• MESO: Mesoscale Discussion 0367

    From COD Weather Processor@1:2320/107 to wx-storm@lists.illinois.edu on Thursday, April 09, 2026 18:40:17
    ACUS11 KWNS 091840
    SWOMCD
    SPC MCD 091839=20
    KSZ000-NEZ000-092115-

    Mesoscale Discussion 0367
    NWS Storm Prediction Center Norman OK
    0139 PM CDT Thu Apr 09 2026

    Areas affected...north central into northeastern Kansas and adjacent
    portions of southern Nebraska

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

    Valid 091839Z - 092115Z

    Probability of Watch Issuance...60 percent

    SUMMARY...Intensifying thunderstorm development accompanied by at
    least increasing risk for large hail appears possible as early as
    3-5 PM CDT. Trends are being monitored for a severe weather watch,
    which probably will be needed at some point, but timing remains a
    bit uncertain.

    DISCUSSION...To the south of a stalled surface frontal zone near the Kansas/Nebraska border vicinity into northern Missouri, forcing for
    ascent associated with lower/mid-tropospheric warm advection is
    maintaining scattered weak elevated or high based thunderstorm
    development. However, breaks in cloud cover are allowing for
    sufficient insolation to contribute to destabilization, in the
    presence of a still rather modestly moist, but slowly moistening, boundary-layer.

    Beneath a plume of warm elevated mixed-layer air advecting across
    the high plains, stronger heating and deep boundary-layer mixing is
    ongoing across western into central Kansas. Through mid to late
    afternoon, it appears that a dryline may become better defined in
    the vicinity of its intersection with the front, near Concordia KS, south-southwestward.

    As this occurs, it appears that strengthening low-level warm
    advection will become focused near the nose of a persistent 30+ kt
    southerly 850 mb jet, across and northeast of the surface
    front/dryline intersection into southern Nebraska between Hastings
    and Beatrice. Coinciding with destabilization including
    mixed-layer/most unstable CAPE increasing to 1000-1500 J/kg, it
    appears that this will support the initiation of intensifying
    thunderstorm development.

    Based on latest model output, how far to the cool side side of the
    surface front/dryline intersection and how soon remain a bit
    unclear. However, it appears possible as early as the 20-22Z time
    frame, in the presence of sufficiently strong deep-layer shear to
    support supercell structures capable of producing large hail. For
    any storm development rooted closer to the surface near the boundary intersection, the potential for strong surface gusts and perhaps a
    brief tornado or two would be more appreciable.

    ..Kerr/Gleason.. 04/09/2026

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!77OWidEEduR8bdkk2s4az3TT8PUa6u62ALc7JGJuc2lVKqMnrllMb2dCb6VkrUTVaEzrNkY0A= i93S-8Bmk7k4bjUG2A$ for graphic product...

    ATTN...WFO...EAX...OAX...TOP...ICT...GID...DDC...

    LAT...LON 40339864 40709707 40079587 39529537 38989683 38859917
    40339864=20

    MOST PROBABLE PEAK TORNADO INTENSITY...UP TO 95 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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