Glacial isostatic contributions to present day sea level change around Greenland
Present-day sea-level change around Greenland is examined by assessing the roleplayed by glacial-isostatic adjustment (GIA). We consider the contributions from: (1) the ongoing GIA due to changes in the extent and thickness of the Greenland Ice Sheet (GIS) following the Last Glacial Maximum (LGM), (...
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| Format: | Text |
| Language: | English |
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GFZ, Helmholtz-Zentrum
2005
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| Online Access: | https://dx.doi.org/10.23689/fidgeo-572 https://e-docs.geo-leo.de/handle/11858/00-1735-0000-0001-32CD-E |