####018002143#### ACUS03 KWNS 250725 SWODY3 SPC AC 250724 Day 3 Convective Outlook NWS Storm Prediction Center Norman OK 0224 AM CDT Mon Mar 25 2024 Valid 271200Z - 281200Z ...NO SEVERE THUNDERSTORM AREAS FORECAST... ...SUMMARY... Organized severe thunderstorms appear unlikely on Wednesday. ...Synopsis and Discussion... A large-scale upper trough, with split mid-level jets, will move slowly eastward across the central/eastern CONUS on Wednesday. Enhanced southwesterly flow aloft will persist over the Southeast, while a cold front stalls across the FL Panhandle, GA, and Carolinas. At least low to mid 60s surface dewpoints should be present along and southeast of the front. But, poor lapse rates and ongoing convection/cloudiness Wednesday morning are expected to hamper robust destabilization. While occasional gusty winds may occur with the strongest thunderstorms that can develop through the afternoon, the overall wind threat appears too limited at this time to include low severe probabilities. There are some indications in various model guidance that convection may develop Wednesday afternoon on the backside of the upper trough across parts of the southern Plains. Typically, this area would be in a subsident regime, with minimal convective potential owing to a lack of low-level moisture/boundary-layer instability. However, in this case, it appears that cold temperatures aloft combined with shallow/residual low-level moisture and daytime heating will provide modest destabilization as the boundary layer becomes well mixed. Weak instability should preclude an organized severe threat, but isolated strong/gusty winds appear possible with any high-based convection that develops. Finally, occasional lightning flashes may occur with low-topped thunderstorms across coastal portions of the Pacific Northwest. This potential should focus mainly in the afternoon and evening time frame, as cold mid-level temperatures and pronounced ascent associated with an approaching upper trough overspread this region. ..Gleason.. 03/25/2024 $$