• MESO: Mesoscale Discussion 0629

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat May 4 17:37:21 2024
    ACUS11 KWNS 041737
    SWOMCD
    SPC MCD 041736=20
    TXZ000-NMZ000-042000-

    Mesoscale Discussion 0629
    NWS Storm Prediction Center Norman OK
    1236 PM CDT Sat May 04 2024

    Areas affected...West to southwest Texas

    Concerning...Severe potential...Watch likely=20

    Valid 041736Z - 042000Z

    Probability of Watch Issuance...80 percent

    SUMMARY...Thunderstorm development along a southward-surging cold
    front is likely within the next 1-2 hours with additional convection
    expected later this afternoon across southwest TX. Given a favorable environment for organized severe convection, one or more watches
    will likely be needed in the coming hours.

    DISCUSSION...Transient convection, along with a more robust cell
    near Snyder, TX, is noted along and just behind a surface cold front
    per regional radar and GOES visible/IR imagery at around 17:30 UTC.
    Aside from the Snyder, TX cell, this convection has been short-lived
    so far, likely owing to rapid displacement of initial updrafts onto
    the cool side of the boundary. The development of additional
    deep/robust convection is probable in the next couple of hours as
    the downstream air mass continues to destabilize. Initial cells will
    continue to be displaced along/behind the boundary given
    boundary-parallel mean flow and post-frontal deep-layer shear
    vectors. However, MUCAPE within the post-frontal air mass coupled
    with elongated hodographs should support a few more intense storms
    capable of large to very large hail.=20=20

    Further south ahead of the cold front, RAP mesoanalyses suggests
    MLCIN is slowly eroding. However, convective initiation appears less
    imminent based on latest visible imagery trends. Morning CAM
    guidance suggests thunderstorm development along/ahead of the
    dryline is most probable during the 18-21 UTC period closer to peak
    diurnal heating and as modest ascent ahead of an approaching upper
    wave overspreads the region. Thunderstorms developing within the
    warm sector (most likely off the Davis Mountains where shallow
    cumulus is beginning to develop) will likely evolve into high-based
    supercells with a risk for large to very large hail. The tornado
    risk is expected to increase through late afternoon and early
    evening as cells migrate eastward into an increasingly moist air
    mass with strengthening southeasterly winds (which should bolster
    effective SRH to around 150 m2/s2).=20

    Given these two regimes, a severe thunderstorm watch will likely be
    needed for locations north of the cold front with a tornado watch
    required for areas south of the boundary. Convective trends along
    the cold front and dryline/higher terrain will continue to be
    monitored to determine exact timing of either watch issuance.

    ..Moore/Smith.. 05/04/2024

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!_Z2hOAmMYibBjMVOK2BCGokpuqi15m4Ba7PZQx3tAA-t2mDyfFZzbhooI1IIY7mkjIKSG0_PL= w2h0V3rXOiCMeO6KHU$ for graphic product...

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

    LAT...LON 29670283 29820339 30930348 31810370 32270368 32960318
    33290257 33530184 33490034 33299967 32899924 32139904
    31559905 31329913 30869945 30390011 30010091 29740166
    29730237 29670283=20


    =3D =3D =3D
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