• MESO: Mesoscale Discussion 0613

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Fri May 3 18:19:11 2024
    ACUS11 KWNS 031819
    SWOMCD
    SPC MCD 031818=20
    TXZ000-032015-

    Mesoscale Discussion 0613
    NWS Storm Prediction Center Norman OK
    0118 PM CDT Fri May 03 2024

    Areas affected...parts of the Texas South Plains and Permian Basin

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

    Valid 031818Z - 032015Z

    Probability of Watch Issuance...80 percent

    SUMMARY...Isolated to widely scattered thunderstorm development,
    including a couple of evolving supercells, appears increasingly
    probable through 2-4 PM CDT. Strongest storms may eventually become
    capable of producing large hail in excess of 3 inches in diameter,
    and perhaps potential for a tornado.

    DISCUSSION...Seasonably high boundary-layer moisture content beneath
    steep lapse rates associated with warm elevated mixed-layer air is
    allowing for the development of strong to extreme potential
    instability with full insolation. During the next few hours this
    will become focused along a zone of strengthening differential
    surface heating and mixing, where an initial cold frontal surge into
    the Texas South Plains has stalled and is weakening, and along a
    sharpening dryline south of this boundary into the Davis Mountains
    vicinity.

    Mid/upper support for convective development is unclear, but west to southwesterly flow aloft appears to be trending at least broadly
    difluent, as initially weak low-level warm advection becomes a bit
    more enhanced along the boundaries. The Rapid Refresh and
    High-Resolution Rapid Refresh, among other output, suggest that the
    initiation of isolated to widely scattered storms may commence as
    early as 19-21Z, as convective temperatures are approached.

    Lower through mid-level wind fields are at least initially rather
    weak, but veering with height beneath 20-40 kt flow in the 500-300
    mb layer seems likely to be supportive of the evolution of intense
    supercell structures given the instability. Tornadic potential
    appears a bit more unclear, but in the presence of light to modest southwesterly deep layer mean flow, rightward propagating storms
    along the segment of strengthening differential heating roughly
    near/north of Big Spring into areas west of Abilene may pose the
    most appreciable risk.

    ..Kerr/Smith.. 05/03/2024

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!4-f_nNe5mfWo1F9n2Mh5hugIoIiCwjNk8nmO0nM5B9zwfuKyD7-9L_Wz_-vzDRGeLyM-StqPe= AjlU_zadN4L-auGroU$ for graphic product...

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

    LAT...LON 31909934 31220098 30610136 29930172 29780198 29640274
    30990296 31900244 33200179 32849974 31909934=20


    =3D =3D =3D
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