Severe Storm Outlook Narrative (AC)
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Issued by NWS
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112 ACUS01 KWNS 231952 SWODY1 SPC AC 231950 Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0250 PM CDT Mon Sep 23 2024 Valid 232000Z - 241200Z ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS NORTHERN ARKANSAS INTO THE LOWER OHIO AND TENNESSEE RIVER VALLEYS... ...SUMMARY... Isolated strong to severe thunderstorms are possible this afternoon into evening from the Ozarks into parts of the Tennessee and lower Ohio Valleys. ...20z Update... The previous forecast remains on track with only minor adjustments needed based on recent observations and trends in guidance. Latest surface observations and upper-air analyses show the gradual organization of a surface low over northern AR/southern MO. The frontal boundary draped from southeast MO into the upper OH River Valley has begun to stall and is expected to gradually advance north through the evening hours. VWP observations along the frontal zone currently show relatively straight low-level hodographs, but helicity should slowly improve through the 20-03 UTC period as isentropic ascent along the front increases. As a result, the convective environment should become more favorable for organized convection - particularly during the 22-03 UTC period across far southeast MO into far southern IL and western KY. Latest high-res guidance suggests that storms developing along an approaching cold front across north-central AR will intensify as they migrate east towards this zone and should pose the primary severe threat this evening. However, loosely-organized thunderstorms recently developing within the mid-MS River Valley cast some uncertainty onto this scenario due to the potential for overturning portions of the downstream warm sector. This early convection may see improving organization in the coming hours as mid-level flow slowly improves late this afternoon, but limit storm longevity over the past hour cast some uncertainty onto the propensity for severe storms. Regardless, this stalled/warm frontal boundary will still present the best corridor for a more focused severe event through the evening hours, including the potential for a tornado or two. As such, the 2% risk probabilities have been expanded east into western KY. Consideration was given for 15% wind probabilities through this corridor, but confidence in storm mode and coverage remains too limited given the aforementioned concerns. Farther east across southern KY and TN, the forecast remains on track. See MCD #2097 for details regarding recent convective trends. ..Moore.. 09/23/2024 .PREV DISCUSSION... /ISSUED 1143 AM CDT Mon Sep 23 2024/ ...Ozarks to TN/OH Valleys and southern Appalachians... A positive-tilt upper trough will influence the region, with a general increase in relatively strong deep-layer southwesterly winds. Severe storms are possible this afternoon, particularly and initially across the Ozarks including far south-central to southeast Missouri, as well as far northern Arkansas and far southern Illinois. This will be in vicinity of a weak surface wave and a northward-shifting warm front as lingering morning convection along/north of the Ohio River abates and shifts eastward. Increasingly strong deep-layer winds could support some supercells. Some hail is possible given the buoyancy/deep-layer wind profiles, although mid-level lapse rates are not steep. Locally damaging winds may also occur, with some potential for a tornado or two mainly near the warm front. Although uncertainties linger regarding destabilization and the magnitude of the severe risk later this afternoon, portions of southeast Missouri and far southern Illinois will continue to be reevaluated into mid-afternoon (20Z update) for a potential risk upgrade. Farther east, isolated to scattered thunderstorms will probably develop near the ridge tops of the southern Appalachians and adjacent parts of the Carolinas Piedmont this afternoon. Moist low levels coupled with heating will result in around 1000 J/kg MLCAPE. Some modest multicell organization may occur due to adequately strong upper-level westerly flow, with a few locally damaging wind gusts a possibility. $$