• MESO: Mesoscale Discussion 1890

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Tue Aug 5 19:41:16 2025
    ACUS11 KWNS 051941
    SWOMCD
    SPC MCD 051940=20
    NDZ000-SDZ000-052145-

    Mesoscale Discussion 1890
    NWS Storm Prediction Center Norman OK
    0240 PM CDT Tue Aug 05 2025

    Areas affected...south central North Dakota and adjacent north
    central South Dakota

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

    Valid 051940Z - 052145Z

    Probability of Watch Issuance...60 percent

    SUMMARY...Intensifying thunderstorm activity, perhaps including the
    evolution of a sustained supercell appears probable by 5-7 PM CDT,
    if not earlier, before transitioning to an organizing, southeastward propagating cluster into this evening. A severe weather watch will
    likely be needed, but timing remains uncertain.

    DISCUSSION...In the wake of a generally dissipating cluster of
    thunderstorms spreading into the Red River Valley,
    lower/mid-tropospheric warm advection is being maintained across
    much of the Dakotas, on the northern periphery of a plume of warm
    and capping elevated mixed-layer air. This includes temperatures as
    warm as +10 to +12 C around 700 mb, as far northeast as southwestern
    North Dakota through north central and northeastern South Dakota,
    beneath which stronger boundary-layer warming and destabilization is
    ongoing.

    Around and north through east of the Bismarck ND vicinity, the
    boundary-layer has been slower to modify in the wake of the
    preceding convection, but forcing for ascent has been sufficient to
    overcome inhibition and support renewed thunderstorm development.=20
    This has been gradually increasing near the nose of a 30 kt
    southerly low-level jet, which may strengthen a bit further into
    early evening. Northward advection of warmer and more moist
    boundary-layer air along this axis is likely to contribute to
    substantive further boundary-layer destabilization, and, at some
    point, a rapid intensification of thunderstorm activity.=20=20

    Once this occurs, in the presence of strong deep-layer shear beneath
    30-40 kt westerly 500 mb flow, the environment appears conducive to
    the evolution of a significant supercell with potential to produce
    large hail and perhaps a couple of tornadoes, before growing growing
    upscale into an organizing southeastward propagating cluster by this
    evening.

    ..Kerr/Smith.. 08/05/2025

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!_DHNJX68vJ4MqxkRVkXs6WMv66wl0uCq5NmR3kftNlCulzeeddR8nEZzYt0byh1r5AT4ke-w7= YNMr6lBU52lalchInw$ for graphic product...

    ATTN...WFO...FGF...ABR...BIS...UNR...

    LAT...LON 46380187 47080062 46989902 46439791 45929837 45549908
    45379992 45600092 45870202 46380187=20

    MOST PROBABLE PEAK TORNADO INTENSITY...85-115 MPH
    MOST PROBABLE PEAK WIND GUST...55-70 MPH
    MOST PROBABLE PEAK HAIL SIZE...1.50-2.50 IN


    =3D =3D =3D
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