Observation-Based Trends of the Southern Ocean Carbon Sink

International audience The Southern Ocean (SO) carbon sink has strengthened substantially since the year 2000, following a decade of a weakening trend. However, the surface ocean pCO 2 data underlying this trend reversal are sparse, requiring a substantial amount of extrapolation to map the data. He...

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Published in:Geophysical Research Letters
Main Authors: Ritter, R., Landschutzer, P., Gruber, N., Fay, A., Iida, Y., Jones, S., Nakaoka, S., Park, G.-H., Peylin, Philippe, Rodenbeck, C., Rodgers, K., Shutler, J., Zeng, J.
Other Authors: Institute of Biogeochemistry and Pollutant Dynamics ETH Zürich (IBP), Department of Environmental Systems Science ETH Zürich (D-USYS), Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)- Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich), Japan Meteorological Agency (JMA), National Institute for Environmental Studies (NIES), Chemistry Department Massachusetts Institute of Technology, Massachusetts Institute of Technology (MIT), Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Modélisation des Surfaces et Interfaces Continentales (MOSAIC), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Max-Planck-Institut für Biogeochemie (MPI-BGC), Dept. Chemistry, North Dakota, North Dakota State University (NDSU), University of Exeter
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2017
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-02398303
https://hal.archives-ouvertes.fr/hal-02398303/document
https://hal.archives-ouvertes.fr/hal-02398303/file/2017GL074837.pdf
https://doi.org/10.1002/2017GL074837
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language English
topic [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDE.MCG]Environmental Sciences/Global Changes
spellingShingle [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDE.MCG]Environmental Sciences/Global Changes
Ritter, R.
Landschutzer, P.
Gruber, N.
Fay, A.
Iida, Y.
Jones, S.
Nakaoka, S.
Park, G.-H.
Peylin, Philippe
Rodenbeck, C.
Rodgers, K.,
Shutler, J.
Zeng, J.
Observation-Based Trends of the Southern Ocean Carbon Sink
topic_facet [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDE.MCG]Environmental Sciences/Global Changes
description International audience The Southern Ocean (SO) carbon sink has strengthened substantially since the year 2000, following a decade of a weakening trend. However, the surface ocean pCO 2 data underlying this trend reversal are sparse, requiring a substantial amount of extrapolation to map the data. Here we use nine different pCO 2 mapping products to investigate the SO trends and their sensitivity to the mapping procedure. We find a robust temporal coherence for the entire SO, with eight of the nine products agreeing on the sign of the decadal trends, that is, a weakening CO 2 sink trend in the 1990s (on average 0.22 ± 0.24 pg C yr −1 decade −1), and a strengthening sink trend during the 2000s (−0.35 ± 0.23 pg C yr −1 decade −1). Spatially, the multiproduct mean reveals rather uniform trends, but the confidence is limited, given the small number of statistically significant trends from the individual products, particularly during the data-sparse 1990-1999 period. Plain Language Summary The Southern Ocean plays an important role in regulating Earth's climate as it takes up a substantial amount of carbon dioxide from the atmosphere, thereby limiting the effect of global warming. However, this part of the global ocean is also the least well observed and observational data are sparse. Therefore, to study Southern Ocean carbon uptake, data interpolation methods are used to estimate the variability of the carbon uptake from the few existing observations. This poses the question on how reliable these estimates are. The Surface Ocean CO 2 Mapping intercomparison project aims to do exactly that, that is, test how reliable current estimates are by comparing results from different methods. Here we compare the results from nine data interpolation methods in the Southern Ocean from 1990 to 2010 and find a broad and encouraging agreement regarding decadal carbon uptake signals, whereas a spatially more refined analysis reveals much less agreement locally, illustrating the need to continue the measurement effort in the ...
author2 Institute of Biogeochemistry and Pollutant Dynamics ETH Zürich (IBP)
Department of Environmental Systems Science ETH Zürich (D-USYS)
Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)- Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)
Japan Meteorological Agency (JMA)
National Institute for Environmental Studies (NIES)
Chemistry Department Massachusetts Institute of Technology
Massachusetts Institute of Technology (MIT)
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Modélisation des Surfaces et Interfaces Continentales (MOSAIC)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Max-Planck-Institut für Biogeochemie (MPI-BGC)
Dept. Chemistry, North Dakota
North Dakota State University (NDSU)
University of Exeter
format Article in Journal/Newspaper
author Ritter, R.
Landschutzer, P.
Gruber, N.
Fay, A.
Iida, Y.
Jones, S.
Nakaoka, S.
Park, G.-H.
Peylin, Philippe
Rodenbeck, C.
Rodgers, K.,
Shutler, J.
Zeng, J.
author_facet Ritter, R.
Landschutzer, P.
Gruber, N.
Fay, A.
Iida, Y.
Jones, S.
Nakaoka, S.
Park, G.-H.
Peylin, Philippe
Rodenbeck, C.
Rodgers, K.,
Shutler, J.
