Apr 3, 2007 1730 UTC Day 2 Convective Outlook
Updated: Tue Apr 3 17:45:38 UTC 2007
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20070403 1730 UTC Day 2 Outlook Graphic
Probabilistic Graphic
20070403 1730 UTC Day Probabilitic Graphic
   SPC AC 031743
   
   DAY 2 CONVECTIVE OUTLOOK CORR 1
   NWS STORM PREDICTION CENTER NORMAN OK
   1243 PM CDT TUE APR 03 2007
   
   VALID 041200Z - 051200Z
   
   ...THERE IS A SLGT RISK OF SVR TSTMS TIDEWATER REGION -- ERN NC TO
   SRN DELMARVA PENINSULA...
   
   CORRECTED FOR MISSING  15% LINE
   
   ...SYNOPSIS...
   IN MID/UPPER LEVELS...PROGRESSIVE WAVE TRAIN IS FCST TO SLOW AND
   AMPLIFY DURING DAY-2 PERIOD ACROSS NRN CONUS.  SHORTWAVE TROUGH WITH
   SMALL EMBEDDED LOW -- NOW EVIDENT IN MOISTURE CHANNEL IMAGERY OVER
   EXTREME ERN DAKOTAS/WRN MN -- WILL DEEPEN INTO LARGER CLOSED LOW AS
   IT MOVES EWD ACROSS UPPER GREAT LAKES...REACHING MIN 500 MB HEIGHT
   VALUE AROUND END OF PERIOD OVER ERN LH OR ADJACENT PORTIONS ONT. 
   ASSOCIATED SFC CYCLONE -- NOW ANALYZED OVER ERN IA/NWRN IL AND
   SOMEWHAT DIFFUSED BY CONVECTIVE PROCESSES -- SHOULD REGAIN BETTER
   DEFINITION AND DEEPEN CONSIDERABLY THROUGH REMAINDER DAY-1.  BY
   4/12Z...LOW SHOULD BE OCCLUDING OVER LH...BECOMING MORE CLOSELY
   STACKED IN VERTICAL WITH MID-UPPER LEVEL PERTURBATION THEREAFTER.
   
   SFC COLD FRONT -- NOW ANALYZED FROM LOW SWWD ACROSS SERN KS...SWRN
   OK...TO SERN NM -- SHOULD MOVE RAPIDLY FROM CENTRAL/SRN APPALACHIANS
   AT 4/12Z OFFSHORE MOST OF ATLANTIC COAST BY 5/12Z.  SECONDARY
   CYCLOGENESIS REASONABLY IS PROGGED ACROSS DELMARVA REGION WEDNESDAY
   MORNING THROUGH AFTERNOON -- PERHAPS BEGINNING BEFORE 4/18Z INLAND
   OVER VA.  RESULTING SFC LOW SHOULD LIFT NEWD TOWARD CAPE COD BY END
   OF PERIOD.  TRAILING PORTION OF COLD FRONT SHOULD SWEEP SWD OVER
   N-CENTRAL/NERN GULF...BUT WILL MOVE MORE SLOWLY SWD ACROSS S TX.
   
   ...DELMARVA...VA/NC TIDEWATER REGION...
   SFC HEATING BEFORE COLD FROPA SHOULD WEAKEN CAP AND PERMIT TSTM
   DEVELOPMENT.  NRN BOUND OF SVR POTENTIAL SHOULD BE SHARPLY
   DELINEATED BY POSITION OF WARM FRONT -- E OF DEVELOPING SFC
   CYCLONE...LIKELY ACROSS SOME PART OF CHESAPEAKE BAY AND DELMARVA
   PENINSULA.  WARM SECTOR SFC DEW POINTS LOW-MID 60S AND INSOLATION
   MAY RAISE MLCAPES INTO 1000-1500 J/KG RANGE.  35-45 KT DEEP-LAYER
   SHEAR AND PROBABILITY OF LINEAR FORCING ALONG FRONT SUGGEST MAIN
   THREAT WILL BE DAMAGING WIND.  HOWEVER...RELATIVELY BACKED FLOW
   ALONG ATLANTIC COAST WOULD ENLARGE LOW LEVEL HODOGRAPHS...ENHANCING
   SUPERCELL POTENTIAL AND DIVERSIFYING SVR THREAT.
   
