- Moderator
- #21
SPC still holds a large 15% area for Day 5 (Saturday) and says the tornado threat will depend on discrete development ahead of the front. Remember, we are still in winter and it does not take as much instability to have a very, very bad day.

...Day 5/Saturday...
A strong trough, which has trended more amplified in the ECMWF, is
expected to impact the Sabine Valley into the Southeast starting in
the afternoon. The latest model trends also have a more favorable
placement of the surface low in the Tennessee Valley. These factors
will drive strong moisture advection into the region by Saturday
morning, continuing into Sunday. Intense wind fields throughout the
column will support organized storms capable of all hazards.
Damaging winds, particularly with linear convection along the strong
cold front, currently appears as the main threat. The magnitude of
the tornado threat will largely depend on discrete development ahead
of the front. Given the moist environment with minimal inhibition
and strong forcing, that scenario is certainly plausible. Discrete
development or not, low-level wind fields still will support
line-embedded circulations. Despite more limited buoyancy farther
north, the strongly forced convective line and 60-70 kts of 850 mb
flow would support damaging winds even in shallow convection.
Uncertainties still remain along the fringes of the highlighted area
(i.e., how far west will convection form, how unstable will it be to
the north/east). Mid-level lapse rates will also not be overlay
steep. Even so, the overall pattern continues to support the
potential for scattered to numerous severe storms.

...Day 5/Saturday...
A strong trough, which has trended more amplified in the ECMWF, is
expected to impact the Sabine Valley into the Southeast starting in
the afternoon. The latest model trends also have a more favorable
placement of the surface low in the Tennessee Valley. These factors
will drive strong moisture advection into the region by Saturday
morning, continuing into Sunday. Intense wind fields throughout the
column will support organized storms capable of all hazards.
Damaging winds, particularly with linear convection along the strong
cold front, currently appears as the main threat. The magnitude of
the tornado threat will largely depend on discrete development ahead
of the front. Given the moist environment with minimal inhibition
and strong forcing, that scenario is certainly plausible. Discrete
development or not, low-level wind fields still will support
line-embedded circulations. Despite more limited buoyancy farther
north, the strongly forced convective line and 60-70 kts of 850 mb
flow would support damaging winds even in shallow convection.
Uncertainties still remain along the fringes of the highlighted area
(i.e., how far west will convection form, how unstable will it be to
the north/east). Mid-level lapse rates will also not be overlay
steep. Even so, the overall pattern continues to support the
potential for scattered to numerous severe storms.