Department of Physics, Institute for Marine and Atmospheric research Utrecht (IMAU), Utrecht University, Utrecht, the Netherlands
Centre for Complex Systems Studies, Utrecht University, Utrecht, the Netherlands
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: 796 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
784
6
6
796
3
0
0
HTML: 784
PDF: 6
XML: 6
Total: 796
Supplement: 3
BibTeX: 0
EndNote: 0
Views and downloads (calculated since 10 Apr 2025)
Cumulative views and downloads
(calculated since 10 Apr 2025)
Total article views: 55 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
47
6
2
55
3
0
0
HTML: 47
PDF: 6
XML: 2
Total: 55
Supplement: 3
BibTeX: 0
EndNote: 0
Views and downloads (calculated since 21 Oct 2025)
Cumulative views and downloads
(calculated since 21 Oct 2025)
Total article views: 741 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
737
0
4
741
0
0
HTML: 737
PDF: 0
XML: 4
Total: 741
BibTeX: 0
EndNote: 0
Views and downloads (calculated since 10 Apr 2025)
Cumulative views and downloads
(calculated since 10 Apr 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: 796 (including HTML, PDF, and XML)
Thereof 778 with geography defined
and 18 with unknown origin.
Total article views: 55 (including HTML, PDF, and XML)
Thereof 55 with geography defined
and 0 with unknown origin.
Total article views: 741 (including HTML, PDF, and XML)
Thereof 723 with geography defined
and 18 with unknown origin.
The subpolar gyre is a wind-driven circulation in the North Atlantic Ocean that enables the mixing of water between the surface and deeper layers. We investigate the interactions between the strength of the gyre circulation, salinity, temperature, and mixing in climate models. We find that most models capture an increase in salinity or a decrease in temperature, leading to mixing. However, the feedback from the density in the gyre centre to the strength of its circulation is poorly represented.
The subpolar gyre is a wind-driven circulation in the North Atlantic Ocean that enables the...