• MESO: Mesoscale Discussion 1834

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Jul 29 20:00:24 2025
    ACUS11 KWNS 292000
    SWOMCD
    SPC MCD 291959=20
    NEZ000-292200-

    Mesoscale Discussion 1834
    NWS Storm Prediction Center Norman OK
    0259 PM CDT Tue Jul 29 2025

    Areas affected...parts of southwest into central Nebraska

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

    Valid 291959Z - 292200Z

    Probability of Watch Issuance...40 percent

    SUMMARY...Strongest thunderstorm development may become focused
    across parts of southwestern into central Nebraska through 4-7 PM
    CDT. This may include a few evolving supercell structures posing a
    risk for large hail, locally damaging wind gusts and perhaps a brief
    tornado.

    DISCUSSION...Within lee surface troughing across much of western
    Kansas and adjacent portions of the high plains, a strongly heating
    (including surface temperatures approaching 100 F) and increasingly
    deeply mixed boundary layer is becoming characterized by moderate
    CAPE based on latest objective analysis. Mid-level inhibition is
    gradually eroding and deepening convective development is evident,
    including the initiation of scattered thunderstorm activity. As a
    weak mid-level perturbation shifts east of the Front Range, models
    suggest that thunderstorm development may increase either side of a
    remnant frontal zone within the lee surface trough, which is
    forecast to slowly shift southeast of the high plains through early evening.=20=20

    Near the nose of the stronger pre-frontal heating, now developing
    north and east of the McCook NE vicinity toward areas between North
    Platte and Kearney, surface dew points in the lower 70s F are
    contributing to moderate to large CAPE along an initially stalled
    segment of the frontal zone, where low-level convergence may
    eventually focus strongest thunderstorm development. Although wind
    fields in lower through mid-levels are rather weak, easterly
    near-surface flow veering to northerly near the eastward migrating
    frontal wave (beneath southerly mid-level flow) may contribute to
    sufficient shear for intensifying supercell structures posing a risk
    for severe hail and perhaps a brief tornado. Otherwise, storms,
    particularly those forming in the strongly heated pre-frontal
    environment, may pose a risk for locally strong to severe surface
    gusts.

    ..Kerr/Smith.. 07/29/2025

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!9RF9vKvQgg9g5gXCYrrxh0NzYz5DXcSlw5ZjneNHteZHBh4fFE_XSwwqqZ0isIVY-lQ1_wPwB= lKSvLvqRVxwqcA518M$ for graphic product...

    ATTN...WFO...GID...LBF...GLD...

    LAT...LON 41370111 41600024 41509902 40809880 40069930 40170045
    40220138 40670161 41370111=20

    MOST PROBABLE PEAK TORNADO INTENSITY...UP TO 95 MPH
    MOST PROBABLE PEAK WIND GUST...65-80 MPH
    MOST PROBABLE PEAK HAIL SIZE...1.50-2.50 IN


    =3D =3D =3D
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