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From | To | Subject | Date/Time | |||
COD Weather Processor | wx-storm | MESO: Nws Weather Prediction Center College Park Md |
July 29, 2019 5:30 PM * |
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This is a multi-part message in MIME format... ------------=_1564421441-118394-1792 Content-Type: text/plain AWUS01 KWNH 291730 FFGMPD TNZ000-MOZ000-ARZ000-OKZ000-292200- Mesoscale Precipitation Discussion 0686 NWS Weather Prediction Center College Park MD 129 PM EDT Mon Jul 29 2019 Areas affected...central/northern Arkansas...eastern Oklahoma...extreme southern Missouri Concerning...Heavy rainfall...Flash flooding possible Valid 291728Z - 292200Z Summary...Increasing convection is expected over the next few hours in a moist and unstable air mass ahead of a slow-moving cold front. Isolated areas of training convection could lead to localized 2-3 inch rainfall amounts. Flash flooding is possible. Discussion...A highly moist (PWs of 2.0-2.2 in) and moderately unstable (MLCAPEs of 1000-2000 J/kg) air mass is in place ahead of a slow-moving cold front. Latest visible satellite imagery along with radar data show new convection beginning to develop along the western Arkansas/Missouri border, likely aided by low-level convergence along a boundary left over from convection earlier this morning. The region lies within a broad area of low-level confluent flow as evident by RAP 850 hPa wind field. Relatively weak CINH which was in place earlier this morning is beginning to erode per latest SPC mesoanalysis, which should allow convection to increasingly tap into the highly moist air mass in place at the low-levels, as indicated by surface dew points in the mid-70s F across central Arkansas. Weak lapse rates should contribute to a relatively deep warm cloud layer and fairly efficient rainfall processes, which should be more fully utilized once convection can become surface-based. The HRRR seemed to have a reasonably good handle on ongoing convection from southeastern Oklahoma to northern Arkansas and southern Missouri. While the overall environment is not supportive of persistent or long-lived backward propagation, the latest HRRR does show some potential for at least brief periods of localized backward propagation and/or training. In any areas where this occurs, hourly rainfall amounts of 2-3 inches would be possible. These amounts could lead to instances of flash flooding. Relatively dry ground and high flash flood guidance values should keep the threat of flash flooding relatively isolated. Ryan ...Please see www.wpc.ncep.noaa.gov for graphic product... ATTN...WFO...LZK...MEG...PAH...SGF...SHV...TSA... ATTN...RFC...ABRFC...LMRFC... LAT...LON 36758995 36588962 36288965 35888987 35359027 34719126 33999295 33739402 33919475 34789513 35649539 36329520 36669481 36679434 36499385 36409309 36379250 36369198 36419117 36629052 ------------=_1564421441-118394-1792 Content-Type: text/plain; charset="US-ASCII" Content-Disposition: inline Content-Transfer-Encoding: 7BIT = = = To unsubscribe from WX-STORM and you already have a login, go to https://lists.illinois.edu and use the "Unsubscribe" link. Otherwise email Chris Novy at cnovy@cox.net and ask to be removed from WX-STORM. ------------=_1564421441-118394-1792-- --- SBBSecho 3.07-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105) |
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