SPC AC 170550
DAY 2 CONVECTIVE OUTLOOK
NWS STORM PREDICTION CENTER NORMAN OK
1150 PM CST SAT FEB 16 2013
VALID 181200Z - 191200Z
...NO SVR TSTM AREAS FORECAST...
...SYNOPSIS...
MODELS CONTINUE TO INDICATE THE EVOLUTION OF A SIGNIFICANT
LARGE-SCALE TROUGH EAST OF THE ROCKIES DURING THIS FORECAST PERIOD.
THIS IS EXPECTED IN ASSOCIATION WITH THE PHASING OF A COUPLE OF
SHORT WAVE IMPULSES...WITHIN A SPLIT BELT OF WESTERLIES EMERGING
FROM THE MID LATITUDE PACIFIC...AND PERHAPS ANOTHER IMPULSE WITHIN A
BELT OF WESTERLIES EMERGING FROM THE SUBTROPICAL EASTERN PACIFIC.
THIS FEATURE IS FORECAST TO TURN EAST OF THE MISSISSIPPI VALLEY BY
LATE MONDAY NIGHT...AS A STRONG DIGGING UPSTREAM SHORT WAVE IMPULSE
CONTRIBUTES TO THE EVOLUTION OF ANOTHER LARGE-SCALE TROUGH ALONG THE
PACIFIC COAST.
IN ASSOCIATION WITH THE LEAD WAVE...SURFACE LOW PRESSURE IS EXPECTED
TO CONSOLIDATE AND DEEPEN OVER THE GREAT LAKES REGION BY THE LATTER
HALF OF THE PERIOD...WITH A TRAILING SURFACE COLD FRONT SURGING
SOUTHEAST OF THE NORTHERN PLAINS...THROUGH MUCH OF THE UPPER HALF OF
THE MISSISSIPPI VALLEY. ANOTHER COLD FRONT...OF PACIFIC
ORIGINS...IS EXPECTED TO ADVANCE SOUTH AND EAST OF THE CENTRAL AND
SOUTHERN PLAINS...PERHAPS OVERTAKING A DEVELOPING/SHARPENING DRY
LINE ACROSS THE ARKLATEX REGION DURING THE LATE AFTERNOON HOURS.
A VERY STRONG SOUTHERLY 850 MB JET /50-70+ KT/ APPEARS LIKELY TO
FORM AHEAD OF THE COLD FRONT...BUT MOSTLY WELL INLAND OF WESTERN AND
CENTRAL GULF COASTAL AREAS...WHERE FLOW OFF THE GULF OF MEXICO IS
FORECAST TO REMAIN RATHER MODEST. GIVEN THIS...AND A WESTERN GULF
OF MEXICO BOUNDARY LAYER STILL IN THE EARLY STAGES OF RECOVERY FROM
RECENT COOLING/DRYING...IT STILL APPEARS PROBABLE THAT INLAND
MOISTURE RETURN WILL REMAIN WEAK IN MAGNITUDE. SUFFICIENT
DESTABILIZATION FOR THUNDERSTORM ACTIVITY PROBABLY WILL OCCUR
MONDAY/MONDAY NIGHT ACROSS THE LOWER MISSISSIPPI VALLEY...AND
PERHAPS AS FAR NORTH AS THE GREAT LAKES REGION. MOST OF
THIS...HOWEVER...IS EXPECTED TO BE ASSOCIATED WITH THE DEVELOPMENT
OF A PRE-FRONTAL CORRIDOR OF VERY WEAK CAPE...ABOVE A RESIDUAL COOL
AND STABLE SURFACE BASED LAYER. AS A RESULT SEVERE WEATHER
POTENTIAL APPEARS NEGLIGIBLE FOR MOST AREAS.
...PARTS OF ERN TX AND THE ARKLATEX INTO SRN AR...
MODELS DO SUGGEST THAT WEAK BOUNDARY LAYER DESTABILIZATION COULD
DEVELOP IN A NARROW PRE-FRONTAL CORRIDOR...ALONG THE DEVELOPING DRY
LINE BY LATE AFTERNOON. MID/UPPER 50S SURFACE DEW POINTS MAY RETURN
AS FAR NORTH AS THE ARKLATEX...CONTRIBUTING TO CAPE GENERALLY ON THE
ORDER OF 500 J/KG OR LESS...WITH SLIGHTLY HIGHER DEW POINTS AND CAPE
FARTHER TO THE SOUTH. VARIABILITY EXISTS AMONG THE MODELS
CONCERNING THE DETAILS OF THE PHASING OF THE SHORT WAVE IMPULSES
...AND ASSOCIATED MID/UPPER FORCING FOR UPWARD VERTICAL MOTION
ACROSS THE REGION. HOWEVER...A WINDOW OF OPPORTUNITY APPEARS TO
EXIST FOR LATE AFTERNOON BOUNDARY LAYER BASED STORM
DEVELOPMENT...BEFORE THE FRONT OVERTAKES THE DRY LINE. AND...IF
THIS OCCURS...THE ENVIRONMENT MAY BE AT LEAST MARGINALLY CONDUCIVE
TO THE DEVELOPMENT OF A SUPERCELL OR TWO.
..KERR.. 02/17/2013
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NOTE: THE NEXT DAY 2 OUTLOOK IS SCHEDULED BY 1730Z
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