336  
ACUS11 KWNS 061215  
SWOMCD  
SPC MCD 061214  
NEZ000-SDZ000-061415-  
 
MESOSCALE DISCUSSION 1574  
NWS STORM PREDICTION CENTER NORMAN OK  
0714 AM CDT SUN JUL 06 2025  
 
AREAS AFFECTED...SOUTHWEST SOUTH DAKOTA AND NORTH-CENTRAL NEBRASKA  
 
CONCERNING...SEVERE POTENTIAL...WATCH UNLIKELY  
 
VALID 061214Z - 061415Z  
 
PROBABILITY OF WATCH ISSUANCE...20 PERCENT  
 
SUMMARY...ONGOING THUNDERSTORMS SHOULD PERSIST FOR ANOTHER COUPLE OF  
HOURS BEFORE WEAKENING. ISOLATED HAIL AND A DAMAGING WIND GUST OR  
TWO WILL REMAIN POSSIBLE IN THE NEAR TERM. A WATCH IS NOT CURRENTLY  
EXPECTED.  
 
DISCUSSION...THUNDERSTORMS CONTINUE THIS MORNING ACROSS SOUTHWEST  
SOUTH DAKOTA ALONG THE SOUTHWEST PORTION OF A REMNANT MCS THAT MOVED  
ACROSS THIS REGION OVERNIGHT. THESE THUNDERSTORMS APPEAR TO BE  
DRIVEN BY ISENTROPIC ASCENT FOCUSED ATOP A RESIDUAL COLD POOL LEFT  
OVER FROM THE OVERNIGHT CONVECTION. THIS SHOWS UP AS STRONG WARM-AIR  
ADVECTION CENTERED AROUND 700 MB IN REGIONAL MESOANALYSIS.  
MESOANALYSIS ALSO INDICATES A RICH CAPE RESERVOIR TO THE SOUTHWEST  
OF THE ONGOING STORMS, WITHIN THE THUNDERSTORM SOURCE/INFLOW REGION,  
PROVIDING ADDITIONAL BUOYANCY. WITH TIME, DIURNAL HEATING SHOULD  
BEGIN TO MODIFY THE EXISTING COLD POOL AND WEAKEN THE ISENTROPIC  
ASCENT/WAA LEADING TO A DOWNWARD TREND IN THUNDERSTORM INTENSITY.  
BEFORE THIS WEAKENING OCCURS, LAPSE RATES DO NOT APPEAR PARTICULAR  
STEEP THIS MORNING PER RAP-MODEL FORECAST SOUNDINGS, AND AN  
ISOTHERMS LAYER EXTENDS UPWARD FROM THE SURFACE TO AROUND 800 MB.  
THIS SHOULD LIMIT THE SEVERE POTENTIAL TO ISOLATED HAIL AND PERHAPS  
A DAMAGING WIND GUST OR TWO -- REALISTICALLY ONLY IN THE MOST  
INTENSE CORES.  
 
A WATCH IS NOT ANTICIPATED.  
 
..MARSH/BUNTING.. 07/06/2025  
   
..PLEASE SEE WWW.SPC.NOAA.GOV FOR GRAPHIC PRODUCT  
 
ATTN...WFO...LBF...UNR...CYS...  
 
LAT...LON 42700288 43310326 43780292 43860217 43680064 43250033  
42590021 42300061 42170165 42700288  
 
MOST PROBABLE PEAK WIND GUST...55-70 MPH  
MOST PROBABLE PEAK HAIL SIZE...1.00-1.75 IN  
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