across the discussion area from northeastern KS through northern
    MO. Forcing mechanisms for this activity are a bit unclear/weak -
    though storms are collocated with the axis of 1) strongest
    regional instability (2500+ J/kg MLCAPE), 2) high moisture content
    (1.6 inch PW), and 3) weak/negligible convective inhibition. The
    storms were in a weakly sheared environment, with very little
    steering flow to aid in storm movement and/or propagation. The
    storms were also forming over wet/waterlogged soils from prior
    rainfall over the past 48 hours, with lowered FFG thresholds
    (around 1-1.25 inch/hr) further indicating the sensitive nature of
    the ground conditions in the area.

    Flash flooding will become more of a concern as these storms
    persist/expand in coverage through the early evening. As cold
    pools mature beneath expanding convection, occasional mergers and
    erratic local motions could foster 2 inch/hr rain rates at times
    -- well above local FFG. Flash flooding is expected on at least
    an isolated basis, with models/CAMs suggestive of this threat
    persisting through at least 02Z/9p central this evening.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!4fk8-cJtJVtc7NhhZztkxgxIvEvkQ77YxXRm7gN-PPuv20e0Xq8JzzTEGqtNBke9Yasv= upYZo2FRvxBErhwlMhV-TqI$ for graphic product...

    ATTN...WFO...DMX...DVN...EAX...GID...LSX...OAX...TOP...

    ATTN...RFC...KRF...MSR...NWC...

    LAT...LON 41329336 40789193 39799182 39049358 39249664=20
    39819800 40649732 41189607=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 20:36:46 2026
    AWUS01 KWNH 062036
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-KSZ000-070234-

    Mesoscale Precipitation Discussion 0341
    NWS Weather Prediction Center College Park MD
    435 PM EDT Sat Jun 06 2026

    Areas affected...eastern Oklahoma, far western Arkansas

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 062034Z - 070234Z

    Summary...Flash flood potential continues. Several areas of rain
    rates exceeding 1 inch/hr continue as storms move slowly northward
    across the discussion area.=20

    Discussion...Flash flood potential continues across the discussion
    area. Recent radar/MRMS depicts scattered, but occasionally
    strong convection drifting northward across eastern Oklahoma.=20
    Storms have exhibited occasional local backbuilding/training from
    time to time, and continue to develop/regenerate over southeastern
    Oklahoma, where buoyancy is maximized (around 2000 J/kg MLCAPE)
    and moisture is abundant (2+ inch PW values). Modest low-level
    confluence (surface through 850mb) also continues across this
    region, fueling convective development. Lastly, these cells were
    forming over wet ground conditions from prior rainfall, which
    exceeded 2 inches in many areas (and locally 5-8 inches just
    west/southwest of Tulsa). Local FFG thresholds are near 0 in a
    few spots, although 1-1.5 inch/hr thresholds are common.

    Models/CAMs suggest that this regime (which continues to support
    occasional flash flood risk) will continue for several more hours
    - perhaps through 02Z/9p central or so. There is some risk that
    convection over western north Texas makes it into western portions
    of the discussion area (south-central Oklahoma) with greater
    progression, lower rain rates, and a more mature upstream cold
    pool that may disrupt the overall convective regime, though this
    scenario is conditional and could take several hours to play out.=20
    Convection may be more directly modulated by the degree of
    insolation, with guidance showing a weakening trend possible after
    sunset. Through that time, occasional 1-2 inch/hr rates and wet
    soils will pose a continued flash flood risk, with locally
    significant impacts possible near urban areas and other locally
    sensitive areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!9ou8Ftn7V10ikXQqS2KkD3h_JJMGlCUHKfktEgnsy_3Z21279U1mOPAvTkBiIlI_FVF6= 7FCnM0FD44L1fkDOq-CxHlo$ for graphic product...

    ATTN...WFO...FWD...ICT...LZK...OUN...SGF...SHV...TSA...

    ATTN...RFC...ORN...TUA...NWC...

    LAT...LON 37169398 36179334 34079354 33299437 33409600=20
    34129694 36009674 37079568=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 21:10:50 2026
    AWUS01 KWNH 062110
    FFGMPD
    FLZ000-ALZ000-MSZ000-LAZ000-070309-

    Mesoscale Precipitation Discussion 0342
    NWS Weather Prediction Center College Park MD
    509 PM EDT Sat Jun 06 2026

    Areas affected...southern Mississippi, southeastern Louisiana, and
    far southern Alabama

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 062109Z - 070309Z

    Summary...Flash flood potential continues as a weak mid/upper
    disturbance continues to force deep convection over the discussion
    area.

