• MESO: Mesoscale Discussion 1530

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Saturday, October 06, 2018 17:40:32
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    ACUS11 KWNS 061740
    SWOMCD
    SPC MCD 061739
    INZ000-ILZ000-MOZ000-061945-

    Mesoscale Discussion 1530
    NWS Storm Prediction Center Norman OK
    1239 PM CDT Sat Oct 06 2018

    Areas affected...eastern Missouri...central Illinois...and
    northern/central Indiana

    Concerning...Severe potential...Watch possible

    Valid 061739Z - 061945Z

    Probability of Watch Issuance...40 percent

    SUMMARY...An increasingly unstable and weakly capped environment
    will favor thunderstorms this afternoon. Ongoing thunderstorms
    should slowly intensify through the afternoon as they move
    east-northeast. Strong/gusty winds appear to be the primary hazard.

    DISCUSSION...Showers and thunderstorms continue along and north of a southeastward moving cold front. Additional thunderstorms have
    developed and will continue to develop to the east of the cold front
    (across east-central Illinois and northern Indiana) along a weak,
    pre-frontal trough.

    Ahead of the surface cold front, broken cloud cover will allow for
    temperatures to warm into the mid-80s amidst surface dewpoints in
    the upper-60s to low-70s. The result will be an increasingly
    unstable and weakly capped environment. As the cold front moves into
    the area, convergence along the front should allow for continued
    thunderstorm development. Although low-level flow is weak, strong mid-upper-level flow should be sufficient to maintain continued
    thunderstorm development with the surface front convergence.

    Despite a cold front moving into an increasingly unstable and weakly
    capped environment, there are several limiting factors to a more
    robust severe threat. Seasonably warm mid-level temperatures have
    resulted in weak mid-level lapse rates, which, in turn, will limit
    the overall hail threat. Additionally, deep-layer flow is mostly
    parallel to slightly front-to-back across the frontal boundary. This
    will promote thunderstorms developing along the front being quickly
    undercut by the advancing cold front. This should keep thunderstorms
    elevated for most of their lifetime. However, given the strength of
    the deep-layer flow, an isolated strong/gusty wind report or two may
    remain possible, especially with convection along/near the front.

    ..Marsh/Guyer.. 10/06/2018

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

    ATTN...WFO...IWX...IND...PAH...LOT...ILX...LSX...SGF...

    LAT...LON 37549181 38229159 38979021 40298816 41588585 40648534
    38988729 37538982 37549181



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