May 26, 2009 0100 UTC Day 1 Convective Outlook
Updated: Tue May 26 00:59:16 UTC 2009
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20090526 0100 UTC Day 1 Outlook Graphic
Probabilistic Tornado Graphic
20090526 0100 UTC Day 1 Tornado Probabilities Graphic
Torndao Legend Image
Probabilistic Damaging Wind Graphic
20090526 0100 UTC Day 1 Damaging Wind Probabilities Graphic
Wind Legend Image
Probabilistic Large Hail Graphic
20090526 0100 UTC Day 1 Large Hail Probabilities Graphic
Hail Legend Image
   SPC AC 260054
   
   DAY 1 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   0754 PM CDT MON MAY 25 2009
   
   VALID 260100Z - 261200Z
   
   ...NO SVR TSTM AREAS FORECAST...
   
   ...OK/TX PNHDLS INTO DEEP S TX...
   
   SURFACE COLD FRONT FROM WRN KS SWWD THROUGH THE WRN OK PNHDL INTO
   NERN NM AS OF 00Z WILL PROGRESS SWD THROUGH THE PNHDLS AND THE TX S
   PLAINS BY 26/12Z.  PRE-FRONTAL STORMS HAVE DEVELOPED THIS AFTERNOON
   AND EVENING INVOF DRYLINE AND PRE-EXISTING OUTFLOW BOUNDARIES...
   NAMELY ACROSS THE OK AND NRN TX PNHDLS.  HIGH RESOLUTION RADAR AND
   VISIBLE SATELLITE DATA INDICATE THAT CONSIDERABLE COLD POOL
   GENERATION IS OCCURRING WITH THIS ACTIVITY WITH A NARROW AXIS OVER
   THE CNTRL TX PNHDL REMAINING UNCONTAMINATED.  MODIFICATION OF 00Z
   AMA SOUNDING FOR SLIGHTLY HIGHER DEWPOINTS OBSERVED TO THE E WITHIN
   THIS AXIS SUGGESTS THAT AIR MASS REMAINS MODERATELY UNSTABLE WITH
   MLCAPE OF 1000-1500 J/KG.
   
   UPSCALE GROWTH INTO LARGER TSTM CLUSTERS OR AN MCS STILL REMAINS
   POSSIBLE TONIGHT OVER THE SRN TX PNHDL INTO NWRN TX/WRN OK AS
   STRENGTHENING LLJ ENHANCES LOW-LEVEL CONVERGENCE ALONG MERGING
   MESOSCALE COLD POOLS AND SYNOPTIC FRONT.  LATEST OBSERVATIONAL DATA
   INDICATE THAT DEEP-LAYER BULK SHEAR REMAINS QUITE MARGINAL /I.E.
   GENERALLY LESS THAN 25-30 KT/ AND THIS WILL LIMIT THE POTENTIAL FOR
   A MORE ORGANIZED CONVECTIVE SYSTEM.  NONETHELESS...THE MORE INTENSE
   STORMS WILL REMAIN CAPABLE OF LOCALLY STRONG WIND GUSTS AND SOME
   HAIL.
   
   FOR ADDITIONAL SHORT TERM GUIDANCE IN THIS AREA...SEE MCD 869.
   
   FARTHER S...SCATTERED TSTMS HAVE DEVELOPED ALONG DRYLINE OVER THE
   LOW ROLLING PLAINS INTO THE CONCHO VALLEY AND WRN PARTS OF THE
   EDWARDS PLATEAU REGION.  EVENING WATER VAPOR IMAGERY SUGGESTS THAT
   FORCING FOR ASCENT ASSOCIATED WITH LOW LATITUDE IMPULSE TRANSLATING
   ACROSS NWRN MEXICO MAY BE IN PART CONTRIBUTING TO THIS DEVELOPMENT. 
   00Z DRT SOUNDING INDICATES DEEPLY MIXED BOUNDARY LAYER CONDITIONS
   WITH STEEP LAPSE RATES CONTRIBUTING TO MLCAPE OF AROUND 1000 J/KG. 
   THIS ENVIRONMENT WILL CONTINUE TO SUPPORT CLUSTERS OF STRONG TO
   POTENTIALLY SEVERE STORMS FOR THE NEXT SEVERAL HOURS WITH THE THREAT
   FOR HAIL AND STRONG WIND GUSTS.  LATER TONIGHT...STRENGTHENING
   CONVECTIVE INHIBITION SHOULD RESULT IN A DECREASE IN STORM COVERAGE
   AND INTENSITY.
   
   FINALLY OVER DEEP S TX...A TSTM HAS RECENTLY DEVELOPED S OF ALI
   ALONG WWD-MOVING SEA BREEZE BOUNDARY.  00Z BRO SOUNDING IS LIKELY
   QUITE REPRESENTIVE OF STORM PROXIMITY ENVIRONMENT WITH MARITIME
   TROPICAL BOUNDARY LAYER AND STEEP MIDLEVEL LAPSE RATES CONTRIBUTING
   TO MLCAPE AROUND 2000 J/KG.  THIS INSTABILITY COMBINED WITH MODEST
   MID AND HIGH-LEVEL FLOW SUGGESTS THE POTENTIAL FOR UPDRAFT ROTATION
   WITH ABOVE-MENTIONED STORM OR ANY ACTIVITY MOVING ACROSS THE RIO
   GRANDE.  GIVEN THE PRESENCE OF THE RATHER STRONG CAP IN
   PLACE...STORMS SHOULD BEGIN TO WEAKEN AFTER SUNSET AS THE BOUNDARY
   LAYER BEGINS TO COOL.
   
   ..MEAD.. 05/26/2009
   
   CLICK TO GET WUUS01 PTSDY1 PRODUCT

   NOTE: THE NEXT DAY 1 OUTLOOK IS SCHEDULED BY 0600Z