Firn data compilation reveals widespread decrease of firn air content in western Greenland
Vandecrux, BaptisteDepartment of Glaciology and Climate, Geological Survey of Denmark and Greenland, Copenhagen, Denmark - Department of Civil Engineering, Technical University of Denmark, Kongens Lyngby, Denmark
MacFerrin, MichaelCooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, USA
Machguth, HorstDepartment of Geosciences, University of Fribourg, Switzerland - Department of Geography, University of Zurich, Switzerland
Colgan, William T.Department of Glaciology and Climate, Geological Survey of Denmark and Greenland, Copenhagen, Denmark
As, Dirk vanDepartment of Glaciology and Climate, Geological Survey of Denmark and Greenland, Copenhagen, Denmark
Heilig, AchimDepartment of Earth and Environmental Sciences, Ludwig Maximilian University, Munich, Germany
Stevens, C. MaxDepartment of Earth and Space Sciences, University of Washington, Seattle, USA
The Cryosphere. - 2019, vol. 13, no. 3, p. 845–859
English
The perennial snow, or firn, on the Greenland ice sheet each summer stores part of the meltwater formed at the surface, buffering the ice sheet’s contribution to sea level. We gathered observations of firn air content, indicative of the space available in the firn to retain meltwater, and find that this air content remained stable in cold regions of the firn over the last 65 years but recently decreased significantly in western Greenland.