Feb 17, 2009 2000 UTC Day 1 Convective Outlook
Updated: Tue Feb 17 19:48:13 UTC 2009
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20090217 2000 UTC Day 1 Outlook Graphic
Probabilistic Tornado Graphic
20090217 2000 UTC Day 1 Tornado Probabilities Graphic
Torndao Legend Image
Probabilistic Damaging Wind Graphic
20090217 2000 UTC Day 1 Damaging Wind Probabilities Graphic
Wind Legend Image
Probabilistic Large Hail Graphic
20090217 2000 UTC Day 1 Large Hail Probabilities Graphic
Hail Legend Image
   SPC AC 171944
   
   DAY 1 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   0144 PM CST TUE FEB 17 2009
   
   VALID 172000Z - 181200Z
   
   ...THERE IS A SLGT RISK OF SVR TSTMS TONIGHT ACROSS PARTS OF THE LWR
   MS VALLEY....
   
   ...SOUTHEAST TEXAS THROUGH THE LWR MS/OH AND TENNESSEE VALLEYS...
   SURFACE CYCLOGENESIS IS WELL UNDERWAY TO THE LEE OF THE CENTRAL
   ROCKIES.  AS THE SURFACE LOW CENTER CONTINUES TO DEEPEN AND MIGRATE
   EAST OF THE CENTRAL HIGH PLAINS...TOWARD THE MIDDLE MISSISSIPPI
   VALLEY THROUGH THE REMAINDER OF THE PERIOD...A SOUTHERLY RETURN FLOW
   OF MOISTURE WILL STRENGTHEN OFF THE WESTERN OF MEXICO.  UPPER
   60S/LOWER 70S SURFACE DEW POINTS ARE CURRENTLY PRESENT ACROSS THE
   WESTERN GULF OF MEXICO INTO THE TEXAS COASTAL PLAIN.  AND...AT LEAST
   UPPER 50S/LOWER 60S SURFACE DEW POINTS ARE EXPECTED TO ADVECT
   NORTHEASTWARD ALONG AN AXIS THROUGH THE LOWER MISSISSIPPI VALLEY BY
   12Z WEDNESDAY.
   
   MOISTURE RETURN HAS BEEN QUICKER THAN THE RETREAT OF A COLD SURFACE
   RIDGE...NOW ENCOMPASSING MOST AREAS FROM THE MISSISSIPPI VALLEY
   EASTWARD.  THIS HAS RESULTED IN INCREASING SHALLOW CONVECTION AND
   PRECIPITATION WITHIN A ZONE OF BROAD ISENTROPIC ASCENT ALONG AND
   EAST OF THE LOWER MISSISSIPPI VALLEY.  HOWEVER...WARMING ALOFT
   BENEATH SHORT WAVE RIDGING IS SUPPRESSING THE FORMATION OF
   THUNDERSTORMS.  THIS PROBABLY WILL REMAIN THE CASE THROUGH THE MID
   EVENING HOURS...PERHAPS MUCH OF THE NIGHT...PARTICULARLY ALONG THE
   AXIS OF SURFACE-BASED...OR NEAR SURFACE-BASED...DESTABILIZATION
   DEVELOPING NORTHEASTWARD OUT OF SOUTHEAST TEXAS.
   
   MODELS ARE STILL NOT PARTICULARLY CLEAR ON THE TIMING/LOCATION OF
   THE INITIATION OF STORMS TONIGHT.  HOWEVER...THE JUXTAPOSITIONING OF
   STRONGER LOW-LEVEL MOISTENING AND STEEPENING ISENTROPIC ASCENT SEEMS
   MOST PROBABLE BENEATH THE DIFLUENT REGIME BETWEEN THE POLAR AND
   SUBTROPICAL JET AXES...EAST OF THE CREST OF THE UPPER RIDGE...
   ACROSS EASTERN ARKANSAS INTO WESTERN TENNESSEE/NORTHERN MISSISSIPPI 
   DURING THE 03-06Z TIME FRAME.  THIS ACTIVITY SHOULD DEVELOP EASTWARD
   TOWARD THE UPPER TENNESSEE VALLEY OVERNIGHT.  THE ONSET OF AT LEAST
   WEAK COOLING IN THE CAPPING LAYER TOWARD THE 09-12Z TIME FRAME MAY
   SUPPORT ADDITIONAL STORM DEVELOPMENT NEAR OR JUST WEST OF THE
   MISSISSIPPI/ARKANSAS BORDER AREA.  IF THIS OCCURS... 
   DESTABILIZATION IN THE PRESENCE OF STRONG SHEAR WILL BE MORE
   SUPPORTIVE OF A SEVERE THREAT...WITH A FEW SUPERCELLS CAPABLE OF
   PRODUCING AT LEAST LARGE HAIL POSSIBLE.
   
   ...CENTRAL CALIFORNIA...
   A RESIDUAL CYCLONIC MID-LEVEL CIRCULATION CENTER IS IN THE PROCESS
   OF MIGRATING INLAND....NORTH OF SAN FRANCISCO BAY.  BUT...
   OROGRAPHICALLY BACKED...SOUTHEASTERLY SURFACE WINDS BENEATH 20-30 KT
   SOUTHERLY 850 FLOW ARE MAINTAINING SIZABLE CLOCKWISE CURVED
   LOW-LEVEL HODOGRAPHS ACROSS THE INTERIOR VALLEY.  THIS MAY PERSIST
   THROUGH A LARGE PORTION OF THE AFTERNOON.  GIVEN THE COLD MID-LEVEL
   ENVIRONMENT ACROSS THIS REGION...THERE APPEARS TO BE ENOUGH
   DEVELOPING BREAKS IN THE OVERCAST TO ALLOW FOR POCKETS OF SURFACE
   HEATING AND DESTABILIZATION SUPPORTIVE OF LOW TOPPED STORM
   DEVELOPMENT.  IF THIS OCCURS...THE RISK FOR ROTATING UPDRAFTS
   CAPABLE OF PRODUCING SOME HAIL OR A BRIEF TORNADO IS NOT COMPLETELY
   NEGLIGIBLE.
   
   ..KERR.. 02/17/2009
   
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   NOTE: THE NEXT DAY 1 OUTLOOK IS SCHEDULED BY 0100Z