Aug 5, 2013 1630 UTC Day 1 Convective Outlook | |||||||||
Updated: Mon Aug 5 16:32:39 UTC 2013 ( | ) | |||||||||
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. |
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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. |
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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. |
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SPC AC 051628 DAY 1 CONVECTIVE OUTLOOK NWS STORM PREDICTION CENTER NORMAN OK 1128 AM CDT MON AUG 05 2013 VALID 051630Z - 061200Z ...THERE IS A SLGT RISK OF SVR TSTMS THIS AFTERNOON INTO TONIGHT ACROSS PARTS OF THE NORTHERN AND CENTRAL PLAINS... ...SYNOPSIS... TO THE SOUTH OF A HIGHER LATITUDE BLOCKING UPPER RIDGE...MODELS INDICATE THAT A SIGNIFICANT CLOSED LOW WILL CONTINUE TO SHIFT SLOWLY WEST SOUTHWEST OF HUDSON BAY THROUGH THE REMAINDER OF THIS FORECAST PERIOD. AS THIS OCCURS...A WEAK CYCLONIC CIRCULATION... NOW OVER SOUTHERN ALBERTA/BRITISH COLUMBIA...APPEARS LIKELY TO SLOWLY PROGRESS INTO THE CONFLUENT REGIME ACROSS THE NORTHERN ROCKIES INTO NORTHERN PLAINS...BECOMING INCREASING SHEARED/DEFORMED AS IT DOES. HOWEVER...THE ONSET OF WEAK MID-LEVEL HEIGHT FALLS MAY NOT REACH PORTIONS OF EASTERN MONTANA UNTIL LATE AFTERNOON/EARLY EVENING...AND PORTIONS OF NORTHERN WYOMING AND THE DAKOTAS UNTIL LATER TONIGHT. OTHERWISE...LITTLE CHANGE TO UPPER HEIGHTS ARE PROGGED THROUGH THE PERIOD FROM THE INTERMOUNTAIN REGION THROUGH THE PLAINS AND MISSISSIPPI VALLEY...WHERE FLOW WILL REMAIN BROADLY ANTICYCLONIC. IN THE WAKE OF SUBTLE MID-LEVEL HEIGHT FALLS ...ASSOCIATED WITH A COUPLE OF WEAK IMPULSES NOW MIGRATING EAST SOUTHEASTWARD THROUGH THE MIDDLE MISSOURI AND UPPER MISSISSIPPI VALLEYS...MID-LEVEL HEIGHTS MAY REBOUND. AND THERE MAY BE LITTLE ...IF ANY...CHANGE TO THE VERY WARM AND CAPPING ELEVATED MIXED LAYER NOW PRESENT ACROSS MUCH OF THE CENTRAL AND SOUTHERN PLAINS ...WHERE HIGHER MOISTURE CONTENT AIR...CHARACTERIZED BY LOWER 70S SURFACE DEW POINTS...LINGERS ALONG A RESIDUAL BAROCLINIC ZONE ROUGHLY ACROSS NORTHEAST COLORADO/WESTERN AND SOUTHERN KANSAS INTO THE OZARK PLATEAU/LOWER MISSISSIPPI VALLEY. BUT MID/UPPER FLOW REMAINS SEASONABLY STRONG...FROM THE WEST NORTHWEST...ACROSS THE NORTHERN ROCKIES AND MUCH OF THE NORTHERN HALF OF THE PLAINS/UPPER MISSISSIPPI VALLEY. ...NORTHERN AND CENTRAL PLAINS.... UNTIL LARGE-SCALE ASCENT INCREASES ACROSS EASTERN MONTANA AND THE DAKOTAS THIS EVENING INTO THE OVERNIGHT HOURS...WITH THE