Sea-air CO 2 fluxes in the Southern Ocean for the period 1990-2009
International audience The Southern Ocean (44-75° S) plays a critical role in the global carbon cycle, yet remains one of the most poorly sampled ocean regions. Different approaches have been used to estimate sea-air CO 2 fluxes in this region: synthesis of surface ocean observations, ocean biogeoch...
Published in: | Biogeosciences |
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Main Authors: | , , , , , , , , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2013
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Subjects: | |
Online Access: | https://hal.science/hal-00873441 https://hal.science/hal-00873441/document https://hal.science/hal-00873441/file/bg-10-4037-2013.pdf https://doi.org/10.5194/BG-10-4037-2013 |
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ftepunivpsaclay:oai:HAL:hal-00873441v1 |
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openpolar |
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Open Polar |
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École Polytechnique, Université Paris-Saclay: HAL |
op_collection_id |
ftepunivpsaclay |
language |
English |
topic |
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes Lenton, Andrew Tilbrook, Bronte Law, R. M. Bakker, Dorothee C. E. Doney, Scott C. Gruber, Nicolas Ishii, Masao Hoppema, Mario Lovenduski, N. S. Matear, Richard J. Mcneil, B. I. Metzl, Nicolas Mikaloff Fletcher, S. E. Monteiro, Pedro M. S. Rödenbeck, Christian Sweeney, Colm Takahashi, Taro Sea-air CO 2 fluxes in the Southern Ocean for the period 1990-2009 |
topic_facet |
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience The Southern Ocean (44-75° S) plays a critical role in the global carbon cycle, yet remains one of the most poorly sampled ocean regions. Different approaches have been used to estimate sea-air CO 2 fluxes in this region: synthesis of surface ocean observations, ocean biogeochemical models, and atmospheric and ocean inversions. As part of the RECCAP (REgional Carbon Cycle Assessment and Processes) project, we combine these different approaches to quantify and assess the magnitude and variability in Southern Ocean sea-air CO 2 fluxes between 1990-2009. Using all models and inversions (26), the integrated median annual sea-air CO 2 flux of -0.42 ± 0.07 Pg C yr -1 for the 44-75° S region, is consistent with the -0.27 ± 0.13 Pg C yr -1 calculated using surface observations. The circumpolar region south of 58° S has a small net annual flux (model and inversion median: -0.04 ± 0.07 Pg C yr -1 and observations: +0.04 ± 0.02 Pg C yr -1 ), with most of the net annual flux located in the 44 to 58° S circumpolar band (model and inversion median: -0.36 ± 0.09 Pg C yr -1 and observations: -0.35 ± 0.09 Pg C yr -1 ). Seasonally, in the 44-58° S region, the median of 5 ocean biogeochemical models captures the observed sea-air CO 2 flux seasonal cycle, while the median of 11 atmospheric inversions shows little seasonal change in the net flux. South of 58° S, neither atmospheric inversions nor ocean biogeochemical models reproduce the phase and amplitude of the observed seasonal sea-air CO 2 flux, particularly in the Austral Winter. Importantly, no individual atmospheric inversion or ocean biogeochemical model is capable of reproducing both the observed annual mean uptake and the observed seasonal cycle. This raises concerns about projecting future changes in Southern Ocean CO 2 fluxes. The median interannual variability from atmospheric inversions and ocean biogeochemical models is substantial in the Southern Ocean; up to 25% of the annual mean flux, with 25% of this interannual variability attributed to ... |
author2 |
CSIRO Marine and Atmospheric Research Hobart, Castray Esplanade, Hobart Tasmani 7000, Australia Antarctic Climate and Ecosystems Cooperative Research Centre (ACE-CRC) Centre for Australian Weather and Climate Research, CSIRO Marine and Atmospheric Research, Aspendale, VIC, Australia University of East Anglia Norwich (UEA) Woods Hole Oceanographic Institution (WHOI) Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich) Meteorological Research Institute Tsukuba (MRI) Japan Meteorological Agency (JMA) Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine (AWI) Helmholtz-Gemeinschaft = Helmholtz Association University of Colorado Boulder University of New South Wales Sydney (UNSW) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) National Institute of Water and Atmospheric Research Wellington (NIWA) South Africa and ocean systems & climate group (CSIR) Max-Planck-Institut Lamont-Doherty Earth Observatory (LDEO) Columbia University New York |
format |
Article in Journal/Newspaper |
author |
Lenton, Andrew Tilbrook, Bronte Law, R. M. Bakker, Dorothee C. E. Doney, Scott C. Gruber, Nicolas Ishii, Masao Hoppema, Mario Lovenduski, N. S. Matear, Richard J. Mcneil, B. I. Metzl, Nicolas Mikaloff Fletcher, S. E. Monteiro, Pedro M. S. Rödenbeck, Christian Sweeney, Colm Takahashi, Taro |
author_facet |
Lenton, Andrew Tilbrook, Bronte Law, R. M. Bakker, Dorothee C. E. Doney, Scott C. Gruber, Nicolas Ishii, Masao Hoppema, Mario Lovenduski, N. S. Matear, Richard J. Mcneil, B. I. Metzl, Nicolas Mikaloff Fletcher, S. E. Monteiro, Pedro M. S. Rödenbeck, Christian Sweeney, Colm Takahashi, Taro |
author_sort |
Lenton, Andrew |
title |
Sea-air CO 2 fluxes in the Southern Ocean for the period 1990-2009 |
title_short |
Sea-air CO 2 fluxes in the Southern Ocean for the period 1990-2009 |
title_full |
Sea-air CO 2 fluxes in the Southern Ocean for the period 1990-2009 |
