Aug 28, 2006 1730 UTC Day 2 Convective Outlook
Updated: Mon Aug 28 17:41:36 UTC 2006
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20060828 1730 UTC Day 2 Outlook Graphic
Probabilistic Graphic
20060828 1730 UTC Day Probabilitic Graphic
   SPC AC 281739
   
   DAY 2 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   1239 PM CDT MON AUG 28 2006
   
   VALID 291200Z - 301200Z
   
   ...THERE IS A SLGT RISK OF SVR TSTMS PORTIONS DELMARVA/MID-ATLANTIC
   REGION...
   
   ...SYNOPSIS...
   SEASONALLY HIGH-AMPLITUDE AND PROGRESSIVE SYNOPTIC PATTERN WILL
   PERSIST OVER MUCH OF CONUS THROUGH PERIOD.  HEIGHTS WILL FALL ACROSS
   PACIFIC NW IN ADVANCE OF TROUGH NOW EVIDENT IN MOISTURE CHANNEL
   IMAGERY OVER SERN GULF OF AK AND ADJACENT NERN PACIFIC.  MID-UPPER
   LEVEL LOW NOW LOCATED INVOF YKN IS PROGGED TO MOVE ESEWD ACROSS
   IL/INDIANA THROUGH PERIOD.  CONFIDENCE IN THIS TRACK IS GAINED FROM
   REASONABLY STRONG CONSENSUS AND LITTLE VARIATION AMONGST 28/12Z
   DETERMINISTIC SHORT-RANGE MODELS...REGARDING LOCATION AND POSITIVE
   TILT OF ASSOCIATED TROUGH.  SOME DIFFERENCES ARE EVIDENT IN
   STRENGTH...NAMELY WHETHER TROUGH WILL CONTINUE HOLDING CLOSED LOW OR
   EVOLVE TO OPEN-WAVE STRUCTURE. ASSOCIATED SFC LOW -- NOW ANALYZED
   OVER MO/IA BORDER -- IS FCST TO MOVE GENERALLY EWD ALONG FRONTAL
   ZONE TO COASTAL DELMARVA/MID-ATLANTIC BY 30/00Z.  TRAILING COLD
   FRONT WILL MOVE SEWD OVER OH VALLEY...SRN/CENTRAL APPALACHIANS...AND
   ALL BUT COASTAL PLAIN OF TX BY SAME TIME.
   
   AS OF THIS WRITING...TS ERNESTO IS MOVING NWWD ACROSS SERN CUBA. 
   LATEST NHC TRACK FCST FOR ITS CENTER...AS WELL AS TRENDS IN THESE
   FCSTS...SUGGEST MOST FAVORABLE AREA FOR TORNADOES WILL REMAIN
   OFFSHORE OVER ATLANTIC.  AS SUCH...NO PROBABILITIES ARE INCORPORATED
   ATTM...THOUGH ANY LEFTWARD DEVIATION FROM THIS TRACK MIGHT RESULT IN
    PERIPHERAL SUPERCELL POTENTIAL ALONG FL E COAST.
   
   ...MID-ATLANTIC/DELMARVA REGION...
   WIDELY SCATTERED TSTMS ARE EXPECTED TO DEVELOP IN ZONE OF MAXIMIZED
   LOW LEVEL ASCENT AND HEATING...SE THROUGH E OF SFC LOW...LATE
   MORNING THROUGH AFTERNOON.  THERE IS SOME CONCERN THAT CLOUD COVER
   MAY LIMIT DIURNAL HEATING...HOWEVER WEAK CINH AND CONVERGENCE INVOF
   LOW SHOULD SUPPORT ENOUGH SUPERCELL POTENTIAL TO WARRANT CATEGORICAL
   SLGT RISK.  MOST FAVORABLE ZONE FOR SVR SHOULD BE FROM LOW EWD INVOF
   FRONT...WHERE SUPERCELLS ARE MOST PROBABLE.  PRIND THIS AREA WILL
   COMPRISE A NARROW CORRIDOR -- JUXTAPOSING NRN PERIPHERY OF MOST
   FAVORABLE BOUNDARY LAYER HEATING/MOISTURE...SRN PERIPHERY OF
   STRONGER MIDLEVEL FLOW...AND RELATIVELY BACKED LOW LEVEL WINDS IN
   ORDER TO MAXIMIZE DEEP-LAYER VERTICAL SHEAR.  ACCORDINGLY...MODEL
   FCST SOUNDINGS INDICATE 35-35 KT EFFECTIVE SHEAR...AND 0-1 KM SRH
   100-200 J/KG FOR EWD STORM MOTIONS.  IN ENVIRONMENT OF RELATIVELY
   LOW LCL AND FAVORABLE KINEMATIC PROFILES NEAR WARM FRONT...A TORNADO
   OR TWO IS POSSIBLE.  DAMAGING GUST THREAT MAINLY WOULD BE FROM
   AFTERNOON CONVECTION WHOSE SUBCLOUD LAYERS ARE OPTIMALLY MIXED BY
   HEATING.  LOW-MIDLEVEL ABSOLUTE WARMTH AND LAPSE RATES NEAR
   MOIST-ADIABATIC ALOFT WILL LIMIT BOTH RATE OF CONVECTIVE DEVELOPMENT
   AND POTENTIAL FOR LARGE HAIL.
   
   ...MID-UPPER MS VALLEY REGION...
   ALTHOUGH BOUNDARY LAYER WILL BE POSTFRONTAL AND CHARACTERIZED BY
   AMBIENT CAA OVER THIS REGION...WIDELY SCATTERED TSTMS ARE POSSIBLE
   DURING AFTERNOON..BENEATH COLD CORE REGION OF MID/UPPER LOW. 
   DIABATIC HEATING WILL OFFSET SFC CAA ENOUGH TO REMOVE CINH IN SOME
   AREAS...IN COMBINATION WITH RESIDUAL/EVAPOTRANSPIRATED MOISTURE. 
   LAPSE RATES SHOULD BECOME STEEP ENOUGH TO SUPPORT MLCAPES LOCALLY
   EXCEEDING 1000 J/KG.  STRONGEST CELLS MAY PRODUCE HAIL AND GUSTS
   NEAR SVR LEVELS.
   
   ...SRN AND PERHAPS CENTRAL AZ...
   STRONG SFC HEATING IS ANTICIPATED ACROSS MUCH OF THIS REGION
   CONCURRENT WITH INCREASE IN LOW LEVEL MOISTURE...SUPPORTING
   CONVECTIVE POTENTIAL DURING MID-LATE AFTERNOON OVER HIGHER
   ELEVATIONS AND LATE AFTERNOON INTO EVENING OVER LOWER DESERTS. 
   DEEP/LOW-MIDLEVEL ELY FLOW COMPONENT -- PARTICULARLY OVER SRN AZ --
   WOULD AID MOVEMENT OF CONVECTION OFF MOUNTAINS AND OVER HOT/DEEPLY
   MIXED DESERT BOUNDARY LAYERS...IN SUPPORT OF AT LEAST MRGL POTENTIAL
   FOR STG-SVR GUSTS.
   
   ..EDWARDS.. 08/28/2006
   
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   NOTE: THE NEXT DAY 2 OUTLOOK IS SCHEDULED BY 0800Z