111  
ACUS02 KWNS 291732  
SWODY2  
SPC AC 291730  
 
DAY 2 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK  
1230 PM CDT WED APR 29 2026  
 
VALID 301200Z - 011200Z  
 
...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS FROM THE TEXAS  
BIG BEND INTO THE CENTRAL TEXAS...  
   
..SUMMARY  
 
A COUPLE OF STRONG TO MARGINALLY SEVERE STORMS MAY IMPACT THE BIG  
BEND REGION INTO CENTRAL TEXAS LATE THURSDAY AFTERNOON INTO THURSDAY  
NIGHT.  
   
..SYNOPSIS  
 
STRONG MID-LEVEL WINDS WILL PERSIST ALONG/NEAR A SURFACE FRONT IN  
CENTRAL/SOUTH TEXAS. THROUGH THE PERIOD, A COMPACT SHORTWAVE TROUGH  
WILL APPROACH THE TRANS-PECOS/BIG BEND, ARRIVING LATE THURSDAY INTO  
FRIDAY MORNING. A VERY MOIST AIRMASS WILL BE IN PLACE NEAR/SOUTH OF  
THE SURFACE BOUNDARY. ISOLATED TO WIDELY SCATTERED STRONG/MARGINALLY  
SEVERE STORMS MAY OCCUR DURING THE AFTERNOON INTO THE OVERNIGHT.  
   
..HILL COUNTRY/CENTRAL TEXAS  
 
A VERY MOIST AIRMASS (MID/UPPER 60S F DEWPOINTS) NEAR AND SOUTH OF  
THE SURFACE BOUNDARY WILL BE IN PLACE. AS THIS AIRMASS INTERACTS  
WITH THE TERRAIN IN NORTHERN MEXICO, A COUPLE OF STRONG TO SEVERE  
STORMS MAY MOVE INTO THE RIO GRANDE VALLEY REGION AND INTO THE  
EDWARDS PLATEAU/HILL COUNTRY. A LESS CERTAIN SCENARIO WILL BE STORMS  
DEVELOPING ON THE BOUNDARY MORE TOWARDS PARTS OF CENTRAL TEXAS.  
GUIDANCE DOES SUGGEST SOME POTENTIAL CLOUD CLEARING AND SURFACE  
HEATING THAT COULD SUPPORT MODEST SURFACE-BASED BUOYANCY. FORCING  
FOR ASCENT WILL BE WEAK DURING THE AFTERNOON AND LARGELY DEPEND ON  
FRONTAL CONVERGENCE. IN EITHER CASE, STRONG WESTERLY MID-LEVEL FLOW  
AND SUFFICIENT MID-LEVEL LAPSE RATES WOULD SUPPORT MARGINALLY SEVERE  
HAIL WITH THE STRONGEST ACTIVITY. ADDITIONAL DEVELOPMENT COULD OCCUR  
OVERNIGHT AS THE UPPER TROUGH APPROACHES THE BIG BEND REGION. THESE  
ELEVATED STORMS WOULD POSE A SIMILAR MARGINAL HAIL THREAT.  
   
..BIG BEND  
 
DURING THE AFTERNOON, A MODEST DRYLINE FEATURE WILL BE SITUATED  
WITHIN THE PERMIAN BASIN/BIG BEND REGIONS. THIS DRYLINE CIRCULATION  
IS NOT EXPECTED TO BE OVERLY STRONG GIVEN THE CLOUD COVER  
ANTICIPATED, THOUGH DOWNSLOPE WARMING/DRYING WILL STILL LEAD TO A  
SHARP MOISTURE GRADIENT. IT IS POSSIBLE AN ISOLATED STORM OR TWO  
COULD DEVELOP ON THIS BOUNDARY, BUT CONFIDENCE IS NOT HIGH GIVEN THE  
SHORTWAVE RIDGING THAT WILL BE PRESENT DURING THE AFTERNOON. THERE  
IS HIGHER CONFIDENCE IN STORMS INITIATING WITHIN THE DAVIS MOUNTAINS  
AND NEARBY HIGHER TERRAIN IN MEXICO AS THE SHORTWAVE TROUGH  
APPROACHES OVERNIGHT THURSDAY. MOIST, UPSLOPE FLOW INTO THE REGION  
WILL INCREASE BY MID EVENING. ISOLATED TO WIDELY SCATTERED SUPERCELL  
STRUCTURES ARE POSSIBLE, THOUGH OVERALL INTENSITY OF STORMS MAY BE  
LIMITED BY THE COOLER TEMPERATURES BY THAT POINT IN THE PERIOD.  
MARGINALLY SEVERE HAIL WOULD BE THE MAIN CONCERN WITH THIS ACTIVITY.  
SOME GUIDANCE DOES SUGGEST THE DEVELOPMENT OF LINEAR STRUCTURES  
PROGRESSING EASTWARD TOWARD THE EDWARDS PLATEAU. POTENTIAL FOR WIND  
GUSTS WITH THAT ACTIVITY APPEARS LOW GIVEN NEAR-SURFACE STABILITY  
EVIDENT IN FORECAST SOUNDINGS.  
 
..WENDT.. 04/29/2026  
 
 
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