Article ID Journal Published Year Pages File Type
4688294 Journal of Geodynamics 2012 13 Pages PDF
Abstract

- We inferred the Greenland ice sheet mass balance from the analysis of satellite data.
- Volume change rates were derived from repeated ICESat laser altimetry data.
- GRACE monthly gravity field solutions were used to estimate the mass change rates.
- Both results were combined in order to determine the density of the mass change.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Authors
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