297  
ACUS02 KWNS 030535  
SWODY2  
SPC AC 030533  
 
DAY 2 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK  
1233 AM CDT FRI JUL 03 2026  
 
VALID 041200Z - 051200Z  
 
...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS SATURDAY AFTERNOON  
INTO SATURDAY NIGHT ACROSS PARTS OF THE OHIO VALLEY INTO MID  
ATLANTIC AND ACROSS PARTS OF THE CENTRAL GREAT PLAINS...  
   
..SUMMARY  
 
CLUSTERS OF STORMS MAY EVOLVE ACROSS PARTS OF THE ALLEGHENY PLATEAU  
INTO MID ATLANTIC AND ACROSS THE CENTRAL GREAT PLAINS SATURDAY  
AFTERNOON AND EVENING, POSING A RISK FOR DAMAGING WIND GUSTS. LARGE  
HAIL IS ALSO POSSIBLE ACROSS THE GREAT PLAINS  
   
..DISCUSSION  
 
MODELS INDICATE THAT A REMNANT MID-LEVEL HIGH, NOW CENTERED NEAR OR  
JUST EAST THE SOUTHERN APPALACHIANS, WILL BECOME SUPPRESSED BY THE  
BEGINNING OF THIS PERIOD. A NEW HIGH MAY BECOME A BIT MORE  
PROMINENT UPSTREAM, NEAR AND TO THE LEE OF THE SOUTHERN ROCKIES,  
WITH RIDGING ALSO BUILDING TO ITS NORTHWEST, FROM PORTIONS OF THE  
EASTERN GREAT BASIN THROUGH PORTIONS OF THE MID MISSOURI VALLEY. TO  
THE EAST OF THIS RIDGING, WEAK INITIALLY ZONAL FLOW MAY TRANSITION  
TO A BROADLY CYCLONIC REGIME ACROSS THE UPPER MIDWEST AND LOWER  
MISSOURI INTO OHIO VALLEYS. STRONGER WESTERLIES ARE LIKELY TO  
REMAIN CONFINED TO HIGHER LATITUDES, BUT ONE EMBEDDED LARGER-SCALE  
TROUGH IS FORECAST TO DIG ACROSS THE CANADIAN MARITIMES AND NEW  
ENGLAND SATURDAY THROUGH SATURDAY NIGHT.  
 
IN LOWER LEVELS, MORE SUBSTANTIVE COOLING/DRYING MAY OVERSPREAD MUCH  
OF NORTHERN NEW ENGLAND DURING THE DAY, AND PERHAPS THE ADIRONDACKS  
VICINITY AND PORTIONS OF THE UPPER GREAT LAKES BY LATE SATURDAY  
NIGHT. HOWEVER, THIS MAY BE PRECEDED BY A DIFFUSE/WEAK FRONT,  
PERHAPS AUGMENTED BY CONVECTIVE OUTFLOW IS SOME LOCATIONS, ADVANCING  
SOUTHWARD ACROSS THE MID ATLANTIC, OHIO AND LOWER MISSOURI VALLEYS  
AND CENTRAL GREAT PLAINS THROUGH THE PERIOD.  
 
ALONG AND SOUTH OF THE LEAD FRONT/CONVECTIVE OUTFLOW, A  
BOUNDARY-LAYER CHARACTERIZED BY SEASONABLY HIGH MOISTURE CONTENT MAY  
AGAIN BECOME CHARACTERIZED BY LARGE POTENTIAL INSTABILITY WITH  
DAYTIME HEATING. THIS WILL PROBABLY BECOME SUPPORTIVE OF WIDELY  
SCATTERED TO SCATTERED STRONG THUNDERSTORM DEVELOPMENT POSING AT  
LEAST SOME SEVERE WEATHER RISK. THE MAGNITUDE/AREAL COVERAGE OF  
THIS POTENTIAL REMAINS UNCERTAIN, AND WILL LARGELY BE INFLUENCED BY  
SUB-SYNOPTIC DEVELOPMENTS THAT ARE OF LOW PREDICTABILITY AT THIS  
EXTENDED TIME FRAME, AS EVIDENCED BY SIZABLE MODEL SPREAD STILL  
APPARENT IN LATEST MODEL OUTPUT, INCLUDING CONVECTION-ALLOWING  
GUIDANCE.  
   
