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...

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

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