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Mesoscale Discussion 1909 |
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MESOSCALE DISCUSSION 1909
NWS STORM PREDICTION CENTER NORMAN OK
1100 PM CDT MON AUG 08 2011
AREAS AFFECTED...PORTIONS CENTRAL-ERN OK...EXTREME SERN KS...EXTREME
NERN OK..SWRN MO...AR.
CONCERNING...SEVERE THUNDERSTORM WATCH 748...751...
VALID 090400Z - 090600Z
THE SEVERE WEATHER THREAT FOR SEVERE THUNDERSTORM WATCH
748...751...CONTINUES.
ALTHOUGH SVR CANNOT BE RULED OUT WITH ANY SUSTAINED TSTMS...MOST
CONCENTRATED/ORGANIZED POTENTIAL APPEARS TO HAVE FOCUSED INTO
COMPLEX MOVING SEWD ON EITHER SIDE OF OLD OUTFLOW BOUNDARY. AREAS
FARTHER SE ACROSS AR WILL BE MONITORED FOR POSSIBLE WW...BASED ON
TRENDS IN UPSHEAR CONVECTION AND PRECONVECTIVE INSTABILITY.
AS OF 330Z...OUTFLOW BOUNDARY FROM COMPLEX NOW OVER WW 752 WAS
ANALYZED FROM GLH NWD ACROSS PIKE COUNTY AR TO HASKELL COUNTY
OK...INTERSECTING GUST FRONT PRODUCED BY BKN BAND OF TSTMS OVER NWRN
AR AND ERN OK. ISENTROPIC ASCENT OF LOW-LEVEL AIR ABOVE COOL SIDE
OF THAT BOUNDARY MAY FOCUS STRONGEST LIFT AND MOST LONG-LIVED
CONVECTIVE POTENTIAL TO ITS N...ESPECIALLY WITH DIABATIC SFC COOLING
LEADING TO GREATER MLCINH WITH TIME IN UNDISTURBED WARM SECTOR.
THIS PROCESS MAY HELP TO SUSTAIN CONVECTION LONGER ACROSS NWRN
THROUGH CENTRAL AR. MODIFIED FCST SOUNDINGS SUGGEST SHALLOW LAYER
OF SFC-BASED STATIC STABILITY N OF BOUNDARY...BUT ALSO...REMNANT
MIXED LAYER BETWEEN THAT AND CLOUD BASE THAT COULD SUPPORT
EVAPORATIVE COOLING/ACCELERATION OF MOST INTENSE DOWNDRAFTS THROUGH
THAT STABLE LAYER. AS SUCH...SVR WIND THREAT MAY BECOME MORE
SPORADIC WITH TIME...BUT REMAINS SUFFICIENT TO CONTINUE WW.
STRENGTH/DEPTH OF STABLE LAYER SHOULD INCREASE WITH NWD
EXTENT...DIMINISHING WIND POTENTIAL ACROSS OZARKS INTO SRN MO.
..EDWARDS.. 08/09/2011
ATTN...WFO...LZK...SGF...SHV...TSA...ICT...OUN...
LAT...LON 35229783 35719712 35689646 35559557 35889476 36319414
36639480 36979534 37399489 37339385 36189217 35369155
34949150 33619196 33839345 34689582 35229783
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