039  
ACUS01 KWNS 181953  
SWODY1  
SPC AC 181952  
 
DAY 1 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK  
0252 PM CDT TUE MAR 18 2025  
 
VALID 182000Z - 191200Z  
 
...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS TONIGHT ACROSS  
PARTS OF SOUTHEASTERN NEBRASKA THROUGH SOUTHWESTERN AND CENTRAL  
IOWA...  
   
..SUMMARY
 
 
ISOLATED, MARGINALLY SEVERE HAIL IS POSSIBLE BY LATE TONIGHT IN A  
CORRIDOR FROM NORTH CENTRAL KANSAS THROUGH CENTRAL IOWA.  
   
..20Z UPDATE
 
 
THE MARGINAL RISK AREA WAS EXPANDED SLIGHTLY EASTWARD INTO  
EAST-CENTRAL IOWA. ANY ELEVATED THUNDERSTORM CLUSTERS THAT EVOLVE  
AND TRACK EAST-NORTHEASTWARD ALONG THE WARM FRONT (AS INDICATED BY  
THE LATEST MPAS RUNS) WILL POSE AN ISOLATED SEVERE-HAIL RISK INTO  
THIS AREA. FOR ADDITIONAL DETAILS, SEE THE PREVIOUS DISCUSSION  
BELOW.  
 
..WEINMAN.. 03/18/2025  
   
PREV DISCUSSION
 
/ISSUED 1123 AM CDT TUE MAR 18 2025/  
   
..DISCUSSION
 
 
MUCH OF THE NATION REMAINS UNDER THE INFLUENCE OF ONE PROMINENT BELT  
OF WESTERLIES EMANATING FROM THE NORTHERN MID-LATITUDE PACIFIC.  
WITHIN THIS REGIME, MID-LEVEL TROUGHING IS IN THE PROCESS OF DIGGING  
ACROSS THE INTERMOUNTAIN WEST AND ROCKIES. THIS INCLUDES ONE  
SIGNIFICANT EMBEDDED SMALLER-SCALE PERTURBATION APPROACHING THE  
SOUTHERN ROCKIES, WHICH IS FORECAST TO ACCELERATE EAST-NORTHEASTWARD  
ACROSS THE SOUTH CENTRAL GREAT PLAINS BY LATE TONIGHT.  
 
MODELS INDICATE THAT THIS WILL BE ACCOMPANIED BY A STRONG MID/UPPER  
JET STREAK, INCLUDING A CORE INTENSIFYING IN EXCESS OF 100 KT AROUND  
500 MB, NOSING ACROSS THE TEXAS PANHANDLE VICINITY THROUGH THE LOWER  
MISSOURI VALLEY FROM EARLY THIS EVENING THROUGH 12Z WEDNESDAY. IT  
APPEARS THAT THIS MAY BE ACCOMPANIED BY SUBSTANTIVE FURTHER  
DEEPENING OF A DEVELOPING LOW ACROSS CENTRAL THROUGH NORTHEASTERN  
KANSAS, WITHIN ALREADY DEEP SURFACE TROUGHING NOW PRESENT ACROSS THE  
CENTRAL/SOUTHERN GREAT PLAINS INTO LOWER/MIDDLE MISSOURI VALLEY.  
 
IN THE WAKE OF THE PRIOR CYCLONE WHICH IMPACTED MUCH OF THE CENTRAL  
AND EASTERN U.S. AND GULF BASIN LATE LAST WEEK INTO THE WEEKEND,  
BOUNDARY-LAYER MOISTENING ACROSS THE WESTERN GULF IS UNDERWAY, BUT  
STILL ONLY SUPPORTIVE OF RATHER MODEST LOW-LEVEL MOISTENING ACROSS  
THE TEXAS GULF COAST INTO SOUTHEASTERN GREAT PLAINS (INCLUDING LOW  
TO MID 50S F SURFACE DEW POINTS). IT APPEARS THAT THIS WILL REACH  
PORTIONS OF THE LOWER CENTRAL GREAT PLAINS INTO UPPER MIDWEST LATE  
THIS EVENING THROUGH EARLY WEDNESDAY. HOWEVER, RELATIVELY WARM AND  
DRY AIR IN THE LOWER/MID-TROPOSPHERE, ASSOCIATED WITH A BROAD PLUME  
OF ELEVATED MIXED-LAYER AIR OVERSPREADING THE CENTRAL/SOUTHERN GREAT  
PLAINS AND MIDDLE/LOWER MISSISSIPPI VALLEY, WILL TEND TO IMPEDE AN  
APPRECIABLE RISK FOR THUNDERSTORM DEVELOPMENT.  
   
..CENTRAL GREAT PLAINS TOWARD THE UPPER MIDWEST
 
 
PERHAPS AS EARLY AS LATE THIS EVENING, INTO THE OVERNIGHT HOURS,  
MODEL OUTPUT CONTINUES TO INDICATE THAT STRENGTHENING MID/UPPER  
FORCING FOR ASCENT, COUPLED WITH BETTER LOW-LEVEL MOISTURE RETURN,  
WILL OVERCOME THE INHIBITION AND SUPPORT A CORRIDOR OF THUNDERSTORM  
DEVELOPMENT. THIS LIKELY WILL BE FOCUSED WITHIN STRENGTHENING  
LOWER/MID-TROPOSPHERIC WARM ADVECTION, ALONG A FRONTAL ZONE  
EXTENDING TO THE EAST-NORTHEAST OF THE SURFACE CYCLONE, ACROSS  
SOUTHEASTERN NEBRASKA THROUGH CENTRAL IOWA BY LATE TONIGHT.  
 
BASED AT LEAST ON THE LATEST NAM, IT APPEARS THAT THE MORE SUSTAINED  
AND STRONGER THUNDERSTORM DEVELOPMENT MAY INITIATE AS EARLY AS LATE  
EVENING NEAR/EAST-NORTHEAST OF THE CONCORDIA KS VICINITY, BEFORE  
SPREADING NORTHEASTWARD. THIS SEEMS LIKELY TO OCCUR AS CONVECTION  
BEGINS TO BECOME INCREASINGLY ROOTED BELOW THE 700 MB LEVEL, CLOSER  
TO 850 MB, WITH SOUNDINGS PERHAPS BECOMING CHARACTERIZED BY "LOADED  
GUN" THERMODYNAMIC PROFILES ABOVE THE NEAR-SURFACE STABLE LAYER.  
 
ALTHOUGH MOST UNSTABLE CAPE MAY MOSTLY PEAK IN THE 500-750 J/KG  
RANGE, STRONGER CELLS MAY BECOME CONDUCIVE TO MARGINALLY SEVERE  
HAIL, AIDED BY STRONG SHEAR IN THE CONVECTIVE LAYER.  
 
THE POTENTIAL FOR STRONG SURFACE GUSTS IS SOMEWHAT MORE UNCERTAIN.  
ALTHOUGH THE RISK FOR STRONG DOWNDRAFTS TO REACH THE SURFACE APPEARS  
NEGLIGIBLE, GRAVITY WAVE INDUCED SURFACE PRESSURE PERTURBATIONS  
SUPPORTIVE OF GUSTY WINDS MAY NOT BE ENTIRELY OUT OF THE QUESTION.  
 

 
 
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