• MESO: Mesoscale Discussion 0313

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sat Mar 30 20:27:37 2024
    ACUS11 KWNS 302027
    SWOMCD
    SPC MCD 302027=20
    WVZ000-OHZ000-KYZ000-INZ000-302300-

    Mesoscale Discussion 0313
    NWS Storm Prediction Center Norman OK
    0327 PM CDT Sat Mar 30 2024

    Areas affected...Far East-Central IN into Central/Southern OH

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

    Valid 302027Z - 302300Z

    Probability of Watch Issuance...60 percent

    SUMMARY...Strong to severe thunderstorms capable of hail (1" to
    1.75") and/or damaging gusts (from 40 to 60 mph) are possible this
    afternoon and evening.

    DISCUSSION...Latest surface analysis places a low over north-central
    OH (about 30 miles east-northeast of FDY). A warm front extends east-southeastward from this low across southeast OH into far
    northern WV. A modest surface trough also extends southwestward from
    this low across central IN and central IL. Filtered heating in the
    wake of the early morning cloud cover has allowed temperatures to
    climb into the upper 60s/low 70s within the warm sector
    south/southwest of the warm front and to the east of the surface
    troughing. Low-level moisture remains modest, with dewpoints in the
    upper 40s/low 50s. Even though the low-level thermodynamic
    conditions are relatively modest, these conditions combined cold
    mid-level temperatures (i.e. around -20 deg C at 500 mb) and
    associated steep mid-level lapse rates are contributing to air mass destabilization.

    This destabilization is verified by increasingly agitated cumulus
    just ahead of the surface trough over far east-central IN and far
    western OH. Given the veered low-level flow, convergence along the
    boundary is limited. However, ascent along the boundary will be
    augmented by large-scale ascent attendant to a fast-moving shortwave
    embedded within the strong westerly flow aloft. This combination of
    ascent and destabilization will likely result in convective
    initiation. Buoyancy will be modest, but deep-layer vertical shear
    will be strong. Recent mesoanalysis estimates 50 to 60 kt of 0-6 km
    bulk shear across the region. As such, any deeper updrafts could
    become organized, capable of producing large hail (1" to 1.75")
    and/or damaging wind gusts (40 to 60 mph this afternoon and evening.

    ..Mosier/Thompson.. 03/30/2024

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!7Qg_M7lCWzOTdvc2tgtoOLyGzdk-6gne_LhxjprEFlEzEwc9F_hrp8avvtoO4ulAtMWVdrvii= DYug0g8NlMd7hwv1wI$ for graphic product...

    ATTN...WFO...PBZ...RLX...CLE...ILN...IWX...IND...

    LAT...LON 40828361 40618083 39268057 38738137 38618264 38898430
    40018520 40828361=20


    =3D =3D =3D
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