Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4688294 | Journal of Geodynamics | 2012 | 13 Pages |
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
H. Ewert, A. Groh, R. Dietrich,