• MESO: Mesoscale Discussion 1210

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Jun 22 19:51:44 2023
    ACUS11 KWNS 221951
    SWOMCD
    SPC MCD 221951=20
    OKZ000-TXZ000-222145-

    Mesoscale Discussion 1210
    NWS Storm Prediction Center Norman OK
    0251 PM CDT Thu Jun 22 2023

    Areas affected...the eastern Texas Panhandle and western/southern
    Oklahoma

    Concerning...Severe potential...Watch unlikely=20

    Valid 221951Z - 222145Z

    Probability of Watch Issuance...20 percent

    SUMMARY...A persistent cluster of thunderstorms could still further
    intensify and organize, posing increasing potential for strong
    surface gusts across the eastern Texas Panhandle through
    western/southwestern Oklahoma late this afternoon. Although it is
    not yet clear that a severe weather watch will be needed, due to
    lingering uncertainties, trends will continue to be monitored for
    this possibility.

    DISCUSSION...Lower/mid-tropospheric warm advection (around 700 mb),
    focused within the thermal gradient along the periphery of warm and
    more strongly capping elevated mixed-layer air, has supported
    persistent convective development within an evolving cluster across
    the Oklahoma into Texas Panhandle vicinity. Based on MRMS data,
    stronger cells have been occasionally producing severe hail. More
    recently stronger outflow surface gusts have been observed near and
    southwest of Perryton, TX.

    With at least a core of colder cloud tops and higher lightning flash
    rates being maintained across the northeastern Texas Panhandle,
    north/east of Pampa into areas near/west and south of Gage, OK,
    further strengthening of the associated surface cold pool could
    provide support for intensifying new thunderstorm development during
    the next few hours. It appears that a forward (southeastward)
    propagating segment of the outflow will begin to encounter an
    increasingly unstable boundary-layer characterized by moderately
    large CAPE, in the presence of steep mid-level lapse rates, as
    mid-level inhibition continues to weaken.

    Although this is embedded within a generally weak westerly mean
    environmental flow, with modest shear, the environment may be
    conducive to the gradual evolution of a substantive mesoscale
    convective vortex, accompanied by strengthening rear inflow and a
    further increase in potential for potentially damaging wind gusts .

    ..Kerr/Hart.. 06/22/2023

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!56Q9LUJhNS6H7lnm7SAOccs8qMJDa79B19Ds1JTUi7ASqbUP-KHoYkokDk2K0bnkex4RCyc3h= BiLt8SarlVjgqsuMRk$ for graphic product...

    ATTN...WFO...OUN...LUB...AMA...

    LAT...LON 36239958 35739891 34669712 33979839 34460027 35610076
    35790003 36239958=20


    =3D =3D =3D
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