Oct 4, 2009 0600 UTC Day 1 Convective Outlook
Updated: Sun Oct 4 04:55:17 UTC 2009
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20091004 1200 UTC Day 1 Outlook Graphic
Probabilistic Tornado Graphic
20091004 1200 UTC Day 1 Tornado Probabilities Graphic
Torndao Legend Image
Probabilistic Damaging Wind Graphic
20091004 1200 UTC Day 1 Damaging Wind Probabilities Graphic
Wind Legend Image
Probabilistic Large Hail Graphic
20091004 1200 UTC Day 1 Large Hail Probabilities Graphic
Hail Legend Image
   SPC AC 040450
   
   DAY 1 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   1150 PM CDT SAT OCT 03 2009
   
   VALID 041200Z - 051200Z
   
   ...NO SVR TSTM AREAS FORECAST...
   
   ...SYNOPSIS...
   UPPER AIR PATTERN ACROSS CONUS WILL CONTINUE TO BE DOMINATED BY
   THREE PRIMARY FEATURES...
   1. BROAD CYCLONE LIFTING NWD FROM UPPER GREAT LAKES OVER NRN ONT.
   2. STRONGER VORTEX DIGGING SWD FROM NWRN GREAT BASIN...THEN PIVOTING
   EWD OR ENEWD ACROSS NV...WHICH WILL INDUCE HEIGHT/PRESSURE FALLS
   OVER CENTRAL ROCKIES REGION...AND BROAD ZONE OF LOW-LEVEL WAA OVER
   CENTRAL/SRN PLAINS NW OF GULF COAST CONVECTIVE REGIME.
   3. BROAD FETCH OF WSWLY SRN STREAM FLOW FROM NRN MEX ACROSS WRN GULF
   COAST REGION...WITHIN WHICH HEIGHTS ARE FCST TO RISE THROUGH MOST OF
   PERIOD.  LIKEWISE...SRN RIM OF UPPER JET WILL SHIFT NWD ACROSS
   SRN/CENTRAL TX...WITH FLOW BECOMING SLIGHTLY ANTICYCLONIC ALOFT.
   
   ON SMALLER SCALES...CONVECTIVELY INDUCED/REINFORCED MID-UPPER LEVEL
   VORTICITY LOBE...APPARENTLY EMBEDDED WITHIN TSTM CLUSTER OVER SRN
   GULF OF CA THAT HAS BEEN SHEARED AWAY FROM RESIDUAL LOW LEVEL
   CIRCULATION OF TD OLAF.  MOST MODELS CONTINUE TO RESOLVE THIS
   FEATURE BUT WITH TIMING DIFFERENCES IN ITS DOWNSTREAM PASSAGE ACROSS
   S TX...SOMETIME DURING DAYLIGHT HOURS.  LOW-AMPLITUDE SHORTWAVE
   TROUGH -- EVIDENT IN TIME SERIES OF PLANAR VWP DATA OVER MID/UPPER
   TX COAST ATTM...WILL MOVE ACROSS LA COAST EARLY IN PERIOD.
   
   MEANWHILE...LOW-LEVEL BAROCLINIC ZONE -- NOW ANALYZED FROM NEAR COT
   ACROSS TX COASTAL BEND...OFFSHORE UPPER TX COAST AND WRN LA...AND
   ACROSS SERN LA -- IS FCST TO LIFT NWD AS WARM FRONT ACROSS PORTIONS
   SRN/CENTRAL TX AND SRN LA.  WEAK FRONTAL-WAVE LOW LAY DEVELOP OVER
   SE TX OR SWRN LA AS SRN-STREAM/MID-UPPER LEVEL PERTURBATION APCHS.
   WRN SEGMENT OF WARM FRONT WILL RETREAT FARTHER NWD ACROSS RIO GRANDE
   VALLEY AND SW TX...WHILE BECOMING MORE DIFFUSE AMIDST
   BROAD/LOW-LEVEL WAA REGIME.
   
