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SPC Jul 26, 2015 2000 UTC Day 1 Convective Outlook

SPC 2000Z Day 1 Outlook

Day 1 Outlook Image

DAY 1 CONVECTIVE OUTLOOK  
NWS STORM PREDICTION CENTER NORMAN OK
0257 PM CDT SUN JUL 26 2015

VALID 262000Z - 271200Z

...THERE IS A SLGT RISK OF SVR TSTMS LATE THIS AFTERNOON AND EVENING
ACROSS THE NORTHERN AND CENTRAL HIGH PLAINS...

...THERE IS A MRGL RISK OF SVR TSTMS ACROSS SURROUNDING AREAS OF THE
PLAINS...

...THERE IS A MRGL RISK OF SVR TSTMS ACROSS PARTS OF THE OHIO
VALLEY...ALLEGHENY PLATEAU INTO THE HUDSON VALLEY...

...THERE IS A MRGL RISK OF SVR TSTMS ACROSS PARTS OF SOUTHWEST
THROUGH CENTRAL MONTANA...

...SUMMARY...
A FEW SEVERE STORMS ARE POSSIBLE THIS AFTERNOON ACROSS PARTS OF THE
NORTHERN AND CENTRAL HIGH PLAINS.  WIDELY SCATTERED STRONG STORMS
ARE ALSO POSSIBLE ACROSS PARTS OF THE OHIO VALLEY...AND THE
ALLEGHENY PLATEAU REGION INTO THE HUDSON VALLEY...AS WELL AS ACROSS
PARTS OF SOUTHWESTERN INTO CENTRAL MONTANA.

...20Z OUTLOOK UPDATE...
CATEGORICAL AND PROBABILISTIC LINES HAVE BEEN ADJUSTED TO ACCOUNT
FOR THE LATEST TRENDS CONCERNING CONVECTIVE DEVELOPMENT AND
DESTABILIZATION.

...PLAINS...
WIDELY SCATTERED THUNDERSTORM DEVELOPMENT IS ALREADY UNDERWAY NEAR
THE LEE SURFACE TROUGH ACROSS THE CENTRAL AND NORTHERN HIGH
PLAINS...LIKELY TO DUE AT LEAST THE APPROACH OF CONVECTIVE
TEMPERATURES...WHERE LOW-LEVEL CONVERGENCE HAS BECOME LOCALLY
ENHANCED.  THIS ACTIVITY IS EXPECTED TO PERSIST AND GRADUALLY
INTENSIFY THROUGH LATE AFTERNOON IN AN ENVIRONMENT THAT APPEARS
CHARACTERIZED BY STEEP LOWER/MID TROPOSPHERIC LAPSE RATES...SIZABLE
CAPE AND WEAK TO MODEST SHEAR.  AN INCREASE IN STORM COVERAGE IS
ALSO PROBABLE...PARTICULARLY ACROSS PARTS OF EASTERN COLORADO AND
NORTHWEST KANSAS INTO WESTERN NEBRASKA...LIKELY AIDED BY FORCING
ASSOCIATED WITH A WEAK IMPULSE EMBEDDED WITHIN THE MID-LEVEL MOIST
PLUME WRAPPING AROUND THE WESTERN PERIPHERY OF THE SOUTHERN PLAINS
SUBTROPICAL HIGH CENTER.

...OHIO VALLEY INTO NORTHEAST...
LOW PROBABILITIES FOR MARGINALLY SEVERE HAIL AND WIND ARE BEING
MAINTAINED ALONG AN AXIS OF MODEST BOUNDARY LAYER DESTABILIZATION
WHICH HAS TAKEN PLACE WITH DAYTIME HEATING ACROSS PARTS OF THE OHIO
VALLEY...AND THE ALLEGHENY PLATEAU INTO THE HUDSON VALLEY.  IN THE
PRESENCE OF WEAK DEEP LAYER MEAN FLOW AND SHEAR...SUBSTANTIVE
FURTHER CONVECTIVE INTENSIFICATION DOES NOT SEEM TOO LIKELY...BUT
CONSIDERABLE THUNDERSTORM ACTIVITY IS ALREADY UNDERWAY.

