Ocean carbon sink assessment via temperature and salinity data assimilation into a global ocean biogeochemistry model

Global ocean biogeochemistry models are frequently used to derive a comprehensive estimate of the global ocean carbon uptake. These models are designed to represent the most important processes of the ocean carbon cycle, but the idealized process representation and uncertainties in the initializatio...

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Published in:Ocean Science
Main Authors: Bunsen, Frauke, Hauck, Judith, Torres-valdes, Sinhue, Nerger, Lars
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Gesellschaft Mbh 2025
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00940/105216/118001.pdf
https://archimer.ifremer.fr/doc/00940/105216/118002.pdf
https://doi.org/10.5194/os-21-437-2025
https://archimer.ifremer.fr/doc/00940/105216/
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author Bunsen, Frauke
Hauck, Judith
Torres-valdes, Sinhue
Nerger, Lars
author_facet Bunsen, Frauke
Hauck, Judith
Torres-valdes, Sinhue
Nerger, Lars
author_sort Bunsen, Frauke
collection Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer)
container_issue 1
container_start_page 437
container_title Ocean Science
container_volume 21
description Global ocean biogeochemistry models are frequently used to derive a comprehensive estimate of the global ocean carbon uptake. These models are designed to represent the most important processes of the ocean carbon cycle, but the idealized process representation and uncertainties in the initialization of model variables lead to errors in their predictions. Here, observations of ocean physics (temperature and salinity) are assimilated into the ocean biogeochemistry model FESOM2.1-REcoM3 over the period 2010-2020 to study the effect on the air-sea carbon dioxide (CO2) flux and other biogeochemical (BGC) variables. The assimilation nearly halves the model-observation differences in sea surface temperature and salinity, with modest effects on the modeled ecosystem and CO2 fluxes. The main effects of the assimilation on the air-sea CO2 flux occur on small scales in highly dynamic regions, which pose challenges to ocean models. Its largest imprint is in the Southern Ocean during winter. South of 50 degrees S, winter CO2 outgassing is reduced; thus the regional CO2 uptake increases by 0.18 Pg C yr-1 through the assimilation. Other particularly strong regional effects on the air-sea CO2 flux are located in the area of the North Atlantic Current (NAC). However, the effect on the global ocean carbon uptake is a comparatively small increase by 0.05 Pg C yr-1 induced by the assimilation, yielding a global mean uptake of 2.78 Pg C yr-1 for the period 2010-2020.
format Article in Journal/Newspaper
genre north atlantic current
North Atlantic
Southern Ocean
genre_facet north atlantic current
North Atlantic
Southern Ocean
geographic Southern Ocean
geographic_facet Southern Ocean
id ftarchimer:oai:archimer.ifremer.fr:105216
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op_doi https://doi.org/10.5194/os-21-437-2025
op_relation https://archimer.ifremer.fr/doc/00940/105216/118001.pdf
https://archimer.ifremer.fr/doc/00940/105216/118002.pdf
https://archimer.ifremer.fr/doc/00940/105216/
op_rights info:eu-repo/semantics/openAccess
restricted use
op_source Ocean Science (1812-0784) (Copernicus Gesellschaft Mbh), 2025-02 , Vol. 21 , N. 1 , P. 437-471
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spelling ftarchimer:oai:archimer.ifremer.fr:105216 2025-04-06T14:59:23+00:00 Ocean carbon sink assessment via temperature and salinity data assimilation into a global ocean biogeochemistry model Bunsen, Frauke Hauck, Judith Torres-valdes, Sinhue Nerger, Lars 2025-02 application/pdf https://archimer.ifremer.fr/doc/00940/105216/118001.pdf https://archimer.ifremer.fr/doc/00940/105216/118002.pdf https://doi.org/10.5194/os-21-437-2025 https://archimer.ifremer.fr/doc/00940/105216/ eng eng Copernicus Gesellschaft Mbh https://archimer.ifremer.fr/doc/00940/105216/118001.pdf https://archimer.ifremer.fr/doc/00940/105216/118002.pdf https://archimer.ifremer.fr/doc/00940/105216/ info:eu-repo/semantics/openAccess restricted use Ocean Science (1812-0784) (Copernicus Gesellschaft Mbh), 2025-02 , Vol. 21 , N. 1 , P. 437-471 text Article info:eu-repo/semantics/article 2025 ftarchimer https://doi.org/10.5194/os-21-437-2025 2025-03-13T05:23:15Z Global ocean biogeochemistry models are frequently used to derive a comprehensive estimate of the global ocean carbon uptake. These models are designed to represent the most important processes of the ocean carbon cycle, but the idealized process representation and uncertainties in the initialization of model variables lead to errors in their predictions. Here, observations of ocean physics (temperature and salinity) are assimilated into the ocean biogeochemistry model FESOM2.1-REcoM3 over the period 2010-2020 to study the effect on the air-sea carbon dioxide (CO2) flux and other biogeochemical (BGC) variables. The assimilation nearly halves the model-observation differences in sea surface temperature and salinity, with modest effects on the modeled ecosystem and CO2 fluxes. The main effects of the assimilation on the air-sea CO2 flux occur on small scales in highly dynamic regions, which pose challenges to ocean models. Its largest imprint is in the Southern Ocean during winter. South of 50 degrees S, winter CO2 outgassing is reduced; thus the regional CO2 uptake increases by 0.18 Pg C yr-1 through the assimilation. Other particularly strong regional effects on the air-sea CO2 flux are located in the area of the North Atlantic Current (NAC). However, the effect on the global ocean carbon uptake is a comparatively small increase by 0.05 Pg C yr-1 induced by the assimilation, yielding a global mean uptake of 2.78 Pg C yr-1 for the period 2010-2020. Article in Journal/Newspaper north atlantic current North Atlantic Southern Ocean Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Southern Ocean Ocean Science 21 1 437 471
spellingShingle Bunsen, Frauke
Hauck, Judith
Torres-valdes, Sinhue
Nerger, Lars
Ocean carbon sink assessment via temperature and salinity data assimilation into a global ocean biogeochemistry model
title Ocean carbon sink assessment via temperature and salinity data assimilation into a global ocean biogeochemistry model
title_full Ocean carbon sink assessment via temperature and salinity data assimilation into a global ocean biogeochemistry model
title_fullStr Ocean carbon sink assessment via temperature and salinity data assimilation into a global ocean biogeochemistry model
title_full_unstemmed Ocean carbon sink assessment via temperature and salinity data assimilation into a global ocean biogeochemistry model
title_short Ocean carbon sink assessment via temperature and salinity data assimilation into a global ocean biogeochemistry model
title_sort ocean carbon sink assessment via temperature and salinity data assimilation into a global ocean biogeochemistry model
url https://archimer.ifremer.fr/doc/00940/105216/118001.pdf
https://archimer.ifremer.fr/doc/00940/105216/118002.pdf
https://doi.org/10.5194/os-21-437-2025
https://archimer.ifremer.fr/doc/00940/105216/