• MESO: Mesoscale Discussion 1151

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Jun 18 20:13:24 2023
    ACUS11 KWNS 182013
    SWOMCD
    SPC MCD 182012=20
    LAZ000-ARZ000-TXZ000-OKZ000-182145-

    Mesoscale Discussion 1151
    NWS Storm Prediction Center Norman OK
    0312 PM CDT Sun Jun 18 2023

    Areas affected...portions of northeastern Texas into northwestern
    Louisiana

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

    Valid 182012Z - 182145Z

    Probability of Watch Issuance...40 percent

    SUMMARY...Trends are being monitored for the possibility of
    thunderstorm development over the next few hours. The severe threat
    is highly conditional on storm development. Should storms develop,
    severe hail/wind will be possible and a tornado cannot be ruled out.

    DISCUSSION...Insolation following earlier storms has allowed for
    ample surface heating and associated modification of the boundary
    layer around/just south of the Arklatex. Some slightly agitated
    cumulus have recently become apparent ahead of a southward sagging
    boundary, which also intersects another outflow boundary left behind
    by earlier storms. Surface temperatures reaching 90 F amid 75+ F
    dewpoints, overspread by 8.5 C/km mid-level lapse rates, is
    contributing up to 4500 J/kg MLCAPE. While some billow clouds are
    evident via visible satellite, the agitation of cumulus also
    suggests that remaining convective inhibition/boundary-layer
    stabilization continues to erode. The presence of a 30 kt
    southwesterly low-level jet, overspread by 50+ kts of
    west-northwesterly 500 mb flow, is also supporting modestly curved,
    elongated hodographs bearing 50+ kts of effective bulk shear across
    the warm sector. As such, supercells would likely be the primary
    mode of convection, with any storm mergers supporting
    southeastward-propagating bow-echo MCSs.

    The ambient environment clearly supports the potential for
    significant severe storms, including very large hail and perhaps a
    tornado with supercells, and severe gusts with bowing structures.
    However, relatively neutral height falls introduces uncertainty of
    convective initiation, with high-resolution model guidance
    demonstrating little consensus for a given solution. Nonetheless,
    convective trends will continue to be monitored and a WW issuance
    may be needed if clearer signals of thunderstorm development become
    apparent.

    ..Squitieri/Hart.. 06/18/2023

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!9A0HsY5MWb0V1I7gbSnVjCB8A49cHhpkCA5YkXVWcwH9IIL5qBkULKb2zGx-dmO4SyzYknRdA= HB5ApDdlRFwpYK2gCM$ for graphic product...

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

    LAT...LON 31589669 31929710 32419717 33169639 33749525 33889444
    33709410 33349387 32769367 32069358 31749378 31529432
    31369515 31319577 31369619 31589669=20


    =3D =3D =3D
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