US Mesoscale Discussions

Storm Prediction Center Mesoscale Discussion 2378

Published Date and Time: 2026-10-15 15:15:00



   Mesoscale Discussion 2378
   NWS Storm Prediction Center Norman OK
   0213 PM CDT Thu Oct 15 2026

   Areas affected...portions of the greater northwest Texas region

   Concerning...Severe potential...Watch unlikely 

   Valid 151913Z - 152145Z

   Probability of Watch Issuance...5 percent

   SUMMARY...Scattered thunderstorms will continue to develop in an
   increasingly unstable airmass this afternoon. Although vertical
   shear will support some thunderstorm organization, weak lapse rates
   and thunderstorms quickly moving into a cooler airmass to the north
   will limit the potential for an organized wind threat. A watch is
   currently not expected.

   DISCUSSION...A messy surface pattern is found across the southern
   Plains, with a congealed outflow/stationary front stretching across
   northwest Texas into southeast Oklahoma and west-central Arkansas. A
   slowly moving synoptic front is located to the west and north of the
   stationary front. In between widespread light to moderate
   precipitation is falling across far northwest Texas and much of
   western/central Oklahoma. 

   Along and south of the stationary front, temperatures have warmed
   into the mid to upper-80Fs in the presence of widespread dewpoints
   in the mid-60Fs to lower-70Fs. The result is MUCAPE values in excess
   of 3000 J/kg ahead of the cold front across west Texas and south of
   the stationary front. Here scattered thunderstorms are developing
   along the surface cold front and also along the remnant stationary
   front as convective temperatures are reached. 

   Vertical profiles across the area show deep-layer shear on the order
   of 30-40 knots, oriented from southwest to northeast. They also show
   moist-adiabatic profiles, with weak mid-level lapse rates. Thus,
   while thunderstorm organization is possible, including transient
   mid-level thunderstorm rotation, the large hail threat should be
   muted. 

   The deep-layer shear vector is also oriented in such a manner that
   will favor updrafts developing in the warm sector to move across the
   stationary front and into the cooler surface airmass. Thus, while
   warm-sector low-level lapse rates on the order of 7-8 C/km exist,
   thunderstorms will likely spend little time realizing them before
   moving into an airmass with low-level lapse rates closer to 4-5
   C/km. This should limit the potential for organized widespread wind
   threat, and limit the potential to isolated wet downbursts. 

   Should a thunderstorm develop a sufficiently strong cold pool that
   can stay ahead of the synoptic front and outflow boundary, a small
   window for damaging winds will exist this afternoon/evening. This
   scenario is far from certain, but will be monitored.

   ..Marsh/Guyer.. 10/15/2026

   ...Please see www.spc.noaa.gov for graphic product...

   ATTN...WFO...FWD...OUN...SJT...LUB...MAF...

   LAT...LON   31590130 31770140 32110127 32410109 32840109 32990111
               33250092 33520033 33659951 33659891 33669834 33639788
               33439768 32959771 32519787 32159814 31739903 31569952
               31530025 31590130 

   MOST PROBABLE PEAK WIND GUST...UP TO 60 MPH
   MOST PROBABLE PEAK HAIL SIZE...UP TO 1.25 IN



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