Department of Earth Sciences, University of Oxford, South Parks Road, Oxford, OX1 3AN, UK
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Total article views: 3,629 (including HTML, PDF, and XML)
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3,228
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103
3,629
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HTML: 3,228
PDF: 298
XML: 103
Total: 3,629
BibTeX: 118
EndNote: 196
Views and downloads (calculated since 17 Apr 2024)
Cumulative views and downloads
(calculated since 17 Apr 2024)
Total article views: 2,205 (including HTML, PDF, and XML)
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1,820
298
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2,205
118
196
HTML: 1,820
PDF: 298
XML: 87
Total: 2,205
BibTeX: 118
EndNote: 196
Views and downloads (calculated since 19 Jun 2025)
Cumulative views and downloads
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Total article views: 1,424 (including HTML, PDF, and XML)
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1,408
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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: 3,629 (including HTML, PDF, and XML)
Thereof 3,571 with geography defined
and 58 with unknown origin.
Total article views: 2,205 (including HTML, PDF, and XML)
Thereof 2,155 with geography defined
and 50 with unknown origin.
Total article views: 1,424 (including HTML, PDF, and XML)
Thereof 1,416 with geography defined
and 8 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...