####018009830#### ACUS01 KWNS 081256 SWODY1 SPC AC 081255 Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0755 AM CDT Wed May 08 2024 Valid 081300Z - 091200Z ...THERE IS A MODERATE RISK OF SEVERE THUNDERSTORMS OVE PORTIONS OF SOUTHERN/SOUTHEASTERN MISSOURI...EXTREME NORTHEASTERN AR...EXTREME SOUTHERN ILLINOIS...WESTERN/SOUTH-CENTRAL KENTUCKY...AND NORTHWESTERN TO MIDDLE TENNESSEE... ...SUMMARY... Severe thunderstorms appear likely from parts of the mid Mississippi, Ohio, and Tennessee Valleys into the southern Plains. All severe hazards, including tornadoes, very large to giant hail, and potentially significant damaging winds are possible. Some tornadoes may be strong. ...Synopsis... In mid/upper levels, a temporarily blocky pattern has evolved around a cutoff cyclone over the northern Great Plains. The associated 500-mb low is expected to drift erratically southeastward and fill slowly through the remainder of the period, while a series of shortwaves amplify associated synoptic troughing extending southwestward across the Intermountain West and Great Basin. Meanwhile, a northern-stream perturbation over the Upper Great Lakes, that peeled eastward off the cyclone's influence, has a compact cyclone aloft centered near ANJ. This feature should devolve into an open shortwave trough and accelerate eastward as it enters the northern stream today, reaching eastern NY and western New England around 00Z. In the southern stream, broadly cyclonic flow will prevail over the western CONUS. A weak perturbation -- apparent in moisture-channel imagery over the central Gulf of California -- should move east-northeastward through the period, reaching northern Coahuila and adjoining southwest TX around 00Z, then parts of LA/northern MS by the end of the period. Downstream perturbations over the Southeast and central/southern Appalachians should be predominantly convectively derived. At 11Z, a surface lows were evident over southwestern ND and between OFK-YKN, along an occluded front. An occluded/cold front arched from the NE low across northeastern KS to another weak low near CNU, then southwestward over southwestern OK and the TX South Plains. Today, the cold front will overtake the northern part of a dryline now over northwest TX to the Big Bend region. By 00Z, the front and dryline together will act as a western limit of substantial convective/severe potential, from eastern OK to north-central/central TX. A Gulf warm front over northeastern OK and central/northeastern AR was moving northward and should cross the Ozarks this morning, moving into southern MO. A progressive outflow boundary was apparent from northern VA across southern WV, southeastern KY, to northern parts of middle/western TN and southeastern MO. The western part of this boundary is stalling, and soon should retreat northward through the rest of the morning across parts of western KY and southeastern MO, essentially linking with the warm front to form a baroclinic zone focusing the greatest of today's severe risks. ...Ozarks to Mid Mississippi, lower Ohio and Tennessee Valleys... A complicated, potentially dangerous severe-weather event is possible today into this evening. Multiple rounds of strong-severe thunderstorms are expected today across this region, additively contributing enough severe hazard for the "moderate" (level 4 of 5) risk area. A swath of damaging to severe gusts and at least a few embedded tornadoes are likely to accompany a complex of thunderstorms from southern MO across parts of the multi-state area near the Ohio/Mississippi River junction, to at least northern parts of the Tennessee Valley region. The main MCS should move east-southeastward to southeastward along and near the instability gradient associated with the aforementioned outflow boundary. Before and during that process, several supercells are expected, offering tornadoes (a few potentially significant/EF2+), large to very large hail, and localized severe gusts. An ongoing area of strong-severe thunderstorms across portions of MO should pose mainly a severe-hail threat for another couple hours, though the gust potential will increase as it grows upscale. See severe thunderstorm watch 202 and related mesoscale discussions for the near-term threat. As the morning progresses, the wind threat will ramp up further, with some tornado potential starting as well, as this activity and/or additional convection developing later over western MO interacts with 1) a northward-moving plume of surface-based inflow air and 2) rich low-level moisture now found south of the outflow boundary. Meanwhile, diurnal destabilization of an already richly moist airmass south of the boundary will grow MLCAPE commonly