Evaluation of Data‐Based Estimates of Anthropogenic Carbon in the Arctic Ocean

International audience The Arctic Ocean is particularly vulnerable to ocean acidification, a process that is mainly driven by the uptake of anthropogenic carbon (C ant) from the atmosphere. Although C ant concentrations cannot be measured directly in the ocean, they have been estimated using data-ba...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Terhaar, Jens, Tanhua, Toste, Stöven, T., Orr, James C., Bopp, Laurent
Other Authors: 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), Helmholtz Centre for Ocean Research Kiel (GEOMAR), 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)), Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL), ANR-16-CE01-0014,SOBUMS,Comprendre la réponse du cycle du carbone dans l'océan austral au stress climatique(2016)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2020
Subjects:
Online Access:https://hal.science/hal-02971199
https://hal.science/hal-02971199/document
https://hal.science/hal-02971199/file/2020JC016124.pdf
https://doi.org/10.1029/2020JC016124
id ftepunivpsaclay:oai:HAL:hal-02971199v1
record_format openpolar
institution Open Polar
collection École Polytechnique, Université Paris-Saclay: HAL
op_collection_id ftepunivpsaclay
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
Terhaar, Jens
Tanhua, Toste
Stöven, T.
Orr, James C.
Bopp, Laurent
Evaluation of Data‐Based Estimates of Anthropogenic Carbon in the Arctic Ocean
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
description International audience The Arctic Ocean is particularly vulnerable to ocean acidification, a process that is mainly driven by the uptake of anthropogenic carbon (C ant) from the atmosphere. Although C ant concentrations cannot be measured directly in the ocean, they have been estimated using data-based methods such as the transient time distribution (TTD) approach, which characterizes the ventilation of water masses with inert transient tracers, such as CFC-12. Here, we evaluate the TTD approach in the Arctic Ocean using an eddying ocean model as a test bed. When the TTD approach is applied to simulated CFC-12 in that model, it underestimates the same model's directly simulated C ant concentrations by up to 12%, a bias that stems from its idealized assumption of gas equilibrium between atmosphere and surface water, both for CFC-12 and anthropogenic CO 2. Unlike the idealized assumption, the simulated partial pressure of CFC-12 (pCFC-12) in Arctic surface waters is undersaturated relative to that in the atmosphere in regions and times of deep-water formation, while the simulated equivalent for C ant is supersaturated. After accounting for the TTD approach's negative bias, the total amount of C ant in the Arctic Ocean in 2005 increases by 8% to 3.3 ± 0.3 Pg C. By combining the adjusted TTD approach with scenarios of future atmospheric CO 2 , it is estimated that all Arctic waters, from surface to depth, would become corrosive to aragonite by the middle of the next century even if atmospheric CO 2 could be stabilized at 540 ppm.
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)
Helmholtz Centre for Ocean Research Kiel (GEOMAR)
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))
Laboratoire de Météorologie Dynamique (UMR 8539) (LMD)
Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris
École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)
ANR-16-CE01-0014,SOBUMS,Comprendre la réponse du cycle du carbone dans l'océan austral au stress climatique(2016)
format Article in Journal/Newspaper
author Terhaar, Jens
Tanhua, Toste
Stöven, T.
Orr, James C.
Bopp, Laurent
author_facet Terhaar, Jens
Tanhua, Toste
Stöven, T.
Orr, James C.
