Jun 16, 2009 1730 UTC Day 2 Convective Outlook
Updated: Tue Jun 16 17:24:48 UTC 2009
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20090616 1730 UTC Day 2 Outlook Graphic
Probabilistic Graphic
20090616 1730 UTC Day Probabilitic Graphic
Probability Legend Image
   SPC AC 161721
   
   DAY 2 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   1221 PM CDT TUE JUN 16 2009
   
   VALID 171200Z - 181200Z
   
   ...THERE IS A SLGT RISK OF SVR TSTMS FROM PARTS OF THE CNTRL PLAINS
   SEWD INTO THE OH/TN VALLEYS AND SRN APPALACHIANS...
   
   ...SYNOPSIS...
   
   CURRENTLY FLATTENED UPPER RIDGE WILL INTENSIFY NWD INTO THE CNTRL
   CONUS WITH THE PASSAGE OF MIDLEVEL TROUGH /NOW OVER THE MIDWEST/
   THROUGH THE GREAT LAKES REGION.  UPSTREAM...POSITIVELY TILTED TROUGH
   FROM THE GREAT BASIN TO OFF BAJA WILL BECOME INCREASINGLY
   SHEARED....WHILE FARTHER N...A SERIES OF MIDLEVEL IMPULSES TRANSLATE
   EWD THROUGH THE PACIFIC NW AND NRN INTERMOUNTAIN REGION AND WRN
   CANADA.
   
   AT THE SURFACE...LOW INITIALLY NEAR CHI WILL DEVELOP EWD INTO THE
   UPPER OH VALLEY DURING THE DAY WITH AN ATTENDANT N-S ORIENTED WARM
   FRONT INTENSIFYING FROM ERN OH/WRN PA SWD INTO THE CNTRL
   APPALACHIANS.  TRAILING FRONTAL BOUNDARY WILL SETTLE SWD THROUGH THE
   MID/LOWER OH VALLEY WHILE WRN EXTENSION OF BOUNDARY LIFTS NWD
   THROUGH THE CNTRL PLAINS IN RESPONSE TO DEEPENING SURFACE LOW OVER
   KS.
   
   ...CNTRL PLAINS INTO MID MS VALLEY...
   
   CAPPING WILL STRENGTHEN OVER THE SRN INTO CNTRL PLAINS BENEATH
   BUILDING MIDLEVEL RIDGE AXIS WHICH WILL LIMIT STORM DEVELOPMENT TO N
   OF ABOVE-MENTIONED SURFACE BOUNDARY.  CURRENT GOES SOUNDER AND GPS
   PW DATA INDICATE THAT THE RICHEST MOISTURE NOW RESIDES ALONG AND E
   OF THE MS RIVER.  DEEPENING KS LOW SHOULD ALLOW FOR THE NWWD
   ADVECTION OF THIS MOISTURE THROUGH THE LOWER AND MID MO
   VALLEYS...BENEATH STEEP MIDLEVEL LAPSE RATES...CONTRIBUTING TO
   MODERATE TO STRONG INSTABILITY WITH MLCAPE OF 2000-4000 J/KG INVOF
   BOUNDARY.
   
   LATEST MODEL GUIDANCE CONTINUES TO INDICATE THAT A WEAK MIDLEVEL
   IMPULSE WILL CREST BUILDING RIDGE OVER THE CNTRL PLAINS NEAR THE
   PEAK IN THE DIURNAL HEATING CYCLE.  FORCING FOR ASCENT ASSOCIATED
   WITH THIS FEATURE COUPLED WITH PERSISTENT LOW-LEVEL WAA ARE EXPECTED
   TO FOSTER STORM DEVELOPMENT FROM MID AFTERNOON INTO EARLY EVENING
   FROM WRN NEB EWD THROUGH THE MID MO VALLEY.  
   
   FORECAST HODOGRAPHS INDICATE CONSIDERABLE VEERING IN THE LOW-LEVELS
   AND 40-50 KT OF DEEP-LAYER SHEAR WHICH WILL SUPPORT THE DEVELOPMENT
   OF SUPERCELLS CAPABLE OF LARGE HAIL...DAMAGING WINDS AND A FEW
   TORNADOES.  THE GREATEST TORNADO THREAT WILL EXIST WITH ANY
   SUPERCELLS N OF SURFACE BOUNDARY DURING THE EVENING OVER S-CNTRL
   INTO ERN NEB WHERE BOUNDARY LAYER WILL BE MORE MOIST/UNSTABLE AND
   MODERATELY SHEARED.  OTHERWISE...EXPECT UPSCALE GROWTH INTO ONE OR
   MORE LARGE TSTM CLUSTERS OVERNIGHT WITHIN STRENGTHENING WAA REGIME
   WITH A WIND AND HAIL THREAT SPREADING EWD/SEWD INTO PARTS OF THE MID
   MS VALLEY. 
   
   ...OH/TN VALLEYS INTO SRN APPALACHIANS...
   
   SCENARIO IS A BIT MORE COMPLICATED ACROSS THIS REGION DUE TO
   EXPECTED ONGOING STORMS WEDNESDAY MORNING AND THEIR EFFECTS ON AIR
   MASS DESTABILIZATION AND BOUNDARY LOCATIONS.  AS MENTIONED
   ABOVE...CURRENT OBSERVED PW DATA INDICATE A MOIST AIR MASS IN PLACE
   E OF THE MS VALLEY.  THIS MOISTURE WILL BE DRAWN NWD INTO THE UPPER
   OH VALLEY IN ADVANCE OF EWD-MIGRATING SURFACE LOW...CONTRIBUTING TO
   A MODERATELY UNSTABLE AIR MASS /MLCAPE OF 1000-2000 J PER KG/ W OF
   WARM FRONT AND E/SE OF COLD FRONT TRAILING LOW.  MOREOVER...A LOCAL
   N-S CORRIDOR OF STRONGER LOW-LEVEL SHEAR WILL COINCIDE WITH THIS
   INSTABILITY FROM NERN KY INTO OH WITH THE POTENTIAL FOR A FEW
   SUPERCELLS CAPABLE OF HAIL...DAMAGING WINDS AND PERHAPS TORNADOES
   DURING THE AFTERNOON INTO EVENING.
   
   OTHER EPISODIC STRONG/SEVERE STORMS WILL BE POSSIBLE FROM VICINITY
   OF TRAILING FRONTAL BOUNDARY OVER KY/TN SSEWD ALONG RETREATING WEDGE
   FRONT OVER PORTIONS OF GA/SC.  THIS AREA WILL RESIDE TO THE S OF
   STRONGER MID/HIGH-LEVEL FLOW...BUT THE PRESENCE OF A MODERATELY
   UNSTABLE AIR MASS INVOF SURFACE BOUNDARY WILL BE SUPPORTIVE OF A FEW
   ORGANIZED TSTM CLUSTERS CAPABLE OF DAMAGING WINDS AND SOME HAIL.
   
   ..MEAD.. 06/16/2009
   
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