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: 2,188 (including HTML, PDF, and XML)
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1,922
202
64
2,188
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167
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PDF: 202
XML: 64
Total: 2,188
BibTeX: 100
EndNote: 167
Views and downloads (calculated since 17 Apr 2024)
Cumulative views and downloads
(calculated since 17 Apr 2024)
Total article views: 1,763 (including HTML, PDF, and XML)
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1,505
202
56
1,763
100
167
HTML: 1,505
PDF: 202
XML: 56
Total: 1,763
BibTeX: 100
EndNote: 167
Views and downloads (calculated since 19 Jun 2025)
Cumulative views and downloads
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Total article views: 425 (including HTML, PDF, and XML)
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417
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8
425
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Views and downloads (calculated since 17 Apr 2024)
Cumulative views and downloads
(calculated since 17 Apr 2024)
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: 2,188 (including HTML, PDF, and XML)
Thereof 2,140 with geography defined
and 48 with unknown origin.
Total article views: 1,763 (including HTML, PDF, and XML)
Thereof 1,718 with geography defined
and 45 with unknown origin.
Total article views: 425 (including HTML, PDF, and XML)
Thereof 422 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...