325  
ACUS02 KWNS 200456  
SWODY2  
SPC AC 200455  
 
DAY 2 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK  
1155 PM CDT SAT JUL 19 2025  
 
VALID 211200Z - 221200Z  
 
...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS MONDAY INTO  
MONDAY NIGHT ACROSS PARTS OF THE NORTHERN GREAT PLAINS AND TENNESSEE  
VALLEY INTO SOUTH ATLANTIC SEABOARD...  
   
..SUMMARY  
 
STRONG THUNDERSTORM DEVELOPMENT MAY POSE AT LEAST SOME RISK FOR  
SEVERE WIND AND HAIL ACROSS PARTS OF THE NORTHERN GREAT PLAINS AND  
PARTS OF THE SOUTHEAST MONDAY INTO MONDAY NIGHT.  
   
..SYNOPSIS  
 
MODELS CONTINUE TO INDICATE AT LEAST SOME SHEARING OF MID-LEVEL  
TROUGHING INITIALLY ACROSS THE PACIFIC NORTHWEST AT THE OUTSET OF  
THE PERIOD, BETWEEN FAIRLY PROMINENT AND PERSISTENT LOWER LATITUDE  
RIDGING ENCOMPASSING MUCH OF THE INTERIOR U.S. AND STRONGER HIGHER  
LATITUDE RIDGING CENTERED OVER THE NORTHEASTERN PACIFIC. HOWEVER,  
ONE SHORT WAVE IMPULSE EMBEDDED WITHIN THE TROUGHING MAY MAINTAIN  
FAIRLY VIGOROUS STRENGTH WHILE SLOWLY ACCELERATING NORTHEASTWARD  
INTO THE MOUNTAINS OF WESTERN MONTANA. DOWNSTREAM OF THIS  
PERTURBATION, THE INTERIOR U.S. RIDGING MAY TEND TO BUILD A BIT  
FURTHER NORTHEASTWARD ACROSS PARTS OF THE NORTHERN U.S. GREAT PLAINS  
AND UPPER MIDWEST/ADJACENT GREAT LAKES VICINITY, IN THE WAKE OF  
SIGNIFICANT MID-LEVEL TROUGHING PROGRESSING OFFSHORE OF THE NORTHERN  
U.S. AND CANADIAN ATLANTIC COAST. ANOTHER SIGNIFICANT TROUGH AND  
EMBEDDED MID-LEVEL LOW EMERGING FROM THE NORTHWESTERN CANADIAN  
ARCTIC LATITUDES IS FORECAST TO SLOWLY TURN EAST OF THE NORTHWEST  
TERRITORIES TOWARD HUDSON BAY.  
 
IN LOWER LEVELS, IT APPEARS THAT A COLD FRONT ASSOCIATED WITH THE  
HIGHER LATITUDE PERTURBATION MAY ADVANCE THROUGH THE CANADIAN  
PRAIRIES, BUT REMAIN NORTH OF THE INTERNATIONAL BORDER THROUGH THIS  
PERIOD. A PRECEDING COLD FRONT MAY PROGRESS SLOWLY SOUTHWARD  
THROUGH PORTIONS OF THE SOUTHERN MID ATLANTIC, WHILE STALLING ACROSS  
PARTS OF THE LOWER OHIO INTO MIDDLE MISSISSIPPI VALLEYS AND  
WEAKENING ACROSS THE MIDDLE MISSOURI VALLEY/NORTHERN GREAT PLAINS.  
   
..NORTHERN GREAT PLAINS  
 
BENEATH A PLUME OF WARM AND CAPPING ELEVATED MIXED-LAYER AIR, MODELS  
INDICATE THAT A SEASONABLY MOIST BOUNDARY LAYER WILL AGAIN BECOME  
CHARACTERIZED BY MODERATE TO LARGE POTENTIAL INSTABILITY ACROSS  
PARTS OF THE MIDDLE MISSOURI VALLEY AND ADJACENT GREAT PLAINS. THE  
NAM HAS BEEN MORE AGGRESSIVE IN RECENT RUNS WITH BOUNDARY-LAYER  
MOISTENING ON NORTHEASTERLY TO EASTERLY LOW-LEVEL FLOW INTO  
DEEPENING SURFACE TROUGHING ACROSS CENTRAL AND SOUTHEASTERN MONTANA.  
 
HOWEVER, ASIDE FROM THE HIGHER TERRAIN OF CENTRAL MONTANA,  
DOWNSTREAM OF THE SHORT WAVE IMPULSE EMERGING FROM THE PACIFIC  
NORTHWEST, FORCING FOR ASCENT TO SUPPORT CONVECTIVE DEVELOPMENT  
REMAINS A BIT UNCLEAR ACROSS MUCH OF THE REMAINDER OF THE NORTHERN  
GREAT PLAINS, GIVEN THE INHIBITION ASSOCIATED WITH THE ELEVATED  
MIXED-LAYER AIR.  
 
THERE DOES APPEAR AN INCREASING SIGNAL THAT A SUBTLE SHORT WAVE  
IMPULSE, MIGRATING AROUND THE WESTERN/NORTHWESTERN PERIPHERY OF THE  
STRONGER MID-LEVEL RIDGING, MAY CONTRIBUTE TO SCATTERED VIGOROUS  
HIGH-BASED THUNDERSTORM DEVELOPMENT WITHIN THE DRIER AND MORE DEEPLY  
MIXED ENVIRONMENT ACROSS PARTS OF EASTERN WYOMING AND NORTHEASTERN  
COLORADO. THIS ACTIVITY MAY POSE A RISK FOR SEVERE HAIL AND WIND  
WHILE TENDING TO ADVECT ACROSS AND NORTHEAST/EAST OF THE HIGHER  
PLAINS LATE MONDAY AFTERNOON AND EVENING.  
 
OTHERWISE, LOCALLY ENHANCED LOW-LEVEL CONVERGENCE DURING AND SHORTLY  
AFTER PEAK HEATING MIGHT WEAKEN INHIBITION SUFFICIENTLY TO SUPPORT  
ISOLATED SUPERCELL DEVELOPMENT WITHIN THE SEASONABLY MOIST/HIGHER  
CAPE ENVIRONMENT, WITH VARIOUS MODEL OUTPUT CONTINUING TO INDICATE  
ONE POSSIBLE FOCUS ACROSS PARTS OF CENTRAL OR NORTH CENTRAL SOUTH  
DAKOTA.  
   
..TENNESSEE VALLEY INTO SOUTHERN ATLANTIC SEABOARD  
 
EVEN AS THE LEAD COLD FRONT CONTINUES TO ADVANCE SOUTH OF THE  
STRONGER WESTERLIES, DESTABILIZATION ALONG AND AHEAD OF IT MAY  
BECOME CONDUCIVE TO SCATTERED UPSCALE GROWING THUNDERSTORM ACTIVITY  
POSING A RISK FOR POTENTIALLY DAMAGING WIND GUSTS BY LATE MONDAY  
AFTERNOON INTO EARLY EVENING. BASED ON MODEL OUTPUT, IT STILL  
APPEARS POSSIBLE THAT THIS COULD BE AIDED BY A REMNANT CONVECTIVELY  
GENERATED OR ENHANCED PERTURBATION EMERGING FROM THE LOWER OHIO  
VALLEY.  
 
..KERR.. 07/20/2025  
 
 
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