What I notice most is how backed up the mid-latitude jet is, as there are 3 regions with lower 500mb heights than the warmth to the north. When I mapped DC and Baltimore's top snowfalls/snowfall months/snowfall seasons, the same thing is true.. there are 3 areas of lower heights than even the -AO/-NAO +500mb heights to the north. This tells me that general -H5 is more important than having Polar blocking. I think the problem with my analogs is that the northern ridge is too far north: over 90N. 90N puts a mean trough at 45N, but not as much 39N. We need classic Greenland/Davis Strait blocking to do better. Unfortunately with Arctic ice melt, it's something that reverses 100% the following Winter, and that's centered 90N. I think this is why the new Euro seasonal has ridging/blocking centered at 90N.