There’s a lot that factors into it, IMO. Veering in the low levels under 850mb, speed/velocity, inversions, stability, etc. That’s why BTV studies the Froude number so much. In some events a certain wind direction at 850mb can result in a downslope, but then in another event that same wind direction seems to be pushing the moisture over the barrier so effectively it’s a QPF jackpot.
Here sort of explains it... if there’s blocking then the Lee side down slopes, if it’s unblocked the Lee side actually jackpots. BTV often references it on NW flow but it goes for all wind directions... sometimes I think we do great with an east flow in a synoptic storm only to find the precip maximum ended up on the west side because it was unblocked...likewise sometimes we jackpot in NW upslope on the east side. It’s not as simple as just looking at a straight wind direction.
“The Froude Number represents the flow of air when it comes in contact with a barrier, in Vermont's case, the Green Mountains. It is an estimation of whether the flow can make it over the mountains or not and is basically a ratio of the wind perpendicular to the mountain chain versus the atmospheric stability.
Under northwesterly flow, if the Froude Number is low (< 1), or subcritical and blocked, the air will not make it over the mountain and the precipitation will back up and fall primarily along the spine of the Green Mountains and the western slopes. If it is very low (< 0.5), the precipitation will back further west into parts of the eastern Champlain Valley and the western slopes of the Green Mountains.
If the Froude Number is high (> 1), or supercritical and unblocked, the air will flow freely over the mountains and deposit the heaviest precipitation on the east side. A Froude Number near 1 is critical and the heaviest precipitation will likely fall along the barrier.”