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: 5,372 (including HTML, PDF, and XML)
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4,863
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5,372
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191
HTML: 4,863
PDF: 308
XML: 201
Total: 5,372
Supplement: 213
BibTeX: 283
EndNote: 191
Views and downloads (calculated since 25 Jun 2025)
Cumulative views and downloads
(calculated since 25 Jun 2025)
Total article views: 798 (including HTML, PDF, and XML)
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315
308
175
798
213
283
191
HTML: 315
PDF: 308
XML: 175
Total: 798
Supplement: 213
BibTeX: 283
EndNote: 191
Views and downloads (calculated since 22 Jun 2026)
Cumulative views and downloads
(calculated since 22 Jun 2026)
Total article views: 4,574 (including HTML, PDF, and XML)
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4,548
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26
4,574
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Total: 4,574
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: 5,372 (including HTML, PDF, and XML)
Thereof 5,291 with geography defined
and 81 with unknown origin.
Total article views: 798 (including HTML, PDF, and XML)
Thereof 740 with geography defined
and 58 with unknown origin.
Total article views: 4,574 (including HTML, PDF, and XML)
Thereof 4,551 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,...