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Measured and Modeled Snow Cover Properties across the Greenland Ice Sheet
2017
The Cryosphere Discussions
The Greenland ice sheet (GrIS) is known to be contributing to sea level rise in a warming climate. The snow cover on the ice sheet is the direct link between a potentially warmer atmosphere and the ice itself. However, little is known about the microstructure and especially about the spatial and temporal variability of the snow cover, except from indirect evidence from remote sensing. The detailed snowpack stratigraphy is relevant for processes such as the albedo feedback, water infiltration
doi:10.5194/tc-2017-55
fatcat:66qbhldwpfadbcwdhuqy3hue4m