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: 4,196 (including HTML, PDF, and XML)
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3,635
422
139
4,196
150
219
HTML: 3,635
PDF: 422
XML: 139
Total: 4,196
BibTeX: 150
EndNote: 219
Views and downloads (calculated since 17 Apr 2024)
Cumulative views and downloads
(calculated since 17 Apr 2024)
Total article views: 2,627 (including HTML, PDF, and XML)
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2,083
422
122
2,627
150
219
HTML: 2,083
PDF: 422
XML: 122
Total: 2,627
BibTeX: 150
EndNote: 219
Views and downloads (calculated since 19 Jun 2025)
Cumulative views and downloads
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Total article views: 1,569 (including HTML, PDF, and XML)
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1,552
0
17
1,569
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HTML: 1,552
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XML: 17
Total: 1,569
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: 4,196 (including HTML, PDF, and XML)
Thereof 4,050 with geography defined
and 146 with unknown origin.
Total article views: 2,627 (including HTML, PDF, and XML)
Thereof 2,497 with geography defined
and 130 with unknown origin.
Total article views: 1,569 (including HTML, PDF, and XML)
Thereof 1,553 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...