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 address this ap...
Main Authors: | M. Kuhn, W.E. Featherstone, O. Makarynskyy, W. Keller |
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Format: | Article |
Language: | English |
Published: |
SAGE Publishing
2010-06-01
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Series: | International Journal of Ocean and Climate Systems |
Online Access: | https://doi.org/10.1260/1759-3131.1.2.67 |
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