


Severe Storm Outlook Narrative (AC)
Issued by NWS
Issued by NWS
578 ACUS02 KWNS 011729 SWODY2 SPC AC 011728 Day 2 Convective Outlook NWS Storm Prediction Center Norman OK 1228 PM CDT Tue Jul 01 2025 Valid 021200Z - 031200Z ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS ACROSS PORTIONS OF THE NORTHERN ROCKIES AND UPPER MIDWEST INTO THE GREAT LAKES... ...SUMMARY... At least scattered storms are possible across a large portion of the continental U.S. on Wednesday. Isolated severe gusts may accompany the stronger storms over portions of the Northern Rockies and the Upper Midwest to central Michigan region. ...Synopsis... A mid-level trough will amplify while tracking toward New England, with an upper ridge poised to build over the central U.S. as another mid-level trough impinges on the Pacific Northwest tomorrow (Wednesday). Widespread, rich low-level moisture will encourage at least scattered thunderstorm development across much of the CONUS. However, the best chance for strong to isolated severe thunderstorms will be over parts of the Northern Rockies and the Upper Midwest/Great Lakes regions. Here, low-level moisture and instability will best overlap with modest mid-level westerly flow along the periphery of the upper ridge, where some vertical wind shear will be present to encourage storm organization. ...Portions of the Northern Rockies... Through the day, surface heating will support mixing of a dry boundary layer, which may deepen to 500 mb in spots. Tropospheric lapse rates will steepen to around 9 C/km, boosting SBCAPE into the 500-1500 J/kg range. High-based thunderstorms should develop by afternoon peak heating. Modest mid-level flow along the periphery of the ridge will overspread the dry boundary layer, resulting in elongated, straight hodographs and 30 kts of effective bulk shear. Multicell structures or perhaps a transient supercell will be the likely storm modes. Given the dry boundary layer, the stronger storm cores may produce a few severe gusts. ...Upper Midwest into the Great Lakes... Along the eastern periphery of the upper ridge, broad northwesterly mid/upper flow will overspread the Upper Midwest and Great Lakes region during the afternoon. Modest low-level moisture and mid-level lapse rates will contribute to 1000-2000 J/kg MLCAPE by afternoon peak heating. A belt of stronger northwesterly 500 mb flow will overspread the Great Lakes as the eastern trough deepens in the 18-00Z time frame, contributing to vertical speed shear and elongated, straight hodographs. Over 30 kts of unidirectional effective bulk shear will support multicells capable of producing a few instances of severe wind and/or hail. ..Squitieri.. 07/01/2025 $$