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Mike Powell | All | DAY2 2/5 Risk Area Posted |
March 31, 2026 8:12 AM * |
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ACUS02 KWNS 310603 SWODY2 SPC AC 310601 Day 2 Convective Outlook NWS Storm Prediction Center Norman OK 0101 AM CDT Tue Mar 31 2026 Valid 011200Z - 021200Z ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS FROM NORTHWEST TEXAS INTO CENTRAL OKLAHOMA...EASTERN KANSAS...AND WESTERN MISSOURI... ...SUMMARY... Severe thunderstorms are likely across the southern and central Plains on Wednesday afternoon and evening. Severe wind gusts, large hail, and a few tornadoes are the primary concerns. Isolated strong/severe storms are also possible over parts of the upper Ohio Valley into the Mid-Atlantic. ...Synopsis... By 12 UTC Wednesday, a stalled frontal boundary will likely be draped from the southern/central Plains eastward along the OH Valley and into the Mid-Atlantic. Aloft, a progressive upper wave will traverse the Southwest during the day, eventually ejecting into the southern Plains around or after 00 UTC. The approach of the upper wave will support lee cyclogenesis across southeast CO into western KS, which will foster northward advection of low 60s dewpoints (already noted in early-morning surface observations along the TX coast) into OK and eastern KS by late afternoon. The intensification of the low will also promote a northward advancement of the boundary as a warm front into northern MO and possibly southern IA by late evening, as well as the sharpening of a dryline across western OK into northwest and western TX through the day. Strong to severe thunderstorm potential will mainly be focused along/ahead of the dryline and in proximity to the warm front as the upper wave begins to eject during the early evening hours. ...Southern Kansas into Oklahoma and northwest Texas... Initiation along the dryline appears likely during the 21-00 UTC period across western OK into northwest TX as a combination of diurnal heating and increasing synoptic ascent act to erode inhibition. Elongated hodographs featuring effective bulk shear values between 35-45 knots will support initially discrete supercells capable of large/very large hail and tornadoes (though uncertainty persists regarding low-level SRH through early evening). Upscale growth is anticipated at some point during the evening hours, though there is some uncertainty on when this transition will occur and the primary threat becomes severe wind. Regardless, an increase in the nocturnal jet will enlarge low-level hodographs and maintain the tornado potential into the late evening hours. ...Eastern Kansas and western Missouri... Latest guidance shows fairly strong consistency in the development of semi-discrete convection along the lifting warm front across eastern KS into western MO during the late afternoon/evening hours - likely owing to weaker capping and focused low/mid-level warm advection that is noted in most forecast soundings. Veering winds within the warm frontal zone will support effective SRH values on the order of 200-300 m2/s2, and surface-based LCLs near or below 1 km will likely support a tornado threat in addition to large/very large hail. While the potential for robust supercells is noted, the weak capping and focused ascent may promote thunderstorm clustering and upscale growth (as hinted by 00z HRRR/RRFS solutions) that could limit the longevity of these threats; however, the strong signal in guidance for deep convection within a favorable environment warrants an expansion of probabilities. ...Ohio Valley and Mid-Atlantic... Diurnal heating along and focused low-level ascent along the stalled boundary will likely support isolated to widely scattered convection by mid-afternoon. While mid-level flow will be somewhat modest compared to locations further west, sufficient hodograph elongation should promote at least a few more organized storms capable of posing a large hail threat. Deep-layer flow along the boundary may promote clustering during peak heating with an attendant threat for damaging/severe winds. ..Moore.. 03/31/2026 $$ --- SBBSecho 3.28-Linux * Origin: Capitol City Online (618:250/10) |
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