Accurate modeling of snow accumulation and melt processes under forest canopy is relevant for a variety of applications across a wide range of spatial scales. At the stand scale, the presence and duration of snow impacts eco-physiological and biogeochemical processes such as vegetation growth and microbial decomposition (Sorensen et al., 2016;Wipf & Rixen, 2010). At watershed scales, seasonal snow and its depletion in spring create distinct runoff patterns (Barnhart et al., 2016;Viviroli & Weingartner, 2004). In the Northern Hemisphere, forest covers 19% of the seasonally snow-covered land surface (Rutter et al., 2009), making forest snow an important determinant of wintertime land surface albedo in these environments, with further influences on global-scale climate feedback mechanisms (Abe et al., 2017;Thackeray et al., 2014). In today's changing environment, both snow regimes and vegetation cover are subject to shifts (Derksen & Brown, 2012;Mote et al., 2018;Pearson et al., 2013): Consistent and dramatic snow cover declines have been reported, with decreases in June snow cover extents of ∼13% per decade in arctic regions (Mudryk et al., 2017) and consistent reductions in spring snow cover duration of on average 5 days per decade in alpine regions (Marty et al., 2017) since the 1960s. These trends are expected to continue. Warming temperatures are further intensifying wildfire risk and insect outbreaks, causing a threat to boreal and mountain forest health (Gauthier et al., 2015). Reliable forest snow models can help us to better predict the consequences of these environmental changes. This is paramount in support of ecosystem and water management and further mitigation and adaptation strategies (Sturm et al., 2017;Viviroli et al., 2011).Modeling forest snow remains challenging. The forest snow model intercomparison project SnowMIP2 demonstrated most snow models to perform worse in forests than in open areas (Essery et al., 2009;Rutter et al., 2009). Forest snow cover dynamics are shaped by canopy-induced processes, including snow interception, radiation transfer, and wind attenuation (