• MESO: Mesoscale Discussion 1142

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Monday, July 23, 2018 07:32:30
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    ACUS11 KWNS 230732
    SWOMCD
    SPC MCD 230731
    FLZ000-231000-

    Mesoscale Discussion 1142
    NWS Storm Prediction Center Norman OK
    0231 AM CDT Mon Jul 23 2018

    Areas affected...portions of near-coastal west-central/northwestern
    FL

    Concerning...Severe potential...Watch unlikely

    Valid 230731Z - 231000Z

    Probability of Watch Issuance...5 percent

    SUMMARY...Isolated gusts near severe limits may occur over the
    discussion area from the eastern edge of a complex of thunderstorms
    initially over the Gulf. Magnitude and coverage of severe threat
    appear too low for a watch.

    DISCUSSION...A loosely organized, bowing MCS that developed over the
    FL Panhandle is moving southeastward to south-southeastward about 30
    kt across waters west of coastal Citrus/Hernando/Pasco Counties as
    of 715Z. The eastern portion of this complex will straddle an
    outflow boundary from an older, decayed MCS. The older boundary was
    analyzed from between VRB-SUA across northern Lake Okeechobee to
    near PGD, just east and north of VNC, near SRQ, and roughly 10-15 NM
    offshore Pinellas County. That portion of this boundary near the
    Gulf coast has stalled, and may be retreating slowly eastward toward
    areas between SRQ-PIE. Northeast of the boundary, relatively
    cool/stable outflow air will reduce the potential for damaging gusts
    to reach the surface, with eastward extent. Within and west of its
    narrow, mesobeta-scale baroclinic zone, the air mass is richly
    moist, unstable, and weakly convergent, acting as a potential focus
    for maintenance of the eastern part of the newer MCS as the latter
    obliquely approaches the coast. Modified RAOBs and RAP soundings
    suggest dew points mid-70s to 80 F and seasonably steep
    low/middle-level lapse rates supporting MLCAPE 2000-3000 J/kg along
    and southwest of the boundary, within minimal CINH, while CINH
    increases to its northeast and inland.

    Northwesterly 35-45-kt effective-shear vectors also are evident over
    the TBW region and northwestward, and forced ascent related to
    cold-pool processes may maintain the MCS longer than progged by
    CAMs. However, both deep shear and low-level lift decrease markedly
    with southward extent toward FMY, away from the boundary and from
    the stronger winds aloft. As such, the most probable area of the
    coastline to be affected by marginal severe-wind potential the next
    few hours is over the discussion area.

    ..Edwards/Peters.. 07/23/2018

    ...Please see www.spc.noaa.gov for graphic product...

    ATTN...WFO...TBW...

    LAT...LON 28818267 28668249 28418239 28018225 27598237 26968238
    27608280 27858283 28248279 28648265 28738266 28818267



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