...MIDDLE MISSISSIPPI VALLEY...
CONVECTIVE OUTFLOW HAS STABILIZED THE BOUNDARY LAYER NEAR THE
IMMEDIATE VICINITY OF THE MISSISSIPPI RIVER ACROSS MISSOURI/
ILLINOIS AND IOWA.  ON THE WESTERN FLANK OF A REMNANT OUTFLOW
BOUNDARY NOW ARCING ACROSS WESTERN TENNESSEE AND NORTHEAST ARKANSAS
INTO PARTS OF SOUTH CENTRAL MISSOURI...MOISTURE CONTENT REMAINS
SEASONABLY HIGH AND IS CONTRIBUTING TO LARGE MIXED LAYER CAPE. 
ALTHOUGH SOME RECENT INCREASE IN THUNDERSTORMS IS NOTED TO THE EAST
AND SOUTHEAST OF FORT LEONARD WOOD...THE TENDENCY FOR WARMING ALOFT
IN CONJUNCTION WITH GENERALLY WEAK FORCING FOR ASCENT...DEEP LAYER
MEAN FLOW AND SHEAR SEEM TO LIMIT CONVECTIVE POTENTIAL THROUGH THE
REMAINDER OF THE PERIOD.

...NORTHERN ROCKIES...
THE LACK OF MORE SUBSTANTIVE POST-FRONTAL BOUNDARY LAYER MOISTENING
AND DESTABILIZATION APPEARS THE MAIN LIMITING FACTOR AS
THUNDERSTORMS DEVELOP ACROSS THE MOUNTAINS OF SOUTHWEST INTO CENTRAL
MONTANA IN RESPONSE TO STRENGTHENING FORCING FOR ASCENT.  DEEP LAYER
SHEAR IS SUFFICIENT TO SUPPORT ORGANIZED SEVERE STORMS...INCLUDING
SUPERCELLS.  HOWEVER...AT THIS POINT...TOO MUCH UNCERTAINTY REMAINS
TO SUPPORT ANYTHING BEYOND MARGINAL SEVERE PROBABILITIES.

..KERR.. 07/26/2015

.PREV DISCUSSION... /ISSUED 1130 AM CDT SUN JUL 26 2015/

...CNTRL/NRN HIGH PLAINS...
MORNING SATELLITE IMAGERY DEPICTS MOSTLY CLEAR SKIES ACROSS THE HIGH
PLAINS FROM THE RIO GRANDE TO CANADIAN BORDER. DIURNAL
HEATING/MIXING AND WEAK BACKGROUND ASCENT/HEIGHT FALLS FROM ERN CO
NWD SHOULD CONTRIBUTE TO WIDELY SCATTERED CONVECTIVE INITIATION
ALONG/AHEAD OF HIGH PLAINS LEE/THERMAL TROUGH LATER THIS AFTERNOON.
DESPITE VERY WARM MID-LEVEL TEMPS DELINEATING LOWER LAYER OF EML
PLUME...DEEPER BOUNDARY LAYER MIXING/HEATING SHOULD BE ABLE TO AID
IN OVERCOMING CONVECTIVE INHIBITION WITH AT LEAST A FEW STORMS ABLE
TO TAP INTO STRONG SURFACE-BASED INSTABILITY. EFFECTIVE SHEAR ON THE
ORDER OF 25-30KT SHOULD SUPPORT A COUPLE OF MORE PERSISTENT STORM
UPDRAFTS/SUPERCELLS WITH THE CAPABILITY OF PRODUCING HAIL AND HIGH
WINDS. SOMEWHAT GREATER STORM COVERAGE AND PERSISTENCE MAY EXIST
ACROSS ERN CO WHERE STORMS MAY DRIFT TOWARD AXIS OF GREATER LOW
LEVEL MOISTURE/DESTABILIZATION ALONG THE CO/KS BORDER WITH TIME.
SOME OF THIS ACTIVITY MAY ALSO PERSIST INTO THE NIGHTTIME HOURS AS
MASS TRANSPORT AND LOW LEVEL ASCENT ARE MAXIMIZED ON THE NOSE OF
PLAINS LLJ.

...MIDWEST/TO NORTH OF OH VALLEY/ALLEGHENY PLATEAU...
FORECAST IS COMPLICATED ACROSS THE MIDWEST GIVEN THE DECAYING
REMNANTS OF A PAIR OF OVERNIGHT MCS/S...ONE NOW CROSSING THE LOWER
OH RIVER VALLEY IN WRN KY AND THE MO BOOTHEEL...THE OTHER MOVING
INTO WRN IL FROM SERN IA AND ERN MO. NRN SYSTEM APPEARS TO BE
ASSOCIATED WITH A RELATIVELY STRONG SHORTWAVE TROUGH EVIDENT ON
WATER VAPOR SATELLITE IMAGERY OVER MN/IA...AND A PACKET OF STRONGER
30-35 KT MIDLEVEL FLOW PER REGIONAL VWP OBSERVATIONS.

