Time-evolving mass loss of the Greenland Ice Sheet from satellite altimetry
Mass changes of the Greenland Ice Sheet may be estimated by the input–output method (IOM), satellite gravimetry, or via surface elevation change rates (d<i>H</i>/d<i>t</i>). Whereas the first two have been shown to agree well in reconstructing ice-sheet wide mass changes over...
| Main Authors: | , , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2014-09-01
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| Series: | The Cryosphere |
| Online Access: | http://www.the-cryosphere.net/8/1725/2014/tc-8-1725-2014.pdf |