into the 3000-4000 J/kg range, beneath favorable (50-60 kt) deep shear. Low-level shear/vorticity, SRH and hodograph size will peak near the boundary, supporting a corridor of relatively maximized tornado potential with any sustained/discrete or semi-discrete supercells in the area, as well as a focus for MCS forward propagation from the northwest. MCS activity should merge upscale further this evening and tonight, maintaining severe-wind potential into parts of the Tennessee Valley region before moving into gradually less instability late tonight. ...Eastern OK to AR, Mid-South and central TX... Thunderstorms should develop by late afternoon near the front and dryline, as a combination of lift along those boundaries and strong surface heating combine with very rich low-level moisture to erode the EML cap sampled well by the 12Z FWD RAOB. Large to giant hail, occasional severe gusts, and a few tornadoes are possible as activity shifts eastward to northeastward across central/east TX, the Arklatex, and AR through the evening. The northern part of this convection may merge with or be overtaken by MCS activity moving out of MO and into parts of the Mid-South. The afternoon/preconvective environment should be characterized by steep low/middle level lapse rates on either side of the weakening cap, along with surface dewpoints commonly in the 70s F. This will contribute to strong buoyancy with the peak/preconvective MLCAPE reaching 4500-5500 J/kg, and SBCAPE values topping 6000 J/kg. Although near-surface flow generally will be 10 kt or less, limiting lowest-km hodographs/shear, effective-shear magnitudes in the 40-55-kt range indicate supercells will be possible. These will be capable of very large/destructive hail exceeding 3 inches in diameter. Clusters or upscale mergers of convection also may offer deep, precip-loaded, hail-cooled downdrafts with locally severe gusts. Cell mergers and interactions with boundaries will factor into tornado potential on the storm scale, since the environmental low-level shear appears on the margins. ...Southern Appalachians/Cumberland Plateau into Carolinas... Thunderstorms are ongoing along and behind the outflow boundary near the TN/KY border area, and may pose a severe threat through the remainder of the morning while moving generally southeastward. See SPC mesoscale discussion 693 for near-term details. Further intensification and/or additional development is possible into the afternoon over and east of the mountains, moving into an environment of favorable moisture and diurnal destabilization. MLCAPE in the 1500-2500 J/kg range appears attainable, amidst roughly 35-45-kt effective-shear magnitudes. A mix of supercell and multicell modes is expected, with small bows possible, supporting localized threats for damaging wind, large hail and at least marginal tornado potential. ...Northeastern CONUS... Widely scattered to scattered thunderstorms may develop as soon as mid/late morning over parts of eastern NY and New England. Activity should form atop a diurnally destabilizing and weakly capped boundary layer, along/ahead of a prefrontal surface trough and behind a plume of non-severe thunderstorms and precip now crossing parts of the region. Thunderstorms should move generally eastward, offering damaging to isolated severe gusts and isolated large hail. A combination of low-level warm advection, spotty/irregular diurnal surface heating, and cooling aloft related to the approaching Great Lakes shortwave trough, will steepen low/middle-level lapse rates substantially. With favorable moisture (surface dewpoints generally 50s to low 60s F), a plume of 500-1000 J/kg MLCAPE should develop, amidst effective-shear magnitudes that reach 40-50 kt, and despite strongly veered/westerly surface wind components. A mix of multicell and modest supercell characteristics should be observed before activity moves over more-stable air and/or offshore, and weakens by early evening. ...Eastern SD to eastern IA and vicinity... Widely scattered to scattered thunderstorms are possible from early afternoon in western parts to evening closer to the Mississippi River, with isolated damaging gusts, large hail and possibly a tornado or two. Activity should form in an area of deep-layer lift (including low-level convergence/mass response) related to a vorticity lobe in the southeastern part of the mid/upper-level cyclone. Associated cooling aloft will combine with residual low-level moisture (dewpoints mid 40s to mid 50s F) to yield pockets of around 500-1000 J/kg MLCAPE. Backed low-level winds will aid convergence and storm-relative low-level flow, and may contribute to locally enlarged hodographs. ..Edwards.. 05/08/2024 $$