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: 1,939 (including HTML, PDF, and XML)
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1,685
190
64
1,939
99
161
HTML: 1,685
PDF: 190
XML: 64
Total: 1,939
BibTeX: 99
EndNote: 161
Views and downloads (calculated since 17 Apr 2024)
Cumulative views and downloads
(calculated since 17 Apr 2024)
Total article views: 1,514 (including HTML, PDF, and XML)
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1,268
190
56
1,514
99
161
HTML: 1,268
PDF: 190
XML: 56
Total: 1,514
BibTeX: 99
EndNote: 161
Views and downloads (calculated since 19 Jun 2025)
Cumulative views and downloads
(calculated since 19 Jun 2025)
Total article views: 425 (including HTML, PDF, and XML)
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417
0
8
425
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0
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Total: 425
BibTeX: 0
EndNote: 0
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: 1,939 (including HTML, PDF, and XML)
Thereof 1,905 with geography defined
and 34 with unknown origin.
Total article views: 1,514 (including HTML, PDF, and XML)
Thereof 1,483 with geography defined
and 31 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...