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: 2,369 (including HTML, PDF, and XML)
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2,035
255
79
2,369
105
176
HTML: 2,035
PDF: 255
XML: 79
Total: 2,369
BibTeX: 105
EndNote: 176
Views and downloads (calculated since 17 Apr 2024)
Cumulative views and downloads
(calculated since 17 Apr 2024)
Total article views: 1,943 (including HTML, PDF, and XML)
HTML
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XML
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BibTeX
EndNote
1,617
255
71
1,943
105
176
HTML: 1,617
PDF: 255
XML: 71
Total: 1,943
BibTeX: 105
EndNote: 176
Views and downloads (calculated since 19 Jun 2025)
Cumulative views and downloads
(calculated since 19 Jun 2025)
Total article views: 426 (including HTML, PDF, and XML)
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418
0
8
426
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0
HTML: 418
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Total: 426
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: 2,369 (including HTML, PDF, and XML)
Thereof 2,315 with geography defined
and 54 with unknown origin.
Total article views: 1,943 (including HTML, PDF, and XML)
Thereof 1,892 with geography defined
and 51 with unknown origin.
Total article views: 426 (including HTML, PDF, and XML)
Thereof 423 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...