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From | To | Subject | Date/Time | |||
Mike Powell | All | Heavy Rain/Flood KS/OK/AR |
August 17, 2024 9:35 AM * |
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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 --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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