• MESO: Mesoscale Discussion 1565

    From COD Weather Processor@1:2320/105 to [email protected] on Tue Jul 9 18:40:16 2024
    ACUS11 KWNS 091840
    SWOMCD
    SPC MCD 091839=20
    KYZ000-INZ000-TNZ000-ILZ000-092045-

    Mesoscale Discussion 1565
    NWS Storm Prediction Center Norman OK
    0139 PM CDT Tue Jul 09 2024

    Areas affected...western/central Kentucky and adjacent portions of
    southeastern Illinois/southern Indiana

    Concerning...Severe potential...Watch likely=20

    Valid 091839Z - 092045Z

    Probability of Watch Issuance...95 percent

    SUMMARY...Potential for supercells posing a risk for tornadoes
    appears likely to increase through 5-7 PM EDT, particularly near the
    Ohio River from Evansville/Owensboro through the Greater Louisville
    area.

    DISCUSSION...Beryl's remnant surface low is currently in the process
    of migrating east-northeastward across southeastern Missouri into
    the lower Ohio Valley, with a zone of strengthening differential
    surface heating becoming better defined near the Ohio River
    downstream toward the Greater Cincinnati area. South of this zone, boundary-layer destabilization is ongoing, supported by both
    insolation and slowly increasing moisture. The increasingly buoyant
    low-level environment is supporting the development of showers and
    isolated to widely scattered weak thunderstorms, but this is
    occurring beneath a notably warm and warming mid-level environment,
    which will tend to slow, if not suppress, intensifying convective
    development.

    Into the 21-23Z time frame, in the peaking boundary-layer
    instability, latest Rapid Refresh suggests that a relatively minimum
    in mid-level inhibition may linger near the Ohio River, roughly from
    Evansville IN/Owensboro Ky through the Greater Louisville area, near
    the nose of the stronger southerly flow around 850 mb associated
    with Beryl. Although this jet streak is forecast to weak some,
    speeds on the order of 30+ kt appear likely to still contribute to
    sizable clockwise-curved low-level hodographs, particularly along=20
    or just south of the differential heating zone.=20=20

    Given dynamic forcing associated with occasionally strengthening
    low-level mesocyclones, and the near-surface buoyancy associated
    with the high boundary-layer dew points (increasing to 75+ F),
    low-level upward accelerations may become increasingly conducive to
    tornadic potential in evolving supercell structures.

    ..Kerr/Guyer.. 07/09/2024

    ...Please see https://urldefense.com/v3/__http://www.spc.noaa.gov__;!!DZ3fj= g!4CqpeZEM-X9sNx65Za_HAyJc6ci0B87YUlPeAPqK9Lx0QCqWqlQv3aQfrL8vylSgmf_92GgF_= XBMCuVq8HgQgxPtdw8$ for graphic product...

    ATTN...WFO...ILN...LMK...OHX...IND...PAH...

    LAT...LON 37748853 38258783 38588668 38588480 37518524 36938580
    36488720 36598814 37748853=20


    =3D =3D =3D
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