University of Waterloo, Department of Applied Mathematics, 200 University Ave W, Waterloo, ON N2L 3G1, Canada
Viewed
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: 1,857 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,699
96
62
1,857
48
38
33
HTML: 1,699
PDF: 96
XML: 62
Total: 1,857
Supplement: 48
BibTeX: 38
EndNote: 33
Views and downloads (calculated since 08 Dec 2025)
Cumulative views and downloads
(calculated since 08 Dec 2025)
Total article views: 481 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
355
96
30
481
48
38
33
HTML: 355
PDF: 96
XML: 30
Total: 481
Supplement: 48
BibTeX: 38
EndNote: 33
Views and downloads (calculated since 26 Aug 2026)
Cumulative views and downloads
(calculated since 26 Aug 2026)
Total article views: 1,376 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,344
0
32
1,376
0
0
HTML: 1,344
PDF: 0
XML: 32
Total: 1,376
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: 1,857 (including HTML, PDF, and XML)
Thereof 1,839 with geography defined
and 18 with unknown origin.
Total article views: 481 (including HTML, PDF, and XML)
Thereof 481 with geography defined
and 0 with unknown origin.
Total article views: 1,376 (including HTML, PDF, and XML)
Thereof 1,358 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....