


Severe Storm Outlook Narrative (AC)
Issued by NWS
Issued by NWS
655 ACUS03 KWNS 030728 SWODY3 SPC AC 030727 Day 3 Convective Outlook NWS Storm Prediction Center Norman OK 0227 AM CDT Wed Sep 03 2025 Valid 051200Z - 061200Z ...NO SEVERE THUNDERSTORM AREAS FORECAST... ...SUMMARY... Thunderstorms will be possible across much of the West, the southern Rockies, Florida, and along and near a frontal boundary from New England into the southern Plains. Widespread organized severe weather is not anticipated. ... Discussion ... The amplified midlevel pattern of the previous few days will persist through Friday/Day-3 across North America, with a western Canada ridge and a continental-scale trough across eastern Canada and the eastern US. Within the eastern trough, a seasonably strong closed low over Ontario should begin to fill by late in the forecast period. As this is occurring, multiple shortwave troughs traversing the larger scale flow field will rotate around the Ontario low. The strongest of these shortwave troughs will have moved south through Canada the day before and should be located in the vicinity of the Lower Great Lakes at the start of the forecast period. In response to this shortwave trough, strong northerly low-to-mid-level flow across the Plains overnight Thursday into Friday will help tighten the low-level thermal gradient across the Plains. This front will slowly move south through Friday into Friday night. A modest surface low is expected to develop across southwest Oklahoma or northwest Texas, along the surface front, by Friday morning. This surface low should slowly sag south through the day with the front. Despite moving south, away from Oklahoma, the flow around this surface low will still be able to draw Gulf moisture northward into Oklahoma and Arkansas. As this increasing low-level moisture converges along the front, diurnal heating of this moistening airmass will yield most-unstable CAPE values perhaps in excess of 3000 J/kg along and south of the surface front. Despite the strong instability and strong thermal gradient, the slow moving nature of the front will tend to favor anafrontal circulations. This appears to be borne out in the latest operational guidance suite with precipitation being favored on the cold side of the thermal gradient. This would tend to limit the overall risk of severe weather. However, given the degree of instability and the presence of a strong cold front, the risk of warm-sector convection remains. If confidence in warm-sector convection occurring increases, severe probabilities may be warranted across portions of eastern Oklahoma east through Arkansas into western Tennessee and northern Mississippi. ..Marsh.. 09/03/2025 $$