• MESO: Mesoscale Discussion 1369

    From COD Weather Processor@1:2320/127 to wx-storm@lists.illinois.edu on Sun Jun 28 23:44:19 2026
    ACUS11 KWNS 282344
    SWOMCD
    SPC MCD 282343=20
    NDZ000-SDZ000-290145-

    Mesoscale Discussion 1369
    NWS Storm Prediction Center Norman OK
    0643 PM CDT Sun Jun 28 2026

    Areas affected...parts of northwestern North Dakota

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

    Valid 282343Z - 290145Z

    Probability of Watch Issuance...20 percent

    SUMMARY...Isolated to widely scattered strong thunderstorm
    development with potential to produce large hail and localized
    strong downbursts is possible into the 7-9 PM CDT time frame, before
    rapidly weakening.

    DISCUSSION...In the wake of one notable mid-level short wave trough,
    pivoting north-northwestward across Saskatchewan/Manitoba, around
    the northeastern periphery of an occluded cyclone centered over far southeastern Alberta, mid/upper support for convective development
    across the region is weak. Low-level flow is also weak within
    broad weak lingering surface troughing centered over the western
    Dakotas, but convergence has become strong enough in locations to
    contribute to the initiation of isolated thunderstorms.=20
    Boundary-layer destabilization has maximized, and mid-level
    inhibition associated with a plume of warm elevated mixed-layer air
    has been suppressed southeastward.

    Despite the weak low-level flow and shear, deep-layer shear beneath
    40-50 kt southwesterly 500 mb flow is strong and supportive of
    supercells with potential to produce large hail, as likely was the
    case with one initial storm which evolved across the international
    border to the east-northeast of Williston earlier. It is possible
    ongoing convection may persist and intensify further the next couple
    of hours, particularly the cell developing to the south-southwest of
    Bismarck, which appears likely to have the most prolonged access to
    updraft inflow of moist air characterized by CAPE on the order of
    3000 J/kg. However, with the onset diurnal cooling and increasing
    inhibition for boundary-layer parcels, weakening and dissipation of
    storms may be rapid.

    ..Kerr/Thompson.. 06/28/2026

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!8FGjcxIRbkajEK8WUMDi1bgOFm4jSr3Onkh9bIrs-CoIOBZ57Febs1TfpmFXtUfamL3uR7nTN= fdbeWDQPnISmhhgbl0$ for graphic product...

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

    LAT...LON 48920251 49060203 48849924 48479885 47669903 46460049
    45900148 46320191 47210140 47470187 48250278 48920251=20

    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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    * Origin: Capitol City Weather Station (1:2320/127)