How this storm goes appears to be largely tied to the timing of NS energy and the degree of interaction/phasing. Two of the last 3 GFS runs have a healthy precip shield with moderate snow in the Tenn valley, but a piece of NS vorticity drops down on top and damps the wave, thus we see weaker surface reflection and the precip weakens as it moves eastward. The 2 basic options for a 'good' outcome seem to be- phase the NS energy with the southern wave right around the Mississippi river valley- a lot more dig and more potential, but not too far west where it amplifies too soon and tracks inland; the other option is the southern shortwave slides eastward underneath that NS vorticity ribbon with little to no interaction. A flatter solution but less complicated.