May 25, 2006 1100 UTC Day 3 Severe Thunderstorm Outlook
Updated: Thu May 25 07:29:38 UTC 2006
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20060525 1100 UTC Day 3 Outlook Graphic
Probabilistic Graphic
20060525 1100 UTC Day Probabilitic Graphic
   SPC AC 250728
   
   DAY 3 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   0228 AM CDT THU MAY 25 2006
   
   VALID 271200Z - 281200Z
   
   ...NO SVR TSTM AREAS FORECAST...
   
   ...SYNOPSIS...
   
   MODELS AGREE THAT PATTERN WILL TRANSITION TO AN UPPER RIDGE IN THE
   ERN U.S. WITH AN UPPER TROUGH AMPLIFYING IN THE W. BETWEEN THESE TWO
   FEATURES THE NRN PLAINS WILL BE UNDER THE INFLUENCE OF SWLY FLOW
   ALOFT. A NE-SW ORIENTED COLD FRONT WILL MOVE SLOWLY EWD INTO THE NRN
   PLAINS. THE POTENTIAL WILL EXIST FOR A SERIES OF VORTICITY MAXIMA TO
   ROTATE NEWD OUT OF THE UPPER TROUGH INTO THE NRN PLAINS IN VICINITY
   OF THE FRONT. SUBTLE DIFFERENCES DO EXIST BETWEEN THE MODELS WITH
   THE ECMWF BEING A LITTLE FARTHER W WITH THE UPPER TROUGH RESULTING
   IN HEIGHT RISES OVER THE NRN PLAINS ON SATURDAY.
   
   ...NRN PLAINS...
   
   A STRONG LOW LEVEL JET WILL DEVELOP E OF LEE TROUGH THAT WILL BECOME
   ESTABLISHED OVER THE PLAINS DOWNSTREAM FROM AMPLIFYING UPPER TROUGH.
   THIS WILL CONTRIBUTE TO THE NWD ADVECTION OF LOW LEVEL MOISTURE INTO
   THE NRN PLAINS BENEATH STEEP LAPSE RATES. MODERATE INSTABILITY IS
   EXPECTED WITHIN THE PRE-FRONTAL WARM SECTOR ACROSS THE DAKOTAS. ONE
   CONCERN IS POSSIBILITY FOR A STRONG CAP GIVEN PRESENCE OF SWLY
   700-500 MB FLOW DOWNSTREAM FROM UPPER TROUGH WHICH WILL HAVE THE
   POTENTIAL TO ADVECT THE EML EWD INTO THE NRN PLAINS. ANOTHER CONCERN
   IS HOW MUCH HEIGHTS WILL RISE OVER THE NRN PLAINS DOWNSTREAM FROM
   AMPLIFYING UPPER TROUGH. THE ECMWF HAS BEEN FARTHER W WITH THE WRN
   U.S. UPPER TROUGH...RESULTING IN MORE RIDGINESS AND HEIGHT RISES
   OVER THE NRN PLAINS. THIS WOULD TEND TO KEEP ANY IMPULSES ROTATING
   THROUGH THE UPPER TROUGH W OF THE WARM SECTOR AND SUPPORT MORE POST
   FRONTAL CONVECTION. THE GFS AND NAM ARE FARTHER EAST WITH THE UPPER
   TROUGH WITH MORE SWLY FLOW AND LESS OF A RIDGE OVER THE NRN PLAINS.
   THESE SOLUTIONS WOULD SUPPORT A BETTER SEVERE POTENTIAL THAN THE
   ECMWF. GIVEN THE MODEL DIFFERENCES AND POTENTIAL FOR A STRONG
   CAP...WILL KEEP 5% SEVERE PROBABILITIES AT THIS TIME. HOWEVER...A
   SLIGHT RISK MAY BE NEEDED FOR PORTIONS OF THIS AREA ONCE THESE
   UNCERTAINTIES AND CONCERNS HAVE BEEN MITIGATED.
   
   ..DIAL.. 05/25/2006
   
   CLICK TO GET WUUS03 PTSDY3 PRODUCT

   NOTE: THE NEXT DAY 3 OUTLOOK IS SCHEDULED BY 1100Z