Regional Impacts of Climate Change and Atmospheric CO2 on Future Ocean Carbon Uptake: A Multimodel Linear Feedback Analysis
International audience The increase in atmospheric CO2 over this century depends on the evolution of the oceanic air–sea CO2 uptake, which will be driven by the combined response to rising atmospheric CO2 itself and climate change. Here, the future oceanic CO2 uptake is simulated using an ensemble o...
Published in: | Journal of Climate |
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Main Authors: | , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2011
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Subjects: | |
Online Access: | https://hal.science/hal-03113010 https://hal.science/hal-03113010/document https://hal.science/hal-03113010/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Regional%20Impacts%20of%20Climate%20Change%20and%20Atmospheric%20CO2%20on%20Future%20Ocean%20Carbon%20Uptake%20A%20Multimodel%20Linear%20Feedback%20Analysis.pdf https://doi.org/10.1175/2010JCLI3787.1 |
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HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) |
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ftceafr |
language |
English |
topic |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
spellingShingle |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology Roy, Tilla Bopp, Laurent Gehlen, Marion Schneider, Birgit Cadule, Patricia Frölicher, Thomas Segschneider, Joachim Tjiputra, Jerry Heinze, Christoph Joos, Fortunat Regional Impacts of Climate Change and Atmospheric CO2 on Future Ocean Carbon Uptake: A Multimodel Linear Feedback Analysis |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
description |
International audience The increase in atmospheric CO2 over this century depends on the evolution of the oceanic air–sea CO2 uptake, which will be driven by the combined response to rising atmospheric CO2 itself and climate change. Here, the future oceanic CO2 uptake is simulated using an ensemble of coupled climate–carbon cycle models. The models are driven by CO2 emissions from historical data and the Special Report on Emissions Scenarios (SRES) A2 high-emission scenario. A linear feedback analysis successfully separates the regional future (2010–2100) oceanic CO2 uptake into a CO2-induced component, due to rising atmospheric CO2 concentrations, and a climate-induced component, due to global warming. The models capture the observation-based magnitude and distribution of anthropogenic CO2 uptake. The distributions of the climate-induced component are broadly consistent between the models, with reduced CO2 uptake in the subpolar Southern Ocean and the equatorial regions, owing to decreased CO2 solubility; and reduced CO2 uptake in the midlatitudes, owing to decreased CO2 solubility and increased vertical stratification. The magnitude of the climate-induced component is sensitive to local warming in the southern extratropics, to large freshwater fluxes in the extratropical North Atlantic Ocean, and to small changes in the CO2 solubility in the equatorial regions. In key anthropogenic CO2 uptake regions, the climate-induced component offsets the CO2-induced component at a constant proportion up until the end of this century. This amounts to approximately 50% in the northern extratropics and 25% in the southern extratropics and equatorial regions. Consequently, the detection of climate change impacts on anthropogenic CO2 uptake may be difficult without monitoring additional tracers, such as oxygen. |
author2 |
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) 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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics (MERMAID) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Institute of Geosciences Kiel Christian-Albrechts-Universität zu Kiel = Christian-Albrechts University of Kiel = Université Christian-Albrechts de Kiel (CAU) Climate and Environmental Physics Bern (CEP) Physikalisches Institut Bern Universität Bern = University of Bern = Université de Berne (UNIBE)-Universität Bern = University of Bern = Université de Berne (UNIBE) Max-Planck-Institut für Meteorologie (MPI-M) Max-Planck-Gesellschaft Geophysical Institute Bergen (GFI / BiU) University of Bergen (UiB) |
format |
Article in Journal/Newspaper |
author |
Roy, Tilla Bopp, Laurent Gehlen, Marion Schneider, Birgit Cadule, Patricia Frölicher, Thomas Segschneider, Joachim Tjiputra, Jerry Heinze, Christoph Joos, Fortunat |
author_facet |
Roy, Tilla Bopp, Laurent Gehlen, Marion Schneider, Birgit Cadule, Patricia Frölicher, Thomas Segschneider, Joachim Tjiputra, Jerry Heinze, Christoph Joos, Fortunat |
author_sort |
Roy, Tilla |
title |
Regional Impacts of Climate Change and Atmospheric CO2 on Future Ocean Carbon Uptake: A Multimodel Linear Feedback Analysis |
title_short |
Regional Impacts of Climate Change and Atmospheric CO2 on Future Ocean Carbon Uptake: A Multimodel Linear Feedback Analysis |
title_full |
Regional Impacts of Climate Change and Atmospheric CO2 on Future Ocean Carbon Uptake: A Multimodel Linear Feedback Analysis |
title_fullStr |
Regional Impacts of Climate Change and Atmospheric CO2 on Future Ocean Carbon Uptake: A Multimodel Linear Feedback Analysis |
title_full_unstemmed |
Regional Impacts of Climate Change and Atmospheric CO2 on Future Ocean Carbon Uptake: A Multimodel Linear Feedback Analysis |
title_sort |
regional impacts of climate change and atmospheric co2 on future ocean carbon uptake: a multimodel linear feedback analysis |
