Dec 23, 2006 1100 UTC Day 3 Severe Thunderstorm Outlook
Updated: Sat Dec 23 07:47:40 UTC 2006
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20061223 1100 UTC Day 3 Outlook Graphic
Probabilistic Graphic
20061223 1100 UTC Day Probabilitic Graphic
   SPC AC 230745
   
   DAY 3 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   0145 AM CST SAT DEC 23 2006
   
   VALID 251200Z - 261200Z
   
   ...THERE IS A SLGT RISK OF SVR TSTMS ACROSS PARTS OF ERN SC/GA AND
   MUCH OF FL...
   
   ...SYNOPSIS...
   AS MENTIONED IN DAY 2 OUTLOOK...SOME UNCERTAINTY WITH RESPECT TO
   LARGE SCALE PATTERN EVOLUTION BEGINS TO IMPACT FORECAST CONFIDENCE
   FOR CHRISTMAS DAY OVER THE SOUTH. NCEP-SREF MEAN DEPICTS A SURFACE
   LOW ASSOCIATED WITH A STRONG SRN LATITUDE UPPER TROUGH NEAR THE WRN
   FL PNHDL. MEANWHILE...LATEST DETERMINISTIC GUIDANCE FROM GFS AND
   ECMWF PLACE THE SURFACE LOW FARTHER INLAND...PERHAPS OVER AL. DEEP
   CONVECTION SHOULD BE ACTIVE NEAR THE LOW AND ALSO OVER THE NERN GULF
   ALONG ATTENDANT COLD FRONT. THE COLD FRONT IS EXPECTED TO MOVE EAST
   ACROSS FL AND THE SOUTHEAST U.S. COAST THROUGH CHRISTMAS DAY WITH
   THE EWD PROGRESSION AND INTENSITY OF THE FRONTAL FORCING BEING
   MODULATED BY LARGER SCALE TROUGH AMPLIFICATION AND PHASING EXPECTED
   TO OCCUR ACROSS MS/OH VALLEY AREAS THROUGH EARLY TUESDAY.
   
   ...GA/SC AND FL...
   SIMILARITIES AMONG 00Z GFS/ECMWF AND LATEST GFS ENSEMBLE MEAN IN THE
   TIMING OF THE COLD FRONT AND STRENGTH OF LARGE SCALE PHASING LEND
   SUPPORT FOR A MORE AMPLIFIED AND ENERGETIC FLOW REGIME OVER THE
   SOUTHEAST THROUGH CHRISTMAS DAY. DEGREE OF DESTABILIZATION AHEAD OF
   THE FRONT...ACROSS PARTS OF ERN GA/SC AND FL...CONTINUES TO BE
   SOMEWHAT PROBLEMATIC GIVEN THE POTENTIAL FOR WEAK LAPSE RATES
   DEPICTED IN MODEL SOUNDINGS. HOWEVER...RELATIVELY MOIST PRE-FRONTAL
   BOUNDARY LAYER WITH 65-70F DEWPOINTS APPEARS REASONABLE AND SHOULD
   SUPPORT AT LEAST MARGINAL SURFACE-BASED CAPE. FORCING ON THE
   ADVANCING FRONT SHOULD PROVE SUFFICIENT TO MAINTAIN DEEP CONVECTION
   WHICH SHOULD EVOLVE INTO A SQUALL LINE AS FRONTAL FORCING
   STRENGTHENS THROUGH THE DAY. THE SQUALL LINE SHOULD CROSS THE SERN
   U.S. COAST AND CNTRL FL THROUGH THE LATE AFTERNOON BASED ON
   GFS/ECMWF. STRENGTHENING OF DEEP-LAYER WIND FIELDS WILL CONTRIBUTE
   TO BOWING LINE SEGMENTS AND/OR SUPERCELLS EMBEDDED WITHIN THE
   CONVECTIVE LINE WITH DAMAGING WINDS POSSIBLE.
   
   ..CARBIN.. 12/23/2006
   
   CLICK TO GET WUUS03 PTSDY3 PRODUCT

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