Globally consistent estimates of high-resolution Antarctic ice mass balance and spatially resolved glacial isostatic adjustment

<p>A detailed understanding of how the Antarctic ice sheet (AIS) responds to a warming climate is needed because it will most likely increase the rate of global mean sea level rise. Time-variable satellite gravimetry, realized by the Gravity Recovery and Climate Experiment (GRACE) and Gravity...

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Bibliographic Details
Main Authors: M. O. Willen, M. Horwath, E. Buchta, M. Scheinert, V. Helm, B. Uebbing, J. Kusche
Format: Article
Language:English
Published: Copernicus Publications 2024-02-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/18/775/2024/tc-18-775-2024.pdf