Severe Storm Outlook Narrative (AC)
Issued by NWS
Issued by NWS
388 ACUS03 KWNS 260728 SWODY3 SPC AC 260726 Day 3 Convective Outlook NWS Storm Prediction Center Norman OK 0226 AM CDT Sun Jul 26 2026 Valid 281200Z - 291200Z ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS FROM THE SOUTHERN MID-ATLANTIC INTO THE CAROLINAS AND CENTRAL AND SOUTHERN APPALACHIANS... ...SUMMARY... Severe thunderstorms capable of mainly damaging winds appear possible from the southern Mid-Atlantic into the Carolinas and central and southern Appalachians Tuesday into Tuesday evening. Isolated severe wind gusts may occur in the central High Plains. ...Synopsis... A short-wave trough initially over the lower Great Lakes Tuesday morning is forecast to evolve into a closed low over the Mid-Atlantic. Within the base of that feature, a belt of enhanced mid-level flow will spread from the OH Valley into VA and NC by afternoon. At the surface, an area of low pressure over southwest ON Tuesday morning is expected to reform in the Delmarva by afternoon with a lee trough extending southwest along the Piedmont. Meanwhile, a cold front will advance southeast through the central and southern Appalachians, the southern Mid-Atlantic into the Carolinas. ...Mid-Atlantic into Southern Appalachians... Showers and thunderstorms (some potentially strong) are expected to be ongoing Tuesday morning from the upper OH Valley into the Mid-Atlantic and central Appalachians within a zone of forcing for ascent preceding the short-wave trough. Various 00Z model data indicate deep convection lingering into afternoon from the central Appalachians into the Delmarva and points north, leading to uncertainty in the degree of air mass destabilization in those areas. Where stronger heating can occur, the presence of a moist air mass will contribute to moderate instability by afternoon within a kinematic environment featuring anywhere from 30 to 45 kt of deep-layer shear. Thunderstorms are expected to increase in coverage and intensity during the afternoon preferentially along the cold front and lee trough where sufficient destabilization has occurred. Organized storm modes appear possible, including supercells and bowing structures, with the primary hazards being damaging wind gusts. Some tornado threat could materialize Tuesday afternoon in the Delmarva near the surface low. That threat is conditional on sufficient air mass destabilization and the presence of a supercell mode. ...Northern and Central High Plains... Between a deepening lee trough over the northern High Plains and a stalled surface front along the KS-OK border, a zone of moist and moderately unstable upslope flow is forecast. Thunderstorms are expected to develop during the afternoon and evening along favored terrain with 30-35 kt of deep-layer shear supporting some level of organization. Severe wind gusts appear to be the primary hazard with the strongest storms. ..Mead.. 07/26/2026 $$