• MESO: Mesoscale Discussion 2133

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sun Sep 10 20:14:35 2023
    ACUS11 KWNS 102014
    SWOMCD
    SPC MCD 102013=20
    OKZ000-KSZ000-TXZ000-COZ000-NMZ000-102245-

    Mesoscale Discussion 2133
    NWS Storm Prediction Center Norman OK
    0313 PM CDT Sun Sep 10 2023

    Areas affected...parts of northeastern New Mexico...southeastern
    Colorado...and the Texas and Oklahoma Panhandles into southwestern
    Kansas

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

    Valid 102013Z - 102245Z

    Probability of Watch Issuance...60 percent

    SUMMARY...Isolated to widely scattered strong thunderstorm
    development is possible through 5-6 PM CDT. This may include an
    isolated supercell or two, posing a risk for severe hail, locally
    strong surface gusts and perhaps a brief tornado.

    DISCUSSION...Low-level moistening is still ongoing within weak, but
    slowly deepening surface troughing to the lee of the southern
    Rockies. This is occurring beneath warm and capping elevated
    mixed-layer, and mid-level ridging to the north of a still fairly
    prominent subtropical high centered over the northwestern Mexican
    Plateau. In response to a series of short wave perturbations
    progressing around the periphery of the ridge in the near term, and,
    later, digging mid-level troughing across the northern Great Plains,
    mid-level heights are gradually beginning to fall.

    It appears that large-scale forcing for ascent will lead to
    increasing convective development spreading off the Front Range into
    the destabilizing boundary layer across and east of northeastern New
    Mexico and southeastern Colorado by early this evening. Potential
    for the initiation of sustained thunderstorm development in advance
    of this activity, through late afternoon, remains more unclear.=20=20

    Based on objective analysis, mixed-layer CAPE remains fairly modest
    to the north of the Texas Panhandle vicinity, currently maximized
    around 1000 J/kg near the Colorado/Kansas border. However, shear
    for boundary-layer based thunderstorm development is sufficient for
    supercells beneath 30 kt west-northwesterly mid-level flow (around
    500 mb). Farther south, mixed-layer CAPE is more substantive, but
    shear remains weaker.

    With additional surface heating, it appears possible that weakening
    of lingering mid-level inhibition may become sufficient for at least
    widely scattered thunderstorm development. A zone of enhanced lower/mid-tropospheric warm advection, currently centered to the
    west/northwest of Garden City KS, may provide one potential focus
    for thunderstorm initiation during the next hour or two. As this
    activity acquires increasing inflow of destabilizing boundary-layer,
    it may rapidly intensify and organize, accompanied by increasing
    potential for severe hail and perhaps some risk for a tornado
    through 22-23Z.

    ..Kerr/Guyer.. 09/10/2023

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!9bPRE8jCUIuRe0bU2gpkPdUwCswOIqumMgx77rzBUKFwgwnSfdUMF0zWgK_d88yQfnZk5tKiK= iJtQtUGgGT29gBNcj8$ for graphic product...

    ATTN...WFO...OUN...DDC...GLD...LUB...AMA...PUB...ABQ...

    LAT...LON 37350277 38420253 38800174 38540046 38029982 36909958
    33770062 34030194 34280395 35780381 37350277=20


    =3D =3D =3D
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