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SPC May 10, 2012 0600 UTC Day 2 Convective Outlook

SPC 0600Z Day 2 Outlook

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DAY 2 CONVECTIVE OUTLOOK
NWS STORM PREDICTION CENTER NORMAN OK
1246 AM CDT THU MAY 10 2012

VALID 111200Z - 121200Z

...NO SVR TSTM AREAS FORECAST...

...SYNOPSIS...
PROGRESSIVE MID-UPPER LEVEL PATTERN FCST THROUGH PERIOD...FEATURING
THREE PRIMARY TROUGHS...
1. ERN-CONUS SYNOPTIC TROUGH -- NOW EXTENDING FROM QUE/ONT BORDER
SWD ACROSS SRN APPALACHIANS TO FL COASTAL BEND.  SEVERAL SHORTWAVE
TROUGHS OF VARYING AMPLITUDE WILL PIVOT CYCLONICALLY THROUGH THIS
FEATURE...WITH NET EWD MOTION OF MAIN TROUGH TO NRN/WRN NEW ENGLAND
AND COASTAL MID-ATLC REGION BY 11/12Z.  THIS TROUGH WILL MOVE
OFFSHORE NRN ATLC COAST AND OVER PORTIONS CANADIAN MARITIMES BY
1200Z.

2. NRN-STREAM SHORTWAVE TROUGH -- NOW MOVING INLAND PAC NW.  FEATURE
SHOULD MOVE ENEWD OBLIQUELY ACROSS CANADIAN BORDER REGION AND NRN
ROCKIES DAY-1.  BY START OF PERIOD...POSITIVELY TILTED TROUGH SHOULD
EXTEND FROM WRN MB SWD ACROSS MT AND NWRN WY... SHIFTING EWD TO FAR
NWRN ONT AND MN BY END OF PERIOD.

3. SRN-STREAM LOW -- NOW EVIDENT IN MOISTURE CHANNEL IMAGERY OVER
NWRN MEX -- FCST TO MOVE EWD ACROSS TX BIG-BEND AREA DAY-1...THEN
PIVOT NEWD OVER PORTIONS NW/N-CENTRAL TX BY ABOUT 12/00Z.  BY
12/12Z...REMNANTS OF THIS LOW SHOULD BE OVER NE TX...WITH BROADLY
CYCLONIC FLOW FROM PERMIAN BASIN/LOWER PECOS VALLEY REGION ACROSS
LOWER RIO GRANDE VALLEY TO LOWER MS DELTA.  SYSTEM IS EXPECTED TO
FILL GRADUALLY THROUGHOUT THIS PROCESS.  PROGS ARE NOT AS DIVERGENT
AS BEFORE WITH TRACK/TIMING OF THIS SYSTEM...BUT STILL OFFER
IMPORTANT MESO-ALPHA SCALE DIFFERENCES PARTICULARLY FROM ABOUT
MID-PERIOD ONWARD.

AT SFC...COLD FRONT WAS ANALYZED AT 10/03Z FROM JUST OFFSHORE NC
SWWD ACROSS NRN FL THEN WSWWD OVER NERN THROUGH W-CENTRAL
GULF...BECOMING QUASISTATIONARY AND DIFFUSE INTO MTNS OF NERN MEX.
SECONDARY BAROCLINIC ZONE WAS EVIDENT FROM MIDDLE TX COAT WSWWD
ACROSS RIO GRANDE BETWEEN DRT-LRD.  THESE BOUNDARIES SHOULD BLEND
THEN LIFT NWD ACROSS MIDDLE-UPPER TX COAST AS WARM FRONT DAY-2...IN
ADVANCE OF LOW SLOWLY EJECTING OUT OF MEX.  INLAND PENETRATION OF
THIS BOUNDARY IS UNCERTAIN...DEPENDING STRONGLY ON TRACK OF
MID-UPPER WAVE AND ON REINFORCEMENT/REALIGNMENT BY ANTECEDENT
CONVECTIVE PROCESSES.

...S-CENTRAL/SE TX...
SCATTERED TO LOCALLY NUMEROUS TSTMS SHOULD OCCUR EPISODICALLY
THROUGH PERIOD...WHERE RICH LOW-LEVEL THETAE KEEPS EFFECTIVE LIFTED
PARCELS SFC-BASED.  ISOLATED SVR GUSTS AND HAIL ARE POSSIBLE...AND
THERE IS AT LEAST MRGL/CONDITIONAL TORNADO RISK.  RICH LOW-LEVEL
MOISTURE WAS ANALYZED INVOF FRONT AND WITHIN ABOUT 200 NM TO ITS
N...WITH INLAND SFC DEW POINTS MID-UPPER 60S F AND 70S OFFSHORE.
FAVORABLE MOISTURE IS EXPECTED TO REMAIN IN PRIMARY FRONTAL
ZONE...THROUGH DAY-1 INTO THIS PERIOD.  SVR POTENTIAL APPEARS
GREATEST DURING AFTERNOON/EVENING HOURS WHEREVER THIS AIR MASS
EXPERIENCES SUSTAINED/SFC DIABATIC HEATING...YIELDING 1500-2500 J/KG
MLCAPE IN MODIFIED FCST SOUNDINGS.  MIDDLE-UPPER TX COASTAL PLAIN
SHOULD RESIDE BENEATH DIFLUENT LEFT-EXIT REGION OF SOMEWHAT
CYCLONICALLY CURVED/SUBTROPICAL JET MAX S-SE OF UPPER LOW...AIDING
LARGE SCALE ASCENT IN WAKE OF EARLIER CONVECTION.  MOST FAVORABLE
LOW-LEVEL SHEAR SHOULD OCCUR INVOF WARM FRONT...WHERE BACKED SFC
WINDS WILL YIELD ENLARGED LOW-LEVEL HODOGRAPHS.  MESOSCALE
DEPENDENCY OF BOTH CONVECTIVE PROCESSES AND FRONTAL POSITION RENDER
OUTLOOK TOO UNCERTAIN FOR CATEGORICAL AREA ATTM.

...WI-KS...
WIDELY SCATTERED TO SCATTERED TSTMS ARE POSSIBLE INVOF SFC COLD
FRONT...PRIMARILY DURING AFTERNOON INTO EARLY EVENING WHEN
BOUNDARY-LAYER LAPSE RATES AND BUOYANCY WILL BE MAXIMIZED.  MRGL
MOISTURE WILL BE MAIN LIMITING FACTOR FOR CONVECTIVE LONGEVITY AND
FOR SVR POTENTIAL...WITH NEAR-SFC TRAJECTORIES EMANATING FROM
CONTINENTAL ANTICYCLONE THAT FOLLOWS NERN-CONUS TROUGH AND RELATED
FROPA.  STILL...RESIDUAL/EVAPOTRANSPIRATIVE CONTRIBUTIONS TO
BOUNDARY-LAYER MOISTURE SHOULD RESULT IN NARROW PREFRONTAL PLUME OF
50S SFC DEW POINTS.  VERY ISOLATED STG-SVR GUST CANNOT BE RULED
OUT...SINCE THERE WILL BE SOME SFC-BASED TSTMS ACCESSING
DIABATICALLY HEATED/MIXED PREFRONTAL BOUNDARY LAYER.
HOWEVER...GIVEN VERY WEAK LOW-MIDDLE LEVEL BULK SHEAR FCST OVER
FRONTAL CORRIDOR...ANY SUCH THREAT APPEARS TOO CONDITIONAL/SPARSE
ATTM TO ASSIGN UNCONDITIONAL SVR PROBABILITIES.

..EDWARDS.. 05/10/2012

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