Oregon at the moment. I agree, the eastern troughing has been the persistent theme since about mid December and I am also skeptical that the SE ridge develops, although the ridge shifting back to ~160 W should help focus the cold a bit further W, assuming it occurs. The ridge as shown would need to amplify more to drive the cold down west of the Rockies, as it stands here this would mainly support cold from the divide to about MN/Dakotas with more ephemeral effects further E. The highly anomalous NE Pac/AK blocks have largely controlled the position of the mean trough downstream. Take away the block and you'd see a lot more zonal flow across the lower 48 and a much milder pattern in general. This becomes more obvious when you look at the entire NH longwave pattern, NE Pac ridge is the initial perturbation, then downstream you have longwaves of generally decreasing amplitude until and unless there is a new feature that serves to perturb the 500 mb pattern (usually some sort of high-latitude block). Stronger waves crest and beat down the NE Pac ridge which then rebounds in their wake, often a bit further W than previously. Around New Years a strong trough developed over the Bering Sea/Alaska in response to ridging popping over Siberia. That Bering trough then translated east and was absorbed into the PV over Hudson Bay, lobes of which have been far enough S to deliver arctic air into the OH valley and SE US as well as the more usual locations. Yes I realize we don't live at 500 mb.