   ...S-CENTRAL/SE TX...SRN LA...
   CONSIDERABLE UNCERTAINTY EXISTS REGARDING EXTENT OF NWD MOTION OF
   WARM FRONT...GIVEN LIKELIHOOD OF EXTENSIVE CONVECTION AND PRECIP TO
   ITS N FOR MUCH OF PERIOD.  WEAK TROUGH ALOFT NOW OVER MID/UPPER TX
   COAST MAY AID IN MAINTAINING FAVORABLE ENVIRONMENT FOR CONVECTION
   OFFSHORE UPPER TX COAST AND LA EARLY IN PERIOD AND DELAY NWD FRONTAL
   RETREAT OVER THERE.  LAPSE RATES ALOFT GENERALLY SHOULD REMAIN
   MRGLLY UNSTABLE...AS MESOSCALE/WEAK DPVA REGIONALLY COUNTERACTS
   BROADER STABILIZING EFFECTS ALOFT FROM SYNOPTIC HEIGHT RISES AND
   PLUME OF TROPICAL MID-UPPER AIR ADVECTING FROM NWRN MEX.
   LOW-LEVEL THERMODYNAMICS WILL REMAIN FAVORABLE WITHIN AND S OF SFC
   FRONTAL ZONE...WITH DEW POINTS COMMONLY IN 70S AND SFC HEATING OVER
   LAND AREAS REMOVED FROM CLOUD COVER.  MLCAPE 2000-3000 J/KG MAY
   DEVELOP ALONG AND JUST S OF EFFECTIVE FRONT.  PRIND BOUNDARY WILL
   NOT RETREAT NWD AS FAST AS FAVORABLE MID-UPPER WINDS OVER REGION. 
   THIS EFFECT SHOULD MAKE SUPERCELL POTENTIAL
   SHORT-LIVED...HEAVY-PRECIP IN MODE...AND TORNADO THREAT VERY MRGL
   AND CONDITIONAL ON BOUNDARY INTERACTIONS.  ISOLATED STG/DAMAGING
   GUSTS ALSO ARE POSSIBLE FROM MOST INTENSE CELLS.
   
   ...SRN HIGH PLAINS...AFTER 5/06Z...
   WIDELY SCATTERED TO SCATTERED TSTMS MAY DEVELOP LATE IN PERIOD
   WITHIN SWATH FROM W-CENTRAL TX NWD ACROSS PORTIONS NW TX AND
   PANHANDLE.  NARROW...LARGELY MERIDIONAL PLUME OF VIGOROUS MOIST
   ADVECTION/TRANSPORT IS FCST WITHIN BROADER LOW LEVEL WAA ZONE.  AS
   THETAE INCREASES WITHIN 30-40 KT LLJ OVERNIGHT...INCREASINGLY MOIST
   PARCELS MAY BE LIFTED ISENTROPICALLY TO LFC.  FCST VERTICAL SHEAR
   PROFILE IS FAVORABLE FOR AT LEAST MRGL STORM ORGANIZATION...WITH
   PROGGED EFFECTIVE SHEAR VARYING FROM 30-35 KT RANGE FOR SHALLOW/WEAK
   MUCAPES TO NEAR 500 J/KG...AS PROGGED BY MOST MODELS...TO 50-60 KT
   RANGE FOR VERY DEEP MUCAPES 1000-1500 J/KG PER ETA-KF.  MOST
   AGGRESSIVE PROGS SUGGEST POTENTIAL FOR  HAIL WITH MOST INTENSE
   CONVECTION...DESPITE MEAGER MID-UPPER LAPSE RATES. 
   HOWEVER...POTENTIAL APPEARS TOO CONDITIONAL ATTM TO ASSIGN AOA
   5-PERCENT UNCONDITIONAL PROBABILITIES FOR LAST FEW HOURS OF PERIOD.
   
   ..EDWARDS/GARNER.. 10/04/2009
   
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