• MESO: Mesoscale Discussion 0850

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Sunday, June 24, 2018 06:25:25
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    ACUS11 KWNS 240625
    SWOMCD
    SPC MCD 240625
    OKZ000-KSZ000-TXZ000-240800-

    Mesoscale Discussion 0850
    NWS Storm Prediction Center Norman OK
    0125 AM CDT Sun Jun 24 2018

    Areas affected...Southern Kansas and central/northern Oklahoma

    Concerning...Severe Thunderstorm Watch 209...

    Valid 240625Z - 240800Z

    The severe weather threat for Severe Thunderstorm Watch 209
    continues.

    SUMMARY...Severe thunderstorms capable of strong, damaging winds
    continue to move east-southeast across portions of southwest Kansas
    and are now beginning to impact northwest Oklahoma. These
    thunderstorms will continue through the morning hours posing a
    continued threat of strong winds and some hail.

    DISCUSSION...Well organized mesoscale convective system (MCS)
    continues to move east-southeast across southwest Kansas. The
    leading edge of the MCS is characterized by a bow echo that has
    produced measured wind gusts in excess of 60 knots within the past
    few hours. This MCS appears to move moving along the north side of a
    strong 850 theta-e gradient, which loosely coincides with the
    most-unstable CAPE gradient.

    In the near-term, expectation is that this MCS will continue along
    the 850 millibar theta-e gradient. This would take the MCS across
    north-central Oklahoma and far southern south-central Kansas. Given
    the organization of the MCS and an environment characterized by
    most-unstable CAPE values of 1500-2500 J/kg within the CAPE
    reservoir to the south and deep layer shear of 35-50 knots, severe
    thunderstorm winds and possibly some hail will remain possible
    through the morning hours. A local extension of WW208 or possibly a
    new WW across portions of northeast Oklahoma may be necessary later
    this morning and the evolution of the ongoing MCS will be monitored
    for this need.

    One potential hindrance to the longevity of the MCS (and in turn WW
    issuance needs) is the ongoing convection across central and eastern
    Oklahoma that is moving north into northeast Oklahoma. As this
    convection moves into northeast Oklahoma, it could exhaust some of
    the higher octane airmass across central Oklahoma. This would induce
    a weakening trend within the aforementioned MCS as it moves into and
    through Oklahoma.

    ..Marsh/Guyer.. 06/24/2018

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

    ATTN...WFO...TSA...ICT...OUN...DDC...AMA...

    LAT...LON 35029783 35769948 36750116 37179956 37989922 36689635
    36229563 35299579 34819644 35029783



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