    Discussion...Flash flood potential continues. Deep convection
    remains slow-moving (with weak steering flow aloft per
    mesoanalyses) but focused along a couple of low-level convergence
    axes (evident per surface obs), 1) from near Natchez, MS to
    Hammond/Slidell, LA and 2) along a small bowing convective segment
    over Harrison County, MS north of Gulfport. The storms were
    ingesting extremely moist/buoyant air in the pre-convective
    airmass (2+ inch PW values, 1500 J/kg MLCAPE along and west of the aforementioned convergence zones), while subtle ascent supported
    by the mid-level vort max over the region further supports deep,
    slow-moving convection. Rain rates above 2 inch/hr have been
    common especially from Slidell/St. Tammany eastward into the
    southern MS coastal counties, and that's where impacts have been
    reported so far today.

    These trends are expected to continue for at least another 2-4
    hours or so. Models suggest that most convective will be
    diurnally driven, with some weakening expected after sunset,
    though locally heavy rainfall cannot be ruled out even after
    02Z/9p central. High rain rates (perhaps reaching 2-3.5 inch/hr)
    may occur where training is most pronounced. These rates will
    cause continued flash flood potential especially in areas 1)
    already experiencing impacts, 2) that have soaked soils from
    abundant prior rainfall, or 3) fall in urbanized areas.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_gwfLopQcc5yz4bF0rA_pXuBgkwkvD2XdLPbRRK9bNvKvWXJd7pG5YBHUiWqZv1OE3CA= _tWBUSRaWmZVzPfv08PNtaQ$ for graphic product...

    ATTN...WFO...JAN...LCH...LIX...MOB...

    ATTN...RFC...ALR...ORN...NWC...

    LAT...LON 31969095 31878874 30848752 29678801 29078930=20
    29269102 30259184 31189156=20

    =3D =3D =3D
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  • From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Sat Jun 6 21:39:22 2026
    AWUS01 KWNH 062139
    FFGMPD
    TXZ000-OKZ000-070337-

    Mesoscale Precipitation Discussion 0343
    NWS Weather Prediction Center College Park MD
    538 PM EDT Sat Jun 06 2026

    Areas affected...portions of west-central into north-central Texas
    and south-central Oklahoma

    Concerning...Heavy rainfall...Flash flooding likely

    Valid 062137Z - 070337Z

    Summary...Scattered thunderstorms may pose a flash flood threat
    across the discussion area through at least 03Z/10p central.

    Discussion...Scattered thunderstorms continue to focus along a
    general axis form near Decatur south-southwest to near San Angelo,
    with a separate cluster of storms noted west of Ardmore, OK.
    Convection in northern portions of this axis near Decatur was
    fairly progressive, which has kept rain rates relatively low
    (around 1 inch/hr or less). Northeast of this axis (near
    Ardmore), local backbuilding has led to spotty rain rates
    exceeding 2 inches/hr. Rain rates remain limited with
    southwestward extent toward west-central Texas mainly due to the
    more scattered, progressive nature of storms (with motions toward
    the northeast at around 25 knots). Flash flood potential has
    remained isolated so far in this regime.

    Over time though, models/observations suggest that convection may
    begin to focus/concentrate along an axis from near Fort Worth to
    near San Angelo. An outflow from more mature convection off to
    the northeast of this region may stall, while ascent from a
    mid-level low centered over the TX Panhandle, low-level confluence
    ahead of the convection, and abundant moisture/instability should
    result in more focused axes of training over time. Orientation of
    convection more parallel to steering flow aloft may also aid in
    training convection over time as well. Should this scenario unfold
    as models/obs suggest, rain rates should increase into the 2
    inch/hr range in spots and locally exceed FFG thresholds -
    especially between Fort Worth and San Angelo. Deep convection and
    heavier rain rates may also eventually reach the more of the DFW
    metro are as well. Flash flooding is possible in this regime on
    an isolated basis over the next couple hours, but this risk may
    increase with progression into the evening. A more isolated flash
    flood risk may also occur in south-central Oklahoma, though it
    appears that convection west of Ardmore may eventually merge with faster-moving, forward-propagating convection over north-central
    Texas that may temper this threat somewhat. Flash flooding is
    still possible in this area pending convective trends.

    Cook

    ...Please see https://urldefense.com/v3/__http://www.wpc.ncep.noaa.gov__;!!= DZ3fjg!_HpmkIEDH1NRdpPBBzznBzhBWyQM8V4K5w_bh7iP9bC0kUHrEdArmqnyO7-JXAz6W4MQ= RnOgkwp16enChQTYV9zs2ZQ$ for graphic product...

    ATTN...WFO...EWX...FWD...MAF...OUN...SJT...TSA...

    ATTN...RFC...FWR...ORN...TUA...NWC...

    LAT...LON 35589629 34249570 32089630 30999772 30509999=20
    31310103 32820062 32769939 33199852 34779828=20
    35509745=20

    =3D =3D =3D
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