University of Waterloo, Department of Applied Mathematics, 200 University Ave W, Waterloo, ON N2L 3G1, Canada
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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: 1,613 (including HTML, PDF, and XML)
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1,497
66
50
1,613
31
22
18
HTML: 1,497
PDF: 66
XML: 50
Total: 1,613
Supplement: 31
BibTeX: 22
EndNote: 18
Views and downloads (calculated since 08 Dec 2025)
Cumulative views and downloads
(calculated since 08 Dec 2025)
Total article views: 283 (including HTML, PDF, and XML)
HTML
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Total
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BibTeX
EndNote
199
66
18
283
31
22
18
HTML: 199
PDF: 66
XML: 18
Total: 283
Supplement: 31
BibTeX: 22
EndNote: 18
Views and downloads (calculated since 26 Aug 2026)
Cumulative views and downloads
(calculated since 26 Aug 2026)
Total article views: 1,330 (including HTML, PDF, and XML)
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1,298
0
32
1,330
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0
HTML: 1,298
PDF: 0
XML: 32
Total: 1,330
BibTeX: 0
EndNote: 0
Views and downloads (calculated since 08 Dec 2025)
Cumulative views and downloads
(calculated since 08 Dec 2025)
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: 1,613 (including HTML, PDF, and XML)
Thereof 1,595 with geography defined
and 18 with unknown origin.
Total article views: 283 (including HTML, PDF, and XML)
Thereof 283 with geography defined
and 0 with unknown origin.
Total article views: 1,330 (including HTML, PDF, and XML)
Thereof 1,312 with geography defined
and 18 with unknown origin.
When sea ice moves along the ocean surface, it can generate waves below the ocean surface. Because these processes occur at spatial and temporal scales smaller than those captured by climate models, they need to be approximated. Here, we (1) find the relevant value ranges and spatial distributions of the parameters that describe this problem to improve this approximation and (2) examine the wave generation and turbulence using numerical experiments for a selected set of parameter values.
When sea ice moves along the ocean surface, it can generate waves below the ocean surface....