A unique climatological view of this behavior comes from from profiling radars in the northern Sierra Nevada deployed as part of NOAA's Hydrometeorlogy Testbed. They show that the mesoscale lowering of the snowline is a robust feature common to nearly all major storms. Typically the snowline drops by at least 200 m as it approaches the terrain, but this lowering has significant storm-to-storm variations.
The mesoscale behavior of the snowline is investigated in detail for a major storm over the northern Sierra Nevada. Comparisons of observations from sondes and profiling radars with high-resolution simulations using the WRF model show that WRF is capable of reproducing the observed lowering of the snowline in a realistic manner. Diagnosis of model output reveals that pseudo-adiabatic transport related to orographic blocking, localized cooling due to melting of orographically enhanced snowfall, and spatial variations in hydrometeor melting distance all play important roles in lowering the snowline. Simulation of this behavior is surprisingly insensitive to model horizontal resolution, but has important sensitivities to microphysical parameterization.