Sunday, January 15, 2017

SPC Jan 15, 2017 1300 UTC Day 1 Convective Outlook

SPC 1300Z Day 1 Outlook
Day 1 Outlook Image
Day 1 Convective Outlook  
NWS Storm Prediction Center Norman OK
0655 AM CST Sun Jan 15 2017

Valid 151300Z - 161200Z

...THERE IS A SLIGHT RISK OF SEVERE THUNDERSTORMS WEST-CENTRAL TO
NORTH-CENTRAL TX...

...THERE IS A MARGINAL RISK OF SEVERE THUNDERSTORMS SURROUNDING THE
SLIGHT INTO SOUTHEAST OK...

...SUMMARY...
Scattered severe storms will be possible this afternoon into tonight
across parts of west-central to north-central Texas. A few
tornadoes, damaging winds, and large hail are anticipated.

...Synopsis...
Compact shortwave trough along the Sonora/Chihuahua border will
eject northeast into OK by early Monday. Attendant surface low
should become established over the Permian Basin this afternoon and
track northeast into central OK overnight along an advancing warm
front. As this occurs, a Pacific cold front will push east into
central TX. 

...Southern Great Plains...
A modifying warm sector across southern TX will attempt to advance
north as a swath of 35-50 kt low-level southerlies persist through
this afternoon, and further strengthen tonight. Model mean mixing
ratios appear too moist compared to 12Z Del Rio and Corpus Christi
observed soundings. In addition, a modified continental air mass,
reinforced by ongoing and additional elevated convection today,
should limit the northwest advancement of the warm sector to parts
of west-central and north-central TX. Largest buoyancy with around
1000 J/kg MLCAPE should be confined to the Edwards Plateau where an
elevated mixed layer will be most pronounced.

Surface-based storms appear most likely to form across the Pecos
Valley in the early afternoon as mid-level DCVA/height falls
overspread the destabilizing northwest periphery of the modified
warm sector. This activity should further expand in coverage and
shift east-northeast, with an extensive squall line probable by late
evening from parts of south-central OK through central TX. 

30-50 kt effective bulk shear will support organized storm
structures including supercells and bowing line segments. Along the
southern periphery of development over the Edwards Plateau, where
convection would seemingly have the best potential to remain
discrete, model soundings indicate veer-back-veer vertical wind
profiles with a weakness in the hodograph around 700 mb. This may
temper a greater tornado risk from being realized. Farther northeast
along the Red River, where mode should become increasingly linear
with time, the primary uncertainty is how far north surface-based
instability and a corresponding damaging wind/brief tornado risk
will extend into OK tonight.

..Grams/Smith.. 01/15/2017

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