Evaluation of parameterization schemes in the detailed Snow Metamorphism and Albedo Process (SMAP) snowpack model
Using 15 years of observational data from Sapporo, this study evaluates the Snow Metamorphism and Albedo Process (SMAP) model to determine that new snow density, compression viscosity, and effective thermal conductivity are the primary sources of parameterization uncertainty affecting short-term snowfall, seasonal densification, and late-winter heat transfer, respectively, while water movement schemes have minimal impact under dry-snow conditions.