Regional glacial-isostatic adjustment in Antarctica inferred from combining space borne geodetic observations (ESA-STSE CryoSat + Project REGINA)
A major uncertainty in determining the mass balance of the Antarctic ice sheet from satellite gravimetry, and to a lesser extent altimetry, measurements is the poorly known correction for the glacial isostatic adjustment (GIA) of the solid Earth. Although much progress has been made in consistently...
Main Authors: | , , , , , , , , , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2016
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Subjects: | |
Online Access: | https://gfzpublic.gfz-potsdam.de/pubman/item/item_1503947 |