May 5, 2008 2000 UTC Day 1 Convective Outlook
Updated: Mon May 5 19:54:19 UTC 2008
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20080505 2000 UTC Day 1 Outlook Graphic
Probabilistic Tornado Graphic
20080505 2000 UTC Day 1 Tornado Probabilities Graphic
Torndao Legend Image
Probabilistic Damaging Wind Graphic
20080505 2000 UTC Day 1 Damaging Wind Probabilities Graphic
Wind Legend Image
Probabilistic Large Hail Graphic
20080505 2000 UTC Day 1 Large Hail Probabilities Graphic
Hail Legend Image
   SPC AC 051950
   
   DAY 1 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   0250 PM CDT MON MAY 05 2008
   
   VALID 052000Z - 061200Z
   
   ...THERE IS A SLGT RISK OF SVR TSTMS PORTIONS ERN SC AND SRN NC...
   
   ...THERE IS A SLGT RISK OF SVR TSTMS PORTIONS CENTRAL PLAINS AND SRN
   HIGH PLAINS TO LOWER PECOS VALLEY...
   
   ...SYNOPSIS...
   PROGRESSIVE UPPER AIR PATTERN IS FCST THROUGH REMAINDER
   PERIOD...WITH MEAN TROUGHING EXTENDING FROM HUDSON BAY CYCLONE SSEWD
   OFFSHORE SRN ATLANTIC COAST.  CLOSED AND NEARLY CUT OFF LOW ALOFT --
   EVIDENT IN MOISTURE CHANNEL IMAGERY OFFSHORE NRN BAJA -- HAS BEGUN
   ITS EWD TURN AND SHOULD MOVE INLAND AROUND 6/00Z.  THIS LOW THEN
   SHOULD MOVE ENEWD ACROSS CO RIVER DELTA REGION TO SWRN AZ BY END OF
   PERIOD.
   
   DOWNSTREAM...WEAK UPPER PERTURBATION NOW OVER NWRN/N-CENTRAL MEX IS
   EXPECTED TO LIFT NEWD TOWARD DEEP S TX.  WEAK SHORTWAVE TROUGH IS
   EMBEDDED IN NWLY FLOW ALOFT OVER CENTRAL/SRN APPALACHIANS
   REGION...AND IS FCST TO MOVE OFFSHORE COASTAL CAROLINAS DURING
   6/00Z-6/03Z TIME FRAME.
   
   AT SFC...DRYLINE IS ANALYZED JUST E OF NM MOUNTAINS...WITH LITTLE
   MOVEMENT EXPECTED THROUGH REMAINDER PERIOD.  RESIDUAL SYNOPTIC
   FRONTAL ZONE -- LEFT OVER FROM PREVIOUS NRN GULF COLD FROPA -- IS
   ANALYZED FROM ABOUT 150-200 NM S OF LA COAST WNWWD ACROSS SE AND
   S-CENTRAL TX...BECOMING DIFFUSE AMIDST GEN SELY FLOW FARTHER NWWD
   OVER LOWER PECOS VALLEY AND PERMIAN BASIN REGIONS.  WEAK LOW IS
   ANALYZED OVER ERN SC...AND SHOULD REMAIN ILL-DEFINED AS UPPER LEVEL
   TROUGH MOVES PAST.  CONVECTIVE PROCESSES IN THAT AREA WILL BE
   DOMINATED MORE BY LOCALIZED/BOUNDARY EFFECTS.
   
   ...CENTRAL/SRN HIGH PLAINS...
   TSTMS SHOULD CONTINUE TO DEVELOP AND INCREASE IN COVERAGE OVER
   HIGHER TERRAIN OF ERN NM...MOVING NEWD ONTO ADJACENT HIGH PLAINS
   THROUGH REMAINDER AFTERNOON.  SOME OF THIS ACTIVITY ALREADY HAS 
   EVOLVED SUPERCELL STRUCTURES...WITH MORE TO COME.  LARGE HAIL IS
   PRIMARY THREAT...AS FOREGOING AIR MASS HEATS/DESTABILIZES FOLLOWING
   BREAKUP OF EARLIER LOW LEVEL CLOUD COVER.  ISOLATED HAIL EXCEEDING
   TWO INCHES DIAMETER IS POSSIBLE...GIVEN STEEP LAPSE
   RATES...INCREASING INFLOW-LAYER WATER CONTENT...AND LIKELIHOOD OF
   SUSTAINED STORM-SCALE ROTATION.  A FEW TORNADOES ALSO MAY OCCUR. REF
   WW 261 AND SUBSEQUENT MESOSCALE DISCUSSION FOR THAT AREA...FOR
   LATEST SHORT-TERM GUIDANCE REGARDING THIS SITUATION.  SIGNIFICANT
   HAIL THREAT ALSO EXTENDS SSEWD FROM ERN NM ACROSS FAR W TX AND LOWER
   PECOS VALLEY REGIONS...SHIFTING EWD TOWARD PORTIONS PERMIAN
   BASIN...PER MESOSCALE DISCUSSION 789.
   
