Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, Canada
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Total article views: 1,283 (including HTML, PDF, and XML)
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1,218
40
25
1,283
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11
HTML: 1,218
PDF: 40
XML: 25
Total: 1,283
Supplement: 17
BibTeX: 14
EndNote: 11
Views and downloads (calculated since 07 Jan 2026)
Cumulative views and downloads
(calculated since 07 Jan 2026)
Total article views: 164 (including HTML, PDF, and XML)
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113
40
11
164
17
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11
HTML: 113
PDF: 40
XML: 11
Total: 164
Supplement: 17
BibTeX: 14
EndNote: 11
Views and downloads (calculated since 02 Sep 2026)
Cumulative views and downloads
(calculated since 02 Sep 2026)
Total article views: 1,119 (including HTML, PDF, and XML)
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1,105
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14
1,119
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HTML: 1,105
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XML: 14
Total: 1,119
BibTeX: 0
EndNote: 0
Views and downloads (calculated since 07 Jan 2026)
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: 1,283 (including HTML, PDF, and XML)
Thereof 1,275 with geography defined
and 8 with unknown origin.
Total article views: 164 (including HTML, PDF, and XML)
Thereof 164 with geography defined
and 0 with unknown origin.
Total article views: 1,119 (including HTML, PDF, and XML)
Thereof 1,111 with geography defined
and 8 with unknown origin.
The ocean mixed layer needs to be correctly represented in climate models to provide reliable future projections. We evaluate the mixed layer depth in 15 climate models against reconstructions for the mid-Holocene North Atlantic. The lack of meltwater input to models causes the simulated mixed layer to be deeper than reconstructed in the Labrador Sea but does not affect the Nordic Seas. Deep ocean mixing in the Labrador Sea may be particularly sensitive to ice-sheet melting under global warming.
The ocean mixed layer needs to be correctly represented in climate models to provide reliable...