942  
ACUS02 KWNS 111710  
SWODY2  
SPC AC 111709  
 
DAY 2 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK  
1209 PM CDT MON AUG 11 2025  
 
VALID 121200Z - 131200Z  
 
...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS TUESDAY INTO  
TUESDAY NIGHT ACROSS PARTS OF EASTERN WISCONSIN...UPPER AND LOWER  
MICHIGAN...AND PARTS OF NORTHEASTERN ILLINOIS...NORTHERN  
INDIANA...NORTHWESTERN OHIO...  
   
..SUMMARY  
 
STRONG THUNDERSTORMS MAY IMPACT PARTS OF THE UPPER GREAT LAKES  
REGION TUESDAY INTO TUESDAY EVENING, ACCOMPANIED BY AT LEAST SOME  
RISK FOR SEVERE WIND AND HAIL.  
   
..DISCUSSION  
 
THE WESTERLIES WILL REMAIN CONFINED TO THE NORTHERN MID-LATITUDES,  
BUT MODELS SUGGEST THAT FLOW NEAR/NORTH OF THE CANADIAN/U.S. BORDER  
WILL TREND A BIT MORE ZONAL, AS AN INITIALLY PROMINENT MID-LEVEL  
HIGH CENTERED OFFSHORE OF THE PACIFIC NORTHWEST CONTINUES TO BECOME  
SUPPRESSED WEST-SOUTHWESTWARD ACROSS THE NORTHEASTERN PACIFIC.  
WITHIN THIS REGIME, MODELS CONTINUE TO INDICATE THE CONSOLIDATION OF  
SEVERAL SHORT WAVE PERTURBATIONS INTO LARGER-SCALE MID-LEVEL  
TROUGHING ACROSS ONTARIO INTO QUEBEC BY LATE TUESDAY NIGHT,  
ACCOMPANIED BY SIGNIFICANT SURFACE CYCLOGENESIS ACROSS FAR NORTHERN  
ONTARIO INTO THE SOUTHERN HUDSON/JAMES BAY VICINITY.  
 
IN LOWER LEVELS, A MODEST INITIAL INTRUSION OF COOLER/DRIER AIR MAY  
OVERSPREAD MUCH OF THE DAKOTAS AND PORTIONS OF THE UPPER MIDWEST AND  
ADJACENT GREAT LAKES REGION BY 12Z TUESDAY, BEFORE SLOWLY ADVANCING  
EAST-SOUTHEASTWARD ACROSS THE UPPER GREAT LAKES AND EVENTUALLY BEING  
OVERTAKEN BY A MORE SUBSTANTIVE COOL INTRUSION LATER TUESDAY THROUGH  
TUESDAY NIGHT. COMPLICATING MATTERS WITH RESPECT TO  
DESTABILIZATION, GUIDANCE CONTINUES TO INDICATE THAT THE LEAD FRONT  
WILL BE PRECEDED BY A STALLED LINGERING REMNANT FRONTAL ZONE, WHICH  
MAY STILL BE REINFORCED BY CONVECTIVE PRECIPITATION/OUTFLOW ACROSS  
PARTS OF SOUTHERN LOWER MICHIGAN AND NORTHERN ILLINOIS, INTO THE  
LOWER MISSOURI VALLEY AND THE SOUTHERN GREAT PLAINS, AT THE OUTSET  
OF THE PERIOD.  
   
..UPPER GREAT LAKES  
 
SHORT WAVE DEVELOPMENTS WITHIN THE EVOLVING PATTERN REMAIN UNCLEAR  
DUE TO SPREAD WITHIN THE VARIOUS MODEL OUTPUT, BUT GUIDANCE  
CONTINUES TO INDICATE THAT ONE NOTABLE SHORT WAVE IMPULSE WILL  
CONTINUE DIGGING ACROSS PARTS OF THE UPPER MIDWEST AND ADJACENT  
GREAT LAKES REGION DURING THE DAY TUESDAY, BEFORE PIVOTING ACROSS  
AND EAST-NORTHEAST OF LAKE HURON/GEORGIAN BAY. IT APPEARS THAT THIS  
MAY BE PRECEDED BY ONE OR TWO CONVECTIVELY GENERATED PERTURBATIONS  
WHICH WILL BECOME INCREASING SHEARED WHILE MERGING INTO THE  
SOUTHWESTERLY CYCLONIC MID-LEVEL REGIME OVERSPREADING THE GREAT  
LAKES VICINITY.  
 
