


Severe Storm Outlook Narrative (AC)
Issued by NWS
Issued by NWS
953 ACUS02 KWNS 291712 SWODY2 SPC AC 291710 Day 2 Convective Outlook NWS Storm Prediction Center Norman OK 1210 PM CDT Sun Jun 29 2025 Valid 301200Z - 011200Z ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS FOR PARTS OF THE MIDWEST INTO THE OHIO VALLEY...THE MID-ATLANTIC...AND ALONG THE CALIFORNIA/OREGON BORDER... ...SUMMARY... Scattered strong to severe thunderstorms remain possible across parts of the Ohio Valley, Midwest and the Mid-Atlantic tomorrow (Monday). A couple of severe thunderstorms also cannot be ruled out over parts of the Pacific Northwest. ...Synopsis... A mid-level trough will amplify while traversing the Great Lakes and Ohio Valley regions, as upper ridging builds over the Plains states and an upper-level low impinges on the California coastline tomorrow (Monday). A cold front will accompany the Midwest mid-level trough, and is poised to progress across the Mid-MS and OH Valley regions while draping across the southern Plains through the day. In advance of the cold front, adequate moisture and overall instability will be present to support at least scattered thunderstorms. Given the presence of modest vertical wind shear, a few of the storms could become strong to locally severe. Thunderstorms may also develop north of a surface low along the CA/OR border, amid an unstable airmass supportive of scattered strong thunderstorms. ...Midwest into the OH Valley... Preceding an advancing cold front, diurnal heating of a moist boundary layer, atop relatively poor mid-level lapse rates, will result in airmass destabilization and 1500-3000 J/kg SBCAPE by afternoon. While MLCINH will minimize by late morning, the poor mid-level lapse rates suggest that CAPE should be constrained to tall/thin profiles. Furthermore, unidirectional vertical wind profiles with little strengthening with height, should lead to mediocre deep-layer shear. While many scattered storms should develop along the cold front, and ahead in the uncapped warm sector, most storms should be pulse-cellular to multicellular in nature. A few of the stronger storms may support wet downbursts capable of producing localized damaging gusts. ...Mid-Atlantic... Similar to the Great Lakes/OH Valley vicinity, strong boundary-layer heating will quickly reduce convective inhibition and support scattered thunderstorm development amid weak vertical wind shear. 2000+ J/kg of tall/thin SBCAPE will support wet downburst potential, and a couple of damaging wind gusts are possible. ...Southern Plains... Scattered thunderstorms should develop by afternoon peak heating ahead of the trailing cold front over the southern Plains. Surface temperatures should warm to near 90 F amid low to mid 70s F dewpoints, yielding as much as 3000-4000 J/kg MLCAPE given modest mid-level lapse rates. Though vertical wind shear should be relatively poor, the strong buoyancy in place may compensate to support wet downbursts and associated isolated severe gusts with the stronger storms. ...Northern California into Southern Oregon... Scattered thunderstorms will develop immediately north of a weak surface low, where localized forcing for ascent will be in place. These thunderstorms should develop atop a mixed boundary layer that may deepen to 600-500 mb. Furthermore, the presence of 9+ C/km lapse rates through the troposphere may promote enough thermodynamically-driven downward momentum transport to support isolated strong to severe wind gusts. Point forecast soundings also depict curved/elongated hodographs, which may support multicells and transient supercells with a marginal hail threat. ..Squitieri.. 06/29/2025 $$