ACUS03 KWNS 050641 SWODY3 SPC AC 050640 Day 3 Convective Outlook NWS Storm Prediction Center Norman OK 0140 AM CDT Tue May 05 2026 Valid 071200Z - 081200Z ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS ACROSS THE CENTRAL GULF COAST TO SOUTH CAROLINA... ...SUMMARY... Isolated strong to severe thunderstorms are possible on Thursday across portions of the central Gulf coast into South Carolina. ...Gulf coast to SC... A large upper trough will pivot over the eastern U.S. on Thursday. Strong west/southwesterly deep-layer flow will be in place across the Southeast into the Mid-Atlantic. At the surface, a cold front will develop south/southeast across portions of south TX, the central Gulf coast states and the Southeast/Mid-Atlantic vicinity. A seasonally moist airmass will be in place ahead of the boundary, and some risk for strong to severe storms will exist near the progressing cold front from southern MS/AL into SC. There is some uncertainty regarding the position of the cold front Thursday morning. The NAM is faster compared to the GFS and ECMWF. Nevertheless, rich Gulf moisture ahead of the boundary will support at least modest destabilization. Convection will likely be ongoing near the front Thursday morning. Redevelopment or intensification into midday and through the afternoon appears plausible given strong deep-layer flow within the modestly unstable airmass. Clusters and linear convection appear most likely, with an attendant risk of damaging wind. ...South TX... Severe potential across south TX is uncertain and will depend on cold frontal position Thursday morning. If southward progress of the front is slowly, some risk of severe could develop across south TX where 70s dewpoints and daytime heating could support strong instability. If storms develop, a risk for hail appears possible. However, some forecast guidance surges the cold front southward across the region during the morning and maintains capping through the day. Low confidence precludes severe probabilities at this time. ..Leitman.. 05/05/2026 $$