Effect of GIA models with 3D composite mantle viscosity on GRACE mass balance estimates for Antarctica
Abstract
Seismic data indicate that there are large viscosity variations in the mantle beneath Antarctica. Consideration of such variations would affect predictions of models of Glacial Isostatic Adjustment (GIA), which are used to correct satellite measurements of ice mass change. However, most GIA models used for that purpose have assumed the mantle to be uniformly stratified in terms of viscosity. The goal of this study is to estimate the effect of...
Paper Details
Title
Effect of GIA models with 3D composite mantle viscosity on GRACE mass balance estimates for Antarctica
Published Date
Mar 1, 2015
Volume
414
Pages
134 - 143
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