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From | To | Subject | Date/Time | |||
COD Weather Processor | wx-storm | MESO: Nws Weather Prediction Center College Park Md |
August 3, 2019 7:27 AM * |
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This is a multi-part message in MIME format... ------------=_1564817230-118394-4434 Content-Type: text/plain AWUS01 KWNH 030727 FFGMPD OKZ000-KSZ000-031200- Mesoscale Precipitation Discussion 0704 NWS Weather Prediction Center College Park MD 326 AM EDT Sat Aug 03 2019 Areas affected...North Central Oklahoma Concerning...Heavy rainfall...Flash flooding possible Valid 030725Z - 031200Z Summary...Thunderstorms may continue to affect north central Oklahoma during the early morning hours, producing locally heavy rainfall. Rain rates of 1 to 2 inches per hour, if sustained for a couple hours, may produce flash flooding. Discussion...Although backbuilding convection continues to be observed over north-central Oklahoma on IR satellite channels and regional radars, the convection has thus far remained relatively unfocused. This may be due to a lack of strong low-level convergence. Therefore, although backbuilding is occurring with the convection generally oriented parallel to the mean wind, individual convective clusters have generally avoided tracking over the same locations. And with a lack of strong low-level focus, rain rates have generally been peaking closer to 1 in/hr despite relatively strong elevated instability (2000+ j/kg MUCAPE) and high PW values (2+ inches). Convective intensity may also be hindered somewhat by a pocket of dry air situated near the OK-KS border, evident on the GOES-16 Simple Water Vapor RGB. Nevertheless, the mesoscale environment remains suited for continued upstream development of new convection for at least another few hours. The nose of a LLJ remains positioned close to the central portion of the OK-KS border, near PNC. This is close to the northern extent of convection as of 07Z. Additionally, there is an upstream shortwave, evident in GOES-16 water vapor imagery, over C KS. This digging wave would reach N OK around 12-14Z per an extrapolated motion, and convection would be likely to begin waning around that time due to increasing subsidence behind the wave and a climatologically less active time of the diurnal cycle for convection. Therefore, a window of several hours exists for continued backbuilding. Recent runs of the experimental Warn-on Forecast System show very low probabilities of 2 in/hr rain rates. Therefore, modest but still heavy rain rates around 1 in/hr would be more likely. This would be unlikely to lead to flash flooding on short durations of 60 minutes or less, but if backbuilding convection can be sustained in a corridor for several hours flash flooding will be possible. Localized rainfall totals could exceed 4 inches by 12Z. Lamers ...Please see www.wpc.ncep.noaa.gov for graphic product... ATTN...WFO...ICT...OUN...TSA... ATTN...RFC...ABRFC... LAT...LON 37409729 37209665 36689614 35659558 34899591 34919692 35509747 36379782 37059794 ------------=_1564817230-118394-4434 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. ------------=_1564817230-118394-4434-- --- SBBSecho 3.07-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (1:2320/105) |
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