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: 3,792 (including HTML, PDF, and XML)
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3,364
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3,792
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HTML: 3,364
PDF: 317
XML: 111
Total: 3,792
BibTeX: 126
EndNote: 204
Views and downloads (calculated since 17 Apr 2024)
Cumulative views and downloads
(calculated since 17 Apr 2024)
Total article views: 2,347 (including HTML, PDF, and XML)
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1,936
317
94
2,347
126
204
HTML: 1,936
PDF: 317
XML: 94
Total: 2,347
BibTeX: 126
EndNote: 204
Views and downloads (calculated since 19 Jun 2025)
Cumulative views and downloads
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Total article views: 1,445 (including HTML, PDF, and XML)
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1,428
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17
1,445
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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: 3,792 (including HTML, PDF, and XML)
Thereof 3,670 with geography defined
and 122 with unknown origin.
Total article views: 2,347 (including HTML, PDF, and XML)
Thereof 2,241 with geography defined
and 106 with unknown origin.
Total article views: 1,445 (including HTML, PDF, and XML)
Thereof 1,429 with geography defined
and 16 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...