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: 1,279 (including HTML, PDF, and XML)
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1,142
94
43
1,279
81
107
HTML: 1,142
PDF: 94
XML: 43
Total: 1,279
BibTeX: 81
EndNote: 107
Views and downloads (calculated since 17 Apr 2024)
Cumulative views and downloads
(calculated since 17 Apr 2024)
Total article views: 855 (including HTML, PDF, and XML)
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726
94
35
855
81
107
HTML: 726
PDF: 94
XML: 35
Total: 855
BibTeX: 81
EndNote: 107
Views and downloads (calculated since 19 Jun 2025)
Cumulative views and downloads
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Total article views: 424 (including HTML, PDF, and XML)
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416
0
8
424
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HTML: 416
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Total: 424
BibTeX: 0
EndNote: 0
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: 1,279 (including HTML, PDF, and XML)
Thereof 1,274 with geography defined
and 5 with unknown origin.
Total article views: 855 (including HTML, PDF, and XML)
Thereof 853 with geography defined
and 2 with unknown origin.
Total article views: 424 (including HTML, PDF, and XML)
Thereof 421 with geography defined
and 3 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...