• MESO: Mesoscale Discussion 0511

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Thu Apr 25 08:30:37 2024
    ACUS11 KWNS 250830
    SWOMCD
    SPC MCD 250829=20
    OKZ000-KSZ000-NEZ000-251200-

    Mesoscale Discussion 0511
    NWS Storm Prediction Center Norman OK
    0329 AM CDT Thu Apr 25 2024

    Areas affected...parts of south central Nebraska through eastern
    Kansas and adjacent northeastern Oklahoma

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

    Valid 250829Z - 251200Z

    Probability of Watch Issuance...20 percent

    SUMMARY...Developing thunderstorm activity may occasionally
    intensify with at least some increase in potential to produce severe
    hail through 6-8 AM CDT. While it still appears unlikely that this
    will require a severe weather watch, trends will be monitored for
    this possibility.

    DISCUSSION...Scattered thunderstorm development is well underway in
    response to lift and destabilization associated with elevated
    moisture return within bands of strengthening
    lower/mid-tropospheric warm advection across the central Great
    Plains. This is initially focused in corridors across parts of
    western Nebraska into northwestern Kansas, and across eastern Kansas
    into northeastern Oklahoma, where initial moistening and
    destabilization has been weak. However, more substantive moistening
    within the 850-700 mb layer is ongoing across much of western and
    central Kansas through eastern Oklahoma, beneath increasingly warm
    elevated mixed-layer air advecting east of the southern Rockies.

    Into the 11-13Z time frame, the latest Rapid Refresh suggests that
    the better low-level moistening may begin to increasingly underrun
    the sharpening eastern periphery of the stronger mid-level
    inhibition in a corridor roughly from Kearney/Hastings NE through
    the Emporia and Chanute KS vicinities. Based on forecast soundings,
    it appears that this may lead to most unstable CAPE increasing in
    excess of 1000 J/kg, in the presence of sufficient cloud-bearing
    layer shear (beneath 30-50 kt westerly flow in the 500-300 mb layer)
    for persistent supercell structures capable of producing severe
    hail.

    ..Kerr/Thompson.. 04/25/2024

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!5aJpFQ-Wi0UDDEHt6WS5AaQc-ScnyfqlnmAZVQRbfFSbY7THiKUG8wCiaIrmIhS6sCEx6rKc8= SQYf9wohsFZZOqE6pQ$ for graphic product...

    ATTN...WFO...SGF...TSA...OAX...TOP...ICT...GID...

    LAT...LON 40209749 38379542 37259470 36689491 36409563 36569624
    38729754 40149974 40209749=20


    =3D =3D =3D
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