When we have high latitude blocking, northern Canada is going to be "relatively warm". The intrinsic state is lower heights in the HL regions, and the cold tends to stay there. We need that to be inverted to get persistent cold down here in the midlatitudes...BUT, the primary issue so far is the strong, sustained NE Pac vortex pumping warm Pac air into our nearby source region for cold. So the HL blocking is not really the issue(although the NA ridge has been positioned too far east so far)- rather there is simply a lack of cold air to drive far enough southward, and the baroclinic zone ends up further NW. That zone represents a thermal gradient, or zone of conflict, and is where low pressure will develop/track along the eastern side of a trough. Unfortunately that has been generally west of our area so far this early winter. It remains to be seen if that can shift further SE as we move forward. A combo of relaxation of the NE PAC trough (colder in the Yukon)and a continuation of the negative AO plus more of a west based -NAO would allow for some favorable outcomes as we head into our best snow climo period. So yeah, patience lol.