680  
ACUS03 KWNS 210731  
SWODY3  
SPC AC 210730  
 
DAY 3 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK  
0230 AM CDT SAT JUN 21 2025  
 
VALID 231200Z - 241200Z  
 
...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS FOR PARTS OF THE  
UPPER MIDWEST AND NORTHERN GREAT LAKES...  
   
..SUMMARY
 
 
STRONG TO POTENTIALLY SEVERE STORMS MAY DEVELOP MONDAY FROM PARTS OF  
THE GREAT LAKES INTO THE CENTRAL PLAINS.  
   
..SYNOPSIS
 
 
LITTLE CHANGE TO THE LARGE-SCALE PATTERN IS EXPECTED ON MONDAY, WITH  
A PERSISTENT UPPER TROUGH OVER THE WESTERN CONUS, AND AN AMPLIFIED  
UPPER RIDGE COVERING MUCH OF THE EAST. A SHORTWAVE EJECTING FROM THE  
WESTERN TROUGH IS FORECAST TO MOVE QUICKLY NORTHEASTWARD TOWARD  
HUDSON BAY BY MONDAY EVENING. IN THE WAKE OF THIS FEATURE, GUIDANCE  
GENERALLY DEPICTS ONLY LOW-AMPLITUDE VORTICITY MAXIMA MOVING AROUND  
THE PERIPHERY OF THE RIDGE FROM THE CENTRAL/SOUTHERN PLAINS INTO THE  
GREAT LAKES.  
 
AT THE SURFACE, A FRONT IS FORECAST TO BE DRAPED FROM THE CENTRAL  
PLAINS INTO THE GREAT LAKES. THE NORTHEAST PORTION OF THIS FRONT MAY  
CONTINUE TO MOVE EASTWARD THROUGH THE DAY, AS A SURFACE LOW MOVES  
ACROSS ONTARIO. TO THE SOUTHWEST, THE FRONT MAY STALL OR BEGIN TO  
MOVE NORTHWARD AS A WARM FRONT, AS A WEAK SURFACE WAVE PERSISTS OVER  
THE CENTRAL HIGH PLAINS.  
   
..UPPER MIDWEST/GREAT LAKES
 
 
POTENTIAL FOR EXTENSIVE CONVECTION ON D2/SUNDAY CREATES SOME  
UNCERTAINTY REGARDING FRONTAL POSITION ON MONDAY. LOCALLY STRONG  
STORMS MAY BE ONGOING MONDAY MORNING, WITH A GENERAL INCREASE IN  
STORM COVERAGE EXPECTED DURING THE AFTERNOON WHERE STRONG HEATING IS  
REALIZED IN THE VICINITY OF THE FRONT. STRONGER DEEP-LAYER FLOW WILL  
AGAIN BE DISPLACED TO THE COOL SIDE OF THE FRONT, BUT 30-40 KT OF  
MIDLEVEL FLOW OVERLAPPING MODERATE TO STRONG BUOYANCY WILL SUPPORT  
SOME POTENTIAL FOR ORGANIZED STORMS. MOSTLY UNIDIRECTIONAL  
SOUTHWESTERLY FLOW COULD SUPPORT ONE OR MORE FORWARD-PROPAGATING  
CLUSTERS, WITH A THREAT OF DAMAGING WIND AND ISOLATED HAIL.  
   
..CENTRAL PLAINS VICINITY
 
 
DEEP-LAYER FLOW/SHEAR WILL BE SOMEWHAT WEAKER ACROSS PARTS OF THE  
CENTRAL PLAINS, COMPARED TO AREAS FARTHER NORTHEAST. HOWEVER, STRONG  
HEATING WILL RESULT IN DEVELOPMENT OF MODERATE TO LOCALLY STRONG  
INSTABILITY. SCATTERED STORM DEVELOPMENT IS EXPECTED WITHIN A WEAKLY  
CAPPED ENVIRONMENT, AND A FEW MODESTLY ORGANIZED CELLS/CLUSTERS  
COULD EVOLVE WITH TIME, POSING A THREAT FOR STRONG TO SEVERE GUSTS  
AND ISOLATED HAIL.  
 
SOME WESTWARD MOISTURE TRANSPORT WILL BE POSSIBLE INTO PARTS OF THE  
CENTRAL HIGH PLAINS AND FRONT RANGE, WITHIN A POST-FRONTAL REGIME.  
ISOLATED STORMS MAY DEVELOP WITHIN THIS REGIME, THOUGH GENERALLY  
MODEST MIDLEVEL LAPSE RATES MAY TEND TO LIMIT ROBUST  
DESTABILIZATION.  
   
..NORTHERN NEW ENGLAND
 
 
STRONG TO EXTREME INSTABILITY WILL AGAIN RESIDE ACROSS PARTS OF THE  
NORTHEAST AND NEW ENGLAND MONDAY AFTERNOON, ALONG THE NORTHERN  
PERIPHERY OF THE UPPER RIDGE. HOWEVER, THE INFLUENCE OF THE UPPER  
RIDGE IS STILL EXPECTED TO LIMIT STORM POTENTIAL THROUGH THE DAY.  
THIS REGION WILL CONTINUE TO BE MONITORED FOR THE POSSIBILITY THAT  
STORMS DEVELOPING ACROSS QUEBEC MAY AFFECT PARTS OF NORTHERN NEW  
ENGLAND, THOUGH THIS SCENARIO IS TOO UNCERTAIN FOR SEVERE  
PROBABILITIES AT THIS TIME.  
 
..DEAN.. 06/21/2025  
 

 
 
CLICK HERE TO GO TO PREVIOUS BULLETINS.

The Nexlab SPC Page Main Text Page