title_fullStr |
Sea-air CO 2 fluxes in the Southern Ocean for the period 1990-2009 |
title_full_unstemmed |
Sea-air CO 2 fluxes in the Southern Ocean for the period 1990-2009 |
title_sort |
sea-air co 2 fluxes in the southern ocean for the period 1990-2009 |
publisher |
HAL CCSD |
publishDate |
2013 |
url |
https://hal.science/hal-00873441 https://hal.science/hal-00873441/document https://hal.science/hal-00873441/file/bg-10-4037-2013.pdf https://doi.org/10.5194/BG-10-4037-2013 |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
ISSN: 1726-4170 EISSN: 1726-4189 Biogeosciences https://hal.science/hal-00873441 Biogeosciences, 2013, 10, pp.4037-4054. ⟨10.5194/BG-10-4037-2013⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/BG-10-4037-2013 hal-00873441 https://hal.science/hal-00873441 https://hal.science/hal-00873441/document https://hal.science/hal-00873441/file/bg-10-4037-2013.pdf BIBCODE: 2013BGeo.10.4037L doi:10.5194/BG-10-4037-2013 |
op_rights |
http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.5194/BG-10-4037-2013 |
container_title |
Biogeosciences |
container_volume |
10 |
container_issue |
6 |
container_start_page |
4037 |
op_container_end_page |
4054 |
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1799467245249757184 |
spelling |
ftepunivpsaclay:oai:HAL:hal-00873441v1 2024-05-19T07:48:52+00:00 Sea-air CO 2 fluxes in the Southern Ocean for the period 1990-2009 Lenton, Andrew Tilbrook, Bronte Law, R. M. Bakker, Dorothee C. E. Doney, Scott C. Gruber, Nicolas Ishii, Masao Hoppema, Mario Lovenduski, N. S. Matear, Richard J. Mcneil, B. I. Metzl, Nicolas Mikaloff Fletcher, S. E. Monteiro, Pedro M. S. Rödenbeck, Christian Sweeney, Colm Takahashi, Taro CSIRO Marine and Atmospheric Research Hobart, Castray Esplanade, Hobart Tasmani 7000, Australia Antarctic Climate and Ecosystems Cooperative Research Centre (ACE-CRC) Centre for Australian Weather and Climate Research, CSIRO Marine and Atmospheric Research, Aspendale, VIC, Australia University of East Anglia Norwich (UEA) Woods Hole Oceanographic Institution (WHOI) Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich) Meteorological Research Institute Tsukuba (MRI) Japan Meteorological Agency (JMA) Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine (AWI) Helmholtz-Gemeinschaft = Helmholtz Association University of Colorado Boulder University of New South Wales Sydney (UNSW) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) National Institute of Water and Atmospheric Research Wellington (NIWA) South Africa and ocean systems & climate group (CSIR) Max-Planck-Institut Lamont-Doherty Earth Observatory (LDEO) Columbia University New York 2013-06 https://hal.science/hal-00873441 https://hal.science/hal-00873441/document https://hal.science/hal-00873441/file/bg-10-4037-2013.pdf https://doi.org/10.5194/BG-10-4037-2013 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/BG-10-4037-2013 hal-00873441 https://hal.science/hal-00873441 https://hal.science/hal-00873441/document https://hal.science/hal-00873441/file/bg-10-4037-2013.pdf BIBCODE: 2013BGeo.10.4037L doi:10.5194/BG-10-4037-2013 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1726-4170 EISSN: 1726-4189 Biogeosciences https://hal.science/hal-00873441 Biogeosciences, 2013, 10, pp.4037-4054. ⟨10.5194/BG-10-4037-2013⟩ [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2013 ftepunivpsaclay https://doi.org/10.5194/BG-10-4037-2013 2024-04-25T00:57:09Z International audience The Southern Ocean (44-75° S) plays a critical role in the global carbon cycle, yet remains one of the most poorly sampled ocean regions. Different approaches have been used to estimate sea-air CO 2 fluxes in this region: synthesis of surface ocean observations, ocean biogeochemical models, and atmospheric and ocean inversions. As part of the RECCAP (REgional Carbon Cycle Assessment and Processes) project, we combine these different approaches to quantify and assess the magnitude and variability in Southern Ocean sea-air CO 2 fluxes between 1990-2009. Using all models and inversions (26), the integrated median annual sea-air CO 2 flux of -0.42 ± 0.07 Pg C yr -1 for the 44-75° S region, is consistent with the -0.27 ± 0.13 Pg C yr -1 calculated using surface observations. The circumpolar region south of 58° S has a small net annual flux (model and inversion median: -0.04 ± 0.07 Pg C yr -1 and observations: +0.04 ± 0.02 Pg C yr -1 ), with most of the net annual flux located in the 44 to 58° S circumpolar band (model and inversion median: -0.36 ± 0.09 Pg C yr -1 and observations: -0.35 ± 0.09 Pg C yr -1 ). Seasonally, in the 44-58° S region, the median of 5 ocean biogeochemical models captures the observed sea-air CO 2 flux seasonal cycle, while the median of 11 atmospheric inversions shows little seasonal change in the net flux. South of 58° S, neither atmospheric inversions nor ocean biogeochemical models reproduce the phase and amplitude of the observed seasonal sea-air CO 2 flux, particularly in the Austral Winter. Importantly, no individual atmospheric inversion or ocean biogeochemical model is capable of reproducing both the observed annual mean uptake and the observed seasonal cycle. This raises concerns about projecting future changes in Southern Ocean CO 2 fluxes. The median interannual variability from atmospheric inversions and ocean biogeochemical models is substantial in the Southern Ocean; up to 25% of the annual mean flux, with 25% of this interannual variability attributed to ... Article in Journal/Newspaper Southern Ocean École Polytechnique, Université Paris-Saclay: HAL Biogeosciences 10 6 4037 4054 |