Nov 5, 2006 0100 UTC Day 1 Convective Outlook
Updated: Sun Nov 5 01:04:11 UTC 2006
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20061105 0100 UTC Day 1 Outlook Graphic
Probabilistic Tornado Graphic
20061105 0100 UTC Day 1 Tornado Probabilities Graphic
Probabilistic Damaging Wind Graphic
20061105 0100 UTC Day 1 Damaging Wind Probabilities Graphic
Probabilistic Large Hail Graphic
20061105 0100 UTC Day 1 Large Hail Probabilities Graphic
   SPC AC 050100
   
   DAY 1 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   0700 PM CST SAT NOV 04 2006
   
   VALID 050100Z - 051200Z
   
   ...NO SVR TSTM AREAS FORECAST...
   
   ...SYNOPSIS...
   IN MID/UPPER LEVELS...NEARLY ZONAL MEAN FLOW PATTERN IS EVIDENT OVER
   MOST OF CONUS...DISTORTED PRIMARILY BY SHORTWAVE TROUGH ANALYZED
   FROM CENTRAL HIGH PLAINS SWWD ACROSS SWRN NM.  THIS TROUGH SHOULD
   DRIFT EWD OVERNIGHT.  UPSTREAM...MID-UPPER LEVEL SHORTWAVE TROUGH --
   EVIDENT IN MOISTURE CHANNEL IMAGERY FROM 130-133W OFFSHORE WA/BC --
   IS FCST TO MOVE INLAND BY APPROXIMATELY 06Z.
   
   AT SFC...WEAK QUASISTATIONARY FRONT AND CONFLUENT LINE WAS ANALYZED
   FROM NW OK SWWD ACROSS CENTRAL TX PANHANDLE...THROUGH LOW INVOF
   TCC...THEN BECOMING DIFFUSE FARTHER WSW.  DRYLINE WAS ANALYZED FROM
   NRN COAHUILA NWD BETWEEN MAF-INK THEN NNEWD ACROSS CDS
   AREA...BECOMING DIFFUSE OVER WRN OK WHERE ONLY WEAK MOISTURE HAS
   RETURNED TO ITS E.  LOW CLOUD TRENDS AND GPS-PW DATA INDICATE
   BOUNDARY LAYER DRYLINE HAS BEEN QUASISTATIONARY SE OF REGION DURING
   PAST FEW HOURS...HOWEVER MORE INTENSE PRESSURE/HEIGHT FALLS ARE
   EXPECTED IN LOW LEVELS OVERNIGHT THAT SHOULD SHIFT W/NW EDGE OF
   MOIST PLUME AT LEAST INTO POSITION OF QUASISTATIONARY FRONT OVER
   PANHANDLE...AND WWD TO VICINITY NM BORDER AND DAVIS MOUNTAINS
   FARTHER S.
   
   ...OZARKS TO SRN HIGH PLAINS...
   AHEAD OF AFOREMENTIONED SHORTWAVE TROUGH...ELEVATED LOW LEVEL WAA
   REGIME WILL PERSIST THROUGH TONIGHT...ACCOMPANIED BY
   MOISTENING/STRENGTHENING LLJ FROM NRN COAHUILA NWD THEN NEWD ACROSS
   W-CENTRAL/N-CENTRAL TX AND ERN OK.  TWO ASSOCIATED AREAS OF GEN TSTM
   POTENTIAL EXIST FOR REMAINDER PERIOD...WITH JUST ENOUGH UNCERTAINTY
   IN POSSIBLE SPATIAL OVERLAP THAT THEY STILL FORM ONE COMPOSITE AREA
   ON 01Z-12Z GRAPHIC DEPICTION.
   
   1. CONVECTION IS INCREASING IN COVERAGE AND INTENSITY ACROSS SERN
   KS...NWRN AR...NERN OK AND SWRN MO ATTM.  THIS ACTIVITY CORRESPONDS
   TO LEADING PORTION OF FAVORABLE LOW LEVEL MOIST ADVECTION ABOVE
   SFC...AND ISENTROPIC ASCENT TO LFC.  ELEVATED MUCAPES 100-200 J/KG
   ALREADY EVIDENT IN SGF RAOB WERE UNDERFCST BY LATEST RUNS OF BOTH
   ETA AND RUC...INDICATING THESE MODELS MAY SIMILARLY UNDERFCST
   SIZE/COVERAGE OF CONVECTIVE AREA THIS EVENING UNTIL LATEST RAOB DATA
   IS INPUT.  PRIND ACTIVITY OVER THIS REGION WILL WEAKEN AFTER ABOUT
   08Z AS PRIMARY FOCI FOR ELEVATED CONVECTION SHIFT SW.
   
   2.  AFTER ABOUT 06Z...WIDELY SCATTERED TSTMS ARE EXPECTED TO DEVELOP
   OVER PORTIONS NW TX....ERN TX PANHANDLE AND/OR WRN OK. MODIFIED RUC
   SOUNDINGS SUGGEST SUFFICIENT MOISTENING IN 750-900 MB LAYER --
   BENEATH 7-8 DEG C/KM MIDLEVEL LAPSE RATES...FOR ELEVATED MUCAPES TO
   REACH 800 J/KG BY END OF PERIOD OVER SWRN OK AND NW TX...WITH
   MINIMAL CINH.  ADDITIONAL/CONDITIONAL THUNDER AREA MAY DEVELOP
   BENEATH OR JUST W OF LLJ AXIS FROM CENTRAL TX NNEWD ACROSS CENTRAL
   OK...AMIDST STRONGEST LOW LEVEL MOISTURE TRANSPORT.
   
   ...WRN/NRN OLYMPIC PENINSULA...
   STRONGEST MID-UPPER LEVEL ASCENT WITH MIDLEVEL TROUGH SHOULD REMAIN
   JUST N OF AREA ACROSS VANCOUVER ISLAND.  GIVEN WEAKLY BUOYANT
   PROFILE EVIDENT IN UIL RAOB...BRIEF/ISOLATED LIGHTNING CANNOT BE
   RULED OUT...HOWEVER POTENTIAL APPEARS TOO TRANSIENT AND CONDITIONAL
   TO WARRANT GEN THUNDER OUTLOOK.
   
   ..EDWARDS.. 11/05/2006
   
   CLICK TO GET WUUS01 PTSDY1 PRODUCT

   NOTE: THE NEXT DAY 1 OUTLOOK IS SCHEDULED BY 0600Z