EXCELLENT discussion by Davis out of BMX on all of the caveats to tomorrow's forecast.
"A complex forecast is setting up for Thursday`s potential severe
weather event. Synoptically, a longwave neutrally tilted 
trough
will be advancing into the area, taking on a negative 
tilt by
Thursday evening. Within this 
trough, an upper low will be moving
through the Ozarks while a pronounced southern stream 
shortwave
will be moving along the Gulf Coast/northern Gulf, extending well
south into the Gulf in association with a strong subtropical 
jet.
Strong upper-level forcing will overspread the Deep South and Gulf
Coast due to 
vorticity advection and diffluent 
flow aloft. A
surface low will be located near St. Louis with a cold
front/surface 
trough extending southward through the Mississippi
Valley.
Favorable 
dynamics, 
shear, lapse rates, and 
moisture will
be present for severe weather, but there are still two main
uncertain 
mesoscale details that will determine whether
significant destabilization occurs. The first question is if the
line of storms expected to develop late this afternoon/early this
evening over the Arklatex region will hold together and move into
the area Thursday morning in association with a lead 
shortwave and
low level jet. If it were to hold together then a scenario
similar to last Saturday could evolve where later activity is
inhibited. However, the majority of the model guidance including
the CAMs and the typically reliable WRF-ARW and 
NSSL WRF currently
indicates this activity will either dissipate or become 
scattered
enough to be a non-factor. Therefore, current thinking is that
morning 
convection will not be a limiting factor. The second
question is whether 
convection developing along the LA/MS Gulf
Coast associated with the southern stream wave/subtropical 
jet
will cause 
convection further north to be "cut off"/suppressed.
This will be something to 
watch in future CAM runs. Currently,
however, CAMs seem to suggest that this activity may develop too
late, be too far south, or be too 
scattered to prevent strong
destabilization/
supercell development ahead of the 
front over
northern Mississippi. Additionally, forcing with the upper low and
higher 
dew points already being in place may prevent coastal
convection from being an inhibiting factor.
In that case, a favorable environment for 
supercell development
will be in place over northern Mississippi with 1000-2000 
J/kg of
CAPE and 50+ 
kts of southwesterly 
shear helping to keep storms
ahead of the slow-moving 
front. These supercells would then have
the potential to move into West Alabama during the late
afternoon/early evening, with sufficient 
helicity/backed surface
winds for a couple tornadoes and large 
hail. Keeping in mind the
above uncertainties, the enhanced risk area from 
SPC in our far
western/northwestern counties depicts the potential threat well,
with a threat gradually decreasing off to the east. In addition,
southwesterly Corfidi vectors indicate that some of the
convection associated with the southern stream wave will move into
mainly our southern counties Thursday afternoon and pose a threat
for mainly damaging winds and 
hail. Please stay tuned to future
updates and remain weather aware on Thursday, as the forecast will
be sensitive to small scale details."