Subj : DAY1SVR: Day 1 Convective To : All From : Mike Powell Date : Wed Sep 10 2025 08:03:04 ACUS01 KWNS 101247 SWODY1 SPC AC 101245 Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0745 AM CDT Wed Sep 10 2025 Valid 101300Z - 111200Z ....NO SEVERE THUNDERSTORM AREAS FORECAST... ....SUMMARY... Scattered showers and thunderstorms are possible over parts of the Northwest and northern Rockies with more isolated storms over the High Plains. Severe potential is generally low. ....Synopsis... Water-vapor imagery this morning shows an upper low situated over northern CA, and it will remain nearly stationary during the period with a large area of cyclonic flow extending from southern CA into the eastern Great Basin and central Rockies. A downstream upper ridge over the High Plains will feature a lee trough that will act to focus isolated to scattered thunderstorms from MT southward into the central High Plains. Strong heating and weak upslope flow beneath the aforementioned upper-level ridge will favor a few isolated cells developing during peak heating. A couple of the more vigorous storms may be capable of localized strong gusts near 1) NM/OK/TX/CO border, 2) east of the CO Front Range in the High Plains, and 3) in eastern WY. Warming aloft is expected to mitigate the overall potential with these storms. Farther west, a mid-level shortwave trough will move through the base of the West Coast mid- to upper low/trough and to near the UT/NV border by late afternoon/early evening. A corresponding belt of 50-kt southwesterly 500-mb flow will overspread western UT. Isolated dry microbursts may accompany the stronger storms over central UT into western CO during the 22-02z period. Elsewhere, scattered afternoon storms will occur beneath the upper trough from northern NV into OR and western ID, and a few of these storms could produce at least small hail given such cool temperatures aloft and modest deep-layer shear. ...Smith/Broyles.. 09/10/2025 $$ --- SBBSecho 3.28-Linux * Origin: ILink: CCO - capitolcityonline.net (454:3/105) .