   REF MESOSCALE DISCUSSION 788 FOR NOWCAST GUIDANCE REGARDING SVR
   POTENTIAL INCREASING ATTM OVER S-CENTRAL HIGH PLAINS FROM WRN KS SWD
   INTO TX PANHANDLE.  MOISTURE LIKEWISE IS FCST TO INCREASE ACROSS
   THIS REGION THROUGHOUT REMAINDER PERIOD...LEADING TO POTENTIAL FOR
   SUPERCELL DEVELOPMENT THIS AFTERNOON AND EARLY EVENING...AND
   POSSIBLE UPSCALE GROWTH INTO MCS OVERNIGHT.  SVR HAIL AND GUSTS ARE
   MAIN THREATS WITH BOTH MODES OF CONVECTION.
   
   ...ERN CAROLINAS...
   SCATTERED TSTMS ARE UNDERWAY ACROSS THIS REGION IN WEAKLY CAPPED AND
   FAVORABLY HEATED/UNSTABLE AIR MASS...PERTURBED AND DESTABILIZED
   ALOFT BY WEAK SHORTWAVE TROUGH NOW EVIDENT OVER REGION.  DAMAGING
   DOWNDRAFT WINDS AND SCTD REPORTS OF MRGL SEVERE HAIL ARE EXPECTED. 
   ALTHOUGH LOW LEV LEVEL FLOW IS FCST TO REMAIN RATHER WEAK IN MOST
   AREAS...LIMITING HODOGRAPH SIZE...RELATIVELY STG UPPER LEVEL WINDS
   -- E.G. 60-70 KT AT ANVIL LEVEL -- SHOULD AID IN STORM ORGANIZATION.
    PREDOMINANT STORM MODE SHOULD BE MULTICELLULAR...ALTHOUGH
   BRIEF/MESSY SUPERCELL MODES MAY DEVELOP LOCALLY AS STORMS INTERACT
   WITH OUTFLOW/SEA BREEZE BOUNDARIES AND WITH OTHER STORMS.  REF WW
   260 AND RELATED MESOSCALE DISCUSSIONS FOR LATEST NOWCAST INFO.  SVR
   THREAT IS EXPECTED TO DIMINISH AFTER DARK...AS AIR MASS BECOMES MORE
   STABLE FROM COMBINATION OF DIABATIC SFC COOLING...INCREASING
   COVERAGE OF OUTFLOW-COOLED AIR...AND DEPARTURE OF MID-UPPER WAVE AND
   OF ASSOCIATED LARGE SCALE ASCENT.
   
   ...NWRN THROUGH CENTRAL/S TX...E-SE OF HIGH PLAINS...
   ERN PORTION OF RETURNING WARM/MARINE FRONT HAS MERGED WITH -- AND
   BECOME REINFORCED BY  -- QUASISTATIONARY DIFFERENTIAL HEATING
   BOUNDARY THAT EXTENDS FROM MIDDLE TX COAST NEAR MATAGORDA BAY...NWWD
   ACROSS NRN HILL COUNTRY AND LOW ROLLING PLAINS REGIONS OF CENTRAL-NW
   TX.  ADDITIONAL/ELEVATED TSTM DEVELOPMENT SHOULD CONTINUE IN ZONE OF
   ELEVATED ISENTROPIC LIFT TO LFC...JUST NE OF THIS BOUNDARY. 
   ISOLATED HAIL NEAR SVR LEVELS CANNOT BE RULED OUT...HOWEVER
   ORGANIZED SVR POTENTIAL APPEARS MINIMAL ATTM.
   
   FARTHER W...CONDITIONAL POTENTIAL EXISTS FOR TSTMS TO DEVELOP OVER
   SERRANIAS DEL BURRO RANGE AND ADJACENT PIEDMONT SLOPE OF NRN
   COAHUILA...THEN MOVE EWD-NEWD ACROSS RIO GRANDE INTO S TX.  CINH
   SHOULD CONTINUE TO WEAKEN OVER HIGHER TERRAIN THROUGH REMAINDER
   AFTERNOON...ESPECIALLY AS REMAINING LOW CLOUDS BREAK UP AND ALLOW
   STRONGER SFC DIABATIC HEATING.  ANY SUCH ACTIVITY MAY PRODUCE LARGE
   HAIL AND STG-SVR GUSTS LATE AFTERNOON INTO EARLY EVENING BEFORE
   WEAKENING.
   
   ..EDWARDS.. 05/05/2008
   
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   NOTE: THE NEXT DAY 1 OUTLOOK IS SCHEDULED BY 0100Z