• MESO: Mesoscale Discussion 1968

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Aug 12 19:57:12 2023
    ACUS11 KWNS 121957
    SWOMCD
    SPC MCD 121956=20
    NEZ000-SDZ000-WYZ000-122200-

    Mesoscale Discussion 1968
    NWS Storm Prediction Center Norman OK
    0256 PM CDT Sat Aug 12 2023

    Areas affected...west-central SD and the vicinity

    Concerning...Severe potential...Watch possible=20

    Valid 121956Z - 122200Z

    Probability of Watch Issuance...60 percent

    SUMMARY...Continued thunderstorm development is expected this afternoon/evening. Severe wind gusts and large hail will be the
    primary threats. Watch issuance is possible.

    DISCUSSION...Convective development is underway near the Black Hills
    northward through northwestern SD. These thunderstorms are located
    to the northeast of a surface low -- centered over eastern WY -- at
    the periphery of a low-level warm, moist axis extending northward
    through western NE and SD. A belt of west-southwesterlies aloft
    overspreads the northern Plains, with 30-35 kt 500-mb flow currently
    analyzed over west-central SD. Large-scale ascent in the
    right-entrance region of this mid-level jet, as well as enhanced
    surface convergence to the northeast of the surface cyclone, are
    expected to support continued updraft development and
    intensification this afternoon in the delineated area.

    The richest low-level moisture resides to the south, with 60s-F
    dewpoints reaching to around the SD/NE border. However, temperatures
    in the lower 80s F and dewpoints generally in the mid-50s F are
    contributing to MLCAPE around 1000-1500 J/kg in southwest SD.
    Continued diurnal heating into the mid-80s F should promote
    sufficiently deep boundary-layer mixing to erode remaining
    inhibition and support thunderstorm development. Forecast profiles
    depict rather dry air near the top of the boundary layer and at
    mid-levels, suggesting realized updraft buoyancy will be tempered
    somewhat by entrainment. However, straight hodographs with 0-6-km
    shear around 40 kts should be sufficient to support supercell
    development with successful initiation attempts. The shear profile
    will favor updraft splitting early in individual storms' lifecycles,
    with both flanks offering a threat for severe wind gusts and large
    hail. Given relatively dry boundary layers and weak low-level shear,
    individual supercells/clusters should grow upscale by the evening,
    yielding more of a severe-wind threat thereafter. A Severe
    Thunderstorm Watch will likely be needed sometime this afternoon to
    address these threats.

    ..Flournoy/Smith.. 08/12/2023

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!8IwwZGZ_pfEy1LwgMbBqVCY4iAIwPpS50fAhtoXXPOmT66Kvq9CjOwRgJ8q-WAIKKPzNMDber= pW4cLDIva7CzEIab2Q$ for graphic product...

    ATTN...WFO...ABR...LBF...UNR...CYS...

    LAT...LON 43410404 44060433 44640428 44990378 44990227 44650087
    43999973 43289960 42700011 42550193 42800335 43410404=20


    =3D =3D =3D
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