Oct 2, 2009 0600 UTC Day 1 Convective Outlook
Updated: Fri Oct 2 05:59:26 UTC 2009
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20091002 1200 UTC Day 1 Outlook Graphic
Probabilistic Tornado Graphic
20091002 1200 UTC Day 1 Tornado Probabilities Graphic
Torndao Legend Image
Probabilistic Damaging Wind Graphic
20091002 1200 UTC Day 1 Damaging Wind Probabilities Graphic
Wind Legend Image
Probabilistic Large Hail Graphic
20091002 1200 UTC Day 1 Large Hail Probabilities Graphic
Hail Legend Image
   SPC AC 020555
   
   DAY 1 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   1255 AM CDT FRI OCT 02 2009
   
   VALID 021200Z - 031200Z
   
   ...NO SVR TSTM AREAS FORECAST...
   
   ...SYNOPSIS...
   AMPLIFIED YET PROGRESSIVE UPPER AIR PATTERN FCST TO CONTINUE ACROSS
   CONUS THROUGH PERIOD.  MID-UPPER LOW -- NOW OVER ST LAWRENCE VALLEY
   AREA OF SRN QUE -- IS EXPECTED TO LIFT NEWD WHILE STG/TRAILING
   SHORTWAVE TROUGH STRENGTHENS CONSIDERABLY...EFFECTIVELY SHIFTING
   UPPER TROUGHING EWD ACROSS NEW ENGLAND EARLY IN PERIOD.  AS THIS
   OCCURS...BROAD UPPER CYCLONE NOW CENTERED OVER NWRN IA SHOULD MOVE
   EWD ACROSS SRN WI TO VICINITY CENTRAL/SRN LM BY 3/12Z. 
   MEANWHILE...SPEED MAX ALOFT FROM ERN GULF OF AK TO SRN BC -- AND
   ACCOMPANYING CHAIN OF MIDLEVEL VORTICITY LOBES -- IS FCST TO AMPLIFY
   INTO CLOSED/BROAD CYCLONE OVER WA BY END OF PERIOD.
   
   AT SFC...COLD FRONT IS ANALYZED FROM SERN MO SWWD ACROSS AR AND E TX
   TO S-CENTRAL/SW TX.  FRONT IS FCST TO CONTINUE SEWD ACROSS MID-SOUTH
   AND W GULF COAST REGIONS...REACHING FROM CENTRAL/SRN APPALACHIANS
   SWWD TO S-CENTRAL/SERN LA AND S-CENTRAL TX BY 3/00Z.  S TX SEGMENT
   OF THIS FRONT SHOULD STALL EARLY IN PERIOD...AND MAY START TO
   RETREAT NWD AROUND 3/12Z.  MEANWHILE...REMAINDER OF LA-GA FRONTAL
   SEGMENT SHOULD DECELERATE...WITH NRN PORTION OF COLD FRONT MOVING
   SLOWLY EWD FROM CENTRAL APPALACHIANS ACROSS PIEDMONT AND INLAND
   MID-ATLANTIC.  MARINE/WARN FRONTAL ZONE EXTENDS FROM SERN GULF NWWD
   OVER SERN LA...THEN ROUGHLY NWD TO WHERE ONGOING CONVECTIVE BAND
   CROSSES MS RIVER.  THIS CONVECTION...AND COLD FRONT IMMEDIATELY
   FOLLOWING IT...WILL OVERTAKE MARINE FRONT FROM N-S WHILE MARINE
   FRONT MOVES SLOWLY EWD ACROSS LOWER DELTA REGION AND SRN PORTIONS
   MS/AL.
   
