Articles | Volume 17, issue 11
https://doi.org/10.5194/se-17-1271-2026
https://doi.org/10.5194/se-17-1271-2026
Review article
 | Highlight paper
 | 
13 Nov 2026
Review article | Highlight paper |  | 13 Nov 2026

Solid-Earth geophysics and geodesy in Antarctica: achievements, current capabilities, and future directions

Mirko Scheinert, Weisen Shen, Richard C. Aster, Lambert Caron, Michael D. Hartinger, Matt A. King, Andrew Lloyd, Anya M. Reading, J. Paul Winberry, Terry Wilson, Lucilla Alfonsi, Michael J. Bentley, Eric Buchta, Thomas Y. Chen, Peter J. Clarke, Jörg Ebbing, Olaf Eisen, Natalya Gomez, Esra Günaydın, Samantha Hansen, Erik R. Ivins, Achraf Koulali, Grace A. Nield, Frederick Richards, M. Oğuz Selbesoğlu, Stephanie Sherman, Pippa L. Whitehouse, and Matthias Willen

Viewed

Total article views: 4,524 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,427 1,968 129 4,524 156 232
  • HTML: 2,427
  • PDF: 1,968
  • XML: 129
  • Total: 4,524
  • BibTeX: 156
  • EndNote: 232
Views and downloads (calculated since 23 Feb 2026)
Cumulative views and downloads (calculated since 23 Feb 2026)

Viewed (geographical distribution)

Total article views: 4,524 (including HTML, PDF, and XML) Thereof 4,459 with geography defined and 65 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Nov 2026
Download
Editorial statement
This paper provides a timely, state-of-the-art overview of geophysical measurements in Antarctica assembled by a broad community of Antarctic scientists, advancing our understanding of solid-Earth processes and their impact on the cryosphere. The societal relevance of Antarctic observations is profound: the ongoing mass loss of the Antarctic Ice Sheet contributes to global-mean sea-level rise at 0.4 mm/yr. To generate reliable sea-level projections for the future, reviews like this manuscript are essential. The authors make a case for science-driven, multidisciplinary geophysical observations in combination with improved modelling in order to develop precise and reliable projections for Antarctica’s future mass change and associated contribution to sea-level change at both regional and global scales.
Short summary
With an ongoing mass loss the Antarctic Ice Sheet contributes to global-mean sea level rise at a rate of 0.4 mm/a. Thus, it plays a key role in global climate and provides a natural laboratory to study processes that interlink cryosphere, solid Earth, atmosphere and ocean. We discuss how geodetic-geophysical networks in Antarctica were used to significantly advance our understanding of these processes, and how they should be maintained and extended to answer key science questions in the future.
Share
Altmetrics
Final-revised paper
Preprint