


Severe Storm Outlook Narrative (AC)
Issued by NWS
Issued by NWS
596 ACUS02 KWNS 220534 SWODY2 SPC AC 220532 Day 2 Convective Outlook NWS Storm Prediction Center Norman OK 1232 AM CDT Tue Apr 22 2025 Valid 231200Z - 241200Z ...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS ACROSS PARTS OF THE SOUTHERN HIGH PLAINS... ...SUMMARY... Isolated severe thunderstorms are possible across portions of the central and southern High Plains on Wednesday. ...Central/Southern Plains... A low-amplitude, modest southwesterly flow regime will persist across the Plains on Wednesday. At the surface, a stalled frontal boundary will extend from the Upper Midwest to the central High Plains, while a dryline extends south from southeast CO into southwest TX. Southerly low-level flow will maintain northward transport of modified Gulf moisture across TX/OK into the central Plains. Forecast guidance varies considerably regarding ongoing precipitation Wednesday morning. Some CAMs show widespread convection across KS, while other place morning convection further south along the Red River. This morning convection will potentially have implications for afternoon/evening severe potential as it may hinder diurnal destabilization, or produce outflow boundaries which could aid in redevelopment later in the day. Nevertheless, adequate boundary layer moisture beneath steep midlevel lapse rates and modest vertical shear (25-35 kt effective shear magnitudes) will support a broad area of at least Marginal (level 1 of 5) severe risk (strong winds and hail) from the central Plains along the stalled frontal boundary, south/southwest into the southern High Plains along the dry line. Some greater risk for a few supercells may develop along the dryline across west Texas. Stronger heating and higher surface dewpoints will foster greater destabilization. Elongated hodographs suggest isolated supercells capable of producing large hail will be possible. Furthermore, steep low-level lapse rates and deep boundary layer mixing may support sporadic strong/severe gusts. Given nebulous/weak large-scale ascent, storm coverage along the dryline is uncertain, and probabilities may need to be adjusted/extended northward if confidence increases in greater storm coverage. ..Leitman.. 04/22/2025 $$