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From | To | Subject | Date/Time | |||
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Mike Powell | All | DAY48: D4 SEVERE OUTBREAK |
March 30, 2025 8:07 AM * |
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ACUS48 KWNS 300901 SWOD48 SPC AC 300859 Day 4-8 Convective Outlook NWS Storm Prediction Center Norman OK 0359 AM CDT Sun Mar 30 2025 Valid 021200Z - 071200Z ...SEVERE WEATHER OUTBREAK POSSIBLE ON D4/WED... ...DISCUSSION... Medium-range models appear to be in good agreement with overall evolution of the synoptic-scale pattern into the Day 7 (Saturday April 5) time period, when divergence in solutions increases. Earlier in the period however, model consistency lends fairly high confidence that a widespread/potentially substantial outbreak of severe weather will evolve Wednesday/Day 4, from Lower Michigan and the Ohio Valley, southwestward across the Middle and Lower Mississippi Valleys, and into eastern portions of Texas and Oklahoma. Convection will likely be ongoing or developing early in the day, over western portions of the risk area -- from Wisconsin southwestward to Oklahoma/North Texas. As an upper low shifts northeastward across the northern Plains toward the upper Mississippi Valley through the day, and the cold front crosses Iowa/Missouri/eastern Oklahoma, steep lapse rates atop a moist/diurnally heating warm sector will support widespread convective development. With ascent along the front somewhat modest as stronger large-scale ascent focuses northward into the western Upper Great Lakes and into Ontario, storm mode may tend toward isolated storms, as opposed to more linear development. This, combined with flow that is forecast to weakly veer but dramatically strengthen with height, suggests a primarily supercell storm mode. In additional to very large hail (particularly with southward extent), widespread damaging winds and several tornadoes are expected, some possibly significant. Risk is expected to continue well into the evening and likely overnight, shifting slowly eastward across the Midwest and mid/lower Mississippi Valley through the end of the period. Day 5/Thursday, trailing portions of the cold front should become aligned east-northeast to west-southwest across the Ohio and mid Mississippi Valleys and into the southern Plains, as the upper system shifts quickly across eastern Canada. While weak short-wave ridging will evolve atop the surface frontal zone in the wake of the departing system, daytime heating of a very moist boundary layer along and south of the front combined with strong flow aloft will support reinvigorated convection through the afternoon and evening hours, along with attendant severe-weather risk. Day 6/Friday, the surface front should remain quasi-stationary, but short-wave ridging should increase as a cut-off low evolves across the West. As such, much of the Day 6 convection may occur to the cool side of the surface front, in the zone of warm advection/isentropic ascent. While some severe risk will likely evolve, mainly in the form of hail, uncertainty overall (given the ridging aloft) precludes inclusion of a Day 6 risk area. By the weekend, deviation in model solutions increases, due to uncertain evolution of the low/trough over the West. As such, no risk areas will be included. ..Goss.. 03/30/2025 $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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