Institut de Ciències del Mar (ICM), Pg. Marítim de la Barceloneta, 37, Ciutat Vella, 08003 Barcelona, Catalonia, Spain
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Total article views: 4,722 (including HTML, PDF, and XML)
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4,600
68
54
4,722
46
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48
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PDF: 68
XML: 54
Total: 4,722
Supplement: 46
BibTeX: 51
EndNote: 48
Views and downloads (calculated since 25 Jun 2025)
Cumulative views and downloads
(calculated since 25 Jun 2025)
Total article views: 198 (including HTML, PDF, and XML)
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102
68
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198
46
51
48
HTML: 102
PDF: 68
XML: 28
Total: 198
Supplement: 46
BibTeX: 51
EndNote: 48
Views and downloads (calculated since 22 Jun 2026)
Cumulative views and downloads
(calculated since 22 Jun 2026)
Total article views: 4,524 (including HTML, PDF, and XML)
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4,498
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26
4,524
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Total: 4,524
BibTeX: 0
EndNote: 0
Views and downloads (calculated since 25 Jun 2025)
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: 4,722 (including HTML, PDF, and XML)
Thereof 4,653 with geography defined
and 69 with unknown origin.
Total article views: 198 (including HTML, PDF, and XML)
Thereof 152 with geography defined
and 46 with unknown origin.
Total article views: 4,524 (including HTML, PDF, and XML)
Thereof 4,501 with geography defined
and 23 with unknown origin.
We use a biogeochemical model to examine how particulate organic carbon (POC) is produced, transformed and transported to the deep ocean. Vertical flux attenuation arises from several interacting processes: export pathways, particle lability, temperature-dependent degradation, and zooplankton transformations, leading to strongest attenuation in the most productive region. Together with extensive comparison to observations, such a budgeting approach can help constrain model projections.
We use a biogeochemical model to examine how particulate organic carbon (POC) is produced,...