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What is Snow Mass Balance in Wolf Creek, Yukon about?

This document discusses snow accumulation processes in the Wolf Creek Research Basin in Yukon, Canada. It describes two key processes: 1) interception of snowfall by forest canopies, which can retain up to 67% of snowfall and lead to 38-45% sublimation losses over winter, and 2) redistribution of snow by wind, which can remove 50% of snowfall from exposed alpine areas and 25% from low-lying shrublands, redistributing it to sheltered slopes and valleys. The snow accumulation patterns have implications for wa

Author

Eladimir

Language

EN