A lot of people repeatedly forget that Dixie alley can very easily produce tornadoes even with messy storm mode.
Let alone during the winter when the tropopause above the PBL is far colder than it is during the spring or summer, which means surface temps don’t need to be as high or surface laspe rates as steep to get a tornado outbreak.
A broad longitudinal warm sector provides plenty of room and time for supercells to establish themselves.
The wind vector in the jet streak is more perpendicular than parallel above the low level jet, which favors discrete development.
Watch for the strength of the surface low, if it’s on the stronger side <1005, then surface winds will be more backed allowing for stronger entrainment.
This has the potential to be a quite a substantial outbreak if this comes to pass.
On the other hand, this has just as much to be a minor event tornado wise. The failure mode will not be low instability, but instead if the height falls fail to produce a strong enough surface low.
A weaker surface low would not produce as strong a low level jet and the surface winds would be more parallel to said low level jet.
The messy storm mode would really become a detriment in this scenario as mass cold pooling would definitely cause outflow dominate cells.