• MESO: Mesoscale Discussion 2026

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Aug 29 02:42:08 2024
    ACUS11 KWNS 290242
    SWOMCD
    SPC MCD 290241=20
    NDZ000-SDZ000-290445-

    Mesoscale Discussion 2026
    NWS Storm Prediction Center Norman OK
    0941 PM CDT Wed Aug 28 2024

    Areas affected...parts of north central South Dakota and south
    central North Dakota

    Concerning...Tornado Watch 661...

    Valid 290241Z - 290445Z

    The severe weather threat for Tornado Watch 661 continues.

    SUMMARY...Thunderstorm development, in general, is beginning to
    weaken, with the risk for tornadoes likely to become increasingly
    negligible through 10-11 PM CDT. Some risk for severe hail and,
    perhaps, localized strong wind gusts may persist into the overnight
    hours across parts of the central and eastern Dakotas. However, a
    new severe weather watch is not currently anticipated.

    DISCUSSION...Ongoing convection appears to be undergoing notable
    weakening trends, including the the isolated supercell just south of
    the state border vicinity, across eastern Campbell county South
    Dakota. This has occurred as the loss of daytime heating has
    resulted in increasing inhibition for the seasonably moist boundary
    parcels near the surface trough across the central Dakotas.=20
    However, forcing associated with strong low-level warm advection may
    maintain at least a severe hail threat with the Campbell county
    storm as it accelerates north-northeastward, and becomes
    increasingly rooted above the boundary layer during the next hour or
    two.

    Strongest potential instability remains focused near a weak surface
    low, centered within the surface trough to the north-northwest of
    Pierre SD. However, as the slow moving upstream low, now centered
    over southern Saskatchewan just to the north of the international
    border, continues east-northeastward, models suggest that warming
    elevated mixed-layer air will gradually advect across the central
    North and South Dakota state border area through 04-05Z. As this
    occurs, the potential for renewed thunderstorm development rooted
    within the unstable boundary layer is expected to diminish.

    ..Kerr.. 08/29/2024

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!9d3uAkroYGINVxLFxYuAClOKz3AjXfETFzL_rztY1v6Vuy3dDB93Vex-pedCrZAySOAH1e6Gc= M9XmJrbCrQHSMKlLwQ$ for graphic product...

    ATTN...WFO...ABR...BIS...

    LAT...LON 45960044 47149937 46599839 45019952 45030058 45960044=20


    =3D =3D =3D
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