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: 4,572 (including HTML, PDF, and XML)
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3,842
506
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4,572
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238
HTML: 3,842
PDF: 506
XML: 224
Total: 4,572
BibTeX: 223
EndNote: 238
Views and downloads (calculated since 17 Apr 2024)
Cumulative views and downloads
(calculated since 17 Apr 2024)
Total article views: 2,932 (including HTML, PDF, and XML)
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EndNote
2,220
506
206
2,932
223
238
HTML: 2,220
PDF: 506
XML: 206
Total: 2,932
BibTeX: 223
EndNote: 238
Views and downloads (calculated since 19 Jun 2025)
Cumulative views and downloads
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Total article views: 1,640 (including HTML, PDF, and XML)
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1,622
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18
1,640
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Total: 1,640
BibTeX: 0
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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: 4,572 (including HTML, PDF, and XML)
Thereof 4,421 with geography defined
and 151 with unknown origin.
Total article views: 2,932 (including HTML, PDF, and XML)
Thereof 2,797 with geography defined
and 135 with unknown origin.
Total article views: 1,640 (including HTML, PDF, and XML)
Thereof 1,624 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...