That being said, we see some of the same features that we saw during the storm the previous weekend. In particular, the peak depth of string radar reflectivities (organge colors) occurs at about mid canyon. Farther up canyon, the storm shallows.
Later, after the frontal band moves through, this structure persists.
In particular, note how the strongest/deepest returns are mid canyon. In this instance, precipitation rates are probably greatest from about the White Pine Parking lot to the High Rustler ridge and much weaker in Albion Basin and the Supreme-lift area.
It will be fun to diagnose the processes responsible for this storm structure and see if our computer models can replicate it.