Apr 28, 2010 0600 UTC Day 2 Convective Outlook
Updated: Wed Apr 28 06:01:46 UTC 2010
Probabilistic to Categorical Outlook Conversion Table
Categorical Graphic
20100428 0600 UTC Day 2 Outlook Graphic
Probabilistic Graphic
20100428 0600 UTC Day Probabilitic Graphic
Probability Legend Image
   SPC AC 280600
   
   DAY 2 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   0100 AM CDT WED APR 28 2010
   
   VALID 291200Z - 301200Z
   
   ...THERE IS A SLGT RISK OF SVR TSTMS FROM A PORTION OF THE SRN AND
   CNTRL PLAINS INTO THE UPPER MS VALLEY...
   
   ...SYNOPSIS...
   
   THE BROAD UPPER TROUGH NOW MOVING INTO THE WRN U.S. WILL CONTINUE
   SLOWLY EWD THROUGH THURSDAY. AT LEAST A COUPLE OF IMPULSES
   ORIGINATING WITHIN THE UPPER TROUGH WILL EJECT NEWD THROUGH THE
   CNTRL PLAINS AND UPPER MS VALLEY DURING THE DAY. A STRONGER IMPULSE
   IS FORECAST TO EJECT INTO THE SRN AND CNTRL PLAINS LATER THURSDAY
   NIGHT. MODEL CONSENSUS IS THAT A SURFACE LOW INITIALLY OVER NEB
   EARLY THURSDAY WILL LIFT NEWD INTO MN DURING THE DAY IN ASSOCIATION
   WITH EJECTING SHORTWAVE TROUGH. THIS WILL FORCE A COLD FRONT SEWD
   THROUGH ERN NEB AND NRN KS DURING THE AFTERNOON. FARTHER SOUTH A
   DRYLINE WILL RESIDE ACROSS WRN TX...OK AND NWD INTO KS. A LEE
   CYCLONE WITH TRAILING PACIFIC FRONT WILL SHIFT EWD THROUGH SRN
   KS/WRN OK THURSDAY NIGHT IN ASSOCIATION WITH AN IMPULSE MOVING
   THROUGH BASE OF UPPER TROUGH. THIS FRONT WILL OVERTAKE THE DRYLINE
   ACROSS THE SRN/CNTRL HIGH PLAINS.  
   
   ...CNTRL PLAINS THROUGH UPPER MS VALLEY AREA...
   
   SURFACE RIDGE WILL MAINTAIN ELY-NELY TRAJECTORIES OVER THE NRN GULF
   AND DELAY MORE SIGNIFICANT GULF BOUNDARY LAYER MODIFICATION UNTIL
   WEDNESDAY NIGHT. THIS WILL RESULT IN ONLY PARTIALLY MODIFIED GULF
   AIR WITH DEWPOINTS IN THE 50S TO AROUND 60 ADVECTING NWD INTO THE
   CNTRL PLAINS AND UPPER MS VALLEY BENEATH ERN PERIPHERY OF STEEPER
   LAPSE RATE PLUME. THESE PROCESSES AND DIABATIC WARMING WILL
   CONTRIBUTE TO 800-1200 J/KG MLCAPE. EWD ADVECTION OF THE EML PLUME
   ABOVE THE MODEST MOIST AXIS WILL LIKELY RESULT IN A CAP TO SURFACE
   BASED STORMS. MOST LIKELY AREA OF INITIATION WILL BE WITHIN ZONE OF
   DEEPER ASCENT ALONG COLD FRONT FROM ERN NEB AND WRN IA DURING THE
   AFTERNOON...THOUGH AN ISOLATED STORM OR TWO CANNOT BE RULED OUT
   ALONG THE DRYLINE ACROSS KS. ADDITIONAL STORMS MAY EVENTUALLY
   BACKBUILD SWD INTO KS AS THE COLD FRONT OVERTAKES THE DRYLINE AND AS
   THE SLY LOW LEVEL JET STRENGTHENS TO IN EXCESS OF 60 KT. VERTICAL
   SHEAR IN EXCESS OF 60 KT WILL SUPPORT ORGANIZED STORMS INCLUDING
   SUPERCELLS. HOWEVER...STORMS SHOULD EVENTUALLY GROW UPSCALE INTO
   LINES ALONG THE SEWD ADVANCING COLD FRONT.  
    
   
   ...SRN PLAINS...
   
   THREAT IN THIS AREA IS MORE CONDITIONAL DUE TO LOWER PROBABILITY OF
   THUNDERSTORM INITIATION. THE ATMOSPHERE WILL BECOME MODERATELY
   UNSTABLE DURING THE AFTERNOON AS PARTIALLY MODIFIED GULF AIR ADVECTS
   NWD BENEATH STEEP LAPSE RATES ASSOCIATED WITH EML PLUME. HOWEVER...A
   STOUT CAPPING INVERSION WILL EXIST OVER MUCH OF THE WARM SECTOR. IN
   WAKE OF IMPULSE MOVING THROUGH THE CNTRL PLAINS AND UPPER MS VALLEY
   REGION...DRYLINE CONVERGENCE WILL NOT BE PARTICULARLY PRONOUNCED.
   HOWEVER...HEATING AND MIXING ALONG THIS BOUNDARY MIGHT BE SUFFICIENT
   TO INITIATE AN ISOLATED STORM OR TWO. IF A STORM DEVELOPS IT WOULD
   RAPIDLY BECOME SUPERCELLULAR GIVEN THE STRONG VERTICAL SHEAR IN
   PLACE. GREATER PROBABILITY FOR STORM INITIATION WILL OCCUR LATER
   THURSDAY NIGHT WHEN THE PACIFIC FRONT ACCOMPANYING A SPEED MAX
   MOVING THROUGH BASE OF UPPER TROUGH OVERTAKES THE DRYLINE. 
   
   MODELS ALSO INDICATE STORMS MAY DEVELOP TOWARD THE END OF THIS
   PERIOD WITHIN WARM ADVECTION REGIME FROM ERN PARTS OF THE SRN PLAINS
   INTO THE LOWER MS VALLEY COINCIDENT WITH SURGE OF RICHER GULF
   MOISTURE.
   
   ..DIAL.. 04/28/2010
   
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   NOTE: THE NEXT DAY 2 OUTLOOK IS SCHEDULED BY 1730Z