962  
ACUS01 KWNS 050549  
SWODY1  
SPC AC 050547  
 
DAY 1 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK  
1247 AM CDT THU JUN 05 2025  
 
VALID 051200Z - 061200Z  
 
...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS ACROSS PORTIONS OF  
THE CENTRAL AND SOUTHERN PLAINS...  
   
..SUMMARY
 
 
SCATTERED SEVERE THUNDERSTORMS ARE EXPECTED ACROSS THE HIGH PLAINS  
FROM SOUTHWESTERN KANSAS INTO WEST TEXAS. A FEW TORNADOES, LARGE TO  
ISOLATED VERY LARGE HAIL, AND SEVERE GUSTS ARE POSSIBLE.  
   
..CENTRAL/SOUTHERN HIGH PLAINS
 
 
LARGE-SCALE PATTERN IS NOT FORECAST TO CHANGE APPRECIABLY DURING THE  
DAY1 PERIOD AS BROAD UPPER RIDGING HOLDS ACROSS NORTHEAST MEXICO  
INTO THE LOWER MS VALLEY. ALONG THE NORTHERN PERIPHERY OF THIS  
FEATURE, A FEW WEAK DISTURBANCES ARE FORECAST TO TRANSLATE ACROSS  
THE SOUTHWESTERN U.S. INTO THE SOUTHERN/CENTRAL HIGH PLAINS REGION.  
EACH OF THESE FEATURES SHOULD ENCOURAGE POTENTIALLY ROBUST, DEEP  
CONVECTION.  
 
EARLY THIS MORNING, A NOTABLE MCS HAS EVOLVED OVER THE TX PANHANDLE.  
THIS COMPLEX HAS BEEN PARTLY AIDED BY A LOW-AMPLITUDE SHORT-WAVE  
TROUGH THAT WILL TRANSLATE INTO EASTERN KS/OK LATER TODAY. WHILE  
THIS CONVECTION IS CURRENTLY WELL-ORGANIZED, WITH TIME THIS ACTIVITY  
SHOULD GRADUALLY WEAKEN DOWNSTREAM OVER WESTERN OK/NORTHWEST TX. OF  
POTENTIAL CONCERN WILL BE THE INFLUENCE ON BOUNDARY-LAYER STABILITY  
AND THE POSITION OF CONVECTIVE OUTFLOW BOUNDARIES. IF THE MCS  
CONTINUES AS CURRENTLY ANTICIPATED, A POSSIBLE DEMARCATION IN  
BUOYANCY MAY EXTEND ACROSS THE TX SOUTH PLAINS INTO FAR EASTERN NM  
BY PEAK HEATING. REMNANT OUTFLOW WILL LIKELY SERVE AS THE FOCUS FOR  
ROBUST CONVECTION LATER THIS AFTERNOON AS TEMPERATURES WARM INTO THE  
MID 80S-LOWER 90S, WEST AND SOUTH OF THE OUTFLOW. FORECAST SOUNDINGS  
ALONG THIS CORRIDOR EXHIBIT STRONG DEEP-LAYER SHEAR AND SUBSTANTIAL  
0-3KM SRH. SUPERCELLS SHOULD DEVELOP ACROSS THE SOUTHERN HIGH PLAINS  
AND VERY LARGE HAIL MAY ACCOMPANY THESE ROBUST UPDRAFTS.  
ADDITIONALLY, PROFILES APPEAR FAVORABLE FOR TORNADOES, ESPECIALLY IF  
THE AFOREMENTIONED CONVECTIVE OUTFLOW MAINTAINS SOME IDENTITY.  
 
A SECONDARY AREA OF POTENTIAL CONVECTIVE CONCENTRATION WILL BE  
ACROSS SOUTHEAST CO INTO SOUTHWEST KS. MODELS SUGGEST STRONG  
BOUNDARY-LAYER HEATING WILL DEVELOP ACROSS NORTHEAST NM INTO THE  
WESTERN OK PANHANDLE, JUST SOUTH OF A SECONDARY WEAK FRONTAL ZONE  
THAT SHOULD DRAPE ITSELF ACROSS THIS REGION. SUPERCELLS SHOULD  
EASILY DEVELOP ALONG THIS BOUNDARY THEN POSSIBLY GROW UPSCALE INTO A  
LARGER COMPLEX OF STORMS AS IT SPREADS DOWNSTREAM ALONG THE KS/OK  
BORDER AFTER SUNSET. ALL HAZARDS ARE POSSIBLE WITH THIS ACTIVITY,  
BUT ANY TORNADO THREAT WILL LIKELY BE CONCENTRATED WITH MORE  
ISOLATED SUPERCELLS EARLY IN THE CONVECTIVE EVOLUTION.  
   
..ELSEWHERE
 
 
HIGH-PW PLUME CURRENTLY STRETCHES ACROSS THE LOWER MS VALLEY-OH  
VALLEY-LOWER GREAT LAKES-SOUTHEAST CANADA. SCATTERED CONVECTION WILL  
READILY DEVELOP ALONG THIS CORRIDOR, JUXTAPOSED ALONG A WEAK FRONTAL  
ZONE. POOR LAPSE RATES SHOULD LIMIT UPDRAFT STRENGTH, BUT SOME RISK  
FOR AN ISOLATED SEVERE WIND GUST DOES EXIST.  
 
..DARROW/WENDT.. 06/05/2025  
 

 
 
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