AS THIS OCCURS, VARIOUS MODEL OUTPUT (NOTABLY INCLUDING CALIBRATED  
THUNDERSTORM PROBABILITY GUIDANCE FROM THE HIGH RESOLUTION ENSEMBLE  
SYSTEM) SUGGESTS THAT DESTABILIZATION AND FORCING FOR ASCENT WILL  
BECOME SUPPORTIVE OF A COUPLE OF CORRIDORS OF INCREASING  
THUNDERSTORM DEVELOPMENT BY LATE TUESDAY AFTERNOON. THESE GENERALLY  
COINCIDE WITH THE STALLED REMNANT FRONTAL ZONE ACROSS PARTS OF  
SOUTHEASTERN LOWER MICHIGAN INTO NORTHEASTERN ILLINOIS AND THE  
INITIAL COLD FRONT ADVANCING ACROSS UPPER MICHIGAN/EASTERN  
WISCONSIN.  
 
ALONG THE SOUTHERN BOUNDARY, WHICH MAY STRENGTHEN SOME WITH  
DIFFERENTIAL SURFACE HEATING, MID-LEVEL THERMODYNAMIC PROFILES MAY  
BE RELATIVELY WARM WITH WEAK LAPSE RATES. HOWEVER, IT STILL APPEARS  
THAT SEASONABLY HIGH BOUNDARY-LAYER MOISTURE CONTENT, COUPLED WITH  
DAYTIME HEATING, WILL CONTRIBUTE TO SIZABLE CAPE. COINCIDING WITH A  
BELT OF STRENGTHENING SOUTHWESTERLY LOWER/MID-LEVEL FLOW (INCLUDING  
30-40 KT IN THE 700-500 MB LAYER), THE ENVIRONMENT MAY BECOME  
CONDUCIVE TO ORGANIZED CONVECTION, INCLUDING EVOLVING SUPERCELL  
STRUCTURES AND UPSCALE GROWING CLUSTERS WITH POTENTIAL TO PRODUCE  
STRONG TO SEVERE WIND GUSTS BY LATE TUESDAY AFTERNOON INTO EVENING.  
 
ACROSS UPPER MICHIGAN INTO EASTERN WISCONSIN, PRE-FRONTAL  
DESTABILIZATION REMAINS MORE UNCLEAR DUE TO THE POSSIBLE INFLUENCE  
OF CONVECTIVE CLOUD COVER AND/OR OUTFLOW. BUT, WITH BREAKS IN CLOUD  
COVER ALLOWING FOR A NARROW CORRIDOR OF HEATING, COOLING ALOFT AND  
STRENGTHENING SHEAR ALONG THE FRONTAL ZONE MIGHT CONTRIBUTE TO AN  
ENVIRONMENT CONDUCIVE TO STRONG THUNDERSTORM DEVELOPMENT WITH  
POTENTIAL TO PRODUCE MARGINALLY SEVERE HAIL AND LOCALIZED STRONG  
SURFACE GUSTS LATE TUESDAY AFTERNOON.  
   
..SOUTHWEST  
 
FORECAST DEEP-LAYER MEAN WIND FIELDS ARE GENERALLY LIGHT, BUT  
INCLUDE A WEST-NORTHWESTERLY UPSLOPE COMPONENT TO THE LOW-LEVEL FLOW  
BENEATH NORTH-NORTHEASTERLY MID-LEVEL FLOW. THIS MAY AID  
PROPAGATION OF CONVECTION OFF THE HIGHER TERRAIN OF SOUTHWESTERN NEW  
MEXICO AND SOUTHEASTERN ARIZONA, INTO LOWER ELEVATIONS WITH A WARM  
AND DEEPLY MIXED BOUNDARY LAYER CHARACTERIZED BY MODEST POTENTIAL  
INSTABILITY BY LATE TUESDAY AFTERNOON. AS THIS OCCURS, A FEW STRONG  
TO SEVERE DOWNBURSTS AND GUSTS ALONG STRENGTHENING OUTFLOWS APPEARS  
POSSIBLE.  
 
..KERR.. 08/11/2025  
 
 
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