This is sort of a chicken/egg argument and both can feed on eachother...if the vortmax is stronger, it will help force the flow to buckle and you'll see this tugged back west...on the flip side, if the flow was already a bit more buckled, you'll see the vortmax curl up to the north easier....even if it's weaker. The problem is we are dealing with a relatively weak vortmax right now...it's not this intense ball of vorticity which would make this a really big storm. So smallish features like convection can wreak havoc on the eventual progression of the whole thing.
The pros: The shortwave is already negatively tilted pretty good...so that is going to help a lot. It's why even on these really ugly strung out solutions, we're still somehow getting advisory snow from ASH to ORH and SE and warning snows over SE MA.
Cons: Vortmax is weak and the shortwave is relatively "shallow"....meaning it is somewhat disconnected from the main shortwave over the western lakes. This will give a bit of tendency to try and slide the low east....but it can also work in our favor if we deform where that happens.