• MESO: Mesoscale Discussion 1249

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 13 19:02:56 2024
    ACUS11 KWNS 131902
    SWOMCD
    SPC MCD 131902=20
    ILZ000-IAZ000-MOZ000-KSZ000-NEZ000-132100-

    Mesoscale Discussion 1249
    NWS Storm Prediction Center Norman OK
    0202 PM CDT Thu Jun 13 2024

    Areas affected...Northwest/West-Central IL...Southern IA...Northern
    MO...Far Southeast NE...Northeast KS

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

    Valid 131902Z - 132100Z

    Probability of Watch Issuance...95 percent

    SUMMARY...Severe thunderstorms are expected to develop along and
    ahead of a cold front from northwest/west-central Illinois into far
    southeast Nebraska and northeast Kansas this afternoon. Very large
    hail up to 3" in diameter and gusts from 60 to 80 mph are possible
    and a watch will be needed to cover this severe potential.

    DISCUSSION...Recent visible satellite imagery has recently shown an
    increase in deepening cumulus along a pre-frontal trough from northwest/west-central IL west-southwestward into far southeast NE
    and northeast KS. Temperatures in this region have warmed into the
    upper 80s/low 90s amid dewpoints in the low 70s, contributing to
    very strong buoyancy. Recent mesoanalysis estimates MLCAPE currently
    ranges from 2500 J/kg over IL to over 3500 J/kg across far southeast
    NE and northeast KS. These values will likely increase as strong
    diurnal heating persists throughout the afternoon. As observed in
    recent ACARS soundings and the 18Z DVN sounding, some convective
    inhibition remains in place, but continued diurnal heating should
    help to erode this inhibition as well.=20

    Robust thunderstorm development is expected to take place quickly
    once inhibition erodes and convective initiation occurs. Large to
    very large hail up to 3" in diameter is possible with the initial,
    more cellular development. Strong buoyancy amid high cloud bases and
    steep low-level lapse rates will foster strong outflow, with the
    potential for this outflow to amalgamate with resultant upscale
    growth into a coherent convective line. When this occurs, the
    primary severe risk should shift to severe gusts (i.e. 60 to 80
    mph). Veered low-level flow and a mixed boundary layer should
    mitigate the tornado potential, although a low probability for a
    tornado or two exists whenever there is a predominantly
    supercellular mode.

    ..Mosier/Gleason.. 06/13/2024

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!8yFvYoiZqh_a97M8MBQG3Mv4sCOojIUgQn96yq8B0iEienkYhMUW1woNtoPGfKgIJegdpu4zH= x_2nG-bOhEtGvBEkbE$ for graphic product...

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

    LAT...LON 41828982 41308948 40268979 39839035 39449156 38959420
    39019582 40349654 41159471 41469241 41899111 41828982=20


    =3D =3D =3D
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