Two keys to this setup:
1. We need the energy to be vigorous and consolidated. The 0z GFS, as we just saw, has a few weak pieces of energy running around instead of one big, strong one. The Canadian also does this to a lesser extent. If the energy doesn’t consolidate this either misses to the south or gives us a weak light snow event or two.
2. The high to the north needs to keep pressing down. Let’s say we have our strong shortwave to the southwest, but the high trends much weaker. This causes the storm to be another front end snow to ice/rain event. Not only does a strong high to the north keep temperatures cold, but it enhances the thermal gradient which increases lift and makes the snow heavier, despite a sfc low that’s not as strong. This is why PDII was such a big storm with a low that never really bombed out like most KU storms.