publisher |
HAL CCSD |
publishDate |
2011 |
url |
https://hal.science/hal-03113010 https://hal.science/hal-03113010/document https://hal.science/hal-03113010/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Regional%20Impacts%20of%20Climate%20Change%20and%20Atmospheric%20CO2%20on%20Future%20Ocean%20Carbon%20Uptake%20A%20Multimodel%20Linear%20Feedback%20Analysis.pdf https://doi.org/10.1175/2010JCLI3787.1 |
genre |
North Atlantic Southern Ocean |
genre_facet |
North Atlantic Southern Ocean |
op_source |
ISSN: 0894-8755 EISSN: 1520-0442 Journal of Climate https://hal.science/hal-03113010 Journal of Climate, 2011, 24 (9), pp.2300-2318. ⟨10.1175/2010JCLI3787.1⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1175/2010JCLI3787.1 hal-03113010 https://hal.science/hal-03113010 https://hal.science/hal-03113010/document https://hal.science/hal-03113010/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Regional%20Impacts%20of%20Climate%20Change%20and%20Atmospheric%20CO2%20on%20Future%20Ocean%20Carbon%20Uptake%20A%20Multimodel%20Linear%20Feedback%20Analysis.pdf doi:10.1175/2010JCLI3787.1 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1175/2010JCLI3787.1 |
container_title |
Journal of Climate |
container_volume |
24 |
container_issue |
9 |
container_start_page |
2300 |
op_container_end_page |
2318 |
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1810464337972690944 |
spelling |
ftceafr:oai:HAL:hal-03113010v1 2024-09-15T18:24:03+00:00 Regional Impacts of Climate Change and Atmospheric CO2 on Future Ocean Carbon Uptake: A Multimodel Linear Feedback Analysis Roy, Tilla Bopp, Laurent Gehlen, Marion Schneider, Birgit Cadule, Patricia Frölicher, Thomas Segschneider, Joachim Tjiputra, Jerry Heinze, Christoph Joos, Fortunat Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) 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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics (MERMAID) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Institute of Geosciences Kiel Christian-Albrechts-Universität zu Kiel = Christian-Albrechts University of Kiel = Université Christian-Albrechts de Kiel (CAU) Climate and Environmental Physics Bern (CEP) Physikalisches Institut Bern Universität Bern = University of Bern = Université de Berne (UNIBE)-Universität Bern = University of Bern = Université de Berne (UNIBE) Max-Planck-Institut für Meteorologie (MPI-M) Max-Planck-Gesellschaft Geophysical Institute Bergen (GFI / BiU) University of Bergen (UiB) 2011 https://hal.science/hal-03113010 https://hal.science/hal-03113010/document https://hal.science/hal-03113010/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Regional%20Impacts%20of%20Climate%20Change%20and%20Atmospheric%20CO2%20on%20Future%20Ocean%20Carbon%20Uptake%20A%20Multimodel%20Linear%20Feedback%20Analysis.pdf https://doi.org/10.1175/2010JCLI3787.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/2010JCLI3787.1 hal-03113010 https://hal.science/hal-03113010 https://hal.science/hal-03113010/document https://hal.science/hal-03113010/file/%5B15200442%20-%20Journal%20of%20Climate%5D%20Regional%20Impacts%20of%20Climate%20Change%20and%20Atmospheric%20CO2%20on%20Future%20Ocean%20Carbon%20Uptake%20A%20Multimodel%20Linear%20Feedback%20Analysis.pdf doi:10.1175/2010JCLI3787.1 info:eu-repo/semantics/OpenAccess ISSN: 0894-8755 EISSN: 1520-0442 Journal of Climate https://hal.science/hal-03113010 Journal of Climate, 2011, 24 (9), pp.2300-2318. ⟨10.1175/2010JCLI3787.1⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2011 ftceafr https://doi.org/10.1175/2010JCLI3787.1 2024-07-29T23:36:00Z International audience The increase in atmospheric CO2 over this century depends on the evolution of the oceanic air–sea CO2 uptake, which will be driven by the combined response to rising atmospheric CO2 itself and climate change. Here, the future oceanic CO2 uptake is simulated using an ensemble of coupled climate–carbon cycle models. The models are driven by CO2 emissions from historical data and the Special Report on Emissions Scenarios (SRES) A2 high-emission scenario. A linear feedback analysis successfully separates the regional future (2010–2100) oceanic CO2 uptake into a CO2-induced component, due to rising atmospheric CO2 concentrations, and a climate-induced component, due to global warming. The models capture the observation-based magnitude and distribution of anthropogenic CO2 uptake. The distributions of the climate-induced component are broadly consistent between the models, with reduced CO2 uptake in the subpolar Southern Ocean and the equatorial regions, owing to decreased CO2 solubility; and reduced CO2 uptake in the midlatitudes, owing to decreased CO2 solubility and increased vertical stratification. The magnitude of the climate-induced component is sensitive to local warming in the southern extratropics, to large freshwater fluxes in the extratropical North Atlantic Ocean, and to small changes in the CO2 solubility in the equatorial regions. In key anthropogenic CO2 uptake regions, the climate-induced component offsets the CO2-induced component at a constant proportion up until the end of this century. This amounts to approximately 50% in the northern extratropics and 25% in the southern extratropics and equatorial regions. Consequently, the detection of climate change impacts on anthropogenic CO2 uptake may be difficult without monitoring additional tracers, such as oxygen. Article in Journal/Newspaper North Atlantic Southern Ocean HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) Journal of Climate 24 9 2300 2318 |