• MESO: Mesoscale Discussion 0197

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Wednesday, March 13, 2019 23:52:38
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    ACUS11 KWNS 132252
    SWOMCD
    SPC MCD 132251
    TNZ000-MOZ000-ARZ000-MSZ000-LAZ000-140045-

    Mesoscale Discussion 0197
    NWS Storm Prediction Center Norman OK
    0551 PM CDT Wed Mar 13 2019

    Areas affected...Parts of northern Louisiana...eastern
    Arkansas...northwestern Mississippi...and western Tennessee...into
    the Missouri Bootheel

    Concerning...Severe potential...Watch possible

    Valid 132251Z - 140045Z

    Probability of Watch Issuance...40 percent

    SUMMARY...An evolving line of intensifying thunderstorms is possible
    near the Mississippi River through the 9-10 PM CDT time frame, in an environment conducive to the generation of potentially damaging wind
    gusts and perhaps a few tornadoes.

    DISCUSSION...A remnant, convectively reinforced surface front
    continues to advance very slowly eastward toward the Mississippi
    River, largely parallel to 50-60 kt deep layer ambient flow now
    present across much of the mid and lower Mississippi Valley. This
    front has generally cut-off the northward transport of richer
    boundary layer moisture, associated with a continuing return flow
    off the western Gulf of Mexico; but, mid 60s F surface dew points
    are still present in narrow corridor as far north as the
    Mississippi Delta region, with a narrowing plume of lower 60s
    extending northward toward the Missouri Bootheel.

    Model output, including the latest Rapid Refresh and HRRR, is
    suggestive that, as stronger mid-level height falls continue
    overspreading the region, cooling aloft will support further
    destabilization and potential for intensifying thunderstorm
    development along the boundary within the next hour or two. The
    evolution of a narrow squall line appears possible through 02-03Z.

    This may coincide with further strengthening of southerly low-level
    flow, including to in excess of 70 kt around 850 mb. Given the
    strong to extreme nature of the low-level wind fields and shear, the environment likely will be conducive to at least the risk for a few
    strong, damaging wind gusts. Due to the uncertain character of near
    surface thermodynamic profiles, tornadic potential is a little more
    unclear. However, low-level hodographs are supportive of potential
    for a strong tornado, particularly with any discrete storm
    development just ahead of, or within the line.

    ..Kerr/Hart.. 03/13/2019

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

    ATTN...WFO...MEG...JAN...LZK...SHV...

    LAT...LON 35579087 36429029 36308931 34998988 33609054 32699140
    32469218 33679162 35579087



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