091  
ACUS03 KWNS 020718  
SWODY3  
SPC AC 020717  
 
DAY 3 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK  
0217 AM CDT SUN AUG 02 2026  
 
VALID 041200Z - 051200Z  
 
...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS OVER SOUTHEAST  
ARIZONA...  
   
..SUMMARY  
 
WIDELY SCATTERED SEVERE STORMS CAPABLE OF SEVERE WIND GUSTS APPEAR  
POSSIBLE IN SOUTHEAST ARIZONA TUESDAY AFTERNOON AND EVENING.  
   
..SYNOPSIS  
 
A BROAD, CYCLONIC FLOW REGIME IS FORECAST FROM THE NORTHERN ROCKIES  
INTO THE GREAT LAKES, TO THE NORTH OF AN ELONGATING UPPER HIGH OVER  
THE LOWER CO VALLEY INTO THE SOUTHERN ROCKIES. WITHIN THAT PATTERN,  
THERE IS A MODEL SIGNAL THAT A LOW-AMPLITUDE DISTURBANCE AND  
ASSOCIATED MID-LEVEL WIND MAXIMUM WILL MOVE THROUGH THE MID MO  
VALLEY TUESDAY NIGHT. AT THE SURFACE, A FRONT WILL PROGRESS THROUGH  
PORTIONS OF THE UPPER GREAT LAKES WITH THE BOUNDARY TRAILING  
SOUTHWEST THROUGH THE MID MO VALLEY TO AN AREA OF LOW PRESSURE OVER  
THE CENTRAL HIGH PLAINS.  
 
   
..SOUTHEAST ARIZONA  
 
A SIMILAR SETUP TO THAT ON MONDAY IS EXPECTED TUESDAY AFTERNOON WITH  
A DEEP, WELL-MIXED BOUNDARY LAYER AND MODERATE INSTABILITY ENHANCING  
DOWNDRAFT POTENTIAL AS STORMS MOVE INTO THE LOWER DESERT. SLIGHTLY  
STRONGER EASTERLY MID-LEVEL FLOW MAY BOOST DEEP-LAYER SHEAR TO  
AROUND 30 KT, POTENTIALLY LEADING TO SOME COLD POOL ORGANIZATION AND  
AN ASSOCIATED THREAT FOR A FEW SEVERE WIND GUSTS.  
 
   
..MID MISSOURI VALLEY  
 
ELEVATED THUNDERSTORMS MAY BE ONGOING TUESDAY MORNING NORTH OF THE  
SURFACE FRONT WITH THE POTENTIAL FOR LINGERING CLOUDS TO LIMIT AIR  
MASS DESTABILIZATION IN SOME AREAS. A CORRIDOR OF MODERATE  
INSTABILITY MAY DEVELOP SOUTH OF THE FRONT BY AFTERNOON FROM  
NORTHEAST KS INTO SOUTHERN IA; HOWEVER, THE ABSENCE OF APPRECIABLE  
FORCING MECHANISMS LEADS TO CONSIDERABLE UNCERTAINTY IN WHETHER ANY  
SURFACE-BASED STORMS WILL DEVELOP DURING THE DAYLIGHT HOURS.  
 
THERE IS A GREATER CONFIDENCE IN ELEVATED STORM POTENTIAL TUESDAY  
NIGHT NORTH OF THE FRONT WITH THE APPROACH OF THE MID-LEVEL  
DISTURBANCE. WHILE THERE IS SOME MODEL VARIANCE WITH RESPECT TO THE  
DEGREE OF ELEVATED INSTABILITY, THE GENERAL CONSENSUS IS FOR MUCAPE  
LESS THAN 1000 J/KG WITH POOR MID-LEVEL LAPSE RATES. THUS, DESPITE  
THE PRESENCE OF SEASONABLY STRONG VERTICAL SHEAR, THE MARGINAL  
THERMODYNAMIC ENVIRONMENT IS CURRENTLY EXPECTED TO LIMIT SEVERE  
WEATHER POTENTIAL.  
 
   
..CENTRAL HIGH PLAINS  
 
MODEL DIFFERENCES IN THE BOUNDARY-LAYER STRUCTURE WITHIN THE  
POST-FRONTAL UPSLOPE ALONG WITH THE PRESENCE OF A CAP CENTERED  
AROUND 600 MB LEAD TO UNCERTAINTY IN SURFACE-BASED STORM DEVELOPMENT  
AND SUSTENANCE TUESDAY AFTERNOON AND EVENING. SHOULD STORMS DEVELOP,  
THE PRESENCE OF 30-40+ KT OF DEEP-LAYER SHEAR WOULD SUPPORT SOME  
SEVERE WEATHER THREAT. HOWEVER, CONFIDENCE IN THAT SCENARIO IS  
CURRENTLY TOO LOW TO INCLUDE A 5% PROBABILITY CONTOUR.  
 
..MEAD.. 08/02/2026  
 
 
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