• Heavy Rain/Flood KS/OK/AR

    From Dumas Walker@21:1/175 to All on Sat Aug 17 08:38:00 2024
    AWUS01 KWNH 171135
    FFGMPD
    MOZ000-ARZ000-TXZ000-OKZ000-KSZ000-171630-

    Mesoscale Precipitation Discussion 0890
    NWS Weather Prediction Center College Park MD
    734 AM EDT Sat Aug 17 2024

    Areas affected...far southeast KS, eastern OK, western AR

    Concerning...Heavy rainfall...Flash flooding possible

    Valid 171134Z - 171630Z

    Summary...A persistent MCS with training showers and thunderstorms
    will persist for a few more hours this morning. Rainfall rates of
    1-2"/hr will gradually weaken, but an additional 1-3" of rain is
    possible which could result in instances of flash flooding.

    Discussion...The regional radar mosaic depicts a persistent MCS
    aligned near the OK/AR border and extending back into far
    southeast KS this morning. This MCS is being driven by a weak
    mid-level impulse interacting with a decaying front, now analyzed
    as a trough by WPC. A modest outflow boundary from earlier
    convection continues to align to the south, into which still
    robust 850mb inflow measured by regional VWPs to be 25-35 kts is
    converging. The overlap of this residual boundary and the nose of
    this LLJ is fueling regenerating convection within a region of
    elevated PWs above 1.75 inches combined with MUCAPE that, while
    waning, is still analyzed by the SPC RAP to be around 1000 J/kg.
    Recent radar-estimated rainfall rates from KSRX have been as high
    as 1.5"/hr, and 6-hr rainfall from MRMS across this region has
    been generally 2-4" leading to saturated soils and ongoing FFWs.

    This MCS should gradually begin to decay in the next few hours,
    although the recent HRRR and 3kmNAM may be too quick to erode
    convection. Leaning more on the ARW/ARW2 output, it is likely this
    MCS will gradually ease as the focus of convection drifts W/SW in
    response to the veering and weakening of the 850mb LLJ. Even as
    the LLJ veers, it will still originate from a ribbon of higher
    MUCAPE and a bubble of warmer temperatures, suggesting continued
    WAA isentropically ascending into the MCS through late morning.
    Some evidence of this is already occurring as noted by fresh
    convection bubbling west of the MCS across eastern OK. So even
    though lightning cast probabilities are slowly falling, the
    ingredients suggest there will be plentiful ascent and instability
    to persist this MCS for several more hours, which is again
    supported by the ARWs. This will drive rainfall rates of 1-2"/hr
    at times for a few more hours, which will likely train to the
    south as propagation vectors align to the convergent nose of this
    LLJ.

    Where the most impressive training occurs, total rainfall could
    reach as much as 3", although generally should be more widespread
    of 1-2". This could cause instances of flash flooding despite HREF
    FFG exceedance probabilities being modest, especially where heavy
    rain rates move across urban areas, or atop soils pre-conditioned
    from overnight rainfall.

    Weiss


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

    ATTN...RFC...ABRFC...LMRFC...NWC...

    LAT...LON 37549569 36929447 35769350 34689343 33819412
    33879543 34219600 34649615 36439600 37369599

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