Articles | Volume 20, issue 3
https://doi.org/10.5194/os-20-725-2024
https://doi.org/10.5194/os-20-725-2024
Research article
 | 
11 Jun 2024
Research article |  | 11 Jun 2024

Anthropogenic CO2, air–sea CO2 fluxes, and acidification in the Southern Ocean: results from a time-series analysis at station OISO-KERFIX (51° S–68° E)

Nicolas Metzl, Claire Lo Monaco, Coraline Leseurre, Céline Ridame, Gilles Reverdin, Thi Tuyet Trang Chau, Frédéric Chevallier, and Marion Gehlen

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Cited articles

Akhoudas, C. H., Sallée, J.-B., Reverdin, G., Haumann, F. A., Pauthenet, E., Chapman, C. C., Margirier, F., Lo Monaco, C., Metzl, N., Meilland, J., and Stranne, C.: Isotopic evidence for an intensified hydrological cycle in the Indian sector of the Southern Ocean, Nat. Commun., 14, 2763, https://doi.org/10.1038/s41467-023-38425-5, 2023. 
Aminot, A. and Kérouel, R.: Hydrologie des écosystèmes marins: paramètres et analyses, Ed. Ifremer, 336 pp., ISBN 2-84433-133-5, 2004. 
Akhoudas, C. H., Sallée, J.-B., Reverdin, G., Haumann, F. A., Pauthenet, E., Chapman, C. C., Margirier, F., Lo Monaco, C., Metzl, N., Meilland, J., and Stranne, C.: Isotopic evidence for an intensified hydrological cycle in the Indian sector of the Southern Ocean, Nat. Commun., 14, 2763, https://doi.org/10.1038/s41467-023-38425-5, 2023. 
Antonov, J. I., Locarnini, R. A., Boyer, T. P., Mishonov, A. V., and Garcia, H. E.: World Ocean Atlas 2005, in: Volume 2: Salinity, edited by: Levitus, S., NOAA Atlas NESDIS 62, US Government Printing Office, Washington, DC, 182 pp., https://repository.library.noaa.gov/view/noaa/1127 (last access: 15 January 2024), 2006. 
Arrigo, K. R., van Dijken, G. L., and Bushinsky, S.: Primary production in the Southern Ocean, 1997–2006, J. Geophys. Res.-Oceans, 113, C08004, https://doi.org/10.1029/2007jc004551, 2008. 
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In the southern Indian Ocean, south of the polar front, an observed increase of sea surface fCO2 and a decrease of pH over 1985–2021 are mainly driven by anthropogenic CO2 uptake, but in the last decade (2010–2020) fCO2 and pH were stable in summer, highlighting the competitive balance between anthropogenic CO2 and primary production. In the water column the increase of anthropogenic CO2 concentrations leads to migration of the aragonite saturation state from 600 m in 1985 up to 400 m in 2021.