May 28, 2008 2000 UTC Day 1 Convective Outlook
Updated: Wed May 28 19:47:11 UTC 2008
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Categorical Graphic
20080528 2000 UTC Day 1 Outlook Graphic
Probabilistic Tornado Graphic
20080528 2000 UTC Day 1 Tornado Probabilities Graphic
Torndao Legend Image
Probabilistic Damaging Wind Graphic
20080528 2000 UTC Day 1 Damaging Wind Probabilities Graphic
Wind Legend Image
Probabilistic Large Hail Graphic
20080528 2000 UTC Day 1 Large Hail Probabilities Graphic
Hail Legend Image
   SPC AC 281943
   
   DAY 1 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   0243 PM CDT WED MAY 28 2008
   
   VALID 282000Z - 291200Z
   
   ...THERE IS A SLGT RISK OF SVR TSTMS THIS AFTN/EVE ACROSS PARTS OF
   ERN NM....
   
   ...THERE IS A SLGT RISK OF SVR TSTMS THIS AFTN/EVE ACROSS PARTS OF
   CNTRL/ERN CO AND WY....
   
   ...SYNOPSIS...
   ALTHOUGH ANOTHER STRONG SHORT WAVE TROUGH IS NOW DIGGING TO THE EAST
   SOUTHEAST OF HUDSON BAY...THE BROADER SCALE COLD NORTHERN BRANCH
   TROUGH IS IN THE PROCESS OF BEGINNING TO SHIFT EASTWARD OUT OF THE
   EASTERN CANADIAN PROVINCES AND NORTHEASTERN UNITED STATES.  AS THIS
   OCCURS...THE CENTER OF THE COLD SURFACE RIDGE ENCOMPASSING MUCH OF
   THE NORTH CENTRAL AND NORTHEASTERN U.S. IS GRADUALLY WEAKENING...AND
   SHIFTING EASTWARD.  COOLER BOUNDARY LAYER AIR IS BEGINNING TO NOSE
   SOUTHWARD TO THE LEE OF THE SOUTHERN APPALACHIANS...BUT THE FRONTAL
   ZONE EXTENDING ACROSS THE TENNESSEE VALLEY AND OZARK PLATEAU INTO
   THE SOUTHERN HIGH PLAINS IS IN THE PROCESS OF WEAKENING...AND WILL
   CONTINUE TO DO SO THROUGH THE REMAINDER OF THE PERIOD.  WITH
   DESTABILIZATION LIMITED/SLOW TO OCCUR IN THE WAKE OF THIS
   FEATURE...CONVECTIVE POTENTIAL ACROSS MUCH OF THE NATION IS AT A
   RELATIVE MINIMUM.
   
   HOWEVER...A STRONG MID/UPPER JET STREAK IS BEGINNING TO EMERGE FROM
   THE BASE OF THE BROAD EASTERN PACIFIC/WESTERN U.S. SOUTHERN BRANCH
   TROUGH...AND NOSE TOWARD THE CREST OF AN AMPLIFYING SUBTROPICAL
   RIDGE OVER THE CENTRAL/SOUTHERN PLAINS.  SMALLER SCALE PERTURBATIONS
   ASSOCIATED WITH THIS FEATURE MAY CONTRIBUTE TO AREAS OF ENHANCED
   CONVECTIVE DEVELOPMENT ACROSS PARTS OF THE NORTHERN INTERMOUNTAIN
   REGION/NORTHERN ROCKIES AND IMMEDIATE LEE OF THE CENTRAL/SOUTHERN
   ROCKIES.  THIS IS WHERE MOISTURE LEVELS ARE STILL SOMEWHAT LOW...BUT
   STEEP LAPSE RATES COULD SUPPORT ISOLATED SEVERE STORMS.
   
   ...PARTS OF CNTRL/ERN NEW MEXICO...
   THE BEST LOW-LEVEL MOISTURE IS AVAILABLE TO CONVECTION NOW  FORMING
   ACROSS THE HIGHER TERRAIN FROM THE MOUNTAINS OF CENTRAL NEW MEXICO
   INTO SOUTHWEST TEXAS.  AS UPPER 50S/LOWER 60S SURFACE DEW POINTS
   RETURN TO THE SOUTH OF THE RESIDUAL WEAKENING FRONTAL ZONE...MIXED
   LAYER CAPE INCREASING UP TO 1000 J/KG...PERHAPS LOCALLY AS HIGH AS
   2000 J/KG...WILL SUPPORT INTENSIFICATION OF ACTIVITY AS IT
   PROPAGATES OFF THE HIGHER TERRAIN WITHIN MODEST SOUTHWESTERLY
   MID/UPPER FLOW.  COUPLED WITH VEERING WINDS WITH HEIGHT IN THE LOWER
   THROUGH MID-LEVELS...DEEP LAYER SHEAR IS SUFFICIENT FOR SUPERCELLS
   CAPABLE OF PRODUCING LARGE HAIL/LOCALIZED DAMAGING WIND GUSTS. 
   VORTICITY ASSOCIATED WITH A REMNANT SURFACE BAROCLINIC ZONE
   EAST/SOUTHEAST OF ALBUQUERQUE MAY EVEN CONTRIBUTE TO THE RISK FOR A
   TORNADO OR TWO.
   
   ...CENTRAL ROCKIES INTO THE MID MISSOURI VALLEY...
   FORCING DOWNSTREAM OF AN IMPULSE NOW LIFTING INTO/THROUGH THE LOWER
   COLORADO VALLEY MAY CONTRIBUTE TO SCATTERED STRONG/SEVERE STORMS TO
   THE LEE OF THE FRONT RANGE OF THE ROCKIES.  BUT...A MORE PROMINENT
   CONVECTIVE CLUSTER MAY EVENTUALLY EVOLVE LATER TONIGHT IN A
   DOWNSTREAM LOWER/MID TROPOSPHERIC WARM ADVECTION ACROSS PARTS OF THE
   MID MISSOURI VALLEY.  THIS IS WHERE AN ELEVATED MOISTURE RETURN MAY
   ALSO CONTRIBUTE TO SUFFICIENT DESTABILIZATION FOR STORMS CAPABLE OF
   PRODUCING MAINLY SMALL TO MARGINALLY SEVERE HAIL.
   
   ...GULF COAST/SOUTH ATLANTIC COAST STATES...
   CONVECTIVE POTENTIAL STILL SEEMS LOW WITH STORMS NOW DEVELOPING NEAR
   COLD FRONT ADVANCING TO THE LEE OF THE SOUTHERN APPALACHIANS ...AND
   ALONG A REMNANT CONVECTIVELY GENERATED BOUNDARY ACROSS THE GULF
   STATES.  THIS IS PRIMARILY DUE TO WEAK INSTABILITY.  BUT... RATHER
   STEEP LOW-LEVEL LAPSE RATES IN THE PEAK AFTERNOON HEATING COULD
   SUPPORT GUSTY WINDS NEAR STRONGER CELLS.
   
   ..KERR/KIS.. 05/28/2008
   
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