I am kind of ignorant but it seems to me that this is saying something different than the NWS Huntsville's AFD.
		
		
	 
Yes, it does seem to contradict the HSV AFD. Watched Brad Travis at 5 and he seemed to think initially it would weaken in northwest AL and restrengthen as it moves east. 
LONG TERM...(Saturday night through Wednesday)
Issued at 345 PM CDT Thu Apr 11 2019
Models continue to show a strong storm system moving from Oklahoma/Texas
towards the Tennessee Valley Saturday evening. A large area of
rainfall with strong to severe thunderstorms will 
likely be ongoing
and moving from western Mississippi into northwestern Alabama in the
by the late evening hours. Models have continue to trend slightly
slower with the movement of this 
convection into the area. Ample bulk
shear and 
helicity will be in place over northern Alabama and
southern middle Tennessee by midnight and will continue to be in
place overnight ahead of this system. However, the better 
instability
will remain further west over Mississippi and eastern Louisiana.
However, models do show between 200 and 800 
J/KG of 
SBCAPE extending
into much of northern Alabama and portions of southern middle
Tennessee. Most models focus the better 
instability around 500 
J/KG
or more in northwestern Alabama southeast to near Cullman county.
Given the very strong winds aloft and ample forcing this should be
able to sustain strong to 
severe thunderstorm activity at least near
and west of I-65. Further east, there is more uncertainty but just
enough 
instability may be available to keep this threat going. The
main window for this severe weather looks to be between midnight and
6 AM. This activity is shown by models to be along a pre-frontal
trough axis ahead of the main cold 
front.
Additional redevelopment of strong to severe thunderstorms may occur
as the actually cold 
front moves through during the afternoon hours
with this storm system. However, timing of this activity and how
widespread it will be is highly uncertain at this point. Especially
with earlier 
rainfall and continued cloud cover expected. However,
models do show between 500 and 1200 
J/KG of surface based 
CAPE
re-surging ahead of the 
front Sunday afternoon. Ample bulk 
shear and
a continue strong 
wind field could allow severe thunderstorms capable
of producing damaging winds, large 
hail, and possibly tornadoes to
develop. At this point there is some disagreement in model guidance
whether the 
tornado threat will be realized, as a few models show
very little 
helicity remaining ahead of the 
front. A good 1 to 2
inches of 
rainfall with some locally higher amounts looks possible
with this activity. Any linger 
isolated showers or thunderstorms
should push east into Georgia during the early evening hours. A wind
advisory in addition may be needed Sunday afternoon, as soundings
show the 
atmosphere mixing up to winds around 40 to 45 knots. Much
cooler air will push into the area behind the 
front, as lows drop
into the upper 30s to lower 40s by daybreak on Saturday.