• MESO: Mesoscale Discussion 0165

    From COD Weather Processor@1:2320/105 to wx-storm@lists.illinois.edu on Saturday, March 09, 2019 10:04:06
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    ACUS11 KWNS 090904
    SWOMCD
    SPC MCD 090903
    LAZ000-ARZ000-TXZ000-OKZ000-091100-

    Mesoscale Discussion 0165
    NWS Storm Prediction Center Norman OK
    0303 AM CST Sat Mar 09 2019

    Areas affected...portions of north Texas and adjacent southeast
    Oklahoma across the Arklatex

    Concerning...Severe potential...Watch likely

    Valid 090903Z - 091100Z

    Probability of Watch Issuance...80 percent

    SUMMARY...Risk for large hail -- eventually evolving to include
    potential for damaging winds and a tornado or two -- is expected to
    increase over the next few hours. WW issuance is expected.

    DISCUSSION...Latest radar imagery shows an increase in convective
    intensity east of the ABI/DYS area at this time, at the leading edge
    of increasing large-scale ascent ahead of the advancing/potent upper
    system.

    Downstream of the convective increase, the airmass remains slightly
    stable at low levels despite 60s dewpoints, but with steep lapse
    rates above 850 mb. As ascent continues to overspread this area, a
    increase in convective coverage/intensity is expected near and ahead
    of the Pacific front. Convective mode remains somewhat uncertain,
    though at this time it appears that a loose band of storms will
    evolve near the boundary initially, with some increase in potential
    for pre-frontal/more isolated storms to occur later this morning
    into the Arklatex region. In any case, deep-layer shear already
    supports mid-level rotation, with increasing flow aloft ahead of the
    advancing upper system enhancing the favorability of the kinematic
    environment with time.

    At this time, it appears that severe risk will remain primarily in
    the form of hail in the short term. However, even slight
    destabilization of the boundary layer would support increasing
    potential for surface-based convection, and an associated/
    corresponding increase of risk for damaging winds and a tornado or
    two. While this low-level destabilization would seem most likely to
    evolve after sunrise -- when some weak heating could contribute,
    enough destabilization due to moisture transport alone could support
    an increase in surface-based severe risk prior to sunrise --
    especially over eastern portions of the discussion area.

    ..Goss/Edwards.. 03/09/2019

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

    ATTN...WFO...LZK...SHV...TSA...FWD...OUN...

    LAT...LON 31789828 32159872 32839875 33479822 34239773 34899640
    35049528 34609352 34429271 32459259 31829357 31729621
    31789828



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