Abstract
Using the most recently published regional and global deglaciation histories we provide updated estimates of the Glacial Isostatic Adjustment (GIA) component of present day uplift at a suite of GPS sites in Greenland. The GIA of the solid Earth beneath Greenland contributes -6 to +10 Gt/yr to the present day mass trends observed by the Gravity Recovery and Climate Experiment (GRACE), representing
Original language | English |
---|---|
Pages (from-to) | 101-111 |
Journal | Current Climate Change Reports |
Volume | 2 |
Issue number | 3 |
Early online date | 5 Jul 2016 |
DOIs | |
Publication status | Published - Sept 2016 |
Keywords
- Geodesy
- Greenland Ice Sheet
- Glacial Isostatic Adjustment