Feb 24, 2014 1300 UTC Day 1 Convective Outlook
Updated: Mon Feb 24 12:36:32 UTC 2014 (20140224 1300Z Day 1 shapefile | 20140224 1300Z Day 1 KML)
Probabilistic to Categorical Outlook Conversion Table
Categorical Graphic
20140224 1300 UTC Day 1 Outlook Graphic
Probabilistic Tornado Graphic
20140224 1300 UTC Day 1 Tornado Probabilities Graphic
Probability of a tornado within 25 miles of a point.
Hatched Area: 10% or greater probability of EF2 - EF5 tornadoes within 25 miles of a point.
Probabilistic Damaging Wind Graphic
20140224 1300 UTC Day 1 Damaging Wind Probabilities Graphic
Probability of damaging thunderstorm winds or wind gusts of 50 knots or higher within 25 miles of a point.
Hatched Area: 10% of greater probability of wind gusts 65 knots or greater within 25 miles of a point.
Probabilistic Large Hail Graphic
20140224 1300 UTC Day 1 Large Hail Probabilities Graphic
Probability of hail 1" or larger within 25 miles of a point.
Hatched Area: 10% or greater probability of hail 2" or larger within 25 miles of a point.
Risk Area (sq. mi.) Area Pop. Some Larger Population Centers in Risk Area
No Risk Areas Forecast
   SPC AC 241233

   DAY 1 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   0633 AM CST MON FEB 24 2014

   VALID 241300Z - 251200Z

   ...NO SVR TSTM AREAS FORECAST...

   ...SYNOPSIS...
   UPPER-AIR PATTERN WILL BE CHARACTERIZED BY PERSISTENT/BROAD CYCLONIC
   FLOW OVER MUCH OF CENTRAL/ERN CONUS.  STG UPPER-LEVEL CYCLONE -- NOW
   EVIDENT IN MOISTURE-CHANNEL IMAGERY OVER NERN PAC AND CENTERED INVOF
   38N148W -- IS FCST TO EJECT NEWD...AS DOWNSTREAM RIDGE AMPLIFIES
   FROM NWRN MEX UP W COAST STATES AND BC/YUKON.  PRIMARY SHORTWAVE
   TROUGH -- CURRENTLY EVIDENT OVER SRN PORTIONS SK/MB BORDER WWD
   ACROSS SRN AB -- IS FCST TO MOVE SEWD ACROSS DAKOTAS BY 00Z THEN
   PIVOT/ACCELERATE EWD ACROSS WI TO LOWER MI BY END OF PERIOD.  IN SRN
   STREAM...MOISTURE-CHANNEL LOOPS INDICATE WEAK PERTURBATION OVER SERN
   NM...W TX PERMIAN BASIN AND COAHUILA.  THIS FEATURE IS RESOLVED TO
   SOME EXTENT BY 6Z OPERATIONAL NAM/SPECTRAL MODELS...WHICH PROG SRN
   PORTION TO MOVE ACROSS NRN GULF BETWEEN UPPER TX COAST AND FL
   COASTAL BEND DURING 00Z-12Z TIME FRAME.

   AT SFC...RESIDUAL/DIFFUSE AND QUASISTATIONARY FRONTAL ZONE WAS
   EVIDENT FROM S FL NWWD ACROSS NERN GULF THEN WWD ACROSS MOSTLY SHELF
   WATERS TO LOWER TX COAST.  THAT FRONT WILL BE OVERTAKEN FROM W-E BY
   COLD FRONT NOW MOVING SEWD ACROSS GA...SRN AL...SRN LA AND S-CENTRAL
   TX.  COMBINED FRONTAL ZONE SHOULD STALL ACROSS NWRN GULF AND S
   TX...RETURNING NWD AS WARM FRONT OVERNIGHT OVER TX.