   FRONTAL BAND OF CONVECTION MAY EXTEND MUCH FARTHER N OVER PORTIONS
   PA/NJ AND POSSIBLY NY.  HOWEVER...ASSOCIATED POTENTIAL FOR STG-SVR
   GUSTS TO REACH SFC WILL BE GREATLY LIMITED BY STABLE BOUNDARY LAYER
   THAT WILL BE PROGRESSIVELY DEEPER WITH NWD EXTENT.
   
   ...SC TO FL PANHANDLE...
   SCATTERED TSTMS SHOULD DEVELOP FROM LATE MORNING THROUGH
   AFTERNOON...INVOF SFC COLD FRONT.  MOIST ADVECTION AND SFC HEATING
   WILL RAISE BOUNDARY LAYER THETAE AND REMOVE CINH...WITH MLCAPES
   1000-2000 J/KG RANGE POSSIBLE.  LOW LEVEL SHEAR WILL BE
   SIGNIFICANTLY LIMITED BY NEARLY UNIDIRECTIONAL COMPONENT OF FLOW
   FROM SFC-700 MB...AND DEEP-LAYER BULK SHEAR SHOULD WEAKEN WITH SWWD
   EXTENT...SW OF CATEGORICAL SLGT RISK AREA.  THIS WILL LIMIT
   ORGANIZATION OF SVR POTENTIAL...HOWEVER A FEW MULTICELLS OR SHORT
   BANDS OF CONVECTION MAY PRODUCE GUSTS/HAIL NEAR SVR LEVELS. 
   ACTIVITY SHOULD DIMINISH CONSIDERABLY WITH LOSS OF DIURNAL HEATING.
   
   ...S TX...
   PLUME OF VERY MOIST SFC AIR -- ALREADY IN PLACE ACROSS THIS REGION
   -- WILL PERSIST THROUGH DIURNAL HEATING CYCLE DAY-2...AHEAD OF SFC
   FRONT.  ASSOCIATED BOUNDARY LAYER WILL BE CAPPED THROUGH MOST OF DAY
   BY PRONOUNCED ELEVATED MIXED LAYER EMANATING FROM MEX HIGHLANDS. 
   HOWEVER...TSTMS MAY DEVELOP IN STRONGLY HEATED AND VERY UNSTABLE
   AFTERNOON ENVIRONMENT...WITH AID FROM NEAR-FRONTAL CONVERGENCE. 
   MLCAPES 3000-4000 J/KG APPEAR LIKELY...SUPPORTING POTENTIAL FOR
   STG-SVR GUSTS AND HAIL WITH ANY ACTIVITY THAT CAN DEVELOP OVER S TX.
    FLOW IS FCST TO BE RELATIVELY WEAK THROUGH LOW-MIDDLE LEVELS...ONLY
   5-15 KT.  STRONG DIRECTIONAL SHEAR SHOULD EXIST IN ASSOCIATION WITH
   BOUNDARY LAYER ELY COMPONENT NEAR FRONT...WHICH ALSO WOULD AID IN
   STORM-RELATIVE INFLOW.  DEVELOPMENT IS MORE PROBABLE OVER NEARBY
   PORTIONS MEX WHERE OROGRAPHIC ASCENT ALSO WILL CONTRIBUTE.  IN THIS
   KINEMATIC PROFILE...STRONG ELEMENT OF DISCRETE PROPAGATION SHOULD BE
   MAJOR INFLUENCE ON STORM MOTION -- KEEPING MOST STORMS THAT FORM ON
   MEX SIDE OF RIO GRANDE AWAY FROM TX.
   
   ..EDWARDS.. 04/03/2007
   
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