   ...S TX...
   TWO PERIODS OF MRGL/CONDITIONAL SVR POTENTIAL ARE APPARENT ACROSS
   THIS REGION...OVERLAPPING SPATIALLY.  AIR MASS INVOF SFC FRONTAL
   ZONE...AND SWD TO LOWER RIO GRANDE VALLEY -- IS FCST TO DESTABILIZE
   DURING AFTERNOON LARGELY BECAUSE OF SFC DIABATIC HEATING...GIVEN
   LACK OF APPRECIABLE LARGE-SCALE/UPPER LEVEL SUPPORT.  UPSTREAM CLOUD
   TRENDS ATTM INDICATE CIRRUS-LEVEL  EFFLUENT FROM PACIFIC TS OLAF
   SHOULD BE RATHER THIN AND PATCHY...AND NOT A SIGNIFICANT IMPEDIMENT
   TO SFC HEATING.  WITH DEW POINTS GENERALLY UPPER 60S AND 70S
   F...WEAKLY CAPPED MLCAPE TO NEAR 3000 J/KG IS POSSIBLE BY MID-LATE
   AFTERNOON...ACCORDING TO MODIFIED WRF AND ETA-KF SOUNDINGS. NEGATIVE
   FACTORS WILL INCLUDE WEAK LOW-MIDLEVEL WINDS...I.E. 10 KT OR LESS
   THROUGH MOST OF SFC-700 MB LAYER.  HOWEVER...STG UPPER WINDS --
   AROUND 50-75 KT AT  250 MB NEAR SRN RIM OF UPPER JET MAX -- MAY
   CONTRIBUTE TO ORGANIZATION OF ANY TSTMS THAT CAN DEVELOP.  ANOTHER
   LIMITING EFFECT WILL BE WEAKNESS OF LOW LEVEL CONVERGENCE...WITH STG
   ELY FLOW COMPONENT ALONG BOTH SIDES OF SFC FRONTAL ZONE.  A FEW
   GUSTS/HAIL EVENTS NEAR SVR LEVELS ARE POSSIBLE.
   
   LOW LEVEL MOIST/WARM ADVECTION MAY SUPPORT INCREASE IN ELEVATED
   BUOYANCY AND POTENTIAL FOR STG/ISOLATED SVR TSTMS LATE IN PERIOD
   OVER PORTIONS S-CENTRAL TX -- EITHER FROM ACTIVITY DEVELOPING OVER
   THIS REGION OR MOVING NEWD FROM COAHUILA.  MODIFIED FCST SOUNDINGS
   SUGGEST POTENTIAL FOR 35-45 KT EFFECTIVE SHEAR MAGNITUDES AMIDST
   ELEVATED MUCAPES 500-1500 J/KG.  MAIN CONCERN WOULD BE MRGL
   HAIL...ESPECIALLY AFTER APPROXIMATELY 06/03Z.
   
   ...COASTAL DELTA REGION TO WRN FL PANHANDLE...
   ISOLATED STG/DAMAGING GUSTS CANNOT BE RULED OUT FROM CLUSTERS OR
   SHORT LINEAR SEGMENTS OF TSTMS DEVELOPING IN NARROW WEDGE OF
   HIGH-THETAE WARM SECTOR AIR NEAR COAST.  COVERAGE IS IN QUESTION
   GIVEN WEAKNESS OF LOW LEVEL WINDS AND OF NEAR-FRONTAL CONVERGENCE AS
   A RESULT.  HOWEVER...MLCINH ALSO SHOULD BE RATHER
   LIMITED...ESPECIALLY DURING PERIOD OF DIABATICALLY-DRIVEN SFC
   WARMING MID-DAY THROUGH MID-AFTERNOON.  THIS AREA ALSO WILL RESIDE
   BENEATH SOMEWHAT FAVORABLE UPPER LEVEL WINDS...AS ERN LOBE OF 250 MB
   JET MAX PROPAGATES NWD ACROSS THIS AREA...WITH 60-80 KT FLOW
   POSSIBLE AROUND ANVIL LEVEL.  LACK OF MORE ROBUST LOW-MIDLEVEL SHEAR
   WILL LIMIT ORGANIZED SVR THREAT.
   
   ..EDWARDS/GARNER.. 10/02/2009
   
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