


Severe Storm Outlook Narrative (AC)
Issued by NWS
Issued by NWS
725 ACUS02 KWNS 040558 SWODY2 SPC AC 040557 Day 2 Convective Outlook NWS Storm Prediction Center Norman OK 1257 AM CDT Fri Jul 04 2025 Valid 051200Z - 061200Z ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS FOR PORTIONS OF THE NORTHERN HIGH PLAINS... ...SUMMARY... Strong to severe storms are likely across portions of the northern High Plains tomorrow (Saturday), with hail and wind being the main concerns. Isolated damaging gusts may also accompany the stronger storms over the Upper Midwest. ...Synopsis... Generally zonal mid-level flow will overspread the northern CONUS as an upper trough impinges on the West Coast tomorrow (Saturday). A pair of mid-level impulses will traverse the zonal flow, with one impulse passing over the Great Lakes as the other impulse ejects into the Northern High Plains. Over both locations, adequate moisture and instability will be in place to support strong thunderstorms. The best chance for severe thunderstorms will be over the northern High Plains, where stronger vertical wind shear will encourage storm organization. ...Northern into the central High Plains... A belt of strong westerly 500 mb flow will overspread MT into the northern High Plains Saturday afternoon with the passage of the aforementioned mid-level impulse. A surface low will develop somewhere across northern WY into southern MT, promoting moist southeasterly low-level flow beneath the stronger mid-level westerlies, resulting in over 50 kts of effective bulk shear. Adequate low-level moisture, overspread by 8+ C/km low to mid-level lapse rates, will boost MLCAPE to over 2000 J/kg in spots. The moderate instability and strong deep-layer shear will promote supercells and bowing segments capable of producing some severe wind and hail. A tornado is also possible with the longer-lived, dominant supercells. Farther south into the central High Plains, deep-layer ascent and shear should be considerably weaker, resulting in a lower coverage of relatively less organized multicellular clusters. Storms here should be high-based, overspreading a dry boundary layer deepening into the 700-500 mb range by afternoon peak heating. Isolated severe gusts are possible with the stronger multicellular clusters, and an instance or two of severe hail cannot be ruled out. ...Great Lakes into the central Plains... A weak surface cold front, associated with a surface low over the Great Lakes, will progress southeastward across the western Great Lakes into the central Plains as the eastern mid-level impulse glances by to the north. Flow closer to the surface and aloft, and thus vertical wind shear, will not be overly strong ahead of the front. However, rich low-level moisture amid afternoon surface heating will promote 2000-3000 J/kg MLCAPE and minimal convective inhibition. Scattered multicells should develop along/ahead of the front through the afternoon, the stronger storms of which may produce wet downbursts and accompanying isolated damaging gusts. ..Squitieri.. 07/04/2025 $$