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1000 Titel
  • Globally consistent estimates of high-resolution Antarctic ice mass balance and spatially resolved glacial isostatic adjustment
1000 Autor/in
  1. Willen, Matthias O. |
  2. Horwath, Martin |
  3. Buchta, Eric |
  4. Scheinert, Mirko |
  5. Helm, Veit |
  6. Uebbing, Bernd |
  7. Kusche, Jürgen |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-02-20
1000 Erschienen in
1000 Quellenangabe
  • 18(2):775-790
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/tc-18-775-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. 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 Recovery and Climate Experiment Follow-On (GRACE-FO) missions, is directly sensitive to AIS mass changes. However, gravimetric mass balances are subject to two major limitations. First, the usual correction of the glacial isostatic adjustment (GIA) effect by modelling results is a dominant source of uncertainty. Second, satellite gravimetry allows for a resolution of a few hundred kilometres only, which is insufficient to thoroughly explore causes of AIS imbalance. We have overcome both limitations by the first global inversion of data from GRACE and GRACE-FO, satellite altimetry (CryoSat-2), regional climate modelling (RACMO2), and firn densification modelling (IMAU-FDM). The inversion spatially resolves GIA in Antarctica independently from GIA modelling jointly with changes of ice mass and firn air content at 50 km resolution. We find an AIS mass balance of −144 ± 27 Gt a−1 from January 2011 to December 2020. This estimate is the same, within uncertainties, as the statistical analysis of 23 different mass balances evaluated in the Ice sheet Mass Balance Inter-comparison Exercise (IMBIE; Otosaka et al., 2023b). The co-estimated GIA corresponds to an integrated mass effect of 86 ± 21 Gt a−1 over Antarctica, and it fits better with global navigation satellite system (GNSS) results than other GIA predictions. From propagating covariances to integrals, we find a correlation coefficient of −0.97 between the AIS mass balance and the GIA estimate. Sensitivity tests with alternative input data sets lead to results within assessed uncertainties. </jats:p>
1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/uri/V2lsbGVuLCBNYXR0aGlhc8KgTy4=|https://frl.publisso.de/adhoc/uri/SG9yd2F0aCwgTWFydGlu|https://frl.publisso.de/adhoc/uri/QnVjaHRhLCBFcmlj|https://frl.publisso.de/adhoc/uri/U2NoZWluZXJ0LCBNaXJrbw==|https://frl.publisso.de/adhoc/uri/SGVsbSwgVmVpdA==|https://frl.publisso.de/adhoc/uri/VWViYmluZywgQmVybmQ=|https://frl.publisso.de/adhoc/uri/S3VzY2hlLCBKw7xyZ2Vu
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  1. Deutsche Forschungsgemeinschaft |
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    1000 Förderer Deutsche Forschungsgemeinschaft |
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1000 Erstellt am 2024-05-24T04:58:02.209+0200
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1000 Zuletzt bearbeitet 2024-05-27T11:01:59.984+0200
1000 Objekt bearb. Mon May 27 11:01:59 CEST 2024
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