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You are looking at an outlook that is part of the medium range forecast (the outlook for days 4-8). The most important thing to note is that lack of a risk does not mean zero risk. Generally speaking, confidence has to be pretty high for the Storm Prediction Center to have an outlook area this far into the future.
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| Day 4 | Friday, October 9 | potential too low |
| Day 5 | Saturday, October 10 | 15% |
| Day 6 | Sunday, October 11 | predictability too low |
| Day 7 | Monday, October 12 | predictability too low |
| Day 8 | Tuesday, October 13 | predictability too low |
ZCZC SPCSWOD48 ALL ACUS48 KWNS 060812 SPC AC 060812
Day 4-8 Convective Outlook NWS Storm Prediction Center Norman OK 0312 AM CDT Tue Oct 06 2026
Valid 091200Z - 141200Z
DISCUSSION
A surface high will move from the OH Valley into the Northeast on Fri/D4 as an upper trough lifts out of the region and temporary upper ridging occurs. A stationary boundary is still forecast to be along the northern Gulf Coast at this time, and a weak midlevel wave will begin to form over TX. Meanwhile, a potential tropical cyclone may develop toward the central Gulf of America.
Low-level winds will begin to veer to a southeasterly direction along the Gulf Coast late Fri/D4 into Sat/D5, as the potential tropical cyclone evolves. NHC currently gives a high probability of this occurring. As such, an influx of rich moisture will develop out of the south, with a substantial rain shield and embedded thunderstorms likely along the northern Gulf Coast beginning Fri/D4 night. Initially, surface temperatures over land will remain cool due to precipitation and initial modification of the surface ridge air mass.
At this time, it appears Sat/D5 is the most likely time for the more substantial low-level warming to occur, with tropical yet sufficiently unstable profiles. Of particular note is how the developing shortwave trough over TX interacts with the tropical low. Some models indicate 40-45 kt midlevel winds, which would complement the strong low-level shear and favor low-topped supercells with tornado potential. The greatest threat area should be along the coastal counties given expected poor low-level lapse rates farther inland. Initial elevated convection may give way to an east-west zone of supercells as the coastal baroclinic zone moves inland. Some additional threat into Sun/D6 may exist as well.
For the period Mon/D7 into Tue/D8, models are now developing an amplified upper trough over the western CONUS. Low-level moistening will be most prominent later in the period, and could eventually result in a zone of strong to severe storm potential, however, predictability is quite low at this time.
..Jewell.. 10/06/2026
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