206  
ACUS02 KWNS 170533  
SWODY2  
SPC AC 170530  
 
DAY 2 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK  
1230 AM CDT THU SEP 17 2026  
 
VALID 181200Z - 191200Z  
 
...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS FRIDAY INTO  
FRIDAY NIGHT ACROSS PARTS OF THE NORTHERN INTERMOUNTAIN WEST...THE  
CENTRAL GREAT PLAINS INTO SOUTHERN PORTIONS OF THE MIDDLE MISSOURI  
VALLEY...AND PIEDMONT OF CAROLINAS INTO GEORGIA...  
   
..SUMMARY
 
 
AREAS OF SCATTERED STRONG THUNDERSTORM DEVELOPMENT POSING AT LEAST  
SOME RISK FOR SEVERE HAIL OR WIND APPEAR POSSIBLE ACROSS PARTS OF  
THE NORTHERN INTERMOUNTAIN WEST INTO THE CENTRAL GREAT PLAINS AND  
SOUTHERN MIDDLE MISSOURI VALLEY, AND PORTIONS OF THE CAROLINA INTO  
GEORGIA PIEDMONT FRIDAY AFTERNOON AND EVENING.  
   
..DISCUSSION
 
 
LATEST MODEL OUTPUT CONTINUES TO INDICATE THAT LARGER-SCALE  
MID-LEVEL TROUGHING, WITH A VIGOROUS LEAD EMBEDDED SHORT WAVE  
IMPULSE, WILL DIG ACROSS THE NORTHERN ATLANTIC SEABOARD ACCOMPANIED  
BY SIGNIFICANT SURFACE CYCLOGENESIS NEAR AND EAST OF THE CANADIAN  
MARITIMES THROUGH THIS PERIOD. IN THE WAKE OF THE CYCLONE, IT  
APPEARS THAT A COLD FRONT WILL CONTINUE ADVANCING OFFSHORE AND  
THROUGH THE SOUTHERN MID ATLANTIC SEABOARD, BEFORE BECOMING  
QUASI-STATIONARY BENEATH THE NORTHERN PERIPHERY OF PERSISTENT  
MID-LEVEL RIDGING, ACROSS THE LOWER OHIO THROUGH LOWER AND MIDDLE  
MISSOURI VALLEYS.  
 
UPSTREAM OF THE MID-LEVEL RIDGE, A MID-LEVEL TROUGH AND EMBEDDED LOW  
ARE FORECAST TO SLOWLY PROGRESS ACROSS THE INTERMOUNTAIN WEST  
THROUGH ROCKIES VICINITY, PRECEDED BY A COUPLE OF MORE SUBTLE  
PERTURBATIONS MIGRATING AROUND THE NORTHWESTERN THROUGH NORTHERN  
PERIPHERY OF THE RIDGE.  
   
..PIEDMONT OF CAROLINAS INTO GEORGIA
 
 
LOW-LEVEL LAPSE RATES MAY BECOME RATHER STEEP BY FRIDAY AFTERNOON,  
WITHIN PRE-FRONTAL SURFACE TROUGHING TO THE LEE OF THE SOUTHERN  
APPALACHIANS, WHERE A RELATIVELY MOIST AND MIXED BOUNDARY-LAYER  
MIGHT BECOME CHARACTERIZED BY CAPE ON THE ORDER OF 1000-2000 J/KG.  
PERHAPS AIDED BY FORCING FOR ASCENT ASSOCIATED WITH A CONVECTIVELY  
AUGMENTED PERTURBATION, STORMS MAY INCREASE OFF THE HIGHER TERRAIN  
AND POSE A RISK FOR LOCALIZED DOWNBURSTS. IT APPEARS POSSIBLE THAT  
ACTIVITY COULD EVENTUALLY CONSOLIDATE INTO A SOUTHWARD/SOUTHWESTWARD  
PROPAGATING CLUSTER, WITH THE COLD POOL STRENGTHENING SUFFICIENTLY  
TO MAINTAIN A RISK FOR POTENTIALLY DAMAGING WIND GUSTS INTO FRIDAY  
EVENING, DESPITE THE WEAKNESS OF THE AMBIENT DEEP-LAYER MEAN FLOW.  
   
..NORTHERN INTERMOUNTAIN WEST AND ADJACENT ROCKIES
 
 
BENEATH THE LEADING EDGE OF THE COLD CORE OF THE MID-LEVEL LOW, COOL  
THERMODYNAMIC PROFILES, WITH AT LEAST MODESTLY STEEP MID-LEVEL LAPSE  
RATES, MAY CONTRIBUTE TO SCATTERED STRONG STORMS CAPABLE OF  
PRODUCING SEVERE HAIL FRIDAY AFTERNOON, IN THE PRESENCE OF STRONG  
DEEP-LAYER SHEAR AND DIFLUENT MID/UPPER FLOW.  
   
..GREAT PLAINS INTO MIDDLE MISSOURI VALLEY
 
 
CONVECTIVE POTENTIAL REMAINS UNCERTAIN, WITH THE TIMING OF THE SHORT  
WAVE PERTURBATIONS IMPACTING THE REGION UNCLEAR.  
 
THE LATEST MODEL OUTPUT, INCLUDING CONVECTION-ALLOWING AND RELATED  
GUIDANCE, SUGGEST THAT FORCING FOR ASCENT WITH A SECONDARY IMPULSE  
MAY NOT BEGIN TO EMERGE FROM THE RATON MESA VICINITY UNTIL FRIDAY  
EVENING. HOWEVER, THE REMNANTS OF A VERY WARM AND DEEPLY  
MIXED-BOUNDARY LAYER WITHIN THE LEE SURFACE TROUGHING MAY STILL BE  
CONDUCIVE TO A FEW STRONG DOWNBURSTS NEAR CONVECTION OVERSPREADING  
SOUTHEASTERN COLORADO THROUGH AT LEAST PORTIONS OF WESTERN KANSAS  
BEFORE WEAKENING LATER FRIDAY NIGHT.  
 
CLOSER TO A WEAK FRONTAL WAVE/WARM FRONTAL ZONE ACROSS PARTS OF  
EASTERN NEBRASKA INTO WESTERN IOWA AND NORTHWESTERN MISSOURI, A  
CORRIDOR OF MODERATE TO LARGE CAPE WILL CONTRIBUTE TO AN ENVIRONMENT  
CONDITIONALLY SUPPORTIVE OF ORGANIZED STRONG THUNDERSTORM  
DEVELOPMENT. HOWEVER, FORCING FOR ASCENT TO SUPPORT BOUNDARY-LAYER  
BASED THUNDERSTORMS REMAINS UNCLEAR THROUGH LATE FRIDAY AFTERNOON.  
BY MID TO LATE EVENING, IF NOT EARLIER, WARM ADVECTION ALONG A  
NOCTURNALLY STRENGTHENING BOUNDARY-LAYER JET, BENEATH AN  
INCREASINGLY DIVERGENT UPPER REGIME, MAY SUPPORT AN EVOLVING  
SUPERCELL STRUCTURE AND SMALL UPSCALE GROWING CLUSTER. THIS MAY  
STILL OCCUR MOSTLY ABOVE A STABLE AND/OR STABILIZING BOUNDARY-LAYER,  
BUT THE ENVIRONMENT MIGHT STILL BE CONDUCIVE TO THE DEVELOPMENT OF A  
FEW STRONG SURFACE GUSTS. RELATIVELY WARM THERMODYNAMIC PROFILES  
SEEM LIKELY TO MINIMIZE THE RISK FOR SEVERE HAIL.  
 
..KERR.. 09/17/2026  
 

 
 
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