Deglaciation-induced spatially variable sea level change: a simple-model case study for the Greenland and Antarctic ice sheets
Some studies on deglaciation-induced sea-level change provide only a global average change, thus neglecting the fact that sea-level change is spatially variable. This is due mainly to the gravitational and visco-elastic feedback effects of the changing surface mass loads. In order to redress this...
| Main Authors: | , , , |
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| Format: | Journal Article |
| Published: |
Multi-Science Publishing
2010
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| Subjects: | |
| Online Access: | http://hdl.handle.net/20.500.11937/35151 |