####018002971#### ACUS02 KWNS 181657 SWODY2 SPC AC 181655 Day 2 Convective Outlook NWS Storm Prediction Center Norman OK 1155 AM CDT Thu Apr 18 2024 Valid 191200Z - 201200Z ...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS FOR PARTS OF THE SOUTHEAST TOWARD THE CAROLINA PIEDMONT... ...SUMMARY... Sporadic strong to marginally severe storms are still possible tomorrow (Friday) over parts of the Southeast. ...Synopsis... A broad mid-level trough will traverse Ontario and Quebec, with mainly zonal flow overspreading the central and northern CONUS tomorrow (Friday). Meanwhile, a smaller mid-level trough is poised to eject into the southern High Plains at the end of the period. A surface cold front will sweep across the eastern U.S. in advance of the first mid-level trough, providing enough low-level ascent to support scattered strong thunderstorm development given adequate buoyancy and vertical wind shear preceding the front. For Friday night into Saturday morning, the approach of the southwestern mid-level trough will encourage low-level jet development over the southern Plains, with scattered to widespread thunderstorm development expected along the low-level jet terminus, where low-level convergence will be strongest. ...Parts of the Southeast toward the Carolina Piedmont... Surface temperatures are expected to warm above 80 F amid low to mid 60s F dewpoints ahead of the surface cold front, boosting SBCAPE from 1000-2000 J/kg across the warm sector. Modest westerly 500 mb flow from the glancing mid-level trough will overspread a 15-20 kt southwesterly 850 mb wind field, resulting in elongated hodographs and 40+ kts of effective bulk shear. As such, organized multicells and transient supercells are expected to initiate ahead of the cold front by afternoon, accompanied by occasional instances of hail and gusty winds. A couple instances of severe hail/wind could occur with some of the stronger storms, especially if a more pronounced supercell structure can become established. ...Central and northern Texas... A strongly capped boundary layer is expected to reside across much of TX through the period, limiting the chances for surface-based convective initiation. As the low level jet strengthens overnight, the jet terminus is expected to become situated somewhere near the Red River, where isentropic ascent should lift elevated buoyant parcels to their LFC and initiate scattered to potentially numerous thunderstorms. LFCs are expected to be between 700-600 mb, which should restrict CAPE to thin profiles, limiting severe hail production. Nonetheless, given elongated hodographs and steep mid-level lapse rates, at least small hail is possible and a sparse instance of severe hail cannot be ruled out, though the coverage seems too isolated/localized to warrant probabilities at this time. ..Squitieri.. 04/18/2024 $$