Thursday, August 10, 2017

SPC Aug 11, 2017 0100 UTC Day 1 Convective Outlook

SPC 0100Z Day 1 Outlook
Day 1 Outlook Image
Day 1 Convective Outlook  
NWS Storm Prediction Center Norman OK
0740 PM CDT Thu Aug 10 2017

Valid 110100Z - 111200Z

...THERE IS AN ENHANCED RISK OF SEVERE THUNDERSTORMS ACROSS PARTS OF
SOUTHEASTERN COLORADO AND SOUTHWESTERN KANSAS INTO THE OKLAHOMA AND
TEXAS PANHANDLE REGION...

...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS ACROSS SURROUNDING
AREAS OF THE CENTRAL PLAINS...

...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS SURROUNDING THE
SLIGHT RISK AREA...NORTHEASTWARD INTO PARTS OF THE UPPER MIDWEST...

...SUMMARY...
An organizing cluster of thunderstorms still appears possible this
evening across parts of the central high Plains, which may be
accompanied by a swath of potentially damaging wind gusts.

...01Z Outlook Update...
Ahead of the cold front trailing from the modest lower/mid
tropospheric cyclone over the Upper Midwest/upper Great Lakes
region, scattered vigorous thunderstorm activity is ongoing near
Lake Michigan through northern Illinois and the Missouri/Iowa border
area.  Pockets of moderately large CAPE and modest deep layer shear
has supported some severe hail and wind in the stronger storms, but
this threat appears in the process of diminishing as the pre-frontal
instability corridor begins to wane.

Stronger deep layer shear is generally focused across the central
Plains, on the southwestern periphery of the mid-level troughing now
shifting east of the northern Rockies, supported by more pronounced
veering of winds with height beneath 30-40 kt west northwesterly 500
mb flow.  This has contributed to widely scattered strong to severe
storm development.  Some of this activity probably will linger into
and through the evening hours, particularly near a remnant pre-cold
frontal corridor of stronger differential surface heating, from
portions of southeastern Colorado into northwestern Oklahoma. 
Forcing for ascent associated with warm advection, enhanced by a
weak to modest southerly low-level jet, could still support the
evolution of an upscale growing and organizing convective cluster
this evening.  In the presence of thermodynamic profiles
characterized by modestly steep mid-level lapse rates and sizable
CAPE on the order of 2000+ J/kg, the environment may be conducive to
convection capable of producing a swath of potentially damaging wind
gusts into and through the 03-06Z time frame, before activity
weakens overnight.

..Kerr.. 08/11/2017

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