The SNOWPACK model simulates the development of the snowpack during the winter, based on meteorological input data.
In a wind tunnel and at measuring sites we investigate where snow is eroded and deposited by wind and how snow changes during transport.
Improving our understanding of snow distribution processes can enable us to forecast high and low water levels more accurately in future.
What happens at the boundary between the snowpack and atmosphere or when snow melt begins? And why do some patches of snow endure longer than others?
We study polar snow and how it "ages". These findings help us reconstruct past climates and improve our predictions.