• MESO: Mesoscale Discussion 1158

    From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Tuesday, June 16, 2026 22:26:13
    ACUS11 KWNS 162226
    SWOMCD
    SPC MCD 162225=20
    NDZ000-MTZ000-170030-

    Mesoscale Discussion 1158
    NWS Storm Prediction Center Norman OK
    0525 PM CDT Tue Jun 16 2026

    Areas affected...northern into northeast MT and northwest ND

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

    Valid 162225Z - 170030Z

    Probability of Watch Issuance...20 percent

    SUMMARY...The risk for isolated severe gusts and perhaps marginally
    severe hail will develop as storms intensify during the next few
    hours.

    DISCUSSION...Widely scattered thunderstorms are developing ahead of
    an amplifying upper trough over southern Alberta. GOES and
    model-based upper flow fields show very strong westerly flow with
    80+ kt flow at 8 km AGL per the Glasgow, MT WSR-88D VAD. Although
    low-level moisture is modest (surface dewpoints ranging from 45-50
    deg F), steepened 0-3 km lapse rates and cool mid levels are
    supporting upwards of 500-1000 J/kg SBCAPE. Very long hodographs
    will support storm organization mainly in the form of a couple of
    supercells early during the convective life cycle before more storms
    and coalescing cold pools promotes more of a multicell mode. The
    greater risk for severe hail will accompany the supercells before
    the risk for severe gusts also begins to increase owing to higher
    storm coverage.

    ..Smith/Gleason.. 06/16/2026

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!89TC0c_tyxdtScwveM45SD50NnI7nM1ZFd-B-SLGOvgJy_TruTuXEyNr2QHLepEbn27VKAKmx= atkrbdM9TcIk6JMXWc$ for graphic product...

    ATTN...WFO...BIS...GGW...TFX...

    LAT...LON 48780942 48970824 48960393 48750161 48360088 47780094
    47310121 47200232 47450518 47960798 48260907 48490943
    48780942=20

    MOST PROBABLE PEAK WIND GUST...55-70 MPH
    MOST PROBABLE PEAK HAIL SIZE...UP TO 1.25 IN


    =3D =3D =3D
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