Dec 8, 2009 0700 UTC Day 2 Convective Outlook
Updated: Tue Dec 8 06:08:50 UTC 2009
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20091208 0700 UTC Day 2 Outlook Graphic
Probabilistic Graphic
20091208 0700 UTC Day Probabilitic Graphic
Probability Legend Image
   SPC AC 080538
   
   DAY 2 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   1138 PM CST MON DEC 07 2009
   
   VALID 091200Z - 101200Z
   
   ...NO SVR TSTM AREAS FORECAST...
   
   ...SYNOPSIS...
   
   NEGATIVELY-TILTED MIDLEVEL TROUGH SITUATED ALONG CYCLONIC SIDE OF
   POWERFUL MID/HIGH-LEVEL JET STREAKS WILL LIFT RAPIDLY NEWD THROUGH
   THE OH VALLEY...GREAT LAKES AND NERN STATES WITH 12-HR HEIGHT FALLS
   EXCEEDING 200 M ALONG SYSTEM TRACK.  AT THE SURFACE...ALREADY
   INTENSE SURFACE LOW WILL DEEPEN FURTHER WHILE DEVELOPING NEWD
   THROUGH THE GREAT LAKES...PRIOR TO OCCLUDING OVER SWRN ONTARIO INTO
   SWRN QUEBEC.  MEANWHILE...TRAILING COLD FRONT...INITIALLY FROM THE
   MIDDLE OH VALLEY TO CNTRL GULF COAST WILL PUSH EWD THROUGH THE
   APPALACHIANS AND EVENTUALLY OFF THE ATLANTIC COAST BY WEDNESDAY
   NIGHT.  TRAILING EXTENSION OF COLD FRONT WILL SAG MORE SLOWLY SWD
   THROUGH THE NRN/CNTRL FL PENINSULA. 
   
   ...MID ATLANTIC COAST INTO NRN FL...
   
   08/00Z MODEL GUIDANCE REMAINS RELATIVELY CONSISTENT IN THE EVOLUTION
   OF THE SYNOPTIC-SCALE FEATURES THROUGH THE DAY TWO PERIOD.  THE
   RAPID NEWD TRANSLATION OF UPPER SYSTEM AND SURFACE LOW WILL RESULT
   IN STRONGER ISALLOBARIC FORCING AND DEEPER-LAYER FORCING FOR ASCENT
   BECOMING INCREASINGLY REMOVED FROM SYSTEM WARM SECTOR WITH TIME.  AS
   A CONSEQUENCE...LOW-LEVEL WINDS WILL TEND TO VEER...RESULTING IN
   WEAKENING CONVERGENCE ALONG PROGRESSIVE COLD FRONT.
   
   EXPECT CLUSTERS OF TSTMS TO BE ONGOING WEDNESDAY MORNING ALONG/AHEAD
   OF COLD FRONT FROM PARTS OF VA SWWD INTO ERN AL AND THE FL PNHDL. 
   INTERESTINGLY...OPERATIONAL NAM-BMJ...GFS AND SREF ETA-KF CONTROL
   MEMBER QPF ALL SUGGEST A GENERAL DECREASE IN CONVECTIVE
   PRECIPITATION THROUGH THE DAY FROM CHESAPEAKE BAY SSWWD TO THE
   SAVANNAH RIVER WITH MORE PERSISTENT DEEP...MOIST CONVECTION OVER SRN
   GA/NRN FL.  THIS MAY...IN PART...BE A FUNCTION OF THE WEAKENING DEEP
   CONVERGENCE ALONG THE COLD FRONT.
   
   VERTICAL SHEAR WILL REMAIN VERY STRONG ACROSS FRONTAL ZONE
   /PARTICULARLY ACROSS THE TIDEWATER REGION SWD THROUGH THE
   CAROLINAS/...INDICATING A THREAT FOR DAMAGING WINDS AND PERHAPS
   TORNADOES SHOULD TSTMS BECOME SUSTAINED.  DUE TO THE UNCERTAINTY OF
   THIS CONDITION...ONLY LOW SEVERE PROBABILITIES WILL BE MAINTAINED
   ACROSS THIS AREA.
   
   OVER SRN GA/NRN FL...STORMS WILL LIKELY PERSIST THROUGH THE DAY /AS
   MENTIONED ABOVE/ WITHIN KINEMATIC ENVIRONMENT FEATURING 35-45 KT OF
   DEEP-LAYER SHEAR AND BOUNDARY LAYER DEWPOINTS IN THE 60S.  WHILE
   ISOLATED SEVERE WEATHER WILL REMAIN POSSIBLE...THE WEAK LAPSE RATES
   AND MLCAPE OF GENERALLY LESS THAN 500-700 J/KG SHOULD PRECLUDE MORE
   ORGANIZED STORM POTENTIAL.
   
   ...UPPER OH VALLEY...
   
   THE POTENTIAL FOR CONVECTIVELY-GENERATED DAMAGING WINDS IN THIS AREA
   IS CONDITIONAL ON TSTM DEVELOPMENT.  NAM/GOES SIMULATED WATER VAPOR
   IMAGERY SUGGESTS THAT REGION WILL RESIDE ON NRN FRINGE OF DRY SLOT
   ATTENDANT TO VORTICITY MAXIMUM...POTENTIALLY ALLOWING FOR DEEPER
   MIXING AND STEEPENING OF LAPSE RATES THROUGH THE DIURNAL HEATING
   CYCLE.  A STRONGLY FORCED CONVECTIVE BAND WILL LIKELY DEVELOP ALONG
   THE FRONT BY AFTERNOON WITHIN ZONE OF STRONG DCVA IN ADVANCE OF
   MIDLEVEL SYSTEM.  GIVEN THE EXTREMELY STRONG AMBIENT WIND FIELD AND
   VERTICAL SHEAR...ANY DEEPER CONVECTIVE ELEMENTS WILL POSE A DAMAGING
   WIND THREAT.
   
   ..MEAD.. 12/08/2009
   
   CLICK TO GET WUUS02 PTSDY2 PRODUCT

   NOTE: THE NEXT DAY 2 OUTLOOK IS SCHEDULED BY 1730Z