   ...CENTRAL/ERN FL PENINSULA...
   WIDELY SCATTERED TSTMS MAY DEVELOP THIS AFTN ALONG
   SEA-BREEZE/CONVERGENCE ZONE OVER ERN PENINSULA...BENEATH DEEP-LAYER
   WLYS...AND AFTER PASSAGE OF CLOUD DEBRIS FROM MORNING ACTIVITY OVER
   GULF.  ALTHOUGH E-COAST CONVERGENCE ZONE SHOULD CONCENTRATE BULK OF
   CONVECTIVE POTENTIAL...FRONT AND/OR OUTFLOW/DIFFERENTIAL-HEATING
   BOUNDARIES FROM EARLY CONVECTION ALSO MIGHT FOSTER SECONDARY TSTM
   INITIATION.  FCST SOUNDINGS SUGGEST DIABATIC SFC HEATING AND MID-60S
   TO LOW-70S F SFC DEW POINTS WILL BE SUFFICIENT TO YIELD AROUND
   1000-1500 J/KG MLCAPE ALONG I-95 CORRIDOR IN CENTRAL FL...BUT WITH
   MORE PRONOUNCED AND POTENTIALLY BUOYANCY-LIMITING MIDLEVEL STABLE
   LAYER FARTHER S.

   WEAK NEAR-SFC WIND SPEEDS WILL KEEP BOUNDARY-LAYER HODOGRAPHS
   SMALL...HOWEVER CONCENTRATIONS OF VORTICITY ALONG CONVERGENCE LINE
   MAY BRIEFLY SUPPORT STORM ROTATION.  MULTICELLS SHOULD BE
   PREDOMINANT MODE...SOME OF WHICH MAY BECOME ORGANIZED AMIDST 70-KT
   ANVIL-LEVEL FLOW AND 30-40 KT EFFECTIVE SHEAR MAGNITUDES.  FCST
   SOUNDINGS REASONABLY SUGGEST SHALLOW INVERTED-V THERMODYNAMIC
   PROFILES IN BOUNDARY LAYER AND SEASONALLY COLD AIR ALOFT -- E.G. -10
   TO -12 C AT 500 MB.  GIVEN THESE CONDITIONS...ISOLATED/MRGLLY SVR
   HAIL AND/OR ISOLATED DAMAGING GUSTS MAY OCCUR.

   ...N TX...RED RIVER REGION TO ARKLATEX...
   ISOLATED TO WIDELY SCATTERED ELEVATED TSTMS MAY DEVELOP LATE
   OVERNIGHT -- E.G. INITIALLY AFTER 06Z AND MOSTLY AFTER 09Z -- IN
   ZONE OF ELEVATED LOW-LEVEL WAA AND MRGL MOISTURE.  UPPER-LEVEL
   SUPPORT WILL BE MINIMAL BY THAT TIME...WITH SRN-STREAM PERTURBATION
   WELL E OF AREA AND NO SUBSTANTIAL FEATURES EVIDENT UPSTREAM. 
   HOWEVER...PLANAR PROGS AND TIME SERIES OF FCST SOUNDINGS SUGGEST
   GRADUAL INCREASE IN BOTH THETAE AND RH OF AIR MASS AROUND 850 MB
   OVERNIGHT.  MINIMALLY INHIBITED MUCAPE OF 300-700 J/KG SHOULD
   DEVELOP BY 09-12Z TIME FRAME...ROOTED AROUND 850 MB...WITH
   CONVECTION SUPPORTED BY ISENTROPIC LIFT TO LFC.  DEEP SHEAR AND
   BUOYANCY EACH APPEAR TOO MODEST FOR SVR THREAT.

   ...S TX...
   ISOLATED TO WIDELY SCATTERED TSTMS MAY SPREAD ENEWD FROM NUEVO LEON
   AND/OR REDEVELOP TODAY AHEAD OF MEXICAN LOBE OF AFOREMENTIONED
   SHORTWAVE TROUGH...AFFECTING PORTIONS S TX.  WEAKENING OF INITIALLY
   ROBUST EML-RELATED CINH IS EVIDENT WITH SWD EXTENT AND WITH TIME
   TODAY ACROSS S TX...ALONG WITH UPPER 60S TO LOW 70S F SFC DEW POINTS
   AND POCKETS OF STG SFC HEATING MAINLY AHEAD OF FRONT.  ALTHOUGH NLY
   COMPONENT OF PREFRONTAL FLOW WILL LIMIT CONVERGENCE...SOME FRONTAL
   LIFT MAY COMBINE WITH SFC HEATING IN SUPPORTING UPDRAFT DEVELOPMENT.
    ISOLATED TSTMS ALSO MAY DEVELOP BEHIND FRONT.  OVERALL COVERAGE
   SHOULD BE LIMITED BY LACK OF MORE ROBUST LIFT AGAINST ANTECEDENT EML
   CINH.

   ..EDWARDS/BOTHWELL.. 02/24/2014

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