..ALLEGHENY PLATEAU INTO MID ATLANTIC  
 
POTENTIAL CONVECTIVE EVOLUTION REMAINS UNCERTAIN, WITH FORCING FOR  
ASCENT TO SUPPORT THUNDERSTORM DEVELOPMENT UNCLEAR. HOWEVER, THERE  
APPEARS SOME GENERAL CONSENSUS IN MODEL OUTPUT THAT AT LEAST  
SCATTERED THUNDERSTORM DEVELOPMENT WILL INITIATE IN RESPONSE TO  
DAYTIME BOUNDARY-LAYER DESTABILIZATION ACROSS THE ALLEGHENY PLATEAU,  
AS MID-LEVEL HEIGHTS SUBTLY BEGIN TO FALL. THIS IS FORECAST TO  
DEVELOP EASTWARD ACROSS THE MID ATLANTIC BY EARLY EVENING.  
 
GIVEN THE DEGREE OF INSTABILITY FORECAST, AND POSSIBLY A BELT OF  
CONVECTIVELY AUGMENTED FLOW (INCLUDING 30-40 KT IN THE 850-500 MB  
LAYER) SPREADING EAST-SOUTHEAST OF THE LOWER GREAT LAKES/UPPER OHIO  
VALLEY VICINITY, THERE APPEARS POTENTIAL FOR ONE OR TWO ORGANIZING  
CLUSTERS CAPABLE OF PRODUCING DAMAGING WIND GUSTS TO EVOLVE.  
   
..CENTRAL GREAT PLAINS  
 
GIVEN THE POSSIBLE GENERAL TENDENCY FOR LARGER-SCALE MID-LEVEL  
HEIGHT RISES ACROSS THE ROCKIES AND ADJACENT GREAT PLAINS, AND  
SPREAD EVIDENT IN MODEL OUTPUT, CONVECTIVE POTENTIAL FOR THIS PERIOD  
REMAINS UNCERTAIN. HOWEVER, LINGERING CONVECTIVELY GENERATED OR  
AUGMENTED PERTURBATIONS WITHIN EVOLVING NORTHWESTERLY MID-LEVEL FLOW  
COULD SUPPORT WIDELY SCATTERED STRONG TO SEVERE THUNDERSTORM  
DEVELOPMENT, INCLUDING A FEW SUPERCELLS BY EARLY SATURDAY EVENING.  
THIS MAY BE FOCUSED IN MOISTENING SOUTHEASTERLY LOW-LEVEL FLOW  
ACROSS PARTS OF NORTHEASTERN COLORADO AND WESTERN NEBRASKA, AND NEAR  
A ZONE OF STRENGTHENING DIFFERENTIAL HEATING ON THE SOUTHWESTERN  
FLANK OF A STALLED OUTFLOW BOUNDARY ACROSS WESTERN INTO CENTRAL  
KANSAS.  
 
WARM ADVECTION AND CONVERGENCE NEAR THE NOSE OF A NOCTURNALLY  
STRENGTHENING SOUTHERLY LOW-LEVEL JET, WITH BOUNDARY-LAYER  
DECOUPLING ACROSS THE OKLAHOMA/TEXAS PANHANDLE VICINITY INTO  
SOUTHWESTERN KANSAS, SEEMS TO OFFER THE BEST SUPPORT FOR A POSSIBLE  
UPSCALE GROWING CLUSTER, WHICH COULD MAINTAIN A RISK FOR LARGE HAIL  
AND STRONG TO SEVERE SURFACE GUSTS INTO SATURDAY NIGHT.  
 
..KERR.. 07/03/2026  
 
 
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