Department of Earth Sciences, University of Oxford, South Parks Road, Oxford, OX1 3AN, UK
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Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 3,710 (including HTML, PDF, and XML)
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3,304
300
106
3,710
121
198
HTML: 3,304
PDF: 300
XML: 106
Total: 3,710
BibTeX: 121
EndNote: 198
Views and downloads (calculated since 17 Apr 2024)
Cumulative views and downloads
(calculated since 17 Apr 2024)
Total article views: 2,280 (including HTML, PDF, and XML)
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1,890
300
90
2,280
121
198
HTML: 1,890
PDF: 300
XML: 90
Total: 2,280
BibTeX: 121
EndNote: 198
Views and downloads (calculated since 19 Jun 2025)
Cumulative views and downloads
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Total article views: 1,430 (including HTML, PDF, and XML)
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1,414
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16
1,430
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Total: 1,430
BibTeX: 0
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Views and downloads (calculated since 17 Apr 2024)
Cumulative views and downloads
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Viewed (geographical distribution)
Since the preprint corresponding to this journal article was posted outside of Copernicus Publications, the preprint-related metrics are limited to HTML views.
Total article views: 3,710 (including HTML, PDF, and XML)
Thereof 3,605 with geography defined
and 105 with unknown origin.
Total article views: 2,280 (including HTML, PDF, and XML)
Thereof 2,188 with geography defined
and 92 with unknown origin.
Total article views: 1,430 (including HTML, PDF, and XML)
Thereof 1,417 with geography defined
and 13 with unknown origin.
In Antarctica, supraglacial lakes often form near grounding lines due to surface melting. We model viscoelastic tidal flexure in these regions to assess its contribution to lake drainage via hydrofracturing. Results show that tidal flexure and lake-water pressure jointly control drainage near unconfined grounding lines. Sensitivity analysis indicates the importance of the Maxwell time of ice in modulating the tidal response.
In Antarctica, supraglacial lakes often form near grounding lines due to surface melting. We...