I'm making my visuals right now....I think its all about how quickly that energy transfers to the coast, which will be determine by how deep the parent system and how pervasive the polar airmass is. We want weaker parent energy and strong, stubborn antecedent polar air mass to induce a faster transfer to truncate the SW flow aloft....THAT is what will change this from a SWFE to a miller B. Could get best of both worlds, too, in the you get a SWFE, that then gives way to a miller B, especially north and east. 12z OP GFS shows this. You can toss the rules regarding how much snow you can get in a SWFE at that point because its no longer a SWFE..its a coastal.