AT2k Design BBS Message Area
Casually read the BBS message area using an easy to use interface. Messages are categorized exactly like they are on the BBS. You may post new messages or reply to existing messages! You are not logged in. Login here for full access privileges. |
Previous Message | Next Message | Back to General Weather-related Discussi... <-- <--- | Return to Home Page |
|
||||||
From | To | Subject | Date/Time | |||
Mike Powell | All | Heavy Rain/Flooding South |
May 23, 2024 7:56 AM * |
|||
AWUS01 KWNH 230901 FFGMPD LAZ000-ARZ000-TXZ000-OKZ000-231500- Mesoscale Precipitation Discussion 0306 NWS Weather Prediction Center College Park MD 500 AM EDT Thu May 23 2024 Areas affected...southeast OK into the Ark-La-Tex Concerning...Heavy rainfall...Flash flooding possible Valid 230900Z - 231500Z Summary...A compact MCS will produce heavy rainfall across recently soaked portions of southeast OK into the Ark-La-Tex, possibly resulting in isolated to scattered instances of flash flooding. Discussion...A cluster of thunderstorms that formed overnight in southern OK has gradually organized into a compact MCS over the past several hours, largely being missed by the recent 00z HREF suite. While hi-res CAMs entirely failed to initiate convection in a timely matter in this region, the mesoscale environment does appear favorable for continued MCS maintenance and growth into the early morning hours (which the 06z and 07z HRRR did finally pick up on after a run or two of the model that failed to properly assimilate the WSR-88d data). Looking downstream into the Ark-La-Tex region, SPC mesoscale analysis indicates PWATs of 1.5-1.8 inches (above the 90th percentile, per SHV sounding climatology), ML CAPE of 1000-1500 J/kg, and effective bulk shear of 40-50 kts. Additionally, the storms appear positioned near a quasi-stationary surface front with a diurnally strengthening 20-30 kt LLJ bringing ample low-level moisture transport. These meteorological factors and parameter space suggest high favorability for maintaining an MCS into the early morning hours (as indicated by an MCS maintenance parameter of 90-100). While the hi-res CAMs are not particularly useful in this case, the latest HRRR runs do provide a decent depiction of what is expected (though perhaps still a bit underdone in the overall coverage and intensity of heavy rainfall compared to observational trends). The expectation is for storms to become increasingly organized and cold pool dominate, which would favor a more southerly component to storm motion (following the upwind propagation vector towards the southeast, rather than the mostly easterly dominate motion thus far). Concerns for localized flash flooding are highest along the southern flank of the developing MCS, where 1-3"/hr rainfall rates may have their greatest residence time, resulting in localized totals of 2-4". Given that the bulk of the region has seen at least moderate to heavy rainfall over the past 6-12 hours (with localized totals of 2-4" from the prior storms as well), isolated to scattered instances of flash flooding are possible (with 3-hr FFGs still generally ranging from 2-4". Should the MCS make it all the way into northwest LA (and particularly into the Shreveport metro area) where FFGs are generally 2.5" or less, flash flooding may be locally significant. Churchill ATTN...WFO...FWD...LZK...OUN...SHV...TSA... ATTN...RFC...ABRFC...LMRFC...WGRFC...NWC... LAT...LON 35489564 35269400 34039241 32749265 32479418 33189612 33789729 34509652 35169627 = = = --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
||||||
|
Previous Message | Next Message | Back to General Weather-related Discussi... <-- <--- | Return to Home Page |
Execution Time: 0.0169 seconds If you experience any problems with this website or need help, contact the webmaster. VADV-PHP Copyright © 2002-2024 Steve Winn, Aspect Technologies. All Rights Reserved. Virtual Advanced Copyright © 1995-1997 Roland De Graaf. |