Jul 17, 2011 0600 UTC Day 1 Convective Outlook | |
Updated: Sun Jul 17 05:39:05 UTC 2011 | |
Probabilistic to Categorical Outlook Conversion Table |
Categorical Graphic |
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Probabilistic Tornado Graphic |
Probability of a tornado within 25 miles of a point. Hatched Area: 10% or greater probability of EF2 - EF5 tornadoes within 25 miles of a point. |
Probabilistic Damaging Wind Graphic |
Probability of damaging thunderstorm winds or wind gusts of 50 knots or higher within 25 miles of a point. Hatched Area: 10% of greater probability of wind gusts 65 knots or greater within 25 miles of a point. |
Probabilistic Large Hail Graphic |
Probability of hail 1" or larger within 25 miles of a point. Hatched Area: 10% or greater probability of hail 2" or larger within 25 miles of a point. |
SPC AC 170535 DAY 1 CONVECTIVE OUTLOOK NWS STORM PREDICTION CENTER NORMAN OK 1235 AM CDT SUN JUL 17 2011 VALID 171200Z - 181200Z ...THERE IS A SLGT RISK OF SVR TSTMS FROM NRN MT...EWD INTO THE CNTRL GREAT LAKES... ...MT TO THE UPPER GREAT LAKES... WEAK HEIGHT RISES WILL ENCOMPASS MUCH OF THE CONUS SUNDAY AS A DOMINANT UPPER HIGH BUILDS OVER THE CNTRL PLAINS. DESPITE THIS EVOLUTION IT APPEARS THERE WILL BE A RISK OF SEVERE TSTMS ALONG A CORRIDOR FROM THE NRN ROCKIES...EWD INTO THE UPPER GREAT LAKES. ISOLATED SEVERE STORMS...SOME SUPERCELLULAR IN NATURE...DEVELOPED ACROSS THE NRN PLAINS SATURDAY IN SPITE OF NONDESCRIPT MID-UPPER LEVEL FLOW REGIME WITH NO IDENTIFIABLE SHORT WAVE TROUGHS. STRONG HEATING AND WEAK WARM ADVECTION MOST LIKELY WERE RESPONSIBLE FOR THIS ACTIVITY AND THESE PROCESSES WILL LIKELY BE THE DRIVING MECHANISMS FOR TSTM DEVELOPMENT ALONG/NORTH OF A FRONT THAT WILL BE DRAPED FROM CNTRL MT...ESEWD ACROSS NRN SD INTO WI. EPISODIC BOUTS OF WARM ADVECTION MAY INDUCE CONVECTION ATOP THE COOLER BOUNDARY LAYER...POSSIBLY ACROSS MT/WRN ND EARLY IN THE PERIOD. THIS ACTIVITY COULD THEN SPREAD/DEVELOP EWD ACROSS THE DAKOTAS INTO THE UPPER MS VALLEY BY MID DAY AS REMNANT LLJ VEERS INTO THIS PORTION OF THE SLGT RISK REGION. IT/S NOT ENTIRELY CLEAR WHETHER STORMS WILL EVOLVE INTO THE WARM SECTOR AS STRONG CAPPING WILL LIKELY INHIBIT DEEPER UPDRAFTS. FOR THIS REASON WILL OPT TO INCLUDE AREAS PRIMARILY NORTH OF THE WIND SHIFT WHERE WARM ADVECTION WILL BE MAXIMIZED. IF AN MCS CAN EVOLVE OVER THE UPPER MS VALLEY THEN A COLD POOL WILL PROVE INSTRUMENTAL IN SUBSEQUENT MOVEMENT TOWARD THE GREAT LAKES...POSSIBLY AS FAR SE AS CHI METRO AREA LATE IN THE PERIOD. FARTHER WEST DURING THE MID-LATE AFTERNOON HOURS...SHORT RANGE MODELS SUGGEST A SIGNIFICANT ELY COMPONENT WILL BE MAINTAINED WITHIN THE BOUNDARY LAYER ACROSS MT. THIS ELY COMPONENT WILL FORCE HIGHER LOW LEVEL MOISTURE INTO CNTRL MT WHERE SWLY FLOW ALOFT WILL ENHANCE DEEP LAYER SHEAR AND THE PROSPECT FOR SUPERCELLS. LATEST NAM SUGGESTS A MID LEVEL SPEED MAX WILL EJECT NEWD ACROSS SWRN INTO CNTRL MT DURING THE AFTERNOON HOURS. THIS COULD ENHANCE SEVERE CONVECTION...THOUGH COVERAGE MAY REMAIN ISOLATED IN NATURE. ...NERN U.S... STRONG SHORT WAVE TROUGH WILL TOP THE U.S. UPPER RIDGE OVER NWRN ONTARIO AND DRIVE SEWD TOWARD NEW ENGLAND LATE IN THE PERIOD. THIS WILL FORCE A PLUME OF MOIST/UNSTABLE AIR ACROSS THE SERN CANADIAN PROVINCES TOWARD UPSTATE NY/VT/NY AND ME. AT THIS TIME WILL NOT INTRODUCE A SLGT RISK BUT RATHER 5% PROBS FOR ISOLATED SEVERE THUNDERSTORMS AHEAD OF SURGING COLD FRONT AS TIMING OF WIND SHIFT WILL NOT COINCIDE WITH DIURNAL HEATING CYCLE. EVEN SO STRONG SHEAR AND INCREASINGLY BUOYANT ENVIRONMENT MAY SUPPORT AN ISOLATED RISK OF ROBUST CONVECTION DURING THE LATTER HALF OF THE PERIOD. ..DARROW/HURLBUT.. 07/17/2011 CLICK TO GET WUUS01 PTSDY1 PRODUCT NOTE: THE NEXT DAY 1 OUTLOOK IS SCHEDULED BY 1300Z