SPC Forecast Products
SPC Jan 23, 2026 0700 UTC Day 2 Convective Outlook
Published: Fri, 23 Jan 2026 at 12:39:35 AM CST
SPC 0700Z Day 2 Outlook
Day 2 Outlook Image
Day 2 Convective Outlook  
NWS Storm Prediction Center Norman OK
1236 AM CST Fri Jan 23 2026

Valid 241200Z - 251200Z

...NO SEVERE THUNDERSTORM AREAS FORECAST...

...SUMMARY...
Severe thunderstorms are not anticipated across the U.S. Saturday
through Saturday night.

...Synopsis...
The mid-level pattern over the CONUS is forecast to amplify
significantly this weekend as initially split flow consolidates
behind a departing East Coast upper trough. Several short wave
perturbations (over the Southwest, northern Mexico, and southern
Canada) will gradually consolidate into larger-scale mid-level
troughing across the Rockies and Great Plains by late Saturday
night.

As upper troughing becomes established, a strong Arctic cold front
will rapidly move south with high pressure (1045+ mb) building in
its wake. An extensive cold intrusion will occur with significant
latitudinal suppression of lee cyclogenesis to far northern Mex and
the southern Gulf Coast. This will greatly limit inland moisture
return. Still, strong lift in the form of isentropic ascent over top
the front will support widespread winter precipitation (some
possibly with isolated lightning) over the Plains and south-central
US much of Saturday.

...South Texas Coast...
As the strong Arctic high pressure building over the southern Plains
forces the cold front to surge south, the Arctic air mass will
rapidly undercut the a remnant warm sector over parts of Far South
TX. Strong isentropic ascent over the shallow surface front will
allow for modest elevated destabilization. However, poor mid-level
lapse rates (6-6.5 C/km) and the overnight arrival of the more
consolidated upper ascent should preclude the development of larger
buoyancy. Thus, while a stronger storm is briefly possible along the
immediate coast or elevated behind the front, the overall severe
risk appears quite limited.

..Lyons.. 01/23/2026

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SPC - No watches are valid as of Fri Jan 23 06:40:02 UTC 2026
Published: Fri, 23 Jan 2026 at 12:39:05 AM CST
No watches are valid as of Fri Jan 23 06:40:02 UTC 2026.

SPC - No MDs are in effect as of Fri Jan 23 06:40:02 UTC 2026
Published: Fri, 23 Jan 2026 at 12:39:05 AM CST
No Mesoscale Discussions are in effect as of Fri Jan 23 06:40:02 UTC 2026.

SPC Jan 23, 2026 0600 UTC Day 1 Convective Outlook
Published: Thu, 22 Jan 2026 at 11:42:55 PM CST
SPC 1200Z Day 1 Outlook
Day 1 Outlook Image
Day 1 Convective Outlook  
NWS Storm Prediction Center Norman OK
1139 PM CST Thu Jan 22 2026

Valid 231200Z - 241200Z

...NO SEVERE THUNDERSTORM AREAS FORECAST...

...SUMMARY...
Scattered weak thunderstorm activity is likely today into tonight
across the Texas Big Bend region into central Texas.

...Synopsis...
Late-evening water-vapor imagery depicts increasing ascent across
northern Mexico into the Southwest/Big Bend region of TX as an upper
low off the southern CA coast begins to slowly shift east. At the
surface, a cold front continues to push south across the Plains with
modest moisture return ongoing along the TX Coastal Plain.
Precipitation is expected to slowly increase from the Big Bend
region northeastward into the southern Plains/Ozark Plateau through
the day as isentropic ascent strengthens across central TX. Isolated
to scattered thunderstorm development is anticipated along and north
of the cold front as it impinges on a plume of returning moisture. 

...Big Bend Region to Central Texas...
Moisture return of mid 50s to low 60s dewpoints along and south of
the I-10 corridor and into the Big Bend region is expected by
evening and should support a swath of 500-1000 J/kg MLCAPE.
Scattered thunderstorm development is expected along the front
across the Edwards Plateau by early evening, spreading east as the
front pushes further into the unstable air mass. While a few storms
may initially be surface-based, northeastward storm motions will
quickly displace any deep convection onto the cool side of the
boundary. Wind profiles are expected to strengthen through the day
in response to the approaching upper wave, and could support
effective shear values on the order of 40 knots. Despite this, a
combination of modest buoyancy profiles (lifted indices generally -2
to -3 C), rapid undercutting by the front, and a propensity for
storm interactions/upscale growth should largely mitigate the
potential for severe convection. 

A few CAM solutions, notably the 00z HRRR, hint at the potential for
upscale growth of a surface-based convective cluster as it
propagates eastward along the front with an attendant threat for
damaging winds. While plausible given the aforementioned CAPE/shear
parameter space, the lack of supporting signal in other CAM
solutions and ensemble/calibrated guidance, along with unfavorable
phasing with the diurnal cycle, suggest that this is a relatively
low probability scenario.

..Moore/Thornton.. 01/23/2026

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