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)
The temporal variation of the carbonate system, air–sea CO 2 fluxes, and pH is analyzed in the southern Indian Ocean, south of the polar front, based on in situ data obtained from 1985 to 2021 at a fixed station (50°40 ′ S–68°25 ′ E) and results from a neural network model that reconstructs the fuga...
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Online Access: | https://doi.org/10.5194/os-20-725-2024 https://os.copernicus.org/articles/20/725/2024/ |
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ftcopernicus:oai:publications.copernicus.org:os115716 2024-09-15T18:37:25+00:00 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) Metzl, Nicolas Monaco, Claire Leseurre, Coraline Ridame, Céline Reverdin, Gilles Chau, Thi Tuyet Trang Chevallier, Frédéric Gehlen, Marion 2024-06-11 application/pdf https://doi.org/10.5194/os-20-725-2024 https://os.copernicus.org/articles/20/725/2024/ eng eng doi:10.5194/os-20-725-2024 https://os.copernicus.org/articles/20/725/2024/ eISSN: 1812-0792 Text 2024 ftcopernicus https://doi.org/10.5194/os-20-725-2024 2024-08-28T05:24:22Z The temporal variation of the carbonate system, air–sea CO 2 fluxes, and pH is analyzed in the southern Indian Ocean, south of the polar front, based on in situ data obtained from 1985 to 2021 at a fixed station (50°40 ′ S–68°25 ′ E) and results from a neural network model that reconstructs the fugacity of CO 2 ( f CO 2 ) and fluxes at monthly scale. Anthropogenic CO 2 (C ant ) is estimated in the water column and is detected down to the bottom (1600 m) in 1985, resulting in an aragonite saturation horizon at 600 m that migrated up to 400 m in 2021 due to the accumulation of C ant . At the subsurface, the trend of C ant is estimated at + 0.53 ± 0.01 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="64pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="0335676cdfde01c2427480e63a96dffe"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="os-20-725-2024-ie00001.svg" width="64pt" height="10pt" src="os-20-725-2024-ie00001.png"/> </svg:svg> µ mol kg −1 yr −1 with a detectable increase in the trend in recent years. At the surface during austral winter the oceanic f CO 2 increased at a rate close to or slightly lower than in the atmosphere. To the contrary, in summer, we observed contrasting f CO 2 and dissolved inorganic carbon (C T ) trends depending on the decade and emphasizing the role of biological drivers on air–sea CO 2 fluxes and pH inter-annual variability. The regional air–sea CO 2 fluxes evolved from an annual source to the atmosphere of 0.8 molC m −2 yr −1 in 1985 to a sink of −0.5 molC m −2 yr −1 in 2020. Over 1985–2020, the annual pH trend in surface waters of - 0.0165 ± 0.0040 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="88pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="f78ffdaaa34caa0f5eaa9c9ca35bfe50"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="os-20-725-2024-ie00002.svg" width="88pt" height="10pt" src="os-20-725-2024-ie00002.png"/> </svg:svg> per decade was mainly controlled by the ... Text Southern Ocean Copernicus Publications: E-Journals Ocean Science 20 3 725 758 |
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Open Polar |
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Copernicus Publications: E-Journals |
op_collection_id |
ftcopernicus |
language |
English |
description |
The temporal variation of the carbonate system, air–sea CO 2 fluxes, and pH is analyzed in the southern Indian Ocean, south of the polar front, based on in situ data obtained from 1985 to 2021 at a fixed station (50°40 ′ S–68°25 ′ E) and results from a neural network model that reconstructs the fugacity of CO 2 ( f CO 2 ) and fluxes at monthly scale. Anthropogenic CO 2 (C ant ) is estimated in the water column and is detected down to the bottom (1600 m) in 1985, resulting in an aragonite saturation horizon at 600 m that migrated up to 400 m in 2021 due to the accumulation of C ant . At the subsurface, the trend of C ant is estimated at + 0.53 ± 0.01 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="64pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="0335676cdfde01c2427480e63a96dffe"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="os-20-725-2024-ie00001.svg" width="64pt" height="10pt" src="os-20-725-2024-ie00001.png"/> </svg:svg> µ mol kg −1 yr −1 with a detectable increase in the trend in recent years. At the surface during austral winter the oceanic f CO 2 increased at a rate close to or slightly lower than in the atmosphere. To the contrary, in summer, we observed contrasting f CO 2 and dissolved inorganic carbon (C T ) trends depending on the decade and emphasizing the role of biological drivers on air–sea CO 2 fluxes and pH inter-annual variability. The regional air–sea CO 2 fluxes evolved from an annual source to the atmosphere of 0.8 molC m −2 yr −1 in 1985 to a sink of −0.5 molC m −2 yr −1 in 2020. Over 1985–2020, the annual pH trend in surface waters of - 0.0165 ± 0.0040 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="88pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="f78ffdaaa34caa0f5eaa9c9ca35bfe50"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="os-20-725-2024-ie00002.svg" width="88pt" height="10pt" src="os-20-725-2024-ie00002.png"/> </svg:svg> per decade was mainly controlled by the ... |
format |
Text |
author |
Metzl, Nicolas Monaco, Claire Leseurre, Coraline Ridame, Céline Reverdin, Gilles Chau, Thi Tuyet Trang Chevallier, Frédéric Gehlen, Marion |
spellingShingle |
Metzl, Nicolas Monaco, Claire Leseurre, Coraline Ridame, Céline Reverdin, Gilles Chau, Thi Tuyet Trang Chevallier, Frédéric Gehlen, Marion 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) |
author_facet |
Metzl, Nicolas Monaco, Claire Leseurre, Coraline Ridame, Céline Reverdin, Gilles Chau, Thi Tuyet Trang Chevallier, Frédéric Gehlen, Marion |
author_sort |
Metzl, Nicolas |
title |
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) |
title_short |
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) |
title_full |
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) |
title_fullStr |
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) |
title_full_unstemmed |
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) |
title_sort |
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) |
publishDate |
2024 |
url |
https://doi.org/10.5194/os-20-725-2024 https://os.copernicus.org/articles/20/725/2024/ |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
eISSN: 1812-0792 |
op_relation |
doi:10.5194/os-20-725-2024 https://os.copernicus.org/articles/20/725/2024/ |
op_doi |
https://doi.org/10.5194/os-20-725-2024 |
container_title |
Ocean Science |
container_volume |
20 |
container_issue |
3 |
container_start_page |
725 |
op_container_end_page |
758 |
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1810481798285623296 |