Bopp, Laurent
author_sort Terhaar, Jens
title Evaluation of Data‐Based Estimates of Anthropogenic Carbon in the Arctic Ocean
title_short Evaluation of Data‐Based Estimates of Anthropogenic Carbon in the Arctic Ocean
title_full Evaluation of Data‐Based Estimates of Anthropogenic Carbon in the Arctic Ocean
title_fullStr Evaluation of Data‐Based Estimates of Anthropogenic Carbon in the Arctic Ocean
title_full_unstemmed Evaluation of Data‐Based Estimates of Anthropogenic Carbon in the Arctic Ocean
title_sort evaluation of data‐based estimates of anthropogenic carbon in the arctic ocean
publisher HAL CCSD
publishDate 2020
url https://hal.science/hal-02971199
https://hal.science/hal-02971199/document
https://hal.science/hal-02971199/file/2020JC016124.pdf
https://doi.org/10.1029/2020JC016124
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Ocean acidification
genre_facet Arctic
Arctic Ocean
Ocean acidification
op_source ISSN: 2169-9275
EISSN: 2169-9291
Journal of Geophysical Research. Oceans
https://hal.science/hal-02971199
Journal of Geophysical Research. Oceans, 2020, 125 (6), pp.e2020JC016124. ⟨10.1029/2020JC016124⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2020JC016124
hal-02971199
https://hal.science/hal-02971199
https://hal.science/hal-02971199/document
https://hal.science/hal-02971199/file/2020JC016124.pdf
doi:10.1029/2020JC016124
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2020JC016124
container_title Journal of Geophysical Research: Oceans
container_volume 125
container_issue 6
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spelling ftepunivpsaclay:oai:HAL:hal-02971199v1 2024-06-09T07:43:16+00:00 Evaluation of Data‐Based Estimates of Anthropogenic Carbon in the Arctic Ocean Terhaar, Jens Tanhua, Toste Stöven, T. Orr, James C. Bopp, Laurent 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) Helmholtz Centre for Ocean Research Kiel (GEOMAR) 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)) Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) ANR-16-CE01-0014,SOBUMS,Comprendre la réponse du cycle du carbone dans l'océan austral au stress climatique(2016) 2020 https://hal.science/hal-02971199 https://hal.science/hal-02971199/document https://hal.science/hal-02971199/file/2020JC016124.pdf https://doi.org/10.1029/2020JC016124 en eng HAL CCSD Wiley-Blackwell info:eu-repo/semantics/altIdentifier/doi/10.1029/2020JC016124 hal-02971199 https://hal.science/hal-02971199 https://hal.science/hal-02971199/document https://hal.science/hal-02971199/file/2020JC016124.pdf doi:10.1029/2020JC016124 info:eu-repo/semantics/OpenAccess ISSN: 2169-9275 EISSN: 2169-9291 Journal of Geophysical Research. Oceans https://hal.science/hal-02971199 Journal of Geophysical Research. Oceans, 2020, 125 (6), pp.e2020JC016124. ⟨10.1029/2020JC016124⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography info:eu-repo/semantics/article Journal articles 2020 ftepunivpsaclay https://doi.org/10.1029/2020JC016124 2024-05-16T12:10:49Z International audience The Arctic Ocean is particularly vulnerable to ocean acidification, a process that is mainly driven by the uptake of anthropogenic carbon (C ant) from the atmosphere. Although C ant concentrations cannot be measured directly in the ocean, they have been estimated using data-based methods such as the transient time distribution (TTD) approach, which characterizes the ventilation of water masses with inert transient tracers, such as CFC-12. Here, we evaluate the TTD approach in the Arctic Ocean using an eddying ocean model as a test bed. When the TTD approach is applied to simulated CFC-12 in that model, it underestimates the same model's directly simulated C ant concentrations by up to 12%, a bias that stems from its idealized assumption of gas equilibrium between atmosphere and surface water, both for CFC-12 and anthropogenic CO 2. Unlike the idealized assumption, the simulated partial pressure of CFC-12 (pCFC-12) in Arctic surface waters is undersaturated relative to that in the atmosphere in regions and times of deep-water formation, while the simulated equivalent for C ant is supersaturated. After accounting for the TTD approach's negative bias, the total amount of C ant in the Arctic Ocean in 2005 increases by 8% to 3.3 ± 0.3 Pg C. By combining the adjusted TTD approach with scenarios of future atmospheric CO 2 , it is estimated that all Arctic waters, from surface to depth, would become corrosive to aragonite by the middle of the next century even if atmospheric CO 2 could be stabilized at 540 ppm. Article in Journal/Newspaper Arctic Arctic Ocean Ocean acidification École Polytechnique, Université Paris-Saclay: HAL Arctic Arctic Ocean Journal of Geophysical Research: Oceans 125 6