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SPC May 26, 2012 1630 UTC Day 1 Convective Outlook

SPC 1630Z Day 1 Outlook

Day 1 Outlook Thumbnail Image

DAY 1 CONVECTIVE OUTLOOK RESENT 1
NWS STORM PREDICTION CENTER NORMAN OK
1141 AM CDT SAT MAY 26 2012

VALID 261630Z - 271200Z

...THERE IS A SLGT RISK OF SVR TSTMS OVER MANY LOCATIONS OF THE
GREAT PLAINS INTO PARTS OF THE MIDWEST...

...CORRECTED FOR TYPOS/WORDING...

...CNTRL PLAINS TO MIDWEST...
A DIFFICULT AND UNCERTAIN FORECAST SCENARIO TODAY WITH MANY FACTORS
POTENTIALLY CONTRIBUTING TO SIGNIFICANT TSTM DEVELOPMENT AND OTHER
FACTORS POSSIBLY HINDERING THIS DEVELOPMENT. LARGE SCALE PATTERN
FEATURES A DEEP UPPER TROUGH ACROSS THE WEST AND A STRONG RIDGE
DOMINATING THE SOUTH AND SOUTHEAST. IN BETWEEN THESE TWO LARGE SCALE
FEATURES...DEEP-LAYER SLY FLOW HAS CONTRIBUTED TO COPIOUS LOW LEVEL
MOISTURE TRANSPORT ACROSS THE GREAT PLAINS/MIDWEST WHILE AT THE SAME
TIME RESULTING IN AN EXPANSIVE ELEVATED MIXED LAYER AIRMASS/CAP THAT
WILL INHIBIT MOST CONVECTIVE DEVELOPMENT IN THE ABSENCE OF STRONG
FORCED ASCENT AND/OR DIABATIC INFLUENCES.

STORM SCALE GUIDANCE FROM 00Z...THE 12Z WRF-NMM...AND THE 12Z
NAM-WRF MODELS ALL DEPICT SOME POTENTIAL FOR LATE AFTERNOON STORM
INITIATION ALONG OR IMMEDIATELY NORTH OF THE WARM FRONT OVER IA.
THIS DEVELOPMENT MAY BE A RESULT OF WEAK DCVA ACCOMPANYING A SERIES
OF LOW AMPLITUDE SHORT WAVES TRAVELING WITHIN THE DEEP-LAYER
MERIDIONAL FLOW ACROSS THE PLAINS. THESE MAY CREST THE RIDGE AXIS
COINCIDENT WITH A MAXIMUM IN DIURNAL HEATING/DESTABILIZATION AND
CONTRIBUTE TO TSTM DEVELOPMENT IN A VERY UNSTABLE AIRMASS. RESULTING
CONVECTION COULD THEN ORGANIZE INTO A FORWARD PROPAGATING MCS WITH
HAIL AND WIND SPREADING EWD ALONG THE INSTABILITY GRADIENT/WARM
FRONT FROM IA TO THE UPPER MIDWEST. THUS PARTS OF THESE AREAS HAVE
BEEN INCLUDED IN A SLGT RISK WITH THIS UPDATE.

EVEN GREATER UNCERTAINTY IN A SCENARIO EXISTS WITH WWD EXTENT ALONG
THE WARM FRONT ACROSS NEB. MOST GUIDANCE DEPICTS SOME DEVELOPMENT
NEAR THE FRONT...AND ALONG THE DRYLINE/LEE TROUGH FROM NERN CO
ACROSS PARTS OF WRN/CNTRL KS BY EVENING. ANY STORMS THAT CAN
OVERCOME INHIBITION IN THESE AREAS WILL EXIST IN A KINEMATIC REGIME
SUPPORTIVE OF SUPERCELLS. HAIL AND HIGH WINDS WILL BE POSSIBLE AND
TORNADO POTENTIAL WILL BE ENHANCED NEAR THE WARM FRONT THAT WILL
LIKELY BE SITUATED ACROSS NRN/CNTRL NEB. ADDITIONAL STORMS MAY
DEVELOP NORTH OF THE FRONT ACROSS SD THROUGH THE EVENING AND POSE A
TREAT OF LARGE HAIL.

...CNTRL HIGH PLAINS SOUTH ALONG LEE TROUGH/DRYLINE TO WEST TX...
INFLUENCE FROM THE LARGE WRN TROUGH WILL AID STORM
DEVELOPMENT...ESPECIALLY ACROSS WY LATER THIS AFTERNOON. STORMS IN
THIS AREA WILL GENERALLY LACK ACCESS TO GREATER INSTABILITY BUT THIS
MAY BE COMPENSATED BY MAGNITUDE OF FORCING AND SHEAR. THE RESULT MAY
BE A NUMBER OF HIGH BASED CELLS WITH HAIL AND SOME WIND POTENTIAL
SPREAD NEWD FROM WY THROUGH THE EVENING.

ADDITIONAL HIGH-BASED STORMS...POSSIBLY IN THE FORM OF LP SUPERCELLS
APPEAR LIKELY ALONG THE DRYLINE SOUTH TO WEST TX. LARGE SCALE
FORCING WILL BE MORE AMBIGUOUS HERE AND MUCH OF THIS ACTIVITY MAY BE
DIURNALLY DRIVEN AND SHOULD BEGIN TO DECAY WITHIN AN HOUR OR TWO
AFTER SUNSET. HAIL/WIND EVENTS AND POSSIBLY A TORNADO APPEAR
POSSIBLE WITH THIS DEVELOPMENT.

..CARBIN/BOTHWELL.. 05/26/2012

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via SPC Forecast Products http://www.spc.noaa.gov/products/outlook/day1otlk_1630.html

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