Ahhh ok so it wasn't necessarily a downslope valley event but more a pure elevation event. I usually put downslope in the "it doesn't precipitate much" category while moisture gets wrung out on the slopes. Not sure what anyone classifies that storm as.So massive QPF event with a very tight rain/snow line. Obviously probably some upslope assist in dynamic cooling, and compressional warming on the downside, but I love those tight snow lines. We see those gradients on the mountain but it's much more dramatic when it happens in populated areas so close to the surface. Rain below 2,000ft and 30" of snow at 3,000ft isn't as dramatic as rain at sea level and 30" at 1,000ft.
Reminds me of the April 2012 upslope event at Stowe where the office at 1,500ft had 3" of like white water, but it was 18"+ just 500ft higher at 2kft, and 30"+ above 2,500ft. Total QPF was almost 4" at the summit Coop. One of the highest QPF events I've ever seen from orographics. No thermal advection, just a steady state heavy precip event where heavy rates can only bring the snow level down so far.