DAY 1 CONVECTIVE OUTLOOK NWS STORM PREDICTION CENTER NORMAN OK 0758 PM CDT WED JUN 27 2012 VALID 280100Z - 281200Z ...NO SVR TSTM AREAS FORECAST... ...SYNOPSIS... UPPER-AIR PATTERN OVER CONUS REMAINS DOMINATED BY LARGE ANTICYCLONE CENTERED OVER CENTRAL PLAINS...WITH RIDGING NNEWD ACROSS SRN HUDSON BAY...EWD OVER SRN APPALACHIANS AND WSWWD OVER NRN SONORA. UPPER LOW OVER MAINE/NEW BRUNSWICK SHOULD MEANDER SLOWLY/ERRATICALLY NEWD THROUGH REMAINDER PERIOD...WHILE SMALLER UPPER LOW OVER SK/MB BORDER CROSSES NRN MB. POSITIVELY TILTED/LOW-AMPLITUDE SHORTWAVE TROUGH IS EVIDENT FROM BLACK HILLS REGION SSWWD ACROSS 4-CORNERS REGION. THIS TROUGH IS EXPECTED TO MOVE ENEWD TO UPPER MS VALLEY...ERN NEB AND NRN KS BY END OF PERIOD...BECOMING MORE POSITIVELY TILTED DUE TO FASTER TRANSLATION OF NRN SEGMENT OF ASSOCIATED 500-MB VORTICITY BANNER. AT SFC...23Z ANALYSIS SHOWED WAVY FRONTAL ZONE FROM LS/UPPER MI SWWD ACROSS SRN MN...ERN/SRN NEB AND NWRN KS. WRN PORTION OF FRONT BECOMES DIFFUSED BY CONVECTIVE OUTFLOWS ACROSS ERN CO. NRN PORTION OF FRONT SHOULD MOVE EWD ACROSS LS/WI THROUGH PERIOD...WHILE REMAINDER BECOMES QUASISTATIONARY OVER CENTRAL PLAINS....MODULATED LOCALLY BY TSTM OUTFLOWS. ...AZ AND CENTRAL HIGH PLAINS TO MN... POSITIVELY TILTED SHORTWAVE TROUGH ALOFT ALSO DEMARCATES WRN EDGE OF PLUME OF LOW-MIDDLE LEVEL MOISTURE CONTRIBUTING TO CONVECTION FROM SRN AZ TO SD/WRN MN. SCATTERED TO WIDELY SCATTERED TSTMS SHOULD CONTINUE OVER AZ...BECOMING WIDELY SCATTERED TO ISOLATED NEWD OVER CENTRAL HIGH PLAINS...THEN ISOLATED FARTHER NE. 00Z SOUNDINGS SHOW STRENGTHENING CAP WITH NEWD EXTENT FROM HIGH PLAINS...INVOF FRONTAL ZONE...AS ELEVATION LESSENS BENEATH EML. PLUME OF 16-19 DEG C 700 MB TEMPS FROM LBF-OAX-MPX IS SYMPTOMATIC OF STG CAPPING BELOW THAT LEVEL...EVIDENT IN OBSERVED RAOBS. A FEW GUSTS NEAR SVR LIMITS STILL ARE POSSIBLE...ESPECIALLY OVER PRECONVECTIVE AIR MASS REMAINING IN PARTS OF CENTRAL HIGH PLAINS AND SWRN/S-CENTRAL AZ. ALREADY MRGL SVR THREAT WITH EXISTING CONVECTION OVER HIGHER TERRAIN SHOULD DIMINISH WITH TIME THROUGH REMAINDER EVENING...AS COMBINATION OF SPREADING OUTFLOWS AND DIABATIC SFC COOLING CONTRIBUTE TO BOUNDARY-LAYER STABILIZATION. ..EDWARDS.. 06/28/2012
via SPC Forecast Products http://www.spc.noaa.gov/products/outlook/day1otlk_0100.html





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