Jul 31, 2008 1300 UTC Day 1 Convective Outlook
Updated: Thu Jul 31 12:53:14 UTC 2008
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20080731 1300 UTC Day 1 Outlook Graphic
Probabilistic Tornado Graphic
20080731 1300 UTC Day 1 Tornado Probabilities Graphic
Torndao Legend Image
Probabilistic Damaging Wind Graphic
20080731 1300 UTC Day 1 Damaging Wind Probabilities Graphic
Wind Legend Image
Probabilistic Large Hail Graphic
20080731 1300 UTC Day 1 Large Hail Probabilities Graphic
Hail Legend Image
   SPC AC 311249
   
   DAY 1 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   0749 AM CDT THU JUL 31 2008
   
   VALID 311300Z - 011200Z
   
   ...THERE IS A SLGT RISK OF SVR TSTMS FROM THE NRN MS RIVER VALLEY
   ACROSS THE SRN GREAT LAKES REGION...
   
   ...THERE IS A SLGT RISK OF SVR TSTMS OVER MUCH OF THE CAROLINAS...
   
   ...UPPER MIDWEST...
   LONG-LIVED BOW ECHO WITH HISTORY OF SIGNIFICANT DAMAGING WINDS EARLY
   THURSDAY MORNING CONTINUES ALONG WELL-DEFINED SURFACE FRONT
   EXTENDING FROM THE SRN GREAT LAKES INTO SERN MN AS OF 13Z.  SOME
   QUESTION ABOUT WHETHER OR NOT SYSTEM WILL SURVIVE STRONG CAPPING
   THROUGH THE MID/LATE MORNING ACROSS THE UPPER MS RIVER VALLEY. 
   HOWEVER...CLEAR SKIES AND STEEP LAPSE RATES AHEAD OF THE
   SYSTEM...ALONG WITH WELL-DEFINED MCV...SUGGEST SYSTEM MAY EITHER
   CONTINUE SEVERE OR WEAKEN BRIEFLY BEFORE RE-INTENSIFYING LATER THIS
   MORNING/EARLY THIS AFTERNOON DOWNSTREAM.  IF SYSTEM DOES WEAKEN
   CONSIDERABLY THIS MORNING...RELATED OUTFLOW/DIFFERENTIAL HEATING
   ZONE WILL BLEND WITH SYNOPTIC WARM FRONT OVER NRN IA/SRN WI INTO NRN
   IL.  THIS SHOULD SERVE AS PRIMARY FOCUS FOR AFTERNOON/EVENING SVR
   POTENTIAL INCLUDING SUPERCELL RISK.
   
   BY AFTERNOON...VERY STG INSTABILITY SHOULD DEVELOP WITHIN AND S OF
   WARM FRONTAL/DIFFERENTIAL HEATING ZONE...WITH STG SFC HEATING AND
   FRONTAL CONVERGENCE TO YIELD WEAK CINH.  SFC DEW POINTS IN THE UPPER
   60S TO LOW 70S F WILL BE COMMON BY MID-LATE AFTERNOON BENEATH 7-8
   DEG C/KM MIDLEVEL LAPSE RATES...CONTRIBUTING TO MLCAPES IN 3000-4000
   J/KG RANGE.  ALTHOUGH SFC WINDS ARE NOT FCST TO BE PARTICULARLY
   STG...DIRECTIONAL SHEAR IS.  RELATIVELY BACKED FLOW INVOF BOUNDARY
   SHOULD YIELD LOOPED HODOGRAPHS...AS WELL AS ENHANCED STORM-RELATIVE
   INFLOW IN NARROW CORRIDOR.  DISCRETE SUPERCELLS WOULD HAVE POTENTIAL
   FOR DAMAGING HAIL GIVEN THEIR INTERNAL FORCING AND LARGE AMBIENT
   BUOYANCY.  INSTABILITY GRADIENT WILL BE FAVORED CORRIDOR FOR MOTION
   OF ANY SUBSEQUENT MCS...EXPANDED UPSCALE OR RE-INTENSIFIED FROM
   EARLIER ACTIVITY.  ASSOCIATED WIND THREAT MAY EXTEND ACROSS MUCH OF
   THE SRN GREAT LAKES AND CENTRAL IND/IL GIVEN BROAD REGION OF
   MODERATE NWLY FLOW ALOFT.
   
   ...SERN CONUS...
   RELATIVE CONCENTRATION OF PULSE/MULTICELL EVENTS -- PRIMARILY
   DAMAGING DOWNBURST WINDS -- MAY DEVELOP DURING AFTERNOON AS CINH
   WEAKENS...NEAR AND E OF WEAK LEE-SIDE TROUGH.  SCATTERED-NUMEROUS
   TSTMS IN CLUSTERS ARE POSSIBLE.  SFC DEW POINTS COMMONLY 70S F --
   WITH SOME POCKETS MIXED INTO UPPER 60S -- COMBINED WITH STG DIABATIC
   HEATING SHOULD BE SUFFICIENT TO OVERCOME WEAK LAPSE RATES ALOFT. 
   RESULT SHOULD BE MLCAPES 1500-2500 J/KG ATOP STEEP THERMAL LAPSE
   RATES IN SUB CLOUD LAYER.  FCST SOUNDINGS SUGGEST SHALLOW INVERTED-V
   PROFILE CHARACTERISTIC OF WELL-MIXED ENVIRONMENTS AND SUPPORTING
   DOWNDRAFT ACCELERATION.  COLD POOL ORGANIZATION AND OUTFLOW
   BOUNDARIES WILL STRONGLY INFLUENCE THREAT WITHIN OUTLOOK AREA.
   
   ...NERN CONUS...
   WEAK CONVERGENCE INVOF FRONT/TROUGH...DIURNAL HEATING...AND
   FAVORABLE MOISTURE SHOULD SUPPORT POTENTIAL FOR SCATTERED LATE
   MORNING THROUGH LATE AFTERNOON TSTMS WITH RISK FOR STRONG/MARGINALLY
   SEVERE WIND GUSTS AND/OR HAIL.  SHEAR WILL REMAIN SUPPORTIVE OF WEAK
   STORM-SCALE ORGANIZATION...ALTHOUGH VERY WEAK LOW-MID LEVEL LAPSE
   RATES WILL LIMIT BOTH AVAILABLE INSTABILITY AND RESULTANT UPDRAFT
   INTENSITIES.
   
   ...TN-TX...
   FRONTAL ZONE WILL CONCENTRATE CONVECTIVE POTENTIAL DURING
   AFTERNOON...AND MAY BE ENHANCED BY DIFFERENTIAL HEATING OVER TN/KY
   AREA -- S OF LARGE/PERSISTENT AREA OF PRECIP AND CLOUDS PRESENTLY
   UNDERWAY AND LIKELY TO PERSIST THROUGH MUCH OF REMAINDER OF MORNING.
    LOCALIZED AREAS OF ENHANCED PULSE/MULTICELL POTENTIAL MAY DEVELOP
   INVOF STRONGER BOUNDARIES OR THEIR INTERSECTIONS...HOWEVER
   COMBINATION OF SUCH MESOSCALE UNCERTAINTIES AND WEAKNESS OF
   DEEP-LAYER WIND FIELDS PRECLUDES CATEGORICAL OUTLOOK ATTM.
   
   ..EVANS/EDWARDS/SMITH.. 07/31/2008
   
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