Thursday, September 12, 2013

Sep 12, 2013 0600 UTC Day 1 Convective Outlook

DAY 1 CONVECTIVE OUTLOOK  
   NWS STORM PREDICTION CENTER NORMAN OK
1230 AM CDT THU SEP 12 2013

VALID 121200Z - 131200Z

...THERE IS A SLGT RISK OF SVR TSTMS FOR PARTS OF THE NORTHEAST...

...SYNOPSIS...
A PAIR OF MID-LEVEL VORTICITY MAXIMA WILL AID IN THE AMPLIFICATION
OF A LARGER-SCALE TROUGH ACROSS SERN CANADA/NERN CONUS INTO EARLY
FRI. THE LEAD IMPULSE OVER THE UPPER GREAT LAKES WILL MOVE EWD
ACROSS ONTARIO/QUEBEC...DAMPENING SOMEWHAT AS THE UPSTREAM IMPULSE
OVER MANITOBA DIGS SEWD ACROSS THE GREAT LAKES. AT THE
SURFACE...COLD FRONTS WILL ACCOMPANY EACH VORTICITY MAXIMA WITH THE
STRONGER SURGE OCCURRING WITH THE LATTER IMPULSE.

...NORTHEAST...
ISOLATED DAMAGING WIND/SEVERE HAIL AND PERHAPS A TORNADO APPEARS
MOST PROBABLE ACROSS NRN NEW ENGLAND TODAY GIVEN A 30-40 KT SWLY
LLJ. ISOLATED DAMAGING WIND SHOULD BE THE PRIMARY THREAT FARTHER TO
THE S/SW WHERE DEEP-LAYER FLOW IS WEAKER.

SCATTERED SHOWERS AND ISOLATED STORMS WILL LIKELY BE ONGOING THIS
MORNING IN ASSOCIATION WITH THE AFOREMENTIONED LEAD SHORTWAVE
IMPULSE AND FRONTAL ZONE. THIS CONVECTION ALONG WITH EXTENSIVE
OVERTURNING SINCE WED AFTERNOON SHOULD SERVE TO LIMIT INSTABILITY
COMPARED TO YESTERDAY. THE TRACK OF THE LEAD IMPULSE WILL RESULT IN
STRONG DEEP-LAYER SHEAR LARGELY REMAINING CONFINED IN THE WARM
SECTOR TO NRN NEW ENGLAND. BUT WITH WIDESPREAD MIDDLE 60S TO LOWER
70S SURFACE DEW POINTS...DIURNAL HEATING /MORE PRONOUNCED WITH SRN
EXTENT/ SHOULD YIELD WEAK TO MODERATE BUOYANCY WITH MLCAPE
INCREASING TO 750-1500 J/KG BY EARLY AFTERNOON. THIS SHOULD BE
CONCOMITANT WITH STORMS INCREASING IN COVERAGE WITH THE POSSIBILITY
OF ORGANIZED LINE SEGMENTS AND EMBEDDED SUPERCELLS TO THE NE AND
SEMI-ORGANIZED BROKEN BANDS TO THE SW.

...OH VALLEY...
A MARGINAL RISK FOR LOCALLY DAMAGING WIND/SEVERE HAIL IS EXPECTED
THIS AFTERNOON AND EVENING.

STRONG SURFACE HEATING IS ANTICIPATED ALONG/AHEAD OF AN INITIAL COLD
FRONT NEAR THE OH RIVER...YIELDING MODERATE BUOYANCY WITH MLCAPE
LIKELY REACHING 1000-2000 J/KG S OF THE RIVER. CONVECTION SHOULD
INITIALLY FORM ALONG THIS BOUNDARY AND DEVELOP SEWD WITHIN MODEST
NWLY STEERING FLOW. MUCH STRONGER DEEP-LAYER NWLYS WILL ACCOMPANY A
SECONDARY FRONTAL SURGE IN ASSOCIATION WITH THE SHORTWAVE TROUGH
DIGGING TOWARDS THE GREAT LAKES. ALTHOUGH LOW-LEVEL MOISTURE MAY BE
SCANT FOR DEEP CONVECTION...STRONG FORCING FOR ASCENT/SHEAR COULD
YIELD MARGINAL SEVERE WITH ISOLATED STORMS ALONG THE LATTER COLD
FRONT.
Any source

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