An analysis of how observed snow depths and simulated compaction rates can be used to infer solidprecipitation rates and enhance physics-based snow models.

Adam H Winstral, WSL Institute for Snow and Avalanche Research SLF, Davos Dorf, Switzerland, Jan Magnusson, Unaffiliated, Oslo, Norway and Tobias Jonas, SLF / WSL, Davos Dorf, Switzerland