Mar 23, 2009 2000 UTC Day 1 Convective Outlook
Updated: Mon Mar 23 19:44:19 UTC 2009
Probabilistic to Categorical Outlook Conversion Table (Effective Feb 14, 2006).
Public Severe Weather Outlook

The SPC is forecasting ...severe thunderstorms expected over parts of the central and southern plains....   Please read the latest public statement about this event.

Categorical Graphic
20090323 2000 UTC Day 1 Outlook Graphic
Probabilistic Tornado Graphic
20090323 2000 UTC Day 1 Tornado Probabilities Graphic
Torndao Legend Image
Probabilistic Damaging Wind Graphic
20090323 2000 UTC Day 1 Damaging Wind Probabilities Graphic
Wind Legend Image
Probabilistic Large Hail Graphic
20090323 2000 UTC Day 1 Large Hail Probabilities Graphic
Hail Legend Image
   SPC AC 231940
   
   DAY 1 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
   0240 PM CDT MON MAR 23 2009
   
   VALID 232000Z - 241200Z
   
   ...THERE IS A MDT RISK OF SVR TSTMS LATE THIS AFTN/EARLY EVE ACROSS
   PARTS OF N CNTRL/NE OK INTO CNTRL/ERN KS....
   
   ...THERE IS A SLGT RISK OF SVR TSTMS LATE THIS AFTN INTO TONIGHT
   ACROSS PARTS OF THE CNTRL/SRN PLAINS AND MID/LWR MO VALLEY....
   
   ...PLAINS/MISSOURI VALLEY...
   THE EXIT REGION OF THE STRONG POLAR JET STREAK IS ALREADY SHIFTING
   NORTHEASTWARD ACROSS THE NORTH CENTRAL PLAINS...WITH AN INITIAL
   IMPULSE PIVOTING AROUND THE EASTERN PERIPHERY OF A CLOSED MID-LEVEL
   CIRCULATION OVER WEST CENTRAL NEBRASKA.  FORCING ASSOCIATED WITH
   THIS FEATURE HAS CONTRIBUTED TO ONGOING CONVECTIVE DEVELOPMENT ALONG
   THE DRY LINE...WHICH ARCS SOUTH OF A THE DEEP SURFACE LOW...ACROSS
   SOUTH CENTRAL NEBRASKA INTO CENTRAL KANSAS AND WESTERN OKLAHOMA.
   
   THROUGH THE REMAINDER OF THE AFTERNOON...ALL INDICATIONS CONTINUE TO
   SUGGEST THAT THE SURFACE LOW WILL SLOWLY DEEPEN AND MIGRATE
   NORTHEASTWARD THROUGH THE MID MISSOURI VALLEY...WITH A COLD FRONT
   OVERTAKING THE DRY LINE ACROSS CENTRAL/EASTERN NEBRASKA AND NORTH
   CENTRAL KANSAS.  THE SPEED AT WHICH THIS OCCURS IS STILL SOMEWHAT
   UNCERTAIN...AND PRIMARILY AFFECTS THE TRANSITION FROM A MORE
   DISCRETE CONVECTIVE MODE TO A SOLIDIFYING SQUALL LINE.  AS THIS
   OCCURS...THE POTENTIAL FOR DAMAGING WINDS MAY BECOME MOST
   PROMINENT...IN THE PRESENCE OF A 50-60 KT DEEP LAYER MEAN FLOW
   FIELD.  LOW-LEVEL MOISTURE VALUES ARE LIKELY TO REMAIN SEEMINGLY
   ONLY MARGINALLY SUPPORTIVE OF TORNADIC POTENTIAL...BUT LARGE
   CLOCKWISE CURVED LOW-LEVEL HODOGRAPHS AND AMBIENT VERTICAL VORTICITY
   MAY COMPENSATE...PARTICULARLY LATE THIS AFTERNOON/EARLY EVENING AS
   ACTIVITY CROSSES DEVELOPING WARM FRONT CLOSER TO THE MISSOURI RIVER.
   
   
   FARTHER SOUTH...THE COLD FRONT IS EXPECTED TO BE SLOWER TO OVERTAKE
   THE DRY LINE NEAR THE KANSAS/OKLAHOMA BORDER AREA...WHERE FORCING
   FOR DISCRETE STORMS IS EXPECTED TO REMAIN FAVORABLE INTO AND PERHAPS
   THROUGH MUCH OF THE EVENING HOURS.  SOUTHWESTERLY FLOW BENEATH THE
   STRONG CYCLONIC MID/UPPER JET AXIS IS EXPECTED TO ADVECT SUSTAINED
   STORMS...LIKELY SUPERCELLS...AWAY FROM THE DRY LINE.  BUT...A
   RELATIVELY NARROW PRE-FRONT/DRY LINE LOW-LEVEL MOIST TONGUE STILL
   APPEARS LIKELY TO LIMIT THE PRIMARY SEVERE THREAT WITH THIS ACTIVITY
   TO PARTS OF NORTH CENTRAL/NORTHEAST OKLAHOMA INTO THE I-35 CORRIDOR
   OF CENTRAL/EASTERN KANSAS.  SLIGHTLY HIGHER BOUNDARY LAYER MOISTURE
   CONTENT ACROSS THIS REGION /MID TO UPPER 50S SURFACE DEW POINTS/
   SHOULD BE MORE CONDUCIVE TO THE RISK FOR TORNADOES...AS COMPARED TO
   AREAS FARTHER NORTH.
   
   EVENTUALLY...THE SURFACE COLD FRONT IS EXPECTED TO OVERTAKE THE DRY
   LINE LATER THIS EVENING/OVERNIGHT...FROM PARTS OF SOUTHEAST KANSAS
   THROUGH OKLAHOMA INTO NORTHWEST TEXAS.  THIS MAY BE ACCOMPANIED BY
   AN INCREASE IN CONVECTIVE DEVELOPMENT...PERHAPS AIDED BY FORCING
   ASSOCIATED WITH THE NEXT IMPULSE...EMANATING FROM THE SOUTHERN GREAT
   BASIN...BEFORE PIVOTING AROUND THE SOUTHERN/ EASTERN PERIPHERY OF
   THE CLOSED LOW.  WHILE THE SEVERE THREAT DIMINISHES WITH THE STORMS
   SPREADING EAST OF THE MID MISSOURI VALLEY...AS THEY BECOME CUT-OFF
   FROM THE BETTER GULF RETURN FLOW ...IT IS POSSIBLE THAT
   STRONG/SEVERE CONVECTION MAY PERSIST A BIT DEEPER INTO THE NIGHT
   ACROSS THE SOUTH CENTRAL PLAINS...BEFORE BOUNDARY LAYER BASED
   INSTABILITY WANES.
   
   ..KERR.. 03/23/2009
   
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   NOTE: THE NEXT DAY 1 OUTLOOK IS SCHEDULED BY 0100Z