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: 5,597 (including HTML, PDF, and XML)
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4,970
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5,597
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250
HTML: 4,970
PDF: 363
XML: 264
Total: 5,597
Supplement: 306
BibTeX: 367
EndNote: 250
Views and downloads (calculated since 25 Jun 2025)
Cumulative views and downloads
(calculated since 25 Jun 2025)
Total article views: 1,009 (including HTML, PDF, and XML)
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408
363
238
1,009
306
367
250
HTML: 408
PDF: 363
XML: 238
Total: 1,009
Supplement: 306
BibTeX: 367
EndNote: 250
Views and downloads (calculated since 22 Jun 2026)
Cumulative views and downloads
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Total article views: 4,588 (including HTML, PDF, and XML)
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4,562
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26
4,588
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Total: 4,588
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: 5,597 (including HTML, PDF, and XML)
Thereof 5,516 with geography defined
and 81 with unknown origin.
Total article views: 1,009 (including HTML, PDF, and XML)
Thereof 951 with geography defined
and 58 with unknown origin.
Total article views: 4,588 (including HTML, PDF, and XML)
Thereof 4,565 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,...