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From | To | Subject | Date/Time | |||
Mike Powell | All | DAY1SVR: Day 1 Convective |
July 20, 2024 10:01 AM * |
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ACUS01 KWNS 201253 SWODY1 SPC AC 201252 Day 1 Convective Outlook NWS Storm Prediction Center Norman OK 0752 AM CDT Sat Jul 20 2024 Valid 201300Z - 211200Z ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS OVER PARTS OF THE SOUTHEAST AND CENTRAL TO SOUTHERN HIGH PLAINS... ...SUMMARY... Strong to isolated severe thunderstorms are possible over parts of the Southeast and central to southern High Plains, mainly from mid-afternoon to evening. ...Synopsis... The large-scale pattern in mid/upper levels will continue to feature longwave troughing over eastern North America, and ridging in the West. The latter will be anchored by an anticyclone -- now centered over AZ -- that will retrograde slowly northwestward through the period. This process -- and a broad field of minor shortwaves and vorticity lobes in northerly/northwesterly flow -- will contribute to net height falls over much of the central CONUS. A downstream shortwave trough was evident in moisture-channel imagery from the lower Ohio Valley southwestward across western TN to eastern LA. This perturbation should move eastward across the Tennessee Valley region through midday, then over parts of GA and the Carolinas through this evening. The 11Z surface map showed a weak, quasistationary frontal zone from southern VA across eastern TN, western MS, central LA, and south-central TX. Except where locally reconfigured by convection, this frontal zone should remain quasistationary, while gradually losing definition. A lee trough -- drawn from western MT to western SD and western KS, should remain nearly in place through the day, with slight shifts possible in late afternoon toward strongly heated areas. ...Southeast... Widely scattered to scattered thunderstorms should form and move northeastward over the area this afternoon, as large-scale lift ahead of the approaching trough spreads atop a richly moist, strongly heated, weakly capped boundary layer. Damaging to isolated severe gusts are possible. Some of the activity may aggregate into loosely organized clusters that maximize damage potential locally. Somewhat enhanced mid/upper flow will contribute to spotty effective-shear magnitudes of 30-35 kt, aiding in organization of some of this activity. The inflow layer will be characterized by surface dewpoints commonly in the low-mid 70s F and favorable lapse rates from surface heating beneath a deep troposphere. As such, and despite the lack of large mid/upper-level lapse rates, a deeply buoyant preconvective profile should take shape, with peak MLCAPE in the 2000-3000 J/kg range over the Low Country/coastal plain, and 1500-2500 J/kg across the Piedmont. ...Central/southern High Plains... Isolated to scattered thunderstorms are expected to develop this afternoon along the Front Range/Sangre de Cristo corridor from southeastern WY to NM, as well as over the Raton Mesa, near the lee trough, and along leftover outflow/differential-heating boundaries from prior overnight/morning convection. Isolated severe gusts and hail are possible. This activity will be moving into a generally less-buoyant airmass than the previous day, thanks to extensive prior convection and outflow over much of the region. Nevertheless, sufficient diurnal heating and residual boundary-layer moisture are expected to support both well-mixed subcloud layers and enough CAPE for deep convection. Though outflow-driven forward propagation may contribute to erratic storm motions locally, a general southeastward to southward translation is forecast, given the ambient midlevel winds. Although strong directional shear is expected, forecast soundings indicate much of this will be in the form of backing with height instead of veering, and with weak low/middle-level winds limiting vertical bulk shear. Peak afternoon MLCAPE of 1000-1500 J/kg is possible near an irregularly defined moist axis extending from the eastern Panhandles and southwestern KS northeastward, and over eastern CO. Buoyancy will diminish atop a drier, more deeply mixed layer westward toward the mountains. Overall, convection should diminish in coverage and intensity throughout the evening. ..Edwards/Broyles.. 07/20/2024 $$ --- SBBSecho 3.20-Linux * Origin: capitolcityonline.net * Telnet/SSH:2022/HTTP (618:250/1) |
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