I'm having a hard time buying the progressive solutions w/ the 50-50 low.
It's a tough sell for me knowing a persistent, shallow, and unusually intense cold air mass sitting east of the Appalachians will tug on/slow down the +PVa aloft more than forecast by NWP (through generation of low-mid level static stability above the CAD dome >> +PV )
Here's the graphic I made ~ 5 weeks ago to explain how this physical process works:
If we had -NAO over the top, the easterly flow under the ridge would slow this trough down even further, but beggars can't be choosers.