On the upper Toll Road. This past multi-week cycle was largely upslope driven. There have been synoptic episodes at times, but multiple CAA intrusions into moist, higher than normal PWAT air masses is going to precipitate efficiently in the NW flow zones.
Blocked and unblocked flow, but either way it has dumped over the Spine. Blocked SE flow on front side followed by NW flow can absolutely load the upper east side. Upslope flow with spring moisture levels has historically led to snowier (higher QPF) events than expected in the mountains.
In the end, regardless of location it has been the longest high elevation observation in the state of Vermont. NWS has an elaborate camera set up on “the Stake.” Almost 70 years of observations to compare to at the exact same spot.