STRONG HEATING IN THE WAKE OF THE SHORTWAVE/MCV ACROSS MN/IA WILL
CONTRIBUTE TO AN AXIS OF STRONG INSTABILITY ALONG THE EDGE OF THE
PLAINS CAPPING INVERSION/EML. WHILE LARGE SCALE SUPPORT FOR ASCENT
WILL PROBABLY BE WANING ALONG THIS CORRIDOR...A CONDITIONAL SEVERE
HAIL/WIND RISK WILL BE MAINTAINED IN THE EVENT ISOLATED STORMS CAN
DEVELOP GIVEN CONTINUING LOW LEVEL CONVERGENCE ALONG RESIDUAL FRONT
AND OUTFLOW BOUNDARIES REMAINING IN THE PRESENCE OF STRONG TO
LOCALLY EXTREME DESTABILIZATION.

FARTHER EAST....FROM IND TO PA...INSTABILITY AND WEAK LIFT WILL BE
FOCUSED ALONG THE STALLED FRONT SITUATED ACROSS THESE AREAS. A FEW
AFTERNOON OR EARLY EVENING STORMS COULD RESULT IN LOCALLY STRONG
GUSTS AND PERHAPS A COUPLE OF TREE-DOWN EVENTS.

...NORTHEAST...
MODEST WARM SECTOR DESTABILIZATION WAS UNDERWAY WITH LATEST
OBJECTIVE DATA INDICATING MLCAPE OF AROUND 1000 J/KG ACROSS MUCH OF
NY AND LITTLE IN THE WAY OF INHIBITION. LARGE SCALE PATTERN ACROSS
NEW ENGLAND IS MARGINALLY SUPPORTIVE OF SEVERE STORMS IF STORMS CAN
DEVELOP WITHIN THE WARM SECTOR...AND NEAR/ALONG CT RIVER VALLEY WARM
FRONT LATER THIS AFTERNOON. NWLY FLOW AT MIDLEVELS AND WEAK SLY/SELY
FLOW NEAR THE SURFACE WILL RESULT IN LOCALLY SUFFICIENT SHEAR FOR A
FEW STRONGER UPDRAFTS CAPABLE OF GUSTY WINDS AND PERHAPS SOME HAIL.
MAIN LIMITING FACT IS THE LACK OF STRONGER DEEP-LAYER ASCENT AS
PRIMARY SHORTWAVE TROUGH APPEARS TO BE CROSSING THE REGION NOW
FOLLOWED BY NEUTRAL TO WEAK HEIGHT RISES AROUND THE TIME OF MAXIMUM
STORM INITIATION POTENTIAL. NONETHELESS...IF STORMS CAN
DEVELOP...THERE MAY EVOLVE A BRIEF PERIOD OF SEVERE WEATHER IN THE
FORM OF MARGINALLY STRONG WIND GUSTS AND HAIL LATER THIS AFTERNOON.

...NRN ROCKIES...
AN AMPLIFYING MID/UPPER TROUGH ACROSS BC AND THE PACIFIC NORTHWEST
WILL SUPPORT THE INTENSIFICATION OF A SWLY MID/UPPER JET ACROSS THE
NRN ROCKIES THIS PERIOD. HEATING ACROSS THE HIGHER TERRAIN SHOULD
AID IN CONVECTIVE INITIATION LATER THIS AFTERNOON GIVEN DECREASING
STATIC STABILITY AND SUFFICIENT MOISTURE TO SUPPORT MLCAPE ON THE
ORDER OF 500 J/KG. WITH MEAN WIND AROUND 50KT AND MODEST DIRECTIONAL
SHEAR AROUND CLOUD BASE THERE IS THE POSSIBILITY FOR A FEW
FAST-MOVING LOW-TOPPED SUPERCELLS WITH SOME CHANCE FOR HAIL AROUND
AN INCH AND LOCALLY NEAR-SEVERE WIND GUSTS.

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from SPC Convective Outlooks http://1.usa.gov/1OIoOEG

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