534  
ACUS02 KWNS 011732  
SWODY2  
SPC AC 011730  
 
DAY 2 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK  
1230 PM CDT WED APR 01 2026  
 
VALID 021200Z - 031200Z  
 
...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS THURSDAY  
AFTERNOON AND EVENING ACROSS PARTS OF EASTERN IOWA...NORTHERN AND  
CENTRAL ILLINOIS...AND SOUTHERN WISCONSIN...  
   
..SUMMARY
 
 
SEVERE THUNDERSTORMS CAPABLE OF PRODUCING A FEW TORNADOES APPEAR  
PROBABLE ACROSS PARTS OF EASTERN IOWA INTO SOUTHERN WISCONSIN,  
NORTHERN AND CENTRAL ILLINOIS LATE THURSDAY AFTERNOON AND EVENING.  
SOME OF THESE TORNADOES MAY BECOME FAST MOVING AND STRONG.  
   
..DISCUSSION
 
 
WHILE A NOTABLE MID/UPPER HIGH PERSISTS ACROSS THE SOUTHWESTERN MID-  
INTO SUBTROPICAL WESTERN ATLANTIC, FLOW EMANATING FROM THE NORTHERN  
MID-LATITUDE PACIFIC IS FORECAST TO REMAIN PROGRESSIVE INTO AND  
ACROSS THE PACIFIC COAST THROUGH THIS PERIOD. WITHIN THIS REGIME, A  
STRONG MID/UPPER JET STREAK, SHORT WAVE TROUGH AND EMBEDDED  
MID-LEVEL CYCLONE ARE FORECAST TO DIG ACROSS THE NORTHERN U.S.  
PACIFIC COAST THROUGH THE NORTHERN GREAT BASIN/INTERMOUNTAIN REGION  
AND ROCKIES BY EARLY FRIDAY. IT APPEARS THAT THIS WILL BE  
ACCOMPANIED BY RENEWED SURFACE CYCLOGENESIS TO THE LEE OF THE  
COLORADO ROCKIES LATE THURSDAY THROUGH THURSDAY NIGHT.  
 
AS THIS OCCURS, A PRECEDING SHORT WAVE TROUGH, WHICH HAS EMERGED  
FROM THE SOUTHERN MID-LATITUDE PACIFIC, LIKELY WILL BE FORCED  
NORTH-NORTHEAST OF THE CENTRAL GREAT PLAINS THROUGH THE UPPER  
MIDWEST AND UPPER GREAT LAKES REGION BY LATE THURSDAY NIGHT. MODELS  
SUGGEST THAT IT WILL DEAMPLIFY AS IT DOES, BUT AN INITIALLY DEEP  
ASSOCIATED SURFACE CYCLONE MAY MAINTAIN CONSIDERABLE STRENGTH AS ITS  
CENTER MIGRATES FROM NORTHEASTERN KANSAS THROUGH NORTHEASTERN IOWA  
BY LATE AFTERNOON, BEFORE UNDERGOING MORE APPRECIABLE WEAKENING  
WHILE CONTINUING ACROSS THE EASTERN WISCONSIN/LOWER MICHIGAN  
VICINITY OVERNIGHT.  
   
..GREAT PLAINS INTO MISSISSIPPI VALLEY/GREAT LAKES
 
 
CONSIDERABLE CONVECTIVE DEVELOPMENT MAY BE ONGOING AT THE OUTSET OF  
THE PERIOD ACROSS THE MID/LOWER MISSISSIPPI VALLEY INTO THE GREAT  
LAKES, AND SOUTHWARD ACROSS THE EASTERN GREAT PLAINS INTO CENTRAL  
TEXAS. MUCH OF THIS IS LIKELY TO BE WELL IN THE PROCESS OF  
WEAKENING, PARTICULARLY ACROSS THE SOUTHEASTERN GREAT PLAINS, AS THE  
MID/UPPER WAVE CONTINUES ACCELERATING ACROSS/NORTH-NORTHEAST OF THE  
CENTRAL GREAT PLAINS DURING THE DAY.  
 
DUE TO STILL SOMEWHAT MODEST WARM SECTOR BOUNDARY-LAYER MOISTURE,  
AND CONVECTIVE CLOUD COVER SPREADING DOWNSTREAM ACROSS THE POTENTIAL  
NEAR-SURFACE INFLOW ENVIRONMENT, MODELS SUGGEST LITTLE POTENTIAL FOR  
APPRECIABLE DESTABILIZATION AND RE-INTENSIFICATION OF THE INITIAL  
PRE-COLD FRONTAL CONVECTIVE DEVELOPMENT AS IT SPREADS ACROSS AND  
EAST OF THE MID/UPPER MISSISSIPPI VALLEY DURING THE DAY.  
 
HOWEVER, IN ITS WAKE, A CORRIDOR OF BETTER PRE-COLD FRONTAL  
LOW-LEVEL MOISTURE RETURN, BENEATH A PLUME OF A STEEPER MID-LEVEL  
LAPSE RATES ASSOCIATED WITH A DEVELOPING DRY SLOT, IS FORECAST TO  
CONTRIBUTE TO AT LEAST A NARROW CORRIDOR OF SUBSTANTIVE  
BOUNDARY-LAYER DESTABILIZATION. IT APPEARS THAT THIS MAY INCLUDE  
CAPE IN EXCESS OF 1000 J/KG ALONG/AHEAD OF A DEVELOPING  
DRYLINE/CLOSELY TRAILING COLD FRONT, FROM THE VICINITY OF THE LOW  
ACROSS EAST CENTRAL IOWA SOUTHWESTWARD TOWARD THE MISSOURI OZARKS BY  
20-21Z.  
 
PARTICULARLY NEAR THE SURFACE LOW AND WARM FRONT INTERSECTION,  
FORCING FOR ASCENT PROBABLY WILL BE SUFFICIENT TO SUPPORT INTENSE  
CONVECTIVE DEVELOPMENT, IN THE PRESENCE OF STRONG DEEP-LAYER SHEAR  
AND LARGE CLOCKWISE-CURVED LOW-LEVEL HODOGRAPHS (BENEATH A 50+ KT  
SOUTHERLY 850 MB JET). THIS SHOULD, AT LEAST INITIALLY, INCLUDE  
DISCRETE SUPERCELL DEVELOPMENT WITH POTENTIAL TO PRODUCE TORNADOES,  
BEFORE PERHAPS GROWING UPSCALE WHILE DEVELOPING EAST-NORTHEASTWARD  
AHEAD OF THE SURFACE CYCLONE INTO THURSDAY EVENING.  
 
ADDITIONAL SUPERCELLS ARE LIKELY TO CONTINUE DEVELOPING  
SOUTH-SOUTHWESTWARD ALONG THE TRAILING DRYLINE, BEFORE IT IS  
OVERTAKEN BY THE COLD FRONT, TOWARD THE LOWER MISSOURI VALLEY.  
EMBEDDED WITHIN SOUTH-SOUTHWESTERLY DEEP-LAYER MEAN FLOW ON THE  
ORDER OF 50+ KTS, FAST STORM MOTIONS ROUGHLY ALIGNED WITH THE AXIS  
OF DESTABILIZATION COULD SUPPORT A COUPLE OF LONG-LIVED/LONG TRACK  
SUPERCELLS WITH POTENTIAL FOR STRONG TORNADOES, BEFORE CONVECTION  
WEAKENS THURSDAY EVENING.  
 
..KERR.. 04/01/2026  
 

 
 
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