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...
Huvudupphovsmän: | M. O. Willen, M. Horwath, E. Buchta, M. Scheinert, V. Helm, B. Uebbing, J. Kusche |
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Materialtyp: | Artikel |
Språk: | English |
Publicerad: |
Copernicus Publications
2024-02-01
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Serie: | The Cryosphere |
Länkar: | https://tc.copernicus.org/articles/18/775/2024/tc-18-775-2024.pdf |
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