076  
ACUS02 KWNS 170552  
SWODY2  
SPC AC 170551  
 
DAY 2 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK  
1251 AM CDT THU APR 17 2025  
 
VALID 181200Z - 191200Z  
 
...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS FROM LOWER  
MICHIGAN TO THE SOUTHERN PLAINS...  
   
..SUMMARY
 
 
SCATTERED SEVERE THUNDERSTORMS ARE POSSIBLE FROM THE PARTS OF THE  
GREAT LAKES TO THE SOUTHERN GREAT PLAINS, MAINLY DURING THE LATE  
AFTERNOON FRIDAY INTO FRIDAY NIGHT. LARGE HAIL AND ISOLATED SEVERE  
GUSTS WILL BE THE MAIN HAZARDS WITH THIS ACTIVITY.  
   
..SYNOPSIS
 
 
A POSITIVE-TILT LARGE-SCALE UPPER TROUGH WILL PIVOT SOUTH AND EAST  
ACROSS PORTIONS OF THE NORTH-CENTRAL TO WESTERN U.S. ON FRIDAY. A  
SWATH OF 60-80 KT 500 MB FLOW WILL STRETCH FROM THE SOUTHERN ROCKIES  
TO THE GREAT LAKES AHEAD OF THE UPPER TROUGH. AT THE SURFACE, LOW  
PRESSURE WILL DEVELOP NORTHEAST FROM THE KS/MO/IA VICINITY FRIDAY  
MORNING, TO SOUTHERN ONTARIO/QUEBEC BY EARLY SATURDAY. AS THIS  
OCCURS, A COLD FRONT WILL DEVELOP SOUTHEAST ACROSS PORTIONS OF THE  
MID-MS VALLEY/GREAT LAKES AND SOUTHERN PLAINS. A WEAK SECONDARY  
SURFACE LOW LIKELY WILL DEVELOP ACROSS WEST TX, WHERE A DRYLINE WILL  
EXTEND SOUTHWARD FROM THE EASTERN PANHANDLE TO THE BIG BEND REGION.  
 
SOUTHERLY LOW-LEVEL FLOW WILL TRANSPORT MODEST BOUNDARY-LAYER  
MOISTURE NORTHWARD AHEAD OF THESE SURFACE FEATURES AND BENEATH FAST  
MID/UPPER SOUTHWESTERLY FLOW. THIS WILL SUPPORT SCATTERED SEVERE  
STORMS LATE FRIDAY AFTERNOON INTO THE OVERNIGHT HOURS FROM PORTIONS  
OF THE SOUTHERN PLAINS TO THE GREAT LAKES.  
   
..LOWER-MO/MID-MS VALLEY TO GREAT LAKES
 
 
ELEVATED THUNDERSTORMS NORTH OF A WARM FRONT WILL LIKELY BE ONGOING  
DURING THE MORNING INTO THE AFTERNOON ACROSS WI/NORTHERN MI. THIS  
ACTIVITY MAY POSE A RISK FOR MARGINALLY SEVERE HAIL.  
 
MEANWHILE, A SHORTWAVE UPPER TROUGH EMBEDDED WITHIN THE NORTHERN  
BRANCH OF THE LARGER-SCALE WESTERN U.S. UPPER TROUGH WILL SHIFT EAST  
ACROSS THE NORTHERN PLAINS AND UPPER MIDWEST DURING THE  
EVENING/OVERNIGHT. THIS WILL FACILITATE THE EASTWARD PROGRESSION OF  
THE SURFACE FRONT THROUGH THE PERIOD, CREATING A FOCUS FOR  
THUNDERSTORM DEVELOPMENT. HOWEVER, STRONG CAPPING WILL LIMIT  
DEVELOPMENT ALONG THE FRONT, LIKELY UNTIL CLOSER TO 00Z, WHEN  
STRONGER LARGE-SCALE ASCENT OVERSPREADS THE SURFACE BOUNDARY AND  
COOLING ALOFT ENSUES. THUNDERSTORMS WILL LIKELY REMAIN ELEVATED ATOP  
THE STRONG EML IN THE 850-700 MB LAYER, AND WILL LIKELY BECOME  
UNDERCUT BY THE SURFACE COLD FRONT GIVEN BOUNDARY-PARALLEL FLOW  
THROUGH THE CLOUD-BEARING LAYER. NEVERTHELESS, STEEP MIDLEVEL LAPSE  
RATES AND SUFFICIENT MUCAPE WILL SUPPORT ORGANIZED CONVECTION  
CAPABLE OF PRODUCING LARGE HAIL. WITH TIME, CELLS MAY BECOME  
TRAINING CLUSTERS, POSING SOME ISOLATED RISK FOR DAMAGING GUSTS.  
   
..SOUTHERN PLAINS VICINITY
 
 
AS A SURFACE LOW DEVELOPS ACROSS WEST TX, A TRIPLE POINT WILL EMERGE  
NEAR THE EASTERN TX PANHANDLE/SOUTH PLAINS VICINITY. A STOUT EML  
WILL PRECLUDE CONVECTIVE DEVELOPMENT FOR MUCH OF THE DAY. NEAR THE  
TRIPLE POINT AND NORTHEAST ALONG THE ADVANCING COLD FRONT, ISOLATED  
TO SCATTERED THUNDERSTORMS SHOULD FORM IN THE 22-00Z TIME FRAME.  
SUPERCELL WIND PROFILES WITH LARGE MUCAPE, VERY STEEP LAPSE RATES,  
AND ELONGATED HODOGRAPHS SUGGESTS INITIAL SUPERCELLS WILL POSE A  
RISK FOR LARGE TO VERY LARGE HAIL THROUGH EARLY EVENING. THEREAFTER,  
BOUNDARY-PARALLEL FLOW WILL RESULT IN CLUSTERING/TRAINING AS  
CONVECTION ALSO BECOMES UNDERCUT BY THE FRONT. DAMAGING GUSTS ALSO  
MAY OCCUR WITH INITIAL SUPERCELLS GIVEN A WELL-MIXED BOUNDARY  
LAYER/STEEP LOW-LEVEL LAPSE RATES BENEATH THE EML. ADDITIONALLY,  
SOME STRONG GUST POTENTIAL COULD OCCUR INTO THE OZARKS VICINITY AS  
CLUSTERING ENSUES, BUT HAIL IS EXPECTED TO BE THE MAIN CONCERN.  
 
..LEITMAN.. 04/17/2025  
 

 
 
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