Zeng, J.
author_sort Ritter, R.
title Observation-Based Trends of the Southern Ocean Carbon Sink
title_short Observation-Based Trends of the Southern Ocean Carbon Sink
title_full Observation-Based Trends of the Southern Ocean Carbon Sink
title_fullStr Observation-Based Trends of the Southern Ocean Carbon Sink
title_full_unstemmed Observation-Based Trends of the Southern Ocean Carbon Sink
title_sort observation-based trends of the southern ocean carbon sink
publisher HAL CCSD
publishDate 2017
url https://hal.archives-ouvertes.fr/hal-02398303
https://hal.archives-ouvertes.fr/hal-02398303/document
https://hal.archives-ouvertes.fr/hal-02398303/file/2017GL074837.pdf
https://doi.org/10.1002/2017GL074837
geographic Southern Ocean
geographic_facet Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source ISSN: 0094-8276
EISSN: 1944-8007
Geophysical Research Letters
https://hal.archives-ouvertes.fr/hal-02398303
Geophysical Research Letters, American Geophysical Union, 2017, 44 (24), pp.12,339-12,348. ⟨10.1002/2017GL074837⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1002/2017GL074837
hal-02398303
https://hal.archives-ouvertes.fr/hal-02398303
https://hal.archives-ouvertes.fr/hal-02398303/document
https://hal.archives-ouvertes.fr/hal-02398303/file/2017GL074837.pdf
doi:10.1002/2017GL074837
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1002/2017GL074837
container_title Geophysical Research Letters
container_volume 44
container_issue 24
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spelling ftccsdartic:oai:HAL:hal-02398303v1 2023-05-15T18:24:39+02:00 Observation-Based Trends of the Southern Ocean Carbon Sink Ritter, R. Landschutzer, P. Gruber, N. Fay, A. Iida, Y. Jones, S. Nakaoka, S. Park, G.-H. Peylin, Philippe Rodenbeck, C. Rodgers, K., Shutler, J. Zeng, J. Institute of Biogeochemistry and Pollutant Dynamics ETH Zürich (IBP) Department of Environmental Systems Science ETH Zürich (D-USYS) Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)- Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich) Japan Meteorological Agency (JMA) National Institute for Environmental Studies (NIES) Chemistry Department Massachusetts Institute of Technology Massachusetts Institute of Technology (MIT) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Modélisation des Surfaces et Interfaces Continentales (MOSAIC) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Max-Planck-Institut für Biogeochemie (MPI-BGC) Dept. Chemistry, North Dakota North Dakota State University (NDSU) University of Exeter 2017-12-28 https://hal.archives-ouvertes.fr/hal-02398303 https://hal.archives-ouvertes.fr/hal-02398303/document https://hal.archives-ouvertes.fr/hal-02398303/file/2017GL074837.pdf https://doi.org/10.1002/2017GL074837 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1002/2017GL074837 hal-02398303 https://hal.archives-ouvertes.fr/hal-02398303 https://hal.archives-ouvertes.fr/hal-02398303/document https://hal.archives-ouvertes.fr/hal-02398303/file/2017GL074837.pdf doi:10.1002/2017GL074837 info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.archives-ouvertes.fr/hal-02398303 Geophysical Research Letters, American Geophysical Union, 2017, 44 (24), pp.12,339-12,348. ⟨10.1002/2017GL074837⟩ [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2017 ftccsdartic https://doi.org/10.1002/2017GL074837 2021-12-19T00:55:22Z International audience The Southern Ocean (SO) carbon sink has strengthened substantially since the year 2000, following a decade of a weakening trend. However, the surface ocean pCO 2 data underlying this trend reversal are sparse, requiring a substantial amount of extrapolation to map the data. Here we use nine different pCO 2 mapping products to investigate the SO trends and their sensitivity to the mapping procedure. We find a robust temporal coherence for the entire SO, with eight of the nine products agreeing on the sign of the decadal trends, that is, a weakening CO 2 sink trend in the 1990s (on average 0.22 ± 0.24 pg C yr −1 decade −1), and a strengthening sink trend during the 2000s (−0.35 ± 0.23 pg C yr −1 decade −1). Spatially, the multiproduct mean reveals rather uniform trends, but the confidence is limited, given the small number of statistically significant trends from the individual products, particularly during the data-sparse 1990-1999 period. Plain Language Summary The Southern Ocean plays an important role in regulating Earth's climate as it takes up a substantial amount of carbon dioxide from the atmosphere, thereby limiting the effect of global warming. However, this part of the global ocean is also the least well observed and observational data are sparse. Therefore, to study Southern Ocean carbon uptake, data interpolation methods are used to estimate the variability of the carbon uptake from the few existing observations. This poses the question on how reliable these estimates are. The Surface Ocean CO 2 Mapping intercomparison project aims to do exactly that, that is, test how reliable current estimates are by comparing results from different methods. Here we compare the results from nine data interpolation methods in the Southern Ocean from 1990 to 2010 and find a broad and encouraging agreement regarding decadal carbon uptake signals, whereas a spatially more refined analysis reveals much less agreement locally, illustrating the need to continue the measurement effort in the ... Article in Journal/Newspaper Southern Ocean Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Southern Ocean Geophysical Research Letters 44 24