I think the main divergence is in if we can get the coastal to help us out. The 18z Euro shows a solution where we get pretty much no help from the coastal besides aiding in some moisture fetch and instead rely on the H5 dynamics to get any sort of snowfall. Meanwhile, the other camp of the GFS and CMC instead have the coastal prominently help out the H5 max through aiding in lift, moisture transport, and even cold air through the CCB. Is a bit of a egg and chicken game too where a stronger H5 vortmax is more likely to capture/induce a more favorable surface low position.