Friday, June 22, 2012

MESOSCALE DISCUSSION 1239, AREAS AFFECTED...PORTIONS NRN/ERN VA...CENTRAL/ERN PA...SWRN NEW ENGLAND...SRN NY...DE...MD...NJ...DC. CONCERNING...SEVERE POTENTIAL...WATCH POSSIBLE





        MESOSCALE DISCUSSION 1239     NWS STORM PREDICTION CENTER NORMAN OK     1118 AM CDT FRI JUN 22 2012          AREAS AFFECTED...PORTIONS NRN/ERN  VA...CENTRAL/ERN PA...SWRN NEW     ENGLAND...SRN NY...DE...MD...NJ...DC.          CONCERNING...SEVERE POTENTIAL...WATCH POSSIBLE           VALID 221618Z - 221845Z          PROBABILITY OF WATCH ISSUANCE...60 PERCENT          SUMMARY...SVR THREAT FCST TO INCREASE FROM MULTICELLULAR     CONVECTION...OF DISCRETE...CLUSTERED AND QUASI-LINEAR     CHARACTER...DEVELOPING THROUGH MID-AFTERNOON AND MOVING OVER THIS     AREA.  MAIN CONCERN IS DAMAGING GUSTS.          DISCUSSION...TSTMS ARE FCST TO DEVELOP IN AT LEAST TWO PRIMARY     SWATHS OR BANDS...     1. NEAR AND E OF DIFFERENTIAL HEATING ZONE...ASSOCIATED WITH     LOW-MIDDLE LEVEL CLOUD BAND NOW EVIDENT ON VIS IMAGERY FROM ERN PA     SWWD ACROSS VA/WV BORDER REGION.  ANY SUCH TSTMS WILL POSE EARLIEST     SVR RISK FROM TIDEWATER AREA NEWD OVER COASTAL MID-ATLC AND SRN NEW     ENGLAND.     2. ALONG/AHEAD OF SFC COLD FRONT...INITIALLY OVER HIGHER TERRAIN OF     CENTRAL PA INTO NRN WV.  FRONT PRECEDES POSITIVELY TILTED MID-UPPER     TROUGH BY ABOUT 100-150 NM USING MOISTURE CHANNEL IMAGERY...BUT WITH     SOME LARGE-SCALE ASCENT EVIDENT OVER FRONTAL ZONE.  THESE FEATURES     WILL SHIFT EWD OVER MID-ATLC REGION THIS AFTERNOON.          16Z SFC ANALYSIS SHOWED COLD FRONT FROM NRN NY SWWD ACROSS     CENTRAL/SWRN PA AND WRN WV.  SFC TROUGH WITH WEAK EMBEDDED LOWS WAS     EVIDENT PARALLEL TO COLD FRONT AND FARTHER E...EXTENDING FROM SERN     VA NNEWD OVER SRN CHESAPEAKE BAY AND ERN NJ TO RI AND ERN     MA...INTERSECTING WARM FRONT JUST OFFSHORE NH.  WARM FRONT EXTENDED     NNEWD FROM THERE OVER MAINE.  TROUGH APPEARS COLLOCATED WITH SEA     BREEZE BOUNDARY OVER ERN NJ...AND A COUPLE OF TSTMS ALREADY HAVE     DEVELOPED THERE.          MODIFIED IAD/APG/WAL/OKX RAOBS SUGGEST PREFRONTAL BOUNDARY LAYER      SHOULD MIX VIGOROUSLY ACROSS MUCH OF NEAR-COASTAL CORRIDOR IN     RESPONSE TO CONTINUED STG SFC DIABATIC HEATING.  SIMILAR PROCESS     SHOULD OCCUR BEHIND AFOREMENTIONED PREFRONTAL CLOUD BAND.  RESULT     WOULD BE POCKETS OF REDUCED SFC DEW POINTS...AT BASE OF INVERTED-V     THERMODYNAMIC PROFILE FEATURING NEARLY DRY-ADIABATIC LOW-LEVEL LAPSE     RATES.  YET MOISTURE WILL REMAIN SUFFICIENT EVEN IN THOSE RELATIVELY     DRY AREAS TO OFFSET MODEST MIDLEVEL LAPSE RATES AND KEEP AT LEAST     MRGL BUOYANCY OVER REGION.  GIVEN HORIZONTALLY INHOMOGENEOUS NATURE     OF EXPECTED MIXING/MOISTURE FIELDS...MLCAPE WILL VARY GREATLY WITH     VALUES RANGING FROM 500-2500 J/KG...TRENDING INVERSELY WITH STRENGTH     OF VERTICAL MIXING.  30-35 KT EFFECTIVE SHEAR MAGNITUDES SUPPORT     SOME ORGANIZATION TO MULTICELL MODES...AND POTENTIAL FOR SMALL BOWS     WITH LOCALLY ENHANCED COLD-POOL FORCING.          ..EDWARDS/WEISS.. 06/22/2012               ATTN...WFO...BOX...OKX...ALY...PHI...BGM...AKQ...CTP...LWX...          LAT...LON   40577881 43297415 41777296 41317279 40647311 40567396                 40587407 40487425 40417399 39797408 39447430 39217462                 38977484 38947498 38737510 38347509 37947531 37837545                 37537632 37627736 38077913 40577881      

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