APPROACH OF THE UPPER IMPULSE...FORCING FOR CONVECTIVE DEVELOPMENT REMAINS UNCLEAR. HIGHEST CONFIDENCE FOR STORM DEVELOPMENT...WHICH COULD REMAIN FAIRLY WIDELY SCATTERED...APPEARS TO BE IN ASSOCIATION WITH FAVORABLE OROGRAPHIC FORCING ON THE EASTERN SLOPES OF THE NORTHERN ROCKIES...POSSIBLY THE BLACK HILLS...LATE THIS AFTERNOON...BEFORE PROPAGATING EAST SOUTHEASTWARD INTO THE PLAINS. IF THIS OCCURS...THE ENVIRONMENT ACROSS THE NORTHERN HIGH PLAINS IS EXPECTED TO BE CONDUCIVE TO ORGANIZED STRONG/SEVERE STORM DEVELOPMENT... INCLUDING ISOLATED SUPERCELLS. IT ALSO APPEARS POSSIBLE THAT A WEAK IMPULSE EMERGING FROM THE CENTRAL ROCKIES...AROUND THE PERIPHERY OF THE SUBTROPICAL HIGH...COULD CONTRIBUTE TO STORM DEVELOPMENT IN THE PRESENCE OF STEEP LAPSE RATES AND LARGE CAPE ACROSS WESTERN/CENTRAL KANSAS LATE THIS AFTERNOON. IF MID-LEVEL INHIBITION IS OVERCOME...THE ENVIRONMENT APPEARS CONDUCIVE TO THE RISK FOR SEVERE HAIL AND WIND GUSTS...WITH POTENTIAL FOR UPSCALE CONVECTIVE GROWTH ACROSS KANSAS THIS EVENING AIDED BY MODEST STRENGTHENING OF A SOUTHERLY LOW-LEVEL JET. OTHERWISE...INCREASING THUNDERSTORM ACTIVITY IS POSSIBLE LATE THIS EVENING ACROSS THE DAKOTAS WITH THE STRENGTHENING LARGE-SCALE FORCING FOR UPWARD VERTICAL MOTION. HOWEVER...THIS MAY NOT OCCUR UNTIL WELL AFTER THE ONSET OF BOUNDARY LAYER STABILIZATION...AND THE EXTENT OF THE SEVERE POTENTIAL REMAINS UNCLEAR AT THE PRESENT TIME. ...MID MISSOURI INTO UPPER MISSISSIPPI VALLEYS... IT STILL DOES NOT APPEAR OUT OF THE QUESTION THAT DESTABILIZATION IN THE PRESENCE OF STRONG SHEAR COULD BECOME SUFFICIENT TO SUPPORT AT LEAST LOW PROBABILITIES FOR SEVERE STORMS TODAY. HOWEVER...WHERE POCKETS OF GREATER DESTABILIZATION COULD OCCUR REMAIN UNCLEAR...AND COVERAGE OF STORM DEVELOPMENT MAY REMAIN SPARSE AS THE MOST SIGNIFICANT FORCING FOR UPWARD VERTICAL MOTION TENDS TO SPREAD EASTWARD INTO THE MORE STABLE ENVIRONMENT ACROSS THE GREAT LAKES/OHIO VALLEY. ...ARIZONA... DAYTIME HEATING COULD YIELD A HOT AND DEEPLY MIXED BOUNDARY LAYER ACROSS THE PHOENIX METRO AREA AND ADJACENT DESERTS. AS AN UPPER IMPULSE...WITHIN THE MONSOONAL MOISTURE PLUME WRAPPING ACROSS THE SOUTHERN PLAINS SUBTROPICAL HIGH CENTER...MIGRATES NORTHWARD OUT OF MEXICO ACCOMPANIED BY INCREASING CONVECTIVE DEVELOPMENT THIS EVENING...THE LOW-LEVEL ENVIRONMENT MAY REMAIN CONDUCIVE TO DOWNBURSTS AND STRONG CONVECTIVE SURFACE GUSTS. ..KERR/BUNTING.. 08/05/2013 CLICK TO GET WUUS01 PTSDY1 PRODUCT NOTE: THE NEXT DAY 1 OUTLOOK IS SCHEDULED BY 2000Z |