Severe Storm Outlook Narrative (AC)
Issued by NWS
Issued by NWS
678 ACUS03 KWNS 051908 SWODY3 SPC AC 051907 Day 3 Convective Outlook NWS Storm Prediction Center Norman OK 0107 PM CST Wed Feb 05 2025 Valid 071200Z - 081200Z ...NO THUNDERSTORM AREAS FORECAST... ...SUMMARY... The risk for thunderstorms appears negligible across the U.S., Friday through Friday night. ...Discussion... General, broad mid/upper ridging centered over the subtropical latitudes is likely to be maintained, and a prominent influence across the southern into central tier of the U.S. through this period, downstream of persistent ridging in the northern mid-latitudes, and troughing in the southern mid- to subtropic latitudes, of the eastern Pacific. To the east of the Pacific ridging, broad mean troughing, with more progressive embedded smaller scale perturbations, will linger across British Columbia and the Pacific Northwest, while developing eastward across the Canadian Prairies, northern U.S. Rockies and Great Plains. This is likely to support deepening surface troughing, and perhaps cyclogenesis, to the lee of the Rockies. However, there remains substantive spread concerning this, as models continue to struggle with their varying ability to account for the seasonably cold air now entrenched to the east of the Rockies. Some erosion, from south to north, of the shallow leading edge of this air mass is possible, beneath a continuing southerly to westerly return flow across parts of the southern Great Plains into southern Mid Atlantic. However, it appears that associated moisture emanating from a modifying western Gulf boundary layer will not become supportive of more than weak destabilization, or an appreciable risk for thunderstorms, due to negligible forcing for ascent and warm, capping layers aloft. Models do indicate that forcing for ascent and cooling mid-levels may contribute to pockets of weak destabilization across parts of the Northwest into northern Great Plains. However, based on latest forecast soundings, it remains unclear whether associated boundary-layer based and/or elevated convective development will become capable of producing more than very transient/isolated lightning. ..Kerr.. 02/05/2025 $$