324  
ACUS02 KWNS 251735  
SWODY2  
SPC AC 251734  
 
DAY 2 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK  
1234 PM CDT SAT APR 25 2026  
 
VALID 261200Z - 271200Z  
 
...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS CENTRAL/EASTERN  
KANSAS...WEST-CENTRAL MISSOURI...SOUTHEAST NEBRASKA...  
   
..SUMMARY  
 
ISOLATED TO WIDELY SCATTERED SEVERE STORMS WITH POTENTIAL TO PRODUCE  
LARGE/VERY-LARGE HAIL SEVERE/DAMAGING WINDS AND A COUPLE OF STRONG  
TORNADOES ARE POSSIBLE BY EARLY SUNDAY EVENING ACROSS PARTS OF THE  
CENTRAL AND SOUTHERN GREAT PLAINS.  
   
..SYNOPSIS  
 
A SHORTWAVE TROUGH WILL EJECT INTO THE CENTRAL PLAINS LATE SATURDAY.  
A SURFACE LOW DEVELOP IN WESTERN/CENTRAL KANSAS. A DRYLINE WILL  
DRAPE SOUTH AND WESTWARD INTO OKLAHOMA AND TEXAS. A WARM FRONT WILL  
BE SITUATED WITHIN PARTS OF THE MID-MISSOURI/MID-MISSISSIPPI  
VALLEYS.  
   
..CENTRAL PLAINS INTO MID-MISSOURI VALLEY  
 
UNCERTAINTY REMAINS IN THE EXACT EVOLUTION OF CONVECTION ACROSS THE  
CENTRAL PLAINS AND MID-MISSOURI VALLEY. WHILE STRONGER MID-LEVEL  
ASCENT IS EXPECTED THIS FAR NORTH, THE TIMING OF THE SHORTWAVE  
TROUGH WILL LIKELY BE AFTER 00Z. OUTFLOW FROM CONVECTION ON SATURDAY  
WILL PLAY A ROLE IN WHERE SEVERE CONVECTION EVENTUALLY DEVELOPS. TWO  
ZONES ARE CURRENTLY EVIDENT IN MODEL GUIDANCE. ONE WILL BE ALONG  
POTENTIAL OUTFLOW NEAR THE KS/MO BORDER INTO SOUTHEAST NE WHERE A  
WEAK SURFACE LOW COULD DEVELOP. THE TRIPLE POINT AND MAIN SURFACE  
LOW IN WESTERN/CENTRAL KS WILL BE THE OTHER. SOME GUIDANCE SHOWS  
WARM ADVECTION STORMS SPREADING NORTHEASTWARD EARLY SUNDAY WHICH  
WOULD COMPLICATE THE FORECAST FOR THE MID-MISSOURI VALLEY. THERE IS  
MODESTLY HIGHER CONFIDENCE IN STORMS DEVELOPING NEAR THE MAIN  
SURFACE LOW/TRIPLE POINT. EFFECTIVE SHEAR WILL BE GREATER THAN 50  
KT, STRONG BUOYANCY OF GREATER THAN 2500 J/KG MLCAPE, AND STEEP  
MID-LEVEL LAPSE RATES WILL PROMOTE A RISK FOR LARGE/VERY-LARGE HAIL  
WITH INITIAL SUPERCELLS. THE TORNADO RISK WILL LIKELY BE MAXIMIZED  
NEAR THE TRIPLE POINT, BUT HOW LONG THE GREATER THREAT LASTS DEPENDS  
ON SPEED OF UPSCALE GROWTH. WITH TIME, ONE OR MORE CLUSTERS/LINEAR  
SEGMENTS ARE EXPECTED TO MOVE EASTWARD AND LEAD TO A GREATER  
SEVERE/DAMAGING WIND THREAT. THE SOUTHERN EXTENT OF THIS POTENTIAL  
REMAINS UNCERTAIN AS MOST GUIDANCE HAS SUGGESTED THIS ACTIVITY WILL  
BE FARTHER NORTH, MORE CLOSELY TIED TO THE EJECTING SHORTWAVE  
TROUGH.  
   
..OKLAHOMA  
 
THE LEVEL OF SEVERE RISK WILL BE HIGHLY DEPENDENT UPON WHAT OCCURS  
SATURDAY EVENING INTO SUNDAY MORNING. OUTFLOW FROM THIS ACTIVITY HAS  
THE POTENTIAL TO LIMIT DESTABILIZATION ACROSS AT LEAST PORTIONS OF  
CENTRAL/EASTERN OKLAHOMA. THIS COULD POTENTIALLY LEAVE A FAIRLY  
NARROW CORRIDOR NEAR THE DRYLINE WHERE INHIBITION WOULD BE  
MINIMIZED. THAT SAID, THE LARGE-SCALE ASCENT WILL BE NEBULOUS AT  
BEST AND OVERCOMING THE CAP WILL LARGELY BE DEPENDENT ON STRONG  
HEATING ALONG THE DRYLINE. THE NOSE OF THE MID-LEVEL JET WILL MOVE  
INTO THE TEXAS PANHANDLE/WESTERN OKLAHOMA BY LATE AFTERNOON. LOCALLY  
STRONGER CONVERGENCE ALONG THE DRYLINE MAY BE ENOUGH TO INITIATE AN  
ISOLATED STORM OR TWO. THIS SCENARIO REMAINS QUITE UNCERTAIN AS  
GUIDANCE UNIFORMLY DOES NOT CONVECT ALONG THE DRYLINE. GIVEN GREATER  
THAN 50 KT DEEP-LAYER SHEAR PERPENDICULAR TO THE DRYLINE, STEEP  
MID-LEVEL LAPSE RATES, AND STRONG LOW-LEVEL SHEAR (ESPECIALLY DURING  
THE EVENING), STORMS WOULD BE CAPABLE OF ALL SEVERE HAZARDS --  
INCLUDING VERY-LARGE HAIL AND A STRONG TORNADO -- SHOULD THEY  
DEVELOP.  
   
..LOWER MISSISSIPPI VALLEY  
 
A REMNANT MCV FROM CONVECTION ON SATURDAY IN OK/NORTHEAST TEXAS WILL  
LIKELY MOVE SOUTHEASTWARD DURING THE DAY. MODERATE MID,  
NORTHWESTERLY MID-LEVEL WINDS WILL ALLOW FOR SOME CONTINUED STORM  
ORGANIZATION. THE MAIN QUESTION WILL BE HOW MUCH DESTABILIZATION  
WILL OCCUR AHEAD OF THIS FEATURE. FURTHERMORE, WEAKENING 850 MB  
WINDS WILL HAVE TO OVERCOME BY COLD POOL ORGANIZATION. AT LEAST  
ISOLATED WIND DAMAGE AND LARGE HAIL WOULD BE POSSIBLE.  
   
..NORTHWEST TEXAS INTO EDWARDS PLATEAU/HILL COUNTRY  
 
STORM INITIATION ALONG THE DRYLINE IS NOT CERTAIN GIVEN THE LACK OF  
FORCING ALOFT. HOWEVER, STRONG HEATING COULD PROMOTE ISOLATED  
DEVELOPMENT. SHEAR WOULD BE SUFFICIENT FOR SUPERCELLS AND STEEP  
LAPSE RATES THROUGH THE MIDDLE TROPOSPHERE WOULD PROMOTE A THREAT  
FOR LARGE/VERY-LARGE HAIL AS WELL AS SEVERE WINDS.  
 
..WENDT.. 04/25/2026  
 
 
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